{"type": "FeatureCollection", "features": [{"id": "10.7910/DVN/T8CMAT", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:21:57Z", "type": "Dataset", "created": "2016-02-28", "title": "GMCSD-2. Global Mangrove Carbon, 2000 to 2012, 1 Arc-second, 1 m soil.", "description": "Open AccessGlobal Mangrove Carbon, 2000 to 2012, 1 Arc-Second, 1 m Soil, mid, EQ5.  <p> Annual stocks.  <p> Each of these 13 years is 3TB when extracted. So that is 39 TB as a tif. <p> We needed to use file geodatabase format to compress enough to post on the Dataverse. Hence no TIffs.", "keywords": ["Earth and Environmental Sciences", "Raster", "ArcGIS file Geodatabase rasters", "Global Mangrove Carbon"], "contacts": [{"organization": "Hamilton, Stuart", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.7910/DVN/T8CMAT"}, {"rel": "self", "type": "application/geo+json", "title": "10.7910/DVN/T8CMAT", "name": "item", "description": "10.7910/DVN/T8CMAT", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.7910/DVN/T8CMAT"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2016-01-01T00:00:00Z"}}, {"id": "10.1016/j.agee.2007.01.008", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:15:06Z", "type": "Journal Article", "created": "2007-02-10", "title": "Predicted Soil Organic Carbon Stocks And Changes In The Brazilian Amazon Between 2000 And 2030", "description": "Abstract   Currently we have little understanding of the impacts of land use change on soil C stocks in the Brazilian Amazon. Such information is needed to determine impacts on the global C cycle and the sustainability of agricultural systems that are replacing native forest. The aim of this study was to predict soil carbon stocks and changes in the Brazilian Amazon during the period between 2000 and 2030, using the GEFSOC soil carbon (C) modelling system. In order to do so, we devised current and future land use scenarios for the Brazilian Amazon, taking into account: (i) deforestation rates from the past three decades, (ii) census data on land use from 1940 to 2000, including the expansion and intensification of agriculture in the region, (iii) available information on management practices, primarily related to well managed pasture versus degraded pasture and conventional systems versus no-tillage systems for soybean ( Glycine max ) and (iv) FAO predictions on agricultural land use and land use changes for the years 2015 and 2030. The land use scenarios were integrated with spatially explicit soils data (SOTER database), climate, potential natural vegetation and land management units using the recently developed GEFSOC soil C modelling system. Results are presented in map, table and graph form for the entire Brazilian Amazon for the current situation (1990 and 2000) and the future (2015 and 2030). Results include soil organic C (SOC) stocks and SOC stock change rates estimated by three methods: (i) the Century ecosystem model, (ii) the Rothamsted C model and (iii) the intergovernmental panel on climate change (IPCC) method for assessing soil C at regional scale. In addition, we show estimated values of above and belowground biomass for native vegetation, pasture and soybean. The results on regional SOC stocks compare reasonably well with those based on mapping approaches. The GEFSOC system provided a means of efficiently handling complex interactions among biotic-edapho-climatic conditions (>363,000 combinations) in a very large area (\u223c500\u00a0Mha) such as the Brazilian Amazon. All of the methods used showed a decline in SOC stock for the period studied; Century and RothC simulated values for 2030 being about 7% lower than those in 1990. Values from Century and RothC (30,430 and 25,000\u00a0Tg for the 0\u201320\u00a0cm layer for the Brazilian Amazon region were higher than those obtained from the IPCC system (23,400\u00a0Tg in the 0\u201330\u00a0cm layer). Finally, our results can help understand the major biogeochemical cycles that influence soil fertility and help devise management strategies that enhance the sustainability of these areas and thus slow further deforestation.", "keywords": ["land use change", "2. Zero hunger", "clay loam acrisol", "550", "330", "no-tillage", "cropping systems", "04 agricultural and veterinary sciences", "Brazilian Amazon", "regional-scale", "15. Life on land", "matter dynamics", "soil organic carbon", "land-use change", "long-term experiments", "southern brazil", "tropical deforestation", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "regional estimates", "eastern amazonia"]}, "links": [{"href": "https://doi.org/10.1016/j.agee.2007.01.008"}, {"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.2007.01.008", "name": "item", "description": "10.1016/j.agee.2007.01.008", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.agee.2007.01.008"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2007-09-01T00:00:00Z"}}, {"id": "050793f8-b173-46f3-81ce-ce97b3673187", "type": "Feature", "geometry": null, "properties": {"updated": "2025-03-04T00:00:00Z", "type": "Dataset", "language": "de", "title": "Inspire SH Floor ALKIS", "description": "This dataset provides a data set derived from ALKIS for the INSPIRE topic soil.", "formats": [{"name": "WFS_SRVC"}], "keywords": ["High value dataset", "adv", "adv-inspire-produktspezifikation-version-2.0.0", "adv-ows-basisprofi", "advmis", "alkis", "amtliches-liegenschaftskatasterinformationssystem", "annex_iii", "boden", "de", "erdbeobachtung-und-umwelt", "geobasisdaten", "inspire_sh_boden_alkis", "inspireidentifiziert", "opendata", "regional", "schleswig-holstein", "sh", "wms"], "contacts": [{"organization": "Landesamt f\u00fcr Vermessung und Geoinformation Schleswig-Holstein", "roles": ["creator"]}]}, "links": [{"href": "https://service.gdi-sh.de/SH_INSPIREDOWNLOAD_AIII_SO?service=WFS&version=2.0.0&request=GetCapabilities"}, {"href": "https://service.gdi-sh.de/SH_INSPIREVIEW_AIII_SO?service=WMS&version=1.3.0&request=GetCapabilities"}, {"href": "http://data.europa.eu/88u/dataset/050793f8-b173-46f3-81ce-ce97b3673187~~1"}, {"rel": "self", "type": "application/geo+json", "title": "050793f8-b173-46f3-81ce-ce97b3673187", "name": "item", "description": "050793f8-b173-46f3-81ce-ce97b3673187", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/050793f8-b173-46f3-81ce-ce97b3673187"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"interval": ["2023-04-14T00:00:00Z", "2023-04-14T00:00:00Z"]}}, {"id": "07e8a679-31b4-ae8c-eaee-6ac56ecb7439", "type": "Feature", "geometry": {"type": "Polygon", "coordinates": [[[6.0, 48.9], [6.0, 51.0], [8.6, 51.0], [8.6, 48.9], [6.0, 48.9]]]}, "properties": {"themes": [{"concepts": [{"id": "boundaries"}], "scheme": "https://standards.iso.org/iso/19139/resources/gmxCodelists.xml#MD_TopicCategoryCode"}, {"concepts": [{"id": "Regional"}], "scheme": "Spatial scope"}, {"concepts": [{"id": "2f23ed6e-0186-4c2b-8380-748389036509"}], "scheme": "mapbender.2.registryId"}, {"concepts": [{"id": "Bodenbedeckung"}, {"id": "Geografische Bezeichnungen"}, {"id": "Verwaltungseinheiten"}, {"id": "Adressen"}, {"id": "Flurst\u00fccke/Grundst\u00fccke (Katasterparzellen)"}, {"id": "Gew\u00e4ssernetz"}, {"id": "Boden"}, {"id": "Geb\u00e4ude"}, {"id": "Bodennutzung"}, {"id": "Verkehrsnetze"}], "scheme": "GEMET - INSPIRE themes, version 1.0"}], "updated": "2023-11-29", "type": "Dataset", "language": "ger", "title": "House coordinates", "description": "House coordinates (georereferenced building addresses) are the connection between the address of a building and its exact location. A house coordinate consists of the building identifier (key administrative unit, address) and the associated building coordinate.", "formats": [{"name": "Database"}], "keywords": ["Regional", "2f23ed6e-0186-4c2b-8380-748389036509", "DummyKeyword", "inspireidentifiziert", "Bodenbedeckung", "Geografische Bezeichnungen", "Verwaltungseinheiten", "Adressen", "Flurst\u00fccke/Grundst\u00fccke (Katasterparzellen)", "Gew\u00e4ssernetz", "Boden", "Geb\u00e4ude", "Bodennutzung", "Verkehrsnetze"], "contacts": [{"name": null, "organization": "Landesamt f\u00fcr Vermessung und Geobasisinformationen", "position": null, "roles": ["pointOfContact"], "phones": [{"value": null}], "emails": [{"value": "vertrieb-geodienste@vermkv.rlp.de"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": null}]}], "denominator": "1000"}, "links": [{"rel": "self", "type": "application/geo+json", "title": "07e8a679-31b4-ae8c-eaee-6ac56ecb7439", "name": "item", "description": "07e8a679-31b4-ae8c-eaee-6ac56ecb7439", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/07e8a679-31b4-ae8c-eaee-6ac56ecb7439"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"interval": ["2015-01-01T00:00:00Z", "2022-11-29T00:00:00Z"]}}, {"id": "0dd547c4-fc28-4c15-9261-43d125e66fdf", "type": "Feature", "geometry": null, "properties": {"updated": "2023-09-04", "type": "Dataset", "title": "Inspire-WFS SL Floor ALKIS \u2013 OGC WFS Interface", "description": "This service provides data for the INSPIRE topic soil from ALKIS.", "formats": [{"name": "INSPIRE DOWNLOAD SERVICE"}], "keywords": ["adv", "adv-inspire-produktspezifikation-(version-2.0)", "adv-ows-basisprofil", "adv-wfs-profil-1.0.0", "alkis", "amtliches-liegenschaftskatasterinformationssystem", "boden", "de", "geobasisdaten", "hvd", "infofeatureaccessservice", "inspire-wfs_sl_boden_alkis", "inspireidentifiziert", "opendata", "saarland", "sl", "soil", "wfs"], "contacts": [{"organization": "GIS Administration", "roles": ["creator"]}]}, "links": [{"href": "https://geoportal.saarland.de/gdi-sl/inspirewfs_Boden_ALKIS?Service=WFS&Request=GetCapabilities"}, {"href": "http://data.europa.eu/88u/dataset/0dd547c4-fc28-4c15-9261-43d125e66fdf"}, {"rel": "self", "type": "application/geo+json", "title": "0dd547c4-fc28-4c15-9261-43d125e66fdf", "name": "item", "description": "0dd547c4-fc28-4c15-9261-43d125e66fdf", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/0dd547c4-fc28-4c15-9261-43d125e66fdf"}, {"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": "10.1002/joc.7241", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:14:14Z", "type": "Journal Article", "created": "2021-06-06", "title": "Long\u2010term changes in drought indices in eastern and central Europe", "description": "Abstract<p>This study analyses long\uffe2\uff80\uff90term changes in drought indices (Standardised Precipitation Index\uffe2\uff80\uff94SPI, Standardised Precipitation\uffe2\uff80\uff93Evapotranspiration Index\uffe2\uff80\uff94SPEI) at 1 and 3\uffe2\uff80\uff89months scales at 182 stations in 11 central and eastern European countries during 1949\uffe2\uff80\uff932018. For comparative purposes, the necessary atmospheric evaporative demand (AED) to obtain SPEI was calculated using two methods, Hargreaves\uffe2\uff80\uff90Samani (SPEIH) and Penman\uffe2\uff80\uff90Monteith (SPEIP). The results show some relevant changes and tendencies in the drought indices. Statistically significant increase in SPI and SPEI during the cold season (November\uffe2\uff80\uff93March), reflecting precipitation increase, was found in the northern part of the study region, in Estonia, Latvia, Lithuania, northern Belarus and northern Poland. In the rest of study domain, a weak and mostly insignificant decrease prevailed in winter. Summer season (June\uffe2\uff80\uff93August) is characterized by changes in the opposite sign. An increase was observed in the north, while a clear decrease in SPEI, reflecting a drying trend, was typical for the southern regions: the Czech Republic, Slovakia, Hungary, Romania, Moldova and southern Poland. A general drying tendency revealed also in April, which was statistically significant over a wide area in the Czech Republic and Poland. Increasing trends in SPI and SPEI for September and October were detected in Romania, Moldova and Hungary. The use of SPEI instead of SPI generally enhances drying trends.</p", "keywords": ["Central Europe", "Evaporative demands", "0207 environmental engineering", "Drought indices", "02 engineering and technology", "15. Life on land", "01 natural sciences", "6. Clean water", "Precipitation indices", "Central and Eastern European Countries", "13. Climate action", "Long term change", "Penman Monteith", "Czech Republic", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1002/joc.7241"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/International%20Journal%20of%20Climatology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1002/joc.7241", "name": "item", "description": "10.1002/joc.7241", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1002/joc.7241"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-06-24T00:00:00Z"}}, {"id": "10.1007/bf00336449", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:14:24Z", "type": "Journal Article", "created": "2004-10-27", "title": "Near-Infrared Characteristics Of Forest Humus Are Correlated With Soil Respiration And Microbial Biomass In Burnt Soil", "description": "Near-infrared spectroscopy and soil physicochemical determinations (pHH2O, organic matter content, total C content, NH                   inf4                   sup+                 , total N content, cation-exchange capacity, and base saturation) were used to characterize fire-or wood ash-treated humus samples. The spectroscopic and the soil physicochemical analysis data from the humus samples were used separately to explain observed variations in soil respiration and microbial biomass C by partial least-square regression. The first regression component obtained from the physicochemical and spectroscopic characterization explained 10\u201312% and 60\u201380% of the biological variation, respectively. This suggests that information on organic material collected from near-infrared spectra is very useful for explaining biological variations in forest humus.", "keywords": ["havumets\u00e4t", "570", "0401 agriculture", " forestry", " and fisheries", "mikrobibiomassa", "moniasteregressio", "04 agricultural and veterinary sciences", "15. Life on land", "maan hengitys", "biologinen variaatio", "630", "l\u00e4hi-infrapuna-aluespektri"], "contacts": [{"organization": "Fritze, H., J\u00e4rvinen, P., Hiukka, R.,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1007/bf00336449"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biology%20and%20Fertility%20of%20Soils", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/bf00336449", "name": "item", "description": "10.1007/bf00336449", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/bf00336449"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "1994-06-01T00:00:00Z"}}, {"id": "10.1007/s10342-012-0672-z", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:14:38Z", "type": "Journal Article", "created": "2012-11-22", "title": "Do Thinnings Influence Biomass And Soil Carbon Stocks In Mediterranean Maritime Pinewoods?", "description": "Open AccessPeer reviewed", "keywords": ["0106 biological sciences", "2. Zero hunger", "Dead wood", "Forest management", "Carbon stock", "Pinus pinaster", "Forest floor", "15. Life on land", "Mineral soil", "01 natural sciences"]}, "links": [{"href": "https://doi.org/10.1007/s10342-012-0672-z"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/European%20Journal%20of%20Forest%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s10342-012-0672-z", "name": "item", "description": "10.1007/s10342-012-0672-z", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s10342-012-0672-z"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2012-11-23T00:00:00Z"}}, {"id": "10.1016/j.agee.2003.12.008", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:15:05Z", "type": "Journal Article", "created": "2004-02-05", "title": "Effects Of Forest Conversion To Pasture On Soil Carbon Content And Dynamics In Brazilian Amazonia", "description": "Abstract   Soils play an important role in the carbon cycle, and deforestation in the tropics affects both soil carbon storage and CO2 release into the atmosphere. The consequences of deforestation and conversion to pasture for soil carbon content and dynamics were examined in two soil types differing mainly by their texture. Two chronosequences were selected, each consisting of an intact forest and three pastures of different ages (4, 8, 15 years and 3, 9, 15 years, respectively). One chronosequence is located in the central part of the Brazilian Amazon basin, where the soils are clayey ferralsols, and the second in the Eastern Brazilian Amazon Basin, where the soils are sandy clayey acrisols. In the upper layer the C content of clayey soils was three times higher than in the sandy soils, but despite the differences in soil texture, the C distribution in the particle-size fractions was quite similar. In the two chronosequences, the conversion to pasture induced a slight increase in C content. Bulk density increases were greater on soils with lower clay contents. The       13   C    measurements, which allowed to calculate the distribution of C derived from forest and from pasture, showed that all the particle-size fractions incorporated C derived from pasture and that a significant proportion of the young organic matter is rapidly trapped in the finest fractions. Although the proportions of pasture-derived C were higher in the sandy soils than in the clayey soils, the amounts of pasture-derived C in the particle-size fractions were 2\u20133 times larger in the clayey soils than in the sandy soils.", "keywords": ["rain-forest", "550", "ZONE TROPICALE", "c-13 natural abundance", "TEXTURE", "[SDV.SA.SDS]Life Sciences [q-bio]/Agricultural sciences/Soil study", "630", "Carbon Cycle", "C-13 isotope", "Amazonia", "EVOLUTION DES SOLS SOUS CULTURE", "STRUCTURE DU SOL", "soil carbon storage", "particle-size fractions", "Pasture", "cultivated oxisols", "ANALYSE ISOTOPIQUE", "SABLE", "eastern amazonia", "Deforestation", "[SDV.SA.SDS] Life Sciences [q-bio]/Agricultural sciences/Soil study", "Acrisol", "2. Zero hunger", "tropical soils Organic-matter dynamics", "Brasil", "size-fractions", "PATURAGE", "turnover", "Soil Carbon", "04 agricultural and veterinary sciences", "South America", "15. Life on land", "CARBONE ORGANIQUE", "STOCK ORGANIQUE", "ARGILE", "0401 agriculture", " forestry", " and fisheries", "DEFORESTATION", "texture"], "contacts": [{"organization": "Desjardins, T., Barros, E., Sarrazin, M., Girardin, C., Mariotti, A.,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1016/j.agee.2003.12.008"}, {"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.2003.12.008", "name": "item", "description": "10.1016/j.agee.2003.12.008", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.agee.2003.12.008"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2004-07-01T00:00:00Z"}}, {"id": "10.1007/s13280-016-0836-z", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:15:02Z", "type": "Journal Article", "created": "2016-11-17", "title": "The impact of swidden decline on livelihoods and ecosystem services in Southeast Asia: A review of the evidence from 1990 to 2015", "description": "Open AccessEl cambio econ\u00f3mico global y las intervenciones pol\u00edticas est\u00e1n impulsando las transiciones de los sistemas de golondrina larga (EPA) a usos alternativos de la tierra en las tierras altas del sudeste asi\u00e1tico. Este estudio presenta una revisi\u00f3n sistem\u00e1tica de c\u00f3mo estas transiciones impactan en los medios de vida y los servicios ecosist\u00e9micos en la regi\u00f3n. M\u00e1s de 17 000 estudios publicados entre 1950 y 2015 se redujeron, en funci\u00f3n de la relevancia y la calidad, a 93 estudios para su posterior an\u00e1lisis. Nuestro an\u00e1lisis de las transiciones del uso de la tierra de los sistemas de cultivo sucios a los intensificados mostr\u00f3 varios resultados: m\u00e1s hogares hab\u00edan aumentado los ingresos generales, pero estos beneficios tuvieron un costo significativo, como la reducci\u00f3n de las pr\u00e1cticas consuetudinarias, el bienestar socioecon\u00f3mico, las opciones de medios de vida y los rendimientos de los productos b\u00e1sicos. El examen de los efectos de las transiciones en las propiedades del suelo revel\u00f3 impactos negativos en el carbono org\u00e1nico del suelo, la capacidad de intercambio cati\u00f3nico y el carbono sobre el suelo. En conjunto, los impulsores inmediatos y subyacentes de las transiciones de la EPA a los usos alternativos de la tierra, especialmente la intensificaci\u00f3n de los cultivos comerciales perennes y anuales, condujeron a disminuciones significativas en la seguridad de los medios de vida preexistentes y los servicios ecosist\u00e9micos que respaldan esta seguridad. Nuestros resultados sugieren que las pol\u00edticas que imponen transiciones en el uso de la tierra a los agricultores de las tierras altas para mejorar los medios de vida y los entornos han sido err\u00f3neas; en el contexto de los diversos usos de la tierra, la agricultura sucia puede apoyar los medios de vida y los servicios ecosist\u00e9micos que ayudar\u00e1n a amortiguar los impactos del cambio clim\u00e1tico en el sudeste asi\u00e1tico.", "keywords": ["Economics", "Cropping", "Geography", " Planning and Development", "0211 other engineering and technologies", "Optimal Operation of Water Resources Systems", "Review", "02 engineering and technology", "livelihoods", "910", "630", "Agricultural and Biological Sciences", "land-use change", "Livelihood", "Engineering", "Context (archaeology)", "Natural resource economics", "11. Sustainability", "Business", "Asia", " Southeastern", "2. Zero hunger", "Global and Planetary Change", "Payments for Ecosystem Services", "Geography", "Ecology", "1. No poverty", "Life Sciences", "Agriculture", "Southeast Asia", "swidden agriculture", "Land Tenure and Property Rights in Agriculture", "Programming language", "Archaeology", "2304 Environmental Chemistry", "Physical Sciences", "Conservation of Natural Resources", "330", "Climate Change", "Soil Science", "Ocean Engineering", "Environmental science", "Livelihood security", "Environmental Chemistry", "Ecosystem services", "Alternative land uses", "Agroforestry", "Biology", "Land use", " land-use change and forestry", "Ecosystem", "Planning and Development", "3305 Geography", "land use", "Food security", "15. Life on land", "shifting cultivation", "Computer science", "Deforestation (computer science)", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "Land use", "Shifting cultivation", "ecosystem services", "Drivers and Impacts of Tropical Deforestation", "2303 Ecology"]}, "links": [{"href": "https://openresearch-repository.anu.edu.au/bitstream/1885/248831/3/01_Dressler_The_impact_of_swidden_decline_2017.pdf.jpg"}, {"href": "https://doi.org/10.1007/s13280-016-0836-z"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Ambio", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s13280-016-0836-z", "name": "item", "description": "10.1007/s13280-016-0836-z", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s13280-016-0836-z"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2016-11-16T00:00:00Z"}}, {"id": "10.1016/j.rse.2016.11.010", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:16:03Z", "type": "Journal Article", "created": "2016-11-26", "title": "Normalizing land surface temperature data for elevation and illumination effects in mountainous areas: A case study using ASTER data over a steep-sided valley in Morocco", "description": "Abstract   The remotely sensed land surface temperature (LST) is a key parameter to monitor surface energy and water fluxes but the strong impact of topography on LST has limited its use to mostly flat areas. To fill the gap, this study proposes a physically-based method to normalize LST data for topographic - namely illumination and elevation - effects over mountainous areas. Both topographic effects are first quantified by inverting a dual-source soil/vegetation energy balance (EB) model forced by 1) the instantaneous solar radiation simulated by a 3D radiative transfer model named DART (Discrete Anisotropic Radiative Transfer) that uses a digital elevation model (DEM), 2) a satellite-derived vegetation index, and 3) local meteorological (air temperature, air relative humidity and wind speed) data available at a given location. The satellite LST is then normalized for topography by simulating the LST using both pixel- and image-scale DART solar radiation and elevation data. The approach is tested on three ASTER (Advanced Spaceborne Thermal Emission and Reflection Radiometer) overpass dates over a steep-sided 6\u00a0km by 6\u00a0km area in the Atlas Mountain in Morocco. The mean correlation coefficient and root mean square difference (RMSD) between EB-simulated and ASTER LST is 0.80 and 3\u00a0\u00b0C, respectively. Moreover, the EB-based method is found to be more accurate than a more classical approach based on a multi-linear regression with DART solar radiation and elevation data. The EB-simulated LST is also evaluated against an extensive ground dataset of 135 autonomous 1-cm depth temperature sensors deployed over the study area. While the mean RMSD between 90\u00a0m resolution ASTER LST and localized ibutton measurements is 6.1\u00a0\u00b0C, the RMSD between EB-simulated LST and ibutton soil temperature is 5.4 and 5.3\u00a0\u00b0C for a DEM at 90\u00a0m and 8\u00a0m resolution, respectively. The proposed topographic normalization is self-calibrated from (LST, DEM, vegetation index and in situ meteorological data) data available over large extents. As a significant perspective this approach opens the path to using normalized LST as input to evapotranspiration retrieval methods based on LST.", "keywords": ["[SDE] Environmental Sciences", "550", "Topographic normalization", "DEM", "0207 environmental engineering", "Energy balance", "02 engineering and technology", "01 natural sciences", "ASTER", "13. Climate action", "[SDE]Environmental Sciences", "DART", "Land surface temperature", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.rse.2016.11.010"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Remote%20Sensing%20of%20Environment", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.rse.2016.11.010", "name": "item", "description": "10.1016/j.rse.2016.11.010", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.rse.2016.11.010"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-02-01T00:00:00Z"}}, {"id": "10.1016/j.biortech.2017.06.076", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:15:23Z", "type": "Journal Article", "created": "2017-06-17", "title": "Trends in food waste valorization for the production of chemicals, materials and fuels: Case study South and Southeast Asia", "description": "Staggering amounts of food waste are being generated in Asia by means of agricultural processing, food transportation and storage, and human food consumption activities. This along with the recent sustainable development goals of food security, environmental protection, and energy efficiency are the key drivers for food waste valorization. The aim of this review is to provide an insight on the latest trends in food waste valorization in Asian countries such as India, Thailand, Singapore, Malaysia and Indonesia. Landfilling, incineration, and composting are the first-generation food waste processing technologies. The advancement of valorisation alternatives to tackle the food waste issue is the focus of this review. Furthermore, a series of examples of key food waste valorization schemes in this Asian region as case studies to demonstrate the advancement in bioconversions in these countries are described. Finally, important legislation aspects for food waste disposal in these Asian countries are also reported.", "keywords": ["2. Zero hunger", "Singapore", "Malaysia", "1. No poverty", "0211 other engineering and technologies", "India", "02 engineering and technology", "Thailand", "01 natural sciences", "Refuse Disposal", "12. Responsible consumption", "Food", "Indonesia", "13. Climate action", "11. Sustainability", "Humans", "Asia", " Southeastern", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.biortech.2017.06.076"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Bioresource%20Technology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.biortech.2017.06.076", "name": "item", "description": "10.1016/j.biortech.2017.06.076", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.biortech.2017.06.076"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-01-01T00:00:00Z"}}, {"id": "10.1016/j.chemosphere.2023.139965", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:15:27Z", "type": "Journal Article", "created": "2023-08-24", "title": "Expanding the applicability domain of QSPRs for predicting water solubility and vapor pressure of PFAS", "description": "Manuscript of the publication 'Expanding the applicability domain of QSPRs for predicting water solubility and vapor pressure of PFAS'.", "keywords": ["water solubility", "Fluorocarbons", "vapor pressure", "Vapor Pressure", "Water solubility", "PFAS", "H2020", "Water", "Applicability domain (AD)", "Asteraceae", "Vapor pressure", "PROMISCES", "Solubility", "QSPR", "applicability domain (AD)", "COSMO-RS"]}, "links": [{"href": "https://doi.org/10.1016/j.chemosphere.2023.139965"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Chemosphere", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.chemosphere.2023.139965", "name": "item", "description": "10.1016/j.chemosphere.2023.139965", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.chemosphere.2023.139965"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-11-01T00:00:00Z"}}, {"id": "10.1016/j.chemosphere.2007.06.085", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:15:27Z", "type": "Journal Article", "created": "2007-08-21", "title": "Warming And Drought Change Trace Element Bioaccumulation Patterns In A Mediterranean Shrubland", "description": "A field experiment consisting of drought and warming manipulation was conducted in a Mediterranean shrubland dominated by the shrubs Erica multiflora and Globularia alypum. The aim was to investigate the effects of the climatic changes predicted by IPCC models for the coming decades on trace element concentration and accumulation in aboveground biomass, plant litter, and soil. Warming increased concentrations and aboveground accumulation of some trace elements related to plant root uptake, such as Al, As, Cr, Cu, and partially Pb. This effect was more general in E. multiflora than in G. alypum. The stronger effects were increases in Al leaf concentrations (42%) and aboveground accumulation (500gha(-1)) in E. multiflora, in As stem biomass accumulation (0.2gha(-1)) in E. multiflora, and in Cr leaf concentrations (51%) in G. alypum and stem aboveground accumulation in E. multiflora (1.1gha(-1)). These species-specific increases were related to greater retranslocation, photosynthetic capacity and growth in E. multiflora than in G. alypum. Warming decreased the concentrations of some trace elements in leaf litter, implying the existence of an increased leaf retranslocation. Drought increased As (40%) and Cd (55%) in E. multiflora stems, whereas it decreased Cu (50%) in leaves, Ni (28%) in stems and Pb (32%) in leaf litter of G. alypum. The increasing concentrations of some trace elements in E. multiflora and not in G. alypum were related to a greater growth reduction in E. multiflora than in G. alypum. Warming increased As soil solubility (67%) and decreased total soil As (21%). Those changes were related to a greater Fe mobilization in warming plot and to a greater plant capture. Drought increased Hg (350%) concentrations in soils but had no significant effects on trace element accumulation in aboveground biomass. The different response to warming and drought in the two dominant species implies uneven changes in the quality of the plant tissues that may have implications for herbivores. This may be specially important for the performance of the studied Mediterranean ecosystems under the warmer and drier conditions predicted by the next decades by the GCM and ecophysiological models.", "keywords": ["2. Zero hunger", "Trace elements", "Biomass concentrations", "Mediterranean Region", "15. Life on land", "Models", " Biological", "01 natural sciences", "Soil content", "6. Clean water", "Trace Elements", "Disasters", "Mediterranean shrubland", "Heavy metals", "13. Climate action", "Metals", " Heavy", "Climate change", "Soil Pollutants", "Biomass", "Seasons", "Weather", "Ecosystem", "Environmental Monitoring", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.chemosphere.2007.06.085"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Chemosphere", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.chemosphere.2007.06.085", "name": "item", "description": "10.1016/j.chemosphere.2007.06.085", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.chemosphere.2007.06.085"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2008-01-01T00:00:00Z"}}, {"id": "10.1016/j.crm.2021.100375", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:15:28Z", "type": "Journal Article", "created": "2021-11-09", "title": "Playing the long game: Anticipatory action based on seasonal forecasts", "description": "Acting in advance of floods, drought and cyclones often requires decision-makers to work with weather forecasts. The inherently probabilistic nature of these forecasts can be problematic when deciding whether to act or not. Cost-loss analysis has previously been employed to support forecast based decision-making such as Forecast-based Financing (FbF), providing insight to when an FbF system has \u2018potential economic value\u2019 relative to a no-forecast alternative. One well-known limitation of cost-loss analysis is the difficulty of estimating losses (which vary with hazard magnitude and extent, and with the dynamics of population vulnerability and exposure). A less-explored limitation is ignorance of the temporal dynamics (sequencing) of costs and losses. That is, even if the potential economic value of a forecast system is high, the stochastic nature of the atmosphere and the probabilistic nature of forecasts could conspire over the first few forecasts to increase the expense of using the system over the no-forecast alternative. Thus, for a forecast-based action system to demonstrate value, it often needs to be used over a prolonged length of time. However, knowing exactly how long it must be used to guarantee value is unquantified. This presents difficulties to institutions mandated to protect those at risk, who must justify the use of limited funds to act in advance of a potential, but not definite disaster, whilst planning multi-year strategies. Here we show how to determine the period over which decision makers must use forecasts in order to be confident of achieving \u2018value\u2019 over a no-forecast alternative. Results show that in the context of seasonal forecasting it is plausible that more than a decade may pass before a FbF system will have some certainty of showing value, and that if a particular user requires an almost-certain guarantee that using a forecast will be better than a no-forecast strategy, they must hold out until a near-perfect forecast system is available. The implication: there is potential value in seasonal forecasts, but to exploit it one must be prepared to play the long game.", "keywords": ["Early warning", "Forecast-based financing", "13. Climate action", "Climate adaptation", "Seasonal climate forecasting", "Meteorology. Climatology", "0207 environmental engineering", "Anticipatory action", "Disaster risk reduction", "02 engineering and technology", "QC851-999", "01 natural sciences", "0105 earth and related environmental sciences"]}, "links": [{"href": "http://sro.sussex.ac.uk/id/eprint/103124/1/macleod_2021_CRM.pdf"}, {"href": "https://doi.org/10.1016/j.crm.2021.100375"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Climate%20Risk%20Management", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.crm.2021.100375", "name": "item", "description": "10.1016/j.crm.2021.100375", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.crm.2021.100375"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-01-01T00:00:00Z"}}, {"id": "10.1016/j.envpol.2005.01.039", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:15:36Z", "type": "Journal Article", "created": "2005-04-08", "title": "California Black Oak Response To Nitrogen Amendment At A High O3, Nitrogen-Saturated Site", "description": "In a nitrogen (N) saturated forest downwind from Los Angeles, California, the cumulative response to long-term background-N and N-amendment on black oak (Quercus kelloggii) was described in a below-average and average precipitation year. Monthly measurements of leaf and branch growth, gas exchange, and canopy health attributes were conducted. The effects of both pollutant exposure and drought stress were complex due to whole tree and leaf level responses, and shade versus full sun leaf responses. N-amended trees had lower late summer carbon (C) gain and greater foliar chlorosis in the drought year. Leaf water use efficiency was lower in N-amended trees in midsummer of the average precipitation year, and there was evidence of poor stomatal control in full sun. In shade, N-amendment enhanced stomatal control. Small differences in instantaneous C uptake in full sun, lower foliar respiration, and greater C gain in low light contributed to the greater aboveground growth observed.", "keywords": ["0106 biological sciences", "Nitrogen", "Acclimatization", "Plant Transpiration", "15. Life on land", "Los Angeles", "01 natural sciences", "6. Clean water", "Disasters", "Quercus", "Ozone", "13. Climate action", "Sunlight", "Environmental Pollutants", "Seasons", "Photosynthesis", "Environmental Monitoring", "0105 earth and related environmental sciences"], "contacts": [{"organization": "Nancy Grulke, P. Mingus, W. Dobrowolski, Mark E. Fenn,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1016/j.envpol.2005.01.039"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Environmental%20Pollution", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.envpol.2005.01.039", "name": "item", "description": "10.1016/j.envpol.2005.01.039", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.envpol.2005.01.039"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2005-10-01T00:00:00Z"}}, {"id": "10.1016/j.foreco.2007.11.013", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:15:43Z", "type": "Journal Article", "created": "2008-01-14", "title": "Beyond Reduced-Impact Logging: Silvicultural Treatments To Increase Growth Rates Of Tropical Trees", "description": "Abstract   Use of reduced-impact logging (RIL) techniques has repeatedly been shown to reduce damage caused by logging. Unfortunately, these techniques do not necessarily ameliorate the low growth rates of many commercial species or otherwise assure recovery of the initial volume harvested during the next cutting cycle. In this study, we analyze the effect of logging and application of additional silvicultural treatments (liana cutting and girdling of competing trees) on the growth rates on trees in general and on of future crop trees (FCTs) of 24 commercial timber species. The study was carried out in a moist tropical forest in Bolivia, where we monitored twelve 27-ha plots for 4 years. Plots received one of four treatments in which logging intensity and silvicultural treatments were varied: control (no logging); normal (reduced-impact) logging; normal logging and low-intensity silviculture; and, increased logging intensity and high-intensity silviculture. Tree growth rates increased with intensity of logging and silvicultural treatments. The growth rates of FCTs of commercial species were 50\u201360% higher in plots that received silvicultural treatments than in the normal logging and control plots. Responses to silvicultural treatments varied among functional groups. The largest increase in growth rates was observed in FCTs belonging to the partially shade-tolerant and the shade-tolerant groups. These results indicate that silvicultural treatments, in addition to the use of RIL techniques, are more likely to result in a higher percentage of timber volume being recovered after the first cutting cycle than RIL alone.", "keywords": ["tropical forest", "0106 biological sciences", "Bolivia", "dry forest", "rain-forest", "Sustainable forest management", "01 natural sciences", "Tropical forest", "reduced-impact logging", "bolivia", "580", "silvicultural treatments", "04 agricultural and veterinary sciences", "15. Life on land", "sustainable forest management", "Reduced-impact logging", "Silvicultural treatments", "sustainable forestry", "trade-offs", "regeneration", "timber production", "0401 agriculture", " forestry", " and fisheries", "brazilian amazon", "Environmental Sciences", "management", "eastern amazon"]}, "links": [{"href": "https://doi.org/10.1016/j.foreco.2007.11.013"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Forest%20Ecology%20and%20Management", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.foreco.2007.11.013", "name": "item", "description": "10.1016/j.foreco.2007.11.013", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.foreco.2007.11.013"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2008-09-01T00:00:00Z"}}, {"id": "10.1016/j.quageo.2018.07.011", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:16:02Z", "type": "Journal Article", "created": "2018-07-24", "title": "Luminescence age constraints on the Pleistocene-Holocene transition recorded in loess sequences across SE Europe", "description": "\u00a9 2018 The Authors Here we investigate the timing of the last glacial loess (L1) - Holocene soil (S0) transition recorded in loess-paleosol sequences from SE Europe (Ukraine, Romania, Serbia) by applying comparative luminescence dating techniques on quartz and feldspars. Equivalent dose measurements were carried out using the single-aliquot regenerative-dose (SAR) protocol on silt (4\u201311 \u03bcm) and sand-sized (63\u201390 \u03bcm and coarser fraction when available) quartz. Feldspar infrared stimulated luminescence (IRSL) emitted by 4\u201311 \u03bcm polymineral grains was measured using the post IR-IRSL290 technique. The paleoenvironmental transition from the last glacial loess to the current interglacial soil was characterized using magnetic susceptibility and its frequency dependence. SAR-OSL dating of 4\u201311 \u03bcm, 63\u201390 \u03bcm and 90\u2013125 \u03bcm quartz provided consistent ages in the loess-paleosol sites investigated, while the post-IR IRSL290 protocol proved unreliable for dating such young samples. Based on these ages and the threshold of the magnetic signal enhancement the onset of soil formation has been placed around 16.6 \u00b1 1.1 ka at Roxolany (Ukraine), 13.5 \u00b1 0.9 ka at Mo\u0161orin (Serbia) and between 17.6 \u00b1 1.4 ka and 12.4 \u00b1 1.0 ka at R\u00e2mnicu S\u0103rat (Romania). The trend observed in the magnetic parameters reflects the intensity of pedogenesis induced by regional climate amelioration during the Late Glacial, but the onset of magnetic susceptibility enhancement precedes the stratigraphic boundary of Pleistocene-Holocene dated at 11.7 ka in ice core records. Thus, magnetic susceptibility indicates a gradual increase in pedogenesis after Termination 1 (\u223c17 ka in the North Atlantic) at the sampling sites. Based on current data, it is not possible to define a synchronous threshold of change for all sections. However, the trend in the magnetic susceptibility data closely reflects the gradual transition from Last Glacial Maximum (LGM) towards the Holocene, with the onset of humus accumulation (A1 horizon) possibly linked to the prevalence of full interglacial conditions.", "keywords": ["PROTOCOL", "Luminescence dating", "Loess", "01 natural sciences", "Southeastern europe", "Magnetic susceptibility", "13. Climate action", "PROXIES", "QUARTZ", "/dk/atira/pure/sustainabledevelopmentgoals/climate_action; name=SDG 13 - Climate Action", "Pleistocene-holocene transition", "IRSL", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.quageo.2018.07.011"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Quaternary%20Geochronology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.quageo.2018.07.011", "name": "item", "description": "10.1016/j.quageo.2018.07.011", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.quageo.2018.07.011"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-02-01T00:00:00Z"}}, {"id": "10.1016/j.quascirev.2018.09.037", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:16:02Z", "type": "Journal Article", "created": "2018-10-06", "title": "Short-term soil formation events in last glacial east European loess, evidence from multi-method luminescence dating", "description": "Here we provide a robust luminescence chronology for Stayky (Ukraine), a reference profile in European Late Pleistocene loess stratigraphy, based on optically stimulated luminescence (OSL) dating on quartz (4-11 \u03bcm, 63-90 \u03bcm) and post infrared-infrared stimulated luminescence (pIR-IRSL)) on polymineral fine grains. For the Bug loess unit, the equivalent of Marine Isotope Stage (MIS 2), results are in agreement between methods, demonstrating that the suite of embryonic soils previously interpreted as reflecting climate variability similar to Greenland interstadials (GI) actually date to \u223c29/27-15 ka, with most emplaced around or after 20 ka. This temporal span is further confirmed by age-depth modelling of available data. Apart from GI-2, no interstadial-type climate events are recorded in Greenland ice core data for that time interval. As short-term pedogenetic phases are also documented in records from central-western Europe, there is a need for more research into the European mid-latitude terrestrial environments response to MIS 2 hydroclimate variability. The dating of Vytachiv paleosol, previously debatably linked to various GI events within MIS 3 resulted in ages of \u223c40 \u00b1 4 ka and \u223c53 \u00b1 4 ka at the lower transition, and \u223c26 \u00b1 2 ka to \u223c30 \u00b1 2 ka in the overlying loess. These ages indicate that the truncated Vytachiv paleosol is either not continuous, or that it encompasses a broader age range within MIS 3 than previously considered. In both cases, data would not allow for an unambiguous linking of this paleosol with specific GI events as previously attempted. The pIR-IRSL290 dating of the loams immediately underneath Pryluky unit in the range of \u223c120 ka to \u223c168 ka and of the Pryluky mollisol from \u223c90 ka to 126 ka confirm the broad correspondence of this unit with MIS 5, although poor dose recovery results open the possibility for further testing on the degree these ages provide overestimated results. Quartz data severely underestimate the pIR-IRSL290 ages for these samples. The application of pIR-IRSL290 dating for the underlying Dnieper till previously linked to the Saalian glaciation resulted in natural signals at the level of laboratory saturation, yielding minimum ages of c. 700 ka. For the same sample, the natural SAR-OSL signals for 4-11 \u03bcm quartz were found significantly below laboratory saturation level, resulting in finite ages of \u223c250-270 ka interpreted here as underestimates, while coarse quartz (63-90 \u03bcm) signals reached about 85% of the laboratory saturation level. These data suggest extreme caution must be taken when dating such old samples using quartz OSL. Results from our high-resolution luminescence dating raises important implications for the chronological representativeness of Stayky as a key loess site in Eastern Europe beyond MIS 2.", "keywords": ["Embryonic soils", "550", "Millennial-scale loess records", "Luminescence dating", "Loess", "Eastern Europe", "551", "Climate dynamics", "Pleistocene", "[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/Climatology", "[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology", "13. Climate action", "[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy", "[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy", "MIS 2 embryonic soils"]}, "links": [{"href": "https://doi.org/10.1016/j.quascirev.2018.09.037"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Quaternary%20Science%20Reviews", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.quascirev.2018.09.037", "name": "item", "description": "10.1016/j.quascirev.2018.09.037", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.quascirev.2018.09.037"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-11-01T00:00:00Z"}}, {"id": "10.1016/j.scitotenv.2004.09.032", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:16:04Z", "type": "Journal Article", "created": "2004-12-15", "title": "Differences In Cd And Zn Bioaccumulation For The Flood-Tolerant Salix Cinerea Rooting In Seasonally Flooded Contaminated Sediments", "description": "Several authors suggest that a hydrological regime aiming at wetland creation is a potential management option that favours reducing bioavailability for metal-contaminated sites. The hydrological conditions on a site constitute one of the many factors that may affect the availability of potentially toxic trace metals for uptake by plants. Bioavailability of Cd, Mn and Zn on a contaminated dredged sediment landfill (DSL) with variable duration of submersion was evaluated by measuring metal concentrations in the wetland plant species Salix cinerea in field conditions. Longer submersion periods in the field caused lower Cd and Zn concentrations in the leaves in the first weeks of the growing season. Foliar Cd and Zn concentrations at the end of the growing season were highest on the initially flooded plot that emerged early in the growing season. Foliar Zn concentrations were also high at a sandy-textured oxic plot with low soil metal concentrations. Zn uptake in the leaves was markedly slower than Cd uptake for trees growing on soils with prolonged waterlogging during the growing season, pointing at a different availability. Zn availability was lowest when soil was submerged, but metal transfer from stems and twigs to leaves may mask the lower availability of Cd in submerged soils. Especially for Cd, a transfer effect from one growing season to the next season was observed: oxic conditions at the end of the previous growing season seem to determine at least partly the foliar concentrations for S. cinerea through this metal transfer mechanism. Duration of the submersion period is a key factor for bioavailability inasmuch as initially submerged soils emerging only in the second half of the growing season resulted in elevated Cd and Zn foliar concentrations at that time.", "keywords": ["Geologic Sediments", "Plant Stems", "Salix", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "6. Clean water", "Disasters", "Plant Leaves", "13. Climate action", "Metals", " Heavy", "Soil Pollutants", "0401 agriculture", " forestry", " and fisheries", "Seasons", "Sulfur", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.scitotenv.2004.09.032"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Science%20of%20The%20Total%20Environment", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.scitotenv.2004.09.032", "name": "item", "description": "10.1016/j.scitotenv.2004.09.032", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.scitotenv.2004.09.032"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2005-04-01T00:00:00Z"}}, {"id": "10.1071/sr07021", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:17:00Z", "type": "Journal Article", "created": "2007-09-19", "title": "Burning Crop Residues Under No-Till In Semi-Arid Land, Northern Spain\u2014Effects On Soil Organic Matter, Aggregation, And Earthworm Populations", "description": "<p>  Stubble burning has traditionally been used in semi-arid land for pest and weed control, and to remove the excess of crop residues before seeding in no-tillage systems. We compared differences in soil properties in a long-term (10 years) tillage trial on a carbonated soil in semi-arid north-east Spain under no-tillage with stubble returned and stubble burnt, with the conventional tillage system (mouldboard plough, stubble returned) as a reference. Differences in total soil organic C and C in particulate organic matter, mineralisation potential, soil physical properties (bulk density, penetration resistance, and aggregate size distribution and stability), and earthworm populations were quantified. The effect of stubble burning was absent or insignificant compared with that of tillage in most of the parameters studied. The most significant effect of stubble burning was the change in soil organic matter quality in the topsoil and penetration resistance. No-till plus stubble burning stocked an amount of organic C in the soil similar to no-till without burning, but the particulate organic matter content and mineralisation potential were smaller. Earthworm activity was similar under the 2 no-till systems, although a trend towards bigger earthworms with increasing penetration resistance was observed under the system with burning. Our results indicate that the role of burnt plant residues and earthworms in organic matter accumulation and soil aggregation in Mediterranean carbonated soils under no tillage is of major importance, meriting further attention and research. </p>", "keywords": ["2. Zero hunger", "long-term", "microbial biomass", "carbon", "australia", "stubble management", "dynamics", "04 agricultural and veterinary sciences", "15. Life on land", "eastern victoria", "conservation tillage", "systems", "0401 agriculture", " forestry", " and fisheries", "agricultural soils"]}, "links": [{"href": "https://doi.org/10.1071/sr07021"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1071/sr07021", "name": "item", "description": "10.1071/sr07021", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1071/sr07021"}, {"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": "10.1093/jpe/rtw066", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:17:16Z", "type": "Journal Article", "created": "2016-06-29", "title": "Effects Of Soil Warming History On The Performances Of Congeneric Temperate And Boreal Herbaceous Plant Species And Their Associations With Soil Biota", "description": "Aims Climate warming raises the probability of range expansions of warm-adapted temperate species into areas currently dominated by cold-adapted boreal species. Warming-induced plant range expansions could partly depend on how warming modifies relationships with soil biota that promote plant growth, such as by mineralizing nutrients. Here, we grew two pairs of congeneric herbaceous plants species together in soil with a 5-year warming history (ambient, +1.7\u00b0C, +3.4\u00b0C) and related their performances to plant-beneficial soil biota. Methods Each plant pair belonged to either the mid-latitude temperate climate or the higher latitude southern boreal climate. Warmed soils were extracted from a chamberless heating experiment at two field sites in the temperate-boreal ecotone of North America. To isolate potential effects of different soil warming histories, air temperature for the greenhouse experiment was identical across soils. We hypothesized that soil with a 5-year warming history in the field would enhance the performance of temperate plant species more than boreal plant species and expected improved plant performances to have positive associations with plant growth-promoting soil biota (microbial-feeding nematodes and arbuscular mycorrhizal fungi). Important Findings Our main hypothesis was partly confirmed as only one temperate species performed better in soil with warming history than in soil with history of ambient temperature. Further, this effect was restricted to the site with higher soil water content in the growing season of the sampling year (prior to soil collection). One of the boreal species performed consistently worse in previously warmed soil, whereas the other species showed neutral responses to soil warming history. We found a positive correlation between the density of microbial-feeding nematodes and the performance of one of the temperate species in previously wetter soils, but this correlation was negative at the site with previously drier soil. We found no significant correlations between the ...", "keywords": ["Aster cordifolius", "0106 biological sciences", "ecotone", "seedling emergence", "XXXXXX - Unknown", "ecotones", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "seeds", "biotic communities", "01 natural sciences", "soil biota", "range shift"]}, "links": [{"href": "https://doi.org/10.1093/jpe/rtw066"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Plant%20Ecology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1093/jpe/rtw066", "name": "item", "description": "10.1093/jpe/rtw066", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1093/jpe/rtw066"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2016-06-28T00:00:00Z"}}, {"id": "10.1890/12-1760.1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:18:40Z", "type": "Journal Article", "created": "2013-07-09", "title": "Earthworm Effects On The Incorporation Of Litter C And N Into Soil Organic Matter In A Sugar Maple Forest", "description": "<p>To examine the mechanisms of earthworm effects on forest soil C and N, we double\uffe2\uff80\uff90labeled leaf litter with13C and15N, applied it to sugar maple forest plots with and without earthworms, and traced isotopes into soil pools. The experimental design included forest plots with different earthworm community composition (dominated byLumbricus terrestrisorL. rubellus). Soil carbon pools were 37% lower in earthworm\uffe2\uff80\uff90invaded plots largely because of the elimination of the forest floor horizons, and mineral soil C:N was lower in earthworm plots despite the mixing of high C:N organic matter into soil by earthworms. Litter disappearance over the first winter\uffe2\uff80\uff93spring was highest in theL. terrestris(T) plots, but during the warm season, rapid loss of litter was observed in bothL. rubellus(R) and T plots. After two years, 22.0% \uffc2\uffb1 5.4% of13C released from litter was recovered in soil with no significant differences among plots. Total recovery of added13C (decaying litter plus soil) was much higher in no\uffe2\uff80\uff90worm (NW) plots (61\uffe2\uff80\uff9368%) than in R and T plots (20\uffe2\uff80\uff9329%) as much of the litter remained in the former whereas it had disappeared in the latter. Much higher percentage recovery of15N than13C was observed, with significantly lower values for T than R and NW plots. Higher overwinter earthworm activity in T plots contributed to lower soil N recovery. In earthworm\uffe2\uff80\uff90invaded plots isotope enrichment was highest in macroaggregates and microaggregates whereas in NW plots silt plus clay fractions were most enriched. The net effect of litter mixing and priming of recalcitrant soil organic matter (SOM), stabilization of SOM in soil aggregates, and alteration of the soil microbial community by earthworm activity results in loss of SOM and lowering of the C:N ratio. We suggest that earthworm stoichiometry plays a fundamental role in regulating C and N dynamics of forest SOM.</p>", "keywords": ["Time Factors", "Nitrogen", "TEMPERATE HARDWOOD FOREST", "New York", "Acer", "C:N ratio", "Trees", "OLD-GROWTH FOREST", "Soil", "litter", "EXOTIC EARTHWORMS", "Animals", "NORTHEASTERN FORESTS", "Oligochaeta", "CARBON DYNAMICS", "Ecosystem", "2. Zero hunger", "decomposition", "NITROGEN DEPOSITION", "Ecology", "Lumbricus", "MICROBIAL BIOMASS", "04 agricultural and veterinary sciences", "15. Life on land", "DECIDUOUS FOREST", "Carbon", "stoichiometry", "aggregate", "0401 agriculture", " forestry", " and fisheries", "LUMBRICUS-TERRESTRIS", "Environmental Sciences", "CENTRAL NEW-YORK", "Environmental Monitoring"]}, "links": [{"href": "https://doi.org/10.1890/12-1760.1"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Ecological%20Applications", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1890/12-1760.1", "name": "item", "description": "10.1890/12-1760.1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1890/12-1760.1"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2013-07-01T00:00:00Z"}}, {"id": "10.3389/fenvs.2020.591695", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:19:14Z", "type": "Journal Article", "created": "2020-12-09", "title": "Assessment of Soil Functions: An Example of Meeting Competing National and International Obligations by Harnessing Regional Differences", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>The increased demand for bio based products worldwide provides an opportunity for Eastern European countries to increase their production in agriculture and forestry. At the same time, such economic development must be congruent with the European Union\u2019s long-term climate and biodiversity objectives. As a country that is rich in bioresources, the Latvian case study is highly relevant to many other countries\u2014especially those in Central and Eastern Europe\u2014and faces a choice of transition pathways to meet both economic and environmental objectives. In order to assess the trade-offs between investments in the bioeconomy and the achievement of climate and biodiversity objectives, we used the Functional Land Management (FLM) framework for the quantification of the supply and demand for the primary productivity, carbon regulation and biodiversity functions. We related the supply of these three soil functions to combinations of land use and soil characteristics. The demand for the same functions were derived from European, national and regional policy objectives. Our results showed different spatial scales at which variation in demand and supply is manifested. High demand for biodiversity was associated with areas dominated by agricultural land at the local scale, while regional differences of unemployment rates and the target for GDP increases framed the demand for primary productivity. National demand for carbon regulation focused on areas dominated by forests on organic soils. We subsequently identified mismatches between the supply and demand for soil functions, and we selected spatial locations for specific land use changes and improvements in management practices to promote sustainable development of the bio-economy. Our results offer guidance to policy makers that will help them to form a national policy that will underpin management practices that are effective and tailored toward local climate conditions and national implementation pathways.</p></article>", "keywords": ["2. Zero hunger", "functional land management", "forestry", "1. No poverty", "04 agricultural and veterinary sciences", "soil functions", "15. Life on land", "central and Eastern European countries", "climate regulation", "12. Responsible consumption", "Environmental sciences", "primary productivity", "13. Climate action", "8. Economic growth", "11. Sustainability", "0401 agriculture", " forestry", " and fisheries", "GE1-350", "agriculture", "biodiversity"]}, "links": [{"href": "https://doi.org/10.3389/fenvs.2020.591695"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Frontiers%20in%20Environmental%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3389/fenvs.2020.591695", "name": "item", "description": "10.3389/fenvs.2020.591695", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3389/fenvs.2020.591695"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-12-09T00:00:00Z"}}, {"id": "10.1080/02571862.2005.10634705", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:17:07Z", "type": "Journal Article", "created": "2013-01-15", "title": "Ecosystem Carbon Storage Under Different Land Uses In Three Semi-Arid Shrublands And A Mesic Grassland In South Africa", "description": "Carbon (C) storage in biomass and soils is a function of climate, vegetation type, soil type and land management. Carbon storage was examined in intact indigenous vegetation and under different land uses in thicket (250\u2013400 mm mean annual precipitation), xeric shrubland (350 mm), karoo (250 mm), and grassland (900\u20131200 mm). Carbon storage was as follows: (i) mean soil C (0\u201350 cm): thicket (T) = grassland (G) > xeric shrubland on Dwyka sediments (XS) > xeric shrubland on dolerite (XSD) > karoo (K) (168, 164, 65, 34 & 26 t ha\u22121, respectively); (ii) mean root C: T > G > XS = XSD (25.4, 11.4, 7.2 & 7.1 t ha\u22121); (iii) mean above-ground C including leaf litter: T>XS>G>K> XSD (51.6, 12.9, 2.0, 1.7 & 1.51 ha\u22121). Carbon stocks in intact indigenous vegetation were related more to woodiness of vegetation and frequency of fire than to climate. Biomass C was greatest in woody thicket and soil C stocks were greatest in thicket and grassland. Total C storage of 245 t ha\u22129 in thicket is exceptionally high for a semi-arid...", "keywords": ["580", "2. Zero hunger", "biomass", "Sub-Saharan Africa", "Eastern Hemisphere", "World", "land management", "land use", "04 agricultural and veterinary sciences", "15. Life on land", "South Africa", "carbon cycle", "Africa", "0401 agriculture", " forestry", " and fisheries", "Arida", "Southern Africa"]}, "links": [{"href": "https://doi.org/10.1080/02571862.2005.10634705"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/South%20African%20Journal%20of%20Plant%20and%20Soil", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1080/02571862.2005.10634705", "name": "item", "description": "10.1080/02571862.2005.10634705", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1080/02571862.2005.10634705"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2005-01-01T00:00:00Z"}}, {"id": "10.1080/03066150.2010.512460", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:17:08Z", "type": "Journal Article", "created": "2010-09-24", "title": "Processes Of Inclusion And Adverse Incorporation: Oil Palm And Agrarian Change In Sumatra, Indonesia", "description": "Changes in globalised agriculture raise critical questions as rapid agricultural development leads to widespread social and environmental transformation. With increased global demand for vegetable oils and biofuel, in Indonesia the area under oil palm has doubled over the last decade. This paper presents a case study of how micro-processes that are linked to wider dynamics shape oil palm related agrarian change in villages in Sumatra, Indonesia. It pursues related questions regarding the impact of agribusiness-driven agriculture, the fate of smallholders experiencing contemporary agrarian transition, and the impact of increased demand for vegetable oils and biofuels on agrarian structures in Sumatra. It argues that the paths of agrarian change are highly uneven and depend on how changing livelihood strategies are enabled or constrained by economic, social and political relations that vary over time and space. In contrast to simplifying narratives of inclusion/exclusion, it argues that outcomes depend on the terms under which smallholders engage with oil palm. Distinguishing between exogenous processes of agribusiness expansion and endogenous commodity market expansion, it finds each is associated with characteristic processes of change. It concludes that the way successive policy interventions have worked with the specific characteristics of oil palm have cumulatively shaped the space where agrarian change occurs in Sumatra.", "keywords": ["Crops", " Agricultural", "commodity market", "Economics", "eth Adverse incorporation", "smallholder", "0211 other engineering and technologies", "02 engineering and technology", "History", " 21st Century", "agricultural development", "strategic approach", "Social differentiation", "11. Sustainability", "agricultural policy", "Plant Oils", "crop", "demand analysis", "Social Change", "Asia", " Southeastern", "agriculture", "2. Zero hunger", "education", "article", "1. No poverty", "Agriculture", "Keywords: biofuel", "economics", "History", " 20th Century", "15. Life on land", "Southeast Asia", "socioeconomic impact", "Commodity markets", "agrarian change", "vegetable oil", "Indonesia", "13. Climate action", "Biofuels", "Oil palm", "biofuel"], "contacts": [{"organization": "McCarthy, John", "roles": ["creator"]}]}, "links": [{"href": "https://openresearch-repository.anu.edu.au/bitstream/1885/53926/5/processes_of_mccarthy_2010.pdf.jpg"}, {"href": "https://openresearch-repository.anu.edu.au/bitstream/1885/53926/7/01_McCarthy_Processes_of_inclusion_and_2010.pdf.jpg"}, {"href": "https://doi.org/10.1080/03066150.2010.512460"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/The%20Journal%20of%20Peasant%20Studies", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1080/03066150.2010.512460", "name": "item", "description": "10.1080/03066150.2010.512460", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1080/03066150.2010.512460"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2010-09-23T00:00:00Z"}}, {"id": "10.1098/rstb.2007.0031", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:17:21Z", "type": "Journal Article", "created": "2008-02-16", "title": "Drought Effects On Litterfall, Wood Production And Belowground Carbon Cycling In An Amazon Forest: Results Of A Throughfall Reduction Experiment", "description": "<p>             The Amazon Basin experiences severe droughts that may become more common in the future. Little is known of the effects of such droughts on Amazon forest productivity and carbon allocation. We tested the prediction that severe drought decreases litterfall and wood production but potentially has multiple cancelling effects on belowground production within a 7-year partial throughfall exclusion experiment. We simulated an approximately 35\uffe2\uff80\uff9341% reduction in effective rainfall from 2000 through 2004 in a 1\uffe2\uff80\uff8aha plot and compared forest response with a similar control plot. Wood production was the most sensitive component of above-ground net primary productivity (ANPP) to drought, declining by 13% the first year and up to 62% thereafter. Litterfall declined only in the third year of drought, with a maximum difference of 23% below the control plot. Soil CO             2             efflux and its             14             C signature showed no significant treatment response, suggesting similar amounts and sources of belowground production. ANPP was similar between plots in 2000 and declined to a low of 41% below the control plot during the subsequent treatment years, rebounding to only a 10% difference during the first post-treatment year. Live aboveground carbon declined by 32.5\uffe2\uff80\uff8aMg\uffe2\uff80\uff8aha             \uffe2\uff88\uff921             through the effects of drought on ANPP and tree mortality. Results of this unreplicated, long-term, large-scale ecosystem manipulation experiment demonstrate that multi-year severe drought can substantially reduce Amazon forest carbon stocks.           </p>", "keywords": ["0106 biological sciences", "Time Factors", "wood production", "above-ground net primary productivity", "drought", "Medical and Health Sciences", "01 natural sciences", "Trees", "Disasters", "Soil", "Amazon", "litterfall", "global change", "Ecosystem", "2. Zero hunger", "Evolutionary Biology", "Tropical Climate", "Water", "Biological Sciences", "Carbon Dioxide", "15. Life on land", "Wood", "Carbon", "6. Clean water", "13. Climate action", "Research Article"]}, "links": [{"href": "https://escholarship.org/content/qt1b27s752/qt1b27s752.pdf"}, {"href": "https://doi.org/10.1098/rstb.2007.0031"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Philosophical%20Transactions%20of%20the%20Royal%20Society%20B%3A%20Biological%20Sciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1098/rstb.2007.0031", "name": "item", "description": "10.1098/rstb.2007.0031", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1098/rstb.2007.0031"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2008-02-11T00:00:00Z"}}, {"id": "10.1111/gcb.12126", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:17:32Z", "type": "Journal Article", "created": "2012-12-22", "title": "Winter Climate Change And Coastal Wetland Foundation Species: Salt Marshes Vs. Mangrove Forests In The Southeastern United States", "description": "Abstract<p>We live in an era of unprecedented ecological change in which ecologists and natural resource managers are increasingly challenged to anticipate and prepare for the ecological effects of future global change. In this study, we investigated the potential effect of winter climate change upon salt marsh and mangrove forest foundation species in the southeastern United States. Our research addresses the following three questions: (1) What is the relationship between winter climate and the presence and abundance of mangrove forests relative to salt marshes; (2) How vulnerable are salt marshes to winter climate change\uffe2\uff80\uff90induced mangrove forest range expansion; and (3) What is the potential future distribution and relative abundance of mangrove forests under alternative winter climate change scenarios? We developed simple winter climate\uffe2\uff80\uff90based models to predict mangrove forest distribution and relative abundance using observed winter temperature data (1970\uffe2\uff80\uff932000) and mangrove forest and salt marsh habitat data. Our results identify winter climate thresholds for salt marsh\uffe2\uff80\uff93mangrove forest interactions and highlight coastal areas in the southeastern United States (e.g., Texas, Louisiana, and parts of Florida) where relatively small changes in the intensity and frequency of extreme winter events could cause relatively dramatic landscape\uffe2\uff80\uff90scale ecosystem structural and functional change in the form of poleward mangrove forest migration and salt marsh displacement. The ecological implications of these marsh\uffe2\uff80\uff90to\uffe2\uff80\uff90mangrove forest conversions are poorly understood, but would likely include changes for associated fish and wildlife populations and for the supply of some ecosystem goods and services.</p>", "keywords": ["0106 biological sciences", "Conservation of Natural Resources", "13. Climate action", "Climate Change", "Wetlands", "Seasons", "14. Life underwater", "15. Life on land", "01 natural sciences", "Southeastern United States"]}, "links": [{"href": "https://doi.org/10.1111/gcb.12126"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Change%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/gcb.12126", "name": "item", "description": "10.1111/gcb.12126", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcb.12126"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2013-02-11T00:00:00Z"}}, {"id": "10.1111/gcb.70247", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:17:36Z", "type": "Journal Article", "created": "2025-05-23", "title": "Carbon Emissions From Fires in Eastern Siberian Larch Forests", "description": "ABSTRACT<p>Siberian boreal forests have experienced increases in fire extent and intensity in recent years, which may threaten their role as carbon (C) sinks. Larch forests (Larix spp.) cover approximately 2.6 million km2 across Siberia, yet little is known about the magnitude and drivers of carbon combustion in these ecosystems. To address the paucity of field\uffe2\uff80\uff90based estimates of fuel load and consumption in Siberian larch forests, we sampled 41 burned plots, one to two years after fire, in Cajander larch (Larix cajanderi) forests in the Republic of Sakha (Yakutia), Russia. We estimated pre\uffe2\uff80\uff90fire carbon stocks and combustion with the objective of identifying the main drivers of carbon emissions. Pre\uffe2\uff80\uff90fire aboveground (trees and woody debris) and belowground carbon stocks at our study plots were 3.12\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff891.26\uffe2\uff80\uff89kg C m\uffe2\uff88\uff922 (mean\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff89standard deviation) and 3.50\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff890.93\uffe2\uff80\uff89kg C m\uffe2\uff88\uff922. We found that combustion averaged 3.20\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff890.75\uffe2\uff80\uff89kg C m\uffe2\uff88\uff922, of which 78% (2.49\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff890.56\uffe2\uff80\uff89kg C m\uffe2\uff88\uff922) stemmed from organic soil layers. These results suggest that severe fires in Cajander larch forests can result in combustion rates comparable to those observed in North American boreal forests and exceeding those previously reported for other forest types and burning conditions in Siberia. Carbon combustion was driven by both fire weather conditions and landscape variables, with pre\uffe2\uff80\uff90fire organic soil depth being the strongest predictor across our plots. Our study highlights the need to better account for Siberian larch forest fires and their impact on the carbon balance, especially given the expected climate\uffe2\uff80\uff90induced increase in fire extent and severity in this region.</p", "keywords": ["Larix cajanderi", "[SDU.OCEAN] Sciences of the Universe [physics]/Ocean", " Atmosphere", "eastern Siberia", "boreal forest carbon combustion climate change eastern Siberia fire severity larch forests Larix cajanderi", "Larix", "Forests", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "larch forests", "Fires", "Carbon", "Wildfires", "Siberia", "climate change", "fire severity", "carbon combustion", "boreal forest", "Research Article"], "contacts": [{"organization": "Delcourt, Clement, Rogers, Brendan, Akhmetzyanov, Linar, Izbicki, Brian, Scholten, Rebecca, Shestakova, Tatiana, van Wees, Dave, Mack, Michelle, Sass\u2010klaassen, Ute, Veraverbeke, Sander,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1111/gcb.70247"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Change%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/gcb.70247", "name": "item", "description": "10.1111/gcb.70247", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcb.70247"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-05-01T00:00:00Z"}}, {"id": "10.1111/j.1365-2389.2008.01059.x", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:17:38Z", "type": "Journal Article", "created": "2008-08-27", "title": "Influence Of Land Use (Savanna, Pasture,Eucalyptusplantations) On Soil Carbon And Nitrogen Stocks In Brazil", "description": "Summary<p>In Brazil, mostEucalyptusstands have been planted on Cerrado (shrubby savanna) or on Cerrado converted into pasture. Case studies are needed to assess the effect of such land use changes on soil fertility and C sequestration. In this study, the influence of Cerrado land development (pasture andEucalyptusplantations) on soil organic carbon (SOC) and nitrogen (SON) stocks were quantified in southern Brazil. Two contrasted silvicultural practices were also compared: 60\uffe2\uff80\uff83years of short\uffe2\uff80\uff90rotation silviculture (EUCSR) versus 60\uffe2\uff80\uff83years of continuous growth (EUCHF). C and N soil concentrations and bulk densities were measured and modelled for each vegetation type, and SOC and SON stocks were calculated down to a depth of 1\uffe2\uff80\uff83m by a continuous function.</p><p>Changes in SOC and SON stocks mainly occurred in the forest floor (no litter in pasture and up to 0.87\uffe2\uff80\uff83kg C\uffe2\uff80\uff83m\uffe2\uff88\uff922and 0.01\uffe2\uff80\uff83kg N\uffe2\uff80\uff83m\uffe2\uff88\uff922in EUCSR) and upper soil horizons. C and N stocks and their confidence intervals were greatly influenced by the methodology used to compute these layers. C/N ratio and13C analysis showed that down to a depth of 30\uffe2\uff80\uff83cm, the Cerrado organic matter was replaced by organic matter from newly introduced vegetation by as much as 75\uffe2\uff80\uff93100% for pasture and about 50% for EUCHF, poorer in N forEucalyptusstands (C/N larger than 18 forEucalyptusstands). Under pasture, 0\uffe2\uff80\uff9330\uffe2\uff80\uff83cm SON stocks (0.25\uffe2\uff80\uff83kg N\uffe2\uff80\uff83m\uffe2\uff88\uff922) were between 10 and 20% greater than those of the Cerrado (0.21\uffe2\uff80\uff83kg N\uffe2\uff80\uff83m\uffe2\uff88\uff922), partly due to soil compaction (limit bulk density at soil surface from 1.23 for the Cerrado to 1.34 for pasture). Land development on the Cerrado increased SOC stocks in the 0\uffe2\uff80\uff9330\uffe2\uff80\uff83cm layer by between 15 and 25% (from 2.99 (Cerrado) to 3.86 (EUCSR)\uffe2\uff80\uff83kg C\uffe2\uff80\uff83m\uffe2\uff88\uff922). When including litter layers, total 0\uffe2\uff80\uff9330\uffe2\uff80\uff83cm carbon stocks increased by 35% for EUCHF(4.50\uffe2\uff80\uff83kg C\uffe2\uff80\uff83m\uffe2\uff88\uff922) and 53% for EUCSR(5.08\uffe2\uff80\uff83kg C\uffe2\uff80\uff83m\uffe2\uff88\uff922), compared with the Cerrado (3.28\uffe2\uff80\uff83kg C\uffe2\uff80\uff83m\uffe2\uff88\uff922), independently of soil compaction.</p>", "keywords": ["P33 - Chimie et physique du sol", "sol", "http://aims.fao.org/aos/agrovoc/c_24420", "http://aims.fao.org/aos/agrovoc/c_7071", "http://aims.fao.org/aos/agrovoc/c_5192", "STOCKS ET FLUX", "stockage", "[SDV.SA.SDS]Life Sciences [q-bio]/Agricultural sciences/Soil study", "910", "ORGANIC-MATTER DYNAMICS", "utilisation des terres", "p\u00e2turages", "http://aims.fao.org/aos/agrovoc/c_7427", "MANAGEMENT", "http://aims.fao.org/aos/agrovoc/c_5626", "savane", "http://aims.fao.org/aos/agrovoc/c_1301", "[SDV.SA.SDS] Life Sciences [q-bio]/Agricultural sciences/Soil study", "http://aims.fao.org/aos/agrovoc/c_35657", "azote", "2. Zero hunger", "Eucalyptus", "340", "CONGO", "04 agricultural and veterinary sciences", "15. Life on land", "FOREST", "sylviculture", "K10 - Production foresti\u00e8re", "TREE PLANTATIONS", "CONVERSION", "http://aims.fao.org/aos/agrovoc/c_1070", "13. Climate action", "http://aims.fao.org/aos/agrovoc/c_4182", "AFFORESTATION", "http://aims.fao.org/aos/agrovoc/c_6825", "0401 agriculture", " forestry", " and fisheries", "EASTERN AUSTRALIA", "P01 - Conservation de la nature et ressources fonci\u00e8res", "carbone", "impact sur l'environnement", "plantations", "http://aims.fao.org/aos/agrovoc/c_7156", "http://aims.fao.org/aos/agrovoc/c_5990", "LEAF-LITTER", "STORAGE", "mati\u00e8re organique du sol", "http://aims.fao.org/aos/agrovoc/c_2683"]}, "links": [{"href": "https://doi.org/10.1111/j.1365-2389.2008.01059.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": "10.1111/j.1365-2389.2008.01059.x", "name": "item", "description": "10.1111/j.1365-2389.2008.01059.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/j.1365-2389.2008.01059.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2008-09-15T00:00:00Z"}}, {"id": "10.1111/j.1438-8677.2010.00321.x", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:17:45Z", "type": "Journal Article", "created": "2010-03-02", "title": "Low Rainfall-Induced Shift In Leaf Trait Relationship Within Species Along A Semi-Arid Sandy Land Transect In Northern China", "description": "Abstract<p>It is unclear whether the shift in leaf traits between species of high\uffe2\uff80\uff90 and low\uffe2\uff80\uff90rainfall sites is caused by low rainfall or by species replacement, because leaf traits vary substantially among species and sites. Our objective was to test if the within\uffe2\uff80\uff90species relationship between specific leaf area (SLA) and leaf N concentration (Nmass) shifts across a rainfall gradient in the semi\uffe2\uff80\uff90arid sandy lands of northern China. Data for SLA and Nmass of dominant species and related canopy and soil variables were collected from 33 plots along a rainfall transect (270\uffe2\uff80\uff93390\uffe2\uff80\uff83mm) having similar temperatures in the Mu Us, Inner Mongolia. We further investigated the generality of Mu Us data using 12 additional plots in the southeastern Qaidam Basin, Qinghai. Artemisia ordosica is a widespread species in both regions. Across and within species, the positive SLA\uffe2\uff80\uff93Nmass relationship shifted between two plant groups in the lowest rainfall plots (270\uffe2\uff80\uff83mm) and other higher rainfall plots (320\uffe2\uff80\uff93390\uffe2\uff80\uff83mm), which was confirmed by additional data from Qinghai. For A.\uffc2\uffa0ordosica populations, leaf area index (LAI) decreased and Nmass increased with decreasing rainfall, while the foliage N pool and SLA varied little. Rainfall was the limiting factor that determined variations in Nmass and LAI. Accordingly, Nmass/SLA ratios continually increased with decreasing LAI along the rainfall gradient (r\uffe2\uff80\uff83=\uffe2\uff80\uff83\uffe2\uff88\uff920.76, P\uffe2\uff80\uff83&lt;\uffe2\uff80\uff830.001). Results indicate a low rainfall\uffe2\uff80\uff90induced shift in the SLA\uffe2\uff80\uff93Nmass relationship associated with changes in LAI and foliage N pool, suggesting a link between leaf characteristics and ecosystem function.</p>", "keywords": ["0301 basic medicine", "Plant Leaves", "0106 biological sciences", "0303 health sciences", "03 medical and health sciences", "China", "Rain", "Adaptation", " Biological", "15. Life on land", "Asteraceae", "01 natural sciences", "Ecosystem"], "contacts": [{"organization": "Haixia Wei, Tianxiang Luo, W. Yang, B. Wu,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1111/j.1438-8677.2010.00321.x"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Plant%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/j.1438-8677.2010.00321.x", "name": "item", "description": "10.1111/j.1438-8677.2010.00321.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/j.1438-8677.2010.00321.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2010-12-10T00:00:00Z"}}, {"id": "10.1890/06-2113.1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:18:38Z", "type": "Journal Article", "created": "2007-12-12", "title": "Effects Of Restoration And Reflooding On Soil Denitrification In A Leveed Midwestern Floodplain", "description": "<p>River floodplains have the potential to remove nitrate from water through denitrification, the anaerobic microbial conversion of nitrate to nitrogen gas. An important factor in this process is the interaction of river water with floodplain soil; however, many rivers have been disconnected from their historic floodplains by levees. To test the effect of reflooding a degraded floodplain on nitrate removal, we studied changes in soil denitrification rates on the Baraboo River floodplain in Wisconsin, USA, as it underwent restoration. Prior to this study, the site had been leveed, drained, and farmed for more than 50 years. In late fall 2002, the field drainage system was removed, and a gate structure was installed to allow controlled flooding of this site with river water. Soil moisture was extremely variable among zones and months and reflected local weather. Soil organic matter was stable over the study period with differences occurring along the elevation gradient. High soil nitrate concentrations occurred in dry, relatively organic\uffe2\uff80\uff90poor soil samples and, conversely, all samples with high moisture soils characterized by low nitrate. We measured denitrification in static cores and potential denitrification in bulk samples amended with carbon and nitrogen, one year before and two years following the manipulation. Denitrification rates showed high temporal and spatial variability. Static core rates of individual sites ranged widely (from 0.00 to 16.7 \uffce\uffbcg N2O\uffe2\uff80\uff90N\uffc2\uffb7[kg soil]\uffe2\uff88\uff921\uffc2\uffb7h\uffe2\uff88\uff921, mean \uffc2\uffb1 SD = 1.10 \uffc2\uffb1 3.02), and denitrification enzyme activity (DEA) rates were similar with a slightly higher mean (from 0.00 to 15.0 \uffce\uffbcg N2O\uffe2\uff80\uff90N\uffc2\uffb7[kg soil]\uffe2\uff88\uff921\uffc2\uffb7h\uffe2\uff88\uff921, 1.41 \uffc2\uffb1 1.98). Denitrification was not well\uffe2\uff80\uff90correlated with soil nitrate, organic matter content, or moisture levels, the three parameters typically thought to control denitrification. Static core denitrification rates were not significantly different across years, and DEA rates decreased slightly the second year after restoration. These results demonstrate that restored agricultural soil has the potential for denitrification, but that floodplain restoration did not immediately improve this potential. Future floodplain restorations should be designed to test alternative methods of increasing denitrification.</p>", "keywords": ["floodplain", "2. Zero hunger", "Conservation of Natural Resources", "Time Factors", "Nitrogen", "riparian", "Water", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "nitrogen", "wetland", "6. Clean water", "Midwestern United States", "Disasters", "Soil", "soil denitrification", "0401 agriculture", " forestry", " and fisheries", "river restoration", "Environmental Sciences", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1890/06-2113.1"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Ecological%20Applications", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1890/06-2113.1", "name": "item", "description": "10.1890/06-2113.1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1890/06-2113.1"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2007-12-01T00:00:00Z"}}, {"id": "10.17171/1-9-328", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:18:33Z", "type": "Dataset", "title": "MM.hr:08", "keywords": ["Ancient Near Eastern Studies"], "contacts": [{"organization": "Dr. Joanne Rowland,  Dr. Geoffrey Tassie,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.17171/1-9-328"}, {"rel": "self", "type": "application/geo+json", "title": "10.17171/1-9-328", "name": "item", "description": "10.17171/1-9-328", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.17171/1-9-328"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-01-01T00:00:00Z"}}, {"id": "10.3389/fevo.2021.619215", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:19:15Z", "type": "Journal Article", "created": "2021-03-16", "title": "Ant Communities Resist Even in Small and Isolated Gypsum Habitat Remnants in a Mediterranean Agroecosystem", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Natural and seminatural habitat remnants play a crucial ecological role in intensified agroecosystems. Assumptions on the conservation value of small and poorly connected fragments in a hostile matrix come from generalization obtained from a limited number of taxa, mostly plants, and vertebrates. To date, few studies have analyzed the effect of fragmentation on ant communities in Mediterranean agroecosystems, despite the importance of this group of animals on several key ecosystem functions and services. Here, we analyze the effects of fragment area and connectivity on ant communities in gypsum outcrops in a large cereal agroecosystem of Central Spain. Ant communities were described by their species composition, abundance (total number of occurrences), and number of species, standardized both by area (species density), and abundance (species richness). Observed number of species was relatively high in comparison with other studies in the Mediterranean, and we found no effects of fragment characteristics on species density, species richness and species composition, which implies that even small and isolated patches do have a value for ant conservation. Moreover, total number of occurrences were higher for smaller and more isolated fragments. This finding contrasts with the results reported for other taxa in similar gypsum habitats and suggests that certain ant traits and strategies make them particularly resistant to fragmentation and capable to take advantage of small habitat patches. Given the important ecological role played by ants, we recommend the preservation of these small habitat fragments in the management plans of agroecosystems in these drylands, especially in those cases in which intensification of agricultural practices greatly diminish natural habitat availability.</p></article>", "keywords": ["0106 biological sciences", "2. Zero hunger", "drylands", "agroecosystems", "gypsum habitats", "Ecology", "Evolution", "Ants", "ants", "Biodiversity", "15. Life on land", "Biolog\u00eda y Biomedicina / Biolog\u00eda", "01 natural sciences", "13. Climate action", "fragmentation", "QH359-425", "biodiversity conservation", "Crematogaster", "14. Life underwater", "QH540-549.5"]}, "links": [{"href": "https://doi.org/10.3389/fevo.2021.619215"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Frontiers%20in%20Ecology%20and%20Evolution", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3389/fevo.2021.619215", "name": "item", "description": "10.3389/fevo.2021.619215", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3389/fevo.2021.619215"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-03-16T00:00:00Z"}}, {"id": "442c863e-1e52-4176-8a32-87ae3cac9ae7", "type": "Feature", "geometry": {"type": "Polygon", "coordinates": [[[6.6, 47.35], [6.6, 54.86], [14.62, 54.86], [14.62, 47.35], [6.6, 47.35]]]}, "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"}], "scheme": "Individual"}, {"concepts": [{"id": "Boden"}], "scheme": "GEMET - INSPIRE themes, version 1.0"}, {"concepts": [{"id": "Monitoring"}, {"id": "Kohlenstoff"}, {"id": "Stickstoff"}, {"id": "Humus"}, {"id": "Bodenfruchtbarkeit"}, {"id": "pH-Wert"}, {"id": "Carbonat"}, {"id": "Bodenprofil"}, {"id": "Probenahme"}, {"id": "Raster"}, {"id": "Ackerland"}, {"id": "Gr\u00fcnland"}], "scheme": "GEMET - Concepts, version 2.4"}, {"concepts": [{"id": "organisch"}, {"id": "Organische Bodensubstanz"}, {"id": "Lagerungsdichte"}, {"id": "Feinbodenvorrat"}, {"id": "Korngr\u00f6\u00dfenverteilung"}, {"id": "Karbonat"}, {"id": "Pedogene Oxide"}, {"id": "Bodenprofil"}, {"id": "Raster"}, {"id": "Acker"}, {"id": "Gr\u00fcnland"}, {"id": "Sonderkultur"}, {"id": "Landnutzung"}, {"id": "LULUCF"}, {"id": "organic"}, {"id": "organic matter"}, {"id": "soil fertility"}, {"id": "fine soil stock"}, {"id": "pedogenic oxides"}, {"id": "soil profile"}, {"id": "grid"}, {"id": "special permanent crop"}, {"id": "land use"}], "scheme": "Individual"}], "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 Th\u00fcnen Institute's research activities.\"\n\nAlthough every care has been taken in preparing and testing the data, the Th\u00fcnen Institute and the BonaRes Data Centre cannot guarantee that the data are correct; neither does the Th\u00fcnen Institute 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 Th\u00fcnen Institute and BonaRes Data Centre will not be responsible for any direct or indirect use which might be made of the data.", "updated": "2020-09-16", "type": "Dataset", "created": "2020-01-20", "language": "eng", "title": "First German Agricultural Soil Inventory \u2013 Core dataset: HORIZON DATA", "description": "The Federal Republic of Germany is obliged to report all anthropogenic sources and sinks of greenhouse gases on a national scale. Changes in soil organic carbon (SOC) stocks are among these sources and sinks. Furthermore, soil organic matter is a key indicator of soil fertility. The Th\u00fcnen Institute of Climate-Smart Agriculture was commissioned by the German Federal Ministry of Food and Agriculture to conduct the first German agricultural soil inventory and obtain a first representative and consistent baseline of SOC stocks in agricultural soils across Germany. Potential explanatory variables were also assessed. Between 2009 and 2018, a total of 3104 field sites were sampled in a 8x8 km grid (Jacobs et al., 2018). The dataset contains the key data (laboratory and field) of the first German agricultural soil inventory. It consists of three parts with associated readme-files, which explain the data: LABORATORY_DATA.xlsx: This file contains all relevant laboratory results. SITE.xlsx: This file contains the most important general information on the sampled sites. HORIZON_DATA.xlsx: This file contains the soil profile description as determined in the field with several key horizon parameters. In SITE.xlsx and HORIZON_DATA.xlsx, several parameters were determined using the German soil description guidelines (Ad-Hoc-Ag Boden, 2005) and are not explained here in detail. Single parameters, such as soil texture class or carbonate content class/ carbonate content are given in LABORATORY_DATA.xlsx and HORIZON_DATA.xlsx and can slightly deviate due to different methodologies (Estimation of soil scientist vs. laboratory analysis). Methodological details can be found in the Th\u00fcnen Report 64. References Ad-Hoc-Ag Boden (2005) Bodenkundliche Kartieranleitung. E.Schweizerbart'sche Verlagsbuchhandlung, Hannover. Jacobs, A., Flessa, H., Don, A., Heidkamp, A., Prietz, R., Dechow, R., Gensior, A., Poeplau, C., Riggers, C. & Schneider, F. (2018) Landwirtschaftlich genutzte B\u00f6den in Deutschland: Ergebnisse der Bodenzustandserhebung. Th\u00fcnen Report 64.\n\nResearch domain: Soil Sciences\n\nResearch question: What is the condition of agricultural soils in Germany, especially with regard to stocks of soil organic carbon?\n\nThis dataset is available in Open Agrar.", "keywords": ["Soil", "opendata", "Boden", "Monitoring", "Kohlenstoff", "Stickstoff", "Humus", "Bodenfruchtbarkeit", "pH-Wert", "Carbonat", "Bodenprofil", "Probenahme", "Raster", "Ackerland", "Gr\u00fcnland", "organisch", "Organische Bodensubstanz", "Lagerungsdichte", "Feinbodenvorrat", "Korngr\u00f6\u00dfenverteilung", "Karbonat", "Pedogene Oxide", "Bodenprofil", "Raster", "Acker", "Gr\u00fcnland", "Sonderkultur", "Landnutzung", "LULUCF", "organic", "organic matter", "soil fertility", "fine soil stock", "pedogenic oxides", "soil profile", "grid", "special permanent crop", "land use"], "contacts": [{"name": "Poeplau, Christopher", "organization": "Johann Heinrich von Th\u00fcnen-Institut", "position": "Scientist", "roles": ["author"], "phones": [{"value": "+49 531 596 2679"}], "emails": [{"value": "christopher.poeplau@thuenen.de"}], "addresses": [{"deliveryPoint": ["Bundesallee 68"], "city": "Braunschweig", "administrativeArea": "Niedersachsen", "postalCode": "38116", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Don, Axel", "organization": "Johann Heinrich von Th\u00fcnen-Institut", "position": "Scientist", "roles": ["author"], "phones": [{"value": "+49 531 596 2641"}], "emails": [{"value": "axel.don@thuenen.de"}], "addresses": [{"deliveryPoint": ["Bundesallee 68"], "city": "Braunschweig", "administrativeArea": "Niedersachsen", "postalCode": "38116", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Flessa, Heinz", "organization": "Johann Heinrich von Th\u00fcnen-Institut", "position": "Scientist", "roles": ["projectLeader"], "phones": [{"value": "+49 531 596 2601"}], "emails": [{"value": "heinz.flessa@thuenen.de"}], "addresses": [{"deliveryPoint": ["Bundesallee 65"], "city": "Braunschweig", "administrativeArea": "Niedersachsen", "postalCode": "38116", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Heidkamp, Arne", "organization": "Johann Heinrich von Th\u00fcnen-Institut", "position": "Scientist", "roles": ["author"], "phones": [{"value": "+49 531 596 2672"}], "emails": [{"value": "arne.heidkamp@thuenen.de"}], "addresses": [{"deliveryPoint": ["Bundesallee 35A"], "city": "Braunschweig", "administrativeArea": "Niedersachsen", "postalCode": "38116", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Jacobs, Anna", "organization": "Johann Heinrich von Th\u00fcnen-Institut", "position": "Scientist", "roles": ["author"], "phones": [{"value": "+49 531 596 1112"}], "emails": [{"value": "anna.jacobs@thuenen.de"}], "addresses": [{"deliveryPoint": ["Bundesallee 49"], "city": "Braunschweig", "administrativeArea": "Niedersachsen", "postalCode": "38116", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Prietz, Roland", "organization": "Johann Heinrich von Th\u00fcnen-Institut", "position": "Scientist", "roles": ["author"], "phones": [{"value": "+49 531 596 2714"}], "emails": [{"value": "roland.prietz@thuenen.de"}], "addresses": [{"deliveryPoint": ["Bundesallee 68"], "city": "Braunschweig", "administrativeArea": "Niedersachsen", "postalCode": "38116", "country": "Germany"}], "links": [{"href": null}]}, {"name": "OA", "organization": "Open Agrar Repositorium", "position": null, "roles": ["publisher"], "phones": [{"value": null}], "emails": [{"value": "IB@julius-kuehn.de"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": {"url": "https://www.re3data.org/", "protocol": null, "protocol_url": "", "name": "http://doi.org/10.17616/R3XF45", "name_url": "", "description": "re3data", "description_url": "", "applicationprofile": null, "applicationprofile_url": "", "function": null}}]}, {"organization": "Johann Heinrich von Th\u00fcnen-Institut", "roles": ["contributor"]}], "title_alternate": "BZE-LW"}, "links": [{"href": "https://doi.org/10.3220/DATA20200203151139", "rel": "download"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/e40d73fe-d5b8-408f-aadd-ca154cc63882", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "442c863e-1e52-4176-8a32-87ae3cac9ae7", "name": "item", "description": "442c863e-1e52-4176-8a32-87ae3cac9ae7", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/442c863e-1e52-4176-8a32-87ae3cac9ae7"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"interval": ["2009-01-01T00:00:00Z", "2018-12-31T00:00:00Z"]}}, {"id": "10.3389/feart.2020.00359", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:19:14Z", "type": "Journal Article", "created": "2020-10-26", "title": "On the Definition of the Strategy to Obtain Absolute InSAR Zenith Total Delay Maps for Meteorological Applications", "description": "Atmospheric Phase Screens (APSs) derived from Interferometric Synthetic Aperture Radar (InSAR) observations contain the difference between the tropospheric water-vapor-induced delay of two acquisition epochs, i.e., the slave and the master (or reference) epochs. Using estimates of the atmospheric state coming from independent sources, for example numerical models and/or Global Navigation Satellite System (GNSS) observations, the APSs can be transformed into absolute maps of Tropospheric Delay (Zenith Total Delay or ZTD), related to the columnar atmospheric water vapor content. In this work, a systematic comparison between various APS and ZTD products aims to determine a convenient strategy to go from APSs to InSAR-derived absolute ZTD maps, highlighting the uncertainties and approximations introduced in the entire processing. The main problem to solve is the evaluation of a sufficiently accurate high-resolution master delay map. Different sources of data and two different approaches to derive the master are validated and compared to define the most suitable strategy for meteorological applications. Maps of ZTD obtained by an iterative interpolation of a global atmospheric circulation model values results in being more suited than those derived from the assimilation of GNSS observations into an NWP model. A time average approach to estimate the master map is more robust than the single epoch approach with respect to the choice of the master epoch. Still, the choice of a proper master epoch in the InSAR processing chain as well as that of the maps to be averaged crucially result in the estimate of the master.", "keywords": ["ZTD", "Science", "Q", "0211 other engineering and technologies", "numerical weather prediction", "02 engineering and technology", "01 natural sciences", "master estimate", "GNSS meteorology", "13. Climate action", "water vapor", "APS; data assimilation; GNSS meteorology; master estimate; numerical weather prediction; SAR meteorology; water vapor; ZTD;", "SAR meteorology", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://boa.unimib.it/bitstream/10281/527752/2/feart-08-00359.pdf"}, {"href": "https://re.public.polimi.it/bitstream/11311/1158610/1/feart-08-00359.pdf"}, {"href": "https://doi.org/10.3389/feart.2020.00359"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Frontiers%20in%20Earth%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3389/feart.2020.00359", "name": "item", "description": "10.3389/feart.2020.00359", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3389/feart.2020.00359"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-10-26T00:00:00Z"}}, {"id": "10.3390/land12020388", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:19:25Z", "type": "Journal Article", "created": "2023-02-01", "title": "The Soils of Early Farmers and Their Neighbors in the Southern Buh Catchment (Ukraine): Micromorphology and Archaeological Context", "description": "<p>The problems regarding hunter-gatherer/early farmer interactions are quite an important topic in southeast European archaeology. According to the available data, the two economic subsistence systems have coexisted for some 2000 years during the 6th\uffe2\uff80\uff934th millennia cal BC (Telegin 1985; Lillie et al., 2001). In some areas, hunter-gatherer and early farmer sites are located just a few kilometers apart. The Southern Buh River valley has yielded evidence of Linear Pottery culture, early Trypillia and Trypillia B1 Neolithic settlements as well as hunter-gatherer sites with pottery attributable to the so-called sub-Neolithic or para-Neolithic (Haskevych et al., 2019; Kiosak et al., 2021). Trial-trenches have been opened within some of these sites, which have been radiocarbon-dated from Bern University laboratory (LARA). Soil samples for micromorphological analysis have been collected from these sites to interpret their paleogenetic formation. The soil development is attested since, at least, the beginning of the 5th mill BC, followed by the developed of chernozem soils, which was interrupted by an erosional episode in the end of 5th millennium BC. The available data show that the soils of early farmers arable as are the present day ones. The early farmers were able to exploit relatively heavy soils to cultivate wheat and barley as early as 5250\uffe2\uff80\uff935050 cal BC. In contrast, the sites of ceramic hunter-gatherers were often located on the soils which formed under wet conditions along seasonally flooded riverbanks, which were almost unsuitable for agricultural practices.</p>", "keywords": ["2. Zero hunger", "S", "radiocarbon dates", "Neolithization of eastern Europe", "Agriculture", "0601 history and archaeology", "06 humanities and the arts", "15. Life on land", "Ukraine", "paleopedogenesis", "Neolithization of eastern Europe; Ukraine; radiocarbon dates; soil micromorphology; paleopedogenesis", "soil micromorphology"]}, "links": [{"href": "http://www.mdpi.com/2073-445X/12/2/388/pdf"}, {"href": "https://iris.unive.it/bitstream/10278/5017342/1/land-12-00388%20%283%29.pdf"}, {"href": "https://www.mdpi.com/2073-445X/12/2/388/pdf"}, {"href": "https://doi.org/10.3390/land12020388"}, {"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/land12020388", "name": "item", "description": "10.3390/land12020388", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3390/land12020388"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-01-31T00:00:00Z"}}, {"id": "10.3390/molecules27092683", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-09-21T16:19:27Z", "type": "Journal Article", "created": "2022-04-24", "title": "Dating sediments by EPR using Al-h centre: a comparison be-tween the properties of fine (4-11 \u03bcm) and coarse (> 63 \u03bcm) quartz grains", "description": "<p>The possibility of EPR dating for sediments using Al-h signals of fine (4\uffe2\uff80\uff9311 \uffce\uffbcm) grains of quartz has not been previously discussed. Here, the Al-h and peroxy EPR spectra of fine (4\uffe2\uff80\uff9311 \uffce\uffbcm) and coarse (63\uffe2\uff80\uff9390, 125\uffe2\uff80\uff93180 \uffce\uffbcm) sedimentary quartz from thoroughly investigated loess sites in Eastern Europe were examined. By comparing experimental spectra with a simulated signal, we evaluated the overestimation observed when using the standard approach established by Toyoda and Falgu\uffc3\uffa8res to measure Al-h intensity for different doses of radiation, up to 40,000 Gy. This overestimation, caused by the presence of peroxy signals, was much more pronounced for fine grains. Fine grains exhibited some additional dose-dependent signals, which, for some samples, caused a complete distortion of the Al-h spectra at high doses, making it impossible to measure the standard amplitude. We propose a new approach to measuring Al-h signal intensity, focusing on the peak-to-baseline amplitude of the part of the signal at g \uffe2\uff89\uff88 2.0603, which is not affected by the peroxy signals and therefore has the potential of providing more accurate results. The shapes of dose response curves constructed for coarse and fine grains using the new approach show considerable similarity, suggesting that Al-h centre formation in fine and coarse grains upon artificial radiation at room temperature follows the same pattern.</p>", "keywords": ["dose response curve", "fine grains", "Electron Spin Resonance Spectroscopy", "Organic chemistry", "Quartz", "electron paramagnetic resonance (EPR); electron spin resonance (ESR); quartz; Al-h centre; fine grains; dose response curve", "quartz", "01 natural sciences", "Article", "electron paramagnetic resonance (EPR)", "QD241-441", "Al-h centre", "electron spin resonance (ESR)", "Europe", " Eastern", "0105 earth and related environmental sciences"]}, "links": [{"href": "http://www.mdpi.com/1420-3049/27/9/2683/pdf"}, {"href": "https://www.mdpi.com/1420-3049/27/9/2683/pdf"}, {"href": "https://doi.org/10.3390/molecules27092683"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Molecules", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3390/molecules27092683", "name": "item", "description": "10.3390/molecules27092683", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3390/molecules27092683"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-04-21T00:00:00Z"}}, {"id": "10.3832/ifor1605-008", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:19:36Z", "type": "Journal Article", "created": "2016-03-17", "title": "Post-fire soil hydrology, water erosion and restoration strategies in Andosols: a review of evidence from the Canary Islands (Spain)", "description": "Andosols are the most characteristic soils of volcanic regions such as the forested, fire-prone, hillslopes of the mountainous Canary Islands (Spain). Due to their volcanic nature, these soils have traditionally been considered highly resistant to water erosion processes in undisturbed conditions, but are also highly susceptible to environmental disturbances. In addition, volcanic terrains often underlie heavily-populated, steep areas where torrential rains are frequent, increasing the threat to the population and infrastructures down-slope. Numerous hydrological and erosional catastrophic events in disturbed Andosols in the Canary Islands and worldwide, leading to major losses to lives and properties, have been historically and recently reported. The impact of environmental alterations such as land use change on hydrological and erosional response of Andosols has been widely studied in the Canary Islands and worldwide. However, the effect on this soil type of wildfires, generally considered one of the main geomorphological agents, and historically connected to the forested fire-prone Andosols of the islands, has had scant attention to date. This review seeks to redress this knowledge gap by: (i) evaluating the factors affecting the susceptibility of Andosols to catastrophic hydrological and erosional events; (ii) summarizing the published studies on the impact of fire and the post-fire response of this soil type and the specific restoration measures developed to date; and (iii) identifying research gaps and suggesting new lines of investigation in order to reduce the hydrological and erosional risks in these particular terrains.", "keywords": ["Volcanic Ash Soils", "2. Zero hunger", "Disaster Risk Reduction", "Post-fire Restoration", "Forestry", "04 agricultural and veterinary sciences", "SD1-669.5", "15. Life on land", "Wildfires", "13. Climate action", "Erosion Mitigation", "11. Sustainability", "0401 agriculture", " forestry", " and fisheries", "Catastrophic Events"]}, "links": [{"href": "https://doi.org/10.3832/ifor1605-008"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/iForest%20-%20Biogeosciences%20and%20Forestry", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3832/ifor1605-008", "name": "item", "description": "10.3832/ifor1605-008", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3832/ifor1605-008"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2016-08-09T00:00:00Z"}}, {"id": "10.4039/tce.2018.21", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-09-21T16:19:38Z", "type": "Journal Article", "created": "2018-05-08", "title": "The genusXanthogrammaSchiner, 1861 (Diptera: Syrphidae) in southeastern Europe, with descriptions of two new species", "description": "Abstract<p>Examination of 122 specimens ofXanthogrammaSchiner, 1861 (Diptera: Syrphidae) from varied localities in Europe (+Turkey) resulted in the description of two new species (X. aeginaeRicarte, Nedeljkovi\uffc4\uff87, and Vuji\uffc4\uff87new speciesandX. pilosumNedeljkovi\uffc4\uff87, Ricarte, and Vuji\uffc4\uff87new species), as well as new data on six other species. Most of the examined material originated from the Balkan Peninsula and Greek islands. New species concepts were supported by morphological and molecular evidence. Relationships among the eight studied species were analysed and discussed based on the data of nuclear (ITS2) and mitochondrial (COI) genes sequences. An identification key to the European species ofXanthogrammais provided. Lectotypes are designated forDoros decoratumZetterstedt, 1843,Lasiophthicus novusRondani, 1857,Syrphus laetusFabricius, 1794,Syrphus ornatusMeigen, 1822, andXanthogramma nobilitatumFrey, 1946.</p", "keywords": ["0106 biological sciences", "2. Zero hunger", "Xanthogramma Schiner", "Southeastern Europe", "9. Industry and infrastructure", "Diptera", "Zoolog\u00eda", "Syrphidae", "15. Life on land", "01 natural sciences"]}, "links": [{"href": "https://doi.org/10.4039/tce.2018.21"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/The%20Canadian%20Entomologist", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.4039/tce.2018.21", "name": "item", "description": "10.4039/tce.2018.21", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.4039/tce.2018.21"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-05-08T00:00:00Z"}}, {"id": "10.5281/zenodo.1252987", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:20:21Z", "type": "Journal Article", "title": "The role of FM in disaster resilience: Integrating the Sendai Framework into disaster risk management", "description": "Conference paper presented at EFMC 2017, Madrid.", "keywords": ["13. Climate action", "Built Asset Management", "11. Sustainability", "1. No poverty", "Community Resilience", "Disaster Management", "Contingency Planning", "12. Responsible consumption", "Sendai Framework"], "contacts": [{"organization": "Jones, Keith, Bartolucci, Andrea, Hiscock, Katie,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5281/zenodo.1252987"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Research%20papers%20for%20EUROFM%2016th%20research%20symposium%20EFMC%202017", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.5281/zenodo.1252987", "name": "item", "description": "10.5281/zenodo.1252987", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5281/zenodo.1252987"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-01-01T00:00:00Z"}}, {"id": "10.5281/zenodo.14583868", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:20:39Z", "type": "Dataset", "title": "geoSABINA: Environmental variables", "description": "This dataset provides environmental variables from Spain, selected for their relevance in modeling the distribution of plant species. However, they can also be applied to other species and purposes. It includes a total of 103 raster layers in tif format at 250-meter resolution. The detailed list of layers available is provided in data_table_env_variables.csv, which includes information on the category, dataset, description, resolution, time period, and path.  This dataset includes:\u00a0\u00a0    \u00a0Climatic variables: 19 bioclimatic variables under current (1990-2010) and 4 future (2071-2100) climate scenarios. Climatic variables were sourced from the climatologies for the Earth\u2019s Land Surface Areas (CHELSA) and downscaled to 250 m in https://doi.org/10.1111/ecog.07328. The future scenarios were generated according two global climate models [the latest Institute Pierre Simon Laplace climate model (IPSL_CM6A_LR) and the Meteorological Research Institute Earth System Model version 2.0 (MRI_ESM2)] and two socio-economic pathways: an optimistic low greenhouse gas emissions scenario (SSP126) and a pessimistic high emissions scenario (SSP585). The climatic variables of each scenario are compressed within a zip file.  Edaphic variables: Four soil characteristics (pH, nitrogen, sand content, organic carbon) at 0 to 5 cm depth sourced from SoilGrids. The four edaphic variables are compressed within a zip file.  Hydrologic variables: Three hydrologic variables (distance to rivers, flow accumulation, and topographic index) derived from the digital elevation model DAT-193-en (Copernicus Land Cover Service)\u00a0in https://doi.org/10.1111/ecog.07328. \u00a0  Solar radiation:\u00a0\u00a0Annual solar exposure values calculated from the digital elevation model DAT-193-en \u00a0in https://doi.org/10.1111/ecog.07328.\u00a0   Raster information:    Resolution: 250 m  Extent: -75888.32, 1031611.68, 3977269.52, 4870519.52 (xmin, xmax, ymin, ymax)  CRS: WGS 84 / UTM Zone 30N (EPSG:32630)   References: The references in this list should be added to any publication using these data:    Goicolea, T., Morales-Barbero, J., Garc\u00eda-Vi\u00f1as, J.I, Gast\u00f3n, A., Aroca-Fern\u00e1ndez, M.J., Calleja, J.A., Moren, J.C. , Ramos-Guti\u00e9rrez, I., Rodr\u00edguez, M.A., Lima, H., Broennimann, O., Guisan, A, Adde, A., P\u00e9rez-Latorre, A.V., G. Mateo, R. (2025) Scientific Data.  Goicolea, T., Adde, A., Broennimann, O., Garc\u00eda-Vi\u00f1as, J.I., Gast\u00f3n, A., Aroca-Fern\u00e1ndez, M.J. et al. (2024). Spatially-Nested Hierarchical Species Distribution Models to Overcome Niche Truncation in National-Scale Studies. Ecography. https://doi.org/10.1111/ecog.07328", "keywords": ["hydrologic", "climate projections", "Spain", "solar radiation", "spatial data", "raster", "covariates", "edaphic", "climate", "environmental variables"], "contacts": [{"organization": "Goicolea, Teresa, Morales-Barbero, Jennifer, Mateo, Rub\u00e9n G.,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5281/zenodo.14583868"}, {"rel": "self", "type": "application/geo+json", "title": "10.5281/zenodo.14583868", "name": "item", "description": "10.5281/zenodo.14583868", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5281/zenodo.14583868"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-01-01T00:00:00Z"}}, {"id": "10.5281/zenodo.3049007", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:21:05Z", "type": "Journal Article", "title": "Cost-benefit analysis of liquefaction mitigation strategies", "description": "This paper presents a cost-benefit model as part of the options appraisal process to evaluate<br> alternative ground mitigation interventions to reduce vulnerability and/or improve resilience of<br> built assets to earthquake induced liquefaction disaster (EILD) events. The paper presents a review<br> of alternative approaches to cost-benefit analysis and develops forward looking (risk based) and<br> backward looking (impact based) cost-benefit models that can be used by practitioners and policy<br> makers to improve community resilience through better contingency and disaster management<br> planning. The paper customises the models against EILD scenarios and identifies the cost and benefit<br> attributes that need to be assessed if the models are to be effectively integrated into a resilience<br> assessment and improvement framework for improved community resilience to EILD events.", "keywords": ["community resilience", "liquefaction", "built asset management.", "disaster management", "cost-benefit modelling;", "ground mitigation", "contingency planning"], "contacts": [{"organization": "Keith Jones,, Morga, Mariantonietta, Nadeeshani Wanigarathna, Pascale, Federica,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5281/zenodo.3049007"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/IABSE%20Symposium%202019%20Guimaraes%20-%20Towards%20a%20Resilient%20Built%20Environment", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.5281/zenodo.3049007", "name": "item", "description": "10.5281/zenodo.3049007", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5281/zenodo.3049007"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-01-01T00:00:00Z"}}, {"id": "10.5281/zenodo.4384530", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:21:09Z", "type": "Dataset", "title": "Soil profile, climatic, physiographic, overstory and understory data in mixed and monospecific plots of Pinus sylvestris and Pinus pinaster in Spain", "description": "Open AccessThis dataset provides valuable environmental information about a triplets\u2019 essay of Scots pine and Maritime pine in Spain. The data characterizes the soil profile (physicochemical parameters of organic and mineral horizons), climate, physiography, understory and overstory. The essay, located in North-Central Spain, consists of eighteen forest plots divided in six triplets. Each triplet includes three circular plots of 15 m-radius located less than 1 km from each other: two monospecific plots dominated by <em>P. sylvestris</em> or <em>P. pinaster</em>, and one mixed plot of both species. In each plot, one pit up to 50 cm depth, one 15 m-radius overstory features inventory and ten understory 1x1 m inventories were carried out. Additionally, physiographic and climatic variables were collected per plot. The file contains information about the 215 environmental variables studied in the eighteen forest plots. Triplet: Triplet to which the plot belongs(1: Triplet 1; 2: Triplet 2; 3: Triplet 3; 4: Triplet 4; 5: Triplet 5; 6: Triplet 6). Stand_type: Type of stand (PS: monospecific stand of <em>Pinus sylvestris</em> L.; PP: monospecific stand of <em>Pinus pinaster</em> Ait.; MM: mixed stand of <em>Pinus sylvestris</em> L.and <em>Pinus pinaster</em> Ait.). Plot: Plot identification (PS01: monospecific stand of <em>Pinus sylvestris</em> L. of triplet 1; PS02: monospecific stand of <em>Pinus sylvestris</em> L. of triplet 2; PS03: monospecific stand of <em>Pinus sylvestris</em> L. of triplet 3; PS04: monospecific stand of <em>Pinus sylvestris</em> L. of triplet 4; PS05: monospecific stand of <em>Pinus sylvestris</em> L. of triplet 5; PS06: monospecific stand of <em>Pinus sylvestris</em> L. of triplet 6; MM01: mixed stand of <em>Pinus sylvestris</em> L.and <em>Pinus pinaster</em> Ait. of triplet 1; MM02: mixed stand of <em>Pinus sylvestris </em>L.and <em>Pinus pinaster</em> Ait. of triplet 2; MM03: mixed stand of <em>Pinus sylvestris</em> L.and <em>Pinus pinaster</em> Ait. of triplet 3; MM04: mixed stand of <em>Pinus sylvestris</em> L.and <em>Pinus pinaster</em> Ait. of triplet 4; MM05: mixed stand of <em>Pinus sylvestris </em>L.and <em>Pinus pinaster</em> Ait. of triplet 5; MM06: mixed stand of <em>Pinus sylvestris </em>L.and <em>Pinus pinaster Ait</em>. of triplet 6; PP01: monospecific stand of <em>Pinus pinaster</em> Ait. of triplet 1; PP02: monospecific stand of <em>Pinus pinaster</em> Ait. of triplet 2; PP03: monospecific stand of <em>Pinus pinaster </em>Ait. of triplet 3; PP04: monospecific stand of <em>Pinus pinaster</em> Ait. of triplet 4; PP05: monospecific stand of <em>Pinus pinaster</em> Ait. of triplet 5; PP06: monospecific stand of<em> Pinus pinaster </em>Ait. of triplet 6). Lat: Plot latitude in degrees. Long: Plot longitude in degrees. Province: Province to which the plot belongs (B:Province of Burgos; Sp: Province of Soria). Municipality: Municipality to which the plot belongs (M: Town of Mamolar; HP: Town of Hontoria del Pinar; N: Town of Navaleno; St: Town of Soria; CP: Town of Cabrejas del Pinar). Forest: Name of the forest where is located the plot (MB: Mata Blanca; MR: Mata Robledo; FP: Fuente del Pardo; PM: Pajar de la molinera; MP: Mojon Pardo; CM: Cueva de Matarubias). Alti: Plot elevation above sea level in m a.s.l. Slope: Slope (gradient) of the plot in percentage. Ori: Plot orientation in degrees. Clim: Climate clasification acording to K\u00f6ppen classification (1936) (Cfb: Temperate without dry season and temperate summer climate; Csb: Temperate with dry summer climate). XR: Accumulated rainfall in one year according to \u2018Atlas Agroclim\u00e1tico de Castilla y Le\u00f3n-ITACYL-AEMET\u2019 in mm. JR: January rainfall according to \u2018Atlas Agroclim\u00e1tico de Castilla y Le\u00f3n-ITACYL-AEMET\u2019 mm FR: February rainfall according to \u2018Atlas Agroclim\u00e1tico de Castilla y Le\u00f3n-ITACYL-AEMET\u2019 in mm. MR: March rainfall according to \u2018Atlas Agroclim\u00e1tico de Castilla y Le\u00f3n-ITACYL-AEMET\u2019 in mm. AR: April rainfall according to \u2018Atlas Agroclim\u00e1tico de Castilla y Le\u00f3n-ITACYL-AEMET\u2019 in mm. MyR: May rainfall according to \u2018Atlas Agroclim\u00e1tico de Castilla y Le\u00f3n-ITACYL-AEMET\u2019 in mm. JnR: June rainfall according to \u2018Atlas Agroclim\u00e1tico de Castilla y Le\u00f3n-ITACYL-AEMET\u2019 in mm. JlR: July rainfall according to \u2018Atlas Agroclim\u00e1tico de Castilla y Le\u00f3n-ITACYL-AEMET\u2019 in mm. AgR: August rainfall according to \u2018Atlas Agroclim\u00e1tico de Castilla y Le\u00f3n-ITACYL-AEMET\u2019 in mm. SR: September rainfall according to \u2018Atlas Agroclim\u00e1tico de Castilla y Le\u00f3n-ITACYL-AEMET\u2019 in mm. OR: October rainfall according to \u2018Atlas Agroclim\u00e1tico de Castilla y Le\u00f3n-ITACYL-AEMET\u2019 in mm. NR: November rainfall according to \u2018Atlas Agroclim\u00e1tico de Castilla y Le\u00f3n-ITACYL-AEMET\u2019 in mm. DR: December rainfall according to \u2018Atlas Agroclim\u00e1tico de Castilla y Le\u00f3n-ITACYL-AEMET\u2019 in mm. XT: Anual mean temperature according to \u2018Atlas Agroclim\u00e1tico de Castilla y Le\u00f3n-ITACYL-AEMET\u2019 in \u00baC. JT: January temperature according to \u2018Atlas Agroclim\u00e1tico de Castilla y Le\u00f3n-ITACYL-AEMET\u2019 in \u00baC. FT: February temperature according to \u2018Atlas Agroclim\u00e1tico de Castilla y Le\u00f3n-ITACYL-AEMET\u2019 in \u00baC. MT: March temperature according to \u2018Atlas Agroclim\u00e1tico de Castilla y Le\u00f3n-ITACYL-AEMET\u2019 in \u00baC. AT: April temperature according to \u2018Atlas Agroclim\u00e1tico de Castilla y Le\u00f3n-ITACYL-AEMET\u2019 in \u00baC. MyT: May temperature according to \u2018Atlas Agroclim\u00e1tico de Castilla y Le\u00f3n-ITACYL-AEMET\u2019 in \u00baC. JnT: June temperature according to \u2018Atlas Agroclim\u00e1tico de Castilla y Le\u00f3n-ITACYL-AEMET\u2019 in \u00baC. JlT: July temperature according to \u2018Atlas Agroclim\u00e1tico de Castilla y Le\u00f3n-ITACYL-AEMET\u2019 in \u00baC. AgT: August temperature according to \u2018Atlas Agroclim\u00e1tico de Castilla y Le\u00f3n-ITACYL-AEMET\u2019 in \u00baC. ST: September temperature according to \u2018Atlas Agroclim\u00e1tico de Castilla y Le\u00f3n-ITACYL-AEMET\u2019 in \u00baC. OT: October temperature according to \u2018Atlas Agroclim\u00e1tico de Castilla y Le\u00f3n-ITACYL-AEMET\u2019 in \u00baC. NT: November temperature according to \u2018Atlas Agroclim\u00e1tico de Castilla y Le\u00f3n-ITACYL-AEMET\u2019 in \u00baC. DT: December temperature according to \u2018Atlas Agroclim\u00e1tico de Castilla y Le\u00f3n-ITACYL-AEMET\u2019 in \u00baC. Par_mat: Soil parental material according to Spanish Geological Map on a 1M scale. (IGME , 2015) (SM: Sandstones and Marls). Geo_age: Geological age of plot according to Spanish Geological Map on a 1M scale. (IGME, 2015) (Mz: Mesozoic age). Soil: Soil type according to Soil-Survey-Staff (2014) (TpDx: Typic Dystroxerept; TpHx:: Typic Humixerept; AqHx:: Aquic humixerept) Litter_B: Total Leaf Litter Biomass in Mg/ha. FF_Th: Forest floor Thickness in cm. Fsh: Percentage of Fresh to Total Leaf Litter in %. Frg: Percentage of Fragmented to Total Leaf Litter in %. Hmf: Percentage of Humified to Total Leaf Litter in %. GH1: Fist genetic soil horizon according to Soil-Survey-Staff (2014) (Ah:: Mineral horizon with accumulation of organic matter. This horizon is formed at the soil surface or below an O horizon). GH2: Second genetic soil horizon according to Soil-Survey-Staff (2014) (AB: Transition horizon between A and B. A is a mineral horizon formed at the surface or below an O horizon, B is a subsurface horizon in which the structure of the rock is obliterated; AC: Transition horizon between A and C. A is a mineral horizon formed at the surface or below an O horizon; C is a mineral horizon, excluding hard bedrock, that is little affected by pedogenetic processes; Bw: Mineral B horizon where the development of colour or structure are its more important diagnostic characteristics). GH3: Third genetic soil horizon according to Soil-Survey-Staff (2014) (Bw: : Mineral B horizon where the development of colour or structure are its more important diagnostic characteristics; C: Mineral horizon, excluding hard bedrock, that is little affected by pedogenetic processes; Cg: Mineral horizon in which a distinct pattern of mottling occurs that reflects alternating conditions of oxidation and reduction of sesquioxides, caused by seasonal surface waterlogging). Th_H1: Thickness of the first soil horizon in cm. Th_H2: Thickness of the second soil horizon in cm. Th_H3: Thickness of the third soil horizon in cm. wetCol_H1: Wet matrix colour (Hue Value/Chroma) of the first soil horizon according to Munsell soil color chards (10YR2/1: black; 10YR2/2: very dark brown; 10YR3/1: very dark grey; 10YR3/2: very dark greyish brown; 10YR4/1: dark grey; 10YR6/3: pale brown). wetCol_H2: Wet matrix colour (Hue Value/Chroma) of the second soil horizon according to Munsell soil color chards (5YR5/8: yellowish red; 7.5YR4/6: strong brown; 10YR3/2: very dark greyish brown; 10YR4/1: dark grey; 10YR4/2: dark greyish brown; 10YR4/4: dark yellowish brown with chroma 4; 10YR4/6: dark yellowish brown with chroma 6; 10YR5/3: brown; 10YR5/4: yellowish brown with chroma 4; 10YR5/6: yellowish brown with chroma 6; 10YR5/8: yellowish brown with chroma 8; 10YR6/4: light yellowish brown; 10YR6/6: brownish yellow). wetCol_H3: Wet matrix colour (Hue Value/Chroma) of the third soil horizon according to Munsell soil color chards (5YR4/6: yellowish red; 10YR4/4: dark yellowish brown with chroma 4; 10YR4/6: dark yellowish brown with chroma 6; 10YR5/8: yellowish brown; 10YR6/1: grey). dryCol_H1:Dry matrix colour (Hue Value/Chroma) of the first soil horizon according to Munsell soil color chards (10YR4/1: dark grey; 10YR4/2: dark greyish brown; 10YR5/1: grey with value 5; 10YR5/2: greyish brown; 10YR5/3: brown; 10YR6/1: grey with value 6; 10YR6/2: light yellowish brown; 10YR7/2: light grey). dryCol_H2: Dry matrix colour (Hue Value/Chroma) of the second soil horizon according to Munsell soil color chards (7.5YR6/6: redish brown; 10YR4/1: dark grey; 10YR6/1: grey with value 6; 10YR6/2: light yellowish brown with chroma 2; 10YR6/3: pale brown; 10YR6/4: light yellowish brown with chroma 4; 10YR6/6: brownish yellow; 10YR7/3: very pale brown with value 7 and choma 3; 10YR7/4: very pale brown withvalue 7 and choma 4; 10YR8/4: very pale brown with value 8 and choma 4). dryCol_H3: Dry matrix colour (Hue Value/Chroma) of the third soil horizon according to Munsell soil color chards (5YR5/6: yellowish red; 7.5YR5/6: strong brown; 10YR6/4: light yellowish brown; 10YR6/6: brownish yellow; 10YR7/4: very pale brown; 10YR8/1: white). Sand_H1: Percentage of sand of the first soil horizon determined by the pipette method (MAPA 1994) according to Soil-Survey-Staff (2014) in % weight/weight. Sand_H2: Percentage of sand of the second soil horizon determined by the pipette method (MAPA 1994) according to Soil-Survey-Staff (2014) in % weight/weight. Sand_H3: Percentage of sand of the third soil horizon determined by the pipette method (MAPA 1994) according to Soil-Survey-Staff (2014) in % weight/weight. Silt_H1: Percentage of silt of the first soil horizon determined by the pipette method (MAPA 1994) according to Soil-Survey-Staff (2014) in % weight/weight. Silt_H2: Percentage of silt of the second soil horizon determined by the pipette method (MAPA 1994) according to Soil-Survey-Staff (2014) in % weight/weight. Silt_H3: Percentage of silt of the third soil horizon determined by the pipette method (MAPA 1994) according to Soil-Survey-Staff (2014) in % weight/weight. Clay_H1: Percentage of clay of the first soil horizon determined by the pipette method (MAPA 1994) according to Soil-Survey-Staff (2014) in % weight/weight. Clay_H2: Percentage of clay of the second soil horizon determined by the pipette method (MAPA 1994) according to Soil-Survey-Staff (2014) in % weight/weight. Clay_H3: Percentage of clay of the third soil horizon determined by the pipette method (MAPA 1994) according to Soil-Survey-Staff (2014) in % weight/weight. Tex_H1: Textural class of the first soil horizon according to Soil-Survey-Staff (2014) (SL: Sandy Loam; LfS: Loamy Fine Sand; L: Loam). Tex_H2: Textural class of the second soil horizon according to Soil-Survey-Staff (2014) (SL: Sandy Loam; LfS: Loamy Fine Sand; L: Loam, CL: Clay loam). Tex_H3: Textural class of the third soil horizon according to Soil-Survey-Staff (2014) (SL: Sandy Loam; L: Loam; C: Clay). Stones_H1: Coarse soil material (&gt; 2 mm) of the first soil horizon in % weight/weight. Stones_H2: Coarse soil material (&gt; 2 mm) of the second soil horizon in % weight/weight. Stones_H3: Coarse soil material (&gt; 2 mm) of the third soil horizon in % weight/weight. %FR_H1: Fine roots (&lt; 5 mm) of the first soil horizon in %. %FR_H2: Fine roots (&lt; 5 mm) of the second soil horizon in %. %FR_H3: Fine roots (&lt; 5 mm) of the third soil horizon in %. %CR_H1: Coarse roots (&gt; 5 mm) of the first soil horizon in %. %CR_H2: Coarse roots (&gt; 5 mm) of the second soil horizon in %. %CR_H3: Coarse roots (&gt; 5 mm) of the third soil horizon in %. bD_H1: Bulk density of the first soil horizon according to MAPA (1994) in g/cm<sup>3</sup>. bD_H2: Bulk density of the second soil horizon according to MAPA (1994) in g/cm<sup>3</sup>. bD_H3: Bulk density of the third soil horizon according to MAPA (1994) in g/cm<sup>3</sup>. pD_H1: Particle density of the first soil horizon according to MAPA (1994) in g/cm<sup>3</sup>. pD_H2: Particle density of the second soil horizon according to MAPA (1994) in g/cm<sup>3</sup>. pD_H3: Particle density of the third soil horizon according to MAPA (1994) in g/cm<sup>3</sup>. Poro_H1: Porosity of the first soil horizon according to MAPA (1994) in % vol/vol. Poro_H2: Porosity of the second soil horizon according to MAPA (1994) in % vol/vol. Poro_H3: Porosity of the third soil horizon according to MAPA (1994) in % vol/vol. pH_H1: pH (1:2.5 H2O) of the first soil horizon according to MAPA (1994) pH_H2: pH (1:2.5 H2O) of the second soil horizon according to MAPA (1994) pH_H3: pH (1:2.5 H2O) of the third soil horizon according to MAPA (1994) EC_H1: Electrical conductivity of the first soil horizon according to MAPA (1994) in dS/m. EC_H2: Electrical conductivity of the second soil horizon according to MAPA (1994) in dS/m. EC_H3: Electrical conductivity of the third soil horizon according to MAPA (1994) in dS/m. avP_H1: Available phosphorus of the first soil horizon according to Olsen and Sommers (1982) in mg/kg. avP_H2: Available phosphorus of the second soil horizon according to Olsen and Sommers (1982) in mg/kg. avP_H3: Available phosphorus of the third soil horizon according to Olsen and Sommers (1982) in mg/kg. avPstock_H1: Available phosphorus stock of the first soil horizon according to L\u00f3pez-Marcos et al. (2019) in Mg/ha. avPstock_H2: Available phosphorus stock of the second soil horizon according to L\u00f3pez-Marcos et al. (2019) in Mg/ha. avPstock_H3: Available phosphorus stock of the third soil horizon up to 50 cm depth according to L\u00f3pez-Marcos et al. (2019) in Mg/ha. avPstock_50: Available phosphorus stock of whole soil profile up to 50 cm depth accorging to L\u00f3pez-Marcos et al. (2019) in Mg/ha. TN_H1. Total nitrogen of the first soil horizon analyzed with a LECO-CHN 2000 elemental analyser in mg/kg. TN_H2: Total nitrogen of the second soil horizon analyzed with a LECO-CHN 2000 elemental analyser in mg/kg. TN_H3: Total nitrogen of the third soil horizon analyzed with a LECO-CHN 2000 elemental analyser in mg/kg. TNstock_H1: Total nitrogen stock of the first soil horizon according to L\u00f3pez-Marcos et al. (2019) in Mg/ha. TNstock_H2: Total nitrogen stock of the second soil horizon according to L\u00f3pez-Marcos et al. (2019) in Mg/ha. TNstock_H3: Total nitrogen stock of the third soil horizon up to 50 cm depth according to L\u00f3pez-Marcos et al. (2019) in Mg/ha. TNstock_50: Total nitrogen stock of whole soil profile up to 50 cm depth according to L\u00f3pez-Marcos et al. (2019) in Mg/ha. TOC_H1: Total organic carbon of the first soil horizon analyzed with a LECO-CHN 2000 elemental analyser in mg/kg. TOC_H2: Total organic carbon of the second soil horizon analyzed with a LECO-CHN 2000 elemental analyser in mg/kg. TOC_H3: Total organic carbon of the third soil horizon analyzed with a LECO-CHN 2000 elemental analyser in mg/kg. TOCstock_H1:Total organic carbon stock of the first soil horizon according to L\u00f3pez-Marcos et al. (2019) in Mg/ha. TOCstock_H2: Total organic carbon stock of the second soil horizon according to L\u00f3pez-Marcos et al. (2019) in Mg/ha. TOCstock_H3: Total organic carbon stock of the third soil horizon up to 50 cm depth according to L\u00f3pez-Marcos et al. (2019) in Mg/ha. TOCstock_50: Total organic carbon stock of whole soil profile up to 50 cm depth according to L\u00f3pez-Marcos et al. (2019) in Mg/ha. C/N_H1: Ratio of total organic carbon to total nitrogen of the first soil horizon C/N_H2 : Ratio of total organic carbon to total nitrogen of the second soil horizon C/N_H3: Ratio of total organic carbon to total nitrogen of the third soil horizon OxC_H1: Easily oxidizable carbon of the first soil horizon according to Walkley (1947) in mg/kg. OxC_H2: Easily oxidizable carbon of the second soil horizon according to Walkley (1947) in mg/kg. OxC_H3: Easily oxidizable carbon of the third soil horizon according to Walkley (1947) in mg/kg. OxCstock_H1: Easily oxidizable carbon stock of the first soil horizon according to L\u00f3pez-Marcos et al. (2019) in Mg/ha. OxCstock_H2: Easily oxidizable carbon stock of the second soil horizon according to L\u00f3pez-Marcos et al. (2019) in Mg/ha. OxCstock_H3: Easily oxidizable carbon stock of the third soil horizon up to 50 cm depth according to L\u00f3pez-Marcos et al. (2019) in Mg/ha. OxCstock_50: Easily oxidizable carbon stock of whole soil profile up to 50 cm depth according to L\u00f3pez-Marcos et al. (2019) in Mg/ha. CEC_H1: Cation exchange capacity of the first soil horizon according to Mehlich (1953) in cmol<sub>+</sub>/kg. CEC_H2: Cation exchange capacity of the second soil horizon according to Mehlich (1953) in cmol<sub>+</sub>/kg. CEC_H3: Cation exchange capacity of the third soil horizon according to Mehlich (1953) in cmol<sub>+</sub>/kg. Na<sup>+</sup>_H1: Exchangeable sodium of the first soil horizon by means of extracting with 1N ammonium acetate (pH=7) (Schollenberger and Simon 1945) in cmol<sub>+</sub>/kg. Na<sup>+</sup>_H2: Exchangeable sodium", "keywords": ["Physicochemical soil profile parameters", "Mixed stand", "Understory characterization", "Overstory features", "Pinus sylvestris", "Pinus pinaster", "15. Life on land", "Climatic parameters"], "contacts": [{"organization": "Marcos, Daphne L\u00f3pez, Turri\u00f3n, Mar\u00eda-Bel\u00e9n, Bravo, Felipe, Mart\u00ednez-Ruiz, Carolina,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5281/zenodo.4384530"}, {"rel": "self", "type": "application/geo+json", "title": "10.5281/zenodo.4384530", "name": "item", "description": "10.5281/zenodo.4384530", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5281/zenodo.4384530"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-07-03T00:00:00Z"}}, {"id": "10.5281/zenodo.4748444", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:21:10Z", "type": "Dataset", "title": "The extent of woody plant invasion in selected sites of the communally managed Molopo District, North West Province.", "description": "EmbargoWoody plant invasion (bush encroachment) is a problem in the semi arid communal areas of the North West Province which had been affecting the Molopo Area as early as 1960. It affects the livelihoods of the communal farmer because it reduces carrying capacity and is a form of veld degradation. The extent of woody plant encroachment was quantified at selected sites and reference sites in the Molopo District. There was a study site and reference site selected in a commercially managed area. Soil samples from these selected sites were also analysed for chemical and physical properties as well as nutrient content that could have an influence on the proliferation of the woody plants. Social surveys were also conducted to investigate the perceptions and influence of the affected communities towards woody plant invasion. The prominent species identified in the area included Acacia mellifera, Dichrostachys cenerea, Prosopis velutina and Terminalia sericea. All of the study sites, except the benchmark sites, had woody plant densities of more than 2 000 TE/ha that according to Moore &amp; Odendaal (1987), almost totally suppress grass growth. It was clear from the data that the nutrient status of soils of encroached areas was higher than the benchmark sites although some of the differences were statistically insignificant. Organic carbon was higher at most of the encroached sites (71 % of the sites) where 80 % of the enriched sites had significantly higher organic carbon than that of the benchmark sites. There is a need to develop small scale farming practices that are appropriate in terms of sustainable development in the local context.", "keywords": ["2. Zero hunger", "woody plants", "Molopo district", "Prosopis velutina", "Dichrostachys cenerea", "Masters", "15. Life on land", "Acacia mellifera", "North West Province", "Terminalia sericea", "Molopo Area"], "contacts": [{"organization": "Mogodi, Phemelo", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5281/zenodo.4748444"}, {"rel": "self", "type": "application/geo+json", "title": "10.5281/zenodo.4748444", "name": "item", "description": "10.5281/zenodo.4748444", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5281/zenodo.4748444"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2010-01-01T00:00:00Z"}}, {"id": "2552941062", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:22:50Z", "type": "Journal Article", "created": "2016-11-26", "title": "Normalizing land surface temperature data for elevation and illumination effects in mountainous areas: A case study using ASTER data over a steep-sided valley in Morocco", "description": "Abstract   The remotely sensed land surface temperature (LST) is a key parameter to monitor surface energy and water fluxes but the strong impact of topography on LST has limited its use to mostly flat areas. To fill the gap, this study proposes a physically-based method to normalize LST data for topographic - namely illumination and elevation - effects over mountainous areas. Both topographic effects are first quantified by inverting a dual-source soil/vegetation energy balance (EB) model forced by 1) the instantaneous solar radiation simulated by a 3D radiative transfer model named DART (Discrete Anisotropic Radiative Transfer) that uses a digital elevation model (DEM), 2) a satellite-derived vegetation index, and 3) local meteorological (air temperature, air relative humidity and wind speed) data available at a given location. The satellite LST is then normalized for topography by simulating the LST using both pixel- and image-scale DART solar radiation and elevation data. The approach is tested on three ASTER (Advanced Spaceborne Thermal Emission and Reflection Radiometer) overpass dates over a steep-sided 6\u00a0km by 6\u00a0km area in the Atlas Mountain in Morocco. The mean correlation coefficient and root mean square difference (RMSD) between EB-simulated and ASTER LST is 0.80 and 3\u00a0\u00b0C, respectively. Moreover, the EB-based method is found to be more accurate than a more classical approach based on a multi-linear regression with DART solar radiation and elevation data. The EB-simulated LST is also evaluated against an extensive ground dataset of 135 autonomous 1-cm depth temperature sensors deployed over the study area. While the mean RMSD between 90\u00a0m resolution ASTER LST and localized ibutton measurements is 6.1\u00a0\u00b0C, the RMSD between EB-simulated LST and ibutton soil temperature is 5.4 and 5.3\u00a0\u00b0C for a DEM at 90\u00a0m and 8\u00a0m resolution, respectively. The proposed topographic normalization is self-calibrated from (LST, DEM, vegetation index and in situ meteorological data) data available over large extents. As a significant perspective this approach opens the path to using normalized LST as input to evapotranspiration retrieval methods based on LST.", "keywords": ["[SDE] Environmental Sciences", "550", "Topographic normalization", "DEM", "0207 environmental engineering", "Energy balance", "02 engineering and technology", "01 natural sciences", "ASTER", "13. Climate action", "[SDE]Environmental Sciences", "DART", "Land surface temperature", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/2552941062"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Remote%20Sensing%20of%20Environment", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "2552941062", "name": "item", "description": "2552941062", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2552941062"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-02-01T00:00:00Z"}}, {"id": "10.7910/DVN/SQI3IR", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:21:57Z", "type": "Dataset", "title": "GMCSD-1. Global Mangrove Carbon, 2000 and 2012, 1 Arc-second, 1 m soil.", "description": "Open AccessGlobal Mangrove Carbon, 2000 and 2012, 1 Arc-Second, 1 m Soil, low, mid, high, EQ1, EQ2, EQ3, EQ4, EQ5.  <p> These are large file and we needed to use file geodatabase format to compress enough to post on the Dataverse. Hence no Tiffs.", "keywords": ["Earth and Environmental Sciences", "Raster", "ArcGIS file Geodatabase rasters", "Global Mangrove Carbon"], "contacts": [{"organization": "Hamilton, Stuart", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.7910/DVN/SQI3IR"}, {"rel": "self", "type": "application/geo+json", "title": "10.7910/DVN/SQI3IR", "name": "item", "description": "10.7910/DVN/SQI3IR", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.7910/DVN/SQI3IR"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2016-01-01T00:00:00Z"}}, {"id": "10.7910/DVN/ZJMJ7K", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:21:57Z", "type": "Dataset", "created": "2018-01-01", "title": "Predicted soil organic carbon (SOC) content (g/kg) and SOC stock (t/ha) in the Eastern Plains of Colombia", "description": "Open AccessMaps allocated in this repository were predicted using a digital soil mapping (DSM) approach (McBratney et al, 2003) based on random forest (Breiman, 2001). A dataset consisting of 653 geo-referenced soil points and a series of environmental covariates that represent the soil-forming factors were used in order to adjust the DSM models. Models\u2019 assessment for SOC content was performed using the 100-fold cross-validation, through the coefficient of determination (R2), root mean squared error (RMSE) and the mean error. Results showed 50.3% of the variance explained, and a RMSE and ME of 0.461 g/kg and 0.038 g/kg, respectively.", "keywords": ["digital surface models", "Eastern Plains", "carbon stock", "carbono org\u00e1nico del suelo", "Colombia", "land use mapping", "Latin America and the Caribbean", "soil", "soil organic carbon", "cartograf\u00eda del uso de la tierra", "Orinoco region", "Earth and Environmental Sciences", "digital soil mapping", "Soil and Water Management", "reconocimiento de suelos", "Multifunctional landscapes", "soil surveys"]}, "links": [{"href": "https://doi.org/10.7910/DVN/ZJMJ7K"}, {"rel": "self", "type": "application/geo+json", "title": "10.7910/DVN/ZJMJ7K", "name": "item", "description": "10.7910/DVN/ZJMJ7K", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.7910/DVN/ZJMJ7K"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-01-01T00:00:00Z"}}, {"id": "10029/626925", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:21:58Z", "type": "Journal Article", "created": "2023-08-24", "title": "Expanding the applicability domain of QSPRs for predicting water solubility and vapor pressure of PFAS", "description": "Manuscript of the publication 'Expanding the applicability domain of QSPRs for predicting water solubility and vapor pressure of PFAS'.", "keywords": ["water solubility", "Fluorocarbons", "vapor pressure", "Vapor Pressure", "Water solubility", "PFAS", "H2020", "Water", "Applicability domain (AD)", "Asteraceae", "Vapor pressure", "PROMISCES", "Solubility", "QSPR", "applicability domain (AD)", "COSMO-RS"]}, "links": [{"href": "https://doi.org/10029/626925"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Chemosphere", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10029/626925", "name": "item", "description": "10029/626925", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10029/626925"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-11-01T00:00:00Z"}}, {"id": "10045/77172", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-21T16:21:59Z", "type": "Journal Article", "created": "2018-05-08", "title": "The genusXanthogrammaSchiner, 1861 (Diptera: Syrphidae) in southeastern Europe, with descriptions of two new species", "description": "Abstract<p>Examination of 122 specimens ofXanthogrammaSchiner, 1861 (Diptera: Syrphidae) from varied localities in Europe (+Turkey) resulted in the description of two new species (X. aeginaeRicarte, Nedeljkovi\uffc4\uff87, and Vuji\uffc4\uff87new speciesandX. pilosumNedeljkovi\uffc4\uff87, Ricarte, and Vuji\uffc4\uff87new species), as well as new data on six other species. Most of the examined material originated from the Balkan Peninsula and Greek islands. New species concepts were supported by morphological and molecular evidence. Relationships among the eight studied species were analysed and discussed based on the data of nuclear (ITS2) and mitochondrial (COI) genes sequences. An identification key to the European species ofXanthogrammais provided. Lectotypes are designated forDoros decoratumZetterstedt, 1843,Lasiophthicus novusRondani, 1857,Syrphus laetusFabricius, 1794,Syrphus ornatusMeigen, 1822, andXanthogramma nobilitatumFrey, 1946.</p", "keywords": ["0106 biological sciences", "2. Zero hunger", "Xanthogramma Schiner", "Southeastern Europe", "9. Industry and infrastructure", "Diptera", "Zoolog\u00eda", "Syrphidae", "15. Life on land", "01 natural sciences"]}, "links": [{"href": "https://doi.org/10045/77172"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/The%20Canadian%20Entomologist", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10045/77172", "name": "item", "description": "10045/77172", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10045/77172"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-05-08T00:00:00Z"}}], "links": [{"rel": "self", "type": "application/geo+json", "title": "This document as GeoJSON", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=ASTER&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=ASTER&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=ASTER&", "hreflang": "en-US"}, {"rel": "next", "type": "application/geo+json", "title": "items (next)", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=ASTER&offset=50", "hreflang": "en-US"}], "numberMatched": 187, "numberReturned": 50, "distributedFeatures": [], "timeStamp": "2026-09-22T08:47:47.612225Z"}