{"type": "FeatureCollection", "features": [{"id": "a0b4c95f-9a55-4362-bd73-1c3ab2a5f32e", "type": "Feature", "geometry": null, "properties": {"updated": "2025-09-02T09:56:51", "type": "Dataset", "language": "de", "title": "INSPIRE Soil / Hazard Levels Water Erosion (RxKxS) BB", "description": "Der interoperable INSPIRE-Datensatz beinhaltet Daten vom LBGR \u00fcber die Gef\u00e4hrdungsstufen Wassererosion (RxKxS) Brandenburg, transformiert in das INSPIRE-Zielschema Boden. Der Datensatz wird \u00fcber je einen interoperablen Darstellungs- und Downloaddienst bereitgestellt. Im Datensatz Gef\u00e4hrdungsstufen wird die r\u00e4umliche Verteilung der potenziellen Bodenerosionsgef\u00e4hrdung durch Wasser auf den landwirtschaftlichen Fl\u00e4chen Brandenburgs dargestellt. Die Bestimmung erfolgte in Anlehnung an DIN19708 (https://dx.doi.org/10.31030/2676773), deren zu Grunde liegende Methode als Allgemeine Bodenabtragsgleichung (ABAG) bezeichnet wird. Die Erosionsgef\u00e4hrdung wird in einer r\u00e4umlichen Aufl\u00f6sung von 5x5 Meter dargestellt. Die potenzielle Erosionsgef\u00e4hrdung durch Wasser, die auch als nat\u00fcrlicher Erosionsgef\u00e4hrdung bezeichnet wird, ergibt sich aus der Klassifizierung des potenziellen Bodenabtrags nach DIN19708 in Gef\u00e4hrdungsstufen. Der potenzielle Bodenabtrag durch Wasser ergibt sich aus der Kombination des Regenerosivit\u00e4tsfaktors R, des Bodenerodierbarkeitsfaktors K und des Hangneigungsfaktors S. Die Gef\u00e4hrdung wird in sieben Stufen von 0 (keine Gef\u00e4hrdung) bis 6 (extrem hohe Gef\u00e4hrdung) angegeben.      ---      The compliant INSPIRE data set contains data about the risk levels for water erosion (RxKxS) Brandenburg from the LBGR, transformed into the INSPIRE annex schema Soil. The data set is provided via compliant view and download services. It shows the spatial distribution of the potential soil erosion risk caused by water on agricultural land in Brandenburg. The determination was based on DIN19708 (https://dx.doi.org/10.31030/2676773), for which the underlying method is referred to as the Allgemeine Bodenabtragsgleichung (ABAG). The soil erosion risk is presented in a spatial resolution of 5x5 meters. The potential soil erosion risk caused by water, which is also known as natural soil erosion risk, results from the classification of the potential soil loss according to DIN19708 into risk levels. The potential soil loss caused by water results from the combination of the rainfall-runoff erosivity factor R, the soil erodibility factor K and the slope steepness factor S. The erosion risk is indicated in seven levels from 0 (no risk) to 6 (extremely high risk).", "formats": [{"name": "WCS_SRVC"}], "keywords": ["High value dataset", "boden", "bodenerosion", "bodenerosionsgefa\u0308hrdung", "bodenerosionsgefa\u0308hrdung-durch-wasser-in-brandenburg", "bodenkunde", "brandenburg", "de", "erdbeobachtung-und-umwelt", "erosion", "erosionsgefa\u0308hrdung", "gefa\u0308hrdungsstufen", "geologie", "inspireidentifiziert", "interoperabel", "interoperability", "interoperable-daten", "opendata", "process", "regional", "soil", "soillayer", "wassererosion", "water-erosion", "watererosionrisktopsoil"], "contacts": [{"organization": "Landesamt f\u00fcr Bergbau, Geologie und Rohstoffe Brandenburg (LBGR)", "roles": ["creator"]}]}, "links": [{"href": "https://inspire.brandenburg.de/services/boerosion_wms?REQUEST=GetCapabilities&SERVICE=WMS"}, {"href": "https://inspire.brandenburg.de/services/so_boerosion_wcs?REQUEST=GetCapabilities&SERVICE=WCS"}, {"href": "https://inspire.brandenburg.de/services/so_boerosion_wms?REQUEST=GetCapabilities&SERVICE=WMS"}, {"href": "http://data.europa.eu/88u/dataset/a0b4c95f-9a55-4362-bd73-1c3ab2a5f32e~~2"}, {"rel": "self", "type": "application/geo+json", "title": "a0b4c95f-9a55-4362-bd73-1c3ab2a5f32e", "name": "item", "description": "a0b4c95f-9a55-4362-bd73-1c3ab2a5f32e", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/a0b4c95f-9a55-4362-bd73-1c3ab2a5f32e"}, {"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": "10.5281/zenodo.14230855", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:22:31Z", "type": "Dataset", "title": "Maps of topsoil (0-30 cm) properties of Tuscany (Italy)", "description": "Open AccessThe internal EJP SOIL project SERENA contributed to the evaluation of soil multifunctionality aiming at providing assessment tools for land planning and soil policies at different scales. By co-working with relevant stakeholders, the project provided co-developed indicators and associated cookbooks to assess and map them, to report both on soil degradation, soil-based ecosystem services and their bundles, under actual conditions and for climate and land-use changes, at the regional, national, and European scales.  The topsoil (0-30 cm) properties maps are prepared to evaluate soil ecosystem services in SERENA/EJP-Soil and for applying SOC loss Cookbook and SOIL Loss Cookbook. In particular Soil Organic Carbon content map was directly considered as an application of SOC loss Cookbook (DOI: 10.5281/zenodo.13951265\u00a0Version 3).  They are based on Tuscany Region soil database available at Geoscopio (https://www502.regione.toscana.it/geoscopio/pedologia.html) and on point soil data not freely available (Lamma Consortium). More information and requests to:\u00a0info@lamma.toscana.it.  In accordance with the methodology reported in the Soil Organic Carbon Mapping Cookbook (Yigini et al., 2018), the following soil properties were mapped for all Tuscany Region:    soil organic carbon content (dag/kg),  soil organic carbon stock (t/ha),  textural fractions (sand, silt and clay, USDA limits, dag/kg),  rock fragments (vol/vol),  pH in water,  bulk density (g/cm3).   They were obtained through Digital Soil Mapping (DSM) approach, based on correlations with numerous environmental factors and using Random Forest algorithm.  All the maps have a 100 m spatial resolution.", "keywords": ["silt", "bulk density", "pH", "soil organic carbon content", "sand", "clay", "Grant n. 862695", "Digital Soil Mapping", "textural fractions", "Italy", "topsoil properties", "Tuscany", "soil organic carbon stock", "EJP-SOIL", "SERENA Project"]}, "links": [{"href": "https://doi.org/10.5281/zenodo.14230855"}, {"rel": "self", "type": "application/geo+json", "title": "10.5281/zenodo.14230855", "name": "item", "description": "10.5281/zenodo.14230855", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5281/zenodo.14230855"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-11-05T00:00:00Z"}}, {"id": "10.1016/j.geoderma.2022.115915", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:16:19Z", "type": "Journal Article", "created": "2022-05-02", "title": "Mineral element recycling in topsoil following permafrost degradation and a vegetation shift in sub-Arctic tundra", "description": "Climate change affects the Arctic and sub-Arctic regions by exposing previously frozen permafrost to thaw, unlocking soil nutrients, changing hydrological processes, and boosting plant growth. As a result, sub-Arctic tundra is subject to a shrub expansion, called \u201cshrubification\u201d, at the expense of sedge species. Depending on the intrinsic foliar properties of these plant species, changes in foliar mineral element fluxes with shrubification in the context of permafrost degradation may influence topsoil mineral element composition. Despite the potential implications of changes in topsoil mineral element concentrations for the fate of organic carbon, this remains poorly quantified. Here, we investigate vegetation foliar and topsoil mineral element composition (Si, K, Ca, P, Mn, Zn, Cu, Mo, V) across a natural gradient of permafrost degradation at a typical sub-Arctic tundra at Eight Mile Lake (Alaska, USA). Results show that foliar mineral element concentrations are higher (up to 9 times; Si, K, Mo for all species, and for some species Zn) or lower (up to 2 times; Ca, P, Mn, Cu, V for all species, and for some species Zn) in sedge than in shrub species. As a result, a vegetation shift over ~40 years has resulted in lower topsoil concentrations in Si, K, Zn, and Mo (respectively of 52, 24, 20, and 51%) in highly degraded permafrost sites compared to poorly degraded permafrost sites due to lower foliar fluxes of these elements. For other elements (Ca, P, Mn, Cu, and V), the vegetation shift has not induced a marked change in topsoil concentrations at this current stage of permafrost degradation. A modeled amplified shrubification associated with a further permafrost degradation is expected to increase foliar Ca, P, Mn, Cu, and V fluxes, which will likely change these element concentrations in topsoil. These data can serve as a first estimate to assess the influence of other shifts in vegetation in Arctic and sub-Arctic tundra such as sedge expansion under wetter soil conditions.", "keywords": ["topsoil", "[SDV.SA.STA] Life Sciences [q-bio]/Agricultural sciences/Sciences and technics of agriculture", "mineral elements", "04 agricultural and veterinary sciences", "sub-Arctic tundra", "15. Life on land", "01 natural sciences", "vegetation change", "13. Climate action", "[SDV.SA.STA]Life Sciences [q-bio]/Agricultural sciences/Sciences and technics of agriculture", "0401 agriculture", " forestry", " and fisheries", "shrubification", "permafrost degradation", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.geoderma.2022.115915"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Geoderma", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.geoderma.2022.115915", "name": "item", "description": "10.1016/j.geoderma.2022.115915", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.geoderma.2022.115915"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-09-01T00:00:00Z"}}, {"id": "10.1007/s11104-004-0599-3", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:14:43Z", "type": "Journal Article", "created": "2005-05-31", "title": "Senna Siamea Trees Recycle Ca From A Ca-Rich Subsoil And Increase The Topsoil Ph In Agroforestry Systems In The West African Derived Savanna Zone", "description": "The functioning of trees as a safety-net for capturing nutrients leached beyond the reach of crop roots was evaluated by investigating changes in exchangeable cations (Ca, Mg, and K) and pH in a wide range of medium to long term alley cropping trials in the derived savanna of West Africa, compared to no-tree control plots. Topsoil Ca content, effective cation exchange capacity, and pH were substantially higher under Sennasiamea than under Leucaena leucocephala, Gliricidia sepium, or the no-tree control plots in sites with a Bt horizon rich in exchangeable Ca. This was shown to be largely related to the recovery of Ca from the subsoil under Senna trees. The increase of the Ca content of the topsoil under Senna relative to the no-tree control treatment was related to the total amount of dry matter applied since trial establishment. The lack of increase in Ca accumulation under the other species was related to potential recovery of Ca from the topsoil itself and/or substantial Ca leaching. The accumulation of Ca in the topsoil under Senna had a marked effect on the topsoil pH, the latter increasing significantly compared with the Leucaena, Gliridia, and no-tree control treatments. In conclusion, the current work shows that the functioning of the often hypothesized \u2018safety-net\u2019 of trees in a cropping system depends on (i) the tree species and on (ii) the presence of a subsoil of suitable quality, i.e., clay enriched and with high Ca saturation.", "keywords": ["0106 biological sciences", "senna siamea", "topsoil", "01 natural sciences", "savannas", "agroforestry", "plant litter", "calcio", "subsoil", "top soil", "sabanas", "2. Zero hunger", "calcium", "biomass", "cerca viva", "capa arable del suelo", "litterfall prunings", "ph del suelo", "hojarasca", "trees", "04 agricultural and veterinary sciences", "15. Life on land", "subsoil ca content", "soil ph", "gliricidia sepium", "leucaena leucocephala", "0401 agriculture", " forestry", " and fisheries", "hedges", "agroforesteria", "leucaena lecocephala"]}, "links": [{"href": "https://doi.org/10.1007/s11104-004-0599-3"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Plant%20and%20Soil", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s11104-004-0599-3", "name": "item", "description": "10.1007/s11104-004-0599-3", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s11104-004-0599-3"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2005-02-01T00:00:00Z"}}, {"id": "10.1007/s13593-022-00773-9", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:15:05Z", "type": "Journal Article", "created": "2022-05-16", "title": "Soil compaction raises nitrous oxide emissions in managed agroecosystems. A review", "description": "Abstract<p>Nitrous oxide (N2O) is the contributor to agricultural greenhouse gas emissions with the highest warming global potential. It is widely recognised that traffic and animal-induced compaction can lead to an increased potential for N2O emissions by decreasing soil oxygen supply. The extent to which the spatial and temporal variability of N2O emissions can be explained by soil compaction is unclear. This review aims to comprehensively discuss soil compaction effects on N2O emissions, and to understand how compaction may promote N2O emission hotspots and hot moments. An impact factor of N2O emissions due to compaction was calculated for each selected study; compaction effects were evaluated separately for croplands, grasslands and forest lands. Topsoil compaction was found to increase N2O emissions by 1.3 to 42 times across sites and land uses. Large impact factors were especially reported for cropland and grassland soils when topsoil compaction\uffe2\uff80\uff94induced by field traffic and/or grazing\uffe2\uff80\uff94is combined with nitrogen input from fertiliser or urine. Little is known about the contribution of subsoil compaction to N2O emissions. Water-filled pore space is the most common water metric used to explain N2O emission variability, but gas diffusivity is a parameter with higher prediction potential. Microbial community composition may be less critical than the soil environment for N2O emissions, and there is a need for comprehensive studies on association between environmental drivers and soil compaction. Lack of knowledge about the interacting factors causing N2O accumulation in compacted soils, at different degrees of compactness and across different spatial scales, limits the identification of high-risk areas and development of efficient mitigation strategies. Soil compaction mitigation strategies that aim to loosen the soil and recover pore system functionality, in combination with other agricultural management practices to regulate N2O emission, should be evaluated for their effectiveness across different agro-climatic conditions and scales.</p", "keywords": ["2. Zero hunger", "Gas diffusivity", "04 agricultural and veterinary sciences", "15. Life on land", "6. Clean water", "[SDV] Life Sciences [q-bio]", "Subsoil compaction", "Topsoil compaction", "13. Climate action", "11. Sustainability", "0401 agriculture", " forestry", " and fisheries", "Hotspots", "Hot moments"]}, "links": [{"href": "https://link.springer.com/content/pdf/10.1007/s13593-022-00773-9.pdf"}, {"href": "https://doi.org/10.1007/s13593-022-00773-9"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Agronomy%20for%20Sustainable%20Development", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s13593-022-00773-9", "name": "item", "description": "10.1007/s13593-022-00773-9", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s13593-022-00773-9"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-05-16T00:00:00Z"}}, {"id": "10.1016/j.agwat.2016.04.009", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:15:23Z", "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.ecolind.2024.111796", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:15:47Z", "type": "Journal Article", "created": "2024-02-29", "title": "Ascomycota and Basidiomycota fungal phyla as indicators of land use efficiency for soil organic carbon accrual with woody plantations", "description": "As soil fungi are major players in the carbon accumulation process, the two main fungal degraders in topsoil, Ascomycetes and Basidiomycetes, were investigated as indicators of land use effectiveness in increasing soil carbon accumulation and soil function. The study focused on the soil organic carbon content increase in a 20-year short rotation forest cycle with broadleaf woody plantations compared to a nearby arable cropping system. Total fungi, Ascomycota and Basidiomycota, were quantified in terms of DNA copy number, with specific probes using SYBR\u00ae Green I dye on the QuantStudio\u2122 3D digital PCR system (dPCR). Previously, next generation sequencing analysis using a general primer confirmed that Ascomycota and Basidiomycota were the most represented phyla and that fungal community composition significantly differed between treatments. A range of key soil enzyme activities for the C-cycle were also assessed. Total organic carbon content (TOC), microbial biomass in term of dsDNA and enzyme activities significantly increased in woody plantations compared to arable soil. The TOC increase differed significantly also between wood species, Salix and Robina gave the greatest increase (+30 and 20\u00a0% respectively), followed by Populus (+12), microbial biomass highly correlated with TOC showing the same trend. Total fungi, Ascomycota and Basidiomycota increased significantly in three woody plantations compared to the arable soil system. Ascomycota in the woody plantations increased two to four times (average 3144 n copies \u00b5l\u22121 of DNA) compared to the arable soil (1419 n copies \u00b5l\u22121); Basidiomycota were almost absent in arable soil (av. 94n copies \u00b5l\u22121) and increased five to six times in woody plantations (av. 490 n copies \u00b5l\u22121). Total fungi and ascomycetes correlated strongly with microbial biomass and TOC, whereas basidiomycetes did not. These findings showed that Ascomycota represent the largest portion of fungi in agricultural soils even after a 20-years short rotation forest cycle and they can be taken as indicators of carbon accumulation processes. Therefore, this study suggests that joining the Ascomycetes quantity in the topsoil to the Ascomycota:Basidiomycota ratio seems a good option when setting regional strategies for improving C accrual in farmland with the short-term afforestation.", "keywords": ["Carbon sequestration", "2. Zero hunger", "Ecology", "04 agricultural and veterinary sciences", "15. Life on land", "Topsoil", "01 natural sciences", "Saproptrophic soil fungi", "Land use", "0401 agriculture", " forestry", " and fisheries", "Short rotation forest", "Digital PCR", "QH540-549.5", "0105 earth and related environmental sciences"], "contacts": [{"organization": "Manici, Luisa M., Caputo, Francesco, Fornasier, Flavio, Paletto, Alessandro, Ceotto, Enrico, De Meo, Isabella,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1016/j.ecolind.2024.111796"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Ecological%20Indicators", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.ecolind.2024.111796", "name": "item", "description": "10.1016/j.ecolind.2024.111796", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.ecolind.2024.111796"}, {"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": "10.1093/nsr/nwab120", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:18:19Z", "type": "Journal Article", "created": "2021-06-29", "title": "Significant loss of soil inorganic carbon at the continental scale", "description": "Abstract                <p>Widespread soil acidification due to atmospheric acid deposition and agricultural fertilization may greatly accelerate soil carbonate dissolution and CO2 release. However, to date, few studies have addressed these processes. Here, we use meta-analysis and nationwide-survey datasets to investigate changes in soil inorganic carbon (SIC) stocks in China. We observe an overall decrease in SIC stocks in topsoil (0\uffe2\uff80\uff9330\uffc2\uffa0cm) (11.33\uffc2\uffa0g C m\uffe2\uff80\uff932 yr\uffe2\uff80\uff931) from the 1980s to the 2010s. Total SIC stocks have decreased by \uffe2\uff88\uffbc8.99\uffc2\uffa0\uffc2\uffb1\uffc2\uffa02.24% (1.37\uffc2\uffa0\uffc2\uffb1\uffc2\uffa00.37\uffc2\uffa0Pg C). The average SIC losses across China (0.046 Pg C yr\uffe2\uff80\uff931) and in cropland (0.016 Pg C yr\uffe2\uff80\uff931) account for \uffe2\uff88\uffbc17.6%\uffe2\uff80\uff9324.0% of the terrestrial C sink and 57.1% of the soil organic carbon sink in cropland, respectively. Nitrogen deposition and climate change have profound influences on SIC cycling. We estimate that \uffe2\uff88\uffbc19.12%\uffe2\uff80\uff9319.47% of SIC stocks will be further lost by 2100. The consumption of SIC may offset a large portion of global efforts aimed at ecosystem carbon sequestration, which emphasizes the importance of achieving a better understanding of the indirect coupling mechanisms of nitrogen and carbon cycling and of effective countermeasures to minimize SIC loss.</p", "keywords": ["Carbon sequestration", "Cartography", "China", "Mechanics and Transport in Unsaturated Soils", "Carbonate", "Nitrogen", "Soil Science", "Organic chemistry", "Carbon Dynamics in Peatland Ecosystems", "soil inorganic carbon stocks", "Soil pH", "Environmental science", "Carbon sink", "Agricultural and Biological Sciences", "carbonate", "Engineering", "Soil water", "Soil Carbon Sequestration", "Biology", "global change", "Ecosystem", "Soil acidification", "Civil and Structural Engineering", "Soil science", "2. Zero hunger", "Soil organic matter", "Soil Fertility", "Ecology", "Geography", "Soil Water Retention", "Life Sciences", "Cycling", "Forestry", "Carbon cycle", "04 agricultural and veterinary sciences", "15. Life on land", "Topsoil", "Soil carbon", "Chemistry", "Sink (geography)", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "Physical Sciences", "Environmental chemistry", "0401 agriculture", " forestry", " and fisheries", "soil acidification", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems", "Research Article"]}, "links": [{"href": "https://doi.org/10.1093/nsr/nwab120"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/National%20Science%20Review", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1093/nsr/nwab120", "name": "item", "description": "10.1093/nsr/nwab120", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1093/nsr/nwab120"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-07-02T00:00:00Z"}}, {"id": "10.1111/gcb.15496", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:18:39Z", "type": "Journal Article", "created": "2020-12-20", "title": "Topsoil organic matter build\u2010up in glacier forelands around the world", "description": "Abstract<p>Since the last glacial maximum, soil formation related to ice\uffe2\uff80\uff90cover shrinkage has been one major sink of carbon accumulating as soil organic matter (SOM), a phenomenon accelerated by the ongoing global warming. In recently deglacierized forelands, processes of SOM accumulation, including those that control carbon and nitrogen sequestration rates and biogeochemical stability of newly sequestered carbon, remain poorly understood. Here, we investigate the build\uffe2\uff80\uff90up of SOM during the initial stages (up to 410\uffc2\uffa0years) of topsoil development in 10 glacier forelands distributed on four continents. We test whether the net accumulation of SOM on glacier forelands (i) depends on the time since deglacierization and local climatic conditions (temperature and precipitation); (ii) is accompanied by a decrease in its stability and (iii) is mostly due to an increasing contribution of organic matter from plant origin. We measured total SOM concentration (carbon, nitrogen), its relative hydrogen/oxygen enrichment, stable isotopic (13C, 15N) and carbon functional groups (C\uffe2\uff80\uff90H, C=O, C=C) compositions, and its distribution in carbon pools of different thermal stability. We show that SOM content increases with time and is faster on forelands experiencing warmer climates. The build\uffe2\uff80\uff90up of SOM pools shows consistent trends across the studied soil chronosequences. During the first decades of soil development, the low amount of SOM is dominated by a thermally stable carbon pool with a small and highly thermolabile pool. The stability of SOM decreases with soil age at all sites, indicating that SOM storage is dominated by the accumulation of labile SOM during the first centuries of soil development, and suggesting plant carbon inputs to soil (SOM depleted in nitrogen, enriched in hydrogen and in aromatic carbon). Our findings highlight the potential vulnerability of SOM stocks from proglacial areas to decomposition and suggest that their durability largely depends on the relative contribution of carbon inputs from plants.</p>", "keywords": ["[SDV.BID.SPT]Life Sciences [q-bio]/Biodiversity/Systematics", "550", "Nitrogen", "Chronosequence", "551", "01 natural sciences", "[SDV.BV.BOT] Life Sciences [q-bio]/Vegetal Biology/Botanics", "Soil", "soil organic matter", "carbon stability; chronosequence; climate sensitivity; soil organic matter; topsoil development; Carbon; Nitrogen; Temperature; Ice Cover; Soil", "[SDV.BID.SPT] Life Sciences [q-bio]/Biodiversity/Systematics", " Phylogenetics and taxonomy", "[SDV.EE.ECO] Life Sciences [q-bio]/Ecology", " environment/Ecosystems", "Ice Cover", "topsoil development", "Carbon stability", "0105 earth and related environmental sciences", "2. Zero hunger", "Soil organic matter", "Temperature", "Phylogenetics and taxonomy", "04 agricultural and veterinary sciences", "[SDV.BV.BOT]Life Sciences [q-bio]/Vegetal Biology/Botanics", "15. Life on land", "Climate sensitivity", "Primary Research Articles", "Carbon", "chronosequence", "[SDE.BE] Environmental Sciences/Biodiversity and Ecology", "13. Climate action", "[SDV.EE.ECO]Life Sciences [q-bio]/Ecology", "[SDE]Environmental Sciences", "Topsoil development", "climate sensitivity", "carbon stability; chronosequence; climate sensitivity; soil organic matter; topsoil development;", "0401 agriculture", " forestry", " and fisheries", "[SDE.BE]Environmental Sciences/Biodiversity and Ecology", "environment/Ecosystems", "carbon stability"]}, "links": [{"href": "https://air.unimi.it/bitstream/2434/851691/2/khedim%202021%20submitted.pdf"}, {"href": "https://air.unimi.it/bitstream/2434/851691/3/khedim%202021%20Global%20Change%20Biol.pdf"}, {"href": "https://boa.unimib.it/bitstream/10281/300214/2/10281-300214_VoR.pdf"}, {"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.15496"}, {"href": "https://doi.org/10.1111/gcb.15496"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Change%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/gcb.15496", "name": "item", "description": "10.1111/gcb.15496", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcb.15496"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-01-16T00:00:00Z"}}, {"id": "10.3390/rs13224615", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:21:02Z", "type": "Journal Article", "created": "2021-11-17", "title": "Spatiotemporal Prediction and Mapping of Heavy Metals at Regional Scale Using Regression Methods and Landsat 7", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Soil contamination by heavy metals is of particular concern, due to the direct negative impact on crop yield, food quality and human health. Although the conventional approach to monitor heavy metals relies on field sampling and lab analysis, the proliferation in the use of portable spectrometers has reduced the cost and time of investigation. However, discrepancies in spectral data from different spectrometers increase the modeling time and undermine the model accuracy for spatial mapping. This study, therefore, took advantage of the readily accessible Landsat 7 data to predict and map the spatiotemporal distribution of ten heavy metals (i.e., Sb, Pb, Ni, Mn, Hg, Cu, Cr, Co, Cd and As) over a 640 km2 area in Belgium. The Land Use/Cover Area Frame Survey (LUCAS) database of a region in north-eastern Belgium was used to retrieve variation in heavy metals concentrations over time and space, using the Landsat 7 imagery for four single dates in 2009, 2013, 2016 and 2020. Three regression methods, namely, partial least squares regression (PLSR), random forest (RF) and support vector machine (SVM) were used to model and predict the heavy metal concentrations for 2009. By comparing these models unbiasedly, the best model was selected for predicting and mapping the heavy metal distributions for 2013, 2016 and 2020. RF turned out to be the optimal model for 2009 with a coefficient of determination of prediction (R2P) and residual prediction deviation of prediction (RPDP) ranging from 0.62 to 0.92, and 1.23 to 2.79, respectively. The measured heavy metal distributions along the river floodplains, at the highlands and in the lowlands, were generally high, compared to their RF spatiotemporal predictions, which decreased over time. Increasing moisture contents in the floodplains adjacent to the river channels and the lowlands were the primary contributors to the reduction in the satellite reflectance spectra. However, topsoil erosion from rainfall, snowmelt as well as wind into the lowlands could have influenced the reduction in heavy metal spatiotemporal predicted values over time in the highlands. The spatiotemporal prediction maps produced for the heavy metals for the four different years revealed a good spatial similarity and consistency with the measured maps for 2009, which indicates their stability over the years.</p></article>", "keywords": ["PROVINCE", "Landsat 7", "analysis", "Science", "random forest (RF)", "MOISTURE", "01 natural sciences", "NIR SPECTROSCOPY", "spatiotemporal analysis", "AGRICULTURAL SOILS", "spatiotemporal", "0105 earth and related environmental sciences", "2. Zero hunger", "RANGE", "Q", "04 agricultural and veterinary sciences", "15. Life on land", "6. Clean water", "3. Good health", "MULTIVARIATE", "TOPSOILS", "13. Climate action", "Earth and Environmental Sciences", "soil heavy metal; Landsat 7; partial least squares regression (PLSR); random forest (RF); support vector machine (SVM); spatiotemporal analysis", "0401 agriculture", " forestry", " and fisheries", "support vector machine (SVM)", "soil heavy metal", "partial least squares regression (PLSR)"]}, "links": [{"href": "http://www.mdpi.com/2072-4292/13/22/4615/pdf"}, {"href": "https://www.mdpi.com/2072-4292/13/22/4615/pdf"}, {"href": "https://doi.org/10.3390/rs13224615"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Remote%20Sensing", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3390/rs13224615", "name": "item", "description": "10.3390/rs13224615", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3390/rs13224615"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-11-16T00:00:00Z"}}, {"id": "10.1371/journal.pone.0038858", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:19:26Z", "type": "Journal Article", "created": "2012-06-11", "title": "Decline In Topsoil Microbial Quotient, Fungal Abundance And C Utilization Efficiency Of Rice Paddies Under Heavy Metal Pollution Across South China", "description": "Open AccessLos suelos agr\u00edcolas han estado cada vez m\u00e1s sujetos a la contaminaci\u00f3n por metales pesados en todo el mundo. Sin embargo, los impactos en la estructura y actividad de la comunidad microbiana del suelo de los suelos de campo a\u00fan no se han caracterizado bien. En 2009 se recolectaron muestras de tierra vegetal de campos de arroz contaminados con metales pesados (PS) y sus campos de fondo (BGS) en cuatro sitios del sur de China. Los cambios con la contaminaci\u00f3n met\u00e1lica en relaci\u00f3n con el BGS en el tama\u00f1o y la estructura de la comunidad de los microorganismos del suelo se examinaron con m\u00faltiples ensayos microbiol\u00f3gicos de medici\u00f3n de carbono de biomasa (MBC) y nitr\u00f3geno (MBN), recuento en placa de colonias cultivables y an\u00e1lisis de \u00e1cidos grasos fosfol\u00edpidos (PLFA) junto con el perfil de electroforesis en gel de gradiente desnaturalizante (DGGE) del gen de ARNr 16S y ARNr 18S y ensayo de PCR en tiempo real. Adem\u00e1s, se llev\u00f3 a cabo una incubaci\u00f3n de laboratorio de 7 d\u00edas a una temperatura constante de 25 \u00b0C para realizar un seguimiento adicional de los cambios en la actividad metab\u00f3lica. Si bien la disminuci\u00f3n de la contaminaci\u00f3n por metales en MBC y MBN, as\u00ed como en el tama\u00f1o de la poblaci\u00f3n cultivable, el contenido total de PLFA y el n\u00famero de bandas DGGE de bacterias no se observaron de manera significativa y consistente, de hecho se observ\u00f3 una reducci\u00f3n significativa de la contaminaci\u00f3n por metales en el cociente microbiano, en el tama\u00f1o de la poblaci\u00f3n f\u00fangica cultivable y en la proporci\u00f3n de PLFA f\u00fangicos a bacterianos de manera consistente en todos los sitios en una medida que var\u00eda de 6% a 74%. Adem\u00e1s, se observ\u00f3 un aumento consistentemente significativo en el cociente metab\u00f3lico de hasta un 68% bajo contaminaci\u00f3n en todos los sitios. Estas observaciones apoyaron un cambio de la comunidad microbiana con disminuci\u00f3n en su abundancia, disminuci\u00f3n en la proporci\u00f3n de hongos y, por lo tanto, en la eficiencia de utilizaci\u00f3n de C bajo contaminaci\u00f3n en los suelos. Adem\u00e1s, las proporciones de cociente microbiano, de hongos a bacterias y qCO2 son mejores indicativas de los impactos de los metales pesados en la estructura y actividad de la comunidad microbiana. Los efectos potenciales de estos cambios en el ciclo del carbono y la producci\u00f3n de CO2 en los arrozales contaminados merecen m\u00e1s estudios de campo.", "keywords": ["Microbial population biology", "Colony Count", " Microbial", "Agricultural and Biological Sciences", "Sociology", "Soil water", "Soil Pollutants", "Soil Microbiology", "2. Zero hunger", "Principal Component Analysis", "Temperature gradient gel electrophoresis", "Ecology", "Q", "Fatty Acids", "R", "Life Sciences", "Agriculture", "04 agricultural and veterinary sciences", "Biota", "Pollution", "6. Clean water", "FOS: Sociology", "Chemistry", "Physical Sciences", "Environmental chemistry", "Medicine", "Research Article", "Environmental Monitoring", "16S ribosomal RNA", "China", "Microorganism", "Environmental Impact of Heavy Metal Contamination", "Nitrogen", "Science", "Population", "Soil Science", "Real-Time Polymerase Chain Reaction", "Environmental science", "Microbial Ecology", "12. Responsible consumption", "Metals", " Heavy", "Genetics", "Biology", "Demography", "Bacteria", "Denaturing Gradient Gel Electrophoresis", "Marine Microbial Diversity and Biogeography", "Oryza", "15. Life on land", "Topsoil", "Carbon", "Agronomy", "RNA", " Ribosomal", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "0401 agriculture", " forestry", " and fisheries", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems"]}, "links": [{"href": "https://doi.org/10.1371/journal.pone.0038858"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/PLoS%20ONE", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1371/journal.pone.0038858", "name": "item", "description": "10.1371/journal.pone.0038858", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1371/journal.pone.0038858"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2012-06-11T00:00:00Z"}}, {"id": "10.3390/agriculture15080852", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:20:46Z", "type": "Journal Article", "created": "2025-04-15", "title": "Evaluating Soil Degradation in Agricultural Soil with Ground-Penetrating Radar: A Systematic Review of Applications and Challenges", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Soil degradation is a critical challenge to global agricultural sustainability, driven by intensive land use, unsustainable farming practices, and climate change. Conventional soil monitoring techniques often rely on invasive sampling methods, which can be labor-intensive, disruptive, and limited in spatial coverage. In contrast, non-invasive geophysical techniques, particularly ground-penetrating radar, have gained attention as tools for assessing soil properties. However, an assessment of ground-penetrating radar\u2019s applications in agricultural soil research\u2014particularly for detecting soil structural changes related to degradation\u2014remains undetermined. To address this issue, a systematic literature review was conducted following the Preferred Reporting Items for Systematic Reviews and Meta-Analyses 2020 guidelines. A search was conducted across Scopus and Web of Science databases, as well as relevant review articles and study reference lists, up to 31 December 2024. This process resulted in 86 potentially relevant studies, of which 24 met the eligibility criteria and were included in the final review. The analysis revealed that the ground-penetrating radar allows the detection of structural changes associated with tillage practices and heavy machinery traffic in agricultural lands, namely topsoil disintegration and soil compaction, both of which are important indicators of soil degradation. These variations are reflected in changes in electrical permittivity and reflectivity, particularly above the tillage horizon. These shifts are associated with lower soil water content, increased soil homogeneity, and heightened wave reflectivity at the upper boundary of compacted soil. The latter is linked to density contrasts and waterlogging above this layer. Additionally, ground-penetrating radar has demonstrated its potential in mapping alterations in electrical permittivity related to preferential water flow pathways, detecting shifts in soil organic carbon distribution, identifying disruptions in root systems due to tillage, and assessing soil conditions potentially affected by excessive fertilization in iron oxide-rich soils. Future research should focus on refining methodologies to improve the ground-penetrating radar\u2019s ability to quantify soil degradation processes with greater accuracy. In particular, there is a need for standardized experimental protocols to evaluate the effects of monocultures on soil fertility, assess the impact of excessive fertilization effects on soil acidity, and integrate ground-penetrating radar with complementary geophysical and remote sensing techniques for a holistic approach to soil health monitoring.</p></article>", "keywords": ["soil compaction", "sustainable agriculture", "Agriculture (General)", "non-invasive geophysical techniques", "electrical permittivity", "soil structural changes", "topsoil disintegration", "S1-972"]}, "links": [{"href": "https://www.mdpi.com/2077-0472/15/8/852/pdf"}, {"href": "https://doi.org/10.3390/agriculture15080852"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Agriculture", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3390/agriculture15080852", "name": "item", "description": "10.3390/agriculture15080852", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3390/agriculture15080852"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-04-15T00:00:00Z"}}, {"id": "10.3390/agronomy11122403", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:20:48Z", "type": "Journal Article", "created": "2021-11-29", "title": "Impacts of Farming Layer Constructions on Cultivated Land Quality under the Cultivated Land Balance Policy", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Cultivated Land Balance Policy (CLBP) has led to the \u201cbetter land occupied and worse land supplemented\u201d program. At the same time, the current field-scale cultivated land quality (CLQ) evaluation cannot meet the work requirements of the CLBP. To this end, this study selected 24 newly added farmland in Fuping County and performed eight different high quality farming layer construction experiments to improve the CLQ. A new comprehensive model was constructed on a field scale to evaluate the CLQ using different tests from multi-dimensional perspectives of soil fertility, engineering, environment, and ecology, and to determine the best test mode. The results showed that after the test, around 62% of the cultivated land improved by one level, and the average cultivated land quality level and quality index of the test area increased by 0.63 and 30.63, respectively. The treatment of \u201cwoody peat + rotten crop straw + biostimulation regulator II + conventional fertilization\u201d had the best effect on the improvement of organic matter, soil aggregates, and soil microbial activity, and was the best treatment method. In general, application of soil amendments, such as woody peat when constructing high quality farmland, could quickly improve CLQ, and field-scale CLQ evaluation model constructed from a multi-dimensional perspective could accurately assess the true quality of farmland and allow managers to improve and manage arable land resources under CLBP.</p></article>", "keywords": ["Scale (ratio)", "cultivated land quality evaluation", "Agricultural engineering", "Agricultural and Biological Sciences", "Engineering", "Soil Evaluation", "Agricultural land", "Soil water", "Arable land", "cultivated land quality evaluation; field scale; high-quality farming layer; woody peat", "2. Zero hunger", "Global and Planetary Change", "Global Analysis of Ecosystem Services and Land Use", "Geography", "Ecology", "S", "high-quality farming layer", "Life Sciences", "Land Suitability", "Land-Use Suitability Assessment Using GIS", "Land reclamation", "Agriculture", "04 agricultural and veterinary sciences", "woody peat", "Soil Erosion and Agricultural Sustainability", "Agricultural Land Use", "6. Clean water", "FOS: Philosophy", " ethics and religion", "Physical Sciences", "Quality (philosophy)", "field scale", "Cartography", "Soil Science", "Epistemology", "Management", " Monitoring", " Policy and Law", "Soil quality", "Environmental science", "Crop Suitability", "Agroforestry", "Biology", "Soil science", "Peat", "15. Life on land", "Topsoil", "Philosophy", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "Land use", "0401 agriculture", " forestry", " and fisheries"]}, "links": [{"href": "http://www.mdpi.com/2073-4395/11/12/2403/pdf"}, {"href": "https://doi.org/10.3390/agronomy11122403"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Agronomy", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3390/agronomy11122403", "name": "item", "description": "10.3390/agronomy11122403", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3390/agronomy11122403"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-11-25T00:00:00Z"}}, {"id": "10.3390/land14061217", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:20:56Z", "type": "Journal Article", "created": "2025-06-05", "title": "Variation in Soil Organic Carbon and Total Nitrogen Stocks Across Elevation Gradients and Soil Depths in the Mount Kenya East Forest", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Understanding how elevation gradients and soil depths influence soil organic carbon stocks (SOCS) and total nitrogen stocks (TNS) is essential for sustainable forest management (SFM) and climate change mitigation. This study investigated the effects of elevation and soil depth on SOCS and TNS in the Mount Kenya East Forest (MKEF). A stratified systematic sampling approach was applied, involving collection of 38 soil samples from two depths (0\u201320 cm and 20\u201340 cm) across three elevation zones: Lower Forest (1700\u20132000 m), Middle Forest (2000\u20132350 m), and Upper Forest (2350\u20132650 m). Samples were analysed for bulk density (BD), pH, texture, soil organic carbon (SOC), and total nitrogen (TN), using standard laboratory methods. In topsoil (0\u201320 cm), SOCS ranged from 109.28 \u00b1 23.41 to 151.27 \u00b1 17.61 Mg C ha\u22121, while TNS varied from 8.89 \u00b1 1.77 to 12.00 \u00b1 2.46 Mg N ha\u22121. In subsoil (20\u201340 cm), SOCS ranged from 72.03 \u00b1 19.90 to 132.23 \u00b1 11.80 Mg C ha\u22121, with TNS varying between 5.71 \u00b1 1.63 and 10.50 \u00b1 1.90 Mg N ha\u22121. SOCS and TNS increased significantly with elevation (p &lt; 0.05), exhibiting the following trend: Lower Forest &lt; Middle Forest &lt; Upper Forest. Topsoil consistently stored significantly higher SOCS than subsoil (p &lt; 0.05), emphasizing the critical role of surface soils in carbon sequestration. Regression analysis revealed a significant positive relationship between SOCS and TNS (R2 = 0.84, p &lt; 0.001). Both SOCS and TNS were positively correlated with elevation, SOC, TN, and total annual precipitation (TAP), but negatively correlated with BD and mean annual temperature (MAT). These findings provide baseline data for monitoring SOCS and TNS in the MKEF, offering insights into sustainable forest management strategies to improve soil health and enhance climate change mitigation efforts.</p></article>", "keywords": ["topsoil", "S", "soil organic matter", "vegetation type", "subsoil", "Agriculture", "carbon sequestration", "environmental variables"]}, "links": [{"href": "https://www.mdpi.com/2073-445X/14/6/1217/pdf"}, {"href": "https://doi.org/10.3390/land14061217"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Land", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3390/land14061217", "name": "item", "description": "10.3390/land14061217", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3390/land14061217"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-06-05T00:00:00Z"}}, {"id": "10.5281/zenodo.14012785", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:22:24Z", "type": "Dataset", "title": "SERENA EJPSOIL IT TUS SOC Loss SOC", "description": "Open AccessThe data are derived from the calculation of indicators based on a standard methodology established as\u00a0part of the EJP Soil SERENA\u00a0programme. Please keep in mind that:       It is the result of a modelling exercise and does not necessarily reflect reality.     Despite the efforts made to provide reliable data, the results\u00a0may contain inconsistencies,\u00a0depending\u00a0in particular on\u00a0the raw data\u00a0available\u00a0and level of accuracy of the techniques chosen\u00a0and\u00a0their prior knowledge\u00a0.     It is necessary to consider how the results have been obtained\u00a0in order to\u00a0decide on their\u00a0relevance\u00a0in relation to the intended\u00a0purpose\u00a0of reuse.     These results are interesting from a scientific point of view, but their use\u00a0for environmental\u00a0management and policy issues should be done keeping the previous aspects in mind and\u00a0complementing when\u00a0necessary\u00a0the provided results with the best available data.      ==> Finally, it is the responsibility of the users of this information to decide whether it is appropriate to use these data and whether the data meet their needs. The authors of this resource can in no way be held responsible for the results obtained from the use of this data.", "keywords": ["EJP Soil", "Random Forest", "Italy", "Tuscany", "Soil Organic Carbon (SOC)", "SOC loss", "Topsoil", "SERENA", "Grant n 862695", "Digital Soil Mapping"]}, "links": [{"href": "https://doi.org/10.5281/zenodo.14012785"}, {"rel": "self", "type": "application/geo+json", "title": "10.5281/zenodo.14012785", "name": "item", "description": "10.5281/zenodo.14012785", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5281/zenodo.14012785"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-10-31T00:00:00Z"}}, {"id": "10.5281/zenodo.14039385", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:22:26Z", "type": "Dataset", "title": "Maps of topsoil (0-30 cm) properties of Tuscany (Italy)", "description": "Open AccessThe internal EJP SOIL project SERENA contributed to the evaluation of soil multifunctionality aiming at providing assessment tools for land planning and soil policies at different scales. By co-working with relevant stakeholders, the project provided co-developed indicators and associated cookbooks to assess and map them, to report both on soil degradation, soil-based ecosystem services and their bundles, under actual conditions and for climate and land-use changes, at the regional, national, and European scales.  The topsoil (0-30 cm) properties maps are prepared to evaluate soil ecosystem services in SERENA/EJP-Soil and for applying SOC loss Cookbook and SOIL Loss Cookbook. In particular Soil Organic Carbon content map was directly considered as an application of SOC loss Cookbook (DOI: 10.5281/zenodo.13951265\u00a0Version 3).  They are based on Tuscany Region soil database available at Geoscopio (https://www502.regione.toscana.it/geoscopio/pedologia.html) and on point soil data not freely available (Lamma Consortium). More information and requests to:\u00a0info@lamma.toscana.it.  In accordance with the methodology reported in the Soil Organic Carbon Mapping Cookbook (Yigini et al., 2018), the following soil properties were mapped for all Tuscany Region:    soil organic carbon content (dag/kg),  soil organic carbon stock (t/ha),  textural fractions (sand, silt and clay, USDA limits, dag/kg),  rock fragments (vol/vol),  pH in water,  bulk density (g/cm3).   They were obtained through Digital Soil Mapping (DSM) approach, based on correlations with numerous environmental factors and using Random Forest algorithm.  All the maps have a 100 m spatial resolution.", "keywords": ["silt", "bulk density", "pH", "soil organic carbon content", "sand", "clay", "Grant n. 862695", "Digital Soil Mapping", "textural fractions", "Italy", "topsoil properties", "Tuscany", "soil organic carbon stock", "EJP-SOIL", "SERENA Project"]}, "links": [{"href": "https://doi.org/10.5281/zenodo.14039385"}, {"rel": "self", "type": "application/geo+json", "title": "10.5281/zenodo.14039385", "name": "item", "description": "10.5281/zenodo.14039385", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5281/zenodo.14039385"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-11-05T00:00:00Z"}}, {"id": "10.60692/2ezcc-55g95", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:24:07Z", "type": "Journal Article", "created": "2021-11-28", "title": "Impacts of Farming Layer Constructions on Cultivated Land Quality under the Cultivated Land Balance Policy", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Cultivated Land Balance Policy (CLBP) has led to the \u201cbetter land occupied and worse land supplemented\u201d program. At the same time, the current field-scale cultivated land quality (CLQ) evaluation cannot meet the work requirements of the CLBP. To this end, this study selected 24 newly added farmland in Fuping County and performed eight different high quality farming layer construction experiments to improve the CLQ. A new comprehensive model was constructed on a field scale to evaluate the CLQ using different tests from multi-dimensional perspectives of soil fertility, engineering, environment, and ecology, and to determine the best test mode. The results showed that after the test, around 62% of the cultivated land improved by one level, and the average cultivated land quality level and quality index of the test area increased by 0.63 and 30.63, respectively. The treatment of \u201cwoody peat + rotten crop straw + biostimulation regulator II + conventional fertilization\u201d had the best effect on the improvement of organic matter, soil aggregates, and soil microbial activity, and was the best treatment method. In general, application of soil amendments, such as woody peat when constructing high quality farmland, could quickly improve CLQ, and field-scale CLQ evaluation model constructed from a multi-dimensional perspective could accurately assess the true quality of farmland and allow managers to improve and manage arable land resources under CLBP.</p></article>", "keywords": ["Scale (ratio)", "cultivated land quality evaluation", "Agricultural engineering", "Agricultural and Biological Sciences", "Engineering", "Soil Evaluation", "Agricultural land", "Soil water", "Arable land", "cultivated land quality evaluation; field scale; high-quality farming layer; woody peat", "2. Zero hunger", "Global and Planetary Change", "Global Analysis of Ecosystem Services and Land Use", "Geography", "Ecology", "S", "high-quality farming layer", "Life Sciences", "Land Suitability", "Land-Use Suitability Assessment Using GIS", "Land reclamation", "Agriculture", "04 agricultural and veterinary sciences", "woody peat", "Soil Erosion and Agricultural Sustainability", "Agricultural Land Use", "6. Clean water", "FOS: Philosophy", " ethics and religion", "Physical Sciences", "Quality (philosophy)", "field scale", "Cartography", "Soil Science", "Epistemology", "Management", " Monitoring", " Policy and Law", "Soil quality", "Environmental science", "Crop Suitability", "Agroforestry", "Biology", "Soil science", "Peat", "15. Life on land", "Topsoil", "Philosophy", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "Land use", "0401 agriculture", " forestry", " and fisheries"]}, "links": [{"href": "http://www.mdpi.com/2073-4395/11/12/2403/pdf"}, {"href": "https://doi.org/10.60692/2ezcc-55g95"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Agronomy", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.60692/2ezcc-55g95", "name": "item", "description": "10.60692/2ezcc-55g95", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.60692/2ezcc-55g95"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-11-25T00:00:00Z"}}, {"id": "2078.1/260550", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:25:21Z", "type": "Journal Article", "created": "2022-05-02", "title": "Mineral element recycling in topsoil following permafrost degradation and a vegetation shift in sub-Arctic tundra", "description": "Climate change affects the Arctic and sub-Arctic regions by exposing previously frozen permafrost to thaw, unlocking soil nutrients, changing hydrological processes, and boosting plant growth. As a result, sub-Arctic tundra is subject to a shrub expansion, called \u201cshrubification\u201d, at the expense of sedge species. Depending on the intrinsic foliar properties of these plant species, changes in foliar mineral element fluxes with shrubification in the context of permafrost degradation may influence topsoil mineral element composition. Despite the potential implications of changes in topsoil mineral element concentrations for the fate of organic carbon, this remains poorly quantified. Here, we investigate vegetation foliar and topsoil mineral element composition (Si, K, Ca, P, Mn, Zn, Cu, Mo, V) across a natural gradient of permafrost degradation at a typical sub-Arctic tundra at Eight Mile Lake (Alaska, USA). Results show that foliar mineral element concentrations are higher (up to 9 times; Si, K, Mo for all species, and for some species Zn) or lower (up to 2 times; Ca, P, Mn, Cu, V for all species, and for some species Zn) in sedge than in shrub species. As a result, a vegetation shift over ~40 years has resulted in lower topsoil concentrations in Si, K, Zn, and Mo (respectively of 52, 24, 20, and 51%) in highly degraded permafrost sites compared to poorly degraded permafrost sites due to lower foliar fluxes of these elements. For other elements (Ca, P, Mn, Cu, and V), the vegetation shift has not induced a marked change in topsoil concentrations at this current stage of permafrost degradation. A modeled amplified shrubification associated with a further permafrost degradation is expected to increase foliar Ca, P, Mn, Cu, and V fluxes, which will likely change these element concentrations in topsoil. These data can serve as a first estimate to assess the influence of other shifts in vegetation in Arctic and sub-Arctic tundra such as sedge expansion under wetter soil conditions.", "keywords": ["topsoil", "[SDV.SA.STA] Life Sciences [q-bio]/Agricultural sciences/Sciences and technics of agriculture", "mineral elements", "04 agricultural and veterinary sciences", "sub-Arctic tundra", "15. Life on land", "01 natural sciences", "vegetation change", "13. Climate action", "[SDV.SA.STA]Life Sciences [q-bio]/Agricultural sciences/Sciences and technics of agriculture", "0401 agriculture", " forestry", " and fisheries", "shrubification", "permafrost degradation", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/2078.1/260550"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Geoderma", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "2078.1/260550", "name": "item", "description": "2078.1/260550", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2078.1/260550"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-09-01T00:00:00Z"}}, {"id": "10.5281/zenodo.7079582", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:23:28Z", "type": "Report", "title": "Satellite based estimation of the arable topsoil texture at regional scale using Sentinel-2 data", "description": "Although satellite imaging has been present as a source of valuable spatial data for a long time, it was not until very recently that high quality satellite imagery products produced by high resolution multispectral instruments became affordable and broadly available. On the other hand, information contained in such measurements proved to have significant impact on the overall improvement of the best practices in agricultural production and environmental monitoring. One of the applications that could benefit from the large scale satellite based measurements is characterization of topsoil properties of arable land. More exactly, bare soil spectra acquired by multispectral instruments can directly provide information about soil texture, represented by the content of clay, sand, or silt, over the observed vegetation free area. There have been a few attempts to investigate such possibilities in the context of the current and forthcoming multispectral and hyperspectral imagers. In a recently published study, a comprehensive evaluation of the capabilities of several imagers in the task of soil texture estimation was performed. However, those findings were based only on the simulated and resampled spectral responses derived from the soil spectral signature libraries acquired under controlled laboratory conditions using high precision hyperspectral instruments. Among the simulated imagers was also Sentinel-2 MSI. In line with these efforts, aim of this paper is to further investigate applicability of this instrument in the real working environment, characterized by the challenging factors introduced by the atmosphere, tillage and plant remains, missing data due to cloud coverage, variable soil moisture as a consequence of climate and volatile weather conditions, as well as natural soil spatial variability, due to the large spatial extent of the performed analysis.", "keywords": ["2. Zero hunger", "13. Climate action", "Sentinel-2", " Satellite imaging", " Topsoil texture", " Estimation", "15. Life on land"], "contacts": [{"organization": "Predrag Lugonja, Branko Brklja\u010d, Vladimir \u0106iri\u0107, Pavel Benka, Vladimir Crnojevi\u0107,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5281/zenodo.7079582"}, {"rel": "self", "type": "application/geo+json", "title": "10.5281/zenodo.7079582", "name": "item", "description": "10.5281/zenodo.7079582", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5281/zenodo.7079582"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-09-28T00:00:00Z"}}, {"id": "10.5281/zenodo.7079583", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:23:28Z", "type": "Report", "title": "Satellite based estimation of the arable topsoil texture at regional scale using Sentinel-2 data", "description": "Although satellite imaging has been present as a source of valuable spatial data for a long time, it was not until very recently that high quality satellite imagery products produced by high resolution multispectral instruments became affordable and broadly available. On the other hand, information contained in such measurements proved to have significant impact on the overall improvement of the best practices in agricultural production and environmental monitoring. One of the applications that could benefit from the large scale satellite based measurements is characterization of topsoil properties of arable land. More exactly, bare soil spectra acquired by multispectral instruments can directly provide information about soil texture, represented by the content of clay, sand, or silt, over the observed vegetation free area. There have been a few attempts to investigate such possibilities in the context of the current and forthcoming multispectral and hyperspectral imagers. In a recently published study, a comprehensive evaluation of the capabilities of several imagers in the task of soil texture estimation was performed. However, those findings were based only on the simulated and resampled spectral responses derived from the soil spectral signature libraries acquired under controlled laboratory conditions using high precision hyperspectral instruments. Among the simulated imagers was also Sentinel-2 MSI. In line with these efforts, aim of this paper is to further investigate applicability of this instrument in the real working environment, characterized by the challenging factors introduced by the atmosphere, tillage and plant remains, missing data due to cloud coverage, variable soil moisture as a consequence of climate and volatile weather conditions, as well as natural soil spatial variability, due to the large spatial extent of the performed analysis.", "keywords": ["2. Zero hunger", "13. Climate action", "Sentinel-2", " Satellite imaging", " Topsoil texture", " Estimation", "15. Life on land"]}, "links": [{"href": "https://doi.org/10.5281/zenodo.7079583"}, {"rel": "self", "type": "application/geo+json", "title": "10.5281/zenodo.7079583", "name": "item", "description": "10.5281/zenodo.7079583", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5281/zenodo.7079583"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-09-28T00:00:00Z"}}, {"id": "3178537690", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:26:03Z", "type": "Journal Article", "created": "2021-06-29", "title": "Significant loss of soil inorganic carbon at the continental scale", "description": "Abstract                <p>Widespread soil acidification due to atmospheric acid deposition and agricultural fertilization may greatly accelerate soil carbonate dissolution and CO2 release. However, to date, few studies have addressed these processes. Here, we use meta-analysis and nationwide-survey datasets to investigate changes in soil inorganic carbon (SIC) stocks in China. We observe an overall decrease in SIC stocks in topsoil (0\uffe2\uff80\uff9330\uffc2\uffa0cm) (11.33\uffc2\uffa0g C m\uffe2\uff80\uff932 yr\uffe2\uff80\uff931) from the 1980s to the 2010s. Total SIC stocks have decreased by \uffe2\uff88\uffbc8.99\uffc2\uffa0\uffc2\uffb1\uffc2\uffa02.24% (1.37\uffc2\uffa0\uffc2\uffb1\uffc2\uffa00.37\uffc2\uffa0Pg C). The average SIC losses across China (0.046 Pg C yr\uffe2\uff80\uff931) and in cropland (0.016 Pg C yr\uffe2\uff80\uff931) account for \uffe2\uff88\uffbc17.6%\uffe2\uff80\uff9324.0% of the terrestrial C sink and 57.1% of the soil organic carbon sink in cropland, respectively. Nitrogen deposition and climate change have profound influences on SIC cycling. We estimate that \uffe2\uff88\uffbc19.12%\uffe2\uff80\uff9319.47% of SIC stocks will be further lost by 2100. The consumption of SIC may offset a large portion of global efforts aimed at ecosystem carbon sequestration, which emphasizes the importance of achieving a better understanding of the indirect coupling mechanisms of nitrogen and carbon cycling and of effective countermeasures to minimize SIC loss.</p", "keywords": ["Carbon sequestration", "Cartography", "China", "Mechanics and Transport in Unsaturated Soils", "Carbonate", "Nitrogen", "Soil Science", "Organic chemistry", "Carbon Dynamics in Peatland Ecosystems", "soil inorganic carbon stocks", "Soil pH", "Environmental science", "Carbon sink", "Agricultural and Biological Sciences", "carbonate", "Engineering", "Soil water", "Soil Carbon Sequestration", "Biology", "global change", "Ecosystem", "Soil acidification", "Civil and Structural Engineering", "Soil science", "2. Zero hunger", "Soil organic matter", "Soil Fertility", "Ecology", "Geography", "Soil Water Retention", "Life Sciences", "Cycling", "Forestry", "Carbon cycle", "04 agricultural and veterinary sciences", "15. Life on land", "Topsoil", "Soil carbon", "Chemistry", "Sink (geography)", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "Physical Sciences", "Environmental chemistry", "0401 agriculture", " forestry", " and fisheries", "soil acidification", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems", "Research Article"]}, "links": [{"href": "https://doi.org/3178537690"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/National%20Science%20Review", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "3178537690", "name": "item", "description": "3178537690", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/3178537690"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-07-02T00:00:00Z"}}, {"id": "1854/LU-01GM39MMFY2YP4FTDY102R50HB", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:25:01Z", "type": "Journal Article", "created": "2021-11-17", "title": "Spatiotemporal Prediction and Mapping of Heavy Metals at Regional Scale Using Regression Methods and Landsat 7", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Soil contamination by heavy metals is of particular concern, due to the direct negative impact on crop yield, food quality and human health. Although the conventional approach to monitor heavy metals relies on field sampling and lab analysis, the proliferation in the use of portable spectrometers has reduced the cost and time of investigation. However, discrepancies in spectral data from different spectrometers increase the modeling time and undermine the model accuracy for spatial mapping. This study, therefore, took advantage of the readily accessible Landsat 7 data to predict and map the spatiotemporal distribution of ten heavy metals (i.e., Sb, Pb, Ni, Mn, Hg, Cu, Cr, Co, Cd and As) over a 640 km2 area in Belgium. The Land Use/Cover Area Frame Survey (LUCAS) database of a region in north-eastern Belgium was used to retrieve variation in heavy metals concentrations over time and space, using the Landsat 7 imagery for four single dates in 2009, 2013, 2016 and 2020. Three regression methods, namely, partial least squares regression (PLSR), random forest (RF) and support vector machine (SVM) were used to model and predict the heavy metal concentrations for 2009. By comparing these models unbiasedly, the best model was selected for predicting and mapping the heavy metal distributions for 2013, 2016 and 2020. RF turned out to be the optimal model for 2009 with a coefficient of determination of prediction (R2P) and residual prediction deviation of prediction (RPDP) ranging from 0.62 to 0.92, and 1.23 to 2.79, respectively. The measured heavy metal distributions along the river floodplains, at the highlands and in the lowlands, were generally high, compared to their RF spatiotemporal predictions, which decreased over time. Increasing moisture contents in the floodplains adjacent to the river channels and the lowlands were the primary contributors to the reduction in the satellite reflectance spectra. However, topsoil erosion from rainfall, snowmelt as well as wind into the lowlands could have influenced the reduction in heavy metal spatiotemporal predicted values over time in the highlands. The spatiotemporal prediction maps produced for the heavy metals for the four different years revealed a good spatial similarity and consistency with the measured maps for 2009, which indicates their stability over the years.</p></article>", "keywords": ["Technology", "PROVINCE", "Landsat 7", "analysis", "Science", "Environmental Sciences & Ecology", "random forest (RF)", "MOISTURE", "01 natural sciences", "NIR SPECTROSCOPY", "0203 Classical Physics", "Remote Sensing", "0909 Geomatic Engineering", "spatiotemporal analysis", "AGRICULTURAL SOILS", "Geosciences", " Multidisciplinary", "Imaging Science & Photographic Technology", "spatiotemporal", "0105 earth and related environmental sciences", "2. Zero hunger", "Science & Technology", "RANGE", "Q", "Geology", "04 agricultural and veterinary sciences", "15. Life on land", "6. Clean water", "3. Good health", "MULTIVARIATE", "TOPSOILS", "13. Climate action", "Earth and Environmental Sciences", "Physical Sciences", "soil heavy metal; Landsat 7; partial least squares regression (PLSR); random forest (RF); support vector machine (SVM); spatiotemporal analysis", "0401 agriculture", " forestry", " and fisheries", "support vector machine (SVM)", "4013 Geomatic engineering", "0406 Physical Geography and Environmental Geoscience", "soil heavy metal", "partial least squares regression (PLSR)", "Life Sciences & Biomedicine", "3701 Atmospheric sciences", "Environmental Sciences", "3709 Physical geography and environmental geoscience"]}, "links": [{"href": "http://www.mdpi.com/2072-4292/13/22/4615/pdf"}, {"href": "https://www.mdpi.com/2072-4292/13/22/4615/pdf"}, {"href": "https://doi.org/1854/LU-01GM39MMFY2YP4FTDY102R50HB"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Remote%20Sensing", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "1854/LU-01GM39MMFY2YP4FTDY102R50HB", "name": "item", "description": "1854/LU-01GM39MMFY2YP4FTDY102R50HB", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/1854/LU-01GM39MMFY2YP4FTDY102R50HB"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-11-16T00:00:00Z"}}, {"id": "1854/LU-01JV4A4VV9MSQATBRHJD3K77RH", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:25:01Z", "type": "Journal Article", "created": "2025-04-25", "title": "Multi-dimensional evaluation of site-specific tillage using mouldboard ploughing", "description": "Due to the lack of high-resolution data on soil compaction using proximal sensing technology, mouldboard (MB) ploughing is carried out at uniform speed and depth, which does not necessarily respond to tillage needs due to compaction level and depth that are spatially variable across the field area. This study aims at simulating the comparative performance of different site specific tillage (SST) schemes (e.g., speed and depth) and uniform tillage of a MB plough using a high resolution soil packing density (PD) maps. An on-the-go soil sensing platform was used to predict and map topsoil PD in a Luvisol field in Belgium and two Cambisol fields in Spain. All fields were divided into three management zones, to each of which different tillage speed and depth were assigned based on PD maps. A MATLAB simulation code was developed to predict and compare the power efficiency, fuel consumption, emission of carbon dioxide (CO2) from diesel combustion and total operating time of uniform, SST depth, SST speed, and hybrid SST depth and speed MB ploughing schemes. Results revealed that the degree of soil compaction varies from field to field and within fields, which necessitates SST tillage practices. It was found that the depth control was the best performing SST in fields having large areas with low (PD < 1.55) and medium (PD = 1.55 - 1.70) compaction levels, resulting in the largest reduction in draught (33.7 % - 57 %), fuel consumption and CO2 emission (29.6 % - 50.1 %), while using the same operational time as that of the uniform tillage. However, in cases when the majority of the field area was highly compacted (PD > 1.70), potential savings were smaller at 22.5 %, with the speed control emerged as a more effective control scheme. It is recommended to validate the simulation results of SST of MB ploughing in fields to enable assessing the impacts they have on crop responses and soil quality.", "keywords": ["Agriculture and Food Sciences", "CALIBRATION", "NEAR-INFRARED SPECTROSCOPY", "Precision agriculture", "IN-SITU", "SOIL COMPACTION", "Compaction", "LOAM", "Energy consumption", "DENSITY", "ONLINE SENSOR", "On-the-go soil sensing", "Simulation", "TOPSOIL COMPACTION"]}, "links": [{"href": "https://doi.org/1854/LU-01JV4A4VV9MSQATBRHJD3K77RH"}, {"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": "1854/LU-01JV4A4VV9MSQATBRHJD3K77RH", "name": "item", "description": "1854/LU-01JV4A4VV9MSQATBRHJD3K77RH", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/1854/LU-01JV4A4VV9MSQATBRHJD3K77RH"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-10-01T00:00:00Z"}}, {"id": "1c591de0-f438-4dcb-857c-a6e4803e7eee", "type": "Feature", "geometry": null, "properties": {"updated": "2025-09-02T09:56:59", "type": "Dataset", "language": "de", "title": "INSPIRE Soil / Carbon Stocks in the Soil BB", "description": "Der interoperable INSPIRE-Datensatz beinhaltet Daten vom LBGR \u00fcber die Kohlenstoffvorr\u00e4te im Boden Brandenburg, transformiert in das INSPIRE-Zielschema Boden. Der Datensatz wird \u00fcber je einen interoperablen Darstellungs- und Downloaddienst bereitgestellt.      ---      The compliant INSPIRE data set contains data about the carbon stocks in the soil of the State of Brandenburg from the LBGR, transformed into the INSPIRE annex schema Soil. The data set is provided via compliant view and download services.", "formats": [{"name": "WFS_SRVC"}], "keywords": ["High value dataset", "bboxbebb", "boden", "bodenkunde", "bodenschutz", "brandenburg", "de", "depthinterval", "derivedsoilprofile", "erdbeobachtung-und-umwelt", "geologie", "inspireidentifiziert", "interoperabel", "interoperability", "interoperable-daten", "kohlenstoff", "kohlenstoffvorra\u0308te", "kohlenstoffvorra\u0308te-im-boden-brandenburg", "om_observation", "opendata", "organic-carbon-stock", "organiccarbonstock", "process", "regional", "soil", "soilderivedobject", "soillayer", "topsoil"], "contacts": [{"organization": "Landesamt f\u00fcr Bergbau, Geologie und Rohstoffe Brandenburg (LBGR)", "roles": ["creator"]}]}, "links": [{"href": "https://inspire.brandenburg.de/services/so_cvorr_wfs?REQUEST=GetCapabilities&SERVICE=WFS"}, {"href": "https://inspire.brandenburg.de/services/so_cvorr_wms?REQUEST=GetCapabilities&SERVICE=WMS"}, {"href": "http://data.europa.eu/88u/dataset/1c591de0-f438-4dcb-857c-a6e4803e7eee~~2"}, {"rel": "self", "type": "application/geo+json", "title": "1c591de0-f438-4dcb-857c-a6e4803e7eee", "name": "item", "description": "1c591de0-f438-4dcb-857c-a6e4803e7eee", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/1c591de0-f438-4dcb-857c-a6e4803e7eee"}, {"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": "2a792d87-9fb6-489d-8afb-188b1190c881", "type": "Feature", "geometry": {"type": "Polygon", "coordinates": [[[11.27, 51.36], [11.27, 53.56], [14.77, 53.56], [14.77, 51.36], [11.27, 51.36]]]}, "properties": {"themes": [{"concepts": [{"id": "geoscientificInformation"}], "scheme": "https://standards.iso.org/iso/19139/resources/gmxCodelists.xml#MD_TopicCategoryCode"}, {"concepts": [{"id": "Boden"}], "scheme": "GEMET - INSPIRE themes, version 1.0"}, {"concepts": [{"id": "Regional"}], "scheme": "Spatial scope"}], "updated": "2023-08-04T14:11:10", "type": "Dataset", "created": "2019-10-23T00:00:00", "language": "ger", "title": "INSPIRE Data Set: Soil / Soil erosion hazard due to wind in Brandenburg (LBGR)", "description": "Der interoperable INSPIRE-Datensatz beinhaltet Daten vom LBGR \u00fcber die potentielle Erosionsgef\u00e4hrdung durch Wind in Brandenburg, transformiert in das INSPIRE-Zielschema Soil. Der Datensatz wird \u00fcber je einen interoperablen Darstellungs- und Downloaddienst bereitgestellt. \n\t  \t--- \n\t  \tThe compliant INSPIRE data set contains data about the potential erosion risk by wind in the State of Brandenburg from the LBGR, transformed into the INSPIRE annex schema Soil. The data set is provided via compliant view and download services.", "formats": [{"name": "Soil GML Application Schema"}, {"name": "OGC:WFS"}], "keywords": ["inspireidentifiziert", "SoilBody", "Brandenburg", "topSoil", "SoilLayer", "Geologie", "Oberboden", "Soil", "DerivedSoilProfile", "OM_Observation", "interoperability", "Bodenkunde", "Bodenschutz", "siteSpecificWindErosionRisk", "SoilDerivedObject", "interoperabel", "Bodenerosionsgef\u00e4hrdung durch Wind in Brandenburg", "windErosionRiskTopSoil", "Process", "Bodenerosionsgef\u00e4hrdung", "interoperable Daten", "Boden", "Regional"], "contacts": [{"name": "Herr Arvid Markert", "organization": "Landesamt f\u00fcr Bergbau, Geologie und Rohstoffe Brandenburg (LBGR)", "position": null, "roles": ["pointOfContact"], "phones": [{"value": "+49 355 48640 167"}], "emails": [{"value": "arvid.markert@lbgr.brandenburg.de"}], "addresses": [{"deliveryPoint": ["Inselstra\u00dfe 26"], "city": "Cottbus", "administrativeArea": "Brandenburg", "postalCode": "03046", "country": null}], "links": [{"href": null}]}, {"name": "INSPIRE-Zentrale im Land Brandenburg", "organization": "Landesvermessung und Geobasisinformation Brandenburg (LGB)", "position": null, "roles": ["publisher"], "phones": [{"value": "+49-331-8844-123"}], "emails": [{"value": "kundenservice@inspire.brandenburg.de"}], "addresses": [{"deliveryPoint": ["Heinrich-Mann-Allee 104 B"], "city": "Potsdam", "administrativeArea": "Brandenburg", "postalCode": "14473", "country": null}], "links": [{"href": null}]}], "denominator": "300000"}, "links": [{"href": "https://inspire.brandenburg.de/services/so_boerosionwi_wfs?REQUEST=GetCapabilities&SERVICE=WFS", "description": "Download-Service", "protocol": "OGC:WFS", "rel": "download"}, {"href": "https://isk.geobasis-bb.de/md-thumbnail/ds-so-boerosionwi.png", "name": "preview", "description": "Web image thumbnail (URL)", "protocol": "WWW:LINK-1.0-http--image-thumbnail", "rel": "preview"}, {"rel": "self", "type": "application/geo+json", "title": "2a792d87-9fb6-489d-8afb-188b1190c881", "name": "item", "description": "2a792d87-9fb6-489d-8afb-188b1190c881", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2a792d87-9fb6-489d-8afb-188b1190c881"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date-time": "2023-08-04T14:11:10Z"}}, {"id": "5322e3b2-2292-4c8f-b000-ea782fc8283a", "type": "Feature", "geometry": null, "properties": {"updated": "2025-09-02T09:55:46", "type": "Dataset", "language": "de", "title": "INSPIRE-WFS Soil / Kohlenstoffvorr\u00e4te im Boden BB", "description": "Der interoperable INSPIRE-WFS ist ein Downloaddienst, der Daten im Annex-Schema Boden (abgeleitet aus dem origin\u00e4ren Datensatz: Kohlenstoffvorr\u00e4te im Boden Brandenburg) bereitstellt. Er gibt einen \u00dcberblick \u00fcber die Kohlenstoffvorr\u00e4te bis 0,3 m, 1 m und 2 m Tiefe unter der Gel\u00e4ndeoberfl\u00e4che im Land Brandenburg. Die Karte basiert auf den Legendeneinheiten der Boden\u00fcbersichtskarte (B\u00dcK300) mit entsprechender Zuordnung von parametrisierten Fl\u00e4chenbodenformen, die durch Gel\u00e4nde- und Laboruntersuchungen bestimmt wurden. Dazu wurden f\u00fcr gleiche Horizont-Substrat-Kombinationen die entsprechenden Parameter (wie Corg-Gehalte) statistisch abgeleitet (i.d.R. der Medianwert). Die Abfolge von Horizont-Substrat-Kombinationen der Fl\u00e4chenbodenformen mit ihren Corg-Gehalten bildet die Grundlage f\u00fcr die Mengenberechnung in t/ha. Diese wurden in Stufen von je 30 t/ha klassifiziert. Gem\u00e4\u00df der INSPIRE-Datenspezifikation Soil (D2.8.III.3_v3.0) liegen die Inhalte der Karte INSPIRE-konform vor. Der WFS beinhaltet die folgenden FeatureTypes:     - Beobachtungsprozess (ompr:Process) mit Angaben zu der am Prozess beteiligten Organisation LBGR,      - abgeleitetes Bodenobjekt (so:SoilDerivedObject) mit Angaben zur Beobachtung der Bodeneigenschaft zur Beschreibung des abgeleiteten Bodenobjekts,     - Beobachtung einer Bodeneigenschaft (om:OM_Observation) mit Angaben zum Charakter des vom Boden abgeleiteten Objekts, der beobachtete Eigenschaft, der vom Boden abgeleiteten Beobachtung bodenbezogene Eigenschaften (SoilDerivedObjectParameterNameValue:organicCarbonStock), dem Ergebnis der Beobachtungen des abgeleiteten Bodenobjekts,        - Bodenk\u00f6rper (so:SoilBody), abgegrenzter und hinsichtlich bestimmter Bodeneigenschaften und/oder r\u00e4umlicher Muster homogener Teil der Bodendecke, und     - Bodenschicht (so:SoilLayer) mit Angaben zur Zuordnung der Schicht zu einem ihrer Art entsprechenden Begriff (LayerTypeValue: topsoil und depthInterval), zum abgeleiteten Profil, das als Referenzprofil f\u00fcr eine bestimmte Art von Boden in einem bestimmten geografischen Gebiet dient, der oberen und unteren Tiefe des Profilelements, gemessen von der Oberfl\u00e4che (0 cm) eines Bodenprofils (in cm).     ---      The compliant INSPIRE-WFS Soil / Kohlenstoffvorr\u00e4te im Boden Brandenburg is a download service that delivers data in the annex schema Soil (derived from the original data set: Carbon stocks in the soil Brandenburg). It provides an overview of the carbon stocks up to 0.3 m, 1 m and 2 m depth below ground level in the state of Brandenburg. The map is based on the legend units of the soil map (B\u00dcK300) with corresponding assignment of parameterized soil forms determined by field and laboratory investigations. For the same horizon-substrate combinations, the corresponding parameters (such as Corg contents) were statistically derived (usually the median value). The sequence of horizon-substrate combinations of the soil forms with their Corg contents formed the basis for the quantity calculation in t/ha. These were classified in steps of 30 t/ha each. The content of the soil map is compliant to the INSPIRE data specification for the annex theme Soil (D2.8.III.3_v3.0). The WFS includes the following feature types:      - Observation process (ompr:Process) with information about the organization LBGR involved in the process,     - Soil derived object (so:SoilDerivedObject) with information on the observation of the soil property for characterizing the soil derived object,     - Observations of a soil derived object (om:OM_Observation) with information about the character of the soil derived object, the observed property, the soil derived observation of soil related properties (SoilDerivedObjectParameterNameValue:organicCarbonStock), the result of the observations of the soil derived object,      - Soil body (so:SoilBody), part of the soil cover that is delineated and that is homogeneous with regard to certain soil properties and/or spatial patterns, and     - Soil layer (so:SoilLayer) with information about the assignation of the layer according to the concept that fits its kind (LayerTypeValue: topsoil and depthInterval), to the derived soil profile, which serves as a reference profile for a particular type of soil in a specific geographical area, including the upper and lower depth of the profile element from the surface (0 cm) of a soil profile (in cm).", "formats": [{"name": "HTML"}], "keywords": ["bboxbebb", "boden", "bodenkunde", "bodenschutz", "brandenburg", "de", "depthinterval", "derivedsoilprofile", "geologie", "infofeatureaccessservice", "inspireidentifiziert", "interoperabel", "interoperability", "kohlenstoff", "kohlenstoffvorra\u0308te", "kohlenstoffvorra\u0308te-im-boden-brandenburg", "om_observation", "opendata", "organic-carbon-stock", "organiccarbonstock", "process", "soil", "soilbody", "soilderivedobject", "soillayer", "topsoil", "wfs"], "contacts": [{"organization": "Landesamt f\u00fcr Bergbau, Geologie und Rohstoffe Brandenburg (LBGR)", "roles": ["creator"]}]}, "links": [{"href": "https://geoportal.brandenburg.de/detailansichtdienst/render?view=gdibb&url=https%3A%2F%2Fgeoportal.brandenburg.de%2Fgs-json%2Fxml%3Ffileid%3D5322e3b2-2292-4c8f-b000-ea782fc8283a"}, {"href": "https://inspire.brandenburg.de/services/so_cvorr_wfs?REQUEST=GetCapabilities&SERVICE=WFS"}, {"href": "https://isk.geobasis-bb.de/geodienste/Sonstiges/Hilfe_Nutzung_Downloaddienst.pdf"}, {"href": "http://data.europa.eu/88u/dataset/5322e3b2-2292-4c8f-b000-ea782fc8283a~~1"}, {"rel": "self", "type": "application/geo+json", "title": "5322e3b2-2292-4c8f-b000-ea782fc8283a", "name": "item", "description": "5322e3b2-2292-4c8f-b000-ea782fc8283a", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/5322e3b2-2292-4c8f-b000-ea782fc8283a"}, {"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": "3217045336", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:26:07Z", "type": "Journal Article", "created": "2021-11-29", "title": "Impacts of Farming Layer Constructions on Cultivated Land Quality under the Cultivated Land Balance Policy", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Cultivated Land Balance Policy (CLBP) has led to the \u201cbetter land occupied and worse land supplemented\u201d program. At the same time, the current field-scale cultivated land quality (CLQ) evaluation cannot meet the work requirements of the CLBP. To this end, this study selected 24 newly added farmland in Fuping County and performed eight different high quality farming layer construction experiments to improve the CLQ. A new comprehensive model was constructed on a field scale to evaluate the CLQ using different tests from multi-dimensional perspectives of soil fertility, engineering, environment, and ecology, and to determine the best test mode. The results showed that after the test, around 62% of the cultivated land improved by one level, and the average cultivated land quality level and quality index of the test area increased by 0.63 and 30.63, respectively. The treatment of \u201cwoody peat + rotten crop straw + biostimulation regulator II + conventional fertilization\u201d had the best effect on the improvement of organic matter, soil aggregates, and soil microbial activity, and was the best treatment method. In general, application of soil amendments, such as woody peat when constructing high quality farmland, could quickly improve CLQ, and field-scale CLQ evaluation model constructed from a multi-dimensional perspective could accurately assess the true quality of farmland and allow managers to improve and manage arable land resources under CLBP.</p></article>", "keywords": ["Scale (ratio)", "cultivated land quality evaluation", "Agricultural engineering", "Agricultural and Biological Sciences", "Engineering", "Soil Evaluation", "Agricultural land", "Soil water", "Arable land", "cultivated land quality evaluation; field scale; high-quality farming layer; woody peat", "2. Zero hunger", "Global and Planetary Change", "Global Analysis of Ecosystem Services and Land Use", "Geography", "Ecology", "S", "high-quality farming layer", "Life Sciences", "Land Suitability", "Land-Use Suitability Assessment Using GIS", "Land reclamation", "Agriculture", "04 agricultural and veterinary sciences", "woody peat", "Soil Erosion and Agricultural Sustainability", "Agricultural Land Use", "6. Clean water", "FOS: Philosophy", " ethics and religion", "Physical Sciences", "Quality (philosophy)", "field scale", "Cartography", "Soil Science", "Epistemology", "Management", " Monitoring", " Policy and Law", "Soil quality", "Environmental science", "Crop Suitability", "Agroforestry", "Biology", "Soil science", "Peat", "15. Life on land", "Topsoil", "Philosophy", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "Land use", "0401 agriculture", " forestry", " and fisheries"]}, "links": [{"href": "http://www.mdpi.com/2073-4395/11/12/2403/pdf"}, {"href": "https://doi.org/3217045336"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Agronomy", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "3217045336", "name": "item", "description": "3217045336", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/3217045336"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-11-25T00:00:00Z"}}, {"id": "3bddcde7-4f52-4b64-be4b-3bb1ab10a3af", "type": "Feature", "geometry": null, "properties": {"updated": "2025-09-02T09:57:34", "type": "Dataset", "language": "de", "title": "INSPIRE-WCS Soil / Bodenerosionsgef\u00e4hrdung BB", "description": "Der interoperable INSPIRE-WCS ist ein Downloaddienst, der Daten im Annex-Schema Boden (abgeleitet aus dem origin\u00e4ren Datensatz: Bodenerosionsgef\u00e4hrdung Brandenburg) bereitstellt. Er gibt einen \u00dcberblick zur r\u00e4umlichen Verteilung der potenziellen Bodenerosionsgef\u00e4hrdung sowie des Bodenabtrags durch Wind und Wasser auf den landwirtschaftlichen Fl\u00e4chen Brandenburgs. Der WCS beinhaltet die f\u00fcnf Coverages. Im Coverage \u201eGef\u00e4hrdungsstufen Winderosion\u201c sind die landwirtschaftlichen Fl\u00e4chen in einer r\u00e4umlichen Aufl\u00f6sung von 2x2 Meter nach ihrer potenziellen Winderosionsgef\u00e4hrdung in Anlehnung an die Berechnungsvorschrift DIN19706 (https://dx.doi.org/10.31030/1934215) sowie Funk et al. 2023 (https://dx.doi.org/10.1016/j.aeolia.2023.100878) klassifiziert.  Im Coverage \u201eBodenabtrag (t/ha/a) Wassererosion (RxKxS)\u201c ist der potenzielle Bodenabtrag durch Wasser abgeleitet aus den Erosionsfaktoren R, K und S nach DIN19708 (https://dx.doi.org/10.31030/2676773) in einer r\u00e4umlichen Aufl\u00f6sung von 5x5 Meter dargestellt. Im Coverage \u201eBodenabtrag (t/ha/a) Wassererosion (RxKxSxL)\u201c ist der potenzielle Bodenabtrag durch Wasser abgeleitet aus den Erosionsfaktoren R, K, S und L nach DIN19708 (https://dx.doi.org/10.31030/2676773) in einer r\u00e4umlichen Aufl\u00f6sung von 5x5 Meter dargestellt.  In den Layern \u201eGef\u00e4hrdungsstufen Wassererosion (RxKxS)\u201c und \u201eGef\u00e4hrdungsstufen Wassererosion (RxKxSxL)\u201c ist eine Einstufung der potenziellen Wassererosionsgef\u00e4hrdung der landwirtschaftlichen Fl\u00e4chen nach DIN19708 in einer r\u00e4umlichen Aufl\u00f6sung von 5x5 Meter dargestellt. Die potenzielle Erosionsgef\u00e4hrdung entspricht der Gef\u00e4hrdung der Fl\u00e4chen auf Grund naturr\u00e4umlicher Bedingungen, d.h. ohne Ber\u00fccksichtigung von landwirtschaftlichen Bewirtschaftungsma\u00dfnahmen wie Bodenbearbeitung, Bodenbedeckung und Fruchtfolge. Gem\u00e4\u00df der INSPIRE-Datenspezifikation Soil (D2.8.III.3_v3.0) liegen die Inhalte der Bodenkarte INSPIRE-konform vor. Der WCS beinhaltet die folgenden Coverages: SO.SoilLossWaterErosion (RxKxS), SO.RiskLevelsWaterErosion (RxKxS), SO.SoilLossWaterErosion (RxKxSxL), SO.RiskLevelsWaterErosion (RxKxSxL), SO.RiskLevelsWindErosion      ---      The compliant INSPIRE-WCS is a download service that delivers data in the annex schema Soil (derived from the original data set: Geomorphographic assessments Brandenburg). It provides an overview of the spatial distribution of the potential soil erosion risk as well as soil loss caused by wind and water on agricultural land in Brandenburg. The service contains five layers. In the coverage \u201eRisk levels wind erosion\u201c the agricultural areas are classified in a spatial resolution of 2x2 meters according to their potential wind erosion risk based on the methods DIN19706 (https://dx.doi.org/10.31030/1934215) and Funk et al. 2023 (https://dx.doi.org/10.1016/j.aeolia.2023.100878).  In the coverage \u201eSoil loss (t/ha/a) water erosion (RxKxS)\u201c the potential soil loss caused by water derived from the erosion factors R, K and S according to DIN19708 (https://dx.doi.org/10.31030/2676773) is presented in a spatial resolution of 5x5 meters. In the coverage \u201eSoil loss (t/ha/a) water erosion (RxKxSxL)\u201c the potential soil loss caused by water derived from the erosion factors R, K, S and L according to DIN19708 (https://dx.doi.org/10.31030/2676773) is presented in a spatial resolution of 5x5 meters. In the layers \u201eRisk levels water erosion (RxKxS)\u201c and \u201eRisk levels water erosion (RxKxSxL)\u201c a classification of the potential erosion risk of the agricultural land caused by water according to DIN19708 is presented in a spatial resolution of 5x5 meters. The potential soil erosion risk reflects the erosion of bare soil under natural environmetal conditions, i.e. without taking into account cultivation methods such as tillage, soil cover and crop rotation. The content of the soil map is compliant to the INSPIRE data specification for the annex theme Soil (D2.8.III.3_v3.0). The WCS includes the following coverages: SO.SoilLossWaterErosion (RxKxS), SO.RiskLevelsWaterErosion (RxKxS), SO.SoilLossWaterErosion (RxKxSxL), SO.RiskLevelsWaterErosion (RxKxSxL), SO.RiskLevelsWindErosion", "formats": [{"name": "HTML"}], "keywords": ["boden", "bodenerosion", "bodenerosionsgefa\u0308hrdung", "bodenerosionsgefa\u0308hrdung-durch-wasser-in-brandenburg", "bodenerosionsgefa\u0308hrdung-durch-wind-in-brandenburg", "bodenkunde", "brandenburg", "de", "erosion", "erosionsgefa\u0308hrdung", "gefa\u0308hrdungsstufen", "geologie", "infocoverageaccessservice", "inspireidentifiziert", "interoperabel", "interoperability", "interoperable-daten", "opendata", "process", "regional", "soil", "soillayer", "wassererosion", "water-erosion", "watererosionrisktopsoil", "wcs", "wind-erosion", "winderosion", "winderosionrisktopsoil"], "contacts": [{"organization": "Landesamt f\u00fcr Bergbau, Geologie und Rohstoffe Brandenburg (LBGR)", "roles": ["creator"]}]}, "links": [{"href": "https://geoportal.brandenburg.de/detailansichtdienst/render?view=gdibb&url=https%3A%2F%2Fgeoportal.brandenburg.de%2Fgs-json%2Fxml%3Ffileid%3D3bddcde7-4f52-4b64-be4b-3bb1ab10a3af"}, {"href": "https://inspire.brandenburg.de/services/so_boerosion_wcs?REQUEST=GetCapabilities&SERVICE=WCS"}, {"href": "https://isk.geobasis-bb.de/geodienste/Sonstiges/Hilfe_Nutzung_Downloaddienst.pdf"}, {"href": "http://data.europa.eu/88u/dataset/3bddcde7-4f52-4b64-be4b-3bb1ab10a3af~~1"}, {"rel": "self", "type": "application/geo+json", "title": "3bddcde7-4f52-4b64-be4b-3bb1ab10a3af", "name": "item", "description": "3bddcde7-4f52-4b64-be4b-3bb1ab10a3af", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/3bddcde7-4f52-4b64-be4b-3bb1ab10a3af"}, {"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": "44808c9f-5512-4d2d-b89c-3d042577116a", "type": "Feature", "geometry": null, "properties": {"updated": "2025-09-02T09:57:23", "type": "Dataset", "language": "de", "title": "INSPIRE Soil / Relative binding strength for heavy metals in the topsoil BB", "description": "The interoperable INSPIRE dataset includes data from the LBGR on the relative binding strength for heavy metals in the Brandenburg topsoil, transformed into the INSPIRE target soil scheme. The dataset is provided via an interoperable display and download service.  --- The compliant INSPIRE data set contains data about the relative sorption strength for heavy metals in the top soil in the State of Brandenburg from the LBGR, transformed into the INSPIRE annex schema Soil. The data set is provided via compliant view and download services.", "formats": [{"name": "WFS_SRVC"}], "keywords": ["High value dataset", "adsorptionsvermo\u0308gen", "bboxbebb", "boden", "bodenkunde", "bodenschutz", "brandenburg", "de", "depthinterval", "derivedsoilprofile", "erdbeobachtung-und-umwelt", "geologie", "inspireidentifiziert", "interoperabel", "interoperability", "interoperable-daten", "om_observation", "opendata", "ph-wert", "process", "regional", "relative-bindungssta\u0308rke-fu\u0308r-schwermetalle", "schwermetall", "soil", "soilderivedobject", "soillayer", "sorption-strength-for-heavy-metals", "sorptionstrengthheavymetals", "topsoil"], "contacts": [{"organization": "Landesamt f\u00fcr Bergbau, Geologie und Rohstoffe Brandenburg (LBGR)", "roles": ["creator"]}]}, "links": [{"href": "https://inspire.brandenburg.de/services/so_boschwermoben_wfs?REQUEST=GetCapabilities&SERVICE=WFS"}, {"href": "https://inspire.brandenburg.de/services/so_boschwermoben_wms?REQUEST=GetCapabilities&SERVICE=WMS"}, {"href": "http://data.europa.eu/88u/dataset/44808c9f-5512-4d2d-b89c-3d042577116a~~1"}, {"rel": "self", "type": "application/geo+json", "title": "44808c9f-5512-4d2d-b89c-3d042577116a", "name": "item", "description": "44808c9f-5512-4d2d-b89c-3d042577116a", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/44808c9f-5512-4d2d-b89c-3d042577116a"}, {"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": "477cfc2a-31fa-4809-9475-5ac044a010a5", "type": "Feature", "geometry": null, "properties": {"updated": "2025-09-02T09:57:20", "type": "Dataset", "language": "de", "title": "INSPIRE Soil / Potential Compression Sensitivity BB", "description": "Der interoperable INSPIRE-Datensatz beinhaltet Daten vom LBGR \u00fcber die potenzielle Verdichtungsempfindlichkeit Brandenburg in 35 cm Bezugstiefe, transformiert in das INSPIRE-Zielschema Boden. Der Datensatz wird \u00fcber je einen interoperablen Darstellungs- und Downloaddienst bereitgestellt.      ---      The compliant INSPIRE data set contains data about potential compaction sensitivity in the topsoil in the State of Brandenburg from the LBGR, transformed into the INSPIRE annex schema Soil. The data set is provided via compliant view and download services.", "formats": [{"name": "WFS_SRVC"}], "keywords": ["High value dataset", "bboxbebb", "boden", "bodenkunde", "bodenschutz", "brandenburg", "compactionsensitivity", "de", "derivedsoilprofile", "erdbeobachtung-und-umwelt", "geologie", "inspireidentifiziert", "interoperabel", "interoperability", "interoperable-daten", "oberboden", "om_observation", "opendata", "process", "regional", "sedimentarymaterial", "soil", "soilbody", "soilderivedobject", "soillayer", "topsoil", "verdichtungsempfindlichkeit"], "contacts": [{"organization": "Landesamt f\u00fcr Bergbau, Geologie und Rohstoffe Brandenburg (LBGR)", "roles": ["creator"]}]}, "links": [{"href": "https://inspire.brandenburg.de/services/so_verdicht_wfs?REQUEST=GetCapabilities&SERVICE=WFS"}, {"href": "https://inspire.brandenburg.de/services/so_verdicht_wms?REQUEST=GetCapabilities&SERVICE=WMS"}, {"href": "http://data.europa.eu/88u/dataset/477cfc2a-31fa-4809-9475-5ac044a010a5~~2"}, {"rel": "self", "type": "application/geo+json", "title": "477cfc2a-31fa-4809-9475-5ac044a010a5", "name": "item", "description": "477cfc2a-31fa-4809-9475-5ac044a010a5", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/477cfc2a-31fa-4809-9475-5ac044a010a5"}, {"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": "PMC8824702", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:28:07Z", "type": "Journal Article", "created": "2021-06-29", "title": "Significant loss of soil inorganic carbon at the continental scale", "description": "Abstract                <p>Widespread soil acidification due to atmospheric acid deposition and agricultural fertilization may greatly accelerate soil carbonate dissolution and CO2 release. However, to date, few studies have addressed these processes. Here, we use meta-analysis and nationwide-survey datasets to investigate changes in soil inorganic carbon (SIC) stocks in China. We observe an overall decrease in SIC stocks in topsoil (0\uffe2\uff80\uff9330\uffc2\uffa0cm) (11.33\uffc2\uffa0g C m\uffe2\uff80\uff932 yr\uffe2\uff80\uff931) from the 1980s to the 2010s. Total SIC stocks have decreased by \uffe2\uff88\uffbc8.99\uffc2\uffa0\uffc2\uffb1\uffc2\uffa02.24% (1.37\uffc2\uffa0\uffc2\uffb1\uffc2\uffa00.37\uffc2\uffa0Pg C). The average SIC losses across China (0.046 Pg C yr\uffe2\uff80\uff931) and in cropland (0.016 Pg C yr\uffe2\uff80\uff931) account for \uffe2\uff88\uffbc17.6%\uffe2\uff80\uff9324.0% of the terrestrial C sink and 57.1% of the soil organic carbon sink in cropland, respectively. Nitrogen deposition and climate change have profound influences on SIC cycling. We estimate that \uffe2\uff88\uffbc19.12%\uffe2\uff80\uff9319.47% of SIC stocks will be further lost by 2100. The consumption of SIC may offset a large portion of global efforts aimed at ecosystem carbon sequestration, which emphasizes the importance of achieving a better understanding of the indirect coupling mechanisms of nitrogen and carbon cycling and of effective countermeasures to minimize SIC loss.</p", "keywords": ["Carbon sequestration", "Cartography", "China", "Mechanics and Transport in Unsaturated Soils", "Carbonate", "Nitrogen", "Soil Science", "Organic chemistry", "Carbon Dynamics in Peatland Ecosystems", "soil inorganic carbon stocks", "Soil pH", "Environmental science", "Carbon sink", "Agricultural and Biological Sciences", "carbonate", "Engineering", "Soil water", "Soil Carbon Sequestration", "Biology", "global change", "Ecosystem", "Soil acidification", "Civil and Structural Engineering", "Soil science", "2. Zero hunger", "Soil organic matter", "Soil Fertility", "Ecology", "Geography", "Soil Water Retention", "Life Sciences", "Cycling", "Forestry", "Carbon cycle", "04 agricultural and veterinary sciences", "15. Life on land", "Topsoil", "Soil carbon", "Chemistry", "Sink (geography)", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "Physical Sciences", "Environmental chemistry", "0401 agriculture", " forestry", " and fisheries", "soil acidification", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems", "Research Article"]}, "links": [{"href": "https://doi.org/PMC8824702"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/National%20Science%20Review", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "PMC8824702", "name": "item", "description": "PMC8824702", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/PMC8824702"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-07-02T00:00:00Z"}}, {"id": "88c9faca-29cb-4e0a-a75b-60450a4b68fc", "type": "Feature", "geometry": null, "properties": {"updated": "2025-09-02T10:09:13", "type": "Dataset", "language": "de", "title": "INSPIRE Soil / Soil removal (t/ha/a) Water erosion (RxKxS) BB", "description": "Der interoperable INSPIRE-Datensatz beinhaltet Daten vom LBGR \u00fcber den Bodenabtrag (t/ha/a) durch Wassererosion (RxKxS) Brandenburg, transformiert in das INSPIRE-Zielschema Boden. Der Datensatz wird \u00fcber je einen interoperablen Darstellungs- und Downloaddienst bereitgestellt. Im Datensatz Bodenabtrag wird die r\u00e4umliche Verteilung des potenziellen Bodenabtrags durch Wasser auf den landwirtschaftlichen Fl\u00e4chen Brandenburgs dargestellt. Die Bestimmung erfolgte in Anlehnung an DIN19708 (https://dx.doi.org/10.31030/2676773), deren zu Grunde liegende Methode als Allgemeine Bodenabtragsgleichung (ABAG) bezeichnet wird. Der Bodenabtrag wird in einer r\u00e4umlichen Aufl\u00f6sung von 5x5 Meter dargestellt. Der potenzielle Bodenabtrag durch Wasser, der auch als nat\u00fcrlicher Bodenabtrag bezeichnet wird, ergibt sich aus der Kombination des Regenerosivit\u00e4tsfaktors R, des Bodenerodierbarkeitsfaktors K und des Hangneigungsfaktors S. Der Abtrag ist in der Einheit t/ha/a angegeben.     ---      The compliant INSPIRE data set contains data about the soil loss (t/ha/a) by water erosion (RxKxS) Brandenburg from the LBGR, transformed into the INSPIRE annex schema Soil. The data set is provided via compliant view and download services. It shows the spatial distribution of the potential soil loss caused by water on agricultural land in Brandenburg. The determination was based on DIN19708 (https://dx.doi.org/10.31030/2676773), for which the underlying method is referred to as the Allgemeine Bodenabtragsgleichung (ABAG). The soil loss is presented in a spatial resolution of 5x5 meters. The potential soil loss caused by water, which is also known as natural soil loss, results from the combination of the rainfall-runoff erosivity factor R, the soil erodibility factor K and the slope steepness factor S. The soil loss is specified in the unit t/ha/a.", "formats": [{"name": "WCS_SRVC"}], "keywords": ["High value dataset", "boden", "bodenerosion", "bodenerosionsgefa\u0308hrdung", "bodenerosionsgefa\u0308hrdung-durch-wasser-in-brandenburg", "bodenkunde", "brandenburg", "de", "erdbeobachtung-und-umwelt", "erosion", "erosionsgefa\u0308hrdung", "gefa\u0308hrdungsstufen", "geologie", "inspireidentifiziert", "interoperabel", "interoperability", "interoperable-daten", "opendata", "process", "regional", "soil", "soillayer", "wassererosion", "water-erosion", "watererosionrisktopsoil"], "contacts": [{"organization": "Landesamt f\u00fcr Bergbau, Geologie und Rohstoffe Brandenburg (LBGR)", "roles": ["creator"]}]}, "links": [{"href": "https://inspire.brandenburg.de/services/boerosion_wms?REQUEST=GetCapabilities&SERVICE=WMS"}, {"href": "https://inspire.brandenburg.de/services/so_boerosion_wcs?REQUEST=GetCapabilities&SERVICE=WCS"}, {"href": "https://inspire.brandenburg.de/services/so_boerosion_wms?REQUEST=GetCapabilities&SERVICE=WMS"}, {"href": "http://data.europa.eu/88u/dataset/88c9faca-29cb-4e0a-a75b-60450a4b68fc~~2"}, {"rel": "self", "type": "application/geo+json", "title": "88c9faca-29cb-4e0a-a75b-60450a4b68fc", "name": "item", "description": "88c9faca-29cb-4e0a-a75b-60450a4b68fc", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/88c9faca-29cb-4e0a-a75b-60450a4b68fc"}, {"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": "50|od______2659::694ff7c599ecdc11f0dd8cd4c4d84634", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:26:35Z", "type": "Dataset", "title": "SERENA EJPSOIL IT TUS SOC Loss SOC", "description": "The internal EJP SOIL project SERENA contributed to the evaluation of soil multifunctionality aiming at providing assessment tools for land planning and soil policies at different scales. By co-working with relevant stakeholders, the project provided co-developed indicators and associated cookbooks to assess and map them, to report both on soil degradation, soil-based ecosystem services and their bundles, under actual conditions and for climate and land-use changes, at the regional, national, and European scales.  The map is the result of applying the SOC loss cookbook developed in SERENA/EJP-Soil. It is based on Tuscany Region SOCdatabase (Gardin et al., 2021). Not freely available (Lamma Consortium). More information and requests to: info@lamma.toscana.it.  Three versions of the map were produced.  In versions v1 and v2, the dataset corresponds to a map of SOC concentrations for the Tuscany Region produced using a geostatistical approach. Ordinary kriging (Chil\u00e8s & Delfiner, 2012) coupled with local geostatistics (LGS) was used to map SOC concentration (%) in the topsoil (0-30 cm) at a regional scale in the Tuscany Region (Italy). The map has a 50 m spatial resolution.  In version v3, a different approach to applying SOC loss cookbook was used. Particularly, Random Forest regression algorithm with numerous spatial covariates was applied for mapping SOC content (%) in the topsoil (0-30 cm) at regional scale in Tuscany Region (Italy). \u00a0The map has a 100 m spatial resolution.", "keywords": ["EJP Soil", "Random Forest", "Italy", "Tuscany", "Soil Organic Carbon (SOC)", "SOC loss", "Topsoil", "SERENA", "Grant n 862695", "Digital Soil Mapping"], "contacts": [{"organization": "Buttafuoco, Gabriele, Gardin, Lorenzo, Lorenzetti, Romina, Medina-Rold\u00e1n, Eduardo, Ungaro, Fabrizio,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/50|od______2659::694ff7c599ecdc11f0dd8cd4c4d84634"}, {"rel": "self", "type": "application/geo+json", "title": "50|od______2659::694ff7c599ecdc11f0dd8cd4c4d84634", "name": "item", "description": "50|od______2659::694ff7c599ecdc11f0dd8cd4c4d84634", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/50|od______2659::694ff7c599ecdc11f0dd8cd4c4d84634"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-10-31T00:00:00Z"}}, {"id": "7520bfe1-d548-4ffb-bdd8-18cc534df855", "type": "Feature", "geometry": null, "properties": {"updated": "2024-09-25T14:47:06", "type": "Dataset", "language": "en", "title": "Tellus Geochemistry \u2014 topsoil", "description": "The latest topsoils data from the Tellus project, managed by the Geological Survey Ireland.  The topsoil (c.5\u201320 cm deep) samples were analysed for: Analytical Method: ICP(-OES/-MS) following aqua regia digestion; soil loss-on-ignition at 450\u00a0\u00b0C The survey was conducted on foot; samples were collected approx. every 4 sq km from. For more information please visit tellus.ie.  The following elements were analysed: Aluminium, Antimony, Arsenic, Barium, Beryllium, Bismuth, Cadmium, caesium, Calcium, Cerium, Chromium, Cobalt, Copper, Gallium, Germanium, Hafnium, indium, Iron, Lanthanum, Lead, Lithium, Loss-on-ignition, Lutetium, Magnesium, Manganese, Mercury, Molybdenum, Nickel, Niobium, pH, Phosphorus, Potassium, Rubidium, scandium, Selenium, Silver, Sodium, Strontium, Sulphur, Tantalum, Tellurium, Terbium, Thallium, Thorium, Tin, Titanium, Tungsten, Uranium, vanadium, Ytterbium, Yttrium, Zinc, Zinc, Zirconium (Al, B, Ba, Ca, Cr, Cu, Fe, K, Li, Mg, Mn, Na, Ni, P, S, S, Sr, Ti, V, Zn, Zr, Ag, Be, Be, Bi, Cd, Ce, Co, Cs, Ga, Ge, Hf, In, La, Lu, P, Mo, Mo, Pb, Rb, Sb, Sb, Sb, Sn, Sn, Tb, Te, Th, Tl, U, W, Yb) The current coverage includes:  Tellus Border survey block (2011-2013, Co Donegal, Sligo, Leitrim, Cavan, Monaghan, Louth)  Some elements have been merged with topsoil data from Northern Ireland conducted in the mid ninties and Noughties.", "formats": [{"name": "ESRI REST"}], "keywords": ["aintrim", "aluminium", "antimony", "aqua-regia", "aqua-regia-digestion", "armagh", "arsenic", "barium", "beryllium", "bismuth", "cadmium", "caesium", "calcium", "cavan", "cerium", "chemistry", "chromium", "cobalt", "copper", "derry", "donegal", "down", "dublin", "earth-science", "environment", "european-union", "fermanagh", "gallium", "galway", "geochemical", "geochemical-survey", "geochemistry", "geological", "geological-survey-ireland", "geology", "geoscientificinformation", "germanium", "hafnium", "icp-ms", "icp-oes", "icpms", "icpoes", "ie", "indium", "interreg", "ireland", "iron", "kildare", "lanthanum", "lead", "lietrim", "lithium", "lithology", "lithosphere", "londonderry", "longford", "loss-on-ignition", "louth", "lutetium", "magnesium", "manganese", "mayo", "meath", "mercury", "molybdenum", "monaghan", "nickel", "niobium", "offaly", "organics", "phosphorus", "potassium", "rocks", "roscommon", "rubidium", "scandium", "selenium", "silver", "sligo", "sodium", "soil", "soil-loss-on-ignition", "soil-ph", "strontium", "sulphur", "tantalum", "tellurium", "tellus", "tellus-border", "terbium", "thallium", "thorium", "tin", "titanium", "top-soil", "topsoil", "tungsten", "tyrone", "uranium", "vanadium", "westmeath", "wicklow", "ytterbium", "yttrium", "zinc", "zirconium"], "contacts": [{"organization": "https://data.gov.ie/organization/geological-survey-of-ireland", "roles": ["publisher"]}]}, "links": [{"href": "http://dcenr.maps.arcgis.com/apps/MapSeries/index.html?appid=6304e122b733498b99642707ff72f754"}, {"href": "https://gsi.geodata.gov.ie/server/rest/services/Geochemistry"}, {"href": "https://secure.dccae.gov.ie/GSI_DOWNLOAD/Tellus/PDFs/EBook_Topsoils_Final_03Feb2016.pdf"}, {"href": "https://www.gsi.ie/en-ie/data-and-maps/Pages/Geochemistry.aspx#DeeperTopsoilS"}, {"href": "https://www.gsi.ie/en-ie/data-and-maps/Pages/Geochemistry.aspx#ShallowTopsoilA"}, {"href": "https://www.gsi.ie/en-ie/programmes-and-projects/tellus/activities/ground-survey/Pages/default.aspx"}, {"href": "http://data.europa.eu/88u/dataset/7520bfe1-d548-4ffb-bdd8-18cc534df855"}, {"rel": "self", "type": "application/geo+json", "title": "7520bfe1-d548-4ffb-bdd8-18cc534df855", "name": "item", "description": "7520bfe1-d548-4ffb-bdd8-18cc534df855", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/7520bfe1-d548-4ffb-bdd8-18cc534df855"}, {"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": "76a352b3-f223-4b29-88d2-7bd9cbe83c3a", "type": "Feature", "geometry": null, "properties": {"updated": "2025-09-02T09:54:12", "type": "Dataset", "language": "de", "title": "INSPIRE-WFS Soil / Relative Bindungsst\u00e4rke f\u00fcr Schwermetalle im Oberboden BB", "description": "Der interoperable INSPIRE-WFS ist ein Downloaddienst, der Daten im Annex-Schema Boden (abgeleitet aus dem origin\u00e4ren Datensatz: Relative Bindungsst\u00e4rke f\u00fcr Schwermetalle im Oberboden Brandenburg) bereitstellt. Er gibt einen \u00dcberblick \u00fcber die relative Bindungsst\u00e4rke f\u00fcr Schwermetalle im Oberboden in Brandenburg. Die Karte basiert auf den Legendeneinheiten der Boden\u00fcbersichtskarte (B\u00dcK300) mit entsprechender Zuordnung von parametrisierten Fl\u00e4chenbodenformen, die durch Gel\u00e4nde- und Laboruntersuchungen bestimmt wurden. Dazu wurden f\u00fcr gleiche Horizont-Substrat-Kombinationen die entsprechenden Parameter statistisch abgeleitet. Die Abfolge von Horizont-Substrat-Kombinationen in den Fl\u00e4chenbodenformen mit ihren Parametern bildeten die Grundlage f\u00fcr die Berechnung der relativen Bindungsst\u00e4rke gegen\u00fcber Schwermetallen (s. Methodendokumentation Bodenkunde,  Hennings 2000, Verkn\u00fcpfungsregel 7.1 bis 7.3). Gem\u00e4\u00df der INSPIRE-Datenspezifikation Soil (D2.8.III.3_v3.0) liegen die Inhalte der Karte INSPIRE-konform vor. Der WFS beinhaltet die folgenden FeatureTypes:     - Beobachtungsprozess (ompr:Process) mit Angaben zu der am Prozess beteiligten Organisation LBGR,     - abgeleitetes Bodenobjekt (so:SoilDerivedObject) mit Angaben zur Beobachtung der Bodeneigenschaft zur Beschreibung des abgeleiteten Bodenobjekts,     - Beobachtung einer Bodeneigenschaft (om:OM_Observation) mit Angaben zum Charakter des vom Boden abgeleiteten Objekts, der beobachtete Eigenschaft (observedProperty), der vom Boden abgeleiteten Beobachtung bodenbezogene Eigenschaften, dem Ergebnis der Beobachtungen des abgeleiteten Bodenobjekts,      - Bodenk\u00f6rper (so:SoilBody), abgegrenzter und hinsichtlich bestimmter Bodeneigenschaften und/oder r\u00e4umlicher Muster homogener Teil der Bodendecke, und     - Bodenschicht (so:SoilLayer) mit Angaben zur Zuordnung der Schicht zu einem ihrer Art entsprechenden Begriff, zum abgeleiteten Profil (DerivedSoilProfile), das als Referenzprofil f\u00fcr eine bestimmte Art von Boden in einem bestimmten geografischen Gebiet dient, der oberen und unteren Tiefe des Profilelements, gemessen von der Oberfl\u00e4che (0 cm) eines Bodenprofils (in cm).     ---      The compliant INSPIRE-WFS Soil / Relative Bindungsst\u00e4rke f\u00fcr Schwermetalle im Oberboden Brandenburg is a download service that delivers data in the annex schema Soil (derived from the original data set: Relative sorption strength for heavy metals in the top soil Brandenburg). It provides an overview of the relative sorption strength for heavy metals in the top soil in Brandenburg. The map is based on the legend units of the soil map (B\u00dcK300) with corresponding assignment of parameterized soil forms determined by field and laboratory investigations. For this purpose, the corresponding parameters were statistically derived for the same horizon-substrate combinations. The sequence of horizon-substrate combinations in the soil forms with their parameters formed the basis for the calculation of the relative sorption strength for heavy metals (see Methodendokumentation Bodenkunde, Hennings 2000, methods 7.1 to 7.3). The content of the soil map is compliant to the INSPIRE data specification for the annex theme Soil (D2.8.III.3_v3.0). The WFS includes the following feature types:     - Observation process (ompr:Process) with information about the organization LBGR involved in the process,     - Soil derived object (so:SoilDerivedObject) with information on the observation of the soil property for characterizing the soil derived object,     - Observations of a soil derived object (om:OM_Observation) with information about the character of the soil derived object, the observed property, the soil derived observation of soil related properties, the result of the observations of the soil derived object,      - Soil body (so:SoilBody), part of the soil cover that is delineated and that is homogeneous with regard to certain soil properties and/or spatial patterns, and     - Soil layer (so:SoilLayer) with information about the assignation of the layer according to the concept that fits its kind, to the derived soil profile (DerivedSoilProfile), which serves as a reference profile for a particular type of soil in a specific geographical area, including the upper and lower depth of the profile element from the surface (0 cm) of a soil profile (in cm).", "formats": [{"name": "HTML"}], "keywords": ["adsorptionsvermo\u0308gen", "bboxbebb", "boden", "bodenkunde", "bodenschutz", "brandenburg", "de", "depthinterval", "derivedsoilprofile", "geologie", "infofeatureaccessservice", "inspireidentifiziert", "interoperabel", "interoperability", "oberboden", "om_observation", "opendata", "ph-wert", "process", "relative-bindungssta\u0308rke-fu\u0308r-schwermetalle", "schwermetall", "soil", "soilbody", "soilderivedobject", "soillayer", "sorption-strength-for-heavy-metals", "sorptionstrengthheavymetals", "topsoil", "wfs"], "contacts": [{"organization": "Landesamt f\u00fcr Bergbau, Geologie und Rohstoffe Brandenburg (LBGR)", "roles": ["creator"]}]}, "links": [{"href": "https://geoportal.brandenburg.de/detailansichtdienst/render?view=gdibb&url=https%3A%2F%2Fgeoportal.brandenburg.de%2Fgs-json%2Fxml%3Ffileid%3D76a352b3-f223-4b29-88d2-7bd9cbe83c3a"}, {"href": "https://inspire.brandenburg.de/services/so_boschwermoben_wfs?REQUEST=GetCapabilities&SERVICE=WFS"}, {"href": "https://isk.geobasis-bb.de/geodienste/Sonstiges/Hilfe_Nutzung_Downloaddienst.pdf"}, {"href": "http://data.europa.eu/88u/dataset/76a352b3-f223-4b29-88d2-7bd9cbe83c3a~~1"}, {"rel": "self", "type": "application/geo+json", "title": "76a352b3-f223-4b29-88d2-7bd9cbe83c3a", "name": "item", "description": "76a352b3-f223-4b29-88d2-7bd9cbe83c3a", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/76a352b3-f223-4b29-88d2-7bd9cbe83c3a"}, {"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": "811a7ed5-16fc-4594-9d83-8c00c6a02d02", "type": "Feature", "geometry": null, "properties": {"updated": "2025-09-02T09:55:59Z", "type": "Dataset", "language": "de", "title": "INSPIRE-WFS Soil / Potenzielle Verdichtungsempfindlichkeit BB", "description": "Der interoperable INSPIRE-WFS ist ein Downloaddienst, der Daten im Annex-Schema Boden (abgeleitet aus dem origin\u00e4ren Datensatz: Potenzielle Verdichtungsempfindlichkeit Brandenburg in 35 cm Bezugstiefe) bereitstellt. Er gibt einen \u00dcberblick \u00fcber die potenzielle Verdichtungsempfindlichkeit des Bodens in 35 cm Bezugstiefe im Land Brandenburg. Die Karte basiert auf den Legendeneinheiten der Boden\u00fcbersichtskarte (B\u00dcK300). Diese stellen Bodenformengesellschaften dar. Die einzelnen Fl\u00e4chenbodenformen (FBF) wurden mit bodenphysikalischen Kennwerten belegt, die durch Gel\u00e4nde-und Laboruntersuchungen bestimmt wurden. Auf Basis dieser Bodenkennwerte wurde die Verdichtungsempfindlichkeit des Bodens abgeleitet. Diese klassifiziert das Erstverdichtungsverhalten (im Sinne einer Verdichtungsintensit\u00e4t) eines nat\u00fcrlich gelagerten, abgesetzten Unterbodens auf Grund seiner physikalischen und hydrologischen Eigenschaften. Weiterf\u00fchrende Informationen sind hier zu finden: http://www.geo.brandenburg.de/ows/htdocs/21042020_Verdichtung.pdf. Gem\u00e4\u00df der INSPIRE-Datenspezifikation Soil (D2.8.III.3_v3.0) liegen die Inhalte der Boden\u00fcbersichtskarte INSPIRE-konform vor. Der WFS beinhaltet die folgenden FeatureTypes:      - Beobachtungsprozess (ompr:Process) mit Angaben zu der am Prozess beteiligten Organisation LBGR,      - abgeleitetes Bodenobjekt (so:SoilDerivedObject) mit Angaben zur Beobachtung der Bodeneigenschaft zur Beschreibung des abgeleiteten Bodenobjekts,     - Beobachtung einer Bodeneigenschaft (so:OM_Observation) mit Angaben zum Charakter des vom Boden abgeleiteten Objekts, der beobachtete Eigenschaft, der vom Boden abgeleiteten Beobachtung bodenbezogene Eigenschaften, dem Ergebnis der Beobachtungen des abgeleiteten Bodenobjekts,     - Bodenk\u00f6rper (so:SoilBody), abgegrenzter und hinsichtlich bestimmter Bodeneigenschaften und/oder r\u00e4umlicher Muster homogener Teil der Bodendecke, und     - Bodenschicht (so:SoilLayer) mit Angaben zur Zuordnung der Schicht zu einem ihrer Art entsprechenden Begriff (LayerTypeValue: topsoil), zum abgeleiteten Profil, das als Referenzprofil f\u00fcr eine bestimmte Art von Boden in einem bestimmten geografischen Gebiet dient, der oberen und unteren Tiefe des Profilelements, gemessen von der Oberfl\u00e4che (0 cm) eines Bodenprofils (in cm).     ---      The compliant INSPIRE-WFS Soil / Potenzielle Verdichtungsempfindlichkeit Brandenburg is a download service that delivers data in the annex schema Soil (derived from the original data set: Potential compaction sensitivity Brandenburg at 35 cm reference depth). It provides an overview of the potential compaction sensitivity of the soil at a reference depth of 35 cm in the state of Brandenburg. The map is based on the legend units of the soil survey map (B\u00dcK300). Based on the soil properties of the legend units and the corresponding soil forms, the compaction sensitivity of the soil was derived. This classifies the initial compaction behavior (in terms of compaction intensity) of a naturally layered, settled subsoil based on its physical and hydrological properties. Further information can be found here: http://www.geo.brandenburg.de/ows/htdocs/21042020_Verdichtung.pdf. The content of the soil map is compliant to the INSPIRE data specification for the annex theme Soil (D2.8.III.3_v3.0). The WFS includes the following feature types:      - Observation process (ompr:Process) with information about the organization LBGR involved in the process,     - Soil derived object (so:SoilDerivedObject) with information on the observation of the soil property for characterizing the soil derived object,     - Observations of a soil derived object (om:OM_Observation) with information about the character of the soil derived object, the observed property, the soil derived observation of soil related properties, the result of the observations of the soil derived object,     - Soil body (so:SoilBody), part of the soil cover that is delineated and that is homogeneous with regard to certain soil properties and/or spatial patterns, and     - Soil layer (so:SoilLayer) with information about the assignation of the layer according to the concept that fits its kind (LayerTypeValue: topsoil), to the derived soil profile, which serves as a reference profile for a particular type of soil in a specific geographical area, including the upper and lower depth of the profile element from the surface (0 cm) of a soil profile (in cm).", "formats": [{"name": "HTML"}], "keywords": ["bboxbebb", "boden", "bodenkunde", "bodenschutz", "brandenburg", "compactionsensitivity", "de", "derivedsoilprofile", "geologie", "infofeatureaccessservice", "inspireidentifiziert", "interoperabel", "interoperability", "oberboden", "om_observation", "opendata", "process", "sedimentarymaterial", "soil", "soilbody", "soilderivedobject", "soillayer", "topsoil", "verdichtungsempfindlichkeit", "wfs"], "contacts": [{"organization": "Landesamt f\u00fcr Bergbau, Geologie und Rohstoffe Brandenburg (LBGR)", "roles": ["creator"]}]}, "links": [{"href": "https://geoportal.brandenburg.de/detailansichtdienst/render?view=gdibb&url=https%3A%2F%2Fgeoportal.brandenburg.de%2Fgs-json%2Fxml%3Ffileid%3D811a7ed5-16fc-4594-9d83-8c00c6a02d02"}, {"href": "https://inspire.brandenburg.de/services/so_verdicht_wfs?REQUEST=GetCapabilities&SERVICE=WFS"}, {"href": "https://isk.geobasis-bb.de/geodienste/Sonstiges/Hilfe_Nutzung_Downloaddienst.pdf"}, {"href": "http://data.europa.eu/88u/dataset/811a7ed5-16fc-4594-9d83-8c00c6a02d02~~1"}, {"rel": "self", "type": "application/geo+json", "title": "811a7ed5-16fc-4594-9d83-8c00c6a02d02", "name": "item", "description": "811a7ed5-16fc-4594-9d83-8c00c6a02d02", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/811a7ed5-16fc-4594-9d83-8c00c6a02d02"}, {"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": "8383d16e-dd8c-4872-bcbf-f31c9ca24f42", "type": "Feature", "geometry": null, "properties": {"updated": "2025-09-02T09:55:49", "type": "Dataset", "language": "de", "title": "INSPIRE-WFS Soil / Mittlere Elementgehalte im Oberboden BB", "description": "Der interoperable INSPIRE-WFS ist ein Downloaddienst, der Daten im Annex-Schema Boden (abgeleitet aus dem origin\u00e4ren Datensatz: Mittlere Elementgehalte im Oberboden Brandenburg) bereitstellt. Er gibt einen \u00dcberblick \u00fcber die mittleren Gehalte ausgew\u00e4hlter, umweltrelevanter Elemente im Oberboden (0 - 30 cm) im Land Brandenburg. Die Gehaltsklassen der jeweils f\u00fcr den Oberboden einheitlichen Kartenlegenden richten sich nach der Spannweite s\u00e4mtlicher Werte f\u00fcr das betreffende Element. Gem\u00e4\u00df der INSPIRE-Datenspezifikation Soil (D2.8.III.3_v3.0) liegen die Inhalte der Boden\u00fcbersichtskarte INSPIRE-konform vor. Der WFS beinhaltet die folgenden FeatureTypes:      - Beobachtungsprozess (ompr:Process) mit Angaben zu der am Prozess beteiligten Organisation LBGR,      - abgeleitetes Bodenobjekt (so:SoilDerivedObject) mit Angaben zur Beobachtung der Bodeneigenschaft zur Beschreibung des abgeleiteten Bodenobjekts,     - Beobachtung einer Bodeneigenschaft (om:OM_Observation) mit Angaben zum Charakter des vom Boden abgeleiteten Objekts, der beobachtete Eigenschaft, der vom Boden abgeleiteten Beobachtung bodenbezogene Eigenschaften, dem Ergebnis der Beobachtungen des abgeleiteten Bodenobjekts,     - Bodenk\u00f6rper (so:SoilBody), abgegrenzter und hinsichtlich bestimmter Bodeneigenschaften und/oder r\u00e4umlicher Muster homogener Teil der Bodendecke, und     - Bodenschicht (so:SoilLayer) mit Angaben zur Zuordnung der Schicht zu einem ihrer Art entsprechenden Begriff (LayerTypeValue: topsoil), zum abgeleiteten Profil, das als Referenzprofil f\u00fcr eine bestimmte Art von Boden in einem bestimmten geografischen Gebiet dient, der oberen und unteren Tiefe des Profilelements, gemessen von der Oberfl\u00e4che (0 cm) eines Bodenprofils (in cm).     ---      The compliant INSPIRE-WFS Soil / Mittlere Elementgehalte im Oberboden Brandenburg is a download service that delivers data in the annex schema Soil (derived from the original data set: Average element contents in topsoil Brandenburg). It provides an overview of the mean contents of selected environmentally relevant elements in the topsoil (0 - 30 cm) in the state of Brandenburg. The content classes of the map legends, which are uniform for the topsoil in each case, are based on the range of all values for the relevant element. The content of the soil map is compliant to the INSPIRE data specification for the annex theme Soil (D2.8.III.3_v3.0). The WFS includes the following feature types:      - Observation process (ompr:Process) with information about the organization LBGR involved in the process,     - Soil derived object (so:SoilDerivedObject) with information on the observation of the soil property for characterizing the soil derived object,     - Observations of a soil derived object (om:OM_Observation) with information about the character of the soil derived object, the observed property, the soil derived observation of soil related properties, the result of the observations of the soil derived object,     - Soil body (so:SoilBody), part of the soil cover that is delineated and that is homogeneous with regard to certain soil properties and/or spatial patterns, and     - Soil layer (so:SoilLayer) with information about the assignation of the layer according to the concept that fits its kind (LayerTypeValue: topsoil), to the derived soil profile, which serves as a reference profile for a particular type of soil in a specific geographical area, including the upper and lower depth of the profile element from the surface (0 cm) of a soil profile (in cm).", "formats": [{"name": "HTML"}], "keywords": ["bboxbebb", "boden", "bodenkunde", "bodenschutz", "brandenburg", "de", "derivedsoilprofile", "geologie", "infofeatureaccessservice", "inspireidentifiziert", "interoperabel", "interoperability", "mittlere-elementgehalte-im-oberboden", "oberboden", "om_observation", "opendata", "process", "soil", "soilbody", "soilderivedobject", "soillayer", "topsoil", "wfs"], "contacts": [{"organization": "Landesamt f\u00fcr Bergbau, Geologie und Rohstoffe Brandenburg (LBGR)", "roles": ["creator"]}]}, "links": [{"href": "https://geoportal.brandenburg.de/detailansichtdienst/render?view=gdibb&url=https%3A%2F%2Fgeoportal.brandenburg.de%2Fgs-json%2Fxml%3Ffileid%3D8383d16e-dd8c-4872-bcbf-f31c9ca24f42"}, {"href": "https://inspire.brandenburg.de/services/so_elementoben_wfs?REQUEST=GetCapabilities&SERVICE=WFS"}, {"href": "https://isk.geobasis-bb.de/geodienste/Sonstiges/Hilfe_Nutzung_Downloaddienst.pdf"}, {"href": "http://data.europa.eu/88u/dataset/8383d16e-dd8c-4872-bcbf-f31c9ca24f42~~1"}, {"rel": "self", "type": "application/geo+json", "title": "8383d16e-dd8c-4872-bcbf-f31c9ca24f42", "name": "item", "description": "8383d16e-dd8c-4872-bcbf-f31c9ca24f42", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/8383d16e-dd8c-4872-bcbf-f31c9ca24f42"}, {"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": "9c4d0d64-3ddd-419d-a002-5a725b778274-envidat", "type": "Feature", "geometry": null, "properties": {"updated": "2021-10-20T11:24:57Z", "type": "Dataset", "language": "en", "title": "Long-term recovery of above-and belowground interactions in restored grasslands", "description": "This dataset contains all data, on which the following publication below is based.  Paper Citation:  _Resch, M.C., Sch\u00fctz, M., Ochoa-Hueso, R., Buchmann, N., Frey, B., Graf, U., van der Putten, W.H., Zimmermann, S., Risch, A.C. (in review). Long-term recovery of above- and belowground interactions in restored grassland after topsoil removal and seed addition. Journal of Applied Ecology_  Please cite this paper together with the citation for the datafile.  Study area and experimental design The study was conducted in and around two nature reserves, Eigental and Altl\u00e4ufe der Glatt, which were located approximately 5 km apart (47\u00b027\u00b4 to 47\u00b029\u00b4 N, 8\u00b037\u00b4 to 8\u00b032\u00b4 E, 417 to 572 m a.s.l., Canton of Zurich, Switzerland; Figure S1 and S2, Table S1). Mean annual temperature and precipitation are 9.8 \u00b1 0.6 \u00b0C and 990 \u00b1 168 mm (Kloten climate station 1988-2018; MeteoSchweiz, 2019). TFor this study, we used a space-for-time approach based on eight restoration sites that were between 3 and 32 years old. We measured recovery and restoration success by comparing the restored grasslands with intensively managed and semi-natural grasslands. Using a space-for-time approach requires high similarities in historical properties of the site, such as soil conditions and management regimes, to assure that temporal processes are appropriately represented by spatial patterns (Walker et al., 2010). This was the case in our study. The restored sites had similar soil conditions (i.e., soil type, structure, water availability) as the targeted semi-natural grasslands, while they shared the same agricultural legacy with intensively managed grasslands, i.e., biomass harvest and fertilization (manure and/or slurry) three to five times a year as well as tillage. We randomly established three 5 m x 5 m (25-m2) plots for plant identification and three 2 m x 2 m (4-m2) subplots for soil biotic and abiotic data collection at least 2 m away from the 25-m2 plots in each restoration site. Sites of similar age were grouped into four age classes: Y.4 (3 & 4 years after restoration), Y.18 (17 & 19 years), Y.24 (23 & 25 years), and Y.30 (27 & 32 years). Six intensively managed (Initial) and six semi-natural grassland (Target) sites complemented the experimental set-up, for a total of 36 plots. All plots were sampled under similar conditions, i.e., day of the year, air temperature, soil moisture, and time since last rain event, in June/July 2017 (intensively managed and semi-natural plots) and 2018 (restored plots).  Collection of plants and selected soil biota data Plant species cover (in %) was visually estimated in each 25-m2 plot in mid-June (Braun-Blanquet, 1964; nomenclature: Lauber & Wagner, 1996). We calculated Shannon diversity and assessed plant community structure. We included soil microbial (fungi, procaryotes) and nematodes in our study as they represent the majority of soil biotic diversity and abundance (Bardgett & van der Putten, 2014), cover various trophic levels of the soil food web (Bongers & Ferris, 1999), and play key roles in soil functioning and ecosystem processes (Bardgett & van der Putten, 2014). In particular, soil nematodes were found to be well suited belowground indicators to evaluate recovery/development after restoration (e.g. Frouz, et al. 2008; Kardol et al., 2009; Resch et al., 2019). We randomly collected ten soil cores (2.2 cm diameter x 12 cm depths; sampler from Giddings Machine Company, Windsor, USA) in the 4-m2 subplots to assess soil nematode and microbial (fungal, prokaryotic) diversities and community structures. For soil nematodes, eight of the soil cores were combined and gently homogenized, placed in coolers and stored at 4 \u00b0C and transported to the laboratory (Netherlands Institute of Ecology, NIOO, Wageningen, Netherlands) within three days after collection. Free-living nematodes were extracted from 200 g of fresh soil using Oostenbrink elutriators (Oostenbrink, 1960). After extraction, each sample was divided into three subsamples, two for molecular identification and one to determine nematode abundance (see Resch et al., 2019). For the molecular work, two subsamples were stored in 70% ethanol (final volume 10 mL each) and transported to the laboratory at the Swiss Federal Research Institute WSL (Birmensdorf, Switzerland). Each subsample was reduced to roughly 200 \u03bcL by centrifugation and removal of the supernatant. The remaining ethanol was vaporized (65 \u00b0C for 3 h). Thereafter, 180 \u03bcL ATL buffer solution (Qiagen, Hilden, Germany) was immediately added and samples were stored at 4 \u00b0C until further processing. From these samples, nematode metagenomic DNA was extracted using the DNeasy Blood & Tissue Kit (Qiagen, Hilden, Germany) according to the manufacturer`s protocol, except for the incubation step which was run at 56 \u00b0C for 4 h. PCR amplification of the V6-V8 region of the eukaryotic small-subunit (18S) was performed with 7.5 \u03bcL of genomic DNA template (ca. 1 ng/\u03bcL) in 25 \u03bcL reactions containing 5 \u03bcL PCR reaction buffer, 2.5 mM MgCL2, 0.2 mM dNTPs, 0.8 \u03bcM of each primer (NemF: Sapkota & Nicolaisen, 2015; 18Sr2b: Porazinska et al., 2009), 0.5 \u03bcL BSA, and 0.25 \u03bcL GoTaq G2 Hot Start Polymerase (Promega Corporation, Madison, USA). Amplification was using an initial DNA denaturation step of 95 \u00b0C for 2 min, followed by 35 cycles at 94 \u00b0C for 40 sec, 58 \u00b0C for 40 sec, 72 \u00b0C for 1 min, and a final elongation step at 72 \u00b0C for 10 min. Filtering, dereplication, sample inference, chimera identification, and merging of paired-end reads was implemented using the DADA2 pipeline (v.1.12; Callahan et al., 2016) to finally assign amplicon sequence variants (ASVs) as taxonomic units. We combined and homogenized the remaining two soil cores to assess soil microbes, placed them in coolers (4 \u00b0C) and transported them to the laboratory at WSL. Metagenomic DNA was extracted from 8 g sieved soil (2 mm) using the DNAeasy PowerMax Soil Kit (Qiagen, Hilden, Germany) according to the manufacturer\u00b4s protocol. PCR amplification of the V3-V4 region of the small-subunit (16S) of prokaryotes (i.e., bacteria and archaea) and the ribosomal internal transcribed spacer region (ITS2) of fungi was performed with 1 ng of template DNA using PCR primers and conditions as previously described (Frey et al., 2016). PCRs were run in triplicates, pooled and sent to the Genome Quebec Innovation Centre (Montreal, QC, Canada) for barcoding using the Fluidigm Access Array technology (Fluidigm) and paired-end sequencing on the Illumina MiSeq v3 platform (Illumina Inc., San Diego, USA). Quality filtering, clustering into operational taxonomic units (OTUs, 97% similarity cutoffs) and taxonomic assignment were performed as previously described (Resch et al., 2021).Taxonomic classification of nematode, prokaryotic and fungal sequences was conducted querying against the most recent versions of PR2 (v.4.11.1; Guillou et al., 2013), SILVA (v.132; Quast et al., 2013), and UNITE (v.8; Nilsson et al., 2019) reference sequence databases. Taxonomic assignment cutoffs were set to confidence rankings \u2265 0.8 (below ranked as unclassified). Prokaryotic OTUs assigned to mitochondria or chloroplasts as well as OTUs or ASVs assigned to other than Fungi or Nematoda were manually removed prior to data analysis. The three datasets were filtered to discard singletons and doubletons. Taxonomic abundance matrices were rarefied to the lowest number of sequences per community to achieve parity of the total number of reads between samples (Prokaryotes: 10,929 reads; Fungi: 18,337 reads; Nematodes: 6,662 reads). We calculated Shannon diversity and assessed community structures for soil nematodes, prokaryotes and fungi based on their relative abundances of ASV or OTU at the taxon level.  Collection of soil physical and chemical properties We randomly collected one undisturbed soil core (5 cm diameter, 12 cm depth) per 4-m2 subplot using a steel cylinder that fit into the soil corer. The cylinders were capped to avoid disturbance during transport and used to measure field capacity, rock content and fine earth density as previously described (Resch et al., 2021). We randomly collected another three soil cores (5 cm diameter, 12 cm depths) in each 4-m2 subplot to determine soil chemical properties. The cores were pooled, dried at 60 \u00b0C for 48 h and passed through a 2 mm sieve. We measured soil pH (CaCl2) on dried samples, total nitrogen (N) and organic carbon (C) concentration on dried and fine-ground samples (\u2264 0.5 mm; for details see Resch et al., 2021). We calculated total N and organic C pools after correcting its concentration for soil depth, rock content and fine earth density.", "formats": [{"name": "XLS"}], "keywords": ["bacteria", "biodiversity", "ch", "fungi", "grassland", "nematodes", "plants", "restoration", "soil", "soil-biodiversity", "soil-biology", "soil-chemistry", "topsoil-removal"], "contacts": [{"organization": "Anita C. Risch", "roles": ["creator"]}, {"organization": "https://envidat.ch/#/about", "roles": ["publisher"]}]}, "links": [{"href": "https://www.envidat.ch/#/metadata/long-term-recovery-of-above-and-belowground-interactions-in-restored-grasslands"}, {"href": "https://www.envidat.ch/dataset/long-term-recovery-of-above-and-belowground-interactions-in-restored-grasslands/resource/046d129c-3bc2-4214-8d9c-ffbf8659b245"}, {"href": "https://www.envidat.ch/dataset/long-term-recovery-of-above-and-belowground-interactions-in-restored-grasslands/resource/143c6e0e-1aa5-4510-b333-9c00e99c59fd"}, {"href": "https://www.envidat.ch/dataset/long-term-recovery-of-above-and-belowground-interactions-in-restored-grasslands/resource/3f35aa3b-5f64-4d55-907f-ac6c1f2d490c"}, {"href": "https://www.envidat.ch/dataset/long-term-recovery-of-above-and-belowground-interactions-in-restored-grasslands/resource/3f820b86-ee6b-4466-bc40-4346eac4cbcd"}, {"href": "https://www.envidat.ch/dataset/long-term-recovery-of-above-and-belowground-interactions-in-restored-grasslands/resource/64d9bac3-d7ce-4ae9-8922-f0ee496292a9"}, {"href": "https://www.envidat.ch/dataset/long-term-recovery-of-above-and-belowground-interactions-in-restored-grasslands/resource/9940b2c1-35a6-46e8-9604-4fb866f1ddd4"}, {"href": "https://www.envidat.ch/dataset/long-term-recovery-of-above-and-belowground-interactions-in-restored-grasslands/resource/ed2658c5-c2c2-4b13-b29a-187f199f9f47"}, {"href": "http://data.europa.eu/88u/dataset/9c4d0d64-3ddd-419d-a002-5a725b778274-envidat"}, {"rel": "self", "type": "application/geo+json", "title": "9c4d0d64-3ddd-419d-a002-5a725b778274-envidat", "name": "item", "description": "9c4d0d64-3ddd-419d-a002-5a725b778274-envidat", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/9c4d0d64-3ddd-419d-a002-5a725b778274-envidat"}, {"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": "8e31cc42-65d1-4859-9f70-6d6cfe87b9b2", "type": "Feature", "geometry": null, "properties": {"updated": "2025-09-02T09:56:52", "type": "Dataset", "language": "de", "title": "INSPIRE Soil / Hazard Levels Water Erosion (RxKxSxL) BB", "description": "Der interoperable INSPIRE-Datensatz beinhaltet Daten vom LBGR \u00fcber die Gef\u00e4hrdungsstufen Wassererosion (RxKxSxL) Brandenburg, transformiert in das INSPIRE-Zielschema Boden. Der Datensatz wird \u00fcber je einen interoperablen Darstellungs- und Downloaddienst bereitgestellt. Im Datensatz Gef\u00e4hrdungsstufen wird die r\u00e4umliche Verteilung der potenziellen Bodenerosionsgef\u00e4hrdung durch Wasser auf den landwirtschaftlichen Fl\u00e4chen Brandenburgs dargestellt. Die Bestimmung erfolgte in Anlehnung an DIN19708 (https://dx.doi.org/10.31030/2676773), deren zu Grunde liegende Methode als Allgemeine Bodenabtragsgleichung (ABAG) bezeichnet wird. Die Erosionsgef\u00e4hrdung wird in einer r\u00e4umlichen Aufl\u00f6sung von 5x5 Meter dargestellt. Die potenzielle Erosionsgef\u00e4hrdung durch Wasser ergibt sich aus der Klassifizierung des potenziellen Bodenabtrags in Gef\u00e4hrdungsstufen. Der potenzielle Bodenabtrag durch Wasser ergibt sich aus der Kombination des Regenerosivit\u00e4tsfaktors R, des Bodenerodierbarkeitsfaktors K, des Hangneigungsfaktors S und des Hangl\u00e4ngenfaktors L. Die Gef\u00e4hrdung wird in sieben Stufen von 0 (keine Gef\u00e4hrdung) bis 6 (extrem hohe Gef\u00e4hrdung) angegeben.      ---      The compliant INSPIRE data set contains data about the risk levels for water erosion (RxKxSxL) Brandenburg from the LBGR, transformed into the INSPIRE annex schema Soil. The data set is provided via compliant view and download services. It shows the spatial distribution of the potential soil erosion risk caused by water on agricultural land in Brandenburg. The determination was based on DIN19708 (https://dx.doi.org/10.31030/2676773), for which the underlying method is referred to as the Allgemeine Bodenabtragsgleichung (ABAG). The soil erosion risk is presented in a spatial resolution of 5x5 meters. The potential soil erosion risk caused by water results from the classification of the potential soil loss into risk levels. The potential soil loss caused by water results from the combination of the rainfall-runoff erosivity factor R, the soil erodibility factor K, the slope steepness factor S and the slope length factor L. The erosion risk is indicated in seven levels from 0 (no risk) to 6 (extremely high risk).", "formats": [{"name": "WCS_SRVC"}], "keywords": ["High value dataset", "boden", "bodenerosion", "bodenerosionsgefa\u0308hrdung", "bodenerosionsgefa\u0308hrdung-durch-wasser-in-brandenburg", "bodenkunde", "brandenburg", "de", "erdbeobachtung-und-umwelt", "erosion", "erosionsgefa\u0308hrdung", "gefa\u0308hrdungsstufen", "geologie", "inspireidentifiziert", "interoperabel", "interoperability", "interoperable-daten", "opendata", "process", "regional", "soil", "soillayer", "wassererosion", "water-erosion", "watererosionrisktopsoil"], "contacts": [{"organization": "Landesamt f\u00fcr Bergbau, Geologie und Rohstoffe Brandenburg (LBGR)", "roles": ["creator"]}]}, "links": [{"href": "https://inspire.brandenburg.de/services/boerosion_wms?REQUEST=GetCapabilities&SERVICE=WMS"}, {"href": "https://inspire.brandenburg.de/services/so_boerosion_wcs?REQUEST=GetCapabilities&SERVICE=WCS"}, {"href": "https://inspire.brandenburg.de/services/so_boerosion_wms?REQUEST=GetCapabilities&SERVICE=WMS"}, {"href": "http://data.europa.eu/88u/dataset/8e31cc42-65d1-4859-9f70-6d6cfe87b9b2~~2"}, {"rel": "self", "type": "application/geo+json", "title": "8e31cc42-65d1-4859-9f70-6d6cfe87b9b2", "name": "item", "description": "8e31cc42-65d1-4859-9f70-6d6cfe87b9b2", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/8e31cc42-65d1-4859-9f70-6d6cfe87b9b2"}, {"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": "91a08ff2-84e4-40f1-bdde-6442de42203d", "type": "Feature", "geometry": null, "properties": {"updated": "2025-09-02T09:07:44", "type": "Dataset", "language": "de", "title": "INSPIRE-WMS Soil / Mittlere Elementgehalte im Oberboden BB", "description": "Der interoperable INSPIRE-WMS ist ein Darstellungsdienst, der Daten im Annex-Schema Boden (abgeleitet aus dem origin\u00e4ren Datensatz: Mittlere Elementgehalte im Oberboden Brandenburg) bereitstellt. Er gibt einen \u00dcberblick zu den mittleren Gehalte ausgew\u00e4hlter, umweltrelevanter Elemente im Oberboden (0 - 30 cm) im Land Brandenburg. Die Gehaltsklassen der jeweils f\u00fcr den Oberboden einheitlichen Kartenlegenden richten sich nach der Spannweite s\u00e4mtlicher Werte f\u00fcr das betreffende Element. Gem\u00e4\u00df der INSPIRE-Datenspezifikation Soil (D2.8.III.3_v3.0) liegen die Inhalte der Boden\u00fcbersichtskarte INSPIRE-konform vor. Der WMS beinhaltet die folgenden Layer:      - SO.elementContentArsenic: Mittlere Elementgehalt (Median) von Arsen im Boden.      - SO.elementContentCadmium: Mittlere Elementgehalt (Median) von Cadmium im Boden.      - SO.elementContentChromium: Mittlere Elementgehalt (Median) von Chrom im Boden.      - SO.elementContentCopper: Mittlere Elementgehalt (Median) von Kupfer im Boden.      - SO.elementContentLead: Mittlere Elementgehalt (Median) von Blei im Boden.      - SO.elementContentMercury: Mittlere Elementgehalt (Median) von Quecksilber im Boden.      - SO.elementContentNickel: Mittlere Elementgehalt (Median) von Nickel im Boden.      - SO.elementContentZinc: Mittlere Elementgehalt (Median) von Zink im Boden.      - SO.SoilBody: Abgegrenzter und hinsichtlich bestimmter Bodeneigenschaften und/oder r\u00e4umlicher Muster homogener Teil der Bodendecke.      ---      The compliant INSPIRE-WMS Soil / Mittlere Elementgehalte im Oberboden Brandenburg is a view service that delivers data in the annex schema Soil (derived from the original data set: Average element contents in topsoil Brandenburg). It provides an overview of the mean contents of selected environmentally relevant elements in the topsoil (0 - 30 cm) in the state of Brandenburg. The content classes of the map legends, which are uniform for the topsoil in each case, are based on the range of all values for the relevant element. The content of the soil map is compliant to the INSPIRE data specification for the annex theme Soil (D2.8.III.3_v3.0). The WMS includes the following layers:      - SO.elementContentArsenic: Mean element content (median) of arsenic in the soil.      - SO.elementContentCadmium: Mean element content (median) of cadmium in the soil.      - SO.elementContentChromium: Mean element content (median) of chromium in the soil.      - SO.elementContentCopper: Mean element content (median) of copper in the soil.      - SO.elementContentLead: Mean element content (median) of lead in the soil.      - SO.elementContentMercury: Mean element content (median) of arsenic in the soil.      - SO.elementContentNickel: Mean element content (median) of nickel in the soil.      - SO.elementContentZinc: Mean element content (median) of zinc in the soil.      - SO.SoilBody: Part of the soil cover that is delineated and that is homogeneous with regard to certain soil properties and/or spatial patterns.", "formats": [{"name": "HTML"}], "keywords": ["bboxbebb", "boden", "bodenkunde", "bodenschutz", "brandenburg", "de", "derivedsoilprofile", "elementcontentarsenic", "elementcontentcadmium", "elementcontentchromium", "elementcontentcopper", "elementcontentlead", "elementcontentmercury", "elementcontentnickel", "elementcontentzinc", "geologie", "infomapaccessservice", "inspireidentifiziert", "interoperabel", "interoperability", "mittlere-elementgehalte-im-oberboden", "oberboden", "om_observation", "opendata", "process", "soil", "soilbody", "soilderivedobject", "soillayer", "topsoil"], "contacts": [{"organization": "Landesamt f\u00fcr Bergbau, Geologie und Rohstoffe Brandenburg (LBGR)", "roles": ["creator"]}]}, "links": [{"href": "https://geoportal.brandenburg.de/detailansichtdienst/render?view=gdibb&url=https%3A%2F%2Fgeoportal.brandenburg.de%2Fgs-json%2Fxml%3Ffileid%3D91a08ff2-84e4-40f1-bdde-6442de42203d"}, {"href": "https://inspire.brandenburg.de/services/so_elementoben_wms?REQUEST=GetCapabilities&SERVICE=WMS"}, {"href": "http://data.europa.eu/88u/dataset/91a08ff2-84e4-40f1-bdde-6442de42203d~~1"}, {"rel": "self", "type": "application/geo+json", "title": "91a08ff2-84e4-40f1-bdde-6442de42203d", "name": "item", "description": "91a08ff2-84e4-40f1-bdde-6442de42203d", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/91a08ff2-84e4-40f1-bdde-6442de42203d"}, {"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": "9525e0da-2579-4a71-b08e-70b628e012b8", "type": "Feature", "geometry": null, "properties": {"updated": "2025-09-02T09:07:53", "type": "Dataset", "language": "de", "title": "INSPIRE-WMS Soil / Potenzielle Verdichtungsempfindlichkeit BB", "description": "Der interoperable INSPIRE-WMS ist ein Darstellungsdienst, der Daten im Annex-Schema Boden (abgeleitet aus dem origin\u00e4ren Datensatz: Potenzielle Verdichtungsempfindlichkeit Brandenburg in 35 cm Bezugstiefe) bereitstellt. Er gibt einen \u00dcberblick \u00fcber die potenzielle Verdichtungsempfindlichkeit des Bodens in 35 cm Bezugstiefe im Land Brandenburg. Die Karte basiert auf den Legendeneinheiten der Boden\u00fcbersichtskarte (B\u00dcK300). Diese stellen Bodenformengesellschaften dar. Die einzelnen Fl\u00e4chenbodenformen (FBF) wurden mit bodenphysikalischen Kennwerten belegt, die durch Gel\u00e4nde-und Laboruntersuchungen bestimmt wurden. Auf Basis dieser Bodenkennwerte wurde die Verdichtungsempfindlichkeit des Bodens abgeleitet. Diese klassifiziert das Erstverdichtungsverhalten (im Sinne einer Verdichtungsintensit\u00e4t) eines nat\u00fcrlich gelagerten, abgesetzten Unterbodens auf Grund seiner physikalischen und hydrologischen Eigenschaften. Weiterf\u00fchrende Informationen sind hier zu finden: http://www.geo.brandenburg.de/ows/htdocs/21042020_Verdichtung.pdf. Gem\u00e4\u00df der INSPIRE-Datenspezifikation Soil (D2.8.III.3_v3.0) liegen die Inhalte der Boden\u00fcbersichtskarte INSPIRE-konform vor. Der WMS beinhaltet die folgenden Layer:     - SO.compactionSensitivity: Gesch\u00e4tzte potentielle Erstverdichtungsintensit\u00e4t.     - SO.SoilBody: Abgegrenzter und hinsichtlich bestimmter Bodeneigenschaften und/oder r\u00e4umlicher Muster homogener Teil der Bodendecke.     ---      The compliant INSPIRE-WMS Soil / Potenzielle Verdichtungsempfindlichkeit Brandenburg is a view service that delivers data in the annex schema Soil (derived from the original data set: Potential compaction sensitivity Brandenburg at 35 cm reference depth). It provides an overview of the potential compaction sensitivity of the soil at a reference depth of 35 cm in the state of Brandenburg. The map is based on the legend units of the soil survey map (B\u00dcK300). Based on the soil properties of the legend units and the corresponding soil forms, the compaction sensitivity of the soil was derived. This classifies the initial compaction behavior (in terms of compaction intensity) of a naturally layered, settled subsoil based on its physical and hydrological properties. Further information can be found here: http://www.geo.brandenburg.de/ows/htdocs/21042020_Verdichtung.pdf. The content of the soil map is compliant to the INSPIRE data specification for the annex theme Soil (D2.8.III.3_v3.0). The WMS includes the following layers:     - SO.compactionSensitivity: Estimated potential intensity to initial compaction.     - SO.SoilBody: Part of the soil cover that is delineated and that is homogeneous with regard to certain soil properties and/or spatial patterns.", "formats": [{"name": "HTML"}], "keywords": ["bboxbebb", "boden", "bodenkunde", "bodenschutz", "brandenburg", "compactionsensitivity", "de", "derivedsoilprofile", "geologie", "infomapaccessservice", "inspireidentifiziert", "interoperabel", "interoperability", "oberboden", "om_observation", "opendata", "process", "sedimentarymaterial", "soil", "soilbody", "soilderivedobject", "soillayer", "topsoil", "verdichtungsempfindlichkeit"], "contacts": [{"organization": "Landesamt f\u00fcr Bergbau, Geologie und Rohstoffe Brandenburg (LBGR)", "roles": ["creator"]}]}, "links": [{"href": "https://geoportal.brandenburg.de/detailansichtdienst/render?view=gdibb&url=https%3A%2F%2Fgeoportal.brandenburg.de%2Fgs-json%2Fxml%3Ffileid%3D9525e0da-2579-4a71-b08e-70b628e012b8"}, {"href": "https://inspire.brandenburg.de/services/so_verdicht_wms?REQUEST=GetCapabilities&SERVICE=WMS"}, {"href": "http://data.europa.eu/88u/dataset/9525e0da-2579-4a71-b08e-70b628e012b8~~1"}, {"rel": "self", "type": "application/geo+json", "title": "9525e0da-2579-4a71-b08e-70b628e012b8", "name": "item", "description": "9525e0da-2579-4a71-b08e-70b628e012b8", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/9525e0da-2579-4a71-b08e-70b628e012b8"}, {"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": "cd0edb25-b364-4c8d-bbc2-48cd53c0deb7", "type": "Feature", "geometry": {"type": "Polygon", "coordinates": [[[64.87, 64.86], [64.87, 64.87], [64.87, 64.87], [64.87, 64.86], [64.87, 64.86]]]}, "properties": {"themes": [{"concepts": [{"id": "farming"}], "scheme": "https://standards.iso.org/iso/19139/resources/gmxCodelists.xml#MD_TopicCategoryCode"}, {"concepts": [{"id": "Soil"}, {"id": "permafrost"}, {"id": "soil organic matter"}, {"id": "climate change"}, {"id": "carbon sinks"}, {"id": "biogeochemical cycle"}, {"id": "topsoil"}, {"id": "subsoil"}, {"id": "losses from soil"}], "scheme": "AGROVOC Multilingual agricultural thesaurus"}, {"concepts": [{"id": "carbon source"}, {"id": "aggregate fractionation"}, {"id": "density fractionation"}, {"id": "soil degradation"}], "scheme": "Individual"}, {"concepts": [{"id": "Boden"}, {"id": "Soil"}], "scheme": "GEMET - INSPIRE themes, version 1.0"}], "rights": "Restrictions applied to assure the protection of privacy or intellectual property, and any special restrictions or limitations or warnings on using the resource or metadata. Reports, articles, papers, scientific and non - scientific works of any form, including tables, maps, or any other kind of output, in printed or electronic form, based in whole or in part on the data supplied, must contain an acknowledgement of the form: \"Data reused from the BonaRes Data Centre www.bonares.de. This data were created as part of the Other's research activities.\" Although every care has been taken in preparing and testing the data, the Other and the BonaRes Data Centre cannot guarantee that the data are correct; neither does the Other and the BonaRes Data Centre accept any liability whatsoever for any error, missing data or omission in the data, or for any loss or damage arising from its use. 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Reports, articles, papers, scientific and non - scientific works of any form, including tables, maps, or any other kind of output, in printed or electronic form, based in whole or in part on the data supplied, must contain an acknowledgement of the form: \"Data reused from the BonaRes Data Centre www.bonares.de. This data were created as part of the ZALF Datenerfassung's research activities.\" Although every care has been taken in preparing and testing the data, the ZALF Datenerfassung and the BonaRes Data Centre cannot guarantee that the data are correct; neither does the ZALF Datenerfassung and the BonaRes Data Centre accept any liability whatsoever for any error, missing data or omission in the data, or for any loss or damage arising from its use. 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Reports, articles, papers, scientific and non - scientific works of any form, including tables, maps, or any other kind of output, in printed or electronic form, based in whole or in part on the data supplied, must contain an acknowledgement of the form: \"Data reused from the BonaRes Data Centre www.bonares.de. This data were created as part of the ZALF Datenerfassung's research activities.\" Although every care has been taken in preparing and testing the data, the ZALF Datenerfassung and the BonaRes Data Centre cannot guarantee that the data are correct; neither does the ZALF Datenerfassung and the BonaRes Data Centre accept any liability whatsoever for any error, missing data or omission in the data, or for any loss or damage arising from its use. 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Reports, articles, papers, scientific and non - scientific works of any form, including tables, maps, or any other kind of output, in printed or electronic form, based in whole or in part on the data supplied, must contain an acknowledgement of the form: \"Data reused from the BonaRes Data Centre www.bonares.de. This data were created as part of the Rhizo4Bio - CROP's research activities.\" Although every care has been taken in preparing and testing the data, the Rhizo4Bio - CROP and the BonaRes Data Centre cannot guarantee that the data are correct; neither does the Rhizo4Bio - CROP and the BonaRes Data Centre accept any liability whatsoever for any error, missing data or omission in the data, or for any loss or damage arising from its use. The Rhizo4Bio - CROP and BonaRes Data Centre will not be responsible for any direct or indirect use which might be made of the data.", "updated": "2024-04-15", "type": "Dataset", "created": "2023-06-01", "language": "eng", "title": "How does the root architecture of wheat influence the microbial community and activity in soil?  - Enzymatic activity within the rhizosphere", "description": "The data set includes the enzyme gradient of \u03b2-Glucosidase from the root center towards the surrounding soil at different sampling times, soil depths, and spring wheat genotypes. Enzyme data was collected using the soil zymography according to Spohn et al. (2013). The spring wheat genotypes used (Rambla et al., 2022) form different root architectures (UQR012 = shallow root system, UQR015 = deep root system). Plants were grown in columns under controlled environmental conditions in a climate chamber and sampled at four sampling dates (4, 5, 6, and 7 weeks after sowing). Zymography was performed on the surface of soil segments at two soil depths (4.5 cm and 31.5 cm). The soil used originated from the upper 30 cm of an agricultural Haplic Luvisol near Selhausen (Germany). 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Workgroup Research Data Management", "roles": ["publisher"], "phones": [{"value": "+49 33432 82 300"}], "emails": [{"value": "dataservice@zalf.de"}], "addresses": [{"deliveryPoint": ["Eberswalder Strasse 84"], "city": "M\u00fcncheberg", "administrativeArea": "Brandenburg", "postalCode": "15374", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Christian Poll", "organization": "University of Hohenheim", "position": null, "roles": ["author"], "phones": [{"value": null}], "emails": [{"value": "christian.poll@uni-hohenheim.de"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": {"url": null, "protocol": null, "protocol_url": "", "name": "0000-0002-9674-4447", "name_url": "", "description": "ORCID", "description_url": "", "applicationprofile": null, "applicationprofile_url": "", "function": null}}]}, {"name": "Ellen Kandeler", "organization": "University of Hohenheim", "position": null, "roles": ["author"], "phones": [{"value": null}], "emails": [{"value": "ellen.kandeler@uni-hohenheim.de"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": {"url": null, "protocol": null, "protocol_url": "", "name": "0000-0002-2854-0012", "name_url": "", "description": "ORCID", "description_url": "", "applicationprofile": null, "applicationprofile_url": "", "function": null}}]}, {"name": "Samuel Le Gall", "organization": "Forschungszentrum J\u00fclich", "position": null, "roles": ["author"], "phones": [{"value": null}], "emails": [{"value": "s.le.gall@fz-juelich.de"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": null}]}, {"name": "Youri Rothfuss", "organization": "Forschungszentrum J\u00fclich", "position": null, "roles": ["author"], "phones": [{"value": null}], "emails": [{"value": "y.rothfuss@fz-juelich.de"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": {"url": null, "protocol": null, "protocol_url": "", "name": "0000-0002-8874-5036", "name_url": "", "description": "ORCID", "description_url": "", "applicationprofile": null, "applicationprofile_url": "", "function": null}}]}, {"organization": "Forschungszentrum J\u00fclich;University of Hohenheim", "roles": ["contributor"]}], "title_alternate": "LTE: Part 4/5, table: Enzymatic activity within the rhizosphere"}, "links": [{"href": "https://maps.bonares.de/mapapps/resources/apps/bonares/index.html?lang=en&mid=339f09f3-71e7-4c0c-83ca-dc8fe2f74c9b", "rel": "information"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/5f100775-eac0-4596-b90e-1cb4d2847410", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "339f09f3-71e7-4c0c-83ca-dc8fe2f74c9b", "name": "item", "description": "339f09f3-71e7-4c0c-83ca-dc8fe2f74c9b", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/339f09f3-71e7-4c0c-83ca-dc8fe2f74c9b"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-04-15T00:00:00Z"}}, {"id": "aa54a7b6-ad28-408a-91f5-a2c789604708", "type": "Feature", "geometry": {"type": "Polygon", "coordinates": [[[11.37, 51.66], [11.37, 52.12], [12.1, 52.12], [12.1, 51.66], [11.37, 51.66]]]}, "properties": {"themes": [{"concepts": [{"id": "farming"}], "scheme": "https://standards.iso.org/iso/19139/resources/gmxCodelists.xml#MD_TopicCategoryCode"}, {"concepts": [{"id": "Soil"}, {"id": "nitrogen fertilizers"}, {"id": "tillage"}, {"id": "crop rotation"}, {"id": "winter wheat"}, {"id": "winter barley"}, {"id": "rapeseed"}, {"id": "maize"}, {"id": "yields"}, {"id": "topsoil"}, {"id": "roots"}, {"id": "rhizosphere"}, {"id": "microbiomes"}, {"id": "soil bacteria"}, {"id": "soil fungi"}, {"id": "arid zones"}], "scheme": "AGROVOC Multilingual agricultural thesaurus"}, {"concepts": [{"id": "opendata"}], "scheme": "Individual"}, {"concepts": [{"id": "nitrogenous fertiliser"}, {"id": "cultivation"}, {"id": "yield (agricultural)"}], "scheme": "GEMET - Concepts, version 2.4"}], "rights": "Restrictions applied to assure the protection of privacy or intellectual property, and any special restrictions or limitations or warnings on using the resource or metadata. Reports, articles, papers, scientific and non - scientific works of any form, including tables, maps, or any other kind of output, in printed or electronic form, based in whole or in part on the data supplied, must contain an acknowledgement of the form: \"Data reused from the BonaRes Data Centre www.bonares.de. This data were created as part of the LTE Westerfeld's research activities.\" Although every care has been taken in preparing and testing the data, the LTE Westerfeld and the BonaRes Data Centre cannot guarantee that the data are correct; neither does the LTE Westerfeld and the BonaRes Data Centre accept any liability whatsoever for any error, missing data or omission in the data, or for any loss or damage arising from its use. The LTE Westerfeld and BonaRes Data Centre will not be responsible for any direct or indirect use which might be made of the data.", "updated": "2024-09-10", "type": "Dataset", "created": "2024-05-06", "language": "eng", "title": "Westerfeld: Long-term field trial on tillage and fertilization in crop rotation - GENE_EXPRESSION", "description": "Table with information about gene expression of the plants\n\nGeneral description see mother table: (https://doi.org/10.20387/bonares-w669-gdsd); Related datasets are listed in the metadata element 'Related Identifier'.\nDataset version 1.0", "formats": [{"name": "CSV"}], "keywords": ["Soil", "nitrogen fertilizers", "tillage", "crop rotation", "winter wheat", "winter barley", "rapeseed", "maize", "yields", "topsoil", "roots", "rhizosphere", "microbiomes", "soil bacteria", "soil fungi", "arid zones", "opendata", "nitrogenous fertiliser", "cultivation", "yield (agricultural)"], "contacts": [{"name": "Marie Raab", "organization": "Anhalt University of Applied Sciences (AUAS)", "position": null, "roles": ["author"], "phones": [{"value": null}], "emails": [{"value": "Marie.Raab@hs-anhalt.de"}], "addresses": [{"deliveryPoint": [null], "city": "Bernburg", "administrativeArea": null, "postalCode": "06406", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Annette Deubel", "organization": "Anhalt University of Applied Sciences (AUAS)", "position": null, "roles": ["author"], "phones": [{"value": null}], "emails": [{"value": "Annette.Deubel@hs-anhalt.de"}], "addresses": [{"deliveryPoint": [null], "city": "Bernburg", "administrativeArea": null, "postalCode": "06406", "country": "Germany"}], "links": [{"href": null}]}, {"name": "J\u00f6rg Geistlinger", "organization": "Anhalt University of Applied Sciences (AUAS)", "position": null, "roles": ["author"], "phones": [{"value": null}], "emails": [{"value": "Joerg.Geistlinger@hs-anhalt.de"}], "addresses": [{"deliveryPoint": [null], "city": "Bernburg", "administrativeArea": null, "postalCode": "06406", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Loreen Sommermann", "organization": "Anhalt University of Applied Sciences (AUAS)", "position": null, "roles": ["author"], "phones": [{"value": null}], "emails": [{"value": "Loreen.Sommermann@hs-anhalt.de"}], "addresses": [{"deliveryPoint": [null], "city": "Bernburg", "administrativeArea": null, "postalCode": "06406", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Doreen Babin", "organization": "Julius-K\u00fchn-Institut", "position": null, "roles": ["author"], "phones": [{"value": null}], "emails": [{"value": "Doreen.Babin@julius-kuehn.de"}], "addresses": [{"deliveryPoint": [null], "city": "Braunschweig", "administrativeArea": null, "postalCode": "38104", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Ioannis Kampouris", "organization": "Julius K\u00fchn-Institute (JKI)", "position": null, "roles": ["author"], "phones": [{"value": null}], "emails": [{"value": 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