{"type": "FeatureCollection", "features": [{"id": "10.1016/j.soilbio.2006.02.021", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:16:40Z", "type": "Journal Article", "created": "2006-04-19", "title": "Response Of Soil Microbial Biomass And Enzyme Activities To The Transient Elevation Of Carbon Dioxide In A Semi-Arid Grassland", "description": "Abstract   Although elevation of CO 2  has been reported to impact soil microbial functions, little information is available on the spatial and temporal variation of this effect. The objective of this study was to determine the microbial response in a northern Colorado shortgrass steppe to a 5-year elevation of atmospheric CO 2  as well as the reversibility of the microbial response during a period of several months after shutting off the CO 2  amendment. The experiment was comprised of nine experimental plots: three chambered plots maintained at ambient CO 2  levels of 360\u00a0\u03bcmol\u00a0mol \u22121  (ambient treatment), three chambered plots maintained at 720\u00a0\u03bcmol\u00a0mol \u22121  CO 2  (elevated treatment) and three unchambered plots of equal ground area used as controls to monitor the chamber effect.  Elevated CO 2  induced mainly an increase of enzyme activities (protease, xylanase, invertase, alkaline phosphatase, arylsulfatase) in the upper 5\u00a0cm of the soil and did not change microbial biomass in the soil profile. Since rhizodeposition and newly formed roots enlarged the pool of easily available substrates mainly in the upper soil layers, enzyme regulation (production and activity) rather than shifts in microbial abundance was the driving factor for higher enzyme activities in the upper soil. Repeated soil sampling during the third to fifth year of the experiment revealed an enhancement of enzyme activities which varied in the range of 20\u201380%. Discriminant analysis including all microbiological properties revealed that the enzyme pattern in 1999 and 2000 was dominated by the CO 2  and chamber effect, while in 2001 the influence of elevated CO 2  increased and the chamber effect decreased.  Although microbial biomass did not show any response to elevated CO 2  during the main experiment, a significant increase of soil microbial N was detected as a post-treatment effect probably due to lower nutrient (nitrogen) competition between microorganisms and plants in this N-limited ecosystem. Whereas most enzyme activities showed a significant post-CO 2  effect in spring 2002 (following the conclusion of CO 2  enrichment the previous autumn, 2001), selective depletion of substrates is speculated to be the cause for non-significant treatment effects of most enzyme activities later in summer and autumn, 2002. Therefore, additional belowground carbon input mainly entered the fast cycling carbon pool and contributed little to long-term carbon storage in the semi-arid grassland.", "keywords": ["Carbon cycling", "2. Zero hunger", "Carbon dioxide", "13. Climate action", "Shortgrass steppe", "Microbial biomass", "Climate change", "0401 agriculture", " forestry", " and fisheries", "Soil enzymes", "Below ground processes", "04 agricultural and veterinary sciences", "15. Life on land", "6. Clean water"]}, "links": [{"href": "https://doi.org/10.1016/j.soilbio.2006.02.021"}, {"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.2006.02.021", "name": "item", "description": "10.1016/j.soilbio.2006.02.021", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.soilbio.2006.02.021"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2006-08-01T00:00:00Z"}}, {"id": "-Str\u00e4nders-jordart-och-eroderbarhet", "type": "Feature", "geometry": {"type": "Polygon", "coordinates": [[[11.03, 55.36], [11.03, 69.11], [23.9, 69.11], [23.9, 55.36], [11.03, 55.36]]]}, "properties": {"themes": [{"concepts": [{"id": "geoscientificInformation"}], "scheme": "https://standards.iso.org/iso/19139/resources/gmxCodelists.xml#MD_TopicCategoryCode"}, {"concepts": [{"id": "National"}], "scheme": "https://inspire.ec.europa.eu/metadata-codelist/SpatialScope"}, {"concepts": [{"id": "MensMeu"}], "scheme": "Source"}, {"concepts": [{"id": "Sweden"}], "scheme": "http://publications.europa.eu/resource/authority/country"}, {"concepts": [{"id": "soil erosion"}], "scheme": "http://aims.fao.org/aos/agrovoc/c_330883"}], "updated": "2019-01-01", "type": "Dataset", "language": "swe", "title": "Beach soil type and erodability", "description": "Localisation of erosion of soil and beaches", "formats": [{"name": "application/pdf"}, {"name": "web"}, {"name": "OGC:WMS"}, {"name": "canonical"}], "keywords": ["soil degradation processes", "National", "MensMeu", "Sweden", "soil erosion"], "contacts": [{"name": "Johan Stendahl,", "organization": "Swedish University of Agricultural Sciences (SLU)", "position": null, "roles": ["pointOfContact"], "phones": [{"value": null}], "emails": [{"value": "johan.stendahl@slu.se"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": "Sweden"}], "links": [{"href": {"url": null, "protocol": null, "protocol_url": "", "name": null, "name_url": "", "description": null, "description_url": "", "applicationprofile": null, "applicationprofile_url": "", "function": null}}]}]}, "links": [{"href": "https://resource.sgu.se/dokument/produkter/produktblad/strandernas-jordart-och-eroderbarhet.pdf", "name": "PDF", "protocol": "application/pdf", "rel": null}, {"href": "https://apps.sgu.se/sgumapviewer/kartvisare-stranders-jordart-eroderbarhet.html", "name": "Web application", "protocol": "web", "rel": null}, {"href": "https://maps3.sgu.se/geoserver/jord/wms", "name": "jord:SE.GOV.SGU.JORD.GRUNDLAGER.STRAND_JORDART.25K", "description": "JORDART", "protocol": "OGC:WMS", "rel": null}, {"href": "https://maps3.sgu.se/geoserver/jord/wms", "name": "jord:SE.GOV.SGU.JORD.GRUNDLAGER.STRAND_ERODERBARHET.25K", "description": "ERODERBARHET", "protocol": "OGC:WMS", "rel": null}, {"href": "https://github.com/ejpsoil/ejpsoildatahub/tree/main/datasets/mensmeu/Sweden/-Stranders-jordart-och-eroderbar.yml", "name": "Source of the record", "protocol": "canonical", "rel": "canonical"}, {"rel": "self", "type": "application/geo+json", "title": "-Str\u00e4nders-jordart-och-eroderbarhet", "name": "item", "description": "-Str\u00e4nders-jordart-och-eroderbarhet", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/-Str\u00e4nders-jordart-och-eroderbarhet"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"null": "date"}}, {"id": "10.1007/s00248-003-9001-x", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:14:16Z", "type": "Journal Article", "created": "2004-06-15", "title": "Microbial Community Structure And Oxidative Enzyme Activity In Nitrogen-Amended North Temperate Forest Soils", "description": "Large regions of temperate forest are subject to elevated atmospheric nitrogen (N) deposition which can affect soil organic matter dynamics by altering mass loss rates, soil respiration, and dissolved organic matter production. At present there is no general model that links these responses to changes in the organization and operation of microbial decomposer communities. Toward that end, we studied the response of litter and soil microbial communities to high levels of N amendment (30 and 80 kg ha(-1) yr(-1)) in three types of northern temperate forest: sugar maple/basswood (SMBW), sugar maple/red oak (SMRO), and white oak/black oak (WOBO). We measured the activity of extracellular enzymes (EEA) involved directly in the oxidation of lignin and humus (phenol oxidase, peroxidase), and indirectly, through the production of hydrogen peroxide (glucose oxidase, glyoxal oxidase). Community composition was analyzed by extracting and quantifying phospholipid fatty acids (PLFA) from soils. Litter EEA responses at SMBW sites diverged from those at oak-bearing sites (SMRO, BOWO), but the changes were not statistically significant. For soil, EEA responses were consistent across forests types: phenol oxidase and peroxidase activities declined as a function of N dose (33-73% and 5-41%, respectively, depending on forest type); glucose oxidase and glyoxal oxidase activities increased (200-400% and 150-300%, respectively, depending on forest type). Principal component analysis (PCA) ordinated forest types and treatment responses along two axes; factor 1 (44% of variance) was associated with phenol oxidase and peroxidase activities, factor 2 (31%) with glucose oxidase. Microbial biomass did not respond to N treatment, but nine of the 23 PLFA that formed >1 mol% of total biomass showed statistically significant treatment responses. PCA ordinated forest types and treatment responses along three axes (36%, 26%, 12% of variance). EEA factors 1 and 2 correlated negatively with PLFA factor 1 ( r = -0.20 and -0.35, respectively, n = 108) and positively with PLFA factor 3 ( r = +0.36 and +0.20, respectively, n = 108). In general, EEA responses were more strongly tied to changes in bacterial PLFA than to changes in fungal PLFA. Collectively, our data suggests that N inhibition of oxidative activity involves more than the repression of ligninase expression by white-rot basidiomycetes.", "keywords": ["Michigan", "Nitrogen", "Science", "Ecology and Evolutionary Biology", "Nature Conservation", "Microbiology", "Trees", "Soil", "Geoecology/Natural Processes", "Health Sciences", "Cellular and Developmental Biology", "Ecosystem", "Phospholipids", "Soil Microbiology", "2. Zero hunger", "Analysis of Variance", "Principal Component Analysis", "Ecology", "Life Sciences", "Natural Resources and Environment", "Molecular", "04 agricultural and veterinary sciences", "15. Life on land", "Enzymes", "13. Climate action", "0401 agriculture", " forestry", " and fisheries"]}, "links": [{"href": "https://doi.org/10.1007/s00248-003-9001-x"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Microbial%20Ecology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s00248-003-9001-x", "name": "item", "description": "10.1007/s00248-003-9001-x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s00248-003-9001-x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2004-04-19T00:00:00Z"}}, {"id": "10.1002/ppp.2162", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:14:04Z", "type": "Journal Article", "created": "2022-07-25", "title": "Thermokarst processes increase the supply of stabilizing surfaces and elements (Fe, Mn, Al, and Ca) for mineral\u2013organic carbon interactions", "description": "Abstract<p>The stabilizing properties of mineral\uffe2\uff80\uff93organic carbon (OC) interactions have been studied in many soil environments (temperate soils, podzol lateritic soils, and paddy soils). Recently, interest in their role in permafrost regions is increasing as permafrost was identified as a hotspot of change. In thawing ice\uffe2\uff80\uff90rich permafrost regions, such as the Yedoma domain, 327\uffe2\uff80\uff93466 Gt of frozen OC is buried in deep sediments. Interactions between minerals and OC are important because OC is located very near the mineral matrix. Mineral surfaces and elements could mitigate recent and future greenhouse gas emissions through physical and/or physicochemical protection of OC. The dynamic changes in redox and pH conditions associated with thermokarst lake formation and drainage trigger metal\uffe2\uff80\uff90oxide dissolution and precipitation, likely influencing OC stabilization and microbial mineralization. However, the influence of thermokarst processes on mineral\uffe2\uff80\uff93OC interactions remains poorly constrained. In this study, we aim to characterize Fe, Mn, Al, and Ca minerals and their potential protective role for OC. Total and selective extractions were used to assess the crystalline and amorphous oxides or complexed metal pools as well as the organic acids found within these pools. We analyzed four sediment cores from an ice\uffe2\uff80\uff90rich permafrost area in Central Yakutia, which were drilled (i) in undisturbed Yedoma uplands, (ii) beneath a recent lake formed within Yedoma deposits, (iii) in a drained thermokarst lake basin, and (iv) beneath a mature thermokarst lake from the early Holocene period. We find a decrease in the amount of reactive Fe, Mn, Al, and Ca in the deposits on lake formation (promoting reduction reactions), and this was largely balanced by an increase in the amount of reactive metals in the deposits on lake drainage (promoting oxidation reactions). We demonstrate an increase in the metal to C molar ratio on thermokarst process, which may indicate an increase in metal\uffe2\uff80\uff93C bindings and could provide a higher protective role against microbial mineralization of organic matter. Finally, we find that an increase in mineral\uffe2\uff80\uff93OC interactions corresponded to a decrease in CO2 and CH4 gas emissions on thermokarst process. Mineral\uffe2\uff80\uff93OC interactions could mitigate greenhouse gas production from permafrost thaw as soon as lake drainage occurs.</p", "keywords": ["Yedoma", "ddc:550", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "redox processes", "Arctic", "organic carbon stabilization", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "Institut f\u00fcr Geowissenschaften", "thaw", "permafrost", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.2162"}, {"href": "https://doi.org/10.1002/ppp.2162"}, {"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.2162", "name": "item", "description": "10.1002/ppp.2162", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1002/ppp.2162"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-07-24T00:00:00Z"}}, {"id": "10.1007/s00226-022-01398-7", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:14:16Z", "type": "Journal Article", "created": "2022-07-11", "title": "Timber tensile strength in mixed stands of European beech (Fagus sylvatica L.).", "description": "Abstract<p>The conversion to climate-stable, resilient and productive forests has resulted in an increasing share of mixed stands. Different growth conditions and silvicultural treatments lead to an increased scatter in strength compared to what is expected from monoculture experience. The study (i) quantified the magnitude of variation in strength of European beech timber from stands of different composition and (ii) showed the impact of grading on the characteristic strength value of timber coming from those stands. Strength grading models and machine settings for hardwood tensile classes on over 900 European beech (Fagus sylvatica L.) boards were derived. One model used only the dynamic modulus of elasticity (Edyn), and a more complex model used a knot value in addition. Afterwards, 407 boards from pure beech stands as well as mixed stands of beech with Douglas fir (Pseudotsuga menziesii (Mirb.) Franco), Norway spruce (Picea abies (L.) Karst.), sessile oak (Quercus petraea (Matt.) Liebl.), and Scots pine (Pinus sylvestris L.) were graded and analyzed for their material properties from tension tests parallel to grain. Although a variance components analysis attributed only 4.2% of the variation to mixture, the ungraded timber showed significant strength differences between the pure and the beech-pine stands (65.2 versus 46.6\uffc2\uffa0MPa). The yield of the material graded to the highest class in a class combination was higher in pure beech stands. The required characteristic strength values were mostly met for boards from the pure stands; while boards from the beech-pine mixed stands hardly ever reached the required values. To reduce strength variation and guarantee reliable timber products, strength grading should consider the various growth situations in forests when sampling material for the derivation of settings.</p>", "keywords": ["690", "0106 biological sciences", "Original ; Wood Science & Technology ; Ceramics", " Glass", " Composites", " Natural Materials ; Manufacturing", " Machines", " Tools", " Processes", "ddc:630", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "ddc:"]}, "links": [{"href": "https://link.springer.com/content/pdf/10.1007/s00226-022-01398-7.pdf"}, {"href": "https://doi.org/10.1007/s00226-022-01398-7"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Wood%20Science%20and%20Technology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s00226-022-01398-7", "name": "item", "description": "10.1007/s00226-022-01398-7", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s00226-022-01398-7"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-07-01T00:00:00Z"}}, {"id": "10.1007/s10021-005-0085-7", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:14:28Z", "type": "Journal Article", "created": "2006-03-20", "title": "Microbial Cycling Of C And N In Northern Hardwood Forests Receiving Chronic Atmospheric No3- Deposition", "description": "Sugar maple (Acer saccharum Marsh.)-dominated northern hardwood forests in the upper Lakes States region appear to be particularly sensitive to chronic atmospheric NO                   3                   \u2212                  deposition. Experimental NO                   3                   \u2212                  deposition (3 g NO                   3                   \u2212                  N m\u22122 y\u22121) has significantly reduced soil respiration and increased the export of DOC/DON and NO                   3                   \u2212                  across the region. Here, we evaluate the possibility that diminished microbial activity in mineral soil was responsible for these ecosystem-level responses to NO                   3                   \u2212                  deposition. To test this alternative, we measured microbial biomass, respiration, and N transformations in the mineral soil of four northern hardwood stands that have received 9 years of experimental NO                   3                   \u2212                  deposition. Microbial biomass, microbial respiration, and daily rates of gross and net N transformations were not changed by NO                   3                   \u2212                  deposition. We also observed no effect of NO                   3                   \u2212                  deposition on annual rates of net N mineralization. However, NO                   3                   \u2212                  deposition significantly increased (27%) annual net nitrification, a response that resulted from rapid microbial NO                   3                   \u2212                  assimilation, the subsequent turnover of NH                   4                   +                 , and increased substrate availability for this process. Nonetheless, greater rates of net nitrification were insufficient to produce the 10-fold observed increase in NO                   3                   \u2212                  export, suggesting that much of the exported NO                   3                   \u2212                  resulted directly from the NO                   3                   \u2212                  deposition treatment. Results suggest that declines in soil respiration and increases in DOC/DON export cannot be attributed to NO                   3                   \u2212                 -induced physiological changes in mineral soil microbial activity. Given the lack of response we have observed in mineral soil, our results point to the potential importance of microbial communities in forest floor, including both saprotrophs and mycorrhizae, in mediating ecosystem-level responses to chronic NO                   3                   \u2212                  deposition in Lake States northern hardwood forests.", "keywords": ["0106 biological sciences", "Ecology", "Science", "Plant Sciences", "Soil C and N Cycling", "Ecology and Evolutionary Biology", "Life Sciences", "Natural Resources and Environment", "Nature Conservation", "Northern Hardwood Forests", "04 agricultural and veterinary sciences", "15. Life on land", "Microbial Respiration", "Nitrification", "01 natural sciences", "Environmental Management", "N Mineralization", "Geoecology/Natural Processes", "13. Climate action", "Atmospheric NO 3 \u2212 Deposition", "0401 agriculture", " forestry", " and fisheries", "Zoology"]}, "links": [{"href": "https://doi.org/10.1007/s10021-005-0085-7"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Ecosystems", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s10021-005-0085-7", "name": "item", "description": "10.1007/s10021-005-0085-7", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s10021-005-0085-7"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2006-03-01T00:00:00Z"}}, {"id": "10.1007/s10533-021-00759-x", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:14:37Z", "type": "Journal Article", "created": "2021-01-26", "title": "How much carbon can be added to soil by sorption?", "description": "Abstract<p>Quantifying the upper limit of stable soil carbon storage is essential for guiding policies to increase soil carbon storage. One pool of carbon considered particularly stable across climate zones and soil types is formed when dissolved organic carbon sorbs to minerals. We quantified, for the first time, the potential of mineral soils to sorb additional dissolved organic carbon (DOC) for six soil orders. We compiled 402 laboratory sorption experiments to estimate the additional DOC sorption potential, that is the potential of excess DOC sorption in addition to the existing background level already sorbed in each soil sample. We estimated this potential using gridded climate and soil geochemical variables within a machine learning model. We find that mid- and low-latitude soils and subsoils have a greater capacity to store DOC by sorption compared to high-latitude soils and topsoils. The global additional DOC sorption potential for six soil orders is estimated to be 107 $$ pm$$                   \uffc2\uffb1                  13 Pg C to 1\uffc2\uffa0m depth. If this potential was realized, it would represent a 7% increase in the existing total carbon stock.</p", "keywords": ["550", "Mineral association", "Organic chemistry", "Carbon Dynamics in Peatland Ecosystems", "Markvetenskap", "01 natural sciences", "7. Clean energy", "Agricultural and Biological Sciences", "Soil water", "11. Sustainability", "Carbon fibers", "Water Science and Technology", "2. Zero hunger", "Latitude", "Ecology", "Total organic carbon", "Life Sciences", "Composite number", "Geology", "04 agricultural and veterinary sciences", "Saturation", "Milj\u00f6vetenskap", "Soil carbon", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "Algorithm", "Chemistry", "Physical Sciences", "Environmental chemistry", "Sorption", "Additional sorption potential", "environment", "Geodesy", "Biogeochemical Cycling of Nutrients in Aquatic Ecosystems", "Soil Science", "Environmental science", "FOS: Mathematics", "Environmental Chemistry", "14. Life underwater", "Soil Carbon Sequestration", "Earth-Surface Processes", "0105 earth and related environmental sciences", "Soil science", "[SDU.OCEAN]Sciences of the Universe [physics]/Ocean", "Atmosphere", "Soil organic carbon", "[SDU.OCEAN] Sciences of the Universe [physics]/Ocean", " Atmosphere", "FOS: Earth and related environmental sciences", "15. Life on land", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "0401 agriculture", " forestry", " and fisheries", "Adsorption", "[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems", "Dissolved organic carbon", "Environmental Sciences", "Mathematics"]}, "links": [{"href": "http://link.springer.com/content/pdf/10.1007/s10533-021-00759-x.pdf"}, {"href": "https://doi.org/10.1007/s10533-021-00759-x"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biogeochemistry", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s10533-021-00759-x", "name": "item", "description": "10.1007/s10533-021-00759-x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s10533-021-00759-x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-01-26T00:00:00Z"}}, {"id": "10.1007/s10533-015-0169-1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:14:37Z", "type": "Journal Article", "created": "2015-12-09", "title": "Elevated Co2 Increased Phosphorous Loss From Decomposing Litter And Soil Organic Matter At Two Face Experiments With Trees", "description": "Sustained increased productivity of trees growing in elevated CO2 depends in part on their stoichiometric flexibility, i.e., increasing their nutrient use efficiency, or on increased nutrient uptake from the soil. Phosphorus (P) may be a nutrient as limiting as nitrogen (N) in terrestrial ecosystems and may play a key-process in global terrestrial C storage. For this study archived litter and soil samples of two free air CO2 enrichment (FACE) experiments were analyzed for C, N and P. Populus euramericana, nigra and alba and Betula pendula, Alnus glutinosa and Fagus sylvatica were grown in ambient and elevated CO2 at respectively the Euro- and BangorFACE experiments. At EuroFACE, aboveground litter accumulated in L, F and H layers, while at BangorFACE almost all aboveground litter was incorporated into the mineral soil due to bioturbation. At EuroFACE, more P was lost from the F and H litter layers due to trees growing in elevated CO2, while at BangorFACE more P was lost from the mineral soil. Results of this study imply that trees growing in elevated CO2 were P limited at both experiments. Therefore, with increasing atmospheric CO2, P may play a more pronounced role than previous thought in regulating secondary forest growth. Moreover, increased atmospheric CO2 and ample N may allow a larger pool of P to become available for uptake due to, for instance, increased phosphatase activity resulting in increased organic matter turnover and biogenic weathering. Therefore, it may be postulated that under non-N-limited conditions, e.g., during regrowth, under high N deposition or in systems with high N2-fixation, increased P availability and uptake may allow P-limited forests to sustain increased growth under increasing atmospheric CO2.", "keywords": ["0106 biological sciences", "4. Education", "Litter and soil stoichiometry", "04 agricultural and veterinary sciences", "15. Life on land", "Soil phosphorous", "01 natural sciences", "Secondary forest growth", "13. Climate action", "Elevated CO", "Environmental Chemistry", "0401 agriculture", " forestry", " and fisheries", "FACE experiment", "Earth-Surface Processes", "Water Science and Technology"], "contacts": [{"organization": "Hoosbeek, Marcel R.", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1007/s10533-015-0169-1"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biogeochemistry", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s10533-015-0169-1", "name": "item", "description": "10.1007/s10533-015-0169-1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s10533-015-0169-1"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2015-12-08T00:00:00Z"}}, {"id": "10.1007/s10533-008-9182-y", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:14:36Z", "type": "Journal Article", "created": "2008-02-13", "title": "Stabilization Of Recent Soil Carbon In The Humid Tropics Following Land Use Changes: Evidence From Aggregate Fractionation And Stable Isotope Analyses", "description": "Quantitative knowledge of stabilization- and decomposition processes is necessary to under- stand, assess and predict effects of land use changes on storage and stability of soil organic carbon (soil C) in the tropics. Although it is well documented that different soil types have different soil C stocks, it is presently unknown how different soil types affect the stability of recently formed soil C. Here, we analyze the main controls of soil C storage in the top 0.1 m of soils developed on Tertiary sediments and soils developed on volcanic ashes. Using a combination of fractionation techniques with 13 C isotopes analyses we had the opportunity to trace origin and stability of soil carbon in different aggregate fractions under pasture and secondary forest. Soil C contents were higher in volcanic ash soils (47-130 g kg -1 ) than in sedimentary soils (19-50 g kg -1 ). Mean residence time (MRT) of forest-derived carbon in pastures increased from 37 to 57 years with increasing silt + clay content in sedimentary soils, but was indepen- dent from soil properties in volcanic ash soils. MRTs of pasture-derived carbon in secondary forests were considerably shorter, especially in volcanic ash soils, where no pasture-derived carbon could be detected in any of the four studied secondary forests. The implications of these results are that the MRT of recently incorporated organic carbon depends on clay mineralogy and is longer in soils dominated by smectite than non-crystalline minerals. Our results show that the presence of soil C stabilization processes, does not necessarily mean that recent incorporated soil C will also be effectively stabilized.", "keywords": ["2. Zero hunger", "Carbon sequestration; Ecuador; Mean residence time; Pasture; Secondary forest; Soil type; Texture; Water-stable aggregates", "13. Climate action", "Environmental Chemistry", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land", "Earth-Surface Processes", "Water Science and Technology"]}, "links": [{"href": "https://doi.org/10.1007/s10533-008-9182-y"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biogeochemistry", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s10533-008-9182-y", "name": "item", "description": "10.1007/s10533-008-9182-y", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s10533-008-9182-y"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2008-02-14T00:00:00Z"}}, {"id": "10.1007/s10533-008-9205-8", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:14:36Z", "type": "Journal Article", "created": "2008-06-17", "title": "Evaluation Of Effects Of Sustained Decadal Precipitation Manipulations On Soil Carbon Stocks", "description": "Throughout a 13\u00a0year period, the Throughfall Displacement Experiment sustained both increased (+33; wet) and decreased (\u221233%; dry) throughfall into an upland oak forest in Tennessee. Organic (O) horizon carbon (C) stocks were measured at several occasions before, during and after the experiment and mineral soil C stocks before and after the experiment. In the O horizon, higher C stocks were observed in the dry treatment compared to the ambient and wet, attributable to a combination of enhanced litter inputs and reduced decomposition. No precipitation treatment effects on mineral soil C stocks were found to a depth of 60\u00a0cm. Conversely, long-term reductions in surface mineral soil C stocks were surprisingly high for all treatments (3.5\u20132.7% C in the 0\u201315\u00a0cm layer and from 0.6 to 0.5% in the 15\u201330\u00a0cm layer) over the duration of the experiment. A clear explanation for this temporal trend in C storage was not readily apparent.", "keywords": ["Environmental Chemistry", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "Earth-Surface Processes", "Water Science and Technology", "0105 earth and related environmental sciences", "12. Responsible consumption"]}, "links": [{"href": "https://doi.org/10.1007/s10533-008-9205-8"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biogeochemistry", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s10533-008-9205-8", "name": "item", "description": "10.1007/s10533-008-9205-8", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s10533-008-9205-8"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2008-06-01T00:00:00Z"}}, {"id": "10.1007/s10533-009-9381-1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:14:36Z", "type": "Journal Article", "created": "2009-10-13", "title": "Plant-Soil Interactions And Acclimation To Temperature Of Microbial-Mediated Soil Respiration May Affect Predictions Of Soil Co2 Efflux", "description": "Open AccessPeer reviewed", "keywords": ["Life Sciences", " general", "Carbon cycle modeling", "2. Zero hunger", "Ecosystem ecology", "Life Sciences", "Soil respiration", "04 agricultural and veterinary sciences", "15. Life on land", "Biogeosciences", "Ecosystems", "6. Clean water", "general", "13. Climate action", "Earth Sciences", "Environmental Chemistry", "Climate change", "0401 agriculture", " forestry", " and fisheries", "Earth-Surface Processes", "Water Science and Technology"]}, "links": [{"href": "https://escholarship.org/content/qt74h8k7gh/qt74h8k7gh.pdf"}, {"href": "https://doi.org/10.1007/s10533-009-9381-1"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biogeochemistry", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s10533-009-9381-1", "name": "item", "description": "10.1007/s10533-009-9381-1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s10533-009-9381-1"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2009-10-14T00:00:00Z"}}, {"id": "10.1007/s10533-010-9426-5", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:14:36Z", "type": "Journal Article", "created": "2010-03-15", "title": "Deepened Snow Increases Late Thaw Biogeochemical Pulses In Mesic Low Arctic Tundra", "description": "Pulses of plant-available nutrients to the soil solution are expected to occur during the dynamic winter\u2013spring transition in arctic tundra. Our aims were to quantify the magnitude of these potential nutrient pulses, to understand the sensitivity of these pulses to winter conditions, and to characterize and integrate the environmental and biogeochemical dynamics of this period. To test the hypotheses that snow depth, temperature and soil water\u2014and not snow nutrient content\u2014are important controls on winter and spring biogeochemistry, we sampled soil from under ambient and deepened snow every 3 days from late winter to spring, in addition to the snowpack at the start of thaw. Soil and microbial biogeochemical dynamics were divided into distinct phases that correlated with steps in soil temperature and soil water. Soil solution and microbial pools of C, N and P fluctuated with strong peaks and declines throughout the thaw, especially under deepened snow. Snowpack nutrient accumulation was negligible relative to these biogeochemical peaks. All nutrient and microbial peaks declined simultaneously at the end of snowmelt and so this decline was delayed by 15 days under deepened snow. The timing of these nutrient pulses is critical for plant species nutrient availability and landscape nutrient budgets. This detailed and statistically-based characterisation of the winter\u2013spring transition in terms of environmental and biogeochemical variables should provide a useful foundation for future biogeochemical process-based studies of thaw, and indicate that spring thaw and possibly growing season biogeochemical dynamics are sensitive to present and future variability in winter snow depth.", "keywords": ["2. Zero hunger", "13. Climate action", "Environmental Chemistry", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "Earth-Surface Processes", "Water Science and Technology", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1007/s10533-010-9426-5"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biogeochemistry", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s10533-010-9426-5", "name": "item", "description": "10.1007/s10533-010-9426-5", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s10533-010-9426-5"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2010-03-16T00:00:00Z"}}, {"id": "10.1007/s10533-010-9496-4", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:14:36Z", "type": "Journal Article", "created": "2010-07-11", "title": "Effects Of Nitrogen Additions On Above- And Belowground Carbon Dynamics In Two Tropical Forests", "description": "Anthropogenic nitrogen (N) deposition is increasing rapidly in tropical regions, adding N to ecosystems that often have high background N availability. Tropical forests play an important role in the global carbon (C) cycle, yet the effects of N deposition on C cycling in these ecosystems are poorly understood. We used a field N-fertilization experiment in lower and upper elevation tropical rain forests in Puerto Rico to explore the responses of above- and belowground C pools to N addition. As expected, tree stem growth and litterfall productivity did not respond to N fertilization in either of these N-rich forests, indicating a lack of N limitation to net primary productivity (NPP). In contrast, soil C concentrations increased significantly with N fertilization in both forests, leading to larger C stocks in fertilized plots. However, different soil C pools responded to N fertilization differently. Labile (low density) soil C fractions and live fine roots declined with fertilization, while mineral-associated soil C increased in both forests. Decreased soil CO2 fluxes in fertilized plots were correlated with smaller labile soil C pools in the lower elevation forest (R2\u00a0=\u00a00.65, p\u00a0<\u00a00.05), and with lower live fine root biomass in the upper elevation forest (R2\u00a0=\u00a00.90, p\u00a0<\u00a00.05). Our results indicate that soil C storage is sensitive to N deposition in tropical forests, even where plant productivity is not N-limited. The mineral-associated soil C pool has the potential to respond relatively quickly to N additions, and can drive increases in bulk soil C stocks in tropical forests.", "keywords": ["58 Geosciences Aboveground Biomass", "15. Life on land", "Roots", "Aboveground Biomass", "Environmental sciences", "Soil Respiration", "Dissolved Organic Carbon", "Soil Density Fractions", "Environmental Chemistry", "Nutrient Limitation", "54 Environmental Sciences", "Geosciences", "Earth-Surface Processes", "Water Science and Technology"]}, "links": [{"href": "https://escholarship.org/content/qt7ww245cp/qt7ww245cp.pdf"}, {"href": "https://doi.org/10.1007/s10533-010-9496-4"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biogeochemistry", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s10533-010-9496-4", "name": "item", "description": "10.1007/s10533-010-9496-4", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s10533-010-9496-4"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2010-07-11T00:00:00Z"}}, {"id": "10.1007/s10533-015-0082-7", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:14:37Z", "type": "Journal Article", "created": "2015-02-23", "title": "Deeper Snow Alters Soil Nutrient Availability And Leaf Nutrient Status In High Arctic Tundra", "description": "Nitrogen (N) mineralization, nutrient availability, and plant growth in the Arctic are often restricted by low temperatures. Predicted increases of cold-season temperatures may be important for plant nutrient availability and growth, given that N mineralization is also taking place during the cold season. Changing nutrient availability may be reflected in plant N and chlorophyll content and lead to increased photosynthetic capacity, plant growth, and ultimately carbon (C) assimilation by plants. In this study, we increased snow depth and thereby cold-season soil temperatures in high Arctic Svalbard in two vegetation types spanning three moisture regimes. We measured growing-season availability of ammonium (NH4 +), nitrate (NO3 \u2212), total dissolved organic carbon (DOC) and nitrogen (TON) in soil; C, N, \u03b415N and chlorophyll content in Salix polaris leaves; and leaf sizes of Salix, Bistorta vivipara, and Luzula arcuata at peak season. Nutrient availability was significantly higher with increased snow depth in the two mesic meadow vegetation types, but not in the drier heath vegetation. Nitrogen concentrations and \u03b415N values of Salix leaves were significantly higher in all vegetation types, but the leaf sizes were unchanged. Leaves of Bistorta and Luzula were significantly larger but only significantly so in one moist vegetation type. Increased N and chlorophyll concentrations in leaves indicate a potential for increased growth (C uptake), supported by large leaf sizes for some species. Responses to cold-season soil warming are vegetation type- and species-specific, with potentially stronger responses in moister vegetation types. This study therefore highlights the contrasting effect of snow in a tundra landscape and has important implications for projections of whole tundra responses to climate change", "keywords": ["winter processes", "Mineralization", "Winter processes", "4. Education", "plant growth", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "Svalbard", "Arctic", "106026 \u00d6kosystemforschung", "13. Climate action", "SDG 13 \u2013 Ma\u00dfnahmen zum Klimaschutz", "SDG 13 - Climate Action", "0401 agriculture", " forestry", " and fisheries", "mineralization", "106026 Ecosystem research", "Plant growth", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1007/s10533-015-0082-7"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biogeochemistry", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s10533-015-0082-7", "name": "item", "description": "10.1007/s10533-015-0082-7", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s10533-015-0082-7"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2015-02-24T00:00:00Z"}}, {"id": "10.1007/s10533-015-0157-5", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:14:37Z", "type": "Journal Article", "created": "2015-11-14", "title": "Chronic Nitrogen Fertilization And Carbon Sequestration In Grassland Soils: Evidence Of A Microbial Enzyme Link", "description": "Chronic nitrogen (N) fertilization can greatly affect soil carbon (C) sequestration by altering biochemical interactions between plant detritus and soil microbes. In lignin-rich forest soils, chronic N additions tend to increase soil C content partly by decreasing the activity of lignin-degrading enzymes. In cellulose-rich grassland soils it is not clear whether cellulose-degrading enzymes are also inhibited by N additions and what consequences this might have on changes in soil C content. Here we address whether chronic N fertilization has affected (1) the C content of light versus heavier soil fractions, and (2) the activity of four extracellular enzymes including the C-acquiring enzyme \u03b2-1,4-glucosidase (BG; necessary for cellulose hydrolysis). We found that 19\u00a0years of chronic N-only addition to permanent grassland have significantly increased soil C sequestration in heavy but not in light soil density fractions, and this C accrual was associated with a significant increase (and not decrease) of BG activity. Chronic N fertilization may increase BG activity because greater N availability reduces root C:N ratios thus increasing microbial demand for C, which is met by C inputs from enhanced root C pools in N-only fertilized soils. However, BG activity and total root mass strongly decreased in high pH soils under the application of lime (i.e. CaCO3), which reduced the ability of these organo-mineral soils to gain more C per units of N added. Our study is the first to show a potential \u2018enzyme link\u2019 between (1) long-term additions of inorganic N to grassland soils, and (2) the greater C content of organo-mineral soil fractions. Our new hypothesis is that the \u2018enzyme link\u2019 occurs because (a) BG activity is stimulated by increased microbial C demand relative to N under chronic fertilization, and (b) increased BG activity causes more C from roots and from microbial metabolites to accumulate and stabilize into organo-mineral C fractions. We suggest that any combination of management practices that can influence the BG \u2018enzyme link\u2019 will have far reaching implications for long-term C sequestration in grassland soils.", "keywords": ["DECOMPOSITION", "DYNAMICS", "570", "\u03b2-1", "4-Glucosidase", "/dk/atira/pure/subjectarea/asjc/2300/2304", "NUTRIENT RELEASE", "Environmental Sciences & Ecology", "Root C:N ratio", "Extracellular enzyme activity", "LITTER DECAY", "FOREST ECOSYSTEMS", "0399 Other Chemical Sciences", "0402 Geochemistry", "Environmental Chemistry", "Geosciences", " Multidisciplinary", "beta-1", "4-Glucosidase", "Earth-Surface Processes", "Water Science and Technology", "2. Zero hunger", "Multidisciplinary", "Science & Technology", "/dk/atira/pure/subjectarea/asjc/1900/1904", "Geology", "sequestration", "Agronomy & Agriculture", "04 agricultural and veterinary sciences", "15. Life on land", "Soil carbon", "N DEPOSITION", "ORGANIC-MATTER", "PHOSPHORUS", "Fertilization", "Physical Sciences", "N ratio [Root C]", "0401 agriculture", " forestry", " and fisheries", "Soil carbon sequestration", "Liming", "TURNOVER", "Life Sciences & Biomedicine", "Geosciences", "/dk/atira/pure/subjectarea/asjc/2300/2312", "Environmental Sciences", "RESPONSES"]}, "links": [{"href": "https://doi.org/10.1007/s10533-015-0157-5"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biogeochemistry", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s10533-015-0157-5", "name": "item", "description": "10.1007/s10533-015-0157-5", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s10533-015-0157-5"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2015-11-14T00:00:00Z"}}, {"id": "10.1007/s11104-005-1257-0", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:14:44Z", "type": "Journal Article", "created": "2005-11-17", "title": "Increased Topsoil Mineral Nutrient Concentrations Under Exotic Invasive Plants In Belgium", "description": "Exotic invasive plants can alter ecosystem processes. For the first time in Europe, we have analysed the impacts of exotic invasive plants on topsoil chemical properties. At eight sites invaded by five exotic invasive species (Fallopia                         japonica, Heracleum                         mantegazzianum, Solidago                         gigantea, Prunus                         serotina and Rosa                         rugosa), soil mineral element composition was compared between invaded patches and adjacent, uninvaded vegetation. We found increased concentrations of exchangeable essential nutrients under the canopy of exotic invasive plants, most strikingly so for K and Mn (32% and 34% increase, respectively). This result fits in well with previous reports of enhanced N dynamics in invaded sites, partly due to higher net primary productivity in exotic invasive plants compared to native vegetation.", "keywords": ["Soil nutrients", "0106 biological sciences", "Plant-soil interactions", "Invasive species", "Alien species", "Ecosystem processes", "Plant invasions", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "P\u00e9dologie", "Agronomie du sol", "0401 agriculture", " forestry", " and fisheries", "Botanique g\u00e9n\u00e9rale"]}, "links": [{"href": "https://doi.org/10.1007/s11104-005-1257-0"}, {"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/s11104-005-1257-0", "name": "item", "description": "10.1007/s11104-005-1257-0", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s11104-005-1257-0"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2005-08-01T00:00:00Z"}}, {"id": "10.1016/j.still.2010.12.006", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:16:58Z", "type": "Journal Article", "created": "2011-01-18", "title": "Organic Carbon And Total Nitrogen Stocks In A Vertisol Following 40 Years Of No-Tillage, Crop Residue Retention And Nitrogen Fertilisation", "description": "Abstract   Conservation agricultural practices such as no-till (NT) and crop residue retention (CRR), and nutrient application, increases soil organic C (SOC) and are considered effective measures of C sequestration in soil. However, long-term effects of individual components of conservation agriculture and their interactions on SOC are rarely evaluated; as a result, conflicting findings of these practices on SOC are reported in the literature. We measured SOC and soil total N in a balanced factorial experiment, conducted on a Vertisol, consisting of tillage practices (conventional mechanical tillage, CT; and no-tillage, NT), crop residue management (crop residue burned, CRB; and crop residue retained, CRR) and N fertiliser application (no N, 30\u00a0kg\u00a0N\u00a0ha \u22121 \u00a0year \u22121 ; and 90\u00a0kg\u00a0N\u00a0ha \u22121 \u00a0year \u22121 ). The site, in a semiarid subtropical region, was cropped with wheat ( Triticum aestivum  L.) except for 3 years of barley ( Hordeum vulgare  L.), for 40 years using conservation practices.  In general, tillage effects on SOC and soil total N were small. Crop residue and N fertiliser interactively increased SOC and total N stocks at 0\u20130.1\u00a0m depth and cumulative stocks at 0\u20130.2\u00a0m and 0\u20130.3\u00a0m depths; that is, CRR increased SOC and soil total N only when N fertiliser was applied, and fertilisation increased SOC and soil total N only under CRR treatment. Depletion of \u03b4 13 C values in CRR treatments and \u03b4 15 N values in N treatments strongly indicated the contribution of crop residue (and root biomass) and N fertiliser to soil organic matter in this Vertisol. From this study and previous findings from this site, it appears, however, the effects of crop residue retention and N fertiliser occurred in early years, and did not continually increase SOC and total soil N with increasing period of conservation practices.", "keywords": ["2. Zero hunger", "Soil organic matter", "Agricultural", "Nitrogen", "1904 Earth-Surface Processes", "No-till", "04 agricultural and veterinary sciences", "15. Life on land", "Carbon", "630", "Land capability and soil productivity", "Environmental sciences", "Biological sciences", "veterinary and food sciences", "0401 agriculture", " forestry", " and fisheries", "1102 Agronomy and Crop Science", "1111 Soil Science"]}, "links": [{"href": "https://doi.org/10.1016/j.still.2010.12.006"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20and%20Tillage%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.still.2010.12.006", "name": "item", "description": "10.1016/j.still.2010.12.006", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.still.2010.12.006"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2011-04-01T00:00:00Z"}}, {"id": "10.1029/2018JE005899", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:17:24Z", "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": "10.1007/s11368-011-0382-z", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:14:57Z", "type": "Journal Article", "created": "2011-05-23", "title": "In Situ Phytoremediation Of Pah-Contaminated Soil By Intercropping Alfalfa (Medicago Sativa L.) With Tall Fescue (Festuca Arundinacea Schreb.) And Associated Soil Microbial Activity", "description": "Purpose  A 7-month field experiment was conducted to investigate the polycyclic aromatic hydrocarbon (PAH) remediation potential of two plant species and changes in counts of soil PAH-degrading bacteria and microbial activity.", "keywords": ["2. Zero hunger", "/dk/atira/pure/subjectarea/asjc/1900/1904", "Stratigraphy", "/dk/atira/pure/subjectarea/asjc/1900/1913", "15. Life on land", "01 natural sciences", "6. Clean water", "Earth-Surface Processes", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1007/s11368-011-0382-z"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Soils%20and%20Sediments", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s11368-011-0382-z", "name": "item", "description": "10.1007/s11368-011-0382-z", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s11368-011-0382-z"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2011-05-24T00:00:00Z"}}, {"id": "10.1007/s11368-017-1657-9", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:14:58Z", "type": "Journal Article", "created": "2017-01-21", "title": "Contrasting Impacts Of Two Subtropical Earthworm Species On Leaf Litter Carbon Sequestration Into Soil Aggregates", "description": "Earthworms influence soil carbon sequestration based on the balance between mineralization and stabilization of litter carbon. However, specific impacts and mechanisms of epi-endogeic or endogeic earthworms on litter carbon sequestration need to be clarified. A 126-day laboratory experiment examined how two ecological group earthworms (Amynthas sp. (epi-endogeic species) and Pontoscolex corethrurus (endogeic species)) with distinct feeding habits influence the dynamics and distribution of 13C labeled Schima superba carbon leaf litter into soil aggregates. Accordingly, three treatments were set as: (i) soil and litter (CK), (ii) soil, litter, and endogeic earthworms (En), (iii) soil, litter, and epi-endogeic earthworms (Ep).                            Amynthas sp. significantly increased decomposition rate of litter and soil respiration due to the increase of the total phospholipid fatty acids (PLFAs), bacterial PLFAs, and fungal PLFAs and the direct consumption of leaf litter, while P. corethrurus had no effects on these two aspects. Higher proportion of large macroaggregates (>2000\u00a0\u03bcm) was generated in the presence of earthworms, with the highest in the treatment with endogeic earthworms. Besides, both the two species increased the proportion of non-labile organic carbon in large macroaggregates, which was conducive to carbon protection. At the end of incubation, the 13C signatures of soil indicated that the distribution of litter-derived carbon was significantly affected by the consumption and excretion activities of earthworms, with the result that more carbon was sequestrated in large macroaggregates (>2000\u00a0\u03bcm). Consistent with our hypothesis, Amynthas sp., an epi-endogeic earthworms, could rapidly consume organic residues and stimulate microbial biomass to increase litter decomposition rate and incorporate organic carbon into soil structures, while P. corethrurus, an endogeic earthworms, would stabilize the organic carbon that has been already incorporated into the soil through the formation of large macroaggregates and the transformation of soil organic carbon fractions to more recalcitrant forms.", "keywords": ["2. Zero hunger", "13. Climate action", "Stratigraphy", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land", "Earth-Surface Processes"]}, "links": [{"href": "https://doi.org/10.1007/s11368-017-1657-9"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Soils%20and%20Sediments", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s11368-017-1657-9", "name": "item", "description": "10.1007/s11368-017-1657-9", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s11368-017-1657-9"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-01-22T00:00:00Z"}}, {"id": "10.1007/s11368-017-1899-6", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:14:59Z", "type": "Journal Article", "created": "2017-12-22", "title": "A meta-analysis and critical evaluation of influencing factors on soil carbon priming following biochar amendment", "description": "Previous studies have found biochar-induced effects on native soil organic carbon (NSOC) decomposition, with a range of positive, negative and no priming reported. However, many uncertainties still exist regarding which parameters drive the amplitude and the direction of the biochar priming. We conducted a quantitative analysis of 1170 groups of data from 27 incubation studies using boosted regression trees (BRTs). BRT is a machine learning method combining regression trees and a boosting algorithm, which can effectively partition independent influences of various factors on the target variable in the complex ecological processes. The BRT model explained a total of 72.4% of the variation in soil carbon (C) priming following biochar amendment, in which incubation conditions (36.5%) and biochar properties (33.7%) explained a larger proportion than soil properties (29.8%). The predictors that substantially accounted for the explained variation included incubation time (27.1%) and soil moisture (5.0%), biochar C/N ratio (6.2%), nitrogen content (5.5%), pyrolysis time during biochar production (5.1%), biochar pH (4.5%), soil C content (5.2%), sand (4.7%) and clay content (4.1%). In contrast, other incubation conditions (temperature, biochar dose, whether nutrient was added), biochar properties (biochar C, feedstock type, ash content, pyrolysis temperature, whether biochar was activated) and soil properties (nitrogen content, silt content, C/N ratio, pH, land use type) had small contribution (each <\u20094%). Positive priming occurred within the first 2\u00a0years of incubations, with a change to negative priming afterwards. The priming was negative for low N biochar or in high-moisture soils but positive on their reverse sides. The size of negative priming increased with rising biochar C/N ratio, pyrolysis time and soil clay content, but deceased with soil C/N ratio. We determine the critical drivers for biochar effect on native soil organic C cycling, which can help us to better predict soil C sequestration following biochar amendment.", "keywords": ["2. Zero hunger", "Agricultural", "550", "1904 Earth-Surface Processes", "Soil respiration", "04 agricultural and veterinary sciences", "15. Life on land", "Boosted regression tree", "Incubation time", "Native soil organic matter", "Environmental sciences", "Earth sciences", "veterinary and food sciences", "0401 agriculture", " forestry", " and fisheries", "Priming effect", "1913 Stratigraphy", "Pyrogenic organic matter"]}, "links": [{"href": "https://doi.org/10.1007/s11368-017-1899-6"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Soils%20and%20Sediments", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s11368-017-1899-6", "name": "item", "description": "10.1007/s11368-017-1899-6", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s11368-017-1899-6"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-12-22T00:00:00Z"}}, {"id": "10.1016/j.agwat.2016.04.009", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:15:20Z", "type": "Journal Article", "created": "2016-04-27", "title": "Irrigation Regime Affected Soc Content Rather Than Plow Layer Thickness Of Rice Paddies: A County Level Survey From A River Basin In Lower Yangtze Valley, China", "description": "Abstract   While the impacts of farm management practices such as fertilization, tillage and straw return on soil organic carbon dynamics in croplands have been widely studied, the effects of irrigation management in irrigated rice paddies have not yet been widely assessed. Changes in plow layer thickness and soil organic carbon content of rice paddies were analyzed using data obtained in a county-level survey of soil fertility conducted in 2005 and 2006 in Guichi County, Anhui Province, China. Both soil thickness and organic carbon content of plow layer showed skewed normal distributions, with their averages of 14.58\u00a0\u00b1\u00a03.92\u00a0cm, and 16.45\u00a0\u00b1\u00a06.02\u00a0g/kg, respectively. The irrigation method was found to have significant influences on both plow layer thickness and soil organic carbon content, as the plow layer thickness and soil organic carbon content had an inverse response to the irrigation intensity derived from different irrigation methods. The land-level performance of irrigation/drainage infrastructure and the irrigation water sources were detected to have significant effect on plow layer thickness, but little influence on soil organic carbon content. While the capacity of irrigation/drainage infrastructure had a remarkable effect on soil organic carbon content but little impact on plow layer thickness. However, the irrigation condition for surveyed fields was detected to have little effect on both plow layer thickness and soil organic carbon content. These results indicated that irrigation management should keep the balance between surface erosion on plow layer thickness and soil organic carbon accumulation. Hence, developing new technique for good irrigation infrastructure and water management in future will help soil organic carbon accumulation as well as improve the soil for enhanced crop growth in rice agriculture.", "keywords": ["330", "QH301 Biology", "01 natural sciences", "QH301", "water management", "land-use", "sequential reduction processes", "P losses", "fields", "SDG 15 - Life on Land", "0105 earth and related environmental sciences", "2. Zero hunger", "Soil organic carbon", "04 agricultural and veterinary sciences", "Irrigation water source", "15. Life on land", "topsoil organic-carbon", "6. Clean water", "lowland rice", "Irrigation management", "13. Climate action", "soil colloidal suspensions", "0401 agriculture", " forestry", " and fisheries", "Rice paddy", "lake region", "stability behavior", "Soil thickness"]}, "links": [{"href": "https://doi.org/10.1016/j.agwat.2016.04.009"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Agricultural%20Water%20Management", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.agwat.2016.04.009", "name": "item", "description": "10.1016/j.agwat.2016.04.009", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.agwat.2016.04.009"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2016-07-01T00:00:00Z"}}, {"id": "10.1016/j.electacta.2025.146049", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:15:47Z", "type": "Journal Article", "created": "2025-03-13", "title": "Intensification of peroxone production through the paired generation of hydrogen peroxide and ozone in a continuous flow electrochemical reactor", "description": "The paired electrochemical production of ozone and hydrogen peroxide is evaluated in a novel 3-D printed electrochemical cell in which the oxidants produced are tested in the removal of fluoxetine hydrochloride (FLX). To properly pair the anodic production of ozone and the cathodic production of hydrogen peroxide in the same cell, that is, with the same intensity in anode and cathode, an innovative composite 3-D gas diffusion cathode was used to decrease the current density (by increasing the effective cathode surface area) in the cathodic compartment, attaining soft operation conditions in this compartment. Meanwhile, a grid DIACHEM\u00ae lattice BDD was used in the anode to increase the harsh oxidative conditions in the anodic compartment. The results confirm the viability of pairing both processes. Current intensity positively affects the production of ozone and, less importantly, the production of hydrogen peroxide (because the current efficiency decreases with the intensity), with the contribution of electrolytes containing sulfate and bicarbonates being evaluated in the search of greener processes. The oxidants produced were dosed to solutions containing FLX confirming that the addition of both products (electro-peroxone process) attains a significant improvement in the removal of FLX, which was explained in terms of promoting radical mechanisms for ozone oxidation (peroxone reagent).", "keywords": ["Ozone", "Advanced oxidation processes", "Peroxone", "Electrochemical treatment", "Hydrogen peroxide", "Process integration"]}, "links": [{"href": "https://doi.org/10.1016/j.electacta.2025.146049"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Electrochimica%20Acta", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.electacta.2025.146049", "name": "item", "description": "10.1016/j.electacta.2025.146049", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.electacta.2025.146049"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-06-01T00:00:00Z"}}, {"id": "10.1016/j.enpol.2013.07.078", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:15:48Z", "type": "Journal Article", "created": "2013-08-13", "title": "Retro-Analysis Of Liquid Bio-Ethanol And Bio-Diesel In New Zealand", "description": "This paper uses a new approach of retro-analysis. Typically policy is informed by forward-looking analysis of potential for alternative energy technologies. But historical knowledge of energy and processing requirements and greenhouse effects is more reliable for engineering evaluation of biofuel production systems. This study calculates energy inputs and greenhouse gas emissions for the most efficient biomass feedstocks in New Zealand if the policy had been implemented to maximize liquid biofuel production in the year 2004/2005. The study uses existing processing technologies and agricultural statistics. Bioethanol production is calculated from putrescible wastes and starch crops, and biodiesel production from rapeseed, tallow, wood and waste paper. Each production system is further evaluated using measures of land use, energy input, crop production related to the energy product, plus relative measures of efficiency and renewability. The research findings are that maximum biofuel production in 2004/2005 would have provided only a few per cent of demand, and would not have reduced dependence on foreign imported oil or exposure to fuel price rise. Finally, we conclude that demand management and efficiency are more effective means of meeting policy objectives.", "keywords": ["2. Zero hunger", "670", "330", "ANZSRC::4407 Policy and administration", "02 engineering and technology", "sustainability", "renewable energy", "7. Clean energy", "ANZSRC::3304 Urban and regional planning", "12. Responsible consumption", "ANZSRC::4802 Environmental and resources law", "Field of Research::10 - Technology::1002 - Environmental Biotechnology::100299 - Environmental Biotechnology not elsewhere classified", "13. Climate action", "strategic analysis", "ANZSRC::070108 Sustainable Agricultural Development", "11. Sustainability", "0202 electrical engineering", " electronic engineering", " information engineering", "biofuel", "ANZSRC::070304 Crop and Pasture Biomass and Bioproducts", "ANZSRC::090608 Renewable Power and Energy Systems Engineering (excl. Solar Cells)", "Fields of Research::40 - Engineering::4004 - Chemical engineering::400402 - Chemical and thermal processes in energy and combustion"]}, "links": [{"href": "https://doi.org/10.1016/j.enpol.2013.07.078"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Energy%20Policy", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.enpol.2013.07.078", "name": "item", "description": "10.1016/j.enpol.2013.07.078", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.enpol.2013.07.078"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2013-11-01T00:00:00Z"}}, {"id": "10.1016/j.catena.2013.06.021", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:15:34Z", "type": "Journal Article", "created": "2013-07-21", "title": "Effects Of Biochar On Soil Properties And Erosion Potential In A Highly Weathered Soil", "description": "AbstractHighly weathered soils in humid Asia are characterized by low soil fertility and high soil erosion potential. This study evaluates the influences of biochar made from the waste wood of white lead trees (Leucaena leucocephala (Lam.) de Wit) on the physicochemical and biological properties of long-term cultivated, acidic Ultisol. This study used three application rates (0%, 2.5%, and 5% (wt/wt)) of the biochar with an incubation time of 105d for all cases. Soils were collected at 21d, 42d, 63d, 84d and 105d during the incubation period to evaluate changes in soil properties over time. A simulated rainfall event (80mmh\u22121) was performed to estimate soil loss for all treatments at the end of the incubation time. Experimental results indicate that applying biochar improved the physicochemical and biological properties of the highly weathered soils, including significant increases in soil pH from 3.9 to 5.1, cation exchange capacity from 7.41 to 10.8cmol (+) kg\u22121, base cation percentage from 6.40 to 26.0%, and microbial biomass carbon (MBC) from 835 to 1262mgkg\u22121. Compared with the control (i.e., no biochar), biochar application decreased bulk density from 1.4 to 1.1Mgm\u22123, increased Ksat by 1.8 times and increased the mean weight diameter (MWD) of soil aggregates from 2.6cm to 4.0cm. Incorporating biochar into the soil significantly reduced soil loss by 50% and 64% at 2.5% and 5% application rates, respectively, compared with the control. The formation of macroaggregates in the biochar-amended soils is the critical factor to improve soil erosion potential. Based on these results, a 5% application rate of biochar is considered as suitable for highly weathered soil because this application rate efficiently improves soil physiochemical properties and reduces soil loss.", "keywords": ["2. Zero hunger", "Biochar", "Erosion", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "Highly weathered soil", "15. Life on land", "Soil loss", "Soil quality", "6. Clean water", "Earth-Surface Processes"], "contacts": [{"organization": "Chien Sheng Wang, Shih-Hao Jien,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1016/j.catena.2013.06.021"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/CATENA", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.catena.2013.06.021", "name": "item", "description": "10.1016/j.catena.2013.06.021", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.catena.2013.06.021"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2013-11-01T00:00:00Z"}}, {"id": "10.1016/j.catena.2015.02.024", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:15:34Z", "type": "Journal Article", "created": "2015-04-11", "title": "Effects Of Wildfire On Mercury Mobilisation In Eucalypt And Pine Forests", "description": "Abstract   Wildfires and subsequent rainfall play an important role in the redistribution of major, minor and trace chemical elements, which could be mobilised from burnt soils and ashes. In particular, the fire-induced release of mercury (Hg) into the environment is relevant to study due to its volatilisation and toxicity. However, the impact of wildfire followed by rainfall on mercury redistribution is poorly documented. Hence, eucalypt- and pine-covered hillslopes (1\u20133) were surveyed in two burnt areas (Ermida and S. Pedro do Sul, Portugal), as well as in a non-burnt eucalypt slope (Ermida). Top-soils (0\u20132\u00a0cm) and ashes were sampled 4 and 14\u00a0weeks after the fire, the latter following an episode of heavy precipitation. In order to clarify the effect of temperature on Hg release from the soil, a heating experiment was also conducted. Results revealed that 30% of the Hg retained in eucalypt soils was released by the fire, corresponding to a loss of 1.0\u20131.1\u00a0g\u00a0Hg\u00a0ha\u2212\u00a01 of burnt soil. Levels in burnt eucalypt soils were twice the values registered in burnt pine soils for both fire severities. Mercury in ashes pointed to similar trend between the two types of vegetation. Results from the heating experiment with soil suggest that temperature reached in the wildfire was insufficient to destroy the most stable bonds of Hg-ligands. Mercury concentrations were not correlated with organic matter content, both in soils and ashes. It was estimated that rainfall caused a loss of 1.0\u00a0g\u00a0Hg\u00a0ha\u2212\u00a01 from ashes and an uptake of 0.5\u00a0g\u00a0Hg\u00a0ha\u2212\u00a01 of soil washed out. The difference between the previous estimations, 0.5\u00a0g\u00a0Hg\u00a0ha\u2212\u00a01, corresponds to the quantity of Hg transported to the surrounding area or eventually introduced into aquatic systems. Hence, the results obtained in the present study highlight the importance of wildfire and subsequent rainfall in the mobilisation of Hg in the environment.", "keywords": ["Mercury pathway", "Portugal", "Runoff", "13. Climate action", "Wildfire", "15. Life on land", "01 natural sciences", "Earth-Surface Processes", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.catena.2015.02.024"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/CATENA", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.catena.2015.02.024", "name": "item", "description": "10.1016/j.catena.2015.02.024", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.catena.2015.02.024"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2015-08-01T00:00:00Z"}}, {"id": "10.1016/j.colsurfb.2023.113433", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:15:38Z", "type": "Journal Article", "created": "2023-06-28", "title": "Contrasting transport and fate of hydrophilic and hydrophobic bacteria in wettable and water-repellent porous media: Straining or attachment?", "description": "Bacterial transport and retention likely depend on bacterial and soil surface properties, especially hydrophobicity. We used a controlled experimental setup to explore hydrophilic Escherichia coli (E. coli) and hydrophobic Rhodococcus erythropolis (PTCC1767) (R. erythropolis) transport through dry (-\u00a015,000\u00a0cm water potential) and water saturated (0\u00a0cm water potential) wettable and water-repellent sand columns. A pulse of bacteria (1\u00a0\u00d7\u00a0108 CFU mL-1) and bromide (10\u00a0mmol\u00a0L-1) moved through the columns under saturated flow (0\u00a0cm) for four pore volumes. A second bacteria and bromide pulse was then poured on the column surfaces and leaching was extended six more pore volumes. In dry wettable sand attachment dominated E. coli retention, whereas R. erythropolis was dominated by straining. Once wetted, the dominant retention mechanisms flipped between these bacteria. Attachment by either bacteria decreased markedly in water-repellent sand, so straining was the main retention mechanism. We explain this from capillary potential energy, which enhanced straining under the formation of water films at very early times (i.e., imbibing) and film thinning at much later times (i.e., draining). The interaction between the hydrophobicity of bacteria and soil on transport, retention and release mechanisms needs greater consideration in predictions.", "keywords": ["Bromides", "2040 Environment and Biodiversity", "570", "Supplementary Information", "Wetting characteristics", "Vadose zone", "610", "Soil", "Colloid and Surface Chemistry", "Sand", "Pore-scale processes", "Escherichia coli", "Physical and Theoretical Chemistry", "European Commission", "101026287", "SDG 15 - Life on Land", "Drought", "T", "Water", "Surfaces and Interfaces", "T Technology", "Interfacial processes", "3. Good health", "TC Hydraulic engineering. Ocean engineering", "Marie Sklodowska-Curie grant", "EU Horizon 2020", "SDG 6 - Clean Water and Sanitation", "TC", "Porosity", "Hydrophobic and Hydrophilic Interactions", "Biotechnology"]}, "links": [{"href": "https://doi.org/10.1016/j.colsurfb.2023.113433"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Colloids%20and%20Surfaces%20B%3A%20Biointerfaces", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.colsurfb.2023.113433", "name": "item", "description": "10.1016/j.colsurfb.2023.113433", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.colsurfb.2023.113433"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-08-01T00:00:00Z"}}, {"id": "10.1016/j.ijbiomac.2018.12.270", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:16:15Z", "type": "Journal Article", "created": "2019-01-03", "title": "Improving polyhydroxyalkanoates production in phototrophic mixed cultures by optimizing accumulator reactor operating conditions", "description": "Open AccessPolyhydroxyalkanoates (PHAs) production with phototrophic mixed cultures (PMCs) has been recently proposed. These cultures can be selected under the permanent presence of carbon and the PHA production can be enhanced in subsequent accumulation steps. To optimize the PHA production in accumulator reactors, this work evaluated the impact of 1) initial acetate concentration, 2) light intensity, 3) removal of residual nitrogen on the culture performance. Results indicate that low acetate concentration (&lt;30CmM) and specific light intensities around 20W/gX are optimal operating conditions that lead to high polyhydroxybutyrate (PHB) storage yields (0.83+-0.07 Cmol-PHB/Cmol-Acet) and specific PHB production rates of 2.21+-0.07 Cmol-PHB/Cmol X d. This rate is three times higher than previously registered in non-optimized accumulation tests and enabled a PHA content increase from 15 to 30% in less than 4h. Also, it was shown for the first time, the capability of a PMC to use a real waste, fermented cheese whey, to produce PHA with a hydroxyvalerate (HV) content of 12%. These results confirm that fermented wastes can be used as substrates for PHA production with PMCs and that the energy levels in sunlight that lead to specific light intensities from 10 to 20W/gX are sufficient to drive phototrophic PHA production processes.", "keywords": ["0106 biological sciences", "1303 Biochemistry", "Light", "Nitrogen", "Polyhydroxyalkanoates (PHA)", "Fermented cheese whey (FCW)", "Phototrophic mixed cultures (PMCs)", "Acetates", "7. Clean energy", "01 natural sciences", "1315 Structural Biology", "Bioreactors", "Cheese", "Whey", "1312 Molecular Biology", "0105 earth and related environmental sciences", "Polyhydroxyalkanoates", "Volatile fatty acids (VFAs)", "Other Quantitative Biology (q-bio.OT)", "Quantitative Biology - Other Quantitative Biology", "Purple phototrophic bacteria (PPB)", "Kinetics", "Phototrophic Processes", "13. Climate action", "FOS: Biological sciences", "Fermentation"]}, "links": [{"href": "https://doi.org/10.1016/j.ijbiomac.2018.12.270"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/International%20Journal%20of%20Biological%20Macromolecules", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.ijbiomac.2018.12.270", "name": "item", "description": "10.1016/j.ijbiomac.2018.12.270", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.ijbiomac.2018.12.270"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-04-01T00:00:00Z"}}, {"id": "10.1016/j.jenvman.2018.01.064", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:16:20Z", "type": "Journal Article", "created": "2018-02-05", "title": "Elemental sulfur-based autotrophic denitrification and denitritation: microbially catalyzed sulfur hydrolysis and nitrogen conversions", "description": "The hydrolysis of elemental sulfur (S0) coupled to S0-based denitrification and denitritation was investigated in batch bioassays by microbiological and modeling approaches. In the denitrification experiments, the highest obtained NO3--N removal rate was 20.9\u202fmg/l\u00b7d. In the experiments with the biomass enriched on NO2-, a NO2--N removal rate of 10.7\u202fmg/l\u00b7d was achieved even at a NO2--N concentration as high as 240\u202fmg/l. The Helicobacteraceae family was only observed in the biofilm attached onto the chemically-synthesized S0 particles with a relative abundance up to 37.1%, suggesting it was the hydrolytic biomass capable of S0 solubilization in the novel surface-based model. S0-driven denitrification was modeled as a two-step process in order to explicitly account for the sequential reduction of NO3- to NO2- and then to N2 by denitrifying bacteria.", "keywords": ["Surface-based hydrolysis", "Autotrophic Processes", "Autotrophic denitrification; Autotrophic denitritation; Community structure; Elemental sulfur; Mathematical modeling; Surface-based hydrolysis", "Elemental sulfur", "Nitrates", "Nitrogen", "Hydrolysis", "0211 other engineering and technologies", "02 engineering and technology", "Autotrophic denitrification", "01 natural sciences", "6. Clean water", "Community structure", "Bioreactors", "Autotrophic denitritation", "Denitrification", "Autotrophic denitrification; Autotrophic denitritation; Elemental sulfur; Community structure; Surface-based hydrolysis; Mathematical modeling", "Mathematical modeling", "14. Life underwater", "Sulfur", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://www.iris.unina.it/bitstream/11588/698214/5/anastasiia%20JEMA.pdf"}, {"href": "https://doi.org/10.1016/j.jenvman.2018.01.064"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Environmental%20Management", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.jenvman.2018.01.064", "name": "item", "description": "10.1016/j.jenvman.2018.01.064", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.jenvman.2018.01.064"}, {"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": "10.1016/j.pedobi.2017.05.003", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:16:27Z", "type": "Journal Article", "created": "2017-05-13", "title": "Priorities for research in soil ecology", "description": "The ecological interactions that occur in and with soil are of consequence in many ecosystems on the planet. These interactions provide numerous essential ecosystem services, and the sustainable management of soils has attracted increasing scientific and public attention. Although soil ecology emerged as an independent field of research many decades ago, and we have gained important insights into the functioning of soils, there still are fundamental aspects that need to be better understood to ensure that the ecosystem services that soils provide are not lost and that soils can be used in a sustainable way. In this perspectives paper, we highlight some of the major knowledge gaps that should be prioritized in soil ecological research. These research priorities were compiled based on an online survey of 32 editors of Pedobiologia - Journal of Soil Ecology. These editors work at universities and research centers in Europe, North America, Asia, and Australia.The questions were categorized into four themes: (1) soil biodiversity and biogeography, (2) interactions and the functioning of ecosystems, (3) global change and soil management, and (4) new directions. The respondents identified priorities that may be achievable in the near future, as well as several that are currently achievable but remain open. While some of the identified barriers to progress were technological in nature, many respondents cited a need for substantial leadership and goodwill among members of the soil ecology research community, including the need for multi-institutional partnerships, and had substantial concerns regarding the loss of taxonomic expertise.", "keywords": ["0301 basic medicine", "aboveground-belowground interactions", "Biologia", "Aboveground-belowground interactions", "910", "soil processes", "soil microbial ecology", "Microbial ecology", "Novel environments", "Soil food web", "11. Sustainability", "Climate change", "0503 Soil Sciences", "Global change", "biodiversity", "ecosystem management", "2. Zero hunger", "biodiversity\u2013ecosystem functioning", "0303 health sciences", "Plant-microbe interaction", "Agronomy & Agriculture", "Soil processes", "climate change", "ekosysteemipalvelut", "Biogeography", "international", "570", "Soil management", "Ecosystem service", "Biodiversity\u2013ecosystem functioning", "0607 Plant Biology", "plant-microbe interactions", "soil biodiversity", "Chemical ecology", "Aboveground-belowground interactions; Biodiversity\u2013ecosystem functioning; Biogeography; Chemical ecology; Climate change; Ecosystem services; Global change; Microbial ecology; Novel environments; Plant-microbe interactions; Soil biodiversity; Soil food web; Soil management; Soil processes", "climatic changes", "eli\u00f6maantiede", "12. Responsible consumption", "Aboveground-belowground interaction", "03 medical and health sciences", "soil food web", "Novel environment", "XXXXXX - Unknown", "Ecosystem services", "Biology", "global change", "maaper\u00e4nsuojelu", "chemical ecology", "500", "15. Life on land", "Soil biodiversity", "biodiversiteetti", "ekosysteemit (ekologia)", "mikrobiekologia", "13. Climate action", "ilmastonmuutos", "novel environments", "ta1181", "soil management", "Plant-microbe interactions", "0703 Crop And Pasture Production"]}, "links": [{"href": "https://usiena-air.unisi.it/bitstream/11365/1134372/2/Eisenhauer_et_al_research_priorities_20170503.pdf"}, {"href": "https://doi.org/10.1016/j.pedobi.2017.05.003"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Pedobiologia", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.pedobi.2017.05.003", "name": "item", "description": "10.1016/j.pedobi.2017.05.003", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.pedobi.2017.05.003"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-07-01T00:00:00Z"}}, {"id": "10.1016/j.scitotenv.2023.169662", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:16:37Z", "type": "Journal Article", "created": "2023-12-28", "title": "Plant-mediated CH4 exchange in wetlands: A review of mechanisms and measurement methods with implications for modelling", "description": "Plant-mediated CH4 transport (PMT) is the dominant pathway through which soil-produced CH4 can escape into the atmosphere and thus plays an important role in controlling ecosystem CH4 emission. PMT is affected by abiotic and biotic factors simultaneously, and the effects of biotic factors, such as the dominant plant species and their traits, can override the effects of abiotic factors. Increasing evidence shows that plant-mediated CH4 fluxes include not only PMT, but also within-plant CH4 production and oxidation due to the detection of methanogens and methanotrophs attached to the shoots. Despite the inter-species and seasonal differences, and the probable contribution of within-plant microbes to total plant-mediated CH4 exchange (PME), current process-based ecosystem models only estimate PMT based on the bulk biomass or leaf area index of aerenchymatous plants. We highlight five knowledge gaps to which more research efforts should be devoted. First, large between-species variation, even within the same family, complicates general estimation of PMT, and calls for further work on the key dominant species in different types of wetlands. Second, the interface (rhizosphere-root, root-shoot, or leaf-atmosphere) and plant traits controlling PMT remain poorly documented, but would be required for generalizations from species to relevant functional groups. Third, the main environmental controls of PMT across species remain uncertain. Fourth, the role of within-plant CH4 production and oxidation is poorly quantified. Fifth, the simplistic description of PMT in current process models results in uncertainty and potentially high errors in predictions of the ecosystem CH4 flux. Our review suggest that flux measurements should be conducted over multiple growing seasons and be paired with trait assessment and microbial analysis, and that trait-based models should be developed. Only then we are capable to accurately estimate plant-mediated CH4 emissions, and eventually ecosystem total CH4 emissions at both regional and global scales.", "keywords": ["Drivers", "330", "Plants", "Carbon Dioxide", "metaani", "Modelling", "Processes", "Soil", "Wetland plants", "Wetlands", "Mechanisms", "suot", "suokasvillisuus", "Plant CH4 transport", "Biomass", "Methane", "Ecosystem"]}, "links": [{"href": "https://doi.org/10.1016/j.scitotenv.2023.169662"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Science%20of%20The%20Total%20Environment", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.scitotenv.2023.169662", "name": "item", "description": "10.1016/j.scitotenv.2023.169662", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.scitotenv.2023.169662"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-03-01T00:00:00Z"}}, {"id": "10.1016/j.scitotenv.2024.176196", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:16:37Z", "type": "Journal Article", "created": "2024-09-13", "title": "Modeling bacterial transport and fate: Insight into the cascading consequences of soil water repellency and contrasting hydraulic conditions", "description": "The mechanisms governing bacteria transport and fate rely on their hydrophobicity and the wettability of porous media across a wide range of soil moisture conditions, extending from extreme dryness to highly saturated states. However, it largely remains unknown how transport, retention, and release mechanisms change in natural soil systems in such conditions. We thus optimized our previously published unique transport data for hydrophilic Escherichia coli (E. coli) and hydrophobic Rhodococcus erythropolis (R. erythropolis) bacteria, and bromide (Br-) in two distinct wettable and water-repellent soils at column scale. The soils were initially dry, followed by injecting influents in two pulses followed by a flushing step under saturated flow conditions for six pore volumes. We conducted simulations for each pulse separately and simultaneously for soils. There were differences in hydraulic properties of the soils due to their contrasting wetting characteristic in separate and simultaneously modeling of each pulse affecting Br- and bacteria transport fate. Bacteria attachment was the dominant retention mechanism in both soils in these conditions. Notably, the 82.4\u00a0min-1 attachment rate in wettable soil was almost 10\u00d7 greater than in the water-repellent soil and it governed optimization of bacteria die-off. Physicochemical detachment and physical release unraveled the effect of bacteria size and hydrophobicity interacting with soil wettability. The smaller and hydrophobic R. erythropolis detached more easily while hydrophilic E. coli released; the rates were enhanced by soil water repellency. Further research is needed to reveal the effects of surface wettability properties on bacteria survival especially at the nanoscale.", "keywords": ["690", "Bromides", "Bacteria", "QH301 Biology", "Transport processes", "610", "Attachment", "Water", "QH301", "Water repellency", "Soil", "Straining", "Escherichia coli", "Wettability", "Rhodococcus", "Hydrophobic and Hydrophilic Interactions", "Soil Microbiology"]}, "links": [{"href": "https://doi.org/10.1016/j.scitotenv.2024.176196"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Science%20of%20The%20Total%20Environment", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.scitotenv.2024.176196", "name": "item", "description": "10.1016/j.scitotenv.2024.176196", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.scitotenv.2024.176196"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-12-01T00:00:00Z"}}, {"id": "10.1016/j.soilbio.2017.12.003", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:16:49Z", "type": "Journal Article", "created": "2017-12-09", "title": "New insights into the role of microbial community composition in driving soil respiration rates", "description": "New insights into the role of microbial community composition in driving soil respiration rates. Published in Soil Biology and Biochemistry", "keywords": ["Carbon cycling", "2. Zero hunger", "Bacteria", "550", "carbon", "Fungi", "Ecosystem processes", "04 agricultural and veterinary sciences", "15. Life on land", "soil microbial ecology", "13. Climate action", "Microbial community", "XXXXXX - Unknown", "Bacteria", " fungi", " carbon cycling", " ecosystem processes", " microbial community", " global change", "0401 agriculture", " forestry", " and fisheries", "fungi", "bacteria", "Global change"]}, "links": [{"href": "https://doi.org/10.1016/j.soilbio.2017.12.003"}, {"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.2017.12.003", "name": "item", "description": "10.1016/j.soilbio.2017.12.003", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.soilbio.2017.12.003"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-03-01T00:00:00Z"}}, {"id": "10.1016/j.still.2005.11.005", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:16:54Z", "type": "Journal Article", "created": "2005-12-22", "title": "Carbon Inventory For A Cereal Cropping System Under Contrasting Tillage, Nitrogen Fertilisation And Stubble Management Practices", "description": "Abstract   Conservation farming practices are often considered effective measures to increase soil organic C (SOC) sequestration and/or to reduce CO 2  emissions resulting from farm machinery operation. The long-term CO 2  mitigation potentials of no-till (NT) versus conventional till (CT), stubble retention (SR) versus stubble burning (SB) and N fertilisation (NF) versus no N application (N0) as well as their interactions were examined on a Vertosol (Vertisol) in semi-arid subtropical Queensland, Australia by taking into account their impacts on SOC content, crop residue C storage, on-farm fossil fuel consumption and CO 2  emissions associated with N fertiliser application. The experimental site had been cropped with wheat ( Triticum aestivum  L.) or barley ( Hordeum vulgare  L.) with a summer fallow for 33 years.  Where NT, SR or NF was applied alone, no significant effect on SOC was found in the 0\u201310, 10\u201320 and 0\u201320\u00a0cm depths. Nonetheless, the treatment effects in the 0\u201310\u00a0cm depth were interactive and maximum SOC sequestration was achieved under the NT\u00a0+\u00a0SR\u00a0+\u00a0NF treatment. Carbon storage in crop residues decreased substantially during the fallow period, to a range between 0.4\u00a0Mg\u00a0CO 2 -e\u00a0ha \u22121  under the CT\u00a0+\u00a0SB\u00a0+\u00a0NF treatment and 2.4\u00a0Mg\u00a0CO 2 -e\u00a0ha \u22121  under the NT\u00a0+\u00a0SR\u00a0+\u00a0N0 treatment (CO 2 -e stands for CO 2  equivalent). The cumulative fossil fuel CO 2  emission over 33 years was estimated to be 2.2\u00a0Mg\u00a0CO 2 -e\u00a0ha \u22121  less under NT than under CT systems. Cumulative CO 2  emissions from N fertiliser application amounted to 3.0\u00a0Mg\u00a0CO 2 \u00a0ha \u22121 . The farm-level C accounting indicated that a net C sequestration of 4.5\u00a0Mg\u00a0CO 2 -e was achieved under the NT\u00a0+\u00a0SR\u00a0+\u00a0NF treatment, whilst net CO 2  emissions ranging from 0.5 to 6.0\u00a0Mg\u00a0CO 2 -e\u00a0ha \u22121  over 33 years occurred under other treatments.", "keywords": ["Carbon sequestration", "2. Zero hunger", "571", "550", "Greenhouse", "Nitrogen", "1904 Earth-Surface Processes", "No-till", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "Carbon", "Stubble retention", "Tillage", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "1102 Agronomy and Crop Science", "Global change", "1111 Soil Science", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.still.2005.11.005"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20and%20Tillage%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.still.2005.11.005", "name": "item", "description": "10.1016/j.still.2005.11.005", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.still.2005.11.005"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2006-12-01T00:00:00Z"}}, {"id": "10.1016/j.still.2006.08.005", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:16:54Z", "type": "Journal Article", "created": "2006-09-19", "title": "No-Till Effects On Organic Matter, Ph, Cation Exchange Capacity And Nutrient Distribution In A Luvisol In The Semi-Arid Subtropics", "description": "No-till (NT) system for grain cropping is increasingly being practised in Australia. While benefits of NT, accompanied by stubble retention, are almost universal for soil erosion control, effects on soil organic matter and other soil properties are inconsistent, especially in a semi-arid, subtropical environment. We examined the effects of tillage, stubble and fertilizer management on the distribution of organic matter and nutrients in the topsoil (0\u201030 cm) of a Luvisol in a semi-arid, subtropical environment in southern Queensland, Australia. Measurements were made at the end of 9 years of NT, reduced till (RT) and conventional till (CT) practices, in combination with stubble retention and fertilizer N (as urea) application strategies for wheat (Triticum aestivum L.) cropping. In the top 30 cm depth, the mean amount of organic C increased slightly after 9 years, although it was similar under all tillage practices, while the amount of total N declined under CTand RT practices, but not under NT. In the 0\u201010 cm depth, the amounts of organicC and total N were significantly greater under NT than under RTor CT. No-till had 1.94 Mg ha 1 (18%) more organicC and 0.20 Mg ha 1 (21%) more total N than CT. In the 0\u201030 cm depth, soil under NT practice had 290 kg N ha 1 more than that under the CT practice, most of it in the top 10 cm depth. Microbial biomass N was similar for all treatments. Under NT, there was a concentration gradient in organic C, total N and microbial biomass N, with concentrations decreasing from 0\u20102.5 to 5\u201010 cm depths. SoilpHwasnotaffectedbytillageorstubbletreatmentsinthe0\u201010 cmdepth,butdecreasedsignificantlyfrom7.5to7.2withN fertilizer application. Exchangeable Mg and Na concentration, cation exchange capacity and exchangeable Na percentage in the 0\u201010 cmdepthweregreaterunderCTthanunderRTandNT,whileexchangeableKandbicarbonate-extractablePconcentrations were greater under NT than under CT. Therefore, NTand RT practices resulted in significant changes in soil organic C and N and exchangeable cations in the topsoil of a Luvisol, when compared with CT. The greater organic matter accumulation close to the soil surface and solute movement in these soils under NT practice would be beneficial to soil chemical and physical status and crop production in the long-term, whereas the concentration of nutrients such as P and K in surface layers may reduce their availability to crops. # 2006 Elsevier B.V. All rights reserved.", "keywords": ["2. Zero hunger", "550", "pH", "1904 Earth-Surface Processes", "Luvisol", "No-till", "04 agricultural and veterinary sciences", "Total nitrogen", "15. Life on land", "01 natural sciences", "630", "6. Clean water", "Cations", "0401 agriculture", " forestry", " and fisheries", "1102 Agronomy and Crop Science", "Organic carbon", "1111 Soil Science", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.still.2006.08.005"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20and%20Tillage%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.still.2006.08.005", "name": "item", "description": "10.1016/j.still.2006.08.005", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.still.2006.08.005"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2007-06-01T00:00:00Z"}}, {"id": "10.1016/j.still.2008.10.012", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:16:56Z", "type": "Journal Article", "created": "2008-12-07", "title": "Controlled Traffic Farming With No Tillage For Improved Fallow Water Storage And Crop Yield On The Chinese Loess Plateau", "description": "On the semi-arid Loess Plateau of northern China, water is typically the biggest constraint to rainfed wheat production. Controlled traffic, combined with zero tillage and residue cover has been proposed to improve soil water, crop yield and water use efficiency. From 1998 to 2005, we conducted a field experiment comparing the water storage and wheat productivity of controlled traffic farming and conventional tillage farming. Three treatments were studied: controlled traffic with no tillage and full residue cover (NTCN), controlled traffic with shallow tillage and full residue cover (STCN) and random traffic with traditional tillage and partial residue cover (CT). Compared to CT, the controlled traffic treatments significantly reduced soil bulk density in 10-20 cm soil layer, significantly increased soil water content in the 0-150 cm soil profile at sowing, 9.3% for NTCN, 9.6% for STCN. These effects were greater in dry seasons, thus reducing the yearly variation in water conservation. Consequently, mean wheat yield of NTCN, STCN and CT were 3.25, 3.27 and 3.05 t ha-1, respectively, in which controlled traffic treatments increased by 6.9% with less yearly variation, compared to traditional tillage. Furthermore, controlled traffic had greater economic benefits than conventional tillage. Within controlled traffic treatments, NTCN showed better overall performance. In conclusion, controlled traffic farming has a better performance with respect to conserving water, improves yields and increases economic benefits. No tillage controlled traffic farming appears to be a solution to the water problem facing farmers on the Loess Plateau of China.", "keywords": ["macropore density", "0106 biological sciences", "2. Zero hunger", "Yields", "bulk density", "571", "available water capacity", "Fallow water storage", "1904 Earth-Surface Processes", "permanent beds", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "6. Clean water", "Zero tillage", "Vertosol", "Controlled traffic", "controlled traffic", "0401 agriculture", " forestry", " and fisheries", "compaction", "1102 Agronomy and Crop Science", "amelioration", "zero tillage", "1111 Soil Science"]}, "links": [{"href": "https://doi.org/10.1016/j.still.2008.10.012"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20and%20Tillage%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.still.2008.10.012", "name": "item", "description": "10.1016/j.still.2008.10.012", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.still.2008.10.012"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2009-06-01T00:00:00Z"}}, {"id": "10.1016/j.still.2010.10.009", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:16:58Z", "type": "Journal Article", "created": "2010-11-20", "title": "Soil Organic Matter Humification Under Different Tillage Managements Evaluated By Laser Induced Fluorescence (Lif) And C/N Ratio", "description": "AbstractIn this work is presented the use of the C/N ratio and the Laser Induced Fluorescence (LIF) spectroscopy for determining the humification of soil organic matter (SOM) in an Oxisol under three different long-term tillage managements (no-tillage (NT), reduced tillage (RT) and conventional tillage (CT)). Humification of SOM was evaluated in the soil and its fractions (clay<2\u03bcm, silt 2\u201320\u03bcm, sand 20\u20131000\u03bcm). The obtained results show that lower SOM humification was observed in soil under NT, mainly at the surface (0\u20135cm). In CT, SOM humification values maintained constant for all investigated depths (0\u20135, 5\u201310, 10\u201315 and 15\u201320cm). Also, clay was the soil fraction that exhibited the lesser humification of SOM. Based on the obtained results it can be said that NT favors the accumulation of SOM on its surface, increasing aggregate stability and presenting samples with lower humification indexes. These results indicate a larger availability of nutrients for the plants in this management.", "keywords": ["Degree of humification", "No-tillage management system", "Soil fractions", "Soil Science", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land", "Agronomy and Crop Science", "6. Clean water", "Earth-Surface Processes"], "contacts": [{"organization": "Jadir Aparecido Rosa, Luiz F. Pires, F.A.M. C\u00e1ssaro, S\u00e9rgio da Costa Saab, Andr\u00e9 Maur\u00edcio Brinatti, T. Martins, D\u00e9bora Marcondes Bastos Pereira Milori,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1016/j.still.2010.10.009"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20and%20Tillage%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.still.2010.10.009", "name": "item", "description": "10.1016/j.still.2010.10.009", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.still.2010.10.009"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2011-01-01T00:00:00Z"}}, {"id": "10.1016/j.still.2015.03.005", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:17:01Z", "type": "Journal Article", "created": "2015-03-13", "title": "Corn Residue, Tillage, And Nitrogen Rate Effects On Soil Properties", "description": "A B S T R A C T Harvesting corn (Zea mays L.) residue for use as a biofuel feedstock may alter important chemical and physical properties of soils. Long-term residue removal, linked with tillage and fertilizer practices, could lower soil organic carbon (SOC), as well as increase soil compaction and susceptibility to erosion. A study initiated in 2006 included three levels of residue removal (none, partial, or full removal), two tillage treatments (no-till or chisel plow), and two N application rates (134 and 268 kg N/ha). These experiments were established in continuous corn (CC) at four Illinois sites, with treatments remaining in the same plots each year. In the spring at the beginning of the eighth growing season, we measured total carbon stocks (SOC), water aggregate stability (WAS), soil bulk density (BD), and penetration resistance (PR). Results showed that with all crop residue retained in the field, SOC stocks 13% lower under chisel tillage than in no-tilled plots, but removal of some or all of the residue lowered the SOC levels of no-tilled plots to those of tilled plots. On average for the studied depths, no-till plots had 5% and 39% higher BD and PR, respectively, than tilled plots, and residue removal significantly increased PR under no-till. Regardless of tillage treatment, the highest WAS values were found without residue removal at the lower N rate and with partial removal at the higher N rate. The higher N rate slightly lowered the BD under partial removal of residue for both tillage treatments at both studied depths. Our results indicate that residue harvest generates modest changes in soil properties under continuous corn, likely smaller than the effects of tillage and N fertilizer use in these systems. But as long as residue amount and tillage practices are sufficient to limit losses of soil by erosion to acceptable levels, we believe that corn residue represents a viable feedstock for a sustainable bioenergy industry in the U.S. Midwest.", "keywords": ["2. Zero hunger", "Soil Science", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land", "Agronomy and Crop Science", "Earth-Surface Processes"]}, "links": [{"href": "https://doi.org/10.1016/j.still.2015.03.005"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20and%20Tillage%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.still.2015.03.005", "name": "item", "description": "10.1016/j.still.2015.03.005", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.still.2015.03.005"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2015-08-01T00:00:00Z"}}, {"id": "10.1016/j.still.2016.08.012", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:17:02Z", "type": "Journal Article", "created": "2016-08-23", "title": "Aggregate Size Distribution In A Biochar-Amended Tropical Ultisol Under Conventional Hand-Hoe Tillage", "description": "Biochar (or pyrogenic organic matter) is increasingly proposed as a soil amendment for improving fertility, carbon sequestration and reduction of greenhouse gas emissions. However, little is known about its effects on aggregation, an important indicator of soil quality and functioning. The aim of this study was to assess the effect of Eucalyptus wood biochar (B, pyrolyzed at 550\u00a0\u00b0C, at 0 or 2.5\u00a0t\u00a0ha-1), green manure (T, from Tithonia diversifolia at 0, 2.5 or 5.0\u00a0t\u00a0ha-1) and mineral nitrogen (U, urea, at 0, or 120\u00a0kg\u00a0N\u00a0ha-1) on soil respiration, aggregate size distribution and SOC in these aggregate size fractions in a 2-year field experiment on a low-fertility Ultisol in western Kenya under conventional hand-hoe tillage. Air-dry 2-mm sieved soils were divided into four fractions by wet sieving: Large Macro-aggregates (LM; >1000\u00a0\u03bcm); Small Macro-aggregates (SM, 250-1000\u00a0\u03bcm); Micro-aggregates (M, 250-53\u00a0\u03bcm) and Silt\u00a0+\u00a0Clay (S\u00a0+\u00a0C,\u2009<\u00a053\u00a0\u03bcm). We found that biochar alone did not affect a mean weight diameter (MWD) but combined application with either T. diversifolia (BT) or urea (BU) increased MWD by 34\u00a0\u00b1\u00a05.2\u00a0\u03bcm (8%) and 55\u00a0\u00b1\u00a05.4\u00a0\u03bcm (13%), respectively, compared to the control (P\u00a0=\u00a00.023; n\u00a0=\u00a036). The B\u00a0+\u00a0T\u00a0+\u00a0U combination increased the proportion of the LM and SM by 7.0\u00a0\u00b1\u00a00.8%, but reduced the S\u00a0+\u00a0C fraction by 5.2\u00a0\u00b1\u00a00.23%. SOC was 30%, 25% and 23% in S\u00a0+\u00a0C,\u00a0M and LM/SM fractions, and increased by 9.6\u00a0\u00b1\u00a01.0, 5.7\u00a0\u00b1\u00a00.8, 6.3\u00a0\u00b1\u00a01.1 and 4.2\u00a0\u00b1\u00a00.9\u00a0g\u00a0kg-1 for LM, SM, M and S\u00a0+\u00a0C, respectively. MWD was not related to either soil respiration or soil moisture but decreased with higher SOC (R2 \u00a0=\u00a00.37, P\u00a0=\u00a00.014, n\u00a0=\u00a026) and increased with greater biomass production (R2 \u00a0=\u00a00.11, P\u00a0=\u00a00.045, n\u00a0=\u00a033). Our data suggest that within the timeframe of the study, biochar is stored predominantly as free particulate OC in the silt and clay fraction and promoted a movement of native SOC from larger-size aggregates to the smaller-sized fraction in the short-term (2 years).", "keywords": ["2. Zero hunger", "Soil organic carbon", "Soil Science", "Soil respiration", "04 agricultural and veterinary sciences", "15. Life on land", "Hand-hoe tillage", "Article", "6. Clean water", "Biochar", "13. Climate action", "Soil aggregation", "Ultisol", "0401 agriculture", " forestry", " and fisheries", "Agronomy and Crop Science", "Earth-Surface Processes"]}, "links": [{"href": "https://doi.org/10.1016/j.still.2016.08.012"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20and%20Tillage%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.still.2016.08.012", "name": "item", "description": "10.1016/j.still.2016.08.012", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.still.2016.08.012"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-01-01T00:00:00Z"}}, {"id": "10.1029/2021ms002730", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:17:25Z", "type": "Journal Article", "created": "2022-02-17", "title": "Characterising the response of vegetation cover to water limitation in Africa using geostationary satellites", "description": "Abstract<p>Hydrological interactions between vegetation, soil, and topography are complex, and heterogeneous in semi\uffe2\uff80\uff90arid landscapes. This along with data scarcity poses challenges for large\uffe2\uff80\uff90scale modeling of vegetation\uffe2\uff80\uff90water interactions. Here, we exploit metrics derived from daily Meteosat data over Africa at ca. 5\uffc2\uffa0km spatial resolution for ecohydrological analysis. Their spatial patterns are based on Fractional Vegetation Cover (FVC) time series and emphasize limiting conditions of the seasonal wet to dry transition: the minimum and maximum FVC of temporal record, the FVC decay rate and the FVC integral over the decay period. We investigate the relevance of these metrics for large scale ecohydrological studies by assessing their co\uffe2\uff80\uff90variation with soil moisture, and with topographic, soil, and vegetation factors. Consistent with our initial hypothesis, FVC minimum and maximum increase with soil moisture, while the FVC integral and decay rate peak at intermediate soil moisture. We find evidence for the relevance of topographic moisture variations in arid regions, which, counter\uffe2\uff80\uff90intuitively, is detectable in the maximum but not in the minimum FVC. We find no clear evidence for wide\uffe2\uff80\uff90spread occurrence of the \uffe2\uff80\uff9cinverse texture effect\uffe2\uff80\uff9d on FVC. The FVC integral over the decay period correlates with independent data sets of plant water storage capacity or rooting depth while correlations increase with aridity. In arid regions, the FVC decay rate decreases with canopy height and tree cover fraction as expected for ecosystems with a more conservative water\uffe2\uff80\uff90use strategy. Thus, our observation\uffe2\uff80\uff90based products have large potential for better understanding complex vegetation\uffe2\uff80\uff90water interactions from regional to continental scales.</p>", "keywords": ["Physical geography", "GROUNDWATER-DEPENDENT ECOSYSTEMS", "water limitation", "GC1-1581", "geostationary", "SOIL-MOISTURE", "Oceanography", "01 natural sciences", "ecohydrology", "ROOTING DEPTH", "ACTIVE-ROLE", "WOODY COVER", "0105 earth and related environmental sciences", "fractional vegetation cover", "HYDROLOGIC PROCESSES", "15. Life on land", "6. Clean water", "GB3-5030", "MODEL", "CLIMATE", "13. Climate action", "Earth and Environmental Sciences", "PRECIPITATION", "Africa", "PATTERNS", "Research Article"]}, "links": [{"href": "https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2021MS002730"}, {"href": "https://doi.org/10.1029/2021ms002730"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Advances%20in%20Modeling%20Earth%20Systems", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1029/2021ms002730", "name": "item", "description": "10.1029/2021ms002730", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1029/2021ms002730"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-11-25T00:00:00Z"}}, {"id": "10.1021/acs.est.1c03586", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:17:11Z", "type": "Journal Article", "created": "2021-11-02", "title": "Impact of Periodic Polarization on Groundwater Denitrification in Bioelectrochemical Systems.", "description": "Nitrate contamination is a common problem in groundwater around the world. Nitrate can be cathodically reduced in bioelectrochemical systems using autotrophic denitrifiers with low energy investment and without chemical addition. Successful denitrification was demonstrated in previous studies in both microbial fuel cells and microbial electrolysis cells (MECs) with continuous current flow, whereas the impact of intermittent current supply (e.g., in a fluidized-bed system) on denitrification and particularly the electron-storing capacity of the denitrifying electroactive biofilms (EABs) on the cathodes have not been studied in depth. In this study, two continuously fed MECs were operated in parallel under continuous and periodic polarization modes over 280 days, respectively. Under continuous polarization, the maximum denitrification rate reached 233 g NO3--N/m3/d with 98% nitrate removal (0.6 mg NO3--N/L in the effluent) with negligible intermediate production, while under a 30 s open-circuit/30 s polarization mode, 86% of nitrate was removed at a maximum rate of 205 g NO3--N/m3/d (4.5 mg NO3--N/L in the effluent) with higher N2O production (6.6-9.3 mg N/L in the effluent). Conversely, periodic polarization could be an interesting approach in other bioelectrochemical processes if the generation of chemical intermediates (partially reduced or oxidized) should be favored. Similar microbial communities dominated byGallionellaceaewere found in both MECs; however, swapping the polarization modes and the electrochemical analyses suggested that the periodically polarized EABs probably developed a higher ability for electron storage and transfer, which supported the direct electron transfer pathway in discontinuous operation or fluidized biocathodes.", "keywords": ["bioelectrochemical systems (BESs)", "periodic polarization", "Autotrophic Processes", "Technology and Engineering", "denitrification", "Nitrates", "AUTOTROPHIC DENITRIFICATION", "EABs", "Bioelectric Energy Sources", "NITRATE-CONTAMINATED GROUNDWATER", "02 engineering and technology", "6. Clean water", "REDUCTION", "REMOVAL", "13. Climate action", "Earth and Environmental Sciences", "BACTERIA", "ACETATE", "Denitrification", "MICROBIAL FUEL-CELLS", "ELECTRON-TRANSFER", "BIOFILM", "0210 nano-technology", "Groundwater", "STORAGE"]}, "links": [{"href": "https://pubs.acs.org/doi/pdf/10.1021/acs.est.1c03586"}, {"href": "https://doi.org/10.1021/acs.est.1c03586"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Environmental%20Science%20%26amp%3B%20Technology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1021/acs.est.1c03586", "name": "item", "description": "10.1021/acs.est.1c03586", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1021/acs.est.1c03586"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-11-02T00:00:00Z"}}, {"id": "10.1029/2020gb006719", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:17:24Z", "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": "10.1071/sr04044", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:17:51Z", "type": "Journal Article", "created": "2005-02-17", "title": "Total Soil Organic Matter And Its Labile Pools Following Mulga (Acacia Aneura) Clearing For Pasture Development And Cropping 1. Total And Labile Carbon", "description": "<p> Mulga (Acacia aneura) dominated vegetation originally occupied 11.2 Mha in Queensland, of which 12% has been cleared, mostly for pasture production, but some areas are also used for cereal cropping. Since mulga communities generally occupy fragile soils, mostly Kandosols and Tenosols, in semi-arid environments, clearing of mulga, which continues at a rate of at least 35 000 ha/year in Queensland, has considerable impact on soil organic carbon (C), and may also have implications for the greenhouse gas emissions associated with land use change in Australia. We report here the changes in soil C and labile C pools following mulga clearing to buffel pasture (Cenchrus ciliaris) and cereal (mostly wheat) cropping for 20 years in a study using paired sites. Soil organic C in the top 0.05 m of soil declined by 31% and 35% under buffel pasture and cropping, respectively. Land use change from mulga to buffel and cropping led to declines in soil organic C of 2.4 and 4.7 t/ha, respectively, from the top 0.3 m of soil. Using changes in the \uffce\uffb413C values of soil organic C as an approximate representation of C derived from C3 and C4 vegetation from mulga and buffel, respectively, up to 31% of soil C was C4-derived after 20 years of buffel pasture. The turnover rates of mulga-derived soil C ranged from 0.035/year in the 0\uffe2\uff80\uff930.05 m depth to 0.008/year in the 0.6\uffe2\uff80\uff931 m depths, with respective turnover times of 29 and 133 years. Soil organic matter quality, as measured by the proportion/amount of labile fraction C (light fraction, &lt; 1.6 t/m3) declined by 55% throughout the soil profile (0\uffe2\uff80\uff931 m depth) under both pasture and cropping. There is immediate concern for the long-term sustainable use of land where mulga has been cleared for pasture and/or cropping with a continuing decline in soil organic matter quality and, hence, soil fertility and biomass productivity. In addition, the removal of mulga forest over a 20-year period in Queensland for pasture and cropping may have contributed to the atmosphere at least 12 Mt CO2-equivalents. </p>", "keywords": ["2. Zero hunger", "13. Climate action", "1904 Earth-Surface Processes", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land", "Greenhouse effect", "\u03b4C", "Labile C", "Organic matter quality", "Soil C loss", "1111 Soil Science", "12. Responsible consumption"]}, "links": [{"href": "https://doi.org/10.1071/sr04044"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1071/sr04044", "name": "item", "description": "10.1071/sr04044", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1071/sr04044"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2005-01-01T00:00:00Z"}}, {"id": "10.1071/sr12225", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:17:53Z", "type": "Journal Article", "created": "2013-02-19", "title": "Organic Carbon Stocks In Cropping Soils Of Queensland, Australia, As Affected By Tillage Management, Climate, And Soil Characteristics", "description": "<p>  Research both nationally and internationally has indicated that no-till (NT) management used in combination with stubble retention has the potential to increase soil organic carbon (SOC) stocks in cropping soils relative to conventional tillage (CT). However, rates of SOC increase can vary depending on cropping system, climate, and soil type, making the quantification of carbon change difficult on a regional level. Various long-term trials and commercial sites throughout Queensland were used to compare rates of SOC change under CT and NT management in cropping soils, and to determine how climate and soil type interact to influence rates of change. It was observed that NT management was not capable of increasing SOC stocks under the crop\uffe2\uff80\uff93fallow rotation systems practised throughout Queensland, and was unlikely even to hold SOC stocks steady under current management practices. However, SOC losses under NT systems did appear to be slower than under CT, indicating that NT may slow SOC loss following a period of organic carbon input, for example, from a pasture ley. On a regional scale, biomass production (estimated through remote sensing), climate (specifically the vapour pressure deficit), and soil sand content could be used to adequately predict SOC stocks on commercial sites, indicating the importance of considering these factors when assessing SOC stocks following management change across the region. </p>", "keywords": ["2. Zero hunger", "550", "Climate", "1904 Earth-Surface Processes", "2301 Environmental Science (miscellaneous)", "No-till", "04 agricultural and veterinary sciences", "15. Life on land", "Organic carbon stocks", "Stubble retention", "Vapour pressure deficit", "0401 agriculture", " forestry", " and fisheries", "1111 Soil Science", "Sand content"]}, "links": [{"href": "https://doi.org/10.1071/sr12225"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1071/sr12225", "name": "item", "description": "10.1071/sr12225", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1071/sr12225"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2013-01-01T00:00:00Z"}}, {"id": "10.1071/sr18210", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:17:53Z", "type": "Journal Article", "created": "2018-11-16", "title": "Effect of long-term irrigation and tillage practices on X-ray CT and gas transport derived pore-network characteristics", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p> The gas transport parameters, diffusivity and air-filled porosity are crucial for soil aeration, microbial activity and greenhouse gas emission, and directly depend on soil structure. In this study, we analysed the effect of long-term tillage and irrigation practices on the surface structure of an arable soil in New Zealand. Our hypothesis was that topsoil structure would change under intensification of arable production, affecting gas exchange. Intact soil cores were collected from plots under intensive tillage (IT) and direct drill (DD), irrigated or rainfed. In total, 32 cores were scanned by X-ray computed tomography (CT) to derive the pore network &amp;gt;30\u00b5m. The cores were then used to measure soil-gas diffusivity, air-permeability and air-filled porosity of pores close to the resolution of the X-ray CT scans, namely \u226530\u00b5m. The gas measurements allow the calculation of pore-network connectivity and tortuosity parameters, which were compared with the CT-derived structural characteristics. Long-term irrigation had little effect on any of the parameters analysed. Total porosity tended to be lower under IT than DD, whereas the CT-derived porosity was comparable. Both the CT-derived mean pore diameter (MPD) and other morphological parameters, as well as gas measurement-derived parameters, highlighted a less developed structure under IT. The differences in the functional pore-network structure were attributed to SOC depletion and the mechanical disturbance through IT. Significant correlations between CT-derived parameters and functional gas transport parameters such as tortuosity and MPD were found, which suggest that X-ray CT could be useful in the prediction of gas transport. </p></article>", "keywords": ["AGRICULTURE", "soil structure.", "P-parameter", "Soil structure", "carbon depletion", "MANAGEMENT", "COMPUTED-TOMOGRAPHY", "PERMEABILITY", "CONSERVATION TILLAGE", "Dexter index", "Intensive tillage", "SOIL ORGANIC-CARBON", "carbon depletion; Dexter index; intensive tillage; P -parameter; soil organic carbon; soil structure.; Environmental Science (miscellaneous); Soil Science; Earth-Surface Processes", "P -parameter", "LOAM SOIL", "Soil organic carbon", "POROSITY", "04 agricultural and veterinary sciences", "15. Life on land", "soil organic carbon", "NO-TILL", "NITROGEN", "[SDE.MCG] Environmental Sciences/Global Changes", "0401 agriculture", " forestry", " and fisheries", "Carbon depletion", "soil structure", "intensive tillage"]}, "links": [{"href": "https://www.publish.csiro.au/SR/pdf/SR18210"}, {"href": "https://doi.org/10.1071/sr18210"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1071/sr18210", "name": "item", "description": "10.1071/sr18210", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1071/sr18210"}, {"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": "10.1111/gcb.16042", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:18:35Z", "type": "Journal Article", "created": "2021-12-19", "title": "Stimulation of ammonia oxidizer and denitrifier abundances by nitrogen loading: Poor predictability for increased soil N2O emission", "description": "Abstract<p>Unprecedented nitrogen (N) inputs into terrestrial ecosystems have profoundly altered soil N cycling. Ammonia oxidizers and denitrifiers are the main producers of nitrous oxide (N2O), but it remains unclear how ammonia oxidizer and denitrifier abundances will respond to N loading and whether their responses can predict N\uffe2\uff80\uff90induced changes in soil N2O emission. By synthesizing 101 field studies worldwide, we showed that N loading significantly increased ammonia oxidizer abundance by 107% and denitrifier abundance by 45%. The increases in both ammonia oxidizer and denitrifier abundances were primarily explained by N loading form, and more specifically, organic N loading had stronger effects on their abundances than mineral N loading. Nitrogen loading increased soil N2O emission by 261%, whereas there was no clear relationship between changes in soil N2O emission and shifts in ammonia oxidizer and denitrifier abundances. Our field\uffe2\uff80\uff90based results challenge the laboratory\uffe2\uff80\uff90based hypothesis that increased ammonia oxidizer and denitrifier abundances by N loading would directly cause higher soil N2O emission. Instead, key abiotic factors (mean annual precipitation, soil pH, soil C:N ratio, and ecosystem type) explained N\uffe2\uff80\uff90induced changes in soil N2O emission. Altogether, these findings highlight the need for considering the roles of key abiotic factors in regulating soil N transformations under N loading to better understand the microbially mediated soil N2O emission.</p", "keywords": ["IMPACTS", "0301 basic medicine", "570", "GENES", "Nitrogen", "REGIMES", "Nitrous Oxide", "Precipitation", "Soil pH", "precipitation", "NITRIFICATION", "nitrogen addition", "01 natural sciences", "630", "OXIDE EMISSIONS", "Nitrogen/analysis", "soil pH", "Soil", "03 medical and health sciences", "Ammonia", "FERTILIZATION", "MANAGEMENT", "Nitrous Oxide/analysis", "Biological and chemical processes", "METAANALYSIS", "Research Articles", "Ecosystem", "Soil Microbiology", "0105 earth and related environmental sciences", "Microbial gene abundance", "2. Zero hunger", "biological and chemical processes", "Nitrogen addition", "0303 health sciences", "denitrification", "Nitrous oxide", "nitrous oxide", "15. Life on land", "Nitrification", "nitrification", "6. Clean water", "microbial gene abundance", "13. Climate action", "Denitrification", "COMMUNITIES", "GRASSLANDS"]}, "links": [{"href": "https://doi.org/10.1111/gcb.16042"}, {"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.16042", "name": "item", "description": "10.1111/gcb.16042", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcb.16042"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-12-29T00:00:00Z"}}, {"id": "10.1109/jphotov.2019.2943706", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:18:24Z", "type": "Journal Article", "created": "2019-10-23", "title": "Extracting and Generating PV Soiling Profiles for Analysis, Forecasting, and Cleaning Optimization", "description": "<p>&lt;div&gt;&lt;div&gt;&lt;div&gt;&lt;div&gt;The identification and prediction of the daily soiling profiles of a photovoltaic site is essential to plan the optimal cleaning schedule. In this article, we analyze and propose various methods to extract and generate photovoltaic soiling profiles, in order to improve the analysis and the forecast of the losses. New soiling rate extraction methods are proposed to reflect the seasonal variability of the soiling rates and, for this reason, are found to identify the most convenient cleaning day with the highest accuracy for the investigated sites. Also, we present an approach that could be used to predict future soiling losses through the implementation of stochastic weather generation algorithms whose ability to identify in advance the best cleaning schedule is also successfully tested. The methods presented in this article can optimize the operation and maintenance schedule and could make it possible, in the future, to predict soiling losses through analysis based only on environmental parameters, such as rainfall and particulate matter, without the need of long-term soiling data.&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;</p>", "keywords": ["Optimization", "Power", " Energy and Industry Applications", "Schedules", "Rain", "Cleaning", "Field Performance", "solar energy", "0211 other engineering and technologies", "02 engineering and technology", "Prediction methods", "7. Clean energy", "13. Climate action", "Soil measurements", "time series analysis", "0202 electrical engineering", " electronic engineering", " information engineering", "soiling", "stochastic processes", "Data mining", "Photovoltaic systems", "field performance; optimization; photovoltaic (PV) systems; prediction methods; soiling; solar energy; stochastic processes; time series analysis"]}, "links": [{"href": "https://iris.uniroma1.it/bitstream/11573/1625584/3/Micheli_postprint_Extracting_2020.pdf"}, {"href": "http://xplorestaging.ieee.org/ielx7/5503869/8939133/08880477.pdf?arnumber=8880477"}, {"href": "https://doi.org/10.1109/jphotov.2019.2943706"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/IEEE%20Journal%20of%20Photovoltaics", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1109/jphotov.2019.2943706", "name": "item", "description": "10.1109/jphotov.2019.2943706", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1109/jphotov.2019.2943706"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-11-03T00:00:00Z"}}, {"id": "10.1111/arcm.12605", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:18:28Z", "type": "Journal Article", "created": "2020-08-07", "title": "Ceramic productions and human interactions during the Early Bronze Age in northern Iberia", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>The Early Bronze Age ceramic collection found into the caves of La Llana and El Toral III in Asturias (Spain) presents common decoration such as that found in the centre of Cantabrian Spain from the same period, which resembles others found in the Ebro Valley and Atlantic Europe. Therefore, the main objective of this study it is to identify the raw material origin and understand the pottery production process during the Early Bronze Age in the Cantabrian region. A methodological approach based on the chemical and mineralogical analysis of vessels and experimentally fired clay samples collected all over the centre of this region was developed. Furthermore, the post\u2010depositional processes affecting the sherds\u2019 composition was evaluated by employing the rare earth elements as markers. The results showed that the studied assemblage has important similarities with the raw materials of the surrounding area, which supports the hypothesis of a regional mobility.</p></article>", "keywords": ["Human mobility", "Pottery", "Rare earth element", "Chemical-mineralogical characterisation", "Post-depositional processes", "0601 history and archaeology", "06 humanities and the arts", "01 natural sciences", "Raw material", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1111/arcm.12605"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Archaeometry", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/arcm.12605", "name": "item", "description": "10.1111/arcm.12605", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/arcm.12605"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-09-02T00:00:00Z"}}, {"id": "10.1111/ejss.12487", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:18:30Z", "type": "Journal Article", "created": "2017-10-27", "title": "Plant exudates may stabilize or weaken soil depending on species, origin and time", "description": "Summary<p>We hypothesized that plant exudates could either gel or disperse soil depending on their chemical characteristics. Barley (Hordeum vulgare L. cv. Optic) and maize (Zea mays L. cv. Freya) root exudates were collected using an aerated hydroponic method and compared with chia (Salvia hispanica L.) seed exudate, a commonly used root exudate analogue. Sandy loam soil was passed through a 500\uffe2\uff80\uff90\uffce\uffbcm mesh and treated with each exudate at a concentration of 4.6 mg exudate g\uffe2\uff88\uff921 dry soil. Two sets of soil samples were prepared. One set of treated soil samples was maintained at 4\uffc2\uffb0C to suppress microbial processes. To characterize the effect of decomposition, the second set of samples was incubated at 16\uffc2\uffb0C for 2 weeks at \uffe2\uff88\uff9230 kPa matric potential. Gas chromatography\uffe2\uff80\uff93mass spectrometry (GC\uffe2\uff80\uff93MS) analysis of the exudates showed that barley had the largest organic acid content and chia the largest content of sugars (polysaccharide\uffe2\uff80\uff90derived or free), and maize was in between barley and chia. Yield stress of amended soil samples was measured by an oscillatory strain sweep test with a cone plate rheometer. When microbial decomposition was suppressed at 4\uffc2\uffb0C, yield stress increased 20\uffe2\uff80\uff90fold for chia seed exudate and twofold for maize root exudate compared with the control, whereas for barley root exudate decreased to half. The yield stress after 2 weeks of incubation compared with soil with suppressed microbial decomposition increased by 85% for barley root exudate, but for chia and maize it decreased by 87 and 54%, respectively. Barley root exudation might therefore disperse soil and this could facilitate nutrient release. The maize root and chia seed exudates gelled soil, which could create a more stable soil structure around roots or seeds.</p>Highlights<p>  <p>Rheological measurements quantified physical behaviour of plant exudates and effect on soil stabilization.</p> <p>Barley root exudates dispersed soil, which could release nutrients and carbon.</p> <p>Maize root and chia seed exudates had a stabilizing effect on soil.</p> <p>Physical engineering of soil in contact with plant roots depends on the nature and origin of exudates.</p>  </p>", "keywords": ["construction", "0301 basic medicine", "EP/M020355/1", "seed exudate", "QH301 Biology", "610", "root exudate", "630", "QH301", "03 medical and health sciences", "DIMR 646809", "microbial decompisition", "Physical Processes and Function", "NE/L00237/1", "2. Zero hunger", "soil gelling", "BB/J000868/1", "Civil_env_eng", "Natural Environment Research Council (NERC)", "04 agricultural and veterinary sciences", "15. Life on land", "6. Clean water", "yield stress", "BB/J011460/1", "BB/L026058/1", "Engineering and Physical Sciences Research Council (EPSRC)", "soil dispersion", "viscosity", "Biotechnology and Biological Sciences Research Council (BBSRC)", "0401 agriculture", " forestry", " and fisheries", "microbial decomposition", "yeild stress", "European Research Council"]}, "links": [{"href": "https://repository.uwl.ac.uk/id/eprint/4980/1/Naveed_et_al-2017-European_Journal_of_Soil_Science.pdf"}, {"href": "https://eprints.soton.ac.uk/414238/1/EJSS_submitted_Manuscript.pdf"}, {"href": "http://onlinelibrary.wiley.com/wol1/doi/10.1111/ejss.12487/fullpdf"}, {"href": "https://doi.org/10.1111/ejss.12487"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/European%20Journal%20of%20Soil%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/ejss.12487", "name": "item", "description": "10.1111/ejss.12487", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/ejss.12487"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-10-27T00:00:00Z"}}, {"id": "10.1111/gcb.14399", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:18:33Z", "type": "Journal Article", "created": "2018-07-14", "title": "Pathways regulating decreased soil respiration with warming in a biocrust\u2010dominated dryland", "description": "Abstract<p>A positive soil carbon (C)\uffe2\uff80\uff90climate feedback is embedded into the climatic models of the IPCC. However, recent global syntheses indicate that the temperature sensitivity of soil respiration (RS) in drylands, the largest biome on Earth, is actually lower in warmed than in control plots. Consequently, soil C losses with future warming are expected to be low compared with other biomes. Nevertheless, the empirical basis for these global extrapolations is still poor in drylands, due to the low number of field experiments testing the pathways behind the long\uffe2\uff80\uff90term responses of soil respiration (RS) to warming. Importantly, global drylands are covered with biocrusts (communities formed by bryophytes, lichens, cyanobacteria, fungi, and bacteria), and thus,RSresponses to warming may be driven by both autotrophic and heterotrophic pathways. Here, we evaluated the effects of 8\uffe2\uff80\uff90year experimental warming onRS, and the different pathways involved, in a biocrust\uffe2\uff80\uff90dominated dryland in southern Spain. We also assessed the overall impacts on soil organic C (SOC) accumulation over time. Across the years and biocrust cover levels, warming reducedRSby 0.30\uffc2\uffa0\uffce\uffbcmol\uffc2\uffa0CO2\uffc2\uffa0m\uffe2\uff88\uff922\uffc2\uffa0s\uffe2\uff88\uff921(95% CI\uffc2\uffa0=\uffc2\uffa0\uffe2\uff88\uff920.24 to 0.84), although the negative warming effects were only significant after 3\uffc2\uffa0years of elevated temperatures in areas with low initial biocrust cover. We found support for different pathways regulating the warming\uffe2\uff80\uff90induced reduction inRSat areas with low (microbial thermal acclimation via reduced soil mass\uffe2\uff80\uff90specific respiration and \uffce\uffb2\uffe2\uff80\uff90glucosidase enzymatic activity) vs. high (microbial thermal acclimation jointly with a reduction in autotrophic respiration from decreased lichen cover) initial biocrust cover. Our 8\uffe2\uff80\uff90year experimental study shows a reduction in soil respiration with warming and highlights that biocrusts should be explicitly included in modeling efforts aimed to quantify the soil C\uffe2\uff80\uff93climate feedback in drylands.</p", "keywords": ["0301 basic medicine", "Lichens", "Climate Change", "Bryophyta", "Bacterial Physiological Phenomena", "Cyanobacteria", "Carbon Cycle", "Soil", "03 medical and health sciences", "XXXXXX - Unknown", "soil organic carbon accumulation", "Ecosystem", "Soil Microbiology", "2. Zero hunger", "Autotrophic Processes", "0303 health sciences", "Fungi", "Temperature", "substrate depletion", "Heterotrophic Processes", "15. Life on land", "Carbon", "3. Good health", "climate change", "Spain", "13. Climate action", "autotrophic soil respiration", "microbial thermal acclimation"]}, "links": [{"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.14399"}, {"href": "https://doi.org/10.1111/gcb.14399"}, {"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.14399", "name": "item", "description": "10.1111/gcb.14399", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcb.14399"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-08-03T00:00:00Z"}}], "links": [{"rel": "self", "type": "application/geo+json", "title": "This document as GeoJSON", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=Processes&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=Processes&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=Processes&", "hreflang": "en-US"}, {"rel": "next", "type": "application/geo+json", "title": "items (next)", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=Processes&offset=50", "hreflang": "en-US"}], "numberMatched": 193, "numberReturned": 50, "distributedFeatures": [], "timeStamp": "2026-07-27T07:52:50.801066Z"}