{"type": "FeatureCollection", "features": [{"id": "10.1016/j.jhydrol.2021.126551", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-27T16:18:02Z", "type": "Journal Article", "created": "2021-06-08", "title": "Smartphone-based tension disc infiltrometer for soil hydraulic characterisation", "description": "31 Pags.- 18 Figs.- 1 Tabl.  The definitive version is available at: https://www.sciencedirect.com/science/journal/00221694 The tension disc infiltrometer has become a widespread method to measure soil hydraulic properties under unsaturated conditions. Although several automated devices have been developed, most designs include an elongated water reservoir and a pressure transducer with electronic components to register the water level, increasing its cost and limiting its application. The objective of this work is to present a new tension disc infiltrometer with a compact design of 10 cm diameter and height, where the water level is monitored by a smartphone camera. The infiltration curve is determined from the automated analysis of the images recorded by the smartphone without additional electronic components. The device was first validated in the laboratory by comparing visual measurements (V), the camera imagery (Ca) and a pressure transducer (PT). Next, it was tested on field infiltration experiments. Robust fits (R2 = 0.99) were found between the water level measured with Ca in the laboratory and those obtained with V and PT procedures. The Ca method is accurate, robust and independent of the relative camera position. Good fits were also observed between Ca water level and those obtained with PT in the field experiments. Similar hydraulic conductivity and sorptivity values were obtained with both sensors using the numerical solution of the Haverkamp (NSH) equation. The compact infiltrometer, in conjunction with the smartphone camera, is an accurate, accessible, portable and easy-to-use field-based device for soil hydraulic characterisation. This research was supported by the MINECO project ASBIO (PGC2018-094332-B-100) and the European Union\u2019s Horizon 2020 research and innovation program under grant agreement No [H2020-MSCA-RISE-777803]. Peer reviewed", "keywords": ["Automated single-ring infiltrometer", "Compact design", "0207 environmental engineering", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "02 engineering and technology", "Soil hydraulic properties", "Infiltration rate measurements", "NSH", "6. Clean water"]}, "links": [{"href": "https://doi.org/10.1016/j.jhydrol.2021.126551"}, {"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.2021.126551", "name": "item", "description": "10.1016/j.jhydrol.2021.126551", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.jhydrol.2021.126551"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-09-01T00:00:00Z"}}, {"id": "10.1002/eco.1490", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-27T16:15:03Z", "type": "Journal Article", "created": "2014-03-15", "title": "Shrub Encroachment Alters The Spatial Patterns Of Infiltration", "description": "Abstract<p>Encroachment of open woodlands by shrubs is a global phenomenon associated with marked changes in ecosystem structure and function. We measured sorptivity and steady\uffe2\uff80\uff90state infiltration at two supply potentials under shrubs and grasses and in their interspaces where shrubs were encroaching into grassland. Steady\uffe2\uff80\uff90state infiltration (ponded) and sorptivity were greater at the grassland than the shrubland site, and there was substantially greater infiltration under shrubs (48.2\uffe2\uff80\uff89mm\uffe2\uff80\uff89h\uffe2\uff88\uff921) and grasses (50.0\uffe2\uff80\uff89mm\uffe2\uff80\uff89h\uffe2\uff88\uff921) than the corresponding interspaces (17.0 and 32.3\uffe2\uff80\uff89mm\uffe2\uff80\uff89h\uffe2\uff88\uff921for shrubland and grassland, respectively). The difference between grasses and their interspaces was substantially less (1.5 times) than that between shrubs and their interspaces (three times). Shrub encroachment also affected the spatial patterns of infiltration. Although the autocorrelation range for shrublands coincided almost exactly with the average distance between shrub canopies (3.5\uffe2\uff80\uff89m), the range for grasslands was three times greater (1.5\uffe2\uff80\uff89m) than the mean grass canopy, indicating a greater connectivity of infiltration in the grasslands than the shrublands. Our study indicates that encroachment by shrubs does not change infiltration under individual plants. Rather, it reduces the interspace infiltration rates significantly, resulting in lower estimated site\uffe2\uff80\uff90level infiltration rates in shrublands. Our research suggests therefore that it is the shrubland interspaces that are the likely drivers of reduced infiltration rates when grasslands are encroached, rather than increase in the total cover of shrubsper se. Management strategies that result in greater retention of grass cover and minimize the level of interspace disturbances are likely to result in increased infiltration. Copyright \uffc2\uffa9 2014 John Wiley &amp; Sons, Ltd.</p>", "keywords": ["drylands", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land", "infiltration", "encroachment"]}, "links": [{"href": "https://doi.org/10.1002/eco.1490"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Ecohydrology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1002/eco.1490", "name": "item", "description": "10.1002/eco.1490", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1002/eco.1490"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2014-04-23T00:00:00Z"}}, {"id": "10.1016/j.agee.2006.05.002", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-27T16:16:36Z", "type": "Journal Article", "created": "2006-06-13", "title": "Effects Of Grazing Intensity And Prescribed Fire On Soil Physical And Hydrological Properties And Pasture Yield In The Savanna Woodlands Of Burkina Faso", "description": "In West Africa policies for prescribed early fire and livestock grazing in the savanna woodlands are rarely based on long-term experimental studies. The inherently different management characteristics and their effects on the vegetation dynamics make landscape degradation a contentious issue. The effects of grazing intensity were investigated by a comparison of non-grazed areas, lightly grazed areas, moderately grazed areas, heavily grazed areas and very heavily grazed areas that received one of two fire treatments: early burning and fire protection in a long-term 12-year study. The parameters assessed reflected changes in herbaceous plant cover, biomass as well as soil physical and hydrological properties. The main findings were by and large specific for the grazing level. This supports the argument for devolution of management responsibility to the local level where there is indigenous site-specific knowledge but at the same time insufficient management capacity. A comparison of composite soil samples taken at a depth of 0-10 cm did not differentiate significantly between treatments. This is probably because the composite soil sampling procedure hid the properties of the top first few centimeters. Grazing pressure had a tendency to reduce total above ground biomass (p = 0.081). This was related to increased biomass removal and the trampling pressure (static load) exerted by the animals. The infiltration measurements indicated that the deleterious impact of cattle trampling increased as stocking rate increased. Livestock grazing significantly (p = 0.038) lowered the infiltrability. Prescribed early fire had a tendency (p = 0.073) to reduce the soil water infiltration rate. The subplots subjected to prescribed burning had a lower steady state infiltration rate compared to unburnt areas (means of 49.2 \u00b1 27.5 mm h-1 versus 78 \u00b1 70.5 mm h-1 for burnt and unburnt subplots, respectively). A partial least squares projection to latent structures showed that 34% of the steady state infiltrability was explained by the stocking rate and soil organic matter. Also all soil characteristics were significantly connected to steady state infiltrability suggesting that they are related to the soil hydrological response to trampling. From a management perspective, adoption of a short duration grazing system should avoid high stocking rates because they may adversely affect soil infiltrability, increase susceptibility to erosion in the savannas and decrease biomass productivity.", "keywords": ["soil compaction", "2. Zero hunger", "vegetation", "13. Climate action", "trampling", "0401 agriculture", " forestry", " and fisheries", "grazing", "04 agricultural and veterinary sciences", "15. Life on land", "infiltration", "pastures", "woodlands", "savannas"], "contacts": [{"organization": "Savadogo, P., Sawadogo, L., Tiveau, D.,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1016/j.agee.2006.05.002"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Agriculture%2C%20Ecosystems%20%26amp%3B%20Environment", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.agee.2006.05.002", "name": "item", "description": "10.1016/j.agee.2006.05.002", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.agee.2006.05.002"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2007-01-01T00:00:00Z"}}, {"id": "10.1016/j.eja.2012.03.002", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-27T16:17:18Z", "type": "Journal Article", "created": "2012-04-04", "title": "Changes Of Soil Properties And Tree Performance Induced By Soil Management In A High-Density Olive Orchard", "description": "Abstract   Long-term effects of plant covers on yield and oil quality in olive orchards are poorly known. We compared performance of  Olea europaea  trees grown under either tillage (CT) or permanent natural cover (NC) in a sandy-loam soil over five years and determined changes in soil properties. The soil was tilled from the year of planting until the end of the second growing season, when both soil management treatments were established. The CT treatment was kept weed-free using a harrow with vertical blades (0.10\u00a0m depth), whereas the NC was obtained by letting the natural flora grow. Trees were fully irrigated until year 3 after planting, when deficit irrigation (about 50% of full) was started for both soil treatments. Trunk cross sectional area (TCSA) of NC trees was 77 and 87% to that of CT trees at the end of the 2006 and 2010 growing seasons, respectively. Fruit yield and oil yield of NC trees were 65 and 69% to those of CT ones, respectively (means of five years), however, when expressed on a TCSA basis, they resulted 87 and 95%, respectively. The fruit number of NC trees was lower than CT ones, whereas the oil content was similar. There were no differences in free acidity, peroxide value, spectrophotometric indexes, and fatty acid composition, but phenolic concentrations of the NC treatment were slightly higher than those of CT oils. Soil macroporosity in the topsoil was 5.2 and 2% for the NC and CT treatments, respectively. Water infiltration rate in CT plots was lower than in NC ones because of soil surface crusting; NC had higher values of total organic carbon and total extractable carbon than CT, whereas the humic carbon content was unaffected.", "keywords": ["Olea europaea L.; Oil quality; Plant cover; Soil macroporosity; Tillage; Water infiltration.", "2. Zero hunger", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land", "6. Clean water"]}, "links": [{"href": "https://doi.org/10.1016/j.eja.2012.03.002"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/European%20Journal%20of%20Agronomy", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.eja.2012.03.002", "name": "item", "description": "10.1016/j.eja.2012.03.002", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.eja.2012.03.002"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2012-08-01T00:00:00Z"}}, {"id": "10.1046/j.1365-2389.2000.00310.x", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-27T16:19:35Z", "type": "Journal Article", "created": "2003-03-11", "title": "Changes In Organic Matter, Nitrogen, Phosphorus And Cations In Soil As A Result Of Fire And Water Erosion In A Mediterranean Landscape", "description": "Summary<p>Fire affects large parts of the dry Mediterranean shrubland, resulting in erosion and losses of plant nutrients. We have attempted to measure these effects experimentally on a calcareous hillside representative of such shrubland. Experimental fires were made on plots (4\uffe2\uff80\uff83m \uffc3\uff97 20\uffe2\uff80\uff83m) in which the fuel was controlled to obtain two different fire intensities giving means of soil surface temperature of 439\uffc2\uffb0C and 232\uffc2\uffb0C with temperatures exceeding 100\uffc2\uffb0C lasting for 36\uffe2\uff80\uff83min and 17\uffe2\uff80\uff83min. The immediate and subsequent changes induced by fire on the soil's organic matter content and other soil chemical properties were evaluated, together with the impact of water erosion.</p><p>Seven erosive rain events, which occurred after the experimental fires (from August 1995 to December 1996), were selected, and on them runoff and sediment produced from each plot were measured. The sediments collected were weighed and analysed. Taking into account the variations induced by fire on the soil properties and their losses by water erosion, estimates of the net inputs and outputs of the soil system were made. Results show that the greatest losses of both soil and nutrients took place in the 4\uffe2\uff80\uff83months immediately after the fire. Plots affected by the most intense fire showed greater losses of soil (4077\uffe2\uff80\uff83kg\uffe2\uff80\uff83ha\uffe2\uff88\uff921) than those with moderate fire intensity (3280\uffe2\uff80\uff83kg\uffe2\uff80\uff83ha\uffe2\uff88\uff921). The unburned plots produced the least sediment (72.8\uffe2\uff80\uff83kg\uffe2\uff80\uff83ha\uffe2\uff88\uff921). Organic matter and nutrient losses by water erosion were related to the degree of fire intensity. However, the largest losses of N\uffe2\uff80\uff90NH4+ and N\uffe2\uff80\uff90NO3\uffe2\uff80\uff93 by water erosion corresponded to the moderate fire (8.1 and 7.5\uffe2\uff80\uff83mg\uffe2\uff80\uff83N\uffe2\uff80\uff83m\uffe2\uff88\uff922, respectively).</p>", "keywords": ["13. Climate action", "Parameters", "Infiltration", "0401 agriculture", " forestry", " and fisheries", "Vegetation fires", "04 agricultural and veterinary sciences", "15. Life on land"]}, "links": [{"href": "https://doi.org/10.1046/j.1365-2389.2000.00310.x"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/European%20Journal%20of%20Soil%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1046/j.1365-2389.2000.00310.x", "name": "item", "description": "10.1046/j.1365-2389.2000.00310.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1046/j.1365-2389.2000.00310.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2000-06-01T00:00:00Z"}}, {"id": "10.1051/agro:2004010", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-27T16:19:40Z", "type": "Journal Article", "created": "2004-07-01", "title": "Grass Strip Effects On Runoff And Soil Loss", "description": "The effects of grass strips on runoff interception, sediment trapping and soil loss were studied during two agricultural seasons. Field studies, conducted on loamy soil susceptible to sealing, allowed the comparison of three situations corresponding to buffer strip widths of 0, 3 and 6 m located at the downslope end of a winter wheat field. In 1997-98 the 6-m grass strips led to an average increase in infiltration of 87% with a coefficient of variation of 16% in comparison with a situation where no grass strip was present. The 3-m grass strip showed a slightly lower and more variable efficiency (average: 80%, coefficient of variation: 19% in 97/98). Maximum grass strip infiltrability was estimated at about 50 mm/h. Grass strips reduced the event mean sediment concentration by a factor of four on average. Sediments deposited in the grass strip were enriched in sand and coarse silt, whereas exported sediments contained twice as much clay and fine silt as the soil surface horizon. Net soil loss from the field was decreased by 76% in 96/97 and by 98% in 97/98 for the 6-m grass strip.", "keywords": ["[SDV.SA]Life Sciences [q-bio]/Agricultural sciences", "[SDV.SA] Life Sciences [q-bio]/Agricultural sciences", "[SDV.EE] Life Sciences [q-bio]/Ecology", " environment", "grass strip", "infiltration capacity", "sediment trapping", "[SDV.EE]Life Sciences [q-bio]/Ecology", "soil loss", "0401 agriculture", " forestry", " and fisheries", "runoff", "04 agricultural and veterinary sciences", "15. Life on land", "environment"]}, "links": [{"href": "https://hal.science/hal-00886045/file/hal-00886045.pdf"}, {"href": "https://doi.org/10.1051/agro:2004010"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Agronomie", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1051/agro:2004010", "name": "item", "description": "10.1051/agro:2004010", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1051/agro:2004010"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2004-04-01T00:00:00Z"}}, {"id": "10.1080/01140670909510261", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-27T16:19:57Z", "type": "Journal Article", "created": "2010-08-13", "title": "Soil Physical Properties And Infiltration After Long-Term No-Tillage And Ploughing On The Chinese Loess Plateau", "description": "Abstract Water is the most limiting factor for crop production in dryland farming. A better understanding of the long\u2010term impact of tillage and residue management systems on soil structure and water infiltration is necessary for the further development of conservation tillage practice to improve water use efficiency. The objectives of this study were to assess the influence of no\u2010till with residue retention (NT) and conventional (plough) tillage with residue removal (CT) on soil properties and soil water transmission characteristics in a winter wheat (Triticum aestivum) monoculture system in Shanxi, on the Chinese Loess Plateau. Soil physical parameter measurements were made in the top 30 cm depth in September 2007 after 16 years under the two tillage treatments. Compared with CT treatment, NT significantly (P  60 \u03bcm, 17.0%) and saturated hydraulic conductivity (249%) in the 15\u201330 cm soil layer. There were n...", "keywords": ["2. Zero hunger", "550", "soil water retention characteristics", "Soil porosity", "saturated hydraulic conductivity", "soil porosity", "Infiltration", "04 agricultural and veterinary sciences", "15. Life on land", "1108 Horticulture", "infiltration", "Saturated hydraulic conductivity", "630", "6. Clean water", "soil aggregates", "Conservation Tillage", "conservation tillage", "0401 agriculture", " forestry", " and fisheries", "1102 Agronomy and Crop Science", "Soil aggregates", "Soil water retention characteristics"]}, "links": [{"href": "https://doi.org/10.1080/01140670909510261"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/New%20Zealand%20Journal%20of%20Crop%20and%20Horticultural%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1080/01140670909510261", "name": "item", "description": "10.1080/01140670909510261", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1080/01140670909510261"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2009-09-01T00:00:00Z"}}, {"id": "10.1080/15324982.2022.2119901", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-27T16:20:04Z", "type": "Journal Article", "created": "2022-09-21", "title": "Plant-soil interactions in response to grazing intensity in a semi-arid ecosystem from NE Spain", "description": "Livestock grazing is an important element in ecosystem regulation since it may affect essential ecosystem functions, such as nutrient acquisition, organic matter decomposition, or litter accumulation in the soil. Overgrazing can threaten the conservation of ecosystems through excessive defoliation of plants or trampling. On the contrary, moderate grazing can have benefits on ecosystem dynamics by favoring nutrient cycling or the soil microbial activity. The aim of this study was to analyze these effects in a semi-arid Mediterranean shrubland located in NE Spain. We established six study sites including three grazing intensities, where we sampled vegetation biomass and soil properties: nitrogen content, microbial biomass, water infiltration capacity, porosity, and gypsum content. These parameters were included in a plant-soil interaction model tested through Structural Equation Modeling. Grazing had a direct negative effect on plant biomass (<i>p</i> &lt; 0.01) and water infiltration capacity (<i>p</i> &lt; 0.05) affecting soil nitrogen content (<i>p</i> &lt; 0.001) and microbial biomass (<i>p</i> &lt; 0.5), respectively. Infiltration capacity and porosity were primary drivers of plant biomass (<i>p</i> &lt; 0.05, both cases), and plant biomass was the main contributor to the soil nitrogen pool. Microbial biomass was dependent on infiltration capacity (<i>p</i> &lt; 0.05), porosity (<i>p</i> &lt; 0.01), and nitrogen (<i>p</i> &lt; 0.01). Grazing directly or indirectly affected the functioning of the ecosystem through effects on plant and soil attributes, which may result in changes in plant growth, litter decomposition, or plant nutrient acquisition. This study revealed that moderate grazing can maintain optimal ecosystem features and prevent ecosystem degradation.", "keywords": ["plant-soil feedbacks", "2. Zero hunger", "Plant biomass", "porosity", "microbial biomass", "Plant-soil feedbacks", "soil fertility", "Microbial biomass", "Infiltration", "04 agricultural and veterinary sciences", "15. Life on land", "Soil fertility", "Protect", " restore and promote sustainable use of terrestrial ecosystems", " sustainably manage forests", " combat\u00a0desertification", " and halt and reverse land degradation and halt biodiversity loss", "rangelands", "13. Climate action", "Rangelands", "http://metadata.un.org/sdg/15", "0401 agriculture", " forestry", " and fisheries", "Porosity", "plant biomass"]}, "links": [{"href": "https://www.tandfonline.com/doi/pdf/10.1080/15324982.2022.2119901"}, {"href": "https://doi.org/10.1080/15324982.2022.2119901"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Arid%20Land%20Research%20and%20Management", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1080/15324982.2022.2119901", "name": "item", "description": "10.1080/15324982.2022.2119901", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1080/15324982.2022.2119901"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-09-21T00:00:00Z"}}, {"id": "10.1590/1807-1929/agriambi.v19n11p1021-1027", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-27T16:21:56Z", "type": "Journal Article", "created": "2015-10-31", "title": "Water Infiltration Rate In Yellow Latosol Under Different Soil Management Systems", "description": "<p>ABSTRACTThe management systems affect soil structure, causing changes in porosity that can influence soil water infiltration. In order to study the water infiltration rate in a Yellow Latosol under different tillage systems and different mathematical models, an experiment was conducted from October to December 2012, at the Center for Agricultural Sciences at the Federal University of Alagoas, using a randomized block design with five replicates, in a split-plot scheme. In the plots, the management systems were evaluated (conventional tillage, no-tillage and minimum tillage) and, in the sub-plots, the empirical mathematical models of Kostiakov, Kostiakov-Lewis and Horton, and the ring method. The method used to measure soil water infiltration rate was adapted from the classic double-ring infiltrometer method. The minimum tillage system provided better results compared with the others, with water infiltration rate of 167 mm h-1, and the equation that best fitted the data of the ring infiltrometer was Kostiakov\uffe2\uff80\uff99s, in the no-tillage system.</p>", "keywords": ["soil tillage systems", "m\u00e9todos de infiltra\u00e7\u00e3o", "sistemas de preparo do solo", "0401 agriculture", " forestry", " and fisheries", "irriga\u00e7\u00e3o", "infiltration methods", "04 agricultural and veterinary sciences", "15. Life on land", "irrigation"], "contacts": [{"organization": "Cunha, Jorge L. X. L., Coelho, Maria E. H., Albuquerque, Abel W. de, Silva, Cicero A., Silva J\u00fanior, Ant\u00f4nio B. da, Carvalho, Islan D. E. de,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1590/1807-1929/agriambi.v19n11p1021-1027"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Revista%20Brasileira%20de%20Engenharia%20Agr%C3%ADcola%20e%20Ambiental", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1590/1807-1929/agriambi.v19n11p1021-1027", "name": "item", "description": "10.1590/1807-1929/agriambi.v19n11p1021-1027", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1590/1807-1929/agriambi.v19n11p1021-1027"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2015-11-01T00:00:00Z"}}, {"id": "10.2134/agronj1995.00021962008700040009x", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-27T16:22:24Z", "type": "Journal Article", "created": "2010-07-29", "title": "Infiltration And Soil Properties As Affected By Annual Cropping In The Northern Great-Plains", "description": "Abstract<p>Fallow\uffe2\uff80\uff90wheat (Triticum aestivum L.) cropping systems may be responsible for declines in soil organic matter and degradation of soil physical properties. A change to annual cropping may improve or at least maintain soil properties. Tillage and crop sequence effects on soil properties and water infiltration were tested after 9 yr of cropping on a Dooley sandy loam (fine\uffe2\uff80\uff90loamy, mixed Typic Argiborolls) derived in glacial till. Annual cropping tillage of fall sweep and spring disk (AWFST), and no tillage (AWNT) were compared with conventional tillage in wheatfallow (FWCT) as the control. Statistical design was a randomized complete block with four replications. Soil samples were taken at 0.03\uffe2\uff88\uff92m increments to a depth of 0.3 m and were used to measure organic carbon (OC), pH, bulk density (BD), and particle size. Point resistance was measured in 0.02\uffe2\uff88\uff92m increments. Water infiltration into dry and wet soil was measured using a rainfall simulator. Maximum soil BD was 1.61 Mg m\uffe2\uff88\uff923 on FWCT and 1.56 Mg m\uffe2\uff88\uff923 on AWNT. Soil BD was not changed by one winter of freezing and thawing. Maximum point resistance was 2.2 MPa on FWCT and 1.7 MPa on AWNT. Cumulative 3\uffe2\uff80\uff90h infiltration into dry soil was 52 mm for FWCT and 69 mm for AWNT. Final infiltration rate into wet soil was 5 mm h\uffe2\uff88\uff921 for FWCT and 6 mm h\uffe2\uff88\uff921 for AWNT. There was a significant difference in the depth distribution of OC between annual crop and FWCT treatments. Mass of OC in the top 0.09 m of soil was 1.65 kg m\uffe2\uff88\uff922 on annual crop treatments and 1.45 kg m\uffe2\uff88\uff922 on FWCT. Greater amounts of OC on the annual crop treatments compared with the FWCT attest to the beneficial aspect of annual cropping in maintaining a level of soil quality that is greater than FWCT. From a soil conservation perspective, no\uffe2\uff80\uff90tillage has an additional advantage because surface cover is maintained throughout the year, thereby reducing the potential for soil erosion.</p>", "keywords": ["2. Zero hunger", "Soil", "Infiltration", "0401 agriculture", " forestry", " and fisheries", "Mass Import - autoclassified (may be erroneous)", "04 agricultural and veterinary sciences", "15. Life on land", "6. Clean water"], "contacts": [{"organization": "Pikul, J.L., Aase, J.K.,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.2134/agronj1995.00021962008700040009x"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Agronomy%20Journal", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.2134/agronj1995.00021962008700040009x", "name": "item", "description": "10.2134/agronj1995.00021962008700040009x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.2134/agronj1995.00021962008700040009x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "1995-07-01T00:00:00Z"}}, {"id": "10.3390/land13111759", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-27T16:23:37Z", "type": "Journal Article", "created": "2024-10-28", "title": "Temperate Soils Exposed to Drought\u2014Key Processes, Impacts, Indicators, and Unknowns", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>The summer drought in the United Kingdom (UK) in 2022 produced significant speculation concerning how its termination may impact and interact with the soil resource. Whilst knowledge regarding soils and droughts exists in the scientific literature, a coherent understanding of the wider range of impacts on soil properties and functions has not been compiled for temperate soils. Here, we draw together knowledge from studies in the UK and other temperate countries to understand how soils respond to drought, and importantly what and where our knowledge gaps are. First, we define the different types of droughts and their frequency in the UK and provide a brief overview on the likely societal impacts that droughts place on the soil and related ecosystems. Our focus is on \u2018agricultural and ecosystem drought\u2019, as this is when soils experience dry periods affecting crops and ecosystem function, followed by rewetting. The behaviour of moisture in soils and the key processes that contribute to its storage and transport are examined. The principal changes in the physical, chemical, and biological properties of soils resulting from drought, and rewetting (i.e., drought termination) are discussed and their extensive interactions are demonstrated. Processes that are involved in the rewetting of soils are explored for soil and catchment-scale soil responses. Lastly, soils\u2019 recovery after drought is considered, knowledge gaps are identified, and areas to improve understanding are highlighted.</p></article>", "keywords": ["soil health", "rewetting", "soil microbes", "S", "soil water infiltration", "soil water repellency", "drought recovery", "soil nutrients", "Agriculture", "drought termination", "meteorological drought", "soil moisture", "soil fauna"]}, "links": [{"href": "https://www.mdpi.com/2073-445X/13/11/1759/pdf"}, {"href": "https://doi.org/10.3390/land13111759"}, {"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": "10.3390/land13111759", "name": "item", "description": "10.3390/land13111759", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3390/land13111759"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-10-26T00:00:00Z"}}, {"id": "10.3390/w10060688", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-27T16:23:52Z", "type": "Journal Article", "created": "2018-05-28", "title": "Monitoring of a Full-Scale Embankment Experiment Regarding Soil\u2013Vegetation\u2013Atmosphere Interactions", "description": "<p>Slope mass-wasting like shallow slides are mostly triggered by climate effects, such as rainfall, and soil\uffe2\uff80\uff93vegetation\uffe2\uff80\uff93atmosphere (SVA) interactions play a key role. SVA interactions are studied by a full-scale embankment with different orientations (North and South) and vegetation covers (bare and vegetated) in the framework of the prediction of climate change effects on slope stability in the Pyrenees. A clayey sand from the Llobregat river delta was used for the construction of the embankment and laboratory tests showed the importance of suction on the strength and hydraulic conductivity. Sixty sensors, which are mostly installed at the upper soil layer of the embankment, registered 122 variables at four vertical profiles and the meteorological station with a 5 min scan rate. Regarding temperature, daily temperature fluctuation at the shallow soil layer disappeared at a depth of about 0.5 m. There was great influence of orientation with much higher values at the South-facing slope (up to 55 \uffc2\uffb0C at \uffe2\uff88\uff921 cm depth) due to solar radiation. Regarding rainfall infiltration, only long duration rainfalls produced an important increase of soil moisture and pore water pressure, while short duration rainfalls did not trigger significant variations. However, these changes mostly affected the surface soil layer and decreased with depth.</p>", "keywords": ["rainfall infiltration", "\u00c0rees tem\u00e0tiques de la UPC::Enginyeria civil::Geot\u00e8cnia::Mec\u00e0nica de s\u00f2ls", "Terraplens", "0211 other engineering and technologies", "heat flux", "02 engineering and technology", "15. Life on land", "01 natural sciences", "6. Clean water", "monitoring", "13. Climate action", ":Enginyeria civil::Geot\u00e8cnia::Mec\u00e0nica de s\u00f2ls [\u00c0rees tem\u00e0tiques de la UPC]", "monitoring; embankment; rainfall infiltration; heat flux", "Embankments", "embankment", "0105 earth and related environmental sciences"]}, "links": [{"href": "http://www.mdpi.com/2073-4441/10/6/688/pdf"}, {"href": "https://doi.org/10.3390/w10060688"}, {"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/w10060688", "name": "item", "description": "10.3390/w10060688", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3390/w10060688"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-05-25T00:00:00Z"}}, {"id": "10.3390/w8120604", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-27T16:23:53Z", "type": "Journal Article", "created": "2016-12-23", "title": "Riverbed Clogging and Sustainability of Riverbank Filtration", "description": "<p>Clogging refers to a reduction of riverbed hydraulic conductivity. Due to difficulties in determining the thickness of the clogging layer, the leakage coefficient (L) is introduced and used to quantify the recoverable portion of bank filtrate. L was determined at several riverbank filtration (RBF) sites in field tests and using an analytical solution. Results were compared with data from similar experiments in the early 1970s and 1991\uffe2\uff80\uff931993. In the 1980s, severe river water pollution in conjunction with high water abstraction led to partly unsaturated conditions beneath the riverbed. A leakage coefficient L of 5 \uffc3\uff97 10\uffe2\uff88\uff927 s\uffe2\uff88\uff921 was determined. After water quality improvement, L increased to 1\uffe2\uff80\uff931.5 \uffc3\uff97 10\uffe2\uff88\uff926 s\uffe2\uff88\uff921. An alternative, cost and time efficient method is presented to estimate accurate leakage coefficients. The analytical solution is based on groundwater level monitoring data from observation wells next to the river, which can later feed into numerical models. The analytical approach was able to reflect long-term changes as well as seasonal variations. Recommendations for its application are given based on experience.</p>", "keywords": ["clogging; leakage factor; infiltration resistance; riverbank filtration", "13. Climate action", "0207 environmental engineering", "02 engineering and technology", "01 natural sciences", "6. Clean water", "0105 earth and related environmental sciences"]}, "links": [{"href": "http://www.mdpi.com/2073-4441/8/12/604/pdf"}, {"href": "https://doi.org/10.3390/w8120604"}, {"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/w8120604", "name": "item", "description": "10.3390/w8120604", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3390/w8120604"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2016-12-20T00:00:00Z"}}, {"id": "10.4067/s0717-92002011000100002", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-27T16:24:03Z", "type": "Journal Article", "created": "2011-05-23", "description": "Se estudiaron las propiedades hidrologicas del suelo y la exportacion de sedimentos en una microcuenca con bosque nativo siempreverde y otra con plantacion de Eucalyptus globulus, localizadas en la Cordillera de la Costa en el sur de Chile. Se instalaron registradores de escorrentia y colectores de sedimentos en suspension y de fondo, se midieron las tasas de infiltracion y se determinaron las propiedades hidrologicas del suelo: conductividad hidraulica saturada, indice de continuidad de poros e hidrofobia. Las tasas de infiltracion fueron mayores (P < 0,05) en el bosque nativo: entre 703,3 \u00b1 380,0 y 76,9 \u00b1 56,7 mm h-1, en marzo y julio, respectivamente; que en la plantacion: 23,0 \u00b1 19,7 y 6,7 \u00b1 5,0 mm h-1 en agosto y abril, respectivamente (promedio \u00b1 S). La conductividad hidraulica saturada bajo bosque nativo, fue mayor (P < 0,05) que bajo plantacion, lo que indicaria una mayor capacidad de conduccion de agua del suelo bajo bosque nativo. El indice de continuidad de poros fue mayor (P < 0,05) en el suelo bajo bosque nativo. Las concentraciones de sedimentos en suspension, en ambas microcuencas, mostraron grandes variaciones intraanuales, en respuesta a las fluctuaciones de las precipitaciones y escorrentia. La exportacion de sedimentos en suspension fue de 305 y 368 kg ha-1 ano-1 en el bosque nativo y plantacion, respectivamente. El uso historico del suelo, especialmente en el caso de E. globulus, que reflejaba condiciones de transicion de pradera a plantacion, permitio explicar las diferencias en las propiedades hidrologicas del suelo con respecto al bosque nativo.", "keywords": ["plantaci\u00f3n de Eucalyptus", "infiltraci\u00f3n", "bosque nativo siempreverde", "escorrent\u00eda", "sedimentos en suspensi\u00f3n", "0208 environmental biotechnology", "0207 environmental engineering", "native evergreen forest", "streamflow", "02 engineering and technology", "Eucalyptus plantation", "suspended sediments", "infiltration"]}, "links": [{"href": "https://doi.org/10.4067/s0717-92002011000100002"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Bosque%20%28Valdivia%29", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.4067/s0717-92002011000100002", "name": "item", "description": "10.4067/s0717-92002011000100002", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.4067/s0717-92002011000100002"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2011-01-01T00:00:00Z"}}, {"id": "10.6084/m9.figshare.21175472.v2", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-27T16:28:27Z", "type": "Journal Article", "created": "2022-09-21", "title": "Plant-soil interactions in response to grazing intensity in a semi-arid ecosystem from NE Spain", "description": "Livestock grazing is an important element in ecosystem regulation since it may affect essential ecosystem functions, such as nutrient acquisition, organic matter decomposition, or litter accumulation in the soil. Overgrazing can threaten the conservation of ecosystems through excessive defoliation of plants or trampling. On the contrary, moderate grazing can have benefits on ecosystem dynamics by favoring nutrient cycling or the soil microbial activity. The aim of this study was to analyze these effects in a semi-arid Mediterranean shrubland located in NE Spain. We established six study sites including three grazing intensities, where we sampled vegetation biomass and soil properties: nitrogen content, microbial biomass, water infiltration capacity, porosity, and gypsum content. These parameters were included in a plant-soil interaction model tested through Structural Equation Modeling. Grazing had a direct negative effect on plant biomass (<i>p</i> &lt; 0.01) and water infiltration capacity (<i>p</i> &lt; 0.05) affecting soil nitrogen content (<i>p</i> &lt; 0.001) and microbial biomass (<i>p</i> &lt; 0.5), respectively. Infiltration capacity and porosity were primary drivers of plant biomass (<i>p</i> &lt; 0.05, both cases), and plant biomass was the main contributor to the soil nitrogen pool. Microbial biomass was dependent on infiltration capacity (<i>p</i> &lt; 0.05), porosity (<i>p</i> &lt; 0.01), and nitrogen (<i>p</i> &lt; 0.01). Grazing directly or indirectly affected the functioning of the ecosystem through effects on plant and soil attributes, which may result in changes in plant growth, litter decomposition, or plant nutrient acquisition. This study revealed that moderate grazing can maintain optimal ecosystem features and prevent ecosystem degradation.", "keywords": ["2. Zero hunger", "Plant biomass", "13. Climate action", "Plant-soil feedbacks", "Infiltration", "Microbial biomass", "Rangelands", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land", "Soil fertility", "Porosity"]}, "links": [{"href": "https://www.tandfonline.com/doi/pdf/10.1080/15324982.2022.2119901"}, {"href": "https://doi.org/10.6084/m9.figshare.21175472.v2"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Arid%20Land%20Research%20and%20Management", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.6084/m9.figshare.21175472.v2", "name": "item", "description": "10.6084/m9.figshare.21175472.v2", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.6084/m9.figshare.21175472.v2"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-09-21T00:00:00Z"}}, {"id": "10261/252724", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-27T16:28:52Z", "type": "Journal Article", "created": "2021-06-08", "title": "Smartphone-based tension disc infiltrometer for soil hydraulic characterisation", "description": "Open AccessPeer reviewed", "keywords": ["Automated single-ring infiltrometer", "Compact design", "0207 environmental engineering", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "02 engineering and technology", "Soil hydraulic properties", "Infiltration rate measurements", "NSH", "6. Clean water"]}, "links": [{"href": "https://doi.org/10261/252724"}, {"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": "10261/252724", "name": "item", "description": "10261/252724", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10261/252724"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-09-01T00:00:00Z"}}, {"id": "10261/295679", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-27T16:28:55Z", "type": "Journal Article", "created": "2022-09-21", "title": "Plant-soil interactions in response to grazing intensity in a semi-arid ecosystem from NE Spain", "description": "Livestock grazing is an important element in ecosystem regulation since it may affect essential ecosystem functions, such as nutrient acquisition, organic matter decomposition, or litter accumulation in the soil. Overgrazing can threaten the conservation of ecosystems through excessive defoliation of plants or trampling. On the contrary, moderate grazing can have benefits on ecosystem dynamics by favoring nutrient cycling or the soil microbial activity. The aim of this study was to analyze these effects in a semi-arid Mediterranean shrubland located in NE Spain. We established six study sites including three grazing intensities, where we sampled vegetation biomass and soil properties: nitrogen content, microbial biomass, water infiltration capacity, porosity, and gypsum content. These parameters were included in a plant-soil interaction model tested through Structural Equation Modeling. Grazing had a direct negative effect on plant biomass (<i>p</i> &lt; 0.01) and water infiltration capacity (<i>p</i> &lt; 0.05) affecting soil nitrogen content (<i>p</i> &lt; 0.001) and microbial biomass (<i>p</i> &lt; 0.5), respectively. Infiltration capacity and porosity were primary drivers of plant biomass (<i>p</i> &lt; 0.05, both cases), and plant biomass was the main contributor to the soil nitrogen pool. Microbial biomass was dependent on infiltration capacity (<i>p</i> &lt; 0.05), porosity (<i>p</i> &lt; 0.01), and nitrogen (<i>p</i> &lt; 0.01). Grazing directly or indirectly affected the functioning of the ecosystem through effects on plant and soil attributes, which may result in changes in plant growth, litter decomposition, or plant nutrient acquisition. This study revealed that moderate grazing can maintain optimal ecosystem features and prevent ecosystem degradation.", "keywords": ["plant-soil feedbacks", "2. Zero hunger", "Plant biomass", "porosity", "microbial biomass", "Plant-soil feedbacks", "soil fertility", "Microbial biomass", "Infiltration", "04 agricultural and veterinary sciences", "15. Life on land", "Soil fertility", "Protect", " restore and promote sustainable use of terrestrial ecosystems", " sustainably manage forests", " combat\u00a0desertification", " and halt and reverse land degradation and halt biodiversity loss", "rangelands", "13. 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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. The access to this data is restricted during embargo time. If prior access is requested, contact the data owner / author.", "updated": "2022-06-01", "type": "Dataset", "created": "2022-02-02", "language": "eng", "title": "Effects of agricultural diversification practices on near-saturated soil hydraulic conductivity assessed with the hood infiltrometer.", "description": "During October and November 2020, infiltration rate was measured in each soil quadrant of the 30 patches. Three points, one meter next to the permanent traffic lane were chosen to conduct the measurements. At every point, the infiltration rate was measured three times applying 0, -2 and -5 cm pressure, respectively until a constant flow rate was reached. A constant flow rate was assumed when two successive values did not differentiate more than 5%. Afterwards, 19 further values were taken, from which an average was calculated.", "formats": [{"name": "CSV"}], "keywords": ["Soil", "infiltration water", "hydraulic conductivity", "opendata", "Boden", "infiltration rate", "hood infiltrometer", "hydraulic conductivity"], "contacts": [{"name": "BonaRes Data Centre", "organization": "Leibniz Centre for Agricultural Landscape Research (ZALF)", "position": "Research Platform 'Data Analysis & Simulation' - WG Geodata", "roles": ["publisher"], "phones": [{"value": "+49 33432 82 171"}], "emails": [{"value": "bonares-datenzentrum@zalf.de"}], "addresses": [{"deliveryPoint": ["Eberswalder Strasse 84"], "city": "M\u00fcncheberg", "administrativeArea": "Brandenburg", "postalCode": "15374", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Dr. Kathrin Grahmann", "organization": "Leibniz Center for Agricultural Landscape Research (ZALF e.V.)", "position": null, "roles": ["author"], "phones": [{"value": null}], "emails": [{"value": "kathrin.grahmann@zalf.de"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": {"url": null, "protocol": null, "protocol_url": "", "name": "0000-0002-9589-7441", "name_url": "", "description": "ORCID", "description_url": "", "applicationprofile": null, "applicationprofile_url": "", "function": null}}]}, {"name": "David Caracciolo", "organization": "Humboldt University of Berlin", "position": null, "roles": ["author"], "phones": [{"value": null}], "emails": [{"value": "david.caracciolo@zalf.de"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": null}]}, {"name": "Dr. Kathrin Grahmann", "organization": "Leibniz Center for Agricultural Landscape Research (ZALF e.V.)", "position": null, "roles": ["projectLeader"], "phones": [{"value": null}], "emails": [{"value": "kathrin.grahmann@zalf.de"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": {"url": null, "protocol": null, "protocol_url": "", "name": "0000-0002-9589-7441", "name_url": "", "description": "ORCID", "description_url": "", "applicationprofile": null, "applicationprofile_url": "", "function": null}}]}, {"name": "Motaz Abdelaziz", "organization": "Leibniz Center for Agricultural Landscape Research (ZALF e.V.)", "position": null, "roles": ["dataCurator"], "phones": [{"value": null}], "emails": [{"value": "Motaz.Abdelaziz@zalf.de"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": null}]}, {"organization": "Humboldt University of Berlin;Leibniz Center for Agricultural Landscape Research (ZALF e.V.)", "roles": ["contributor"]}]}, "links": [{"href": "https://maps.bonares.de/mapapps/resources/apps/bonares/index.html?lang=en&mid=d791146e-7ab8-4db5-8c80-1dc58e496df8", "rel": "information"}, {"rel": "self", "type": "application/geo+json", "title": "d791146e-7ab8-4db5-8c80-1dc58e496df8", "name": "item", "description": "d791146e-7ab8-4db5-8c80-1dc58e496df8", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/d791146e-7ab8-4db5-8c80-1dc58e496df8"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"interval": ["2020-10-06T00:00:00Z", "2020-11-18T00:00:00Z"]}}, {"id": "af9183f2-43ec-4eda-b772-35b117d396b4", "type": "Feature", "geometry": {"type": "Polygon", "coordinates": [[[13.45, 51.9], [13.45, 52.74], [14.5, 52.74], [14.5, 51.9], [13.45, 51.9]]]}, "properties": {"themes": [{"concepts": [{"id": "farming"}], "scheme": "https://standards.iso.org/iso/19139/resources/gmxCodelists.xml#MD_TopicCategoryCode"}, {"concepts": [{"id": "Soil"}], "scheme": "AGROVOC Multilingual agricultural thesaurus"}, {"concepts": [{"id": "opendata"}, {"id": "Managed Aquifer Recharge (MAR); Surface infiltration; Water sustainability; Site suitability analysis"}], "scheme": "Individual"}, {"concepts": [{"id": "Boden"}], "scheme": "GEMET - INSPIRE themes, version 1.0"}, {"concepts": [{"id": "Germany"}, {"id": "Brandenburg"}, {"id": "Oder-Spree"}, {"id": "M\u00e4rkisch-Oderland"}, {"id": "Untere Spree"}], "scheme": "individual"}], "license": "CC BY", "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": "2025-07-25", "type": "Dataset", "created": "2025-07-23", "language": "eng", "title": "Natural and constructively enlarged depressions for surface induced managed aquifer recharge (MAR) within Brandenburg\u00b4s lower Spree catchment", "description": "The included subsets outline natural and construcively enlarged depressions to be utilized for surface induced recharge measures to counteract water withdrawals and reduce the vulnerability of the groundwater as well as connected surface waters and ecosystems. In case of constructively enlarged sinks this included the locations for trapezoidal embankment structures to be introduced to utilized the outlined recharge areas. The result are expressed by a numerical indexation and summarized in a final index for each sink.\n\nRelated datasets are listed in the metadata element 'Related Identifier'.\nDataset version 1.0", "formats": [{"name": "CSV"}], "keywords": ["Soil", "opendata", "Managed Aquifer Recharge (MAR); Surface infiltration; Water sustainability; Site suitability analysis", "Boden", "Germany", "Brandenburg", "Oder-Spree", "M\u00e4rkisch-Oderland", "Untere Spree"], "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": "Jan Stautzebach", "organization": "Leibniz Centre for Agricultural Landscape Research", "position": null, "roles": ["author"], "phones": [{"value": null}], "emails": [{"value": "Jan.Stautzebach@zalf.de"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": {"url": null, "protocol": null, "protocol_url": "", "name": "0009-0000-8884-8759", "name_url": "", "description": "ORCID", "description_url": "", "applicationprofile": null, "applicationprofile_url": "", "function": null}}]}, {"name": "J\u00f6rg Steidl", "organization": "Leibniz Centre for Agricultural Landscape Research", "position": null, "roles": ["author"], "phones": [{"value": null}], "emails": [{"value": "jsteidl@zalf.de"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": {"url": null, "protocol": null, "protocol_url": "", "name": "0000-0002-6599-0450", "name_url": "", "description": "ORCID", "description_url": "", "applicationprofile": null, "applicationprofile_url": "", "function": null}}]}, {"name": "Christoph Merz", "organization": "Leibniz Centre for Agricultural Landscape Research", "position": null, "roles": ["projectLeader"], "phones": [{"value": null}], "emails": [{"value": "merz@zalf.de"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": {"url": null, "protocol": null, "protocol_url": "", "name": "0000-0001-7434-9828", "name_url": "", "description": "ORCID", "description_url": "", "applicationprofile": null, "applicationprofile_url": "", "function": null}}]}, {"organization": "Leibniz Centre for Agricultural Landscape Research", "roles": ["contributor"]}], "title_alternate": "Data collection: Part 1/4, table: study area"}, "links": [{"href": "https://maps.bonares.de/mapapps/resources/apps/bonares/index.html?lang=en&mid=af9183f2-43ec-4eda-b772-35b117d396b4", "rel": "information"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/e97fb592-8f94-4b81-af43-32b0cf8af516", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "af9183f2-43ec-4eda-b772-35b117d396b4", "name": "item", "description": "af9183f2-43ec-4eda-b772-35b117d396b4", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/af9183f2-43ec-4eda-b772-35b117d396b4"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-07-25T00:00:00Z"}}, {"id": "5699b586-6dcb-490e-b35d-29fcb2ca921f", "type": "Feature", "geometry": {"type": "Polygon", "coordinates": [[[13.45, 51.9], [13.45, 52.74], [14.5, 52.74], [14.5, 51.9], [13.45, 51.9]]]}, "properties": {"themes": [{"concepts": [{"id": "farming"}], "scheme": "https://standards.iso.org/iso/19139/resources/gmxCodelists.xml#MD_TopicCategoryCode"}, {"concepts": [{"id": "Soil"}], "scheme": "AGROVOC Multilingual agricultural thesaurus"}, {"concepts": [{"id": "opendata"}, {"id": "Managed Aquifer Recharge (MAR); Surface infiltration; Water sustainability; Site suitability analysis"}], "scheme": "Individual"}, {"concepts": [{"id": "Boden"}], "scheme": "GEMET - INSPIRE themes, version 1.0"}, {"concepts": [{"id": "Germany"}, {"id": "Brandenburg"}, {"id": "Oder-Spree"}, {"id": "M\u00e4rkisch-Oderland"}, {"id": "Untere Spree"}], "scheme": "individual"}], "license": "CC BY", "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": "2025-08-18", "created": "2025-07-23", "language": "eng", "title": "Natural and constructively enlarged depressions for surface induced managed aquifer recharge (MAR) within Brandenburg\u00b4s lower Spree catchment  - enlarged sinks", "description": "This layer contains the outlines and suitability parameters of naturally and constructively enlarged topographic depressions for surface induced managed aquifer recharge within the preselected areas of Brandenburg\u00b4s lower Spree catchment.\n\nGeneral description see mother table: (https://doi.org/10.4228/zalf-5qhx-vs57); Related datasets are listed in the metadata element 'Related Identifier'.\nDataset version 1.0", "formats": [{"name": "CSV"}], "keywords": ["Soil", "opendata", "Managed Aquifer Recharge (MAR); Surface infiltration; Water sustainability; Site suitability analysis", "Boden", "Germany", "Brandenburg", "Oder-Spree", "M\u00e4rkisch-Oderland", "Untere Spree"], "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": "Jan Stautzebach", "organization": "Leibniz Centre for Agricultural Landscape Research", "position": null, "roles": ["author"], "phones": [{"value": null}], "emails": [{"value": "Jan.Stautzebach@zalf.de"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": {"url": null, "protocol": null, "protocol_url": "", "name": "0009-0000-8884-8759", "name_url": "", "description": "ORCID", "description_url": "", "applicationprofile": null, "applicationprofile_url": "", "function": null}}]}, {"name": "J\u00f6rg Steidl", "organization": "Leibniz Centre for Agricultural Landscape Research", "position": null, "roles": ["author"], "phones": [{"value": null}], "emails": [{"value": "jsteidl@zalf.de"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": {"url": null, "protocol": null, "protocol_url": "", "name": "0000-0002-6599-0450", "name_url": "", "description": "ORCID", "description_url": "", "applicationprofile": null, "applicationprofile_url": "", "function": null}}]}, {"name": "Christoph Merz", "organization": "Leibniz Centre for Agricultural Landscape Research", "position": null, "roles": ["projectLeader"], "phones": [{"value": null}], "emails": [{"value": "merz@zalf.de"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": {"url": null, "protocol": null, "protocol_url": "", "name": "0000-0001-7434-9828", "name_url": "", "description": "ORCID", "description_url": "", "applicationprofile": null, "applicationprofile_url": "", "function": null}}]}, {"organization": "Leibniz Centre for Agricultural Landscape Research", "roles": ["contributor"]}], "title_alternate": "Data collection: Part 3/4, table: enlarged sinks"}, "links": [{"href": "https://maps.bonares.de/mapapps/resources/apps/bonares/index.html?lang=en&mid=5699b586-6dcb-490e-b35d-29fcb2ca921f", "rel": "information"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/e97fb592-8f94-4b81-af43-32b0cf8af516", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "5699b586-6dcb-490e-b35d-29fcb2ca921f", "name": "item", "description": "5699b586-6dcb-490e-b35d-29fcb2ca921f", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/5699b586-6dcb-490e-b35d-29fcb2ca921f"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-08-18T00:00:00Z"}}, {"id": "bb9ad1c0-88fd-11da-a88f-000d939bc5d8", "type": "Feature", "geometry": {"type": "Polygon", "coordinates": [[[-180.0, -90.0], [-180.0, 90.0], [180.0, 90.0], [180.0, -90.0], [-180.0, -90.0]]]}, "properties": {"themes": [{"concepts": [{"id": "geoscientificInformation"}], "scheme": "https://standards.iso.org/iso/19139/resources/gmxCodelists.xml#MD_TopicCategoryCode"}], "updated": "2024-07-23T14:25:20", "created": "2002", "language": "eng", "title": "Maximum available soil moisture (Global)", "description": "Grid with estimated maximum available soil moisture in mm/m with a spatial resolution of 5 * 5 arc minutes. Information with regard to maximum available soil moisture was calculated from the \"Derived Soil Properties\" of the \"Digital Soil Map of the World\" which contains raster information on soil moisture in different classes.", "formats": [{"name": "WWW:DOWNLOAD-1.0-http--download"}, {"name": "OGC:WMS-1.1.1-http-get-map"}], "keywords": ["soil moisture", "AQUAMAPS_globwat", "infiltration", "rooting depth", "Tag_AQUASTAT", "World"], "contacts": [{"name": "Jippe Hoogeveen (Water Resources Officer)", "organization": "Food and Agriculture Organization of the United Nations - Land and Water Division", "position": null, "roles": ["originator"], "phones": [{"value": null}], "emails": [{"value": null}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": null}]}, {"organization": "Food and Agriculture Organization of the United Nations - Land and Water Division", "roles": ["creator"]}], "distanceuom": ",", "edition": "first"}, "links": [{"href": "https://storage.googleapis.com/fao-maps-catalog-data/geonetwork/aquamaps/GlobWat-Input-smax.zip", "description": "Maximum available soil moisture - GlobWat input, 5 arc min ASCII-grid", "protocol": "WWW:DOWNLOAD-1.0-http--download", "rel": "download"}, {"href": "https://io.apps.fao.org/geoserver/wms", "name": "AQUAMAPS:hwsd_smax", "description": "Maximum available soil moisture (mm/m)", "protocol": "OGC:WMS-1.1.1-http-get-map", "rel": "information"}, {"href": "https://data.apps.fao.org:/map/catalog/srv/api/records/bb9ad1c0-88fd-11da-a88f-000d939bc5d8/attachments/5018_image.gif", "name": "preview", "description": "Web image thumbnail (URL)", "protocol": "WWW:LINK-1.0-http--image-thumbnail", "rel": "preview"}, {"rel": "self", "type": "application/geo+json", "title": "bb9ad1c0-88fd-11da-a88f-000d939bc5d8", "name": "item", "description": "bb9ad1c0-88fd-11da-a88f-000d939bc5d8", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/bb9ad1c0-88fd-11da-a88f-000d939bc5d8"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date-time": "2024-07-23T14:25:20Z"}}, {"id": "52d2d849684efb3d334739f34cd25b3a", "type": "Feature", "geometry": null, "properties": {"license": "https://spdx.org/licenses/CC-BY-4.0.html", "updated": "2024-12-03T00:00:00Z", "type": "Dataset", "language": "fr", "title": "Atlas of Walloon Karst - Point Karst Sites", "description": "This data layer constitutes an inventory of karst sites in a point form appearing in the Atlas of the Walloon Karst.  In Wallonia, 30% of the subsoil is made up of soluble carbonate rocks (limestone, dolomite, chalk, gypsum, etc.). By infiltrating these rocks, runoff generates a dissolution of these rocks, which gives rise to particular phenomena both underground (caves, underground rivers) and on the surface (chantoirs, sinkholes, collapses, cavities, etc.). These phenomena are called \"karstic\". By extension, the word \"karst\" also refers to a limestone region, or more broadly a region of soluble rocks whose landscape is marked by the effects of dissolution. We therefore speak of \"rock\", \"region\" or \"landscape\" karst.  The Atlas of Walloon Karst is the reference document for karst phenomena in Wallonia. In this context, the sites in which these phenomena take place are located and described, and two modes of representation follow: punctual or surface.   This data layer includes all the karst sites, both underground and above ground, located punctually (via their X,Y coordinates). There are more than 8000 phenomena in this layer. The associated table includes an identifier for each phenomenon (IGN map number + unique site number), the name and qualifier of the site (e.g. Grotte d'Eprave), the municipality in which the phenomenon is located, the watercourse draining the area of the site, fields to differentiate the site according to their nature and a hyperlink to the site data sheet.  The data layer is continuously updated by the Walloon Commission for the Study and Protection of Underground Sites (CWEPSS) with the help of many collaborators. It is managed by the Geological Service of Wallonia (SPW - DGO3 - DEE - DRIGM).", "formats": [{"name": "SHP"}], "keywords": ["High value dataset", "akwa", "atlas", "be", "calcaire", "carbonate", "carbone", "carte-ge\u0301ologique", "cavite\u0301", "chantoir", "conservation-de-la-nature", "conservation-des-ressources-naturelles", "conservation-du-sol", "craie", "cwepss", "dissolution", "doline", "eau-d'infiltration", "eau-du-sol", "eaux-souterraines", "faille", "galerie", "ge\u0301ologie", "grotte", "gypse", "hydroge\u0301ologie", "karst", "puits", "ref_autre", "re\u0301gional", "risque-naturel", "roche", "site-naturel", "sol", "spe\u0301le\u0301ologie", "zones-a\u0300-risque-naturel", "zones-naturelles", "-paysages", "-e\u0301cosyste\u0300mes"], "contacts": [{"organization": "Helpdesk carto du SPW (SPW - Secr\u00e9tariat g\u00e9n\u00e9ral - SPW Digital - D\u00e9partement de la G\u00e9omatique - Direction de l'Int\u00e9gration des g\u00e9odonn\u00e9es)", "roles": ["creator"]}, {"organization": "https://org.belgif.be/id/CbeEstablishmentUnit/2204322327", "roles": ["publisher"]}]}, "links": [{"href": "https://geodata.wallonie.be/dataset/21ffa962-8c28-4497-b1b7-697d7cf930ed"}, {"href": "https://geoservices.wallonie.be/geoserver/inspire_nz/ows?service=WMS&version=1.3.0&request=GetCapabilities"}, {"href": "https://metawal.wallonie.be/geonetwork/srv/api/records/21ffa962-8c28-4497-b1b7-697d7cf930ed"}, {"href": "http://data.europa.eu/88u/dataset/https-geodata-wallonie-be-id-21ffa962-8c28-4497-b1b7-697d7cf930ed"}, {"href": "https-geodata-wallonie-be-id-21ffa962-8c28-4497-b1b7-697d7cf930ed"}, {"href": "https://geodata.wallonie.be/id/21ffa962-8c28-4497-b1b7-697d7cf930ed"}, {"rel": "self", "type": "application/geo+json", "title": "52d2d849684efb3d334739f34cd25b3a", "name": "item", "description": "52d2d849684efb3d334739f34cd25b3a", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/52d2d849684efb3d334739f34cd25b3a"}, {"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": "059939806548a8af61e19dbc514dd4bb", "type": "Feature", "geometry": null, "properties": {"license": "https://spdx.org/licenses/CC-BY-4.0.html", "updated": "2020-02-05T00:00:00Z", "type": "Dataset", "language": "fr", "title": "LIDAXES (version 2) - Axes of concentration of runoff (vector)", "description": "This vector data layer represents the natural concentration axes of runoff water, which correspond to thalwegs, valleys and dry valleys, established on the basis of the MNT LiDAR 2013-2014.  The mapping of the natural concentration axes of runoff (LiDAXES) highlights areas at risk of runoff flooding and/or muddy flow arising from the natural concentration of surface runoff.  It is a linear vector data layer with 5 classes defined by the size of the watershed drained by the concentration axes. The amount of runoff increases as the size of the upstream watershed increases. The following classes are distinguished: - concentrated runoff routes draining water from a catchment area between 3 and 10 ha; - concentrated runoff routes draining water from a catchment area between 10 and 20 ha; - concentrated runoff routes draining water from a catchment area between 20 and 50 ha; - concentrated runoff routes draining water from a catchment area between 50 and 100 ha; - concentrated runoff routes draining water from a catchment area of more than 100 ha.  This layer has been established throughout the Walloon territory covered by the MNT LiDAR 2013-2014 (1m resolution). A pre-treatment of this NTM was first carried out to transform it into a 2m resolution with the aim of optimising the route of the axes. Indeed, too precise a resolution risks giving too much importance to too small elements of the landscape that are short-circuited during extreme rainy events. But it is the latter that cause the catastrophic damage. For reasons of readability, the information is only visible on scales between 1/1 000th and 1/5 000th.  Concentrated runoff axes are integrated into the Walloon hydrographic network (RHW). Therefore, this data layer is an indispensable complement to the reading of LIDAXES data. In general, the axes of concentration of runoff find their outlet in a watercourse without leaving it.   This layer is the result of a vectorization made from runoff axes in raster format (based on the \"Internet\" version of the raster).  This version of the data layer is generic and corresponds to the external version made available by the Public Service of Wallonia. It is therefore available through viewing service and download subject to the conditions of access and use.  For more details, refer to the methodological reports available in associated resources.   Finally, the reader will find municipal statistics in the document \"km of axes per municipality\".", "formats": [{"name": "REST"}], "keywords": ["High value dataset", "accumulation", "agriculture", "axe", "be", "catastrophes", "-accidents", "-risques", "cennic", "climat", "concentration", "cours-d'eau", "de\u0301pression", "drainage", "eau", "eau-d'infiltration", "eau-de-drainage", "eau-du-sol", "erruissol", "e\u0301coulement", "flux", "fosse\u0301", "inondation", "lidar", "lidaxe", "lidaxes", "mnt", "mode\u0300le-terrestre-nume\u0301rique", "pe\u0301riode-de-retour", "picc", "pluie", "re\u0301gional", "re\u0301seau-de-drainage", "re\u0301seau-hydrographique", "ruissellement", "ruissellement-concentre\u0301", "sol", "sous-bassin-hydrographique", "stockage-de-l'eau", "talweg", "thalweg", "valle\u0301e", "zones-a\u0300-risque-naturel", "zones-naturelles", "-paysages", "-e\u0301cosyste\u0300mes"], "contacts": [{"organization": "Helpdesk carto du SPW (SPW - Secr\u00e9tariat g\u00e9n\u00e9ral - SPW Digital - D\u00e9partement Donn\u00e9es transversales - Gestion et valorisation de la donn\u00e9e)", "roles": ["creator"]}, {"organization": "https://org.belgif.be/id/CbeEstablishmentUnit/2204322327", "roles": ["publisher"]}]}, "links": [{"href": "https://geodata.wallonie.be/dataset/3915ed27-f869-41ae-8eea-7821aa49d211"}, {"href": "https://geoservices.wallonie.be/arcgis/rest/services/EAU/LIDAXES/MapServer"}, {"href": "https://geoservices.wallonie.be/arcgis/services/EAU/LIDAXES/MapServer/WMSServer?request=GetCapabilities&service=WMS"}, {"href": "https://geoservices.wallonie.be/geoserver/inspire_nz/ows?service=WMS&version=1.3.0&request=GetCapabilities"}, {"href": "https://metawal.wallonie.be/geonetwork/srv/api/records/3915ed27-f869-41ae-8eea-7821aa49d211"}, {"href": "http://data.europa.eu/88u/dataset/https-geodata-wallonie-be-id-3915ed27-f869-41ae-8eea-7821aa49d211"}, {"href": "https-geodata-wallonie-be-id-3915ed27-f869-41ae-8eea-7821aa49d211"}, {"href": "https://geodata.wallonie.be/id/3915ed27-f869-41ae-8eea-7821aa49d211"}, {"rel": "self", "type": "application/geo+json", "title": "059939806548a8af61e19dbc514dd4bb", "name": "item", "description": "059939806548a8af61e19dbc514dd4bb", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/059939806548a8af61e19dbc514dd4bb"}, {"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": "09343f827d6858c6ceea733023b4eda5", "type": "Feature", "geometry": null, "properties": {"license": "https://spdx.org/licenses/CC-BY-4.0.html", "updated": "2024-09-10T00:00:00Z", "type": "Dataset", "language": "fr", "externalIds": [{"value": "https://geodata.wallonie.be/id/b39901a6-9955-48e7-be14-b0ba0636f9bb"}], "title": "INSPIRE - Atlas of Walloon Karst - Underground flows in Wallonia (BE)", "description": "This INSPIRE data layer is based on the tracing of groundwater circulations in the Atlas of Walloon Karst.  This INSPIRE compliant data layer comes from the Atlas data of the Walloon karst - Underground flows.  In Wallonia, 30% of the subsoil is made up of soluble carbonate rocks (limestone, dolomite, chalk, gypsum, etc.). By infiltrating these rocks, runoff generates a dissolution of these rocks, which gives rise to particular phenomena both underground (caves, underground rivers) and on the surface (chantoirs, sinkholes, collapses, cavities, etc.). These phenomena are called \"karstic\". By extension, the word \"karst\" also refers to a limestone region, or more broadly a region of soluble rocks whose landscape is marked by the effects of dissolution. We therefore speak of \"rock\", \"region\" or \"landscape\" karst.  The Atlas of Walloon Karst is the reference document for karst phenomena in Wallonia. This data layer is integrated and symbolizes the tracing of groundwater flows in the karst between an infiltration point and an emergence point (loss/resurgence type relationships. This information is one of the major features of karst hydrology.   The data layer distinguishes underground flows that have been recognised by tracing (injection of a dye - code 1) from those that are hypothetical (not established with certainty - code 0).   On the map, a continuous line represents a traffic recognized by tracing. Hypothetical plots are represented in a discontinuous line (see legend). Each underground flow is uniquely identified. The name of the river is indicated, as well as the loss. A hyperlink allows you to consult the corresponding material safety data sheet.  In the Karst Atlas, loss/resurgence links (whether hypothetical or trace-verified) are very generally represented by straight lines between the \"incoming and outgoing\" of the underground environment. They therefore do not indicate in any way the route taken by the waters to reach the resurgence loss points, which will depend on the nature of the aquifer of the type of terrain, the presence of tectonic accidents and the orientation of the groundwater collector which may, in the karst, be completely independent of the surface relief.   In addition, some injection points refer to piezometers and therefore do not correspond to a karst phenomenon.   The data layer is continuously updated by the Walloon Commission for the Study and Protection of Underground Sites (CWEPSS) with the help of many collaborators. It is managed by the Geological Service of Wallonia (SPW - DGO3 - DEE - DRIGM)", "formats": [{"name": "GEOJSON"}], "keywords": ["High value dataset", "akwa", "atlas", "be", "calcaire", "carbonate", "carbone", "carte-ge\u0301ologique", "cavite\u0301", "chantoir", "conservation-de-la-nature", "conservation-des-ressources-naturelles", "conservation-du-sol", "craie", "cwepss", "dissolution", "doline", "eau-d'infiltration", "eau-du-sol", "eaux-souterraines", "faille", "galerie", "ge\u0301ologie", "grotte", "gypse", "hydroge\u0301ologie", "hydrographie", "karst", "puits", "ref_autre", "re\u0301gional", "risque-naturel", "roche", "site-naturel", "sol", "spe\u0301le\u0301ologie", "zones-naturelles", "-paysages", "-e\u0301cosyste\u0300mes"], "contacts": [{"organization": "Helpdesk carto du SPW (SPW - Secr\u00e9tariat g\u00e9n\u00e9ral - SPW Digital - D\u00e9partement de la G\u00e9omatique - Direction de l'Int\u00e9gration des g\u00e9odonn\u00e9es)", "roles": ["creator"]}, {"organization": "https://org.belgif.be/id/CbeEstablishmentUnit/2204322327", "roles": ["publisher"]}]}, "links": [{"href": "https://geodata.wallonie.be/dataset/4641a948-c4e7-482b-9ebf-023308bfc5b0"}, {"href": "https://geoservices.wallonie.be/geoserver/inspire_hy/ogc/features/v1/openapi"}, {"href": "https://geoservices.wallonie.be/geoserver/inspire_hy/ows?service=WMS&version=1.3.0&request=GetCapabilities"}, {"href": "https://metawal.wallonie.be/geonetwork/srv/api/records/4641a948-c4e7-482b-9ebf-023308bfc5b0"}, {"href": "http://data.europa.eu/88u/dataset/https-geodata-wallonie-be-id-4641a948-c4e7-482b-9ebf-023308bfc5b0"}, {"href": "https-geodata-wallonie-be-id-4641a948-c4e7-482b-9ebf-023308bfc5b0"}, {"href": "https://geodata.wallonie.be/id/4641a948-c4e7-482b-9ebf-023308bfc5b0"}, {"rel": "self", "type": "application/geo+json", "title": "09343f827d6858c6ceea733023b4eda5", "name": "item", "description": "09343f827d6858c6ceea733023b4eda5", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/09343f827d6858c6ceea733023b4eda5"}, {"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": "ad690da62bd6062381983a0ea09f93be", "type": "Feature", "geometry": null, "properties": {"license": "https://spdx.org/licenses/CC-BY-4.0.html", "updated": "2024-09-05T00:00:00Z", "type": "Dataset", "language": "fr", "externalIds": [{"value": "https://geodata.wallonie.be/id/7e1d6ad6-7d68-4c2c-bb3a-942265e9c416"}], "title": "INSPIRE - Natural geomorphological entity - karst entities in Wallonia (BE)", "description": "This INSPIRE data layer is an inventory of karst sites in the Atlas of Walloon Karst.  This INSPIRE compliant data layer is derived from the source data \"Atlas du karst wallon - Sites karstiques surfaciques\".  In Wallonia, 30% of the subsoil is made up of soluble carbonate rocks (limestone, dolomite, chalk, gypsum, etc.). By infiltrating these rocks, runoff generates a dissolution of these rocks, which gives rise to particular phenomena both underground (caves, underground rivers) and on the surface (chantoirs, sinkholes, collapses, cavities, etc.). These phenomena are called \"karstic\". By extension, the word \"karst\" also refers to a limestone region, or more broadly a region of soluble rocks whose landscape is marked by the effects of dissolution. We therefore speak of \"rock\", \"region\" or \"landscape\" karst.  The Atlas of Walloon Karst is the reference document for karst phenomena in Wallonia.   This data layer covers all karst sites, both underground and above ground. These data concern phenomena with a ground right-of-way whose diameter exceeds 30m. In this case, the representation by a single dot is not sufficient and does not render the impact that this site may have on the local environment. For these sites, a polygon resuming the contour of the phenomenon is therefore added with the label of the site in its center.   Particular karst phenomena illustrating the same phenomenon can be represented by the same polygon. These envelope curves mainly concern depressions (such as sinkholes) as well as paleokarst and abannets (former pockets of dissolution of carbonate rock, filled with loose ground partly evacuated and extracted by humans).  The associated winning table includes an identifier for each phenomenon (IGN card number + unique site number), the name and qualifier of the site, the municipality in which the phenomenon is located, fields to differentiate the site according to their nature and a hyperlink to the site data sheet.  The source data layer is continuously updated by the Walloon Commission for the Study and Protection of Underground Sites (CWEPSS) with the help of many collaborators. It is managed by the Geological Service of Wallonia (SPW - Agriculture, Natural Resources and Environment - Department of Environment and Water - Directorate of Industrial, Geological and Mining Risks).", "formats": [{"name": "GEOJSON"}], "keywords": ["High value dataset", "akwa", "atlas", "be", "calcaire", "carbonate", "carbone", "carte-ge\u0301ologique", "cavite\u0301", "chantoir", "conservation-de-la-nature", "conservation-des-ressources-naturelles", "conservation-du-sol", "craie", "cwepss", "dissolution", "doline", "eau-d'infiltration", "eau-du-sol", "eaux-souterraines", "faille", "galerie", "ge\u0301ologie", "grotte", "gypse", "hydroge\u0301ologie", "karst", "puits", "ref_autre", "re\u0301gional", "risque-naturel", "roche", "site-naturel", "sol", "spe\u0301le\u0301ologie", "zones-naturelles", "-paysages", "-e\u0301cosyste\u0300mes"], "contacts": [{"organization": "Helpdesk carto du SPW (SPW - Secr\u00e9tariat g\u00e9n\u00e9ral - SPW Digital - D\u00e9partement de la G\u00e9omatique - Direction de l'Int\u00e9gration des g\u00e9odonn\u00e9es)", "roles": ["creator"]}, {"organization": "https://org.belgif.be/id/CbeEstablishmentUnit/2204322327", "roles": ["publisher"]}]}, "links": [{"href": "https://geodata.wallonie.be/dataset/82cfca80-6c37-423e-8f19-13fadf055ea0"}, {"href": "https://geoservices.wallonie.be/geoserver/inspire_ge/ogc/features/v1/openapi"}, {"href": "https://geoservices.wallonie.be/geoserver/inspire_ge/ows?service=WMS&version=1.3.0&request=GetCapabilities"}, {"href": "https://metawal.wallonie.be/geonetwork/srv/api/records/82cfca80-6c37-423e-8f19-13fadf055ea0"}, {"href": "http://data.europa.eu/88u/dataset/https-geodata-wallonie-be-id-82cfca80-6c37-423e-8f19-13fadf055ea0"}, {"href": "https-geodata-wallonie-be-id-82cfca80-6c37-423e-8f19-13fadf055ea0"}, {"href": "https://geodata.wallonie.be/id/82cfca80-6c37-423e-8f19-13fadf055ea0"}, {"rel": "self", "type": "application/geo+json", "title": "ad690da62bd6062381983a0ea09f93be", "name": "item", "description": "ad690da62bd6062381983a0ea09f93be", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/ad690da62bd6062381983a0ea09f93be"}, {"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": "f3a0be5b1d9b6ae0c8a385c2e50f42cf", "type": "Feature", "geometry": null, "properties": {"license": "https://spdx.org/licenses/CC-BY-4.0.html", "updated": "2024-09-05T00:00:00Z", "type": "Dataset", "language": "fr", "externalIds": [{"value": "https://geodata.wallonie.be/id/7e1d6ad6-7d68-4c2c-bb3a-942265e9c416"}], "title": "INSPIRE - Natural geomorphological entity - natural depressions in Wallonia (BE)", "description": "This INSPIRE data layer is an inventory of natural depressions in the Atlas of Walloon Karst.  This INSPIRE compliant data layer is derived from the source data \"Atlas du karst wallon - Sites karstiques surfaciques\".  In Wallonia, 30% of the subsoil is made up of soluble carbonate rocks (limestone, dolomite, chalk, gypsum, etc.). By infiltrating these rocks, runoff generates a dissolution of these rocks, which gives rise to particular phenomena both underground (caves, underground rivers) and on the surface (chantoirs, sinkholes, collapses, cavities, etc.). These phenomena are called \"karstic\". By extension, the word \"karst\" also refers to a limestone region, or more broadly a region of soluble rocks whose landscape is marked by the effects of dissolution. We therefore speak of \"rock\", \"region\" or \"landscape\" karst.  The Atlas of Walloon Karst is the reference document for karst phenomena in Wallonia.   This data layer covers all karst sites, both underground and above ground. These data concern phenomena with a ground right-of-way whose diameter exceeds 30m. In this case, the representation by a single dot is not sufficient and does not render the impact that this site may have on the local environment. For these sites, a polygon resuming the contour of the phenomenon is therefore added with the label of the site in its center.   Particular karst phenomena illustrating the same phenomenon can be represented by the same polygon. These envelope curves mainly concern depressions (such as sinkholes) as well as paleokarst and abannets (former pockets of dissolution of carbonate rock, filled with loose ground partly evacuated and extracted by humans).  The associated winning table includes an identifier for each phenomenon (IGN card number + unique site number), the name and qualifier of the site, the municipality in which the phenomenon is located, fields to differentiate the site according to their nature and a hyperlink to the site data sheet.  The source data layer is continuously updated by the Walloon Commission for the Study and Protection of Underground Sites (CWEPSS) with the help of many collaborators. It is managed by the Geological Service of Wallonia (SPW - Agriculture, Natural Resources and Environment - Department of Environment and Water - Directorate of Industrial, Geological and Mining Risks).", "formats": [{"name": "GEOJSON"}], "keywords": ["High value dataset", "akwa", "atlas", "be", "calcaire", "carbonate", "carbone", "carte-ge\u0301ologique", "cavite\u0301", "chantoir", "conservation-de-la-nature", "conservation-des-ressources-naturelles", "conservation-du-sol", "craie", "cwepss", "dissolution", "doline", "eau-d'infiltration", "eau-du-sol", "eaux-souterraines", "faille", "galerie", "ge\u0301ologie", "grotte", "gypse", "hydroge\u0301ologie", "karst", "puits", "ref_autre", "re\u0301gional", "risque-naturel", "roche", "site-naturel", "sol", "spe\u0301le\u0301ologie", "zones-naturelles", "-paysages", "-e\u0301cosyste\u0300mes"], "contacts": [{"organization": "Helpdesk carto du SPW (SPW - Secr\u00e9tariat g\u00e9n\u00e9ral - SPW Digital - D\u00e9partement de la G\u00e9omatique - Direction de l'Int\u00e9gration des g\u00e9odonn\u00e9es)", "roles": ["creator"]}, {"organization": "https://org.belgif.be/id/CbeEstablishmentUnit/2204322327", "roles": ["publisher"]}]}, "links": [{"href": "https://geodata.wallonie.be/dataset/a49bb077-a944-466d-9206-042084bd94f9"}, {"href": "https://geoservices.wallonie.be/geoserver/inspire_ge/ogc/features/v1/openapi"}, {"href": "https://geoservices.wallonie.be/geoserver/inspire_ge/ows?service=WMS&version=1.3.0&request=GetCapabilities"}, {"href": "https://metawal.wallonie.be/geonetwork/srv/api/records/a49bb077-a944-466d-9206-042084bd94f9"}, {"href": "http://data.europa.eu/88u/dataset/https-geodata-wallonie-be-id-a49bb077-a944-466d-9206-042084bd94f9"}, {"href": "https-geodata-wallonie-be-id-a49bb077-a944-466d-9206-042084bd94f9"}, {"href": "https://geodata.wallonie.be/id/a49bb077-a944-466d-9206-042084bd94f9"}, {"rel": "self", "type": "application/geo+json", "title": "f3a0be5b1d9b6ae0c8a385c2e50f42cf", "name": "item", "description": "f3a0be5b1d9b6ae0c8a385c2e50f42cf", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/f3a0be5b1d9b6ae0c8a385c2e50f42cf"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"null": "date"}}], "links": [{"rel": "self", "type": "application/geo+json", "title": "This document as GeoJSON", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=infiltration&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=infiltration&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=infiltration&", "hreflang": "en-US"}, {"rel": "last", "type": "application/geo+json", "title": "items (last)", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=infiltration&offset=31", "hreflang": "en-US"}], "numberMatched": 31, "numberReturned": 31, "distributedFeatures": [], "timeStamp": "2026-06-27T22:25:29.253330Z"}