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Next they were joined (40m x 40m grid cells) and finally scaled up to the required 1 by 1 km grid cells. This was done using the following tools: block statistics (mean), mosaic to new raster (mean), project to raster, block statistics (mean), resample (nearest neighbour) and project raster. Given the different origins of the individual maps, the uncertainty varies between maps. For instance, a map of the 90% confidence interval of the SOC stocks was produced for agricultural soils in Wallonia based on a Monte Carlo Approach taking into account both the measurement and the model uncertainties. For Flemish forest soils, spatial and analytical uncertainties were taken into account using bootstrapping techniques. 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This data layer shows the points with the highest modelled sediment supply to watercourses of the Flemish Hydrographic Atlas (VHA), canals and sewers, expressed in tonnes of sediment that reaches the water system at this location on average annually. These points together account for 10% of the total annual sediment supply to watercourses of the Flemish Hydrographic Atlas (VHA), canals and sewers. The modelling was performed with the CN-WS model version 4.2.2 in combination with pycnws version 0.5.4. The calculation was done on a scale of Flanders at a resolution of 20 m. This data layer is an indication of the average sediment supply calculated with an average precipitation erosivity factor of the last 30 years. Scenario A was applied, whereby agricultural parcels are considered grassland when they have a permanent crop cover for at least 2 consecutive years. All other agricultural parcels are considered to be average arable land. 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Elk van deze enkelvoudige observaties wordt gekenmerkt door \u00e9\u00e9n parameter en \u00e9\u00e9n meetwaarde (hetzij numeriek, vrije tekst of een item uit een keuzelijst).\n\nMeervoudige observaties zijn reeksen van metingen \u2013 in dit geval wordt \u00e9\u00e9n parameter beschreven door meerdere numerieke meetwaarden.\n\nObservaties die gekoppeld worden aan een diepteinterval of bodemmonster gelden altijd voor de volledige diepte van dit diepteinterval of monster. 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A soil association is a substantive and spatial grouping of soil series (legendary units of the Belgian soil map 1:20,000). An association is characterized by a fairly constant ratio between the area occupied by a number of typical soil series. Often the nature of the association is indicated in terms of a dominant, associated and included series. For areas for which no soil map was available in the early 1970s, extrapolations were made using geological information and expert knowledge.", "formats": [{"name": "KML"}], "keywords": ["associatiekaart", "be", "bodem", "bodemassociatiekaart", "bodemassociaties-atlas-van-belgie\u0308", "bodemgebruik", "bodemkaart", "bodemprofielontwikkeling", "bodemtextuur", "databank-ondergrond-vlaanderen", "departement-omgeving", "dov", "ondergrond", "streek", "vlaanderen"], "contacts": [{"organization": "Vlaamse overheid, Departement Omgeving, Vlaams Planbureau voor Omgeving (VPO)", "roles": ["creator"]}, {"organization": "https://org.belgif.be/id/CbeEstablishmentUnit/2143719695", "roles": ["publisher"]}]}, "links": [{"href": "https://metadata.vlaanderen.be/srv/dut/catalog.search#/metadata/1c183909-f405-47f2-8dba-942f6016f8c7"}, {"href": "https://www.vlaanderen.be/DataCatalogRecord/1c183909-f405-47f2-8dba-942f6016f8c7"}, {"href": "http://data.europa.eu/88u/dataset/4c25e84f-a8fe-461d-b519-c5dc1808b312"}, {"rel": "self", "type": "application/geo+json", "title": "4c25e84f-a8fe-461d-b519-c5dc1808b312", "name": "item", "description": "4c25e84f-a8fe-461d-b519-c5dc1808b312", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/4c25e84f-a8fe-461d-b519-c5dc1808b312"}, {"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": "4dbc2c1f-12e2-4fca-8930-b853301cfbc3", "type": "Feature", "geometry": null, "properties": {"updated": "2024-02-20T00:00:00Z", "type": "Dataset", "language": "nl", "title": "Specific sediment supply (2020)", "description": "Soil erosion leads to sediment transport through the landscape until sedimentation occurs on land or the sediment flow reaches watercourses, canals or sewers. This data layer shows the areas with the modelled specific sediment supply to watercourses of the Flemish Hydrographic Atlas (VHA), canals and sewerage, expressed in tonnes of sediment that reaches the water system on average annually per hectare. For this purpose, the total sediment input into the area is divided by the area of the area. The area classification is based on the intermediate catchment areas, as defined by the VMM. The modelling was performed with the CN-WS model version 4.2.2 in combination with pycnws version 0.5.4. The calculation was done on a scale of Flanders at a resolution of 20 m. This data layer is an indication of the average sediment supply calculated with an average precipitation erosivity factor of the last 30 years. Scenario A was applied, whereby agricultural parcels are considered grassland when they have a permanent crop cover for at least 2 consecutive years. All other agricultural parcels are considered to be average arable land. The modelling is based on the 2020 agricultural parcel map. The erosion control measures implemented in 2020 through management agreements or through small-scale erosion control works were taken into account. Locally, the modelled values may differ from the real values, as each modelling is only an approximation of reality. 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These data were calculated by means of digital soil mapping based on point observations of this soil property and area-covering predictor layers. The current dataset was calculated on the basis of the historical base data of the soil mapping (1945-1975). 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The map is the sum of water and tillage erosion. The map takes into account 4 types of land use: forest, permanent cover, agricultural crops without permanent cover and other land use. The map is based on the soil erosion map aggregated for each agricultural parcel in Flanders (2010).  The original map on parcel level is a product of computer modeling with a spatial resolution of 5 m * 5 m by the \"Physical and Regional Geography Division, Department of Earth and Environmental Sciences, K.U. Leuven\". The calculation of water erosion is based on the Revised Soil Loss Equation (RUSLE, Renard et al., 1991) using a 2 dimensional approach for calculating the LS factor based on Desmet and Govers (1996).  The water erosion is calculated with a crop factor of 0,001 for forest, a crop factor of 0,01 for permanent cover (excluding forest), a crop factor of 0,37 for other agricultural crops and a crop factor of 0 for other land use. 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This data layer shows the areas with the modelled specific sediment supply to watercourses of the Flemish Hydrographic Atlas (VHA), canals and sewerage, expressed in tonnes of sediment that reaches the water system on average annually per hectare. For this purpose, the total sediment input into the area is divided by the area of the area. The zoning is based on the intermediate catchment areas (A1 areas), as defined by the VMM in the context of the 2022-2027 River Basin Management Plans. The modelling was carried out with the CN-WS model version 4.2.3 in combination with pycnws version 0.6.3. The calculation was done on a scale of Flanders at a resolution of 20 m. This data layer is an indication of the average sediment supply calculated with an average precipitation erosivity factor of the last 30 years. Scenario A was applied, whereby agricultural parcels are considered grassland when they have a permanent crop cover for at least 2 consecutive years. All other agricultural parcels are considered to be average arable land. The modelling is based on the 2022 agricultural parcel map. The anti-erosion measures implemented in 2022 through management agreements or small-scale anti-erosion works were taken into account. Locally, the modelled values may differ from the real values, as each modelling is only an approximation of reality. 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For instance, a map of the 90% confidence interval of the SOC stocks was produced for agricultural soils in Wallonia based on a Monte Carlo Approach taking into account both the measurement and the model uncertainties. For Flemish forest soils, spatial and analytical uncertainties were taken into account using bootstrapping techniques. For Flemish agricultural soils, the uncertainty reported is the model uncertainty on point estimates for each data point, in which the estimated model parameters are simulated 1000 times as being independent normal distributed variables using their model estimation and standard error as distribution parameters. No additional uncertainty is taken into account for the conversion functions that use the stochastic variables \"bulk density\". The SOC stock maps are the first comprehensive map for Belgium integrating grasslands, croplands and forests. 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The data was prepared according to the methodology of SERENA SOC loss cookbook. The objective of SERENA project was to develop methods to calculate and map soil-based ecosystem services and soil threats. Soil organic carbon concentration was used as an indicator for soil organic carbon loss (ST). The map was based on digital soil mapping according to the method used in the EJP SOIL project WP6: Digital soil mapping approach with random forest using ISRIC workflow seedling. To create the soil organic carbon concentration map, we used soil organic carbon data of the regional soil organic carbon monitoring network Cmon in Flanders (0-10 and 10-30 cm soil layer). The soil organic carbon concentration of the 0-20 cm was derived from the 0-10 and 10-30 cm data. 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For a complete view of all attribute information of the soil profiles, please refer to the complete Pottery-Flanders-2010 database. Pottery-Flanders-2010 is a database with the description and analysis results of 7,020 soil profiles and 42,529 associated soil horizons, supplemented with 9,281 surface samples, all located on the territory of Flanders and Brussels. These data (143 variables) were collected during the systematic soil profile study, which was carried out in Belgium between 1949 and 1971, under the auspices of the Institute to encourage Scientific Research in Industry and Agriculture. The Centre for Ground Research of the University of Ghent with departments at the Catholic University of Leuven and the Facult\u00e9s des Sciences Agronomiques de Gembloux was responsible for the realization of this study.", "keywords": ["aardewerk-2010", "aardewerk:-bodemprofielgegevens-voor-vlaanderen", "be", "bewortelingsdiepte", "bodem", "bodemhorizonten", "bodemkaarten", "bodemlagen", "bodemoppervlak", "bodemprofielen", "bodemprofielgegevens", "bodemprofielstudie", "bodemserie", "diepten", "drainage", "fysico-chemische-eigenschappen", "granulometrische-gegevens", "grondonderzoek", "historisch-bodemgebruik-en-vegetatie", "horizontinformatie", "koolstofgehalte", "mineralogische-samenstelling", "oppervlaktemonsters", "profiellocaties", "relief-beschrijving", "roestverschijnselen", "sorptiecapaciteit", "stenen", "verzadigingsgraad", "vochtgehalte", "waterhuishouding", "zuurtegraad"], "contacts": [{"organization": "Vlaamse overheid, Departement Omgeving, Vlaams Planbureau voor Omgeving (VPO)", "roles": ["creator"]}, {"organization": "https://org.belgif.be/id/CbeEstablishmentUnit/2143719695", "roles": ["publisher"]}]}, "links": [{"href": "https://www.vlaanderen.be/DataCatalogRecord/d75bf375-18f1-4d51-af0c-f247f7ad45f1"}, {"href": "http://data.europa.eu/88u/dataset/91003194-b189-40f8-abb9-01a2696d8788"}, {"rel": "self", "type": "application/geo+json", "title": "91003194-b189-40f8-abb9-01a2696d8788", "name": "item", "description": "91003194-b189-40f8-abb9-01a2696d8788", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/91003194-b189-40f8-abb9-01a2696d8788"}, {"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": "965C0C41-DFC6-43F7-9F03-44B4DFB1398C", "type": "Feature", "geometry": null, "properties": {"updated": "2002-07-22T00:00:00Z", "type": "Dataset", "language": "nl", "title": "Inventory Dredging soils in Flanders", "description": "The GIS file is part of a large database built under the auspices of the Ministry of the Flemish Community, Dep. LIN, Waterways and Marine Administration (AWZ). It contains the locations and land use of the dredging soils in Flanders (polygons), the locations where soil samples were taken during the inventory and the analysis results of the soil and leaf samples. Currently, data are available for the Upper Scheldt, the Sea Scheldt, the Lys ( + tourist Lys + diversion channel), the Yser (+ channel Ypres - Yser), the Durme and the Dender. The appropriate usage scale is 1:10,000.", "keywords": ["ae\u0308robe", "afleidingskanaal", "awz", "baggergronden", "baggerspecie", "be", "bladstaal", "bladstalen", "bodem", "bodemprofiel", "bodemstaal", "bodemstalen", "bomen", "bosbouw", "bovenschelde", "bruggen", "caco", "cadmiumconcentratie", "calciumcarbonaat", "chroomconcentratie", "dredgis", "fosfor", "fosforconcentratie", "gentbrugge", "ibw", "ieper", "ijzer", "infrastructuur", "inventarisatie-baggergronden-in-vlaanderen", "kanaal", "krijgt", "landbouwgewassen", "landgebruiksklasse", "lazerdiffractie", "leie", "loodconcentratie", "monstercode", "monsternamepunt", "nikkelconcentratie", "ringvaart", "rivierarmen", "sluizen", "staalname", "stenen", "stikstofconcentratie", "stof", "stroomgebied", "terreincode", "textuur", "vegetatie", "waterloop", "waterlopen", "waterwegen", "wildbeheer", "zeeschelde", "zeewezen", "zinkconcentratie", "zn", "zuurtegraad", "zwavelconcentratie"], "contacts": [{"organization": "Datavindplaats Vlaanderen", "roles": ["creator"]}, {"organization": "https://org.belgif.be/id/CbeEstablishmentUnit/2199335933", "roles": ["publisher"]}]}, "links": [{"href": "https://www.vlaanderen.be/DataCatalogRecord/27AB4BF7-AFF7-4D06-9350-E9FC40AC2480"}, {"href": "http://data.europa.eu/88u/dataset/965c0c41-dfc6-43f7-9f03-44b4dfb1398c"}, {"rel": "self", "type": "application/geo+json", "title": "965C0C41-DFC6-43F7-9F03-44B4DFB1398C", "name": "item", "description": "965C0C41-DFC6-43F7-9F03-44B4DFB1398C", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/965C0C41-DFC6-43F7-9F03-44B4DFB1398C"}, {"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": "974da6e1-b1de-44ee-831a-41b35eb9ccda", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-13T16:29:31Z", "type": "Dataset", "language": "nl", "title": "Minerals model loam", "description": "The 'Delfstoffenmodel Leem' is the first voxel model drawn up by VITO on behalf of the Flemish government, Department LNE, Department of Natural Resources. The volume model shows the Quartaire (niveo)-eolic clay deposits in Flanders. These loam deposits are part of the east-west oriented European loam belt. These sediments are still important in the brick, and more generally, the ceramic industry. These late Pleistocene loam deposits occur in the southern part of Flanders and cover older Quartaire and Neogene and Paleogene sediments. The model divides the loam package into volume units of 100*100*0.5m. 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