{"type": "FeatureCollection", "features": [{"id": "10.5061/dryad.cz8w9gj78", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:22:28Z", "type": "Dataset", "title": "Soil microbial relative resource limitation exhibited contrasting seasonal patterns along an elevational gradient in Yulong snow mountain", "description": "unspecified", "keywords": ["2. Zero hunger", "mountain ecosystems", "13. Climate action", "microbial metabolic mechanisms", "microbial relative C limitation", "microbial relative P limitation", "C use efficiency", "FOS: Earth and related environmental sciences", "15. Life on land", "elevations"], "contacts": [{"organization": "Zhang, Dandan, Wu, Baoyun, Li, Jinsheng, Cheng, Xiaoli,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5061/dryad.cz8w9gj78"}, {"rel": "self", "type": "application/geo+json", "title": "10.5061/dryad.cz8w9gj78", "name": "item", "description": "10.5061/dryad.cz8w9gj78", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5061/dryad.cz8w9gj78"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-02-02T00:00:00Z"}}, {"id": "10.5281/zenodo.5574882", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:24:29Z", "type": "Report", "created": "2020-03-09", "title": "Hyperspectral imaging for high resolution mapping of soil profile organic carbon distribution in an Austrian Alpine landscape", "description": "<p>         &amp;lt;p&amp;gt;Studies on soil organic carbon (SOC) stocks mostly focus on topsoils (&amp;lt; 30 cm). However, 30 to 63% of the SOC are stored in the subsoils (30 to 100 cm), and the factors controlling SOC storage in subsoils may be substantially different than in topsoils. The low mean SOC content in subsoils makes its quantification and characterization challenging. Thus, new approaches are required to depict the SOC stocks distribution in full soil profile. Hyperspectral imaging of soil core samples can provide high spatial resolution of the vertical distribution of SOC in a soil profile. The main objective of the ongoing study, within the Horizon 2020 European Project Circular Agronomics, is to apply laboratory hyperspectral imaging with a variety of machine learning approaches for the mapping of OC distribution in undisturbed soil cores. Soil cores were collected down to a depth of one meter in grasslands of 15 organic farms located in the Lungau Valley, in Austria. Some samples were divided into five depths in the field for classical bulk soil measurements (total carbon and nitrogen, texture, pH, EC and bulk density) on disturbed samples. Undisturbed soil cores were sliced vertically for laboratory hyperspectral imaging in the range of Vis-NIR (400-1000 nm). We were able to reveal the hotspots of OC and map the OC distribution in soil profile by applying a variety of machine learning approaches (i.e. partial least square and random forest regression) as a function of spectral responses. A digital elevation model was further exploited to investigate the effects of topographical factors such as elevation, aspect and slope on SOC profile distribution. Landsat 8 data were also used to depict the spatial variability of land insensitive cover/vegetation in study area.&amp;lt;/p&amp;gt;         </p>", "keywords": ["2. Zero hunger", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land", "Vis-NIR imaging spectroscopy", " Alpine grassland", " Digital elevation model", " Subsoils"], "contacts": [{"organization": "YASER OSTOVARI, K\u00f6ppend\u00f6rfer, Baptist, Guigue, Julien, Van Groenigen, Jan Willem, Creamer, Rachel, Guggenberger, Thomas, Grassauer, Florian, Hobley, Eleanor, Ferron, Laura, Martens, Henk, K\u00f6gel-Knabner, Ingrid, Vidal, Alix,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5281/zenodo.5574882"}, {"rel": "self", "type": "application/geo+json", "title": "10.5281/zenodo.5574882", "name": "item", "description": "10.5281/zenodo.5574882", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5281/zenodo.5574882"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-03-23T00:00:00Z"}}, {"id": "17e5dafc-0450-41d3-ad4b-d698b0f1a9ad", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:30:10Z", "type": "Dataset", "title": "Atlas des d\u00e9partements fran\u00e7ais d'Outre-Mer : 4. La Guyane. 4 mosaics of 4 map sheets and a set of 32 map sheets. Scale of 1:40\u00a0000\u00a0000 to 1:7\u00a0100. Date of publication: 1978-1979.", "description": "4 mosaics of 4 map sheets and a set of 32 additional map sheets 1.   Administrations, banques : la Guyane : planche 29. Scale of 1:3\u00a0000\u00a0000 to 1:10\u00a0000. Date of publication: 1979. 2.   Arch\u00e9ologie, histoire des Am\u00e9rindiens : la Guyane : planche 17. Scale of 1:15\u00a0000\u00a0000 to 1:1\u00a0500\u00a0000. Date of publication: 1979. 3.   Cartes anciennes : la Guyane : planche 18. Scale of 1:2\u00a0500\u00a0000 to 1:630\u00a0000. Date of publication: 1979. 4.   Cayenne : la Guyane : planche 34. Scale of 1:60\u00a0000 to 1:10\u00a0000. Date of publication: 1979. 5.   Circulation, transports : la Guyane : planche 27. Scale of 1:14\u00a0000\u00a0000 to 1:100\u00a0000. Date of publication: 1979. 6.   Climatologie : la Guyane : planche 7. Scale of 1:3\u00a0500\u00a0000. Date of publication: 1979. 7.   Climatologie II : pluviom\u00e9trie annuelle moyenne : la Guyane : planche 8. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1979. 8.   Commerce, industrie, p\u00eache, tourisme : la Guyane : planche 28. Scale of 1:2\u00a0000\u00a0000 to 1:1\u00a0500\u00a0000. Date of publication: 1979. 9.   Energie, eaux, PTT et radiot\u00e9l\u00e9vision : la Guyane : planche 30. Scale of 1:1\u00a0500\u00a0000 to 1:225\u00a0000. Date of publication: 1979. 10.  Exploitation foresti\u00e8re : la Guyane : planche 25. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1979. 11.  Faunes originales : plaines c\u00f4ti\u00e8res : la Guyane : planche 15. Scale of 1:350\u00a0000. Date of publication: 1979. 12.  G\u00e9ologie : la Guyane : planche 4. Scale of 1:2\u00a0500\u00a0000 to 1:1\u00a0000\u00a0000. Date of publication: 1979. 13.  G\u00e9omorphologie : la Guyane : planche 5. Scale of 1:2\u00a0000\u00a0000 to 1:1\u00a0000\u00a0000. Date of publication: 1979. 14.  Groupes humains : la Guyane : planche 20. Scale of 1:2\u00a0000\u00a0000 to 1:300\u00a0000. Date of publication: 1979. 15.  Histoire coloniale : la Guyane : planche 19. Scale of 1:2\u00a0000\u00a0000 to 1:500\u00a0000. Date of publication: 1979. 16.  Hydrologie : la Guyane : planche 9. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1978. 17.  Ile de Cayenne : la Guyane : planche 35. Scale of 1:100\u00a0000 to 1:60\u00a0000. Date of publication: 1978. 18.  Kourou, Saint-Laurent, Sinnamary : la Guyane : planche 36. Scale of 1:100\u00a0000 to 1:7\u00a0100. Date of publication: 1979. 19.  La r\u00e9gion des Guyanes : la Guyane : planche 2. Scale of 1:5\u00a0000\u00a0000. Date of publication: 1979. 20.  Logement : la Guyane : planche 33. Scale of 1:1\u00a0000\u00a0000 to 1:35\u00a0000. Date of publication: 1979. 21.  Milieu marin : la Guyane : planche 14. Scale of 1:1\u00a0500\u00a0000. Date of publication: 1979. 22.  Mouvements migratoires : la Guyane : planche 22. Scale of 1:1\u00a0000\u00a0000 to 1:100\u00a0000. Date of publication: 1979. 23.  Pathologie : la Guyane : planche 16. Scale of 1:2\u00a0000\u00a0000 to 1:150\u00a0000. Date of publication: 1979. 24.  P\u00e9dologie : la Guyane : planche 10. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1979. 25.  P\u00e9dologie : plaines c\u00f4ti\u00e8res : la Guyane : planche 11. Scale of 1:350\u00a0000. Date of publication: 1979. 26.  Population : r\u00e9partition : la Guyane : planche 21. Scale of 1:2\u00a0000\u00a0000 to 1:100\u00a0000. Date of publication: 1979. 27.  Productions agricoles : la Guyane : planche 24. Scale of 1:2\u00a0000\u00a0000. Date of publication: 1979. 28.  Relief : la Guyane : planche 3. Scale of 1:1\u00a0000\u00a0000 to 1:100\u00a0000. Date of publication: 1979. 29.  Ressources mini\u00e8res : la Guyane : planche 26. Scale of 1:1\u00a0000\u00a0000 to 1:25\u00a0000. Date of publication: 1979. 30.  Sant\u00e9 et action sociale, scolarit\u00e9 : la Guyane : planche 31. Scale of 1:1\u00a0500\u00a0000 to 1:50\u00a0000. Date of publication: 1979. 31.  S\u00e9dimentologie : plaines c\u00f4ti\u00e8res : la Guyane : planche 6. Scale of 1:350\u00a0000. Date of publication: 1979. 32.  Situation : la Guyane : planche 1. Scale of 1:40\u00a0000\u00a0000. Date of publication: 1979. 33.  Sports et loisirs, cultes : la Guyane : planche 32. Scale of 1:1\u00a0500\u00a0000 to 1:20\u00a0000. Date of publication: 1979. 34.  Utilisation du sol : la Guyane : planche 23. Scale of 1:1\u00a0000\u00a0000 to 1:200\u00a0000. Date of publication: 1979. 35.  V\u00e9g\u00e9tation : la Guyane : planche 12. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1979. 36.  V\u00e9g\u00e9tation : plaines c\u00f4ti\u00e8res : la Guyane : planche 13. Scale of 1:350\u00a0000. Date of publication: 1979.", "keywords": ["elevation", "fr", "geology", "hydrography", "illustration", "labex-ceba", "land-use", "local-coverage", "map-collection", "meteorological-geographical-features", "mineral-resources", "national-coverage", "oceanographic-geographical-features", "population-distribution-\u2014-demography", "precipitation", "project-numerisud", "regional-coverage", "relief-(land)", "settlements", "soil", "species-distribution", "thematic-map", "topography"]}, "links": [{"href": "http://data.europa.eu/88u/dataset/17e5dafc-0450-41d3-ad4b-d698b0f1a9ad"}, {"rel": "self", "type": "application/geo+json", "title": "17e5dafc-0450-41d3-ad4b-d698b0f1a9ad", "name": "item", "description": "17e5dafc-0450-41d3-ad4b-d698b0f1a9ad", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/17e5dafc-0450-41d3-ad4b-d698b0f1a9ad"}, {"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": "10.1007/s00442-012-2522-6", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:14:50Z", "type": "Journal Article", "created": "2012-11-23", "title": "Nutrient Limitation In Rainforests And Cloud Forests Along A 3,000-M Elevation Gradient In The Peruvian Andes", "description": "We report results from a large-scale nutrient fertilization experiment along a 'megadiverse' (154 unique species were included in the study) 3,000-m elevation transect in the Peruvian Andes and adjacent lowland Amazonia. Our objectives were to test if nitrogen (N) and phosphorus (P) limitation shift along this elevation gradient, and to determine how an alleviation of nutrient limitation would manifest in ecosystem changes. Tree height decreased with increasing elevation, but leaf area index (LAI) and diameter at breast height (DBH) did not vary with elevation. Leaf N:P decreased with increasing elevation (from 24 at 200 m to 11 at 3,000 m), suggesting increased N limitation and decreased P limitation with increasing elevation. After 4 years of fertilization (N, P, N + P), plots at the lowland site (200 m) fertilized with N + P showed greater relative growth rates in DBH than did the control plots; no significant differences were evident at the 1,000 m site, and plots fertilized with N at the highest elevation sites (1,500, 3,000 m) showed greater relative growth rates in DBH than did the control plots, again suggesting increased N constraint with elevation. Across elevations in general N fertilization led to an increase in microbial respiration, while P and N + P addition led to an increase in root respiration and corresponding decrease in hyphal respiration. There was no significant canopy response (LAI, leaf nutrients) to fertilization, suggesting that photosynthetic capacity was not N or P limited in these ecosystems. In sum, our study significantly advances ecological understanding of nutrient cycling and ecosystem response in a region where our collective knowledge and data are sparse: we demonstrate N limitation in high elevation tropical montane forests, N and P co-limitation in lowland Amazonia, and a nutrient limitation response manifested not in canopy changes, but rather in stem and belowground changes.", "keywords": ["tropical forest", "0106 biological sciences", "elevation", "Rain", "01 natural sciences", "experimental study", "nitrogen", "Trees", "Tropical", "montane forest", "Peru", "ecosystem response", "Forest", "phosphorus", "diameter", "2. Zero hunger", "nutrient limitation", "photosynthesis", "leaf area index", "Amaz Fertilization", "Montane", "Keywords: cloud forest", "fertilizer application", "nutrient cycling", "15. Life on land", "growth rate", "rainforest"]}, "links": [{"href": "https://openresearch-repository.anu.edu.au/bitstream/1885/77616/7/f5625xPUB64472013.pdf.jpg"}, {"href": "https://openresearch-repository.anu.edu.au/bitstream/1885/77616/9/Meir_email.pdf.jpg"}, {"href": "https://openresearch-repository.anu.edu.au/bitstream/1885/77616/11/01_Fisher_Nutrient_limitation_in_2013.pdf.jpg"}, {"href": "https://openresearch-repository.anu.edu.au/bitstream/1885/77616/13/02_Fisher_Nutrient_limitation_in_2013.pdf.jpg"}, {"href": "https://doi.org/10.1007/s00442-012-2522-6"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Oecologia", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s00442-012-2522-6", "name": "item", "description": "10.1007/s00442-012-2522-6", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s00442-012-2522-6"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2012-11-24T00:00:00Z"}}, {"id": "10.1007/s11852-015-0390-z", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:15:31Z", "type": "Journal Article", "created": "2015-07-01", "title": "Salinization During Salt-Marsh Restoration After Managed Realignment", "description": "<p>Salt marshes provide an important and unique habitat for plants and animals. To restore salt marshes, numerous coastal realignment projects have been carried out, but restored marshes often show persistent ecological differences from natural marshes. We evaluate the effects of elevation and marsh topography, which are in turn affected by drainage and livestock grazing, on soil salinity after de-embankment. Salinity in the topsoil was monitored during the first 10 years after de-embankment and compared with salinity in an adjacent reference marsh. Additionally, salinity at greater depths (down to 1.2 m below the marsh surface) was monitored during the first 4 years by measuring the electrical conductivity of the groundwater. Chloride concentration in the top soil strongly decreased with increasing elevation; however, it was not affected by marsh topography, i.e. distance to creek or breach. Chloride concentrations higher than 2 g Cl-/litre were found at elevations below 0.6 m + MHT. Salinization of the groundwater, however, took several years. At low marsh elevations, the salinity of the deep groundwater (at 1.2 m depth) increased slowly throughout the full 4-year period of monitoring but did not reach the level of seawater. Compared to the ungrazed treatment, the grazed treatment led to lower accretion rates, lower soil-moisture content and higher chloride content of soil moisture. The de-embankment of the agricultural grasslands resulted in a rapid increase of soil salinity, although deeper ground-water levels showed a much slower response. Elevation accounted for most of the variation in the salinization of the soil. Grazing may enhance salinity of the top soil.</p>", "keywords": ["0106 biological sciences", "2. Zero hunger", "Salinity", "ARGENTINA", "Ecology", "IMPACT", "WADDEN SEA", "HALOPHYTES", "15. Life on land", "Oceanography", "01 natural sciences", "6. Clean water", "DISPERSAL", "Elevation", "SOIL-SALINITY", "Drainage", "VEGETATION", "Grazing management", "INUNDATION FREQUENCY", "ELEVATION", "NITROGEN MINERALIZATION", "Nature and Landscape Conservation"], "contacts": [{"organization": "Roos M. Veenklaas, Peter Esselink, Jan P. Bakker, E.C. Koppenaal,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1007/s11852-015-0390-z"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Coastal%20Conservation", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s11852-015-0390-z", "name": "item", "description": "10.1007/s11852-015-0390-z", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s11852-015-0390-z"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2015-07-03T00:00:00Z"}}, {"id": "10.1016/j.ecss.2013.08.021", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:16:17Z", "type": "Journal Article", "created": "2013-08-20", "title": "Effects Of Long-Term Grazing On Sediment Deposition And Salt-Marsh Accretion Rates", "description": "<p>Many studies have attempted to predict whether coastal marshes will be able to keep up with future acceleration of sea-level rise by estimating marsh accretion rates. However, there are few studies focussing on the long-term effects of herbivores on vegetation structure and subsequent effects on marsh accretion. Deposition of fine-grained, mineral sediment during tidal inundations, together with organic matter accumulation from the local vegetation, positively affects accretion rates of marsh surfaces. Tall vegetation can enhance sediment deposition by reducing current flow and wave action. Herbivores shorten vegetation height and this could potentially reduce sediment deposition. This study estimated the effects of herbivores on 1) vegetation height, 2) sediment deposition and 3) resulting marsh accretion after long-term (at least 16 years) herbivore exclusion of both small (i.e. hare and goose) and large grazers (i.e. cattle) for marshes of different ages. Our results firstly showed that both small and large herbivores can have a major impact on vegetation height. Secondly, grazing processes did not affect sediment deposition. Finally, trampling by large grazers affected marsh accretion rates by compacting the soil. In many European marshes, grazing is used as a tool in nature management as well as for agricultural purposes. Thus, we propose that soil compaction by large grazers should be taken in account when estimating the ability of coastal systems to cope with an accelerating sea-level rise. (C) 2013 Elsevier Ltd. All rights reserved.</p>", "keywords": ["marsh succession", "0106 biological sciences", "Surface elevation change", "Sea-level rise", "FLOW", "Sedimentation rate", "SEA-LEVEL RISE", "SURFACE ELEVATION", "01 natural sciences", "BROWN HARES", "Herbivory", "14. Life underwater", "Marsh succession", "Biology", "Global change", "VEGETATION SUCCESSION", "global change", "COASTAL WETLANDS", "0105 earth and related environmental sciences", "2. Zero hunger", "sedimentation rate", "herbivory", "GEESE", "sea-level rise", "15. Life on land", "PRODUCTIVITY GRADIENT", "surface elevation change", "NORTH-SEA", "13. Climate action", "TIDAL MARSH"]}, "links": [{"href": "https://doi.org/10.1016/j.ecss.2013.08.021"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Estuarine%2C%20Coastal%20and%20Shelf%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.ecss.2013.08.021", "name": "item", "description": "10.1016/j.ecss.2013.08.021", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.ecss.2013.08.021"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2013-11-01T00:00:00Z"}}, {"id": "10.1016/j.ecss.2013.10.026", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:16:17Z", "type": "Journal Article", "created": "2013-11-01", "title": "Does Livestock Grazing Affect Sediment Deposition And Accretion Rates In Salt Marshes?", "description": "<p>Accretion rates, defined as the vertical growth of salt marshes measured in mm per year, may be influenced by grazing livestock in two ways: directly, by increasing soil compaction through trampling, and indirectly, by reducing aboveground biomass and thus decreasing sediment deposition rates measured in g/m(2) per year. Although accretion rates and the resulting surface elevation change largely determine the resilience of salt marshes to sea-level rise (SLR), the effect of livestock grazing on accretion rates has been little studied. Therefore, this study aimed to investigate the effect of livestock grazing on salt-marsh accretion rates. We hypothesise that accretion will be lower in grazed compared to ungrazed salt marshes. In four study sites along the mainland coast of the Wadden Sea (in the south-eastern North Sea), accretion rates, sediment deposition rates, and soil compaction of grazed and ungrazed marshes were analysed using the Cs-137 radionuclide dating method. Accretion rates were on average 11.6 mm yr(-1) during recent decades and thus higher than current and projected rates of SLR. Neither accretion nor sediment deposition rates were significantly different between grazing treatments. Meanwhile, soil compaction was clearly affected by grazing with significantly higher dry bulk density on grazed compared to ungrazed parts. Based on these results, we conclude that other factors influence whether grazing has an effect on accretion and sediment deposition rates and that the effect of grazing on marsh growth does not follow a direct causal chain. It may have a great importance when interacting with other biotic and abiotic processes on the marsh. Crown Copyright (C) 2013 Published by Elsevier Ltd. All rights reserved.</p>", "keywords": ["0106 biological sciences", "F800 - Physical geographical sciences", "550", "137Cs", "geochronology", "SEA-LEVEL RISE", "SURFACE ELEVATION", "01 natural sciences", "630", "Wadden Sea", "inundation", "CS-137", "F820 Geomorphology", "(CS)-C-137", "compaction", "NITROGEN MINERALIZATION", "COASTAL WETLANDS", "0105 earth and related environmental sciences", "land use management", "WADDEN SEA", "15. Life on land", "NORTH-SEA", "13. Climate action", "C180 - Ecology", "TIDAL MARSH", "VEGETATION", "C180 Ecology", "dating", "SW NETHERLANDS"]}, "links": [{"href": "https://doi.org/10.1016/j.ecss.2013.10.026"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Estuarine%2C%20Coastal%20and%20Shelf%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.ecss.2013.10.026", "name": "item", "description": "10.1016/j.ecss.2013.10.026", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.ecss.2013.10.026"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2013-12-01T00:00:00Z"}}, {"id": "10.1016/j.geoderma.2015.03.024", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-07-27T16:16:46Z", "type": "Journal Article", "created": "2015-04-08", "title": "Decomposition Of Beech (Fagus Sylvatica) And Pine (Pinus Nigra) Litter Along An Alpine Elevation Gradient: Decay And Nutrient Release", "description": "Litter decomposition is an important process for cycling of nutrients in terrestrial ecosystems. The objective of this study was to evaluate direct and indirect effects of climate on litter decomposition along an altitudinal gradient in a temperate Alpine region. Foliar litter of European beech (Fagus sylvatica) and Black pine (Pinus nigra) was incubated in litterbags during two years in the Hochschwab massif of the Northern Limestone Alps of Austria. Eight incubation sites were selected following an altitudinal/climatic transect from 1900 to 900\u00a0m\u00a0asl. The average remaining mass after two years of decomposition amounted to 54% (beech) and 50% (pine). Net release of N, P, Na, Al, Fe and Mn was higher in pine than in beech litter due to high immobilization (retention) rates of beech litter. However, pine litter retained more Ca than beech litter. Altitude retarded decay (mass loss and associated C release) in beech litter during the first year only but had a longer lasting effect on decaying pine litter. Altitude comprises a suite of highly auto-correlated characteristics (climate, vegetation, litter, soil chemistry, soil microbiology, snow cover) that influence litter decomposition. Hence, decay and nutrient release of incubated litter is difficult to predict by altitude, except during the early stage of decomposition, which seemed to be controlled by climate. Reciprocal litter transplant along the elevation gradient yielded even relatively higher decay of pine litter on beech forest sites after a two-year adaptation period of the microbial community.", "keywords": ["Pinus nigra", "0106 biological sciences", "Decomposition", "Fagus sylvatica", "Soil Science", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "Article", "Climosequence", "13. Climate action", "Elevation gradient", "0401 agriculture", " forestry", " and fisheries", "Litterbag"]}, "links": [{"href": "https://doi.org/10.1016/j.geoderma.2015.03.024"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Geoderma", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.geoderma.2015.03.024", "name": "item", "description": "10.1016/j.geoderma.2015.03.024", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.geoderma.2015.03.024"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2015-08-01T00:00:00Z"}}, {"id": "10.1029/2024GB008367", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:18:15Z", "type": "Journal Article", "created": "2025-04-05", "title": "Insect Herbivory Releases More Nutrients in Warmer and Drier Forests", "description": "Abstract<p>Climate, forest successional stage, and soil substrate age can alter herbivore communities and their effects on biogeochemical cycling, but the size and spatial variability of these effects are poorly quantified. To address this knowledge gap, we established a globally distributed network of 50 broadleaved old\uffe2\uff80\uff90growth forests across six continents, encompassing well\uffe2\uff80\uff90constrained local\uffe2\uff80\uff90scale gradients in mean annual temperature (MAT), mean annual precipitation (MAP), succession, and soil substrate age. We used this network to investigate how these variables impact insect foliar herbivory and the associated carbon, nitrogen, phosphorus, and silica fluxes in forest ecosystems. Over 1 to 2\uffc2\uffa0years, we measured stand\uffe2\uff80\uff90level foliar biomass production, leaf\uffe2\uff80\uff90level herbivory, and foliar element concentrations. At the global scale, insect herbivores liberated higher amounts of elements from the canopies of warmer and drier sites than those of cooler and wetter sites with patterns for phosphorus being most pronounced. MAT exerted a stronger influence over insect\uffe2\uff80\uff90mediated element fluxes than MAP. Foliar biomass production and leaf\uffe2\uff80\uff90level herbivory responses to MAT and MAP were mainly responsible for the observed changes in insect\uffe2\uff80\uff90mediated element fluxes; we also observed minor effects of foliar phosphorus concentration on phosphorus fluxes. Local\uffe2\uff80\uff90scale trends were mixed and successional stage or soil substrate age did not appear to influence insect herbivore\uffe2\uff80\uff90mediated element fluxes. These results demonstrate that climate effects on plant\uffe2\uff80\uff90herbivore interactions are stronger at large than small scales, at which herbivory rates and nutrient fluxes appear to be more strongly affected by a diversity of non\uffe2\uff80\uff90climate factors.</p", "keywords": ["Skogsvetenskap", "Forest Science", "primary forest", "folivory", "silicon", "elevation gradient", "nutrient cycling", "chronosequence", "Climate Science", "Klimatvetenskap"], "contacts": [{"organization": "Bernice C. Hwang, Christian P. Giardina, M. Noelia Barrios\u2010Garcia, Haoyu Diao, Virginia Gisela Duboscq\u2010Carra, Andreas Hemp, Claudia Hemp, Mylthon Jim\u00e9nez\u2010Castillo, Paulina Lobos\u2010Catal\u00e1n, Levan Mumladze, Ana C. Palma, Ion Catalin Petritan, Mariano A. Rodriguez\u2010Cabal, Tommi Andersson, Kainana S. Francisco, Shelley A. Gage, Giorgi Iankoshvili, Seana K. Walsh, Daniel B. Metcalfe,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1029/2024GB008367"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Biogeochemical%20Cycles", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1029/2024GB008367", "name": "item", "description": "10.1029/2024GB008367", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1029/2024GB008367"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-04-01T00:00:00Z"}}, {"id": "10.1029/2024gb008367", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:18:15Z", "type": "Journal Article", "created": "2025-04-04", "title": "Insect Herbivory Releases More Nutrients in Warmer and Drier Forests", "description": "Abstract<p>Climate, forest successional stage, and soil substrate age can alter herbivore communities and their effects on biogeochemical cycling, but the size and spatial variability of these effects are poorly quantified. To address this knowledge gap, we established a globally distributed network of 50 broadleaved old\uffe2\uff80\uff90growth forests across six continents, encompassing well\uffe2\uff80\uff90constrained local\uffe2\uff80\uff90scale gradients in mean annual temperature (MAT), mean annual precipitation (MAP), succession, and soil substrate age. We used this network to investigate how these variables impact insect foliar herbivory and the associated carbon, nitrogen, phosphorus, and silica fluxes in forest ecosystems. Over 1 to 2\uffc2\uffa0years, we measured stand\uffe2\uff80\uff90level foliar biomass production, leaf\uffe2\uff80\uff90level herbivory, and foliar element concentrations. At the global scale, insect herbivores liberated higher amounts of elements from the canopies of warmer and drier sites than those of cooler and wetter sites with patterns for phosphorus being most pronounced. MAT exerted a stronger influence over insect\uffe2\uff80\uff90mediated element fluxes than MAP. Foliar biomass production and leaf\uffe2\uff80\uff90level herbivory responses to MAT and MAP were mainly responsible for the observed changes in insect\uffe2\uff80\uff90mediated element fluxes; we also observed minor effects of foliar phosphorus concentration on phosphorus fluxes. Local\uffe2\uff80\uff90scale trends were mixed and successional stage or soil substrate age did not appear to influence insect herbivore\uffe2\uff80\uff90mediated element fluxes. These results demonstrate that climate effects on plant\uffe2\uff80\uff90herbivore interactions are stronger at large than small scales, at which herbivory rates and nutrient fluxes appear to be more strongly affected by a diversity of non\uffe2\uff80\uff90climate factors.</p", "keywords": ["Skogsvetenskap", "Forest Science", "primary forest", "folivory", "silicon", "elevation gradient", "nutrient cycling", "chronosequence", "Climate Science", "Klimatvetenskap"]}, "links": [{"href": "https://doi.org/10.1029/2024gb008367"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Biogeochemical%20Cycles", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1029/2024gb008367", "name": "item", "description": "10.1029/2024gb008367", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1029/2024gb008367"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-04-01T00:00:00Z"}}, {"id": "10.1088/2752-664x/ac706a", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:19:02Z", "type": "Journal Article", "created": "2022-05-17", "title": "Spartina alterniflora has the highest methane emissions in a St. Lawrence estuary salt marsh", "description": "Abstract                <p>Salt marshes have the ability to store large amounts of \uffe2\uff80\uff98blue carbon\uffe2\uff80\uff99, potentially mitigating some of the effects of climate change. Salt marsh carbon storage may be partially offset by emissions of CH4, a highly potent greenhouse gas. Sea level rise and invasive vegetation may cause shifts between different elevation and vegetation zones in salt marsh ecosystems. Elevation zones have distinct soil properties, plant traits and rhizosphere characteristics, which affect CH4 fluxes. We investigated differences in CH4 emissions between four elevation zones (mudflat, Spartina alterniflora, Spartina patens and invasive Phragmites australis) typical of salt marshes in the northern Northwest Atlantic. CH4 emissions were significantly higher from the S. alterniflora zone (17.7 \uffc2\uffb1 9.7 mg C m\uffe2\uff88\uff922h\uffe2\uff88\uff921) compared to the other three zones, where emissions were negligible (&lt;0.3 mg C m\uffe2\uff88\uff922h\uffe2\uff88\uff921). These emissions were high for salt marshes and were similar to those typically found in oligohaline marshes with lower salinities. CH4 fluxes were significantly correlated with soil properties (salinity, water table depth, bulk density and temperature), plant traits (rhizome volume and biomass, root volume and dead biomass volume all at 0\uffe2\uff80\uff9315 cm) and CO2 fluxes. The relationships between CH4 emissions, and rhizome and root volume suggest that the aerenchyma tissues in these plants may be a major transport mechanism of CH4 from anoxic soils to the atmosphere. This may have major implications for the mitigation potential carbon sink from salt marshes globally, especially as S. alterniflora is widespread. This study shows CH4 fluxes can vary over orders of magnitude from different vegetation in the same system, therefore, specific emissions factors may need to be used in future climate models and for more accurate carbon budgeting depending on vegetation type.</p>", "keywords": ["13. Climate action", "salt marsh", " methane", " elevation zone", " spartina alterniflora", " spartina patens", " mudflat", " phragmites australis", " quebec", " st lawrence river", "15. Life on land", "6. Clean water"]}, "links": [{"href": "https://doi.org/10.1088/2752-664x/ac706a"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Environmental%20Research%3A%20Ecology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1088/2752-664x/ac706a", "name": "item", "description": "10.1088/2752-664x/ac706a", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1088/2752-664x/ac706a"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-08-30T00:00:00Z"}}, {"id": "10.1111/ddi.13146", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:19:20Z", "type": "Journal Article", "created": "2020-09-02", "title": "Shifting aspect or elevation? The climate change response of ectotherms in a complex mountain topography", "description": "AbstractAim<p>Climate change is expected to cause mountain species to shift their ranges to higher elevations. Due to the decreasing amounts of habitats with increasing elevation, such shifts are likely to increase their extinction risk. Heterogeneous mountain topography, however, may reduce this risk by providing microclimatic conditions that can buffer macroclimatic warming or provide nearby refugia. As aspect strongly influences the local microclimate, we here assess whether shifts from warm south\uffe2\uff80\uff90exposed aspects to cool north\uffe2\uff80\uff90exposed aspects in response to climate change can compensate for an upward shift into cooler elevations.</p>Location<p>Switzerland, Swiss Alps.</p>Methods<p>We built ensemble distribution models using high\uffe2\uff80\uff90resolution climate data for two mountain\uffe2\uff80\uff90dwelling viviparous ectotherms, the Alpine salamander and the Common lizard, and projected them into various future scenarios to gain insights into distributional changes. We further compared elevation and aspect (northness) of current and predicted future locations to analyse preferences and future shifts.</p>Results<p>Future ranges were consistently decreasing for the lizard, but for the salamander they were highly variable, depending on the climate scenario and threshold rule. Aspect preferences were elevation\uffe2\uff80\uff90dependent: warmer, south\uffe2\uff80\uff90exposed microclimates were clearly preferred at higher compared to lower elevations. In terms of presence and future locations, we observed both elevational upward shifts and northward shifts in aspect. Under future conditions, the shift to cooler north\uffe2\uff80\uff90exposed aspects was particularly pronounced at already warmer lower elevations.</p>Main conclusions<p>For our study species, shifts in aspect and elevation are complementary strategies to mitigate climatic warming in the complex mountain topography. This complements the long\uffe2\uff80\uff90standing view of elevational upward shift being their only option to move into areas with suitable future climate. High\uffe2\uff80\uff90resolution climate data are critical in heterogeneous environments to identify microrefugia and thereby improving future impact assessments of climate change.</p>", "keywords": ["0106 biological sciences", "0301 basic medicine", "570", "4290733-0", "elevation", "aspect", "Modellierung", "4077275-5", "ddc:900", "01 natural sciences", "4128128-7", "10127 Institute of Evolutionary Biology and Environmental Studies", "03 medical and health sciences", "4170297-9", "Schweizer Alpen", "Anthropogene Klima\u00e4nderung", "Wechselwarme", "aspect; climate change; ectotherms; microrefugia; mountain topography; Salamandra atra; species distribution modelling; Switzerland; thresholds; Zootoca vivipara", "4189352-9", "shift", "15. Life on land", "reptile", "1105 Ecology", " Evolution", " Behavior and Systematics", "climate change", "Geschichte und Geografie", "900", "13. Climate action", "Anpassung", "570 Life sciences; biology", "590 Animals (Zoology)", "amphibian", "[SDE.BE]Environmental Sciences/Biodiversity and Ecology"]}, "links": [{"href": "https://air.unimi.it/bitstream/2434/785568/2/feldmeier%202020%20divers%20distrib.pdf"}, {"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1111/ddi.13146"}, {"href": "https://doi.org/10.1111/ddi.13146"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Diversity%20and%20Distributions", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/ddi.13146", "name": "item", "description": "10.1111/ddi.13146", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/ddi.13146"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-08-26T00:00:00Z"}}, {"id": "10.1111/avsc.12195", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:19:20Z", "type": "Journal Article", "created": "2015-08-21", "title": "What Factors Determined Restoration Success Of A Salt Marsh Ten Years After De-Embankment?", "description": "AbstractQuestions<p>How successful was the restoration of a salt marsh at a former summer polder on the mainland coast of the Dutch Wadden Sea 10\uffc2\uffa0yr after de\uffe2\uff80\uff90embankment? What were the most important factors determining the level of restoration success?</p>Location<p>Noard\uffe2\uff80\uff90Frysl\uffc3\uffa2n B\uffc3\uffbbtendyks, northwest Netherlands.</p>Methods<p>The frequencies of target plant species were recorded before de\uffe2\uff80\uff90embankment and monitored thereafter (1, 2, 3, 4, 6 and 10\uffc2\uffa0yr later) using permanent transects. Vegetation change was monitored using repeated mapping 14\uffc2\uffa0yr before and 1, 7 and 10\uffc2\uffa0yr after de\uffe2\uff80\uff90embankment. A large\uffe2\uff80\uff90scale factorial experiment with 72 sampling plots was set up to determine the effects of distance to a breach point, distance to a creek and grazing treatment on species composition. Abiotic data were also collected from the permanent transects and sampling plots on elevation, soil salinity and redox potential.</p>Results<p>Ten years after de\uffe2\uff80\uff90embankment, permanent transect data showed that 78% to 96% of the target species were found at the restoration site. Vegetation mapping, however, showed that the diversity of salt marsh communities was low, with 50% of the site covered by the secondary pioneer marsh community. A multivariate analogue of ANOVA indicated that the most important experimental factor determining species composition was the interaction between distance to the nearest creek and livestock grazing. The combination of proximity to a creek and exclusion from livestock grazing always resulted in development of the high marsh community. In contrast, the combination of being located far from a creek, grazed and situated at low elevation with accompanying high salinity resulted in development of the secondary pioneer marsh community.</p>Conclusions<p>Using target species as criteria, restoration success could be claimed 10\uffc2\uffa0yr after de\uffe2\uff80\uff90embankment. However, the diversity of communities in the salt marsh was lower than desired. Variable grazing regimes should be applied to high\uffe2\uff80\uff90elevation areas to prevent dominance by single species of tall grasses and to promote formation of vegetation mosaics. Low\uffe2\uff80\uff90elevation areas need lower grazing pressure. Also, an adequate soil drainage network should be preserved or constructed in low\uffe2\uff80\uff90elevation areas before de\uffe2\uff80\uff90embankment.</p>", "keywords": ["0106 biological sciences", "Salinity", "LAND", "Managed realignment", "Artificial saltmarsh", "NETHERLANDS", "Soil redox", "WADDEN SEA", "Soil drainage", "15. Life on land", "01 natural sciences", "6. Clean water", "Long-term study", "COLONIZATION", "Grazing", "Halophytes", "Elevation", "14. Life underwater", "MANAGED REALIGNMENT", "ELEVATION", "SCALE"], "contacts": [{"organization": "R.M. Veeneklaas, Petra Daniels, Jan P. Bakker, E. R. Chang, Peter Esselink,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1111/avsc.12195"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Applied%20Vegetation%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/avsc.12195", "name": "item", "description": "10.1111/avsc.12195", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/avsc.12195"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2015-08-20T00:00:00Z"}}, {"id": "10.3390/f5040620", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:21:48Z", "type": "Journal Article", "created": "2014-04-04", "title": "Carbon Stocks And Climate Change: Management Implications In Northern Arizona Ponderosa Pine Forests", "description": "<p>Researchers have observed climate-driven shifts of forest types to higher elevations in the Southwestern US and predict further migration coupled with large-scale mortality events proportional to increases in radiative forcing. Range contractions of forests are likely to impact the total carbon stored within a stand. This study examines the dynamics of Pinus ponderosa stands under three climate change scenarios in Northern Arizona using the Climate Forest Vegetation Simulator (Climate-FVS) model to  project changes in carbon pools. A sample of 90 stands were grouped according to three elevational ranges; low- (1951 to 2194 m), mid- (2194 to 2499 m), and high- (2499 to  2682 m.) elevation stands. Growth, mortality, and carbon stores were simulated in the  Climate-FVS over a 100 year timespan. We further simulated three management scenarios for each elevational gradient and climate scenario. Management included (1) a  no-management scenario, (2) an intensive-management scenario characterized by thinning from below to a residual basal area (BA) of 18 m2/ha in conjunction with a prescribed burn every 10 years, and (3) a moderate-management scenario characterized by a  thin-from-below treatment to a residual BA of 28 m2/ha coupled with a prescribed burn every 20 years. Results indicate that any increase in aridity due to climate change will produce substantial mortality throughout the elevational range of ponderosa pine stands, with lower elevation stands projected to experience the most devastating effects. Management was only effective for the intensive-management scenario; stands receiving this treatment schedule maintained moderately consistent levels of basal area and demonstrated a higher level of resilience to climate change relative to the two other management scenarios. The results of this study indicate that management can improve  resiliency to climate change, however, resource managers may need to employ more intensive thinning treatments than currently proposed to achieve the best results.</p>", "keywords": ["0106 biological sciences", "0301 basic medicine", "2. Zero hunger", "03 medical and health sciences", "QC Physics", "13. Climate action", "SD Forestry", "climate forest vegetation simulator; climate change and elevation; forest carbon stores; forest management and climate change; climate-driven forest mortality; representative concentration pathways", "15. Life on land", "01 natural sciences"], "contacts": [{"organization": "Bagdon, Benjamin, Huang, Ching-Hsun,", "roles": ["creator"]}]}, "links": [{"href": "http://www.mdpi.com/1999-4907/5/4/620/pdf"}, {"href": "https://openknowledge.nau.edu/id/eprint/684/1/Bagdon_B_Ching-Hsun_H_2014_Carbon_stocks_climate_change.pdf"}, {"href": "https://doi.org/10.3390/f5040620"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Forests", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3390/f5040620", "name": "item", "description": "10.3390/f5040620", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3390/f5040620"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2014-04-04T00:00:00Z"}}, {"id": "10.1594/pangaea.884151", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-07-27T16:20:34Z", "type": "Dataset", "title": "Radium data in the Lena Delta collected in summer 2013 on board RV Dalnie Zelentsy", "description": "Open AccessActivities of excess 224Ra, 226Ra and 228Ra in water samples collected in September 2013 during the 'Lena Delta 2013' hydrological survey expedition on board RV Dalnie Zelentsy (Gon\u00e7alves-Araujo et al., 2015, doi:10.3389/fmars.2015.00108).", "keywords": ["RU Land_2013_Lena", "Salinity", "Radium 226", "Radium 228", "Marine Geochemistry AWI AWI_MarGeoChem", "water", "Marine Geochemistry @ AWI (AWI_MarGeoChem)", "Radium-226", "Gamma spectroscopy", "DATE TIME", "Radium-224 excess", "14. Life underwater", "ELEVATION", "LONGITUDE", "DEPTH", " water", "Volume", "Multiple investigations", "RaDeCC", "Event label", "AWI Arctic Land Expedition", "Radium-226", " standard deviation", "6. Clean water", "Radium 224 excess", "Radium-228", "DATE/TIME", "13. Climate action", "DEPTH", "Earth System Research", "LATITUDE", "Conductivity meter", "RU-Land_2013_Lena", "Radium-228", " standard deviation", "Radium-224 excess", " standard deviation", "standard deviation", "Station label"], "contacts": [{"organization": "Rutgers van der Loeff, Michiel M", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1594/pangaea.884151"}, {"rel": "self", "type": "application/geo+json", "title": "10.1594/pangaea.884151", "name": "item", "description": "10.1594/pangaea.884151", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1594/pangaea.884151"}, {"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": "10.1594/pangaea.963212", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:20:35Z", "type": "Dataset", "title": "Stream water chemistry and landscape characteristics in Zackenberg Valley, NE Greenland summer 2021", "description": "The data contains water chemistry and spectral catchment NDVI for 14 streams in Zackenberg Valley in Northeast Greenland, sampled summer 2021 from 10th July to 15th September. We collected water samples for measuring water chemistry, and we determined landscape parameters using GIS based tools. The data was collected at three sampling periods in summer 2021 in the Zackenberg Research Station (74\u00b028'N, 20\u00b034'W). The area has a polar tundra climate with mean annual air temperature of -9.1 \u00b0C. Water chemistry (i.e. dissolved and particulate nitrogen, phosphorus, carbon; dissolved iron and silicate) and catchment characteristics (i.e. catchment area, altitude, slope, aspect, NDVI, snow cover) was measured for each of the 14 stream sites. Water chemistry samples were collected and analyzed using standard methods, and landscape characteristics were determined using GIS resources. The data was collected in order to study relationships between landscape characteristics and stream water chemistry. The water samples were collected by a team of two people, and the detailed methods are given below.", "keywords": ["inorganic", "median", "Nitrate Nitrogen", "Nitrogen", " inorganic", " dissolved/Nitrogen", " total dissolved ratio", "Nitrate", "Normalized Difference Vegetation Index", "Latitude of event", "Inductively Coupled Plasma Mass Spectrometry ICP MS", "Arctic", "Temperature", " water", "WTW", "Total organic carbon analyzer TOC VCPH TNM 1", "Total organic carbon analyzer (TOC-VCPH/TNM-1)", " Shimadzu", "Calculated", "dissolved ratio", "Nitrate/Nitrogen", " inorganic", " dissolved ratio", "total dissolved ratio", "Multiple investigations", "Temperature", "Nitrogen", " total dissolved", "Month", "dissolved", "specific", "streams", "6. Clean water", "Nitrogen", " inorganic", " dissolved", "Chemistry", "Inductively Coupled Plasma - Mass Spectrometry (ICP-MS)", " PerkinElmer Instruments", " Optima 2000 DV", "Sum cations", "Natural Sciences", "Ammonium", "Potassium Silicon ratio", "Calcium Magnesium ratio", "Conductivity Meter", " WTW", " ProfiLine Cond 3110", "Longitude of event", "Silicon", "Lachat QuickChem 8500 flow injection autoanalyser", "Nitrogen", "organic", "water chemistry", "Iron", "Calcium/Magnesium ratio", "water", "Site", "Nitrate/Ammonium ratio", "Aspect", "Normalized Differenced Vegetation Index", " median", "Ammonium Nitrogen", "Normalized Differenced Vegetation Index", "Catchment area", "Slope", "PerkinElmer Instruments", "ProfiLine Cond 3110", "Shimadzu", "Date/Time of event", "Conductivity Meter", "Nitrate Ammonium ratio", "total dissolved", "Conductivity", "Event label", "Date Time of event", "Nitrogen", " inorganic", " dissolved/Nitrogen", " organic", " dissolved ratio", "15. Life on land", "Carbon", " organic", " dissolved", "dissolved Nitrogen", "Elevation of event", "Carbon", "rivers", "Snow coverage", "Greening", "Potassium/Silicon ratio", "Optima 2000 DV", "Nitrogen", " organic", " dissolved", "13. Climate action", "Discharge", "Conductivity", " specific", "Ammonium/Nitrogen", " inorganic", " dissolved ratio"], "contacts": [{"organization": "Riis, Tenna, Tank, Jennifer, Holmboe, Cecilie Marie Hartvig, Gim\u00e9nez-Grau, Pau, Mastepanov, Mikhail, Catalan, Nuria, Stott, David, Hansen, Birgitte, Kristiansen, S\u00f8ren M, Pastor, Ada,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1594/pangaea.963212"}, {"rel": "self", "type": "application/geo+json", "title": "10.1594/pangaea.963212", "name": "item", "description": "10.1594/pangaea.963212", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1594/pangaea.963212"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-01-01T00:00:00Z"}}, {"id": "10.1594/pangaea.972409", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:20:35Z", "type": "Dataset", "title": "Organic carbon content, stable carbon isotope ratios, and lignin phenol fingerprint of terrestrial material deposited at the paleo-delta of the Lena River at the transition to the Preboreal", "description": "The dataset was used to reconstruct the release of permafrost organic carbon from the watershed of the Lena River (Russia) between 11.1 and 11.7 calibrated thousand years Before Present (cal. kyr BP, Present = 1950 AD) and to model potential methane emissions from this carbon source. Data were obtained analyzing plant debris isolated from the low density fraction (&lt;1.8 g/cm3) of muddy sediments from the Piston Core 23 (PC23). The sediment core was retrieved in July 2014 in the mid/outer-shelf of the Laptev Sea shelf (76\u00b0 10' 15.6''N; 129\u00b0 20' 13.2''E, water depth of 56 m) during Leg 1 of the SWERUS-C3 expedition (Swedish-Russian-U.S. Arctic Ocean \u2013 Investigation of Climate-Cryosphere-Carbon interactions). Measurement of total organic carbon (TOC) and stable (d\u00b9\u00b3C) carbon isotopes were performed on 0.3 to 0.7 mg of samples on February 2022 using a Thermo DeltaQ isotope-ratio mass spectrometer (IRMS) coupled to a Thermo Flash 2000 Elemental Analyzer via a ConFlo IV interface at the at the Institute of Polar Sciences from the National Research Council of Italy (Bologna Section, Italy). The methodology for sample preparation followed Nieuwenhuize et al. (1994). Data on biomarkers (lignin phenols) were obtained extracting 2 to 3 mg of samples using a Microwave Accelerated Reaction System (MARS) 5 from CEM and following the methodology from Go\u00f1i &amp; Montgomery (2000). The extracts were analysed using a Agilent 7890A gas chromatograph (GC) coupled to an Agilent 5975C mass spectrometer to identify and quantify the compounds of interest. Biomarkers extraction and analyses were carried out on March 2022 in the organic chemistry laboratories of the Ente Nazionale Idrocarburi (ENI)-National Research Council (CNR) of Italy Joint Research Center 'Aldo Pontremoli' (Lecce, Italy). Stable isotope ratios and biomarkers were used to gain insights on the main vegetation source of the plant debris and (biomarkers only) to investigate the degradation state of the terrestrial material.", "keywords": ["5 dihydroxybenzoic acid per unit mass organic carbon", "p Coumaric acid per unit mass organic carbon", "SWERUS C3", "p-Hydroxybenzaldehyde per unit mass organic carbon", "Permafrost", "p Hydroxybenzaldehyde per unit mass organic carbon", "Latitude of event", "Arctic", "Gas chromatography (GC", " Agilent 7890A) equipped with a mass selective detector (MSD", " Agilent 5975C) and a flame ionization detector (FID", " Agilent 7683B)", "p-Hydroxybenzoic acid per unit mass organic carbon", "p-Hydroxyacetophenone/p-hydroxyl phenols ratio", "bottom maximum", "top min", "total", "Sample code/label", "p-Coumaric acid per unit mass organic carbon", "Vanillic acid vanillin ratio", "Deglaciation", "p-Hydroxyl phenols/vanillyl phenols ratio", "Depth", " sediment/rock", " bottom/maximum", "Syringic acid per unit mass organic carbon", "p-Hydroxyl phenols per unit mass organic carbon", "Sample code label", "p Hydroxyl phenols per unit mass organic carbon", "Depth", " top/min", "Acetovanillone per unit mass organic carbon", "Vanillic acid per unit mass organic carbon", "p Hydroxybenzoic acid per unit mass organic carbon", "p Hydroxyacetophenone per unit mass organic carbon", "Vanillic acid/vanillin ratio", "sediment rock", "p Hydroxyl phenols vanillyl phenols ratio", "Syringyl phenols vanillyl phenols ratio", "Earth System Research", "\u03b413C", "Ferulic acid per unit mass organic carbon", "Syringaldehyde per unit mass organic carbon", "Vanillin per unit mass organic carbon", "Methane", "Piston corer", "Isotope ratio mass spectrometer", " Thermo", " DeltaQ; coupled to an Elemental Analyzer; Thermo Flash 2000 via a ConFlo IV", "Longitude of event", "Syringyl phenols per unit mass organic carbon", "organic", "Syringic acid/syringaldehyde ratio", "Cinnamyl phenols/vanillyl phenols ratio", "DEPTH", " sediment/rock", "5 dihydroxybenzoic acid vanillyl phenols ratio", "Oden", "Cinnamyl phenols vanillyl phenols ratio", "Agilent 7683B", "p-Hydroxyacetophenone per unit mass organic carbon", "Date/Time of event", "Acetosyringone per unit mass organic carbon", "3", "5-dihydroxybenzoic acid per unit mass organic carbon", "Depth", "Event label", "Date Time of event", "p Hydroxyacetophenone p hydroxyl phenols ratio", "Vanillyl phenols per unit mass organic carbon", "Elevation of event", "Syringyl phenols/vanillyl phenols ratio", "Agilent 5975C and a flame ionization detector FID", "Carbon", "Cinnamyl phenols per unit mass organic carbon", "Agilent 7890A equipped with a mass selective detector MSD", "DEPTH", "Syringic acid syringaldehyde ratio", "3", "5-dihydroxybenzoic acid/vanillyl phenols ratio", "Gas chromatography GC", "Thermo", "SWERUS-C3", "Isotope ratio mass spectrometer", "DeltaQ coupled to an Elemental Analyzer Thermo Flash 2000 via a ConFlo IV", "Carbon", " organic", " total"], "contacts": [{"organization": "Sabino, Mathia, Gustafsson, \u00d6rjan, Wild, Birgit, Semiletov, Igor P, Dudarev, Oleg V, Ingrosso, Gianmarco, Tesi, Tommaso,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1594/pangaea.972409"}, {"rel": "self", "type": "application/geo+json", "title": "10.1594/pangaea.972409", "name": "item", "description": "10.1594/pangaea.972409", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1594/pangaea.972409"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-01-01T00:00:00Z"}}, {"id": "10.1594/pangaea.972412", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:20:35Z", "type": "Dataset", "title": "Radiocarbon content and age of terrestrial material deposited at the paleo-delta of the Lena River at the transition to the Preboreal", "description": "The dataset was used to reconstruct the release of permafrost organic carbon from the watershed of the Lena River (Russia) between 11.1 and 11.7 calibrated thousand years Before Present (cal. kyr BP, Present = 1950 AD) and to model potential methane emissions from this carbon source. Data were obtained analyzing plant debris isolated from the low density fraction (&lt;1.8 g/cm3) of muddy sediments from the Piston Core 23 (PC23). The sediment core was retrieved in July 2014 in the mid/outer-shelf of the Laptev Sea shelf (76\u00b0 10' 15.6''N; 129\u00b0 20' 13.2''E, water depth of 56 m) during Leg 1 of the SWERUS-C3 expedition (Swedish-Russian-U.S. Arctic Ocean \u2013 Investigation of Climate-Cryosphere-Carbon interactions). Radiocarbon (\u00b9\u2074C) content measurements were performed on 4 to 7 mg of sample on May 2022 using the Continuous Flow Accelerator Mass Spectrometry (CFAMS) system at the National Ocean Sciences Accelerator Mass Spectrometry (NOSAMS) facility (Woods Hole Oceanographic Institution, Woods Hole, MA, USA). The \u00b9\u2074C content was used to calculate \u00b9\u2074C isotope ratios (D\u00b9\u2074C) and to reconstruct non-calibrated and calibrated \u00b9\u2074C ages of plant debris isolated from the sediment fraction with a density lower than 1.8 g/cm3. Additionally, D\u00b9\u2074C values were used to calculate the \u00b9\u2074C content of plant debris at time of sediment deposition (D\u00b9\u2074Ci) and the latter to obtain pre-depositional \u00b9\u2074C ages. The dataset allowed to reconstruct the age of the terrestrial plant material when deposited at the coring site and identify its provenance from within the permafrost OC pool (sub-surface soil within 1 m depth vs deep soil) after remobilization. The average pre-depositional \u00b9\u2074C age of plant debris was ultimately used to model methane emissions from relatively young permafrost organic carbon during the late deglaciation (ca. 10 to 15 cal. kyr BP).", "keywords": ["Piston corer", "SWERUS C3", "Longitude of event", "Age", " 14C", "\u039414C", "Fraction modern carbon", "Calendar age", "Permafrost", "DEPTH", " sediment/rock", "Latitude of event", "Oden", "Age", "Arctic", "AGE", "pre depositional", "bottom maximum", "top min", "Date/Time of event", "Calculated", "\u039414C", " initial", " error", "Fraction modern carbon", " error", "Sample code/label", "Deglaciation", "Depth", " sediment/rock", " bottom/maximum", "\u039414C", " error", "Age", " pre-depositional", " error", "Depth", "Event label", "Date Time of event", "Continuous Flow Accelerator Mass Spectrometry", "initial", "Sample code label", "Depth", " top/min", "Calendar age", " standard error", "Age", " error", "error", "Elevation of event", "sediment rock", "\u039414C", " initial", "14C", "standard error", "DEPTH", "Age", " pre-depositional", "Earth System Research", "SWERUS-C3", "Methane"], "contacts": [{"organization": "Sabino, Mathia, Gustafsson, \u00d6rjan, Wild, Birgit, Semiletov, Igor P, Dudarev, Oleg V, Ingrosso, Gianmarco, Tesi, Tommaso,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1594/pangaea.972412"}, {"rel": "self", "type": "application/geo+json", "title": "10.1594/pangaea.972412", "name": "item", "description": "10.1594/pangaea.972412", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1594/pangaea.972412"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-01-01T00:00:00Z"}}, {"id": "10.2307/2656979", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:21:20Z", "type": "Journal Article", "created": "2006-04-21", "title": "Genotypic Variation For Condensed Tannin Production In Trembling Aspen (Populs Tremuloides, Salicaceae) Under Elevated Co2 And In High- And Low-Fertility Soil", "description": "<p>The carbon/nutrient balance hypothesis suggests that leaf carbon to nitrogen ratios influence the synthesis of secondary compounds such as condensed tannins. We studied the effects of rising atmospheric carbon dioxide on carbon to nitrogen ratios and tannin production. Six genotypes of Populus tremuloides were grown under elevated and ambient CO2 partial pressure and high\uffe2\uff80\uff90 and low\uffe2\uff80\uff90fertility soil in field open\uffe2\uff80\uff90top chambers in northern lower Michigan, USA. During the second year of exposure, leaves were harvested three times (June, August, and September) and analyzed for condensed tannin concentration. The carbon/nutrient balance hypothesis was supported overall, with significantly greater leaf tannin concentration at high CO2 and low soil fertility compared to ambient CO2 and high soil fertility. However, some genotypes increased tannin concentration at elevated compared to ambient CO2, while others showed no CO2 response. Performance of lepidopteran leaf miner (Phyllonorycter tremuloidiella) larvae feeding on these plants varied across genotypes, CO2, and fertility treatments. These results suggest that with rising atmospheric CO2, plant secondary compound production may vary within species. This could have consequences for plant\uffe2\uff80\uff93herbivore and plant\uffe2\uff80\uff93microbe interactions and for the evolutionary response of this species to global climate change.</p>", "keywords": ["0106 biological sciences", "Salicaceae", "genotype", "plant\u2013herbivore interaction", "Phyllonorycter-tremuloidiella", "Quaking aspen", "01 natural sciences", "plant-composition", "tannin", "nitrogen-", "carbon-dioxide: elevation-", "124-38-9: CARBON DIOXIDE", "Spermatophytes-", "Spermatophyta-", "genotypic-variation", "Population-Genetics (Population-Studies)", "2. Zero hunger", "carbon-", "Climatology- (Environmental-Sciences)", "Angiosperms-", "Angiospermae-", "Plants-", "GLOBAL-ECOLOGY", "Populus-tremuloides", "plant-pests", "climate-change", "genetic-variation", "forest-trees", "condensed tannins", "Nitrogen", "Science", "Vascular-Plants", "carbon-dioxide-enrichment", "Nutrition-", "genotypes-", "Phyllonorycter tremuloidiella", "Populus-tremuloides [trembling-aspen] (Salicaceae-)", "soil-fertility", "Populus tremuloides", "Salicaceae-: Dicotyledones-", "Biology", "Plantae-", "global change", "tannins-", "condensed-tannin: production-", "foliage-", "forest-pests", "Tannic acid", "Metabolism-", "Botany", "carbon dioxide", "forest-soils", "15. Life on land", "Carbon", "climate-", "Carbon dioxide", "13. Climate action", "Dicots-", "insect-pests"], "contacts": [{"organization": "Donald R. Zak, Jennifer L Mansfield, Kurt S. Pregitzer, Kurt S. Pregitzer, Peter S. Curtis, Peter S. Curtis,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.2307/2656979"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/American%20Journal%20of%20Botany", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.2307/2656979", "name": "item", "description": "10.2307/2656979", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.2307/2656979"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "1999-08-01T00:00:00Z"}}, {"id": "10.2136/vzj2015.09.0131", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:21:13Z", "type": "Journal Article", "created": "2016-05-13", "title": "Modeling Soil Processes: Review, Key Challenges, and New Perspectives", "description": "Core Ideas<p><p>A community effort is needed to move soil modeling forward.</p><p>Establishing an international soil modeling consortium is key in this respect.</p><p>There is a need to better integrate existing knowledge in soil models.</p><p>Integration of data and models is a key challenge in soil modeling.</p></p><p>The remarkable complexity of soil and its importance to a wide range of ecosystem services presents major challenges to the modeling of soil processes. Although major progress in soil models has occurred in the last decades, models of soil processes remain disjointed between disciplines or ecosystem services, with considerable uncertainty remaining in the quality of predictions and several challenges that remain yet to be addressed. First, there is a need to improve exchange of knowledge and experience among the different disciplines in soil science and to reach out to other Earth science communities. Second, the community needs to develop a new generation of soil models based on a systemic approach comprising relevant physical, chemical, and biological processes to address critical knowledge gaps in our understanding of soil processes and their interactions. Overcoming these challenges will facilitate exchanges between soil modeling and climate, plant, and social science modeling communities. It will allow us to contribute to preserve and improve our assessment of ecosystem services and advance our understanding of climate\uffe2\uff80\uff90change feedback mechanisms, among others, thereby facilitating and strengthening communication among scientific disciplines and society. We review the role of modeling soil processes in quantifying key soil processes that shape ecosystem services, with a focus on provisioning and regulating services. We then identify key challenges in modeling soil processes, including the systematic incorporation of heterogeneity and uncertainty, the integration of data and models, and strategies for effective integration of knowledge on physical, chemical, and biological soil processes. We discuss how the soil modeling community could best interface with modern modeling activities in other disciplines, such as climate, ecology, and plant research, and how to weave novel observation and measurement techniques into soil models. We propose the establishment of an international soil modeling consortium to coherently advance soil modeling activities and foster communication with other Earth science disciplines. Such a consortium should promote soil modeling platforms and data repository for model development, calibration and intercomparison essential for addressing contemporary challenges.</p", "keywords": ["organic-matter dynamics", "550", "QH301 Biology", "0208 environmental biotechnology", "SATURATED-UNSATURATED FLOW", "02 engineering and technology", "soil processes", "01 natural sciences", "Physical Geography and Environmental Geoscience", "Sciences de la Terre", "ARBUSCULAR MYCORRHIZAL FUNGI", "sciences du sol", "ANZSRC::3707 Hydrology", "SYNTHETIC-APERTURE RADAR", "ANZSRC::4106 Soil sciences", "SDG 13 - Climate Action", "2. Zero hunger", "GROUND-PENETRATING RADAR", "diffuse-reflectance spectroscopy", "ANZSRC::050399 Soil Sciences not elsewhere classified", "synthetic-aperture radar", "digital elevation model", "SDG 13 \u2013 Ma\u00dfnahmen zum Klimaschutz", "MULTIPLE ECOSYSTEM SERVICES", "knowledge integration", "Crop and Pasture Production", "101028 Mathematical modelling", "570", "DIFFUSE-REFLECTANCE SPECTROSCOPY", "Environmental Engineering", "international soil modeling consortium", "0207 environmental engineering", "Soil Science", "[SDU.STU]Sciences of the Universe [physics]/Earth Sciences", "arbuscular mycorrhizal fungi", "soil science", "ORGANIC-MATTER DYNAMICS", "QH301", "ANZSRC::0503 Soil Sciences", "Life Science", "SEDIMENT TRANSPORT MODELS", "data integration", "sediment transport models", "approche ecosyst\u00e9mique", "mod\u00e9lisation", "0105 earth and related environmental sciences", "ground-penetrating radar", "info:eu-repo/classification/ddc/550", "soil modeling", "ANZSRC::080110 Simulation and Modelling", "ROOT WATER-UPTAKE", "15. Life on land", "multiple ecosystem services", "root water-uptake", "13. Climate action", "Earth and Environmental Sciences", "Soil Sciences", "[SDU.STU] Sciences of the Universe [physics]/Earth Sciences", "Earth Sciences", "101028 Mathematische Modellierung", "saturated-unsaturated flow", "root water-uptake", " sediment transport models", " diffuse-reflectance spectroscopy", " arbuscular mycorrhizal fungi", " multiple ecosystem services", " saturated-unsaturated flow", " ground-penetrating radar", " synthetic-aperture radar", " digital elevation model", " organic-matter dynamics.", "DIGITAL ELEVATION MODEL"]}, "links": [{"href": "http://onlinelibrary.wiley.com/wol1/doi/10.2136/vzj2015.09.0131/fullpdf"}, {"href": "https://escholarship.org/content/qt6976n34c/qt6976n34c.pdf"}, {"href": "https://doi.org/10.2136/vzj2015.09.0131"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Vadose%20Zone%20Journal", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.2136/vzj2015.09.0131", "name": "item", "description": "10.2136/vzj2015.09.0131", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.2136/vzj2015.09.0131"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2016-05-01T00:00:00Z"}}, {"id": "10.5061/dryad.rv15dv4gn", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:22:33Z", "type": "Dataset", "created": "2024-05-14", "title": "Variable species establishment in response to microhabitat indicates different likelihoods of climate-driven range shifts", "description": "Open Access<b>Abstract</b><br/><p>Climate change is causing geographic range shifts globally, and understanding the factors that influence species\u2019 range expansions is crucial for predicting future biodiversity changes. A common, yet untested, assumption in forecasting approaches is that species will shift beyond current range edges into new habitats as they become macroclimatically suitable, even though microhabitat variability could have overriding effects on local population dynamics. We aim to better understand the role of microhabitat in range shifts in plants through its impacts on establishment by Q1) examining microhabitat variability along large macroclimatic (i.e., elevational) gradients, Q2) testing which of these microhabitat variables explain plant recruitment and seedling survival, and Q3) predicting microhabitat suitability beyond species range limits. We transplanted seeds of 25 common tree, shrub, forb, and graminoid species across and beyond their current elevational ranges in the Washington Cascade Range, USA, along a large elevational gradient spanning a broad range of macroclimates. Over five years, we recorded recruitment, survival, and microhabitat (i.e., high resolution soil, air, and light) characteristics rarely measured in biogeographic studies. We asked whether microhabitat variables correlate with elevation, which variables drive species establishment, and whether microhabitat variables important for establishment are already suitable beyond leading range limits. We found that only 30% of microhabitat parameters covaried with elevation. We further observed extremely low recruitment and moderate seedling survival, and these were generally only weakly explained by microhabitat. Moreover, species and life stages responded in contrasting ways to soil biota, soil moisture, temperature, and snow duration. Microhabitat suitability predictions suggest that distribution shifts are likely to be species-specific, as different species have different suitability and availability of microhabitat beyond their present ranges, thus calling into question low-resolution macroclimatic projections that will miss such complexities. We encourage further research on species responses to microhabitat and including microhabitat in range shift forecasts.</p>", "keywords": ["soil composition", "seed transplant", "Cascades", "recruitment", "seedling survival", "FOS: Biological sciences", "microhabitat suitability", "Other", "Elevational gradient", "range shift"], "contacts": [{"organization": "Chardon, Nathalie Isabelle, McBurnie, Lauren, Goodwin, Katie, Pradhan, Kavya, Hille Ris Lambers, Janneke, Angert, Amy L.,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5061/dryad.rv15dv4gn"}, {"rel": "self", "type": "application/geo+json", "title": "10.5061/dryad.rv15dv4gn", "name": "item", "description": "10.5061/dryad.rv15dv4gn", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5061/dryad.rv15dv4gn"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-01-01T00:00:00Z"}}, {"id": "10.3390/rs13071346", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:21:59Z", "type": "Journal Article", "created": "2021-04-01", "title": "A Low-Rank Group-Sparse Model for Eliminating Mixed Errors in Data for SRTM1", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>The elimination of mixed errors is a key preprocessing technology for the area of digital elevation model data analysis, which is important for further applying data. We associated group sparsity with the low-rank uniqueness of local transformations of mixing errors to effectively remove mixing errors in data from Shuttle Radar Topography Mission 1 (SRTM 1) based on the sparseness of low-rank groups. First, the stripe-error structure that appeared globally in multiple directions was able to be better represented locally using group-sparse regularization and the uniqueness of the data in the low-rank direction of the local range and using variational ideas to constrain the gradient direction of the data to avoid redundant elimination. Second, the nonlocal self-similarity of the weighted kernel norm was used to remove random noise. Finally, the proposed model for eliminating mixed errors was solved using an algorithm based on the multiplier method of alternating direction. Experiments using simulated and real data found that the proposed low-rank group-sparse method (LRGS) eliminated mixed errors in both visual and quantitative evaluations better than the most recent processing methods and existing dataset products.</p></article>", "keywords": ["self-similarity", "digital elevation model", "Science", "Q", "0211 other engineering and technologies", "0202 electrical engineering", " electronic engineering", " information engineering", "group sparse", "02 engineering and technology", "mixed errors", "shuttle radar topography mission 1", "low-rank"]}, "links": [{"href": "http://www.mdpi.com/2072-4292/13/7/1346/pdf"}, {"href": "https://doi.org/10.3390/rs13071346"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Remote%20Sensing", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3390/rs13071346", "name": "item", "description": "10.3390/rs13071346", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3390/rs13071346"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-04-01T00:00:00Z"}}, {"id": "10.3390/s21092980", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:22:01Z", "type": "Journal Article", "created": "2021-04-25", "title": "Towards the Development and Verification of a 3D-Based Advanced Optimized Farm Machinery Trajectory Algorithm", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Efforts related to minimizing the environmental burden caused by agricultural activities and increasing economic efficiency are key contemporary drivers in the precision agriculture domain. Controlled Traffic Farming (CTF) techniques are being applied against soil compaction creation, using the on-line optimization of trajectory planning for soil-sensitive field operations. The research presented in this paper aims at a proof-of-concept solution with respect to optimizing farm machinery trajectories in order to minimize the environmental burden and increase economic efficiency. As such, it further advances existing CTF solutions by including (1) efficient plot divisions in 3D, (2) the optimization of entry and exit points of both plot and plot segments, (3) the employment of more machines in parallel and (4) obstacles in a farm machinery trajectory. The developed algorithm is expressed in terms of unified modeling language (UML) activity diagrams as well as pseudo-code. Results were visualized in 2D and 3D to demonstrate terrain impact. Verifications were conducted at a fully operational commercial farm (Rost\u011bnice, the Czech Republic) against second-by-second sensor measurements of real farm machinery trajectories.</p></article>", "keywords": ["Agriculture and Food Sciences", "2. Zero hunger", "Technology and Engineering", "controlled traffic farming", "Chemical technology", "mission planning", "TP1-1185", "04 agricultural and veterinary sciences", "Biochemistry", "Article", "Analytical Chemistry", "soil compaction", "Atomic and Molecular Physics", "digital elevation model", "AGRICULTURAL ROBOTS", "0401 agriculture", " forestry", " and fisheries", "Electrical and Electronic Engineering", "and Optics", "coverage path planning", "controlled traffic farming; coverage path planning; digital elevation model; mission planning; soil compaction"]}, "links": [{"href": "http://www.mdpi.com/1424-8220/21/9/2980/pdf"}, {"href": "https://www.mdpi.com/1424-8220/21/9/2980/pdf"}, {"href": "https://doi.org/10.3390/s21092980"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Sensors", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3390/s21092980", "name": "item", "description": "10.3390/s21092980", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3390/s21092980"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-04-23T00:00:00Z"}}, {"id": "10.5061/dryad.3xsj3txkf", "type": "Feature", "geometry": null, "properties": {"license": "unspecified", "updated": "2026-07-27T16:22:24Z", "type": "Dataset", "title": "The diversity of mycorrhiza-associated fungi and trees shape subtropical mountain forest ecosystem functioning", "description": "Aim: Mycorrhiza play key roles in ecosystem structure and functioning in  forests. However, how different mycorrhizal types influence mountain  forest biodiversity-ecosystem functioning relationships is largely  unknown. We evaluate how the diversity of distinct mycorrhiza-associated  fungi and trees shape forest carbon storage along elevational gradients.  Location: Gaoligong Mountains within Hengduan Mountains, Southwest China.  Taxon: Seed plants and mycorrhizal fungi. Methods: We used the data from  31 subtropical forest plots along elevational gradients on two aspects  (east and west) of the mountain. We quantified species richness of trees  and symbiotic fungi and assigned both to their mycorrhizal type  (arbuscular mycorrhiza (AM), ectomycorrhiza (EcM) and ericoid mycorrhiza  (ErM)). We then examined the diversity effects of mycorrhiza-associated  fungi and trees on above-ground carbon stored in trees and organic carbon  stored in soils. Results: Species richness was highest for AM trees  (79.5%), followed by ErM trees (13.4%) and then EcM trees (7.1%). Species  richness of AM-associated trees and fungi decreased with increasing  elevation, while ErM-associated trees and fungi showed an opposite trend.  EcM-associated diversity followed a hump-shaped relationship with  elevation. Positive relationships between diversity and above-ground  carbon were detected in all three mycorrhizal associations, but despite  low species number, canopy-dominating EcM trees comprised 64.4% of the  amount of above-ground carbon. Furthermore, community-weighted means of  height exhibited positive correlations with forest above-ground carbon,  indicating that positive selection effects occur. Soil organic carbon was  positively related to EcM-associated fungi diversity, above-ground carbon  mass and soil nitrogen availability, with the latter having the strongest  direct effects. Main conclusions: The distributions of forest biodiversity  and carbon storage can be modulated by distinct mycorrhizal fungi and  trees. Moreover, future global changes (e.g., climate warming,  intensifying nitrogen deposition) could alter the mycorrhizal-mediated  biodiversity-ecosystem functioning relationships in mountain forests.", "keywords": ["Ectomycorrhiza", "soil organic carbon", "13. Climate action", "arbuscular mycorrhiza", "FOS: Biological sciences", "elevational gradients", "14. Life underwater", "15. Life on land", "above-ground carbon", "functional diversity"], "contacts": [{"organization": "Luo, Ya-Huang, Ma, Liang-Liang, Seibold, Sebastian, Cadotte, Marc W., Burgess, Kevin, Tan, Shao-Lin, Ye, Lin-Jiang, Zheng, Wei, Zou, Jia-Yun, Chen, Zhi-Fa, Liu, De-Tuan, Zhu, Guang-Fu, Shi, Xiao-Chun, Zhao, Wei, Li, De-Zhu, Liu, Jie, Gao, Lian-Ming,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5061/dryad.3xsj3txkf"}, {"rel": "self", "type": "application/geo+json", "title": "10.5061/dryad.3xsj3txkf", "name": "item", "description": "10.5061/dryad.3xsj3txkf", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5061/dryad.3xsj3txkf"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-12-20T00:00:00Z"}}, {"id": "10.5061/dryad.h70rxwdqs", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:22:30Z", "type": "Dataset", "created": "2023-11-13", "title": "Data from: Microbial carbon use efficiency and soil organic carbon stocks across an elevational gradient in the Peruvian Andes", "description": "unspecifiedSoils of mountain ecosystems are one of the most vulnerable ecosystems to  climate change, while the ecosystem services they produce are significant  and currently at risk. High altitude soils contain high C stocks, but due  to difficult access to sites these areas are understudied. Moreover, how  the C and N cycling is changing in response to climate change in these  ecosystems, is still unclear. Microbial carbon use efficiency (CUE) and  its dependency on the environmental constraints along the altitudinal  gradients is one important unknown factor. Here we present results from an  altitudinal gradient study (3500 to 4500 m a.s.l.) from a Polylepis forest  in the Peruvian Andes. We measured the soil organic carbon (SOC) stocks  and microbial metabolic CUE by\u00a013C glucose tracing and microbial  resource use efficiency (CUEC:N) based on enzyme activity measurements. We  expected to find an increase in SOC stock, microbial nutrient limitations,  and lower CUE with elevation. SOC stocks depended on soil development and  followed a unimodal curve that peaks at 4000 m in two of the three studied  valleys. Neither 13CUE nor CUEC:N changed significantly with altitude.  Soil C:N ratio, \u03b2-glucosidase, chitinase, and phosphatase enzyme  activities increased with elevation, but peroxidase activity decreased  with elevation. We suggest that more labile organic matter left at high  elevation could compensate for the increasing nutrient limitation at high  elevation, resulting in no noticeable change in CUE with elevation.", "keywords": ["soil organic carbon", "Exoenzyme", "Carbon use efficiency", "FOS: Earth and related environmental sciences", "Stoichiometric modelling", "Elevational gradient"], "contacts": [{"organization": "Martin Vivanco, Angela Katherine, Sieti\u00f6, Outi-Maaria, Meyer, Nele, Mganga, Kevin, Kalu, Subin, Adamczyk, Sylwia, Celis, Susan, Alegre, Julio, Karhu, Kristiina,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5061/dryad.h70rxwdqs"}, {"rel": "self", "type": "application/geo+json", "title": "10.5061/dryad.h70rxwdqs", "name": "item", "description": "10.5061/dryad.h70rxwdqs", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5061/dryad.h70rxwdqs"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-12-18T00:00:00Z"}}, {"id": "10.5281/zenodo.13374006", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:23:19Z", "type": "Dataset", "title": "Microbial biomass and water-extractable carbon on Mt. Kilimanjaro", "description": "This dataset presents the value of microbial biomass carbon (MBC) and water-extractable carbon (WOC) at study plots under KiLi project.  Microbial biomass carbon (MBC) and water-extractable organic carbon (WOC) \u2013 as sensitive and important parameters for soil fertility and C turnover \u2013 are strongly affected by land-use changes all over the world. These effects are particularly distinct upon conversion of natural to agricultural ecosystems due to very fast carbon (C) and nutrient cycles and high vulnerability, especially in the tropics. The objective of this study was to use the unique advantage of Mt. Kilimanjaro \u2013 altitudinal gradient leading to different tropical ecosystems but developed all on the same soil parent material \u2013 to investigate the effects of land-use change and elevation on MBC and WOC contents during a transition phase from dry to wet season. Down to a soil depth of 50\u00a0cm, we compared MBC and WOC contents of 2 natural (Ocotea\u00a0and\u00a0Podocarpus forest), 3 seminatural (lower montane forest, grassland, savannah), 1 sustainably used (homegarden) and 2 intensively used (maize field, coffee plantation) ecosystems on an elevation gradient from 950 to 2850\u00a0m a.s.l.  The KiLi project (2010-2018) is a German Science Foundation (DFG) funded research unit (DFG research unit FOR1246) that focuses on biodiversity and ecosystem processes along altitudinal and disturbance gradients on Mt. Kilimanjaro (Tanzania, Africa), capitalizing on its world-wide unique range of climatic and vegetation zones. The research unit comprises 2 central projects and 7 subprojects from various disciplines. On a total of 60 study sites in both natural and human-disturbed ecosystems biodiversity (e.g. plants, soil arthropods, ants, bees, frogs, lizards, bats, birds), related ecosystem processes (decomposition, seed dispersal, pollination, herbivory, predation), and biogeochemical processes and properties of ecosystems (climate, soil properties and nutrient status, regulation of water and carbon fluxes, trace gas emissions, primary productivity, functional diversity) are analyzed.", "keywords": ["land-use change", "microbial carbon dynamics", "tropical ecosystem", "andosol", "elevation gradient", "water-extractable carbon"]}, "links": [{"href": "https://doi.org/10.5281/zenodo.13374006"}, {"rel": "self", "type": "application/geo+json", "title": "10.5281/zenodo.13374006", "name": "item", "description": "10.5281/zenodo.13374006", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5281/zenodo.13374006"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-08-26T00:00:00Z"}}, {"id": "2a87725879a7535446d3b3e49c603020", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-07-27T16:27:23Z", "type": "Report", "title": "Survival vs. growth trade-off in early recruitment challenges global warming impacts on Mediterranean mountain trees", "description": "Climate change is expected to alter the geographic distribution of many plant species worldwide. However, there is still no clear evidence showing a generalised direction and magnitude of these distribution shifts. Here, we have surveyed, in nine mountainous regions in Spain, an array of tree species along entire elevational ranges, as surrogates of their global climatic ranges, to test for elevational shifts towards cooler locations. We analysed the distribution recruitment patterns of five dominant tree species, recording the abundance and measuring the primary growth of juveniles in 306 plots. Three of the species have a temperate-boreal distribution with populations at their southern edge in the Mediterranean mountain ranges: Pinus sylvestris, Pinus uncinata and Fagus sylvatica; and the other two species have a Mediterranean distribution: Quercus ilex and Pinus nigra. Despite the contrasting phylogenies and biogeographies, we identified a similar pattern in recruitment abundance across species, with an asymmetric distribution of juveniles (more recruits in the middle-upper elevation of their range), but higher annual growths at lower elevations. This survival-growth trade-off at the early recruitment stage may potentially counterbalance at population level the negative effect of global warming on recruit survival at the lower edge of species ranges. These findings suggest a demographic stabilisation process at the early recruitment stage of these tree species, and highlight the importance of considering the different demographic stages across the whole climatic range to understand the effects that climate change may exert on species distributions and population dynamics.", "keywords": ["Mediterranean forests", "Elevational shift", "Climatic gradient", "Demographic stabilising processes", "Climate change", "Forest regeneration", "Species distribution"], "contacts": [{"organization": "Benavides, Raquel, Escudero, Adri\u00e1n, Coll, Llu\u00eds, Ferrandis, Pablo, Gouriveau, Fabrice, H\u00f3dar, Jos\u00e9 Antonio, Ogaya Inurrigarro, Rom\u00e0, Garc\u00eda Rabasa, Sonia, Granda, Elena, Santamar\u00eda, Blanca P., Zamora Rodr\u00edguez, Regino, Espelta Morral, Josep Maria, Pe\u00f1uelas, Josep, Valladares, Fernando,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/2a87725879a7535446d3b3e49c603020"}, {"rel": "self", "type": "application/geo+json", "title": "2a87725879a7535446d3b3e49c603020", "name": "item", "description": "2a87725879a7535446d3b3e49c603020", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2a87725879a7535446d3b3e49c603020"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2015-01-01T00:00:00Z"}}, {"id": "10.5281/zenodo.14839973", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:23:43Z", "type": "Other", "title": "Global Ensemble Digital Terrain Model (GEDTM30): a Tile Example of Local Enhanced Modeling via Transfer Learning", "description": "This repository stores the covariates, the model, the additional samples to run a global-to-local modeling of GEDTM project (https://github.com/openlandmap/GEDTM30). Please visit here for the script of the showcase.\u00a0The script describes a pre-trained random forest model (global.model_gedtm30.lz4) that is successively trained by the additional local samples (local_samples.csv). With the data from (covariates list).\u00a0  Below is the explanation of the covariates, the model and the additional samples.  File description:  global.model_gedtm30.lz4 random forest model trained by global stratified terrain samples of GEDI02 and ICESat-2 ATL08 v6.  local_sample.csv: the local samples of GEDI02 and ICESat-2 ATL08 v6. dtm_y: the terrain height from global Lidar  covariates list:    dsm_glo.tiff: Copenricus GLO30 DEM (doi.org/10.5270/ESA-c5d3d65)\u00a0  dsm_aw3d30 ALOS AW3D30 DEM (Takaku et al. 2014, Tadono et al.)  building.height_ghsbuilth.tiff: GHS building height ~100m resolution, resampled by cubicspline (10.2905/85005901-3A49-48DD-9D19-6261354F56FE)  tree.cover_glad.tiff: tree cover precentile (Potapov et al. 2021)  building.height_3dglobfp.tiff: global three-dimensional building footprint dataset, vector dataset, rasterized to ~30m resolution (Che et al. 2024)  canopy.height_glad.tiff: canopy height from GLAD (Potapov et al. 2021)  edge.canopy.height_glad.tiff: edge canopy height by Sobel filter, derived from GLAD canopy height\u00a0  canopy.height_eth.tiff: canopy height model from ETH (Lang et al. 2023)  edge.canopy.height_eth.tiff:edge canopy height by Sobel filter, derived from ETH canopy height  slope_etopo2022.tiff: earth topography 2022 (etopo 2022) global dem dataset ~500m resolution, resampled by cubicspline (MacFerrin et al. 2024)  lcluc.change_glad.tiff: land use land cover change (Potapov et al. 2020)     Landsat indices (Potapov 2020):   ndvi.p025_2006.2010.tiffndvi.p50_2006.2010.tiffndvi.p975_2006.2010.tiffndvi.p025_2011.2015.tiffndvi.p50_2011.2015.tiffndvi.p975_2011.2015.tiffnir.p025_2006.2010.tiffnir.p50_2006.2010.tiffnir.p975_2006.2010.tifffnir.p025_2011.2015.tiffnir.p50_2011.2015.tiffnir.p975_2011.2015.tifndwi.p025_2006.2010.tiffndwi.p50_2006.2010.tiffndwi.p975_2006.2010.tiffndwi.p025_2011.2015.tiffndwi.p50_2011.2015.tiffndwi.p975_2011.2015.tiff  Note: nir,ndvi,ndwi: Near infra-red, Normalized Difference Vegetation Index, Normalized Difference Wetness Index. p025, p050,p975: precentile 2.5, 50, 97.5.", "keywords": ["geomorphometry", "Digital Elevation Model", "Digital Terrain Model"], "contacts": [{"organization": "Ho, Yu-Feng", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5281/zenodo.14839973"}, {"rel": "self", "type": "application/geo+json", "title": "10.5281/zenodo.14839973", "name": "item", "description": "10.5281/zenodo.14839973", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5281/zenodo.14839973"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-02-09T00:00:00Z"}}, {"id": "10.5281/zenodo.14926032", "type": "Feature", "geometry": null, "properties": {"license": "unspecified", "updated": "2026-07-27T16:23:46Z", "type": "Dataset", "title": "DATASET: Climatic and edaphic drivers of soil organic carbon and pyrogenic carbon stocks across elevation and disturbance gradients in Colombian Andean forests", "description": "The dataset contains information on: entry variables in column: soil pyrogenic carbon PyC (Org) (Mg/ha), PyC (mg cm-3), NDVI(Nrmalized Difference Vegetation Index), Slope (degrees), AMT (Annual Mean Temperature in degrees Celsius), AP (Annual precipitation in mm), pH ( measure of soil acidity or alkalinity), P_available ( phosphorus available, in mg/kg), Tot_ p (Total phosphorus, in mg/kg), sand (%), clay (%), silt (%), Ca_ex (exchangeable calcium, in meq/100g), Mg_ex (exchangeable magnesium, in meq/100g), K_ex (exchangeable potassium, in meq/100g), and Na_ex (exchangeable sodium, in meq/100g). Disturbance (entries by row: low, m\u00e9dium, high, very high); Zone (entries by row: high Andes (h_And), m\u00e9dium Andes (m_And), and low Andes (l_And); and \u00a0Depth (cm), entries by row: 0-5 cm, 20-30 cm, 30-50 cm and 50-100 cm", "keywords": ["elevation gradients", "anthropogenic disturbance", "tropical ecosystem", "Agrosilvopastural systems", "mean annual temperature", " pyrogenic carbon"], "contacts": [{"organization": "Montes-Pulido, Carmen R, Bird, Michael I., Serrano, Julieth, Quesada, Carlos, Feldpausch, Ted R.,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5281/zenodo.14926032"}, {"rel": "self", "type": "application/geo+json", "title": "10.5281/zenodo.14926032", "name": "item", "description": "10.5281/zenodo.14926032", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5281/zenodo.14926032"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-02-21T00:00:00Z"}}, {"id": "10.5281/zenodo.6500189", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:24:33Z", "type": "Dataset", "title": "Methane fluxes from four elevation zones in a St. Lawrence Estuary salt marsh", "description": "Dataset used in Spartina alterniflora has the highest methane emissions in a St. Lawrence estuary salt marsh - IOPscience. The dataset contains methane fluxes calculated from gas measurements taken over a 40 or 60 minute period using a dark static chamber method. Methane fluxes were measured at six locations in four elevation zones of a northern salt marsh on the St. Lawrence River estuary at La Pocati\u00e8re, Quebec (47\u00b022'24.7'N 70\u00b003'26.3'W). Additional environmental data was collected including carbon dioxide fluxes, extractable soil nitrate, extractable soil ammonium, extractable soil dissolved organic carbon, extractable soil total dissolved nitrogen, salinity, temperature, water table depth, soil total organic carbon, soil total nitrogen, soil organic carbon to nitrogen ratio and bulk density. Soil cores were collected from 0-15 cm and used for extractable nutrient analysis, bulk density and soil organic carbon and nitrogen analysis. The work was carried out with funding from the European Union\u2019s Horizon 2020 Research and Innovation Programme under the Marie Sklodowska-Curie Grant Agreement 838296, a NSERC Discovery Grant and a Natural Environment Research Council grant number (NE/T012323/1). This dataset is used in a publication entitled <em>Spartina alterniflora</em> has the highest methane emissions in a St. Lawrence Estuary salt marsh in Environmental Research: Ecology (https://doi.org/10.1088/2752- 664X/ac706a), which also contains more details on fieldsite and methodology. Gas samples were collected from dark, static chambers (18L, 26 cm diameter), which were placed onto pre-inserted collars in the vegetated zones (inserted to 2.5 cm, 3 days prior to sampling) or placed directly onto the mudflat. The chambers were insulated and fitted with fans and venting tubes. Gas samples were collected on the 23rd August 2020 from all sites, soil cores were collected between the 24-25th August 2020 and the 19-20th September 2020. Soil samples were collected at 0-15 cm using a 2.5 cm diameter dutch gouge corer. Soil temperature was measured at 10 cm depth using a soil thermometer, (\u00b0C, DeltaTrak 11050, Pleasanton, USA), salinity was measured in the laboratory using a portable ATC refractometer. Water table depth was measured using a PVC piezometer, a plastic pipe with tubing was inserted into the piezometer and blown into to determine water table depth through bubbling sound (cm). Soil cores were dried at 60 \u00b0C to constant weight and the dry weight over core volume used to calculate bulk density (g cm-3), soil was finely ground and analysed for total organic carbon and total nitrogen (%) using an Elemental Analyser (ThermoFinnigan Flash EA 1112 CN analyser, Carlo Erba, Milan, Italy) with an accuracy of \u00b15 % for N and \u00b11 % for C, and a limit of 171 detection of 0.05 % for both N and C. Extractable nitrate+nitrite (assumed to be nitrate) were analysed in soil extractant (2M KCl, 5:1 of extractant to soil) using a microplate reader and methods in Sims et al., 1995 (https://doi.org/10.1080/00103629509369298) with a limit of detection of 0.1 ppm and accuracy of \u00b15%. Extractable dissolved organic carbon and total dissolved nitrogen were analysed in soil extractant (ultrapure water 18.2 M\u03a9, 5:1 of extractant to soil) on a TOC/TDN analyser (TOC VCSn + TMN-1, Shimadzu, Kyoto, Japan), with a 50 mg C l -1 standard resulting in an accuracy and precision of 3.0 and \u00b14.4 mg l-1, respectively. CH4 and CO2 concentrations were measured in the gas samples using a gas chromatograph (GC-14, Shimadzu, Kyoto, Japan) fitted with a flame ionisation detector, CO2 was methanised to CH4 before analysis. Standards of CH4 (5.1 ppm) and CO2 (5000 ppm) resulted in an accuracy and precision of 6.6\u00b11.5 and 0.4 ppm, and 5324\u00b1324 and 78 ppm, respectively, for CH4 and CO2. Changes in gas concentration over time were converted to fluxes using a linear regression of the linear portion fo the flux and if fluxes were below the minimum detectable concentration difference (see https://doi.org/10.1002/2017JG003783), they were set to zero. Results from the experiments were entered into an Excel spreadsheet for ingestion into the Zenodo data repository.", "keywords": ["13. Climate action", "15. Life on land", "6. Clean water", "methane", " CH4", " salt marsh", " saltmarsh", " greenhouse gas fluxes", " carbon sequestration", " elevation zones"], "contacts": [{"organization": "Comer-Warner, Sophie, Ullah, Sami, Ampuero Reyes, Wendy, Krause, Stefan, Chmura, Gail,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5281/zenodo.6500189"}, {"rel": "self", "type": "application/geo+json", "title": "10.5281/zenodo.6500189", "name": "item", "description": "10.5281/zenodo.6500189", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5281/zenodo.6500189"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-04-28T00:00:00Z"}}, {"id": "10.5281/zenodo.8357642", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-07-27T16:24:54Z", "type": "Dataset", "title": "Mineral Protection rather than Aggregate Stability Enhanced Soil Organic Carbon Along an Elevated Gradient in Alpine Areas of Southwest China", "description": "This data contains Background, Dominant plant and their biomass, Environmental variables, Aggregate stability, Fe/Al oxides, Mass of soil density fractions, Carbon contetn in each density fraction, Mass of aggregates, Carbon content in each aggregate class size, Ratio of carbon content in each soil density and aggregate fractions and Enzyme avtivity of our investigated sites. Total 46 factors were given.", "keywords": ["2. Zero hunger", "soil organic carbon", "elevation", "15. Life on land", "Iron/Aluminium oxides"], "contacts": [{"organization": "Wu, Minghui", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5281/zenodo.8357642"}, {"rel": "self", "type": "application/geo+json", "title": "10.5281/zenodo.8357642", "name": "item", "description": "10.5281/zenodo.8357642", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5281/zenodo.8357642"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-09-19T00:00:00Z"}}, {"id": "10.7910/DVN/IPZGLB", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:25:41Z", "type": "Dataset", "title": "What Happens After Phragmites Is Killed; Effect of Variable Tidal Flooding on Plant Growth and Carbon Allocation: A Marsh Organ Experiment", "description": "This dataset is from a mesocosm experiment where different native wetland species and the invasive species Phragmites australis were planted at different flooding levels in a tidal creek along the Rhode River, a subestuary of the Chesapeake Bay in Edgewater, Maryland. This dataset includes plant growth metrics (height, basal diameter, and stem counts), aboveground and belowground plant biomass, soil oxidation reduction potential, soil carbon, flooding levels, and salinity.", "keywords": ["native wetland planting; Phragmites; marsh elevation; flooding levels", "Earth and Environmental Sciences"], "contacts": [{"organization": "Jacobson, Sylvia, Whigham, Dennis, Brooks, Hope, Baldwin, Andrew H., McCormick, Melissa, Kettenring, Karin, Buehl, Eric,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.7910/DVN/IPZGLB"}, {"rel": "self", "type": "application/geo+json", "title": "10.7910/DVN/IPZGLB", "name": "item", "description": "10.7910/DVN/IPZGLB", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.7910/DVN/IPZGLB"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-01-01T00:00:00Z"}}, {"id": "2781096170", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:27:12Z", "type": "Dataset", "title": "Radium data in the Lena Delta collected in summer 2013 on board RV Dalnie Zelentsy", "description": "Open AccessActivities of excess 224Ra, 226Ra and 228Ra in water samples collected in September 2013 during the 'Lena Delta 2013' hydrological survey expedition on board RV Dalnie Zelentsy (Gon\u00e7alves-Araujo et al., 2015, doi:10.3389/fmars.2015.00108).", "keywords": ["RU Land_2013_Lena", "Salinity", "Radium 226", "Radium 228", "Marine Geochemistry AWI AWI_MarGeoChem", "water", "Marine Geochemistry @ AWI (AWI_MarGeoChem)", "Radium-226", "Gamma spectroscopy", "DATE TIME", "Radium-224 excess", "14. 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It only contains the resources which have been declared for the INSPIRE reporting, i.e. the resources which contain the keyword \u201creporting INSPIRE\u201d.", "formats": [{"name": "OGC:CSW"}], "keywords": ["Government and public sector", "National", "infoCatalogueService", "Buildings", "Addresses", "Elevation", "Meteorological geographical features", "Oceanographic geographical features", "Atmospheric conditions", "Geographical names", "Geology", "Habitats and biotopes", "Hydrography", "Agricultural and aquaculture facilities", "Environmental monitoring facilities", "Production and industrial facilities", "Land cover", "Orthoimagery", "Cadastral parcels", "Coordinate reference systems", "Bio-geographical regions", "Population distribution \u2014 demography", "Species distribution", "Human health and safety", "Utility and governmental services", "Soil", "Energy resources", "Protected sites", "Geographical grid systems", "Administrative units", "Mineral resources", "Statistical units", "Land use", "Area management/restriction/regulation zones and reporting units", "Transport networks", "Sea regions", "Natural risk zones", "Reporting INSPIRE", "federal government"], "contacts": [{"name": null, "organization": "National Geographic Institute", "position": null, "roles": ["custodian"], "phones": [{"value": null}], "emails": [{"value": "products@ngi.be"}], "addresses": [{"deliveryPoint": ["Kortenberglaan 115"], "city": "Brussels", "administrativeArea": null, "postalCode": "1000", "country": "Belgium"}], "links": [{"href": {"url": "http://www.ngi.be", "protocol": null, "protocol_url": "", "name": "http://www.ngi.be", "name_url": "", "description": null, "description_url": "", "applicationprofile": null, "applicationprofile_url": "", "function": null}}]}], "themes": [{"concepts": [{"id": "Government and public sector"}], "scheme": "http://vocab.belgif.be/auth/datatheme"}, {"concepts": [{"id": "National"}], "scheme": "http://inspire.ec.europa.eu/metadata-codelist/SpatialScope"}, {"concepts": [{"id": "infoCatalogueService"}], "scheme": "Commission Regulation (EC) No 1205/2008"}, {"concepts": [{"id": "Buildings"}, {"id": "Addresses"}, {"id": "Elevation"}, {"id": "Meteorological geographical features"}, {"id": "Oceanographic geographical features"}, {"id": "Atmospheric conditions"}, {"id": "Geographical names"}, {"id": "Geology"}, {"id": "Habitats and biotopes"}, {"id": "Hydrography"}, {"id": "Agricultural and aquaculture facilities"}, {"id": "Environmental monitoring facilities"}, {"id": "Production and industrial facilities"}, {"id": "Land cover"}, {"id": "Orthoimagery"}, {"id": "Cadastral parcels"}, {"id": "Coordinate reference systems"}, {"id": "Bio-geographical regions"}, {"id": "Population distribution \u2014 demography"}, {"id": "Species distribution"}, {"id": "Human health and safety"}, {"id": "Utility and governmental services"}, {"id": "Soil"}, {"id": "Energy resources"}, {"id": "Protected sites"}, {"id": "Geographical grid systems"}, {"id": "Administrative units"}, {"id": "Mineral resources"}, {"id": "Statistical units"}, {"id": "Land use"}, {"id": "Area management/restriction/regulation zones and reporting units"}, {"id": "Transport networks"}, {"id": "Sea regions"}, {"id": "Natural risk zones"}], "scheme": "http://inspire.ec.europa.eu/theme"}, {"concepts": [{"id": "federal government"}], "scheme": "https://www.eionet.europa.eu/gemet/en/themes/"}]}, "links": [{"href": "http://inspire.reporting.geo.be/eng/csw?request=GetCapabilities&service=CSW&version=2.0.2", "protocol": "OGC:CSW", "rel": null}, {"href": "https://inspire.reporting.geo.be/eng/csw?request=GetCapabilities&service=CSW&version=2.0.2", "protocol": "OGC:CSW"}, {"href": "https://www.geo.be/thumbs/metadata_discovery.png", "name": "preview", "description": "Web image thumbnail (URL)", "protocol": "WWW:LINK-1.0-http--image-thumbnail", "rel": "preview"}, {"rel": "self", "type": "application/geo+json", "title": "47e996b2-c60c-4cc8-9db3-20dab85ef478", "name": "item", "description": "47e996b2-c60c-4cc8-9db3-20dab85ef478", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/47e996b2-c60c-4cc8-9db3-20dab85ef478"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date-time": "2024-01-19T10:41:54Z"}}, {"id": "1854/LU-8709527", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:26:29Z", "type": "Journal Article", "created": "2021-04-25", "title": "Towards the Development and Verification of a 3D-Based Advanced Optimized Farm Machinery Trajectory Algorithm", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Efforts related to minimizing the environmental burden caused by agricultural activities and increasing economic efficiency are key contemporary drivers in the precision agriculture domain. Controlled Traffic Farming (CTF) techniques are being applied against soil compaction creation, using the on-line optimization of trajectory planning for soil-sensitive field operations. The research presented in this paper aims at a proof-of-concept solution with respect to optimizing farm machinery trajectories in order to minimize the environmental burden and increase economic efficiency. As such, it further advances existing CTF solutions by including (1) efficient plot divisions in 3D, (2) the optimization of entry and exit points of both plot and plot segments, (3) the employment of more machines in parallel and (4) obstacles in a farm machinery trajectory. The developed algorithm is expressed in terms of unified modeling language (UML) activity diagrams as well as pseudo-code. Results were visualized in 2D and 3D to demonstrate terrain impact. Verifications were conducted at a fully operational commercial farm (Rost\u011bnice, the Czech Republic) against second-by-second sensor measurements of real farm machinery trajectories.</p></article>", "keywords": ["Agriculture and Food Sciences", "2. Zero hunger", "Technology and Engineering", "controlled traffic farming", "Chemical technology", "mission planning", "TP1-1185", "04 agricultural and veterinary sciences", "Biochemistry", "Article", "Analytical Chemistry", "soil compaction", "Atomic and Molecular Physics", "digital elevation model", "AGRICULTURAL ROBOTS", "0401 agriculture", " forestry", " and fisheries", "Electrical and Electronic Engineering", "and Optics", "coverage path planning", "controlled traffic farming; coverage path planning; digital elevation model; mission planning; soil compaction"]}, "links": [{"href": "http://www.mdpi.com/1424-8220/21/9/2980/pdf"}, {"href": "https://www.mdpi.com/1424-8220/21/9/2980/pdf"}, {"href": "https://doi.org/1854/LU-8709527"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Sensors", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "1854/LU-8709527", "name": "item", "description": "1854/LU-8709527", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/1854/LU-8709527"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-04-23T00:00:00Z"}}, {"id": "2164/6134", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:27:00Z", "type": "Journal Article", "created": "2016-05-13", "title": "Modeling Soil Processes: Review, Key Challenges, and New Perspectives", "description": "Core Ideas                     <p>                                                                           <p>A community effort is needed to move soil modeling forward.</p>                                                                             <p>Establishing an international soil modeling consortium is key in this respect.</p>                                                                             <p>There is a need to better integrate existing knowledge in soil models.</p>                                                                             <p>Integration of data and models is a key challenge in soil modeling.</p>                                                                     </p>                     <p>The remarkable complexity of soil and its importance to a wide range of ecosystem services presents major challenges to the modeling of soil processes. Although major progress in soil models has occurred in the last decades, models of soil processes remain disjointed between disciplines or ecosystem services, with considerable uncertainty remaining in the quality of predictions and several challenges that remain yet to be addressed. First, there is a need to improve exchange of knowledge and experience among the different disciplines in soil science and to reach out to other Earth science communities. Second, the community needs to develop a new generation of soil models based on a systemic approach comprising relevant physical, chemical, and biological processes to address critical knowledge gaps in our understanding of soil processes and their interactions. Overcoming these challenges will facilitate exchanges between soil modeling and climate, plant, and social science modeling communities. It will allow us to contribute to preserve and improve our assessment of ecosystem services and advance our understanding of climate\uffe2\uff80\uff90change feedback mechanisms, among others, thereby facilitating and strengthening communication among scientific disciplines and society. We review the role of modeling soil processes in quantifying key soil processes that shape ecosystem services, with a focus on provisioning and regulating services. We then identify key challenges in modeling soil processes, including the systematic incorporation of heterogeneity and uncertainty, the integration of data and models, and strategies for effective integration of knowledge on physical, chemical, and biological soil processes. We discuss how the soil modeling community could best interface with modern modeling activities in other disciplines, such as climate, ecology, and plant research, and how to weave novel observation and measurement techniques into soil models. We propose the establishment of an international soil modeling consortium to coherently advance soil modeling activities and foster communication with other Earth science disciplines. Such a consortium should promote soil modeling platforms and data repository for model development, calibration and intercomparison essential for addressing contemporary challenges.</p>", "keywords": ["organic-matter dynamics", "550", "Sciences de l\u2019environnement & \u00e9cologie", "QH301 Biology", "Knowledge management", "0208 environmental biotechnology", "ECOSYSTEM SERVICES", "02 engineering and technology", "soil processes", "01 natural sciences", "Physical Geography and Environmental Geoscience", "Sciences de la Terre", "Biological process", "ANZSRC::3707 Hydrology", "DROUGHT SEVERITY INDEX", "SYNTHETIC-APERTURE RADAR", "ANZSRC::4106 Soil sciences", "SDG 13 - Climate Action", "Climate change", "0503 Soil Sciences", "GROUND-PENETRATING RADAR", "Integration of knowledge", "Life sciences", "ANZSRC::050399 Soil Sciences not elsewhere classified", "synthetic-aperture radar", "Physical Sciences", "Water Resources", "Knowledge and experience", "MULTIPLE ECOSYSTEM SERVICES", "knowledge integration", "570", "DIFFUSE-REFLECTANCE SPECTROSCOPY", "Environmental Engineering", "Physique", " chimie", " math\u00e9matiques & sciences de la terre", "Scientific discipline", "0703 Crop and Pasture Production", "0207 environmental engineering", "Soil Science", "soil science", "ORGANIC-MATTER DYNAMICS", "DATA ASSIMILATION", "Physical", " chemical", " mathematical & earth Sciences", "ANZSRC::0503 Soil Sciences", "Science disciplines", "PEDOTRANSFER FUNCTIONS", "Feedback mechanisms", "mod\u00e9lisation", "ground-penetrating radar", "Science & Technology", "ANZSRC::080110 Simulation and Modelling", "15. Life on land", "Sciences de la terre & g\u00e9ographie physique", "multiple ecosystem services", "root water-uptake", "Observation and measurement", "DIGITAL ELEVATION MODEL", "Quality of predictions", "SATURATED-UNSATURATED FLOW", "ARBUSCULAR MYCORRHIZAL FUNGI", "sciences du sol", "HYDRAULIC-PROPERTIES", "2. Zero hunger", "Agriculture", "diffuse-reflectance spectroscopy", "4106 Soil sciences", "ORGANIC-MATTER", "digital elevation model", "SDG 13 \u2013 Ma\u00dfnahmen zum Klimaschutz", "Sciences du vivant", "Uncertainty analysis", "0406 Physical Geography and Environmental Geoscience", "Life Sciences & Biomedicine", "Crop and Pasture Production", "101028 Mathematical modelling", "international soil modeling consortium", "[SDU.STU]Sciences of the Universe [physics]/Earth Sciences", "Environmental Sciences & Ecology", "arbuscular mycorrhizal fungi", "Ecosystems", "Climate models", "QH301", "Environmental sciences & ecology", "Life Science", "SEDIMENT TRANSPORT MODELS", "data integration", "sediment transport models", "approche ecosyst\u00e9mique", "0105 earth and related environmental sciences", "info:eu-repo/classification/ddc/550", "3707 Hydrology", "soil modeling", "ROOT WATER-UPTAKE", "SOLUTE TRANSPORT", "13. Climate action", "Earth and Environmental Sciences", "Soil Sciences", "[SDU.STU] Sciences of the Universe [physics]/Earth Sciences", "Earth Sciences", "Earth sciences & physical geography", "Soils", "101028 Mathematische Modellierung", "saturated-unsaturated flow", "Environmental Sciences", "root water-uptake", " sediment transport models", " diffuse-reflectance spectroscopy", " arbuscular mycorrhizal fungi", " multiple ecosystem services", " saturated-unsaturated flow", " ground-penetrating radar", " synthetic-aperture radar", " digital elevation model", " organic-matter dynamics."]}, "links": [{"href": "https://orbi.uliege.be/bitstream/2268/263634/1/Vereecken%20VZJ%202016.pdf"}, {"href": "http://onlinelibrary.wiley.com/wol1/doi/10.2136/vzj2015.09.0131/fullpdf"}, {"href": "https://escholarship.org/content/qt6976n34c/qt6976n34c.pdf"}, {"href": "https://doi.org/2164/6134"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Vadose%20Zone%20Journal", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "2164/6134", "name": "item", "description": "2164/6134", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2164/6134"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2016-05-01T00:00:00Z"}}, {"id": "3146066833", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-07-27T16:27:39Z", "type": "Journal Article", "created": "2021-04-01", "title": "A Low-Rank Group-Sparse Model for Eliminating Mixed Errors in Data for SRTM1", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>The elimination of mixed errors is a key preprocessing technology for the area of digital elevation model data analysis, which is important for further applying data. We associated group sparsity with the low-rank uniqueness of local transformations of mixing errors to effectively remove mixing errors in data from Shuttle Radar Topography Mission 1 (SRTM 1) based on the sparseness of low-rank groups. First, the stripe-error structure that appeared globally in multiple directions was able to be better represented locally using group-sparse regularization and the uniqueness of the data in the low-rank direction of the local range and using variational ideas to constrain the gradient direction of the data to avoid redundant elimination. Second, the nonlocal self-similarity of the weighted kernel norm was used to remove random noise. Finally, the proposed model for eliminating mixed errors was solved using an algorithm based on the multiplier method of alternating direction. Experiments using simulated and real data found that the proposed low-rank group-sparse method (LRGS) eliminated mixed errors in both visual and quantitative evaluations better than the most recent processing methods and existing dataset products.</p></article>", "keywords": ["self-similarity", "digital elevation model", "Science", "Q", "0211 other engineering and technologies", "0202 electrical engineering", " electronic engineering", " information engineering", "group sparse", "02 engineering and technology", "mixed errors", "shuttle radar topography mission 1", "low-rank"]}, "links": [{"href": "http://www.mdpi.com/2072-4292/13/7/1346/pdf"}, {"href": "https://doi.org/3146066833"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Remote%20Sensing", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "3146066833", "name": "item", "description": "3146066833", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/3146066833"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-04-01T00:00:00Z"}}, {"id": "IRD_PYF_AAAA_1993_143000000-2600", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:30:11Z", "type": "Dataset", "title": "Atlas de la Polyn\u00e9sie fran\u00e7aise. 16 mosaics of 17 map sheets and a set of 93 map sheets. Scale of 1:143\u00a0000\u00a0000 to 1:2\u00a0600. Date of publication: 1993.", "description": "16 mosaics of 17 map sheets and a set of 93 additional map sheets 1.   Autres atolls des Tuamotu : oro-hydrographie : planche 14. Scale of 1:150\u00a0000. Date of publication: 1993. 2.   L'agriculture et l'utilisation du sol - I : planche 84. Scale of 1:100\u00a0000. Date of publication: 1993. 3.   L'agriculture et l'utilisation du sol - II : planche 85. Scale of 1:15\u00a0000\u00a0000 to 1:62\u00a0000. Date of publication: 1993. 4.   L'am\u00e9nagement et la gestion des milieux : planche 110. Scale of 1:50\u00a0000. Date of publication: 1993. 5.   L'aquaculture nacri\u00e8re et perli\u00e8re - I : planche 89. Scale of 1:8\u00a0000\u00a0000 to 1:15\u00a0500. Date of publication: 1993. 6.   L'aquaculture nacri\u00e8re et perli\u00e8re - II : planche 90. Scale of 1:8\u00a0000\u00a0000 to 1:40\u00a0000. Date of publication: 1993. 7.   L'archipel de la soci\u00e9t\u00e9 : planche 5. Scale of 1:2\u00a0000\u00a0000. Date of publication: 1993. 8.   L'archipel des Australes : planche 15. Scale of 1:3\u00a0000\u00a0000. Date of publication: 1993. 9.   L'archipel des Gambier : planche 16. Scale of 1:2\u00a0000\u00a0000. Date of publication: 1993. 10.  L'archipel des Marquises : oro-hydrographie : planche 10. Scale of 1:150\u00a0000. Date of publication: 1993. 11.  L'archipel des Marquises : planche 9. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1993. 12.  L'archipel des Tuamotu : planche 11. Scale of 1:3\u00a0500\u00a0000. Date of publication: 1993. 13.  L'\u00e9nergie : planche 91. Scale of 1:12\u00a0000\u00a0000 to 1:250\u00a0000. Date of publication: 1993. 14.  L'\u00e9volution de la population 1897-1926 : planche 74. Scale of 1:10\u00a0000\u00a0000. Date of publication: 1993. 15.  L'\u00e9volution r\u00e9cente de la population 1962-1983 : planche 78. Scale of 1:12\u00a0000\u00a0000. Date of publication: 1993. 16.  L'hydrologie : planche 41. Scale of 1:150\u00a0000. Date of publication: 1993. 17.  L'industrie : planche 92. Scale of 1:50\u00a0000 to 1:12\u00a0000. Date of publication: 1993. 18.  L'occupation de l'espace - I : planche 60. Scale of 1:150\u00a0000. Date of publication: 1993. 19.  L'occupation de l'espace - II : planche 61. Scale of 1:150\u00a0000. Date of publication: 1993. 20.  L'utilisation du milieu marin et r\u00e9cifal : planche 64. Scale of 1:150\u00a0000 to 1:2\u00a0600. Date of publication: 1993. 21.  La biog\u00e9ographie r\u00e9cifale et lagonaire : planche 53. Scale of 1:61\u00a0000\u00a0000 to 1:20\u00a0000\u00a0000. Date of publication: 1993. 22.  La christianisation : planche 69. Scale of 1:60\u00a0000\u00a0000 to 1:23\u00a0000\u00a0000. Date of publication: 1993. 23.  La climatologie - I : planche 42. Scale of 1:17\u00a0000\u00a0000. Date of publication: 1993. 24.  La climatologie - II : planche 43. Scale of 1:400\u00a0000 to 1:300\u00a0000. Date of publication: 1993. 25.  La climatologie dynamique : planche 22. unknown. Date of publication: 1993. 26.  La d\u00e9couverte europ\u00e9enne 1521-1841 : planche 68. Scale of 1:17\u00a0000\u00a0000. Date of publication: 1993. 27.  La densit\u00e9 de la population - I : planche 75. Scale of 1:150\u00a0000. Date of publication: 1993. 28.  La densit\u00e9 de la population - II : planche 76. Scale of 1:8\u00a0000\u00a0000 to 1:150\u00a0000. Date of publication: 1993. 29.  La distribution de l'eau : planche 99. Scale of 1:150\u00a0000 to 1:30\u00a0000. Date of publication: 1993. 30.  La g\u00e9ologie - I : \u00eeles du Vent : planche 28. Scale of 1:150\u00a0000. Date of publication: 1993. 31.  La g\u00e9ologie - II : \u00eeles Sous-le-Vent : planche 29. Scale of 1:150\u00a0000. Date of publication: 1993. 32.  La g\u00e9ologie - III : archipel des Marquises, archipel des Australes : planche 30. Scale of 1:150\u00a0000. Date of publication: 1993. 33.  La g\u00e9ologie structurale : planche 25. Scale of 1:10\u00a0000\u00a0000. Date of publication: 1993. 34.  La g\u00e9omorphologie - I : \u00eeles du Vent : planche 35. Scale of 1:150\u00a0000. Date of publication: 1993. 35.  La g\u00e9omorphologie - II : \u00eeles Sous-le-Vent : planche 36. Scale of 1:150\u00a0000. Date of publication: 1993. 36.  La g\u00e9omorphologie - III : planche 37. Scale of 1:150\u00a0000. Date of publication: 1993. 37.  La ma\u00eetrise des milieux terrestres - I : planche 62. Scale of 1:150\u00a0000 to 1:3\u00a0500. Date of publication: 1993. 38.  La ma\u00eetrise des milieux terrestres - II : planche 63. Scale of 1:150\u00a0000. Date of publication: 1993. 39.  La nouvelle organisation de l'espace : planche 71. Scale of 1:16\u00a0500\u00a0000. Date of publication: 1993. 40.  La pathologie infectieuse et parasitaire : planche 101. Scale of 1:40\u00a0000\u00a0000 to 1:450\u00a0000. Date of publication: 1993. 41.  La pathologiechronique et d\u00e9g\u00e9n\u00e9rative : planche 102. Scale of 1:25\u00a0000\u00a0000 to 1:330\u00a0000. Date of publication: 1993. 42.  La p\u00eache lagonaire et l'aquaculture : planche 86. Scale of 1:4\u00a0100\u00a0000 to 1:150\u00a0000. Date of publication: 1993. 43.  La p\u00eache p\u00e9lagique : planche 87. Scale of 1:23\u00a0500\u00a0000 to 1:3\u00a0000\u00a0000. Date of publication: 1993. 44.  La physico-chimie de l'oc\u00e9an : planche 21. Scale of 1:35\u00a0000\u00a0000. Date of publication: 1993. 45.  La Polyn\u00e9sie Fran\u00e7aise dans le Pacifique : planche 1. Scale of 1:60\u00a0000\u00a0000. Date of publication: 1993. 46.  La Polyn\u00e9sie Fran\u00e7aise dans le Pacifique Sud : planche 2. Scale of 1:35\u00a0000\u00a0000. Date of publication: 1993. 47.  La r\u00e9partition de la population : planche 77. Scale of 1:150\u00a0000 to 1:98\u00a0500. Date of publication: 1993. 48.  La r\u00e9partition des esp\u00e8ces oc\u00e9aniques, les ressources : planche 44. Scale of 1:143\u00a0000\u00a0000 to 1:23\u00a0500\u00a0000. Date of publication: 1993. 49.  La scolarisation et la formation - I : planche 103. Scale of 1:150\u00a0000 to 1:50\u00a0000. Date of publication: 1993. 50.  La scolarisation et la formation - II : planche 104. Scale of 1:12\u00a0400\u00a0000 to 1:9\u00a0850\u00a0000. Date of publication: 1993. 51.  La structure et la g\u00e9ologie des atolls - I : Fangataufa du fond de l'oc\u00e9an \u00e0 l'atoll : planche 31. Scale of 1:150\u00a0000. Date of publication: 1993. 52.  La structure et la g\u00e9ologie des atolls - II : l'atoll de Moruroa : planche 32. Scale of 1:150\u00a0000. Date of publication: 1993. 53.  La structure et la g\u00e9ologie des atolls - III : le lagon de Moruroa : planche 33. Scale of 1:150\u00a0000 to 1:15\u00a0000. Date of publication: 1993. 54.  La synth\u00e8se d\u00e9mographique : planche 81. Scale of 1:16\u00a0500\u00a0000 to 1:800\u00a0000. Date of publication: 1993. 55.  La typologie des \u00eeles : planche 23. Scale of 1:10\u00a0000\u00a0000. Date of publication: 1993. 56.  La v\u00e9g\u00e9tation - I : \u00eeles du Vent : planche 54. Scale of 1:150\u00a0000. Date of publication: 1993. 57.  La v\u00e9g\u00e9tation - II : \u00eeles Marquises, \u00eeles Tuamotu, \u00eeles Australes : planche 55. Scale of 1:150\u00a0000. Date of publication: 1993. 58.  La vie politique : planche 111. Scale of 1:16\u00a0500\u00a0000 to 1:400\u00a0000. Date of publication: 1993. 59.  Le champ magn\u00e9tique terrestre : planche 24. Scale of 1:40\u00a0000\u00a0000 to 1:13\u00a0500\u00a0000. Date of publication: 1993. 60.  Le domaine maritime de la Polyn\u00e9sie fran\u00e7aise : planche 3. Scale of 1:111\u00a0111\u00a0100 to 1:28\u00a0000\u00a0000. Date of publication: 1993. 61.  Le peuplement ancien : planche 59. Scale of 1:55\u00a0500\u00a0000. Date of publication: 1993. 62.  Le sport : planche 105. Scale of 1:60\u00a0000\u00a0000 to 1:750\u00a0000. Date of publication: 1993. 63.  Le syst\u00e8me de soins : planche 100. Scale of 1:12\u00a0000\u00a0000 to 1:500\u00a0000. Date of publication: 1993. 64.  Le temps de la mort import\u00e9e : planche 73. Scale of 1:1\u00a0000\u00a0000 to 1:150\u00a0000. Date of publication: 1993. 65.  Le tourisme - I : planche 93. Scale of 1:12\u00a0000\u00a0000 to 1:150\u00a0000. Date of publication: 1993. 66.  Le tourisme - II : planche 94. unknown. Date of publication: 1993. 67.  Le volcanisme et la sismicit\u00e9 - I : planche 26. Scale of 1:17\u00a0500\u00a0000. Date of publication: 1993. 68.  Le volcanisme et la sismicit\u00e9 - II : planche 27. Scale of 1:500\u00a0000. Date of publication: 1993. 69.  Les \"archipels\" de la viabilit\u00e9 : planche 112. Scale of 1:24\u00a0000\u00a0000. Date of publication: 1993. 70.  Les aspects fonciers - I : planche 82. Scale of 1:20\u00a0000 to 1:15\u00a0000. Date of publication: 1993. 71.  Les aspects fonciers - II : planche 83. Scale of 1:83\u00a0000. Date of publication: 1993. 72.  Les centres urbains secondaires : planche 109. Scale of 1:80\u00a0000 to 1:20\u00a0000. Date of publication: 1993. 73.  Les courants et les hydroclimats : planche 20. unknown. Date of publication: 1993. 74.  Les cycles de l'\u00e9conomie coloniale : planche 72. Scale of 1:21\u00a0000\u00a0000 to 1:400\u00a0000. Date of publication: 1993. 75.  Les fonds sous-marins : planche 18. Scale of 1:10\u00a0000\u00a0000. Date of publication: 1993. 76.  Les \u00eeles Australes et les \u00eeles Gambier : oro-hydrographie : planche 17. Scale of 1:21\u00a0000\u00a0000 to 1:150\u00a0000. Date of publication: 1993. 77.  Les \u00eeles du Vent : oro-hydrographie : planche 7. Scale of 1:150\u00a0000. Date of publication: 1993. 78.  Les \u00eeles du Vent : planche 6. Scale of 1:250\u00a0000 to 1:100\u00a0000. Date of publication: 1993. 79.  Les \u00eeles Sous-le-Vent : oro-hydrographie : planche 8. Scale of 1:150\u00a0000. Date of publication: 1993. 80.  Les insectes h\u00e9matophages : planche 58. Scale of 1:17\u00a0000\u00a0000. Date of publication: 1993. 81.  Les langues - I : planche 66. Scale of 1:42\u00a0500\u00a0000. Date of publication: 1993. 82.  Les migrations humaines : planche 80. Scale of 1:15\u00a0000\u00a0000. Date of publication: 1993. 83.  Les monts sous-marins : planche 19. Scale of 1:6\u00a0000\u00a0000. Date of publication: 1993. 84.  Les mouvements naturels de population : planche 79. Scale of 1:12\u00a0000\u00a0000. Date of publication: 1993. 85.  Les oiseaux : planche 57. Scale of 1:23\u00a0500\u00a0000 to 1:450\u00a0000. Date of publication: 1993. 86.  Les Pentes : planche 34. Scale of 1:150\u00a0000. Date of publication: 1993. 87.  Les peuplements coralliens : planche 48. Scale of 1:150\u00a0000 to 1:12\u00a0000. Date of publication: 1993. 88.  Les peuplements d'algues : planche 49. Scale of 1:50\u00a0000 to 1:12\u00a0000. Date of publication: 1993. 89.  Les peuplements de mollusques : planche 50. Scale of 1:250\u00a0000 to 1:50\u00a0000. Date of publication: 1993. 90.  Les peuplements de poissons : planche 52. Scale of 1:150\u00a0000 to 1:12\u00a0000. Date of publication: 1993. 91.  Les peuplements naturels de nacres : planche 51. Scale of 1:150\u00a0000. Date of publication: 1993. 92.  Les production primaire et secondaire des lagons - I : planche 45. Scale of 1:150\u00a0000 to 1:12\u00a0000. Date of publication: 1993. 93.  Les production primaire et secondaire des lagons - II : planche 46. Scale of 1:150\u00a0000. Date of publication: 1993. 94.  Les r\u00e9cifs : construction et \u00e9rosion : planche 47. Scale of 1:150\u00a0000 to 1:45\u00a0000. Date of publication: 1993. 95.  Les religions contemporaines : planche 70. Scale of 1:10\u00a0000\u00a0000 to 1:142\u00a0500. Date of publication: 1993. 96.  Les reptiles et les mollusques : planche 56. Scale of 1:20\u00a0000\u00a0000 to 1:150\u00a0000. Date of publication: 1993. 97.  Les ressources secondaires de la mer : planche 88. Scale of 1:14\u00a0000\u00a0000 to 1:300\u00a0000. Date of publication: 1993. 98.  Les sols - I : planche 38. Scale of 1:150\u00a0000 to 1:55\u00a0000. Date of publication: 1993. 99.  Les sols - II : planche 39. Scale of 1:150\u00a0000. Date of publication: 1993. 100. Les sols - III : planche 40. Scale of 1:500\u00a0000 to 1:150\u00a0000. Date of publication: 1993. 101. Les sources cartographiques : planche 4. Scale of 1:100\u00a0000 to 1:5\u00a0000. Date of publication: 1993. 102. Les transports a\u00e9riens internationaux : planche 95. Scale of 1:105\u00a0000\u00a0000 to 1:74\u00a0000\u00a0000. Date of publication: 1993. 103. Les transports int\u00e9rieurs : planche 97. Scale of 1:19\u00a0700\u00a0000. Date of publication: 1993. 104. Les transports maritimes : planche 96. Scale of 1:74\u00a0000\u00a0000 to 1:2\u00a0000\u00a0000. Date of publication: 1993. 105. Les transports routiers \u00e0 Tahiti : planche 98. Scale of 1:1\u00a0000\u00a0000 to 1:150\u00a0000. Date of publication: 1993. 106. Papeete : les aspects fonciers et sociaux : planche 108. Scale of 1:50\u00a0000 to 1:31\u00a0000. Date of publication: 1993. 107. Papeete : les dominantes ethniques : planche 107. Scale of 1:50\u00a0000. Date of publication: 1993. 108. Papeete : les tissus urbains : planche 106. Scale of 1:25\u00a0000. Date of publication: 1993. 109. Tikehau - Rangiroa : oro-hydrographie 1 : planche 12. Scale of 1:150\u00a0000. Date of publication: 1993. 110. Tikehau - Rangiroa : oro-hydrographie 2 : planche 13. Scale of 1:150\u00a0000. 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Scale of 1:6\u00a0400\u00a0000 to 1:10\u00a0000. Date of publication: 1967-1979.", "description": "2 mosaics of 3 map sheets and a set of 40 additional map sheets 1.   Abidjan : industries : 1970 : planche C5b. Scale of 1:50\u00a0000 to 1:20\u00a0000. Date of publication: 1979. 2.   Abidjan 1975 : administrations, services publics et para-publics : planche C6b. Scale of 1:30\u00a0000 to 1:10\u00a0000. Date of publication: 1979. 3.   Abidjan 1976 : occupation de l'space urbain et peri-urbain : planche B4c. Scale of 1:83\u00a0333. Date of publication: 1979. 4.   Aptitudes culturales et foresti\u00e8res des sols : planche A5b. Scale of 1:2\u00a0000\u00a0000. Date of publication: 1979. 5.   Artisanat : planche C6a. Scale of 1:4\u00a0000\u00a0000. Date of publication: 1979. 6.   Carte administrative : d\u00e9cembre 1976 : planche D1c. Scale of 1:2\u00a0000\u00a0000. Date of publication: 1979. 7.   Commerce : Abidjan : planche D3a. Scale of 1:20\u00a0000. Date of publication: 1979. 8.   Cultures industrielles : planche C1d. Scale of 1:4\u00a0000\u00a0000. Date of publication: 1979. 9.   Cultures industrielles et marchandes : planche C1c. Scale of 1:4\u00a0000\u00a0000. Date of publication: 1979. 10.  Cultures villageoises secondaires : planche C1b. Scale of 1:6\u00a0400\u00a0000 to 1:4\u00a0000\u00a0000. Date of publication: 1970. 11.  Cultures vivri\u00e8res de base : planche C1a. Scale of 1:6\u00a0400\u00a0000 to 1:4\u00a0000\u00a0000. Date of publication: 1969. 12.  D\u00e9ficits hydriques - dur\u00e9e de la saison s\u00e8che : planche A3c. Scale of 1:3\u00a0000\u00a0000. Date of publication: 1979. 13.  Densit\u00e9 de la population rurale : planche B1a. Scale of 1:2\u00a0000\u00a0000. Date of publication: 1979. 14.  El\u00e9ments g\u00e9n\u00e9raux du climat : planche A3a. Scale of 1:2\u00a0000\u00a0000. Date of publication: 1979. 15.  Elevage : planche C3. Scale of 1:6\u00a0400\u00a0000 to 1:4\u00a0000\u00a0000. Date of publication: 1979. 16.  Energie : planche C5c. Scale of 1:6\u00a0400\u00a0000 to 1:3\u00a0000\u00a0000. Date of publication: 1979. 17.  Enseignement : infrastructure scolaire 1967-68 : planche B3a. Scale of 1:6\u00a0400\u00a0000 to 1:2\u00a0000\u00a0000. Date of publication: 1979. 18.  Entreprises mini\u00e8res et industrielles : 1967 : planche C5a. Scale of 1:2\u00a0000\u00a0000. Date of publication: 1979. 19.  G\u00e9ographie m\u00e9dicale : infrastructure sanitaire : janvier 1977 : planche B3b. Scale of 1:2\u00a0000\u00a0000. Date of publication: 1979. 20.  G\u00e9ologie : planche A2. Scale of 1:2\u00a0000\u00a0000. Date of publication: 1972. 21.  Groupes culturels et ethniques : planche B2a. Scale of 1:2\u00a0000\u00a0000. Date of publication: 1979. 22.  Hydrologie : planche A4. Scale of 1:6\u00a0400\u00a0000 to 1:2\u00a0000\u00a0000. Date of publication: 1979. 23.  Infrastructure routi\u00e8re et des transports : 1972 : planche D2a. Scale of 1:6\u00a0400\u00a0000 to 1:2\u00a0000\u00a0000. Date of publication: 1979. 24.  Les activit\u00e9s foresti\u00e8res 1974 : planche C4a. Scale of 1:6\u00a0400\u00a0000 to 1:200\u00a0000. Date of publication: 1975. 25.  Les circonscriptions administratives : I. \u00e9volution 1893-1937 : planche D1a. Scale of 1:6\u00a0400\u00a0000 to 1:4\u00a0000\u00a0000. Date of publication: 1979. 26.  Les circonscriptions administratives : II. \u00e9volution 1938-1975 : planche D1b. Scale of 1:6\u00a0400\u00a0000 to 1:4\u00a0000\u00a0000. Date of publication: 1979. 27.  Les grandes op\u00e9rations agricoles de d\u00e9veloppement : mai 1976 : planche C1. Scale of 1:2\u00a0000\u00a0000. Date of publication: 1979. 28.  Les villes : le secteur tertiaire : planche D4b. Scale of 1:4\u00a0000\u00a0000. Date of publication: 1979. 29.  Localisation de la population 1965 : planche B1 nord. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1967. 30.  Localisation de la population 1965 : planche B1 sud. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1967. 31.  Oro-hydrographie : planche A1. Scale of 1:2\u00a0000\u00a0000. Date of publication: 1979. 32.  Paysages urbains : Bouak\u00e9 1973 : planche B4b1. Scale of 1:30\u00a0000. Date of publication: 1979. 33.  Paysages urbains : Korhogo 1970, Man 1974, Mankono 1973, Gagnoa 1970, Agboville 1974, Guiglo 1970, Grand-Bassam 1974 : planche B4b2. Scale of 1:30\u00a0000. Date of publication: 1979. 34.  Paysages urbains : Odienn\u00e9 1974, Yamoussoukro 1973, San Pedro 1973, Bondoukou 1972 : planche B4b3. Scale of 1:30\u00a0000. Date of publication: 1979. 35.  P\u00e9dologie : planche A5a. Scale of 1:2\u00a0000\u00a0000. Date of publication: 1979. 36.  Peuplement rurale : l'habitat rural : forme, taille, semis : planche B4a. Scale of 1:4\u00a0000\u00a0000 to 1:2\u00a0500\u00a0000. Date of publication: 1979. 37.  Population rurale - \u00e9volution 1955-1965 : planche B1b. Scale of 1:4\u00a0000\u00a0000. Date of publication: 1979. 38.  Pr\u00e9cipitations mensuelles : planche A3b. Scale of 1:6\u00a0400\u00a0000. Date of publication: 1979. 39.  Principaux courants de transports : planche D2b. Scale of 1:6\u00a0400\u00a0000 to 1:4\u00a0000\u00a0000. Date of publication: 1979. 40.  S\u00e9dimentologie : s\u00e9dimentologie du plateau continental : Abidjan, Grand-Lahou, San Pedro : planche A2b. Scale of 1:350\u00a0000. Date of publication: 1972. 41.  Tourisme : sites et infrastructures : ao\u00fbt 1975 : planche C7. Scale of 1:2\u00a0000\u00a0000 to 1:100\u00a0000. Date of publication: 1979. 42.  Trafic de marchandises : planche D2c. Scale of 1:6\u00a0400\u00a0000 to 1:4\u00a0000\u00a0000. Date of publication: 1979. 43.  V\u00e9g\u00e9tation : planche A6a. Scale of 1:2\u00a0000\u00a0000. Date of publication: 1979.", "keywords": ["bio-geographical-regions", "cultural-aptitudes", "elevation", "energy-resources", "ethnic-groups", "fr", "geology", "hydrography", "land-use", "local-coverage", "map-collection", "meteorological-geographical-features", "national-coverage", "orohydrographie", "population-distribution-\u2014-demography", "precipitation", "project-numerisud", "settlements", "soil", "thematic-map", "topography"]}, "links": [{"href": "http://data.europa.eu/88u/dataset/2652cc87-9cb2-4f20-91ac-d519dc8f9adb"}, {"rel": "self", "type": "application/geo+json", "title": "2652cc87-9cb2-4f20-91ac-d519dc8f9adb", "name": "item", "description": "2652cc87-9cb2-4f20-91ac-d519dc8f9adb", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2652cc87-9cb2-4f20-91ac-d519dc8f9adb"}, {"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": "3d6851ae-fcd3-45c4-a46c-957481ae39a6", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:30:11Z", "type": "Dataset", "title": "Atlas de la Nouvelle-Cal\u00e9donie. One mosaic of 2 map sheets and a set of 51 map sheets. Scale of 1:100\u00a0000\u00a0000 to 1:5\u00a0000. Date of publication: 1981.", "description": "One mosaic of 2 map sheets and a set of 51 additional map sheets : 1.   Approche et d\u00e9couverte de la Nouvelle-Cal\u00e9donie : planche 20. Scale of 1:13\u00a0500\u00a0000 to 1:4\u00a0000\u00a0000. Date of publication: 1981. 2.   Aptitudes culturales et foresti\u00e8res : planche 28. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1981. 3.   Arch\u00e9ologie et pr\u00e9histoire : planche 16. Scale of 1:43\u00a0000\u00a0000 to 1:2\u00a0000\u00a0000. Date of publication: 1981. 4.   Autres activit\u00e9s \u00e9conomiques : planche 43. Scale of 1:2\u00a0000\u00a0000 to 1:125\u00a0000. Date of publication: 1981. 5.   Centres urbains secondaires : planche 52. Scale of 1:3\u00a0000\u00a0000 to 1:10\u00a0000. Date of publication: 1981. 6.   Clans autochtones : situation pr\u00e9-coloniale : planche 18. Scale of 1:1\u00a0000\u00a0000 to 1:500\u00a0000. Date of publication: 1981. 7.   Communications et transports : planche 45. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1981. 8.   Densit\u00e9 de la population : planche 25. Scale of 1:4\u00a0000\u00a0000 to 1:1\u00a0000\u00a0000. Date of publication: 1981. 9.   Domaine minier, mines et m\u00e9tallurgie : situation contemporaine : planche 42. Scale of 1:4\u00a0000\u00a0000 to 1:1\u00a0000\u00a0000. Date of publication: 1981. 10.  \u00c9conomie rurale : aspects historiques : planche 21. Scale of 1:2\u00a0000\u00a0000. Date of publication: 1981. 11.  El\u00e9ments g\u00e9n\u00e9raux du climat : planche 11. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1981. 12.  Emplois et activit\u00e9s en 1976 : planche 38. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1981. 13.  Energie : planche 44. Scale of 1:1\u00a0000\u00a0000 to 1:100\u00a0000. Date of publication: 1981. 14.  Enseignement : planche 48. Scale of 1:4\u00a0000\u00a0000 to 1:73\u00a0000. Date of publication: 1981. 15.  Ethnobotanique : planche 17. Scale of 1:76\u00a0000\u00a0000 to 1:2\u00a0000\u00a0000. Date of publication: 1981. 16.  \u00c9volution du peuplement de 1891 \u00e0 1956 : planche 23. Scale of 1:4\u00a0500\u00a0000 to 1:4\u00a0000\u00a0000. Date of publication: 1981. 17.  Extraction mini\u00e8re et m\u00e9tallurgie : planche 41. Scale of 1:2\u00a0000\u00a0000 to 1:1\u00a0000\u00a0000. Date of publication: 1981. 18.  G\u00e9ologie : planche 9. Scale of 1:3\u00a0000\u00a0000 to 1:1\u00a0000\u00a0000. Date of publication: 1981. 19.  G\u00e9omorphologie : planche 13. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1981. 20.  Gites min\u00e9raux et substances utiles : planche 40. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1981. 21.  Gravim\u00e9trie : planche 6. Scale of 1:3\u00a0000\u00a0000 to 1:1\u00a0000\u00a0000. Date of publication: 1981. 22.  Hydroclimats en mers du Corail et de Tasman : planche 4. Scale of 1:25\u00a0000\u00a0000. Date of publication: 1981. 23.  Hydrologie : planche 12. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1981. 24.  L'espace administratif : planche 46. Scale of 1:4\u00a0500\u00a0000 to 1:2\u00a0000\u00a0000. Date of publication: 1981. 25.  L'espace foncier m\u00e9lan\u00e9sien : planche 33. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1981. 26.  L'espace rural europ\u00e9en : planche 36. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1981. 27.  L'habitat rural m\u00e9lan\u00e9sien : planche 35. Scale of 1:5\u00a0000. Date of publication: 1981. 28.  La Nouvelle-Cal\u00e9donie dans l'espace \u00e9conomique oc\u00e9anien : planche 53. Scale of 1:100\u00a0000\u00a0000 to 1:20\u00a0000\u00a0000. Date of publication: 1981. 29.  La Nouvelle-Cal\u00e9donie dans le sud-ouest du Pacifique : planche 2. Scale of 1:12\u00a0000\u00a0000. Date of publication: 1981. 30.  La Nouvelle-Cal\u00e9donie et ses d\u00e9pendances : carte bathym\u00e9trique d\u00e9taill\u00e9e : planche 3. Scale of 1:3\u00a0640\u00a0000. Date of publication: 1981. 31.  La terre dans la soci\u00e9t\u00e9 m\u00e9lan\u00e9sienne : planche 32. Scale of 1:83\u00a0000 to 1:14\u00a0000. Date of publication: 1981. 32.  Le cadre g\u00e9opolitique : planche 1. Scale of 1:32\u00a0000\u00a0000. Date of publication: 1981. 33.  Le Sud-Ouest du Pacifique : donn\u00e9es structurales : planche 5. Scale of 1:12\u00a0000\u00a0000. Date of publication: 1981. 34.  Les \u00e9tapes de la colonisation terrienne : planche 22. Scale of 1:2\u00a0000\u00a0000. Date of publication: 1981. 35.  Les productions du secteur rural : planche 39. Scale of 1:4\u00a0000\u00a0000 to 1:2\u00a0000\u00a0000. Date of publication: 1981. 36.  Linguistique : planche 19. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1981. 37.  Localisation de la population : planche 24. Scale of 1:1\u00a0000\u00a0000 to 1:75\u00a0000. Date of publication: 1981. 38.  Migrations : planche 26. Scale of 1:43\u00a0000\u00a0000 to 1:2\u00a0000\u00a0000. Date of publication: 1981. 39.  Noum\u00e9a : commerce : planche 51. Scale of 1:25\u00a0000. Date of publication: 1981. 40.  Noum\u00e9a : faits de population : planche 50. Scale of 1:130\u00a0000 to 1:60\u00a0000. Date of publication: 1981. 41.  Noum\u00e9a : faits urbains : planche 49. Scale of 1:100\u00a0000 to 1:35\u00a0000. Date of publication: 1981. 42.  Oro-hydrographie : planche 7. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1981. 43.  P\u00e9dologie : planche 14. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1981. 44.  Religions : planche 27. Scale of 1:4\u00a0000\u00a0000 to 1:1\u00a0000\u00a0000. Date of publication: 1981. 45.  Sant\u00e9 : planche 47. Scale of 1:4\u00a0000\u00a0000 to 1:125\u00a0000. Date of publication: 1981. 46.  S\u00e9dimentologie : sud-ouest du Lagon : planche 8. Scale of 1:2\u00a0700\u00a0000 to 1:200\u00a0000. Date of publication: 1981. 47.  Situation fonci\u00e8re d'ensemble : planche 31. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1981. 48.  Terroirs m\u00e9lan\u00e9siens : planche 34. Scale of 1:20\u00a0000. Date of publication: 1981. 49.  Type de temps et cyclones : planche 10. Scale of 1:30\u00a0000\u00a0000 to 1:4\u00a0000\u00a0000. Date of publication: 1981. 50.  Types d'exploitations europ\u00e9ennes : planche 37. Scale of 1:50\u00a0000. Date of publication: 1981. 51.  Utilisation du sol : Grande Terre : partie Nord : planche 29. Scale of 1:500\u00a0000. Date of publication: 1981. 52.  Utilisation du sol : Grande Terre : partie sud et \u00eeles Loyaut\u00e9 : planche 30. Scale of 1:500\u00a0000. Date of publication: 1981. 53.  V\u00e9g\u00e9tation : planche 15. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1981.", "keywords": ["bathymetry", "bio-geographical-regions", "cultural-aptitudes", "elevation", "energy-resources", "ethnic-groups", "ethnobotanics", "fr", "geology", "gravimetry", "hydrography", "illustration", "land-use", "linguistics", "local-coverage", "map-collection", "meteorological-geographical-features", "mineral-resources", "national-coverage", "organisation", "orohydrographie", "population-distribution-\u2014-demography", "project-numerisud", "relief-(land)", "settlements", "situation-map", "soil", "structural-geology", "thematic-map", "topography"]}, "links": [{"href": "http://data.europa.eu/88u/dataset/3d6851ae-fcd3-45c4-a46c-957481ae39a6"}, {"rel": "self", "type": "application/geo+json", "title": "3d6851ae-fcd3-45c4-a46c-957481ae39a6", "name": "item", "description": "3d6851ae-fcd3-45c4-a46c-957481ae39a6", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/3d6851ae-fcd3-45c4-a46c-957481ae39a6"}, {"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": "17c93706-4d68-45ee-8428-65fe7dd524f1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:30:09Z", "type": "Dataset", "title": "Atlas du Cameroun. 2 mosaics of 6 map sheets and a set of 15 map sheets. Scale of 1:10\u00a0000\u00a0000 to 1:1\u00a0000\u00a0000. Date of publication: 1956-1975.", "description": "2 mosaics of 6 map sheets and a set of 15 additional map sheets 1.   Activit\u00e9s de production et de transformation de type industriel au 1er janvier 1970 : planche XIII. Scale of 1:2\u00a0000\u00a0000. Date of publication: 1973. 2.   Cameroun : phytog\u00e9ographie : planche VII. Scale of 1:2\u00a0000\u00a0000. Date of publication: 1959. 3.   Carte g\u00e9ologique du Cameroun : feuille Nord : planche 1 A nord. Scale of 1:5\u00a0000\u00a0000 to 1:1\u00a0000\u00a0000. Date of publication: 1956. 4.   Carte g\u00e9ologique du Cameroun : feuille Sud : planche 1 B sud. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1956. 5.   Carte gravim\u00e9trique, anomalies de Bouguer (d=2,67) : g\u00e9ophysique : planche VIII. Scale of 1:3\u00a0000\u00a0000. Date of publication: 1970. 6.   Densit\u00e9 de la population rurale : calcul\u00e9e par canton d'apr\u00e8s le recensement administratif de 1967-1968 (population des chefs-lieux administratifs exclue) : planche XII. Scale of 1:2\u00a0000\u00a0000. Date of publication: 1974. 7.   Energie \u00e9lectrique, autre aspects de la g\u00e9ographie indusrielle : planche XV. Scale of 1:7\u00a0000\u00a0000 to 1:3\u00a0000\u00a0000. Date of publication: 1975. 8.   Faits d'int\u00e9r\u00eat m\u00e9dical : planche IX. Scale of 1:6\u00a0000\u00a0000 to 1:4\u00a0000\u00a0000. Date of publication: 1970. 9.   Hauteurs moyennes annuelles de pluie (en milim\u00e8tres), isohy\u00e8tes et histogrammes : planche III. Scale of 1:10\u00a0000\u00a0000 to 1:3\u00a0000\u00a0000. Date of publication: unknown. 10.  Les exploitations foresti\u00e8res : planche XVI. Scale of 1:4\u00a0500\u00a0000 to 1:2\u00a0000\u00a0000. Date of publication: 1975. 11.  Les industries du Cameroun au 1er janvier 1970 : planche XIVa. Scale of 1:7\u00a0000\u00a0000. Date of publication: 1972. 12.  Les industries du Cameroun au 1er janvier 1970 : planche XIVb. Scale of 1:7\u00a0000\u00a0000. Date of publication: 1972. 13.  Localisation de la population : feuille nord : planche X. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1973. 14.  Localisation de la population : feuille sud : planche X. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1972. 15.  Localisation des groupes humains : feuille nord : planche XI. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1971. 16.  Localisation des groupes humains : feuille sud : planche XI. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1971. 17.  Oro-hydrographie : planche V. Scale of 1:2\u00a0000\u00a0000. Date of publication: unknown. 18.  P\u00e9dologie : planche VI. Scale of 1:2\u00a0000\u00a0000. Date of publication: 1957. 19.  Temp\u00e9ratures moyennes annuelles, temp\u00e9ratures minima moyennes mensuelles, temp\u00e9ratures maxima moyennes mensuelles : planche IV. Scale of 1:10\u00a0000\u00a0000. 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Atlas r\u00e9gional Ouest 2 : enseignement = Regional atlas : education. Scale of 1:500\u00a0000. Date of publication: 1971. 7.   Atlas r\u00e9gional Ouest 2 : infrastructure = Regional atlas : infrastructure. Scale of 1:500\u00a0000. Date of publication: 1970. 8.   Atlas r\u00e9gional Ouest 2 : milieu physique = Regional atlas : physical environment. Scale of 1:1\u00a0000\u00a0000. Date of publication: 1971. 9.   Atlas r\u00e9gional Ouest 2 : organisation de l'espace = Regional atlas : regional organisation. Scale of 1:500\u00a0000. Date of publication: 1971. 10.  Atlas r\u00e9gional Ouest 2 : populations = Regional atlas : populations. Scale of 1:500\u00a0000. 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