{"type": "FeatureCollection", "features": [{"id": "10.1002/2015wr018233", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:14:49Z", "type": "Journal Article", "created": "2016-04-20", "title": "Modeling soil evaporation efficiency in a range of soil and atmospheric conditions using a meta\u2010analysis approach", "description": "Abstract<p>A meta\uffe2\uff80\uff90analysis data\uffe2\uff80\uff90driven approach is developed to represent the soil evaporative efficiency (SEE) defined as the ratio of actual to potential soil evaporation. The new model is tested across a bare soil database composed of more than 30 sites around the world, a clay fraction range of 0.02\uffe2\uff80\uff930.56, a sand fraction range of 0.05\uffe2\uff80\uff930.92, and about 30,000 acquisition times. SEE is modeled using a soil resistance (rss) formulation based on surface soil moisture (\uffce\uffb8) and two resistance parameters   and \uffce\uffb8efolding. The data\uffe2\uff80\uff90driven approach aims to express both parameters as a function of observable data including meteorological forcing, cut\uffe2\uff80\uff90off soil moisture value   at which SEE=0.5, and first derivative of SEE at  , named  . An analytical relationship between   and   is first built by running a soil energy balance model for two extreme conditions with rss\uffe2\uff80\uff89=\uffe2\uff80\uff890 and   using meteorological forcing solely, and by approaching the middle point from the two (wet and dry) reference points. Two different methods are then investigated to estimate the pair   either from the time series of SEE and \uffce\uffb8 observations for a given site, or using the soil texture information for all sites. The first method is based on an algorithm specifically designed to accomodate for strongly nonlinear   relationships and potentially large random deviations of observed SEE from the mean observed  . The second method parameterizes   as a multi\uffe2\uff80\uff90linear regression of clay and sand percentages, and sets   to a constant mean value for all sites. The new model significantly outperformed the evaporation modules of ISBA (Interaction Sol\uffe2\uff80\uff90Biosph\uffc3\uffa8re\uffe2\uff80\uff90Atmosph\uffc3\uffa8re), H\uffe2\uff80\uff90TESSEL (Hydrology\uffe2\uff80\uff90Tiled ECMWF Scheme for Surface Exchange over Land), and CLM (Community Land Model). It has potential for integration in various land\uffe2\uff80\uff90surface schemes, and real calibration capabilities using combined thermal and microwave remote sensing data.</p", "keywords": ["550", "0207 environmental engineering", "modeling", "02 engineering and technology", "15. Life on land", "551", "01 natural sciences", "evaporation", "soil", "moisture", "[SDU.STU.HY] Sciences of the Universe [physics]/Earth Sciences/Hydrology", "[SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/Hydrology", "texture", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2015WR018233"}, {"href": "https://doi.org/10.1002/2015wr018233"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Water%20Resources%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1002/2015wr018233", "name": "item", "description": "10.1002/2015wr018233", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1002/2015wr018233"}, {"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": "10.1002/2016JF004060", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:14:49Z", "type": "Journal Article", "created": "2017-03-06", "title": "Investigation of rock fragmentation during rockfalls and rock avalanches via 3-D discrete element analyses", "description": "Abstract<p>This paper investigates the characteristics of dynamic rock fragmentation and its influence on the postfailure fragment trajectory. A series of numerical simulations by discrete element method (DEM) were performed for a simple rock block and slope geometry, where a particle agglomerate of prismatic shape is released along a sliding plane and subsequently collides onto a flat horizontal plane at a sharp kink point. The rock block is modeled as an assembly of bonded spherical particles with fragmentation arising from bond breakages. Bond strength and stiffness were calibrated against available experimental data. We analyzed how dynamic fragmentation occurs at impact, together with the generated fragment size distributions and consequently their runout for different slope topographies. It emerges that after impact, the vertical momentum of the granular system decreases sharply to nil, while the horizontal momentum increases suddenly and then decreases. The sudden boost of horizontal momentum can effectively facilitate the transport of fragments along the bottom floor. The rock fragmentation intensity is associated with the input energy and increases quickly with the slope angle. Gentle slopes normally lead to long spreading distance and large fragments, while steep slopes lead to high momentum boosts and impact forces, with efficient rock fragmentation and fine deposits. The fragment size decreases, while the fracture stress and fragment number both increase with the impact loading strain rate, supporting the experimental observations. The fragment size distributions can be well fitted by the Weibull's distribution function.</p>", "keywords": ["550", "DEM; dynamic fragmentation; loading rate; momentum boost; rock avalanche; runout;", "13. Climate action", "0211 other engineering and technologies", "02 engineering and technology", "Fragmentation", " rockslide", " rockavalanche", " DEM", " numerical modeling", " runout", "551", "01 natural sciences", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016JF004060"}, {"href": "https://eprints.ncl.ac.uk/fulltext.aspx?url=237479/388C5B83-7098-4BA3-A221-B7B1CEFCC63B.pdf&pub_id=237479"}, {"href": "https://doi.org/10.1002/2016JF004060"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Geophysical%20Research%3A%20Earth%20Surface", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1002/2016JF004060", "name": "item", "description": "10.1002/2016JF004060", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1002/2016JF004060"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-03-01T00:00:00Z"}}, {"id": "10.1002/2016rg000543", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:14:50Z", "type": "Journal Article", "created": "2017-03-23", "title": "A review of spatial downscaling of satellite remotely sensed soil moisture", "description": "Abstract<p>Satellite remote sensing technology has been widely used to estimate surface soil moisture. Numerous efforts have been devoted to develop global soil moisture products. However, these global soil moisture products, normally retrieved from microwave remote sensing data, are typically not suitable for regional hydrological and agricultural applications such as irrigation management and flood predictions, due to their coarse spatial resolution. Therefore, various downscaling methods have been proposed to improve the coarse resolution soil moisture products. The purpose of this paper is to review existing methods for downscaling satellite remotely sensed soil moisture. These methods are assessed and compared in terms of their advantages and limitations. This review also provides the accuracy level of these methods based on published validation studies. In the final part, problems and future trends associated with these methods are analyzed.</p>", "keywords": ["TIME-DOMAIN REFLECTOMETRY", "550", "IN-SITU", "downscaling", "MODIS TOA RADIANCES", "AMSR-E", "15. Life on land", "551", "01 natural sciences", "LAND-SURFACE TEMPERATURE", "REMEDHUS NETWORK SPAIN", "6. Clean water", "3. Good health", "[SDU] Sciences of the Universe [physics]", "L-BAND RADIOMETER", "remote sensing", "EVAPORATIVE FRACTION", "[SDU]Sciences of the Universe [physics]", "13. Climate action", "Earth and Environmental Sciences", "soil moisture", "SOUTHERN GREAT-PLAINS", "spatial resolution", "HIGH-RESOLUTION", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016RG000543"}, {"href": "https://doi.org/10.1002/2016rg000543"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Reviews%20of%20Geophysics", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1002/2016rg000543", "name": "item", "description": "10.1002/2016rg000543", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1002/2016rg000543"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-04-18T00:00:00Z"}}, {"id": "10.1002/2017JB015210", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:14:50Z", "type": "Journal Article", "created": "2018-03-12", "title": "Dynamic Fragmentation of Jointed Rock Blocks During Rockslide-Avalanches: Insights From Discrete Element Analyses", "description": "Abstract<p>The dynamic fragmentation of jointed rock blocks during rockslide avalanches has been investigated by discrete element method simulations for a multiple arrangement of a rock block sliding over a simple slope geometry. The rock blocks are released along an inclined sliding plane and subsequently collide onto a flat horizontal plane at a sharp kink point. The contact force chains generated by the impact appear initially at the bottom frontal corner of the rock block and then propagate radially upward to the top rear part of the block. The jointed rock blocks exhibit evident contact force concentration and discontinuity of force wave propagation near the joint, associating with high energy dissipation of granular dynamics. The corresponding force wave propagation velocity can be less than 200\uffc2\uffa0m/s, which is much smaller than that of an intact rock (1,316\uffc2\uffa0m/s). The concentration of contact forces at the bottom leads to high rock fragmentation intensity and momentum boosts, facilitating the spreading of many fine fragments to the distal ends. However, the upper rock block exhibits very low rock fragmentation intensity but high energy dissipation due to intensive friction and damping, resulting in the deposition of large fragments near the slope toe. The size and shape of large fragments are closely related to the orientation and distribution of the block joints. The cumulative fragment size distribution can be well fitted by the Weibull's distribution function, with very gentle and steep curvatures at the fine and coarse size ranges, respectively. The numerical results of fragment size distribution can match well some experimental and field observations.</p>", "keywords": ["discrete element method; dynamic fragmentation; force wave; fragment size distribution; jointed rock; rockslide avalanche;", "discrete element method; dynamic fragmentation; force wave; fragment size distribution; jointed rock; rockslide avalanche", "0211 other engineering and technologies", "02 engineering and technology", "551", "530", "01 natural sciences", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2017JB015210"}, {"href": "https://doi.org/10.1002/2017JB015210"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Geophysical%20Research%3A%20Solid%20Earth", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1002/2017JB015210", "name": "item", "description": "10.1002/2017JB015210", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1002/2017JB015210"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-04-01T00:00:00Z"}}, {"id": "10.1002/hyp.14451", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:14:54Z", "type": "Journal Article", "created": "2021-12-11", "title": "Hydrological responses to rainfall events including the extratropical cyclone Gloria in two contrasting Mediterranean headwaters in Spain; the perennial font del Reg\u00e0s and the intermittent Fuirosos", "description": "Abstract<p>Catchment hydrological responses to precipitation inputs, particularly during exceptionally large storms, are complex and variable, and our understanding of the associated runoff generation processes during those events is limited. Hydrological monitoring of climatically and hydrologically distinct catchments can help to improve this understanding by shedding light on the interplay between antecedent soil moisture conditions, hydrological connectivity, and rainfall event characteristics. This knowledge is urgently needed considering that both the frequency and magnitude of extreme precipitation events are increasing worldwide as a consequence of climate change. In autumn 2018, we installed water level sensors to monitor stream water and near\uffe2\uff80\uff90stream groundwater levels at two Mediterranean forest headwater catchments with contrasting hydrological regimes: Font del Reg\uffc3\uffa0s (sub\uffe2\uff80\uff90humid climate, perennial flow regime) and Fuirosos (semi\uffe2\uff80\uff90arid climate, intermittent flow regime). Both catchments are located in northeastern Spain, where the extratropical cyclone Gloria hit in January 2020 and left in ca. 65\uffe2\uff80\uff89h outstanding accumulated rainfalls of 424\uffe2\uff80\uff89mm in Font del Reg\uffc3\uffa0s and 230\uffe2\uff80\uff89mm in Fuirosos. During rainfall events of low mean intensity, hydrological responses to precipitation inputs at the semi\uffe2\uff80\uff90arid Fuirosos were more delayed and more variable than at the sub\uffe2\uff80\uff90humid Font del Reg\uffc3\uffa0s. We explain these divergences by differences in antecedent soil moisture conditions and associated differences in catchment hydrological connectivity between the two catchments, which in this case are likely driven by differences in local climate rather than by differences in local topography. In contrast, during events of moderate and high mean rainfall intensities, including the storm Gloria, precipitation inputs and hydrological responses correlated similarly in the two catchments. We explain this convergence by rapid development of hydrological connectivity independently of antecedent soil moisture conditions. The data set presented here is unique and contributes to our mechanistic understanding on how streams respond to rainfall events and exceptionally large storms in catchments with contrasting flow regimes.</p>", "keywords": ["info:eu-repo/classification/ddc/550", "550", "ddc:550", "rainfall intensity", "climate extreme", "15. Life on land", "551", "extreme hydrological event", "01 natural sciences", "6. Clean water", "antecedent soil moisture conditions", "Earth sciences", "13. Climate action", "heavy rainfall", "Mediterranean climate", "catchment hydrological connectivity", "environmental monitoring", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.14451"}, {"href": "https://doi.org/10.1002/hyp.14451"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Hydrological%20Processes", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1002/hyp.14451", "name": "item", "description": "10.1002/hyp.14451", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1002/hyp.14451"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-12-01T00:00:00Z"}}, {"id": "10.1002/ppp.2250", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:15:00Z", "type": "Journal Article", "created": "2024-09-09", "title": "Rainfall Impacts Dissolved Organic Matter and Cation Export From Permafrost Catchments and a Glacial River During Late Summer in Northeast Greenland", "description": "ABSTRACT<p>Ongoing and amplified climate change in the Arctic is leading to glacier retreat and to the exposure of an ever\uffe2\uff80\uff90larger portion of non\uffe2\uff80\uff90glaciated permafrost\uffe2\uff80\uff90dominated landscapes. Warming will also cause more precipitation to fall as rain, further enhancing the thaw of previously frozen ground. Yet, the impact of those perturbations on the geochemistry of Arctic rivers remains a subject of debate. Here, we determined the geochemical composition of waters from various contrasting non\uffe2\uff80\uff90glacial permafrost catchments and investigated their impact on a glacially dominated river, the Zackenberg River (Northeast Greenland), during late summer (August 2019). We also studied the effect of rainfall on the geochemistry of the Zackenberg River, its non\uffe2\uff80\uff90glacial tributaries, and a nearby independent non\uffe2\uff80\uff90glacial headwater stream Gr\uffc3\uffa6nse. We analyzed water properties, quantified and characterized dissolved organic matter (DOM) using absorbance and fluorescence spectroscopy and radiocarbon isotopes, and set this alongside analyses of the major cations (Ca, Mg, Na, and K), dissolved silicon (Si), and germanium/silicon ratios (Ge/Si). The glacier\uffe2\uff80\uff90fed Zackenberg River contained low concentrations of major cations, dissolved Si and dissolved organic carbon (DOC), and a Ge/Si ratio typical of bulk rock. Glacial DOM was enriched in protein\uffe2\uff80\uff90like fluorescent DOM and displayed relatively depleted radiocarbon values (i.e., old DOM). Non\uffe2\uff80\uff90glacial streams (i.e., tributaries and Gr\uffc3\uffa6nse) had higher concentrations of major cations and DOC and DOM enriched in aromatic compounds. They showed a wide range of values for radiocarbon, Si and Ge/Si ratios associated with variable contributions of surface runoff relative to deep active layer leaching. Before the rain event, Zackenberg tributaries did not contribute notably to the solute export of the Zackenberg River, and supra\uffe2\uff80\uff90permafrost ground waters governed the supply of solutes in Zackenberg tributaries and Gr\uffc3\uffa6nse stream. After the rain event, surface runoff modified the composition of Gr\uffc3\uffa6nse stream, and non\uffe2\uff80\uff90glacial tributaries strongly increased their contribution to the Zackenberg River solute export. Our results show that summer rainfall events provide an additional source of DOM and Si\uffe2\uff80\uff90rich waters from permafrost\uffe2\uff80\uff90underlain catchments to the discharge of glacially dominated rivers. This suggests that the magnitude and composition of solute exports from Arctic rivers are modulated by permafrost thaw and summer rain events. This event\uffe2\uff80\uff90driven solute supply will likely impact the carbon cycle in rivers, estuaries, and oceans and should be included into future predictions of carbon balance in these vulnerable Arctic systems.</p", "keywords": ["[SDV] Life Sciences [q-bio]", "550", "[SDV]Life Sciences [q-bio]", "supra-permafrost groundwater", "Zackenberg", "dissolved silicon", "dissolved organic matter", "551", "PARAFAC"]}, "links": [{"href": "https://doi.org/10.1002/ppp.2250"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Permafrost%20and%20Periglacial%20Processes", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1002/ppp.2250", "name": "item", "description": "10.1002/ppp.2250", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1002/ppp.2250"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-09-09T00:00:00Z"}}, {"id": "10.1007/s00382-016-3308-z", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:15:20Z", "type": "Journal Article", "created": "2016-08-23", "title": "Assessing mid-latitude dynamics in extreme event attribution systems", "description": "Open AccessISSN:1432-0894", "keywords": ["Atmospheric Science", "550", "0207 environmental engineering", "02 engineering and technology", "551", "01 natural sciences", "Dynamics", "[SDU] Sciences of the Universe [physics]", "[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/Climatology", "[SDU]Sciences of the Universe [physics]", "[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology", "13. Climate action", "Mid-latitudes", "Event attribution; Dynamics; Mid-latitudes; Extreme", "Event attribution", "Extreme", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://centaur.reading.ac.uk/66579/7/art%253A10.1007%252Fs00382-016-3308-z.pdf"}, {"href": "https://doi.org/10.1007/s00382-016-3308-z"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Climate%20Dynamics", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s00382-016-3308-z", "name": "item", "description": "10.1007/s00382-016-3308-z", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s00382-016-3308-z"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2016-08-23T00:00:00Z"}}, {"id": "10.1111/j.1365-2486.2008.01643.x", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:19:30Z", "type": "Journal Article", "created": "2008-05-27", "title": "Contrasting Effects Of Repeated Summer Drought On Soil Carbon Efflux In Hydric And Mesic Heathland Soils", "description": "Abstract<p>Current predictions of climate change include altered rainfall patterns throughout Europe, continental USA and areas such as the Amazon. The effect of this on soil carbon efflux remains unclear although several modelling studies have highlighted the potential importance of drought for carbon storage. To test the importance of drought, and more importantly repeated drought year\uffe2\uff80\uff90on\uffe2\uff80\uff90year, we used automated retractable curtains to exclude rain and produce repeated summer drought in three heathlands at varying moisture conditions. This included a hydric system limited by water\uffe2\uff80\uff90excess (in the UK) and two mesic systems with seasonal water limitation in Denmark (DK) and the Netherlands (NL). The experimental rainfall reductions were set to reflect single year droughts observed in the last decade with exclusion of rain for 2\uffe2\uff80\uff933 months of the year resulting in a 20\uffe2\uff80\uff9326% reduction in annual rainfall and 23\uffe2\uff80\uff9338% reduction in mean soil moisture during the drought period. Unexpectedly, sustained reduction in soil moisture over winter (between drought periods) was also observed at all three sites, along with a reduction in the maximum water\uffe2\uff80\uff90holding capacity attained. Three hypotheses are discussed which may have contributed to this lack of recovery in soil moisture: hydrophobicity of soil organic matter, increased water use by plants and increased cracking of the soil. The responses of soil respiration to this change in soil moisture varied among the sites: decreased rates were observed at the water\uffe2\uff80\uff90limited NL and DK sites whilst they increased at the UK site. Reduced sensitivity of soil respiration to soil temperature was observed at soil moisture contents above 55% at the UK site and below 20% and 13% at the NL and DK sites, respectively. Soil respiration rates recovered to predrought levels in the NL and DK sites during the winter re\uffe2\uff80\uff90wetting period that indicates any change in soil C storage due to changes in soil C efflux may be short lived in these mesic systems. In contrast, in the hydric UK site after 2 years of drought treatment, the persistent reduction in soil moisture throughout the year resulted in a year\uffe2\uff80\uff90round increase in soil respiration flux, a response that accelerated over time to 40% above control levels. These findings suggest that carbon\uffe2\uff80\uff90rich soils with high organic matter content may act as a significant source of CO2 to the atmosphere following repeated summer drought. Nonrecovery of soil moisture and a persistent increase in soil respiration may be the primary mechanism underlying the reported substantial losses of soil carbon from UK organic soils over the last 20 years. These findings indicate that the water status of an ecosystem will be a critical factor to consider in determining the impact of drought on the soil carbon fluxes and storage.</p>", "keywords": ["2. Zero hunger", "550", "organic soils", "VULCAN project", "drought", "04 agricultural and veterinary sciences", "15. Life on land", "551", "soil respiration", "6. Clean water", "climate change", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "soil carbon"]}, "links": [{"href": "https://doi.org/10.1111/j.1365-2486.2008.01643.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.1365-2486.2008.01643.x", "name": "item", "description": "10.1111/j.1365-2486.2008.01643.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/j.1365-2486.2008.01643.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2008-09-20T00:00:00Z"}}, {"id": "10.1007/s11104-016-2949-3", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:15:50Z", "type": "Journal Article", "created": "2016-06-14", "title": "Phosphorus Availability And Microbial Community In The Rhizosphere Of Intercropped Cereal And Legume Along A P-Fertilizer Gradient", "description": "Positive below-ground interactions (facilitation) should be more pronounced when resources limit crop growth, according to the stress-gradient hypothesis. Our aim was to test this hypothesis for intercropped durum wheat and faba bean along a P-fertilizer gradient. A field experiment was conducted in a long-term P-fertilizer trial with three rates of P-fertilization (No, Low and High P). Microbial biomass was assessed by chloroform fumigation-extraction. Quantitative PCR was applied to evaluate the abundance of relevant microbial groups. Phosphorus availability and microbial biomass systematically increased in the rhizosphere compared to bulk soil. P-fertilization resulted in higher abundance of targeted bacterial phyla, whole bacterial and fungal communities, and depressed mycorrhizal colonization of durum wheat, but not faba bean. Microbial biomass carbon significantly increased in the rhizosphere only in P-fertilized treatments, pointing to P limitation of microbial communities. Intercropping yielded a significant effect on rhizosphere microbial properties only at High P. Microbial biomass P increased in the rhizosphere of intercropped faba bean only at No P level, and was thus the sole finding supporting the stress-gradient hypothesis. P-fertilization was the main driver of microbial communities in this field trial, and P-fertilizer application modulated the species-specific effect in the intercrop. Plant performance did not validate the stress-gradient hypothesis as positive plant-plant interactions occurred regardless of the level of P-fertilization.", "keywords": ["[SDE] Environmental Sciences", "engrais phosphat\u00e9", "F08 - Syst\u00e8mes et modes de culture", "[SDV]Life Sciences [q-bio]", "F62 - Physiologie v\u00e9g\u00e9tale - Croissance et d\u00e9veloppement", "mycorhization", "Triticum turgidum", "630", "fertilisation", "[SHS]Humanities and Social Sciences", "http://aims.fao.org/aos/agrovoc/c_37554", "http://aims.fao.org/aos/agrovoc/c_5800", "http://aims.fao.org/aos/agrovoc/c_10795", "http://aims.fao.org/aos/agrovoc/c_24199", "2. Zero hunger", "Mycorrhizal colonization", "04 agricultural and veterinary sciences", "Vicia faba", "[SDV] Life Sciences [q-bio]", "fertilit\u00e9 du sol", "http://aims.fao.org/aos/agrovoc/c_6569", "Rhizosphere", "Long-term fertilization", "[SDE]Environmental Sciences", "[SHS] Humanities and Social Sciences", "Intercrop", "http://aims.fao.org/aos/agrovoc/c_8220", "rhizosph\u00e8re", "http://aims.fao.org/aos/agrovoc/c_4819", "http://aims.fao.org/aos/agrovoc/c_7170", "plante c\u00e9r\u00e9ali\u00e8re", "flore microbienne", "disponibilit\u00e9 nutriments (sol)", "http://aims.fao.org/aos/agrovoc/c_25512", "mod\u00e8le math\u00e9matique", "http://aims.fao.org/aos/agrovoc/c_36163", "Microbial community", "http://aims.fao.org/aos/agrovoc/c_3081", "phosphate", "P availability", "P34 - Biologie du sol", "15. Life on land", "http://aims.fao.org/aos/agrovoc/c_16367", "plante l\u00e9gumi\u00e8re", "http://aims.fao.org/aos/agrovoc/c_7958", "628", "http://aims.fao.org/aos/agrovoc/c_3910", "http://aims.fao.org/aos/agrovoc/c_35986", "0401 agriculture", " forestry", " and fisheries", "culture intercalaire", "http://aims.fao.org/aos/agrovoc/c_8165", "F04 - Fertilisation"]}, "links": [{"href": "https://doi.org/10.1007/s11104-016-2949-3"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Plant%20and%20Soil", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s11104-016-2949-3", "name": "item", "description": "10.1007/s11104-016-2949-3", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s11104-016-2949-3"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2016-06-14T00:00:00Z"}}, {"id": "10.1016/j.agee.2009.06.017", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:16:07Z", "type": "Journal Article", "created": "2009-08-03", "title": "Role Of Deforestation And Hillslope Position On Soil Quality Attributes Of Loess-Derived Soils In Golestan Province, Iran", "description": "Conversion of natural land resources into croplands, which is triggered by the rapid population growth, causes serious soil degradation. A loess hillslope located in eastern Golestan province of Iran was selected to study the role of deforestation and slope position on soil quality attributes. Surface (0\u201330 cm) and subsurface (30\u201360 cm) soil samples were taken from five slope positions (summit, SU, shoulder, SH, backslope, BS, footslope, FS and toeslope, TS) of forest (FO) and adjacent deforested cultivated land (DEF) in a factorial trial with completely randomized design. Ten pedons were also investigated and undisturbed soil samples were taken from different horizons for micromorphological studies. The texture of the original loess is silt loam. The soil textural class varies from silty clay loam in FO to silt loam in DEF, mainly due to the loss of finer particles as a result of soil erosion followed by deforestation and long-term cultivation. Mean weight diameter (MWD) of aggregates decreased following deforestation (0.88 mm compared to 1.49 mm in FO), as a result of considerable losses of organic carbon (OC) and breakdown of aggregates. Bulk density (BD) increased and soil infiltration rate decreased by about 50% in DEF. Reduction of annual organic matter input to soil as a result of deforestation and also rapid oxidation of organic matter in DEF were responsible for a significant decrease (>70%) in OC and total nitrogen (TN). Soil microbial respiration (SMR) also decreased significantly, following deforestation. Carbon, and N contents and population of fungi were significantly higher in all hillslope positions of the FO than the DEF. Changes in soil quality attributes were not significant in different slope positions of FO, which might be related to the stability of forest landscape. Effect of different slope positions on soil quality attributes was more pronounced in the DEF. The SH and BS were found as the most susceptible positions to erosion in DEF. Soils of the FO were mainly classified as Alfisols and Mollisols with evidences for clay illuviation compared to the weakly developed Inceptisols formed in the DEF. Micromorphological investigations revealed that the FO soils had strong granular and crumb microstructure with a high porosity indicating the presence of high amount of organic matter. The high microbial and faunal activity was confirmed through the presence of excremental pedofeatures in the topsoil of the FO. Lower organic matter and consequently microbial activity in the topsoil of the DEF have resulted in the massive microstructure with little porosity.", "keywords": ["2. Zero hunger", "Soil Science", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land", "551", "630"]}, "links": [{"href": "https://doi.org/10.1016/j.agee.2009.06.017"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Agriculture%2C%20Ecosystems%20%26amp%3B%20Environment", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.agee.2009.06.017", "name": "item", "description": "10.1016/j.agee.2009.06.017", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.agee.2009.06.017"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2009-12-01T00:00:00Z"}}, {"id": "10.1016/j.asr.2019.05.027", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:16:25Z", "type": "Journal Article", "created": "2019-06-04", "title": "Variability and accuracy of Zenith Total Delay over the East African tropical region", "description": "The Global Navigation Satellite System (GNSS) can be used to derive accurately the Zenith Tropospheric Delay (ZTD) under all-weather conditions. The derived ZTDs play a vital role in climate studies, weather forecasting and are operationally assimilated into numerical weather prediction models. In this study, variations and statistical analysis of GNSS-derived ZTD over the East African tropical region are analysed. The data is collected from 13 geodetic permanent stations for the period of 4 years from 2013 to 2016. The 13 stations consist of 5 International GNSS Service (IGS) stations plus 8 stations as follows: 4 Africa Array stations and 4 Malawi Rifting stations from Uganda, Kenya, Tanzania and Rwanda. The ZTD time series were processed using goGPS software version 1.0 beta1, a MATLAB based GNSS processing software, originally developed for kinematic applications but recently re-engineered for quasi static applications. The annual variation of the ZTD time series was investigated using Lomb Scargle periodograms. The semi-annual frequency has the dominant power in subregion 1 (latitudes 4 \u00b0S and 4 \u00b0N) and the annual frequency has the dominant power in subregion 2 (latitudes 12 \u00b0S to 4 \u00b0S). The highest ZTD estimates occur during the rainy seasons, at all stations, and the lowest estimates occur during the dry seasons. The results also show that the ZTD estimates are largest at stations located at low elevation (regions close to the Indian Ocean). The derived ZTDs are compared to the values derived from the GIPSY-OASIS via Jet Propulsion Laboratory (JPL) online Automatic Precise Positioning Service (APPS) and the Unified Environmental Modelling System (UEMS) numerical weather prediction (NWP) model. The comparison of goGPS and APPS ZTD at the 13 stations shows an overall average bias, Root Mean Square (RMS) and standard deviation (stdev) of \u22120.9 mm, 3.2 mm and 3.0 mm respectively, with correlation coefficients ranging from 0.974 to 0.999. The comparison of goGPS ZTD against UEMS NWP ZTD at 8 selected stations shows average bias, RMS and stdev of \u221212.4 mm, 22.0 mm and 17.6 mm respectively, with correlation coefficients ranging from 0.802 to 0.974. The agreement between the GPS ZTD and the NWP ZTD indicates that goGPS ZTD can be assimilated into NWP models in the East African region.", "keywords": ["GNSS", "goGPS", "Zenith tropospheric delay", "13. Climate action", "UEMS-NWP", "0207 environmental engineering", "02 engineering and technology", "551", "Precise point positioning", "01 natural sciences", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.asr.2019.05.027"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Advances%20in%20Space%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.asr.2019.05.027", "name": "item", "description": "10.1016/j.asr.2019.05.027", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.asr.2019.05.027"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-08-01T00:00:00Z"}}, {"id": "10.1016/j.ecoena.2019.100006", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:16:37Z", "type": "Journal Article", "created": "2019-05-24", "title": "Ecosystem services from combined natural and engineered water and wastewater treatment systems: going beyond water quality enhancement", "description": "Abstract   Combined natural and engineered water and waste water systems (cNES) are nature-based solutions that utilise naturally occurring processes to remove impurities from water and therefore contribute to the ecosystem service of water quality enhancement. We hypothesise that these systems may also have a potential to deliver ecosystem services other than their primary purpose of water purification and we use spatially-explicit modelling tools to determine these benefits. We focused on three different types of cNES: bank filtration (BF), managed aquifer recharge/soil aquifer treatment (MAR/SAT), and constructed wetlands (CW), and combined the ecosystem services cascade, DESSIN and CICES conceptual frameworks with multiple InVEST 3.4.4 models to investigate the spatial distribution of intermediate ecosystem services within the sites as well as in the surrounding landscape. We also determined the role of habitats present within the sites in wider landscape\u2019s connectivity to the nearest Natura 2000 areas using the Circuitscape 4.0 model, assessed the public perception of the aesthetic value of two of the cNES technologies, i.e. CW and MAR/SAT, via an online survey, and linked the determined ecosystem services to their likely beneficiaries. Our results indicated that the sites characterised with semi-natural ecosystems had a good potential for ecosystem services provision and that the selected cNES technologies were favourably received by the public as compared to their engineered equivalents. We concluded that determination of ecosystem services potential from nature-based solutions, such as cNES technologies, should be done in consideration of various contextual factors including the type of habitats/ecosystems present within the proposed solutions, the location within the landscape as well as properties and ecosystem services potential of the areas surrounding the sites, all of which can be facilitated by deployment of spatially-explicit ecosystem service models at early stages of the planning process.", "keywords": ["2. Zero hunger", "Nature-based solutions", "0211 other engineering and technologies", "Water and waste water treatment", "Habitat connectivity", "02 engineering and technology", "15. Life on land", "551", "01 natural sciences", "6. Clean water", "12. Responsible consumption", "Circuitscape", "13. Climate action", "11. Sustainability", "Ecosystem services", "InVEST models", "14. Life underwater", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.ecoena.2019.100006"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Ecological%20Engineering", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.ecoena.2019.100006", "name": "item", "description": "10.1016/j.ecoena.2019.100006", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.ecoena.2019.100006"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-01-01T00:00:00Z"}}, {"id": "10.1016/j.egypro.2018.07.023", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:16:40Z", "type": "Journal Article", "created": "2018-07-18", "title": "Intercalation of aromatic sulfonates in \u2018green rust\u2019 via ion exchange", "description": "\u2018Green rust\u2019 intercalated with aromatic sulfonates can potentially be effective materials for the treatment of soil and groundwater polluted with chlorinated benzenes. We investigated the potential intercalation of benzene sulfonate (BzS) and 1,3-benzene disulfonate (BzDS) into green rust sulfate (GRSO4) via ion exchange. The GRSO4 reacted with various concentrations of sulfonates were characterized by X-ray diffraction, X-ray scattering and transmission electron microscopy. GR interacted with BzDS did not result in intercalation due to stearic hindrance and electrostatic repulsion. For BzS, mixtures of GRSO4 and GR-BzS (d001 = 14.3 \u00c5) were obtained at molar equivalents of ion exchange capacity &gt;5. The intercalation of BzS in the GR structure is limited (~18% intercalation) since BzS cannot fully replace SO42-. The BzS molecules are likely arranged in the interlayer as a dehydrated monolayer with the \u2013SO3 groups facing away in alternate directions.", "keywords": ["layered double hydroxide", "Iron (oxyhydr)oxides", "Iron (oxyhydr)oxides", " layered double hydroxide", " sulfonates", "sulfonates", "iron (oxyhydr)oxides", "500 Naturwissenschaften und Mathematik::550 Geowissenschaften", " Geologie::551 Geologie", " Hydrologie", " Meteorologie", "02 engineering and technology", "551", "0210 nano-technology", "01 natural sciences", "6. Clean water", "0104 chemical sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.egypro.2018.07.023"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Energy%20Procedia", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.egypro.2018.07.023", "name": "item", "description": "10.1016/j.egypro.2018.07.023", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.egypro.2018.07.023"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-07-01T00:00:00Z"}}, {"id": "10.1016/j.epsl.2017.04.002", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:16:49Z", "type": "Journal Article", "created": "2017-04-14", "title": "The origin of volatile element depletion in early solar system material: Clues from Zn isotopes in chondrules", "description": "Abstract   Volatile lithophile elements are depleted in the different planetary materials to various degrees, but the origin of these depletions is still debated. Stable isotopes of moderately volatile elements such as Zn can be used to understand the origin of volatile element depletions. Samples with significant volatile element depletions, including the Moon and terrestrial tektites, display heavy Zn isotope compositions (i.e. enrichment of 66Zn vs. 64Zn), consistent with kinetic Zn isotope fractionation during evaporation. However,  Luck et al. (2005)  found a negative correlation between      \u03b4    66     Zn and 1/[Zn] between CI, CM, CO, and CV chondrites, opposite to what would be expected if evaporation caused the Zn abundance variations among chondrite groups.  We have analyzed the Zn isotope composition of multiple samples of the major carbonaceous chondrite classes: CI (1), CM (4), CV (2), CO (4), CB (2), CH (2), CK (4), and CK/CR (1). The bulk chondrites define a negative correlation in a plot of      \u03b4    66     Zn vs 1/[Zn], confirming earlier results that Zn abundance variations among carbonaceous chondrites cannot be explained by evaporation. Exceptions are CB and CH chondrites, which display Zn systematics consistent with a collisional formation mechanism that created enrichment in heavy Zn isotopes relative to the trend defined by CI\u2013CK.  We further report Zn isotope analyses of chondrite components, including chondrules from Allende (CV3) and Mokoia (CV3), as well as an aliquot of Allende matrix. All chondrules are enriched in light Zn isotopes (\u223c500 ppm on 66Zn/64Zn) relative to the bulk, contrary to what would be expected if Zn were depleted during evaporation, on the other hand the matrix has a complementary heavy isotope composition. We report sequential leaching experiments in un-equilibrated ordinary chondrites, which show sulfides are isotopically heavy compared to silicates and the bulk meteorite by ca. +0.65 per mil on 66Zn/64Zn. We suggest isotopically heavy sulfides were removed from either chondrules or their precursors, thereby producing the light Zn isotope enrichments in chondrules.", "keywords": ["chondrules", "550", "protoplanetary disk", "551", "carbonaceous chondrites", "01 natural sciences", "volatiles", "[SDU.STU.PL]Sciences of the Universe [physics]/Earth Sciences/Planetology", "[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry", "13. Climate action", "[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/Geochemistry", "[SDU.STU.PL] Sciences of the Universe [physics]/Earth Sciences/Planetology", "zinc isotopes", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.epsl.2017.04.002"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Earth%20and%20Planetary%20Science%20Letters", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.epsl.2017.04.002", "name": "item", "description": "10.1016/j.epsl.2017.04.002", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.epsl.2017.04.002"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-06-01T00:00:00Z"}}, {"id": "10.1029/2018JE005899", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:15Z", "type": "Journal Article", "created": "2020-03-09", "title": "Initiation and Flow Conditions of Contemporary Flows in Martian Gullies", "description": "<p>         &amp;lt;p&amp;gt;Understanding the initial and flow conditions of contemporary flows in Martian gullies, generally believed to be triggered and fluidized by CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; sublimation, is crucial for deciphering climate conditions needed to trigger and sustain them. We employ the RAMMS (RApid Mass Movement Simulation) debris flow and avalanche model to back-calculate initial and flow conditions of recent flows in three gullies in Hale crater. We infer minimum release depths of 1.0&amp;amp;#8211;1.5 m and initial release volumes of 100&amp;amp;#8211;200 m&amp;lt;sup&amp;gt;3&amp;lt;/sup&amp;gt;. Entrainment leads to final flow volumes that are 2.5&amp;amp;#8211;5.5 times larger than initially released, and entrainment is found necessary to match the observed flow deposits. Simulated mean cross-channel flow velocities decrease from 3&amp;amp;#8211;4 m s&amp;lt;sup&amp;gt;-1&amp;lt;/sup&amp;gt; to ~1 m s&amp;lt;sup&amp;gt;-1&amp;lt;/sup&amp;gt; from release area to flow terminus, while flow depths generally decrease from 0.5&amp;amp;#8211;1 m to 0.1&amp;amp;#8211;0.2 m. The mean cross-channel erosion depth and deposition thicknesses are _0.1&amp;amp;#8211;0.3 m. Back-calculated dry-Coulomb friction ranges from 0.1 to 0.25 and viscous turbulent friction between 100&amp;amp;#8211;200 m s&amp;lt;sup&amp;gt;-2&amp;lt;/sup&amp;gt;, which are values similar to those of granular debris flows on Earth. These results suggest that recent flows in gullies are fluidized to a similar degree as are granular debris flows on Earth. Using a novel model for mass-flow fluidization by CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; sublimation we are able to show that under Martian atmospheric conditions very small volumetric fractions of CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; of ~1% within mass flows may indeed yield sufficiently large gas fluxes to cause fluidization and enhance flow mobility.&amp;lt;/p&amp;gt;         </p>", "keywords": ["Atmospheric Science", "550", "[SDU.STU.GM] Sciences of the Universe [physics]/Earth Sciences/Geomorphology", "0211 other engineering and technologies", "Soil Science", "Mars", "Hale crater", "02 engineering and technology", "Aquatic Science", "carbon dioxide; gullies; Hale crater; Mars; modeling; RAMMS", "551", "Oceanography", "01 natural sciences", "[SDU.STU.PL]Sciences of the Universe [physics]/Earth Sciences/Planetology", "Geochemistry and Petrology", "Earth and Planetary Sciences (miscellaneous)", "SDG 13 - Climate Action", "Research Articles", "Water Science and Technology", "Earth-Surface Processes", "0105 earth and related environmental sciences", "Ecology", "Palaeontology", "carbon dioxide", "Forestry", "modeling", "RAMMS", "Geophysics", "Space and Planetary Science", "13. Climate action", "[SDU.STU.PL] Sciences of the Universe [physics]/Earth Sciences/Planetology", "gullies"]}, "links": [{"href": "http://dro.dur.ac.uk/28802/1/28802.pdf"}, {"href": "http://dro.dur.ac.uk/28802/2/28802.pdf"}, {"href": "https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2018JE005899"}, {"href": "https://doi.org/10.1029/2018JE005899"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Geophysical%20Research%3A%20Planets", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1029/2018JE005899", "name": "item", "description": "10.1029/2018JE005899", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1029/2018JE005899"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-08-01T00:00:00Z"}}, {"id": "10.1016/j.jhazmat.2020.123327", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:17:15Z", "type": "Journal Article", "created": "2020-06-27", "title": "Arsenic removal from natural groundwater using \u2018green rust\u2019: Solid phase stability and contaminant fate", "description": "Arsenic (As) contamination in groundwater remains a pressing global challenge. In this study, we evaluated the potential of green rust (GR), a redox-active iron phase frequently occurring in anoxic environments, to treat As contamination at a former wood preservation site. We performed long-term batch experiments by exposing synthetic GR sulfate (GRso(4)) to As-free and As-spiked (6 mg L-1) natural groundwater at both 25 and 4 C. At 25 C, GRso4 was metastable in As-free groundwater and transformed to GlIcos, and then fully to magnetite within 120 days; however, GRso(4) stability increased 7-fold by lowering the temperature to 4 degrees C, and 8-fold by adding As to the groundwater at 25 degrees C. Highest GRso4 stability was observed when As was added to the groundwater at 4 C. This stabilizing effect is explained by GR solubility being lowered by adsorbed As and/or lower temperatures, inhibiting partial GR dissolution required for transformation to GlIcos, and ultimately to magnetite. Despite these mineral transformations, all added As was removed from As-spiked samples within 120 days at 25 C, while uptake was 2 times slower at 4 degrees C. Overall, we have successfully documented that GR is an important mineral substrate for As immobilization in anoxic subsurface environments.", "keywords": ["Aging effects", "Iron (oxyhydr)oxides", "550", "13. Climate action", "Groundwater remediation", "Mineral stability", "500 Naturwissenschaften und Mathematik::550 Geowissenschaften", " Geologie::551 Geologie", " Hydrologie", " Meteorologie", "Adsorption", " Aging effects", "Groundwater remediation", " Iron (oxyhydr)oxides", " Mineral stability", "Adsorption", "551", "01 natural sciences", "6. Clean water", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://eprints.whiterose.ac.uk/165515/1/1-s2.0-S0304389420313169-main.pdf"}, {"href": "https://doi.org/10.1016/j.jhazmat.2020.123327"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Hazardous%20Materials", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.jhazmat.2020.123327", "name": "item", "description": "10.1016/j.jhazmat.2020.123327", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.jhazmat.2020.123327"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-01-01T00:00:00Z"}}, {"id": "10.1016/j.jhazmat.2024.136496", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:17:16Z", "type": "Journal Article", "created": "2024-11-17", "title": "Mobilization of poly- and perfluoroalkyl substances (PFAS) from heterogeneous soils: Desorption by ethanol/xanthan gum mixture", "description": "Remediating soils contaminated by per- and polyfluoroalkyl substances (PFAS) is a challenging task due to the unique properties of these compounds, such as variable solubility and resistance to degradation. In-situ soil flushing with solvents has been considered as a remediation technique for PFAS-contaminated soils. The use of non-Newtonian fluids, displaying variable viscosity depending on the applied shear rate, can offer certain advantages in improving the efficiency of the process, particularly in heterogeneous porous media. In this work, the efficacy of ethanol/xanthan mixture (XE) in the recovery of a mixture of perfluorooctane sulfonate (PFOS), perfluorooctanoic acid (PFOA), perfluorohexane sulfonate (PFHxS), and perfluorobutane sulfonate (PFBS) from soil has been tested at lab-scale. XE's non-Newtonian behavior was examined through rheological measurements, confirming that ethanol did not affect xanthan gum's (XG) shear-thinning behavior. The recovery of PFAS in batch-desorption exceeded 95\u00a0% in ethanol, and 99\u00a0% in XE, except for PFBS which reached 94\u00a0%. 1D-column experiments revealed overshoots in PFAS breakthrough curves during ethanol and XE injection, due to over-solubilization. XE, (XG 0.05\u00a0% w/w) could recover 99\u00a0% PFOA, 98\u00a0% PFBS, 97\u00a0% PFHxS, and 92\u00a0% PFOS. Numerical modeling successfully reproduces breakthrough curves for PFOA, PFHxS, and PFBS with the convection-dispersion-sorption equation and Langmuir sorption isotherm.", "keywords": ["Heterogeneity of porous media", "PFAS", "628", "H2020", "[SDU.STU] Sciences of the Universe [physics]/Earth Sciences", "[SDU.STU]Sciences of the Universe [physics]/Earth Sciences", "Desorption", "551", "Alcohol", "PROMISCES", "Poly- and perfluoroalkyl substances (PFAS)", "Non-Newtonian fluids (NNF)"], "contacts": [{"organization": "Batikh, Ali, Colombano, St\u00e9fan, Cochennec, Maxime, Davarzani, Dorian, Perrault, Arnault, Lions, Julie, Grandcl\u00e9ment, Julien, Guyonnet, Dominique, Togola, Anne, Zornig, Cl\u00e9ment, Devau, Nicolas, Lion, Fabien, Alamooti, Amir, Bristeau, S\u00e9bastien, Djemil, Mohamed, van Hullebusch, E.D.,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1016/j.jhazmat.2024.136496"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Hazardous%20Materials", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.jhazmat.2024.136496", "name": "item", "description": "10.1016/j.jhazmat.2024.136496", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.jhazmat.2024.136496"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-01-01T00:00:00Z"}}, {"id": "10.1016/j.quascirev.2018.09.037", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:17:22Z", "type": "Journal Article", "created": "2018-10-06", "title": "Short-term soil formation events in last glacial east European loess, evidence from multi-method luminescence dating", "description": "Here we provide a robust luminescence chronology for Stayky (Ukraine), a reference profile in European Late Pleistocene loess stratigraphy, based on optically stimulated luminescence (OSL) dating on quartz (4-11 \u03bcm, 63-90 \u03bcm) and post infrared-infrared stimulated luminescence (pIR-IRSL)) on polymineral fine grains. For the Bug loess unit, the equivalent of Marine Isotope Stage (MIS 2), results are in agreement between methods, demonstrating that the suite of embryonic soils previously interpreted as reflecting climate variability similar to Greenland interstadials (GI) actually date to \u223c29/27-15 ka, with most emplaced around or after 20 ka. This temporal span is further confirmed by age-depth modelling of available data. Apart from GI-2, no interstadial-type climate events are recorded in Greenland ice core data for that time interval. As short-term pedogenetic phases are also documented in records from central-western Europe, there is a need for more research into the European mid-latitude terrestrial environments response to MIS 2 hydroclimate variability. The dating of Vytachiv paleosol, previously debatably linked to various GI events within MIS 3 resulted in ages of \u223c40 \u00b1 4 ka and \u223c53 \u00b1 4 ka at the lower transition, and \u223c26 \u00b1 2 ka to \u223c30 \u00b1 2 ka in the overlying loess. These ages indicate that the truncated Vytachiv paleosol is either not continuous, or that it encompasses a broader age range within MIS 3 than previously considered. In both cases, data would not allow for an unambiguous linking of this paleosol with specific GI events as previously attempted. The pIR-IRSL290 dating of the loams immediately underneath Pryluky unit in the range of \u223c120 ka to \u223c168 ka and of the Pryluky mollisol from \u223c90 ka to 126 ka confirm the broad correspondence of this unit with MIS 5, although poor dose recovery results open the possibility for further testing on the degree these ages provide overestimated results. Quartz data severely underestimate the pIR-IRSL290 ages for these samples. The application of pIR-IRSL290 dating for the underlying Dnieper till previously linked to the Saalian glaciation resulted in natural signals at the level of laboratory saturation, yielding minimum ages of c. 700 ka. For the same sample, the natural SAR-OSL signals for 4-11 \u03bcm quartz were found significantly below laboratory saturation level, resulting in finite ages of \u223c250-270 ka interpreted here as underestimates, while coarse quartz (63-90 \u03bcm) signals reached about 85% of the laboratory saturation level. These data suggest extreme caution must be taken when dating such old samples using quartz OSL. Results from our high-resolution luminescence dating raises important implications for the chronological representativeness of Stayky as a key loess site in Eastern Europe beyond MIS 2.", "keywords": ["Embryonic soils", "550", "Millennial-scale loess records", "Luminescence dating", "Loess", "Eastern Europe", "551", "Climate dynamics", "Pleistocene", "[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/Climatology", "[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology", "13. Climate action", "[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy", "[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy", "MIS 2 embryonic soils"]}, "links": [{"href": "https://doi.org/10.1016/j.quascirev.2018.09.037"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Quaternary%20Science%20Reviews", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.quascirev.2018.09.037", "name": "item", "description": "10.1016/j.quascirev.2018.09.037", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.quascirev.2018.09.037"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-11-01T00:00:00Z"}}, {"id": "10.1016/j.soilbio.2021.108466", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:17:42Z", "type": "Journal Article", "created": "2021-11-03", "title": "Improved global-scale predictions of soil carbon stocks with Millennial Version 2", "description": "Abstract   Soil carbon (C) models are used to predict C sequestration responses to climate and land use change. Yet, the soil models embedded in Earth system models typically do not represent processes that reflect our current understanding of soil C cycling, such as microbial decomposition, mineral association, and aggregation. Rather, they rely on conceptual pools with turnover times that are fit to bulk C stocks and/or fluxes. As measurements of soil fractions become increasingly available, it is necessary for soil C models to represent these measurable quantities so that model processes can be evaluated more accurately. Here we present Version 2 (V2) of the Millennial model, a soil model developed to simulate C pools that can be measured by extraction or fractionation, including particulate organic C, mineral-associated organic C, aggregate C, microbial biomass, and low molecular weight C. Model processes have been updated to reflect the current understanding of mineral-association, temperature sensitivity and reaction kinetics, and different model structures were tested within an open-source framework. We evaluated the ability of Millennial V2 to simulate total soil organic C (SOC), as well as the mineral-associated and particulate fractions, using three independent data sets of soil fractionation measurements spanning a range of climate and geochemistry in Australia (N\u00a0=\u00a0495), Europe (N\u00a0=\u00a0175), and across the globe (N\u00a0=\u00a0659). When using all the data together (N\u00a0=\u00a01329), the Millennial V2 model predicted SOC (RMSE\u00a0=\u00a03.3\u00a0kg\u00a0C m\u22122, AIC\u00a0=\u00a0675,      R   i  n   2     \u00a0=\u00a00.31,      R   o  u  t   2     \u00a0=\u00a00.26) better than the widely-used first-order decomposition model Century (RMSE\u00a0=\u00a03.4\u00a0kg\u00a0C m\u22122, AIC\u00a0=\u00a0696,      R   i  n   2     \u00a0=\u00a00.21,      R   o  u  t   2     \u00a0=\u00a00.18) across sites, despite the fact that Millennial V2 has an increase in process complexity and number of parameters compared to Century. Millennial V2 also reproduced the observed fraction of C in MAOM and larger particle size fractions for most latitudes and biomes, and allows for a more detailed understanding of the pools and processes that affect model performance. It is important to note that this study evaluates the spatial variation in C stock only, and that the temporal dynamics of Millennial V2 remain to be tested. The Millennial V2 model updates the conceptual Century model pools and processes and represents our current understanding of the roles that microbial activity, mineral association and aggregation play in soil C sequestration.", "keywords": ["2. Zero hunger", "[SDU.OCEAN]Sciences of the Universe [physics]/Ocean", "550", "Mineral association", "Atmosphere", "Soil organic carbon stocks", "[SDU.OCEAN] Sciences of the Universe [physics]/Ocean", " Atmosphere", "15. Life on land", "551", "Microbial decomposition", "01 natural sciences", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "13. Climate action", "Soil carbon modeling", "[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces", "environment", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.soilbio.2021.108466"}, {"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": "10.1016/j.soilbio.2021.108466", "name": "item", "description": "10.1016/j.soilbio.2021.108466", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.soilbio.2021.108466"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-01-01T00:00:00Z"}}, {"id": "10.1111/j.1365-2486.2006.01131.x", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:19:29Z", "type": "Journal Article", "created": "2006-03-24", "title": "Estimating The Uncertainty In Annual Net Ecosystem Carbon Exchange: Spatial Variation In Turbulent Fluxes And Sampling Errors In Eddy-Covariance Measurements", "description": "Abstract<p>Above forest canopies, eddy covariance (EC) measurements of mass (CO2, H2O vapor) and energy exchange, assumed to represent ecosystem fluxes, are commonly made at one point in the roughness sublayer (RSL). A spatial variability experiment, in which EC measurements were made from six towers within the RSL in a uniform pine plantation, quantified large and dynamic spatial variation in fluxes. The spatial coefficient of variation (CV) of the scalar fluxes decreased with increasing integration time, stabilizing at a minimum that was independent of further lengthening the averaging period (hereafter a \uffe2\uff80\uff98stable minimum\uffe2\uff80\uff99). For all three fluxes, the stable minimum (CV=9\uffe2\uff80\uff9311%) was reached at averaging times (\uffcf\uff84p) of 6\uffe2\uff80\uff937\uffe2\uff80\uff83h during daytime, but higher stable minima (CV=46\uffe2\uff80\uff93158%) were reached at longer \uffcf\uff84p (&gt;12\uffe2\uff80\uff83h) during nighttime. To the extent that decreasing CV of EC fluxes reflects reduction in micrometeorological sampling errors, half of the observed variability at \uffcf\uff84p=30\uffe2\uff80\uff83min is attributed to sampling errors. The remaining half (indicated by the stable minimum CV) is attributed to underlying variability in ecosystem structural properties, as determined by leaf area index, and perhaps associated ecosystem activity attributes. We further assessed the spatial variability estimates in the context of uncertainty in annual net ecosystem exchange (NEE). First, we adjusted annual NEE values obtained at our long\uffe2\uff80\uff90term observation tower to account for the difference between this tower and the mean of all towers from this experiment; this increased NEE by up to 55\uffe2\uff80\uff83g\uffe2\uff80\uff83C\uffe2\uff80\uff83m\uffe2\uff88\uff922\uffe2\uff80\uff83yr\uffe2\uff88\uff921. Second, we combined uncertainty from gap filling and instrument error with uncertainty because of spatial variability, producing an estimate of variability in annual NEE ranging from 79 to 127\uffe2\uff80\uff83g\uffe2\uff80\uff83C\uffe2\uff80\uff83m\uffe2\uff88\uff922\uffe2\uff80\uff83yr\uffe2\uff88\uff921. This analysis demonstrated that even in such a uniform pine plantation, in some years spatial variability can contribute \uffe2\uff88\uffbc50% of the uncertainty in annual NEE estimates.</p>", "keywords": ["550", "13. Climate action", "15. Life on land", "551", "01 natural sciences", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1111/j.1365-2486.2006.01131.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.1365-2486.2006.01131.x", "name": "item", "description": "10.1111/j.1365-2486.2006.01131.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/j.1365-2486.2006.01131.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2006-04-03T00:00:00Z"}}, {"id": "2078.1/293942", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:26:29Z", "type": "Journal Article", "created": "2024-09-09", "title": "Rainfall Impacts Dissolved Organic Matter and Cation Export From Permafrost Catchments and a Glacial River During Late Summer in Northeast Greenland", "description": "ABSTRACT<p>Ongoing and amplified climate change in the Arctic is leading to glacier retreat and to the exposure of an ever\uffe2\uff80\uff90larger portion of non\uffe2\uff80\uff90glaciated permafrost\uffe2\uff80\uff90dominated landscapes. Warming will also cause more precipitation to fall as rain, further enhancing the thaw of previously frozen ground. Yet, the impact of those perturbations on the geochemistry of Arctic rivers remains a subject of debate. Here, we determined the geochemical composition of waters from various contrasting non\uffe2\uff80\uff90glacial permafrost catchments and investigated their impact on a glacially dominated river, the Zackenberg River (Northeast Greenland), during late summer (August 2019). We also studied the effect of rainfall on the geochemistry of the Zackenberg River, its non\uffe2\uff80\uff90glacial tributaries, and a nearby independent non\uffe2\uff80\uff90glacial headwater stream Gr\uffc3\uffa6nse. We analyzed water properties, quantified and characterized dissolved organic matter (DOM) using absorbance and fluorescence spectroscopy and radiocarbon isotopes, and set this alongside analyses of the major cations (Ca, Mg, Na, and K), dissolved silicon (Si), and germanium/silicon ratios (Ge/Si). The glacier\uffe2\uff80\uff90fed Zackenberg River contained low concentrations of major cations, dissolved Si and dissolved organic carbon (DOC), and a Ge/Si ratio typical of bulk rock. Glacial DOM was enriched in protein\uffe2\uff80\uff90like fluorescent DOM and displayed relatively depleted radiocarbon values (i.e., old DOM). Non\uffe2\uff80\uff90glacial streams (i.e., tributaries and Gr\uffc3\uffa6nse) had higher concentrations of major cations and DOC and DOM enriched in aromatic compounds. They showed a wide range of values for radiocarbon, Si and Ge/Si ratios associated with variable contributions of surface runoff relative to deep active layer leaching. Before the rain event, Zackenberg tributaries did not contribute notably to the solute export of the Zackenberg River, and supra\uffe2\uff80\uff90permafrost ground waters governed the supply of solutes in Zackenberg tributaries and Gr\uffc3\uffa6nse stream. After the rain event, surface runoff modified the composition of Gr\uffc3\uffa6nse stream, and non\uffe2\uff80\uff90glacial tributaries strongly increased their contribution to the Zackenberg River solute export. Our results show that summer rainfall events provide an additional source of DOM and Si\uffe2\uff80\uff90rich waters from permafrost\uffe2\uff80\uff90underlain catchments to the discharge of glacially dominated rivers. This suggests that the magnitude and composition of solute exports from Arctic rivers are modulated by permafrost thaw and summer rain events. This event\uffe2\uff80\uff90driven solute supply will likely impact the carbon cycle in rivers, estuaries, and oceans and should be included into future predictions of carbon balance in these vulnerable Arctic systems.</p", "keywords": ["[SDV] Life Sciences [q-bio]", "550", "[SDV]Life Sciences [q-bio]", "supra-permafrost groundwater", "Zackenberg", "dissolved silicon", "dissolved organic matter", "551", "PARAFAC"]}, "links": [{"href": "https://doi.org/2078.1/293942"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Permafrost%20and%20Periglacial%20Processes", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "2078.1/293942", "name": "item", "description": "2078.1/293942", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2078.1/293942"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-09-09T00:00:00Z"}}, {"id": "10.1029/2020jg006119", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:15Z", "type": "Journal Article", "created": "2021-08-28", "title": "Impacts of Drying and Rewetting on the Radiocarbon Signature of Respired CO2 and Implications for Incubating Archived Soils", "description": "Abstract<p>The radiocarbon signature of respired CO2 (\uffe2\uff88\uff8614C\uffe2\uff80\uff90CO2) measured in laboratory soil incubations integrates contributions from soil carbon pools with a wide range of ages, making it a powerful model constraint. Incubating archived soils enriched by \uffe2\uff80\uff9cbomb\uffe2\uff80\uff90C\uffe2\uff80\uff9d from mid\uffe2\uff80\uff9020th century nuclear weapons testing would be even more powerful as it would enable us to trace this pulse over time. However, air\uffe2\uff80\uff90drying and subsequent rewetting of archived soils, as well as storage duration, may alter the relative contribution to respiration from soil carbon pools with different cycling rates. We designed three experiments to assess air\uffe2\uff80\uff90drying and rewetting effects on \uffe2\uff88\uff8614C\uffe2\uff80\uff90CO2 with constant storage duration (Experiment 1), without storage (Experiment 2), and with variable storage duration (Experiment 3). We found that air\uffe2\uff80\uff90drying and rewetting led to small but significant (\uffce\uffb1\uffc2\uffa0&lt;\uffc2\uffa00.05) shifts in \uffe2\uff88\uff8614C\uffe2\uff80\uff90CO2 relative to undried controls in all experiments, with grassland soils responding more strongly than forest soils. Storage duration (4\uffe2\uff80\uff9314\uffc2\uffa0y) did not have a substantial effect. Mean differences (95% CIs) for experiments 1, 2, and 3 were: 23.3\uffe2\uff80\uffb0 (\uffc2\uffb16.6), 19.6\uffe2\uff80\uffb0 (\uffc2\uffb110.3), and 29.3\uffe2\uff80\uffb0 (\uffc2\uffb129.1) for grassland soils, versus \uffe2\uff88\uff9211.6\uffe2\uff80\uffb0 (\uffc2\uffb14.1), 12.7\uffe2\uff80\uffb0 (\uffc2\uffb18.5), and \uffe2\uff88\uff9224.2\uffe2\uff80\uffb0 (\uffc2\uffb113.2) for forest soils. Our results indicate that air\uffe2\uff80\uff90drying and rewetting soils mobilizes a slightly older pool of carbon that would otherwise be inaccessible to microbes, an effect that persists throughout the incubation. However, as the bias in \uffe2\uff88\uff8614C\uffe2\uff80\uff90CO2 from air\uffe2\uff80\uff90drying and rewetting is small, measuring \uffe2\uff88\uff8614C\uffe2\uff80\uff90CO2 in incubations of archived soils appears to be a promising technique for constraining soil carbon models.</p", "keywords": ["Dewey Decimal Classification::500 | Naturwissenschaften::550 | Geowissenschaften", "soil archives", "ddc:631.41", "04 agricultural and veterinary sciences", "incubation", "15. Life on land", "01 natural sciences", "climate change", "13. Climate action", "ddc:551.9", "ddc:550.724", "radiocarbon", "0401 agriculture", " forestry", " and fisheries", "soil carbon", "soil carbon modeling", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2020JG006119"}, {"href": "https://doi.org/10.1029/2020jg006119"}, {"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": "10.1029/2020jg006119", "name": "item", "description": "10.1029/2020jg006119", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1029/2020jg006119"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-09-01T00:00:00Z"}}, {"id": "10.1029/2020gb006672", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:15Z", "type": "Journal Article", "created": "2020-09-02", "title": "Assessing the Potential for Mobilization of Old Soil Carbon After Permafrost Thaw: A Synthesis of 14C Measurements From the Northern Permafrost Region", "description": "Abstract<p>The magnitude of future emissions of greenhouse gases from the northern permafrost region depends crucially on the mineralization of soil organic carbon (SOC) that has accumulated over millennia in these perennially frozen soils. Many recent studies have used radiocarbon (14C) to quantify the release of this \uffe2\uff80\uff9cold\uffe2\uff80\uff9d SOC as CO2 or CH4 to the atmosphere or as dissolved and particulate organic carbon (DOC and POC) to surface waters. We compiled ~1,900 14C measurements from 51 sites in the northern permafrost region to assess the vulnerability of thawing SOC in tundra, forest, peatland, lake, and river ecosystems. We found that growing season soil 14C\uffe2\uff80\uff90CO2 emissions generally had a modern (post\uffe2\uff80\uff901950s) signature, but that well\uffe2\uff80\uff90drained, oxic soils had increased CO2 emissions derived from older sources following recent thaw. The age of CO2 and CH4 emitted from lakes depended primarily on the age and quantity of SOC in sediments and on the mode of emission, and indicated substantial losses of previously frozen SOC from actively expanding thermokarst lakes. Increased fluvial export of aged DOC and POC occurred from sites where permafrost thaw caused soil thermal erosion. There was limited evidence supporting release of previously frozen SOC as CO2, CH4, and DOC from thawing peatlands with anoxic soils. This synthesis thus suggests widespread but not universal release of permafrost SOC following thaw. We show that different definitions of \uffe2\uff80\uff9cold\uffe2\uff80\uff9d sources among studies hamper the comparison of vulnerability of permafrost SOC across ecosystems and disturbances. We also highlight opportunities for future 14C studies in the permafrost region.</p", "keywords": ["particulate organic carbon", "[SDE] Environmental Sciences", "0301 basic medicine", "551.9", "550", "permafrost thaw", "methane", "500", "carbon dioxide", "15. Life on land", "551", "dissolved organic carbon", "01 natural sciences", "[SDE.MCG] Environmental Sciences/Global Changes", "03 medical and health sciences", "13. Climate action", "radiocarbon", "0105 earth and related environmental sciences"]}, "links": [{"href": "http://livrepository.liverpool.ac.uk/3106184/1/2020%20Estop%E2%80%90Aragon%C3%A9s%20et%20al%2C%20GBC%20-%20Arctic%2014C%20synthesis.pdf"}, {"href": "https://eprints.gla.ac.uk/222767/13/222767.pdf"}, {"href": "https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2020GB006672"}, {"href": "https://doi.org/10.1029/2020gb006672"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Biogeochemical%20Cycles", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1029/2020gb006672", "name": "item", "description": "10.1029/2020gb006672", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1029/2020gb006672"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-09-01T00:00:00Z"}}, {"id": "10.1029/2020gb006719", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:15Z", "type": "Journal Article", "created": "2020-11-18", "title": "Stream Dissolved Organic Matter in Permafrost Regions Shows Surprising Compositional Similarities but Negative Priming and Nutrient Effects", "description": "Abstract<p>Permafrost degradation is delivering bioavailable dissolved organic matter (DOM) and inorganic nutrients to surface water networks. While these permafrost subsidies represent a small portion of total fluvial DOM and nutrient fluxes, they could influence food webs and net ecosystem carbon balance via priming or nutrient effects that destabilize background DOM. We investigated how addition of biolabile carbon (acetate) and inorganic nutrients (nitrogen and phosphorus) affected DOM decomposition with 28\uffe2\uff80\uff90day incubations. We incubated late\uffe2\uff80\uff90summer stream water from 23 locations nested in seven northern or high\uffe2\uff80\uff90altitude regions in Asia, Europe, and North America. DOM loss ranged from 3% to 52%, showing a variety of longitudinal patterns within stream networks. DOM optical properties varied widely, but DOM showed compositional similarity based on Fourier transform ion cyclotron resonance mass spectrometry (FT\uffe2\uff80\uff90ICR MS) analysis. Addition of acetate and nutrients decreased bulk DOM mineralization (i.e., negative priming), with more negative effects on biodegradable DOM but neutral or positive effects on stable DOM. Unexpectedly, acetate and nutrients triggered breakdown of colored DOM (CDOM), with median decreases of 1.6% in the control and 22% in the amended treatment. Additionally, the uptake of added acetate was strongly limited by nutrient availability across sites. These findings suggest that biolabile DOM and nutrients released from degrading permafrost may decrease background DOM mineralization but alter stoichiometry and light conditions in receiving waterbodies. We conclude that priming and nutrient effects are coupled in northern aquatic ecosystems and that quantifying two\uffe2\uff80\uff90way interactions between DOM properties and environmental conditions could resolve conflicting observations about the drivers of DOM in permafrost zone waterways.</p>", "keywords": ["0106 biological sciences", "550", "permafrost regions", "thermokarst", "vaikutukset", "ta1171", "geosciences", "ikirouta", "carbon cycling", "551", "ravinteet", "01 natural sciences", "nutrients", "cryosphere and high-latitude processes", "Biology", "Research Articles", "organic matter", "0105 earth and related environmental sciences", "compositional similarities", "nutrients and nutrient cycling", "hiilen kierto", "ravinteiden kierr\u00e4tys", "15. Life on land", "rivers", "6. Clean water", "nutrient effects", "13. Climate action", "orgaaninen aines", "1171 Geotieteet", "SDG 6 - Clean Water and Sanitation", "joet", "permafrost"]}, "links": [{"href": "https://digitalcommons.usu.edu/context/biology_facpub/article/2820/viewcontent/2020GB006719.pdf"}, {"href": "https://doi.org/10.1029/2020gb006719"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Biogeochemical%20Cycles", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1029/2020gb006719", "name": "item", "description": "10.1029/2020gb006719", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1029/2020gb006719"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-01-01T00:00:00Z"}}, {"id": "10.1186/s12932-020-00066-8", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:19:59Z", "type": "Journal Article", "created": "2020-02-14", "title": "Effects of metal cation substitution on hexavalent chromium reduction by green rust", "description": "Abstract<p>Chromium contamination is a serious environmental issue in areas affected by leather tanning and metal plating, and green rust sulfate has been tested extensively as a potential material for in situ chemical reduction of hexavalent chromium in groundwater. Reported products and mechanisms for the reaction have varied, most likely because of green rust\uffe2\uff80\uff99s layered structure, as reduction at outer and interlayer surfaces might produce different reaction products with variable stabilities. Based on studies of Cr(III) oxidation by biogenic Mn (IV) oxides, Cr mobility in oxic soils is controlled by the solubility of the Cr(III)-bearing phase. Therefore, careful engineering of green rust properties, i.e., crystal/particle size, morphology, structure, and electron availability, is essential for its optimization as a remediation reagent. In the present study, pure green rust sulfate and green rust sulfate with Al, Mg and Zn substitutions were synthesized and reacted with identical chromate (CrO42\uffe2\uff88\uff92) solutions. The reaction products were characterized by X-ray diffraction, pair distribution function analysis, X-ray absorption spectroscopy and transmission electron microscopy and treated with synthetic \uffce\uffb4-MnO2 to assess how easily Cr(III) in the products could be oxidized. It was found that Mg substitution had the most beneficial effect on Cr lability in the product. Less than 2.5% of the Cr(III) present in the reacted Mg-GR was reoxidized by \uffce\uffb4-MnO2 within 14\uffc2\uffa0days, and the particle structure and Cr speciation observed during X-ray scattering and absorption analyses of this product suggested that Cr(VI) was reduced in its interlayer. Reduction in the interlayer lead to the linkage of newly-formed Cr(III) to hydroxyl groups in the adjacent octahedral layers, which resulted in increased structural coherency between these layers, distinctive rim domains, sequestration of Cr(III) in insoluble Fe oxide bonding environments resistant to reoxidation and partial transformation to Cr(III)-substituted feroxyhyte. Based on the results of this study of hexavalent chromium reduction by green rust sulfate and other studies, further improvements can also be made to this remediation technique by reacting chromate with a large excess of green rust sulfate, which provides excess Fe(II) that can catalyze transformation to more crystalline iron oxides, and synthesis of the reactant under alkaline conditions, which has been shown to favor chromium reduction in the interlayer of Fe(II)-bearing phyllosilicates.</p>", "keywords": ["Chromium", "550", "Geography & travel", "Remediation", "02 engineering and technology", "910", "551", "01 natural sciences", "Chromium", " Green rust", " X-ray absorption spectroscopy", " Remediation", "remediation", "500 Naturwissenschaften und Mathematik::550 Geowissenschaften", " Geologie::551 Geologie", " Hydrologie", " Meteorologie", "GE1-350", "info:eu-repo/classification/ddc/910", "QD1-999", "0105 earth and related environmental sciences", "Green rust", "X-ray absorption spectroscopy", "540", "ddc:910", "6. Clean water", "Environmental sciences", "Chemistry", "green rust", "13. Climate action", "chromium", "500 Naturwissenschaften und Mathematik::540 Chemie::540 Chemie und zugeordnete Wissenschaften", "0210 nano-technology", "Research Article"]}, "links": [{"href": "https://eprints.whiterose.ac.uk/158695/1/s12932-020-00066-8.pdf"}, {"href": "http://link.springer.com/content/pdf/10.1186/s12932-020-00066-8.pdf"}, {"href": "https://doi.org/10.1186/s12932-020-00066-8"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Geochemical%20Transactions", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1186/s12932-020-00066-8", "name": "item", "description": "10.1186/s12932-020-00066-8", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1186/s12932-020-00066-8"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-02-14T00:00:00Z"}}, {"id": "10.1029/2023jd040657", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:17Z", "type": "Journal Article", "created": "2024-06-11", "title": "Impact of Dust Source Patchiness on the Existence of a Constant Dust Flux Layer During Aeolian Erosion Events", "description": "Abstract<p>Dust emission fluxes during wind soil erosion are usually estimated using a dust concentration vertical gradient, by assuming a constant dust flux layer between the surface and the dust measurement levels. Here, we investigate the existence of this layer during erosion events recorded in Iceland and Jordan. Size\uffe2\uff80\uff90resolved dust fluxes were estimated at three levels between 2 and 4\uffc2\uffa0m using the eddy\uffe2\uff80\uff90covariance method. Dust fluxes were found mainly constant only between the two upper levels in Iceland, the lower dust flux being often stronger and richer in coarse particles, while dust fluxes in Jordan were nearly constant across all levels. The wind dynamics could not explain the absence of a constant dust flux layer in Iceland. We show that the presence of stationary dust source patches in Iceland, related to surface humidity, created a non\uffe2\uff80\uff90uniform dust layer near the surface, named dust roughness sublayer (DRSL), where individual plumes behind each patch interact but do not fully mix. The lowest dust measurement level was probably located within this sublayer while the upper ones were located above, such that there the emitted dust became spatially well\uffe2\uff80\uff90mixed. This explains near the surface in Iceland, the more intermittent dust concentration, its low correlation with the dust concentrations above, and the richer dust flux in coarse particles due to their lower deposition contribution. Our findings highlight the importance of estimating dust fluxes above a dust blending height whose characteristics depend on the dust source patchiness caused by surface humidity or the presence of sparse non\uffe2\uff80\uff90erosive elements.</p", "keywords": ["[SDE] Environmental Sciences", "Aeolian erosion events", "550", "dust flux", "Soil wind erosion", "Ensure access to affordable", " reliable", " sustainable and modern energy for all", "Dust flux layer", "0207 environmental engineering", "02 engineering and technology", "Constant flux layer", "\u00c0rees tem\u00e0tiques de la UPC::Enginyeria agroaliment\u00e0ria::Ci\u00e8ncies de la terra i de la vida", "551", "01 natural sciences", "Make cities and human settlements inclusive", " safe", " resilient and sustainable", "Dust flux", "Simulaci\u00f3 per ordinador", "Atmospheric surface layer", "size distribution", "Climate science", "500 Naturwissenschaften und Mathematik::550 Geowissenschaften", " Geologie::551 Geologie", " Hydrologie", " Meteorologie", "0105 earth and related environmental sciences", "info:eu-repo/classification/ddc/550", "ddc:550", "Size distribution", "15. Life on land", "520", "Physical sciences", "Earth sciences", "13. Climate action", "[SDE]Environmental Sciences", "Soil erosion", "soil wind erosion", "constant flux layer"]}, "links": [{"href": "https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2023JD040657"}, {"href": "https://hal.inrae.fr/hal-04618242/file/JGR%20Atmospheres%20-%202024%20-%20Dupont%20-%20Impact%20of%20Dust%20Source%20Patchiness%20on%20the%20Existence%20of%20a%20Constant%20Dust%20Flux%20Layer%20During.pdf"}, {"href": "https://doi.org/10.1029/2023jd040657"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Geophysical%20Research%3A%20Atmospheres", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1029/2023jd040657", "name": "item", "description": "10.1029/2023jd040657", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1029/2023jd040657"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-06-11T00:00:00Z"}}, {"id": "10.1029/2023JG007688", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:18:17Z", "type": "Journal Article", "created": "2023-12-15", "title": "Links Between Stream Water Nitrogen and Terrestrial Vegetation in Northeast Greenland", "description": "Abstract<p>The Arctic is warming and significant changes to the landscape, including increased vegetative cover (\uffe2\uff80\uff9cgreening\uffe2\uff80\uff9d), are expected in the near future. These landscape changes may alter nitrogen (N) availability in terrestrial, stream, and coastal ecosystems, where production is often N limited, but the exact changes in nutrient cycling are uncertain. Here, we analyzed the relationship between vegetation greenness (i.e., NDVI) and dissolved inorganic (DIN) and organic (DON) concentrations in streams draining 14 headwater catchments (mean 3.6\uffc2\uffa0km2, range 0.4\uffe2\uff80\uff9311\uffc2\uffa0km2) across three samplings in the Zackenberg area, Northeast Greenland. We found large variation in DIN and DON concentrations across the sampled streams. We further show that this variation is correlated to water temperature and catchment NDVI, such that increased vegetation greenness and temperature correlated with lower DIN, and increased greenness also correlated with higher DON concentrations in streams. The results suggest that increased terrestrial vegetation due to rising air temperature could substantially alter dissolved N concentrations and form in streams, with potentially cascading impacts on coastal areas.</p", "keywords": ["[SDU.OCEAN]Sciences of the Universe [physics]/Ocean", "570", "Atmosphere", "[SDU.OCEAN] Sciences of the Universe [physics]/Ocean", " Atmosphere", "greening", "stream", "Greenland", "15. Life on land", "551", "01 natural sciences", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "nitrogen", "13. Climate action", "high Arctic", "14. Life underwater", "[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces", "environment", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1029/2023JG007688"}, {"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": "10.1029/2023JG007688", "name": "item", "description": "10.1029/2023JG007688", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1029/2023JG007688"}, {"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": "10.1029/2023jg007688", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:18:17Z", "type": "Journal Article", "created": "2023-12-15", "title": "Links Between Stream Water Nitrogen and Terrestrial Vegetation in Northeast Greenland", "description": "Abstract<p>The Arctic is warming and significant changes to the landscape, including increased vegetative cover (\uffe2\uff80\uff9cgreening\uffe2\uff80\uff9d), are expected in the near future. These landscape changes may alter nitrogen (N) availability in terrestrial, stream, and coastal ecosystems, where production is often N limited, but the exact changes in nutrient cycling are uncertain. Here, we analyzed the relationship between vegetation greenness (i.e., NDVI) and dissolved inorganic (DIN) and organic (DON) concentrations in streams draining 14 headwater catchments (mean 3.6\uffc2\uffa0km2, range 0.4\uffe2\uff80\uff9311\uffc2\uffa0km2) across three samplings in the Zackenberg area, Northeast Greenland. We found large variation in DIN and DON concentrations across the sampled streams. We further show that this variation is correlated to water temperature and catchment NDVI, such that increased vegetation greenness and temperature correlated with lower DIN, and increased greenness also correlated with higher DON concentrations in streams. The results suggest that increased terrestrial vegetation due to rising air temperature could substantially alter dissolved N concentrations and form in streams, with potentially cascading impacts on coastal areas.</p", "keywords": ["[SDU.OCEAN]Sciences of the Universe [physics]/Ocean", "570", "Atmosphere", "[SDU.OCEAN] Sciences of the Universe [physics]/Ocean", " Atmosphere", "greening", "stream", "Greenland", "15. Life on land", "551", "01 natural sciences", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "nitrogen", "13. Climate action", "high Arctic", "14. Life underwater", "[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces", "environment", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1029/2023jg007688"}, {"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": "10.1029/2023jg007688", "name": "item", "description": "10.1029/2023jg007688", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1029/2023jg007688"}, {"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": "10.1029/2024JG008226", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:17Z", "type": "Journal Article", "created": "2025-01-02", "title": "Terrestrial Organic Matter Contributes to CO2 Production From Siberian Shelf Sediments", "description": "Abstract<p>Arctic climate warming is causing permafrost thaw and erosion, which may lead to enhanced inputs of terrestrial organic matter into Arctic Ocean shelf sediments. Degradation of terrestrial organic matter in sediments might contribute to carbon dioxide production and bottom water acidification. Yet, the degradability of organic matter in shallow Arctic Ocean sediments, as well as the contribution of terrestrial input, is poorly quantified. Here, potential organic matter degradation rates were investigated for 16 surface sediments from the Kara Sea, Laptev Sea, and the western East Siberian Sea and compared with physicochemical sediment properties including molecular biomarkers, stable and radioactive carbon isotopes, and grain size. Aerobic oxygen and carbon dioxide fluxes, measured in laboratory incubations of sediment slurry, showed high spatial variability and correlated significantly with organic carbon content as well as with the amount and degradation state of terrestrial organic matter. The dependency on terrestrial organic matter declined with increasing distance from land, indicating that the presence of terrestrial organic matter is likely a constraining factor for organic matter degradation in shallow shelf seas. However, sediment oxygen consumption rates, measured in incubations of intact sediment cores, also exhibited substantial spatial variability but were not related to organic carbon content or terrestrial influence. Oxygen consumption of intact sediments may be more strongly influenced by in situ redox conditions. Together with previous observations, our findings support that terrestrial organic matter is easily degradable in shelf sea sediments and might substantially contribute to aerobic carbon dioxide production and oxygen consumption.</p", "keywords": ["550", "Laptev Sea", "Kara Sea", "sediment O2 consumption", "551", "sediment CO2 release", "molecular biomarkers", "East Siberian Sea"]}, "links": [{"href": "https://doi.org/10.1029/2024JG008226"}, {"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": "10.1029/2024JG008226", "name": "item", "description": "10.1029/2024JG008226", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1029/2024JG008226"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-01-01T00:00:00Z"}}, {"id": "10.1029/2024jg008226", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:17Z", "type": "Journal Article", "created": "2025-01-02", "title": "Terrestrial Organic Matter Contributes to CO2 Production From Siberian Shelf Sediments", "description": "Abstract<p>Arctic climate warming is causing permafrost thaw and erosion, which may lead to enhanced inputs of terrestrial organic matter into Arctic Ocean shelf sediments. Degradation of terrestrial organic matter in sediments might contribute to carbon dioxide production and bottom water acidification. Yet, the degradability of organic matter in shallow Arctic Ocean sediments, as well as the contribution of terrestrial input, is poorly quantified. Here, potential organic matter degradation rates were investigated for 16 surface sediments from the Kara Sea, Laptev Sea, and the western East Siberian Sea and compared with physicochemical sediment properties including molecular biomarkers, stable and radioactive carbon isotopes, and grain size. Aerobic oxygen and carbon dioxide fluxes, measured in laboratory incubations of sediment slurry, showed high spatial variability and correlated significantly with organic carbon content as well as with the amount and degradation state of terrestrial organic matter. The dependency on terrestrial organic matter declined with increasing distance from land, indicating that the presence of terrestrial organic matter is likely a constraining factor for organic matter degradation in shallow shelf seas. However, sediment oxygen consumption rates, measured in incubations of intact sediment cores, also exhibited substantial spatial variability but were not related to organic carbon content or terrestrial influence. Oxygen consumption of intact sediments may be more strongly influenced by in situ redox conditions. Together with previous observations, our findings support that terrestrial organic matter is easily degradable in shelf sea sediments and might substantially contribute to aerobic carbon dioxide production and oxygen consumption.</p", "keywords": ["550", "Laptev Sea", "Kara Sea", "sediment O2 consumption", "551", "sediment CO2 release", "molecular biomarkers", "East Siberian Sea"]}, "links": [{"href": "https://doi.org/10.1029/2024jg008226"}, {"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": "10.1029/2024jg008226", "name": "item", "description": "10.1029/2024jg008226", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1029/2024jg008226"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-01-01T00:00:00Z"}}, {"id": "10.1038/s41467-017-00192-5", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:21Z", "type": "Journal Article", "created": "2017-08-02", "title": "Zhamanshin astrobleme provides evidence for carbonaceous chondrite and post-impact exchange between ejecta and Earth\u2019s atmosphere", "description": "Abstract<p>Chemical fingerprints of impacts are usually compromised by extreme conditions in the impact plume, and the contribution of projectile matter to impactites does not often exceed a fraction of per cent. Here we use chromium and oxygen isotopes to identify the impactor and impact-plume processes for Zhamanshin astrobleme, Kazakhstan. \uffce\uffb554Cr values up to 1.54 in irghizites, part of the fallback ejecta, represent the54Cr-rich extremity of the Solar System range and suggest a CI-like chondrite impactor. \uffce\uff9417O values as low as \uffe2\uff88\uff920.22\uffe2\uff80\uffb0 in irghizites, however, are incompatible with a CI-like impactor. We suggest that the observed17O depletion in irghizites relative to the terrestrial range is caused by partial isotope exchange with atmospheric oxygen (\uffce\uff9417O\uffe2\uff80\uff89=\uffe2\uff80\uff89\uffe2\uff88\uff920.47\uffe2\uff80\uffb0) following material ejection. In contrast, combined \uffce\uff9417O\uffe2\uff80\uff93\uffce\uffb554Cr data for central European tektites (distal ejecta) fall into the terrestrial range and neither impactor fingerprint nor oxygen isotope exchange with the atmosphere are indicated.</p>", "keywords": ["OXYGEN-ISOTOPE COMPOSITION", "NORDLINGER RIES IMPACT", "ORIGIN", "FRACTIONATION", "carbonaceous chondrite; post-impact exchange; ejecta; Earth\u2019s atmosphere", "Science", "Q", "TARGET ROCKS", "[SDU.ASTR.EP] Sciences of the Universe [physics]/Astrophysics [astro-ph]/Earth and Planetary Astrophysics [astro-ph.EP]", "551", "01 natural sciences", "Article", "IVORY-COAST TEKTITES", "13. Climate action", "CRATER", "GLASSES", "ELEMENTS", "WATER", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://www.nature.com/articles/s41467-017-00192-5.pdf"}, {"href": "https://doi.org/10.1038/s41467-017-00192-5"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature%20Communications", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s41467-017-00192-5", "name": "item", "description": "10.1038/s41467-017-00192-5", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41467-017-00192-5"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-08-09T00:00:00Z"}}, {"id": "10.1038/s41467-022-29161-3", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:23Z", "type": "Journal Article", "created": "2022-03-17", "title": "Structure and function of the soil microbiome underlying N2O emissions from global wetlands", "description": "Abstract<p>Wetland soils are the greatest source of nitrous oxide (N2O), a critical greenhouse gas and ozone depleter released by microbes. Yet, microbial players and processes underlying the N2O emissions from wetland soils are poorly understood. Using in situ N2O measurements and by determining the structure and potential functional of microbial communities in 645 wetland soil samples globally, we examined the potential role of archaea, bacteria, and fungi in nitrogen (N) cycling and N2O emissions. We show that N2O emissions are higher in drained and warm wetland soils, and are correlated with functional diversity of microbes. We further provide evidence that despite their much lower abundance compared to bacteria, nitrifying archaeal abundance is a key factor explaining N2O emissions from wetland soils globally. Our data suggest that ongoing global warming and intensifying environmental change may boost archaeal nitrifiers, collectively transforming wetland soils to a greater source of N2O.</p", "keywords": ["0301 basic medicine", "570", "571", "Supplementary Data", "QH301 Biology", "Science", "General Biochemistry", "Genetics and Molecular Biology", "Nitrous Oxide", "General Physics and Astronomy", "Soil Science", "551", "852993", "Article", "DH150187", "QH301", "Greenhouse Gases", "Soil", "03 medical and health sciences", "948219", "General", "Soil Microbiology", "0303 health sciences", "Microbiota", "Q", "General Chemistry", "15. Life on land", "6. Clean water", "BBS/e/F/000Pr10355", "13. Climate action", "BB/r012490/1", "Wetlands", "Biotechnology and Biological Sciences Research Council (BBSRC)", "Other", "European Research Council"]}, "links": [{"href": "https://pub.epsilon.slu.se/27540/1/bahram-m-et-al-220412.pdf"}, {"href": "https://ueaeprints.uea.ac.uk/id/eprint/84269/1/Published_Version.pdf"}, {"href": "https://www.nature.com/articles/s41467-022-29161-3.pdf"}, {"href": "https://doi.org/10.1038/s41467-022-29161-3"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature%20Communications", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s41467-022-29161-3", "name": "item", "description": "10.1038/s41467-022-29161-3", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41467-022-29161-3"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-03-17T00:00:00Z"}}, {"id": "10.1038/s41558-024-02019-w", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:24Z", "type": "Journal Article", "created": "2024-06-07", "title": "Increasing numbers of global change stressors reduce soil carbon worldwide", "description": "Open AccessF.T.M. was supported by European Research Council grant number 647038 (BIODESERT), Generalitat Valenciana grant number CIDEGENT/2018/041, by the Spanish Ministry of Science and Innovation (grant numbers EUR2022-134048 and PID2020-116578RB-I00) and by the contract between ETH Zurich and University of Alicante \u201cMapping terrestrial ecosystem structure at the global scale\u201d. E.G. acknowledges funding from Generalitat Valenciana and Europen Social Fund (grant number APOSTD/2021/188). F.T.M. also acknowledges support from the King Abdullah University of Science and Technology (KAUST) and the KAUST Climate and Livability Initiative. T.S.-S., A.G. and M.D.-B. are supported by grant number TED2021-130908B-C41 (URBANCHANGE). M.D.-B. was also supported by the European Research Council (ERC) grant number 647038 (BIODESERT), BES grant agreement number LRB17 1019 (MUSGONET), the innovation programme under Marie Sklodowska-Curie grant agreement number 702057 (CLIMIFUN), Ram\u00f3n y Cajal grant number RYC2018-025483-I, a project from the Spanish Ministry of Science and Innovation (grant number PID2020-115813RA-I00; SOIL4GROWTH) and project PAIDI 2020 from the Junta de Andaluc\u00eda (grant number P20_00879). C.W.M. acknowledges funding for the research provided by the NSF Postdoctoral Fellowship in Polar Regions Research (grant number 0852036), the German Science Foundation (DFG) for financial support in the frame of the \u201cInitiation of International Collaboration\u201d (grant number MU 3021/2-1) and funding within the DFG Priority Programme 1158 \u201cAntarctic Research with Comparable Investigations in Arctic Sea Ice Areas\u201d (grant number MU 3021/8-1). M.B. acknowledges funding from Spanish Ministry of Science and Innovation through a Ram\u00f3n y Cajal Fellowship (# RYC2021-031797-I).", "keywords": ["Ecolog\u00eda (Biolog\u00eda)", "550", "Global change stressors", "2410.05 Ecolog\u00eda Humana", "Climate-change ecology", "500", "551.588.7", "Edafolog\u00eda (Biolog\u00eda)", "Soil carbon", "631.4", "2511 Ciencias del Suelo (Edafolog\u00eda)", "Climate change", "2511.02 Biolog\u00eda de Suelos", "310308 - Terrestrial ecology", "502.1"]}, "links": [{"href": "https://doi.org/10.1038/s41558-024-02019-w"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature%20Climate%20Change", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s41558-024-02019-w", "name": "item", "description": "10.1038/s41558-024-02019-w", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41558-024-02019-w"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-06-07T00:00:00Z"}}, {"id": "10.1038/s41559-018-0694-0", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:24Z", "type": "Journal Article", "created": "2018-10-19", "title": "Isotopic evidence for oligotrophication of terrestrial ecosystems", "description": "Human societies depend on an Earth system that operates within a constrained range of nutrient availability, yet the recent trajectory of terrestrial nitrogen (N) availability is uncertain. Examining patterns of foliar N concentrations and isotope ratios (\u03b415N) from more than 43,000 samples acquired over 37\u2009years, here we show that foliar N concentration declined by 9% and foliar \u03b415N declined by 0.6-1.6\u2030. Examining patterns across different climate spaces, foliar \u03b415N declined across the entire range of mean annual temperature and mean annual precipitation tested. These results suggest declines in N supply relative to plant demand at the global scale. In all, there are now multiple lines of evidence of declining N availability in many unfertilized terrestrial ecosystems, including declines in \u03b415N of tree rings and leaves from herbarium samples over the past 75-150\u2009years. These patterns are consistent with the proposed consequences of elevated atmospheric carbon dioxide and longer growing seasons. These declines will limit future terrestrial carbon uptake and increase nutritional stress for herbivores.", "keywords": ["0106 biological sciences", "570", "Nitrogen", "[SDV]Life Sciences [q-bio]", "577", "terrestrial nitrogen", "Nutritional stress", "551", "01 natural sciences", "oligotrophication", "Isotopes", "https://purl.org/becyt/ford/1.6", "Terrestrial carbon uptake", "https://purl.org/becyt/ford/1", "Ecosystem", "580", "2. Zero hunger", "Nitrogen Isotopes", "terrestrial ecosystems", "isotopic", "Eutrophication", "Plants", "15. Life on land", "sylviculture", "Nitrogen; Nitrogen Isotopes; Plants; Ecosystem; Eutrophication", "[SDV] Life Sciences [q-bio]", "element cycles", "foliar", "13. Climate action", "nutrient availability"]}, "links": [{"href": "https://cris.unibo.it/bitstream/11585/704621/3/Craine_2018_isotopic.pdf"}, {"href": "https://www.nature.com/articles/s41559-018-0694-0.pdf"}, {"href": "https://doi.org/10.1038/s41559-018-0694-0"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature%20Ecology%20%26amp%3B%20Evolution", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s41559-018-0694-0", "name": "item", "description": "10.1038/s41559-018-0694-0", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41559-018-0694-0"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-10-22T00:00:00Z"}}, {"id": "10.1073/pnas.2309881120", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:45Z", "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": "10.3389/fmicb.2016.00525", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:21:25Z", "type": "Journal Article", "created": "2016-04-20", "title": "Belowground Response To Drought In A Tropical Forest Soil. I. Changes In Microbial Functional Potential And Metabolism", "description": "Global climate models predict a future of increased severity of drought in many tropical forests. Soil microbes are central to the balance of these systems as sources or sinks of atmospheric carbon (C), yet how they respond metabolically to drought is not well-understood. We simulated drought in the typically aseasonal Luquillo Experimental Forest, Puerto Rico, by intercepting precipitation falling through the forest canopy. This approach reduced soil moisture by 13% and water potential by 0.14 MPa (from -0.2 to -0.34). Previous results from this experiment have demonstrated that the diversity and composition of these soil microbial communities are sensitive to even small changes in soil water. Here, we show prolonged drought significantly alters the functional potential of the community and provokes a clear osmotic stress response, including the production of compatible solutes that increase intracellular C demand. Subsequently, a microbial population emerges with a greater capacity for extracellular enzyme production targeting macromolecular carbon. Significantly, some of these drought-induced functional shifts in the soil microbiota are attenuated by prior exposure to a short-term drought suggesting that acclimation may occur despite a lack of longer-term drought history.", "keywords": ["tropical forests", "0301 basic medicine", "2. Zero hunger", "570", "0303 health sciences", "Ecology", "Environmental Science and Management", "osmolytes", "drought", "Biological Sciences", "Medical microbiology", "15. Life on land", "551", "microbial ecology", "Microbiology", "QR1-502", "6. Clean water", "03 medical and health sciences", "13. Climate action", "Soil Sciences", "functional gene microarray"]}, "links": [{"href": "https://escholarship.org/content/qt5ts293tg/qt5ts293tg.pdf"}, {"href": "https://doi.org/10.3389/fmicb.2016.00525"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Frontiers%20in%20Microbiology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3389/fmicb.2016.00525", "name": "item", "description": "10.3389/fmicb.2016.00525", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3389/fmicb.2016.00525"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2016-04-20T00:00:00Z"}}, {"id": "10.1111/gcb.15496", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:19:22Z", "type": "Journal Article", "created": "2020-12-20", "title": "Topsoil organic matter build\u2010up in glacier forelands around the world", "description": "Abstract<p>Since the last glacial maximum, soil formation related to ice\uffe2\uff80\uff90cover shrinkage has been one major sink of carbon accumulating as soil organic matter (SOM), a phenomenon accelerated by the ongoing global warming. In recently deglacierized forelands, processes of SOM accumulation, including those that control carbon and nitrogen sequestration rates and biogeochemical stability of newly sequestered carbon, remain poorly understood. Here, we investigate the build\uffe2\uff80\uff90up of SOM during the initial stages (up to 410\uffc2\uffa0years) of topsoil development in 10 glacier forelands distributed on four continents. We test whether the net accumulation of SOM on glacier forelands (i) depends on the time since deglacierization and local climatic conditions (temperature and precipitation); (ii) is accompanied by a decrease in its stability and (iii) is mostly due to an increasing contribution of organic matter from plant origin. We measured total SOM concentration (carbon, nitrogen), its relative hydrogen/oxygen enrichment, stable isotopic (13C, 15N) and carbon functional groups (C\uffe2\uff80\uff90H, C=O, C=C) compositions, and its distribution in carbon pools of different thermal stability. We show that SOM content increases with time and is faster on forelands experiencing warmer climates. The build\uffe2\uff80\uff90up of SOM pools shows consistent trends across the studied soil chronosequences. During the first decades of soil development, the low amount of SOM is dominated by a thermally stable carbon pool with a small and highly thermolabile pool. The stability of SOM decreases with soil age at all sites, indicating that SOM storage is dominated by the accumulation of labile SOM during the first centuries of soil development, and suggesting plant carbon inputs to soil (SOM depleted in nitrogen, enriched in hydrogen and in aromatic carbon). Our findings highlight the potential vulnerability of SOM stocks from proglacial areas to decomposition and suggest that their durability largely depends on the relative contribution of carbon inputs from plants.</p>", "keywords": ["[SDV.BID.SPT]Life Sciences [q-bio]/Biodiversity/Systematics", "550", "Nitrogen", "Chronosequence", "551", "01 natural sciences", "[SDV.BV.BOT] Life Sciences [q-bio]/Vegetal Biology/Botanics", "Soil", "soil organic matter", "carbon stability; chronosequence; climate sensitivity; soil organic matter; topsoil development; Carbon; Nitrogen; Temperature; Ice Cover; Soil", "[SDV.BID.SPT] Life Sciences [q-bio]/Biodiversity/Systematics", " Phylogenetics and taxonomy", "[SDV.EE.ECO] Life Sciences [q-bio]/Ecology", " environment/Ecosystems", "Ice Cover", "topsoil development", "Carbon stability", "0105 earth and related environmental sciences", "2. Zero hunger", "Soil organic matter", "Temperature", "Phylogenetics and taxonomy", "04 agricultural and veterinary sciences", "[SDV.BV.BOT]Life Sciences [q-bio]/Vegetal Biology/Botanics", "15. Life on land", "Climate sensitivity", "Primary Research Articles", "Carbon", "chronosequence", "[SDE.BE] Environmental Sciences/Biodiversity and Ecology", "13. Climate action", "[SDV.EE.ECO]Life Sciences [q-bio]/Ecology", "[SDE]Environmental Sciences", "Topsoil development", "climate sensitivity", "carbon stability; chronosequence; climate sensitivity; soil organic matter; topsoil development;", "0401 agriculture", " forestry", " and fisheries", "[SDE.BE]Environmental Sciences/Biodiversity and Ecology", "environment/Ecosystems", "carbon stability"]}, "links": [{"href": "https://air.unimi.it/bitstream/2434/851691/2/khedim%202021%20submitted.pdf"}, {"href": "https://air.unimi.it/bitstream/2434/851691/3/khedim%202021%20Global%20Change%20Biol.pdf"}, {"href": "https://boa.unimib.it/bitstream/10281/300214/2/10281-300214_VoR.pdf"}, {"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.15496"}, {"href": "https://doi.org/10.1111/gcb.15496"}, {"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.15496", "name": "item", "description": "10.1111/gcb.15496", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcb.15496"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-01-16T00:00:00Z"}}, {"id": "10.1098/rstb.2017.0302", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:19:07Z", "type": "Journal Article", "created": "2018-10-08", "title": "Tropical land carbon cycle responses to 2015/16 El Ni\u00f1o as recorded by atmospheric greenhouse gas and remote sensing data", "description": "<p>             The outstanding tropical land climate characteristic over the past decades is rapid warming, with no significant large-scale precipitation trends. This warming is expected to continue but the effects on tropical vegetation are unknown. El Ni\uffc3\uffb1o-related heat peaks may provide a test bed for a future hotter world. Here we analyse tropical land carbon cycle responses to the 2015/16 El Ni\uffc3\uffb1o heat and drought anomalies using an atmospheric transport inversion. Based on the global atmospheric CO             2             and fossil fuel emission records, we find no obvious signs of anomalously large carbon release compared with earlier El Ni\uffc3\uffb1o events, suggesting resilience of tropical vegetation. We find roughly equal net carbon release anomalies from Amazonia and tropical Africa, approximately 0.5 PgC each, and smaller carbon release anomalies from tropical East Asia and southern Africa. Atmospheric CO anomalies reveal substantial fire carbon release from tropical East Asia peaking in October 2015 while fires contribute only a minor amount to the Amazonian carbon flux anomaly. Anomalously large Amazonian carbon flux release is consistent with downregulation of primary productivity during peak negative near-surface water anomaly (October 2015 to March 2016) as diagnosed by solar-induced fluorescence. Finally, we find an unexpected anomalous positive flux to the atmosphere from tropical Africa early in 2016, coincident with substantial CO release.           </p>           <p>This article is part of a discussion meeting issue \uffe2\uff80\uff98The impact of the 2015/2016 El Ni\uffc3\uffb1o on the terrestrial tropical carbon cycle: patterns, mechanisms and implications\uffe2\uff80\uff99.</p>", "keywords": ["Life Sciences & Biomedicine - Other Topics", "FLUX", "0301 basic medicine", "Hot Temperature", "550", "551", "global warming", "01 natural sciences", "Carbon Cycle", "Greenhouse Gases", "03 medical and health sciences", "[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/Climatology", "CHEMICAL-TRANSPORT MODEL", "carbon cycle", "INVERSION", "Biology", "TEMPERATURE", "11 Medical and Health Sciences", "0105 earth and related environmental sciences", "tropical forests", "El Nino-Southern Oscillation", "Evolutionary Biology", "Tropical Climate", "Science & Technology", "Atmosphere", "PHOTOSYNTHESIS", "EQUATORIAL PACIFIC", "Articles", "06 Biological Sciences", "15. Life on land", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "6. Clean water", "Droughts", "[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology", "13. Climate action", "PRECIPITATION", "Remote Sensing Technology", "INDUCED CHLOROPHYLL FLUORESCENCE", "CO2", "[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces", "SENSITIVITY", "environment", "Life Sciences & Biomedicine", "fire"]}, "links": [{"href": "https://eprints.whiterose.ac.uk/135234/8/Tropical%20land%20carbon%20cycle%20responses%20to%202015/16%20El%20Ni%C3%B1o%20as%20recorded%20by%20atmospheric%20greenhouse%20gas%20and%20remote%20sensing%20data.pdf"}, {"href": "https://royalsocietypublishing.org/doi/pdf/10.1098/rstb.2017.0302"}, {"href": "https://doi.org/10.1098/rstb.2017.0302"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Philosophical%20Transactions%20of%20the%20Royal%20Society%20B%3A%20Biological%20Sciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1098/rstb.2017.0302", "name": "item", "description": "10.1098/rstb.2017.0302", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1098/rstb.2017.0302"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-10-08T00:00:00Z"}}, {"id": "10.3390/rs10060974", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:21:43Z", "type": "Journal Article", "created": "2018-06-19", "title": "Combining a Two Source Energy Balance Model Driven by MODIS and MSG-SEVIRI Products with an Aggregation Approach to Estimate Turbulent Fluxes over Sparse and Heterogeneous Vegetation in Sahel Region (Niger)", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Estimates of turbulent fluxes (i.e., sensible and latent heat fluxes H and LE) over heterogeneous surfaces is not an easy task. The heterogeneity caused by the contrast in vegetation, hydric and soil conditions can generate a large spatial variability in terms of surface\u2013atmosphere interactions. This study considered the issue of using a thermal-based two-source energy model (TSEB) driven by MODIS (Moderate resolution Imaging Spectroradiometer) and MSG (Meteosat Second Generation) observations in conjunction with an aggregation scheme to derive area-averaged H and LE over a heterogeneous watershed in Niamey, Niger (Wankama catchment). Data collected in the context of the African Monsoon Multidisciplinary Analysis (AMMA) program, including a scintillometry campaign, were used to test the proposed approach. The model predictions of area-averaged turbulent fluxes were compared to data acquired by a Large Aperture Scintillometer (LAS) set up over a transect about 3.2 km-long and spanning three vegetation types (millet, fallow and degraded shrubs). First, H and LE fluxes were estimated at the MSG-SEVIRI grid scale by neglecting explicitly the subpixel heterogeneity. Moreover, the impact of upscaling the model\u2019s inputs was investigated using in-situ input data and three aggregation schemes of increasing complexity based on MODIS products: a simple averaging of inputs at the MODIS resolution scale, another simple averaging scheme that considers scintillometer footprint extent, and the weighted average of inputs based on the footprint weighting function. The H and LE simulated using the footprint weighted method were more accurate than for the two other aggregation rules despite the heterogeneity of the landscape. The statistical values are: correlation coefficient (R) = 0.71, root mean square error (RMSE) = 63 W/m2 and mean bias error (MBE) = \u221223 W/m2 for H and an R = 0.82, RMSE = 88 W/m2 and MBE = 45 W/m2 for LE. This study opens perspectives for the monitoring of convective and evaporative fluxes over heterogeneous landscape based on medium resolution satellite products.</p></article>", "keywords": ["550", "Science", "0207 environmental engineering", "02 engineering and technology", "551", "7. Clean energy", "01 natural sciences", "TSEB model", "aggregation schemes", "scintillometry", "non-uniform and heterogeneous surfaces", "11. Sustainability", "heterogeneous surfaces", "0105 earth and related environmental sciences", "Q", "SEVIRI", "15. Life on land", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "6. Clean water", "3. Good health", "non-uniform and", "MODIS", "13. Climate action", "[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces", "regional surfaces fluxes", "environment"]}, "links": [{"href": "http://www.mdpi.com/2072-4292/10/6/974/pdf"}, {"href": "https://doi.org/10.3390/rs10060974"}, {"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/rs10060974", "name": "item", "description": "10.3390/rs10060974", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3390/rs10060974"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-06-19T00:00:00Z"}}, {"id": "10.1111/gcb.16394", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:19:23Z", "type": "Journal Article", "created": "2022-08-17", "title": "Lowering water table reduces carbon sink strength and carbon stocks in northern peatlands", "description": "Abstract<p>Peatlands at high latitudes have accumulated &gt;400\uffe2\uff80\uff89Pg carbon (C) because saturated soil and cold temperatures suppress C decomposition. This substantial amount of C in Arctic and Boreal peatlands is potentially subject to increased decomposition if the water table (WT) decreases due to climate change, including permafrost thaw\uffe2\uff80\uff90related drying. Here, we optimize a version of the Organizing Carbon and Hydrology In Dynamic Ecosystems model (ORCHIDEE\uffe2\uff80\uff90PCH4) using site\uffe2\uff80\uff90specific observations to investigate changes in CO2 and CH4 fluxes as well as C stock responses to an experimentally manipulated decrease of WT at six northern peatlands. The unmanipulated control peatlands, with the WT &lt;20\uffe2\uff80\uff89cm on average (seasonal max up to 45\uffe2\uff80\uff89cm) below the surface, currently act as C sinks in most years (58\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff8934\uffe2\uff80\uff89g C\uffe2\uff80\uff89m\uffe2\uff88\uff922\uffc2\uffa0year\uffe2\uff88\uff921; including 6\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff897\uffe2\uff80\uff89g C\uffe2\uff80\uff93CH4 m\uffe2\uff88\uff922\uffc2\uffa0year\uffe2\uff88\uff921 emission). We found, however, that lowering the WT by 10\uffe2\uff80\uff89cm reduced the CO2 sink by 13\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff8915\uffe2\uff80\uff89g\uffe2\uff80\uff89C\uffe2\uff80\uff89m\uffe2\uff88\uff922\uffc2\uffa0year\uffe2\uff88\uff921 and decreased CH4 emission by 4\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff894\uffe2\uff80\uff89g CH4 m\uffe2\uff88\uff922\uffc2\uffa0year\uffe2\uff88\uff921, thus accumulating less C over 100\uffe2\uff80\uff89years (0.2\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff890.2\uffe2\uff80\uff89kg\uffe2\uff80\uff89C\uffe2\uff80\uff89m\uffe2\uff88\uff922). Yet, the reduced emission of CH4, which has a larger greenhouse warming potential, resulted in a net decrease in greenhouse gas balance by 310\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff89360\uffe2\uff80\uff89g\uffe2\uff80\uff89CO2\uffe2\uff80\uff90eq\uffc2\uffa0m\uffe2\uff88\uff922\uffc2\uffa0year\uffe2\uff88\uff921. Peatlands with the initial WT close to the soil surface were more vulnerable to C loss: Non\uffe2\uff80\uff90permafrost peatlands lost &gt;2\uffe2\uff80\uff89kg\uffe2\uff80\uff89C\uffe2\uff80\uff89m\uffe2\uff88\uff922 over 100\uffe2\uff80\uff89years when WT is lowered by 50\uffe2\uff80\uff89cm, while permafrost peatlands temporally switched from C sinks to sources. These results highlight that reductions in C storage capacity in response to drying of northern peatlands are offset in part by reduced CH4 emissions, thus slightly reducing the positive carbon climate feedbacks of peatlands under a warmer and drier future climate scenario.</p", "keywords": ["570", "Carbon Sequestration", "permafrost thaw", "land surface model", "551", "01 natural sciences", "manipulation experiment", "Greenhouse Gases", "Soil", "[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces", " environment", "Groundwater", "Research Articles", "Ecosystem", "0105 earth and related environmental sciences", "[SDU.OCEAN]Sciences of the Universe [physics]/Ocean", " Atmosphere", "[SDU.OCEAN]Sciences of the Universe [physics]/Ocean", "Atmosphere", "[SDU.OCEAN] Sciences of the Universe [physics]/Ocean", " Atmosphere", "carbon stock", "high latitude", "Carbon Dioxide", "15. Life on land", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "Carbon", "carbon flux", "13. Climate action", "[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces", "environment", "Methane", "drainage"]}, "links": [{"href": "https://eprints.whiterose.ac.uk/190653/1/Global%20Change%20Biology%20-%202022%20-%20Kwon%20-%20Lowering%20water%20table%20reduces%20carbon%20sink%20strength%20and%20carbon%20stocks%20in%20northern.pdf"}, {"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.16394"}, {"href": "https://doi.org/10.1111/gcb.16394"}, {"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.16394", "name": "item", "description": "10.1111/gcb.16394", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcb.16394"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-08-30T00:00:00Z"}}, {"id": "10.1111/brv.12949", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:19:17Z", "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/gcb.13263", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:19:21Z", "type": "Journal Article", "created": "2016-03-01", "title": "Elevated Atmospheric [Co2] Can Dramatically Increase Wheat Yields In Semi-Arid Environments And Buffer Against Heat Waves", "description": "Abstract<p>Wheat production will be impacted by increasing concentration of atmospheric CO2 [CO2], which is expected to rise from about 400\uffc2\uffa0\uffce\uffbcmol\uffc2\uffa0mol\uffe2\uff88\uff921 in 2015 to 550\uffc2\uffa0\uffce\uffbcmol\uffc2\uffa0mol\uffe2\uff88\uff921 by 2050. Changes to plant physiology and crop responses from elevated [CO2] (e[CO2]) are well documented for some environments, but field\uffe2\uff80\uff90level responses in dryland Mediterranean environments with terminal drought and heat waves are scarce. The Australian Grains Free Air CO2 Enrichment facility was established to compare wheat (Triticum aestivum) growth and yield under ambient (~370\uffc2\uffa0\uffce\uffbcmol\uffe2\uff88\uff921 in 2007) and e[CO2] (550\uffc2\uffa0\uffce\uffbcmol\uffe2\uff88\uff921) in semi\uffe2\uff80\uff90arid environments. Experiments were undertaken at two dryland sites (Horsham and Walpeup) across three years with two cultivars, two sowing times and two irrigation treatments. Mean yield stimulation due to e[CO2] was 24% at Horsham and 53% at Walpeup, with some treatment responses greater than 70%, depending on environment. Under supplemental irrigation, e[CO2] stimulated yields at Horsham by 37% compared to 13% under rainfed conditions, showing that water limited growth and yield response to e[CO2]. Heat wave effects were ameliorated under e[CO2] as shown by reductions of 31% and 54% in screenings and 10% and 12% larger kernels (Horsham and Walpeup). Greatest yield stimulations occurred in the e[CO2] late sowing and heat stressed treatments, when supplied with more water. There were no clear differences in cultivar response due to e[CO2]. Multiple regression showed that yield response to e[CO2] depended on temperatures and water availability before and after anthesis. Thus, timing of temperature and water and the crop's ability to translocate carbohydrates to the grain postanthesis were all important in determining the e[CO2] response. The large responses to e[CO2] under dryland conditions have not been previously reported and underscore the need for field level research to provide mechanistic understanding for adapting crops to a changing climate.</p>", "keywords": ["heat wave", "Yield", "Agricultural Irrigation", "Hot Temperature", "Victoria", "Rain", "070302 Agronomy", "dryland", "551", "Dryland", "Heat wave", "Biomass", "Triticum", "free air CO2 enrichment", "2. Zero hunger", "elevated CO2", "Atmosphere", "Australian grains free air CO2 enrichment", "Water", "04 agricultural and veterinary sciences", "Carbon Dioxide", "15. Life on land", "wheat; yield", "6. Clean water", "Droughts", ": Australian grains free air CO2 enrichment", "13. Climate action", "Free air CO2 enrichment", "Wheat", "0401 agriculture", " forestry", " and fisheries", "Elevated CO2", "Edible Grain", "Environmental Monitoring"]}, "links": [{"href": "https://doi.org/10.1111/gcb.13263"}, {"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.13263", "name": "item", "description": "10.1111/gcb.13263", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcb.13263"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2016-03-31T00:00:00Z"}}, {"id": "10.1111/gcb.13268", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:19:21Z", "type": "Journal Article", "created": "2016-03-06", "title": "Using models to guide field experiments: a priori predictions for the CO 2 response of a nutrient- and water-limited native Eucalypt woodland", "description": "Abstract<p>The response of terrestrial ecosystems to rising atmospheric CO2 concentration (Ca), particularly under nutrient\uffe2\uff80\uff90limited conditions, is a major uncertainty in Earth System models. The Eucalyptus Free\uffe2\uff80\uff90Air CO2 Enrichment (EucFACE) experiment, recently established in a nutrient\uffe2\uff80\uff90 and water\uffe2\uff80\uff90limited woodland presents a unique opportunity to address this uncertainty, but can best do so if key model uncertainties have been identified in advance. We applied seven vegetation models, which have previously been comprehensively assessed against earlier forest FACE experiments, to simulate a priori possible outcomes from EucFACE. Our goals were to provide quantitative projections against which to evaluate data as they are collected, and to identify key measurements that should be made in the experiment to allow discrimination among alternative model assumptions in a postexperiment model intercomparison. Simulated responses of annual net primary productivity (NPP) to elevated Ca ranged from 0.5 to 25% across models. The simulated reduction of NPP during a low\uffe2\uff80\uff90rainfall year also varied widely, from 24 to 70%. Key processes where assumptions caused disagreement among models included nutrient limitations to growth; feedbacks to nutrient uptake; autotrophic respiration; and the impact of low soil moisture availability on plant processes. Knowledge of the causes of variation among models is now guiding data collection in the experiment, with the expectation that the experimental data can optimally inform future model improvements.</p>", "keywords": ["[SDE] Environmental Sciences", "550", "[SDV]Life Sciences [q-bio]", "Climate Change", "ecosystem model", "drought", "Forests", "551", "01 natural sciences", "Carbon Cycle", "XXXXXX - Unknown", "phosphorus", "Photosynthesis", "Ecosystem", "0105 earth and related environmental sciences", "580", "2. Zero hunger", "Eucalyptus", "droughts", "carbon dioxide", "Water", "Carbon Dioxide", "15. Life on land", "Eucalyptus tereticornis", "[SDV] Life Sciences [q-bio]", "13. Climate action", "[SDE]Environmental Sciences", "ecosystems"]}, "links": [{"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.13268"}, {"href": "https://doi.org/10.1111/gcb.13268"}, {"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.13268", "name": "item", "description": "10.1111/gcb.13268", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcb.13268"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2016-05-09T00:00:00Z"}}, {"id": "10.1175/bams-d-19-0316.1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:19:58Z", "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": "10.1111/j.1365-2486.2012.02692.x", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:19:33Z", "type": "Journal Article", "created": "2012-03-10", "title": "Four Years Of Experimental Climate Change Modifies The Microbial Drivers Of N2o Fluxes In An Upland Grassland Ecosystem", "description": "Abstract<p>Emissions of the trace gas nitrous oxide (N2O) play an important role for the greenhouse effect and stratospheric ozone depletion, but the impacts of climate change on N2O fluxes and the underlying microbial drivers remain unclear. The aim of this study was to determine the effects of sustained climate change on field N2O fluxes and associated microbial enzymatic activities, microbial population abundance and community diversity in an extensively managed, upland grassland. We recorded N2O fluxes, nitrification and denitrification, microbial population size involved in these processes and community structure of nitrite reducers (nirK) in a grassland exposed for 4\uffc2\uffa0years to elevated atmospheric CO2 (+200\uffc2\uffa0ppm), elevated temperature (+3.5\uffc2\uffa0\uffc2\uffb0C) and reduction of summer precipitations (\uffe2\uff88\uff9220%) as part of a long\uffe2\uff80\uff90term, multifactor climate change experiment. Our results showed that both warming and simultaneous application of warming, summer drought and elevated CO2 had a positive effect on N2O fluxes, nitrification, N2O release by denitrification and the population size of N2O reducers and NH4 oxidizers. In situ N2O fluxes showed a stronger correlation with microbial population size under warmed conditions compared with the control site. Specific lineages of nirK denitrifier communities responded significantly to temperature. In addition, nirK community composition showed significant changes in response to drought. Path analysis explained more than 85% of in situ N2O fluxes variance by soil temperature, denitrification activity and specific denitrifying lineages. Overall, our study underlines that climate\uffe2\uff80\uff90induced changes in grassland N2O emissions reflect climate\uffe2\uff80\uff90induced changes in microbial community structure, which in turn modify microbial processes.</p>", "keywords": ["d\u00e9nitrification", "Biodiversit\u00e9 et Ecologie", "551", "AOB", "diversity", "Biodiversity and Ecology", "nosZ", "[SDV.EE.ECO] Life Sciences [q-bio]/Ecology", " environment/Ecosystems", "nirK", "Milieux et Changements globaux", "2. Zero hunger", "changement climatique", "denitrification", "grasslands", "N2O", "prairie", "04 agricultural and veterinary sciences", "15. Life on land", "nitrification", "6. Clean water", "[SDE.BE] Environmental Sciences/Biodiversity and Ecology", "climate change", "13. Climate action", "[SDV.EE.ECO]Life Sciences [q-bio]/Ecology", "AOB;changement climatique;d\u00e9nitrification;diversit\u00e9;prairie;N2O;nitrification", "0401 agriculture", " forestry", " and fisheries", "[SDE.BE]Environmental Sciences/Biodiversity and Ecology", "environment/Ecosystems"]}, "links": [{"href": "https://hal.science/halsde-00722571/file/Cantarel_gcb12_1.pdf"}, {"href": "https://doi.org/10.1111/j.1365-2486.2012.02692.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.1365-2486.2012.02692.x", "name": "item", "description": "10.1111/j.1365-2486.2012.02692.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/j.1365-2486.2012.02692.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2012-05-08T00:00:00Z"}}, {"id": "10.13031/trans.56.10215", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:20:03Z", "type": "Journal Article", "created": "2013-11-20", "title": "Impact Of Water And Nitrogen Management Strategies On Maize Yield And Water Productivity Indices Under Linear-Move Sprinkler Irrigation", "description": "Abstract.    With uncertainty in future irrigation water availability and regulations on nutrient application amounts, experimentally determined effects of \u00e2\u20ac\u0153controllable\u00e2\u20ac\u009d management strategies such as nitrogen (N), water, and their combination on crop water productivity (CWP, also known as crop water use efficiency) and actual evapotranspiration (ET a ) are essential. The effects of various N application rates (0, 84, 140, 196, and 252 kg ha -1 ) under fully irrigated (FIT), limited irrigation (75% FIT), and rainfed conditions on maize (Zea mays L.) yield and various CWP indices were investigated in 2011 and 2012 growing seasons under linear-move sprinkler irrigation in south central Nebraska. CWP was presented as crop water use efficiency (CWUE), irrigation water use efficiency (IWUE), and evapotranspiration water use efficiency (ETWUE). The seasonal rainfall amounts in 2011 and 2012 were 371 mm and 296 mm, respectively, as compared with the long-term average of 469 mm. Two experimental seasons were contrasted with extreme warmer temperatures, greater solar radiation, and lower rainfall in 2012. Maximum grain yield of 12.68 metric tons ha -1  and 14.42 tons ha -1  was observed in 2011 and 2012, respectively, under the fully irrigated and 252 kg N ha -1  treatment. Grain yield was linearly related to ET a  and curvilinearly related to N and irrigation application amounts. Lower N treatments were more susceptible to interannual effects on the grain yield response to irrigation water amount. CWUE ranged from 1.52 kg m -3  (FIT and 84 kg N ha -1 ) to 2.58 kg m -3  (rainfed and 196 kg N ha -1 ) with an average of 2.15 kg m -3  in 2011, and from 1.49 kg m -3  (FIT and 0 kg N ha -1 ) to 2.72 kg m -3  (rainfed and 252 kg N ha -1 ) with an average of 2.33 kg m -3  in 2012. CWUE had a positive quadratic relationship with N application amount and decreased with both the presence and amount of irrigation at a given N application amount. The maximum IWUE for 75% FIT and FIT in 2011 was 1.80 kg m -3  (252 kg N ha -1 ) and 1.51 kg m -3  (252 kg N ha -1 ), respectively, whereas in 2012 the maximum IWUE values were 1.40 kg m -3  (196 kg N ha -1 ) and 1.78 kg m -3  (252 kg N ha -1 ), respectively. A curvilinear relationship was observed between IWUE and N application amount. An optimal N application amount of 196 kg ha -1  was identified for the pooled data to maximize the increase in grain yield above rainfed conditions per unit of applied irrigation water under limited irrigation management practices. In 2011, ETWUE ranged from 0.22 kg m -3  (140 kg N ha -1 ) to 1.46 kg m -3  (196 kg N ha -1 ) and from -0.21 kg m -3  (84 kg N ha -1 ) to 3.74 kg m -3  (252 kg N ha -1 ) for 75% FIT and FIT, respectively, whereas in 2012 ETWUE ranged from -0.07 kg m -3  (0 kg N ha -1 ) to 1.87 kg m -3  (252 kg N ha -1 ) and from -0.14 kg m -3  (0 kg N ha -1 ) to 3.65 kg m -3  (196 kg N ha -1 ) for 75% FIT and FIT, respectively. The results support that there is an optimal N level for each irrigation regime and, in general, lower N application amounts are required to reach maximum productivity (e.g., CWUE) under limited and rainfed conditions as compared with the FIT. In other words, there is an optimal N application amount to maximize the effectiveness of irrigation water on increasing grain yield above rainfed yields. The optimal N level for maximum productivity varied not only between the irrigation levels, but also exhibited interannual variability for the same irrigation level, indicating that these variables are impacted by the climatic conditions.", "keywords": ["Civil and Environmental Engineering", "2. Zero hunger", "0106 biological sciences", "Irrigation water use efficiency", "Environmental Engineering", "Evapotranspiration", "Bioresource and Agricultural Engineering", "Limited irrigation", "Nitrogen", "Crop water use efficiency", "Other Civil and Environmental Engineering", "04 agricultural and veterinary sciences", "15. Life on land", "551", "01 natural sciences", "630", "6. Clean water", "Maize", "Engineering", "0401 agriculture", " forestry", " and fisheries", "Evapotranspiration water use efficiency", "Crop water productivity"], "contacts": [{"organization": "Rudnick, Daran, Irmak, Suat,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.13031/trans.56.10215"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Transactions%20of%20the%20ASABE", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.13031/trans.56.10215", "name": "item", "description": "10.13031/trans.56.10215", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.13031/trans.56.10215"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2013-11-18T00:00:00Z"}}, {"id": "10.2134/agronj14.0157", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:20:44Z", "type": "Journal Article", "created": "2014-08-18", "title": "Soil Organic Matter And Root And Rhizome Responses To Management Strategies In Smooth Bromegrass Pastures", "description": "<p>Soil organic matter (SOM) is a key component of pasture production. This study investigated how management strategies that varied amount and form of N input in a long\uffe2\uff80\uff90term experiment affected concentrations and stocks of total\uffe2\uff80\uff90soil organic C and N, particulate organic carbon (POC), particulate organic nitrogen (PON), root and rhizome mass, C and N contents in topsoil of smooth bromegrass (Bromus inermis Leyss.) pastures with silty clay loam soils in a wet (2010) and dry (2012) year. Management strategies included: (i) unfertilized pasture grazed with unsupplemented beef cattle (CONT); (ii) unfertilized pasture grazed with dried distillers grains plus solubles (DDGS)\uffe2\uff80\uff90supplemented beef cattle (SUPP); and (iii) nitrogen\uffe2\uff80\uff90fertilized pasture grazed with unsupplemented beef cattle (FERT). After 8 yr, management strategies had similar concentrations and stocks of total\uffe2\uff80\uff90soil organic C and N, POC, and PON, and there were no management strategy \uffc3\uff97 year interactions. From 2010 to 2012, total\uffe2\uff80\uff90soil organic C and N, POC, and PON stocks increased as soils dried and soil bulk density increased. The CONT and SUPP management strategies had less root and rhizome mass (concentrations and stocks) and greater soil bulk density than FERT. These belowground responses were consistent with earlier research conducted at the site demonstrating greater herbage accumulation and litter deposition in FERT. Management strategies that vary amount and form of N inputs into pasture appear to have low potential to affect total\uffe2\uff80\uff90soil organic C and N concentrations in the short\uffe2\uff80\uff90term, but long\uffe2\uff80\uff90term effects of less root and rhizome contents remain unknown.</p>", "keywords": ["2. Zero hunger", "Animal Sciences", "0401 agriculture", " forestry", " and fisheries", "Genetics and Genomics", "04 agricultural and veterinary sciences", "Meat Science", "15. Life on land", "551", "630", "6. Clean water"], "contacts": [{"organization": "Guretzky, John A., Nuttelman, Ana B., Schacht, Walter H., Klopfenstein, Terry J., Watson, Andrea K,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.2134/agronj14.0157"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Agronomy%20Journal", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.2134/agronj14.0157", "name": "item", "description": "10.2134/agronj14.0157", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.2134/agronj14.0157"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2014-09-01T00:00:00Z"}}, {"id": "10.2136/vzj2017.04.0083", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:21:05Z", "type": "Journal Article", "created": "2018-02-15", "title": "Rhizosphere-Scale Quantification of Hydraulic and Mechanical Properties of Soil Impacted by Root and Seed Exudates", "description": "Core Ideas<p> <p>We hypothesized that plant exudates gel soil particles and on drying enhance water repellency.</p> <p>This has been carried out using rhizosphere\uffe2\uff80\uff90scale mechanical and hydraulic measurements.</p> <p>Plant exudates enhanced soil hardness and modulus of elasticity as chia seed &gt; maize root &gt; barley root.</p> <p>Plant exudates caused measureable decreases in soil wetting rates through water repellency.</p> </p><p>Using rhizosphere\uffe2\uff80\uff90scale physical measurements, we tested the hypothesis that plant exudates gel together soil particles and, on drying, enhance soil water repellency. Barley (Hordeum vulgare L. cv. Optic) and maize (Zea mays L. cv. Freya) root exudates were compared with chia (Salvia hispanica L.) seed exudate, a commonly used root exudate analog. Sandy loam and clay loam soils were treated with root exudates at 0.46 and 4.6 mg exudate g\uffe2\uff88\uff921 dry soil and chia seed exudate at 0.046, 0.46, 0.92, 2.3 and 4.6 mg exudate g\uffe2\uff88\uff921 dry soil. Soil hardness and modulus of elasticity were measured at \uffe2\uff88\uff9210 kPa matric potential using a 3\uffe2\uff80\uff90mm\uffe2\uff80\uff90diameter spherical indenter. The water sorptivity and repellency index of air\uffe2\uff80\uff90dry soil were measured using a miniaturized infiltrometer device with a 1\uffe2\uff80\uff90mm tip radius. Soil hardness increased by 28% for barley root exudate, 62% for maize root exudate, and 86% for chia seed exudate at 4.6 mg g\uffe2\uff88\uff921 concentration in the sandy loam soil. For the clay loam soil, root exudates did not affect soil hardness, whereas chia seed exudate increased soil hardness by 48% at 4.6 mg g\uffe2\uff88\uff921 concentration. Soil water repellency increased by 48% for chia seed exudate and 23% for maize root exudate but not for barley root exudate at 4.6 mg g\uffe2\uff88\uff921 concentration in the sandy loam soil. For the clay loam soil, chia seed exudate increased water repellency by 45%, whereas root exudates did not affect water repellency at 4.6 mg g\uffe2\uff88\uff921 concentration. Water sorptivity and repellency were both correlated with hardness, presumably due to the combined influence of exudates on the hydrological and mechanical properties of the soils.</p>", "keywords": ["/dk/atira/pure/subjectarea/asjc/1100/1111", "550", "EP/M020355/1", "seed exudate", "QH301 Biology", "551", "630", "QH301", "DIMR 646809", "GE1-350", "2. Zero hunger", "soil mechanical stability", "QE1-996.5", "BB/J000868/1", "Civil_env_eng", "name=Soil Science", "Root exudate", "Geology", "04 agricultural and veterinary sciences", "15. Life on land", "6. Clean water", "Environmental sciences", "BB/J011460/1", "BB/L026058/1", "Engineering and Physical Sciences Research Council (EPSRC)", "rhizosphere-scale indenter and infiltrometer", "soil water repellency", "Biotechnology and Biological Sciences Research Council (BBSRC)", "0401 agriculture", " forestry", " and fisheries", "European Research Council"]}, "links": [{"href": "https://repository.uwl.ac.uk/id/eprint/4977/1/vzj-17-1-170083-1.pdf"}, {"href": "https://eprints.soton.ac.uk/415075/1/vzj2017.04.0083_1.pdf"}, {"href": "https://eprints.soton.ac.uk/415075/2/vzj_17_1_170083_1_.pdf"}, {"href": "https://onlinelibrary.wiley.com/doi/pdf/10.2136/vzj2017.04.0083"}, {"href": "https://doi.org/10.2136/vzj2017.04.0083"}, {"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/vzj2017.04.0083", "name": "item", "description": "10.2136/vzj2017.04.0083", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.2136/vzj2017.04.0083"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-01-01T00:00:00Z"}}, {"id": "10.2139/ssrn.4881510", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:21:06Z", "type": "Journal Article", "created": "2024-12-13", "title": "Bedrock modulates the elevational patterns of soil microbial communities", "description": "Elevational gradients are often used to reveal how soil microorganisms will respond to climate change. However, inconsistent microbial distribution patterns across different elevational transects have raised doubts about their practical applicability. We hypothesized that variations in bedrock, which influence soil physical and chemical properties, would explain these inconsistencies. We therefore investigated soil microbial communities (bacterial and fungal) along two adjacent elevational transects with different bedrocks (granite vs. slate) in a subtropical forest. Our findings reveal that soil microbial communities are shaped by complex interactions between bedrock type and environmental factors along elevational gradients. Bacterial biomass was higher on slate, whereas fungal biomass was higher on granite. On granite, both bacterial and fungal biomass increased with elevation, whereas divergent patterns were observed on slate, likely due to the distinct soil properties or combinations of properties influencing microbial biomass on each bedrock. Bedrock and elevation strongly influenced microbial beta-diversity, with beta-diversity on granite driven primarily by soil total phosphorus and moisture, and on slate by soil organic carbon and pH. In contrast, alpha-diversity was impacted less by bedrock and elevation, but its relationship with environmental factors varied markedly between bedrock types. Overall, our results highlight the critical influence of bedrock in determining soil microbial community structure along elevational gradients and their potential responses to climate change.", "keywords": ["[SDU.OCEAN]Sciences of the Universe [physics]/Ocean", "570", "Slate", "Atmosphere", "[SDU.OCEAN] Sciences of the Universe [physics]/Ocean", " Atmosphere", "Altitude", "Climate", "Science", "Granite", "Q", "Soil microbes", "551", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "Soil", "Parent material", "Altitude Climate Granite Parent material Slate Soil microbes", "[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces", "microbes", "environment"]}, "links": [{"href": "https://doi.org/10.2139/ssrn.4881510"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Geoderma", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.2139/ssrn.4881510", "name": "item", "description": "10.2139/ssrn.4881510", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.2139/ssrn.4881510"}, {"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": "10.5194/gmd-12-3503-2019", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:22:30Z", "type": "Journal Article", "created": "2019-08-12", "title": "ORCHIDEE MICT-LEAK (r5459), a global model for the production, transport, and transformation of dissolved organic carbon from Arctic permafrost regions \u2013 Part 1: Rationale, model description, and simulation protocol", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Abstract. Few Earth system models adequately represent the unique permafrost soil biogeochemistry and its respective processes; this significantly contributes to uncertainty in estimating their responses, and that of the planet at large, to warming. Likewise, the riverine component of what is known as the \u201cboundless carbon cycle\u201d is seldom recognised in Earth system modelling. The hydrological mobilisation of organic material from a \u223c1330\u20131580\u2009PgC carbon stock to the river network results in either sedimentary settling or atmospheric \u201cevasion\u201d, processes widely expected to increase with amplified Arctic climate warming. Here, the production, transport, and atmospheric release of dissolved organic carbon (DOC) from high-latitude permafrost soils into inland waters and the ocean are explicitly represented for the first time in the land surface component (ORCHIDEE) of a CMIP6 global climate model (Institut Pierre Simon Laplace \u2013 IPSL). The model, ORCHIDEE MICT-LEAK, which represents the merger of previously described ORCHIDEE versions MICT and LEAK, mechanistically represents (a)\u00a0vegetation and soil physical processes for high-latitude snow, ice, and soil phenomena and (b)\u00a0the cycling of DOC and CO2, including atmospheric evasion, along the terrestrial\u2013aquatic continuum from soils through the river network to the coast at 0.5 to 2\u2218 resolution. This paper, the first in a two-part study, presents the rationale for including these processes in a high-latitude-specific land surface model, then describes the model with a focus on novel process implementations, followed by a summary of the model configuration and simulation protocol. The results of these simulation runs, conducted for the Lena River basin, are evaluated against observational data in the second part of this study.                     </p></article>", "keywords": ["QE1-996.5", "550", "Geology", "15. Life on land", "551", "01 natural sciences", "6. Clean water", "Sciences de la terre et du cosmos", "[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry", "13. Climate action", "[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/Geochemistry", "[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology", "Sciences pharmaceutiques", "[SDU.STU.GL] Sciences of the Universe [physics]/Earth Sciences/Glaciology", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://dipot.ulb.ac.be/dspace/bitstream/2013/292778/1/doi_276405.pdf"}, {"href": "https://doi.org/10.5194/gmd-12-3503-2019"}, {"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-12-3503-2019", "name": "item", "description": "10.5194/gmd-12-3503-2019", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5194/gmd-12-3503-2019"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-03-25T00:00:00Z"}}], "links": [{"rel": "self", "type": "application/geo+json", "title": "This document as GeoJSON", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=551&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=551&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": "first", "title": "items (first)", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=551&", "hreflang": "en-US"}, {"rel": "next", "type": "application/geo+json", "title": "items (next)", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=551&offset=50", "hreflang": "en-US"}], "numberMatched": 89, "numberReturned": 50, "distributedFeatures": [], "timeStamp": "2026-06-25T13:37:21.025280Z"}