{"type": "FeatureCollection", "features": [{"id": "10.1073/pnas.1613401114", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:03Z", "type": "Journal Article", "created": "2017-01-31", "title": "Siberian Arctic black carbon sources constrained by model and observation", "description": "Significance           <p>A successful mitigation strategy for climate warming agents such as black carbon (BC) requires reliable source information from bottom-up emission inventory data, which can only be verified by observation. We measured BC in one of the fastest-warming and, at the same time, substantially understudied regions on our planet, the northeastern Siberian Arctic. Our observations, compared with an atmospheric transport model, imply that quantification and spatial allocation of emissions at high latitudes, specifically in the Russian Arctic, need improvement by reallocating emissions and significantly shifting source contributions for the transport, domestic, power plant, and gas flaring sectors. This strong shift in reported emissions has potentially considerable implications for climate modeling and BC mitigation efforts.</p", "keywords": ["105206 Meteorology", "Emission inventory", "550", "atmospheric transport modeling", "emission inventory", "105206 Meteorologie", "Carbon isotopes", "01 natural sciences", "7. Clean energy", "Zeppelinobservatoriet", "climate change", "Arctic haze", "carbon isotopes", "13. Climate action", "SDG 13 \u2013 Ma\u00dfnahmen zum Klimaschutz", "SDG 13 - Climate Action", "Climate change", "SDG 14 - Life Below Water", "Atmospheric transport modeling", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://pure.iiasa.ac.at/id/eprint/14364/1/PNAS-2017-Winiger-E1054-61.pdf"}, {"href": "http://pure.iiasa.ac.at/id/eprint/14364/1/PNAS-2017-Winiger-E1054-61.pdf"}, {"href": "https://pnas.org/doi/pdf/10.1073/pnas.1613401114"}, {"href": "https://doi.org/10.1073/pnas.1613401114"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Proceedings%20of%20the%20National%20Academy%20of%20Sciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1073/pnas.1613401114", "name": "item", "description": "10.1073/pnas.1613401114", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1073/pnas.1613401114"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-01-30T00:00:00Z"}}, {"id": "10.1073/pnas.1811797116", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:03Z", "type": "Journal Article", "created": "2019-05-14", "title": "Rivers across the Siberian Arctic unearth the patterns of carbon release from thawing permafrost", "description": "<p>             Climate warming is expected to mobilize northern permafrost and peat organic carbon (PP-C), yet magnitudes and system specifics of even current releases are poorly constrained. While part of the PP-C will degrade at point of thaw to CO             2             and CH             4             to directly amplify global warming, another part will enter the fluvial network, potentially providing a window to observe large-scale PP-C remobilization patterns. Here, we employ a decade-long, high-temporal resolution record of             14             C in dissolved and particulate organic carbon (DOC and POC, respectively) to deconvolute PP-C release in the large drainage basins of rivers across Siberia: Ob, Yenisey, Lena, and Kolyma. The             14             C-constrained estimate of export specifically from PP-C corresponds to only 17 \uffc2\uffb1 8% of total fluvial organic carbon and serves as a benchmark for monitoring changes to fluvial PP-C remobilization in a warming Arctic. Whereas DOC was dominated by recent organic carbon and poorly traced PP-C (12 \uffc2\uffb1 8%), POC carried a much stronger signature of PP-C (63 \uffc2\uffb1 10%) and represents the best window to detect spatial and temporal dynamics of PP-C release. Distinct seasonal patterns suggest that while DOC primarily stems from gradual leaching of surface soils, POC reflects abrupt collapse of deeper deposits. Higher dissolved PP-C export by Ob and Yenisey aligns with discontinuous permafrost that facilitates leaching, whereas higher particulate PP-C export by Lena and Kolyma likely echoes the thermokarst-induced collapse of Pleistocene deposits. Quantitative             14             C-based fingerprinting of fluvial organic carbon thus provides an opportunity to elucidate large-scale dynamics of PP-C remobilization in response to Arctic warming.           </p", "keywords": ["15. Life on land", "01 natural sciences", "6. Clean water", "leaching", "climate change", "13. Climate action", "carbon cycle", "Physical Sciences", "peat", "radiocarbon", "SDG 13 - Climate Action", "SDG 14 - Life Below Water", "14. Life underwater", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://pnas.org/doi/pdf/10.1073/pnas.1811797116"}, {"href": "https://doi.org/10.1073/pnas.1811797116"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Proceedings%20of%20the%20National%20Academy%20of%20Sciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1073/pnas.1811797116", "name": "item", "description": "10.1073/pnas.1811797116", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1073/pnas.1811797116"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-05-06T00:00:00Z"}}, {"id": "10.1073/pnas.2309881120", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:03Z", "type": "Journal Article", "created": "2024-01-08", "title": "Extreme drought impacts have been underestimated in grasslands and shrublands globally", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Climate change is increasing the frequency and severity of short-term (~1 y) drought events\u2014the most common duration of drought\u2014globally. Yet the impact of this intensification of drought on ecosystem functioning remains poorly resolved. This is due in part to the widely disparate approaches ecologists have employed to study drought, variation in the severity and duration of drought studied, and differences among ecosystems in vegetation, edaphic and climatic attributes that can mediate drought impacts. To overcome these problems and better identify the factors that modulate drought responses, we used a coordinated distributed experiment to quantify the impact of short-term drought on grassland and shrubland ecosystems. With a standardized approach, we imposed ~a single year of drought at 100 sites on six continents. Here we show that loss of a foundational ecosystem function\u2014aboveground net primary production (ANPP)\u2014was 60% greater at sites that experienced statistically extreme drought (1-in-100-y event) vs. those sites where drought was nominal (historically more common) in magnitude (35% vs. 21%, respectively). This reduction in a key carbon cycle process with a single year of extreme drought greatly exceeds previously reported losses for grasslands and shrublands. Our global experiment also revealed high variability in drought response but that relative reductions in ANPP were greater in drier ecosystems and those with fewer plant species. Overall, our results demonstrate with unprecedented rigor that the global impacts of projected increases in drought severity have been significantly underestimated and that drier and less diverse sites are likely to be most vulnerable to extreme drought.</p></article>", "keywords": ["[SDE] Environmental Sciences", "Medical Sciences", "Drought Severity", "550", "580 Plants (Botany)", "551", "Tierras de Matorral", "Medical Specialties", "Medicine and Health Sciences", "SDG 13 - Climate Action", "climate extreme | Drought-Net | International Drought Experiment | productivity", "Productividad Primaria Neta", "Net Primary Productivity", "Productivity", "2. Zero hunger", "Praderas", "Productividad", "Life Sciences", "Biological Sciences", "Grassland", "6. Clean water", "Droughts", "Grasslands", "[SDE]Environmental Sciences", "Drought-Net", "Public Health", "International Drought Experiment", "Ciclo del Carbono", "Severidad de la Sequ\u00eda", "Global Impacts", "productivity", "Climate Change", "climate extreme", "333", "Carbon Cycle", "Environmental Public Health", "XXXXXX - Unknown", "Impacto Global", "Scrublands", "General", "Biology", "Ecosystem", "Experimento internacional de Sequ\u00eda", "500", "Receptor Protein-Tyrosine Kinases", "15. Life on land", "Clima Extremo", "Climate Science", "13. Climate action", "Cambio Clim\u00e1tico", "Extreme Climate", "Climate extreme", "Klimatvetenskap"]}, "links": [{"href": "https://boris.unibe.ch/191349/1/smith-et-al-2024-extreme-drought-impacts-have-been-underestimated-in-grasslands-and-shrublands-globally.pdf"}, {"href": "https://escholarship.org/content/qt9b707158/qt9b707158.pdf"}, {"href": "https://doi.org/10.1073/pnas.2309881120"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Proceedings%20of%20the%20National%20Academy%20of%20Sciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1073/pnas.2309881120", "name": "item", "description": "10.1073/pnas.2309881120", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1073/pnas.2309881120"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-01-08T00:00:00Z"}}, {"id": "10.1073/pnas.2317332121", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:03Z", "type": "Journal Article", "created": "2024-04-26", "title": "Negative correlation between soil salinity and soil organic carbon variability", "description": "<p>Soil organic carbon (SOC) is vital for terrestrial ecosystems, affecting biogeochemical processes, and soil health. It is known that soil salinity impacts SOC content, yet the specific direction and magnitude of SOC variability in relation to soil salinity remain poorly understood. Analyzing 43,459 mineral soil samples (SOC &lt; 150 g kg\uffe2\uff88\uff921) collected across different land covers since 1992, we approximate a soil salinity increase from 1 to 5 dS m\uffe2\uff88\uff921in croplands would be associated with a decline in mineral soils SOC from 0.14 g kg\uffe2\uff88\uff921above the mean predicted SOC (SOC\uffc2\uffafc= 18.47 g kg\uffe2\uff88\uff921) to 0.46 g kg\uffe2\uff88\uff921belowSOC\uffc2\uffafc(~\uffe2\uff88\uff92430%), while for noncroplands, such decline is sharper, from 0.96 aboveSOC\uffc2\uffafnc= 35.96 g kg\uffe2\uff88\uff921to 4.99 belowSOC\uffc2\uffafnc(~\uffe2\uff88\uff92620%). Although salinity\uffe2\uff80\uff99s significance in explaining SOC variability is minor (&lt;6%), we estimate a one SD increase in salinity of topsoil samples (0 to 7 cm) correlates with respectiveSOC\uffc2\uffafdeclines of ~4.4% and ~9.26%, relative toSOC\uffc2\uffafcandSOC\uffc2\uffafnc. TheSOC\uffc2\uffafdecline in croplands is greatest in vegetation/cropland mosaics while lands covered with evergreen needle-leaved trees are estimated with the highestSOC\uffc2\uffafdecline in noncroplands. We identify soil nitrogen, land cover, and precipitation Seasonality Index as the most significant parameters in explaining the SOC\uffe2\uff80\uff99s variability. The findings provide insights into SOC dynamics under increased soil salinity, improving understanding of SOC stock responses to land degradation and climate warming.</p", "keywords": ["570", "soil salinity", "Supplementary Data", "QH301 Biology", "500", "04 agricultural and veterinary sciences", "environmental impact", "01 natural sciences", "soil organic carbon", "QH301", "biogeochemistry", "carbon cycle", "Physical Sciences", "SDG 13 - Climate Action", "0401 agriculture", " forestry", " and fisheries", "General", "SDG 15 - Life on Land", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1073/pnas.2317332121"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Proceedings%20of%20the%20National%20Academy%20of%20Sciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1073/pnas.2317332121", "name": "item", "description": "10.1073/pnas.2317332121", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1073/pnas.2317332121"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-04-26T00:00:00Z"}}, {"id": "10.1093/aob/mcaa181", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:18Z", "type": "Journal Article", "created": "2020-10-07", "title": "Significance of root hairs for plant performance under contrasting field conditions and water deficit", "description": "AbstractBackground and Aims<p>Previous laboratory studies have suggested selection for root hair traits in future crop breeding to improve resource use efficiency and stress tolerance. However, data on the interplay between root hairs and open-field systems, under contrasting soils and climate conditions, are limited. As such, this study aims to experimentally elucidate some of the impacts that root hairs have on plant performance on a field scale.</p>Methods<p>A field experiment was set up in Scotland for two consecutive years, under contrasting climate conditions and different soil textures (i.e. clay loam vs. sandy loam). Five barley (Hordeum vulgare) genotypes exhibiting variation in root hair length and density were used in the study. Root hair length, density and rhizosheath weight were measured at several growth stages, as well as shoot biomass, plant water status, shoot phosphorus (P) accumulation and grain yield.</p>Key Results<p>Measurements of root hair density, length and its correlation with rhizosheath weight highlighted trait robustness in the field under variable environmental conditions, although significant variations were found between soil textures as the growing season progressed. Root hairs did not confer a notable advantage to barley under optimal conditions, but under soil water deficit root hairs enhanced plant water status and stress tolerance resulting in a less negative leaf water potential and lower leaf abscisic acid concentration, while promoting shoot P accumulation. Furthermore, the presence of root hairs did not decrease yield under optimal conditions, while root hairs enhanced yield stability under drought.</p>Conclusions<p>Selecting for beneficial root hair traits can enhance yield stability without diminishing yield potential, overcoming the breeder\uffe2\uff80\uff99s dilemma of trying to simultaneously enhance both productivity and resilience. Therefore, the maintenance or enhancement of root hairs can represent a key trait for breeding the next generation of crops for improved drought tolerance in relation to climate change.</p", "keywords": ["construction", "0301 basic medicine", "EP/M020355/1", "Supplementary Data", "QH301 Biology", "drought tolerance", "/dk/atira/pure/subjectarea/asjc/1100/1110", "610", "Rural and Environmental Science and Analytical Services (RESAS)", "Plant Roots", "630", "root hairs", "QH301", "Soil", "03 medical and health sciences", "646809DIMR", "agricultural sustainability", "SDG 13 - Climate Action", "BB/L025620/1", "rhizosheath", "phosphorus", "NE/L00237/1", "Hordeum vulgare", "580", "2. Zero hunger", "Natural Environment Research Council (NERC)", "grain yield", "rhizoshealth", "barley", "Water", "soil texture", "Hordeum", "15. Life on land", "NA160430", "6. Clean water", "Droughts", "Plant Breeding", "root traits", "Engineering and Physical Sciences Research Council (EPSRC)", "Biotechnology and Biological Sciences Research Council (BBSRC)", "Other", "plant water status", "name=Plant Science", "BB/P004180/1", "BB/L025825/1"]}, "links": [{"href": "https://repository.uwl.ac.uk/id/eprint/7652/1/12050%20Naveed.pdf"}, {"href": "https://eprints.soton.ac.uk/453165/1/marinsignificance2020.pdf"}, {"href": "https://eprints.soton.ac.uk/453165/2/mcaa181.pdf"}, {"href": "https://doi.org/10.1093/aob/mcaa181"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Annals%20of%20Botany", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1093/aob/mcaa181", "name": "item", "description": "10.1093/aob/mcaa181", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1093/aob/mcaa181"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-10-10T00:00:00Z"}}, {"id": "10.1093/ismeco/ycae116", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:20Z", "type": "Journal Article", "created": "2024-10-08", "title": "Land use effects on soil microbiome composition and traits with consequences for soil carbon cycling", "description": "Abstract                <p>The soil microbiome determines the fate of plant-fixed carbon. The shifts in soil properties caused by land use change leads to modifications in microbiome function, resulting in either loss or gain of soil organic carbon (SOC). Soil pH is the primary factor regulating microbiome characteristics leading to distinct pathways of microbial carbon cycling, but the underlying mechanisms remain understudied. Here, the taxa-trait relationships behind the variable fate of SOC were investigated using metaproteomics, metabarcoding, and a 13C-labeled litter decomposition experiment across two temperate sites with differing soil pH each with a paired land use intensity contrast. 13C incorporation into microbial biomass increased with land use intensification in low-pH soil but decreased in high-pH soil, with potential impact on carbon use efficiency in opposing directions. Reduction in biosynthesis traits was due to increased abundance of proteins linked to resource acquisition and stress tolerance. These trait trade-offs were underpinned by land use intensification-induced changes in dominant taxa with distinct traits. We observed divergent pH-controlled pathways of SOC cycling. In low-pH soil, land use intensification alleviates microbial abiotic stress resulting in increased biomass production but promotes decomposition and SOC loss. In contrast, in high-pH soil, land use intensification increases microbial physiological constraints and decreases biomass production, leading to reduced necromass build-up and SOC stabilization. We demonstrate how microbial biomass production and respiration dynamics and therefore carbon use efficiency can be decoupled from SOC highlighting the need for its careful consideration in managing SOC storage for soil health and climate change mitigation.</p", "keywords": ["soil health", "Supplementary Data", "QH301 Biology", "carbon use efficiency", "carbon cycling", "https://oup.silverchair-cdn.com/oup/backfile/Content_public/Journal/ismecommun/4/1/10.1093_ismeco_ycae116/1/otu_table_16s_table_s1_ycae116.xlsx?Expires=1737538557&Signature=3IutEpMaJIknJFjSbheOQYWpAwXt2atlN4YtPR7BTaTGf3jrf1M6yHgYzlnrttKlwpbFcwz-IqYq96oubC5FxfBQQyiIC0H-az-D~Bkstxc9XHkEmERELO~nurTlszmUndzm3jLsKF05x00PNsiNFlGKUhlsMB6wRmyO3v3GNBqHQVdswXZ3UAjfXvqqinyDLK54UCxfLk8eKpcfFnvVctxQ8Hrk3gP-eMFToKDlXgPD4MXGrdegvcZblx6g8FAvJruLIG1NWIRJ6wzx6HcmAYiZDJcGosKrdjMBIznM8YIJjBrfWwhGvjh15Z7MJnsUWn8PjxLjXfww29q-YfQnw__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA", "https://oup.silverchair-cdn.com/oup/backfile/Content_public/Journal/ismecommun/4/1/10.1093_ismeco_ycae116/1/otu_table_18s_table_s2_ycae116.xlsx?Expires=1737538557&Signature=ZVWC9BaJ2MOsxOOfzrmd-9nuLAy5yHOmeqJQmKHhQ1z7mXxXITIYAvM8BpVkEkQHB7Bo-6dNEm5FlC6eAuTroyq-dvMW3PD6MNP9SN5KgwSrKUeHM6IKNhzav6Q4zd48B95IPreN5UKQTTVPrphpdOxfdVKYKxD3qOMdWqmHXt-IAD~W80PJ0BjvpHXPQ0pYCmGInVv1Fe-L3k~OKo80rD0xtncnBCFRd8DVHTIY5JLjJr4-E~M3Gainkbz2AVLZwys3S6MMEboS8vKSj~rG34Z04ByT6dBjp0XDj2H9K7WjXlEqOoPIwUWUUfcVvn4N5wZ6R6YFZr9mk4qTZKdEow__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA", "004", "soil organic carbon", "QH301", "soil pH", "13C labelling", "land use intensity", "soil microbiome", "metabarcoding", "SDG 13 - Climate Action", "metaproteomics", "Original Article", "SDG 15 - Life on Land"]}, "links": [{"href": "https://doi.org/10.1093/ismeco/ycae116"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/ISME%20Communications", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1093/ismeco/ycae116", "name": "item", "description": "10.1093/ismeco/ycae116", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1093/ismeco/ycae116"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-01-01T00:00:00Z"}}, {"id": "10.1080/10643389.2018.1471957", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:13Z", "type": "Journal Article", "created": "2018-08-24", "title": "A research challenge vision regarding management of agricultural waste in a circular bio-based economy", "description": "Agricultural waste is a huge pool of untapped biomass resources that may even represent economic and environmental burdens. They can be converted into bioenergy and bio-based products by cascading conversion processes, within circular economy, and should be considered residual resources. Major challenges are discussed from a transdisciplinary perspective, focused on Europe situation. Environmental and economic consequences of agricultural residue management chains are difficult to assess due to their complexity, seasonality and regionality. Designing multi-criteria decision support tools, applicable at an early-stage of research, is discussed. Improvement of Anaerobic Digestion (AD), one of the most mature conversion technologies, is discussed from a technological point of view and waste feedstock geographical and seasonal variations. Using agricultural residual resources for producing high-value chemicals is a considerable challenge analysed here, taking into account innovative eco-efficient and cost-effective cascading conversion processes (bio-refinery concept). Moreover, the promotion of agricultural residues-based business is discussed through industrial ecology, to promote synergy, on a local basis, between different agricultural and industrial value chains. Finally, to facilitate a holistic approach and optimise materials and knowledge flows management, the connection of stakeholders is discussed to promote cross-sectorial collaboration and resource exchange at appropriate geographic scales.", "keywords": ["bio-based materials", "circular economy", " agriculture", " biogas", " economics", "330", "Circular economy", "Ing\u00e9nierie des aliments", "Biogas", "/dk/atira/pure/sustainabledevelopmentgoals/responsible_consumption_and_production; name=SDG 12 - Responsible Consumption and Production", "01 natural sciences", "7. Clean energy", "630", "/dk/atira/pure/sustainabledevelopmentgoals/decent_work_and_economic_growth; name=SDG 8 - Decent Work and Economic Growth", "12. Responsible consumption", "[SDV.IDA]Life Sciences [q-bio]/Food engineering", "\u00e9conomie circulaire", "11. Sustainability", "biogas", "Food engineering", "waste", "/dk/atira/pure/sustainabledevelopmentgoals/climate_action; name=SDG 13 - Climate Action", "d\u00e9chet agricole", "0105 earth and related environmental sciences", "2. Zero hunger", "Eco-design", "circular economy", "Agriculture", "15. Life on land", "biogaz", "Agriculture; bio-based materials; biogas; circular economy; eco-design; waste; Environmental Engineering; Water Science and Technology; Waste Management and Disposal; Pollution", "eco-design", "Agriculture;Waste;Eco-design;Biogas;Bio-based materials;Circular economy", "Waste", "Bio-based materials", "13. Climate action", "biomat\u00e9riau", "outil d'aide \u00e0 la d\u00e9cision", "\u00e9coconception"]}, "links": [{"href": "https://cris.unibo.it/bitstream/11585/679111/4/Gontard.pdf"}, {"href": "https://www.tandfonline.com/doi/pdf/10.1080/10643389.2018.1471957"}, {"href": "https://doi.org/10.1080/10643389.2018.1471957"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Critical%20Reviews%20in%20Environmental%20Science%20and%20Technology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1080/10643389.2018.1471957", "name": "item", "description": "10.1080/10643389.2018.1471957", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1080/10643389.2018.1471957"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-03-19T00:00:00Z"}}, {"id": "10.1088/1748-9326/ac4f8d", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:17Z", "type": "Journal Article", "created": "2022-01-27", "title": "Seasonal variability in particulate organic carbon degradation in the Kolyma River, Siberia", "description": "Abstract                <p>Major Arctic rivers are undergoing changes due to climate warming with higher discharge and increased amounts of solutes and organic carbon (OC) draining into rivers and coastal seas. Permafrost thaw mobilizes previously frozen OC to the fluvial network where it can be degraded into greenhouse gases and emitted to the atmosphere. Degradation of OC during downstream transport, especially of the particulate OC (POC), is however poorly characterized. Here, we quantified POC degradation in the Kolyma River, the largest river system underlain with continuous permafrost, during 9\uffe2\uff80\uff9315 d whole-water incubations (containing POC and dissolved OC\uffe2\uff80\uff94DOC) during two seasons: spring freshet (early June) and late summer (end of July). Furthermore, we examined interactions between dissolved and particulate phases using parallel incubations of filtered water (only DOC). We measured OC concentrations and carbon isotopes (\uffce\uffb413C, \uffce\uff9414C) to define carbon losses and to characterize OC composition, respectively. We found that both POC composition and biodegradability differs greatly between seasons. During summer, POC was predominantly autochthonous (47%\uffe2\uff80\uff9395%) and degraded rapidly (\uffe2\uff88\uffbc33% loss) whereas freshet POC was largely of allochthonous origin (77%\uffe2\uff80\uff9396%) and less degradable. Gains in POC concentrations (up to 31%) were observed in freshet waters that could be attributed to flocculation and adsorption of DOC to particles. The demonstrated DOC flocculation and adsorption to POC indicates that the fate and dynamics of the substantially-sized DOC pool may shift from degradation to settling, depending on season and POC concentrations\uffe2\uff80\uff94the latter potentially acting to attenuate greenhouse gas emissions from fluvial systems. We finally note that DOC incubations without POC present may yield degradation estimates that do not reflect degradation in the in situ river conditions, and that interaction between dissolved and particulate phases may be important to consider when determining fluvial carbon dynamics and feedbacks under a changing climate.</p", "keywords": ["Science", "Physics", "QC1-999", "Q", "F800", "15. Life on land", "Environmental technology. Sanitary engineering", "degradation rate", "01 natural sciences", "permafrost; Arctic; degradation rate; carbon isotopes; adsorption; flocculation", "F900", "Environmental sciences", "Arctic", "carbon isotopes", "adsorption", "flocculation", "13. Climate action", "SDG 13 - Climate Action", "GE1-350", "14. Life underwater", "TD1-1066", "permafrost", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://nrl.northumbria.ac.uk/id/eprint/48293/8/Keskitalo_2022_Environ._Res._Lett._17_034007.pdf"}, {"href": "https://doi.org/10.1088/1748-9326/ac4f8d"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Environmental%20Research%20Letters", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1088/1748-9326/ac4f8d", "name": "item", "description": "10.1088/1748-9326/ac4f8d", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1088/1748-9326/ac4f8d"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-02-21T00:00:00Z"}}, {"id": "10.1088/1748-9326/aaeae7", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:17Z", "type": "Journal Article", "created": "2018-10-24", "title": "Using research networks to create the comprehensive datasets needed to assess nutrient availability as a key determinant of terrestrial carbon cycling", "description": "Open AccessA wide range of research shows that nutrient availability strongly influences terrestrial carbon (C) cycling and shapes ecosystem responses to environmental changes and hence terrestrial feedbacks to climate. Nonetheless, our understanding of nutrient controls remains far from complete and poorly quantified, at least partly due to a lack of informative, comparable, and accessible datasets at regional-to-global scales. A growing research infrastructure of multi-site networks are providing valuable data on C fluxes and stocks and are monitoring their responses to global environmental change and measuring responses to experimental treatments. These networks thus provide an opportunity for improving our understanding of C-nutrient cycle interactions and our ability to model them. However, coherent information on how nutrient cycling interacts with observed C cycle patterns is still generally lacking. Here, we argue that complementing available C-cycle measurements from monitoring and experimental sites with data characterizing nutrient availability will greatly enhance their power and will improve our capacity to forecast future trajectories of terrestrial C cycling and climate. Therefore, we propose a set of complementary measurements that are relatively easy to conduct routinely at any site or experiment and that, in combination with C cycle observations, can provide a robust characterization of the effects of nutrient availability across sites. In addition, we discuss the power of different observable variables for informing the formulation of models and constraining their predictions. Most widely available measurements of nutrient availability often do not align well with current modelling needs. This highlights the importance to foster the interaction between the empirical and modelling communities for setting future research priorities.", "keywords": ["Global vegetation models", "550", "manipulation experiments", "Terrestrial-Aquatic Linkages", "Kolefni", "01 natural sciences", "Nutrient cycle", "Agricultural and Biological Sciences", "Terrestrial ecosystem", "SDG 13 - Climate Action", "Climate change", "Jar\u00f0vegur", "Environmental resource management", "Global change", "General Environmental Science", "SDG 15 - Life on Land", "Carbon-nutrient cycle interactions", "2. Zero hunger", "Data syntheses", "Global and Planetary Change", "Ecology", "Geography", "Physics", "Life Sciences", "Application of Stable Isotopes in Trophic Ecology", "Cycling", "Carbon cycle", "04 agricultural and veterinary sciences", "Chemistry", "ORGANIC-MATTER", "Archaeology", "Physical Sciences", "Nutrient availability", "NET PRIMARY PRODUCTIVITY", "Ecosystem Functioning", "570", "LAND", "TROPICAL RAIN-FOREST", "carbon-nutrient cycle interactions", "data syntheses", "Soil Science", "Environmental science", "[SDU] Sciences of the Universe [physics]", "SOIL-PHOSPHORUS AVAILABILITY", "global vegetation models", "SDG 3 - Good Health and Well-being", "nutrients", "USE EFFICIENCY", "SDG 7 - Affordable and Clean Energy", "GLOBAL CHANGE", "Key (lock)", "Biology", "Ecosystem", "Manipulation experiments", "0105 earth and related environmental sciences", "Renewable Energy", " Sustainability and the Environment", "Ecosystem Structure", "Public Health", " Environmental and Occupational Health", "Nutrients", "15. Life on land", "Computer science", "[SDU]Sciences of the Universe [physics]", "13. Climate action", "ECOSYSTEM RESPONSES", "FOS: Biological sciences", "Global Methane Emissions and Impacts", "Environmental Science", "0401 agriculture", " forestry", " and fisheries", "NITROGEN-FIXATION", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems", "Nutrient Limitation", "ELEVATED CO2", "Nutrient"]}, "links": [{"href": "https://doi.org/10.1088/1748-9326/aaeae7"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Environmental%20Research%20Letters", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1088/1748-9326/aaeae7", "name": "item", "description": "10.1088/1748-9326/aaeae7", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1088/1748-9326/aaeae7"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-12-07T00:00:00Z"}}, {"id": "10.1111/ejss.13145", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:37Z", "type": "Journal Article", "created": "2021-07-13", "title": "Sustainable futures over the next decade are rooted in soil science", "description": "Abstract<p>The importance of soils to society has gained increasing recognition over the past decade, with the potential to contribute to most of the United Nations\uffe2\uff80\uff99 Sustainable Development Goals (SDGs). With unprecedented and growing demands for food, water and energy, there is an urgent need for a global effort to address the challenges of climate change and land degradation, whilst protecting soil as a natural resource. In this paper, we identify the contribution of soil science over the past decade to addressing gaps in our knowledge regarding major environmental challenges: climate change, food security, water security, urban development, and ecosystem functioning and biodiversity. Continuing to address knowledge gaps in soil science is essential for the achievement of the SDGs. However, with limited time and budget, it is also pertinent to identify effective methods of working that ensure the research carried out leads to real\uffe2\uff80\uff90world impact. Here, we suggest three strategies for the next decade of soil science, comprising a greater implementation of research into policy, interdisciplinary partnerships to evaluate function trade\uffe2\uff80\uff90offs and synergies between soils and other environmental domains, and integrating monitoring and modelling methods to ensure soil\uffe2\uff80\uff90based policies can withstand the uncertainties of the future.</p>Highlights<p> <p>We highlight the contributions of soil science to five major environmental challenges since 2010.</p> <p>Researchers have contributed to recommendation reports, but work is rarely translated into policy.</p> <p>Interdisciplinary work should assess trade\uffe2\uff80\uff90offs and synergies between soils and other domains.</p> <p>Integrating monitoring and modelling is key for robust and sustainable soils\uffe2\uff80\uff90based policymaking.</p> </p", "keywords": ["330", "550", "QH301 Biology", "Sustainable Development Goals", "NE/R016429/1", "Urban development", "[SDV.SA.SDS]Life Sciences [q-bio]/Agricultural sciences/Soil study", "01 natural sciences", "333", "Ecosystems", "12. Responsible consumption", "QH301", "11. Sustainability", "SDG 13 - Climate Action", "774378", "Climate change", "SDG 2 - Zero Hunger", "European Commission", "[SDV.SA.SDS] Life Sciences [q-bio]/Agricultural sciences/Soil study", "869625", "SDG 15 - Life on Land", "biodiversity", "0105 earth and related environmental sciences", "2. Zero hunger", "Natural Environment Research Council (NERC)", "NE/P019455/1", "biodiversity; climate change; ecosystems; food security; sustainable development goals; urban development; water security", "Food security", "Biodiversity", "food security", "15. Life on land", "sustainable development goals", "water security", "urban development", "[SHS.SCIPO]Humanities and Social Sciences/Political science", "6. Clean water", "climate change", "13. Climate action", "Water security", "ecosystems", "[SHS.SCIPO] Humanities and Social Sciences/Political science"]}, "links": [{"href": "http://livrepository.liverpool.ac.uk/3157809/1/2021%20Evans%20et%20al%20-%20European%20Journal%20of%20Soil%20Science.pdf"}, {"href": "https://eprints.lancs.ac.uk/id/eprint/157184/1/Evans_etal_2021_Decade.pdf"}, {"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1111/ejss.13145"}, {"href": "https://doi.org/10.1111/ejss.13145"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/European%20Journal%20of%20Soil%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/ejss.13145", "name": "item", "description": "10.1111/ejss.13145", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/ejss.13145"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-07-26T00:00:00Z"}}, {"id": "10.1111/brv.12949", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:35Z", "type": "Journal Article", "created": "2023-03-14", "title": "Trade\u2010offs in carbon\u2010degrading enzyme activities limit long\u2010term soil carbon sequestration with biochar addition", "description": "ABSTRACT<p>Biochar amendment is one of the most promising agricultural approaches to tackle climate change by enhancing soil carbon (C) sequestration. Microbial\uffe2\uff80\uff90mediated decomposition processes are fundamental for the fate and persistence of sequestered C in soil, but the underlying mechanisms are uncertain. Here, we synthesise 923 observations regarding the effects of biochar addition (over periods ranging from several weeks to several years) on soil C\uffe2\uff80\uff90degrading enzyme activities from 130 articles across five continents worldwide. Our results showed that biochar addition increased soil ligninase activity targeting complex phenolic macromolecules by 7.1%, but suppressed cellulase activity degrading simpler polysaccharides by 8.3%. These shifts in enzyme activities explained the most variation of changes in soil C sequestration across a wide range of climatic, edaphic and experimental conditions, with biochar\uffe2\uff80\uff90induced shift in ligninase:cellulase ratio correlating negatively with soil C sequestration. Specifically, short\uffe2\uff80\uff90term (&lt;1\uffc2\uffa0year) biochar addition significantly reduced cellulase activity by 4.6% and enhanced soil organic C sequestration by 87.5%, whereas no significant responses were observed for ligninase activity and ligninase:cellulase ratio. However, long\uffe2\uff80\uff90term (\uffe2\uff89\uffa51\uffc2\uffa0year) biochar addition significantly enhanced ligninase activity by 5.2% and ligninase:cellulase ratio by 36.1%, leading to a smaller increase in soil organic C sequestration (25.1%). These results suggest that shifts in enzyme activities increased ligninase:cellulase ratio with time after biochar addition, limiting long\uffe2\uff80\uff90term soil C sequestration with biochar addition. Our work provides novel evidence to explain the diminished soil C sequestration with long\uffe2\uff80\uff90term biochar addition and suggests that earlier studies may have overestimated soil C sequestration with biochar addition by failing to consider the physiological acclimation of soil microorganisms over time.</p", "keywords": ["Carbon Sequestration", "Supplementary Data", "QH301 Biology", "General Biochemistry", "Genetics and Molecular Biology", "soil microorganism", "551", "QH301", "Soil", "soil carbon sequestration", "SDG 13 - Climate Action", "Cellulases", "Biochar addition", "European Commission", "2. Zero hunger", "GE", "15. Life on land", "Carbon", "enzyme activity", "meta-analysis", "enzyme activities", "13. Climate action", "experimental duration", "839806", "Other", "figshare", "General Agricultural and Biological Sciences", "biochar addition", "GE Environmental Sciences", "European Research Council"]}, "links": [{"href": "https://doi.org/10.1111/brv.12949"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biological%20Reviews", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/brv.12949", "name": "item", "description": "10.1111/brv.12949", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/brv.12949"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-03-13T00:00:00Z"}}, {"id": "10.1111/j.1365-2486.2007.01468.x", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:50Z", "type": "Journal Article", "created": "2007-10-04", "title": "Climate Change Effects On Organic Matter Decomposition Rates In Ecosystems From The Maritime Antarctic And Falkland Islands", "description": "Abstract<p>Antarctic terrestrial ecosystems have poorly developed soils and currently experience one of the greatest rates of climate warming on the globe. We investigated the responsiveness of organic matter decomposition in Maritime Antarctic terrestrial ecosystems to climate change, using two study sites in the Antarctic Peninsula region (Anchorage Island, 67\uffc2\uffb0S; Signy Island, 61\uffc2\uffb0S), and contrasted the responses found with those at the cool temperate Falkland Islands (52\uffc2\uffb0S). Our approach consisted of two complementary methods: (1) Laboratory measurements of decomposition at different temperatures (2, 6 and 10\uffe2\uff80\uff83\uffc2\uffb0C) of plant material and soil organic matter from all three locations. (2) Field measurements at all three locations on the decomposition of soil organic matter, plant material and cellulose, both under natural conditions and under experimental warming (about 0.8\uffe2\uff80\uff83\uffc2\uffb0C) achieved using open top chambers. Higher temperatures led to higher organic matter breakdown in the laboratory studies, indicating that decomposition in Maritime Antarctic terrestrial ecosystems is likely to increase with increasing soil temperatures. However, both laboratory and field studies showed that decomposition was more strongly influenced by local substratum characteristics (especially soil N availability) and plant functional type composition than by large\uffe2\uff80\uff90scale temperature differences. The very small responsiveness of organic matter decomposition in the field (experimental temperature increase &lt; 1\uffe2\uff80\uff83\uffc2\uffb0C) compared with the laboratory (experimental increases of 4 or 8\uffe2\uff80\uff83\uffc2\uffb0C) shows that substantial warming is required before significant effects can be detected.</p>", "keywords": ["microbial breakdown", "0106 biological sciences", "13. Climate action", "SDG 13 - Climate Action", "environmental change", "SDG 14 - Life Below Water", "15. Life on land", "soil respiration", "01 natural sciences", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1111/j.1365-2486.2007.01468.x"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Change%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/j.1365-2486.2007.01468.x", "name": "item", "description": "10.1111/j.1365-2486.2007.01468.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/j.1365-2486.2007.01468.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2007-10-04T00:00:00Z"}}, {"id": "10.1111/gcb.15441", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:41Z", "type": "Journal Article", "created": "2020-11-07", "title": "Ensemble modelling, uncertainty and robust predictions of organic carbon in long\u2010term bare\u2010fallow soils", "description": "Abstract<p>Simulation models represent soil organic carbon (SOC) dynamics in global carbon (C) cycle scenarios to support climate\uffe2\uff80\uff90change studies. It is imperative to increase confidence in long\uffe2\uff80\uff90term predictions of SOC dynamics by reducing the uncertainty in model estimates. We evaluated SOC simulated from an ensemble of 26 process\uffe2\uff80\uff90based C models by comparing simulations to experimental data from seven long\uffe2\uff80\uff90term bare\uffe2\uff80\uff90fallow (vegetation\uffe2\uff80\uff90free) plots at six sites: Denmark (two sites), France, Russia, Sweden and the United Kingdom. The decay of SOC in these plots has been monitored for decades since the last inputs of plant material, providing the opportunity to test decomposition without the continuous input of new organic material. The models were run independently over multi\uffe2\uff80\uff90year simulation periods (from 28 to 80\uffc2\uffa0years) in a blind test with no calibration (Bln) and with the following three calibration scenarios, each providing different levels of information and/or allowing different levels of model fitting: (a) calibrating decomposition parameters separately at each experimental site (Spe); (b) using a generic, knowledge\uffe2\uff80\uff90based, parameterization applicable in the Central European region (Gen); and (c) using a combination of both (a) and (b) strategies (Mix). We addressed uncertainties from different modelling approaches with or without spin\uffe2\uff80\uff90up initialization of SOC. Changes in the multi\uffe2\uff80\uff90model median (MMM) of SOC were used as descriptors of the ensemble performance. On average across sites, Gen proved adequate in describing changes in SOC, with MMM equal to average SOC (and standard deviation) of 39.2 (\uffc2\uffb115.5)\uffc2\uffa0Mg\uffc2\uffa0C/ha compared to the observed mean of 36.0 (\uffc2\uffb119.7)\uffc2\uffa0Mg\uffc2\uffa0C/ha (last observed year), indicating sufficiently reliable SOC estimates. Moving to Mix (37.5\uffc2\uffa0\uffc2\uffb1\uffc2\uffa016.7\uffc2\uffa0Mg\uffc2\uffa0C/ha) and Spe (36.8\uffc2\uffa0\uffc2\uffb1\uffc2\uffa019.8\uffc2\uffa0Mg\uffc2\uffa0C/ha) provided only marginal gains in accuracy, but modellers would need to apply more knowledge and a greater calibration effort than in Gen, thereby limiting the wider applicability of models.</p", "keywords": ["[SDE] Environmental Sciences", "330", "550", "Supplementary Data", "soil organic carbon dynamics", "QH301 Biology", "[SDE.MCG]Environmental Sciences/Global Changes", "Soil organic carbon dynamics", "bare\u2010fallow soils", "[SDV.SA.SDS]Life Sciences [q-bio]/Agricultural sciences/Soil study", "630", "protocol for model comparison", "Russia", "QH301", "Soil", "NE/M021327/1", "SDG 13 - Climate Action", "Environmental Chemistry", "774378", "process based models", "European Commission", "[SDV.SA.SDS] Life Sciences [q-bio]/Agricultural sciences/Soil study", "General Environmental Science", "Sweden", "Global and Planetary Change", "Ecology", "Natural Environment Research Council (NERC)", "NE/P019455/1", "bare-fallow soils", "Uncertainty", "Agriculture", "04 agricultural and veterinary sciences", "15. Life on land", "Carbon", "United Kingdom", "process-based models", "[SDE.MCG] Environmental Sciences/Global Changes", "13. Climate action", "[SDE]Environmental Sciences", "bare-fallow soils; model parametrization; process-based models; protocol for model comparison; soil organic carbon dynamics", "0401 agriculture", " forestry", " and fisheries", "774124", "France", "bare fallow soils", "model parametrization"]}, "links": [{"href": "https://air.unimi.it/bitstream/2434/809186/2/GCB-20-1834_Proof_fl.pdf"}, {"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.15441"}, {"href": "https://doi.org/10.1111/gcb.15441"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Change%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/gcb.15441", "name": "item", "description": "10.1111/gcb.15441", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcb.15441"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-11-24T00:00:00Z"}}, {"id": "10.1111/gcb.14815", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:41Z", "type": "Journal Article", "created": "2019-08-30", "title": "How to measure, report and verify soil carbon change to realize the potential of soil carbon sequestration for atmospheric greenhouse gas removal", "description": "Abstract<p>There is growing international interest in better managing soils to increase soil organic carbon (SOC) content to contribute to climate change mitigation, to enhance resilience to climate change and to underpin food security, through initiatives such as international \uffe2\uff80\uff984p1000\uffe2\uff80\uff99 initiative and the FAO's Global assessment of SOC sequestration potential (GSOCseq) programme. Since SOC content of soils cannot be easily measured, a key barrier to implementing programmes to increase SOC at large scale, is the need for credible and reliable measurement/monitoring, reporting and verification (MRV) platforms, both for national reporting and for emissions trading. Without such platforms, investments could be considered risky. In this paper, we review methods and challenges of measuring SOC change directly in soils, before examining some recent novel developments that show promise for quantifying SOC. We describe how repeat soil surveys are used to estimate changes in SOC over time, and how long\uffe2\uff80\uff90term experiments and space\uffe2\uff80\uff90for\uffe2\uff80\uff90time substitution sites can serve as sources of knowledge and can be used to test models, and as potential benchmark sites in global frameworks to estimate SOC change. We briefly consider models that can be used to simulate and project change in SOC and examine the MRV platforms for SOC change already in use in various countries/regions. In the final section, we bring together the various components described in this review, to describe a new vision for a global framework for MRV of SOC change, to support national and international initiatives seeking to effect change in the way we manage our soils.</p>", "keywords": ["[SDE] Environmental Sciences", "550", "BULK-DENSITY", "QH301 Biology", "Climate", "[SDV]Life Sciences [q-bio]", "NEW-ZEALAND", "630", "Soil", "NE/M021327/1", "11. Sustainability", "SDG 13 - Climate Action", "AGRICULTURAL SOILS", "SDG 15 - Life on Land", "General Environmental Science", "agriculture", "2. Zero hunger", "Global and Planetary Change", "reporting", "Measurement", "Ecology", "IN-SITU", "Agricultura", "NE/P019455/1", "carbono org\u00e1nico del suelo", "Agriculture", "LAND-USE CHANGE", "04 agricultural and veterinary sciences", "[SDV] Life Sciences [q-bio]", "climate change", "Sustainability", "[SDE]Environmental Sciences", "Carbon Sequestration", "DIFFUSE-REFLECTANCE SPECTROSCOPY", "LONG-TERM EXPERIMENTS", "330", "Monitoring", "STOCK CHANGES", "MRV", "secuestro de carbon", "12. Responsible consumption", "QH301", "Greenhouse Gases", "ORGANIC-CARBON", "soil organic matter", "greenhouse gases", "Invited Research Reviews", "Environmental Chemistry", "774378", "SDG 2 - Zero Hunger", "European Commission", "resilience", "Climate Solutions", "Soil organic matter", "Soil organic carbon", "Natural Environment Research Council (NERC)", "Verification", "food security", "15. Life on land", "carbon sequestration", "Sustainable Agriculture", "Carbon", "EDDY-COVARIANCE", "soil organic carbon", "monitoring", "Reporting", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "measurement", "verification"]}, "links": [{"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.14815"}, {"href": "https://scholarworks.uvm.edu/context/rsfac/article/1079/viewcontent/Lini2019b.pdf"}, {"href": "https://doi.org/10.1111/gcb.14815"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Change%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/gcb.14815", "name": "item", "description": "10.1111/gcb.14815", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcb.14815"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-10-06T00:00:00Z"}}, {"id": "10.1111/gcb.14878", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:41Z", "type": "Journal Article", "created": "2019-10-22", "title": "Which practices co\u2010deliver food security, climate change mitigation and adaptation, and combat land degradation and desertification?", "description": "Abstract<p>There is a clear need for transformative change in the land management and food production sectors to address the global land challenges of climate change mitigation, climate change adaptation, combatting land degradation and desertification, and delivering food security (referred to hereafter as \uffe2\uff80\uff9cland challenges\uffe2\uff80\uff9d). We assess the potential for 40 practices to address these land challenges and find that: Nine options deliver medium to large benefits for all four land challenges. A further two options have no global estimates for adaptation, but have medium to large benefits for all other land challenges. Five options have large mitigation potential (&gt;3\uffc2\uffa0Gt CO2eq/year) without adverse impacts on the other land challenges. Five options have moderate mitigation potential, with no adverse impacts on the other land challenges. Sixteen practices have large adaptation potential (&gt;25 million people benefit), without adverse side effects on other land challenges. Most practices can be applied without competing for available land. However, seven options could result in competition for land. A large number of practices do not require dedicated land, including several land management options, all value chain options, and all risk management options. Four options could greatly increase competition for land if applied at a large scale, though the impact is scale and context specific, highlighting the need for safeguards to ensure that expansion of land for mitigation does not impact natural systems and food security. A number of practices, such as increased food productivity, dietary change and reduced food loss and waste, can reduce demand for land conversion, thereby potentially freeing\uffe2\uff80\uff90up land and creating opportunities for enhanced implementation of other practices, making them important components of portfolios of practices to address the combined land challenges.</p", "keywords": ["773901", "Invited Primary Research Article", "550", "QH301 Biology", "Acclimatization", "demand management", "TROPICAL FORESTS", "adaptation; adverse side effects; co-benefits; demand management; desertification; food security; land degradation; land management; mitigation; practice; risk management", "ECOSYSTEM SERVICES", "adaptation", "01 natural sciences", "Food Supply", "NE/M021327/1", "PRACTICE", "https://purl.org/becyt/ford/1.5", "11. Sustainability", "SDG 13 - Climate Action", "776810", "LAND MANAGEMENT", "ADVERSE SIDE EFFECTS", "ADAPTATION", "SDG 15 - Life on Land", "General Environmental Science", "2. Zero hunger", "Global and Planetary Change", "Ecology", "DESERTIFICATION", "land degradation", "FOOD SECURITY", "NEGATIVE EMISSIONS", "1. No poverty", "URBAN SPRAWL", "Agriculture", "desertification", "practice", "LIFE-CYCLE ASSESSMENT", "[SDV.EE] Life Sciences [q-bio]/Ecology", " environment", "LAND DEGRADATION", "LIVESTOCK SYSTEMS", "adverse side effects", "FEDERAL CROP INSURANCE", "environment", "GE Environmental Sciences", "European Research Council", "RISK MANAGEMENT", "Conservation of Natural Resources", "SOIL CARBON SEQUESTRATION", "330", "Climate Change", "GREENHOUSE-GAS MITIGATION", "MITIGATION", "risk management", "DEMAND MANAGEMENT", "12. Responsible consumption", "EP/M013200/1", "mitigation", "ORGANIC-CARBON", "[SDV.EE]Life Sciences [q-bio]/Ecology", "co-benefits", "Environmental Chemistry", "774378", "SDG 7 - Affordable and Clean Energy", "SDG 2 - Zero Hunger", "European Commission", "https://purl.org/becyt/ford/1", "0105 earth and related environmental sciences", "info:eu-repo/classification/ddc/550", "ddc:550", "Natural Environment Research Council (NERC)", "land management", "food security", "15. Life on land", "Earth sciences", "CO-BENEFITS", "Engineering and Physical Sciences Research Council (EPSRC)", "13. Climate action", "adverse side-effects", "Biotechnology and Biological Sciences Research Council (BBSRC)", "774124", "BB/N013484/1", "SDG 12 - Responsible Consumption and Production"]}, "links": [{"href": "https://air.unimi.it/bitstream/2434/962658/2/Global%20Change%20Biology%20-%202019%20-%20Smith%20-%20Which%20practices%20co%e2%80%90deliver%20food%20security%20%20climate%20change%20mitigation%20and%20adaptation%20.pdf"}, {"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.14878"}, {"href": "https://doi.org/10.1111/gcb.14878"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Change%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/gcb.14878", "name": "item", "description": "10.1111/gcb.14878", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcb.14878"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-12-14T00:00:00Z"}}, {"id": "10.1111/gcb.15120", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:41Z", "type": "Journal Article", "created": "2020-05-15", "title": "Changes in soil organic carbon under perennial crops", "description": "Abstract<p>This study evaluates the dynamics of soil organic carbon (SOC) under perennial crops across the globe. It quantifies the effect of change from annual to perennial crops and the subsequent temporal changes in SOC stocks during the perennial crop cycle. It also presents an empirical model to estimate changes in the SOC content under crops as a function of time, land use, and site characteristics. We used a harmonized global dataset containing paired\uffe2\uff80\uff90comparison empirical values of SOC and different types of perennial crops (perennial grasses, palms, and woody plants) with different end uses: bioenergy, food, other bio\uffe2\uff80\uff90products, and short rotation coppice. Salient outcomes include: a 20\uffe2\uff80\uff90year period encompassing a change from annual to perennial crops led to an average 20% increase in SOC at 0\uffe2\uff80\uff9330\uffc2\uffa0cm (6.0\uffc2\uffa0\uffc2\uffb1\uffc2\uffa04.6\uffc2\uffa0Mg/ha gain) and a total 10% increase over the 0\uffe2\uff80\uff93100\uffc2\uffa0cm soil profile (5.7\uffc2\uffa0\uffc2\uffb1\uffc2\uffa010.9\uffc2\uffa0Mg/ha). A change from natural pasture to perennial crop decreased SOC stocks by 1% over 0\uffe2\uff80\uff9330\uffc2\uffa0cm (\uffe2\uff88\uff922.5\uffc2\uffa0\uffc2\uffb1\uffc2\uffa04.2\uffc2\uffa0Mg/ha) and 10% over 0\uffe2\uff80\uff93100\uffc2\uffa0cm (\uffe2\uff88\uff9213.6\uffc2\uffa0\uffc2\uffb1\uffc2\uffa08.9\uffc2\uffa0Mg/ha). The effect of a land use change from forest to perennial crops did not show significant impacts, probably due to the limited number of plots; but the data indicated that while a 2% increase in SOC was observed at 0\uffe2\uff80\uff9330\uffc2\uffa0cm (16.81\uffc2\uffa0\uffc2\uffb1\uffc2\uffa055.1\uffc2\uffa0Mg/ha), a decrease in 24% was observed at 30\uffe2\uff80\uff93100\uffc2\uffa0cm (\uffe2\uff88\uff9240.1\uffc2\uffa0\uffc2\uffb1\uffc2\uffa016.8\uffc2\uffa0Mg/ha). Perennial crops generally accumulate SOC through time, especially woody crops; and temperature was the main driver explaining differences in SOC dynamics, followed by crop age, soil bulk density, clay content, and depth. We present empirical evidence showing that the FAO perennialization strategy is reasonable, underscoring the role of perennial crops as a useful component of climate change mitigation strategies.</p", "keywords": ["MISCANTHUS", "QH301 Biology", "Carbon Dynamics in Peatland Ecosystems", "SEQUESTRATION", "01 natural sciences", "630", "BIOMASS", "862695", "Agricultural and Biological Sciences", "Soil", "NE/M021327/1", "woody crops", "Soil water", "SDG 13 - Climate Action", "Development and Impacts of Bioenergy Crops", "STOCKS", "NE/N017854/1", "SDG 15 - Life on Land", "General Environmental Science", "agriculture", "2. Zero hunger", "Global and Planetary Change", "CLIMATE-CHANGE", "Ecology", "NE/P019455/1", "Life Sciences", "Agriculture", "LAND-USE CHANGE", "04 agricultural and veterinary sciences", "fruit crops", "Soil carbon", "NE/M016900/1", "Physical Sciences", "emission factors", "DECOMPOSITION", "land use change", "Crops", " Agricultural", "Carbon Sequestration", "610", "Soil Science", "Environmental science", "arable crops", "QH301", "FOOD", "TEMPERATURE SENSITIVITY", "Environmental Chemistry", "774378", "Agroforestry", "European Commission", "Biology", "carbon crops", "Land use", " land-use change and forestry", "0105 earth and related environmental sciences", "carbon balance", "Soil science", "Soil Fertility", "Natural Environment Research Council (NERC)", "15. Life on land", "Carbon", "Perennial plant", "Agronomy", "meta-analysis", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "Land use", "0401 agriculture", " forestry", " and fisheries", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems", "MATTER", "Agronomy and Crop Science"]}, "links": [{"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.15120"}, {"href": "https://doi.org/10.1111/gcb.15120"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Change%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/gcb.15120", "name": "item", "description": "10.1111/gcb.15120", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcb.15120"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-05-15T00:00:00Z"}}, {"id": "10.1111/j.1365-2486.2003.00718.x", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:47Z", "type": "Journal Article", "created": "2004-12-24", "title": "Summer Warming And Increased Winter Snow Cover Affect Sphagnum Fuscum Growth, Structure And Production In A Sub-Arctic Bog", "description": "Abstract<p> Sphagnum mosses form a major component of northern peatlands, which are expected to experience substantially higher increases in temperature and winter precipitation than the global average. Sphagnum may play an important role in the responses of the global carbon cycle to climate change. We investigated the responses of summer length growth, carpet structure and production in Sphagnum fuscum to experimentally induced changes in climate in a sub\uffe2\uff80\uff90arctic bog. Thereto, we used open\uffe2\uff80\uff90top chambers (OTCs) to create six climate scenarios including changes in summer temperatures, and changes in winter snow cover and spring temperatures. In winter, the OTCs doubled the snow thickness, resulting in 0.5\uffe2\uff80\uff932.8\uffc2\uffb0C higher average air temperatures. Spring air temperatures in OTCs increased by 1.0\uffc2\uffb0C. Summer warming had a maximum effect of 0.9\uffc2\uffb0C, while vapor pressure deficit was not affected. The climate manipulations had strong effects on S. fuscum. Summer warming enhanced the length increment by 42\uffe2\uff80\uff9362%, whereas bulk density decreased. This resulted in a trend (P&lt;0.10) of enhanced biomass production. Winter snow addition enhanced dry matter production by 33%, despite the fact that the length growth and bulk density did not change significantly. The addition of spring warming to snow addition alone did not significantly enhance this effect, but we may have missed part of the early spring growth. There were no interactions between the manipulations in summer and those in winter/spring, indicating that the effects were additive. Summer warming may in the long term negatively affect productivity through the adverse effects of changes in Sphagnum structure on moisture holding and transporting capacity. Moreover, the strong length growth enhancement may affect interactions with other mosses and vascular plants. Because winter snow addition enhanced the production of S. fuscum without affecting its structure, it may increase the carbon balance of northern peatlands.</p>", "keywords": ["0106 biological sciences", "13. Climate action", "SDG 13 - Climate Action", "15. Life on land", "01 natural sciences"]}, "links": [{"href": "https://doi.org/10.1111/j.1365-2486.2003.00718.x"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Change%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/j.1365-2486.2003.00718.x", "name": "item", "description": "10.1111/j.1365-2486.2003.00718.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/j.1365-2486.2003.00718.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2003-12-15T00:00:00Z"}}, {"id": "10.1111/j.1365-2486.2011.02548.x", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:52Z", "type": "Journal Article", "created": "2011-09-27", "title": "Summer Warming Accelerates Sub-Arctic Peatland Nitrogen Cycling Without Changing Enzyme Pools Or Microbial Community Structure", "description": "Abstract<p>The balance of primary production and decomposition in northern peatlands may shift due to climate change, with potential feedbacks to atmosphericCO2concentrations. Nitrogen availability will modulate this shift, but little is known about the drivers of soil nitrogen dynamics in these environments. We used a long\uffe2\uff80\uff90term (9\uffc2\uffa0years) open top chamber (OTC) experiment in an ombrotrophicSphagnumpeat bog in sub\uffe2\uff80\uff90arctic Sweden, to test for the interactive effects of spring warming, summer warming and winter snow addition on soil nitrogen fluxes, potential activities of nitrogen cycle enzymes, and soil microbial community composition. These simultaneous measurements allowed us to identify the level of organization at which climate change impacts are apparent, an important requirement for developing truly mechanistic understanding. Organic\uffe2\uff80\uff90N pools and fluxes were an order of magnitude higher than inorganic\uffe2\uff80\uff90N pools and fluxes. Summer warming approximately doubled fluxes of soil organic nitrogen and ammonia over the growing season. Such a large increase under 1\uffc2\uffa0\uffc2\uffb0C warming is unlikely to be due to kinetic effects, and we propose that it is linked to an observed seasonal decrease in microbial biomass, suggesting that N flux is driven by a substantial late\uffe2\uff80\uff90season dieback of microbes. This change in N cycle dynamics was not reflected in any of the measured potential peptidase activities. Moreover, the soil microbial community structure was apparently stable across treatments, suggesting a non\uffe2\uff80\uff90specific microbial dieback. Our results show that in these widespread peat bogs, where many plant species are capable of organic\uffe2\uff80\uff90N uptake, organic soil N dynamics are quantitatively far more important than the commonly studied inorganic\uffe2\uff80\uff90N dynamics. Understanding of climate change effects on organic soil N cycling in this system will be advanced by closer investigation of the seasonal dynamics of the microbial biomass and the input of substrates that maintain it.</p>", "keywords": ["13. Climate action", "national", "SDG 13 - Climate Action", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land"]}, "links": [{"href": "https://doi.org/10.1111/j.1365-2486.2011.02548.x"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Change%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/j.1365-2486.2011.02548.x", "name": "item", "description": "10.1111/j.1365-2486.2011.02548.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/j.1365-2486.2011.02548.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2011-10-13T00:00:00Z"}}, {"id": "10.1111/j.1365-2486.2007.01439.x", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:49Z", "type": "Journal Article", "created": "2007-10-18", "title": "Co2balance Of Boreal, Temperate, And Tropical Forests Derived From A Global Database", "description": "Abstract<p>Terrestrial ecosystems sequester 2.1\uffe2\uff80\uff83Pg of atmospheric carbon annually. A large amount of the terrestrial sink is realized by forests. However, considerable uncertainties remain regarding the fate of this carbon over both short and long timescales. Relevant data to address these uncertainties are being collected at many sites around the world, but syntheses of these data are still sparse. To facilitate future synthesis activities, we have assembled a comprehensive global database for forest ecosystems, which includes carbon budget variables (fluxes and stocks), ecosystem traits (e.g. leaf area index, age), as well as ancillary site information such as management regime, climate, and soil characteristics. This publicly available database can be used to quantify global, regional or biome\uffe2\uff80\uff90specific carbon budgets; to re\uffe2\uff80\uff90examine established relationships; to test emerging hypotheses about ecosystem functioning [e.g. a constant net ecosystem production (NEP) to gross primary production (GPP) ratio]; and as benchmarks for model evaluations. In this paper, we present the first analysis of this database. We discuss the climatic influences on GPP, net primary production (NPP) and NEP and present the CO2 balances for boreal, temperate, and tropical forest biomes based on micrometeorological, ecophysiological, and biometric flux and inventory estimates. Globally, GPP of forests benefited from higher temperatures and precipitation whereas NPP saturated above either a threshold of 1500\uffe2\uff80\uff83mm precipitation or a mean annual temperature of 10 \uffc2\uffb0C. The global pattern in NEP was insensitive to climate and is hypothesized to be mainly determined by nonclimatic conditions such as successional stage, management, site history, and site disturbance. In all biomes, closing the CO2 balance required the introduction of substantial biome\uffe2\uff80\uff90specific closure terms. Nonclosure was taken as an indication that respiratory processes, advection, and non\uffe2\uff80\uff90CO2 carbon fluxes are not presently being adequately accounted for.</p>", "keywords": ["0106 biological sciences", "environment/Bioclimatology", "550", "[SDV]Life Sciences [q-bio]", "01 natural sciences", "630", "SDG 17 - Partnerships for the Goals", "carbon cycle", "SDG 13 - Climate Action", "carbon cycle; forest ecosystems; global database; gross primary productivity; net ecosystem productivity; net primary productivity", "net primary productivity", "global database", "0105 earth and related environmental sciences", "Ecology", "net ecosystem productivity", "forest ecosystems", "Biological Sciences", "15. Life on land", "Climate Action", "[SDV] Life Sciences [q-bio]", "[SDV.EE.BIO] Life Sciences [q-bio]/Ecology", " environment/Bioclimatology", "13. Climate action", "[SDV.EE.BIO]Life Sciences [q-bio]/Ecology", "CO2", "gross primary productivity", "Environmental Sciences"]}, "links": [{"href": "https://escholarship.org/content/qt57t1t77c/qt57t1t77c.pdf"}, {"href": "https://doi.org/10.1111/j.1365-2486.2007.01439.x"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Change%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/j.1365-2486.2007.01439.x", "name": "item", "description": "10.1111/j.1365-2486.2007.01439.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/j.1365-2486.2007.01439.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2007-08-21T00:00:00Z"}}, {"id": "10.1126/sciadv.aau8052", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:19:08Z", "type": "Journal Article", "created": "2019-02-14", "title": "Source apportionment of circum-Arctic atmospheric black carbon from isotopes and modeling", "description": "<p>Isotopes pinpoint strong seasonal variations in black carbon sources with consistent patterns at sites around the Arctic.</p>", "keywords": ["105206 Meteorology", "550", "13. Climate action", "SDG 13 \u2013 Ma\u00dfnahmen zum Klimaschutz", "105206 Meteorologie", "SDG 13 - Climate Action", "01 natural sciences", "7. Clean energy", "Research Articles", "0105 earth and related environmental sciences", "3. Good health"]}, "links": [{"href": "http://pure.iiasa.ac.at/id/eprint/15763/1/eaau8052.full.pdf"}, {"href": "https://pure.iiasa.ac.at/id/eprint/15763/1/eaau8052.full.pdf"}, {"href": "https://doi.org/10.1126/sciadv.aau8052"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Science%20Advances", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1126/sciadv.aau8052", "name": "item", "description": "10.1126/sciadv.aau8052", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1126/sciadv.aau8052"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-02-01T00:00:00Z"}}, {"id": "10.1111/j.1365-2745.2008.01472.x", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:53Z", "type": "Journal Article", "created": "2009-01-21", "title": "Determinants Of Cryptogam Composition And Diversity In Sphagnum-Dominated Peatlands: The Importance Of Temporal, Spatial And Functional Scales", "description": "Summary<p>  <p>Changing temperature regimes and precipitation patterns in the Subarctic will impact on vegetation composition and diversity including those of bryophyte and lichen communities, which are major drivers of high\uffe2\uff80\uff90latitude carbon and nutrient cycling and hydrology.</p> <p>We investigated the relative importance of such impacts at different temporal, spatial and plant functional scales in subarctic Sphagnum fuscum\uffe2\uff80\uff90dominated peatlands, comprising both an in situ warming experiment and natural climatic and topographic gradients in northern Sweden and Norway. We applied multivariate analyses to investigate the relationships among cryptogam and vascular plant species composition and abiotic (temperature, moisture) and biotic (Sphagnum growth) regimes at various scales.</p> <p>At the short\uffe2\uff80\uff90term temporal scale (4\uffe2\uff80\uff90year warming experiment), increased temperature yielded no clear effect on cryptogam or vascular plant species composition. Spatially, direct effects of temperature were decisive for overall species composition across regions (macro\uffe2\uff80\uff90scale) rather than within one region (meso\uffe2\uff80\uff90scale). Moisture and Sphagnum growth were drivers of species composition at all spatial scales, and Sphagnum growth itself depended on its position on the microtopographic gradient and on temperature.</p> <p>Grouping of bryophytes and lichens at increasing scales of functional aggregation from species, growth form to the major higher taxon level (Sphagnum, other mosses, liverworts, lichens) revealed mostly increasing correlation with climate regimes and Sphagnum growth. Excluding liverworts from the analysis tended to reduce the correlation.</p> <p>Abundances of lichens, liverworts, non\uffe2\uff80\uff90Sphagnum mosses and (to a lesser degree) vascular plants were negatively related to Sphagnum abundance. Few cryptogam and vascular plant species showed a positive relationship with Sphagnum abundance. Correspondingly, cryptogam species richness and Shannon Index on peatlands strongly declined as Sphagnum abundance increased, while indices for vascular plants showed no significant relationship.</p> <p> Synthesis. Scale, be it spatial or functional, strongly determined which environmental drivers showed the clearest relationships with vegetation composition and diversity. Our findings will help to optimize predictions about long\uffe2\uff80\uff90term effects of climate on peatland vegetation composition, and subsequently its feedbacks to carbon and water cycles, at the regional scale.</p>  </p>", "keywords": ["0106 biological sciences", "simulated environmental-change", "species composition", "western canada", "alaskan arctic tundra", "response surfaces", "15. Life on land", "01 natural sciences", "hylocomium-splendens", "13. Climate action", "physical gradients", "SDG 13 - Climate Action", "nutrient availability", "community structure", "global change"]}, "links": [{"href": "https://doi.org/10.1111/j.1365-2745.2008.01472.x"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Ecology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/j.1365-2745.2008.01472.x", "name": "item", "description": "10.1111/j.1365-2745.2008.01472.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/j.1365-2745.2008.01472.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2009-02-11T00:00:00Z"}}, {"id": "10.1111/j.1365-3040.2010.02201.x", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:53Z", "type": "Journal Article", "created": "2010-06-21", "title": "Soil [N] modulates soil C cycling in CO2-fumigated tree stands: a meta-analysis", "description": "ABSTRACT<p>Under elevated atmospheric CO2 concentrations, soil carbon (C) inputs are typically enhanced, suggesting larger soil C sequestration potential. However, soil C losses also increase and progressive nitrogen (N) limitation to plant growth may reduce the CO2 effect on soil C inputs with time. We compiled a data set from 131 manipulation experiments, and used meta\uffe2\uff80\uff90analysis to test the hypotheses that: (1) elevated atmospheric CO2 stimulates soil C inputs more than C losses, resulting in increasing soil C stocks; and (2) that these responses are modulated by N. Our results confirm that elevated CO2 induces a C allocation shift towards below\uffe2\uff80\uff90ground biomass compartments. However, the increased soil C inputs were offset by increased heterotrophic respiration (Rh), such that soil C content was not affected by elevated CO2. Soil N concentration strongly interacted with CO2 fumigation: the effect of elevated CO2 on fine root biomass and \uffe2\uff80\uff93production and on microbial activity increased with increasing soil N concentration, while the effect on soil C content decreased with increasing soil N concentration. These results suggest that both plant growth and microbial activity responses to elevated CO2 are modulated by N availability, and that it is essential to account for soil N concentration in C cycling analyses.</p>", "keywords": ["0301 basic medicine", "Physiology", "Plant Science", "Fine root production", "Carbon Cycle", "Trees", "Soil", "03 medical and health sciences", "Microbial respiration", "microbial respiration", "XXXXXX - Unknown", "C sequestration", "SDG 13 - Climate Action", "Biomass", "Fertilizers", "Biology", "[CO] enrichment", "2. Zero hunger", "[SDU.OCEAN]Sciences of the Universe [physics]/Ocean", "0303 health sciences", "biomass", "[SDU.OCEAN] Sciences of the Universe [physics]/Ocean", " Atmosphere", "Atmosphere", "Root biomass", "Carbon Dioxide", "Nitrogen Cycle", "15. Life on land", "carbon sequestration", "N fertilization", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "nitrogen fertilizers", "roots (botany)", "13. Climate action", "[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces", "environment"]}, "links": [{"href": "https://doi.org/10.1111/j.1365-3040.2010.02201.x"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Plant%2C%20Cell%20%26amp%3B%20Environment", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/j.1365-3040.2010.02201.x", "name": "item", "description": "10.1111/j.1365-3040.2010.02201.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/j.1365-3040.2010.02201.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2010-11-12T00:00:00Z"}}, {"id": "10.1111/j.1461-0248.2007.01051.x", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:55Z", "type": "Journal Article", "created": "2007-05-14", "title": "Global Negative Vegetation Feedback To Climate Warming Responses Of Leaf Litter Decomposition Rates In Cold Biomes", "description": "Abstract<p>Whether climate change will turn cold biomes from large long\uffe2\uff80\uff90term carbon sinks into sources is hotly debated because of the great potential for ecosystem\uffe2\uff80\uff90mediated feedbacks to global climate. Critical are the direction, magnitude and generality of climate responses of plant litter decomposition. Here, we present the first quantitative analysis of the major climate\uffe2\uff80\uff90change\uffe2\uff80\uff90related drivers of litter decomposition rates in cold northern biomes worldwide. Leaf litters collected from the predominant species in 33 global change manipulation experiments in circum\uffe2\uff80\uff90arctic\uffe2\uff80\uff90alpine ecosystems were incubated simultaneously in two contrasting arctic life zones. We demonstrate that longer\uffe2\uff80\uff90term, large\uffe2\uff80\uff90scale changes to leaf litter decomposition will be driven primarily by both direct warming effects and concomitant shifts in plant growth form composition, with a much smaller role for changes in litter quality within species. Specifically, the ongoing warming\uffe2\uff80\uff90induced expansion of shrubs with recalcitrant leaf litter across cold biomes would constitute a negative feedback to global warming. Depending on the strength of other (previously reported) positive feedbacks of shrub expansion on soil carbon turnover, this may partly counteract direct warming enhancement of litter decomposition.</p>", "keywords": ["Greenhouse Effect", "Sweden", "0106 biological sciences", "Analysis of Variance", "Plant Development", "04 agricultural and veterinary sciences", "Plants", "15. Life on land", "Cold Climate", "Models", " Biological", "01 natural sciences", "Carbon", "Plant Leaves", "Species Specificity", "13. Climate action", "SDG 13 - Climate Action", "0401 agriculture", " forestry", " and fisheries", "Alpine; carbon; circum-arctic; global change; growth form; litter turnover; mass loss; vegetation change.", "Ecosystem"]}, "links": [{"href": "https://doi.org/10.1111/j.1461-0248.2007.01051.x"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Ecology%20Letters", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/j.1461-0248.2007.01051.x", "name": "item", "description": "10.1111/j.1461-0248.2007.01051.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/j.1461-0248.2007.01051.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2007-05-14T00:00:00Z"}}, {"id": "10.1111/j.1469-8137.2012.04256.x", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:56Z", "type": "Journal Article", "created": "2012-08-13", "title": "Litter Stoichiometric Traits Of Plant Species Of High-Latitude Ecosystems Show High Responsiveness To Global Change Without Causing Strong Variation In Litter Decomposition", "description": "\u2022 High-latitude ecosystems are important carbon accumulators, mainly as a result of low decomposition rates of litter and soil organic matter. We investigated whether global change impacts on litter decomposition rates are constrained by litter stoichiometry. \u2022 Thereto, we investigated the interspecific natural variation in litter stoichiometric traits (LSTs) in high-latitude ecosystems, and compared it with climate change-induced LST variation measured in the Meeting of Litters (MOL) experiment. This experiment includes leaf litters originating from 33 circumpolar and high-altitude global change experiments. Two-year decomposition rates of litters from these experiments were measured earlier in two common litter beds in sub-Arctic Sweden. \u2022 Response ratios of LSTs in plants of high-latitude ecosystems in the global change treatments showed a three-fold variation, and this was in the same range as the natural variation among species. However, response ratios of decomposition were about an order of magnitude lower than those of litter carbon/nitrogen ratios. \u2022 This implies that litter stoichiometry does not constrain the response of plant litter decomposition to global change. We suggest that responsiveness is rather constrained by the less responsive traits of the Plant Economics Spectrum of litter decomposability, such as lignin and dry matter content and specific leaf area.", "keywords": ["Sweden", "0106 biological sciences", "Nitrogen", "Altitude", "Climate Change", "15. Life on land", "01 natural sciences", "Carbon", "Plant Leaves", "Quantitative Trait", " Heritable", "Species Specificity", "13. Climate action", "SDG 13 - Climate Action", "Ecosystem"]}, "links": [{"href": "https://doi.org/10.1111/j.1469-8137.2012.04256.x"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/New%20Phytologist", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/j.1469-8137.2012.04256.x", "name": "item", "description": "10.1111/j.1469-8137.2012.04256.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/j.1469-8137.2012.04256.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2012-08-13T00:00:00Z"}}, {"id": "10.5194/bg-20-271-2023", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:21:40Z", "type": "Journal Article", "created": "2023-01-17", "title": "Contrasts in dissolved, particulate, and sedimentary organic carbon from the Kolyma River to the East Siberian Shelf", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Abstract. Arctic rivers will be increasingly affected by the hydrological and biogeochemical consequences of thawing permafrost. During transport, permafrost-derived organic carbon (OC) can either accumulate in floodplain and shelf sediments or be degraded into greenhouse gases prior to final burial. Thus, the net impact of permafrost OC on climate will ultimately depend on the interplay of complex processes that occur along the source-to-sink system. Here, we focus on the Kolyma River, the largest watershed completely underlain by continuous permafrost, and marine sediments of the East Siberian Sea, as a transect to investigate the fate of permafrost OC along the land\u2013ocean continuum. Three pools of riverine OC were investigated for the Kolyma main stem and five of its tributaries: dissolved OC (DOC), suspended particulate OC (POC), and riverbed sediment OC (SOC). They were compared with earlier findings in marine sediments. Carbon isotopes (\u03b413C, \u039414C), lignin phenol, and lipid biomarker proxies show a contrasting composition and degradation state of these different carbon pools. Dual C isotope source apportionment calculations imply that old permafrost-OC is mostly associated with sediments (SOC; contribution of 68\u00b110\u2009%), and less dominant in POC (38\u00b18\u2009%), whereas autochthonous primary production contributes around 44\u00b110\u2009% to POC in the main stem and up to 79\u00b111\u2009% in tributaries. Biomarker degradation indices suggest that Kolyma DOC might be relatively degraded, regardless of its generally young age shown by previous studies. In contrast, SOC shows the lowest \u039414C value (oldest OC), yet relatively fresh compositional signatures. Furthermore, decreasing mineral surface area-normalised OC- and biomarker loadings suggest that SOC might be reactive along the land\u2013ocean continuum and almost all parameters were subjected to rapid change when moving from freshwater to the marine environment. This suggests that sedimentary dynamics play a crucial role when targeting permafrost-derived OC in aquatic systems and support earlier studies highlighting the fact that the land\u2013ocean transition zone is an efficient reactor and a dynamic environment. The prevailing inconsistencies between freshwater and marine research (i.e.\u00a0targeting predominantly DOC and SOC respectively) need to be better aligned in order to determine to what degree thawed permafrost OC may be destined for long-term burial, thereby attenuating further global warming.</p></article>", "keywords": ["QE1-996.5", "Ecology", "Permafrost", " Climate Feedback", " Climate Change", " Arctic", "Geology", "15. Life on land", "01 natural sciences", "6. Clean water", "Life", "13. Climate action", "QH501-531", "SDG 13 - Climate Action", "14. Life underwater", "QH540-549.5", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://bg.copernicus.org/articles/20/271/2023/bg-20-271-2023.pdf"}, {"href": "https://doi.org/10.5194/bg-20-271-2023"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biogeosciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.5194/bg-20-271-2023", "name": "item", "description": "10.5194/bg-20-271-2023", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5194/bg-20-271-2023"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-06-27T00:00:00Z"}}, {"id": "10.1128/msystems.00562-19", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:19:11Z", "type": "Journal Article", "created": "2020-01-13", "title": "Transcriptomic Response of Nitrosomonas europaea Transitioned from Ammonia- to Oxygen-Limited Steady-State Growth", "description": "<p>             Nitrification is a ubiquitous microbially mediated process in the environment and an essential process in engineered systems such as wastewater and drinking water treatment plants. However, nitrification also contributes to fertilizer loss from agricultural environments, increasing the eutrophication of downstream aquatic ecosystems, and produces the greenhouse gas nitrous oxide. As ammonia-oxidizing bacteria are the most dominant ammonia-oxidizing microbes in fertilized agricultural soils, understanding their responses to a variety of environmental conditions is essential for curbing the negative environmental effects of nitrification. Notably, oxygen limitation has been reported to significantly increase nitric oxide and nitrous oxide production during nitrification. Here, we investigate the physiology of the best-characterized ammonia-oxidizing bacterium,             Nitrosomonas europaea             , growing under oxygen-limited conditions.           </p", "keywords": ["OXIDIZING BACTERIUM", "0301 basic medicine", "nitrificatio", "Nitrosomonas europaea", "ammonia and oxygen limitation", "NITRIFICATION", "Microbiology", "CYTOCHROME-C", "03 medical and health sciences", "NITROUS-OXIDE PRODUCTION", "SDG 13 - Climate Action", "COMPLETE GENOME SEQUENCE", "ELECTRON-TRANSFER", "14. Life underwater", "SDG 2 \u2013 Kein Hunger", "SDG 2 - Zero Hunger", "Ammonia-oxidizing bacteria", "2. Zero hunger", "106022 Mikrobiologie", "chemostat", "0303 health sciences", "NITRIC-OXIDE", "N2O-PRODUCING PATHWAYS", "15. Life on land", "Ammonia and oxygen limitation", "Nitrification", "HYDROXYLAMINE OXIDOREDUCTASE", "nitrification", "QR1-502", "6. Clean water", "Chemostat", "13. Climate action", "SDG 13 \u2013 Ma\u00dfnahmen zum Klimaschutz", "ammonia-oxidizing bacteria", "106022 Microbiology", "Transcriptome", "transcriptome", "NO REDUCTASE-ACTIVITY", "COMPLETE NITRIFICATION", "Research Article"]}, "links": [{"href": "https://www.biorxiv.org/content/10.1101/765727v1.full.pdf"}, {"href": "https://journals.asm.org/doi/pdf/10.1128/mSystems.00562-19"}, {"href": "https://doi.org/10.1128/msystems.00562-19"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/mSystems", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1128/msystems.00562-19", "name": "item", "description": "10.1128/msystems.00562-19", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1128/msystems.00562-19"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-09-11T00:00:00Z"}}, {"id": "10.1175/bams-d-23-0005.1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:19:18Z", "type": "Journal Article", "created": "2023-08-23", "title": "Observing Mineral Dust in Northern Africa, the Middle East, and Europe: Current Capabilities and Challenges ahead for the Development of Dust Services", "description": "Abstract <p>Mineral dust produced by wind erosion of arid and semiarid surfaces is a major component of atmospheric aerosol that affects climate, weather, ecosystems, and socioeconomic sectors such as human health, transportation, solar energy, and air quality. Understanding these effects and ultimately improving the resilience of affected countries requires a reliable, dense, and diverse set of dust observations, fundamental for the development and the provision of skillful dust-forecast-tailored products. The last decade has seen a notable improvement of dust observational capabilities in terms of considered parameters, geographical coverage, and delivery times, as well as of tailored products of interest to both the scientific community and the various end-users. Given this progress, here we review the current state of observational capabilities, including in situ, ground-based, and satellite remote sensing observations in northern Africa, the Middle East, and Europe for the provision of dust information considering the needs of various users. We also critically discuss observational gaps and related unresolved questions while providing suggestions for overcoming the current limitations. Our review aims to be a milestone for discussing dust observational gaps at a global level to address the needs of users, from research communities to nonscientific stakeholders.</p", "keywords": ["[SDE] Environmental Sciences", "Mineral dusts", "Dust services", "550", "103039 Aerosol physics", "105208 Atmospheric chemistry", "Mineral dust", "Earth system -- environmental sciences", "[SDU] Sciences of the Universe [physics]", "Middle East", "\u00c0rees tem\u00e0tiques de la UPC::Enginyeria agroaliment\u00e0ria::Ci\u00e8ncies de la terra i de la vida::Climatologia i meteorologia", "SDG 3 - Good Health and Well-being", "Simulaci\u00f3 per ordinador", "11. Sustainability", "SDG 13 - Climate Action", "Northern Africa", "103039 Aerosolphysik", "observation capabilities", "current capabilities and challenges", "mineral dust", "info:eu-repo/classification/ddc/550", "Earth radiation", "ddc:550", "health", "15. Life on land", "Remote sensing", "Atmospheric aerosols", "Aerosols/ particulates; In situ atmospheric observations; Remote sensing; Air quality and health", "105208 Atmosph\u00e4renchemie", "Europe", "Earth sciences", "13. Climate action", "103037 Environmental physics", "SDG 3 \u2013 Gesundheit und Wohlergehen", "SDG 13 \u2013 Ma\u00dfnahmen zum Klimaschutz", "In situ atmospheric observations", "Air quality", "dust service", "Aerosols/ particulates", "Dust observation", "Satellite remote sensing observations", "103037 Umweltphysik", "Atmospheric aerosol"]}, "links": [{"href": "https://iris.cnr.it/bitstream/20.500.14243/452880/1/prod_491741-doc_205111.pdf"}, {"href": "https://www.iris.unisa.it/bitstream/11386/4857971/1/bams-BAMS-D-23-0005.1-2.pdf"}, {"href": "https://journals.ametsoc.org/downloadpdf/journals/bams/104/12/BAMS-D-23-0005.1.xml"}, {"href": "https://doi.org/10.1175/bams-d-23-0005.1"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Bulletin%20of%20the%20American%20Meteorological%20Society", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1175/bams-d-23-0005.1", "name": "item", "description": "10.1175/bams-d-23-0005.1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1175/bams-d-23-0005.1"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-12-01T00:00:00Z"}}, {"id": "10.1175/bams-d-19-0316.1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:19:18Z", "type": "Journal Article", "created": "2021-04-29", "title": "Closing the water cycle from observations across scales: Where do we stand?", "description": "ABSTRACT<p>Life on Earth vitally depends on the availability of water. Human pressure on freshwater resources is increasing, as is human exposure to weather-related extremes (droughts, storms, floods) caused by climate change. Understanding these changes is pivotal for developing mitigation and adaptation strategies. The Global Climate Observing System (GCOS) defines a suite of essential climate variables (ECVs), many related to the water cycle, required to systematically monitor Earth\uffe2\uff80\uff99s climate system. Since long-term observations of these ECVs are derived from different observation techniques, platforms, instruments, and retrieval algorithms, they often lack the accuracy, completeness, and resolution, to consistently characterize water cycle variability at multiple spatial and temporal scales. Here, we review the capability of ground-based and remotely sensed observations of water cycle ECVs to consistently observe the hydrological cycle. We evaluate the relevant land, atmosphere, and ocean water storages and the fluxes between them, including anthropogenic water use. Particularly, we assess how well they close on multiple temporal and spatial scales. On this basis, we discuss gaps in observation systems and formulate guidelines for future water cycle observation strategies. We conclude that, while long-term water cycle monitoring has greatly advanced in the past, many observational gaps still need to be overcome to close the water budget and enable a comprehensive and consistent assessment across scales. Trends in water cycle components can only be observed with great uncertainty, mainly due to insufficient length and homogeneity. An advanced closure of the water cycle requires improved model\uffe2\uff80\uff93data synthesis capabilities, particularly at regional to local scales.</p>", "keywords": ["550", "Hydrologic cycle", "0207 environmental engineering", "[SDU.STU]Sciences of the Universe [physics]/Earth Sciences", "02 engineering and technology", "/dk/atira/pure/sustainabledevelopmentgoals/clean_water_and_sanitation; name=SDG 6 - Clean Water and Sanitation", "551", "01 natural sciences", "333", "Water masses", "[SDU] Sciences of the Universe [physics]", "storage", "/dk/atira/pure/sustainabledevelopmentgoals/climate_action; name=SDG 13 - Climate Action", "Water budget/balance", "Water budget", "0105 earth and related environmental sciences", "Surface fluxes", "/dk/atira/pure/sustainabledevelopmentgoals/life_below_water; name=SDG 14 - Life Below Water", "Water masses/storage", "balance", "Surface observations", "15. Life on land", "6. Clean water", "Satellite observations", "[SDU]Sciences of the Universe [physics]", "13. Climate action", "[SDU.STU] Sciences of the Universe [physics]/Earth Sciences"]}, "links": [{"href": "https://centaur.reading.ac.uk/98278/1/Dorigo-2021-Closing-the-water-cycle-from-observ.pdf"}, {"href": "https://journals.ametsoc.org/downloadpdf/journals/bams/102/10/BAMS-D-19-0316.1.xml"}, {"href": "https://doi.org/10.1175/bams-d-19-0316.1"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Bulletin%20of%20the%20American%20Meteorological%20Society", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1175/bams-d-19-0316.1", "name": "item", "description": "10.1175/bams-d-19-0316.1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1175/bams-d-19-0316.1"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-10-01T00:00:00Z"}}, {"id": "10.15376/biores.13.3.5976-6002", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:19:36Z", "type": "Journal Article", "created": "2022-09-21", "title": "Effects of Biomass Type, Carbonization Process, and Activation Method on the Properties of Bio-Based Activated Carbons", "description": "<p>Activated carbons (AC) serve as adsorbents in various applications requiring specific functionalities. In this study, the effects of biomass type, pre-carbonization process, and activation method on the properties of ACs were investigated. Chemical (KOH and H3PO4) and physical (CO2) activations were performed on slow pyrolyzed and hydrothermally carbonized (HTC) biochars produced from two feedstocks, willow and Scots pine bark (SPB). In addition, the adsorption capacities of the ACs were tested with two dyes and zinc metal. Distinct differences were found between the biochars and ACs regarding pore size distributions, surface area (238 \uffe2\uff80\uff93 3505 m2 g-1), and surface chemistry. KOH activation produced highly microporous ACs from all biochars, whereas with H3PO4 and CO2 there was also increase in the meso- and macroporosity with the HTC biochars. Adsorption capacity for dyes was dependent on the surface area, while for zinc it depended on AC\uffe2\uff80\uff99s pH. The results provide interesting insights into tailoring ACs for specific applications.</p>", "keywords": ["bark", "willow", "biohiili", "330", "Willow", "Activated carbon", "Activated carbon;", "pine bark", "pajut", "Pinus sylvestris", "tomography", "bio-based activated carbon", "620", "Biochar", "tomografia", "Pine bark", "SDG 13 - Climate Action", "Bio-based activated carbon", "activated carbon", "biochar", "ta219", "SDG 7 - Affordable and Clean Energy", "X-ray tomography"]}, "links": [{"href": "https://bioresources.cnr.ncsu.edu/wp-content/uploads/2018/06/BioRes_13_3_5976_Siipola_Effects_Biomass_Type_Carbonizat_Process_Activat_Method_Activ_C_13985.pdf"}, {"href": "https://doi.org/10.15376/biores.13.3.5976-6002"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/BioResources", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.15376/biores.13.3.5976-6002", "name": "item", "description": "10.15376/biores.13.3.5976-6002", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.15376/biores.13.3.5976-6002"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-06-15T00:00:00Z"}}, {"id": "10.20944/preprints202304.0088.v1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:19:58Z", "type": "Journal Article", "created": "2023-04-07", "title": "A Review of Permanent Grassland Grazing Management Practices and the Impacts on Principal Soil Quality Indicators", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Grasslands are at risk of degradation due to unsustainable management practices and climate change. Sustainable grassland soil management can promote ecosystem service delivery and improve the resilience of the entire grassland ecosystem to anthropogenic change. Here, we re-view the principal soil quality indicators (SQIs) and how they have been used to evaluate the sustainability of different grassland management practices globally. We then discuss sustainable grazing management practices, before reviewing some novel grassland species which may im-prove grassland resilience with relevance for grassland management in Europe and the UK. We also give an overview of current sustainable grassland management methods and their assessment at field scale. From this, we suggest that sustainable Grazing Management Plans (GMPs), together with the testing of drought-resistant grass species and appropriate SQIs monitoring, is key to increasing resilience of grassland ecosystems to anthropogenic change.</p></article>", "keywords": ["2. Zero hunger", "330", "S", "QH301 Biology", "soil quality indicators; grazing management; ecosystem services; permanent grasslands; management practices", "Agriculture", "15. Life on land", "12. Responsible consumption", "Permanent grasslands", "permanent grasslands", "QH301", "Soil quality indicators", "13. Climate action", "SDG 13 - Climate Action", "agricultural_science_and_agronomy_16", "management practices", "Ecosystem services", "Grazing management", "soil quality indicators", "grazing management", "ecosystem services"]}, "links": [{"href": "https://iris.unito.it/bitstream/2318/1910970/1/A53%20Grassland%20erosion%20Agronomy.pdf"}, {"href": "https://www.mdpi.com/2073-4395/13/5/1366/pdf"}, {"href": "https://doi.org/10.20944/preprints202304.0088.v1"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Agronomy", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.20944/preprints202304.0088.v1", "name": "item", "description": "10.20944/preprints202304.0088.v1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.20944/preprints202304.0088.v1"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-04-06T00:00:00Z"}}, {"id": "10.2136/vzj2015.09.0131", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:20:24Z", "type": "Journal Article", "created": "2016-05-13", "title": "Modeling Soil Processes: Review, Key Challenges, and New Perspectives", "description": "Core Ideas<p><p>A community effort is needed to move soil modeling forward.</p><p>Establishing an international soil modeling consortium is key in this respect.</p><p>There is a need to better integrate existing knowledge in soil models.</p><p>Integration of data and models is a key challenge in soil modeling.</p></p><p>The remarkable complexity of soil and its importance to a wide range of ecosystem services presents major challenges to the modeling of soil processes. Although major progress in soil models has occurred in the last decades, models of soil processes remain disjointed between disciplines or ecosystem services, with considerable uncertainty remaining in the quality of predictions and several challenges that remain yet to be addressed. First, there is a need to improve exchange of knowledge and experience among the different disciplines in soil science and to reach out to other Earth science communities. Second, the community needs to develop a new generation of soil models based on a systemic approach comprising relevant physical, chemical, and biological processes to address critical knowledge gaps in our understanding of soil processes and their interactions. Overcoming these challenges will facilitate exchanges between soil modeling and climate, plant, and social science modeling communities. It will allow us to contribute to preserve and improve our assessment of ecosystem services and advance our understanding of climate\uffe2\uff80\uff90change feedback mechanisms, among others, thereby facilitating and strengthening communication among scientific disciplines and society. We review the role of modeling soil processes in quantifying key soil processes that shape ecosystem services, with a focus on provisioning and regulating services. We then identify key challenges in modeling soil processes, including the systematic incorporation of heterogeneity and uncertainty, the integration of data and models, and strategies for effective integration of knowledge on physical, chemical, and biological soil processes. We discuss how the soil modeling community could best interface with modern modeling activities in other disciplines, such as climate, ecology, and plant research, and how to weave novel observation and measurement techniques into soil models. We propose the establishment of an international soil modeling consortium to coherently advance soil modeling activities and foster communication with other Earth science disciplines. Such a consortium should promote soil modeling platforms and data repository for model development, calibration and intercomparison essential for addressing contemporary challenges.</p", "keywords": ["organic-matter dynamics", "550", "QH301 Biology", "0208 environmental biotechnology", "SATURATED-UNSATURATED FLOW", "02 engineering and technology", "soil processes", "01 natural sciences", "Physical Geography and Environmental Geoscience", "Sciences de la Terre", "ARBUSCULAR MYCORRHIZAL FUNGI", "sciences du sol", "ANZSRC::3707 Hydrology", "SYNTHETIC-APERTURE RADAR", "ANZSRC::4106 Soil sciences", "SDG 13 - Climate Action", "2. Zero hunger", "GROUND-PENETRATING RADAR", "diffuse-reflectance spectroscopy", "ANZSRC::050399 Soil Sciences not elsewhere classified", "synthetic-aperture radar", "digital elevation model", "SDG 13 \u2013 Ma\u00dfnahmen zum Klimaschutz", "MULTIPLE ECOSYSTEM SERVICES", "knowledge integration", "Crop and Pasture Production", "101028 Mathematical modelling", "570", "DIFFUSE-REFLECTANCE SPECTROSCOPY", "Environmental Engineering", "international soil modeling consortium", "0207 environmental engineering", "Soil Science", "[SDU.STU]Sciences of the Universe [physics]/Earth Sciences", "arbuscular mycorrhizal fungi", "soil science", "ORGANIC-MATTER DYNAMICS", "QH301", "ANZSRC::0503 Soil Sciences", "Life Science", "SEDIMENT TRANSPORT MODELS", "data integration", "sediment transport models", "approche ecosyst\u00e9mique", "mod\u00e9lisation", "0105 earth and related environmental sciences", "ground-penetrating radar", "info:eu-repo/classification/ddc/550", "soil modeling", "ANZSRC::080110 Simulation and Modelling", "ROOT WATER-UPTAKE", "15. Life on land", "multiple ecosystem services", "root water-uptake", "13. Climate action", "Earth and Environmental Sciences", "Soil Sciences", "[SDU.STU] Sciences of the Universe [physics]/Earth Sciences", "Earth Sciences", "101028 Mathematische Modellierung", "saturated-unsaturated flow", "root water-uptake", " sediment transport models", " diffuse-reflectance spectroscopy", " arbuscular mycorrhizal fungi", " multiple ecosystem services", " saturated-unsaturated flow", " ground-penetrating radar", " synthetic-aperture radar", " digital elevation model", " organic-matter dynamics.", "DIGITAL ELEVATION MODEL"]}, "links": [{"href": "http://onlinelibrary.wiley.com/wol1/doi/10.2136/vzj2015.09.0131/fullpdf"}, {"href": "https://escholarship.org/content/qt6976n34c/qt6976n34c.pdf"}, {"href": "https://doi.org/10.2136/vzj2015.09.0131"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Vadose%20Zone%20Journal", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.2136/vzj2015.09.0131", "name": "item", "description": "10.2136/vzj2015.09.0131", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.2136/vzj2015.09.0131"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2016-05-01T00:00:00Z"}}, {"id": "10.2307/3546865", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:20:32Z", "type": "Journal Article", "created": "2007-02-02", "title": "Nitrogen Deposition Effects On Carbon Dioxide And Methane Emissions From Temperate Peatland Soils", "description": "Northern peatlands are important sources of carbon dioxide and methane emissions to the atmosphere. Increased atmospheric N deposition may have a significant impact on the emission of these greenhouse gases. We studied CO 2  and CH 4  emissions from untreated temperate peat soils from a eutrophic and a mesotrophic fen in a high N deposition area (the Netherlands) and from a mesotrophic fen in a low N deposition area (north-east Poland). In addition, we investigated the effects of N, P and glucose amendments on the emissions of CO 2  and CH 4  from these soils. Nitrogen availability (extractable NH 4  + ) in untreated peat from the high N area was 2.5-7.5 times higher than in the low N area, whereas the pH was 0.9-1.7 units lower. Using 6-week laboratory incubations of peat columns, we found that mean daily CO 2  emission from untreated peat soils from the high N area was lower than that from the low N area. Both linear and multiple regression analysis showed that CO 2 emission was positively related to soil pH (r 2  = 0.64). Additional N supply led to pH reduction and to lower CO 2  emission, especially in the low N peat soils. Thus, increased atmospheric N deposition leads, probably as a result of soil acidification, to lower CO 2  emission. Although glucose amendments resulted in increased CO, and CH 4  emission, we did not find evidence that this was caused by increased mineralization of native peat. Mean daily CH 4 -C emission was about 1-2 orders of magnitude lower than mean daily CO 2 -C emission. In the untreated peat soils from the high N eutrophic site, methane emission was higher than in the high N mesotrophic site and in the low N mesotrophic site. Linear regression analysis showed a positive relation between methane emission and soil fertility variables (r 2 =0.42-0.55), whereas a multiple regression model revealed that methane emission was determined by N-related soil chemistry variables (r 2  = 0.93). Increased nutrient supply initially resulted in higher methane emission from soils of both mesotrophic sites, but there was no effect on the high N eutrophic soil. These results show that increased atmospheric N deposition leads to increased methane emission from low-fertility peat soils. However, the ultimate effect of atmospheric N deposition on trace gas emissions and thereby on global warming is determined by the balance between the ratios of the change in CO 2 -C emission and CH 4 -C emission and the ratio of their global warming potentials (1:21).", "keywords": ["13. Climate action", "SDG 13 - Climate Action", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "14. Life underwater", "15. Life on land"]}, "links": [{"href": "https://doi.org/10.2307/3546865"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Oikos", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.2307/3546865", "name": "item", "description": "10.2307/3546865", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.2307/3546865"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "1999-01-01T00:00:00Z"}}, {"id": "10.3389/feart.2021.630493", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:20:42Z", "type": "Journal Article", "created": "2021-03-26", "title": "Permafrost Carbon and CO2 Pathways Differ at Contrasting Coastal Erosion Sites in the Canadian Arctic", "description": "<p>Warming air and sea temperatures, longer open-water seasons and sea-level rise collectively promote the erosion of permafrost coasts in the Arctic, which profoundly impacts organic matter pathways. Although estimates on organic carbon (OC) fluxes from erosion exist for some parts of the Arctic, little is known about how much OC is transformed into greenhouse gases (GHGs). In this study we investigated two different coastal erosion scenarios on Qikiqtaruk \uffe2\uff80\uff93 Herschel Island (Canada) and estimate the potential for GHG formation. We distinguished between adelayedrelease represented bymud debrisdraining a coastal thermoerosional feature and adirectrelease represented bycliff debrisat a low collapsing bluff. Carbon dioxide (CO2) production was measured during incubations at 4\uffc2\uffb0C under aerobic conditions for two months and were modeled for four months and a full year. Our incubation results show thatmud debrisandcliff debrislost a considerable amount of OC as CO2(2.5 \uffc2\uffb1 0.2 and 1.6 \uffc2\uffb1 0.3% of OC, respectively). Although relative OC losses were highest in mineralmud debris, higher initial OC content and fresh organic matter incliff debrisresulted in a \uffe2\uff88\uffbcthree times higher cumulative CO2release (4.0 \uffc2\uffb1 0.9 compared to 1.4 \uffc2\uffb1 0.1 mg CO2gdw\uffe2\uff80\uff931), which was further increased by the addition of seawater. After four months, modeled OC losses were 4.9 \uffc2\uffb1 0.1 and 3.2 \uffc2\uffb1 0.3% in set-ups without seawater and 14.3 \uffc2\uffb1 0.1 and 7.3 \uffc2\uffb1 0.8% in set-ups with seawater. The results indicate that adelayedrelease may support substantial cycling of OC at relatively low CO2production rates during long transit timesonshoreduring the Arctic warm season. By contrast,directerosion may result in a single CO2pulse and less substantial OC cyclingonshoreas transfer times are short. Once eroded sediments are deposited in thenearshore, highest OC losses can be expected. We conclude that the release of CO2from eroding permafrost coasts varies considerably between erosion types and residence timeonshore. We emphasize the importance of a more comprehensive understanding of OC degradation during the coastal erosion process to improve thawed carbon trajectories and models.</p", "keywords": ["550", "Science", "Q", "carbon dioxide", "biomarkers", "carbon cycling", "15. Life on land", "01 natural sciences", "Arctic", "biogeochemistry", "13. Climate action", "greenhouse gases", "11. Sustainability", "SDG 13 - Climate Action", "SDG 14 - Life Below Water", "14. Life underwater", "Arctic; coastal erosion; carbon cycling; biogeochemistry; greenhouse gases; carbon dioxide; biomarkers", "coastal erosion", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.3389/feart.2021.630493"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Frontiers%20in%20Earth%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3389/feart.2021.630493", "name": "item", "description": "10.3389/feart.2021.630493", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3389/feart.2021.630493"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-03-26T00:00:00Z"}}, {"id": "10.3389/feart.2021.642675", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:20:42Z", "type": "Journal Article", "created": "2021-03-29", "title": "Downstream Evolution of Particulate Organic Matter Composition From Permafrost Thaw Slumps", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Permafrost soils, which store almost half of the global belowground organic carbon (OC), are susceptible to thaw upon climate warming. On the Peel Plateau of northwestern Canada, the number and size of retrogressive thaw slumps (RTS) has increased in recent decades due to rising temperatures and higher precipitation. These RTS features caused by the rapid thaw of ice-rich permafrost release organic matter dominantly as particulate organic carbon (POC) to the stream network. In this study, we sampled POC and streambank sediments along a fluvial transect (\u223c12 km) downstream from two RTS features and assessed the composition and degradation status of the mobilized permafrost OC. We found that RTS features add old, Pleistocene-aged permafrost POC to the stream system that is traceable kilometers downstream. The POC released consists mainly of recalcitrant compounds that persists within stream networks, whereas labile compounds originate from the active layer and appear to largely degrade within the scar zone of the RTS feature. Thermokarst on the Peel Plateau is likely to intensify in the future, but our data suggest that most of the permafrost OC released is not readily degradable within the stream system and thus may have little potential for atmospheric evasion. Possibilities for the recalcitrant OC to degrade over decadal to millennial time scales while being transported via larger river networks, and within the marine environment, do however, still exist. These findings add to our understanding of the vulnerable Arctic landscapes and how they may interact with the global climate.</p></article>", "keywords": ["pyrolysis-GCMS", "organic carbon", "Science", "carbon", "Q", "15. Life on land", "01 natural sciences", "Arctic", "13. Climate action", "Arctic; climate; carbon; lipid biomarkers; Peel Plateau; permafrost; pyrolysis-GCMS; degradation", "Peel Plateau", "SDG 13 - Climate Action", "lipid biomarkers", "14. Life underwater", "climate", "permafrost", "degradation", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.3389/feart.2021.642675"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Frontiers%20in%20Earth%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3389/feart.2021.642675", "name": "item", "description": "10.3389/feart.2021.642675", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3389/feart.2021.642675"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-03-29T00:00:00Z"}}, {"id": "10.3389/fpls.2018.01158", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:20:46Z", "type": "Journal Article", "created": "2018-08-08", "title": "Simulation of Soil Organic Carbon Effects on Long-Term Winter Wheat (Triticum aestivum) Production Under Varying Fertilizer Inputs", "description": "Soil organic carbon (SOC) has a vital role to enhance agricultural productivity and for mitigation of climate change. To quantify SOC effects on productivity, process models serve as a robust tool to keep track of multiple plant and soil factors and their interactions affecting SOC dynamics. We used soil-plant-atmospheric model viz. DAISY, to assess effects of SOC on nitrogen (N) supply and plant available water (PAW) under varying N fertilizer rates in winter wheat (Triticum aestivum) in Denmark. The study objective was assessment of SOC effects on winter wheat grain and aboveground biomass accumulation at three SOC levels (low: 0.7% SOC; reference: 1.3% SOC; and high: 2% SOC) with five nitrogen rates (0-200 kg N ha-1) and PAW at low, reference, and high SOC levels. The three SOC levels had significant effects on grain yields and aboveground biomass accumulation at only 0-100 kg N ha-1 and the SOC effects decreased with increasing N rates until no effects at 150-200 kg N ha-1. PAW had significant positive correlation with SOC content, with high SOC retaining higher PAW compared to low and reference SOC. The mean PAW and SOC correlation was given by PAW% = 1.0073 \u00d7 SOC% + 15.641. For the 0.7-2% SOC range, the PAW increase was small with no significant effects on grain yields and aboveground biomass accumulation. The higher winter wheat grain and aboveground biomass was attributed to higher N supply in N deficient wheat production system. Our study suggested that building SOC enhances agronomic productivity at only 0-100 kg N ha-1. Maintenance of SOC stock will require regular replenishment of SOC, to compensate for the mineralization process degrading SOC over time. Hence, management can maximize realization of SOC benefits by building up SOC and maintaining N rates in the range 0-100 kg N ha-1, to reduce the off-farm N losses depending on the environmental zones, land use and the production system.", "keywords": ["0301 basic medicine", "Crop productivity; DAISY model; Grain yield; Long-term experiment; Nitrogen; Pedotransfer functions; Plant available water;", "Nitrogen", "QH301 Biology", "DAISY model", "pedotransfer functions", "Plant Science", "nitrogen", "SB1-1110", "QH301", "03 medical and health sciences", "Long-term experiment", "SDG 13 - Climate Action", "Grain yield", "SDG 2 - Zero Hunger", "European Commission", "289694", "crop productivity", "SDG 15 - Life on Land", "2. Zero hunger", "020", "Pedotransfer functions", "0303 health sciences", "grain yield", "Plant culture", "15. Life on land", "plant available water", "13. Climate action", "Crop productivity", "Plant available water", "SMARTSOIL", "long-term experiment"]}, "links": [{"href": "https://flore.unifi.it/bitstream/2158/1138671/1/Ghaley%20et%20al%202018_Frontiers%20in%20Plant%20Science.pdf"}, {"href": "https://doi.org/10.3389/fpls.2018.01158"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Frontiers%20in%20Plant%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3389/fpls.2018.01158", "name": "item", "description": "10.3389/fpls.2018.01158", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3389/fpls.2018.01158"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-08-08T00:00:00Z"}}, {"id": "10.3390/rs13234893", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:21:04Z", "type": "Journal Article", "created": "2021-12-06", "title": "In Situ Observation-Constrained Global Surface Soil Moisture Using Random Forest Model", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>The inherent biases of different long-term gridded surface soil moisture (SSM) products, unconstrained by the in situ observations, implies different spatio-temporal patterns. In this study, the Random Forest (RF) model was trained to predict SSM from relevant land surface feature variables (i.e., land surface temperature, vegetation indices, soil texture, and geographical information) and precipitation, based on the in situ soil moisture data of the International Soil Moisture Network (ISMN.). The results of the RF model show an RMSE of 0.05 m3 m\u22123 and a correlation coefficient of 0.9. The calculated impurity-based feature importance indicates that the Antecedent Precipitation Index affects most of the predicted soil moisture. The geographical coordinates also significantly influence the prediction (i.e., RMSE was reduced to 0.03 m3 m\u22123 after considering geographical coordinates), followed by land surface temperature, vegetation indices, and soil texture. The spatio-temporal pattern of RF predicted SSM was compared with the European Space Agency Climate Change Initiative (ESA-CCI) soil moisture product, using both time-longitude and latitude diagrams. The results indicate that the RF SSM captures the spatial distribution and the daily, seasonal, and annual variabilities globally.</p></article>", "keywords": ["feature importance", "Science", "0207 environmental engineering", "02 engineering and technology", "01 natural sciences", "antecedent precipitation index", "SDG 13 - Climate Action", "Global scale", "Antecedent precipitation index; Feature importance; Global scale; In situ constrained; Random forest; Soil moisture", "soil moisture; random forest; global scale; in situ constrained; feature importance; antecedent precipitation index", "SDG 15 - Life on Land", "0105 earth and related environmental sciences", "Antecedent precipitation index", "Q", "In situ constrained", "15. Life on land", "Feature importance", "13. Climate action", "ITC-ISI-JOURNAL-ARTICLE", "global scale", "Soil moisture", "soil moisture", "ITC-GOLD", "in situ constrained", "random forest", "Random forest"]}, "links": [{"href": "http://www.mdpi.com/2072-4292/13/23/4893/pdf"}, {"href": "https://www.iris.unina.it/bitstream/11588/938135/1/2021_Ljie_Zeng_et_al_remotesensing.pdf"}, {"href": "https://www.mdpi.com/2072-4292/13/23/4893/pdf"}, {"href": "https://doi.org/10.3390/rs13234893"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Remote%20Sensing", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3390/rs13234893", "name": "item", "description": "10.3390/rs13234893", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3390/rs13234893"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-12-02T00:00:00Z"}}, {"id": "10.5194/bg-19-5125-2022", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:21:40Z", "type": "Journal Article", "created": "2022-11-10", "title": "Management-induced changes in soil organic carbon  on global croplands", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Abstract. Soil organic carbon (SOC), one of the largest terrestrial carbon (C) stocks on Earth, has been depleted by anthropogenic land cover change and agricultural management. However, the latter has so far not been well represented in global C stock assessments. While SOC models often simulate detailed biochemical processes that lead to the accumulation and decay of SOC, the management decisions driving these biophysical processes are still little investigated at the global scale. Here we develop a spatially explicit data set for agricultural management on cropland, considering crop production levels, residue returning rates, manure application, and the adoption of irrigation and tillage practices. We combine it with a reduced-complexity model based on the Intergovernmental Panel on Climate Change (IPCC) tier\u00a02 method to create a half-degree resolution data set of SOC stocks and SOC stock changes for the first 30\u2009cm of mineral soils. We estimate that, due to arable farming, soils have lost around 34.6\u2009GtC relative to a counterfactual hypothetical natural state in 1975. Within the period 1975\u20132010, this SOC debt continued to expand by 5\u2009GtC (0.14\u2009GtC\u2009yr\u22121) to around 39.6\u2009GtC. However, accounting for historical management led to 2.1\u2009GtC fewer (0.06\u2009GtC\u2009yr\u22121) emissions than under the assumption of constant management. We also find that management decisions have influenced the historical SOC trajectory most strongly by residue returning, indicating that SOC enhancement by biomass retention may be a promising negative emissions technique. The reduced-complexity SOC model may allow us to simulate management-induced SOC enhancement \u2013 also within computationally demanding integrated (land use) assessment modeling.                     </p></article>", "keywords": ["570", "AGRICULTURE", "550", "Supplementary Data", "QH301 Biology", "agricultural management", "crop production", "SEQUESTRATION", "551", "01 natural sciences", "630", "NITROGEN-CYCLE", "QH301", "Life", "land cover", "QH501-531", "SDG 13 - Climate Action", "soil carbon", "SDG 2 - Zero Hunger", "EMISSIONS", "CROPS", "QH540-549.5", "global change", "SDG 15 - Life on Land", "0105 earth and related environmental sciences", "2. Zero hunger", "QE1-996.5", "Ecology", "INTENSIFICATION", "VEGETATION MODEL", "Geology", "LAND-USE CHANGE", "15. Life on land", "carbon sequestration", "CLIMATE", "COVER CHANGE", "agricultural land", "13. Climate action", "trajectory", "Intergovernmental Panel on Climate Change"]}, "links": [{"href": "https://bg.copernicus.org/articles/19/5125/2022/bg-19-5125-2022.pdf"}, {"href": "https://doi.org/10.5194/bg-19-5125-2022"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biogeosciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.5194/bg-19-5125-2022", "name": "item", "description": "10.5194/bg-19-5125-2022", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5194/bg-19-5125-2022"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-12-22T00:00:00Z"}}, {"id": "20.500.11850/403804", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:25:13Z", "type": "Journal Article", "created": "2020-01-29", "title": "Particulate Organic Matter Dynamics in a Permafrost Headwater Stream and the Kolyma River Mainstem", "description": "Abstract<p>Ongoing rapid arctic warming leads to extensive permafrost thaw, which in turn increases the hydrologic connectivity of the landscape by opening up subsurface flow paths. Suspended particulate organic matter (POM) has proven useful to trace permafrost thaw signals in arctic rivers, which may experience higher organic matter loads in the future due to expansion and increasing intensity of thaw processes such as thermokarst and river bank erosion. Here we focus on the Kolyma River watershed in Northeast Siberia, the world's largest watershed entirely underlain by continuous permafrost. To evaluate and characterize the present\uffe2\uff80\uff90day fluvial release of POM from permafrost thaw, we collected water samples every 4\uffe2\uff80\uff937 days during the 4\uffe2\uff80\uff90month open water season in 2013 and 2015 from the lower Kolyma River mainstem and from a small nearby headwater stream (Y3) draining an area completely underlain by Yedoma permafrost (Pleistocene ice\uffe2\uff80\uff90 and organic\uffe2\uff80\uff90rich deposits). Concentrations of particulate organic carbon generally followed the hydrograph with the highest concentrations during the spring flood in late May/early June. For the Kolyma River, concentrations of dissolved organic carbon showed a similar behavior, in contrast to the headwater stream, where dissolved organic carbon values were generally higher and particulate organic carbon concentrations lower than for Kolyma. Carbon isotope analysis (\uffce\uffb413C, \uffce\uff9414C) suggested Kolyma\uffe2\uff80\uff90POM to stem from both contemporary and older permafrost sources, while Y3\uffe2\uff80\uff90POM was more strongly influenced by in\uffe2\uff80\uff90stream production and recent vegetation. Lipid biomarker concentrations (high\uffe2\uff80\uff90molecular\uffe2\uff80\uff90weight n\uffe2\uff80\uff90alkanoic acids and n\uffe2\uff80\uff90alkanes) did not display clear seasonal patterns, yet implied Y3\uffe2\uff80\uff90POM to be more degraded than Kolyma\uffe2\uff80\uff90POM.</p", "keywords": ["particulate organic carbon", "15. Life on land", "01 natural sciences", "6. Clean water", "particulate organic carbon; permafrost; Kolyma; carbon isotopes; lipid biomarkers; Arctic", "Kolyma", "Arctic", "carbon isotopes", "13. Climate action", "SDG 13 - Climate Action", "lipid biomarkers", "Research Articles", "permafrost", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2019JG005511"}, {"href": "https://doi.org/20.500.11850/403804"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Geophysical%20Research%3A%20Biogeosciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "20.500.11850/403804", "name": "item", "description": "20.500.11850/403804", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/20.500.11850/403804"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-02-01T00:00:00Z"}}, {"id": "10.5194/essd-10-405-2018", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:21:46Z", "type": "Journal Article", "created": "2018-03-12", "title": "Global Carbon Budget 2017", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Abstract. Accurate assessment of anthropogenic carbon dioxide (CO2) emissions and their redistribution among the atmosphere, ocean, and terrestrial biosphere \u2013 the global carbon budget \u2013 is important to better understand the global carbon cycle, support the development of climate policies, and project future climate change. Here we describe data sets and methodology to quantify the five major components of the global carbon budget and their uncertainties. CO2 emissions from fossil fuels and industry (EFF) are based on energy statistics and cement production data, respectively, while emissions from land-use change (ELUC), mainly deforestation, are based on land-cover change data and bookkeeping models. The global atmospheric CO2 concentration is measured directly and its rate of growth (GATM) is computed from the annual changes in concentration. The ocean CO2 sink (SOCEAN) and terrestrial CO2 sink (SLAND) are estimated with global process models constrained by observations. The resulting carbon budget imbalance (BIM), the difference between the estimated total emissions and the estimated changes in the atmosphere, ocean, and terrestrial biosphere, is a measure of imperfect data and understanding of the contemporary carbon cycle. All uncertainties are reported as \u00b11\u03c3. For the last decade available (2007\u20132016), EFF was 9.4\u202f\u00b1\u202f0.5\u202fGtC\u202fyr\u22121, ELUC 1.3\u202f\u00b1\u202f0.7\u202fGtC\u202fyr\u22121, GATM 4.7\u202f\u00b1\u202f0.1\u202fGtC\u202fyr\u22121, SOCEAN 2.4\u202f\u00b1\u202f0.5\u202fGtC\u202fyr\u22121, and SLAND 3.0\u202f\u00b1\u202f0.8\u202fGtC\u202fyr\u22121, with a budget imbalance BIM of 0.6\u202fGtC\u202fyr\u22121 indicating overestimated emissions and/or underestimated sinks. For year 2016 alone, the growth in EFF was approximately zero and emissions remained at 9.9\u202f\u00b1\u202f0.5\u202fGtC\u202fyr\u22121. Also for 2016, ELUC was 1.3\u202f\u00b1\u202f0.7\u202fGtC\u202fyr\u22121, GATM was 6.1\u202f\u00b1\u202f0.2\u202fGtC\u202fyr\u22121, SOCEAN was 2.6\u202f\u00b1\u202f0.5\u202fGtC\u202fyr\u22121, and SLAND was 2.7\u202f\u00b1\u202f1.0\u202fGtC\u202fyr\u22121, with a small BIM of \u22120.3\u202fGtC. GATM continued to be higher in 2016 compared to the past decade (2007\u20132016), reflecting in part the high fossil emissions and the small SLAND consistent with El Ni\u00f1o conditions. The global atmospheric CO2 concentration reached 402.8\u202f\u00b1\u202f0.1\u202fppm averaged over 2016. For 2017, preliminary data for the first 6\u20139\u00a0months indicate a renewed growth in EFF of +2.0\u202f% (range of 0.8 to 3.0\u202f%) based on national emissions projections for China, USA, and India, and projections of gross domestic product (GDP) corrected for recent changes in the carbon intensity of the economy for the rest of the world. This living data update documents changes in the methods and data sets used in this new global carbon budget compared with previous publications of this data set (Le Qu\u00e9r\u00e9 et al., 2016, 2015b, a, 2014, 2013). All results presented here can be downloaded from https://doi.org/10.18160/GCP-2017 (GCP, 2017).                     </p></article>", "keywords": ["ENVIRONMENT SIMULATOR JULES", "550", "530 Physics", "[PHYS.PHYS.PHYS-GEO-PH] Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]", "MIXED-LAYER SCHEME", "INTERNATIONAL-TRADE", "7. Clean energy", "01 natural sciences", "333", "12. Responsible consumption", "FOSSIL-FUEL COMBUSTION", "ANTHROPOGENIC CO2 UPTAKE", "11. Sustainability", "SDG 13 - Climate Action", "Life Science", "GE1-350", "SDG 14 - Life Below Water", "ATMOSPHERIC CO2", "DIOXIDE EMISSIONS", "SDG 15 - Life on Land", "0105 earth and related environmental sciences", "LAND-COVER CHANGE", "QE1-996.5", "info:eu-repo/classification/ddc/550", "EARTH SYSTEM MODEL", "ddc:550", "VEGETATION MODEL", "Geology", "15. Life on land", "Environmental sciences", "Earth sciences", "13. Climate action", "8. Economic growth", "General Earth and Planetary Sciences"]}, "links": [{"href": "https://ueaeprints.uea.ac.uk/id/eprint/66578/1/Published_manuscript.pdf"}, {"href": "http://oceanrep.geomar.de/42391/1/essd-10-405-2018.pdf"}, {"href": "https://boris.unibe.ch/116576/1/lequere18essd.pdf"}, {"href": "https://pure.iiasa.ac.at/id/eprint/15161/1/essd-10-405-2018.pdf"}, {"href": "http://pure.iiasa.ac.at/id/eprint/15161/1/essd-10-405-2018.pdf"}, {"href": "https://essd.copernicus.org/articles/10/405/2018/essd-10-405-2018.pdf"}, {"href": "https://doi.org/10.5194/essd-10-405-2018"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Earth%20System%20Science%20Data", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.5194/essd-10-405-2018", "name": "item", "description": "10.5194/essd-10-405-2018", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5194/essd-10-405-2018"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-03-12T00:00:00Z"}}, {"id": "10.5194/cp-13-1213-2017", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:21:42Z", "type": "Journal Article", "created": "2017-02-21", "title": "Sources and characteristics of terrestrial carbon in Holocene-scale sediments of the East Siberian Sea", "description": "<p>Abstract. Thawing of permafrost carbon (PF-C) due to climate warming can remobilise considerable amounts of terrestrial carbon from its long term storage to the marine environment. PF-C can be then buried in sediments or remineralised to CO2 with implications for the carbon-climate feedback. Studying historical sediment records during past natural climate changes can help to understand the response of permafrost to current climate warming. In this study two sediment cores collected from the East Siberian Sea were used to study terrestrial organic carbon sources, composition and degradation during the past ~\uffe2\uff80\uff899500\uffe2\uff80\uff89cal\uffe2\uff80\uff89yrs\uffe2\uff80\uff89BP. The CuO-derived lignin and cutin products combined with \uffce\uffb413C suggest that there was a higher input of terrestrial organic carbon to the East Siberian Sea between ~\uffe2\uff80\uff899500 and 8200\uffe2\uff80\uff89cal\uffe2\uff80\uff89yrs\uffe2\uff80\uff89BP than in all later periods. This high input was likely caused by marine transgression and permafrost destabilisation in the early Holocene climatic optimum. Based on source apportionment modelling using dual-carbon isotope (\uffe2\uff88\uff8614C, \uffce\uffb413C) data, coastal erosion releasing old Pleistocene permafrost carbon was identified as a significant source of organic matter translocated to the East Siberian Sea during the Holocene.                         </p>", "keywords": ["Environmental sciences", "TD172-193.5", "13. Climate action", "TD169-171.8", "SDG 13 - Climate Action", "GE1-350", "SDG 14 - Life Below Water", "14. Life underwater", "15. Life on land", "Environmental protection", "01 natural sciences", "Environmental pollution", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://cp.copernicus.org/articles/13/1213/2017/cp-13-1213-2017.pdf"}, {"href": "https://doi.org/10.5194/cp-13-1213-2017"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Climate%20of%20the%20Past", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.5194/cp-13-1213-2017", "name": "item", "description": "10.5194/cp-13-1213-2017", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5194/cp-13-1213-2017"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-02-21T00:00:00Z"}}, {"id": "10.5194/cp-2017-20", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:21:42Z", "type": "Journal Article", "created": "2017-02-21", "title": "Sources and characteristics of terrestrial carbon in Holocene-scale sediments of the East Siberian Sea", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Abstract. Thawing of permafrost carbon (PF-C) due to climate warming can remobilise considerable amounts of terrestrial carbon from its long term storage to the marine environment. PF-C can be then buried in sediments or remineralised to CO2 with implications for the carbon-climate feedback. Studying historical sediment records during past natural climate changes can help to understand the response of permafrost to current climate warming. In this study two sediment cores collected from the East Siberian Sea were used to study terrestrial organic carbon sources, composition and degradation during the past ~\u20099500\u2009cal\u2009yrs\u2009BP. The CuO-derived lignin and cutin products combined with \u03b413C suggest that there was a higher input of terrestrial organic carbon to the East Siberian Sea between ~\u20099500 and 8200\u2009cal\u2009yrs\u2009BP than in all later periods. This high input was likely caused by marine transgression and permafrost destabilisation in the early Holocene climatic optimum. Based on source apportionment modelling using dual-carbon isotope (\u220614C, \u03b413C) data, coastal erosion releasing old Pleistocene permafrost carbon was identified as a significant source of organic matter translocated to the East Siberian Sea during the Holocene.                         </p></article>", "keywords": ["Environmental sciences", "TD172-193.5", "13. Climate action", "TD169-171.8", "SDG 13 - Climate Action", "GE1-350", "SDG 14 - Life Below Water", "14. Life underwater", "15. Life on land", "Environmental protection", "01 natural sciences", "Environmental pollution", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://cp.copernicus.org/articles/13/1213/2017/cp-13-1213-2017.pdf"}, {"href": "https://doi.org/10.5194/cp-2017-20"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Climate%20of%20the%20Past", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.5194/cp-2017-20", "name": "item", "description": "10.5194/cp-2017-20", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5194/cp-2017-20"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-02-21T00:00:00Z"}}, {"id": "10.5194/egusphere-egu22-5811", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:21:45Z", "type": "Journal Article", "created": "2022-03-27", "title": "Agricultural management affects active carbon and nitrogen mineralisation potential in soils", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>&amp;lt;p&amp;gt;Soil organic matter (SOM) is important for soil fertility and climate change mitigation. Agricultural management - including soil amendments - can improve soil fertility and contribute to climate change mitigation by stabilising carbon in soils. This calls for cost-effective parameters to assess&amp;amp;#160; the influence of management practices on SOM. The current study aimed at understanding how sensitive the parameters active/permanganate oxidisable carbon (AC) and nitrogen mineralisation potential (NMP) react to different agricultural management practices compared to total organic carbon (TOC) and total nitrogen (Nt). We aimed to gain a better understanding of SOM processes, mainly regarding depth distribution and seasonality of SOM dynamics using AC and NMP.&amp;lt;/p&amp;gt;&amp;lt;p&amp;gt;Data were obtained in five Austrian long-term field experiments (LTEs) testing four management practices: i) tillage, ii) compost application, iii) crop residue management, and iv) mineral fertilisation.&amp;lt;/p&amp;gt;&amp;lt;p&amp;gt;AC was specifically sensitive in detecting the effect of tillage treatment at different soil depths. NMP differentiated between all different tillage treatments in the top soil layer, it showed the temporal dynamics between the years in the compost LTE, and it was identified as an early detection property in the crop residue LTE. Both AC and NMP detected short-term fluctuations better than TOC and Nt over the course of two years in the crop residue LTE. Thus, we suggest that AC and NMP are two valuable soil biochemical parameters providing more detailed information on C and N dynamics regarding depth distribution and seasonal dynamics and react more sensitively to different agricultural management practices compared to TOC and Nt. They should be integrated in monitoring agricultural LTEs and in field analyses conducted by farmers. However, when evaluating results of long-term carbon storage, their sensitivity towards annual fluctuations should be taken into account.&amp;lt;/p&amp;gt;</p></article>", "keywords": ["DYNAMICS", "agricultural long-term experiments", "N-MINERALIZATION", "climate change mitigation", "", "agricultural long-term experiments", "", "climate change mitigation", "ORGANIC-CARBON", "soil organic matter", "SDG 13 - Climate Action", "ENZYME-ACTIVITIES", "SDG 2 \u2013 Kein Hunger", "106026 Ecosystem research", "SDG 2 - Zero Hunger", "early parameters of change", "TILLAGE", "2. Zero hunger", "106022 Mikrobiologie", "MICROBIAL BIOMASS", "CROP", "04 agricultural and veterinary sciences", "15. Life on land", "PERMANGANATE-OXIDIZABLE CARBON", "6. Clean water", "106026 \u00d6kosystemforschung", "13. Climate action", "SDG 13 \u2013 Ma\u00dfnahmen zum Klimaschutz", "106022 Microbiology", "0401 agriculture", " forestry", " and fisheries", "RESIDUE MANAGEMENT", "FRACTIONS"]}, "links": [{"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1002/jpln.202100130"}, {"href": "https://doi.org/10.5194/egusphere-egu22-5811"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Plant%20Nutrition%20and%20Soil%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.5194/egusphere-egu22-5811", "name": "item", "description": "10.5194/egusphere-egu22-5811", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5194/egusphere-egu22-5811"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-03-27T00:00:00Z"}}, {"id": "10.5194/essd-2021-358", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:21:47Z", "type": "Journal Article", "created": "2021-10-28", "title": "The MONARCH high-resolution reanalysis of desert dust aerosol over Northern Africa, the Middle East and Europe (2007\u20132016)", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Abstract. One of the challenges in studying desert dust aerosol along with its numerous interactions and impacts is the paucity of direct in-situ measurements, particularly in the areas most affected by dust storms. Satellites typically provide columnintegrated aerosol measurements, but observationally-constrained continuous 3D dust fields are needed to assess dust variability, climate effects and impacts upon a variety of socio-economic sectors. Here, we present a high resolution regional reanalysis data set of desert dust aerosols that covers Northern Africa, the Middle East and Europe along with the Mediterranean sea and parts of Central Asia, and the Atlantic and Indian Oceans between 2007 and 2016. The horizontal resolution is 0.1\u00b0 latitude\u2009\u00d7\u20090.1\u00b0 longitude, and the temporal resolution is 3 hours. The reanalysis was produced using Local Ensemble Transform Kalman Filter (LETKF) data assimilation in the Multiscale Online Non-hydrostatic AtmospheRe CHemistry model (MONARCH) developed at the Barcelona Supercomputing Center (BSC). The assimilated data are coarse-mode dust optical depth retrieved from the Moderate Resolution Imaging Spectroradiometer (MODIS) Deep Blue Level 2 products. The reanalysis data set consists of upper air (dust mass concentrations and extinction coefficient), surface (dust deposition and solar irradiance fields, among them) and total column (e.g., dust optical depth and load) variables. Some dust variables, such as concentrations and wet and dry deposition, are expressed for a binned size distribution that ranges from 0.2 to 20\u2009\u03bcm in particle diameter. Both analysis and first-guess (analysis-initialized simulation) fields are available for the variables that are diagnosed from the state vector. A set of ensemble statistics is archived for each output variable, namely the ensemble mean, standard deviation, maximum and median. The spatial and temporal distribution of the dust fields follows well-known dust cycle features controlled by seasonal changes in meteorology and vegetation cover. The analysis is statistically closer to the assimilated retrievals than the first-guess, which proves the consistency of the data assimilation method. Independent evaluation using AERONET dust-filtered optical depth retrievals indicates that the reanalysis data set is highly accurate (mean bias\u2009=\u2009\u22120.05, RMSE\u2009=\u20090.12, r\u2009=\u20090.81 when compared to retrievals from the spectral de-convolution algorithm on a 3-hourly basis). Verification statistics are broadly homogeneous in space and time with regional differences that can be partly attributed to model limitations (e.g., poor representation of small-scale emission processes), presence of aerosols other than dust in the observations used in the evaluation, and differences in the number of observations among seasons. Such a reliable high-resolution historical record of atmospheric desert dust will allow a better quantification of dust impacts upon key sectors of society and economy, including health, solar energy production and transportation. The reanalysis data set (Di Tomaso et al., 2021) is distributed via a Thematic Real-time Environmental Distributed Data Service (THREDDS) at BSC and freely available at http://hdl.handle.net/21.12146/c6d4a608-5de3-47f6-a004-67cb1d498d98.                         </p></article>", "keywords": ["Desert dust aerosol", "550", "Climate", "MINERAL-COMPOSITION", "Aerosols atmosf\u00e8rics", "01 natural sciences", "Dust emission", "[SDU] Sciences of the Universe [physics]", "LETKF", "Local ensemble transform Kalman filter", "DATA ASSIMILATION", "\u00c0rees tem\u00e0tiques de la UPC::Enginyeria agroaliment\u00e0ria::Ci\u00e8ncies de la terra i de la vida::Climatologia i meteorologia", "Pols -- Control", "SDG 3 - Good Health and Well-being", "MONARCH", "SAHARAN DUST", "SDG 13 - Climate Action", "SIZE DISTRIBUTION", "GE1-350", "Desert", "CONVECTIVE ADJUSTMENT SCHEME", "Aerosol measurements", "Multiscale Online Nonhydrostatic AtmospheRe CHemistry model", "0105 earth and related environmental sciences", "QE1-996.5", "info:eu-repo/classification/ddc/550", ":Enginyeria agroaliment\u00e0ria::Ci\u00e8ncies de la terra i de la vida::Climatologia i meteorologia [\u00c0rees tem\u00e0tiques de la UPC]", "ddc:550", "Geology", "1 MODEL DESCRIPTION", "OPTICAL-PROPERTIES", "MONARCH modeling system", "Atmospheric aerosols", "Environmental sciences", "Earth sciences", "PM10 CONCENTRATIONS", "900", "Dust aerosol", "13. Climate action", "[SDU.STU] Sciences of the Universe [physics]/Earth Sciences", "SINGLE-SCATTERING ALBEDO", "MEDITERRANEAN BASIN", "Dust control"]}, "links": [{"href": "https://iris.cnr.it/bitstream/20.500.14243/417480/1/prod_471097-doc_191235.pdf"}, {"href": "https://essd.copernicus.org/articles/14/2785/2022/essd-14-2785-2022.pdf"}, {"href": "https://doi.org/10.5194/essd-2021-358"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Earth%20System%20Science%20Data", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.5194/essd-2021-358", "name": "item", "description": "10.5194/essd-2021-358", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5194/essd-2021-358"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-10-28T00:00:00Z"}}, {"id": "10.5194/gmd-10-1945-2017", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:21:48Z", "type": "Journal Article", "created": "2017-05-17", "title": "A non-linear Granger-causality framework to investigate climate\u2013vegetation dynamics", "description": "<p>Abstract. Satellite Earth observation has led to the creation of global climate data records of many important environmental and climatic variables. These come in the form of multivariate time series with different spatial and temporal resolutions. Data of this kind provide new means to further unravel the influence of climate on vegetation dynamics. However, as advocated in this article, commonly used statistical methods are often too simplistic to represent complex climate\uffe2\uff80\uff93vegetation relationships due to linearity assumptions. Therefore, as an extension of linear Granger-causality analysis, we present a novel non-linear framework consisting of several components, such as data collection from various databases, time series decomposition techniques, feature construction methods, and predictive modelling by means of random forests. Experimental results on global data sets indicate that, with this framework, it is possible to detect non-linear patterns that are much less visible with traditional Granger-causality methods. In addition, we discuss extensive experimental results that highlight the importance of considering non-linear aspects of climate\uffe2\uff80\uff93vegetation dynamics.                     </p>", "keywords": ["QE1-996.5", "0207 environmental engineering", "TIME-SERIES", "Geology", "02 engineering and technology", "15. Life on land", "SOIL-MOISTURE", "SAMPLE TESTS", "SURFACE-TEMPERATURE", "01 natural sciences", "RANDOM FORESTS", "CARBON-DIOXIDE", "NDVI DATA", "13. Climate action", "Earth and Environmental Sciences", "PRECIPITATION", "GLOBAL TERRESTRIAL ECOSYSTEMS", "SDG 13 - Climate Action", "SATELLITE", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://gmd.copernicus.org/articles/10/1945/2017/gmd-10-1945-2017.pdf"}, {"href": "https://doi.org/10.5194/gmd-10-1945-2017"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Geoscientific%20Model%20Development", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.5194/gmd-10-1945-2017", "name": "item", "description": "10.5194/gmd-10-1945-2017", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5194/gmd-10-1945-2017"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-05-17T00:00:00Z"}}, {"id": "10.5194/gmd-11-937-2018", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:21:48Z", "type": "Journal Article", "created": "2018-03-15", "title": "ORCHIDEE-SOM: modeling soil organic carbon (SOC) and dissolved organic carbon (DOC) dynamics along vertical soil profiles in Europe", "description": "<p>Abstract. Current land surface models (LSMs) typically represent soils in a\uffc2\uffa0very simplistic way, assuming soil organic carbon (SOC) as a\uffc2\uffa0bulk, and thus impeding a\uffc2\uffa0correct representation of deep soil carbon dynamics. Moreover, LSMs generally neglect the production and export of dissolved organic carbon (DOC) from soils to rivers, leading to overestimations of the potential carbon sequestration on land. This common oversimplified processing of SOC in LSMs is partly responsible for the large uncertainty in the predictions of the soil carbon response to climate change. In this study, we present a\uffc2\uffa0new soil carbon module called ORCHIDEE-SOM, embedded within the land surface model ORCHIDEE, which is able to reproduce the DOC and SOC dynamics in a\uffc2\uffa0vertically discretized soil to 2\uffe2\uff80\uffafm. The model includes processes of biological production and consumption of SOC and DOC, DOC adsorption on and desorption from soil minerals, diffusion of SOC and DOC, and DOC transport with water through and out of the soils to rivers. We evaluated ORCHIDEE-SOM against observations of DOC concentrations and SOC stocks from four European sites with different vegetation covers: a\uffc2\uffa0coniferous forest, a\uffc2\uffa0deciduous forest, a\uffc2\uffa0grassland, and a\uffc2\uffa0cropland. The model was able to reproduce the SOC stocks along their vertical profiles at the four sites and the DOC concentrations within the range of measurements, with the exception of the DOC concentrations in the upper soil horizon at the coniferous forest. However, the model was not able to fully capture the temporal dynamics of DOC concentrations. Further model improvements should focus on a\uffc2\uffa0plant- and depth-dependent parameterization of the new input model parameters, such as the turnover times of DOC and the microbial carbon use efficiency. We suggest that this new soil module, when parameterized for global simulations, will improve the representation of the global carbon cycle in LSMs, thus helping to constrain the predictions of the future SOC response to global warming.                     </p>", "keywords": ["550", "/dk/atira/pure/core/keywords/nachhaltigkeitswissenschaft; name=Sustainability Science", "Climate", "/dk/atira/pure/discipline/B000/B006/B410-bodembeheer", "01 natural sciences", "/dk/atira/pure/thematic/inbo_th_00043", "/dk/atira/pure/thematic/inbo_th_00022", "SDG 13 - Climate Action", "/dk/atira/pure/sustainabledevelopmentgoals/climate_action; name=SDG 13 - Climate Action", "/dk/atira/pure/subjectarea/asjc/2600/2611; name=Modelling and Simulation", "0105 earth and related environmental sciences", "2. Zero hunger", "[SDU.OCEAN]Sciences of the Universe [physics]/Ocean", "Woods and parks", "QE1-996.5", "Atmosphere", "[SDU.OCEAN] Sciences of the Universe [physics]/Ocean", " Atmosphere", "Physics", "/dk/atira/pure/sustainabledevelopmentgoals/life_on_land; name=SDG 15 - Life on Land", "Geology", "Geokemi", "04 agricultural and veterinary sciences", "15. Life on land", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "Sciences de la terre et du cosmos", "Geochemistry", "/dk/atira/pure/subjectarea/asjc/1900; name=Earth and Planetary Sciences(all)", "13. Climate action", "8. Economic growth", "0401 agriculture", " forestry", " and fisheries", "[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces", "environment", "B410-soil-science"]}, "links": [{"href": "https://gmd.copernicus.org/articles/11/937/2018/gmd-11-937-2018.pdf"}, {"href": "https://dipot.ulb.ac.be/dspace/bitstream/2013/282703/1/doi_266330.pdf"}, {"href": "https://doi.org/10.5194/gmd-11-937-2018"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Geoscientific%20Model%20Development", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.5194/gmd-11-937-2018", "name": "item", "description": "10.5194/gmd-11-937-2018", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5194/gmd-11-937-2018"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-11-16T00:00:00Z"}}, {"id": "10.5194/gmd-13-805-2020", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:21:49Z", "type": "Journal Article", "created": "2020-03-02", "title": "Development and testing scenarios for implementing  land use and land cover changes during the Holocene  in Earth system model experiments", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Abstract. Anthropogenic changes in land use and land cover\u00a0(LULC) during the pre-industrial Holocene could have affected regional and global climate. Existing scenarios of LULC changes during the Holocene are based on relatively simple assumptions and highly uncertain estimates of population changes through time. Archaeological and palaeoenvironmental reconstructions have the potential to refine these assumptions and estimates. The Past Global Changes\u00a0(PAGES) LandCover6k initiative is working towards improved reconstructions of LULC globally. In this paper, we document the types of archaeological data that are being collated and how they will be used to improve LULC reconstructions. Given the large methodological uncertainties involved, both in reconstructing LULC from the archaeological data and in implementing these reconstructions into global scenarios of LULC, we propose a protocol to evaluate the revised scenarios using independent pollen-based reconstructions of land cover and climate. Further evaluation of the revised scenarios involves carbon cycle model simulations to determine whether the LULC reconstructions are consistent with constraints provided by ice core records of CO2 evolution and modern-day LULC. Finally, the protocol outlines how the improved LULC reconstructions will be used in palaeoclimate simulations in the Palaeoclimate Modelling Intercomparison Project to quantify the magnitude of anthropogenic impacts on climate through time and ultimately to improve the realism of Holocene climate simulations.                     </p></article>", "keywords": ["[SDU.OCEAN]Sciences of the Universe [physics]/Ocean", "QE1-996.5", "550", "Atmosphere", "[SDU.OCEAN] Sciences of the Universe [physics]/Ocean", " Atmosphere", "Geology", "Arqueologia", "15. Life on land", "ddc:910", "01 natural sciences", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "S\u00f2l", " \u00das del", "13. Climate action", "SDG 13 - Climate Action", "[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces", "environment", "SDG 15 - Life on Land", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://eprints.gla.ac.uk/210927/1/210927.pdf"}, {"href": "https://eprints.bournemouth.ac.uk/33591/1/gmd-13-805-2020.pdf"}, {"href": "https://gmd.copernicus.org/articles/13/805/2020/gmd-13-805-2020.pdf"}, {"href": "https://doi.org/10.5194/gmd-13-805-2020"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Geoscientific%20Model%20Development", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.5194/gmd-13-805-2020", "name": "item", "description": "10.5194/gmd-13-805-2020", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5194/gmd-13-805-2020"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-03-02T00:00:00Z"}}, {"id": "10.5194/gmd-18-3265-2025", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:21:49Z", "type": "Journal Article", "created": "2025-06-03", "title": "HTAP3 Fires: towards a multi-model,   multi-pollutant study of fire impacts", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Abstract. Open biomass burning has major impacts globally and regionally on atmospheric composition. Fire emissions include particulate matter, tropospheric ozone precursors, and greenhouse gases, as well as persistent organic pollutants, mercury, and other metals. Fire frequency, intensity, duration, and location are changing as the climate warms, and modelling these fires and their impacts is becoming more and more critical to inform climate adaptation and mitigation, as well as land management. Indeed, the air pollution from fires can reverse the progress made by emission controls on industry and transportation. At the same time, nearly all aspects of fire modelling \u2013 such as emissions, plume injection height, long-range transport, and plume chemistry \u2013 are highly uncertain. This paper outlines a multi-model, multi-pollutant, multi-regional study to improve the understanding of the uncertainties and variability in fire atmospheric science, models, and fires' impacts, in addition to providing quantitative estimates of the air pollution and radiative impacts of biomass burning. Coordinated under the auspices of the Task Force on Hemispheric Transport of Air Pollution, the international atmospheric modelling and fire science communities are working towards the common goal of improving global fire modelling and using this multi-model experiment to provide estimates of fire pollution for impact studies. This paper outlines the research needs, opportunities, and options for the fire-focused multi-model experiments and provides guidance for these modelling experiments, outputs, and analyses that are to be pursued over the next 3\u00a0to 5\u00a0years. The paper proposes a plan for delivering specific products at key points over this period to meet important milestones relevant to science and policy audiences.                     </p></article>", "keywords": ["QE1-996.5", "\u00c0rees tem\u00e0tiques de la UPC::Desenvolupament hum\u00e0 i sostenible::Degradaci\u00f3 ambiental::Canvi clim\u00e0tic", "Atmospheric composition", "Air pollution", "Geology", "Sediment transport", "Southeast atlantic", "15. Life on land", "Tropospheric ozone", "7. Clean energy", "Fires", "Reactive nitrogen", "Impact studies", "Surface ozone", "13. Climate action", "Air-quality", "11. Sustainability", "Open biomass burning", "SDG 13 - Climate Action", "\u00c0rees tem\u00e0tiques de la UPC::Enginyeria qu\u00edmica::Qu\u00edmica del medi ambient::Qu\u00edmica atmosf\u00e8rica", "Biomass-burning aerosol", "Wild-land fires", "\u00c0rees tem\u00e0tiques de la UPC::Desenvolupament hum\u00e0 i sostenible::Degradaci\u00f3 ambiental::Contaminaci\u00f3 atmosf\u00e8rica", "Particulate matter", "Health impacts"]}, "links": [{"href": "https://doi.org/10.5194/gmd-18-3265-2025"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Geoscientific%20Model%20Development", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.5194/gmd-18-3265-2025", "name": "item", "description": "10.5194/gmd-18-3265-2025", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5194/gmd-18-3265-2025"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-08-28T00:00:00Z"}}, {"id": "10.5281/zenodo.13791160", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:22:20Z", "type": "Journal Article", "created": "2022-03-27", "title": "Agricultural management affects active carbon and nitrogen mineralisation potential in soils", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>&amp;lt;p&amp;gt;Soil organic matter (SOM) is important for soil fertility and climate change mitigation. Agricultural management - including soil amendments - can improve soil fertility and contribute to climate change mitigation by stabilising carbon in soils. This calls for cost-effective parameters to assess&amp;amp;#160; the influence of management practices on SOM. The current study aimed at understanding how sensitive the parameters active/permanganate oxidisable carbon (AC) and nitrogen mineralisation potential (NMP) react to different agricultural management practices compared to total organic carbon (TOC) and total nitrogen (Nt). We aimed to gain a better understanding of SOM processes, mainly regarding depth distribution and seasonality of SOM dynamics using AC and NMP.&amp;lt;/p&amp;gt;&amp;lt;p&amp;gt;Data were obtained in five Austrian long-term field experiments (LTEs) testing four management practices: i) tillage, ii) compost application, iii) crop residue management, and iv) mineral fertilisation.&amp;lt;/p&amp;gt;&amp;lt;p&amp;gt;AC was specifically sensitive in detecting the effect of tillage treatment at different soil depths. NMP differentiated between all different tillage treatments in the top soil layer, it showed the temporal dynamics between the years in the compost LTE, and it was identified as an early detection property in the crop residue LTE. Both AC and NMP detected short-term fluctuations better than TOC and Nt over the course of two years in the crop residue LTE. Thus, we suggest that AC and NMP are two valuable soil biochemical parameters providing more detailed information on C and N dynamics regarding depth distribution and seasonal dynamics and react more sensitively to different agricultural management practices compared to TOC and Nt. They should be integrated in monitoring agricultural LTEs and in field analyses conducted by farmers. However, when evaluating results of long-term carbon storage, their sensitivity towards annual fluctuations should be taken into account.&amp;lt;/p&amp;gt;</p></article>", "keywords": ["DYNAMICS", "agricultural long-term experiments", "N-MINERALIZATION", "climate change mitigation", "", "agricultural long-term experiments", "", "climate change mitigation", "ORGANIC-CARBON", "soil organic matter", "SDG 13 - Climate Action", "ENZYME-ACTIVITIES", "SDG 2 \u2013 Kein Hunger", "106026 Ecosystem research", "SDG 2 - Zero Hunger", "early parameters of change", "TILLAGE", "2. Zero hunger", "106022 Mikrobiologie", "MICROBIAL BIOMASS", "CROP", "04 agricultural and veterinary sciences", "15. Life on land", "PERMANGANATE-OXIDIZABLE CARBON", "6. Clean water", "106026 \u00d6kosystemforschung", "13. Climate action", "SDG 13 \u2013 Ma\u00dfnahmen zum Klimaschutz", "106022 Microbiology", "0401 agriculture", " forestry", " and fisheries", "RESIDUE MANAGEMENT", "FRACTIONS"]}, "links": [{"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1002/jpln.202100130"}, {"href": "https://doi.org/10.5281/zenodo.13791160"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Plant%20Nutrition%20and%20Soil%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.5281/zenodo.13791160", "name": "item", "description": "10.5281/zenodo.13791160", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5281/zenodo.13791160"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-03-27T00:00:00Z"}}, {"id": "2164/20152", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:25:26Z", "type": "Journal Article", "created": "2022-11-10", "title": "Management-induced changes in soil organic carbon  on global croplands", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Abstract. Soil organic carbon (SOC), one of the largest terrestrial carbon (C) stocks on Earth, has been depleted by anthropogenic land cover change and agricultural management. However, the latter has so far not been well represented in global C stock assessments. While SOC models often simulate detailed biochemical processes that lead to the accumulation and decay of SOC, the management decisions driving these biophysical processes are still little investigated at the global scale. Here we develop a spatially explicit data set for agricultural management on cropland, considering crop production levels, residue returning rates, manure application, and the adoption of irrigation and tillage practices. We combine it with a reduced-complexity model based on the Intergovernmental Panel on Climate Change (IPCC) tier\u00a02 method to create a half-degree resolution data set of SOC stocks and SOC stock changes for the first 30\u2009cm of mineral soils. We estimate that, due to arable farming, soils have lost around 34.6\u2009GtC relative to a counterfactual hypothetical natural state in 1975. Within the period 1975\u20132010, this SOC debt continued to expand by 5\u2009GtC (0.14\u2009GtC\u2009yr\u22121) to around 39.6\u2009GtC. However, accounting for historical management led to 2.1\u2009GtC fewer (0.06\u2009GtC\u2009yr\u22121) emissions than under the assumption of constant management. We also find that management decisions have influenced the historical SOC trajectory most strongly by residue returning, indicating that SOC enhancement by biomass retention may be a promising negative emissions technique. The reduced-complexity SOC model may allow us to simulate management-induced SOC enhancement \u2013 also within computationally demanding integrated (land use) assessment modeling.</p></article>", "keywords": ["570", "AGRICULTURE", "550", "Supplementary Data", "QH301 Biology", "agricultural management", "crop production", "SEQUESTRATION", "551", "01 natural sciences", "630", "NITROGEN-CYCLE", "QH301", "Life", "land cover", "QH501-531", "SDG 13 - Climate Action", "soil carbon", "SDG 2 - Zero Hunger", "EMISSIONS", "CROPS", "QH540-549.5", "global change", "SDG 15 - Life on Land", "0105 earth and related environmental sciences", "2. Zero hunger", "QE1-996.5", "Ecology", "INTENSIFICATION", "VEGETATION MODEL", "Geology", "LAND-USE CHANGE", "15. Life on land", "carbon sequestration", "CLIMATE", "COVER CHANGE", "agricultural land", "13. Climate action", "trajectory", "Intergovernmental Panel on Climate Change"]}, "links": [{"href": "https://bg.copernicus.org/articles/19/5125/2022/bg-19-5125-2022.pdf"}, {"href": "https://doi.org/2164/20152"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biogeosciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "2164/20152", "name": "item", "description": "2164/20152", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2164/20152"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-12-22T00:00:00Z"}}, {"id": "10.5281/zenodo.14790778", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:22:39Z", "type": "Journal Article", "created": "2019-04-01", "title": "Coupled carbon and nitrogen losses in response to seven years of chronic warming in subarctic soils", "description": "Increasing temperatures may alter the stoichiometric demands of soil microbes and impair their capacity to stabilize carbon (C) and retain nitrogen (N), with critical consequences for the soil C and N storage at high latitude soils. Geothermally active areas in Iceland provided wide, continuous and stable gradients of\u00a0soil temperatures\u00a0to test this hypothesis. In order to characterize the stoichiometric demands of microbes from these subarctic soils, we incubated soils from ambient temperatures after the factorial addition of C, N and P substrates separately and in combination. In a second experiment, soils that had been exposed to different\u00a0in situ\u00a0warming intensities (+0, +0.5, +1.8, +3.4, +8.7, +15.9\u00a0\u00b0C above ambient) for seven years were incubated after the combined addition of C, N and P to evaluate the capacity of soil microbes to store and immobilize C and N at the different warming scenarios. The seven years of chronic soil warming triggered large and proportional soil C and N losses (4.1\u00a0\u00b1\u00a00.5% \u00b0C\u22121\u00a0of the stocks in unwarmed soils) from the upper 10\u202fcm of soil, with a predominant depletion of the physically accessible organic substrates that were weakly sorbed in\u00a0soil minerals\u00a0up to 8.7\u202f\u00b0C warming. Soil microbes met the increasing respiratory demands under conditions of low C accessibility at the expenses of a reduction of the standing biomass in warmer soils. This together with the strict microbial C:N stoichiometric demands also constrained their capacity of N retention, and increased the vulnerability of soil to N losses. Our findings suggest a strong control of\u00a0microbial physiology and C:N stoichiometric needs on the retention of soil N and on the resilience of soil C stocks from high-latitudes to warming, particularly during periods of vegetation dormancy and low C inputs.", "keywords": ["0301 basic medicine", "Microbial carbon and nutrients limitation", "Microbial biomass", "TERM", "03 medical and health sciences", "Temperature increase", "FOREST SOIL", "Substrate induced respiration", "ORGANIC-CARBON", "SDG 13 - Climate Action", "TEMPERATURE SENSITIVITY", "CYCLE", "106026 Ecosystem research", "METAANALYSIS", "2. Zero hunger", "106022 Mikrobiologie", "0303 health sciences", "Nitrogen loss", "CLIMATE-CHANGE", "AVAILABILITY", "15. Life on land", "106026 \u00d6kosystemforschung", "13. Climate action", "SDG 13 \u2013 Ma\u00dfnahmen zum Klimaschutz", "Nitrogen immobilization", "FEEDBACKS", "106022 Microbiology", "PLANT BIOMASS"]}, "links": [{"href": "https://doi.org/10.5281/zenodo.14790778"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20Biology%20and%20Biochemistry", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.5281/zenodo.14790778", "name": "item", "description": "10.5281/zenodo.14790778", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5281/zenodo.14790778"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-07-01T00:00:00Z"}}], "links": [{"rel": "self", "type": "application/geo+json", "title": "This document as GeoJSON", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=SDG+13+-+Climate+Action&offset=50&f=json", "hreflang": "en-US"}, {"rel": "alternate", "type": "text/html", "title": "This document as HTML", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=SDG+13+-+Climate+Action&offset=50&f=html", "hreflang": "en-US"}, {"rel": "collection", "type": "application/json", "title": "Collection URL", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main", "hreflang": "en-US"}, {"type": "application/geo+json", "rel": "prev", "title": "items (prev)", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=SDG+13+-+Climate+Action&offset=0", "hreflang": "en-US"}, {"rel": "next", "type": "application/geo+json", "title": "items (next)", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=SDG+13+-+Climate+Action&offset=100", "hreflang": "en-US"}], "numberMatched": 158, "numberReturned": 50, "distributedFeatures": [], "timeStamp": "2026-05-02T08:18:42.655429Z"}