{"type": "FeatureCollection", "features": [{"id": "10.1007/s004420100656", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-23T16:15:07Z", "type": "Journal Article", "created": "2003-02-13", "title": "Fine-Root Biomass And Fluxes Of Soil Carbon In Young Stands Of Paper Birch And Trembling Aspen As Affected By Elevated Atmospheric Co2 And Tropospheric O3", "description": "Rising atmospheric CO2 may stimulate future forest productivity, possibly increasing carbon storage in terrestrial ecosystems, but how tropospheric ozone will modify this response is unknown. Because of the importance of fine roots to the belowground C cycle, we monitored fine-root biomass and associated C fluxes in regenerating stands of trembling aspen, and mixed stands of trembling aspen and paper birch at FACTS-II, the Aspen FACE project in Rhinelander, Wisconsin. Free-air CO2 enrichment (FACE) was used to elevate concentrations of CO2 (average enrichment concentration 535\u00a0\u00b5l l-1) and O3 (53\u00a0nl l-1) in developing forest stands in 1998 and 1999. Soil respiration, soil pCO2, and dissolved organic carbon in soil solution (DOC) were monitored biweekly. Soil respiration was measured with a portable infrared gas analyzer. Soil pCO2 and DOC samples were collected from soil gas wells and tension lysimeters, respectively, at depths of 15, 30, and 125\u00a0cm. Fine-root biomass averaged 263\u00a0g m-2 in control plots and increased 96% under elevated CO2. The increased root biomass was accompanied by a 39% increase in soil respiration and a 27% increase in soil pCO2. Both soil respiration and pCO2 exhibited a strong seasonal signal, which was positively correlated with soil temperature. DOC concentrations in soil solution averaged ~12\u00a0mg l-1 in surface horizons, declined with depth, and were little affected by the treatments. A simplified belowground C budget for the site indicated that native soil organic matter still dominated the system, and that soil respiration was by far the largest flux. Ozone decreased the above responses to elevated CO2, but effects were rarely statistically significant. We conclude that regenerating stands of northern hardwoods have the potential for substantially greater C input to soil due to greater fine-root production under elevated CO2. Greater fine-root biomass will be accompanied by greater soil C efflux as soil respiration, but leaching losses of C will probably be unaffected.", "keywords": ["0106 biological sciences", "Ecology and Evolutionary Biology", "Aspen-FACE-project", "root-", "USA-", "pollutants-", "Environmental-Sciences)", "tropospheric-ozone", "forest-productivity", "01 natural sciences", "biomass-", "northern-forests", "124-38-9: CARBON DIOXIDE", "soil-carbon-flux", "terrestrial-ecosystems", "populus-tremuloides", "Cellular and Developmental Biology", "soil-carbon", "7440-44-0: CARBON", "carbon-", "fine-root", "Bioenergetics- (Biochemistry-and-Molecular-Biophysics)", "Natural Resources and Environment", "04 agricultural and veterinary sciences", "GLOBAL-ECOLOGY", "North-America", "Nearctic-region)", "Rhinelander- (Wisconsin-", "carbon-sequestration", "atmosphere-", "biomass-production", "dissolved-organic-carbon [DOC-]", "Science", "respiration-", "carbon-dioxide-enrichment", "forest-plantations", "carbon-dioxide", "carbon-storage", "fine-root-biomass", "belowground-biomass", "United-States-Wisconsin-Rhinelander", "carbon-cycle", "Health Sciences", "ozone-", "soil-respiration", "air-pollution", "global-change", "atmospheric-carbon-dioxide", "biomass", "Molecular", "15. Life on land", "ozone", "13. Climate action", "roots-", "Legacy", "Terrestrial-Ecology (Ecology-", "free-air-carbon-dioxide-enrichment [FREE-]: experimental-method", "0401 agriculture", " forestry", " and fisheries", "Northern Forests Global Change Carbon Sequestration Soil Respiration Dissolved Organic Carbon Soil PCO2"]}, "links": [{"href": "https://doi.org/10.1007/s004420100656"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Oecologia", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s004420100656", "name": "item", "description": "10.1007/s004420100656", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s004420100656"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2001-07-01T00:00:00Z"}}, {"id": "10.1046/j.1469-8137.2003.00911.x", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-23T16:18:37Z", "type": "Journal Article", "created": "2003-11-17", "title": "Fine-Root Respiration In A Loblolly Pine And Sweetgum Forest Growing In Elevated Co2", "description": "\u2022\u2002 The loss of carbon below-ground through respiration of fine roots may be modified by global change. Here we tested the hypothesis that a reduction in N concentration of tree fine-roots grown in an elevated atmospheric CO2 concentration would reduce maintenance respiration and that more energy would be used for root growth and N uptake. We partitioned total fine-root respiration (RT ) between maintenance (RM ), growth (RG ), and N uptake respiration (RN ) for loblolly pine (Pinus taeda) and sweetgum (Liquidambar styraciflua) forests exposed to elevated CO2 . \u2022\u2002 A substantial increase in fine-root production contributed to a 151% increase in RG for loblolly pine in elevated CO2 . Root specific RM for pine was 24% lower under elevated CO2 but when extrapolated to the entire forest, no treatment effect could be detected. \u2022\u2002 R G (<\u00a010%) and RN (<\u00a03%) were small components of RM in both forests. Maintenance respiration was the vast majority of RT , and contributed 92% and 86% of these totals at the pine and sweetgum forests, respectively. \u2022\u2002 The hypothesis was rejected because the majority of fine-root respiration was used for maintenance and was not reduced by changes in root N concentration in elevated CO2 . Because of its large contribution to RT and total soil CO2 efflux, changes in RM caused by warming may greatly alter carbon losses from forests to the atmosphere.", "keywords": ["0106 biological sciences", "Temperate forest", "Sweetgum (Liquidambar styeaciflua)", "Growth respiration", "Loblolly pine (Pinus taeda)", "Maintenance respiration", "Nitrogen uptake respiration", "15. Life on land", "Free-air CO enrichment (FACE) 2", "01 natural sciences", "Annual fine-root respiration"]}, "links": [{"href": "https://doi.org/10.1046/j.1469-8137.2003.00911.x"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/New%20Phytologist", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1046/j.1469-8137.2003.00911.x", "name": "item", "description": "10.1046/j.1469-8137.2003.00911.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1046/j.1469-8137.2003.00911.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2003-11-17T00:00:00Z"}}, {"id": "10.1073/pnas.0706518104", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-23T16:18:45Z", "type": "Journal Article", "created": "2007-08-21", "title": "Increases In Nitrogen Uptake Rather Than Nitrogen-Use Efficiency Support Higher Rates Of Temperate Forest Productivity Under Elevated Co2", "description": "<p>             Forest ecosystems are important sinks for rising concentrations of atmospheric CO             2             . In previous research, we showed that net primary production (NPP) increased by 23 \uffc2\uffb1 2% when four experimental forests were grown under atmospheric concentrations of CO             2             predicted for the latter half of this century. Because nitrogen (N) availability commonly limits forest productivity, some combination of increased N uptake from the soil and more efficient use of the N already assimilated by trees is necessary to sustain the high rates of forest NPP under free-air CO             2             enrichment (FACE). In this study, experimental evidence demonstrates that the uptake of N increased under elevated CO             2             at the Rhinelander, Duke, and Oak Ridge National Laboratory FACE sites, yet fertilization studies at the Duke and Oak Ridge National Laboratory FACE sites showed that tree growth and forest NPP were strongly limited by N availability. By contrast, nitrogen-use efficiency increased under elevated CO             2             at the POP-EUROFACE site, where fertilization studies showed that N was not limiting to tree growth. Some combination of increasing fine root production, increased rates of soil organic matter decomposition, and increased allocation of carbon (C) to mycorrhizal fungi is likely to account for greater N uptake under elevated CO             2             . Regardless of the specific mechanism, this analysis shows that the larger quantities of C entering the below-ground system under elevated CO             2             result in greater N uptake, even in N-limited ecosystems. Biogeochemical models must be reformulated to allow C transfers below ground that result in additional N uptake under elevated CO             2             .           </p>", "keywords": ["rotation poplar plantation", "0106 biological sciences", "Nitrogen", "Climate", "atmospheric carbon-dioxide", "enrichment face", "organic nitrogen", "Biological Transport", "deciduous forest", "04 agricultural and veterinary sciences", "Carbon Dioxide", "15. Life on land", "01 natural sciences", "Trees", "Kinetics", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "populus-tremuloides", "community composition", "soil-n availability", "fine-root production", "Ecosystem", "ecosystem responses"]}, "links": [{"href": "https://doi.org/10.1073/pnas.0706518104"}, {"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.0706518104", "name": "item", "description": "10.1073/pnas.0706518104", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1073/pnas.0706518104"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2007-08-28T00:00:00Z"}}, {"id": "10.1371/journal.pone.0070224", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-23T16:20:14Z", "type": "Journal Article", "created": "2013-07-16", "title": "Effects Of Added Organic Matter And Water On Soil Carbon Sequestration In An Arid Region", "description": "Open AccessEn general, se predice que el calentamiento global estimular\u00e1 la producci\u00f3n primaria y conducir\u00e1 a m\u00e1s aportes de carbono (C) al suelo. Sin embargo, muchos estudios han encontrado que el suelo C no necesariamente aumenta con el aumento de la entrada de basura vegetal. Las precipitaciones han aumentado en Asia central \u00e1rida y se prev\u00e9 que aumenten m\u00e1s, por lo que probamos los efectos de la adici\u00f3n de materia org\u00e1nica fresca (FOM) y agua en el secuestro de C del suelo en una regi\u00f3n \u00e1rida en el noroeste de China. Los resultados sugirieron que el FOM a\u00f1adido se descompuso r\u00e1pidamente y tuvo efectos menores en el dep\u00f3sito de carbono org\u00e1nico del suelo (SOC) a una profundidad de 30 cm. Tanto la FOM como la adici\u00f3n de agua tuvieron efectos significativos en la biomasa microbiana del suelo. La biomasa microbiana del suelo aument\u00f3 con la adici\u00f3n de FOM, alcanz\u00f3 un m\u00e1ximo y luego disminuy\u00f3 a medida que la FOM se descompon\u00eda. El FOM tuvo un efecto estimulante m\u00e1s significativo sobre la biomasa microbiana con la adici\u00f3n de agua. Bajo los rangos de humedad del suelo utilizados en este experimento (21.0% -29.7%), el aporte de FOM fue m\u00e1s importante que la adici\u00f3n de agua en el proceso de mineralizaci\u00f3n del suelo C. Concluimos que la entrada de FOM a corto plazo en el suelo subterr\u00e1neo y la adici\u00f3n de agua no afectan la piscina de SOC en los matorrales en una regi\u00f3n \u00e1rida.", "keywords": ["Carbon sequestration", "550", "Arid", "Growth", "630", "Agricultural and Biological Sciences", "Soil", "Agricultural soil science", "Tropical forest", "Soil water", "Carbon fibers", "Biomass", "Land-use", "2. Zero hunger", "Analysis of Land Cover and Ecosystems", "Ecology", "Respiration", "Q", "Temperature", "R", "Soil Chemical Properties", "Life Sciences", "Composite number", "04 agricultural and veterinary sciences", "Soil carbon", "6. Clean water", "Chemistry", "Physical Sciences", "Environmental chemistry", "Medicine", "Organic matter", "Research Article", "Composite material", "Carbon Sequestration", "China", "Desert shrubs", "Science", "Soil Science", "Ecosystems", "Environmental science", "Meta-analysis in Ecology and Agriculture Research", "Organic Matter Dynamics", "Climate-change", "Soil Carbon Sequestration", "Biology", "Ecology", " Evolution", " Behavior and Systematics", "Soil science", "Soil organic matter", "Soil Fertility", "Water", "Soil Properties", "15. Life on land", "Soil biodiversity", "Materials science", "Microbial activity", "Carbon dioxide", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "Fine-root", "0401 agriculture", " forestry", " and fisheries", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems", "CO2 flux"]}, "links": [{"href": "https://doi.org/10.1371/journal.pone.0070224"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/PLoS%20ONE", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1371/journal.pone.0070224", "name": "item", "description": "10.1371/journal.pone.0070224", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1371/journal.pone.0070224"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2013-07-16T00:00:00Z"}}, {"id": "10.2136/sssaj2006.0069", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-23T16:21:06Z", "type": "Journal Article", "created": "2007-06-30", "description": "<p>We resampled one of the earliest replicated experimental sites used to investigate the impacts of native tropical tree species on soil properties, to examine longer term effects to 1\uffe2\uff80\uff90m depth. The mono\uffe2\uff80\uff90dominant stands, established in abandoned pasture in 1988 at La Selva Biological Station, Costa Rica, contained six species, including one exotic, Pinus patula ssp. tecunumanii (Eguiluz &amp; J.P. Perry) Styles, and five native species: Pentaclethra macroloba (Willd.) Ktze (N2\uffe2\uff80\uff90fixing); Hyeronima alchorneoides Allemao; Virola koschnyi Warb.; Vochysia ferruginea Mart.; and Vochysia guatemalensis J.D. Smith. Soil organic carbon (SOC) differed significantly among species in the surface (0\uffe2\uff80\uff9315\uffe2\uff80\uff90cm) layer, ranging from 44.5 to 55.1 g kg\uffe2\uff88\uff921, compared with 46.6 and 50.3 g kg\uffe2\uff88\uff921 in abandoned pasture and mature forest, respectively. The change in surface SOC over 15 yr ranged from \uffe2\uff88\uff920.03 to 0.66 Mg C ha\uffe2\uff88\uff921 yr\uffe2\uff88\uff921 The species differed in the quantity and chemical composition of their detrital production. Soil organic C was significantly correlated with fine\uffe2\uff80\uff90root growth, but not with aboveground detrital inputs. Soil organic C increased with potential C mineralization on a grams of C basis, indicating that species influenced both the quality and quantity of SOC. Contrary to expectations, SOC declined with increasing fine\uffe2\uff80\uff90root lignin concentrations, indicating that lignin\uffe2\uff80\uff90derived C did not dominate refractory SOC pools. We hypothesize that differences among species in the capacity to increase SOC stocks involved fine\uffe2\uff80\uff90root traits that promoted soil microbial turnover and, thus, greater production of recalcitrant, microbial\uffe2\uff80\uff90derived C fractions.</p>", "keywords": ["soil organic carbon", "580", "Ecology and Evolutionary Biology", "Organic Chemistry", "Natural Resources Management and Policy", "lignin", "0401 agriculture", " forestry", " and fisheries", "Forest Biology", "tropical tree", "04 agricultural and veterinary sciences", "15. Life on land", "630", "fine-root growth"]}, "links": [{"href": "https://doi.org/10.2136/sssaj2006.0069"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20Science%20Society%20of%20America%20Journal", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.2136/sssaj2006.0069", "name": "item", "description": "10.2136/sssaj2006.0069", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.2136/sssaj2006.0069"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2007-07-01T00:00:00Z"}}, {"id": "10.5061/dryad.b8gtht7kg", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-23T16:22:15Z", "type": "Dataset", "created": "2023-11-27", "title": "Data from: The effect of drainage on the fine root biomass, production, and turnover in hemiboreal old-growth forests on organic soils", "description": "Open Access# The effect of drainage on the fine root biomass, production, and  turnover in hemiboreal old-growth forests on organic soils  ## #GWL _temp.csv This  file contains data on study site soil temperature and groundwater level ##  Description of the data and file structure Date - Sampling date Site -  Study object name FT - Forest type (ND - not drained, KS - drained) Year -  Sampling year Cycle - Sampling campaign number in specific sampling year  PL - Sample plot of study object (1-3) Groundwater - Groundwater level  depth from the ground surface, cm Soil_temp_10cm - Soil temperature at  10cm depth, \u00b0C Soil_temp_20cm - Soil temperature at 20cm depth, \u00b0C  Soil_temp_30cm - Soil temperature at 30cm depth, \u00b0C Soil_temp_40cm - Soil  temperature at 40cm depth, \u00b0C --- ## #Soil _data.csv This file contains  data of study site soil analysis ## Description of the data and file  structure Year - Sampling year Date - Sampling date Place - Study objects  name FT - Forest type (ND - not drained, KS - drained) Soil_cm - Soil  sampling depth Repetition - Number of repetitions (1-2) Soil_density -  Soil bulk density, g/kg C_g_kg - Carbon content in sample, g/kg N_g_kg -  Nitrogen content in sample, g/kg C_N - Carbon and Nitrogen ratio in sample  pHKCl - Soil pH Pkop_g_kg - Total Phosphorus content in sample, g/kg  K_mg_kg - Total Potassium content in sample, g/kg Ca_mg_kg - Total Calcium  content in sample, g/kg Mg_mg_kg - Total Magnesium content in sample, g/kg  --- ## #FRP _data.csv This file contains data of study site fine-root  biomass, stand taxation indices and soil analysis per study object sample  plot and fine-root fraction ## Description of the data and file structure  ID - Study site ID Place - Study object name FT - Forest type (ND - not  drained, KS - drained) Cycle - Sampling campaign number in specific  sampling year PL - Sampling plot number Fraction - Fine-root fraction by  name FRB - Fine-root biomass, t/ha FRB_BA - Fine-root biomass per basal  area Pine_yield - Pine tree growing stock, m3/ha N_ha - Tree count per ha  Spruce_yield - Spruce tree growing stock, m3/ha Shrub_percentage -  Percentage of shrubs in ground vegetation Herb_percentage - Percentage of  herbacous plants in ground vegetation D - Diameter at breast height, cm  G_m2ha - basal area, m2/ha CN - soil C and N ratio pHKCl - soil pH CgKg -  Soil Carbon (C) content, g/kg NgKg - Soil Nitrogen (N) content, g/kg ---  ## #Mean _FRB _pa _frakcijam.csv This file contains data of study site  average fine-root biomass per study object sample plot and fine-root  fraction ## Description of the data and file structure ID - Study site ID  Object - Study object name FT - Forest type (ND - not drained, KS -  drained) PL - Sampling campaign number in specific sampling year Fraction  - Fine-root fraction by name AvgFRB - Average fine-root biomass, t/ha  FRB_BA - Average fine-root biomass per basal area Sd - Standarddeviation  of average fine-root biomass n - sampling campaign count se -  Standarderror of average fine-root biomass Basal_Area - basal area, m2/ha  --- ## #PCA _analize.csv This file contains data of study site for PCA  analysis containing fine-root biomass, production and turnover, taxation  indices and soil data per sample plot ## Description of the data and file  structure ID - Study site ID Site - Study object name FT - Forest type (ND  - not drained, KS - drained) Plot - - Sampling plot number SP_FRB - Scots  pine fine-root biomass, t/ha SP_FRP - Scots pine fine-root production,  t/ha/yr SP_T - Scots pine fine-root turnover, t/yr PineFRB_BA - Scots pine  fine-root biomass per stand basal area, t/m2 NS_FRB - Norway spruce  fine-root biomass, t/ha NS_FRP - Norway spruce fine-root production,  t/ha/yr NS_T - Norway spruce fine-root turnover, t/yr SpurceFRB_BA -  Norway spruce fine-root biomass per stand basal area, t/m2 H_FRB - Herb  fine-root biomass, t/ha DS_FRB - Dwarf shrub fine-root biomass, t/ha  DS_FRP - Dwarf shub fine-root production, t/ha/yr TOT_FRP - Total  fine-root production, t/ha/yr SP_dFRB - Scots pine fine-root necromass,  t/ha NS_dFRB - Norway spruce fine-root necromass, t/ha C_g_kg - Soil  Carbon content, g/kg N_g_kg - Soil Nitrogen content, g/kg C_N - Carbon and  Nitrogen ratio in sample pHKCl - Soil pH Pkop - Total soil Phosphorous  content, g/kg Aug_bl - Soil bulk density, g/kg Dg - Diameter at breast  height, cm Hg - Tree height, m G - basal area, m2/ha Yield_1st - First  layer tree growing stock, m3/ha N_ha - Tree count per ha SP_m3ha - Pine  tree growing stock, m3/ha NS_m3ha - Spruce tree growing stock, m3/ha DS_m2  - Dwarf shrub coverage, m2 H_m2 - Herbacous plant coverage, m2 --- ##  #R _frb.csv This file contains raw data of fine-root samples per site,  sample plot, fraction and sampling depth ## Description of the data and  file structure Place - Study objects name ID - Sample ID CM - Sampling  depth, cm Fraction - Fine-root fraction ID Species - Fine-root fraction by  name Status - Fine-root status (living/dead) Weight_g - Sample weight FT -  Forest type (ND - not drained, KS - drained) FRB - Fine-root biomass, t/ja  Cycle - Sampling campaign number ID_cycle - Sample ID per sampling cycle  PL - Sampling plot number Place_pl_cm_cycle - ID containing study object  name, forest type, sampling depth and sampling cycle ## Sharing/Access  information Correspondence: Valters Samariks, Latvian State Forest  Research Institute 'Silava', Latvia, Salaspils, R\u012bgas street  111, LV-2169, Email: ; ORCID:  0000-0001-9953-0455 ## Code Code for this data file is available in  Fine_root_calculations_DRYAD.R", "keywords": ["hemiboreal", "Fine-root production", "forest drainage", "Peat", "fine-root turnover", "FOS: Agriculture", " forestry", " and fisheries"], "contacts": [{"organization": "Samariks, Valters", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5061/dryad.b8gtht7kg"}, {"rel": "self", "type": "application/geo+json", "title": "10.5061/dryad.b8gtht7kg", "name": "item", "description": "10.5061/dryad.b8gtht7kg", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5061/dryad.b8gtht7kg"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-02-20T00:00:00Z"}}], "links": [{"rel": "self", "type": "application/geo+json", "title": "This document as GeoJSON", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=fine-root&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=fine-root&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=fine-root&", "hreflang": "en-US"}, {"rel": "last", "type": "application/geo+json", "title": "items (last)", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=fine-root&offset=6", "hreflang": "en-US"}], "numberMatched": 6, "numberReturned": 6, "distributedFeatures": [], "timeStamp": "2026-06-24T14:08:16.640840Z"}