{"type": "FeatureCollection", "features": [{"id": "10.22541/essoar.171865325.50703739/v1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:20:28Z", "type": "Journal Article", "created": "2024-06-17", "title": "Physics-Informed Neural Networks for Estimating a Continuous Form of the Soil Water Retention Curve from Basic Soil Properties", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p id='p1'>The soil water retention curve (SWRC) is essential for describing water and energy exchange processes at the interface between the solid earth and the atmosphere. Despite its importance, measuring the SWRC using standard laboratory methods is challenging and time-consuming. This paper presents a novel physics-informed neural network (PINN) approach for developing pedotransfer functions (PTFs) to predict continuous SWRCs based on soil texture, organic carbon content, and dry bulk density. In contrast to conventional parametric PTFs developed for specific SWRC models, the PINN learns a non-specific form of the SWRC by effectively integrating both measurements and physical constraints into the training process. This approach allows the estimated SWRC to maintain its physical integrity from saturation to oven-dry conditions, even in scenarios with sparse data. The new approach is particularly effective for tackling the challenges encountered in developing PTFs on large SWRC datasets, which often have an imbalance towards the wet-end and include numerous samples with limited and unevenly distributed measurements. We compared the performance of the PINN with that of a conventional physics-agnostic neural network using a dataset of 4200 soil samples. While both networks performed similarly at the wet-end where data are abundant, the PINN excelled at the dry-end where data are sparse and unevenly distributed, achieving a normalized RMSE of 0.172 compared to 0.522 for the conventional neural network. The SWRC derived from the PINN is differentiable with respect to the matric potential and can be seamlessly integrated into the governing equations of water flow in the unsaturated zone.</p></article>", "keywords": ["Environmental sciences", "physics-constrained machine learning", "physics\u2010constrained machine learning", "soil hydraulic properties", "GE1-350", "15. Life on land", "continuous pedotransfer functions"]}, "links": [{"href": "https://doi.org/10.22541/essoar.171865325.50703739/v1"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Water%20Resources%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.22541/essoar.171865325.50703739/v1", "name": "item", "description": "10.22541/essoar.171865325.50703739/v1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.22541/essoar.171865325.50703739/v1"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-06-17T00:00:00Z"}}, {"id": "10.1002/hyp.14966", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:14:16Z", "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/bs.agron.2022.11.003", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:15:23Z", "type": "Report", "created": "2022-12-23", "title": "The challenge in estimating soil compressive strength for use in risk assessment of soil compaction in field traffic", "description": "<p>Society calls for protection of agricultural soils in order to sustain the production of foods for a growing population. Compaction of subsoil layers is an increasing problem in modern agriculture and a cause of serious concern because of the poor resilience in natural amelioration. The concept of soil precompression stress has been adapted from civil engineering, although in soil science it is applied to unsaturated soils that have developed a secondary structure from the action of weather, biota and tillage. It assumes strain is elastic at loads up to the precompression stress, while plastic deformation is expected at higher stresses. To determine this threshold we performed uniaxial, confined compression tests for a total of 584 minimally disturbed soil cores sampled at three subsoil layers on nine Danish soils ranging in clay content from 0.02 to 0.38 kg kg<sup>\u22121</sup>. The cores were drained to either of three matric potentials (\u221250, \u2212100 or \u2212 300 hPa) prior to loading. Stress was applied by a constant-strain rate method. We estimated the point of maximum curvature of the strain-log<sub>10</sub>(normal stress) relation by a numerical procedure. This point is considered here as a compactive stress threshold, typically labeled the soil precompression stress, \u03c3<sub>pc</sub>. The preload suction stress (PSS) was calculated as the product of initial (i.e., before loading) water suction and initial degree of pore water saturation. Multiple regressions were performed to evaluate the effect of soil properties (textural classes, volumetric water content, bulk density (BD), soil organic matter (SOM), and PSS) on \u03c3<sub>pc</sub>. The best model explained 39% of the variation in \u03c3<sub>pc</sub>, and indicated that \u03c3<sub>pc</sub> increases with increasing PSS, BD and SOM. For a given combination of clay, BD and SOM, PSS affected \u03c3<sub>pc</sub> negatively. We recommend our regression model for use in risk assessment tools for estimating sustainable traffic on agricultural soils. The model was validated by five independent data sets from the literature. Our study shows that caution should be applied when regarding \u03c3<sub>pc</sub> as a fixed threshold for compressive strength. We hypothesize that plastic deformation is initiated over a range of stress rather than at a distinctive single value. Further studies are needed to better understand\u2014and potentially quantify\u2014to what extent the predicted \u03c3<sub>pc</sub> can be regarded a central estimate of allowable stress for a given soil.</p>", "keywords": ["2. Zero hunger", "Suction stress", "Sustainability", "Soil strength", "Uniaxial compression test", "Precompression stress", "15. Life on land", "Pedotransfer function", "Soil compaction", "Soil degradation", "Risk assessment"]}, "links": [{"href": "https://doi.org/10.1016/bs.agron.2022.11.003"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/bs.agron.2022.11.003", "name": "item", "description": "10.1016/bs.agron.2022.11.003", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/bs.agron.2022.11.003"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-01-01T00:00:00Z"}}, {"id": "10.22541/essoar.171926389.99753202/v1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:20:28Z", "type": "Journal Article", "created": "2024-06-17", "title": "Physics-Informed Neural Networks for Estimating a Continuous Form of the Soil Water Retention Curve from Basic Soil Properties", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p id='p1'>The soil water retention curve (SWRC) is essential for describing water and energy exchange processes at the interface between the solid earth and the atmosphere. Despite its importance, measuring the SWRC using standard laboratory methods is challenging and time-consuming. This paper presents a novel physics-informed neural network (PINN) approach for developing pedotransfer functions (PTFs) to predict continuous SWRCs based on soil texture, organic carbon content, and dry bulk density. In contrast to conventional parametric PTFs developed for specific SWRC models, the PINN learns a non-specific form of the SWRC by effectively integrating both measurements and physical constraints into the training process. This approach allows the estimated SWRC to maintain its physical integrity from saturation to oven-dry conditions, even in scenarios with sparse data. The new approach is particularly effective for tackling the challenges encountered in developing PTFs on large SWRC datasets, which often have an imbalance towards the wet-end and include numerous samples with limited and unevenly distributed measurements. We compared the performance of the PINN with that of a conventional physics-agnostic neural network using a dataset of 4200 soil samples. While both networks performed similarly at the wet-end where data are abundant, the PINN excelled at the dry-end where data are sparse and unevenly distributed, achieving a normalized RMSE of 0.172 compared to 0.522 for the conventional neural network. The SWRC derived from the PINN is differentiable with respect to the matric potential and can be seamlessly integrated into the governing equations of water flow in the unsaturated zone.</p></article>", "keywords": ["Environmental sciences", "physics-constrained machine learning", "physics\u2010constrained machine learning", "soil hydraulic properties", "GE1-350", "15. Life on land", "continuous pedotransfer functions"]}, "links": [{"href": "https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2024WR038149"}, {"href": "https://doi.org/10.22541/essoar.171926389.99753202/v1"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Water%20Resources%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.22541/essoar.171926389.99753202/v1", "name": "item", "description": "10.22541/essoar.171926389.99753202/v1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.22541/essoar.171926389.99753202/v1"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-06-17T00:00:00Z"}}, {"id": "10.3389/fpls.2018.01158", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:20:46Z", "type": "Journal Article", "created": "2018-08-08", "title": "Simulation of Soil Organic Carbon Effects on Long-Term Winter Wheat (Triticum aestivum) Production Under Varying Fertilizer Inputs", "description": "Soil organic carbon (SOC) has a vital role to enhance agricultural productivity and for mitigation of climate change. To quantify SOC effects on productivity, process models serve as a robust tool to keep track of multiple plant and soil factors and their interactions affecting SOC dynamics. We used soil-plant-atmospheric model viz. DAISY, to assess effects of SOC on nitrogen (N) supply and plant available water (PAW) under varying N fertilizer rates in winter wheat (Triticum aestivum) in Denmark. The study objective was assessment of SOC effects on winter wheat grain and aboveground biomass accumulation at three SOC levels (low: 0.7% SOC; reference: 1.3% SOC; and high: 2% SOC) with five nitrogen rates (0-200 kg N ha-1) and PAW at low, reference, and high SOC levels. The three SOC levels had significant effects on grain yields and aboveground biomass accumulation at only 0-100 kg N ha-1 and the SOC effects decreased with increasing N rates until no effects at 150-200 kg N ha-1. PAW had significant positive correlation with SOC content, with high SOC retaining higher PAW compared to low and reference SOC. The mean PAW and SOC correlation was given by PAW% = 1.0073 \u00d7 SOC% + 15.641. For the 0.7-2% SOC range, the PAW increase was small with no significant effects on grain yields and aboveground biomass accumulation. The higher winter wheat grain and aboveground biomass was attributed to higher N supply in N deficient wheat production system. Our study suggested that building SOC enhances agronomic productivity at only 0-100 kg N ha-1. Maintenance of SOC stock will require regular replenishment of SOC, to compensate for the mineralization process degrading SOC over time. Hence, management can maximize realization of SOC benefits by building up SOC and maintaining N rates in the range 0-100 kg N ha-1, to reduce the off-farm N losses depending on the environmental zones, land use and the production system.", "keywords": ["0301 basic medicine", "Crop productivity; DAISY model; Grain yield; Long-term experiment; Nitrogen; Pedotransfer functions; Plant available water;", "Nitrogen", "QH301 Biology", "DAISY model", "pedotransfer functions", "Plant Science", "nitrogen", "SB1-1110", "QH301", "03 medical and health sciences", "Long-term experiment", "SDG 13 - Climate Action", "Grain yield", "SDG 2 - Zero Hunger", "European Commission", "289694", "crop productivity", "SDG 15 - Life on Land", "2. Zero hunger", "020", "Pedotransfer functions", "0303 health sciences", "grain yield", "Plant culture", "15. Life on land", "plant available water", "13. Climate action", "Crop productivity", "Plant available water", "SMARTSOIL", "long-term experiment"]}, "links": [{"href": "https://flore.unifi.it/bitstream/2158/1138671/1/Ghaley%20et%20al%202018_Frontiers%20in%20Plant%20Science.pdf"}, {"href": "https://doi.org/10.3389/fpls.2018.01158"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Frontiers%20in%20Plant%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3389/fpls.2018.01158", "name": "item", "description": "10.3389/fpls.2018.01158", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3389/fpls.2018.01158"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-08-08T00:00:00Z"}}, {"id": "10.5281/zenodo.16725281", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:23:02Z", "type": "Dataset", "title": "PTF4Med: two pseudo-continuous neural network pedotransfer functions for the water retention curve in the Mediterranean Region", "description": "This dataset was compiled to develop and validate two pseudo-continuous pedotransfer functions (PTFs), HYDRO-GRAV and HYDRO-VOL, for estimating gravimetric and volumetric soil water content across multiple matric potentials in Mediterranean region. The file, provided in Excel format, contains two sheets: HYDRO-GRAV and HYDRO-VOL. In the HYDRO-GRAV sheet, the field U reports gravimetric soil water content, while in the HYDRO-VOL sheet, it reports volumetric soil water content. Both sheets include the same set of predictors and metadata: SAND (sand content, %), CLAY (clay content, %), OC (organic carbon, %), Pot (soil matric potential, kPa), Dataset (source dataset name), ID (unique sample identifier), Location (site or region), Date (sampling date, when available), Latitude and Longitude (geographic coordinates), Layer description (description of the soil layer), Layer number (sequential number of the soil layer), and Upper limit and Lower limit (depth limits of the soil layer, cm). The dataset harmonizes legacy soil data from multiple Mediterranean sources, providing measurements of soil water content at different matric potentials. These data enabled pseudo-continuous modeling through artificial neural networks and were used to train and evaluate the HYDRO-GRAV and HYDRO-VOL models.", "keywords": ["Mediterranean Region", "water retention curve", "pedotransfer functions", "pseudo-continuous PTFs", "soil legacy data"]}, "links": [{"href": "https://doi.org/10.5281/zenodo.16725281"}, {"rel": "self", "type": "application/geo+json", "title": "10.5281/zenodo.16725281", "name": "item", "description": "10.5281/zenodo.16725281", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5281/zenodo.16725281"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-08-02T00:00:00Z"}}, {"id": "10.5281/zenodo.16926945", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:23:03Z", "type": "Dataset", "title": "Adjusted bulk density data in the Hungarian Soil Information and Monitoring System", "description": "This dataset provides corrected bulk density (BD) values and their associated uncertainty estimates for 4,340 soil genetic horizons across 1,236 monitoring sites of the Hungarian Soil Information and Monitoring System. The correction was achieved by developing a pedotransfer function (PTF) based on the Hungarian Detailed Soil Hydro-physical Database (Hungarian acronym: MARTHA) and advanced machine learning algorithms. Soil properties (i.e., soil organic carbon, pH in water, and sand, silt, and clay content) together with environmental covariates, used as proxies for the soil forming factors, were integrated into the PTF development to improve predictive performance.  Uncertainty of the BD predictions is provided in two forms: (1) the 90% prediction interval (defined by its lower and upper limits, within which the true value is expected to occur nine times out of ten), and (2) the standard error of the corrected BD values. To ensure transparency, reproducibility, and open access, the corrected BD values, their corresponding uncertainty estimates, and the developed code are publicly available.  For more details / to cite this dataset please use:  Sohrab, S., Szab\u00f3, B., P\u00e1sztor, L., Mak\u00f3, A., Szatm\u00e1ri, G. (2025). Adjusting bulk density observations in the Hungarian Soil Information and Monitoring System using advanced pedotransfer functions. European Journal of Soil Science (submitted manuscript)  Codes are available on GitHub:  https://github.com/Mehrsoh/Soil-BD-Correction  Description of the files:  Two versions of the same dataset are provided, differing only in file format: (1) 'HUN-SIMS_BD_corrected.csv' \u2013 CSV format (separated by semicolon), and (2) 'HUN-SIMS_BD_corrected.xlsx' \u2013 Microsoft Excel format. The table below summarizes the column names, units, and data formats, and also provides a description for each column. Note that the coordinate reference system is the Hungarian Unified National Projection System (HD72/EOV; EPSG: 23700). For more details, see https://epsg.io/23700.       Column name    Format    Unit    Description      PROFILE_ID    string    -    Identifier of monitoring sites in the Hungarian Soil Information and Monitoring System      LAYER_ID    string    -    Identifier of soil genetic horizons at a monitoring site      X    numeric    [m]    X coordinate      Y    numeric    [m]    Y coordinate      TOP    numeric    [cm]    Upper depth boundary of soil genetic horizons      BOTTOM    numeric    [cm]    Lower depth boundary of soil genetic horizons      BD_CORRECTED    numeric    [g\u00b7cm-3]    Bias-corrected bulk density value      Q_05    numeric    [g\u00b7cm-3]    5th quantile; lower limit of the 90% prediction interval      Q_95    numeric    [g\u00b7cm-3]    95th quantile; upper limit of the 90% prediction interval      SE    numeric    [g\u00b7cm-3]    Standard error of the bias-corrected bulk density value", "keywords": ["Soil sciences", "Soil health", "Earth and related environmental sciences", "Soil physics", "Soil monitoring", "FOS: Earth and related environmental sciences", "Pedotransfer function"], "contacts": [{"organization": "Sohrab, Seyedehmehrmanzar, Szab\u00f3, Brigitta, P\u00e1sztor, L\u00e1szl\u00f3, Mak\u00f3, Andr\u00e1s, Szatm\u00e1ri, G\u00e1bor,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5281/zenodo.16926945"}, {"rel": "self", "type": "application/geo+json", "title": "10.5281/zenodo.16926945", "name": "item", "description": "10.5281/zenodo.16926945", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5281/zenodo.16926945"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-09-04T00:00:00Z"}}, {"id": "2318/1945820", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:25:29Z", "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": "11577/3454795", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:24:50Z", "type": "Journal Article", "created": "2021-12-09", "title": "Soil Water Retention as Affected by Management Induced Changes of Soil Organic Carbon: Analysis of Long-Term Experiments in Europe", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Soil water retention (SWR) is an important soil property related to soil structure, texture, and organic matter (SOM), among other properties. Agricultural management practices affect some of these properties in an interdependent way. In this study, the impact of management-induced changes of soil organic carbon (SOC) on SWR is evaluated in five long-term experiments in Europe (running from 8 up to 54 years when samples were taken). Topsoil samples (0\u201315 cm) were collected and analysed to evaluate the effects of three different management categories, i.e., soil tillage, the addition of exogenous organic materials, the incorporation of crop residues affecting SOC and water content under a range of matric potentials. Changes in the total SOC up to 10 g C kg\u22121 soil (1%) observed for the different management practices, do not cause statistically significant differences in the SWR characteristics as expected. The direct impact of the SOC on SWR is consistent but negligible, whereas the indirect impact of SOC in the higher matric potentials, which are mainly affected by soil structure and aggregate composition, prevails. The different water content responses under the various matric potentials to SOC changes for each management group implies that one conservation measure alone has a limited effect on SWR and only a combination of several practices that lead to better soil structure, such as reduced soil disturbances combined with increased SOM inputs can lead to better water holding capacity of the soil.</p></article>", "keywords": ["no-till", "compost", "BULK-DENSITY", "Environmental Studies", "PHYSICAL-PROPERTIES", "Environmental Sciences & Ecology", "SEQUESTRATION", "3301 Architecture", "TILLAGE SYSTEMS", "4104 Environmental management", "PEDOTRANSFER FUNCTIONS", "FERTILIZATION", "soil care", "0502 Environmental Science and Management", "soil organic carbon; soil-water content; no-till; reduced tillage; manure; compost; soil care", "soil-water content", "2. Zero hunger", "Science & Technology", "S", "HYDRAULIC CONDUCTIVITY", "3304 Urban and regional planning", "Agriculture", "reduced tillage", "04 agricultural and veterinary sciences", "15. Life on land", "6. Clean water", "soil organic carbon", "manure", "0401 agriculture", " forestry", " and fisheries", "NO-TILLAGE", "RESIDUE MANAGEMENT", "Life Sciences & Biomedicine", "MATTER"]}, "links": [{"href": "http://www.mdpi.com/2073-445X/10/12/1362/pdf"}, {"href": "https://www.research.unipd.it/bitstream/11577/3454795/1/land-10-01362-v2.pdf"}, {"href": "https://www.mdpi.com/2073-445X/10/12/1362/pdf"}, {"href": "https://doi.org/11577/3454795"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Land", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "11577/3454795", "name": "item", "description": "11577/3454795", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/11577/3454795"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-12-09T00:00:00Z"}}, {"id": "11585/1012654", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-05-01T16:24:51Z", "type": "Journal Article", "created": "2023-03-03", "title": "Accounting for the spatial range of soil properties in pedotransfer functions", "description": "Pedotransfer functions (PTF) are widely used in soil hydraulic property modelling. Accounting for spatial structures of soil properties for improving the model performance of PTF is increasingly discussed. To understand how model performance varies when PTF are trained with samples of different spatial structure of the input data, we developed 12 ePTF (ensemble PTF) with data input from differently sized spatial domains to predict field capacity (FC) and wilting point (WP) of agriculturally used soils in Austria. The training domains generally had diameters equal to or larger than the spatial range of the explaining variables (bulk density BD, organic carbon content OC, Sand, Silt, and Clay) and the response variable (FC or WP). A stepwise regression technique was used to train the ePTF, and both bootstrap and random sampling were used to evaluate the uncertainties of the various ePTF. We found that, a training domain considerably larger than the spatial range of the input variables did not help develop a roubust ePTF, particularly when applied on relatively larger scales, independent of their performances during the training stage. We conclude that, covering additional heterogeneous samples from outside of the spatial range of the input variables does not ensure an enhanced prediction capability of ePTF. Also, it might be worth paying more attention to the spatial structure of the predicted variable when its spatial range might be expected to be quite different from the predictors. This would have an implication for guiding sampling practices.", "keywords": ["Pedotransfer function; Ensemble prediction; Spatial structure; uncertainty"]}, "links": [{"href": "https://cris.unibo.it/bitstream/11585/1012654/1/2023_Wang_Geoderma.pdf"}, {"href": "https://doi.org/11585/1012654"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Geoderma", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "11585/1012654", "name": "item", "description": "11585/1012654", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/11585/1012654"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-04-01T00:00:00Z"}}, {"id": "20.500.11850/688246", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:25:15Z", "type": "Journal Article", "created": "2024-07-29", "title": "Hydro-pedotransfer functions: a roadmap for future development", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Abstract. Hydro-pedotransfer functions\u00a0(PTFs) relate easy-to-measure and readily available soil information to soil hydraulic properties\u00a0(SHPs) for applications in a wide range of process-based and empirical models, thereby enabling the assessment of soil hydraulic effects on hydrological, biogeochemical, and ecological processes. At least more than 4 decades of research have been invested to derive such relationships. However, while models, methods, data storage capacity, and computational efficiency have advanced, there are fundamental concerns related to the scope and adequacy of current PTFs, particularly when applied to parameterise models used at the field scale and beyond. Most of the PTF development process has focused on refining and advancing the regression methods, while fundamental aspects have remained largely unconsidered. Most soil systems are not represented in PTFs, which have been built mostly for agricultural soils in temperate climates. Thus, existing PTFs largely ignore how parent material, vegetation, land use, and climate affect processes that shape SHPs. The PTFs used to parameterise the Richards\u2013Richardson equation are mostly limited to predicting parameters of the van\u00a0Genuchten\u2013Mualem soil hydraulic functions, despite sufficient evidence demonstrating their shortcomings. Another fundamental issue relates to the diverging scales of derivation and application, whereby PTFs are derived based on laboratory measurements while often being applied at the field to regional scales. Scaling, modulation, and constraining strategies exist to alleviate some of these shortcomings in the mismatch between scales. These aspects are addressed here in a joint effort by the members of the International Soil Modelling Consortium\u00a0(ISMC) Pedotransfer Functions Working Group with the aim of systematising PTF research and providing a roadmap guiding both PTF development and use. We close with a 10-point catalogue for funders and researchers to guide review processes and research.</p></article>", "keywords": ["Technology", "550", "Bodenanalyse", "Modell", "SPHAGNUM MOSS", "Environmental technology. Sanitary engineering", "630", "Ing\u00e9nierie", " informatique & technologie", "Biogeochemical process", "Earth and Planetary Sciences (miscellaneous)", "Geography. Anthropology. Recreation", "GE1-350", "SATURATED HYDRAULIC CONDUCTIVITY", "Geosciences", " Multidisciplinary", "TD1-1066", "Water Science and Technology", "2. Zero hunger", "T", "Geology", "Hydraulics effects", "Agriculture & agronomy", "Life sciences", "Daten", "Pedo-transfer functions", "6. Clean water", "Soil hydraulics", "REFLECTANCE SPECTROSCOPY", "Roadmap", "Physical Sciences", "Sciences du vivant", "Water Resources", "SOIL-WATER-RETENTION", "0406 Physical Geography and Environmental Geoscience", "3709 Physical geography and environmental geoscience", "Process-based modeling", "Environmental Engineering", "Physique", " chimie", " math\u00e9matiques & sciences de la terre", "PHYSICAL-PROPERTIES", "SENSITIVITY-ANALYSIS", "Soil hydraulic properties", "0905 Civil Engineering", "333", "G", "Physical", " chemical", " mathematical & earth Sciences", "Empirical model", "Agriculture & agronomie", "Life Science", "UNSATURATED CONDUCTIVITY", "SEASONAL-CHANGES", "Pedotransfer functions", "HYSTERETIC MOISTURE PROPERTIES", "info:eu-repo/classification/ddc/550", "Science & Technology", "3707 Hydrology", "Physikochemische Bodeneigenschaft", "500", "15. Life on land", "Engineering", " computing & technology", "Sciences de la terre & g\u00e9ographie physique", "Environmental sciences", "0907 Environmental Engineering", "13. Climate action", "ITC-ISI-JOURNAL-ARTICLE", "Earth sciences & physical geography", "HETEROGENEOUS SOILS", "4013 Geomatic engineering", "ITC-GOLD", "Hydrological process"]}, "links": [{"href": "https://orbi.uliege.be/bitstream/2268/321088/1/hess-28-3391-2024.pdf"}, {"href": "https://hess.copernicus.org/articles/28/3391/2024/hess-28-3391-2024.pdf"}, {"href": "https://doi.org/20.500.11850/688246"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Hydrology%20and%20Earth%20System%20Sciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "20.500.11850/688246", "name": "item", "description": "20.500.11850/688246", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/20.500.11850/688246"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-07-29T00:00:00Z"}}, {"id": "2164/10968", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:25:25Z", "type": "Journal Article", "created": "2018-08-08", "title": "Simulation of Soil Organic Carbon Effects on Long-Term Winter Wheat (Triticum aestivum) Production Under Varying Fertilizer Inputs", "description": "Soil organic carbon (SOC) has a vital role to enhance agricultural productivity and for mitigation of climate change. To quantify SOC effects on productivity, process models serve as a robust tool to keep track of multiple plant and soil factors and their interactions affecting SOC dynamics. We used soil-plant-atmospheric model viz. DAISY, to assess effects of SOC on nitrogen (N) supply and plant available water (PAW) under varying N fertilizer rates in winter wheat (Triticum aestivum) in Denmark. The study objective was assessment of SOC effects on winter wheat grain and aboveground biomass accumulation at three SOC levels (low: 0.7% SOC; reference: 1.3% SOC; and high: 2% SOC) with five nitrogen rates (0-200 kg N ha-1) and PAW at low, reference, and high SOC levels. The three SOC levels had significant effects on grain yields and aboveground biomass accumulation at only 0-100 kg N ha-1 and the SOC effects decreased with increasing N rates until no effects at 150-200 kg N ha-1. PAW had significant positive correlation with SOC content, with high SOC retaining higher PAW compared to low and reference SOC. The mean PAW and SOC correlation was given by PAW% = 1.0073 \u00d7 SOC% + 15.641. For the 0.7-2% SOC range, the PAW increase was small with no significant effects on grain yields and aboveground biomass accumulation. The higher winter wheat grain and aboveground biomass was attributed to higher N supply in N deficient wheat production system. Our study suggested that building SOC enhances agronomic productivity at only 0-100 kg N ha-1. Maintenance of SOC stock will require regular replenishment of SOC, to compensate for the mineralization process degrading SOC over time. Hence, management can maximize realization of SOC benefits by building up SOC and maintaining N rates in the range 0-100 kg N ha-1, to reduce the off-farm N losses depending on the environmental zones, land use and the production system.", "keywords": ["0301 basic medicine", "Crop productivity; DAISY model; Grain yield; Long-term experiment; Nitrogen; Pedotransfer functions; Plant available water;", "Nitrogen", "QH301 Biology", "DAISY model", "pedotransfer functions", "Plant Science", "nitrogen", "SB1-1110", "QH301", "03 medical and health sciences", "Long-term experiment", "SDG 13 - Climate Action", "Grain yield", "SDG 2 - Zero Hunger", "European Commission", "289694", "crop productivity", "SDG 15 - Life on Land", "2. Zero hunger", "020", "Pedotransfer functions", "0303 health sciences", "grain yield", "Plant culture", "15. Life on land", "plant available water", "13. Climate action", "Crop productivity", "Plant available water", "SMARTSOIL", "long-term experiment"]}, "links": [{"href": "https://flore.unifi.it/bitstream/2158/1138671/1/Ghaley%20et%20al%202018_Frontiers%20in%20Plant%20Science.pdf"}, {"href": "https://doi.org/2164/10968"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Frontiers%20in%20Plant%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "2164/10968", "name": "item", "description": "2164/10968", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2164/10968"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-08-08T00:00:00Z"}}, {"id": "2164/6134", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:25:27Z", "type": "Journal Article", "created": "2016-05-13", "title": "Modeling Soil Processes: Review, Key Challenges, and New Perspectives", "description": "Core Ideas                     <p>                                                                           <p>A community effort is needed to move soil modeling forward.</p>                                                                             <p>Establishing an international soil modeling consortium is key in this respect.</p>                                                                             <p>There is a need to better integrate existing knowledge in soil models.</p>                                                                             <p>Integration of data and models is a key challenge in soil modeling.</p>                                                                     </p>                     <p>The remarkable complexity of soil and its importance to a wide range of ecosystem services presents major challenges to the modeling of soil processes. Although major progress in soil models has occurred in the last decades, models of soil processes remain disjointed between disciplines or ecosystem services, with considerable uncertainty remaining in the quality of predictions and several challenges that remain yet to be addressed. First, there is a need to improve exchange of knowledge and experience among the different disciplines in soil science and to reach out to other Earth science communities. Second, the community needs to develop a new generation of soil models based on a systemic approach comprising relevant physical, chemical, and biological processes to address critical knowledge gaps in our understanding of soil processes and their interactions. Overcoming these challenges will facilitate exchanges between soil modeling and climate, plant, and social science modeling communities. It will allow us to contribute to preserve and improve our assessment of ecosystem services and advance our understanding of climate\uffe2\uff80\uff90change feedback mechanisms, among others, thereby facilitating and strengthening communication among scientific disciplines and society. We review the role of modeling soil processes in quantifying key soil processes that shape ecosystem services, with a focus on provisioning and regulating services. We then identify key challenges in modeling soil processes, including the systematic incorporation of heterogeneity and uncertainty, the integration of data and models, and strategies for effective integration of knowledge on physical, chemical, and biological soil processes. We discuss how the soil modeling community could best interface with modern modeling activities in other disciplines, such as climate, ecology, and plant research, and how to weave novel observation and measurement techniques into soil models. We propose the establishment of an international soil modeling consortium to coherently advance soil modeling activities and foster communication with other Earth science disciplines. Such a consortium should promote soil modeling platforms and data repository for model development, calibration and intercomparison essential for addressing contemporary challenges.</p>", "keywords": ["organic-matter dynamics", "550", "Sciences de l\u2019environnement & \u00e9cologie", "QH301 Biology", "Knowledge management", "0208 environmental biotechnology", "ECOSYSTEM SERVICES", "02 engineering and technology", "soil processes", "01 natural sciences", "Physical Geography and Environmental Geoscience", "Sciences de la Terre", "Biological process", "ANZSRC::3707 Hydrology", "DROUGHT SEVERITY INDEX", "SYNTHETIC-APERTURE RADAR", "ANZSRC::4106 Soil sciences", "SDG 13 - Climate Action", "Climate change", "0503 Soil Sciences", "GROUND-PENETRATING RADAR", "Integration of knowledge", "Life sciences", "ANZSRC::050399 Soil Sciences not elsewhere classified", "synthetic-aperture radar", "Physical Sciences", "Water Resources", "Knowledge and experience", "MULTIPLE ECOSYSTEM SERVICES", "knowledge integration", "570", "DIFFUSE-REFLECTANCE SPECTROSCOPY", "Environmental Engineering", "Physique", " chimie", " math\u00e9matiques & sciences de la terre", "Scientific discipline", "0703 Crop and Pasture Production", "0207 environmental engineering", "Soil Science", "soil science", "ORGANIC-MATTER DYNAMICS", "DATA ASSIMILATION", "Physical", " chemical", " mathematical & earth Sciences", "ANZSRC::0503 Soil Sciences", "Science disciplines", "PEDOTRANSFER FUNCTIONS", "Feedback mechanisms", "mod\u00e9lisation", "ground-penetrating radar", "Science & Technology", "ANZSRC::080110 Simulation and Modelling", "15. Life on land", "Sciences de la terre & g\u00e9ographie physique", "multiple ecosystem services", "root water-uptake", "Observation and measurement", "DIGITAL ELEVATION MODEL", "Quality of predictions", "SATURATED-UNSATURATED FLOW", "ARBUSCULAR MYCORRHIZAL FUNGI", "sciences du sol", "HYDRAULIC-PROPERTIES", "2. Zero hunger", "Agriculture", "diffuse-reflectance spectroscopy", "4106 Soil sciences", "ORGANIC-MATTER", "digital elevation model", "SDG 13 \u2013 Ma\u00dfnahmen zum Klimaschutz", "Sciences du vivant", "Uncertainty analysis", "0406 Physical Geography and Environmental Geoscience", "Life Sciences & Biomedicine", "Crop and Pasture Production", "101028 Mathematical modelling", "international soil modeling consortium", "[SDU.STU]Sciences of the Universe [physics]/Earth Sciences", "Environmental Sciences & Ecology", "arbuscular mycorrhizal fungi", "Ecosystems", "Climate models", "QH301", "Environmental sciences & ecology", "Life Science", "SEDIMENT TRANSPORT MODELS", "data integration", "sediment transport models", "approche ecosyst\u00e9mique", "0105 earth and related environmental sciences", "info:eu-repo/classification/ddc/550", "3707 Hydrology", "soil modeling", "ROOT WATER-UPTAKE", "SOLUTE TRANSPORT", "13. Climate action", "Earth and Environmental Sciences", "Soil Sciences", "[SDU.STU] Sciences of the Universe [physics]/Earth Sciences", "Earth Sciences", "Earth sciences & physical geography", "Soils", "101028 Mathematische Modellierung", "saturated-unsaturated flow", "Environmental Sciences", "root water-uptake", " sediment transport models", " diffuse-reflectance spectroscopy", " arbuscular mycorrhizal fungi", " multiple ecosystem services", " saturated-unsaturated flow", " ground-penetrating radar", " synthetic-aperture radar", " digital elevation model", " organic-matter dynamics."]}, "links": [{"href": "https://orbi.uliege.be/bitstream/2268/263634/1/Vereecken%20VZJ%202016.pdf"}, {"href": "http://onlinelibrary.wiley.com/wol1/doi/10.2136/vzj2015.09.0131/fullpdf"}, {"href": "https://escholarship.org/content/qt6976n34c/qt6976n34c.pdf"}, {"href": "https://doi.org/2164/6134"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Vadose%20Zone%20Journal", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "2164/6134", "name": "item", "description": "2164/6134", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2164/6134"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2016-05-01T00:00:00Z"}}], "links": [{"rel": "self", "type": "application/geo+json", "title": "This document as GeoJSON", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=Pedotransfer+function&f=json", "hreflang": "en-US"}, {"rel": "alternate", "type": "text/html", "title": "This document as HTML", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=Pedotransfer+function&f=html", "hreflang": "en-US"}, {"rel": "collection", "type": "application/json", "title": "Collection URL", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main", "hreflang": "en-US"}, {"type": "application/geo+json", "rel": "first", "title": "items (first)", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=Pedotransfer+function&", "hreflang": "en-US"}, {"rel": "last", "type": "application/geo+json", "title": "items (last)", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=Pedotransfer+function&offset=13", "hreflang": "en-US"}], "numberMatched": 13, "numberReturned": 13, "distributedFeatures": [], "timeStamp": "2026-05-02T02:27:00.389031Z"}