{"type": "FeatureCollection", "features": [{"id": "10.1002/hyp.14966", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-24T16:14:04Z", "type": "Journal Article", "created": "2023-09-15", "title": "Testing CASE: A new event\u2010based Morgan\u2010Morgan\u2010Finney\u2010type erosion model for different rainfall experimental scenarios", "description": "Abstract<p>Every application of soil erosion models brings the need of proper parameterisation, that is, finding physically or conceptually plausible parameter values that allow a model to reproduce measured values. No universal approach for model parameterisation, calibration and validation exists, as it depends on the model, spatial and temporal resolution and the nature of the datasets used. We explored some existing options for parameterisation, calibration and validation for erosion modelling exemplary with a specific dataset and modelling approach. A new Morgan\uffe2\uff80\uff90Morgan\uffe2\uff80\uff90Finney (MMF)\uffe2\uff80\uff90type model was developed, representing a balanced position between physically\uffe2\uff80\uff90based and empirical modelling approaches. The resulting model termed \uffe2\uff80\uff98calculator for soil erosion\uffe2\uff80\uff99 (CASE), works in a spatially distributed way on the timescale of individual rainfall events. A dataset of 142 high\uffe2\uff80\uff90intensity rainfall experiments in Central Europe (AT, HU, IT, CZ), covering various slopes, soil types and experimental designs was used for calibration and validation with a modified Monte\uffe2\uff80\uff90Carlo approach. Subsequently, model parameter values were compared to parameter values obtained by alternative methods (measurements, pedotransfer functions, literature data). The model reproduced runoff and soil loss of the dataset in the validation setting with R2adj of 0.89 and 0.76, respectively. Satisfactory agreement for the water phase was found, with calibrated saturated hydraulic conductivity (ksat) values falling within the interquartile range of ksat predicted with 14 different pedotransfer functions, or being within one order of magnitude. The chosen approach also well reflected specific experimental setups contained in the dataset dealing with the effects of consecutive rainfall and different soil water conditions. For the sediment phase of the tested model agreement between calibrated cohesion, literature values and field measurements were only partially in line. The methods we explored may specifically be interesting for use with other MMF\uffe2\uff80\uff90type models, or with similar datasets.</p", "keywords": ["Revised Morgan-Morgan-Finney model", "Model calibration", "Model validation", "Morgan-Morgan-Finney model", "Erosion modelling", "CASE; erosion modelling; model calibration; model validation; Morgan-Morgan-Finney model; pedotransfer function; revised Morgan-Morgan-Finney model; surface runoff", "CASE", "15. Life on land", "Pedotransfer function", "Surface runoff"]}, "links": [{"href": "https://iris.unito.it/bitstream/2318/1945820/1/A54%20HydrProc%20Brunner.pdf"}, {"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.14966"}, {"href": "https://doi.org/10.1002/hyp.14966"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Hydrological%20Processes", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1002/hyp.14966", "name": "item", "description": "10.1002/hyp.14966", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1002/hyp.14966"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-09-01T00:00:00Z"}}, {"id": "10.1016/j.jhydrol.2022.128322", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-24T16:16:33Z", "type": "Journal Article", "created": "2022-08-23", "title": "Soil surface connectivity of tilled soil with wheel tracks and its development under simulated rainfall", "description": "Project Co-ordinators: Dr. Jose Alfonso G\u00f3mez Calero (Instituto de Agricultura Sostenible (IAS-CISC), Dr. Weifeng Xu (Fujian Agriculture and Forest University, FAFU). -- Trabajo desarrollado bajo la financiaci\u00f3n del proyecto \u201cSoil Hydrology research platform underpinning innovation to manage water scarcity in European and Chinese cropping Systems\u201d (773903), coordinado por Jos\u00e9 Alfonso G\u00f3mez Calero, investigador del Instituto de Agricultura Sostenible (IAS). Although wheel tracks cover only a small portion of the surface of agricultural fields, their effect on surface runoff and sediment transport is substantial. Wheel tracks change the microrelief of the soil surface, and influence how the surface is further altered by rainfall and runoff. This study presents a plot-scale microrelief analysis of a tilled surface with wheel tracks under simulated rainfall. Digital elevation models of the microrelief with 1 cm spatial resolution were obtained using the Structure from Motion method. The random roughness, the structural connectivity, and functional connectivity were calculated for before-rainfall and after-rainfall soil surface conditions. The experiments were carried out on inclined, freshly-tilled plots (8 m long, 2 m wide). The wheel tracks were created by four passages of machinery in the slope direction (SWT) and in the contour-line direction (CWT). The experiments were compared to reference plots without wheel tracks (NWT). The wheel tracks increase water and sediment connectivity if they are oriented in slope-wise direction. Microrelief analysis shows that SWT drains water from the surrounding soil. The soil surface adjacent to SWT can also become more connected with the wheel track, due to changes in microrelief introduced by rainfall and runoff. The calculated higher connectivity in the SWT plot corresponded to the measured increased sediment loads. This suggests faster overland flow and therefore shorter flow pathways on the soil surface microrelief. CWT leads to a decrease in the water and sediment connectivity compared to the NWT and SWT plots. Although the surface runoff can overflow the CWT, the network of flow paths results in decreased flow velocity and a slower sediment transport rate. However, the CWT effect is not permanent, and declines as the wheel tracks become silted with the deposited sediment. It is shown that detailed microrelief data provide relevant information for a study of the changes in flow routing in a tilled agricultural field with the presence of a wheel track. SWT accelerates the runoff and especially the sediment transport. During a rainfall event, the hydraulic connection between the wheel track and the surrounding soil increases dramatically. CWT reduces the surface runoff and also the sediment transport. In the long term, rainfall events and surface runoff alter the microrelief connectivity, causing the soil surface to be more hydraulically connected, irrespective of the wheel track orientation. This study demonstrates the effect of wheel tracks on water and sediment transport. The results draw attention to the importance of appropriate soil protection measures, as a bare unprotected surface microrelief exposed to rainfall leads to increased sediment connectivity. This research was supported by Horizon 2020 research and innovation program project no 773903 under the title \u201cShui \u2013 Soil Hydrology research platform underpinning innovation to manage water scarcity in European and Chinese cropping systems\u201d, by Ministry of Education, Youth and Sports of the Czech Republic project no. LTAUSA19019 \u201cConnectivity of sediment transport within intensively-used rural catchments\u201d, and by Ministry of Agriculture of the Czech Republic project no. QK1920224\u201d Ways of soil erosion protection on the farm level after glyphosate ban\u201d. Additional support from Grant Agency of the Czech Technical University in Prague project no. SGS20/156/OHK1/3T/11 \u201cMonitoring, experiments, and mathematical modelling of rainfall runoff and soil erosion processes\u201d is also gratefully acknowledged. Peer reviewed", "keywords": ["2. Zero hunger", "Connectivity", "Erosion", "Structure from motion", "Microrelief", "0207 environmental engineering", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "02 engineering and technology", "15. Life on land", "Surface runoff", "6. Clean water", "Agricultural fields"]}, "links": [{"href": "https://doi.org/10.1016/j.jhydrol.2022.128322"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Hydrology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.jhydrol.2022.128322", "name": "item", "description": "10.1016/j.jhydrol.2022.128322", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.jhydrol.2022.128322"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-10-01T00:00:00Z"}}, {"id": "10.1016/j.polymertesting.2025.108824", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-24T16:16:37Z", "type": "Journal Article", "created": "2025-04-26", "title": "A cost-effective protocol for detecting fluorescent microplastics in arable soils to study redistribution processes", "description": "Understanding microplastics' (MPs) transport from soils to aquatic ecosystems is challenging due to labor-intensive detection methods, especially in large-scale plot experiments analyzing surface runoff and soil erosion. To address this, we used fluorescent MPs as tracers and developed a cost-effective protocol to detect them in dry soils and eroded sediments. We analyzed spherical polyethylene (PE: 125\u2013150\u00a0\u03bcm; 425\u2013500\u00a0\u03bcm) and irregular polylactic acid (PLA: 125\u2013150\u00a0\u03bcm; 250\u2013300\u00a0\u03bcm). Sample assays were prepared primarily based on dry and wet sieving. Subsequent darkroom photography under 365\u00a0nm illumination, and thresholding and segmentation-based image analysis were done. The developed protocol demonstrates high reliability, precision, and F-scores of 88.7\u00a0%\u00a0\u00b1\u00a02.9\u00a0%, 85.2\u00a0%\u00a0\u00b1\u00a03.1\u00a0%, and 86.9\u00a0%\u00a0\u00b1\u00a02.8\u00a0%. PE exhibited slightly higher recovery rates (85\u00a0%\u00a0\u00b1\u00a05\u00a0%) than PLA (79\u00a0%\u00a0\u00b1\u00a08\u00a0%). Particle size influenced recovery, with larger MPs achieving significantly higher recovery. Smaller particles showed slightly lower recovery under dry soil conditions, but their recovery improved under sediment conditions facilitated by wet sieving and ultrasonication. All fluorescent MPs retained >95\u00a0% detectability after three months of storage, highlighting marker temporal stability. Compared to existing methods, this protocol eliminates complex digestion steps, reduces costs, and ensures minimal contamination, providing a robust framework for MP transport studies. It offers potential for enhancement through advanced imaging and machine learning, enabling more efficient and accessible detection in environmental research.", "keywords": ["Soil", "Microplastic transport", "Identification", "TP1080-1185", "Sediment monitoring", "Polymers and polymer manufacture", "Surface runoff", "Fluorescence"]}, "links": [{"href": "https://doi.org/10.1016/j.polymertesting.2025.108824"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Polymer%20Testing", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.polymertesting.2025.108824", "name": "item", "description": "10.1016/j.polymertesting.2025.108824", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.polymertesting.2025.108824"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-06-01T00:00:00Z"}}, {"id": "10.3390/w15061247", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-24T16:20:39Z", "type": "Journal Article", "created": "2023-03-22", "title": "Slowing Down Quick Runoff\u2014A New Approach for the Delineation and Assessment of Critical Points, Contributing Areas, and Proposals of Measures to Reduce Non-Point Water Pollution from Agricultural Land", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Non-point sources of water pollution caused by agricultural crop production are a serious problem in Czechia, at present. This paper describes a new approach for the mutual delineation and assessment of different pollution sources where the critical points method is used to identify the origin of contamination and the source areas. The critical points, i.e., sites presenting the entry of quick surface and drainage runoff into waters, are classified into three (for surface pollution sources using a WaTEM/SEDEM model) or four (subsurface = drainage sources via the catchment-measures need index) categories, respectively. This enabled us to prioritize the most endangered areas at different scales, ranging from the third-order catchments to very small subcatchments, and to design the appropriate combination of control measures to mitigate surface and drainage water runoff, with these being the main drivers of associated pollution. This methodology was applied to a study conducted in the Czech Republic within the entire Vltava River basin, with a total area of 27,578 km2, and utilized in depth to assess a 543 km2 catchment of the Vla\u0161imsk\u00e1 Blanice River. When the effect of the designed surface runoff control measures system had been assessed for sediment transport through outlet profiles of the fourth-order catchments, the average reduction reached 43%. The total reduction in the subsurface transport of nitrogen within the fourth-order catchments was 24%. The approach and results are planned to be projected into river basin management plans for the Vltava River basin. Nevertheless, a thorough reassessment of current legislations and strategies is needed to enable the broader adoption of mitigation measures and sustainable management patterns within agricultural landscapes.</p></article>", "keywords": ["2. Zero hunger", "Non-point agricultural water pollution", "13. Climate action", "11. Sustainability", "Drainage water management", "catchment prioritization; critical point; drainage water management; non-point agricultural water pollution; surface runoff; water retention", "Water retention", "15. Life on land", "Catchment prioritization", "Surface runoff", "6. Clean water", "12. Responsible consumption", "Critical point"]}, "links": [{"href": "http://www.mdpi.com/2073-4441/15/6/1247/pdf"}, {"href": "https://www.mdpi.com/2073-4441/15/6/1247/pdf"}, {"href": "https://doi.org/10.3390/w15061247"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Water", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3390/w15061247", "name": "item", "description": "10.3390/w15061247", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3390/w15061247"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-03-22T00:00:00Z"}}, {"id": "10.5281/zenodo.14773242", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-24T16:22:06Z", "type": "Dataset", "title": "Covariate datasets used to predict soil property distribution in EJP Soil mapping", "description": "These datasets were prepared within the scope of the EJP SOIL programme. The datasets are extracted from different sources, clipped and reprojected to EPSG:3035. The sources are listed in the table below. The datasets were used as environmental layers to prodict soil property distribution (soil maps) at National and continental level within the EJP SOIL programme.\u00a0  Dataset sources:     Copernicus Climate Data Store https://cds.climate.copernicus.eu/cdsapp#!/dataset/reanalysis-era5-land-monthly-means?tab=overview   RESOLVE Biodiversity and Wildlife Solutions https://ecoregions2017.appspot.com/   Copernicus Land Monitoring Service https://sentinel.esa.int/web/sentinel/user-guides/sentinel-1-sar/   European Union/ESA/Copernicus https://sentinel.esa.int/web/sentinel/user-guides/sentinel-1-sar/   GLiM - Global Lithological Map https://www.geo.uni-hamburg.de/en/geologie/forschung/aquatische-geochemie/glim.html", "keywords": ["Europe", "Soil sciences", "Land cover", "Lithology", "Altitude", "Solar radiation", "Temperature", "Atmospheric precipitation", "Surface runoff"], "contacts": [{"organization": "Poggio, Laura", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5281/zenodo.14773242"}, {"rel": "self", "type": "application/geo+json", "title": "10.5281/zenodo.14773242", "name": "item", "description": "10.5281/zenodo.14773242", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5281/zenodo.14773242"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-01-30T00:00:00Z"}}, {"id": "10261/277927", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-24T16:23:48Z", "type": "Journal Article", "created": "2022-08-23", "title": "Soil surface connectivity of tilled soil with wheel tracks and its development under simulated rainfall", "description": "Project Co-ordinators: Dr. Jose Alfonso G\u00f3mez Calero (Instituto de Agricultura Sostenible (IAS-CISC), Dr. Weifeng Xu (Fujian Agriculture and Forest University, FAFU). -- Trabajo desarrollado bajo la financiaci\u00f3n del proyecto \u201cSoil Hydrology research platform underpinning innovation to manage water scarcity in European and Chinese cropping Systems\u201d (773903), coordinado por Jos\u00e9 Alfonso G\u00f3mez Calero, investigador del Instituto de Agricultura Sostenible (IAS). Although wheel tracks cover only a small portion of the surface of agricultural fields, their effect on surface runoff and sediment transport is substantial. Wheel tracks change the microrelief of the soil surface, and influence how the surface is further altered by rainfall and runoff. This study presents a plot-scale microrelief analysis of a tilled surface with wheel tracks under simulated rainfall. Digital elevation models of the microrelief with 1 cm spatial resolution were obtained using the Structure from Motion method. The random roughness, the structural connectivity, and functional connectivity were calculated for before-rainfall and after-rainfall soil surface conditions. The experiments were carried out on inclined, freshly-tilled plots (8 m long, 2 m wide). The wheel tracks were created by four passages of machinery in the slope direction (SWT) and in the contour-line direction (CWT). The experiments were compared to reference plots without wheel tracks (NWT). The wheel tracks increase water and sediment connectivity if they are oriented in slope-wise direction. Microrelief analysis shows that SWT drains water from the surrounding soil. The soil surface adjacent to SWT can also become more connected with the wheel track, due to changes in microrelief introduced by rainfall and runoff. The calculated higher connectivity in the SWT plot corresponded to the measured increased sediment loads. This suggests faster overland flow and therefore shorter flow pathways on the soil surface microrelief. CWT leads to a decrease in the water and sediment connectivity compared to the NWT and SWT plots. Although the surface runoff can overflow the CWT, the network of flow paths results in decreased flow velocity and a slower sediment transport rate. However, the CWT effect is not permanent, and declines as the wheel tracks become silted with the deposited sediment. It is shown that detailed microrelief data provide relevant information for a study of the changes in flow routing in a tilled agricultural field with the presence of a wheel track. SWT accelerates the runoff and especially the sediment transport. During a rainfall event, the hydraulic connection between the wheel track and the surrounding soil increases dramatically. CWT reduces the surface runoff and also the sediment transport. In the long term, rainfall events and surface runoff alter the microrelief connectivity, causing the soil surface to be more hydraulically connected, irrespective of the wheel track orientation. This study demonstrates the effect of wheel tracks on water and sediment transport. The results draw attention to the importance of appropriate soil protection measures, as a bare unprotected surface microrelief exposed to rainfall leads to increased sediment connectivity. This research was supported by Horizon 2020 research and innovation program project no 773903 under the title \u201cShui \u2013 Soil Hydrology research platform underpinning innovation to manage water scarcity in European and Chinese cropping systems\u201d, by Ministry of Education, Youth and Sports of the Czech Republic project no. LTAUSA19019 \u201cConnectivity of sediment transport within intensively-used rural catchments\u201d, and by Ministry of Agriculture of the Czech Republic project no. QK1920224\u201d Ways of soil erosion protection on the farm level after glyphosate ban\u201d. Additional support from Grant Agency of the Czech Technical University in Prague project no. SGS20/156/OHK1/3T/11 \u201cMonitoring, experiments, and mathematical modelling of rainfall runoff and soil erosion processes\u201d is also gratefully acknowledged. Peer reviewed", "keywords": ["2. Zero hunger", "Connectivity", "Structure from motion", "0207 environmental engineering", "04 agricultural and veterinary sciences", "02 engineering and technology", "15. Life on land", "Surface runoff", "6. Clean water", "Agricultural fields", "Erosion", "Microrelief", "0401 agriculture", " forestry", " and fisheries"]}, "links": [{"href": "https://doi.org/10261/277927"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Hydrology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10261/277927", "name": "item", "description": "10261/277927", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10261/277927"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-10-01T00:00:00Z"}}, {"id": "10261/366355", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-24T16:23:51Z", "type": "Journal Article", "created": "2023-03-22", "title": "Slowing Down Quick Runoff\u2014A New Approach for the Delineation and Assessment of Critical Points, Contributing Areas, and Proposals of Measures to Reduce Non-Point Water Pollution from Agricultural Land", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Non-point sources of water pollution caused by agricultural crop production are a serious problem in Czechia, at present. This paper describes a new approach for the mutual delineation and assessment of different pollution sources where the critical points method is used to identify the origin of contamination and the source areas. The critical points, i.e., sites presenting the entry of quick surface and drainage runoff into waters, are classified into three (for surface pollution sources using a WaTEM/SEDEM model) or four (subsurface = drainage sources via the catchment-measures need index) categories, respectively. This enabled us to prioritize the most endangered areas at different scales, ranging from the third-order catchments to very small subcatchments, and to design the appropriate combination of control measures to mitigate surface and drainage water runoff, with these being the main drivers of associated pollution. This methodology was applied to a study conducted in the Czech Republic within the entire Vltava River basin, with a total area of 27,578 km2, and utilized in depth to assess a 543 km2 catchment of the Vla\u0161imsk\u00e1 Blanice River. When the effect of the designed surface runoff control measures system had been assessed for sediment transport through outlet profiles of the fourth-order catchments, the average reduction reached 43%. The total reduction in the subsurface transport of nitrogen within the fourth-order catchments was 24%. The approach and results are planned to be projected into river basin management plans for the Vltava River basin. Nevertheless, a thorough reassessment of current legislations and strategies is needed to enable the broader adoption of mitigation measures and sustainable management patterns within agricultural landscapes.</p></article>", "keywords": ["2. Zero hunger", "Non-point agricultural water pollution", "13. Climate action", "11. Sustainability", "Drainage water management", "catchment prioritization; critical point; drainage water management; non-point agricultural water pollution; surface runoff; water retention", "Water retention", "15. Life on land", "Catchment prioritization", "Surface runoff", "6. Clean water", "12. Responsible consumption", "Critical point"]}, "links": [{"href": "http://www.mdpi.com/2073-4441/15/6/1247/pdf"}, {"href": "https://www.mdpi.com/2073-4441/15/6/1247/pdf"}, {"href": "https://doi.org/10261/366355"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Water", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10261/366355", "name": "item", "description": "10261/366355", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10261/366355"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-03-22T00:00:00Z"}}, {"id": "10.5281/zenodo.3660940", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-24T16:22:36Z", "type": "Dataset", "title": "Long-term data from field erosion plot studies in eastern Austria", "description": "Long-term runoff plot experiments were conducted at three sites in eastern Austria to evaluate the impact of conservation tillage. Following soil tillage treatments were investigated: 1) conventional tillage with ploughing in fall (CT), 2) mulch tillage with cover crops during winter period (MT), and 3) no tillage with cover crops during winter period (NT). Soil textures range from silt loam to loam. Datasets include for each site and each year the period of operation of the plots, the planted crop, the annual precipitation, surface runoff, soil loss, surface losses of nitrogen, phopshorus and soil organic carbon as well as absolute and relative crop yields.", "keywords": ["2. Zero hunger", "soil erosion", " surface runoff", " field erosion plots", " no-till", " tillage practices", "runoff plots", " conservation tillage", " soil erosion", " surface runoff", " crop yield", " nutrient losses", "15. Life on land", "6. Clean water"], "contacts": [{"organization": "Klik, Andreas, Rosner. Josef,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5281/zenodo.3660940"}, {"rel": "self", "type": "application/geo+json", "title": "10.5281/zenodo.3660940", "name": "item", "description": "10.5281/zenodo.3660940", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5281/zenodo.3660940"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-10-11T00:00:00Z"}}, {"id": "2318/1945820", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-24T16:24:44Z", "type": "Journal Article", "created": "2023-09-15", "title": "Testing CASE: A new event\u2010based Morgan\u2010Morgan\u2010Finney\u2010type erosion model for different rainfall experimental scenarios", "description": "Abstract<p>Every application of soil erosion models brings the need of proper parameterisation, that is, finding physically or conceptually plausible parameter values that allow a model to reproduce measured values. No universal approach for model parameterisation, calibration and validation exists, as it depends on the model, spatial and temporal resolution and the nature of the datasets used. We explored some existing options for parameterisation, calibration and validation for erosion modelling exemplary with a specific dataset and modelling approach. A new Morgan\uffe2\uff80\uff90Morgan\uffe2\uff80\uff90Finney (MMF)\uffe2\uff80\uff90type model was developed, representing a balanced position between physically\uffe2\uff80\uff90based and empirical modelling approaches. The resulting model termed \uffe2\uff80\uff98calculator for soil erosion\uffe2\uff80\uff99 (CASE), works in a spatially distributed way on the timescale of individual rainfall events. A dataset of 142 high\uffe2\uff80\uff90intensity rainfall experiments in Central Europe (AT, HU, IT, CZ), covering various slopes, soil types and experimental designs was used for calibration and validation with a modified Monte\uffe2\uff80\uff90Carlo approach. Subsequently, model parameter values were compared to parameter values obtained by alternative methods (measurements, pedotransfer functions, literature data). The model reproduced runoff and soil loss of the dataset in the validation setting with R2adj of 0.89 and 0.76, respectively. Satisfactory agreement for the water phase was found, with calibrated saturated hydraulic conductivity (ksat) values falling within the interquartile range of ksat predicted with 14 different pedotransfer functions, or being within one order of magnitude. The chosen approach also well reflected specific experimental setups contained in the dataset dealing with the effects of consecutive rainfall and different soil water conditions. For the sediment phase of the tested model agreement between calibrated cohesion, literature values and field measurements were only partially in line. The methods we explored may specifically be interesting for use with other MMF\uffe2\uff80\uff90type models, or with similar datasets.</p", "keywords": ["Revised Morgan-Morgan-Finney model", "Model calibration", "Model validation", "Morgan-Morgan-Finney model", "Erosion modelling", "CASE; erosion modelling; model calibration; model validation; Morgan-Morgan-Finney model; pedotransfer function; revised Morgan-Morgan-Finney model; surface runoff", "CASE", "15. Life on land", "Pedotransfer function", "Surface runoff"]}, "links": [{"href": "https://iris.unito.it/bitstream/2318/1945820/1/A54%20HydrProc%20Brunner.pdf"}, {"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.14966"}, {"href": "https://doi.org/2318/1945820"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Hydrological%20Processes", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "2318/1945820", "name": "item", "description": "2318/1945820", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2318/1945820"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-09-01T00:00:00Z"}}, {"id": "b8eac95c-0196-444e-ba04-64fb0b0ee626", "type": "Feature", "geometry": {"type": "Polygon", "coordinates": [[[13.78, 53.38], [13.78, 53.38], [13.79, 53.38], [13.79, 53.38], [13.78, 53.38]]]}, "properties": {"rights": "Restrictions applied to assure the protection of privacy or intellectual property, and any special restrictions or limitations or warnings on using the resource or metadata. Reports, articles, papers, scientific and non - scientific works of any form, including tables, maps, or any other kind of output, in printed or electronic form, based in whole or in part on the data supplied, must contain an acknowledgement of the form: \"Data reused from the BonaRes Data Centre www.bonares.de. This data were created as part of the ZALF Datenerfassung's research activities.\" Although every care has been taken in preparing and testing the data, the ZALF Datenerfassung and the BonaRes Data Centre cannot guarantee that the data are correct; neither does the ZALF Datenerfassung and the BonaRes Data Centre accept any liability whatsoever for any error, missing data or omission in the data, or for any loss or damage arising from its use. The ZALF Datenerfassung and BonaRes Data Centre will not be responsible for any direct or indirect use which might be made of the data.", "updated": "2023-11-29", "type": "Service", "created": "2023-11-23", "language": "eng", "title": "Web Map Service of the dataset 'Soil hydraulic data from laboratory rainfall simulation experiments to induce subsurface lateral subsurface flow in 2D soil monoliths'", "description": "This Web Map Service includes spatial information used by dataset: 'Soil hydraulic data from laboratory rainfall simulation experiments to induce subsurface lateral subsurface flow in 2D soil monoliths''", "keywords": ["infoMapAccessService", "Soil", "laboratory experimentation", "subsurface runoff", "soil hydraulic properties", "tensometers", "soil water content", "Soil", "laboratory experimentation", "subsurface runoff", "soil hydraulic properties", "tensometers", "soil water content", "Germany", "Brandenburg", "Uckermark", "Quillow", "Dedelow", "Site CarboZALF"], "contacts": [{"name": "Leibniz Centre for Agricultural Landscape Research", "organization": "ZALF", "position": "Research Platform 'Data Analysis & Simulation' - Workgroup Research Data Management", "roles": ["publisher"], "phones": [{"value": "+49 33432 82 300"}], "emails": [{"value": "dataservice@zalf.de"}], "addresses": [{"deliveryPoint": ["Eberswalder Strasse 84"], "city": "M\u00fcncheberg", "administrativeArea": "Brandenburg", "postalCode": "15374", "country": "Germany"}], "links": [{"href": {"url": null, "protocol": null, "protocol_url": "", "name": "https://ror.org/01ygyzs83", "name_url": "", "description": "ROR", "description_url": "", "applicationprofile": null, "applicationprofile_url": "", "function": null}}]}, {"name": "Annelie Ehrhardt", "organization": "Leibniz Centre for Agricultural Landscape Research", "position": null, "roles": ["author"], "phones": [{"value": null}], "emails": [{"value": "annelie.ehrhardt@zalf.de"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": {"url": null, "protocol": null, "protocol_url": "", "name": "0000-0003-0512-4814", "name_url": "", "description": "ORCID", "description_url": "", "applicationprofile": null, "applicationprofile_url": "", "function": null}}]}, {"name": "Horst H. 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Reports, articles, papers, scientific and non - scientific works of any form, including tables, maps, or any other kind of output, in printed or electronic form, based in whole or in part on the data supplied, must contain an acknowledgement of the form: \"Data reused from the BonaRes Data Centre www.bonares.de. This data were created as part of the ZALF Datenerfassung's research activities.\" Although every care has been taken in preparing and testing the data, the ZALF Datenerfassung and the BonaRes Data Centre cannot guarantee that the data are correct; neither does the ZALF Datenerfassung and the BonaRes Data Centre accept any liability whatsoever for any error, missing data or omission in the data, or for any loss or damage arising from its use. The ZALF Datenerfassung and BonaRes Data Centre will not be responsible for any direct or indirect use which might be made of the data.", "updated": "2023-12-06", "type": "Dataset", "created": "2023-11-23", "language": "eng", "title": "Soil hydraulic data from laboratory rainfall simulation experiments to induce subsurface lateral subsurface flow in 2D soil monoliths", "description": "The dataset contains results of laboratory experiments to induce subsurface lateral subsurface flow in 2D soil monoliths taken from a horizon boundary of hummocky ground moraine in Dedelow (north Brandenburg, Germany). Four soil monoliths were sampled along a Btg-CBkg horizon boundary of an Eroded Haplic Luvisol (monoliths: e_ha_LV_1, e_ha_LV_2) and a CBkg-sand lense boundary of a Haplic Regosol (monoliths: ha_RG_3, ha_RG_4). The monoliths were placed under a rainfall simulator in the laboratory and 12 tensiometers and 6 FDR-sensors to measure soil matric potential and soil water content were installed in the upper and lower horizon. Vertical flow through the monoliths and lateral flow along the horizon boundary was measured via a bottom and a side suction disc. The experimental procedure is described in detail in the technical note by Ehrhardt et al. (2022). The dataset includes for each monolith a detailed protocol of applied rainfall rates and pressured heads at the side and bottom suctions discs. For each measurement period (data was subdivided in up to four periods due to large data size)of the monoliths data of the tensiometers and FDR-sensors (calibrated and uncalibrated) as well as calibration data for these sensors are included. Also, the location of the sensors and horizon boundary and the amount of water drained from the side and the bottom of the monolith is given. 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