{"type": "FeatureCollection", "features": [{"id": "10.1016/j.scitotenv.2024.174491", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:17:34Z", "type": "Journal Article", "created": "2024-07-03", "title": "GIS mapping of agricultural plastic waste in southern Europe", "description": "The escalating use of plastics in agriculture, driven by global population growth and increasing food demand, has concurrently led to a rise in Agricultural Plastic Waste (APW) production. Effective waste management is imperative, prompting this study to address the initial step of management, that is the quantification and localization of waste generated from different production systems in diverse regions. Focused on four Southern European countries (Italy, Spain, Greece, and Portugal) at the regional level, the study uses Geographic Information System (GIS), land use maps, indices tailored to each specific agricultural application and each crop type for plastic waste mapping. Furthermore, after the data was employed, it was validated by relevant stakeholders of the mentioned countries. The study revealed Spain, particularly the Andalusia region, as the highest contributor to APW equal to 324,000 tons per year, while Portugal's Azores region had the lowest estimate equal to 428 tons per year. Significantly, this research stands out as one of the first to comprehensively consider various plastic applications and detailed crop cultivations within the production systems, representing a pioneering effort in addressing plastic waste management in Southern Europe. This can lead further on to the management of waste in this area and the transfer of the scientific proposition to other countries.", "keywords": ["NUTS 2 regional level", "Agricultural practices", "330", "Estimation of agricultural plastic waste", "National agricultural census", "Plastic pollution", "Geographic information system"]}, "links": [{"href": "https://doi.org/10.1016/j.scitotenv.2024.174491"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Science%20of%20The%20Total%20Environment", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.scitotenv.2024.174491", "name": "item", "description": "10.1016/j.scitotenv.2024.174491", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.scitotenv.2024.174491"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-10-01T00:00:00Z"}}, {"id": "10.1111/gcbb.12255", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:20:00Z", "type": "Journal Article", "created": "2015-02-19", "title": "Bioenergy Harvest, Climate Change, And Forest Carbon In The Oregon Coast Range", "description": "Abstract<p>Forests provide important ecological, economic, and social services, and recent interest has emerged in the potential for using residue from timber harvest as a source of renewable woody bioenergy. The long\uffe2\uff80\uff90term consequences of such intensive harvest are unclear, particularly as forests face novel climatic conditions over the next century. We used a simulation model to project the long\uffe2\uff80\uff90term effects of management and climate change on above\uffe2\uff80\uff90 and belowground forest carbon storage in a watershed in northwestern Oregon. The multi\uffe2\uff80\uff90ownership watershed has a diverse range of current management practices, including little\uffe2\uff80\uff90to\uffe2\uff80\uff90no harvesting on federal lands, short\uffe2\uff80\uff90rotation clear\uffe2\uff80\uff90cutting on industrial land, and a mix of practices on private nonindustrial land. We simulated multiple management scenarios, varying the rate and intensity of harvest, combined with projections of climate change. Our simulations project a wide range of total ecosystem carbon storage with varying harvest rate, ranging from a 45% increase to a 16% decrease in carbon compared to current levels. Increasing the intensity of harvest for bioenergy caused a 2\uffe2\uff80\uff933% decrease in ecosystem carbon relative to conventional harvest practices. Soil carbon was relatively insensitive to harvest rotation and intensity, and accumulated slowly regardless of harvest regime. Climate change reduced carbon accumulation in soil and detrital pools due to increasing heterotrophic respiration, and had small but variable effects on aboveground live carbon and total ecosystem carbon. Overall, we conclude that current levels of ecosystem carbon storage are maintained in part due to substantial portions of the landscape (federal and some private lands) remaining unharvested or lightly managed.\uffc2\uffa0Increasing the intensity of harvest for bioenergy on currently harvested land, however,\uffc2\uffa0led to a relatively small reduction in the ability of forests to store carbon. Climate change is unlikely to substantially alter carbon storage in these forests, absent shifts in disturbance regimes.</p>", "keywords": ["0106 biological sciences", "Carbon dioxide mitigation", "Forest ecology -- Oregon -- Oregon Coast Range", "Forest biomass", "13. Climate action", "Carbon cycle (Biogeochemistry)", "Biomass energy", "Forest Biology", "15. Life on land", "01 natural sciences", "7. Clean energy", "Climatic change", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1111/gcbb.12255"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/GCB%20Bioenergy", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/gcbb.12255", "name": "item", "description": "10.1111/gcbb.12255", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcbb.12255"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2015-05-25T00:00:00Z"}}, {"id": "10.15454/SVDTOU", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:21:02Z", "type": "Dataset", "title": "Statistiques spatio-temporelles sur les propri\u00e9t\u00e9s agronomiques des sols agricoles en France issues de la Base de Donn\u00e9es d'Analyses de Terre (BDAT)", "description": "In France, farmers commission about 250,000 soil-testing analyses per year to assist them managing soil fertility. The number and diversity of origin of the samples make these analyses an interesting and original information source regarding cultivated topsoil variability. Moreover, these analyses relate to several parameters strongly influenced by human activity (macronutrient contents, pH...), for which existing cartographic information is not very relevant. Compiling the results of these analyses into a database makes it possible to re-use these data within both a national and temporal framework. A database compilation relating to data collected over the period 1990-2014 has been recently achieved. So far, commercial soil-testing laboratories approved by the Ministry of Agriculture have provided analytical results from more than 3,600,000 samples. After the initial quality control stage, analytical results from more than 1,900,000 samples were available in the database. The anonymity of the landholders seeking soil analyses is perfectly preserved, as the only identifying information stored is the location of the nearest administrative city to the sample site. We present in this dataset a set of statistical parameters of the spatial distributions for several agronomic soil properties. These statistical parameters are calculated for 4 different nested spatial entities (administrative areas: e.g. regions, departments, counties and agricultural areas) and for 5 time periods (1990-1994, 1995-1999, 2000-2004, 2005-2009, 2010-2014). Two kinds of agronomic soil properties are available: the first one correspond to the quantitative variables like the organic carbon content, and the second one corresponds to the qualitative variables like the texture class. For each spatial unit and temporal period, we calculated the following statistics sets: the first set is calculated for the quantitative variables and corresponds to the number of samples, the mean, the standard deviation and, the 2-,4-,10-quantiles; the second set is calculated for the qualitative variables and corresponds to the number of samples, the value of the dominant class, the number of samples of the dominant class, the second dominant class, the number of samples of the second dominant class.", "keywords": ["2. Zero hunger", "Earth and Environmental Science", "Soils and soil sciences", "Earth and Environmental Sciences", "Soil Sciences", "soil texture", "15. Life on land", "soil analysis", "Environmental Research", "Natural Sciences", "Geosciences"], "contacts": [{"organization": "Saby, Nicolas P.A., Lemercier, Blandine, Arrouays, Dominique, Walter, Christian, Gouny, Laetitia, Swidersky, Chlo\u00e9, Toutain, Beno\u00eet, Bispo, Antonio,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.15454/SVDTOU"}, {"rel": "self", "type": "application/geo+json", "title": "10.15454/SVDTOU", "name": "item", "description": "10.15454/SVDTOU", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.15454/SVDTOU"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-01-01T00:00:00Z"}}, {"id": "10.5194/bg-15-1933-2018", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:23:24Z", "type": "Journal Article", "created": "2017-11-21", "title": "Straw incorporation increases crop yield and soil organic carbon sequestration but varies under different natural conditions and farming practices in China: a system analysis", "description": "<p>Abstract. Loss of soil organic carbon (SOC) from agricultural soils is a key indicator of soil degradation associated with reductions in net primary productivity in crop production systems worldwide. Simple technical and locally appropriate solutions are required for farmers to increase SOC and to improve cropland management. In the last 30 years, straw incorporation has gradually been implemented across China in the context of agricultural intensification and rural livelihood improvement. A meta-analysis of data published before the end of 2016 was undertaken to investigate the effects of straw incorporation on crop production and SOC sequestration. The results of 68 experimental studies throughout China in different edaphic, climate regions and under different farming regimes were analyzed. Compared with straw removal, straw incorporation significantly sequestered SOC (0\uffe2\uff80\uff9320\uffe2\uff80\uff89cm depth) at the rate of 0.35 (range 0.31\uffe2\uff80\uff930.40)\uffe2\uff80\uff89Mg C\uffe2\uff80\uff89ha\uffe2\uff88\uff921\uffe2\uff80\uff89yr\uffe2\uff88\uff921, increased crop grain yield by 13.4\uffe2\uff80\uff89% (range 9.3\uffe2\uff80\uff89%\uffe2\uff80\uff9318.4\uffe2\uff80\uff89%) and had a conversion efficiency of the applied straw-C as 16\uffe2\uff80\uff89%\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff892\uffe2\uff80\uff89% across the whole of China. The combined straw incorporation at the rate of 3\uffe2\uff80\uff89Mg C\uffe2\uff80\uff89ha\uffe2\uff88\uff921\uffe2\uff80\uff89yr\uffe2\uff88\uff921 with mineral fertilizer of 200\uffe2\uff80\uff93400\uffe2\uff80\uff89kg N\uffe2\uff80\uff89ha\uffe2\uff88\uff921\uffe2\uff80\uff89yr\uffe2\uff88\uff921 was demonstrated to be the best combination for farmers to use with crop yield increased by 32.7\uffe2\uff80\uff89% (range 17.9\uffe2\uff80\uff89%\uffe2\uff80\uff9356.4\uffe2\uff80\uff89%) and SOC sequestrated by the rate of 0.85 (range 0.54\uffe2\uff80\uff931.15)\uffe2\uff80\uff89Mg C\uffe2\uff80\uff89ha\uffe2\uff88\uff921\uffe2\uff80\uff89yr\uffe2\uff88\uff921. Straw incorporation achieved higher SOC sequestration rate and crop yield increment when applied to clay soils, under high cropping intensities, and in areas like Northeast China where the soil is being degraded. SOC responses were the greatest in the initial starting phase of straw incorporation and then declined and finally were negligible after 28\uffe2\uff80\uff9362 years, however, crop yield responses were initially low and then increased reaching their highest level at 11\uffe2\uff80\uff9315 years after straw incorporation. Overall, our study confirmed that straw incorporation did create a positive feedback loop of SOC enhancement together with increased crop production, and this is of great practical significance to straw management as agricultural intensifies in China and other regions in the world with different climate conditions.                         </p>", "keywords": ["2. Zero hunger", "QE1-996.5", "info:eu-repo/classification/ddc/550", "Ecology", "Life", "QH501-531", "0401 agriculture", " forestry", " and fisheries", "Geology", "04 agricultural and veterinary sciences", "15. Life on land", "QH540-549.5"]}, "links": [{"href": "https://doi.org/10.5194/bg-15-1933-2018"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biogeosciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.5194/bg-15-1933-2018", "name": "item", "description": "10.5194/bg-15-1933-2018", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5194/bg-15-1933-2018"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-11-21T00:00:00Z"}}, {"id": "10.5194/bg-19-2487-2022", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:23:25Z", "type": "Journal Article", "created": "2022-05-13", "title": "Climatic variation drives loss and restructuring of carbon and nitrogen in boreal forest wildfire", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Abstract. The boreal forest landscape covers approximately 10\u2009% of the earth's land area and accounts for almost 30\u2009% of the global annual terrestrial sink of carbon\u00a0(C). Increased emissions due to climate-change-amplified fire frequency, size, and intensity threaten to remove elements such as C and nitrogen\u00a0(N) from forest soil and vegetation at rates faster than they accumulate. This may result in large areas within the region becoming a net source of greenhouse gases, creating a positive feedback loop with a changing climate. Meter-scale estimates of area-normalized fire emissions are limited in Eurasian boreal forests, and knowledge of their relation to climate and ecosystem properties is sparse. This study sampled 50 separate Swedish wildfires, which occurred during an extreme fire season in 2018, providing quantitative estimates of C and N loss due to fire along a climate gradient. Mean annual precipitation had strong positive effects on total fuel, which was the strongest driver for increasing C and N losses. Mean annual temperature\u00a0(MAT) influenced both pre- and postfire organic layer soil bulk density and C\u2009:\u2009N ratio, which had mixed effects on C and N losses. Significant fire-induced loss of C estimated in the 50 plots was comparable to estimates in similar Eurasian forests but approximately a quarter of those found in typically more intense North American boreal wildfires. N loss was insignificant, though a large amount of fire-affected fuel was converted to a low C\u2009:\u2009N surface layer of char in proportion to increased MAT. These results reveal large quantitative differences in C and N losses between global regions and their linkage to the broad range of climate conditions within Fennoscandia. A need exists to better incorporate these factors into models to improve estimates of global emissions of C and N due to fire in future climate scenarios. Additionally, this study demonstrated a linkage between climate and the extent of charring of soil fuel and discusses its potential for altering C and N dynamics in postfire recovery.</p></article>", "keywords": ["QE1-996.5", "Ecology", "Life", "13. Climate action", "QH501-531", "Geology", "15. Life on land", "01 natural sciences", "QH540-549.5", "Climate Science", "Klimatvetenskap", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.5194/bg-19-2487-2022"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biogeosciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.5194/bg-19-2487-2022", "name": "item", "description": "10.5194/bg-19-2487-2022", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5194/bg-19-2487-2022"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-05-13T00:00:00Z"}}, {"id": "10.5281/zenodo.15328215", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:24:49Z", "type": "Dataset", "title": "1000 Soils Pilot Dataset, version 8, May 2025", "description": "This record hosts data generated by the 1000 Soils Pilot. Data will be updated as more become available. Please see the most recent data upload for current data.  A beta visualization tool is available for some data types at\u00a0https://shinyproxy.emsl.pnnl.gov/app/1000soils. Please submit any suggestions or comments through the 'contact' tab. We are actively working to improve visualizations and value all feedback.  Data completed include:    Geochemistry, texture, respiration, and enzyme activities  FTICR-MS organic matter chemistry  Microbial biomass C and N  TOC/TDN of water-extractable OM  X-ray computed tomography (derived metrics available here, raw data available upon request)  Metagenomes; a variety of data formats are available upon request  Soil hydraulic properties   Data in progress:    LC-MS/MS in development, timeline TBD, inquire for status   1000S_processed_BGC_summary.csv contains all available biogeochemical data; microbial biomass C and N; and TOC/TDN of water-extractable OM; and\u00a0  1000S_Tomography.xslx contains a summary of data generated via X-ray computed tomography.  icr_v2_corems2.csv contains FTICR-MS data processed by CoreMS version 2. These data are merged by formula across instrument runs to enable cross-sample comparisons. Technical replicates are merged by retaining peaks present in 2 out of 3 replicates.  1000Soils_Metadata_Site_Mastersheet_v1.csv contains site information.  Soil Hydraulics_corrected_02042025.xlsx contains soil hydraulics information.  Readme File_v4.xlsx is the readme file.  Please contact the MONet project (monet.emsl@pnnl.gov) or Emily Graham (emily.graham@pnnl.gov) with questions.  The following file and all raw data are\u00a0available upon request:  icr_by_mass_for_single_sample_analysis_only.csv\u00a0contains FTICR-MS data processed by CoreMS and is intended for usage in the calculation of biochemical transformations within samples only. These data are not acceptable for cross-sample comparison of masses because they are from multiple instrument runs.  For more information, please see: https://www.emsl.pnnl.gov/monet and https://sc-data.emsl.pnnl.gov/monet  Acknowledgment:\u00a0  Soil data were provided by the Molecular Observation Network (MONet) at the Environmental Molecular Sciences Laboratory (https://ror.org/04rc0xn13), a DOE Office of Science user facility sponsored by the Biological and Environmental Research program under Contract No. DE-AC05-76RL01830. The work (proposal: 10.46936/10.25585/60008970) conducted by the U.S. Department of Energy, Joint Genome Institute (https://ror.org/04xm1d337), a DOE Office of Science user facility, is supported by the Office of Science of the U.S. Department of Energy operated under Contract No. DE-AC02-05CH11231.\u00a0  The Molecular Observation Network (MONet) database is an open, FAIR, and publicly available compilation of the molecular and microstructural properties of soil. Data in the MONet open science database can be found at\u00a0https://sc-data.emsl.pnnl.gov/.", "keywords": ["2. Zero hunger", "decomposition", "13. Climate action", "FTICR-MS", "biogeochemistry", "carbon", "molecular", "15. Life on land", "6. Clean water", "soil"]}, "links": [{"href": "https://doi.org/10.5281/zenodo.15328215"}, {"rel": "self", "type": "application/geo+json", "title": "10.5281/zenodo.15328215", "name": "item", "description": "10.5281/zenodo.15328215", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5281/zenodo.15328215"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-05-02T00:00:00Z"}}, {"id": "11250/3212345", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:27:09Z", "type": "Journal Article", "created": "2025-01-31", "title": "Contrasting seasonal patterns in particle aggregation and dissolved organic matter transformation in a sub-Arctic fjord", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Abstract. Particulate (POM) and dissolved (DOM) organic matter in the ocean are important components of the Earth's biogeochemical cycle. The two are in a constant state of dynamic change as a result of physical and biochemical processes; however, they are mostly treated as two distinct entities, separated operationally by a filter. We studied the seasonal transition of DOM and POM pools and their drivers in a sub-Arctic fjord by means of monthly environmental sampling and by performing experiments at selected time points. For the experiments, surface water (5\u2009m) was either pre-filtered through a GF/F filter (0.7\u2009\u00b5m) or left unfiltered, followed by 36\u2009h incubations. Before and after incubation, samples were collected for dissolved and particulate organic carbon concentrations (DOC, POC), extracellular polymeric substances (EPSs), microbial community (flow cytometry), and molecular composition of DOM (high-performance liquid chromatography coupled to high-resolution mass spectrometry \u2013 HPLC-HRMS). During the biologically productive period, when environmental POC concentrations were high (April, June, September), the filtered water showed an increase in POC concentrations. While POC concentrations increased in September, DOM lability decreased based on changes in the average hydrogen saturation and aromaticity of DOM molecules. In contrast, during the winter period (December and February), when environmental POC concentrations were low, lower concentrations of POC were measured at the end of the experiments compared to at the start. The change in POC concentrations was significantly different between the biologically productive period and the winter period (t test; p&lt;0.05). Simultaneously, the DOM pool became more labile during the incubation period, as indicated by changes in the average hydrogen saturation, aromaticity, and oxygen saturation, with implications for carbon cycling. The change in POC was not directly associated with an antagonistic change in DOC concentrations, highlighting the complexity of organic matter transformations, making the dynamics between POC and DOC difficult to quantify. However, in both periods, bacterial activity and EPS concentrations increased throughout the incubations, showing that bacterial degradation and physical DOM aggregation drive the transformations of POM and DOM in concert but at varying degrees under different environmental conditions.</p></article>", "keywords": ["particulate organic carbon", "seasonal variation", "QE1-996.5", "Ecology", "saturation", "aggregation", "surface water", "fjord", "Geology", "biogeochemical cycle", "Milj\u00f6vetenskap", "dissolved organic carbon", "microbial activity", "environmental conditions", "Life", "QH501-531", "microbial community", "Environmental Sciences", "QH540-549.5"]}, "links": [{"href": "https://doi.org/11250/3212345"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biogeosciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "11250/3212345", "name": "item", "description": "11250/3212345", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/11250/3212345"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-01-31T00:00:00Z"}}, {"id": "1871.1/0b041c5c-edd1-45f1-895d-546207d34a0a", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:27:27Z", "type": "Journal Article", "created": "2024-03-21", "title": "Environmental drivers and remote sensing proxies of post-fire thaw depth in Eastern Siberian larch forests", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Abstract. Boreal fire regimes are intensifying because of climate change and the northern parts of boreal forests are underlain by permafrost. Boreal fires combust vegetation and organic soils, which insulate permafrost, and as such deepen the seasonally thawed active layer and can lead to further carbon emissions to the atmosphere. Current understanding of the environmental drivers of post-fire thaw depth is limited but of critical importance. In addition, mapping thaw depth over fire scars may enable a better understanding of the spatial variability in post-fire responses of permafrost soils. We assessed the environmental drivers of post-fire thaw depth using field data from a fire scar in a larch-dominated forest in the continuous permafrost zone in Eastern Siberia. Particularly, summer thaw depth was deeper in burned (mean = 127.3 cm, standard deviation (sd) = 27.7 cm) than in unburned (98.1 cm, sd = 26.9 cm) landscapes one year after the fire, yet the effect of fire was modulated by landscape and vegetation characteristics. We found deeper thaw in well-drained landscape positions, in open larch forest often intermixed with Scots pine, and in high severity burns. The environmental drivers, site moisture, forest type and density, and fire severity explained 73.4 % of the measured thaw depth variability at the study sites. In addition, we evaluated the relationships between field-measured thaw depth and several remote sensing proxies. Albedo, the differenced Normalized Burn Ratio (dNBR), land surface temperature (LST), and pre-fire Normalized Difference Vegetation Index (NDVI) derived from Landsat 8 imagery together explained 66.3 % of the variability in field-measured thaw depth. Based on these remote sensing proxies and multiple linear regression analysis, we estimated thaw depth over the entire fire scar, and found that LST displayed particularly strong correlations with post-fire thaw depth (r = 0.65, p &lt; 0.01). Our study reveals some of the governing processes of post-fire thaw depth development and shows the capability of Landsat imagery to estimate thaw depth at a landscape scale.                         </p></article>", "keywords": ["Dynamic and structural geology", "QE1-996.5", "13. Climate action", "Science", "Q", "Geology", "QE500-639.5", "Deforestation", "15. Life on land", "Landsat", "Multiple linear regression", "Atmospheric temperature"]}, "links": [{"href": "https://esd.copernicus.org/articles/15/1459/2024/esd-15-1459-2024.pdf"}, {"href": "https://doi.org/1871.1/0b041c5c-edd1-45f1-895d-546207d34a0a"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Earth%20System%20Dynamics", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "1871.1/0b041c5c-edd1-45f1-895d-546207d34a0a", "name": "item", "description": "1871.1/0b041c5c-edd1-45f1-895d-546207d34a0a", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/1871.1/0b041c5c-edd1-45f1-895d-546207d34a0a"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-03-21T00:00:00Z"}}, {"id": "1871.1/bbc7e25d-d1b9-4c7d-baa4-1a09012f06b2", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:27:28Z", "type": "Journal Article", "created": "2022-11-21", "title": "Global biomass burning fuel consumption and emissions at 500\u2009m spatial resolution based on the Global Fire Emissions Database (GFED)", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Abstract. In fire emission models, the spatial resolution of both the modelling framework and the satellite data used to quantify burned area can have considerable impact on emission estimates. Consideration of this sensitivity is especially important in areas with heterogeneous land cover and fire regimes and when constraining model output with field measurements. We developed a global fire emissions model with a spatial resolution of 500\u2009m using MODerate resolution Imaging Spectroradiometer (MODIS) data. To accommodate this spatial resolution, our model is based on a simplified version of the Global Fire Emissions Database (GFED) modelling framework. Tree mortality as a result of fire, i.e.\u00a0fire-related forest loss, was modelled based on the overlap between 30\u2009m forest loss data and MODIS burned area and active fire detections. Using this new 500\u2009m model, we calculated global average carbon emissions from fire of 2.1\u00b10.2 (\u00b11\u03c3 interannual variability, IAV)\u2009Pg\u2009C\u2009yr\u22121 during 2002\u20132020. Fire-related forest loss accounted for 2.6\u00b10.7\u2009% (uncertainty range =1.9\u2009%\u20133.3\u2009%) of global burned area and 24\u00b16\u2009% (uncertainty range =16\u2009%\u201331\u2009%) of emissions, indicating that fuel consumption in forest fires is an order of magnitude higher than the global average. Emissions from the combustion of soil organic carbon (SOC) in the boreal region and tropical peatlands accounted for 13\u00b14\u2009% of global emissions. Our global fire emissions estimate was higher than the 1.5\u2009Pg\u2009C\u2009yr\u22121 from GFED4 and similar to 2.1\u2009Pg\u2009C\u2009yr\u22121 from GFED4s. Even though GFED4s included more burned area by accounting for small fires undetected by the MODIS burned area mapping algorithm, our emissions were similar to GFED4s due to higher average fuel consumption. The global difference in fuel consumption could mainly be explained by higher SOC emissions from the boreal region as constrained by additional measurements. The higher resolution of the 500\u2009m model also contributed to the difference by improving the simulation of landscape heterogeneity and reducing the scale mismatch in comparing field measurements to model grid cell averages during model calibration. Furthermore, the fire-related forest loss algorithm introduced in our model led to more accurate and widespread estimation of high-fuel-consumption burned area. Recent advances in burned area detection at resolutions of 30\u2009m and finer show a substantial amount of burned area that remains undetected with 500\u2009m sensors, suggesting that global carbon emissions from fire are likely higher than our 500\u2009m estimates. The ability to model fire emissions at 500\u2009m resolution provides a framework for further improvements with the development of new satellite-based estimates of fuels, burned area, and fire behaviour, for use in the next generation of GFED.</p></article>", "keywords": ["QE1-996.5", "13. Climate action", "11. Sustainability", "Geology", "15. Life on land", "7. Clean energy", "01 natural sciences", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/1871.1/bbc7e25d-d1b9-4c7d-baa4-1a09012f06b2"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Geoscientific%20Model%20Development", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "1871.1/bbc7e25d-d1b9-4c7d-baa4-1a09012f06b2", "name": "item", "description": "1871.1/bbc7e25d-d1b9-4c7d-baa4-1a09012f06b2", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/1871.1/bbc7e25d-d1b9-4c7d-baa4-1a09012f06b2"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-05-30T00:00:00Z"}}, {"id": "1959.7/uws:72836", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:27:33Z", "type": "Journal Article", "created": "2023-04-24", "title": "Different Cerrado Ecotypes Show Contrasting Soil Microbial Properties, Functioning Rates, and Sensitivity to Changing Water Regimes", "description": "Abstract<p>Soil moisture is among the most important factors regulating soil biodiversity and functioning. Models forecast changes in the precipitation regime in many areas of the planet, but how these changes will influence soil functioning, and how biotic drivers modulate such effects, is far from being understood. We evaluated the responses of C and N fluxes, and soil microbial properties to different soil water regimes in soils from the main three ecotypes of the world's largest and most diverse tropical savanna. Further, we explored the direct and indirect effects of changes in the ecotype and soil water regimes on these key soil processes. Soils from the woodland savanna showed a better nutritional status than the other ecotypes, as well as higher potential N cycling rates, N2O emissions, and soil bacterial abundance but lower bacterial richness, whereas potential CO2 emissions and CH4 uptake peaked in the intermediate savanna. The ecotype also modulated the effects of changes in the soil water regime on nutrient cycling, greenhouse gas fluxes, and soil bacterial properties, with more intense responses in the intermediate savanna. Further, we highlight the existence of multiple contrasting direct and indirect (via soil microbes and abiotic properties) effects of an intensification of the precipitation regime on soil C- and N-related processes. Our results confirm that ecotype is a fundamental driver of soil properties and functioning in the Cerrado and that it can determine the responses of key soil processes to changes in the soil water regime.</p", "keywords": ["2. Zero hunger", "Ecotype", "0301 basic medicine", "Take urgent action to combat climate change and its impacts", "Naturgeografi", "ecotype", "Cerrado", "greenhouse gases.", "04 agricultural and veterinary sciences", "15. Life on land", "precipitation regime", "Precipitation regime", "cerrado", "03 medical and health sciences", "Greenhouse gases", "Physical Geography", "13. Climate action", "N cycle", "XXXXXX - Unknown", "0401 agriculture", " forestry", " and fisheries", "C cycle", "http://metadata.un.org/sdg/13", "cerrado; ecotype; precipitation regime; C cycle; N cycle; greenhouse gases"]}, "links": [{"href": "https://doi.org/1959.7/uws:72836"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Ecosystems", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "1959.7/uws:72836", "name": "item", "description": "1959.7/uws:72836", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/1959.7/uws:72836"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-04-24T00:00:00Z"}}, {"id": "383c70fe-7169-43da-89da-e45b126f3a70~~1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:35:20Z", "type": "Dataset", "language": "de", "title": "GcB\u00dcK400 \u2014 Zinc in the upper floor", "description": "Zinc is an essential trace element for plants, animals and humans, which, however, can have a toxic effect on plants and microorganisms at extremely high levels. The concentration of Zn in the upper continental crust (Clark value) is 52\u00a0mg/kg, but it can vary greatly depending on the type of rock. The mean Zn (median) grades of the Saxon main rock types range from 11 to 140\u00a0mg/kg, while the regional Clarke of the Ore Mountains is approximately 79\u00a0mg/kg. Sphalerite (zinc aperture) leading polymetallic lathers can locally lead to additional geogenic Zn enrichments in the soils. Anthropogenic Zn entries are mainly carried out by iron and non-ferrous metallurgy or by the Zn-processing industries (colours, alloys, electroplating) and by large combustion plants. In the area of agglomerations, Zn enrichments are relatively common. Anthropogenic Zn entries are possible in agriculture through the use of organic and mineral fertilisers. For uncontaminated soils, Zn levels of 10 to 80\u00a0mg/kg are considered normal. The regional distribution of the Zn content in the Saxon soils is mainly determined by the geogenic embossing of the substrates; low to medium grades can be expected over the periglacial sands and clays in the north and the loess soils in middle axes (10 to 50\u00a0mg/kg) and weathering soils above the solid rocks of the Ore Mountains/Vogtland (50 to 150\u00a0mg/kg). Within the basement units, significant positive Zn anomalies occur via the polymetallic deposits of the Ore Mountains, depending on the intensity of the mineralisation (Freiberg, Annaberg-Buchholz \u2014 Marienberg, Aue \u2014 Schwarzenberg). Soils over substrates with extremely low Zn content (Granite of Eibenstock, Orthogneise of the Ore Mountains Central Zone, Easter Mountain Eruptive Complex, Cretan sandstones) appear as negative Zn anomalies in the map image. Reinforced Zn accumulators are to be detected in the floodplain floors of the trough system. Due to the higher geogenic basic contents in the water catchment area, the occurrence of Zn-conducting polymetallic minerals and in particular the mining and metallurgical activity in the Freiberg region, high concentrations of Zn (median content 370 and 240\u00a0mg/kg respectively) occur mainly in the meadows of the Freiberger and United Mulde. No test and measure values have been established for the soil-human and soil-plant effects pathways for total levels in the Federal Soil Protection and Contaminant Ordinance (BBodSchV), as Zn is of little importance in the risk assessment.", "keywords": ["anorganischer-schadstoff", "boden", "chemie", "chemisches-element", "de", "geologie", "opendata", "zink", "zn"]}, "links": [{"href": "https://luis.sachsen.de/boden/geodatendownload.html"}, {"href": "http://data.europa.eu/88u/dataset/383c70fe-7169-43da-89da-e45b126f3a70~~1"}, {"href": "https://geoportal.sachsen.de/md/383c70fe-7169-43da-89da-e45b126f3a70"}, {"rel": "self", "type": "application/geo+json", "title": "383c70fe-7169-43da-89da-e45b126f3a70~~1", "name": "item", "description": "383c70fe-7169-43da-89da-e45b126f3a70~~1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/383c70fe-7169-43da-89da-e45b126f3a70~~1"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"null": "date"}}, {"id": "10.1007/s10021-013-9650-7", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:14:42Z", "type": "Journal Article", "created": "2013-02-21", "title": "Stimulation Of Different Functional Groups Of Bacteria By Various Plant Residues As A Driver Of Soil Priming Effect", "description": "The turnover of organic matter in soil depends on the activity of microbial decomposers. However, little is known about how modifications of the diversity of soil microbial communities induced by fresh organic matter (FOM) inputs can regulate carbon cycling. Here, we investigated the decomposition of two 13C labeled crop residues (wheat and alfalfa) and the dynamics of the genetic structure and taxonomic composition of the soil bacterial communities decomposing 13C labeled FOM and native unlabeled soil organic matter (SOM), respectively. It was achieved by combining the stable isotope probing method with molecular tools (DNA genotyping and pyrosequencing of 16S rDNA). Although a priming effect (PE) was always induced by residue addition, its intensity increased with the degradability of the plant residue. The input of both wheat and alfalfa residues induced a rapid dynamics of FOM-degrading communities, corresponding to the stimulation of bacterial phyla which have been previously described as copiotrophic organisms. However, the dynamics and the identity of the bacterial groups stimulated depended on the residue added, with Firmicutes dominating in the wheat treatment and Proteobacteria dominating in the alfalfa treatment after 3\u00a0days of incubation. In both treatments, SOM-degrading communities were dominated by Acidobacteria, Verrucomicrobia, and Gemmatimonadetes phyla which have been previously described as oligotrophic organisms. An early stimulation of SOM-degrading populations mainly belonging to Firmicutes and Bacteroidetes groups was observed in the alfalfa treatment whereas no change occurred in the wheat treatment. Our findings support the hypothesis that the succession of bacterial taxonomic groups occurring in SOM- and FOM-degrading communities during the degradation process may be an important driver of the PE, and consequently of carbon dynamics in soil.", "keywords": ["0301 basic medicine", "2. Zero hunger", "570", "0303 health sciences", "[SDE.MCG]Environmental Sciences/Global Changes", "bacterial diversity", "[SDV.SA.SDS]Life Sciences [q-bio]/Agricultural sciences/Soil study", "15. Life on land", "[SDV.MP.BAC]Life Sciences [q-bio]/Microbiology and Parasitology/Bacteriology", "630", "soil", "[SDE.MCG] Environmental Sciences/Global Changes", "03 medical and health sciences", "pyrosequencing", "[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry", "soil organic matter", "carbon cycle", "[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/Geochemistry", "[SDV.MP.BAC] Life Sciences [q-bio]/Microbiology and Parasitology/Bacteriology", "[SDV.SA.SDS] Life Sciences [q-bio]/Agricultural sciences/Soil study", "stable isotope probing"]}, "links": [{"href": "https://doi.org/10.1007/s10021-013-9650-7"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Ecosystems", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s10021-013-9650-7", "name": "item", "description": "10.1007/s10021-013-9650-7", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s10021-013-9650-7"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2013-02-22T00:00:00Z"}}, {"id": "10.1007/s00248-003-9001-x", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:14:25Z", "type": "Journal Article", "created": "2004-06-15", "title": "Microbial Community Structure And Oxidative Enzyme Activity In Nitrogen-Amended North Temperate Forest Soils", "description": "Large regions of temperate forest are subject to elevated atmospheric nitrogen (N) deposition which can affect soil organic matter dynamics by altering mass loss rates, soil respiration, and dissolved organic matter production. At present there is no general model that links these responses to changes in the organization and operation of microbial decomposer communities. Toward that end, we studied the response of litter and soil microbial communities to high levels of N amendment (30 and 80 kg ha(-1) yr(-1)) in three types of northern temperate forest: sugar maple/basswood (SMBW), sugar maple/red oak (SMRO), and white oak/black oak (WOBO). We measured the activity of extracellular enzymes (EEA) involved directly in the oxidation of lignin and humus (phenol oxidase, peroxidase), and indirectly, through the production of hydrogen peroxide (glucose oxidase, glyoxal oxidase). Community composition was analyzed by extracting and quantifying phospholipid fatty acids (PLFA) from soils. Litter EEA responses at SMBW sites diverged from those at oak-bearing sites (SMRO, BOWO), but the changes were not statistically significant. For soil, EEA responses were consistent across forests types: phenol oxidase and peroxidase activities declined as a function of N dose (33-73% and 5-41%, respectively, depending on forest type); glucose oxidase and glyoxal oxidase activities increased (200-400% and 150-300%, respectively, depending on forest type). Principal component analysis (PCA) ordinated forest types and treatment responses along two axes; factor 1 (44% of variance) was associated with phenol oxidase and peroxidase activities, factor 2 (31%) with glucose oxidase. Microbial biomass did not respond to N treatment, but nine of the 23 PLFA that formed >1 mol% of total biomass showed statistically significant treatment responses. PCA ordinated forest types and treatment responses along three axes (36%, 26%, 12% of variance). EEA factors 1 and 2 correlated negatively with PLFA factor 1 ( r = -0.20 and -0.35, respectively, n = 108) and positively with PLFA factor 3 ( r = +0.36 and +0.20, respectively, n = 108). In general, EEA responses were more strongly tied to changes in bacterial PLFA than to changes in fungal PLFA. Collectively, our data suggests that N inhibition of oxidative activity involves more than the repression of ligninase expression by white-rot basidiomycetes.", "keywords": ["Michigan", "Nitrogen", "Science", "Ecology and Evolutionary Biology", "Nature Conservation", "Microbiology", "Trees", "Soil", "Geoecology/Natural Processes", "Health Sciences", "Cellular and Developmental Biology", "Ecosystem", "Phospholipids", "Soil Microbiology", "2. Zero hunger", "Analysis of Variance", "Principal Component Analysis", "Ecology", "Life Sciences", "Natural Resources and Environment", "Molecular", "04 agricultural and veterinary sciences", "15. Life on land", "Enzymes", "13. Climate action", "0401 agriculture", " forestry", " and fisheries"]}, "links": [{"href": "https://doi.org/10.1007/s00248-003-9001-x"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Microbial%20Ecology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s00248-003-9001-x", "name": "item", "description": "10.1007/s00248-003-9001-x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s00248-003-9001-x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2004-04-19T00:00:00Z"}}, {"id": "10.1016/j.epsl.2017.04.002", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:16:43Z", "type": "Journal Article", "created": "2017-04-14", "title": "The origin of volatile element depletion in early solar system material: Clues from Zn isotopes in chondrules", "description": "Abstract   Volatile lithophile elements are depleted in the different planetary materials to various degrees, but the origin of these depletions is still debated. Stable isotopes of moderately volatile elements such as Zn can be used to understand the origin of volatile element depletions. Samples with significant volatile element depletions, including the Moon and terrestrial tektites, display heavy Zn isotope compositions (i.e. enrichment of 66Zn vs. 64Zn), consistent with kinetic Zn isotope fractionation during evaporation. However,  Luck et al. (2005)  found a negative correlation between      \u03b4    66     Zn and 1/[Zn] between CI, CM, CO, and CV chondrites, opposite to what would be expected if evaporation caused the Zn abundance variations among chondrite groups.  We have analyzed the Zn isotope composition of multiple samples of the major carbonaceous chondrite classes: CI (1), CM (4), CV (2), CO (4), CB (2), CH (2), CK (4), and CK/CR (1). The bulk chondrites define a negative correlation in a plot of      \u03b4    66     Zn vs 1/[Zn], confirming earlier results that Zn abundance variations among carbonaceous chondrites cannot be explained by evaporation. Exceptions are CB and CH chondrites, which display Zn systematics consistent with a collisional formation mechanism that created enrichment in heavy Zn isotopes relative to the trend defined by CI\u2013CK.  We further report Zn isotope analyses of chondrite components, including chondrules from Allende (CV3) and Mokoia (CV3), as well as an aliquot of Allende matrix. All chondrules are enriched in light Zn isotopes (\u223c500 ppm on 66Zn/64Zn) relative to the bulk, contrary to what would be expected if Zn were depleted during evaporation, on the other hand the matrix has a complementary heavy isotope composition. We report sequential leaching experiments in un-equilibrated ordinary chondrites, which show sulfides are isotopically heavy compared to silicates and the bulk meteorite by ca. +0.65 per mil on 66Zn/64Zn. We suggest isotopically heavy sulfides were removed from either chondrules or their precursors, thereby producing the light Zn isotope enrichments in chondrules.", "keywords": ["chondrules", "550", "protoplanetary disk", "551", "carbonaceous chondrites", "01 natural sciences", "volatiles", "[SDU.STU.PL]Sciences of the Universe [physics]/Earth Sciences/Planetology", "[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry", "13. Climate action", "[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/Geochemistry", "[SDU.STU.PL] Sciences of the Universe [physics]/Earth Sciences/Planetology", "zinc isotopes", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.epsl.2017.04.002"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Earth%20and%20Planetary%20Science%20Letters", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.epsl.2017.04.002", "name": "item", "description": "10.1016/j.epsl.2017.04.002", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.epsl.2017.04.002"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-06-01T00:00:00Z"}}, {"id": "10.1016/j.sandf.2023.101332", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:17:26Z", "type": "Journal Article", "created": "2023-06-20", "title": "Addressing the challenges of homogeneity, quality control and waste handling in soil bio-cementation: A large-scale experiment", "description": "In an attempt to go beyond the conventional laboratory experiments widely reported in literature around the emerging technique of soil bio-cementation, this work addresses key challenges related to its large-scale application. Precisely, a state-of-the-art installation with a draining bottom boundary is introduced and a novel treatment strategy, based on ex-situ hydrolysis within a 1000 L bioreactor, is described. Hydrolyzed solutions are injected in a tank filled with 0\u20134\u00a0mm sand, via a system of eight injection tubes to treat a total surface of 40\u00a0m2 across a depth of 2\u00a0m. A multilevel, spatial and temporal quality control system is used to monitor the injection processes across several cycles via chemical and hydraulic means. In total, 20.8\u00a0m3 of reactant solutions are supplied to the targeted zone, equal to one pore volume and over 120 chemical analyses are carried-out. Reaction efficiencies overall exceeded 80%, while by increasing the number of treatment cycles, and thus calcification levels, a gradual increase in the recorded pressure at the injection inlet was captured, that reached up to 75\u00a0kPa. Zones where the injection pressure increased the most are found to yield better resistance in the vicinity of the corresponding injection tube. A dynamic penetrometer campaign reveals that increase in the tip resistance, is found to exceed 5\u00a0MPa and yields more homogenous response across the bottom 0.5\u00a0m of the tank, which is believed to reflect the effect of initial confinement on the deposition of calcite. For the zones with the highest cementation, correlated \u03c6\u2019 values yield a 5\u00b0 increase, while the oedometric modulus is found to double. The results suggest that ex-situ bio-cementation, where hydrolysis occurs in bioreactors instead of inside the soil mass, is capable of yielding similar precipitation efficiencies and mechanical improvement compared to traditional bio-cementation, where bacteria are injected directly into the soil. Finally, the monitoring of MICP at the scale of typical geotechnical works is discussed along with the problematic of residual ammonium, which in this study is found to reach absorded quantities of 4\u00a0mol/L.", "keywords": ["MICP", "Upscaling", "0211 other engineering and technologies", "Quality control", "Dynamic penetrometer", "TA703-712", "Engineering geology. Rock mechanics. Soil mechanics. Underground construction", "02 engineering and technology", "Field testing", "6. Clean water", "0201 civil engineering"], "contacts": [{"organization": "Harran, Ray, Terzis, Dimitrios, Laloui, Lyesse,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1016/j.sandf.2023.101332"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soils%20and%20Foundations", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.sandf.2023.101332", "name": "item", "description": "10.1016/j.sandf.2023.101332", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.sandf.2023.101332"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-08-01T00:00:00Z"}}, {"id": "10.1016/j.jrmge.2020.04.003", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:17:18Z", "type": "Journal Article", "created": "2020-06-15", "title": "Combined approach of poroelastic and earthquake nucleation applied to the reservoir-induced seismic activity in the Val d\u2019Agri area, Italy", "description": "Open AccessIn this work, an approach is developed to study the seismicity associated with the impoundment and level changes of a water reservoir (reservoir induced seismicity \u2013 RIS). The proposed methodology features a combination of a semi-analytical poroelastic model with an earthquake nucleation approach based on rate-and-state frictional law. The combined approach was applied to the case of the Pertusillo Lake, located in the Val d\u2019Agri area (Italy), whose large seasonal water level changes are believed to induce protracted micro-seismicity (local magnitude ML < 3). Results show that the lake impoundment in 1962 could have produced up to 0.5 bar (1 bar = 100 kPa) changes in Coulomb failure stress (\u0394CFS), while the seasonal water level variation is responsible for variation up to 0.05 bar. Modeling results of the seismicity rates in 2001\u22122014 show that the observed earthquakes are well correlated with the modeled \u0394CFS. Finally, the reason that the seismicity is only observed at southwest of the Pertusillo Lake is provided, which is likely attributed to different rock lithologies and depletion caused by significant hydrocarbon exploitation in the northeastern sector of the lake.", "keywords": ["550", "Rate-and-state frictional law", "Pertusillo lake", "Reservoir induced seismicity (RIS); Poroelasticity; Rate-and-state frictional law; Pertusillo lake", "TA703-712", "Reservoir induced seismicity (RIS)", "Engineering geology. Rock mechanics. Soil mechanics. Underground construction", "Poroelasticity", "01 natural sciences", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.jrmge.2020.04.003"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Rock%20Mechanics%20and%20Geotechnical%20Engineering", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.jrmge.2020.04.003", "name": "item", "description": "10.1016/j.jrmge.2020.04.003", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.jrmge.2020.04.003"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-08-01T00:00:00Z"}}, {"id": "10.1016/j.chemosphere.2018.05.042", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:16:23Z", "type": "Journal Article", "created": "2018-05-08", "title": "Toxicity screening of biochar-mineral composites using germination tests", "description": "This study assessed the properties and toxicity (water cress germination trials) of 38 waste-derived, novel biochar-mineral composites (BMCs) produced via slow pyrolysis and hydrothermal carbonization (hydrochars). The biochars were produced from sewage sludge and compost-like output (CLO) by varying the type of mineral additive (zeolite, wood ash and lignite fly ash), the mineral-to-feedstock ratio and the carbonization process. While pure hydrochars completely inhibited germination of water cress, this effect was ameliorated by mineral additives. Seedlings grew best in pyrolysis chars and while wood ash addition decreased plant growth in many cases, 1:10 addition to CLO doubled germination rate. The factors responsible for the phytotoxicity can be attributed to pH, salinity and organic contaminants. Importantly, while pure minerals inhibited germination, conversion of minerals into BMCs reduced their inhibitory effects due to buffered release of minerals. Overall, mineral wastes (e.g., combustion ashes) and waste biomass can be used safely as sources of nutrients and stable organic carbon (for soil carbon sequestration) when converted into specific biochar-mineral composites, exploiting synergies between the constituents to deliver superior performance.", "keywords": ["Minerals", "Bioresource and Agricultural Engineering", "Ash", "Germination", "04 agricultural and veterinary sciences", "01 natural sciences", "630", "6. Clean water", "12. Responsible consumption", "Biochar", "Soil", "Engineering", "13. Climate action", "Geological Engineering", "Charcoal", "0401 agriculture", " forestry", " and fisheries", "BMCHTC", "Hydrochar", "Pyrolysis", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://arrow.tudublin.ie/context/beschrecart/article/1073/viewcontent/Toxicity_screening_of_biochar_mineral_composites_using_germination_tests.pdf"}, {"href": "https://doi.org/10.1016/j.chemosphere.2018.05.042"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Chemosphere", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.chemosphere.2018.05.042", "name": "item", "description": "10.1016/j.chemosphere.2018.05.042", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.chemosphere.2018.05.042"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-09-01T00:00:00Z"}}, {"id": "10.1016/j.scitotenv.2018.11.475", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:17:31Z", "type": "Journal Article", "created": "2018-12-01", "title": "Local topographic and edaphic factors largely predict shrub encroachment in Mediterranean drylands", "description": "Shrub encroachment influences several ecosystem services in drylands worldwide. Yet, commonly used strategies to reduce encroachment show a low medium-term success, calling for a better understanding of its causes. Previous works identified multiple drivers responsible for this phenomenon, including anthropogenic and environmental causes. However, the relative effect of climate, topography and edaphic factors on shrub encroachment is not fully understood nor has been properly quantified in Mediterranean Basin drylands. Also, understanding how these drivers lead to changes in plant communities' functional traits associated to shrub encroachment is crucial, considering traits influence ecosystem processes and associated ecosystem services. Here, we studied the understory of a Mediterranean dryland ecosystem composed of savanna-like Holm-oak woodlands, along a regional climatic gradient. We specifically assessed (i) how climatic, topographic and edaphic factors influence understory relative shrub cover (RSC) and (ii) their direct and indirect effects (via RSC) on plant functional traits. We studied the mean and diversity of 12 functional traits related to plant regeneration, establishment, and dispersal, at the community-level. We found that, under similar low-intensity land use, topographic and edaphic factors, namely slope variations and soil C:N ratio, were the most important predictors of shrub encroachment, determining communities' functional characteristics. Climate, namely summer precipitation, had a much lesser influence. Our model explained 52% of the variation in relative shrub cover. Climate had a stronger effect on a set of functional traits weakly involved in shrub encroachment, related to flowering and dispersal strategies. We show that shrub encroachment is largely predicted by topo-edaphic factors in Mediterranean drylands subject to conventional low-intensity land use. Hence, management strategies to reduce encroachment need to take these drivers into account for efficient forecasting and higher cost-effectiveness. Our results suggest that climate change might not greatly impact shrub encroachment in the Mediterranean Basin, but may affect functional structure and reduce functional diversity of plant communities, thus affecting ecosystem functioning.", "keywords": ["0106 biological sciences", "2. Zero hunger", "Geography", "Portugal", "Plant Dispersal", "Climate Change", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "Soil", "climate change", "aridity", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "functional traits", "holm-oak", "Ecosystem"]}, "links": [{"href": "https://doi.org/10.1016/j.scitotenv.2018.11.475"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Science%20of%20The%20Total%20Environment", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.scitotenv.2018.11.475", "name": "item", "description": "10.1016/j.scitotenv.2018.11.475", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.scitotenv.2018.11.475"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-03-01T00:00:00Z"}}, {"id": "10.1016/j.foreco.2004.03.018", "type": "Feature", "geometry": null, "properties": {"license": "Closed Access", "updated": "2026-04-03T16:16:48Z", "type": "Journal Article", "created": "2004-05-29", "title": "Chronic Nitrogen Enrichment Affects The Structure And Function Of The Soil Microbial Community In Temperate Hardwood And Pine Forests", "description": "We examined how chronic nitrogen (N) enrichment of pine and hardwood forest stands has affected the relative abundance, functional capacity, and activity of soil bacteria and fungi. During Fall 2002 we collected one soil core (5.6 cm diameter; organic horizon plus 10 cm of mineral soil) from each of four 5 m \ufffd 5 m subplots within the control, low N (5 g N m \ufffd 2 per year), and high N (15 g N m \ufffd 2 per year) plots in both the hardwood and pine stands at the Chronic Nitrogen Amendment Study at Harvard Forest. The samples were analyzed for total and active bacterial and fungal biomass, microbial catabolic response profiles, the activities of cellulolytic and ligninolytic enzymes, and total, labile and microbially derived organic carbon (C). Live, fine roots were also collected from the control and low N pine plots and analyzed for ectomycorrhizal fungal community composition and diversity. Active fungal biomass was 27\u201061% and 42\u201069% lower in the fertilized compared to control plots in the hardwood and pine stands, respectively. Active bacterial biomass was not greatly affected by N additions, resulting in significantly lower fungal:bacterial biomass ratios in the N-treated plots. This shift in microbial community composition was accompanied by a significant reduction in the activity of phenol oxidase, a lignin-degrading enzyme produced by white-rot fungi. In the pine stand, ectomycorrhizal fungal community diversity was lower in the low N-treated plot than in the control plot. Differences in ectomycorrhizal community structure were also detected between control and fertilized pine plots, including a reduction in those species with the highest relative frequencies in the control community. Finally, N enrichment altered the pattern of microbial substrate use, with the relative response to the addition of carboxylic acids and carbohydrates being significantly lower in the Ntreated plots, even after the data were normalized to account for differences in microbial biomass. These patterns are consistent with lower decomposition rates and altered N cycling observed previously at this site. # 2004 Elsevier B.V. All rights reserved.", "keywords": ["2. Zero hunger", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "Biogeochemistry", "15. Life on land"]}, "links": [{"href": "https://doi.org/10.1016/j.foreco.2004.03.018"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Forest%20Ecology%20and%20Management", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.foreco.2004.03.018", "name": "item", "description": "10.1016/j.foreco.2004.03.018", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.foreco.2004.03.018"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2004-07-01T00:00:00Z"}}, {"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": "caa134ea-ce26-4e82-a48e-8bd5c35c467e~~1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:35:24Z", "type": "Dataset", "language": "de", "title": "GcB\u00dcK400 \u2014 Copper in the upper floor", "description": "Copper is an essential element for the diet of all living beings, which, however, can lead to toxic effects in the event of an extreme oversupply. The mean Cu content of the rocks of the upper continental crust (Clark value) is 14\u00a0mg/kg. Analogous to chromium and nickel, it is mainly enriched in basic rocks (Diabase, Basalte, Metabasite). The mean Cu content (mediane) of the main Saxon rock types ranges from 2 to 67\u00a0mg/kg, and the regional Clarke of the Ore Mountains/Vogtland is 23\u00a0mg/kg. Geogenic Cu enrichments can be found mainly in the Ore Mountains via the widely used mineralisations here. Chalkopyrite (copper jaw) is common in almost all mineral associations as so-called pass-through minerals. Strong anthropogenic Cu entries are mainly caused by non-ferrous metallurgy. Due to the diverse use of Cu, e.g. in electrical engineering, as alloy metal, piping material and rain gutters, the element is also increasingly entered into the wastewater. For uncontaminated soils Cu levels from 2 to 40\u00a0mg/kg are considered normal. The regional distribution of Cu levels in the upper soil is mainly determined by the geogenic proportion of substrates. Due to the increased Cu levels of the diabase widespread in the Vogtland (58\u00a0mg/kg), the point-like tertiary basaltoids (60\u00a0mg/kg) and the locally stored amphibolites (46\u00a0mg/kg) of the metamorphic basement, there is anomalously high Cu content in the weathering soils above the said solid rocks. Increased solubility influence (with relatively low Cu content of about 12\u00a0mg/kg) can lead to a \u201cdilution effect\u201d via Cu-rich substrates, depending on the proportion of the solution (e.g. via the monzonitoid at bites). Extremely low Cu concentrations can be observed in weathering soils over acidic magmatites (Granite of Ei-Benstock, Teplice-Rhyolite), metagranitoids (central zone of ore), sandstones (Elbe sandstone and Zittau mountains) and soil societies from periglaciar sandy deck sediments in northern axes. Important regional anomalies are mainly located in the Freiberg region, the most important former site of mining and the smelting of polymetallic ores. However, the anthropogenic entries are usually limited to the immediate vicinity of the metallurgical sites. This leads to overlay with geogenic proportions in the soil, which are causally linked to the spread of copper gravel leading mineral associations. Analogous conditions can be found, albeit in a weakened form, in the Schneeberg \u2014 Schwarzenberg \u2014 Annaberg-Buchholz \u2014 Marienberg area. Especially high Cu-contents have the meadow soils of the Freiberger Mulde. After the entry of the Freiberger Mulde into the Freiberg mining and metallurgy area, there is a sustainable material burden on the floodplains, which extends across the Aue of the United Mulde to the northern border. Increased Cu levels, but at a much lower level, also occur in the floodplains of the Zwickau Mulde, where the polymetallic mineralisations of the West Ore Mountains are located in the catchment area. As a result of the geogenic and anthropogenic processes described above, in the meadows of the Freiberger and the United Mulde, the measures of the Federal Soil Protection and Contaminant Ordinance (BBodSchV) for grassland use (sheep farming) are partially exceeded.", "keywords": ["anorganischer-schadstoff", "boden", "chemie", "chemisches-element", "cu", "de", "geologie", "kupfer", "opendata"]}, "links": [{"href": "https://luis.sachsen.de/boden/geodatendownload.html"}, {"href": "http://data.europa.eu/88u/dataset/caa134ea-ce26-4e82-a48e-8bd5c35c467e~~1"}, {"href": "https://geoportal.sachsen.de/md/caa134ea-ce26-4e82-a48e-8bd5c35c467e"}, {"rel": "self", "type": "application/geo+json", "title": "caa134ea-ce26-4e82-a48e-8bd5c35c467e~~1", "name": "item", "description": "caa134ea-ce26-4e82-a48e-8bd5c35c467e~~1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/caa134ea-ce26-4e82-a48e-8bd5c35c467e~~1"}, {"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": "f916fd97-f1e4-4516-a95c-7e9af9f98521", "type": "Feature", "geometry": null, "properties": {"updated": "2025-09-02T10:10:04", "type": "Dataset", "language": "de", "title": "WMS Bodenkarten BB (WMS-BOKARTEN)", "description": "Der Darstellungsdienst (WMS) Bodenkarten Brandenburg stellt Daten zu den folgenden drei Kartenwerken bereit: Bodengeologische Karte (BK 50), Bodengeologische \u00dcbersichtskarte (B\u00dcK 300) und Mittelma\u00dfst\u00e4bige landwirtschaftliche Standortkartierung (MMK). Die dargestellten Inhalte der B\u00dcK 300 wurden f\u00fcr den Ma\u00dfstab 1 : 300.000 erstellt und sind f\u00fcr Darstellungen in Ma\u00dfst\u00e4ben gr\u00f6\u00dfer 1 : 50.000 nicht geeignet. Die dargestellten Inhalte der MMK wurden f\u00fcr den Ma\u00dfstab 1 : 100.000 erstellt und sind f\u00fcr Darstellungen in Ma\u00dfst\u00e4ben gr\u00f6\u00dfer 1 : 100.000 nicht geeignet. BK 50: Das Blatt Potsdam (L3744) stellt das erste Blatt der gro\u00dfma\u00dfst\u00e4bigen Bodengeologischen Karte (BK50) im Ma\u00dfstab 1:50.000 f\u00fcr das Land Brandenburg dar. Das Kartenwerk wird in dieser Form jedoch nicht weiterentwickelt sondern methodisch von der Entwicklung der Konzeptbodenkarten (KBK) abgel\u00f6st. B\u00dcK 300: Die Bodengeologische \u00dcbersichtskarte ist das erste nutzungsunabh\u00e4ngige bodengeologische Kartenwerk, das fl\u00e4chendeckend f\u00fcr Brandenburg vorliegt. Die Karte liefert einen \u00dcberblick \u00fcber wesentliche B\u00f6den und ist mit ihren Auswertungen Grundlage f\u00fcr konkrete Aufgaben wie z. B. die Landes-, Bodenschutz- oder Raumplanung auf Landesebene. Die Legende ist nach Substratmerkmalen gegliedert und besteht aus 99 Einheiten, in denen die Leitbodenformengesellschaften dargestellt werden. Die sie kennzeichnenden Fl\u00e4chenbodenformen wurden mit chemischen und physikalischen Parametern belegt, die in einem Fl\u00e4chenbodenformenarchiv abgelegt sind. In einem zus\u00e4tzlichen Layer werden ausgew\u00e4hlte Profilaufnahmepunkten dargestellt, die jeweils mit einem Link zu einer detaillierten Profilbeschreibung verkn\u00fcpft sind. So wird es m\u00f6glich, mit verschiedenen Auswertemethoden auf die Daten der digitalen Karte zuzugreifen. MMK: Die Mittelma\u00dfst\u00e4bige landwirtschaftliche Standortkartierung wurde in den Jahren 1974 bis 1981 unter Leitung des Bereiches Bodenkunde Eberswalde des Forschungszentrums f\u00fcr Bodenfruchtbarkeit der damaligen Akademie der Landwirtschaftswissenschaften erarbeitet und stellt heute noch eine wichtige Informationsgrundlage f\u00fcr verschiedenste Fragestellungen dar. Der heutige Wert dieses Kartenwerkes liegt einerseits in seiner Aussagef\u00e4higkeit f\u00fcr bestimmte Ma\u00dfst\u00e4be und andererseits an dem Umstand, dass ein nach neueren Nomenklaturen erarbeitetes Kartenwerk in einem vergleichbaren bzw. gr\u00f6\u00dferen Ma\u00dfstab f\u00fcr die landwirtschaftliche Nutzfl\u00e4che erst in Bearbeitung ist.     Der WMS beinhaltet die folgenden Layer:      - Grundkarte der B\u00dcK 300 [grundk_buek300],     - Profilaufnahmepunkte [profilaufnahmepkt_buek300],     - Mittelma\u00dfst\u00e4bige landwirtschaftliche Standortkartierung (MMK) [mmk],     - Bodengeologische Karte (BK 50) [bk50].", "formats": [{"name": "HTML"}], "keywords": ["bboxbebb", "bk-50", "boden", "bodengeologie", "bodengeologische-karte", "bodengeologische-u\u0308bersichtskarte", "bodenkarte", "bodenkartierung", "bodenkunde", "bu\u0308k-300", "de", "geologie", "kartenwerk", "landwirtschaft", "mittelma\u00dfsta\u0308bige-landwirtschaftliche-standortkartierung", "mmk", "opendata", "sgd_boden", "wms"], "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%3Df916fd97-f1e4-4516-a95c-7e9af9f98521"}, {"href": "https://inspire.brandenburg.de/services/bokarten_wms?REQUEST=GetCapabilities&SERVICE=WMS"}, {"href": "http://data.europa.eu/88u/dataset/f916fd97-f1e4-4516-a95c-7e9af9f98521~~1"}, {"rel": "self", "type": "application/geo+json", "title": "f916fd97-f1e4-4516-a95c-7e9af9f98521", "name": "item", "description": "f916fd97-f1e4-4516-a95c-7e9af9f98521", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/f916fd97-f1e4-4516-a95c-7e9af9f98521"}, {"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": "f9254b4c-044f-45a1-be03-4875f9d6f7eb~~1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:35:34Z", "type": "Dataset", "title": "INSPIRE-WCS Geology / Reflexionsseismische Horizonte 2D BB: Fl\u00e4chen", "description": "Der interoperable INSPIRE-WCS ist ein Downloaddienst, der Daten im Annex-Schema Geology (abgeleitet aus dem origin\u00e4ren Datensatz: Reflexionssesimische Horizonte 2D Brandenburg) bereitstellt. Die Horizonte entsprechen einer Ableitung aus dem 3D-Untergrundmodell Brandenburgs (B3D) in Form eines 2D-Datensatzes. Das 3D-Modell B3D stellt den Untergrund Brandenburgs in Form ausgew\u00e4hlter reflexionsseismischer Horizonte bis in eine Tiefe von ca. 7000 m dar.   Informationen zum Download der linienhaften Ableitungen (St\u00f6rungszonen/Ausbissgrenzen und Konturlinien) finden Sie unter dem INSPIRE-WFS Geology / Reflexionsseismische Horizonte 2D BB: Linien https://inspire.brandenburg.de/services/ge-core_seismikhorizonte_l_wfs?request=GetCapabilities&service=WFS.  Gem\u00e4\u00df der INSPIRE-Datenspezifikation Geology (D2.8.II.4) liegen die Inhalte INSPIRE-konform vor.  Der WCS beinhaltet die folgenden Layer: GE.TransgressionSurfaceCenozoic (T1 - horizon), GE.TransgressionAreaMiddleAlbToCenomanian (B2-T2 - horizon), GE.TransgressionAreaUnder-AlbToWealden (T3-T4 - horizon), GE.Intra-OxfordToKimmeridge (E1-E2 - horizon), GE.Intra-Toarc (L1 - horizon), GE.TopUpperGypsumKeuper (K2 - horizon), GE.Intra-MainShellLimestone (M1 - horizon), GE.TopSalinaRed (S1 - horizon), GE.TopZechsteinSalinar (X1 - horizon), GE.SurfaceBasalAnhydriteOfTheSta\u00dffurtFormationInTheZechstein (Z1 - horizon), GE.BasisWerraAnhydrit (Z3 - horizon), GE.BaseUpperRedII (R6 - horizon).  ---  The compliant INSPIRE WCS is a download service that provides data in the annex schema Geology (derived from the original dataset: Reflexionsseismische Horizonte 2D BB). The horizons correspond to a derivation from the 3D subsurface model of Brandenburg (B3D) in the form of a 2D data set. The 3D model B3D represents the subsurface of Brandenburg in the form of selected seismic reflection horizons down to a depth of approx. 7000 m.   Information on downloading the fault zones / outcrop limits and contour lines can be found at INSPIRE-WFS Geology / Reflexionsseismische Horizonte 2D BB: Linien https://inspire.brandenburg.de/services/ge-core_seismikhorizonte_l_wfs?request=GetCapabilities&service=WFS.  The content is compliant to the INSPIRE data specification for the annex theme Geology (D2.8.II.4_v3.3.0).  The WCS contains the following layers: GE.TransgressionSurfaceCenozoic (T1 - horizon), GE.TransgressionAreaMiddleAlbToCenomanian (B2-T2 - horizon), GE.TransgressionAreaUnder-AlbToWealden (T3-T4 - horizon), GE.Intra-OxfordToKimmeridge (E1-E2 - horizon), GE.Intra-Toarc (L1 - horizon), GE.TopUpperGypsumKeuper (K2 - horizon), GE.Intra-MainShellLimestone (M1 - horizon), GE.TopSalinaRed (S1 - horizon), GE.TopZechsteinSalinar (X1 - horizon), GE.SurfaceBasalAnhydriteOfTheSta\u00dffurtFormationInTheZechstein (Z1 - horizon), GE.BasisWerraAnhydrit (Z3 - horizon), GE.BaseUpperRedII (R6 - horizon).", "formats": [{"name": "INSPIRE DOWNLOAD SERVICE"}], "keywords": ["3d-untergrundmodell", "b2d", "b3d", "bboxbebb", "boden", "brandenburg", "de", "geologiccollection", "geologicevent", "geologicunit", "geologie", "geologycore", "horizont", "infocoverageaccessservice", "inspireidentifiziert", "interoperabel", "interoperability", "interoperable-daten", "opendata", "reflexionsseismische-horizontkarte", "sheardisplacementstructure", "wcs"], "contacts": [{"organization": "Herr Arvid Markert", "roles": ["creator"]}]}, "links": [{"href": "https://inspire.brandenburg.de/services/ge-core_seismikhorizonte_f_wcs?"}, {"href": "http://data.europa.eu/88u/dataset/f9254b4c-044f-45a1-be03-4875f9d6f7eb~~1"}, {"href": "https://registry.gdi-de.org/id/de.bb.metadata/f9254b4c-044f-45a1-be03-4875f9d6f7eb"}, {"rel": "self", "type": "application/geo+json", "title": "f9254b4c-044f-45a1-be03-4875f9d6f7eb~~1", "name": "item", "description": "f9254b4c-044f-45a1-be03-4875f9d6f7eb~~1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/f9254b4c-044f-45a1-be03-4875f9d6f7eb~~1"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"null": "date"}}, {"id": "10.1007/s11368-022-03203-1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:15:22Z", "type": "Journal Article", "created": "2022-04-23", "title": "Improving the design and implementation of sediment fingerprinting studies: summary and outcomes of the TRACING 2021 Scientific School", "description": "Identifying best practices for sediment fingerprinting or tracing is important to allow the quantification of sediment contributions from catchment sources. Although sediment fingerprinting has been applied with reasonable success, the deployment of this method remains associated with many issues and limitations.Seminars and debates were organised during a 4-day Thematic School in October 2021 to come up with concrete suggestions to improve the design and implementation of tracing methods.First, we suggest a better use of geomorphological information to improve study design. Researchers are invited to scrutinise all the knowledge available on the catchment of interest, and to obtain multiple lines of evidence regarding sediment source contributions. Second, we think that scientific knowledge could be improved with local knowledge and we propose a scale of participation describing different levels of involvement of locals in research. Third, we recommend the use of state-of-the-art sediment tracing protocols to conduct sampling, deal with particle size, and examine data before modelling and accounting for the hydro-meteorological context under investigation. Fourth, we promote best practices in modelling, including the importance of running multiple models, selecting appropriate tracers, and reporting on model errors and uncertainty. Fifth, we suggest best practices to share tracing data and samples, which will increase the visibility of the fingerprinting technique in geoscience. Sixth, we suggest that a better formulation of hypotheses could improve our knowledge about erosion and sediment transport processes in a more unified way.With the suggested improvements, sediment fingerprinting, which is interdisciplinary in nature, could play a major role to meet the current and future challenges associated with global change.The online version contains supplementary material available at 10.1007/s11368-022-03203-1.", "keywords": ["[SDE] Environmental Sciences", "DATA", "550", "[SDU.STU.GM] Sciences of the Universe [physics]/Earth Sciences/Geomorphology", "[SDV.SA.SDS]Life Sciences [q-bio]/Agricultural sciences/Soil study", "01 natural sciences", "333", "source-to-sink", "basin", "local knowledge", "[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry", "[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/Geochemistry", "11. Sustainability", "[SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology", "14. Life underwater", "[SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/Hydrology", "catchment", "[SDV.SA.SDS] Life Sciences [q-bio]/Agricultural sciences/Soil study", "watershed", "FAIR", "0105 earth and related environmental sciences", "sediment tracing", "ddc:550", "Frontiers in Soils and Sediments \u2022 Research Article", "15. Life on land", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "6. Clean water", "sediment fingerprinting", "Chemistry", "critical Zone", "13. Climate action", "Earth and Environmental Sciences", "[SDE]Environmental Sciences", "[SDU.STU.HY] Sciences of the Universe [physics]/Earth Sciences/Hydrology", "[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces", "environment"]}, "links": [{"href": "https://link.springer.com/content/pdf/10.1007/s11368-022-03203-1.pdf"}, {"href": "https://doi.org/10.1007/s11368-022-03203-1"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Soils%20and%20Sediments", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s11368-022-03203-1", "name": "item", "description": "10.1007/s11368-022-03203-1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s11368-022-03203-1"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-04-23T00:00:00Z"}}, {"id": "09AF7F8B-C32B-454F-A28E-8FA9899A19B4", "type": "Feature", "geometry": null, "properties": {"updated": "2025-08-07T21:58:57.534631", "type": "Dataset", "language": "de", "externalIds": [{"value": "https://metaver.de/cswhh"}], "title": "Soil sealing Hamburg", "description": "Sealing card:  With the description of the extent of soil sealing, a quantitative overview of the expansion of urban settlement areas can be given as well as qualitative influences, e.g. on the urban climate and groundwater regeneration can be mapped.   The description of the degree of sealing is based on the biotope mapping in Hamburg and will be updated every five years (latest processing status in 2021).  In order to enable the comparative evaluation and the cartographic representation of the sealing degrees, a classification into sealing classes was additionally carried out - analogous to the procedure of previous evaluations - since the large number of different sealing degrees would make the results illegible. In order to achieve a high and yet clear resolution, class widths of 10% were chosen, which leads to the formation of a total of 10 classes (Class 1 = 0-10%, ..., Class 10 = 90-100%). If the wingspan of the degree of sealing was more than 10%, a sealing class was assigned that corresponded to the dominant sealing (e.g. single-house building, compacted - sealing degree 30-70% with predominantly 60 % = sealing class 6).   The maps were edited and published in February 2022.", "formats": [{"name": "GML"}], "keywords": ["High value dataset", "boden", "de", "geodaten", "hvd", "umweltdaten"], "contacts": [{"organization": "Beh\u00f6rde f\u00fcr Umwelt, Klima, Energie und Agrarwirtschaft (BUKEA)", "roles": ["creator"]}]}, "links": [{"href": "http://metaver.de/trefferanzeige?docuuid=09AF7F8B-C32B-454F-A28E-8FA9899A19B4"}, {"href": "http://suche.transparenz.hamburg.de/dataset/bodenversiegelung-in-hamburg-2017-auswertung-sowie-vergleichende-bewertungen?forceWeb=true"}, {"href": "http://www.geoportal-hamburg.de/Geoportal/geo-online/index.html"}, {"href": "http://www.hamburg.de/fhh-permalink/135300"}, {"href": "https://api.hamburg.de/datasets/v1/versiegelung_bedeckung_hamburg"}, {"href": "https://geodienste.hamburg.de/download?url=https://geodienste.hamburg.de/wfs_versiegelung_bedeckung_hamburg&f=csv"}, {"href": "https://geodienste.hamburg.de/download?url=https://geodienste.hamburg.de/wfs_versiegelung_bedeckung_hamburg&f=json"}, {"href": "https://geodienste.hamburg.de/wfs_versiegelung_bedeckung_hamburg?SERVICE=WFS&VERSION=1.1.0&REQUEST=DescribeFeatureType&typename=de.hh.up:versiegelungskarte_50m_raster%252Cde.hh.up:versiegelungskarte_10m_raster%252Cde.hh.up:bodenbedeckung%252Cde.hh.up:versiegelungskarte_25m_raster"}, {"href": "https://geodienste.hamburg.de/wfs_versiegelung_bedeckung_hamburg?SERVICE=WFS&VERSION=1.1.0&REQUEST=GetFeature&typename=de.hh.up:versiegelungskarte_50m_raster%252Cde.hh.up:versiegelungskarte_10m_raster%252Cde.hh.up:bodenbedeckung%252Cde.hh.up:versiegelungskarte_25m_raster"}, {"href": "https://geodienste.hamburg.de/wfs_versiegelung_bedeckung_hamburg?Service=WFS&Version=1.1.0&Request=GetCapabilities"}, {"href": "https://geodienste.hamburg.de/wms_versiegelung_bedeckung_hamburg?Service=WMS&Version=1.3.0&Request=GetCapabilities"}, {"href": "http://data.europa.eu/88u/dataset/09af7f8b-c32b-454f-a28e-8fa9899a19b4~~2"}, {"rel": "self", "type": "application/geo+json", "title": "09AF7F8B-C32B-454F-A28E-8FA9899A19B4", "name": "item", "description": "09AF7F8B-C32B-454F-A28E-8FA9899A19B4", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/09AF7F8B-C32B-454F-A28E-8FA9899A19B4"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"null": "date"}}, {"id": "10.1007/s10533-021-00759-x", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:14:51Z", "type": "Journal Article", "created": "2021-01-26", "title": "How much carbon can be added to soil by sorption?", "description": "Abstract<p>Quantifying the upper limit of stable soil carbon storage is essential for guiding policies to increase soil carbon storage. One pool of carbon considered particularly stable across climate zones and soil types is formed when dissolved organic carbon sorbs to minerals. We quantified, for the first time, the potential of mineral soils to sorb additional dissolved organic carbon (DOC) for six soil orders. We compiled 402 laboratory sorption experiments to estimate the additional DOC sorption potential, that is the potential of excess DOC sorption in addition to the existing background level already sorbed in each soil sample. We estimated this potential using gridded climate and soil geochemical variables within a machine learning model. We find that mid- and low-latitude soils and subsoils have a greater capacity to store DOC by sorption compared to high-latitude soils and topsoils. The global additional DOC sorption potential for six soil orders is estimated to be 107 $$ pm$$                   \uffc2\uffb1                  13 Pg C to 1\uffc2\uffa0m depth. If this potential was realized, it would represent a 7% increase in the existing total carbon stock.</p>", "keywords": ["550", "Mineral association", "Organic chemistry", "Carbon Dynamics in Peatland Ecosystems", "Markvetenskap", "01 natural sciences", "Agricultural and Biological Sciences", "Soil water", "Carbon fibers", "Water Science and Technology", "2. Zero hunger", "Latitude", "Ecology", "Total organic carbon", "Life Sciences", "Composite number", "Geology", "04 agricultural and veterinary sciences", "Saturation", "Milj\u00f6vetenskap", "Soil carbon", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "Algorithm", "Chemistry", "Physical Sciences", "Environmental chemistry", "Sorption", "Additional sorption potential", "environment", "Geodesy", "Biogeochemical Cycling of Nutrients in Aquatic Ecosystems", "Soil Science", "Environmental science", "FOS: Mathematics", "Environmental Chemistry", "Soil Carbon Sequestration", "Earth-Surface Processes", "0105 earth and related environmental sciences", "Soil science", "[SDU.OCEAN]Sciences of the Universe [physics]/Ocean", "Atmosphere", "Soil organic carbon", "[SDU.OCEAN] Sciences of the Universe [physics]/Ocean", " Atmosphere", "FOS: Earth and related environmental sciences", "15. Life on land", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "0401 agriculture", " forestry", " and fisheries", "Adsorption", "[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems", "Dissolved organic carbon", "Environmental Sciences", "Mathematics"]}, "links": [{"href": "http://link.springer.com/content/pdf/10.1007/s10533-021-00759-x.pdf"}, {"href": "https://doi.org/10.1007/s10533-021-00759-x"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biogeochemistry", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s10533-021-00759-x", "name": "item", "description": "10.1007/s10533-021-00759-x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s10533-021-00759-x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-01-26T00:00:00Z"}}, {"id": "10.1007/s10533-021-00838-z", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:14:51Z", "type": "Journal Article", "created": "2021-08-27", "title": "Soil organic matter turnover rates increase to match increased inputs in grazed grasslands", "description": "Abstract<p>Managed grasslands have the potential to store carbon (C) and partially mitigate climate change. However, it remains difficult to predict potential C storage under a given soil or management practice. To study C storage dynamics due to long-term (1952\uffe2\uff80\uff932009) phosphorus (P) fertilizer and irrigation treatments in New Zealand grasslands, we measured radiocarbon (14C) in archived soil along with observed changes in C stocks to constrain a compartmental soil model. Productivity increases from P application and irrigation in these trials resulted in very similar C accumulation rates between 1959 and 2009. The \uffe2\uff88\uff8614C changes over the same time period were similar in plots that were both irrigated and fertilized, and only differed in a non-irrigated fertilized plot. Model results indicated that decomposition rates of fast cycling C (0.1 to 0.2\uffc2\uffa0year\uffe2\uff88\uff921) increased to nearly offset increases in inputs. With increasing P fertilization, decomposition rates also increased in the slow pool (0.005 to 0.008\uffc2\uffa0year\uffe2\uff88\uff921). Our findings show sustained, significant (i.e. greater than 4 per mille) increases in C stocks regardless of treatment or inputs. As the majority of fresh inputs remain in the soil for less than 10\uffc2\uffa0years, these long term increases reflect dynamics of the slow pool. Additionally, frequent irrigation was associated with reduced stocks and increased decomposition of fresh plant material. Rates of C gain and decay highlight trade-offs between productivity, nutrient availability, and soil C sequestration as a climate change mitigation strategy.</p", "keywords": ["Soil modeling", "Carbon sequestration", "2. Zero hunger", "Environmental management", "Life on Land", "Environmental Science and Management", "Agronomy & Agriculture", "04 agricultural and veterinary sciences", "15. Life on land", "ddc:631.4", "Soil carbon", "Article", "Radiocarbon", "Environmental Management", "Geochemistry", "Transit time", "13. Climate action", "Earth Sciences", "Radiocarbon; Soil carbon; Soil modeling; Carbon sequestration; Transit time; SoilR", "0401 agriculture", " forestry", " and fisheries", "SoilR", "Soil modeling ; Article ; Soil carbon ; Carbon sequestration ; SoilR ; Transit time ; Radiocarbon", "Other Chemical Sciences", "Environmental Sciences"]}, "links": [{"href": "https://link.springer.com/content/pdf/10.1007/s10533-021-00838-z.pdf"}, {"href": "https://escholarship.org/content/qt2nv780zp/qt2nv780zp.pdf"}, {"href": "https://doi.org/10.1007/s10533-021-00838-z"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biogeochemistry", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s10533-021-00838-z", "name": "item", "description": "10.1007/s10533-021-00838-z", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s10533-021-00838-z"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-08-27T00:00:00Z"}}, {"id": "10.1007/s10533-023-01091-2", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:14:51Z", "type": "Journal Article", "created": "2023-10-15", "title": "Global observation gaps of peatland greenhouse gas balances: needs and obstacles", "description": "Abstract           <p>Greenhouse gas (GHGs) emissions from peatlands contribute significantly to ongoing climate change because of human land use. To develop reliable and comprehensive estimates and predictions of GHG emissions from peatlands, it is necessary to have GHG observations, including carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O), that cover different peatland types globally. We synthesize published peatland studies with field GHG flux measurements to identify gaps in observations and suggest directions for future research. Although GHG flux measurements have been conducted at numerous sites globally, substantial gaps remain in current observations, encompassing various peatland types, regions and GHGs. Generally, there is a pressing need for additional GHG observations in Africa, Latin America and the Caribbean regions. Despite widespread measurements of CO2 and CH4, studies quantifying N2O emissions from peatlands are scarce, particularly in natural ecosystems. To expand the global coverage of peatland data, it is crucial to conduct more eddy covariance observations for long-term monitoring. Automated chambers are preferable for plot-scale observations to produce high temporal resolution data; however, traditional field campaigns with manual chamber measurements remain necessary, particularly in remote areas. To ensure that the data can be further used for modeling purposes, we suggest that chamber campaigns should be conducted at least monthly for a minimum duration of one year with no fewer than three replicates and measure key environmental variables. In addition, further studies are needed in restored peatlands, focusing on identifying the most effective restoration approaches for different ecosystem types, conditions, climates, and land use histories.</p", "keywords": ["570", "Atmospheric sciences", "Carbon Dynamics in Peatland Ecosystems", "Eddy covariance", "Greenhouse gas", "01 natural sciences", "Article", "Environmental science", "Methane Emissions", "Impact of Climate Change on Forest Wildfires", "Importance of Mangrove Ecosystems in Coastal Protection", "11. Sustainability", "greenhouse gases", "Climate change", "Biology", "peatlands", "Ecosystem", "Land use", " land-use change and forestry", "0105 earth and related environmental sciences", "[SDU.OCEAN]Sciences of the Universe [physics]/Ocean", "Global and Planetary Change", "Ecology", "Atmosphere", "[SDU.OCEAN] Sciences of the Universe [physics]/Ocean", " Atmosphere", "Peat", "Geology", "FOS: Earth and related environmental sciences", "15. Life on land", "carbon sequestration", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "Global Emissions", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "Physical Sciences", "Land use", "[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces", "environment"]}, "links": [{"href": "https://doi.org/10.1007/s10533-023-01091-2"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biogeochemistry", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s10533-023-01091-2", "name": "item", "description": "10.1007/s10533-023-01091-2", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s10533-023-01091-2"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-10-15T00:00:00Z"}}, {"id": "10.1016/bs.aecr.2019.06.001", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:15:34Z", "type": "Report", "created": "2019-07-23", "title": "A multitrophic perspective on biodiversity\u2013ecosystem functioning research", "description": "Concern about the functional consequences of unprecedented loss in biodiversity has prompted biodiversity-ecosystem functioning (BEF) research to become one of the most active fields of ecological research in the past 25 years. Hundreds of experiments have manipulated biodiversity as an independent variable and found compelling support that the functioning of ecosystems increases with the diversity of their ecological communities. This research has also identified some of the mechanisms underlying BEF relationships, some context-dependencies of the strength of relationships, as well as implications for various ecosystem services that mankind depends upon. In this paper, we argue that a multitrophic perspective of biotic interactions in random and non-random biodiversity change scenarios is key to advance future BEF research and to address some of its most important remaining challenges. We discuss that the study and the quantification of multitrophic interactions in space and time facilitates scaling up from small-scale biodiversity manipulations and ecosystem function assessments to management-relevant spatial scales across ecosystem boundaries. We specifically consider multitrophic conceptual frameworks to understand and predict the context-dependency of BEF relationships. Moreover, we highlight the importance of the eco-evolutionary underpinnings of multitrophic BEF relationships. We outline that FAIR data (meeting the standards of findability, accessibility, interoperability, and reusability) and reproducible processing will be key to advance this field of research by making it more integrative. Finally, we show how these BEF insights may be implemented for ecosystem management, society, and policy. Given that human well-being critically depends on the multiple services provided by diverse, multitrophic communities, integrating the approaches of evolutionary ecology, community ecology, and ecosystem ecology in future BEF research will be key to refine conservation targets and develop sustainable management strategies.", "keywords": ["580", "Biodiversity change", "0301 basic medicine", "570", "0303 health sciences", "Geography & travel", "577", "Food web", "Spatial scaling", "910", "15. Life on land", "ddc:910", "Ecosystem functions", "Management", "[SDE.BE] Environmental Sciences/Biodiversity and Ecology", "03 medical and health sciences", "Eco-evolution", "13. Climate action", "11. Sustainability", "Multifunctionality", "Landscape", "info:eu-repo/classification/ddc/910", "[SDE.BE]Environmental Sciences/Biodiversity and Ecology", "Real-world biodiversity change"]}, "links": [{"href": "https://doi.org/10.1016/bs.aecr.2019.06.001"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/bs.aecr.2019.06.001", "name": "item", "description": "10.1016/bs.aecr.2019.06.001", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/bs.aecr.2019.06.001"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-01-01T00:00:00Z"}}, {"id": "10.1016/j.srs.2024.100118", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:17:51Z", "type": "Journal Article", "created": "2024-01-28", "title": "Satellite-based soil organic carbon mapping on European soils using available datasets and support sampling", "description": "Soil organic carbon (SOC) plays a major role in the global carbon cycle and is an important factor for soil health and fertility. Accurate mapping of SOC and other influencing parameters are crucial to guide the optimization of agricultural land management to maintain and restore soil health, to increase soil fertility, and thus to quantify its potential for sequestering CO2. Remote sensing and machine learning techniques offer promising approaches for predicting SOC distribution. In this study, we used remote sensing data and machine learning algorithms to map SOC at regional to large scale, which we then combined with temporospatial and spectral signature-based soil sampling to integrate local ground measurements. A rigorous validation approach was performed where several independent unseen datasets with a high number of samples were used, which additionally involved densely sampled fields. We found that our approach could predict SOC with an average percentage error of less than 10\u00a0% with an R2 of 0.91 using support sampling on croplands located on mineral soils, demonstrating the potential of remote sensing, machine learning, and specific ground measurements for mapping SOC. Our results suggest that this approach could make small carbon differences measurable and inform carbon sequestration efforts and improve our understanding of the impacts of land use and field management practices on soil carbon cycling.", "keywords": ["2. Zero hunger", "Physical geography", "Precision agriculture", "Science", "Q", "04 agricultural and veterinary sciences", "Remote sensing", "15. Life on land", "01 natural sciences", "GB3-5030", "13. Climate action", "Soil health", "Machine learning", "Soil carbon mapping", "0401 agriculture", " forestry", " and fisheries", "Soil carbon sequestration", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.srs.2024.100118"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Science%20of%20Remote%20Sensing", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.srs.2024.100118", "name": "item", "description": "10.1016/j.srs.2024.100118", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.srs.2024.100118"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-06-01T00:00:00Z"}}, {"id": "78de6d14-264c-4c00-9908-2428a6cd55f3", "type": "Feature", "geometry": {"type": "Polygon", "coordinates": [[[10.59, 53.11], [10.59, 53.81], [12.37, 53.81], [12.37, 53.11], [10.59, 53.11]]]}, "properties": {"themes": [{"concepts": [{"id": "geoscientificInformation"}], "scheme": "https://standards.iso.org/iso/19139/resources/gmxCodelists.xml#MD_TopicCategoryCode"}, {"concepts": [{"id": "Versorgungswirtschaft und staatliche Dienste"}, {"id": "Bodennutzung"}, {"id": "Boden"}], "scheme": "GEMET - INSPIRE themes, version 1.0"}], "updated": "2025-11-06", "type": "Dataset", "created": "2010-01-01", "language": "ger", "externalIds": [{"value": "."}], "title": "Urban planning in the district of Ludwigslust-Parchim (for WFS)", "description": "Urban planning in the district of Ludwigslust-Parchim", "formats": [{"name": "shp"}], "keywords": ["inspireidentifiziert", "infoMapAccessService", "Landkreis Ludwigslust-Parchim", "Geoportal", "Geodaten", "Bauen", "Staedtebauliche Bodenordnung", "Versorgungswirtschaft und staatliche Dienste", "Bodennutzung", "Boden"], "contacts": [{"name": "Geodatenmanagement", "organization": "Landkreis Ludwigslust-Parchim", "position": "GeoAdmin", "roles": ["pointOfContact"], "phones": [{"value": "+49 3871 722-6218"}], "emails": [{"value": "geodatenmanagement@kreis-lup.de"}], "addresses": [{"deliveryPoint": ["Postfach 12 63"], "city": "Parchim", "administrativeArea": "Mecklenburg-Vorpommern", "postalCode": "19362", "country": "Germany"}], "links": [{"href": null}]}], "title_alternate": "Bodenordnung Landkreis Ludwigslust-Parchim"}, "links": [{"href": "https://geoportal.kreis-lup.de/ows/masterportal/bodenordnung-lup?", "rel": "information"}, {"rel": "self", "type": "application/geo+json", "title": "78de6d14-264c-4c00-9908-2428a6cd55f3", "name": "item", "description": "78de6d14-264c-4c00-9908-2428a6cd55f3", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/78de6d14-264c-4c00-9908-2428a6cd55f3"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-11-06T00:00:00Z"}}, {"id": "00fcaa98-fb45-4696-a450-c5dcb1a480d8", "type": "Feature", "geometry": null, "properties": {"updated": "2025-09-02T09:54:15", "type": "Dataset", "language": "de", "title": "INSPIRE-WFS Soil / Sorptionsverm\u00f6gen im effektiven Wurzelraum BB", "description": "Der interoperable INSPIRE-WFS ist ein Downloaddienst, der Daten im Annex-Schema Boden (abgeleitet aus dem origin\u00e4ren Datensatz: Sorptionsverm\u00f6gen im effektiven Wurzelraum Brandenburg) bereitstellt. Er gibt einen \u00dcberblick \u00fcber die Sorptionskapazit\u00e4t im effektiven Wurzelraum der B\u00f6den Brandenburgs. Diese Karte basiert auf den Legendeneinheiten der Boden\u00fcbersichtskarte (B\u00dcK300) mit entsprechender Zuordnung von parametrisierten Fl\u00e4chenbodenformen. Diese stellen je Legendeneinheit eine Bodenformengesellschaft dar. Die einzelnen (Fl\u00e4chen-)Bodenformen wurden mit Parametern belegt, einschlie\u00dflich der entsprechenden Werte zur Kationenaustauschkapazit\u00e4t (KAK), die durch Gel\u00e4nde- und Laboruntersuchungen bestimmt wurden. Gleiche Horizont-Substrat-Kombinationen wurden zusammengefasst und die entsprechenden Parameter statistisch abgeleitet. Die Abfolge von Horizont-Substrat-Kombinationen in den Fl\u00e4chenbodenformen mit ihren KAK-Werten bildeten die Grundlage f\u00fcr die Berechnung des Sorptionskapazit\u00e4t im effektiven Wurzelraum (s. Hennings 2000, Verkn\u00fcpfungsregel 2.3). 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, 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 / Sorptionsverm\u00f6gen im effektiven Wurzelraum Brandenburg is a download service that delivers data in the annex schema Soil (derived from the original data set: Adsorption capacity in the effective root zone Brandenburg). It provides an overview of the adsorption capacity in the effective root zone of the soils in Brandenburg. The map is based on the legend units of the soil map (B\u00dcK300) with corresponding assignment of parameterized soil forms. These represent one soil form society per legend unit. The single soil forms were assigned with parameters, including the corresponding values for cation exchange capacity (CEC), which were determined by field and laboratory investigations. Identical horizon-substrate combinations were summarized and the corresponding parameters were statistically derived. The sequence of horizon-substrate combinations in the soil forms with their CEC values formed the basis for the calculation of the sorption capacity in the effective root zone (see Hennings 2000, method 2.3). 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, 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", "cation-exchange-capacity", "de", "depthinterval", "derivedsoilprofile", "geologie", "infofeatureaccessservice", "inspireidentifiziert", "interoperabel", "interoperability", "kationenaustauschkapazita\u0308t", "oberboden", "om_observation", "opendata", "process", "soil", "soilbody", "soilderivedobject", "soillayer", "sorptioncapacityinrootzonedepth", "sorptioncapacityinrootzonedepthwithorganicsurfacelayer", "sorptionsvermo\u0308gen", "sorptionsvermo\u0308gen-im-effektiven-wurzelraum-brandenburg", "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%3D00fcaa98-fb45-4696-a450-c5dcb1a480d8"}, {"href": "https://inspire.brandenburg.de/services/so_sorption_wfs?REQUEST=GetCapabilities&SERVICE=WFS"}, {"href": "https://isk.geobasis-bb.de/geodienste/Sonstiges/Hilfe_Nutzung_Downloaddienst.pdf"}, {"href": "http://data.europa.eu/88u/dataset/00fcaa98-fb45-4696-a450-c5dcb1a480d8~~1"}, {"rel": "self", "type": "application/geo+json", "title": "00fcaa98-fb45-4696-a450-c5dcb1a480d8", "name": "item", "description": "00fcaa98-fb45-4696-a450-c5dcb1a480d8", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/00fcaa98-fb45-4696-a450-c5dcb1a480d8"}, {"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": "01864187-9c89-45e1-8a4a-dde3f853e982", "type": "Feature", "geometry": {"type": "Polygon", "coordinates": [[[8.09, 54.56], [8.09, 57.75], [15.15, 57.75], [15.15, 54.56], [8.09, 54.56]]]}, "properties": {"themes": [{"concepts": [{"id": "environment"}], "scheme": "https://standards.iso.org/iso/19139/resources/gmxCodelists.xml#MD_TopicCategoryCode"}, {"concepts": [{"id": "Jord"}], "scheme": "GEMET - INSPIRE themes, version 1.0"}, {"concepts": [{"id": "National"}], "scheme": "Spatial scope"}], "updated": "2024-10-16T12:17:47.5062094Z", "type": "Dataset", "created": "1900-01-01", "language": "dan", "title": "Phosphorus mapping of arable land and water bodies in Denmark", "description": "Tab af fosfor (P) til vandmilj\u00f8et med en r\u00e6kke transportveje er opgjort p\u00e5 grundlag af en omfattende indsamling af nye data suppleret af eksisterende data og udvikling af en r\u00e6kke modeller. Der er lavet et samlet kortv\u00e6rk, der viser risikoomr\u00e5der for fosfortab til overfladevand. I kortet med fosforkortl\u00e6gning af dyrkningsjord er kortlagt de landbrugsarealer, hvor risikoen for fosfortab er st\u00f8rst.\nDen samlede kortl\u00e6gning findes p\u00e5 milj\u00f8GIS: https://miljoegis.mim.dk/spatialmap?profile=fosfor_kortlaegning_dk", "formats": [{"name": "GML"}, {"name": "OGC:WFS"}, {"name": "OGC:WMS-1.3.0-http-get-capabilities"}], "keywords": ["INSPIRE", "mim2geodatainfo", "Jord", "National"], "contacts": [{"name": "MST - Hav- og vandmilj\u00f8", "organization": "Milj\u00f8styrelsen", "position": "Dataansvarlig", "roles": ["owner"], "phones": [{"value": null}], "emails": [{"value": "mst@mst.dk"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": "Danmark"}], "links": [{"href": null}]}, {"name": null, "organization": "Milj\u00f8styrelsen", "position": "Fagligt ansvarlig", "roles": ["pointOfContact"], "phones": [{"value": null}], "emails": [{"value": "mst@mst.dk"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": "Denmark"}], "links": [{"href": null}]}], "denominator": "10000"}, "links": [{"rel": "self", "type": "application/geo+json", "title": "01864187-9c89-45e1-8a4a-dde3f853e982", "name": "item", "description": "01864187-9c89-45e1-8a4a-dde3f853e982", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/01864187-9c89-45e1-8a4a-dde3f853e982"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date-time": "2024-10-16T12:17:47Z"}}, {"id": "044835c8-a185-4ddc-a8a0-559a1a6303c0-envidat", "type": "Feature", "geometry": null, "properties": {"updated": "2025-07-10T09:35:00Z", "type": "Dataset", "language": "en", "title": "Biogeochemical data from a transplantation experiment of monolith soil turfs along an altitudinal gradient to simulate climate change scenarios", "description": "Silvopastoral systems are highly productive and combine long-term wood production with annual provision of forage for livestock. In the Swiss Jura Mountains these systems are a key component of the landscape. As in other cold biomes, climate change can potentially accelerate landscape change within these historically sustainable systems.  In order to anticipate the evolution of subalpine wooded pasture ecosystems under future climate and land-use changes, this project focused on the interplay between soil, vegetation and climate. It was aimed at providing experimental evidence for chief ecosystem processes, with emphasis on the quality of the ecosystem services provided. The main interest was placed on vegetation turf resistance to climate change along an unwooded \u2013 sparsely wooded - densely wooded pasture gradient (land-use intensity), where plant productivity, diversity and succession along with rates of carbon cycling and microbial activity provided measures of ecosystem functioning at both plot and landscape level.  Experimental transplantation of monolith soil turfs to lower altitudes allowed to simulate soil warming and reduced annual precipitation. In order to simulate a year-round warmer and drier climate the natural climate variation along an altitudinal gradient was used as a proxy. The aim was to simulate realistic climate change scenarios for the second half of the 21st century predicted by the IPCC report and downscaled for Switzerland providing regionalized interpolated projections integrating therein trends for temperature increase and precipitation decrease. By using permanent meteorological stations within the network of the Federal Office of Meteorology and Climatology (MeteoSwiss), we obtained high resolution regional data on the variation of mean annual temperature (MAT) and mean annual precipitation (MAP) in relation to altitude in the Swiss Jura Mountains. We observed a general increase of +0.5 K in MAT and a decrease of -20 % MAP for each 100 m decrease in altitude along the SE slope of the Swiss Jura Mountains. These relationships served for the selection of the transplantation sites such that in comparison to a control site at 1350 m a.s.l. (Combe des Amburnex, N 46\u00b054\u2019, E 6\u00b023\u2019) a +2 K MAT and -20 % MAP was achieved at 1010 m a.s.l. (Saint-George, N 46\u00b052\u2019, E 6\u00b026\u2019), a +4 K MAT and -40 % MAP at 570 m a.s.l., (Arboretum d\u2019Aubonne, N 46\u00b051\u2019, E 6\u00b037\u2019), and a +5 K MAT and -50 % MAP at 395 m a.s.l. (Les Bois Chamblard, N 46\u00b047\u2019, E 6\u00b041\u2019). The two stations at 1010 m a.s.l. and 570 m a.s.l. corresponded to the IPCC scenario A1B for a moderate increase in greenhouse gas emissions and to scenario A2 for a high increase in greenhouse gas emissions, respectively. The station at 395 m a.s.l. was chosen to represent an extreme scenario with climate variables lying at the positive tail distribution of model predictions under the A2 scenario.  Soil cores were assembled into rectangular PVC boxes of 60 \uf0b4 80 cm2 size and of 35 cm height. All mesocosms were dug down to surface level into previously prepared trenches in the ground thus preventing lateral heat exchange with the atmosphere. Since at each site the mesocosms were placed in a common garden with no light interception, mesocosms with turfs from the two wooded pastures were shaded from direct sun light to simulate the natural light conditions in the corresponding habitats. Each mesocosm was equipped with a drainage system and was connected to a water tank thus representing a zero potential lysimeter collecting soil solution and precipitation/snowmelt runoff. ECH2O EC-TM sensor probes coupled to Em50 data-loggers (Decagon Devices, Inc., USA) recorded soil temperature and volumetric water content in each mesocosm at the top-soil (0 to -3 cm) every minute and data were averaged over one hour intervals. Climate parameters at each transplantation site were monitored continuously throughout the experiment by means of automated weather stations (Sensor Scope S\u00e0rl, Switzerland), measuring rain precipitation (non-heated tipping bucket gauges) and air temperature and humidity 2 m above the ground surface at one minute intervals.  A list of above- and belowground variables were measured to assess the resilience of biogeochemical processes, plant productivity, tree regeneration, and carbon sequestration for each respective land-use practice. Furthermore, the experimental data were used to improve on (parameterization) the existing spatially explicit, dynamic model WoodPaM and refine the model\u02bcs climatic and land-use variables so that different scenarios of climate change and land use change could be simulated. Natural and management induced disturbance patterns were incorporated into the model.  The data have been made available within the project CCES Mounted. The climate stations Sensorscope are still in use within the project CLIMARBRE (Wald und Klimawandel, WSL/BAFU).  #References  1. Puissant, J., C\u00e9cillon, L., Mills, R.T.E., Robroek, B.J.M. Gavazov, K., De Danieli, S., Spiegelberger, T., Buttler, A., Brun, J.J. 2015. Seasonal influence of climate manipulation on microbial community structure and function in mountain soils. Soil Biology and Biochemistry 80: 296\u2013305. 2. Mills, R., K. Gavazov, T. Spiegelberger, D. Johnson and A. Buttler 2014. Diminished soil functions occur under simulated climate change in a sup-alpine pasture, but heterotrophic temperature sensitivity indicates microbial resilience. Science of the Total Environment, vol. 473\u2013474(0): 465-472. 3. Gavazov, K., Spiegelberger, T. and Buttler, A. 2014. Transplantation of subalpine wood-pasture turfs along a natural climatic gradient reveals lower resistance of unwooded pastures to climate change compared to wooded ones. Oecologia\u00a0(174)\u00a0: 1425-1435. 4. Peringer A., Siehoff S., Ch\u00e9telat J., Spiegelberger T., Buttler A. & Gillet F. 2013. Past and future landscape dynamics in pasture-woodlands of the Swiss Jura Mountains under climate change. Ecology and Society, 18, 3: 11. DOI: 10.5751/ES-05600-180311. [online] URL: http://www.ecologyandsociety.org/vol18/iss3/art11/ 5. Gavazov, K. S., A. Peringer, A. Buttler, F. Gillet and T. Spiegelberger. 2013. Dynamics of Forage Production in Pasture-woodlands of the Swiss Jura Mountains under Projected Climate Change Scenarios. Ecology and Society 18 (1): 38. [online] URL: http://www.ecologyandsociety.org/vol18/iss1/art38/", "formats": [{"name": "ZIP"}], "keywords": ["biogeochemisty", "ch", "climate-change", "silvopastoral-systems", "soil", "transplantation-experiment"], "contacts": [{"organization": "Alexandre Buttler", "roles": ["creator"]}, {"organization": "https://envidat.ch/#/about", "roles": ["publisher"]}]}, "links": [{"href": "https://www.envidat.ch/#/metadata/mountland-jura"}, {"href": "https://www.envidat.ch/dataset/mountland-jura/resource/79f4c0b1-cf58-44da-88a7-0e579030894e"}, {"href": "http://data.europa.eu/88u/dataset/044835c8-a185-4ddc-a8a0-559a1a6303c0-envidat"}, {"rel": "self", "type": "application/geo+json", "title": "044835c8-a185-4ddc-a8a0-559a1a6303c0-envidat", "name": "item", "description": "044835c8-a185-4ddc-a8a0-559a1a6303c0-envidat", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/044835c8-a185-4ddc-a8a0-559a1a6303c0-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": "02210bb3-1c51-4c2c-a665-a696286b945c-bundesamt-fur-landwirtschaft-blw", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:13:48Z", "type": "Dataset", "title": "Erosion risk map for arable land \u2013 qualitative classification", "description": "Erosion risk map for arable land \u2013 qualitative classification (Federal Office for Agriculture) Erosion risk map for arable land in Switzerland in a 2x2-metre grid based on SwissALTI3D and cantonal surface-area data on arable land (status 2021). The map shows the potential qualitative erosion risk. The overall rating is allocated to one of three risk levels (no risk; risk; high risk) without taking account of soil use or management method. The long-term mean soil erosion is calculated on the basis of the universal soil loss equation (USLE).", "formats": [{"name": "HTML"}], "keywords": ["bgdi-bundesgeodaten-infrastruktur", "boden", "bodenerosion", "ch", "e-geoch", "erosion", "erosion-du-sol", "erosione", "erosione-del-suolo", "fsdi-federal-spatial-data-infrastructure", "ifdg-infrastruttura-federale-dei-dati-geografici", "ifdg-linfrastructure-federale-de-donnees-geographiques", "soil", "soil-erosion", "sol", "suolo"], "contacts": [{"organization": "info@blw.admin.ch", "roles": ["creator"]}, {"organization": "https://www.blw.admin.ch/blw/de/home.html?_organization=705", "roles": ["publisher"]}]}, "links": [{"href": "https://data.geo.admin.ch/browser/index.html#/collections/ch.blw.erosion"}, {"href": "https://map.geo.admin.ch/?layers=ch.blw.erosion"}, {"href": "https://wms.geo.admin.ch/?SERVICE=WMS&VERSION=1.3.0&REQUEST=GetCapabilities&lang=de"}, {"href": "https://wmts.geo.admin.ch/EPSG/3857/1.0.0/WMTSCapabilities.xml?lang=de"}, {"href": "https://www.blw.admin.ch/blw/de/home/nachhaltige-produktion/umwelt/boden.html"}, {"href": "http://data.europa.eu/88u/dataset/02210bb3-1c51-4c2c-a665-a696286b945c-bundesamt-fur-landwirtschaft-blw"}, {"rel": "self", "type": "application/geo+json", "title": "02210bb3-1c51-4c2c-a665-a696286b945c-bundesamt-fur-landwirtschaft-blw", "name": "item", "description": "02210bb3-1c51-4c2c-a665-a696286b945c-bundesamt-fur-landwirtschaft-blw", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/02210bb3-1c51-4c2c-a665-a696286b945c-bundesamt-fur-landwirtschaft-blw"}, {"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": "02543d0a-f43a-4ab7-886a-c748d714a9e6-bundesamt-fur-umwelt-bafu", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:13:49Z", "type": "Dataset", "title": "Geochemical soil atlas of Switzerland: Thallium", "description": "Interpolierte Element-Konzentrationen (mg/kg Feinerde) in den Oberb\u00f6den (0\u201320 cm) der Schweiz. F\u00fcr die Ordinary Kriging Interpolationen (1 km x 1 km) wurden Messdaten von insgesamt 1'201 Standorten des Biodiversit\u00e4tsmonitorings Schweiz, der Nationalen Bodenbeobachtung und des europ\u00e4ischen geochemischen Bodenatlas ber\u00fccksichtigt. Die Element-Konzentrationen wurden in K\u00f6nigswasser Aufschl\u00fcssen (HNO\u2083:HCl:H\u2082O) von getrockneten (40\u00b0C), gesiebten (< 2 mm) und anschliessend gemahlenen Bodenproben mittels induktiv gekoppelter Plasma Massenspektrometrie analysiert. Standorte mit bekannter anthropogener \u00dcberpr\u00e4gung der Element-Konzentrationen (Punktquellen) wurden vorg\u00e4ngig ausgeschlossen. Bei den Ergebnissen des geochemischen Bodenatlas handelt es sich um eine Momentaufnahme der Element-Konzentrationen in den Oberb\u00f6den der Schweiz (Probenahmezeitraum 2011\u20132015). Die interpolierten Karten dienen der verbesserten Visualisierung von Regionen mit erh\u00f6hten resp. tiefen Konzentrationen. Es k\u00f6nnen daraus jedoch keine parzellenscharfen Informationen oder definitive R\u00fcckschl\u00fcsse auf die Geologie, die Bioverf\u00fcgbarkeit, die prozentualen Verteilung der geogenen und anthropogenen Quellen sowie die Belastung des Bodens abgeleitet werden. Zitat Publikation: J. E. Reusser, M. B. Siegenthaler, L. H. E. Winkel, D. W\u00e4chter, R. Kretzschmar, R. G. Meuli: Geochemischer Bodenatlas der Schweiz. Agroscope; Z\u00fcrich, 2023.", "formats": [{"name": "HTML"}], "keywords": ["atlante", "atlas", "bgdi-bundesgeodaten-infrastruktur", "biogeochemie", "biogeochemistry", "biogeochimica", "biogeochimie", "boden", "bodeneigenschaften", "bodenkartierung", "bund", "cartographie-des-sols", "ch", "confederation", "confederazione", "fsdi-federal-spatial-data-infrastructure", "heavy-metal", "ifdg-infrastruttura-federale-dei-dati-geografici", "ifdg-linfrastructure-federale-de-donnees-geographiques", "interpolation", "interpolazione", "mappatura-del-suolo", "metal-lourd", "metal-toxique", "metalli-tossici", "metallo-pesante", "proprieta-del-suolo", "proprietes-du-sol", "schwermetall", "soil", "soil-mapping", "soil-properties", "sol", "suolo", "toxic-metal", "toxische-metalle"], "contacts": [{"organization": "boden@bafu.admin.ch", "roles": ["creator"]}, {"organization": "https://opendata.swiss/organization/bundesamt-fur-umwelt-bafu", "roles": ["publisher"]}]}, "links": [{"href": "https://data.geo.admin.ch/browser/index.html#/collections/ch.bafu.geochemischer-bodenatlas_schweiz_thallium/items/geochemischer-bodenatlas_schweiz_thallium"}, {"href": "https://map.geo.admin.ch/?layers=ch.bafu.geochemischer-bodenatlas_schweiz_thallium"}, {"href": "https://wms.geo.admin.ch/?SERVICE=WMS&VERSION=1.3.0&REQUEST=GetCapabilities&lang=de"}, {"href": "https://wmts.geo.admin.ch/EPSG/3857/1.0.0/WMTSCapabilities.xml?lang=de"}, {"href": "https://www.agroscope.admin.ch/agroscope/de/home/themen/umwelt-ressourcen/boden-gewaesser-naehrstoffe/nabo/ergaenzende-untersuchungen/geochemischer-bodenatlas.html"}, {"href": "http://data.europa.eu/88u/dataset/02543d0a-f43a-4ab7-886a-c748d714a9e6-bundesamt-fur-umwelt-bafu"}, {"rel": "self", "type": "application/geo+json", "title": "02543d0a-f43a-4ab7-886a-c748d714a9e6-bundesamt-fur-umwelt-bafu", "name": "item", "description": "02543d0a-f43a-4ab7-886a-c748d714a9e6-bundesamt-fur-umwelt-bafu", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/02543d0a-f43a-4ab7-886a-c748d714a9e6-bundesamt-fur-umwelt-bafu"}, {"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": "02de5058-3b3b-421f-a1fc-31e3885fadad-bundesamt-fur-umwelt-bafu", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:13:49Z", "type": "Dataset", "title": "Geochemical soil atlas of Switzerland: Uranium", "description": "Interpolated uranium concentrations (mg/kg fine earth) in the upper soils (0-20 cm) of Switzerland. For the Ordinary Kriging Interpolations (1 km x 1 km), measurement data from a total of 1,201 sites of the Swiss Biodiversity Monitoring System, the National Soil Observation System and the European Soil Geochemical Atlas were taken into account. Element concentrations were analyzed in aqua regia outcrop (HNO3:HCl:H2O) from dried (40\u00b0C), sieved (< 2 mm) and subsequently ground soil samples using inductively coupled plasma mass spectrometry. Sites with known anthropogenic over-embossing of element concentrations (point sources) were excluded in advance. The results of the soil geochemical atlas are a snapshot of the element concentrations in the topsoils of Switzerland (sampling period 2011-2015). The interpolated maps serve to improve the visualization of regions with elevated or low concentrations. However, no parcel-sharp information or definitive conclusions on the geology, bioavailability, the percentage distribution of geogenous and anthropogenic sources as well as the load on the soil can be derived from this. Quotation of Publication: J. E. Reusser, M. B. Siegenthaler, L. H. E. Winkel, D. W\u00e4chter, R. Kretzschmar, R. G. Meuli: Geochemical soil atlas of Switzerland. Agroscope, Zurich, 2023.", "formats": [{"name": "HTML"}], "keywords": ["atlante", "atlas", "bgdi-bundesgeodaten-infrastruktur", "biogeochemie", "biogeochemistry", "biogeochimica", "biogeochimie", "boden", "bodeneigenschaften", "bodenkartierung", "bund", "carico-da-metalli-pesanti", "cartographie-des-sols", "ch", "charge-en-metaux-lourds", "confederation", "confederazione", "fsdi-federal-spatial-data-infrastructure", "heavy-metal-load", "ifdg-infrastruttura-federale-dei-dati-geografici", "ifdg-linfrastructure-federale-de-donnees-geographiques", "interpolation", "interpolazione", "mappatura-del-suolo", "metal-toxique", "metalli-tossici", "proprieta-del-suolo", "proprietes-du-sol", "schwermetallbelastung", "soil", "soil-mapping", "soil-properties", "sol", "suolo", "toxic-metal", "toxische-metalle"], "contacts": [{"organization": "boden@bafu.admin.ch", "roles": ["creator"]}, {"organization": "https://opendata.swiss/organization/bundesamt-fur-umwelt-bafu", "roles": ["publisher"]}]}, "links": [{"href": "https://data.geo.admin.ch/browser/index.html#/collections/ch.bafu.geochemischer-bodenatlas_schweiz_uran/items/geochemischer-bodenatlas_schweiz_uran"}, {"href": "https://map.geo.admin.ch/?layers=ch.bafu.geochemischer-bodenatlas_schweiz_uran"}, {"href": "https://wms.geo.admin.ch/?SERVICE=WMS&VERSION=1.3.0&REQUEST=GetCapabilities&lang=de"}, {"href": "https://wmts.geo.admin.ch/EPSG/3857/1.0.0/WMTSCapabilities.xml?lang=de"}, {"href": "https://www.agroscope.admin.ch/agroscope/de/home/themen/umwelt-ressourcen/boden-gewaesser-naehrstoffe/nabo/ergaenzende-untersuchungen/geochemischer-bodenatlas.html"}, {"href": "http://data.europa.eu/88u/dataset/02de5058-3b3b-421f-a1fc-31e3885fadad-bundesamt-fur-umwelt-bafu"}, {"rel": "self", "type": "application/geo+json", "title": "02de5058-3b3b-421f-a1fc-31e3885fadad-bundesamt-fur-umwelt-bafu", "name": "item", "description": "02de5058-3b3b-421f-a1fc-31e3885fadad-bundesamt-fur-umwelt-bafu", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/02de5058-3b3b-421f-a1fc-31e3885fadad-bundesamt-fur-umwelt-bafu"}, {"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": "03c3d77e-7126-4d21-813f-2d0efef1c47d", "type": "Feature", "geometry": null, "properties": {"updated": "2025-08-21T10:02:50", "type": "Dataset", "language": "de", "title": "annual leachate rate Brandenburg", "description": "The annual leachate rate (SWR) describes the average amount of leachate in mm/a, estimated by a calculation method (TUB-BGR method), which leaves the soil taking into account the capillary rise downwards. The formed leachate contributes to groundwater regeneration and/or leaves the leachate zone as an intermediate runoff. The leachate rate is a crucial input for water balance calculations or hydrogeological groundwater modelling. It also significantly controls the relocation of harmful substances and nutrients (e.g. Nitrate) in the soil and indirectly influences the site suitability for flora and fauna. Further information can be found here:  http://www.geo.brandenburg.de/ows/htdocs/2021_10_26_Sickerwasserrate_pNAG.pdf", "formats": [{"name": "HTML"}], "keywords": ["High value dataset", "boden", "bodenkunde", "de", "erdbeobachtung-und-umwelt", "grundwasser", "grundwasserschutz", "hydrogeologie", "hydrologie", "opendata", "ressource", "wasser"], "contacts": [{"organization": "Landesamt f\u00fcr Bergbau, Geologie und Rohstoffe Brandenburg (LBGR)", "roles": ["creator"]}]}, "links": [{"href": "https://geo.brandenburg.de/?page=Boden---Auswertungen"}, {"href": "https://inspire.brandenburg.de/services/swrpnag_wcs?REQUEST=GetCapabilities&SERVICE=WCS"}, {"href": "https://inspire.brandenburg.de/services/swrpnag_wms?REQUEST=GetCapabilities&SERVICE=WMS"}, {"href": "http://data.europa.eu/88u/dataset/03c3d77e-7126-4d21-813f-2d0efef1c47d~~1"}, {"rel": "self", "type": "application/geo+json", "title": "03c3d77e-7126-4d21-813f-2d0efef1c47d", "name": "item", "description": "03c3d77e-7126-4d21-813f-2d0efef1c47d", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/03c3d77e-7126-4d21-813f-2d0efef1c47d"}, {"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": "04481ab6-e5ee-4742-a330-88649c17b2ce", "type": "Feature", "geometry": {"type": "Polygon", "coordinates": [[[2.75, 49.45], [2.75, 50.85], [6.5, 50.85], [6.5, 49.45], [2.75, 49.45]]]}, "properties": {"themes": [{"concepts": [{"id": "biota"}], "scheme": "https://standards.iso.org/iso/19139/resources/gmxCodelists.xml#MD_TopicCategoryCode"}, {"concepts": [{"id": "Sol et sous-sol"}, {"id": "Nature et environnement"}, {"id": "Agriculture"}], "scheme": "https://metawal.wallonie.be/thesaurus/theme-geoportail-wallon"}, {"concepts": [{"id": "dynamique naturelle"}, {"id": "sol"}, {"id": "biologie"}], "scheme": "http://geonetwork-opensource.org/gemet-theme"}, {"concepts": [{"id": "biologie du sol"}, {"id": "organisme du sol"}, {"id": "carbone organique"}, {"id": "mod\u00e9lisation"}, {"id": "surveillance de l'environnement"}, {"id": "prairie"}, {"id": "qualit\u00e9 du sol"}, {"id": "donn\u00e9es sur l'\u00e9tat de l'environnement"}, {"id": "type de sol"}, {"id": "conservation du sol"}, {"id": "carbone organique total"}, {"id": "sol"}, {"id": "station de surveillance"}, {"id": "cartographie"}, {"id": "mati\u00e8re organique"}, {"id": "carbone"}, {"id": "for\u00eat"}, {"id": "analyse des sols"}, {"id": "cycle du carbone"}, {"id": "cartogramme"}, {"id": "profil du sol"}, {"id": "utilisation du sol"}, {"id": "r\u00e9seau de mesure"}, {"id": "culture"}, {"id": "stockage"}, {"id": "ressources du sol"}, {"id": "sous-sol"}], "scheme": "http://geonetwork-opensource.org/gemet"}, {"concepts": [{"id": "Open Data"}, {"id": "PanierTelechargementGeoportailNO"}, {"id": "Reporting INSPIRE"}, {"id": "WalOnMapNO"}, {"id": "Extraction_DIG"}, {"id": "BDInfraSIG"}], "scheme": "https://metawal.wallonie.be/thesaurus/infrasig"}, {"concepts": [{"id": "Sols"}], "scheme": "http://inspire.ec.europa.eu/theme"}, {"concepts": [{"id": "R\u00e9gional"}], "scheme": "http://inspire.ec.europa.eu/metadata-codelist/SpatialScope"}, {"concepts": [{"id": "2023/138 - High Value Datasets Regulation"}], "scheme": "http://data.europa.eu/r5r/applicableLegislation"}, {"concepts": [{"id": "Observation de la terre et environnement"}], "scheme": "http://data.europa.eu/bna/asd487ae75"}], "updated": "2024-12-11T12:48:19.626322Z", "type": "Dataset", "created": "2024-10-30", "language": "fre", "title": "INSPIRE - CARBIOSOL - Predicted total organic carbon levels - period 2004-2014 in Wallonia (BE)", "description": "Cette couche de donn\u00e9es INSPIRE reprend les teneurs en Carbone Organique Total dans les sols agricoles du territoire wallon pour la p\u00e9riode 2004-2014.\n\nCette donn\u00e9e conforme INSPIRE est issue de la donn\u00e9e source CARBIOSOL - Teneurs pr\u00e9dites en Carbone organique total - p\u00e9riode 2004-2014.\n\nLa qualit\u00e9 d\u2019un sol peut \u00eatre \u00e9valu\u00e9e gr\u00e2ce \u00e0 l\u2019\u00e9tude de divers param\u00e8tres physiques, chimiques ou biologiques. Parmi ces param\u00e8tres, le carbone organique des sols, qui constitue plus de 50% de la masse de la mati\u00e8re organique du sol, est g\u00e9n\u00e9ralement consid\u00e9r\u00e9 comme l'indicateur principal de la qualit\u00e9 des sols, \u00e0 la fois pour ses fonctions agricoles et environnementales.\n\nLa pr\u00e9sente couche de donn\u00e9es constitue la cartographie des teneurs en carbone organique total (COT) pour les sols sous cultures et prairies permanentes en R\u00e9gion wallonne pour une p\u00e9riode comprise entre 2004 et 2014. La couche a \u00e9t\u00e9 cr\u00e9\u00e9e par m\u00e9thode de mod\u00e9lisation spatiale d\u00e9velopp\u00e9e par l'UCL dans le cadre de la convention CARBIOSOL.\n\nPour plus de d\u00e9tails sur la constitution des couches cartographiques g\u00e9n\u00e9r\u00e9es dans le cadre du projet CARBIOSOL, veuillez-vous r\u00e9f\u00e9rer \u00e0 la fiche de m\u00e9tadonn\u00e9es documentant la s\u00e9rie de couches de donn\u00e9es.\n\nEn chaque pixel, la teneur en carbone organique total (COT) est exprim\u00e9e en gramme de carbone par kilogramme de terre fine s\u00e8che (gC/kg). Le r\u00e9sultat en sortie du mod\u00e8le est une couche raster des teneurs en COT \u00e0 90 m\u00e8tres de r\u00e9solution et spatialement continue sur le territoire agricole wallon.\n\nLes teneurs moyennes en COT observ\u00e9es pour les sols (horizons de surface) sous cultures et prairies permanentes sur la p\u00e9riode 2004-2014 \u00e9taient de 1.30 gC/kg et 3.61 gC/kg respectivement, d\u2019apr\u00e8s la base de donn\u00e9es REQUASUD.\n\nSur cette m\u00eame p\u00e9riode, 22 % des superficies sous cultures pr\u00e9sentaient des teneurs en COT < 1.15 gC kg-1 et 73 % pr\u00e9sentaient des teneurs < 1.5 gC/kg. En de\u00e7\u00e0 de 1.15 gC/kg, le sol est d\u00e9structur\u00e9.\n\nEntre 2004 et 2014, les teneurs en COT des sols pour les deux occupations de sols tendent \u00e0 augmenter du nord-ouest au sud-est, de la r\u00e9gion sablo-limoneuse \u00e0 la r\u00e9gion ardennaise, et \u00e0 rebaisser en r\u00e9gion Jurassique.", "formats": [{"name": "TIFF (.tif"}, {"name": " .tiff)"}, {"name": "WWW:LINK"}, {"name": "OGC:WMS"}, {"name": "atom:feed"}], "keywords": ["Sol et sous-sol", "Nature et environnement", "Agriculture", "dynamique naturelle", "sol", "biologie", "biologie du sol", "organisme du sol", "carbone organique", "mod\u00e9lisation", "surveillance de l'environnement", "prairie", "qualit\u00e9 du sol", "donn\u00e9es sur l'\u00e9tat de l'environnement", "type de sol", "conservation du sol", "carbone organique total", "sol", "station de surveillance", "cartographie", "mati\u00e8re organique", "carbone", "for\u00eat", "analyse des sols", "cycle du carbone", "cartogramme", "profil du sol", "utilisation du sol", "r\u00e9seau de mesure", "culture", "stockage", "ressources du sol", "sous-sol", "Open Data", "PanierTelechargementGeoportailNO", "Reporting INSPIRE", "WalOnMapNO", "Extraction_DIG", "BDInfraSIG", "COT", "COS", "CARBIOSOL", "CARBOSOL", "RSS", "teneur en carbone", "Aardewerk", "CNSW", "COSW", "REQUASUD", "RMSE", "GAM", "Mod\u00e8le Additif G\u00e9n\u00e9ralis\u00e9", "MAG", "Monte-Carlo", "covariable", "CO2", "Digital Soil Mapping", "DTM", "Erreur", "horizon de sol", "Sols", "R\u00e9gional", "2023/138 - High Value Datasets Regulation", "Observation de la terre et environnement"], "contacts": [{"name": null, "organization": "Helpdesk carto du SPW (SPW - Secr\u00e9tariat g\u00e9n\u00e9ral - SPW Digital - D\u00e9partement Donn\u00e9es transversales - Gestion et valorisation de la donn\u00e9e)", "position": null, "roles": ["pointOfContact"], "phones": [{"value": null}], "emails": [{"value": "helpdesk.carto@spw.wallonie.be"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": null}]}, {"name": null, "organization": "Direction de la Protection des Sols (SPW - Agriculture, Ressources naturelles et Environnement - D\u00e9partement du Sol et des D\u00e9chets - Direction de la Protection des Sols)", "position": null, "roles": ["custodian"], "phones": [{"value": null}], "emails": [{"value": "esther.goidts@spw.wallonie.be"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": null}]}, {"name": null, "organization": "Service public de Wallonie (SPW)", "position": null, "roles": ["owner"], "phones": [{"value": null}], "emails": [{"value": "helpdesk.carto@spw.wallonie.be"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": {"url": "https://geoportail.wallonie.be", "protocol": "WWW:LINK", "protocol_url": "", "name": "G\u00e9oportail de la Wallonie", "name_url": "", "description": "G\u00e9oportail de la Wallonie", "description_url": "", "applicationprofile": null, "applicationprofile_url": "", "function": "information"}}]}, {"name": "Caroline Chartin", "organization": "Universit\u00e9 catholique de Louvain - Earth and Life Institute (UCL - ELI)", "position": null, "roles": ["originator"], "phones": [{"value": null}], "emails": [{"value": "caroline.chartin@uclouvain.be"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": null}]}, {"name": null, "organization": "Cellule SIG du SPW ARNE (SPW - Agriculture, Ressources naturelles et Environnement - D\u00e9partement de l'\u00c9tude du milieu naturel et agricole - Direction de la Coordination des Donn\u00e9es)", "position": null, "roles": ["processor"], "phones": [{"value": null}], "emails": [{"value": "sig.dgarne@spw.wallonie.be"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": null}]}, {"name": null, "organization": "R\u00e9seau Qualit\u00e9 Sud (REQUASUD ASBL)", "position": null, "roles": ["originator"], "phones": [{"value": null}], "emails": [{"value": "requasud@cra.wallonie.be"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": null}]}, {"organization": "Universit\u00e9 catholique de Louvain - Earth and Life Institute (UCL - ELI);R\u00e9seau Qualit\u00e9 Sud (REQUASUD ASBL)", "roles": ["creator"]}], "title_alternate": "SO.SoilThemeCoverage.COT__TENEURS_2004_2014", "distancevalue": "90", "distanceuom": "m"}, "links": [{"href": "https://geoportail.wallonie.be/walonmap#PANIER=%5B%7B%22serviceId%22%3A%221%22%2C%22visible%22%3Atrue%2C%22url%22%3A%22https%3A%2F%2Fgeoservices.wallonie.be%2Farcgis%2Frest%2Fservices%2FSOL_SOUS_SOL%2FCARBIOSOL%2FMapServer%2F3%22%2C%22label%22%3A%22CARBIOSOL%20-%20Teneurs%20pr%C3%A9dites%20en%20Carbone%20organique%20total%20-%20p%C3%A9riode%202015-2019%22%2C%22type%22%3A%22AGS_DYNAMIC%22%2C%22metadataUrl%22%3A%22https%3A%2F%2Fgeodata.wallonie.be%2Fdoc%2F04481ab6-e5ee-4742-a330-88649c17b2ce%22%7D%5D", "name": "Application WalOnMap - Toute la Wallonie \u00e0 la carte", "description": "Application cartographique du Geoportail (WalOnMap) qui permet de d\u00e9couvrir les donn\u00e9es g\u00e9ographiques de la Wallonie.", "protocol": "WWW:LINK", "rel": "browsing"}, {"href": "https://geoservices.wallonie.be/geoserver/inspire_so/ows?service=WMS&version=1.3.0&request=GetCapabilities", "name": "INSPIRE - Sols en Wallonie (BE) - Service de visualisation WMS", "protocol": "OGC:WMS", "rel": null}, {"href": "https://geoservices.wallonie.be/inspire/atom/SO_Service.xml", "name": "INSPIRE - Sols en Wallonie (BE) - Service de t\u00e9l\u00e9chargement", "protocol": "atom:feed", "rel": null}, {"href": "https://metawal.wallonie.be/geonetwork/srv/api/records/04481ab6-e5ee-4742-a330-88649c17b2ce/attachments/SO.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": "04481ab6-e5ee-4742-a330-88649c17b2ce", "name": "item", "description": "04481ab6-e5ee-4742-a330-88649c17b2ce", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/04481ab6-e5ee-4742-a330-88649c17b2ce"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"interval": ["2004-01-01T00:00:00Z", "2014-01-01T00:00:00Z"]}}, {"id": "10.1007/s00267-013-0148-z", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:14:26Z", "type": "Journal Article", "created": "2013-08-12", "title": "Effect Of Nutrient Management Planning On Crop Yield, Nitrate Leaching And Sediment Loading In Thomas Brook Watershed", "description": "Government priorities on provincial Nutrient Management Planning (NMP) programs include improving the program effectiveness for environmental quality protection, and promoting more widespread adoption. Understanding the effect of NMP on both crop yield and key water-quality parameters in agricultural watersheds requires a comprehensive evaluation that takes into consideration important NMP attributes and location-specific farming conditions. This study applied the Soil and Water Assessment Tool (SWAT) to investigate the effects of crop and rotation sequence, tillage type, and nutrient N application rate on crop yield and the associated groundwater [Formula: see text] leaching and sediment loss. The SWAT model was applied to the Thomas Brook Watershed, located in the most intensively managed agricultural region of Nova Scotia, Canada. Cropping systems evaluated included seven fertilizer application rates and two tillage systems (i.e., conventional tillage and no-till). The analysis reflected cropping systems commonly managed by farmers in the Annapolis Valley region, including grain corn-based and potato-based cropping systems, and a vegetable-horticulture system. ANOVA models were developed and used to assess the effects of crop management choices on crop yield and two water-quality parameters (i.e., [Formula: see text] leaching and sediment loading). Results suggest that existing recommended N-fertilizer rate can be reduced by 10-25\u00a0%, for grain crop production, to significantly lower [Formula: see text] leaching (P\u00a0>\u00a00.05) while optimizing the crop yield. The analysis identified the nutrient N rates in combination with specific crops and rotation systems that can be used to manage [Formula: see text] leaching while balancing impacts on crop yields within the watershed.", "keywords": ["2. Zero hunger", "Analysis of Variance", "Conservation of Natural Resources", "Geologic Sediments", "Nitrates", "Agriculture", "04 agricultural and veterinary sciences", "Models", " Theoretical", "15. Life on land", "01 natural sciences", "6. Clean water", "Environmental Policy", "Nova Scotia", "13. Climate action", "Water Quality", "Humans", "0401 agriculture", " forestry", " and fisheries", "Fertilizers", "Groundwater", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1007/s00267-013-0148-z"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Environmental%20Management", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s00267-013-0148-z", "name": "item", "description": "10.1007/s00267-013-0148-z", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s00267-013-0148-z"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2013-08-13T00:00:00Z"}}, {"id": "04e12ad1-77b4-45a2-9ed2-2f9aedcc013c", "type": "Feature", "geometry": null, "properties": {"updated": "2025-09-03T08:42:09Z", "type": "Dataset", "language": "de", "title": "INSPIRE-WCS Soil / Konzeptbodenkarten BB", "description": "Der interoperable INSPIRE-WCS ist ein Downloaddienst, der Daten im INSPIRE-Zielschema Boden (abgeleitet aus der origin\u00e4ren Serie: Konzeptbodenkarten Brandenburg) bereitstellt. Er gibt einen \u00dcberblick zum Fl\u00e4chentyp Bodenartgruppe und Fl\u00e4chentyp Genese der B\u00f6den Brandenburgs und ist aktuell das hochaufl\u00f6sendste blattschnittfreie bodenkundliche Kartenwerk des LBGR im Rasterformat, mit einer Aufl\u00f6sung von 10 x 10 m. Datengrundlagen der Karten sind Fl\u00e4chendaten der Bodensch\u00e4tzung, Geologie und verschiedene bodenkundliche Punkt- und Fl\u00e4chendaten.      Die Auswertungen liefern die fachliche Basis sowohl f\u00fcr die Planung und Umsetzung bodenkundlicher Kartierungen, als auch f\u00fcr die Synthese und Ableitung der Bodenfunktions- und -gef\u00e4hrdungsbewertungen. Die G\u00fcte der zugrundeliegenden Konzeptbodenkarten (KBK) hat somit einen hohen Einfluss auf die Qualit\u00e4t der abgeleiteten Produkte. Im Land Brandenburg werden die KBK mit einem regelbasierten Ansatz weitgehend automatisiert softwaretechnisch abgeleitet. Das Verfahren implementiert die bislang analog durchgef\u00fchrten Arbeitsschritte und bildet als \u201eExpertensystem\u201c das Verst\u00e4ndnis \u00fcber die Genese und die Verbreitung der B\u00f6den in Brandenburg weitgehend ab.     Derzeit wird ein robustes Verfahren zum Abgleich laufender Erhebungen mit den \u201ePrognosen\u201c der Konzeptkarten und darauf fu\u00dfend deren systematische \u00dcberpr\u00fcfung und Bewertung erarbeitet. Zuk\u00fcnftig sollen in diesem Verfahren erkannte Defizite systematisch in einem modifizierten Ableitungsregelwerk ber\u00fccksichtigt und die Konzeptbodenkarten fortlaufend aktualisiert werden. Eine ausf\u00fchrliche Legende sowie die Erl\u00e4uterungen der Werte ist zu finden unter: https://isk.geobasis-bb.de/geodienste/lbgr/KBK_Erlaeuterungen.pdf.     Gem\u00e4\u00df der INSPIRE-Datenspezifikation f\u00fcr Soil liegen die Inhalte INSPIRE-konform vor. Der WCS beinhaltet die folgenden Coverages:      - SO.SoilTextureClasses:bft,     - SO.SoilGenesis:gft,     - SO.SoilPedogenesis:pft.     ---      The compliant INSPIRE-WCS is a download service that delivers data in the INSPIRE target schema Soil (derived from the original data series: Concept pedological maps in the State of Brandenburg). It provides an overview of the soil texture classes and soil genesis in the State of Brandenburg and is currently the highest-resolution pedological map of the LBGR in raster format with a resolution of 10 x 10 meters. The maps are based on data from German Soil taxonomy classification, geology and various pedological spatial data.     The evaluations provide the technical basis for the planning and implementation of soil surveys as well as for the synthesis and derivation of soil function and risk assessments. The quality of the underlying Concept pedological maps (KBK) therefore has a major influence on the quality of the derived products. In the State of Brandenburg, the KBK is derived using a largely automated software-based approach. The procedure implements the work steps that have been carried out analogously to date and, as an 'expert system', largely reflects the understanding of the genesis and distribution of soils in Brandenburg.     A robust procedure for comparing current surveys with the 'forecasts' of the KBK and, based on this, their systematic review and evaluation is currently being developed. In the future, deficits identified in this procedure will be systematically taken into account in a modified derivation set of rules and the KBK will be continuously updated. A detailed legend and explanations can be found at: https://isk.geobasis-bb.de/geodienste/lbgr/KBK_Erlaeuterungen.pdf. The content is compliant to the INSPIRE Data Specification on Soil. The WCS includes the following coverages:      - SO.SoilTextureClasses:bft,     - SO.SoilGenesis:gft,     - SO.SoilPedogenesis:pft.", "formats": [{"name": "HTML"}], "keywords": ["boden", "bodenart", "bodendaten", "bodenform", "bodengeologie", "bodengesellschaft", "bodenkarte", "bodenkunde", "bodenscha\u0308tzung", "bodensystematische-einheit", "bodentyp", "brandenburg", "de", "fla\u0308chenbodenform", "genese", "geologie", "infocoverageaccessservice", "inspireidentifiziert", "interoperabel", "interoperability", "interoperable-daten", "konzeptbodenkarte", "konzeptkarte", "opendata", "organisch", "pedogenese", "process", "regional", "soil", "soillayer", "soiltexturegroup", "soiltype", "substratsystematische-einheit", "terrestrisch", "wcs"], "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%3D04e12ad1-77b4-45a2-9ed2-2f9aedcc013c"}, {"href": "https://inspire.brandenburg.de/services/so_kbk_wcs?REQUEST=GetCapabilities&SERVICE=WCS"}, {"href": "https://isk.geobasis-bb.de/geodienste/Sonstiges/Hilfe_Nutzung_Downloaddienst.pdf"}, {"href": "http://data.europa.eu/88u/dataset/04e12ad1-77b4-45a2-9ed2-2f9aedcc013c~~1"}, {"rel": "self", "type": "application/geo+json", "title": "04e12ad1-77b4-45a2-9ed2-2f9aedcc013c", "name": "item", "description": "04e12ad1-77b4-45a2-9ed2-2f9aedcc013c", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/04e12ad1-77b4-45a2-9ed2-2f9aedcc013c"}, {"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": "050793f8-b173-46f3-81ce-ce97b3673187", "type": "Feature", "geometry": null, "properties": {"updated": "2025-03-04T00:00:00Z", "type": "Dataset", "language": "de", "title": "Inspire SH Floor ALKIS", "description": "This dataset provides a data set derived from ALKIS for the INSPIRE topic soil.", "formats": [{"name": "WFS_SRVC"}], "keywords": ["High value dataset", "adv", "adv-inspire-produktspezifikation-version-2.0.0", "adv-ows-basisprofi", "advmis", "alkis", "amtliches-liegenschaftskatasterinformationssystem", "annex_iii", "boden", "de", "erdbeobachtung-und-umwelt", "geobasisdaten", "inspire_sh_boden_alkis", "inspireidentifiziert", "opendata", "regional", "schleswig-holstein", "sh", "wms"], "contacts": [{"organization": "Landesamt f\u00fcr Vermessung und Geoinformation Schleswig-Holstein", "roles": ["creator"]}]}, "links": [{"href": "https://service.gdi-sh.de/SH_INSPIREDOWNLOAD_AIII_SO?service=WFS&version=2.0.0&request=GetCapabilities"}, {"href": "https://service.gdi-sh.de/SH_INSPIREVIEW_AIII_SO?service=WMS&version=1.3.0&request=GetCapabilities"}, {"href": "http://data.europa.eu/88u/dataset/050793f8-b173-46f3-81ce-ce97b3673187~~1"}, {"rel": "self", "type": "application/geo+json", "title": "050793f8-b173-46f3-81ce-ce97b3673187", "name": "item", "description": "050793f8-b173-46f3-81ce-ce97b3673187", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/050793f8-b173-46f3-81ce-ce97b3673187"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"interval": ["2023-04-14T00:00:00Z", "2023-04-14T00:00:00Z"]}}, {"id": "056fedb4-93f8-4c0f-a586-044feea6362c", "type": "Feature", "geometry": null, "properties": {"updated": "2025-09-02T09:57:21", "type": "Dataset", "language": "de", "title": "INSPIRE Soil / Relative binding strength for heavy metals up to 1m tread depth BB", "description": "The interoperable INSPIRE dataset contains data from the LBGR on the relative binding strength for heavy metals up to 1m profile depth Brandenburg, transformed into the INSPIRE target scheme soil. 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 for the depth up to 1 m 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"], "contacts": [{"organization": "Landesamt f\u00fcr Bergbau, Geologie und Rohstoffe Brandenburg (LBGR)", "roles": ["creator"]}]}, "links": [{"href": "https://inspire.brandenburg.de/services/so_boschwerm1m_wfs?REQUEST=GetCapabilities&SERVICE=WFS"}, {"href": "https://inspire.brandenburg.de/services/so_boschwerm1m_wms?REQUEST=GetCapabilities&SERVICE=WMS"}, {"href": "http://data.europa.eu/88u/dataset/056fedb4-93f8-4c0f-a586-044feea6362c~~1"}, {"rel": "self", "type": "application/geo+json", "title": "056fedb4-93f8-4c0f-a586-044feea6362c", "name": "item", "description": "056fedb4-93f8-4c0f-a586-044feea6362c", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/056fedb4-93f8-4c0f-a586-044feea6362c"}, {"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": "053bcacc-0ae4-4e03-9a79-9e0ecb56cd77-bundesamt-fur-umwelt-bafu", "type": "Feature", "geometry": null, "properties": {"updated": "2020-02-27T00:00:00", "type": "Dataset", "title": "Monthly rainfall erosivity (R-factor) maps of Switzerland in MJ mm ha\u207b\u00b9 h\u207b\u00b9 month\u207b\u00b9, February", "description": "<p>Monthly rainfall erosivity maps (R-factor maps) of Switzerland with a spatial resolution of 100 m. The maps show the spatial and seasonal variability of rainfall erosivity in MJ mm ha\u207b\u00b9 h\u207b\u00b9 month\u207b\u00b9. Light shades of blue indicate a low erosive impact of rainfall and dark shades a high impact.</p> <p>The monthly R-factors are based on precipitation measurements from 87 automatic gauging stations with measurement intervals of 10 minutes (average measuring period of 19.5 years per station). The stations cover all agricultural zones in Switzerland. To exclude the influence of snow, temperatures are also recorded at an hourly resolution for 71 stations or are derived from the nearest station.</p> <p>A comparison of the 12 monthly R-factor maps shows that the summer months (June, July and August) have the highest rainfall erosivity values during the year. The Southern Alps (canton of Ticino), the mountain zones of the Northern Alps and parts of the valley zone have particularly high R-factors in this period. A proportion of 62% of Switzerland's annual rainfall erosivity is recorded between June and September. Identifying regions and periods in which rainfall with an increased erosive impact occurs enables targeted erosion control and a better understanding of the dynamics of erosion processes over the course of a year.</p> The development of monthly rainfall erosivity maps of Switzerland is described in detail in 'Regionalization of monthly rainfall erosivity patterns in Switzerland' by Schmidt et al. 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