{"type": "FeatureCollection", "features": [{"id": "18968587-3633-4987-a27a-685862803552~~1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-26T16:37:55Z", "type": "Dataset", "language": "de", "title": "GcB\u00dcK400 \u2014 arsenic in the upper floor", "description": "Arsenic is a semi-metal, ubiquitous and toxic element. It is widely found in nature in various mineralisations as arsenic sulphide or oxide and as copper, nickel and iron arsenate. The average As content of the rocks of the upper continental crust (Clark value) is 2\u00a0mg/kg. In the literature, As levels 20\u00a0mg/kg are described as normal levels, the mean content being about 5\u00a0mg/kg. Among the toxic elements, the arsenic is particularly important due to its large spread of increased content in Saxon soils. The causes are undoubtedly to be found in the geochemical-metallogenetic specialisation of the Fichtelgebirgisch Erzgebirgic Anticlinal Zone. The area-related mean A content of the main rock types (petrogeochemical component) is approximately 13\u00a0mg/kg. The chalkogenic component is of particular importance in the Ore Mountains. In addition to the element enrichment in the mineralisation itself, which was the subject of mining, there was also a large-scale influence on the side rocks or their weathering products (primary and secondary geochemical aureoles). The anthropogenic influence of natural soils is mainly due to the ore treatment plants and the emissions of non-ferrous metalworks. Whereas low levels dominate in the upper soils of North and in parts of central axis (as-poor periglaciary sandy to loamy substrates; L\u00f6ss), a relative enrichment occurs in the weathering soils via solid rocks as a result of the higher petrogenic A component. Important regional anomalies are mainly located in the Freiberg region (Osterzgebirge), the most important site of mining and the smelting of polymetallic ores, as well as in the West Ore Mountains (Aure \u2014 Ehrenfriedersdorf area). The great extent and intensity of the spread of As minerals in polymetallic, tin-tungsten and bi-co-Ni-Ag-U ore formations, as well as their prevention, led to large-scale geogenic and anthropogenic enrichments. Both areas are separated by the north-south-souting Fl\u00f6ha zone, an area in which hardly any ore mineralisations occur and thus the chalkogenic component is rarely developed. Large-area elevated As levels in soils of the Vorerzgebirgssenke (Zwickau \u2014 Chemnitz) are due to the geochemically specialised rotary sediments (including removal products of the Ore Mountains). Particularly high levels of As are common in the meadows of the Freiberger Mulde, Zschopau, Zwickauer Mulde and the United Mulde. Due to the geological process of the removal of soils from the ore-mounted deposits as well as anthropogenic inputs by the ore processing and metallurgy industry, the deposit of the river sediments and swine parts in the flooding areas leads to constant as-enrichment in the floodplains. As a result of the geogenic and anthropogenic processes described above, the test and measure values of the Federal Soil Protection and Contaminant Ordinance (BBodSchV) for arsenic are sometimes exceeded.", "keywords": ["anorganischer-schadstoff", "arsen", "boden", "chemie", "chemisches-element", "de", "geologie", "opendata"]}, "links": [{"href": "https://luis.sachsen.de/boden/geodatendownload.html"}, {"href": "http://data.europa.eu/88u/dataset/18968587-3633-4987-a27a-685862803552~~1"}, {"href": "https://geoportal.sachsen.de/md/18968587-3633-4987-a27a-685862803552"}, {"rel": "self", "type": "application/geo+json", "title": "18968587-3633-4987-a27a-685862803552~~1", "name": "item", "description": "18968587-3633-4987-a27a-685862803552~~1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/18968587-3633-4987-a27a-685862803552~~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": "383c70fe-7169-43da-89da-e45b126f3a70~~1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-26T16:37:56Z", "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": "284d94b4-a0f7-4316-8ab9-5c6bf5facc06", "type": "Feature", "geometry": null, "properties": {"updated": "2025-05-27T00:00:00Z", "type": "Dataset", "language": "de", "title": "GcB\u00dcK400 - Lead in the topsoil", "description": "Lead is a toxic heavy metal and is ubiquitous in the environment due to its multiple industrial uses. The input sources are not limited to the area of ore deposits (mainly lead sulfide and its oxidation minerals). Lead is also introduced into the soil through the smelting of lead, copper and zinc ores, the long-range exhaust gas pollution of motor vehicles (up to 60% of atmospheric pollution until the introduction of lead-free petrol), lead scrap recycling plants, the use of sewage sludge and compost containing heavy metals, and coal incineration plants. For unpolluted soils, a Pb content of 2 to 60 mg/kg is given depending on the initial rock. The average Pb concentration of the upper continental crust (clarke value) is 17 mg/kg, the area-related mean Pb content for the Saxon main rock types is 20 mg/kg. The rocks of Saxony have no or little geochemical specialisation with regard to lead. In the northern and northeastern part of Saxony, relatively low Pb levels occur in the upper soils above the loose sediments of the Cenozoic period (periglacian sands, gravel, loess) and the granodiorites of Lusatia. In the case of loose sediments, the Pb content increases slightly with increasing clay content. The weathered soils above the solid rocks of the Ore Mountains, Vogtland and partly the Elbe zone usually have significantly higher lead contents, which are caused by a relative enrichment in the soil starting rocks. The highest lead-contaminated area in Saxony is the Freiberg area. Due to the economically important polymetallic mineralizations (Pb-Zn-Ag), which are also relatively widespread in terms of area, there was a particularly strong Pb enrichment in the secondary rocks and consequently also in the formation of the soils over the gneiss. In addition, enormous anthropogenic pressures have arisen from the centuries-long smelting of primary ores and, more recently, from the recycling of lead-acid batteries. Particularly high Pb contents occur in the immediate vicinity of the smelter sites, including the main wind directions, in the central part of the quartz-sulphide mineralization and in the floodplains. Further areas with large-scale elevated Pb contents are mainly located in the Osterzgebirge, in an area that extends from Freiberg in a south-easterly direction to the national border in the Altenberg area and in the ore regions of the Central and Westerzgebirge, such as Seiffen, Marienberg - Pobershau, Annaberg, Schneeberg, Schwarzenberg and P\u00f6hla. However, the proportion of Pb minerals in the ores of these regions is significantly lower. Due to the frequent socialization of Pb and As in the mineralizations, the distribution area of the elevated Pb contents in the Osterzgebirge and subordinate in the Westerzgebirge as well as in the floodplains of the Freiberger and Vereinigte Mulde is similar to that of the arsenic. The floodplain soils of the Freiberger Mulde lead extremely high lead contents from the Freiberger reservoir area, which continue into the floodplain soils of the United Mulde in northwestern Germany. The floodplains of the Elbe and the Zwickauer Mulde also have areas with higher lead contents due to geogenous or anthropogenic sources (storage sites, industry) in the catchment area. The lead content of the soils in the Freiberg area and in the floodplain soils of the Freiberger and Vereinigte Mulde exceeds the test and action values of the Federal Soil Protection and Contaminated Sites Ordinance (BBodSchV) in some cases.", "formats": [{"name": "HTML"}], "keywords": ["anorganischer-schadstoff", "blei", "boden", "chemie", "chemisches-element", "de", "geologie", "pb"], "contacts": [{"organization": "Kati Kardel", "roles": ["creator"]}, {"organization": "urn:uuid:ef916bfc-5d97-a8bb-a117-b10e5da45c6b", "roles": ["publisher"]}]}, "links": [{"href": "https://luis.sachsen.de/arcgis/services/boden/gcbuek400/MapServer/WFSServer?request=GetCapabilities&service=WFS"}, {"href": "https://luis.sachsen.de/arcgis/services/boden/gcbuek400/MapServer/WMSServer?request=GetCapabilities&service=WMS"}, {"href": "https://luis.sachsen.de/boden/geochemie.html"}, {"href": "https://luis.sachsen.de/boden/geodatendownload.html"}, {"href": "https://umwelt.sachsen.de/umwelt/infosysteme/fme/data/boden/gcbuek400/Steckbrief_GCH_Blei_2025.pdf"}, {"href": "https://www.boden.sachsen.de/uebersichtskarten-fuer-schadstoffe-in-boeden-23988.html?_cp=%7B%22accordion-content-23994%22%253A%7B%220%22%253Atrue%7D%252C%22previousOpen%22%253A%7B%22group%22%253A%22accordion-content-23994%22%252C%22idx%22%253A0%7D%7D"}, {"href": "http://data.europa.eu/88u/dataset/284d94b4-a0f7-4316-8ab9-5c6bf5facc06"}, {"rel": "self", "type": "application/geo+json", "title": "284d94b4-a0f7-4316-8ab9-5c6bf5facc06", "name": "item", "description": "284d94b4-a0f7-4316-8ab9-5c6bf5facc06", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/284d94b4-a0f7-4316-8ab9-5c6bf5facc06"}, {"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": "1317e09d-baf1-4347-ac16-05007d041c6f", "type": "Feature", "geometry": null, "properties": {"updated": "2025-08-21T11:52:14", "type": "Dataset", "language": "de", "title": "Mean potential nitrate discharge hazard (federal method)", "description": "The mean potential risk of nitrate discharge is used to assess the mean risk of nitrate leaching from the root space of vegetation by leaching soil water. The location of the assessment is the lower bound of the rooted soil layer. The ratio of leachate rate and usable field capacity in the effective root space (nFKWe) first provides the exchange frequency of the plant-available soil water. This is classified in 5 stages (very low \u2013 very high) and gives the pNAG. The characteristic value of the potential risk of nitrate discharge is not suitable for deriving quantitative statements, as use-dependent influencing variables (e.g. crop type, quantities of nitrogen added and removed, autumn nitrate content in the soil) are not taken into account. The calculation of the potential nitrate discharge risk according to the federal method is based on the evaluation method 5.3 (AG Boden, 2000b). Further information can be found here:  https://geo.brandenburg.de/karten/htdocs/21042020_Sickerwasserrate.pdf", "formats": [{"name": "HTML"}], "keywords": ["High value dataset", "boden", "bodenkunde", "bodenschutz", "de", "erdbeobachtung-und-umwelt", "geologie", "grundwasser", "grundwasserschutz", "hydrogeologie", "opendata", "regional", "schadstoff", "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/1317e09d-baf1-4347-ac16-05007d041c6f~~1"}, {"rel": "self", "type": "application/geo+json", "title": "1317e09d-baf1-4347-ac16-05007d041c6f", "name": "item", "description": "1317e09d-baf1-4347-ac16-05007d041c6f", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/1317e09d-baf1-4347-ac16-05007d041c6f"}, {"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": "18968587-3633-4987-a27a-685862803552", "type": "Feature", "geometry": null, "properties": {"updated": "2025-05-27T00:00:00Z", "type": "Dataset", "language": "de", "title": "GcB\u00dcK400 - Arsenic in the topsoil", "description": "Arsenic is a semi-metals, ubiquitous and toxic element. It occurs widely in nature in various mineralizations as arsenic sulfide or oxide and as copper, nickel and iron arsenate. The average as-content of the rocks of the upper continental crust (clarke value) is 2 mg/kg. In the literature, as-contents 20 mg/kg are described as normal contents, with average contents of about 5 mg/kg. Among the toxic elements, arsenic is of particular importance due to its large-scale distribution of elevated contents in Saxon soils. The causes are undoubtedly to be found in the geochemical-metallogenetic specialization of the Fichtelgebirgisch Erzgebirgische Antiklinalzone. The area-related average as-content of the main rock types (petrogeochemical component) is approximately 13 mg/kg. The chalkogenic component is of particular importance in the Ore Mountains. In addition to the element enrichment in the mineralization itself, which was the subject of mining, there was also a large-scale influence on the secondary rocks or their weathering products (primary and secondary geochemical aureoles). The anthropogenic influence on the natural soils is mainly due to the ore processing plants and the emissions from the non-ferrous metal smelters. While in the upper soils of northern and parts of central Saxony low contents dominate (as-poor periglacian sandy to loamy substrates; Loess), a relative accumulation occurs in the weathered soils via solid rocks as a result of the higher petrogenic As component. Significant regional anomalies are found mainly in the Freiberg region (Osterzgebirge), the most important location for mining and smelting polymetallic ores, as well as in the Westerzgebirge (Aue - Ehrenfriedersdorf area). The great extensity and intensity of the distribution of as-minerals in the polymetallic, tin-tungsten and Bi-Co-Ni-Ag-U ore formations as well as their smelting led to large-scale geogenous and anthropogenic enrichments. The two areas are separated by the Northwest-Southeast striking Fl\u00f6ha Zone, an area where there is little ore mineralization and the chacogenic component is rarely developed. Largely elevated as-contents in the soils of the Vorerzgebirgssenke (Zwickau - Chemnitz) are due to the geochemically specialized rotliegendsedimente (including removal products of the Ore Mountains). Particularly high A-levels are found in the floodplain soils of the Freiberger Mulde, Zschopau, Zwickauer Mulde and the Vereinigte Mulde. Due to the geological process of the removal of soils from the ore-mountain deposits as well as anthropogenic inputs by the ore processing and metallurgical industry, there is a constant as-enrichment in the floodplain soils when the river sediments and Schweban parts are deposited in the floodplain areas. As a result of the geogenous and anthropogenic processes described, the test and action values of the Federal Soil Protection and Contaminated Sites Ordinance (BBodSchV) for arsenic are exceeded in some areas in the Ore Mountains and in the floodplain soils of the trough system.", "formats": [{"name": "HTML"}], "keywords": ["anorganischer-schadstoff", "arsen", "boden", "chemie", "chemisches-element", "de", "geologie"], "contacts": [{"organization": "Kati Kardel", "roles": ["creator"]}, {"organization": "urn:uuid:ef916bfc-5d97-a8bb-a117-b10e5da45c6b", "roles": ["publisher"]}]}, "links": [{"href": "https://luis.sachsen.de/arcgis/services/boden/gcbuek400/MapServer/WFSServer?request=GetCapabilities&service=WFS"}, {"href": "https://luis.sachsen.de/arcgis/services/boden/gcbuek400/MapServer/WMSServer?request=GetCapabilities&service=WMS"}, {"href": "https://luis.sachsen.de/boden/geochemie.html"}, {"href": "https://luis.sachsen.de/boden/geodatendownload.html"}, {"href": "https://umwelt.sachsen.de/umwelt/infosysteme/fme/data/boden/gcbuek400/Steckbrief_GCH_Arsen_2025.pdf"}, {"href": "https://www.boden.sachsen.de/uebersichtskarten-fuer-schadstoffe-in-boeden-23988.html?_cp=%7B%22accordion-content-23994%22%253A%7B%220%22%253Atrue%7D%252C%22previousOpen%22%253A%7B%22group%22%253A%22accordion-content-23994%22%252C%22idx%22%253A0%7D%7D"}, {"href": "http://data.europa.eu/88u/dataset/18968587-3633-4987-a27a-685862803552"}, {"rel": "self", "type": "application/geo+json", "title": "18968587-3633-4987-a27a-685862803552", "name": "item", "description": "18968587-3633-4987-a27a-685862803552", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/18968587-3633-4987-a27a-685862803552"}, {"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": "1b29f62f-8730-49a8-8418-a0e589083b66", "type": "Feature", "geometry": null, "properties": {"updated": "2025-09-02T10:10:23Z", "type": "Dataset", "language": "de", "title": "WMS Sickerwasserrate und Nitrataustragsgef\u00e4hrdung des Boden BB (WMS-SWRPNAG)", "description": "Der Darstellungsdienst (WMS) Sickerwasserrate und Nitrataustragsgef\u00e4hrdung des Boden Brandenburg stellt Daten zur Sickerwasserrate (SWR) und die potenzielle Nitrataustragsgef\u00e4hrdung (pNAG) bereit. Die j\u00e4hrliche Sickerwasserrate beschreibt die mit dem TUB-BGR-Verfahren gesch\u00e4tzte mittlere Sickerwassermenge in mm/a, die den Boden unter Ber\u00fccksichtigung des kapillaren Aufstiegs abw\u00e4rts verl\u00e4sst. Das gebildete Sickerwasser tr\u00e4gt zur Grundwasserneubildung bei und/oder verl\u00e4sst die Sickerzone als Zwischenabfluss. Die SWR ist eine entscheidende Eingangsgr\u00f6\u00dfe bei Wasserhaushaltsberechnungen oder der hydrogeologischen Grundwassermodellierung. Ebenso steuert sie ma\u00dfgeblich die Verlagerung von Schad- und N\u00e4hrstoffen (bspw. Nitrat) im Boden und beeinflusst indirekt die Standorteignung f\u00fcr Flora und Fauna. Mit der pNAG wird das Risiko einer Nitratauswaschung aus dem Wurzelraum der Vegetation durch versickerndes Bodenwasser bewertet. Der Ort der Beurteilung ist hierbei die Untergrenze der durchwurzelten Bodenschicht. Der Quotient aus SWR und nutzbarer Feldkapazit\u00e4t im effektiven Wurzelraum (nFKWe) liefert zun\u00e4chst die Austauschh\u00e4ufigkeit des pflanzenverf\u00fcgbaren Bodenwassers. Diese wird in 5 Stufen klassifiziert (sehr gering (1), gering (2), mittel (3), hoch (4), sehr hoch (5)) und ergibt die pNAG. Der Kennwert der pNAG ist zur Ableitung quantitativer Aussagen nicht geeignet, da nutzungsabh\u00e4ngige Einflussgr\u00f6\u00dfen (u.a. Kulturart, zu- und abgef\u00fchrte Stickstoffmengen, herbstliche Nitratgehalte im Boden) nicht ber\u00fccksichtigt werden. Die Landesmethode zur Berechnung der pNAG stellt eine Modifikation der Bundesmethode dar, in der die besondere Gef\u00e4hrdung von grundwassernahen Standorten und Moorstandorten ber\u00fccksichtigt wird. Weiterf\u00fchrende Informationen finden Sie hier: https://geo.brandenburg.de/karten/htdocs/21042020_Sickerwasserrate.pdf     Der WMS beinhaltet die folgenden Layer:      - maximale Sickerwasserrate [max_swr_bund],     - mittlere Sickerwasserrate [avg_swr_bund],     - minimale Sickerwasserrate [min_swr_bund],     - maximale Nitrataustragsgef\u00e4hrdung (Bundesmethode) [max_pnag_bund],     - mittlere Nitrataustragsgef\u00e4hrdung (Bundesmethode) [avg_pnag_bund],     - minimale Nitrataustragsgef\u00e4hrdung (Bundesmethode) [min_pnag_bund],     - maximale Nitrataustragsgef\u00e4hrdung (Landesmethode) [max_pnag_land],     - mittlere Nitrataustragsgef\u00e4hrdung (Landesmethode) [avg_pnag_land],     - minimale Nitrataustragsgef\u00e4hrdung (Landesmethode) [min_pnag_land].", "formats": [{"name": "HTML"}], "keywords": ["bboxbebb", "biogasanlage", "boden", "bodenart", "bodenkunde", "bodenschutz", "bodenu\u0308bersichtskarte", "de", "du\u0308nger", "geologie", "grundwasser", "grundwasserneubildung", "grundwasserschutz", "grundwasserverschmutzung", "hydrologie", "landwirtschaft", "landwirtschaftliche-nutzung", "landwirtschaftsnutzung", "mineral", "na\u0308hrstoff", "niederschlag", "nitrat", "nitrataustrag", "nitrataustragsgefa\u0308hrdung", "nitratbelastung", "nitrit", "oberfla\u0308chengewa\u0308sser", "opendata", "pflanze", "sauerstoff", "schadstoff", "sgd_boden", "sickerwasser", "sickerwasserrate", "stickstoff", "substrate", "trinkwasser", "umwelt", "umweltschutz", "umweltverschmutzung", "wasser", "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%3D1b29f62f-8730-49a8-8418-a0e589083b66"}, {"href": "https://inspire.brandenburg.de/services/swrpnag_wms?REQUEST=GetCapabilities&SERVICE=WMS"}, {"href": "http://data.europa.eu/88u/dataset/1b29f62f-8730-49a8-8418-a0e589083b66~~1"}, {"rel": "self", "type": "application/geo+json", "title": "1b29f62f-8730-49a8-8418-a0e589083b66", "name": "item", "description": "1b29f62f-8730-49a8-8418-a0e589083b66", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/1b29f62f-8730-49a8-8418-a0e589083b66"}, {"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": "2106ff3a-3394-4011-9b31-5cee4d4a9364", "type": "Feature", "geometry": null, "properties": {"updated": "2025-08-27T08:54:43", "type": "Dataset", "language": "de", "title": "Criteria for assessing soil functions 2020 (Environmental Atlas)", "description": "Evaluation criteria for six soil functions based on block and block sub-surfaces, 1 : 5,000 as of 2020.", "formats": [{"name": "HTML"}], "keywords": ["austauschha\u0308ufigkeit-des-bodenwassers", "berlin", "besondere-naturra\u0308umliche-eigenart", "bindungssta\u0308rke-fu\u0308r-schwermetalle", "boden", "bodendaten", "bodenfunktionskriterien", "bo\u0308den", "de", "filtervermo\u0308gen", "geodaten", "grundwasserflurabstand", "inspireidentifiziert", "naturna\u0308he", "na\u0308hrstoffspeichervermo\u0308gen", "na\u0308hrstoffversorgung", "open-data", "opendata", "puffervermo\u0308gen-im-organischen-kohlenstoffhaushalt", "regionale-seltenheit-der-bodengesellschaften", "schadstoffbindungsvermo\u0308gen", "sonderstandorte", "umweltatlas", "versickerung", "wasserversorgung"], "contacts": [{"organization": "Senatsverwaltung f\u00fcr Mobilit\u00e4t, Verkehr, Klimaschutz und Umwelt Berlin", "roles": ["creator"]}]}, "links": [{"href": "https://gdi.berlin.de/services/wfs/ua_boden_3_2020?REQUEST=GetCapabilities&SERVICE=wfs"}, {"href": "https://gdi.berlin.de/services/wfs/ua_boden_austauschh_2020?REQUEST=GetCapabilities&SERVICE=wfs"}, {"href": "https://gdi.berlin.de/services/wfs/ua_boden_bindung_2020?REQUEST=GetCapabilities&SERVICE=wfs"}, {"href": "https://gdi.berlin.de/services/wfs/ua_boden_eigenart_2020?REQUEST=GetCapabilities&SERVICE=wfs"}, {"href": "https://gdi.berlin.de/services/wfs/ua_boden_filter_2020?REQUEST=GetCapabilities&SERVICE=wfs"}, {"href": "https://gdi.berlin.de/services/wfs/ua_boden_kohlenstoffpuffer_2020?REQUEST=GetCapabilities&SERVICE=wfs"}, {"href": "https://gdi.berlin.de/services/wfs/ua_boden_naehrstoff_2020?REQUEST=GetCapabilities&SERVICE=wfs"}, {"href": "https://gdi.berlin.de/services/wfs/ua_boden_naturnaehe_2020?REQUEST=GetCapabilities&SERVICE=wfs"}, {"href": "https://gdi.berlin.de/services/wfs/ua_boden_schadstoff_2020?REQUEST=GetCapabilities&SERVICE=wfs"}, {"href": "https://gdi.berlin.de/services/wfs/ua_boden_seltenheit_2020?REQUEST=GetCapabilities&SERVICE=wfs"}, {"href": "https://gdi.berlin.de/services/wfs/ua_boden_wasserversorgung_2020?REQUEST=GetCapabilities&SERVICE=wfs"}, {"href": "http://data.europa.eu/88u/dataset/2106ff3a-3394-4011-9b31-5cee4d4a9364~~1"}, {"rel": "self", "type": "application/geo+json", "title": "2106ff3a-3394-4011-9b31-5cee4d4a9364", "name": "item", "description": "2106ff3a-3394-4011-9b31-5cee4d4a9364", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2106ff3a-3394-4011-9b31-5cee4d4a9364"}, {"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": "220f70d1-6d8c-4019-a44b-bb1c7cb2e32f", "type": "Feature", "geometry": null, "properties": {"updated": "2025-08-21T10:36:03", "type": "Dataset", "language": "de", "title": "Minimum potential risk of nitrate discharge (country method)", "description": "The minimum potential risk of nitrate discharge is used to assess the minimum risk of nitrate leaching from the root space of vegetation by leaching soil water. The location of the assessment is the lower bound of the rooted soil layer. The ratio of leachate rate and usable field capacity in the effective root space (nFKWe) first provides the exchange frequency of the plant-available soil water. This is classified in 5 stages (very low \u2013 very high) and gives the pNAG. The characteristic value of the potential risk of nitrate discharge is not suitable for deriving quantitative statements, as use-dependent influencing variables (e.g. crop type, quantities of nitrogen added and removed, autumn nitrate content in the soil) are not taken into account. The state method for calculating the potential risk of nitrate discharge is a modification of the federal method, which takes into account the particular risk of groundwater and peatland sites. Further information can be found here: The potential risk of nitrate discharge is used to assess the risk of nitrate leaching from the root space of vegetation by leaching soil water. The location of the assessment is the lower bound of the rooted soil layer. The ratio of leachate rate and usable field capacity in the effective root space (nFKWe) first provides the exchange frequency of the plant-available soil water. This is classified in 5 stages (very low \u2013 very high) and gives the pNAG. The characteristic value of the potential risk of nitrate discharge is not suitable for deriving quantitative statements, as use-dependent influencing variables (e.g. crop type, quantities of nitrogen added and removed, autumn nitrate content in the soil) are not taken into account. The state method for calculating the potential risk of nitrate discharge is a modification of the federal method, which takes into account the particular risk of groundwater and peatland sites. 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Die Ableitung der Bodenfunktion erfolgt nach dem Leitfaden \"Bewertung von B\u00f6den nach ihrer Leistungsf\u00e4higkeit\" (LUBW, 2010).", "formats": [{"name": "WMS_SRVC"}], "keywords": ["boden", "bodenfunktionsbewertung", "bodenscha\u0308tzung", "de", "filter-und-puffer-fu\u0308r-schadstoffe", "opendata"], "contacts": [{"organization": "Regierungspr\u00e4sidium Freiburg - Abteilung 9 Landesamt f\u00fcr Geologie, Rohstoffe und Bergbau, Ref. 93 Landesbodenkunde", "roles": ["creator"]}]}, "links": [{"href": "https://services.lgrb-bw.de/bodschis/services/bs_v?REQUEST=GetCapabilities&SERVICE=WMS&VERSION=1.3.0"}, {"href": "http://data.europa.eu/88u/dataset/2fc64103-6c05-4cfa-b152-4fc55abff27d~~1"}, {"rel": "self", "type": "application/geo+json", "title": "2fc64103-6c05-4cfa-b152-4fc55abff27d", "name": "item", "description": "2fc64103-6c05-4cfa-b152-4fc55abff27d", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2fc64103-6c05-4cfa-b152-4fc55abff27d"}, {"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": "30322159-5f0a-46d3-9d55-54543c307eb1", "type": "Feature", "geometry": null, "properties": {"updated": "2025-08-21T10:33:26", "type": "Dataset", "language": "de", "title": "Maximum potential nitrate discharge hazard (country method)", "description": "The maximum potential risk of nitrate discharge is used to assess the maximum risk of nitrate leaching from the root space of vegetation by leaching soil water. The location of the assessment is the lower bound of the rooted soil layer. The ratio of leachate rate and usable field capacity in the effective root space (nFKWe) first provides the exchange frequency of the plant-available soil water. This is classified in 5 stages (very low \u2013 very high) and gives the pNAG. The characteristic value of the potential risk of nitrate discharge is not suitable for deriving quantitative statements, as use-dependent influencing variables (e.g. crop type, quantities of nitrogen added and removed, autumn nitrate content in the soil) are not taken into account. The state method for calculating the potential risk of nitrate discharge is a modification of the federal method, which takes into account the particular risk of groundwater and peatland sites. Further information can be found here: The potential risk of nitrate discharge is used to assess the risk of nitrate leaching from the root space of vegetation by leaching soil water. The location of the assessment is the lower bound of the rooted soil layer. The ratio of leachate rate and usable field capacity in the effective root space (nFKWe) first provides the exchange frequency of the plant-available soil water. This is classified in 5 stages (very low \u2013 very high) and gives the pNAG. The characteristic value of the potential risk of nitrate discharge is not suitable for deriving quantitative statements, as use-dependent influencing variables (e.g. crop type, quantities of nitrogen added and removed, autumn nitrate content in the soil) are not taken into account. The state method for calculating the potential risk of nitrate discharge is a modification of the federal method, which takes into account the particular risk of groundwater and peatland sites. Further information can be found here:  https://geo.brandenburg.de/karten/htdocs/21042020_Sickerwasserrate.pdf", "formats": [{"name": "HTML"}], "keywords": ["High value dataset", "boden", "bodenkunde", "bodenschutz", "de", "erdbeobachtung-und-umwelt", "geologie", "grundwasser", "grundwasserschutz", "hydrogeologie", "opendata", "regional", "schadstoff", "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/30322159-5f0a-46d3-9d55-54543c307eb1~~1"}, {"rel": "self", "type": "application/geo+json", "title": "30322159-5f0a-46d3-9d55-54543c307eb1", "name": "item", "description": "30322159-5f0a-46d3-9d55-54543c307eb1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/30322159-5f0a-46d3-9d55-54543c307eb1"}, {"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": "37bc2a10-30f6-4d4e-be37-caef1453a30c", "type": "Feature", "geometry": null, "properties": {"updated": "2025-09-02T10:09:37Z", "type": "Dataset", "language": "de", "title": "WCS Sickerwasserrate und Nitrataustragsgef\u00e4hrdung des Bodens BB (WCS-SWRPNAG)", "description": "Der Downloaddienst (WCS) Sickerwasserrate und Nitrataustragsgef\u00e4hrdung des Bodens Brandenburg stellt Daten zur Sickerwasserrate (SWR) und die potenzielle Nitrataustragsgef\u00e4hrdung (pNAG) bereit. Die j\u00e4hrliche Sickerwasserrate beschreibt die mit dem TUB-BGR-Verfahren gesch\u00e4tzte mittlere Sickerwassermenge in mm/a, die den Boden unter Ber\u00fccksichtigung des kapillaren Aufstiegs abw\u00e4rts verl\u00e4sst. Das gebildete Sickerwasser tr\u00e4gt zur Grundwasserneubildung bei und/oder verl\u00e4sst die Sickerzone als Zwischenabfluss. Die SWR ist eine entscheidende Eingangsgr\u00f6\u00dfe bei Wasserhaushaltsberechnungen oder der hydrogeologischen Grundwassermodellierung. Ebenso steuert sie ma\u00dfgeblich die Verlagerung von Schad- und N\u00e4hrstoffen (bspw. Nitrat) im Boden und beeinflusst indirekt die Standorteignung f\u00fcr Flora und Fauna. Mit der pNAG wird das Risiko einer Nitratauswaschung aus dem Wurzelraum der Vegetation durch versickerndes Bodenwasser bewertet. Der Ort der Beurteilung ist hierbei die Untergrenze der durchwurzelten Bodenschicht. Der Quotient aus SWR und nutzbarer Feldkapazit\u00e4t im effektiven Wurzelraum (nFKWe) liefert zun\u00e4chst die Austauschh\u00e4ufigkeit des pflanzenverf\u00fcgbaren Bodenwassers. Diese wird in 5 Stufen klassifiziert (sehr gering (1), gering (2), mittel (3), hoch (4), sehr hoch (5)) und ergibt die pNAG. Der Kennwert der pNAG ist zur Ableitung quantitativer Aussagen nicht geeignet, da nutzungsabh\u00e4ngige Einflussgr\u00f6\u00dfen (u.a. Kulturart, zu- und abgef\u00fchrte Stickstoffmengen, herbstliche Nitratgehalte im Boden) nicht ber\u00fccksichtigt werden. Die Landesmethode zur Berechnung der pNAG stellt eine Modifikation der Bundesmethode dar, in der die besondere Gef\u00e4hrdung von grundwassernahen Standorten und Moorstandorten ber\u00fccksichtigt wird. Weiterf\u00fchrende Informationen finden Sie hier: https://geo.brandenburg.de/karten/htdocs/21042020_Sickerwasserrate.pdf     Der WCS beinhaltet die folgenden Coverages:      - maximale Sickerwasserrate [max_swr_bund],     - mittlere Sickerwasserrate [avg_swr_bund],     - minimale Sickerwasserrate [min_swr_bund],     - maximale Nitrataustragsgef\u00e4hrdung (Bundesmethode) [max_pnag_bund],     - mittlere Nitrataustragsgef\u00e4hrdung (Bundesmethode) [avg_pnag_bund],     - minimale Nitrataustragsgef\u00e4hrdung (Bundesmethode) [min_pnag_bund],     - maximale Nitrataustragsgef\u00e4hrdung (Landesmethode) [max_pnag_land],     - mittlere Nitrataustragsgef\u00e4hrdung (Landesmethode) [avg_pnag_land],     - minimale Nitrataustragsgef\u00e4hrdung (Landesmethode) [min_pnag_land].", "formats": [{"name": "HTML"}], "keywords": ["bboxbebb", "biogasanlage", "boden", "bodenart", "bodenkunde", "bodenschutz", "bodenu\u0308bersichtskarte", "de", "du\u0308nger", "geologie", "grundwasser", "grundwasserneubildung", "grundwasserschutz", "grundwasserverschmutzung", "hydrologie", "landwirtschaft", "landwirtschaftliche-nutzung", "landwirtschaftsnutzung", "mineral", "na\u0308hrstoff", "niederschlag", "nitrat", "nitrataustrag", "nitrataustragsgefa\u0308hrdung", "nitratbelastung", "nitrit", "oberfla\u0308chengewa\u0308sser", "opendata", "pflanze", "sauerstoff", "schadstoff", "sgd_boden", "sickerwasser", "sickerwasserrate", "stickstoff", "substrate", "trinkwasser", "umwelt", "umweltschutz", "umweltverschmutzung", "wasser", "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%3D37bc2a10-30f6-4d4e-be37-caef1453a30c"}, {"href": "https://inspire.brandenburg.de/services/swrpnag_wcs?REQUEST=GetCapabilities&SERVICE=WCS"}, {"href": "https://isk.geobasis-bb.de/geodienste/Sonstiges/Hilfe_Nutzung_Downloaddienst.pdf"}, {"href": "http://data.europa.eu/88u/dataset/37bc2a10-30f6-4d4e-be37-caef1453a30c~~1"}, {"rel": "self", "type": "application/geo+json", "title": "37bc2a10-30f6-4d4e-be37-caef1453a30c", "name": "item", "description": "37bc2a10-30f6-4d4e-be37-caef1453a30c", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/37bc2a10-30f6-4d4e-be37-caef1453a30c"}, {"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": "383c70fe-7169-43da-89da-e45b126f3a70", "type": "Feature", "geometry": null, "properties": {"updated": "2025-05-27T00:00:00Z", "type": "Dataset", "language": "de", "title": "GcB\u00dcK400 - Zinc in the topsoil", "description": "Zinc is an essential trace element for plants, animals and humans, but at extremely high levels it can have a toxic effect on plants and microorganisms. The concentration of Zn in the upper continental crust (clarke value) is 52 mg/kg, but it can vary greatly depending on the rock type. The mean Zn-contents (median) of the Saxon main rock types are between 11 and 140 mg/kg, the regional clark of the Ore Mountains is about 79 mg/kg. Sphalerite (zinc orifice) leading polymetallic deposits can locally lead to additional geogenous Zn enrichments in the soils. Anthropogenic Zn entries are mainly made by ferrous and non-ferrous metallurgy or by the Zn processing industries (paints, alloys, electroplating) and by large combustion plants. In the area of agglomerations, Zn enrichments can be observed relatively frequently. Anthropogenic Zn entries are possible in agriculture through the use of organic and mineral fertilizers. For unpolluted soils, Zn levels of 10 to 80 mg/kg are considered normal. The regional distribution of the Zn-contents in the Saxon soils is mainly determined by the geogenetic imprinting of the substrates; low to medium grades are to be expected above the periglacian sands and clays in the north and loess soils in central Saxony (10 to 50 mg/kg) as well as the weathering soils above the solid rocks of the Ore Mountains/Vogtland (50 to 150 mg/kg). Within the basement units, significant positive Zn anomalies occur over the polymetallic deposits of the Ore Mountains, depending on the intensity of the mineralization (Freiberg, Annaberg-Buchholz - Marienberg, Aue - Schwarzenberg). Soils over substrates with extremely low Zn content (granite from Eibenstock, orthogneise of the Erzgebirgs central zone, Osterzgebirgischer eruptive complex, Cretaceous sandstones) appear as negative Zn anomalies in the map image. Increased Zn accumulations can be observed in the floodplain soils of the trench system. Due to the higher geogenic base contents in the water catchment area, the occurrence of Zn-bearing polymetallic mineralization and in particular the mining and metallurgical activity in the Freiberg area, high Zn concentrations occur especially in the floodplain soils of the Freiberger and Vereinigte Mulde (median contents 370 and 240 mg/kg). The Federal Soil Protection and Contaminated Sites Ordinance (BBodSchV) did not stipulate any test and action values for total contents for the soil-human and soil-plant impact pathways, as Zn is only of minor importance in the risk assessment.", "formats": [{"name": "HTML"}], "keywords": ["anorganischer-schadstoff", "boden", "chemie", "chemisches-element", "de", "geologie", "zink", "zn"], "contacts": [{"organization": "Kati Kardel", "roles": ["creator"]}, {"organization": "urn:uuid:ef916bfc-5d97-a8bb-a117-b10e5da45c6b", "roles": ["publisher"]}]}, "links": [{"href": "https://luis.sachsen.de/arcgis/services/boden/gcbuek400/MapServer/WFSServer?request=GetCapabilities&service=WFS"}, {"href": "https://luis.sachsen.de/arcgis/services/boden/gcbuek400/MapServer/WMSServer?request=GetCapabilities&service=WMS"}, {"href": "https://luis.sachsen.de/boden/geochemie.html"}, {"href": "https://luis.sachsen.de/boden/geodatendownload.html"}, {"href": "https://umwelt.sachsen.de/umwelt/infosysteme/fme/data/boden/gcbuek400/Steckbrief_GCH_Zink_2025.pdf"}, {"href": "https://www.boden.sachsen.de/uebersichtskarten-fuer-schadstoffe-in-boeden-23988.html?_cp=%7B%22accordion-content-23994%22%253A%7B%220%22%253Atrue%7D%252C%22previousOpen%22%253A%7B%22group%22%253A%22accordion-content-23994%22%252C%22idx%22%253A0%7D%7D"}, {"href": "http://data.europa.eu/88u/dataset/383c70fe-7169-43da-89da-e45b126f3a70"}, {"rel": "self", "type": "application/geo+json", "title": "383c70fe-7169-43da-89da-e45b126f3a70", "name": "item", "description": "383c70fe-7169-43da-89da-e45b126f3a70", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/383c70fe-7169-43da-89da-e45b126f3a70"}, {"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": "938e156d-161a-4b1f-905a-eaeea3d2a76b", "type": "Feature", "geometry": null, "properties": {"updated": "2025-05-27T00:00:00Z", "type": "Dataset", "language": "de", "title": "GcB\u00dcK400 - Cadmium in the topsoil", "description": "Cadmium deserves special attention among heavy metals, as its toxicity to animals and humans is significantly greater than that of other heavy metals. As an accumulation poison, it is enriched in the body and can remain there for decades. Due to its chemical affinity to zinc, it occurs almost exclusively with zinc, especially in all zinc-bearing minerals (including zinc diaphragm, galmei) and rocks. The average concentration of Cd in the rocks of the upper continental crust (clearness) is 0.1 mg/kg, soils usually contain 0.50 mg/kg. In contrast to As and other heavy metals (e.g. Cr, Ni), no geochemical specialisation on Cd can be detected in the main Saxon rock types near the surface. The petrogeochemical component is in the range of the Clark value by 0.1 mg/kg. In the ore deposits Cd is mainly bound to the zinc ore of the polymetallic hydrothermal aisles and partly to the skarn deposits and stratigen-stratiform formations (chacogenic component). Since the beginning of industrialization, cadmium has been released into the environment through the emissions of non-ferrous metal smelters, the combustion of coal and petroleum, and more recently through electroplating, waste incineration, fertilizers, sewage sludge and compost. While in the upper soils of North and Central Saxony low grades dominate (Cd-poor periglacian sandy to loamy substrates; Loess), there is a relative accumulation in the weathering soils over solid rocks. A dependence on the clay content is to be found in this respect that the sandy substrates have slightly lower Cd contents compared to loamy substrates. On arable and grassland sites, higher Cd levels are found compared to the forest sites in the topsoil, as the very low pH values under forest lead to Cd mobilization and shift to greater soil depths. Particularly high Cd loads are found in the Freiberg area, which are caused by the geogenous Cd enrichment in the formation of colorful metal-bearing veins, but above all anthropogenic by the smelting of zinc ores. The highest grades are found in the upper soils in the immediate vicinity of the smelter sites and in lower concentrations east of them (in the main wind direction). Other zinc mineralized deposits in the Westerzgebirge and the Erzgebirgsnordrandzone have only slightly elevated grades. The floodplain soils of the Freiberger and the Vereinigte Mulde occupies a special position in the loading with cadmium. Due to the removal of soils with geogenous enrichments in the catchment area and the enormous anthropogenic additional loads caused by the ore processing and the metallurgical industry, high Cd enrichments occur when the river sediments and Schweban parts are deposited in the flood areas. In the floodplain soils of the Elbe and Zwickauer Mulde, on the other hand, significantly lower grades occur. The geogenous and anthropogenic processes lead to area-wide exceedances of the test and action values of the Federal Soil Protection and Contaminated Sites Ordinance (BBodSchV) for cadmium in the Freiberger area and in the floodplain soils of the Freiberger and Vereinigte Mulde.", "formats": [{"name": "HTML"}], "keywords": ["anorganischer-schadstoff", "boden", "cadmium", "chemie", "chemisches-element", "de", "geologie"], "contacts": [{"organization": "Kati Kardel", "roles": ["creator"]}, {"organization": "urn:uuid:ef916bfc-5d97-a8bb-a117-b10e5da45c6b", "roles": ["publisher"]}]}, "links": [{"href": "https://luis.sachsen.de/arcgis/services/boden/gcbuek400/MapServer/WFSServer?request=GetCapabilities&service=WFS"}, {"href": "https://luis.sachsen.de/arcgis/services/boden/gcbuek400/MapServer/WMSServer?request=GetCapabilities&service=WMS"}, {"href": "https://luis.sachsen.de/boden/geochemie.html"}, {"href": "https://luis.sachsen.de/boden/geodatendownload.html"}, {"href": "https://umwelt.sachsen.de/umwelt/infosysteme/fme/data/boden/gcbuek400/Steckbrief_GCH_Cadmium_2025.pdf"}, {"href": "https://www.boden.sachsen.de/uebersichtskarten-fuer-schadstoffe-in-boeden-23988.html?_cp=%7B%22accordion-content-23994%22%253A%7B%220%22%253Atrue%7D%252C%22previousOpen%22%253A%7B%22group%22%253A%22accordion-content-23994%22%252C%22idx%22%253A0%7D%7D"}, {"href": "http://data.europa.eu/88u/dataset/938e156d-161a-4b1f-905a-eaeea3d2a76b"}, {"rel": "self", "type": "application/geo+json", "title": "938e156d-161a-4b1f-905a-eaeea3d2a76b", "name": "item", "description": "938e156d-161a-4b1f-905a-eaeea3d2a76b", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/938e156d-161a-4b1f-905a-eaeea3d2a76b"}, {"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": "50D3A9C1-5AF4-4C91-9BF1-B231A30C94AB", "type": "Feature", "geometry": null, "properties": {"updated": "2025-05-08T00:00:00", "type": "Dataset", "language": "de", "title": "Kartenlayer Cadmiumbelastung der Ackerb\u00f6den NRW", "description": "Cadmiumbelastung der Ackerb\u00f6den in mg pro kg", "formats": [{"name": "Geographic Markup Language (GML)"}], "keywords": ["blei", "boden", "bodenbelastung", "bodenscha\u0308digung", "bodenschutz", "cadmium", "de", "fachinformationssystem", "gru\u0308nland", "inspireidentifiziert", "karte", "oberboden", "opendata", "regional", "schadstoffbelastung", "schwermetall", "schwermetallgehalt", "soil", "zink", "zinkgehalt"], "contacts": [{"organization": "Landesamt f\u00fcr Natur, Umwelt und Klima Nordrhein-Westfalen", "roles": ["creator"]}]}, "links": [{"href": "https://www.opengeodata.nrw.de/produkte/umwelt_klima/boden/bodenbelastung/"}, {"href": "https://www.wms.nrw.de/umwelt/stobo?SERVICE=WMS&REQUEST=GetCapabilities"}, {"href": "http://data.europa.eu/88u/dataset/50d3a9c1-5af4-4c91-9bf1-b231a30c94ab~~1"}, {"rel": "self", "type": "application/geo+json", "title": "50D3A9C1-5AF4-4C91-9BF1-B231A30C94AB", "name": "item", "description": "50D3A9C1-5AF4-4C91-9BF1-B231A30C94AB", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/50D3A9C1-5AF4-4C91-9BF1-B231A30C94AB"}, {"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": "54E6A328-57E3-4DB7-80D0-F094AD7EAACF", "type": "Feature", "geometry": null, "properties": {"updated": "2025-05-08T00:00:00", "type": "Dataset", "language": "de", "title": "Kartenlayer Cadmiumbelastung der Gr\u00fcnlandb\u00f6den NRW", "description": "Cadmiumbelastung der Gr\u00fcnlandb\u00f6den in mg pro kg", "formats": [{"name": "Geographic Markup Language (GML)"}], "keywords": ["blei", "boden", "bodenbelastung", "bodenscha\u0308digung", "bodenschutz", "cadmium", "cadmiumbelastung", "de", "fachinformationssystem", "fis", "gru\u0308nland", "inspireidentifiziert", "karte", "kartenlayer", "lanuk-kartenlayer", "oberboden", "opendata", "regional", "schadstoffbelastung", "schwermetall", "schwermetallbelastung", "schwermetallgehalt", "soil", "stobo", "zink", "zinkgehalt"], "contacts": [{"organization": "Landesamt f\u00fcr Natur, Umwelt und Klima Nordrhein-Westfalen", "roles": ["creator"]}]}, "links": [{"href": "https://www.opengeodata.nrw.de/produkte/umwelt_klima/boden/bodenbelastung/"}, {"href": "https://www.wms.nrw.de/umwelt/stobo?SERVICE=WMS&REQUEST=GetCapabilities"}, {"href": "http://data.europa.eu/88u/dataset/54e6a328-57e3-4db7-80d0-f094ad7eaacf~~1"}, {"rel": "self", "type": "application/geo+json", "title": "54E6A328-57E3-4DB7-80D0-F094AD7EAACF", "name": "item", "description": "54E6A328-57E3-4DB7-80D0-F094AD7EAACF", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/54E6A328-57E3-4DB7-80D0-F094AD7EAACF"}, {"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": "54f50b1e-caab-479f-bf56-b840134b0c8e-amt-geoinformation-sz", "type": "Feature", "geometry": null, "properties": {"updated": "2025-09-12T00:00:00Z", "type": "Dataset", "title": "Kataster der belasteten Standorte (KbS)", "description": "Bei den im Kataster aufgenommen Standorten handelt es sich um Standorte mit begrenzter Ausdehnung, bei denen feststeht oder mit grosser Wahrscheinlichkeit zu erwarten ist, dass sie mit Abf\u00e4llen belastet sind (Art. 5 Abs. 3 Altlasten-Verordnung). Nicht in den Kataster eingetragen werden (insbesondere \u00fcber den Luftpfad verursachte) grossfl\u00e4chige diffuse Belastungen sowie Areale mit ausschliesslich belasteter Geb\u00e4udesubstanz (z. B. durch Asbest). Beim Kataster der belasteten Standorte handelt es sich um ein dynamisches Arbeitsinstrument, bei dem abh\u00e4ngig von den aktuellen Erkenntnissen Standorte aufgenommen, ver\u00e4ndert oder wieder gel\u00f6scht werden. Der Kataster gibt somit immer nur den aktuellen Wissensstand wieder, eine Gew\u00e4hr f\u00fcr die Richtigkeit (z. B. dass ein nicht eingetragenes Grundst\u00fcck unbelastet ist) besteht nicht. Insbesondere im Rahmen von Bauvorhaben oder Nutzungs\u00e4nderungen k\u00f6nnen altlastenrechtliche oder abfallrechtliche Massnahmen notwendig werden. Der Datensatz ist auch Bestandteil des Katasters der \u00f6ffentlich-rechtlichen Eigentumsbeschr\u00e4nkungen (\u00d6REB)", "formats": [{"name": "WFS_SRVC"}], "keywords": ["abfall", "altlast", "belasteter-standort", "boden", "bodenbelastung", "ch", "eigentumsbeschrankungoreb", "grundwasserschutz", "schadstoffbelastung", "schwermetallbelastung", "umweltbeobachtung", "umweltschutz"], "contacts": [{"organization": "afu@sz.ch", "roles": ["creator"]}, {"organization": "https://www.sz.ch/afu", "roles": ["publisher"]}]}, "links": [{"href": "https://data.geo.sz.ch/public/Themen/A020b/ch.sz.kataster-belasteter-standorte.mgdm.xtf"}, {"href": "https://data.geo.sz.ch/public/Themen/A020b/ch.sz.kataster-belasteter-standorte.oereb.xtf"}, {"href": "https://map.geo.sz.ch/mapserv_proxy?SERVICE=WMS&REQUEST=GetCapabilities"}, {"href": "https://wfs.geo.sz.ch"}, {"href": "http://data.europa.eu/88u/dataset/54f50b1e-caab-479f-bf56-b840134b0c8e-amt-geoinformation-sz"}, {"rel": "self", "type": "application/geo+json", "title": "54f50b1e-caab-479f-bf56-b840134b0c8e-amt-geoinformation-sz", "name": "item", "description": "54f50b1e-caab-479f-bf56-b840134b0c8e-amt-geoinformation-sz", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/54f50b1e-caab-479f-bf56-b840134b0c8e-amt-geoinformation-sz"}, {"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": "633431AC-D3E2-4306-BE64-B2709AA8C973", "type": "Feature", "geometry": null, "properties": {"updated": "2025-05-08T00:00:00Z", "type": "Dataset", "language": "de", "title": "Map layer Lead pollution of garden floors NRW", "description": "Lead load on garden floors in mg per kg", "formats": [{"name": "view"}], "keywords": ["blei", "bleibelastung", "boden", "bodenbelastung", "bodenscha\u0308digung", "bodenschutz", "cadmium", "de", "fachinformationssystem", "fis", "gru\u0308nland", "inspireidentifiziert", "karte", "kartenlayer", "lanuk-kartenlayer", "oberboden", "opendata", "regional", "schadstoffbelastung", "schwermetall", "schwermetallgehalt", "soil", "stobo", "zink", "zinkgehalt"], "contacts": [{"organization": "Landesamt f\u00fcr Natur, Umwelt und Klima Nordrhein-Westfalen", "roles": ["creator"]}]}, "links": [{"href": "https://www.wms.nrw.de/umwelt/stobo?SERVICE=WMS&REQUEST=GetCapabilities"}, {"href": "http://data.europa.eu/88u/dataset/633431ac-d3e2-4306-be64-b2709aa8c973~~1"}, {"rel": "self", "type": "application/geo+json", "title": "633431AC-D3E2-4306-BE64-B2709AA8C973", "name": "item", "description": "633431AC-D3E2-4306-BE64-B2709AA8C973", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/633431AC-D3E2-4306-BE64-B2709AA8C973"}, {"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": "6618bef0-ab81-4978-94e8-2fd8dac9542d-amt-geoinformation-sz", "type": "Feature", "geometry": null, "properties": {"updated": "2023-01-04T00:00:00", "type": "Dataset", "title": "Pr\u00fcfperimeter f\u00fcr Bodenverschiebungen (PBV)", "description": "Die Hinweiskarte Pr\u00fcfperimeter f\u00fcr Bodenverschiebungen (PBV) stellt Bodenfl\u00e4chen dar, die aufgrund ihrer Nutzung mit Schadstoffen belastet sein k\u00f6nnten. Es werden die Belastungsursache sowie die m\u00f6glicherweise vorhandenen Schadstoffe dargestellt.", "formats": [{"name": "WFS_SRVC"}], "keywords": ["altlast", "altstandort", "belastungshinweis", "boden", "bodenbelastung", "bodenschadstoff", "bodenschutz", "bodenuntersuchung", "bodenverschiebung", "ch", "schadstoffbelastung", "schwermetallbelastung", "umweltbeobachtung", "umweltschutz", "ver-und-entsorgung"], "contacts": [{"organization": "afu@sz.ch", "roles": ["creator"]}, {"organization": "https://www.sz.ch/afu", "roles": ["publisher"]}]}, "links": [{"href": "https://map.geo.sz.ch/mapserv_proxy?SERVICE=WMS&REQUEST=GetCapabilities"}, {"href": "https://wfs.geo.sz.ch"}, {"href": "http://data.europa.eu/88u/dataset/6618bef0-ab81-4978-94e8-2fd8dac9542d-amt-geoinformation-sz"}, {"rel": "self", "type": "application/geo+json", "title": "6618bef0-ab81-4978-94e8-2fd8dac9542d-amt-geoinformation-sz", "name": "item", "description": "6618bef0-ab81-4978-94e8-2fd8dac9542d-amt-geoinformation-sz", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/6618bef0-ab81-4978-94e8-2fd8dac9542d-amt-geoinformation-sz"}, {"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": "693bc36f-8c46-4ffe-9d8d-521177fb274c", "type": "Feature", "geometry": null, "properties": {"updated": "2025-08-21T12:06:35", "type": "Dataset", "language": "de", "title": "Potential risk of nitrate discharge (country method)", "description": "The potential risk of nitrate discharge is used to assess the risk of nitrate leaching from the root space of vegetation by leaching soil water. The location of the assessment is the lower bound of the rooted soil layer. The ratio of leachate rate and usable field capacity in the effective root space (nFKWe) first provides the exchange frequency of the plant-available soil water. This is classified in 5 stages (very low \u2013 very high) and gives the pNAG. The characteristic value of the potential risk of nitrate discharge is not suitable for deriving quantitative statements, as use-dependent influencing variables (e.g. crop type, quantities of nitrogen added and removed, autumn nitrate content in the soil) are not taken into account. The state method for calculating the potential risk of nitrate discharge is a modification of the federal method, which takes into account the particular risk of groundwater and peatland sites. Further information can be found here:  https://geo.brandenburg.de/karten/htdocs/21042020_Sickerwasserrate.pdf", "formats": [{"name": "HTML"}], "keywords": ["High value dataset", "boden", "bodenkunde", "de", "erdbeobachtung-und-umwelt", "grundwasser", "grundwasserschutz", "hydrogeologie", "hydrologie", "opendata", "regional", "ressource", "schadstoff", "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/693bc36f-8c46-4ffe-9d8d-521177fb274c~~1"}, {"rel": "self", "type": "application/geo+json", "title": "693bc36f-8c46-4ffe-9d8d-521177fb274c", "name": "item", "description": "693bc36f-8c46-4ffe-9d8d-521177fb274c", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/693bc36f-8c46-4ffe-9d8d-521177fb274c"}, {"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": "75caccfd-4724-4ce6-b058-573ea82ed5d6", "type": "Feature", "geometry": null, "properties": {"updated": "2011-09-30", "type": "Dataset", "language": "de", "title": "LGRB-BW BSK: Flurst\u00fccksbezogene Bodenfunktionsbewertung auf Grundlage der Bodensch\u00e4tzung nach ALK und ALB (Stand: 2010)", "description": "Der Downloaddienst beinhaltet die vorliegende Bodenfunktionsbewertung f\u00fcr ca. 85 % der landwirtschaftlichen Nutzfl\u00e4chen in Baden-W\u00fcrttemberg. Die Bewertung erfolgt nach dem Leitfaden \"Bewertung von B\u00f6den nach ihrer Leistungsf\u00e4higkeit\" (LUBW, 2010) und umfasst die nach Bundes-Bodenschutzgesetz \u00a7 2 Abs. 2 (Nr. 1 a - c) genannten und von der Bund/L\u00e4nder-Arbeitsgemeinschaft (1998) pr\u00e4zisierten nat\u00fcrlichen Bodenfunktionen: Nat\u00fcrliche Bodenfruchtbarkeit, Ausgleichsk\u00f6rper im Wasserkreislauf, Filter und Puffer f\u00fcr Schadstoffe, Sonderstandort f\u00fcr naturnahe Vegetation sowie dar\u00fcber hinaus deren Gesamtbewertung. \u00dcber die Attributabfrage k\u00f6nnen zus\u00e4tzliche Informationen abgerufen werden.  Die angebotenen und auf Flurst\u00fccksebene aggregierten Bodensch\u00e4tzungsdaten sowie daraus abgeleiteten Bodenfunktionsbewertungen basieren auf ALK und ALB mit Stand 2010. Inzwischen sind neu digitalisierten Bodensch\u00e4tzungsdaten der Finanz- sowie Vermessungsverwaltung, entsprechend dem aktuellsten Datenstand, verf\u00fcgbar. Diese sind den bisherigen Daten auf Basis von ALK und ALB vorzuziehen. Bitte pr\u00fcfen Sie daher, ob f\u00fcr die von Ihnen gew\u00fcnschte Fl\u00e4che die Bodenfunktionsbewertung auf Grundlage der neu digitalisierten Bodensch\u00e4tzungsdaten [https://geoportal.lgrb-bw.de/produkt/dbodschis] vorliegt und nutzen Sie ggf. diese.  F\u00fcr forstwirtschaftliche Fl\u00e4chen ist die Bodenkarte 1 : 50 000 (BK50 GeoLa) heranzuziehen.  Aus Performancegr\u00fcnden liefert der Downloaddienst pro Anfrage im gew\u00e4hlten Kartenausschnitt maximal 5 000 Objekte zur\u00fcck.", "formats": [{"name": "WFS_SRVC"}], "keywords": ["ackerzahl", "ausgleichsko\u0308rper-im-wasserhaushalt", "boden", "bodenfunktionsbewertung", "bodenscha\u0308tzung", "bodenzahl", "de", "filter-und-puffer-fu\u0308r-schadstoffe", "gesamtbewertung", "gru\u0308nlandgrundzahl", "gru\u0308nlandzahl", "klassenzeichen", "natu\u0308rliche-bodenfruchtbarkeit", "sonderstandort-fu\u0308r-naturnahe-vegetation"], "contacts": [{"organization": "Regierungspr\u00e4sidium Freiburg - Abteilung 9 Landesamt f\u00fcr Geologie, Rohstoffe und Bergbau, Ref.", "roles": ["creator"]}]}, "links": [{"href": "https://services.lgrb-bw.de/bodschis/services/bsk_d?REQUEST=GetCapabilities&SERVICE=WFS&VERSION=2.0.0"}, {"href": "http://data.europa.eu/88u/dataset/75caccfd-4724-4ce6-b058-573ea82ed5d6"}, {"rel": "self", "type": "application/geo+json", "title": "75caccfd-4724-4ce6-b058-573ea82ed5d6", "name": "item", "description": "75caccfd-4724-4ce6-b058-573ea82ed5d6", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/75caccfd-4724-4ce6-b058-573ea82ed5d6"}, {"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": "769c877d-12bb-40f8-8214-6a70e5604a85", "type": "Feature", "geometry": null, "properties": {"updated": "2025-08-21T10:35:14", "type": "Dataset", "language": "de", "title": "minimale potenzielle Nitrataustragsgef\u00e4hrdung (Bundesmethode) BB", "description": "Der Datensatz beinhaltet Daten vom LBGR \u00fcber die minimale potenzielle Nitrataustragsgef\u00e4hrdung (Bundesmethode) Brandenburgs und wird \u00fcber je einen Darstellungs- und Downloaddienst bereitgestellt. Mit der minimalen potenziellen Nitrataustragsgef\u00e4hrdung wird das minimale Risiko einer Nitratauswaschung aus dem Wurzelraum der Vegetation durch versickerndes Bodenwasser bewertet. Der Ort der Beurteilung ist hierbei die Untergrenze der durchwurzelten Bodenschicht. Der Quotient aus Sickerwasserrate und nutzbarer Feldkapazit\u00e4t im effektiven Wurzelraum (nFKWe) liefert zun\u00e4chst die Austauschh\u00e4ufigkeit des pflanzenverf\u00fcgbaren Bodenwassers. Diese wird in 5 Stufen klassifiziert (sehr gering \u2013 sehr hoch) und ergibt die pNAG. Der Kennwert der potenziellen Nitrataustragsgef\u00e4hrdung ist zur Ableitung quantitativer Aussagen nicht geeignet, da nutzungsabh\u00e4ngige Einflussgr\u00f6\u00dfen (u.a. Kulturart, zu- und abgef\u00fchrte Stickstoffmengen, herbstliche Nitratgehalte im Boden) nicht ber\u00fccksichtigt werden. Die Berechnung der potenziellen Nitrataustragsgef\u00e4hrdung nach Bundesmethode erfolgt auf Basis der Auswertungsmethode 5.3 (AG Boden, 2000b). 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"date"}}, {"id": "CD611816-996F-4261-A2E3-714FCCF8C11F", "type": "Feature", "geometry": null, "properties": {"updated": "2025-05-08T00:00:00Z", "type": "Dataset", "language": "de", "title": "Map layer Lead pollution of grassland soils NRW", "description": "Lead load on grassland soils in mg per kg", "formats": [{"name": "Geographic Markup Language (GML)"}], "keywords": ["blei", "bleibelastung", "boden", "bodenbelastung", "bodenscha\u0308digung", "bodenschutz", "cadmium", "de", "fachinformationssystem", "fis", "gru\u0308nland", "inspireidentifiziert", "karte", "kartenlayer", "lanuk-kartenlayer", "oberboden", "opendata", "regional", "schadstoffbelastung", "schwermetall", "schwermetallbelastung", "schwermetallgehalt", "soil", "stobo", "zink", "zinkgehalt"], "contacts": [{"organization": "Landesamt f\u00fcr Natur, Umwelt und Klima Nordrhein-Westfalen", "roles": ["creator"]}]}, "links": [{"href": "https://www.opengeodata.nrw.de/produkte/umwelt_klima/boden/bodenbelastung/"}, {"href": 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Datensatz beinhaltet Daten vom LBGR \u00fcber die mittlere potenzielle Nitrataustragsgef\u00e4hrdung (Landesmethode) Brandenburgs und wird \u00fcber je einen Darstellungs- und Downloaddienst bereitgestellt. Mit der mittleren potenziellen Nitrataustragsgef\u00e4hrdung wird das mittlere Risiko einer Nitratauswaschung aus dem Wurzelraum der Vegetation durch versickerndes Bodenwasser bewertet. Der Ort der Beurteilung ist hierbei die Untergrenze der durchwurzelten Bodenschicht. Der Quotient aus Sickerwasserrate und nutzbarer Feldkapazit\u00e4t im effektiven Wurzelraum (nFKWe) liefert zun\u00e4chst die Austauschh\u00e4ufigkeit des pflanzenverf\u00fcgbaren Bodenwassers. Diese wird in 5 Stufen klassifiziert (sehr gering \u2013 sehr hoch) und ergibt die pNAG. Der Kennwert der potenziellen Nitrataustragsgef\u00e4hrdung ist zur Ableitung quantitativer Aussagen nicht geeignet, da nutzungsabh\u00e4ngige Einflussgr\u00f6\u00dfen (u.a. Kulturart, zu- und abgef\u00fchrte Stickstoffmengen, herbstliche Nitratgehalte im Boden) nicht ber\u00fccksichtigt werden. Die Landesmethode zur Berechnung der potenziellen Nitrataustragsgef\u00e4hrdung stellt eine Modifikation der Bundesmethode dar, in der die besondere Gef\u00e4hrdung von grundwassernahen Standorten und Moorstandorten ber\u00fccksichtigt wird. Weiterf\u00fchrende Informationen finden Sie hier: Mit der potenziellen Nitrataustragsgef\u00e4hrdung wird das Risiko einer Nitratauswaschung aus dem Wurzelraum der Vegetation durch versickerndes Bodenwasser bewertet. Der Ort der Beurteilung ist hierbei die Untergrenze der durchwurzelten Bodenschicht. Der Quotient aus Sickerwasserrate und nutzbarer Feldkapazit\u00e4t im effektiven Wurzelraum (nFKWe) liefert zun\u00e4chst die Austauschh\u00e4ufigkeit des pflanzenverf\u00fcgbaren Bodenwassers. Diese wird in 5 Stufen klassifiziert (sehr gering \u2013 sehr hoch) und ergibt die pNAG. Der Kennwert der potenziellen Nitrataustragsgef\u00e4hrdung ist zur Ableitung quantitativer Aussagen nicht geeignet, da nutzungsabh\u00e4ngige Einflussgr\u00f6\u00dfen (u.a. Kulturart, zu- und abgef\u00fchrte Stickstoffmengen, herbstliche Nitratgehalte im Boden) nicht ber\u00fccksichtigt werden. Die Landesmethode zur Berechnung der potenziellen Nitrataustragsgef\u00e4hrdung stellt eine Modifikation der Bundesmethode dar, in der die besondere Gef\u00e4hrdung von grundwassernahen Standorten und Moorstandorten ber\u00fccksichtigt wird. Weiterf\u00fchrende Informationen finden Sie hier: https://geo.brandenburg.de/karten/htdocs/21042020_Sickerwasserrate.pdf", "formats": [{"name": "HTML"}], "keywords": ["High value dataset", "boden", "bodenkunde", "bodenschutz", "de", "erdbeobachtung-und-umwelt", "geologie", "grundwasser", "grundwasserschutz", "hydrogeologie", "opendata", "regional", "schadstoff", "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/e68d7a4c-7cdd-4f4e-a08b-fa29fab425f0~~2"}, {"rel": "self", "type": "application/geo+json", "title": "e68d7a4c-7cdd-4f4e-a08b-fa29fab425f0", "name": "item", "description": "e68d7a4c-7cdd-4f4e-a08b-fa29fab425f0", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/e68d7a4c-7cdd-4f4e-a08b-fa29fab425f0"}, {"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": "b8f55ec8-96de-4e90-9ffb-f1c47c2e3b18", "type": "Feature", "geometry": null, "properties": {"updated": "2025-02-06T15:18:04", "type": "Dataset", "language": "de", "title": "LGRB-BW BS: Bodenfunktionsbewertung auf Grundlage der digitalen Bodensch\u00e4tzungsdaten (FESCH und ALKIS) - Datensatz", "description": "Der Downloaddienst beinhaltet die Bodenfunktionsbewertung landwirtschaftlicher Nutzfl\u00e4chen in Baden-W\u00fcrttemberg nach Leitfaden \"Bewertung von B\u00f6den nach ihrer Leistungsf\u00e4higkeit\" (LUBW, 2010) und umfasst die nach Bundes-Bodenschutzgesetz \u00a7 2 Abs. 2 (Nr. 1 a - c) genannten und von der Bund/L\u00e4nder-Arbeitsgemeinschaft (1998) pr\u00e4zisierten nat\u00fcrlichen Bodenfunktionen: Nat\u00fcrliche Bodenfruchtbarkeit, Ausgleichsk\u00f6rper im Wasserkreislauf, Filter und Puffer f\u00fcr Schadstoffe, Sonderstandort f\u00fcr naturnahe Vegetation und dar\u00fcber hinaus deren Gesamtbewertung. \u00dcber die Attributabfrage k\u00f6nnen zus\u00e4tzliche Informationen abgerufen werden.  Die angebotenen Bodenfunktionsbewertungen und aggregierten Bodensch\u00e4tzungsdaten basieren auf den neu digitalisierten Bodensch\u00e4tzungsdaten der Finanz- sowie Vermessungsverwaltung und entsprechen dem aktuell verf\u00fcgbaren Datenstand, in den originalen Geometrien der Bodensch\u00e4tzung. Diese neuabgeleiteten Daten sind den bisherigen flurst\u00fccksbezogenen Daten auf Grundlage von ALK und ALB (Stand 2010) vorzuziehen. Bisher sind die digitalen Bodensch\u00e4tzungsdaten nicht f\u00fcr s\u00e4mtliche landwirtschaftlich genutzten Fl\u00e4chen in Baden-W\u00fcrttemberg verf\u00fcgbar. Sollte f\u00fcr die von Ihnen gew\u00fcnschte Fl\u00e4che noch keine Bodenfunktionsbewertung aus den digitalen Bodensch\u00e4tzungsdaten abgeleitet vorliegen, nutzen Sie bitte bis auf Weiteres die Daten auf Basis von ALB und ALK mit Stand 2010 [https://geoportal.lgrb-bw.de/produkt/dbsk]. Die Bodenfunktionsbewertung auf Grundlage der neu digitalisierten Bodensch\u00e4tzungsdaten wird fortlaufend erg\u00e4nzt.  F\u00fcr forstwirtschaftliche Fl\u00e4chen ist die Bodenkarte 1 : 50 000 (BK50 GeoLa) heranzuziehen.  Aus Performancegr\u00fcnden liefert der Downloaddienst pro Anfrage im gew\u00e4hlten Kartenausschnitt maximal 5 000 Objekte zur\u00fcck.", "formats": [{"name": "WFS_SRVC"}], "keywords": ["ackerzahl", "ausgleichsko\u0308rper-im-wasserhaushalt", "boden", "bodenfunktionsbewertung", "bodenscha\u0308tzung", "bodenzahl", "de", "filter-und-puffer-fu\u0308r-schadstoffe", "gesamtbewertung", "gru\u0308nlandgrundzahl", "gru\u0308nlandzahl", "klassenzeichen", "natu\u0308rliche-bodenfruchtbarkeit", "opendata", "sonderstandort-fu\u0308r-naturnahe-vegetation"], "contacts": [{"organization": "Regierungspr\u00e4sidium Freiburg - Abteilung 9 Landesamt f\u00fcr Geologie, Rohstoffe und Bergbau, Ref. 93 Landesbodenkunde", "roles": ["creator"]}]}, "links": [{"href": "https://services.lgrb-bw.de/bodschis/services/bs_d?REQUEST=GetCapabilities&SERVICE=WFS&VERSION=2.0.0"}, {"href": "http://data.europa.eu/88u/dataset/b8f55ec8-96de-4e90-9ffb-f1c47c2e3b18~~1"}, {"rel": "self", "type": "application/geo+json", "title": "b8f55ec8-96de-4e90-9ffb-f1c47c2e3b18", "name": "item", "description": "b8f55ec8-96de-4e90-9ffb-f1c47c2e3b18", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/b8f55ec8-96de-4e90-9ffb-f1c47c2e3b18"}, {"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", "type": "Feature", "geometry": null, "properties": {"updated": "2025-05-27T00:00:00Z", "type": "Dataset", "language": "de", "title": "GcB\u00dcK400 - Kupfer im Oberboden", "description": "Kupfer ist ein f\u00fcr die Ern\u00e4hrung aller Lebewesen essentielles Element, das jedoch bei einem extremen \u00dcberangebot zu toxischen Wirkungen f\u00fchren kann. Der mittlere Cu-Gehalt der Gesteine der oberen kontinentalen Erdkruste (Clarkewert) betr\u00e4gt 14 mg/kg. Analog zu Chrom und Nickel ist es vor allem in basischen Gesteinen angereichert (Diabase, Basalte, Metabasite). Die mittleren Cu-Gehalte (Mediane) der s\u00e4chsischen Haupt-gesteinstypen reichen von 2 bis 67 mg/kg, der regionale Clarke des Erzgebirges/Vogtlandes betr\u00e4gt 23 mg/kg. Geogene Cu-Anreicherungen sind vor allem im Erzgebirge \u00fcber den hier weit verbreiteten Mineralisationen zu finden. Chalkopyrit (Kupferkies) ist nahezu in allen Mineralassoziationen als sog. Durchl\u00e4ufermineral verbreitet. Starke anthropogene Cu-Eintr\u00e4ge werden vor allem durch die Buntmetallurgie verursacht. Durch die vielf\u00e4ltige Verwendung von Cu, u. a. in der Elektrotechnik, als Legierungsmetall, Rohrleitungsmaterial und Regenrinnen, wird das Element auch verst\u00e4rkt in das Abwasser eingetragen. F\u00fcr unbelastete B\u00f6den gelten Cu-Gehalte von 2 bis 40 mg/kg als normal. Die regionale Verteilung der Cu-Gehalte im Oberboden wird vor allem durch den geogenen Anteil der Substrate bestimmt. Auf Grund der erh\u00f6hten Cu-Gehalte der im Vogtland weit verbreiteten Diabase (58 mg/kg), der punktf\u00f6rmig auftretenden terti\u00e4ren Basaltoide (60 mg/kg) und der lokal eingelagerten Amphibolite (46 mg/kg) des metamorphen Grundgebirges, kommt es zu anomal hohen Cu-Gehalten in den Verwitterungsb\u00f6den \u00fcber den genannten Festgesteinen. Durch eine verst\u00e4rkte L\u00f6ssbeeinflussung (mit relativ niedrigen Cu-Gehalten von ca. 12 mg/kg), kann es \u00fcber Cu-reichen Substraten, je nach L\u00f6ssanteil, zu einem \"Verd\u00fcnnungseffekt\" kommen (z. B. \u00fcber den Monzonitoiden bei Mei\u00dfen). Extrem niedrige Cu-Konzentrationen sind in den Verwitterungsb\u00f6den \u00fcber sauren Magmatiten (Granit von Ei-benstock, Teplice-Rhyolith), Metagranitoiden (Erzgebirgs-Zentralzone), Sandsteinen (Elbsandstein- und Zittauer Gebirge) und bei Bodengesellschaften aus periglazi\u00e4ren sandigen Decksedimenten in Nordsachsen zu beobachten. Bedeutende regionale Anomalien befinden sich vor allem im Freiberger Raum, dem wichtigsten fr\u00fcheren Standort des Bergbaus und der Verh\u00fcttung polymetallischer Erze. Die anthropogenen Eintr\u00e4ge sind aber i. W. auf die unmittelbare Umgebung der H\u00fcttenstandorte beschr\u00e4nkt. Dabei kommt es zu \u00dcberlagerung mit geogenen Anteilen im Boden, die in urs\u00e4chlichem Zusammenhang mit der Verbreitung von Kupferkies f\u00fchrenden Mineralassoziationen stehen. Analoge Verh\u00e4ltnisse finden sich, wenn auch in abgeschw\u00e4chter Form, im Raum Schneeberg - Schwarzenberg - Annaberg-Buchholz - Marienberg. Besonders hohe Cu-Gehalte weisen die Auenb\u00f6den der Freiberger Mulde auf. Nach Eintritt der Freiberger Mulde in das Freiberger Bergbau- und H\u00fcttenrevier kommt es zu einer nachhaltigen stofflichen Belastung der Auenb\u00f6den, die \u00fcber die Aue der Vereinigten Mulde bis an die n\u00f6rdliche Landesgrenze reicht. Erh\u00f6hte Cu-Gehalte, jedoch auf deutlich niedrigerem Niveau, treten auch in den Auenb\u00f6den der Zwickauer Mulde auf, wo sich im Einzugsgebiet die polymetallischen Vererzungen des Westerzgebirges befinden. Infolge der beschriebenen geogenen und anthropogenen Prozesse werden in den Auenb\u00f6den der Freiberger und der Vereinigten Mulde die Ma\u00dfnahmenwerte der Bundes-Bodenschutz- und Altlastenverordnung (BBodSchV) f\u00fcr Gr\u00fcnlandnutzung (Schafhaltung) teilweise \u00fcberschritten.", "formats": [{"name": "HTML"}], "keywords": ["anorganischer-schadstoff", "boden", "chemie", "chemisches-element", "cu", "de", "geologie", "kupfer"], "contacts": [{"organization": "Kati Kardel", "roles": ["creator"]}, {"organization": "urn:uuid:ef916bfc-5d97-a8bb-a117-b10e5da45c6b", "roles": ["publisher"]}]}, "links": [{"href": "https://luis.sachsen.de/arcgis/services/boden/gcbuek400/MapServer/WFSServer?request=GetCapabilities&service=WFS"}, {"href": "https://luis.sachsen.de/arcgis/services/boden/gcbuek400/MapServer/WMSServer?request=GetCapabilities&service=WMS"}, {"href": "https://luis.sachsen.de/boden/geochemie.html"}, {"href": "https://luis.sachsen.de/boden/geodatendownload.html"}, {"href": "https://umwelt.sachsen.de/umwelt/infosysteme/fme/data/boden/gcbuek400/Steckbrief_GCH_Kupfer_2025.pdf"}, {"href": "https://www.boden.sachsen.de/uebersichtskarten-fuer-schadstoffe-in-boeden-23988.html?_cp=%7B%22accordion-content-23994%22%253A%7B%220%22%253Atrue%7D%252C%22previousOpen%22%253A%7B%22group%22%253A%22accordion-content-23994%22%252C%22idx%22%253A0%7D%7D"}, {"href": "http://data.europa.eu/88u/dataset/caa134ea-ce26-4e82-a48e-8bd5c35c467e~~2"}, {"rel": "self", "type": "application/geo+json", "title": "caa134ea-ce26-4e82-a48e-8bd5c35c467e", "name": "item", "description": "caa134ea-ce26-4e82-a48e-8bd5c35c467e", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/caa134ea-ce26-4e82-a48e-8bd5c35c467e"}, {"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": "cac01424-add3-404c-ae41-abade484f10e", "type": "Feature", "geometry": null, "properties": {"updated": "2025-08-21T12:05:29", "type": "Dataset", "language": "de", "title": "Potential risk of nitrate discharge (federal method)", "description": "The potential risk of nitrate discharge is used to assess the risk of nitrate leaching from the root space of vegetation by leaching soil water. The location of the assessment is the lower bound of the rooted soil layer. The ratio of leachate rate and usable field capacity in the effective root space (nFKWe) first provides the exchange frequency of the plant-available soil water. This is classified in 5 stages (very low \u2013 very high) and gives the pNAG. The characteristic value of the potential risk of nitrate discharge is not suitable for deriving quantitative statements, as use-dependent influencing variables (e.g. crop type, quantities of nitrogen added and removed, autumn nitrate content in the soil) are not taken into account. The calculation of the potential nitrate discharge risk according to the federal method is based on the evaluation method 5.3 (AG Boden, 2000b). 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"boden-dauerbeobachtung", "bodenbiologie", "bodenchemie", "bodeno\u0308kologie", "bodenphysik", "bodenschutz", "bodenzustand", "de", "deutschland", "geowissenschaften", "inspireidentifiziert", "national", "opendata", "schadstoff", "umweltdaten", "umweltzustandsdaten"], "contacts": [{"organization": "Umweltbundesamt", "roles": ["creator"]}]}, "links": [{"href": "https://datahub.uba.de/server/rest/directories/arcgisforinspire/INSPIRE/bdf_MapServer/Daten/BDF_Stammdaten.zip"}, {"href": "http://data.europa.eu/88u/dataset/d42faed4-243e-46ff-9253-b94e9ff3589f"}, {"rel": "self", "type": "application/geo+json", "title": "d42faed4-243e-46ff-9253-b94e9ff3589f", "name": "item", "description": "d42faed4-243e-46ff-9253-b94e9ff3589f", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/d42faed4-243e-46ff-9253-b94e9ff3589f"}, {"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": "d84986c3-30dd-3f39-a3a7-2975bc9a4f84", "type": "Feature", "geometry": null, "properties": {"updated": "2025-09-12T12:29:34", "type": "Dataset", "language": "de", "title": "Kriterien zur Bewertung der Bodenfunktionen 2005 (Umweltatlas)", "description": "Bewertungskriterien zu sechs Bodenfunktionen auf Grundlage der Blockkarte 1 : 50.000 (ISU50, Raumbezug Umweltatlas 2005), Bearbeitungsstand Februar 2009.", "keywords": ["austauschha\u0308ufigkeit-des-bodenwassers", "berlin", "besondere-naturra\u0308umliche-eigenart", "bindungssta\u0308rke-an-schwermetalle", "boden", "bodenbewertung", "bodenfunktionen", "bodenfunktionskarte", "de", "filtervermo\u0308gen", "geodaten", "geologie", "kriterien-zur-bewertung-der-bodenfunktionen", "naturna\u0308he", "na\u0308hrstoffspeichervermo\u0308gen", "na\u0308hrstoffversorgung", "open-data", "opendata", "regelungsfunktion", 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"https://gdi.berlin.de/services/wfs/ua_boden_seltenheit_2005?REQUEST=GetCapabilities&SERVICE=wfs"}, {"href": "https://gdi.berlin.de/services/wfs/ua_boden_wasserversorgung_2005?REQUEST=GetCapabilities&SERVICE=wfs"}, {"href": "http://data.europa.eu/88u/dataset/d84986c3-30dd-3f39-a3a7-2975bc9a4f84"}, {"rel": "self", "type": "application/geo+json", "title": "d84986c3-30dd-3f39-a3a7-2975bc9a4f84", "name": "item", "description": "d84986c3-30dd-3f39-a3a7-2975bc9a4f84", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/d84986c3-30dd-3f39-a3a7-2975bc9a4f84"}, {"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": "feb6008f-25d1-40be-af85-10e286ed72a9", "type": "Feature", "geometry": null, "properties": {"updated": "2025-08-21T10:32:47", "type": "Dataset", "language": "de", "title": "Maximum potential nitrate discharge hazard (federal method)", "description": "The maximum potential risk of nitrate discharge is used to assess the maximum risk of nitrate leaching from the root space of vegetation by leaching soil water. The location of the assessment is the lower bound of the rooted soil layer. The ratio of leachate rate and usable field capacity in the effective root space (nFKWe) first provides the exchange frequency of the plant-available soil water. This is classified in 5 stages (very low \u2013 very high) and gives the pNAG. The characteristic value of the potential risk of nitrate discharge is not suitable for deriving quantitative statements, as use-dependent influencing variables (e.g. crop type, quantities of nitrogen added and removed, autumn nitrate content in the soil) are not taken into account. The calculation of the potential nitrate discharge risk according to the federal method is based on the evaluation method 5.3 (AG Boden, 2000b). Further information can be found here:  https://geo.brandenburg.de/karten/htdocs/21042020_Sickerwasserrate.pdf", "formats": [{"name": "HTML"}], "keywords": ["High value dataset", "boden", "bodenkunde", "bodenschutz", "de", "erdbeobachtung-und-umwelt", "geologie", "grundwasser", "grundwasserschutz", "hydrogeologie", "opendata", "regional", "schadstoff", "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/feb6008f-25d1-40be-af85-10e286ed72a9~~1"}, {"rel": "self", "type": "application/geo+json", "title": "feb6008f-25d1-40be-af85-10e286ed72a9", "name": "item", "description": "feb6008f-25d1-40be-af85-10e286ed72a9", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/feb6008f-25d1-40be-af85-10e286ed72a9"}, {"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": "fffdf08f-8ee8-4802-8354-5e6df694b0c7", "type": "Feature", "geometry": null, "properties": {"themes": [{"concepts": [{"id": "geoscientificInformation"}], "scheme": "https://standards.iso.org/iso/19139/resources/gmxCodelists.xml#MD_TopicCategoryCode"}, {"concepts": [{"id": "National"}], "scheme": "https://inspire.ec.europa.eu/metadata-codelist/SpatialScope"}, {"concepts": [{"id": "MensMeu"}], "scheme": "Source"}, {"concepts": [{"id": "Germany"}], "scheme": "http://publications.europa.eu/resource/authority/country"}, {"concepts": [{"id": "soil contamination"}], "scheme": "http://aims.fao.org/aos/agrovoc/c_330883"}], "updated": "2017-01-01", "type": "Dataset", "created": "2017-01-01", "language": "ger", "title": "Substances in soils in Germany", "description": "Soil substances in Germany. In addition to substances that serve as nutrients for the plants, there are also pollutants in the soil which in higher concentrations can impair the growth of plants and animals. Some substances (e.g., nickel) are essential in low concentrations but in higher concentrations they are toxi", "formats": [{"name": "None"}, {"name": "OGC:WMS"}, {"name": "ogc:wms"}, {"name": "canonical"}], "keywords": ["soil degradation processes", "National", "MensMeu", "Soil", "Boden", "Belastung", "Entstehungsart", "Schadstoff", "Gesteinszusammensetzung", "Bodeneigenschaften", "Deutschland", "Hintergrundwerte", "Anorganische Spurenstoffe", "Boden", "Schwermetall", "Antimon", "Arsen", "Beryllium", "Blei", "Cadmium", "Chrom", "Kobalt", "Cobalt", "Kupfer", "Molybd\u00e4n", "Nickel", "Quecksilber", "Selen", "Thallium", "Uran", "Vanadium", "Zink", "Bundesrepublik Deutschland", "Germany", "soil contamination"], "contacts": [{"name": "Stegger Ulrich", "organization": "Bundesanstalt f\u00fcr Geowissenschaften und Rohstoffe (BGR)", "position": null, "roles": ["pointOfContact"], "phones": [{"value": null}], "emails": [{"value": "geodatenmanagement@bgr.de"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": "None", "country": "Germany"}], "links": [{"href": {"url": "https://www.bgr.bund.de", "protocol": null, "protocol_url": "", "name": null, "name_url": "", "description": null, "description_url": "", "applicationprofile": null, "applicationprofile_url": "", "function": null}}]}]}, "links": [{"href": "https://download.bgr.de/bgr/boden/HGW1000/GeoPackage/hgw1000_v20.zip", "name": "HGW1000 (GeoPackage)", "description": "HGW1000 im Format GeoPackage", "rel": "download"}, {"href": "https://www.labo-deutschland.de/documents/LABO_Fassung_HGW_Bericht_02_2017.pdf", "description": "Bericht der LABO-Bund/L\u00e4nder-Arbeitsgemeinschaft Bodenschutz", "rel": "information"}, {"href": "https://services.bgr.de/boden/hgw1000", "description": "Karte im BGR-Geoviewer", "rel": "information"}, {"href": "https://services.bgr.de/wms/boden/bodenstoffe/?SERVICE=WMS&REQUEST=GetCapabilities", "name": "6", "description": "In mehreren Forschungsvorhaben wurde ein Konzept zur Ableitung von fl\u00e4chenhaft repr\u00e4sentativen Hintergrundwerten f\u00fcr Ober- und Unterb\u00f6den sowie f\u00fcr den Untergrund entwickelt und angewendet. Das Konzept beruht auf einer Zuordnung der 69 bodenkundlichen Legendeneinheiten der B\u00dcK1000N, Version 2.31, zu 15 Bodenausgangsgesteinsgruppen. Au\u00dferdem wird f\u00fcr Oberb\u00f6den zus\u00e4tzlich nach Landnutzung differenziert. Zur Schaffung eines Datensatzes mit entsprechenden Punktinformationen wurden unterschiedliche Datenbest\u00e4nde aus den L\u00e4ndern und vom Bund nach Abgleich gegen\u00fcber den Mindestanforderungen und inhaltlicher Harmonisierung zusammengef\u00fchrt. Auf der Grundlage von ca. 5000 harmonisierten Profildaten konnten repr\u00e4sentative Hintergrundwerte anorganischer Spurenstoffe f\u00fcr Ober- und Unterb\u00f6den sowie den Untergrund mit einer Fl\u00e4chendeckung von ca. 90% der Bundesrepublik abgeleitet werden und diese werden in der Karte dargestellt. Das genaue Vorgehen bei der Ableitung ist dem Bericht der LABO-Bund/L\u00e4nder-Arbeitsgemeinschaft Bodenschutz (2003): 'Hintergrundwerte f\u00fcr anorganische und organische Stoffe in B\u00f6den, 3. \u00fcberarbeitete und erg\u00e4nzte Auflage', zu entnehmen.", "protocol": "OGC:WMS", "rel": null}, {"href": "https://services.bgr.de/wms/boden/bodenstoffe/?SERVICE=WMS&REQUEST=GetCapabilities", "name": "13", "description": "In mehreren Forschungsvorhaben wurde ein Konzept zur Ableitung von fl\u00e4chenhaft repr\u00e4sentativen Hintergrundwerten f\u00fcr Ober- und Unterb\u00f6den sowie f\u00fcr den Untergrund entwickelt und angewendet. Das Konzept beruht auf einer Zuordnung der 69 bodenkundlichen Legendeneinheiten der B\u00dcK1000N, Version 2.31, zu 15 Bodenausgangsgesteinsgruppen. Au\u00dferdem wird f\u00fcr Oberb\u00f6den zus\u00e4tzlich nach Landnutzung differenziert. Zur Schaffung eines Datensatzes mit entsprechenden Punktinformationen wurden unterschiedliche Datenbest\u00e4nde aus den L\u00e4ndern und vom Bund nach Abgleich gegen\u00fcber den Mindestanforderungen und inhaltlicher Harmonisierung zusammengef\u00fchrt. Auf der Grundlage von ca. 5000 harmonisierten Profildaten konnten repr\u00e4sentative Hintergrundwerte anorganischer Spurenstoffe f\u00fcr Ober- und Unterb\u00f6den sowie den Untergrund mit einer Fl\u00e4chendeckung von ca. 90% der Bundesrepublik abgeleitet werden und diese werden in der Karte dargestellt. Das genaue Vorgehen bei der Ableitung ist dem Bericht der LABO-Bund/L\u00e4nder-Arbeitsgemeinschaft Bodenschutz (2003): 'Hintergrundwerte f\u00fcr anorganische und organische Stoffe in B\u00f6den, 3. \u00fcberarbeitete und erg\u00e4nzte Auflage', zu entnehmen.", "protocol": "OGC:WMS", "rel": null}, {"href": "https://services.bgr.de/wms/boden/bodenstoffe/?SERVICE=WMS&REQUEST=GetCapabilities", "name": "20", "description": "In mehreren Forschungsvorhaben wurde ein Konzept zur Ableitung von fl\u00e4chenhaft repr\u00e4sentativen Hintergrundwerten f\u00fcr Ober- und Unterb\u00f6den sowie f\u00fcr den Untergrund entwickelt und angewendet. Das Konzept beruht auf einer Zuordnung der 69 bodenkundlichen Legendeneinheiten der B\u00dcK1000N, Version 2.31, zu 15 Bodenausgangsgesteinsgruppen. Au\u00dferdem wird f\u00fcr Oberb\u00f6den zus\u00e4tzlich nach Landnutzung differenziert. Zur Schaffung eines Datensatzes mit entsprechenden Punktinformationen wurden unterschiedliche Datenbest\u00e4nde aus den L\u00e4ndern und vom Bund nach Abgleich gegen\u00fcber den Mindestanforderungen und inhaltlicher Harmonisierung zusammengef\u00fchrt. Auf der Grundlage von ca. 5000 harmonisierten Profildaten konnten repr\u00e4sentative Hintergrundwerte anorganischer Spurenstoffe f\u00fcr Ober- und Unterb\u00f6den sowie den Untergrund mit einer Fl\u00e4chendeckung von ca. 90% der Bundesrepublik abgeleitet werden und diese werden in der Karte dargestellt. Das genaue Vorgehen bei der Ableitung ist dem Bericht der LABO-Bund/L\u00e4nder-Arbeitsgemeinschaft Bodenschutz (2003): 'Hintergrundwerte f\u00fcr anorganische und organische Stoffe in B\u00f6den, 3. \u00fcberarbeitete und erg\u00e4nzte Auflage', zu entnehmen.", "protocol": "OGC:WMS", "rel": null}, {"href": "https://services.bgr.de/wms/boden/bodenstoffe/?SERVICE=WMS&REQUEST=GetCapabilities", "name": "34", "description": "In mehreren Forschungsvorhaben wurde ein Konzept zur Ableitung von fl\u00e4chenhaft repr\u00e4sentativen Hintergrundwerten f\u00fcr Ober- und Unterb\u00f6den sowie f\u00fcr den Untergrund entwickelt und angewendet. Das Konzept beruht auf einer Zuordnung der 69 bodenkundlichen Legendeneinheiten der B\u00dcK1000N, Version 2.31, zu 15 Bodenausgangsgesteinsgruppen. Au\u00dferdem wird f\u00fcr Oberb\u00f6den zus\u00e4tzlich nach Landnutzung differenziert. Zur Schaffung eines Datensatzes mit entsprechenden Punktinformationen wurden unterschiedliche Datenbest\u00e4nde aus den L\u00e4ndern und vom Bund nach Abgleich gegen\u00fcber den Mindestanforderungen und inhaltlicher Harmonisierung zusammengef\u00fchrt. Auf der Grundlage von ca. 5000 harmonisierten Profildaten konnten repr\u00e4sentative Hintergrundwerte anorganischer Spurenstoffe f\u00fcr Ober- und Unterb\u00f6den sowie den Untergrund mit einer Fl\u00e4chendeckung von ca. 90% der Bundesrepublik abgeleitet werden und diese werden in der Karte dargestellt. Das genaue Vorgehen bei der Ableitung ist dem Bericht der LABO-Bund/L\u00e4nder-Arbeitsgemeinschaft Bodenschutz (2003): 'Hintergrundwerte f\u00fcr anorganische und organische Stoffe in B\u00f6den, 3. \u00fcberarbeitete und erg\u00e4nzte Auflage', zu entnehmen.", "protocol": "OGC:WMS", "rel": null}, {"href": "https://services.bgr.de/wms/boden/bodenstoffe/?SERVICE=WMS&REQUEST=GetCapabilities", "name": "41", "description": "In mehreren Forschungsvorhaben wurde ein Konzept zur Ableitung von fl\u00e4chenhaft repr\u00e4sentativen Hintergrundwerten f\u00fcr Ober- und Unterb\u00f6den sowie f\u00fcr den Untergrund entwickelt und angewendet. Das Konzept beruht auf einer Zuordnung der 69 bodenkundlichen Legendeneinheiten der B\u00dcK1000N, Version 2.31, zu 15 Bodenausgangsgesteinsgruppen. Au\u00dferdem wird f\u00fcr Oberb\u00f6den zus\u00e4tzlich nach Landnutzung differenziert. Zur Schaffung eines Datensatzes mit entsprechenden Punktinformationen wurden unterschiedliche Datenbest\u00e4nde aus den L\u00e4ndern und vom Bund nach Abgleich gegen\u00fcber den Mindestanforderungen und inhaltlicher Harmonisierung zusammengef\u00fchrt. Auf der Grundlage von ca. 5000 harmonisierten Profildaten konnten repr\u00e4sentative Hintergrundwerte anorganischer Spurenstoffe f\u00fcr Ober- und Unterb\u00f6den sowie den Untergrund mit einer Fl\u00e4chendeckung von ca. 90% der Bundesrepublik abgeleitet werden und diese werden in der Karte dargestellt. Das genaue Vorgehen bei der Ableitung ist dem Bericht der LABO-Bund/L\u00e4nder-Arbeitsgemeinschaft Bodenschutz (2003): 'Hintergrundwerte f\u00fcr anorganische und organische Stoffe in B\u00f6den, 3. \u00fcberarbeitete und erg\u00e4nzte Auflage', zu entnehmen.", "protocol": "OGC:WMS", "rel": null}, {"href": "https://services.bgr.de/wms/boden/bodenstoffe/?SERVICE=WMS&REQUEST=GetCapabilities", "name": "48", "description": "In mehreren Forschungsvorhaben wurde ein Konzept zur Ableitung von fl\u00e4chenhaft repr\u00e4sentativen Hintergrundwerten f\u00fcr Ober- und Unterb\u00f6den sowie f\u00fcr den Untergrund entwickelt und angewendet. Das Konzept beruht auf einer Zuordnung der 69 bodenkundlichen Legendeneinheiten der B\u00dcK1000N, Version 2.31, zu 15 Bodenausgangsgesteinsgruppen. Au\u00dferdem wird f\u00fcr Oberb\u00f6den zus\u00e4tzlich nach Landnutzung differenziert. Zur Schaffung eines Datensatzes mit entsprechenden Punktinformationen wurden unterschiedliche Datenbest\u00e4nde aus den L\u00e4ndern und vom Bund nach Abgleich gegen\u00fcber den Mindestanforderungen und inhaltlicher Harmonisierung zusammengef\u00fchrt. Auf der Grundlage von ca. 5000 harmonisierten Profildaten konnten repr\u00e4sentative Hintergrundwerte anorganischer Spurenstoffe f\u00fcr Ober- und Unterb\u00f6den sowie den Untergrund mit einer Fl\u00e4chendeckung von ca. 90% der Bundesrepublik abgeleitet werden und diese werden in der Karte dargestellt. Das genaue Vorgehen bei der Ableitung ist dem Bericht der LABO-Bund/L\u00e4nder-Arbeitsgemeinschaft Bodenschutz (2003): 'Hintergrundwerte f\u00fcr anorganische und organische Stoffe in B\u00f6den, 3. \u00fcberarbeitete und erg\u00e4nzte Auflage', zu entnehmen.", "protocol": "OGC:WMS", "rel": null}, {"href": "https://services.bgr.de/wms/boden/bodenstoffe/?SERVICE=WMS&REQUEST=GetCapabilities", "name": "62", "description": "In mehreren Forschungsvorhaben wurde ein Konzept zur Ableitung von fl\u00e4chenhaft repr\u00e4sentativen Hintergrundwerten f\u00fcr Ober- und Unterb\u00f6den sowie f\u00fcr den Untergrund entwickelt und angewendet. Das Konzept beruht auf einer Zuordnung der 69 bodenkundlichen Legendeneinheiten der B\u00dcK1000N, Version 2.31, zu 15 Bodenausgangsgesteinsgruppen. Au\u00dferdem wird f\u00fcr Oberb\u00f6den zus\u00e4tzlich nach Landnutzung differenziert. Zur Schaffung eines Datensatzes mit entsprechenden Punktinformationen wurden unterschiedliche Datenbest\u00e4nde aus den L\u00e4ndern und vom Bund nach Abgleich gegen\u00fcber den Mindestanforderungen und inhaltlicher Harmonisierung zusammengef\u00fchrt. Auf der Grundlage von ca. 5000 harmonisierten Profildaten konnten repr\u00e4sentative Hintergrundwerte anorganischer Spurenstoffe f\u00fcr Ober- und Unterb\u00f6den sowie den Untergrund mit einer Fl\u00e4chendeckung von ca. 90% der Bundesrepublik abgeleitet werden und diese werden in der Karte dargestellt. Das genaue Vorgehen bei der Ableitung ist dem Bericht der LABO-Bund/L\u00e4nder-Arbeitsgemeinschaft Bodenschutz (2003): 'Hintergrundwerte f\u00fcr anorganische und organische Stoffe in B\u00f6den, 3. \u00fcberarbeitete und erg\u00e4nzte Auflage', zu entnehmen.", "protocol": "OGC:WMS", "rel": null}, {"href": "https://services.bgr.de/wms/boden/bodenstoffe/?SERVICE=WMS&REQUEST=GetCapabilities", "name": "4,6,13,20,27,34,41,48,55,62,69,76,83,90,97,104", "protocol": "ogc:wms", "rel": null}, {"href": "https://github.com/ejpsoil/ejpsoildatahub/tree/main/datasets/mensmeu/Germany/fffdf08f-8ee8-4802-8354-5e6df694.yml", "name": "Source of the record", "protocol": "canonical", "rel": "canonical"}, {"rel": "self", "type": "application/geo+json", "title": "fffdf08f-8ee8-4802-8354-5e6df694b0c7", "name": "item", "description": "fffdf08f-8ee8-4802-8354-5e6df694b0c7", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/fffdf08f-8ee8-4802-8354-5e6df694b0c7"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-01-01T00:00:00Z"}}, {"id": "caa134ea-ce26-4e82-a48e-8bd5c35c467e~~1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-26T16:37:59Z", "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": "8e33abad-7706-3ec7-aaed-68945a752868", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-26T16:38:10Z", "type": "Dataset", "title": "Soil Soils and Soil Species 2010 (Environmental Atlas)", "description": "Material data on soil societies and types of soil.  Room Reference Block/Teiblockkarte ISU 5 (City and Environment Information System) as of 2010.", "formats": [{"name": "WFS_SRVC"}], "keywords": ["ausgangsmaterial", "berlin", "boden", "bodenarten", "bodendaten", "bodenformen", "bodengesellschaften", "bodenkundliche-kennwerte", "bodentypen", "de", "durchla\u0308ssigkeitsbeiwert", "feinboden", "flachwurzelzone", "geodaten", "geomorphologische-einheit", "grobboden", "grundwasserflurabstand", "kf-wert", "konzeptbodendaten", "naturra\u0308umliche-eigenart", "nfk-wert", "nutzbare-feldkapazita\u0308t", "nutzung", "oberboden", "open-data", "opendata", "sachdaten", "sand", "schadstoffbelastung", "schluff", "substrattypen", "tiefwurzelzone", "ton", "torfarten", "umweltatlas", "unterboden", "versiegelungsgrad"], "contacts": [{"organization": "Hr. Dr. Thelemann", "roles": ["creator"]}]}, "links": [{"href": "https://fbinter.stadt-berlin.de/fb/wfs/data/senstadt/s_boden_wfs1_2010"}, {"href": "http://data.europa.eu/88u/dataset/8e33abad-7706-3ec7-aaed-68945a752868"}, {"href": "https://registry.gdi-de.org/id/de.be.csw/0773fc98-b1d7-38c3-a1c2-050a6f1ad0f9"}, {"rel": "self", "type": "application/geo+json", "title": "8e33abad-7706-3ec7-aaed-68945a752868", "name": "item", "description": "8e33abad-7706-3ec7-aaed-68945a752868", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/8e33abad-7706-3ec7-aaed-68945a752868"}, {"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": "284d94b4-a0f7-4316-8ab9-5c6bf5facc06~~1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-26T16:37:55Z", "type": "Dataset", "language": "de", "title": "GcB\u00dcK400 \u2014 Lead in the upper floor", "description": "Lead is a toxic heavy metal and, due to its diverse industrial use, is ubiquitous in the environment. The input sources are not limited only to the range of ore deposits (especially lead sulphide and its oxidation minerals). Lead is also recorded anthropogenically through the prevention of lead, copper and zinc ores, the long-range exhaust pollution of motor vehicles (until the introduction of lead-free gasoline up to 60\u00a0% of atmospheric pollution), recycling plants of lead scrap, the use of heavy metal sewage sludges and composts, as well as by coal incineration plants. For uncontaminated soils, a Pb content of 2 to 60\u00a0mg/kg is indicated depending on the starting rock. The average Pb concentration of the upper continental earth crust (Clark value) is 17\u00a0mg/kg, the area-related mean Pb content for the Saxon main rock types is 20\u00a0mg/kg. The rocks of Saxony have no or only a small geochemical specialisation in terms of lead. In the northern or northeastern part of Saxony, relatively low levels of Pb occur in the upper soils above the curler sediments of the K\u00e4nozoikum (periglaziary sands, gravel, clay, loess) and the granodiorites of the Lusatia. With the looser sediments, the Pb content increases slightly with increasing tone content. The weathering soils above the solid rocks of the Ore Mountains, Vogtland and partly the Elbe Zone usually have significantly higher lead contents, which are caused by a relative enrichment in the base rocks. The most polluted area in Saxony is the Freiberg region. Due to the economically important polymetallic mineralisations (Pb-Zn-Ag), which are also relatively widespread in terms of area, there was a particularly strong Pb enrichment in the secondary rocks and consequently also in the formation of soils over the gneisen. In addition, enormous anthropogenic loads have been caused by the centuries-long prevention of primary ores and more recently in the recycling of lead batteries. Particularly high levels of Pb occur in the immediate vicinity of the metallurgical sites, including the main wind directions, in the central part of the quartz-sulfide mineralisations and in the river floodplains. Other areas with large-area elevated levels of Pb are mainly in the Osterzgebirge, in an area that extends from Freiberg in a southeast direction to the border in the Altenberg area and in the ore areas of the Middle and West Ore Mountains, such as Seiffen, Marienberg \u2014 Pobershau, Annaberg, Schneeberg, Schwarzenberg and P\u00f6hla. However, the percentage of Pb minerals in the ores of these regions is significantly lower. Due to frequent association of Pb and As in the mineralisations, the distribution area of the increased Pb levels in the Osterzgebirge and subordinated in the West Ore Mountains as well as in the meadows of the Freiberger and United Mulde is similar to that of the Arsen. The floodplains of the Freiberger Mulde produce extremely high lead content from the Freiberg deposit area, which continue to the floodplains of the United Mulde in northwestern Saxony. The floodplains of the Elbe and the Zwickau Mulde also have areas with higher lead levels due to geogenic or anthropogenic sources (storages, industry) in the catchment area. The lead content of the soils in the Freiberg area and in the meadows of the Freiberger and United Mulde partly exceeds the test and measure values of the Federal Soil Protection and Contaminant Ordinance (BBodSchV)", "keywords": ["anorganischer-schadstoff", "blei", "boden", "chemie", "chemisches-element", "de", "geologie", "opendata", "pb"]}, "links": [{"href": "https://luis.sachsen.de/boden/geodatendownload.html"}, {"href": "http://data.europa.eu/88u/dataset/284d94b4-a0f7-4316-8ab9-5c6bf5facc06~~1"}, {"href": "https://geoportal.sachsen.de/md/284d94b4-a0f7-4316-8ab9-5c6bf5facc06"}, {"rel": "self", "type": "application/geo+json", "title": "284d94b4-a0f7-4316-8ab9-5c6bf5facc06~~1", "name": "item", "description": "284d94b4-a0f7-4316-8ab9-5c6bf5facc06~~1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/284d94b4-a0f7-4316-8ab9-5c6bf5facc06~~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": "938e156d-161a-4b1f-905a-eaeea3d2a76b~~1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-26T16:37:58Z", "type": "Dataset", "language": "de", "title": "GcB\u00dcK400 \u2014 Cadmium in the upper floor", "description": "Cadmium deserves special attention among heavy metals, as its toxicity to animals and humans is significantly greater than that of other heavy metals. As an accumulation poison, it is enriched in the body and can remain there for decades. Due to its chemical kinship to zinc, it occurs almost exclusively with it, especially in all zinc-bearing minerals (including zinc aperture, galmei) and rocks. The average Cd concentration of the rocks of the upper continental earth crust (Clark value) is 0.1\u00a0mg/kg, in soils content is usually 0.50\u00a0mg/kg. In contrast to As and other heavy metals (e.g. Cr, Ni), no geochemical specialisation in Cd is detectable in the near-surface Saxon main rock types. The petrogeochemical component is 0.1\u00a0mg/kg in the Clark value range. In the ore deposits, Cd is mainly bound to the zinc ores of the polymetallic hydrothermal aisles and partly to the skarn deposits and straty-stratiform formations (chalkogenic component). Since the beginning of industrialisation, cadmium has entered the environment anthropogenically through emissions from the non-ferrous metalworks, the combustion of coal and petroleum, and more recently via electroplating, waste incineration, fertilisers, sewage sludges and composts. Whereas low levels dominate in the upper soils of North and Middle Axis (Cd-poor periglaciary sandy to loamy substrates; L\u00f6ss), a relative enrichment occurs in the weathering soils over solid rocks. A dependency on the clay content can therefore be observed that the sandy substrates have slightly lower Cd levels compared to clayy substrates. Higher Cd levels are found in arable and grassland sites compared to the forest sites in the upper soil, as a result of the very low pH values under forestry, Cd mobilisation and relocation to larger soil depths take place. Particularly high Cd loads are located in the Freiberg region, which are caused by the geogenic Cd enrichment in the formation of non-ferrous metal veins, but above all anthropogenic by the prevention of zinc ores. The highest levels can be found in the upper soils in the immediate vicinity of the metallurgical sites and at lower concentrations east of it (in the main wind direction). Other deposits with zinc debris in the Western Ore Mountains and the Ore Mountains border zone have only slightly increased grades. The meadows of the Freiberger and the United Mulde occupy a special position in the load with cadmium. Due to the removal of soils with geogenic enrichments in the catchment area and the enormous additional anthropogenic loads caused by the ore processing and the metallurgy industry, high Cd enrichments occur when the river sediments and swine parts are deposited in the flooding areas. In the floodplains of the Elbe and Zwickauer Mulde, on the other hand, significantly lower levels occur. The geogenic and anthropogenic processes in the Freiberg area and in the floodplains of the Freiberger and United Mulde lead to extensive exceedances of the test and measures values of the Federal Soil Protection and Contaminant Ordinance (BBodSchV) for cadmium.", "keywords": ["anorganischer-schadstoff", "boden", "cadmium", "chemie", "chemisches-element", "de", "geologie", "opendata"]}, "links": [{"href": "https://luis.sachsen.de/boden/geodatendownload.html"}, {"href": "http://data.europa.eu/88u/dataset/938e156d-161a-4b1f-905a-eaeea3d2a76b~~1"}, {"href": "https://geoportal.sachsen.de/md/938e156d-161a-4b1f-905a-eaeea3d2a76b"}, {"rel": "self", "type": "application/geo+json", "title": "938e156d-161a-4b1f-905a-eaeea3d2a76b~~1", "name": "item", "description": "938e156d-161a-4b1f-905a-eaeea3d2a76b~~1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/938e156d-161a-4b1f-905a-eaeea3d2a76b~~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": "231caf6e-aac7-3850-b578-dd00558df1aa", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-26T16:38:11Z", "type": "Dataset", "title": "Soil nutrient storage/pollutant binding capacity 2001 (environmental atlas)", "description": "Presentation of the nutrient storage/pollutant bonding capacity of soils on a block and block area basis, 1:50\u00a0000, as of 2001.", "formats": [{"name": "WMS_SRVC"}], "keywords": ["berlin", "boden", "bodenbewertung", "bodenfunktionen", "bodenfunktionskarte", "de", "effektive-kationenaustauschkapazita\u0308t", "geodaten", "kakeff", "karten", "na\u0308hrstoffspeichervermo\u0308gen", "open-data", "opendata", "schadstoffbindungsvermo\u0308gen", "schadstoffe", "umweltatlas"], "contacts": [{"organization": "Fr. Haag", "roles": ["creator"]}]}, "links": [{"href": "https://fbinter.stadt-berlin.de/fb/wms/senstadt/kb01_11_06schad"}, {"href": "http://data.europa.eu/88u/dataset/231caf6e-aac7-3850-b578-dd00558df1aa"}, {"href": "https://registry.gdi-de.org/id/de.be.csw/14bc4230-6ff9-3616-a77b-72756d331b26"}, {"rel": "self", "type": "application/geo+json", "title": "231caf6e-aac7-3850-b578-dd00558df1aa", "name": "item", "description": "231caf6e-aac7-3850-b578-dd00558df1aa", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/231caf6e-aac7-3850-b578-dd00558df1aa"}, {"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": "8a31c94e-0887-3b5f-9253-0db491194bd4", "type": "Feature", "geometry": {"type": "Polygon", "coordinates": [[[13.08, 52.33], [13.08, 52.69], [13.77, 52.69], [13.77, 52.33], [13.08, 52.33]]]}, "properties": {"updated": "2025-11-19T00:00:00Z", "type": "Dataset", "created": "2024-01-13", "language": "ger", "title": "Proximity to nature of soils 2020 (Environmental Atlas)", "description": "Proximity to nature of block and block surface soils, 1 : 5,000, as of 2020.", "formats": [{"name": "Text/HTML"}, {"name": "Downloaddienst - Naturn\u00e4he der B\u00f6den 2020 (Umweltatlas) (WFS)"}], "keywords": ["inspireidentifiziert", "open data", "opendata", "Karten", "Sachdaten", "Geodaten", "Berlin", "Umweltatlas", "Boden", "B\u00f6den", "Bodendaten", "Bodenfunktionskriterien", "regionale Seltenheit der Bodengesellschaften", "besondere naturr\u00e4umliche Eigenart", "Naturn\u00e4he", "Austauschh\u00e4ufigkeit des Bodenwassers", "N\u00e4hrstoffspeicherverm\u00f6gen", "Schadstoffbindungsverm\u00f6gen", "N\u00e4hrstoffversorgung", "Wasserversorgung", "Filterverm\u00f6gen", "Bindungsst\u00e4rke f\u00fcr Schwermetalle", "Pufferverm\u00f6gen im organischen Kohlenstoffhaushalt", "Grundwasserflurabstand", "Sonderstandorte", "Versickerung", "Boden", "Regional", "infoFeatureAccessService"], "contacts": [{"name": "Hr. Dr. Thelemann", "organization": "Senatsverwaltung f\u00fcr Mobilit\u00e4t, Verkehr, Klimaschutz und Umwelt Berlin", "position": null, "roles": ["pointOfContact"], "phones": [{"value": "+493090252487"}], "emails": [{"value": "michael.thelemann@senmvku.berlin.de"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": null}]}, {"name": "Fr. Haag", "organization": "Senatsverwaltung f\u00fcr Stadtentwicklung, Bauen und Wohnen Berlin", "position": null, "roles": ["pointOfContact"], "phones": [{"value": "+4930901395270"}], "emails": [{"value": "leilah.haag@senstadt.berlin.de"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": null}]}], "themes": [{"concepts": [{"id": "Boden"}], "scheme": "GEMET - INSPIRE themes, version 1.0"}, {"concepts": [{"id": "Regional"}], "scheme": "http://inspire.ec.europa.eu/metadata-codelist/SpatialScope"}]}, "links": [{"href": "https://gdi.berlin.de/services/wfs/ua_boden_naturnaehe_2020?request=GetCapabilities&service=WFS", "description": "Downloaddienst - Naturn\u00e4he der B\u00f6den 2020 (Umweltatlas) (WFS)", "protocol": "Downloaddienst - Naturn\u00e4he der B\u00f6den 2020 (Umweltatlas) (WFS)", "rel": "download"}, {"href": "https://gdi.berlin.de/services/wfs/ua_boden_naturnaehe_2020"}, {"href": "https://gdi.berlin.de/data/ua_boden_naturnaehe_2020/preview/svor_default.gif", "name": "preview", "description": "Web image thumbnail (URL)", "protocol": "WWW:LINK-1.0-http--image-thumbnail", "rel": "preview"}, {"rel": "self", "type": "application/geo+json", "title": "8a31c94e-0887-3b5f-9253-0db491194bd4", "name": "item", "description": "8a31c94e-0887-3b5f-9253-0db491194bd4", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/8a31c94e-0887-3b5f-9253-0db491194bd4"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date-time": "2025-11-19T00:00:00Z"}}, {"id": "d84986c3-30dd-3f39-a3a7-2975bc9a4f84~~1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-26T16:38:14Z", "type": "Dataset", "language": "de", "title": "Criteria for assessing soil functions 2005 (Environmental Atlas)", "description": "Evaluation criteria for six soil functions based on block map 1: 50,000 (ISU50, spatial reference environmental atlas 2005), processing status February 2009.", "formats": [{"name": "WFS_SRVC"}], "keywords": ["austauschha\u0308ufigkeit-des-bodenwassers", "berlin", "besondere-naturra\u0308umliche-eigenart", "bindungssta\u0308rke-an-schwermetalle", "boden", "bodenbewertung", "bodenfunktionen", "bodenfunktionskarte", "de", "filtervermo\u0308gen", "geodaten", "geologie", "kriterien-zur-bewertung-der-bodenfunktionen", "naturna\u0308he", "na\u0308hrstoffspeichervermo\u0308gen", "na\u0308hrstoffversorgung", "open-data", "opendata", "regelungsfunktion", "regionale-seltenheit-der-bodengesellschaften", "sachdaten", "schadstoffbindungsvermo\u0308gen", "umweltatlas", "versickerung", "wasserhaushalt", "wasserversorgung"], "contacts": [{"organization": "Hr. 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