{"type": "FeatureCollection", "features": [{"id": "10.1016/j.sandf.2023.101332", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:17:26Z", "type": "Journal Article", "created": "2023-06-20", "title": "Addressing the challenges of homogeneity, quality control and waste handling in soil bio-cementation: A large-scale experiment", "description": "In an attempt to go beyond the conventional laboratory experiments widely reported in literature around the emerging technique of soil bio-cementation, this work addresses key challenges related to its large-scale application. Precisely, a state-of-the-art installation with a draining bottom boundary is introduced and a novel treatment strategy, based on ex-situ hydrolysis within a 1000 L bioreactor, is described. Hydrolyzed solutions are injected in a tank filled with 0\u20134\u00a0mm sand, via a system of eight injection tubes to treat a total surface of 40\u00a0m2 across a depth of 2\u00a0m. A multilevel, spatial and temporal quality control system is used to monitor the injection processes across several cycles via chemical and hydraulic means. In total, 20.8\u00a0m3 of reactant solutions are supplied to the targeted zone, equal to one pore volume and over 120 chemical analyses are carried-out. Reaction efficiencies overall exceeded 80%, while by increasing the number of treatment cycles, and thus calcification levels, a gradual increase in the recorded pressure at the injection inlet was captured, that reached up to 75\u00a0kPa. Zones where the injection pressure increased the most are found to yield better resistance in the vicinity of the corresponding injection tube. A dynamic penetrometer campaign reveals that increase in the tip resistance, is found to exceed 5\u00a0MPa and yields more homogenous response across the bottom 0.5\u00a0m of the tank, which is believed to reflect the effect of initial confinement on the deposition of calcite. For the zones with the highest cementation, correlated \u03c6\u2019 values yield a 5\u00b0 increase, while the oedometric modulus is found to double. The results suggest that ex-situ bio-cementation, where hydrolysis occurs in bioreactors instead of inside the soil mass, is capable of yielding similar precipitation efficiencies and mechanical improvement compared to traditional bio-cementation, where bacteria are injected directly into the soil. Finally, the monitoring of MICP at the scale of typical geotechnical works is discussed along with the problematic of residual ammonium, which in this study is found to reach absorded quantities of 4\u00a0mol/L.", "keywords": ["MICP", "Upscaling", "0211 other engineering and technologies", "Quality control", "Dynamic penetrometer", "TA703-712", "Engineering geology. Rock mechanics. Soil mechanics. Underground construction", "02 engineering and technology", "Field testing", "6. Clean water", "0201 civil engineering"], "contacts": [{"organization": "Harran, Ray, Terzis, Dimitrios, Laloui, Lyesse,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1016/j.sandf.2023.101332"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soils%20and%20Foundations", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.sandf.2023.101332", "name": "item", "description": "10.1016/j.sandf.2023.101332", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.sandf.2023.101332"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-08-01T00:00:00Z"}}, {"id": "10.1016/j.jrmge.2020.04.003", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:17:18Z", "type": "Journal Article", "created": "2020-06-15", "title": "Combined approach of poroelastic and earthquake nucleation applied to the reservoir-induced seismic activity in the Val d\u2019Agri area, Italy", "description": "Open AccessIn this work, an approach is developed to study the seismicity associated with the impoundment and level changes of a water reservoir (reservoir induced seismicity \u2013 RIS). The proposed methodology features a combination of a semi-analytical poroelastic model with an earthquake nucleation approach based on rate-and-state frictional law. The combined approach was applied to the case of the Pertusillo Lake, located in the Val d\u2019Agri area (Italy), whose large seasonal water level changes are believed to induce protracted micro-seismicity (local magnitude ML < 3). Results show that the lake impoundment in 1962 could have produced up to 0.5 bar (1 bar = 100 kPa) changes in Coulomb failure stress (\u0394CFS), while the seasonal water level variation is responsible for variation up to 0.05 bar. Modeling results of the seismicity rates in 2001\u22122014 show that the observed earthquakes are well correlated with the modeled \u0394CFS. Finally, the reason that the seismicity is only observed at southwest of the Pertusillo Lake is provided, which is likely attributed to different rock lithologies and depletion caused by significant hydrocarbon exploitation in the northeastern sector of the lake.", "keywords": ["550", "Rate-and-state frictional law", "Pertusillo lake", "Reservoir induced seismicity (RIS); Poroelasticity; Rate-and-state frictional law; Pertusillo lake", "TA703-712", "Reservoir induced seismicity (RIS)", "Engineering geology. Rock mechanics. Soil mechanics. Underground construction", "Poroelasticity", "01 natural sciences", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.jrmge.2020.04.003"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Rock%20Mechanics%20and%20Geotechnical%20Engineering", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.jrmge.2020.04.003", "name": "item", "description": "10.1016/j.jrmge.2020.04.003", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.jrmge.2020.04.003"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-08-01T00:00:00Z"}}, {"id": "10.1002/2016JF004060", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:13:58Z", "type": "Journal Article", "created": "2017-03-06", "title": "Investigation of rock fragmentation during rockfalls and rock avalanches via 3-D discrete element analyses", "description": "Abstract<p>This paper investigates the characteristics of dynamic rock fragmentation and its influence on the postfailure fragment trajectory. A series of numerical simulations by discrete element method (DEM) were performed for a simple rock block and slope geometry, where a particle agglomerate of prismatic shape is released along a sliding plane and subsequently collides onto a flat horizontal plane at a sharp kink point. The rock block is modeled as an assembly of bonded spherical particles with fragmentation arising from bond breakages. Bond strength and stiffness were calibrated against available experimental data. We analyzed how dynamic fragmentation occurs at impact, together with the generated fragment size distributions and consequently their runout for different slope topographies. It emerges that after impact, the vertical momentum of the granular system decreases sharply to nil, while the horizontal momentum increases suddenly and then decreases. The sudden boost of horizontal momentum can effectively facilitate the transport of fragments along the bottom floor. The rock fragmentation intensity is associated with the input energy and increases quickly with the slope angle. Gentle slopes normally lead to long spreading distance and large fragments, while steep slopes lead to high momentum boosts and impact forces, with efficient rock fragmentation and fine deposits. The fragment size decreases, while the fracture stress and fragment number both increase with the impact loading strain rate, supporting the experimental observations. The fragment size distributions can be well fitted by the Weibull's distribution function.</p>", "keywords": ["550", "DEM; dynamic fragmentation; loading rate; momentum boost; rock avalanche; runout;", "13. Climate action", "0211 other engineering and technologies", "02 engineering and technology", "Fragmentation", " rockslide", " rockavalanche", " DEM", " numerical modeling", " runout", "551", "01 natural sciences", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016JF004060"}, {"href": "https://eprints.ncl.ac.uk/fulltext.aspx?url=237479/388C5B83-7098-4BA3-A221-B7B1CEFCC63B.pdf&pub_id=237479"}, {"href": "https://doi.org/10.1002/2016JF004060"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Geophysical%20Research%3A%20Earth%20Surface", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1002/2016JF004060", "name": "item", "description": "10.1002/2016JF004060", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1002/2016JF004060"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-03-01T00:00:00Z"}}, {"id": "10.1002/2017JB015210", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:13:58Z", "type": "Journal Article", "created": "2018-03-12", "title": "Dynamic Fragmentation of Jointed Rock Blocks During Rockslide-Avalanches: Insights From Discrete Element Analyses", "description": "Abstract<p>The dynamic fragmentation of jointed rock blocks during rockslide avalanches has been investigated by discrete element method simulations for a multiple arrangement of a rock block sliding over a simple slope geometry. The rock blocks are released along an inclined sliding plane and subsequently collide onto a flat horizontal plane at a sharp kink point. The contact force chains generated by the impact appear initially at the bottom frontal corner of the rock block and then propagate radially upward to the top rear part of the block. The jointed rock blocks exhibit evident contact force concentration and discontinuity of force wave propagation near the joint, associating with high energy dissipation of granular dynamics. The corresponding force wave propagation velocity can be less than 200\uffc2\uffa0m/s, which is much smaller than that of an intact rock (1,316\uffc2\uffa0m/s). The concentration of contact forces at the bottom leads to high rock fragmentation intensity and momentum boosts, facilitating the spreading of many fine fragments to the distal ends. However, the upper rock block exhibits very low rock fragmentation intensity but high energy dissipation due to intensive friction and damping, resulting in the deposition of large fragments near the slope toe. The size and shape of large fragments are closely related to the orientation and distribution of the block joints. The cumulative fragment size distribution can be well fitted by the Weibull's distribution function, with very gentle and steep curvatures at the fine and coarse size ranges, respectively. The numerical results of fragment size distribution can match well some experimental and field observations.</p>", "keywords": ["discrete element method; dynamic fragmentation; force wave; fragment size distribution; jointed rock; rockslide avalanche;", "discrete element method; dynamic fragmentation; force wave; fragment size distribution; jointed rock; rockslide avalanche", "0211 other engineering and technologies", "02 engineering and technology", "551", "530", "01 natural sciences", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2017JB015210"}, {"href": "https://doi.org/10.1002/2017JB015210"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Geophysical%20Research%3A%20Solid%20Earth", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1002/2017JB015210", "name": "item", "description": "10.1002/2017JB015210", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1002/2017JB015210"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-04-01T00:00:00Z"}}, {"id": "10.1016/j.chemgeo.2019.04.025", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:16:21Z", "type": "Journal Article", "created": "2019-04-24", "title": "Unusual neon isotopic composition in Neoproterozoic sedimentary rocks: Fluorine bearing mineral contribution or trace of an impact event?", "description": "Abstract   Extraterrestrial materials have He and Ne isotopic compositions that are distinct from those of the Earth's surface. In order to track the extraterrestrial material accreted onto Earth during the Ediacaran period, we have analyzed the He and Ne isotopic composition of thirteen sedimentary rocks in the age range ~550\u2013600\u202fMa, coming from the Huqf supergroup in Oman for which carbon and sulfur isotopic data have been characterized previously.  3He/4He ratios range between 0.006\u202f\u00b1\u202f0.003 and 0.27\u202f\u00b1\u202f0.01 RA, with RA being the atmospheric ratio. 3He/4He ratios show a positive relationship with 3He contents ranging between 0.6 and 31\u202f\u00d7\u202f10\u221213\u202fcm3\u202fSTP\u00b7g\u22121. The 3He contents are within the literature data for 3 to 480\u202fMyr old samples with evidence of IDP 3He (IDP for interplanetary dust particles), suggesting that extraterrestrial 3He is still retained in such old samples.  20Ne/22Ne ratios are close to or below the modern atmospheric ratio of 9.8 with the minimum value equal to 9.05\u202f\u00b1\u202f0.03. 21Ne/22Ne ratios show a high range of variation, going from 0.0345\u202f\u00b1\u202f0.0009 to 0.0935\u202f\u00b1\u202f0.0023. The Ne isotopic compositions follow a nucleogenic trend similar to that of crustal fluids from the literature and predicted continental crust. However, one sample (3404) shows an unusual Ne isotopic composition with a lower 20Ne/22Ne at similar 21Ne/22Ne compared to the other samples.  Two hypotheses can explain this singular Ne isotopic composition. First, it could be the result of a particular nucleogenic trend due to the presence of F-bearing minerals in this sample. SEM-EDS elemental mapping showed that although F- and Ca-rich phases, which could correspond to fluorites, are present in sample 3404. However, their abundance of ~0.15% seems too low to explain the unusual Ne isotopic composition. However, due to the high uncertainty of the calculations, we cannot totally rule out this hypothesis. Alternatively, the singular Ne isotopic composition could be due to the presence of a Ne-A component, a component characterizing pre-solar diamonds contained in chondrites. This would indicate that a major object impacted the Earth at the time the sediment was forming, between ~600 and ~550\u202fMa, which is coherent with the estimated age range of the Acraman impact in Australia.", "keywords": ["[SDU] Sciences of the Universe [physics]", "0301 basic medicine", "03 medical and health sciences", "Ne-A", "Nucleogenic", "Ediacaran sedimentary rocks", "13. Climate action", "Noble gas", "Acraman impact", "Fluorite", "01 natural sciences", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.chemgeo.2019.04.025"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Chemical%20Geology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.chemgeo.2019.04.025", "name": "item", "description": "10.1016/j.chemgeo.2019.04.025", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.chemgeo.2019.04.025"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-08-01T00:00:00Z"}}, {"id": "10.1016/j.geoderma.2024.117154", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:17:05Z", "type": "Journal Article", "created": "2024-12-26", "title": "Separating fast from slow cycling soil organic carbon \u2013 A multi-method comparison on land use change sites", "description": "Soil organic carbon (SOC) is significantly affected by land use change (LUC). Consequently, LUC is a major controlling factor of total SOC contents and SOC pool dynamics. Several methods have been developed to assess distinct SOC pools, which includes particle size separation, thermal analysis and soil reflectance mid-infrared spectroscopy. All of which are considered to have a potential as high through put methods to generate large datasets. Here, we used 23 sites covering six different types of LUC to assess differences in fast and slow cycling SOC derived from three approaches. We used i) particle size fractionation to obtain coarse (>50\u00a0\u00a0\u00b5m) and fine (<50\u00a0\u00a0\u00b5m) SOC fractions; ii) thermal Rock-Eval\u00ae 6 analysis in compilation with the PARTYSOCv2.0EU model to estimate active and stable SOC pools and iii) mid-infrared spectroscopy to determine the relative SOC composition and derive fast (aliphatic compounds) and slow (aromatic/carboxylic compounds) cycling SOC pools. The particle size SOC fractions and thermal SOC pools showed similar dynamics but differed substantially in the magnitude with LUC. The fine SOC fraction contained around two-thirds of the total SOC across all land uses and was strongly responsive by nearly matching the relative changes of total SOC (slope of 0.76 and R2\u00a0=\u00a00.91). Therefore, the fine fraction SOC might be more dynamic than considered until now. In comparison, the stable SOC pool calculated using PARTYSOCv2.0EU was less responsive to the relative changes (slope of 0.43 and R2\u00a0=\u00a00.72) and contained around 40\u00a0% of the total SOC. This underlines that both physical and thermal approaches separate biogeochemically distinct pools. The qualitative assessment by mid-infrared spectroscopy related well to the thermal SOC pools but not to the particle size fractions. The initial land-use SOC composition, as a ratio of the corresponding fast and slow cycling SOC pool, can be a suitable predictor for SOC evolution. This was particularly true for thermal and mid-infrared spectroscopy derived SOC pools. We show that three conceptually different methods (physical, thermal and mid-infrared spectroscopic) are suitable to determine SOC pool changes for a large diversity of LUC, but the sensitivity of the individual pools can differ strongly, depending on the method.", "keywords": ["Particle size fractionation", "Science", "Q", "Rock-Eval\u00ae analysis", "Cropland", "Forest", "Grassland", "Mid-infrared spectroscopy"], "contacts": [{"organization": "Schiedung, Marcus, Barr\u00b4e, Pierre, Peoplau, Christopher,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1016/j.geoderma.2024.117154"}, {"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.2024.117154", "name": "item", "description": "10.1016/j.geoderma.2024.117154", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.geoderma.2024.117154"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-01-01T00:00:00Z"}}, {"id": "10.1016/j.gca.2019.02.036", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:16:58Z", "type": "Journal Article", "created": "2019-02-27", "title": "Volatile distributions in and on the Moon revealed by Cu and Fe isotopes in the \u2018Rusty Rock\u2019 66095", "description": "Abstract   The Apollo 16 \u2018Rusty Rock\u2019 impact melt breccia 66095 is a volatile-rich sample, with the volatiles inherited through vapor condensation from an internal lunar source formed during thermo-magmatic evolution of the Moon. We report Cu and Fe isotope data for 66095 and find that bulk-rocks, residues and acid leaches span a relatively limited range of compositions (3.0\u202f\u00b1\u202f1.3\u202fwt.% FeO [range\u202f=\u202f2.0\u20134.8\u202fwt.%], 5.4\u202f\u00b1\u202f3.1\u202fppm Cu [range\u202f=\u202f3\u201312\u202fppm], average \u03b456Fe of 0.15\u202f\u00b1\u202f0.05\u2030 [weighted mean\u202f=\u202f0.156\u2030] and \u03b465Cu of 0.72\u202f\u00b1\u202f0.14\u2030 [weighted mean\u202f=\u202f0.78\u2030]). In contrast to the extreme enrichment of the light isotopes of Zn and heavy isotopes of Cl in 66095, \u03b465Cu and \u03b456Fe in the sample lie within the previously reported range for lunar mare basalts (0.92\u202f\u00b1\u202f0.16\u2030 and 0.12\u202f\u00b1\u202f0.02\u2030, respectively). The lack of extreme isotopic fractionation for Cu and Fe isotopes reflects compositions inherent to 66095, with condensation of a cooling gas from impact-generated fumarolic activity at temperatures too low to lead to the condensation of Cu and Fe in the sample, but higher than required to condense Zn. Together with thermodynamic models, these constraints suggest that the gas condensed within 66095 between 700 and 900\u202f\u00b0C (assuming a pressure of 10\u22126 and an fO2 of IW-2). That the Cu and Fe isotopic compositions of sample 66095 are within the range of mare basalts removes the need for an exotic, volatile-enriched source. The enrichment in Tl, Br, Cd, Sn, Zn, Pb, Rb, Cs, Ga, B, Cl, Li relative to Bi, Se, Te, Ge, Cu, Ag, Sb, Mn, P, Cr and Fe in the \u2018Rusty Rock\u2019 is consistent with volcanic outgassing models and indicates that 66095 likely formed distal from the original source of the gas. The volatile-rich character of 66095 is consistent with impact-generated fumarolic activity in the region of the Cayley Plains, demonstrating that volatile-rich rocks can occur on the lunar surface from outgassing of a volatile-poor lunar interior. The \u2018Rusty Rock\u2019 indicates that the lunar interior is significantly depleted in volatile elements and compounds and that volatile-rich surface rocks likely formed through vapor condensation. Remote sensing studies have detected volatiles on the lunar surface, attributing them dominantly to solar wind. Based on the \u2018Rusty Rock\u2019, some of these surface volatiles may also originate from the Moon\u2019s interior.", "keywords": ["[SDU] Sciences of the Universe [physics]", "0301 basic medicine", "0303 health sciences", "03 medical and health sciences", "Condensates", "Copper isotopes", "13. Climate action", "Evaporation", "Iron isotopes", "Volatile elements", "Moon", "Rusty Rock"]}, "links": [{"href": "https://doi.org/10.1016/j.gca.2019.02.036"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Geochimica%20et%20Cosmochimica%20Acta", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.gca.2019.02.036", "name": "item", "description": "10.1016/j.gca.2019.02.036", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.gca.2019.02.036"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-12-01T00:00:00Z"}}, {"id": "10.1016/j.geodrs.2022.e00560", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:17:05Z", "type": "Journal Article", "created": "2022-07-07", "title": "Estimating organic carbon stocks of mineral soils in Denmark: Impact of bulk density and content of rock fragments", "description": "<p>Management measures to reduce atmospheric carbon dioxide concentrations by increasing soil organic carbon (SOC) storage need verification, e.g., by periodic sampling of soils to estimate resulting changes in SOC stock. Estimates of SOC stocks are affected by content of rock fragments (systematic bias) and soil bulk density (random but significant effect), both of which may vary significantly between soils. We investigated the importance of using site-specific bulk density and correcting for rock fragment content on estimates of SOC stock in 0\u201350 cm depth of agricultural minerals soils, collected in 2019 in the Danish National Square Grid. We found that use of an average bulk density value for a given soil type category produced valid estimates of SOC stocks for regional/national inventories. However, large variations in bulk density were found within a given soil type category, which can result in over- or under-estimation at local sites. This calls for measurement of site-specific bulk density and rock fragment content to produce valid estimates of field-scale SOC stock, e.g., to be used in farm carbon credit schemes.</p>", "keywords": ["Rock fragment content", "Soil bulk density", "13. Climate action", "National soil carbon inventory", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land", "Agricultural mineral soil", "Soil organic carbon stock", "01 natural sciences", "Soil bulk density", " Rock fragment content", " Soil organic carbon stock", " National soil carbon inventory", " Agricultural mineral soil", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.geodrs.2022.e00560"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Geoderma%20Regional", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.geodrs.2022.e00560", "name": "item", "description": "10.1016/j.geodrs.2022.e00560", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.geodrs.2022.e00560"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-09-01T00:00:00Z"}}, {"id": "10.1016/j.jasrep.2019.03.017", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-03T16:17:11Z", "type": "Journal Article", "created": "2019-03-25", "title": "Chemical and mineralogical analyses on stones from Sagunto Castle (Spain)", "description": "For the first time, an archaeometric study was carried out on the carbonate rock ashlars of the Sagunto Castle. The studied site is one of the most important and best preserved Spanish archaeological and architectural monuments, characterized by different construction phases from the Roman period to Modern Ages. Forty samples collected from thirteen different structures of Sagunto Castle and two quarries, located in the Sagunto's hill were used for comparative purposes. The samples were analyzed by X-ray diffraction, X-ray fluorescence and inductively coupled plasma mass spectrometry to determine their mineralogical and elemental composition. The obtained data show similar chemical and mineralogical features between the rocks outcropping in the city quarries and some of those employed to build the structures, suggesting that rocks could have been used to build the structures from different periods along the centuries.", "keywords": ["Building stone; Chemistry; Fortress; Middle ages; Mineralogy; Remains; Roman period", "Building stone; Fortress; Remains; Chemistry; Mineralogy; Roman period; Middle ages", "archaeometrics; carbonate rock ashlars; X-ray fluorescence and inductively coupled plasma mass spectrometry", "01 natural sciences", "0104 chemical sciences", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://iris.unica.it/bitstream/11584/298931.2/3/Ramaciotti%20et%20al%202018_1-s2.0-S2352409X18307454-main.pdf"}, {"href": "https://doi.org/10.1016/j.jasrep.2019.03.017"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Archaeological%20Science%3A%20Reports", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.jasrep.2019.03.017", "name": "item", "description": "10.1016/j.jasrep.2019.03.017", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.jasrep.2019.03.017"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-04-01T00:00:00Z"}}, {"id": "10.1016/j.jrmge.2020.01.004", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-03T16:17:18Z", "type": "Journal Article", "created": "2020-07-14", "title": "Revisiting the methods of determining hydraulic conductivity of saturated expansive clays in low-compressibility zone", "description": "The hydraulic conductivity of saturated clays is commonly determined either directly by monitoring water flux or indirectly based on Terzaghi's consolidation equation. Similar results are generally obtained from the two methods, but sometimes a significant difference can be observed, in particular for expansive soils. In this study, the hydraulic conductivities determined by the two methods are first compared based on existing data in the literature. The indirect method is then revisited attempting to explain the difference identified. A modified effective stress, considering physico-chemical interaction between face-to-face oriented particles, is finally introduced to better describe the compressibility of expansive clays and to further improve the indirect method in determining hydraulic conductivity of such soils in the low-compressibility zone. Extra tests were performed on Gaomiaozi (GMZ) bentonite slurry and the results obtained allowed the modified indirect method to be verified.", "keywords": ["Hydraulic conductivity", "Terzaghi's consolidation equation", "Modified effective stress", "Laboratory tests", "0211 other engineering and technologies", "TA703-712", "Expansive clays", "Engineering geology. Rock mechanics. Soil mechanics. Underground construction", "02 engineering and technology", "[SPI.MECA.MEMA] Engineering Sciences [physics]/Mechanics [physics.med-ph]/Mechanics of materials [physics.class-ph]", "6. Clean water"]}, "links": [{"href": "https://doi.org/10.1016/j.jrmge.2020.01.004"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Rock%20Mechanics%20and%20Geotechnical%20Engineering", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.jrmge.2020.01.004", "name": "item", "description": "10.1016/j.jrmge.2020.01.004", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.jrmge.2020.01.004"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-10-01T00:00:00Z"}}, {"id": "10.1016/j.quaint.2022.09.008", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-03T16:17:24Z", "type": "Journal Article", "created": "2022-10-08", "title": "The Upper Paleolithic rock art of Ukraine between here and nowhere", "description": "The complex of Kamyana Mohyla is the westernmost rock art location of the Eurasian Steppe and the largest accumulation of cave art sites in the Eastern Europe. So far it has been believed that the complex contains the Upper Paleolithic cave art images as well as portable art collection that resemble the instances of Upper Paleolithic worldview. Though this belief lacked the support of archaeological context and chronological attribution it remained neither proved nor disputed. However, the application of digital photogrammetric tools allowed to perform the sub-millimeter surface modeling of the rock art objects and to re-examine and reconsider the engravings that were previously attributed to Pleistocene. The modeling results presented in this article revealed the complete absence of figurative images for the collection of portable art specimens and the dubious character of those for the cave art one. Therefore, the whole collection should be reconsidered, studied and attributed according to the state of the art and contemporary archaeological record in the region. This contribution attempts to think over the possible Upper Paleolithic origin of the motifs from Kamyana Mohyla in the light of new data and proposes three hypotheses towards the understanding of the rock art assemblage from one of the caves in the complex.", "keywords": ["0601 history and archaeology", "06 humanities and the arts", "Composite beings; Kamyana mohyla; Photogrammetry; Rock art; Ukraine; Upper paleolithic;", "01 natural sciences", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://iris.unive.it/bitstream/10278/5015525/1/1-s2.0-S1040618222003081-main.pdf"}, {"href": "https://iris.unito.it/bitstream/2318/1878502/1/1-s2.0-S1040618222003081-main.pdf"}, {"href": "https://doi.org/10.1016/j.quaint.2022.09.008"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Quaternary%20International", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.quaint.2022.09.008", "name": "item", "description": "10.1016/j.quaint.2022.09.008", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.quaint.2022.09.008"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-12-01T00:00:00Z"}}, {"id": "10.3389/fsoil.2022.1020869", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:22:22Z", "type": "Journal Article", "created": "2022-11-16", "title": "Deciphering the microbial composition of biodynamic preparations and their effects on the apple rhizosphere microbiome", "description": "<p>Soil microbial communities are crucial for plant growth and are already depleted by anthropogenic activities. The application of microbial transplants provides a strategy to restore beneficial soil traits, but less is known about the microbiota of traditional inoculants used in biodynamic agriculture. In this study, we used amplicon sequencing and quantitative PCR to decipher microbial communities of composts, biodynamic manures, and plant preparations from Austria and France. In addition, we investigated the effect of extracts derived from biodynamic manure and compost on the rhizosphere microbiome of apple trees. Microbiota abundance, composition, and diversity of biodynamic manures, plant preparations, and composts were distinct. Microbial abundances ranged between 1010-1011(bacterial 16S rRNA genes) and 109-1011(fungal ITS genes). The bacterial diversity was significantly higher in biodynamic manures compared to compost without discernible differences in abundance. Fungal diversity was not significantly different while abundance was increased in biodynamic manures. The microbial communities of biodynamic manures and plant preparations were specific for each production site, but all contain potentially plant-beneficial bacterial genera. When applied in apple orchards, biodynamic preparations (extracts) had the non-significant effect of reducing bacterial and fungal abundance in apple rhizosphere (4 months post-application), while increasing fungal and lowering bacterial Shannon diversity. One to four months after inoculation, individual taxa indicated differential abundance. We observed the reduction of the pathogenic fungusAlternaria, and the enrichment of potentially beneficial bacterial genera such asPseudomonas.Our study paves way for the science-based adaptation of empirically developed biodynamic formulations under different farming practices to restore the vitality of agricultural soils.</p", "keywords": ["2. Zero hunger", "0301 basic medicine", "0303 health sciences", "rhizosphere microbiome", "Engineering geology. Rock mechanics. Soil mechanics. Underground construction", "15. Life on land", "16S rRNA/ITS amplicon sequencing", "biodynamic farming", "Chemistry", "03 medical and health sciences", "biodynamic manures", "compost microbiome", "TA703-712", "ddc:580", "biodynamic preparations", "QD1-999", "Institut f\u00fcr Biochemie und Biologie"]}, "links": [{"href": "https://doi.org/10.3389/fsoil.2022.1020869"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Frontiers%20in%20Soil%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3389/fsoil.2022.1020869", "name": "item", "description": "10.3389/fsoil.2022.1020869", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3389/fsoil.2022.1020869"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-11-16T00:00:00Z"}}, {"id": "10.1038/s41467-017-00192-5", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:18:38Z", "type": "Journal Article", "created": "2017-08-02", "title": "Zhamanshin astrobleme provides evidence for carbonaceous chondrite and post-impact exchange between ejecta and Earth\u2019s atmosphere", "description": "Abstract<p>Chemical fingerprints of impacts are usually compromised by extreme conditions in the impact plume, and the contribution of projectile matter to impactites does not often exceed a fraction of per cent. Here we use chromium and oxygen isotopes to identify the impactor and impact-plume processes for Zhamanshin astrobleme, Kazakhstan. \uffce\uffb554Cr values up to 1.54 in irghizites, part of the fallback ejecta, represent the54Cr-rich extremity of the Solar System range and suggest a CI-like chondrite impactor. \uffce\uff9417O values as low as \uffe2\uff88\uff920.22\uffe2\uff80\uffb0 in irghizites, however, are incompatible with a CI-like impactor. We suggest that the observed17O depletion in irghizites relative to the terrestrial range is caused by partial isotope exchange with atmospheric oxygen (\uffce\uff9417O\uffe2\uff80\uff89=\uffe2\uff80\uff89\uffe2\uff88\uff920.47\uffe2\uff80\uffb0) following material ejection. In contrast, combined \uffce\uff9417O\uffe2\uff80\uff93\uffce\uffb554Cr data for central European tektites (distal ejecta) fall into the terrestrial range and neither impactor fingerprint nor oxygen isotope exchange with the atmosphere are indicated.</p>", "keywords": ["OXYGEN-ISOTOPE COMPOSITION", "NORDLINGER RIES IMPACT", "ORIGIN", "FRACTIONATION", "carbonaceous chondrite; post-impact exchange; ejecta; Earth\u2019s atmosphere", "Science", "Q", "TARGET ROCKS", "[SDU.ASTR.EP] Sciences of the Universe [physics]/Astrophysics [astro-ph]/Earth and Planetary Astrophysics [astro-ph.EP]", "551", "01 natural sciences", "Article", "IVORY-COAST TEKTITES", "13. Climate action", "CRATER", "GLASSES", "ELEMENTS", "WATER", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://www.nature.com/articles/s41467-017-00192-5.pdf"}, {"href": "https://doi.org/10.1038/s41467-017-00192-5"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature%20Communications", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s41467-017-00192-5", "name": "item", "description": "10.1038/s41467-017-00192-5", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41467-017-00192-5"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-08-09T00:00:00Z"}}, {"id": "10.1073/pnas.1708236114", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:19:10Z", "type": "Journal Article", "created": "2017-08-22", "title": "Late-stage magmatic outgassing from a volatile-depleted Moon", "description": "Significance<p>The \uffe2\uff80\uff9cRusty Rock\uffe2\uff80\uff9d 66095 is one of the most volatile-rich rocks from the Moon. The abundance and isotopic composition of volatile elements in the Rusty Rock demonstrates that its lunar interior source became highly depleted in volatile elements and compounds, including Zn, Cl, and Pb. Depletion of these and other volatile elements occurred during thermomagmatic evolution of the Moon and a magma ocean phase. The volatile-rich nature of some rocks on the lunar surface likely originates from extreme degassing and volatile loss from the Moon\uffe2\uff80\uff99s interior. Light zinc isotopic compositions in the Rusty Rock and in the lunar volcanic glass beads (74220, 15426) imply that these samples are partly derived from reservoirs that experienced vapor condensation from a volatile-poor Moon.</p>", "keywords": ["13. Climate action", "condensates", "magma ocean", "volatile-poor", "[SDU.STU.PL] Sciences of the Universe [physics]/Earth Sciences/Planetology", "Moon", "01 natural sciences", "Rusty Rock", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://pnas.org/doi/pdf/10.1073/pnas.1708236114"}, {"href": "https://doi.org/10.1073/pnas.1708236114"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Proceedings%20of%20the%20National%20Academy%20of%20Sciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1073/pnas.1708236114", "name": "item", "description": "10.1073/pnas.1708236114", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1073/pnas.1708236114"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-08-21T00:00:00Z"}}, {"id": "10.1111/1365-2745.12959", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:19:47Z", "type": "Journal Article", "created": "2018-04-16", "title": "Intransitive competition is common across five major taxonomic groups and is driven by productivity, competitive rank and functional traits", "description": "Abstract<p><p>Competition can be fully hierarchical or intransitive, and this degree of hierarchy is driven by multiple factors, including environmental conditions, the functional traits of the species involved or the topology of competition networks. Studies simultaneously analysing these drivers of competition hierarchy are rare. Additionally, organisms compete either directly or via interference competition for resources or space, within a local neighbourhood or across the habitat. Therefore, the drivers of competition could change accordingly and depend on the taxa studied.</p><p>We performed the first multi\uffe2\uff80\uff90taxon study on pairwise competition across major taxonomic groups, including experiments with vascular plants, mosses, saprobic fungi, aquatic protists and soil bacteria. We evaluated how general is competition intransitivity from the pairwise competition matrix including all species and also for each possible three\uffe2\uff80\uff90species combination (triplets). We then examined which species were likely to engage in competitive loops and the effects of environmental conditions, competitive rank and functional traits on intransitive competition.</p><p>We found some degree of competition intransitivity in all taxa studied, with 38% to 5% of triplets being intransitive. Variance in competitive rank between species and more fertile conditions strongly reduced intransitivity, with triplets composed of species differing widely in their competitive ranks much less likely to be intransitive.</p><p>Including functional traits of the species involved more than doubled the variation explained compared to models including competitive rank only. Both trait means and variance within triplets affected the odds of them being intransitive. However, the traits responsible and the direction of trait effects varied widely between taxa, suggesting that traits can have a wide variety of effects on competition.</p><p>Synthesis. We evaluated the drivers of competition across multiple taxa and showed that productivity and competitive rank are fundamental drivers of intransitivity. We also showed that not only the functional traits of each species, but also those of the accompanying species, determine competition intransitivity. Intransitive competition is common across multiple taxa but can dampen under fertile conditions or for those species with large variance in their competitive abilities. This provides a first step towards predicting the prevalence of intransitive competition in natural communities.</p></p", "keywords": ["saprobic fungi", "0106 biological sciences", "bacteria", " bryophytes", " competition hierarchy", " coexistence", " functional traits", " protists", " rock-paper-scissors", " saprobic fungi", " vascular plants", "01 natural sciences", "10127 Institute of Evolutionary Biology and Environmental Studies", "bryophytes", "XXXXXX - Unknown", "Competition hierarchy", "1110 Plant Science", "competition hierarchy", "functional traits", "vascular plants", "bacteria", "580", "protists", "Bacteria", "Vascular plants", "Bryophytes", "Saprobic fungi", "rock\u2013paper\u2013scissors", "Protists", "Ecolog\u00eda", "15. Life on land", "1105 Ecology", " Evolution", " Behavior and Systematics", "570 Life sciences; biology", "590 Animals (Zoology)", "competition", "Rock\u2013paper\u2013scissors", "2303 Ecology", "Functional traits"]}, "links": [{"href": "https://besjournals.onlinelibrary.wiley.com/doi/pdf/10.1111/1365-2745.12959"}, {"href": "https://doi.org/10.1111/1365-2745.12959"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Ecology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/1365-2745.12959", "name": "item", "description": "10.1111/1365-2745.12959", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/1365-2745.12959"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-04-16T00:00:00Z"}}, {"id": "10.1111/maps.13312", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:20:22Z", "type": "Journal Article", "created": "2019-06-10", "title": "Identification of a meteoritic component using chromium isotopic composition of impact rocks from the Lonar impact structure, India", "description": "Abstract<p>The existence of mass\uffe2\uff80\uff90independent chromium isotope variability of nucleosynthetic origin in meteorites and their components provides a means to investigate potential genetic relationship between meteorites and planetary bodies. Moreover, chromium abundances are depleted in most surficial terrestrial rocks relative to chondrites such that Cr isotopes are a powerful tool to detect the contribution of various types of extra\uffe2\uff80\uff90terrestrial material in terrestrial impactites. This approach can thus be used to constrain the nature of the bolide resulting in breccia and melt rocks in terrestrial impact structures. Here, we report the Cr isotope composition of impact rocks from the ~0.57\uffc2\uffa0Ma Lonar crater (India), which is the best\uffe2\uff80\uff90preserved impact structure excavated in basaltic target rocks. Results confirm the\uffc2\uffa0presence of a chondritic component in several bulk rock samples of up to 3%. The impactor that created the Lonar crater had a composition that was most likely similar to that of carbonaceous chondrites, possibly a CM\uffe2\uff80\uff90type chondrite.</p>", "keywords": ["TERRESTRIAL", "TARGET ROCKS", "SYSTEMATICS", "KeyWords Plus:TARGET ROCKS", "01 natural sciences", "PROJECTILES", "[SDU] Sciences of the Universe [physics]", "INSIGHTS", "105105 Geochemistry", "13. Climate action", "CRATER", "GLASSES", "105105 Geochemie", "MELT ROCKS", "PETROGRAPHY", "GEOCHEMISTRY", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1111/maps.13312"}, {"href": "https://doi.org/10.1111/maps.13312"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Meteoritics%20%26amp%3B%20Planetary%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/maps.13312", "name": "item", "description": "10.1111/maps.13312", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/maps.13312"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-06-09T00:00:00Z"}}, {"id": "10.1126/sciadv.1700571", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:20:28Z", "type": "Journal Article", "created": "2017-07-29", "title": "Gallium isotopic evidence for extensive volatile loss from the Moon during its formation", "description": "<p>The Moon is depleted in volatile elements compared to Earth. Gallium isotopes indicate a global-scale evaporation event.</p>", "keywords": ["Earth and Planetary Astrophysics (astro-ph.EP)", "2. Zero hunger", "GIANT IMPACT", "FOS: Physical sciences", "MANTLE", "01 natural sciences", "LUNAR-SAMPLES", "[SDU] Sciences of the Universe [physics]", "ZINC", "ABUNDANCES", "DIFFERENTIATION", "ROCKS", "13. Climate action", "IMPACT ORIGIN", "EARTH", "Research Articles", "MAGMA OCEAN", "Astrophysics - Earth and Planetary Astrophysics", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1126/sciadv.1700571"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Science%20Advances", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1126/sciadv.1700571", "name": "item", "description": "10.1126/sciadv.1700571", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1126/sciadv.1700571"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-07-07T00:00:00Z"}}, {"id": "10.1126/sciadv.aba3269", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:20:29Z", "type": "Journal Article", "created": "2020-06-03", "title": "Calcium isotopic evidence for the mantle sources of carbonatites", "description": "<p>Melting of recycled carbonate in the mantle explains the origin of carbonatitic magmas.</p>", "keywords": ["SILICATE ROCKS", "550", "CA CYCLE", "ORIGIN", "FRACTIONATION", "500", "NOBLE-GAS", "OLDOINYO-LENGAI", "01 natural sciences", "EVOLUTION", "12. Responsible consumption", "SUBDUCTION", "[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry", "13. Climate action", "CLINOPYROXENE", "[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/Geochemistry", "SERPENTINITES", "14. 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Deep-Sea Res 10: 221-231. Chlorophyll a and Phaeopigments were measured with a Turner 700 fluorometre following Shuman and Lorenzen (1975): Quantitative degradation of chlorophyll by a marine herbivore, Limnology and Oceanography, 20.", "keywords": ["Replicates", "PE2xx", "bottom max", "Chlorophyll a", "Depth", "Depth", " top/min", "DEPTH", " sediment/rock", "Hotspot Ecosystem Research on the Margins of European Seas HERMES", "Chlorophyll pigment equivalents", "sediment rock", "Chloroplastic pigment equivalents", "Phaeopigments", " standard deviation", "Chloroplastic pigment equivalents", " standard deviation", "European Margin Strata Formation (EuroSTRATAFORM)", "DEPTH", "top min", "Earth System Research", "Depth", " bottom/max", "14. Life underwater", "standard deviation", "Phaeopigments", "Chlorophyll a", " standard deviation", "European Margin Strata Formation EuroSTRATAFORM", "Hotspot Ecosystem Research on the Margins of European Seas (HERMES)", "MultiCorer"], "contacts": [{"organization": "Garcia, Rosa, Thomsen, Laurenz,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1594/pangaea.615227"}, {"rel": "self", "type": "application/geo+json", "title": "10.1594/pangaea.615227", "name": "item", "description": "10.1594/pangaea.615227", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1594/pangaea.615227"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2007-01-01T00:00:00Z"}}, {"id": "10.1594/pangaea.105302", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:21:11Z", "type": "Dataset", "title": "Alkenones and SST of sediment core GeoB3007-3", "keywords": ["Alkenone", " C37/C38m ratio", "Octatriaconta-16E", "23E-dien-2-one", "Alkenone", " C38:3Et+C38:2Et+C38:3Me+C38:2Me", "Octatriaconta-9E", "16E", "23E-trien-2-one", "unsaturation index UK38Me", "Sea surface temperature", "annual mean", "Octatriaconta-16E", "23E-dien-3-one", "Calculated from C37 alkenones Prahl Wakeham", "unsaturation index UK38", "C38 3Et C38 2Et", "23E trien 2 one", "University of Bremen GeoB", "C38 3Et C38 2Et C38 3Me C38 2Me", "Alkenone", " unsaturation index UK38", "Geosciences", " University of Bremen (GeoB)", "Octatriaconta 9E", "unsaturation index UK 37", "Calculated", "1987", "C37 C38 ratio", "MultiCorer", "Gas chromatography", "1993", "in Engel", "23E dien 2 one", "unsaturation index UK38Et", "sediment rock", "16E", "Calculated from C38 alkenones Brassel", "23E dien 3 one", "Natural Sciences", "C37 C38m ratio", "Geosciences", "Alkenone", " unsaturation index UK'37", "DEPTH", " sediment/rock", "Alkenone", " C38:3Et+C38:2Et", "Salinity correction factor", "Sea surface temperature", " annual mean", "Alkenone", " C37/C38 ratio", "AGE", "M31 3", "Calculated from C38 alkenones (Brassel", " 1993", " in Engel", " Organic Geochemistry)", "Meteor 1986", "Calculated from C37 alkenones (Prahl &amp; Wakeham", " 1987)", "Alkenone", " unsaturation index UK38Et", "M31/3", "Meteor (1986)", "Alkenone", " C37/C38e ratio", "Calculated from C37 alkenones (Prahl & Wakeham", " 1987)", "23E trien 3 one", "C37 C38e ratio", "Alkenone", " unsaturation index UK38Me", "Octatriaconta-9E", "16E", "23E-trien-3-one", "Alkenone", " C38:3Me+C38:2Me", "DEPTH", "Organic Geochemistry", "Octatriaconta 16E", "Alkenone", "C38 3Me C38 2Me"], "contacts": [{"organization": "Budziak, D\u00f6rte, M\u00fcller, Peter J,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1594/pangaea.105302"}, {"rel": "self", "type": "application/geo+json", "title": "10.1594/pangaea.105302", "name": "item", "description": "10.1594/pangaea.105302", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1594/pangaea.105302"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2003-01-01T00:00:00Z"}}, {"id": "10.1594/pangaea.261535", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:21:11Z", "type": "Dataset", "title": "Physical properties of sediment core GIK23291-2", "keywords": ["wet bulk", "M7/3", "Gravity corer (Kiel type)", "Density", "DEPTH", " sediment/rock", "Quaternary Environment of the Eurasian North QUEEN", "Water content", " dry mass", "dry mass", "M7 3", "Density", " dry bulk", "Calculated", "Pore number", "Meteor 1986", "Water content", "Meteor (1986)", "dry bulk", "Calculated from mass volume", "Global Environmental Change: The Northern North Atlantic (SFB313)", "sediment rock", "Gravity corer Kiel type", "Density", " wet bulk", "Calculated from weight/volume", "Quaternary Environment of the Eurasian North (QUEEN)", "DEPTH", "Global Environmental Change The Northern North Atlantic SFB313", "Earth System Research", "Calculated from mass/volume", "Porosity"], "contacts": [{"organization": "Holler, Peter R, Kassens, Heidemarie,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1594/pangaea.261535"}, {"rel": "self", "type": "application/geo+json", "title": "10.1594/pangaea.261535", "name": "item", "description": "10.1594/pangaea.261535", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1594/pangaea.261535"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2005-01-01T00:00:00Z"}}, {"id": "10.1594/pangaea.351631", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:21:11Z", "type": "Dataset", "title": "Calcium carbonate content of sediment core SO79-167KG", "keywords": ["sediment rock", "Sonne", "1994", "Box corer (Reineck)", "DEPTH", "Earth System Research", "Box corer Reineck", "Element analysis (Klosa", " 1994)", "DEPTH", " sediment/rock", "Calcium carbonate", "Element analysis Klosa", "SO79"], "contacts": [{"organization": "Weber, Michael E, Wiedicke-Hombach, Michael, Riech, Volkher, Erlenkeuser, Helmut,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1594/pangaea.351631"}, {"rel": "self", "type": "application/geo+json", "title": "10.1594/pangaea.351631", "name": "item", "description": "10.1594/pangaea.351631", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1594/pangaea.351631"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "1995-01-01T00:00:00Z"}}, {"id": "10.1594/pangaea.972412", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:21:12Z", "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": "10.1594/pangaea.972409", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:21:12Z", "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": "10.21258/1836657", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:21:30Z", "type": "Dataset", "title": "Swiss national forest inventory - Result table No. 1250637", "keywords": ["state 1983/85", "biogeographical region", "growing stock (stemwood)", "accessible forest without shrub forest", "protection forest against rockfall (2022)", "altitudinal vegetation belts (NaiS; 6 classes)", "1.4-km grid", "NFI1"], "contacts": [{"organization": "Abegg, M., Ahles, P., Allgaier Leuch, B., Cioldi, F., Didion, M., D\u00fcggelin, C., Fischer, C., Herold, A., Meile, R., Rohner, B., R\u00f6sler, E., Speich, S., Temperli, C., Traub, B.,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.21258/1836657"}, {"rel": "self", "type": "application/geo+json", "title": "10.21258/1836657", "name": "item", "description": "10.21258/1836657", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.21258/1836657"}, {"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": "10.3389/fsoil.2023.1240930", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:22:22Z", "type": "Journal Article", "created": "2023-07-11", "title": "Editorial: Greenhouse gas measurements in underrepresented areas of the world", "description": "Open Access\u0645\u0642\u0627\u0644 \u062a\u062d\u0631\u064a\u0631\u064a Front. Soil Sci., 11 July 2023Sec. \u0627\u0644\u0643\u064a\u0645\u064a\u0627\u0621 \u0627\u0644\u062d\u064a\u0648\u064a\u0629 \u0644\u0644\u062a\u0631\u0628\u0629 \u0648\u0631\u0643\u0648\u0628 \u0627\u0644\u062f\u0631\u0627\u062c\u0627\u062a \u0627\u0644\u063a\u0630\u0627\u0626\u064a\u0629 \u0627\u0644\u0645\u062c\u0644\u062f 3 - 2023 | https://doi.org/10.3389/fsoil.2023.1240930", "keywords": ["Soil nutrients", "Mechanics and Transport in Unsaturated Soils", "representativeness", "Oceanography", "Greenhouse gas", "Environmental science", "climate change mitigation", "12. Responsible consumption", "Impact of Climate Change on Forest Wildfires", "Engineering", "greenhouse gases", "Soil water", "11. Sustainability", "TA703-712", "QD1-999", "Biology", "Civil and Structural Engineering", "Soil science", "2. Zero hunger", "Global and Planetary Change", "nitrous oxide", "Geography", "Ecology", "greenhouse gas emissions", "Global Forest Drought Response and Climate Change", "methane", "carbon dioxide", "Cycling", "Geology", "Forestry", "Engineering geology. Rock mechanics. Soil mechanics. Underground construction", "FOS: Earth and related environmental sciences", "Biogeochemistry", "15. Life on land", "6. Clean water", "livestock", "Chemistry", "climate change", "Global Emissions", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "Physical Sciences", "Nutrient"]}, "links": [{"href": "https://doi.org/10.3389/fsoil.2023.1240930"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Frontiers%20in%20Soil%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3389/fsoil.2023.1240930", "name": "item", "description": "10.3389/fsoil.2023.1240930", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3389/fsoil.2023.1240930"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-07-11T00:00:00Z"}}, {"id": "10.3389/fsoil.2023.1268037", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:22:22Z", "type": "Journal Article", "created": "2023-12-18", "title": "Sustainable soil and land management: a systems-oriented overview of scientific literature", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Healthy soil is vital for our wellbeing and wealth. However, increasing demand for food and biomass may lead to unsustainable soil and land management practices that threaten soils. Other degradation processes such as soil sealing also endanger soil resources. Identifying and accessing the best available knowledge is crucial to address related sustainability issues and promote the needed transition towards sustainable soil and land management practices. Such knowledge has to cover all knowledge domains, system knowledge, target knowledge, and transformation knowledge. However, a comprehensive overview of existing research addressing societal needs related to soil is still missing, which hinders the identification of knowledge gaps. This study provides a detailed analysis of scientific literature to identify ongoing research activities and trends. A quantitative and qualitative analysis of scientific literature related to sustainable soil and land management was conducted. A systems-oriented analytical framework was used that combines soil and land related societal challenges with related knowledge domains. Our analysis revealed a significant increase in scientific publications and related interest in soil and land use-related research, above the average increase of publications within all scientific fields. Different forms of reduction and remediation of soil degradation processes (e.g. erosion, contamination) have been studied most extensively. Other topic areas like land take mitigation, soil biodiversity increase, increase of ecosystem services provision and climate change mitigation and adaption seem to be rather recent concerns, less investigated. We could highlight the importance of context-specific research, as different regions require different practices. For instance, boreal, tropical, karst and peatland regions were less studied. Furthermore, we found that diversifying soil management practices such as agroforestry or including livestock into arable systems are valuable options for increasing biomass, mitigating/adapting to climate change, and improving soil related ecosystem services. A recent trend towards the latter research topic indicates the transition from a soil conservation-oriented perspective to a soil service-oriented perspective, which may be better suited to integrate the social and economic dimensions of soil health improvement alongside the ecological dimension.</p></article>", "keywords": ["Societal challenge", "2. Zero hunger", "CorTexT", "Soil mission", "Knowledge gaps", "Engineering geology. Rock mechanics. Soil mechanics. Underground construction", "[SDV.SA.SDS]Life Sciences [q-bio]/Agricultural sciences/Soil study", "15. Life on land", "societal challenge", "333", "6. Clean water", "Literature analysis", "knowledge gaps", "12. Responsible consumption", "Chemistry", "13. Climate action", "11. Sustainability", "TA703-712", "Stock assessment", "literature analysis", "[SDV.SA.SDS] Life Sciences [q-bio]/Agricultural sciences/Soil study", "stock assessment", "QD1-999", "soil mission"]}, "links": [{"href": "https://doi.org/10.3389/fsoil.2023.1268037"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Frontiers%20in%20Soil%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3389/fsoil.2023.1268037", "name": "item", "description": "10.3389/fsoil.2023.1268037", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3389/fsoil.2023.1268037"}, {"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": "10.3389/fsoil.2025.1549290", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:22:22Z", "type": "Journal Article", "created": "2025-05-23", "title": "Mapping the conceptual and intellectual structure of soil health research (1996\u20132021): a terms co-occurrence and co-cited reference network analysis", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Soil health has emerged as a critical area of research due to its role in sustainable agriculture, environmental conservation, ecosystem services and policy frameworks like the EU Soil Strategy. Since the 1990s, research has expanded rapidly, yet unevenly, marked by fragmented thematic priorities and methodological approaches. This study employs bibliometric analyses\u2014term co-occurrence and co-cited reference networks\u2014to map the conceptual and intellectual structure of soil health research from 1996 to 2021. By analyzing 984 peer-reviewed articles, we identified three major research clusters: (1) Agricultural Research &amp;amp; Soil Management, emphasizing agronomic practices such as fertilization and crop yield optimization; (2) Soil Health &amp;amp; Agricultural Sustainability, focusing on carbon dynamics, conservation tillage, and policy alignment; and (3) Microbial Ecology &amp;amp; Soil Health, highlighting soil biota, enzyme activity, and long-term biological impacts. Seminal works by Karlen et al., which established foundational frameworks linking soil quality to ecosystem services, and Mbuthia et al., demonstrating microbial resilience under conservation practices, emerged as pivotal drivers of field evolution. Emerging trends favor sustainable practices, amendments, and biological indicators. The analysis reveals critical gaps, including limited integration of pedological modeling to quantify ecosystem services and insufficient long-term studies on conservation agriculture. These findings advocate interdisciplinary collaboration among agronomists, microbiologists, policymakers, and climate scientists to align soil health metrics with global targets (e.g., SDGs, EU Soil Monitoring Law), providing a roadmap to integrate soil health into climate-smart land-use policies.</p></article>", "keywords": ["sustainable agriculture", "Chemistry", "bibliometric analysis", "soil health", "TA703-712", "Engineering geology. Rock mechanics. Soil mechanics. Underground construction", "co-cited network analysis", "soil management", "terms co-occurrence", "QD1-999"], "contacts": [{"organization": "Mohamed Houssemeddine Sellami, Mohamed Houssemeddine Sellami, Mauro Mori, Fabio Terribile,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.3389/fsoil.2025.1549290"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Frontiers%20in%20Soil%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3389/fsoil.2025.1549290", "name": "item", "description": "10.3389/fsoil.2025.1549290", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3389/fsoil.2025.1549290"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-05-23T00:00:00Z"}}, {"id": "10.2478/botcro-2014-0003", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-03T16:22:06Z", "type": "Journal Article", "created": "2014-07-02", "description": "Abstract <p>Optimal grazing pressure on rocky pastures is beneficial to the development of plant species and maintenance of plant diversity. Both abandonment of grazing and overgrazing gradually reduce plant diversity. This paper correlated abundance patterns of the flora on rocky pastures with the values of the chemical composition of the soil resulting from the degree of sheep grazing intensity. The study was carried out in the period from 2008 to 2010 on the islands of Pag, Krk and Cres. At 30 sites, 310 taxa of vascular plants were found. The highest plant diversity and 220 plant taxa were found on moderately grazed pastures. Abandoned pastures with a total of 93 plant taxa observed show the dominance of phanerophytes (35.5%) and the highest proportion of the Mediterranean floral element when compared to pastures of moderate and heavy grazing intensity. The highest concentration of total nitrogen in the soil (0.71%) was recorded on plots of heavy grazing intensity. The results of the study indicate that moderate grazing intensity, from 1 to 1.5 sheep ha\uffe2\uff88\uff921, can be recommended on the northern Adriatic islands. This should contribute not only to the preservation of plant diversity, but also to the improvement of ecological sheep farming.</p>", "keywords": ["chemical composition of the soil; Mediterranean flora; rocky pasture; sheep grazing intesity", "0106 biological sciences", "2. Zero hunger", "13. Climate action", "Mediterranean flora", "sheep grazing intesity", "chemical composition of the soil", "rocky pasture", "15. Life on land", "01 natural sciences"]}, "links": [{"href": "https://doi.org/10.2478/botcro-2014-0003"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Acta%20Botanica%20Croatica", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.2478/botcro-2014-0003", "name": "item", "description": "10.2478/botcro-2014-0003", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.2478/botcro-2014-0003"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2014-10-28T00:00:00Z"}}, {"id": "10.24849/j.geot.2018.142.01", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:22:06Z", "type": "Journal Article", "created": "2018-03-27", "title": "Microzonation of the liquefaction susceptibility: case study in the lower Tagus valley", "description": "<p>Este trabalho enquadra-se no projeto europeu de investiga\uffc3\uffa7\uffc3\uffa3o LIQUEFACT, do qual a Faculdade de Engenharia da Universidade do Porto \uffc3\uffa9 parceira e associada. Durante a realiza\uffc3\uffa7\uffc3\uffa3o deste trabalho, foi recolhida uma vasta informa\uffc3\uffa7\uffc3\uffa3o geol\uffc3\uffb3gico-geot\uffc3\uffa9cnica existente, de modo a constituir uma base de dados s\uffc3\uffb3lida para a escolha de um s\uffc3\uffadtio-piloto, para realiza\uffc3\uffa7\uffc3\uffa3o de ensaios in situ complementares, com vista \uffc3\uffa0 elabora\uffc3\uffa7\uffc3\uffa3o de um microzonamento de suscetibilidade \uffc3\uffa0 liquefa\uffc3\uffa7\uffc3\uffa3o. A an\uffc3\uffa1lise dessa informa\uffc3\uffa7\uffc3\uffa3o geot\uffc3\uffa9cnica (sobretudo SPT, CPT e CH) incluiu a avalia\uffc3\uffa7\uffc3\uffa3o de \uffc3\uffadndices de risco de liquefa\uffc3\uffa7\uffc3\uffa3o, nomeadamente o Fator de Seguran\uffc3\uffa7a \uffc3\uffa0 liquefa\uffc3\uffa7\uffc3\uffa3o (FSliq), \uffc3\uff8dndice Potencial de Liquefa\uffc3\uffa7\uffc3\uffa3o (LPI) e N\uffc3\uffbamero de Severidade de Liquefa\uffc3\uffa7\uffc3\uffa3o (LSN), tendose escolhido um s\uffc3\uffadtio piloto na zona da Lez\uffc3\uffadria Grande de Vila Franca de Xira. A campanha experimental envolveu ensaios SPT, CPTu, SDMT, diversos m\uffc3\uffa9todos geof\uffc3\uffadsicos e ainda a recolha de amostras de alta qualidade para caracteriza\uffc3\uffa7\uffc3\uffa3o laboratorial. O tratamento dos resultados destes ensaios foi subdividido em tr\uffc3\uffaas tipos de an\uffc3\uffa1lises, em termos de \uffc3\uff8dndices de Risco, da classifica\uffc3\uffa7\uffc3\uffa3o de acordo com VS30, e ainda baseada nos assentamentos e deslocamentos laterais esperados. Destas an\uffc3\uffa1lises, foi poss\uffc3\uffadvel estabelecer e propor um microzonamento preliminar de suscetibilidade \uffc3\uffa0 liquefa\uffc3\uffa7\uffc3\uffa3o induzida por sismos.</p>", "keywords": ["Baixo Vale do Tejo", "QE1-996.5", "Liquefa\u00e7\u00e3o s\u00edsmica", "Microzonamento", "Suscetibilidade \u00e0 Liquefa\u00e7\u00e3o", "TA703-712", "Geology", "Engineering geology. Rock mechanics. Soil mechanics. Underground construction"]}, "links": [{"href": "https://doi.org/10.24849/j.geot.2018.142.01"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Geotecnia", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.24849/j.geot.2018.142.01", "name": "item", "description": "10.24849/j.geot.2018.142.01", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.24849/j.geot.2018.142.01"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-10-23T00:00:00Z"}}, {"id": "10.5061/dryad.djh9w0w67", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:23:13Z", "type": "Dataset", "created": "2023-11-08", "title": "Data for: Stabilisation of soil organic matter with rock dust partially counteracted by plants", "description": "unspecifiedIn this study, the effect of rock dust addition on both soil inorganic and  organic carbon contents was investigated. Soil chemical changes were  measured, including soil organic carbon (totals and fractions), soil  inorganic carbon, pH, electric conductivity, and water-extractable and  ammonium acetate-extractable ion levels (Ca, Mg, Al, Fe, Mn, Fe, Zn, Si).  In addition, the effect of plants on soil chemistry and rocks on plant  growth (biomass) and plant ion uptake was studied. The results  demonstrated rock weathering during the 6 months incubation period and a  stabilisation of organic carbon. Plants partially counteracted the  stabilisation of soil organic carbon. This was attributed to interactions  between soil chemical changes induced by rock dust, plant exudation, and  subsequent soil organic carbon stabilisation mechanisms.", "keywords": ["2. Zero hunger", "soil organic carbon", "soil carbon sequestration", "13. Climate action", "Particulate organic matter", "aggregate carbon", "FOS: Earth and related environmental sciences", "15. Life on land", "enhanced rock weathering", "Basalt", "mineral associated organic matter", "6. Clean water", "inorganic carbon"], "contacts": [{"organization": "Buss, Wolfram, Hasemer, Heath, Ferguson, Scott, Borevitz, Justin,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5061/dryad.djh9w0w67"}, {"rel": "self", "type": "application/geo+json", "title": "10.5061/dryad.djh9w0w67", "name": "item", "description": "10.5061/dryad.djh9w0w67", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5061/dryad.djh9w0w67"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-11-27T00:00:00Z"}}, {"id": "10.5281/zenodo.15847855", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:25:02Z", "type": "Dataset", "title": "Enhanced rock weathering altered soil organic carbon fluxes in a plant trial", "description": "Enhanced rock weathering altered soil organic carbon fluxes in a plant triel. Raw and processed datasets in support of the findings of Boito et al. (2025).", "keywords": ["Climate change mitigation", "Soil organic carbon", "Earthworm", "Enhanced rock weathering", "Plants", "CO2 emissions"], "contacts": [{"organization": "Boito, Lucilla, Steinwidder, Laura, Rijnders, Jet, Berwouts, Jesse, Janse, Sarah, Niron, Harun, Roussard, Jasper, Vicca, Sara, Vienne, Arthur,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5281/zenodo.15847855"}, {"rel": "self", "type": "application/geo+json", "title": "10.5281/zenodo.15847855", "name": "item", "description": "10.5281/zenodo.15847855", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5281/zenodo.15847855"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-07-09T00:00:00Z"}}, {"id": "10.5281/zenodo.16412421", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-03T16:25:04Z", "type": "Journal Article", "created": "2024-12-26", "title": "Separating fast from slow cycling soil organic carbon \u2013 A multi-method comparison on land use change sites", "description": "Soil organic carbon (SOC) is significantly affected by land use change (LUC). Consequently, LUC is a major controlling factor of total SOC contents and SOC pool dynamics. Several methods have been developed to assess distinct SOC pools, which includes particle size separation, thermal analysis and soil reflectance mid-infrared spectroscopy. All of which are considered to have a potential as high through put methods to generate large datasets. Here, we used 23 sites covering six different types of LUC to assess differences in fast and slow cycling SOC derived from three approaches. We used i) particle size fractionation to obtain coarse (>50\u00a0\u00a0\u00b5m) and fine (<50\u00a0\u00a0\u00b5m) SOC fractions; ii) thermal Rock-Eval\u00ae 6 analysis in compilation with the PARTYSOCv2.0EU model to estimate active and stable SOC pools and iii) mid-infrared spectroscopy to determine the relative SOC composition and derive fast (aliphatic compounds) and slow (aromatic/carboxylic compounds) cycling SOC pools. The particle size SOC fractions and thermal SOC pools showed similar dynamics but differed substantially in the magnitude with LUC. The fine SOC fraction contained around two-thirds of the total SOC across all land uses and was strongly responsive by nearly matching the relative changes of total SOC (slope of 0.76 and R2\u00a0=\u00a00.91). Therefore, the fine fraction SOC might be more dynamic than considered until now. In comparison, the stable SOC pool calculated using PARTYSOCv2.0EU was less responsive to the relative changes (slope of 0.43 and R2\u00a0=\u00a00.72) and contained around 40\u00a0% of the total SOC. This underlines that both physical and thermal approaches separate biogeochemically distinct pools. The qualitative assessment by mid-infrared spectroscopy related well to the thermal SOC pools but not to the particle size fractions. The initial land-use SOC composition, as a ratio of the corresponding fast and slow cycling SOC pool, can be a suitable predictor for SOC evolution. This was particularly true for thermal and mid-infrared spectroscopy derived SOC pools. We show that three conceptually different methods (physical, thermal and mid-infrared spectroscopic) are suitable to determine SOC pool changes for a large diversity of LUC, but the sensitivity of the individual pools can differ strongly, depending on the method.", "keywords": ["Particle size fractionation", "Science", "Q", "Rock-Eval\u00ae analysis", "Cropland", "Forest", "Grassland", "Mid-infrared spectroscopy"]}, "links": [{"href": "https://doi.org/10.5281/zenodo.16412421"}, {"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": "10.5281/zenodo.16412421", "name": "item", "description": "10.5281/zenodo.16412421", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5281/zenodo.16412421"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-01-01T00:00:00Z"}}, {"id": "10045/75093", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:26:40Z", "type": "Journal Article", "created": "2018-04-16", "title": "Intransitive competition is common across five major taxonomic groups and is driven by productivity, competitive rank and functional traits", "description": "Abstract<p><p>Competition can be fully hierarchical or intransitive, and this degree of hierarchy is driven by multiple factors, including environmental conditions, the functional traits of the species involved or the topology of competition networks. Studies simultaneously analysing these drivers of competition hierarchy are rare. Additionally, organisms compete either directly or via interference competition for resources or space, within a local neighbourhood or across the habitat. Therefore, the drivers of competition could change accordingly and depend on the taxa studied.</p><p>We performed the first multi\uffe2\uff80\uff90taxon study on pairwise competition across major taxonomic groups, including experiments with vascular plants, mosses, saprobic fungi, aquatic protists and soil bacteria. We evaluated how general is competition intransitivity from the pairwise competition matrix including all species and also for each possible three\uffe2\uff80\uff90species combination (triplets). We then examined which species were likely to engage in competitive loops and the effects of environmental conditions, competitive rank and functional traits on intransitive competition.</p><p>We found some degree of competition intransitivity in all taxa studied, with 38% to 5% of triplets being intransitive. Variance in competitive rank between species and more fertile conditions strongly reduced intransitivity, with triplets composed of species differing widely in their competitive ranks much less likely to be intransitive.</p><p>Including functional traits of the species involved more than doubled the variation explained compared to models including competitive rank only. Both trait means and variance within triplets affected the odds of them being intransitive. However, the traits responsible and the direction of trait effects varied widely between taxa, suggesting that traits can have a wide variety of effects on competition.</p><p>Synthesis. We evaluated the drivers of competition across multiple taxa and showed that productivity and competitive rank are fundamental drivers of intransitivity. We also showed that not only the functional traits of each species, but also those of the accompanying species, determine competition intransitivity. Intransitive competition is common across multiple taxa but can dampen under fertile conditions or for those species with large variance in their competitive abilities. This provides a first step towards predicting the prevalence of intransitive competition in natural communities.</p></p", "keywords": ["saprobic fungi", "0106 biological sciences", "01 natural sciences", "10127 Institute of Evolutionary Biology and Environmental Studies", "bryophytes", "XXXXXX - Unknown", "Competition hierarchy", "1110 Plant Science", "competition hierarchy", "functional traits", "vascular plants", "bacteria", "580", "protists", "Bacteria", "Vascular plants", "Bryophytes", "Saprobic fungi", "rock\u2013paper\u2013scissors", "Protists", "Ecolog\u00eda", "15. Life on land", "1105 Ecology", " Evolution", " Behavior and Systematics", "570 Life sciences; biology", "590 Animals (Zoology)", "competition", "Rock\u2013paper\u2013scissors", "2303 Ecology", "Functional traits"]}, "links": [{"href": "https://besjournals.onlinelibrary.wiley.com/doi/pdf/10.1111/1365-2745.12959"}, {"href": "https://doi.org/10045/75093"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Ecology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10045/75093", "name": "item", "description": "10045/75093", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10045/75093"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-04-16T00:00:00Z"}}, {"id": "10568/131171", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:27:01Z", "type": "Journal Article", "created": "2023-07-11", "title": "Editorial: Greenhouse gas measurements in underrepresented areas of the world", "description": "Open Access\u0645\u0642\u0627\u0644 \u062a\u062d\u0631\u064a\u0631\u064a Front. Soil Sci., 11 July 2023Sec. \u0627\u0644\u0643\u064a\u0645\u064a\u0627\u0621 \u0627\u0644\u062d\u064a\u0648\u064a\u0629 \u0644\u0644\u062a\u0631\u0628\u0629 \u0648\u0631\u0643\u0648\u0628 \u0627\u0644\u062f\u0631\u0627\u062c\u0627\u062a \u0627\u0644\u063a\u0630\u0627\u0626\u064a\u0629 \u0627\u0644\u0645\u062c\u0644\u062f 3 - 2023 | https://doi.org/10.3389/fsoil.2023.1240930", "keywords": ["Soil nutrients", "Mechanics and Transport in Unsaturated Soils", "representativeness", "Oceanography", "Greenhouse gas", "Environmental science", "climate change mitigation", "12. Responsible consumption", "Impact of Climate Change on Forest Wildfires", "Engineering", "greenhouse gases", "Soil water", "11. Sustainability", "TA703-712", "QD1-999", "Biology", "Civil and Structural Engineering", "Soil science", "2. Zero hunger", "Global and Planetary Change", "nitrous oxide", "Geography", "Ecology", "greenhouse gas emissions", "Global Forest Drought Response and Climate Change", "methane", "carbon dioxide", "Cycling", "Geology", "Forestry", "Engineering geology. Rock mechanics. Soil mechanics. Underground construction", "FOS: Earth and related environmental sciences", "Biogeochemistry", "15. Life on land", "6. Clean water", "livestock", "Chemistry", "climate change", "Global Emissions", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "Physical Sciences", "Nutrient"]}, "links": [{"href": "https://doi.org/10568/131171"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Frontiers%20in%20Soil%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10568/131171", "name": "item", "description": "10568/131171", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10568/131171"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-07-11T00:00:00Z"}}, {"id": "3146683732", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:28:38Z", "type": "Dataset", "title": "Yedoma domain Mineral Concentrations Assessment (YMCA)", "description": "Mineral elements play a crucial role for organic carbon stabilization, which is key for organic carbon mineralization rates in soils. With thawing permafrost, especially in ice-rich regions such as the Yedoma domain, vast amounts of organic carbon previously stored in deep frozen deposits are unlocked and therefore available to undergo microbial mineralization leading to potential carbon dioxide and methane emissions. Mineral elements interfere with organic carbon degradation through various processes: i) mineral protection (aggregation, adsorption, and complexation) stabilizes organic carbon and mitigates its mineralization, and ii) change in mineral nutrients availability affects microorganisms growth and metabolic activity. Despite huge efforts to assess organic carbon stocks and lability in permafrost regions, there is a lack of studies on the mineral component assessment, which we aim to close with this dataset. Here, we provide a large-scale Yedoma domain Mineral Concentrations Assessment (YMCA) dataset of never thawed (since deposition) ice-rich Yedoma permafrost and previously thawed and partly refrozen Alas deposits. We used a portable X-ray fluorescence device (pXRF) for Si, Al, Fe, Ca, K, Ti, Mn, Zn, Sr and Zr concentration measurements on 1,292 sediment samples. Portable XRF measured concentrations trueness was calibrated using standard alkaline fusion and ICP-OES measurement from a subset of 144 samples (R\u00b2 from 0.725 to 0.996). This methodology lead to the creation of the Yedoma domain Mineral Concentration Assessment (YMCA) dataset, a necessary step to estimate mineral element stocks in never thawed Yedoma and previously thawed Alas deposits. Practically, the YMCA dataset is organized as follow: (i) all site and sample properties: sample ID, type of deposit, site location, profile ID, GPS coordinates, country, lithology, unconsolidated sediment type, geological epoch, samples depth below surface level (b.s.l) or height above sea/river level (a.s.l), sediment characteristics, bulk density, gravimetric and absolute ice content, total organic carbon content; (ii) the Si, Al, Fe, Ca, K, Ti, Mn, Zn, Sr and Zr concentrations (corrected based on linear regressions) in Yedoma and Alas deposits (n=1292).", "keywords": ["Density", "Permafrost", "Profile ID", "gravimetric", "Density", " bulk", " permafrost", "Aluminium", "total", "Sample code/label", "Portable X ray fluorescence device", "Titanium", "Mineral element", "Yedoma", "Portable X-ray fluorescence device", "Description", "Number", "Lithology/composition/facies", "Sample code label", "6. Clean water", "Deposit type", "Country", "sediment rock", "Zinc", "Earth System Research", "Alas", "Profile", "Silicon", "Lithology composition facies", "Height above sea level", "organic", "Iron", "Site", "DEPTH", " sediment/rock", "bulk", "Ice content", " gravimetric", "LONGITUDE", "Organic carbon", "Manganese", "Sediment type", "organic carbon", "15. Life on land", "Ice content", "Carbon", "Epoch", "Sample ID", "13. Climate action", "Strontium", "DEPTH", "LATITUDE", "Potassium", "Calcium", "Zirconium", "permafrost", "Carbon", " organic", " total"]}, "links": [{"href": "https://doi.org/3146683732"}, {"rel": "self", "type": "application/geo+json", "title": "3146683732", "name": "item", "description": "3146683732", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/3146683732"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-01-01T00:00:00Z"}}, {"id": "2158/1353729", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:27:56Z", "type": "Journal Article", "created": "2019-03-25", "title": "Chemical and mineralogical analyses on stones from Sagunto Castle (Spain)", "description": "For the first time, an archaeometric study was carried out on the carbonate rock ashlars of the Sagunto Castle. The studied site is one of the most important and best preserved Spanish archaeological and architectural monuments, characterized by different construction phases from the Roman period to Modern Ages. Forty samples collected from thirteen different structures of Sagunto Castle and two quarries, located in the Sagunto's hill were used for comparative purposes. The samples were analyzed by X-ray diffraction, X-ray fluorescence and inductively coupled plasma mass spectrometry to determine their mineralogical and elemental composition. The obtained data show similar chemical and mineralogical features between the rocks outcropping in the city quarries and some of those employed to build the structures, suggesting that rocks could have been used to build the structures from different periods along the centuries.", "keywords": ["Building stone; Chemistry; Fortress; Middle ages; Mineralogy; Remains; Roman period", "Building stone; Fortress; Remains; Chemistry; Mineralogy; Roman period; Middle ages", "archaeometrics; carbonate rock ashlars; X-ray fluorescence and inductively coupled plasma mass spectrometry", "01 natural sciences", "0104 chemical sciences", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://iris.unica.it/bitstream/11584/298931.2/3/Ramaciotti%20et%20al%202018_1-s2.0-S2352409X18307454-main.pdf"}, {"href": "https://doi.org/2158/1353729"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Archaeological%20Science%3A%20Reports", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "2158/1353729", "name": "item", "description": "2158/1353729", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2158/1353729"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-04-01T00:00:00Z"}}, {"id": "42aefcf3-b6d6-4620-8abd-8b005c070067", "type": "Feature", "geometry": null, "properties": {"updated": "2025-09-25T09:15:25", "type": "Dataset", "language": "en", "title": "Water Framework Directive Groundwater Waterbodies - Cycle 2", "description": "The EU Water Framework Directive (2000/60/EC) (WFD) establishes a framework for the protection, improvement and management of surface water and groundwater. 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If a groundwater is capable of serving 10m\u00b3/day of abstraction, or has other significance, it is designated as a groundwater waterbody.", "formats": [{"name": "HTML"}], "keywords": ["administration", "bedrock", "environment", "gravel", "ground-waterbodies", "groundwater", "groundwater-body", "groundwater-protection", "groundwater-quality", "hydrography", "ie", "soil", "water", "water-quality", "water-quality-monitoring", "waterbody", "wfd"], "contacts": [{"organization": "Environmental Protection Agency", "roles": ["creator"]}, {"organization": "https://data.gov.ie/organization/environmental-protection-agency", "roles": ["publisher"]}]}, "links": [{"href": "http://gis.epa.ie/GetData/Download"}, {"href": "http://gis.epa.ie/data/WFD_NewWaterbodies/AboutNewGroundWaterbodies_Jan2016.pdf"}, {"href": "https://gis.epa.ie/geoserver/EPA/wms?service=WMS&version=1.1.0&request=GetMap&layers=EPA:WFD_GROUNDWATERBODIESActive&styles=&bbox=20178.278199999593%2C16270.345599999651%2C334518.00069999974%2C459757.56159999967&width=544&height=768&srs=EPSG:29902&format=image%2Fpng"}, {"href": "http://data.europa.eu/88u/dataset/42aefcf3-b6d6-4620-8abd-8b005c070067~~1"}, {"rel": "self", "type": "application/geo+json", "title": "42aefcf3-b6d6-4620-8abd-8b005c070067", "name": "item", "description": "42aefcf3-b6d6-4620-8abd-8b005c070067", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/42aefcf3-b6d6-4620-8abd-8b005c070067"}, {"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": "4d80d2d3-d326-4e1f-ac24-c8eaf91587d8", "type": "Feature", "geometry": null, "properties": {"updated": "2025-09-25T09:14:15", "type": "Dataset", "language": "en", "title": "Water Framework Directive Groundwater Waterbodies", "description": "The EU Water Framework Directive (2000/60/EC) (WFD) establishes a framework for the protection, improvement and management of surface water and groundwater. 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Das BULE-Projekt Wassermeisterei ist gef\u00f6rdert vom BMLEH und wird in Kooperation mit dem Smart City Projekt Zukunftsschusterei Bad Belzig umgesetzt.", "formats": [{"name": "CSV"}], "keywords": ["boden", "bodenfeuchte", "citizen-science", "de", "du\u0308rre", "klima", "trockenheit", "wasser"], "contacts": [{"organization": "Daniel Diehl", "roles": ["creator"]}, {"organization": "https://open-data.ble.de/organization/71d64611-a125-4229-8e80-a6d37d219b52", "roles": ["publisher"]}]}, "links": [{"href": "https://open-data.ble.de/dataset/6a941f24-15bb-4ee0-84ea-e21c3ab36bfd/resource/0712da2b-4fbc-49a7-a172-0e888caed907/download/metadata.csv"}, {"href": "https://open-data.ble.de/dataset/6a941f24-15bb-4ee0-84ea-e21c3ab36bfd/resource/1c930012-34a9-45e1-afe1-0303431144a0/download/___"}, {"href": "https://open-data.ble.de/dataset/6a941f24-15bb-4ee0-84ea-e21c3ab36bfd/resource/320f4fe4-0fab-40fc-aa41-961f4d2d89e2/download/___"}, {"href": 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The topsoil (c.5\u201320 cm deep) samples were analysed for: Analytical Method: ICP(-OES/-MS) following aqua regia digestion; soil loss-on-ignition at 450\u00a0\u00b0C The survey was conducted on foot; samples were collected approx. every 4 sq km from. For more information please visit tellus.ie.  The following elements were analysed: Aluminium, Antimony, Arsenic, Barium, Beryllium, Bismuth, Cadmium, caesium, Calcium, Cerium, Chromium, Cobalt, Copper, Gallium, Germanium, Hafnium, indium, Iron, Lanthanum, Lead, Lithium, Loss-on-ignition, Lutetium, Magnesium, Manganese, Mercury, Molybdenum, Nickel, Niobium, pH, Phosphorus, Potassium, Rubidium, scandium, Selenium, Silver, Sodium, Strontium, Sulphur, Tantalum, Tellurium, Terbium, Thallium, Thorium, Tin, Titanium, Tungsten, Uranium, vanadium, Ytterbium, Yttrium, Zinc, Zinc, Zirconium (Al, B, Ba, Ca, Cr, Cu, Fe, K, Li, Mg, Mn, Na, Ni, P, S, S, Sr, Ti, V, Zn, Zr, Ag, Be, Be, Bi, Cd, Ce, Co, Cs, Ga, Ge, Hf, In, La, Lu, P, Mo, Mo, Pb, Rb, Sb, Sb, Sb, Sn, Sn, Tb, Te, Th, Tl, U, W, Yb) The current coverage includes:  Tellus Border survey block (2011-2013, Co Donegal, Sligo, Leitrim, Cavan, Monaghan, Louth)  Some elements have been merged with topsoil data from Northern Ireland conducted in the mid ninties and Noughties.", "formats": [{"name": "ESRI REST"}], "keywords": ["aintrim", "aluminium", "antimony", "aqua-regia", "aqua-regia-digestion", "armagh", "arsenic", "barium", "beryllium", "bismuth", "cadmium", "caesium", "calcium", "cavan", "cerium", "chemistry", "chromium", "cobalt", "copper", "derry", "donegal", "down", "dublin", "earth-science", "environment", "european-union", "fermanagh", "gallium", "galway", "geochemical", "geochemical-survey", "geochemistry", "geological", "geological-survey-ireland", "geology", "geoscientificinformation", "germanium", "hafnium", "icp-ms", "icp-oes", "icpms", "icpoes", "ie", "indium", "interreg", "ireland", "iron", "kildare", "lanthanum", "lead", "lietrim", "lithium", "lithology", "lithosphere", "londonderry", "longford", "loss-on-ignition", "louth", "lutetium", "magnesium", "manganese", "mayo", "meath", "mercury", "molybdenum", "monaghan", "nickel", "niobium", "offaly", "organics", "phosphorus", "potassium", "rocks", "roscommon", "rubidium", "scandium", "selenium", "silver", "sligo", "sodium", "soil", "soil-loss-on-ignition", "soil-ph", "strontium", "sulphur", "tantalum", "tellurium", "tellus", "tellus-border", "terbium", "thallium", "thorium", "tin", "titanium", "top-soil", "topsoil", "tungsten", "tyrone", "uranium", "vanadium", "westmeath", "wicklow", "ytterbium", "yttrium", "zinc", "zirconium"], "contacts": [{"organization": "https://data.gov.ie/organization/geological-survey-of-ireland", "roles": ["publisher"]}]}, "links": [{"href": "http://dcenr.maps.arcgis.com/apps/MapSeries/index.html?appid=6304e122b733498b99642707ff72f754"}, {"href": "https://gsi.geodata.gov.ie/server/rest/services/Geochemistry"}, {"href": "https://secure.dccae.gov.ie/GSI_DOWNLOAD/Tellus/PDFs/EBook_Topsoils_Final_03Feb2016.pdf"}, {"href": "https://www.gsi.ie/en-ie/data-and-maps/Pages/Geochemistry.aspx#DeeperTopsoilS"}, {"href": "https://www.gsi.ie/en-ie/data-and-maps/Pages/Geochemistry.aspx#ShallowTopsoilA"}, {"href": "https://www.gsi.ie/en-ie/programmes-and-projects/tellus/activities/ground-survey/Pages/default.aspx"}, {"href": "http://data.europa.eu/88u/dataset/7520bfe1-d548-4ffb-bdd8-18cc534df855"}, {"rel": "self", "type": "application/geo+json", "title": "7520bfe1-d548-4ffb-bdd8-18cc534df855", "name": "item", "description": "7520bfe1-d548-4ffb-bdd8-18cc534df855", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/7520bfe1-d548-4ffb-bdd8-18cc534df855"}, {"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": "79d81fe8-0914-4d22-861b-0af531989ef8", "type": "Feature", "geometry": {"type": "Polygon", "coordinates": [[[8.66, 50.56], [8.66, 50.61], [8.72, 50.61], [8.72, 50.56], [8.66, 50.56]]]}, "properties": {"themes": [{"concepts": [{"id": "environment"}], "scheme": "https://standards.iso.org/iso/19139/resources/gmxCodelists.xml#MD_TopicCategoryCode"}, {"concepts": [{"id": "Coarse grains"}, {"id": "Subsoil"}, {"id": "gravel"}, {"id": "Soil"}, {"id": "Nitrogen"}, {"id": "nitrogen fertilizers"}, {"id": "Nitrogen fixation"}], "scheme": "AGROVOC Multilingual agricultural thesaurus"}, {"concepts": [{"id": "gravel"}, {"id": "Land use"}, {"id": "Soil"}, {"id": "Bodenchemie"}, {"id": "Stickstoff"}, {"id": "Stickstoffd\u00fcnger"}, {"id": "Stickstoffixierung"}], "scheme": "GEMET - Concepts, version 2.4"}, {"concepts": [{"id": "Rock content"}], "scheme": "Individual"}, {"concepts": [{"id": "Boden"}], "scheme": "GEMET - INSPIRE themes, version 1.0"}, {"concepts": [{"id": "opendata"}], "scheme": "Individual"}], "rights": "Restrictions applied to assure the protection of privacy or intellectual property, and any special restrictions or limitations or warnings on using the resource or metadata. (e.g. Reports, articles, papers, scientific and non-scientific works of any form, including tables, maps, or any other kind of output, in printed or electronic form, based in whole or in part on the data supplied, must contain an acknowledgement of the form: \u201cData re-used from the BonaRes Data Centre www.bonares.de. This data were created as part of BonaRes Module A-Project - SOIL3's research activities.\u201d Although every care has been taken in preparing and testing the data, BonaRes Module A-Project- SOIL3 and BonaRes Data Centre cannot guarantee that the data are correct; neither does BonaRes Module A-Project and BonaRes Data Centre accept any liability whatsoever for any error, missing data or omission in the data, or for any loss or dam-age arising from its use. The BonaRes Module A-Project-SOIL3 and BonaRes Data Centre will not be responsible for any direct or indirect use which might be made of the data. The access to this data is restricted during embargo time. If prior access is requested, contact the data owner/author.)", "updated": "2019-07-26", "type": "Dataset", "created": "2017-10-19", "language": "eng", "title": "Giessen long-term field experiment 'biological nitrogen fixation' - soil coarse fraction", "description": "This data set reports the soil coarse fraction  2 mm as mass proportion of oven dry soil from the Giessen long-term field experiment investigating biological nitrogen fixation.", "formats": [{"name": "CSV"}], "keywords": ["Coarse grains", "Subsoil", "gravel", "Soil", "Nitrogen", "nitrogen fertilizers", "Nitrogen fixation", "gravel", "Land use", "Soil", "Bodenchemie", "Stickstoff", "Stickstoffd\u00fcnger", "Stickstoffixierung", "Rock content", "Boden", "opendata"], "contacts": [{"name": "Eleanor Hobley", "organization": "Technical University Munich", "position": "Scientist", "roles": ["author"], "phones": [{"value": null}], "emails": [{"value": "nellie.hobley@wzw.tum.de"}], "addresses": [{"deliveryPoint": ["Emil-Ramann-Str. 2"], "city": "Freising", "administrativeArea": null, "postalCode": "85354", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Wulf Amelung", "organization": "University of Bonn", "position": "Professor", "roles": ["projectLeader"], "phones": [{"value": null}], "emails": [{"value": "wulf.amelung@uni-bonn.de"}], "addresses": [{"deliveryPoint": [null], "city": null, "administrativeArea": null, "postalCode": null, "country": null}], "links": [{"href": null}]}, {"name": "BonaRes Data Centre", "organization": "Leibniz Centre for Agricultural Landscape Research (ZALF)", "position": "Research Platform 'Data' - WG Geodata", "roles": ["publisher"], "phones": [{"value": "+49 33432 82 171"}], "emails": [{"value": "bonares-datenzentrum@zalf.de"}], "addresses": [{"deliveryPoint": ["Eberswalder Strasse 84"], "city": "M\u00fcncheberg", "administrativeArea": "Brandenburg", "postalCode": "15374", "country": "Germany"}], "links": [{"href": null}]}, {"organization": "Technical University Munich", "roles": ["contributor"]}]}, "links": [{"href": "https://maps.bonares.de/mapapps/resources/apps/bonares/index.html?lang=en&mid=79d81fe8-0914-4d22-861b-0af531989ef8", "rel": "download"}, {"rel": "self", "type": "application/geo+json", "title": "79d81fe8-0914-4d22-861b-0af531989ef8", "name": "item", "description": "79d81fe8-0914-4d22-861b-0af531989ef8", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/79d81fe8-0914-4d22-861b-0af531989ef8"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-07-26T00:00:00Z"}}, {"id": "8a860a7d-e3a9-4e30-bf14-d96fd47a1484", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:30:23Z", "type": "Dataset", "title": "WFS Excavations KLE VIE WES", "description": "The service depicts excavations in the district of Kleve, the district of Viersen and the district of Wesel. The service accesses live data. Extraction of mineral resources (sands, gravel and clays) requires authorisation. For excavations, a distinction is made between wet and dry excavations. In wet excavations, groundwater is exposed by the silting and thus a body of water is produced, in dry excavations not.", "formats": [{"name": "WMS_SRVC"}], "keywords": ["05166000", "abbau", "abgrabung", "abgrabungen", "boden", "bodenschatz", "bodenscha\u0308tze", "de", "econ", "envi", "kies", "kommunales-rechenzentrum-niederrhein", "kreis-kleve", "kreis-viersen", "kreis-wesel", "krzn", "lehm", "nassabgrabung", "nrw", "nw", "opendata", "sand", "ton", "trockenabgrabung", "viewservice", "wfs"], "contacts": [{"organization": "Kreis Kleve - Abt. Bauen und Umwelt - Abgrabungen", "roles": ["creator"]}]}, "links": [{"href": "https://geoservices.krzn.de/security-proxy/services/wfs_verb_abgrabung?Service=WFS&Version=1.1.0&Request=GetCapabilities"}, {"href": "http://data.europa.eu/88u/dataset/8a860a7d-e3a9-4e30-bf14-d96fd47a1484"}, {"rel": "self", "type": "application/geo+json", "title": "8a860a7d-e3a9-4e30-bf14-d96fd47a1484", "name": "item", "description": "8a860a7d-e3a9-4e30-bf14-d96fd47a1484", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/8a860a7d-e3a9-4e30-bf14-d96fd47a1484"}, {"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": "0a69e00d-4a6c-467e-90b3-9d76a538ef18", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:30:33Z", "type": "Dataset", "title": "Soil Map of the Federal Republic of Germany 1:1,000,000 (WMS)", "description": "Web Map Service (WMS) of the BUEK1000. The first country wide soil map at a scale of 1:1,000,000 (BUEK1000) has been compiled on the basis of published soil maps of the former German Democratic Republic and the pre 1990 federal states of Germany. To do this, it was necessary to match the soil systems used in East and West Germany and to develop standardized descriptions of soil units. A relatively homogeneous map has resulted, which permits uniform assessment of the soils throughout Germany. The map shows 71 soil mapping units, described in the legend on the basis of the German and FAO soil systems. Each soil unit has been assigned a characteristic soil profile (Leitprofil) as an aid to map interpretation. For the first time the subdivision of the country into 12 soil regions has been represented on the map. This subdivision was coordinated with the state Geological Surveys. These soil regions will represent the highest hierarchic level of nation wide soil maps in future. The colours of soil units correspond to the standards of the 'Bodenkundliche Kartieranleitung' (KA 3; Guidelines for Soil Mapping). The various hues characterize differences in relief or soil humidity. The BUEK1000 was produced digitally. It is an important part of the spatial database integrated in the Soil Information System currently being established at the Federal Institute for Geosciences and Natural Resources (FISBo BGR). It can be used together with the characteristic soil profiles to derive thematic maps related to nation wide soil protection. The scale of the BUEK1000 makes it especially suitable for small scale evaluations at federal or EU level.", "formats": [{"name": "WMS_SRVC"}], "keywords": ["de", "environmental-protection", "federal-republic-of-germany", "geographical-information-system", "infomapaccessservice", "parent-material", "parent-rock", "soil", "soil-association", "soil-complex", "soil-information-system", "soil-map", "soil-polygon", "soil-profile", "soil-property", "soil-protection", "soil-science", "soil-substrate", "soil-systematics", "soil-textural-class", "soil-type"], "contacts": [{"organization": "Stegger, Ulrich", "roles": ["creator"]}]}, "links": [{"href": "https://services.bgr.de/wms/boden/buek1000en/?"}, {"href": "http://data.europa.eu/88u/dataset/0a69e00d-4a6c-467e-90b3-9d76a538ef18"}, {"rel": "self", "type": "application/geo+json", "title": "0a69e00d-4a6c-467e-90b3-9d76a538ef18", "name": "item", "description": "0a69e00d-4a6c-467e-90b3-9d76a538ef18", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/0a69e00d-4a6c-467e-90b3-9d76a538ef18"}, {"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": "AWS_Soil_INSPIRE_WMS", "type": "Feature", "geometry": {"type": "Polygon", "coordinates": [[[-10.66, 51.42], [-10.66, 55.38], [-5.99, 55.38], [-5.99, 51.42], [-10.66, 51.42]]]}, "properties": {"updated": "2025-11-26", "type": "Service", "created": "2022-12-12", "language": "eng", "title": "TEAGASC Soil Ireland INSPIRE View Service", "description": "TEAGASC Soil Ireland Web Map Service according to INSPIRE Directive.", "formats": [{"name": "OGC Web Map Service"}], "keywords": ["Soil", "National", "soil layer", "sand", "rock", "water body", "Ireland", "Map access service", "infoManagementService", "infoMapAccessService", "1.3.0", "WMS", "OGC"], "contacts": [{"name": null, "organization": "Teagasc. 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Agriculture and Food Development Authority", "position": null, "roles": ["pointOfContact"], "phones": [{"value": "+353 59 917 0200"}], "emails": [{"value": "soils@teagasc.ie"}], "addresses": [{"deliveryPoint": ["Oak Park, Carlow, R93 XE12"], "city": "Carlow", "administrativeArea": "Carlow", "postalCode": "R93 XE12", "country": "Ireland"}], "links": [{"href": {"url": "http://soils.teagasc.ie/", "protocol": null, "protocol_url": "", "name": null, "name_url": "", "description": null, "description_url": "", "applicationprofile": null, "applicationprofile_url": "", "function": null}}]}], "themes": [{"concepts": [{"id": "Soil"}], "scheme": "http://www.eionet.europa.eu/gemet/inspire_themes"}, {"concepts": [{"id": "National"}], "scheme": "http://inspire.ec.europa.eu/metadata-codelist/SpatialScope"}, {"concepts": [{"id": "soil layer"}, {"id": "sand"}, {"id": "rock"}, {"id": "water body"}], "scheme": "General Multilingual Environmental Thesaurus - Concepts, version 4.1.3"}, {"concepts": [{"id": "Feature Access Service"}], "scheme": "http://data.europa.eu/eli/reg/2008/1205"}, {"concepts": [{"id": "infoManagementService"}, {"id": "infoMapAccessService"}], "scheme": "ISO - 19119 geographic services taxonomy"}], "title_alternate": "ATOM feed"}, "links": [{"href": "https://teagasc-inspire-atom.s3.eu-west-1.amazonaws.com/files/atomTEAGASC_INSPIRE_Ireland.xml", "name": "TEAGASC Soil Ireland INSPIRE Download Service ATOM", "protocol": "ATOM Syndication Format", "rel": null}, {"href": "https://teagasc-inspire-atom.s3.eu-west-1.amazonaws.com/files/atomTEAGASC_INSPIRE_Ireland.xml", "protocol": "ATOM Syndication Format"}, {"rel": "self", "type": "application/geo+json", "title": "AWS_Soil_INSPIRE_ATOM", "name": "item", "description": "AWS_Soil_INSPIRE_ATOM", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/AWS_Soil_INSPIRE_ATOM"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-11-26T00:00:00Z"}}, {"id": "PMC5806009", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:31:03Z", "type": "Journal Article", "created": "2018-01-31", "title": "Determination of macro-scale soil properties from pore-scale structures: model derivation", "description": "<p>In this paper, we use homogenization to derive a set of macro-scale poro-elastic equations for soils composed of rigid solid particles, air-filled pore space and a poro-elastic mixed phase. We consider the derivation in the limit of large deformation and show that by solving representative problems on the micro-scale we can parametrize the macro-scale equations. To validate the homogenization procedure, we compare the predictions of the homogenized equations with those of the full equations for a range of different geometries and material properties. We show that the results differ by\uffe2\uff89\uffb22%for all cases considered. The success of the homogenization scheme means that it can be used to determine the macro-scale poro-elastic properties of soils from the underlying structure. Hence, it will prove a valuable tool in both characterization and optimization.</p", "keywords": ["Soil and rock mechanics", "homogenization", "soil mechanics", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "soil modelling", "01 natural sciences", "6. Clean water", "510", "620", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://eprints.soton.ac.uk/416610/1/Poro_elastic01_Accepted.pdf"}, {"href": "https://eprints.soton.ac.uk/416610/2/Poro_elastic01_Supplementary_Accepted.pdf"}, {"href": "https://royalsocietypublishing.org/doi/pdf/10.1098/rspa.2017.0141"}, {"href": "https://doi.org/PMC5806009"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Proceedings%20of%20the%20Royal%20Society%20A%3A%20Mathematical%2C%20Physical%20and%20Engineering%20Sciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "PMC5806009", "name": "item", "description": "PMC5806009", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/PMC5806009"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-01-01T00:00:00Z"}}, {"id": "PMC6083241", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-03T16:31:04Z", "type": "Journal Article", "created": "2018-07-11", "title": "Determination of macro-scale soil properties from pore scale structures: image-based modelling of poroelastic structures", "description": "<p>             We show how a combination of X-ray computed tomography (X-CT) and image-based modelling can be used to calculate the effect of moisture content and compaction on the macroscopic structural properties of soil. Our method is based on the equations derived in Daly &amp; Roose (2018             Proc. R. Soc. A             474             , 20170141. (             doi:10.1098/rspa.2017.0141             )), which we have extended so they can be directly applied to the segmented images obtained from X-CT. We assume that the soils are composed of air-filled pore space, solid mineral grains and a mixed phase composed of both clay particles and water. We considered three different initial soil treatments, composed of two different compaction levels and two different moisture contents. We found that the effective properties of the soils were unaffected by compaction over the range tested in this paper. However, changing the moisture content significantly altered the hydraulic and mechanical properties of the soils. A key strength of this method is that it enables the optimization or even design of soils composed from different constituents, with specific mechanical and hydraulic properties.           </p", "keywords": ["0301 basic medicine", "550", "homogenization", "multiscale analysis", "04 agricultural and veterinary sciences", "15. Life on land", "soil science", "Fluid-solid interactions (including aero- and hydro-elasticity", " porosity", " etc.)", "6. Clean water", "poroelasticity", "03 medical and health sciences", "image-based modelling", "Soil and rock mechanics", "0401 agriculture", " forestry", " and fisheries", "Research Articles"]}, "links": [{"href": "https://eprints.soton.ac.uk/421320/1/180524_Poro_elastic02_Accepted_Main.pdf"}, {"href": "https://eprints.soton.ac.uk/421320/2/180524_Poro_elastic02_Accepted_Supplementary02.pdf"}, {"href": "https://eprints.soton.ac.uk/421320/3/180524_Poro_elastic02_Accepted_Supplementary01.pdf"}, {"href": "https://royalsocietypublishing.org/doi/pdf/10.1098/rspa.2017.0745"}, {"href": "https://doi.org/PMC6083241"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Proceedings%20of%20the%20Royal%20Society%20A%3A%20Mathematical%2C%20Physical%20and%20Engineering%20Sciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "PMC6083241", "name": "item", "description": "PMC6083241", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/PMC6083241"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-07-01T00:00:00Z"}}], "links": [{"rel": "self", "type": "application/geo+json", "title": "This document as GeoJSON", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=rock&f=json", "hreflang": "en-US"}, {"rel": "alternate", "type": "text/html", "title": "This document as HTML", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=rock&f=html", "hreflang": "en-US"}, {"rel": "collection", "type": "application/json", "title": "Collection URL", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main", "hreflang": "en-US"}, {"type": "application/geo+json", "rel": "first", "title": "items (first)", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=rock&", "hreflang": "en-US"}, {"rel": "next", "type": "application/geo+json", "title": "items (next)", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=rock&offset=50", "hreflang": "en-US"}], "numberMatched": 60, "numberReturned": 50, "distributedFeatures": [], "timeStamp": "2026-04-04T01:49:29.865145Z"}