{"type": "FeatureCollection", "features": [{"id": "10.1007/s004420100656", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:14:26Z", "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": "10.1093/treephys/25.12.1511", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:18:16Z", "type": "Journal Article", "created": "2012-01-20", "title": "Effects Of Elevated Concentrations Of Atmospheric Co2 And Tropospheric O-3 On Leaf Litter Production And Chemistry In Trembling Aspen And Paper Birch Communities", "description": "Human activities are increasing the concentrations of atmospheric carbon dioxide ([CO2]) and tropospheric ozone ([O3]), potentially leading to changes in the quantity and chemical quality of leaf litter inputs to forest soils. Because the quality and quantity of labile and recalcitrant carbon (C) compounds influence forest productivity through changes in soil organic matter content, characterizing changes in leaf litter in response to environmental change is critical to understanding the effects of global change on forests. We assessed the independent and combined effects of elevated [CO2] and elevated [O3] on foliar litter production and chemistry in aspen (Populus tremuloides Michx.) and birch-(Betula papyrifera Marsh.) aspen communities at the Aspen free-air CO2 enrichment (FACE) experiment in Rhinelander, WI. Litter was analyzed for concentrations of C, nitrogen (N), soluble sugars, lipids, lignin, cellulose, hemicellulose and C-based defensive compounds (soluble phenolics and condensed tannins). Concentrations of these chemical compounds in naturally senesced litter were similar in aspen and birch-aspen communities among treatments, except for N, the C:N ratio and lipids. Elevated [CO2] significantly increased C:N (+8.7%), lowered mean litter N concentration (-10.7%) but had no effect on the concentrations of soluble sugars, soluble phenolics and condensed tannins. Elevated [CO2] significantly increased litter biomass production (+33.3%), resulting in significant increases in fluxes of N, soluble sugars, soluble phenolics and condensed tannins to the soil. Elevated [O3] significantly increased litter concentrations of soluble sugars (+78.1%), soluble phenolics (+53.1%) and condensed tannins (+77.2%). There were no significant effects of elevated [CO2] or elevated [O3] on the concentrations of individual C structural carbohydrates (cellulose, hemicellulose and lignin). Elevated [CO2] significantly increased cellulose (+37.4%) input to soil, whereas elevated [O3] significantly reduced hemicellulose and lignin inputs to soil (-22.3 and -31.5%, respectively). The small changes in litter chemistry in response to elevated [CO2] and tropospheric [O3] that we observed, combined with changes in litter biomass production, could significantly alter the inputs of N, soluble sugars, condensed tannins, soluble phenolics, cellulose and lignin to forest soils in the future.", "keywords": ["Nitrogen", "aspen", "carbon", "nutrient cycling", "04 agricultural and veterinary sciences", "Carbon Dioxide", "15. Life on land", "Carbon", "Plant Leaves", "ozone", "Soil", "Wisconsin", "Ozone", "Populus", "litter", "FACE", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "CO2", "leaves", "Biomass", "soils", "Forest Sciences", "Betula", "Ecosystem"], "contacts": [{"organization": "Liu, Lingli, King, John S., Giardina, Christian P.,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1093/treephys/25.12.1511"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Tree%20Physiology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1093/treephys/25.12.1511", "name": "item", "description": "10.1093/treephys/25.12.1511", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1093/treephys/25.12.1511"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2005-12-01T00:00:00Z"}}, {"id": "10.1093/treephys/22.7.435", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:18:15Z", "type": "Journal Article", "created": "2012-01-20", "title": "Responses Of Deciduous Broadleaf Trees To Defoliation In A Co2 Enriched Atmosphere", "description": "Relatively little is known about the implications of atmospheric CO2 enrichment for tree responses to biotic disturbances such as folivory. We examined the combined effects of elevated CO2 concentration ([CO2]) and defoliation on growth and physiology of sugar maple (Acer saccharum Marsh.) and trembling aspen (Populus tremuloides Michx.). Seedlings were planted in the ground in eight open-top chambers. Four chambers were ventilated with CO2-enriched air (ambient + 283 micromol mol-1) and four chambers were supplied with ambient air. After 6 weeks of growth, half of the leaf area was removed on a subset of seedlings of each species in each CO2 treatment. We monitored subsequent biomass gain and allocation, along with leaf gas exchange and chemistry. Defoliation did not significantly affect final seedling biomass in either species or CO2 treatment. Growth recovery following defoliation was associated with increased allocation to leaf mass in maple and a slight enhancement of mean photosynthesis in aspen. Elevated [CO2] did not significantly affect aspen growth, and the observed stimulation of maple growth was significant only in mid-season. Correspondingly, simulated responses of whole-tree photosynthesis to elevated [CO2] were constrained by a decrease in photosynthetic capacity in maple, and were partially offset by reductions in specific leaf area and biomass allocation to foliage in aspen. There was a significant interaction between [CO2] and defoliation on only a few of the measured traits. Thus, the data do not support the hypothesis that atmospheric CO2 enrichment will substantially alter tree responses to folivory. However, our findings do provide further indication that regeneration-stage growth rates of certain temperate tree species may respond only moderately to a near doubling of atmospheric [CO2].", "keywords": ["defoliation-", "0106 biological sciences", "Ecophysiology", "Quaking aspen", "biomass-allocation", "growth-response", "Growth", "Environmental-Sciences)", "01 natural sciences", "plant-composition", "Trees", "biomass-", "Spermatophyta-", "Biomass", "Photosynthesis", "plant-physiology", "defoliation", "Angiospermae-", "leaf-area", "GLOBAL-ECOLOGY", "seedling-growth", "source-sink-relations", "Populus-tremuloides", "gas-exchange", "Populus", "broadleaves-", "deciduous-tree", "forest-trees", "atmosphere-", "trees-", "biomass-production", "Acer saccharum", "Nitrogen", "Carbohydrates", "Acer", "carbon-dioxide-enrichment", "photosynthesis-", "growth-", "species-differences", "seedlings-", "wisconsin-", "Populus tremuloides", "photosynthesis", "Climatic changes", "Carbon Dioxide", "15. Life on land", "Plant Leaves", "leaves-", "Aceraceae-: Dicotyledones-", "Carbon dioxide", "Sugar maple", "Seedlings", "Terrestrial-Ecology (Ecology-", "Acer-saccharum"], "contacts": [{"organization": "Volin, John C., Kruger, Eric L., Lindroth, Richard L.,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1093/treephys/22.7.435"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Tree%20Physiology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1093/treephys/22.7.435", "name": "item", "description": "10.1093/treephys/22.7.435", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1093/treephys/22.7.435"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2002-05-01T00:00:00Z"}}, {"id": "10.1111/j.1469-8137.2005.01557.x", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:18:49Z", "type": "Journal Article", "created": "2005-09-02", "title": "Tropospheric O3 Compromises Net Primary Production In Young Stands Of Trembling Aspen, Paper Birch And Sugar Maple In Response To Elevated Atmospheric Co2", "description": "Concentrations of atmospheric CO(2) and tropospheric ozone (O(3)) are rising concurrently in the atmosphere, with potentially antagonistic effects on forest net primary production (NPP) and implications for terrestrial carbon sequestration. Using free-air CO(2) enrichment (FACE) technology, we exposed north-temperate forest communities to concentrations of CO(2) and O(3) predicted for the year 2050 for the first 7 yr of stand development. Site-specific allometric equations were applied to annual nondestructive growth measurements to estimate above- and below-ground biomass and NPP for each year of the experiment. Relative to the control, elevated CO(2) increased total biomass 25, 45 and 60% in the aspen, aspen-birch and aspen-maple communities, respectively. Tropospheric O(3) caused 23, 13 and 14% reductions in total biomass relative to the control in the respective communities. Combined fumigation resulted in total biomass response of -7.8, +8.4 and +24.3% relative to the control in the aspen, aspen-birch and aspen-sugar maple communities, respectively. These results indicate that exposure to even moderate levels of O(3) significantly reduce the capacity of NPP to respond to elevated CO(2) in some forests.", "keywords": ["0106 biological sciences", "aspen", "carbon dioxide", "Acer", "Carbon Dioxide", "15. Life on land", "Wood", "01 natural sciences", "Carbon", "Plant Leaves", "ozone", "Wisconsin", "Ozone", "Populus", "13. Climate action", "pollution", "Biomass", "Forest Sciences", "global change", "Betula", "0105 earth and related environmental sciences"], "contacts": [{"organization": "Kurt S. Pregitzer, Mark E. Kubiske, David F. Karnosky, George R. Hendrey, John S. King, John S. King, Christian P. Giardina, Vanessa S. Quinn, Evan P. McDonald,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1111/j.1469-8137.2005.01557.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": "10.1111/j.1469-8137.2005.01557.x", "name": "item", "description": "10.1111/j.1469-8137.2005.01557.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/j.1469-8137.2005.01557.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2005-09-02T00:00:00Z"}}, {"id": "10.1139/x92-146", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:19:07Z", "type": "Journal Article", "created": "2009-12-18", "title": "Carbon Storage In Lake States Aspen Ecosystems", "description": "<p> Total ecosystem carbon in the soil and vegetation was measured for a range of aspen (Populustremuloides Michx.) ecosystems, including a chronosequence on the same soil ranging in age from 0 to 80 years. Soil carbon stayed relatively constant throughout the stand's life and was not affected by timber harvesting. Changes in ecosystem carbon closely paralleled the changes in standing biomass. Aspen grown on 40-year rotations on good soils will sequester several times as much carbon per year as old-growth forests. </p>", "keywords": ["Management Options", "0106 biological sciences", "Michigan", "Spermatophyta", "Angiosperms", "Broadleaves", "wisconsin", "aspen", "Minnesota", "01 natural sciences", "Dicots", "forest succession", "Spermatophytes", "Populus tremuloides", "Biomass", "Plantae", "Forest Sciences", "USA", "Vascular Plants", "Salicaceae: Dicotyledones", "carbon", "Rotation Length", "age of trees", "Forestry", "Carbon cycle", "plant succession", "Plants", "Timber Harvest", "forest ecosystem", "carbon storage", "15. Life on land", "Angiospermae", "Chronosequence Soil Carbon", "ecosystems"], "contacts": [{"organization": "Alban, David H., Perala, D.A.,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1139/x92-146"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Canadian%20Journal%20of%20Forest%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1139/x92-146", "name": "item", "description": "10.1139/x92-146", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1139/x92-146"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "1992-08-01T00:00:00Z"}}, {"id": "10.1890/06-1819.1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:19:45Z", "type": "Journal Article", "created": "2007-10-23", "title": "Atmospheric Co2 And O-3 Alter The Flow Of N-15 In Developing Forest Ecosystems", "description": "Anthropogenic O3 and CO2-induced declines in soil N availability could counteract greater plant growth in a CO2-enriched atmosphere, thereby reducing net primary productivity (NPP) and the potential of terrestrial ecosystems to sequester anthropogenic CO2. Presently, it is uncertain how increasing atmospheric CO2 and O3 will alter plant N demand and the acquisition of soil N by plants as well as the microbial supply of N from soil organic matter. To address this uncertainty, we initiated an ecosystem-level 15N tracer experiment at the Rhinelander (Wisconsin, USA) free air CO2-O3 enrichment (FACE) facility to understand how projected increases in atmospheric CO2 and 03 alter the distribution and flow of N in developing northern temperate forests. Tracer amounts of 15NH4+ were applied to the forest floor of developing Populus tremuloides and P. tremuloides-Betula papyrifera communities that have been exposed to factorial CO2 and O3 treatments for seven years. One year after isotope addition, both forest communities exposed to elevated CO2 obtained greater amounts of 15N (29%) and N (40%) from soil, despite no change in soil N availability or plant N-use efficiency. As such, elevated CO2 increased the ability of plants to exploit soil for N, through the development of a larger root system. Conversely, elevated O3 decreased the amount of 15N (-15%) and N (-29%) in both communities, a response resulting from lower rates of photosynthesis, decreases in growth, and smaller root systems that acquired less soil N. Neither CO2 nor 03 altered the amount of N or 15N recovery in the forest floor, microbial biomass, or soil organic matter. Moreover, we observed no interaction between CO2 and 03 on the amount of N or 15N in any ecosystem pool, suggesting that 03 could exert a negative effect regardless of CO2 concentration. In a CO2-enriched atmosphere, greater belowground growth and a more thorough exploitation of soil for growth-limiting N is an important mechanism sustaining the enhancement of NPP in developing forests (0-8 years following establishment). However, as CO2 accumulates in the Earth's atmosphere, future O3 concentrations threaten to diminish the enhancement of plant growth, decrease plant N acquisition, and lessen the storage of anthropogenic C in temperate forests.", "keywords": ["0106 biological sciences", "Nitrogen", "Science", "Ecology and Evolutionary Biology", "Plant Roots", "01 natural sciences", "forest floor", "Soil", "developing forest", "Wisconsin", "atmospheric O3", "Ozone", "soil organic matter", "Populus tremuloides", "Biomass", "USA", "Ecosystem", "Soil Microbiology", "atmospheric CO2", "Nitrogen Isotopes", "15N", "plant N uptake", "microbial immobilization", "04 agricultural and veterinary sciences", "Carbon Dioxide", "15. Life on land", "root system size", "Populus", "N cycling", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "Betula papyrifera"]}, "links": [{"href": "https://doi.org/10.1890/06-1819.1"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Ecology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1890/06-1819.1", "name": "item", "description": "10.1890/06-1819.1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1890/06-1819.1"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2007-10-01T00:00:00Z"}}, {"id": "10.5061/dryad.9w0vt4bk0", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-26T16:21:24Z", "type": "Dataset", "title": "The influence of inherent soil factors and agricultural management on soil organic matter", "description": "unspecifiedField descriptions and  sampling.\u00a0  Soil samples were collected  from 218 farm fields across Wisconsin (n=212) and Minnesota (n=6) (Fig. 1)  between 2015 and 2017. The fields represent a range of cropping systems  common in the Upper Midwest. Six distinct regions were sampled and  identified by either general region of a state (northeast Wisconsin,  southeast Wisconsin, and southern Minnesota) or by watershed (Dry Run, Elk  Creek, Jersey Valley) (Fig. 1). Elk Creek and Jersey Valley exist within  the Driftless Region, an area characterized by steep slopes and flash  flood events. All fields were planted into corn the season soil samples  were collected. In each field, three composite soil samples were collected  that consisted of five 0- to 15-cm soil cores collected with a probe of  2.5- or 7.5-cm internal diameter. Most soil samples (194) were collected  prior to fertilizer application and corn planting (mid-April); 24 samples  were in late June (2017 only). Soil sampling was conducted with an area of  36 m<sup>2</sup> within the dominant soil map unit as  identified by the USDA NRCS Web Soil Survey (Soil Survey Staff, 2019) and  from an area identified by the farmer where average crop yields were  obtained. The composite samples were stored cold and transferred into a  freezer with 1 to 6 hours of sampling to stagnate microbial metabolism and  organic matter mineralization. Within 30 days, soil samples were thawed  and dried for 1 week at 32\u02daC in a forced-air drier, ground to pass through  a 2-mm sieve, and stored at room temperature until  analysis. Inherent soil properties such as texture class,  sand and clay content of the surface horizon, and drainage class were  obtained from the USDA NRCS Web Soil Survey (Soil Survey Staff, 2019).  Agronomic management information regarding crop rotation, tillage  practices, cover crop use, tile drainage, and manure and fertilizer  applications were obtained directly from each farmer through an in-person  interview. Long-term crop management practices were difficult to obtain  for all farms; for example, it was difficult to get accurate information  on how long a field had received manure. The dataset constructed uses  recent cropping history (past 5 years) as a representation of specific  management practices (that often have occurred much longer than just the  past 5 years). Based on the collected data, four categories for crop  rotation (continuous corn, corn-soybean, corn with small grain, and corn  with alfalfa) and five categories for previous crop were created  (Supplementary Table 2). Two categorical data were developed for cover  crops: if there was a cover crop planted last fall (yes or no) and the  number of times a cover crop was planted in the past 5 years. Tillage  practices were categorized by practice [no tillage, minimum tillage  (including vertical tillage or strip tillage), and conventional tillage  (chisel, disk or moldboard)] and by the number of tillage passes that  occurred between harvest of the previous year\u2019s crop and the planting of  the current year\u2019s crop (0 to 4). Tillage was only considered no-till or  minimum tillage if practiced for more than 4 years. Manure was categorized  based on the number of manure applications that occurred in the past 5  years (0 to 5), when manure was applied in the past year (none, summer,  fall, winter, or spring), and manure type (species and if solid or  liquid). Tile drainage presence was also noted (yes or no). The manure N,  fertilizer N, and total N input (which includes manure, fertilizer, and  legume N inputs) (kg ha<sup>-1</sup>) to the previous corn  crop were also collected. If farmers did not have manure analysis,  estimates of available N were used (Laboski &amp; Peters, 2012); N  input from alfalfa biomass was assumed to be 101 kg  ha<sup>-1</sup> (Laboski &amp; Peters,  2012).\u00a0 Soil analysis.\u00a0 Soil  pH and SOM were analyzed by the University of Wisconsin Soil and Forage  Analysis Laboratory (Marshfield, Wisconsin). Soil pH was calculated using  a 1:1 slurry of 10 g soil and 10 mL of deionized water and measured with a  glass electrode (Peters et al., 2015). Soil organic matter values were  determined through loss on ignition by heating the soil to 360\u02daC for 2  hours (Combs et al., 2015). Total C (TC) and total N (TN) levels were  determined via the dry combustion method using a Flash EA 1112CN Automatic  Elemental Analyzer (Thermo Finnigan, Milan, Italy). Between 8 to 10 mg of  finely ground soil were packed into a 5 mm by 9 mm tin capsule prior to  combustion at temperatures exceeding 1000\u00b0C. Soils with pH greater than  7.0 were tested for effervescence using 5% HCl as an indicator if  carbonates were present. If carbonates were not observed, TC was assumed  to be TOC; if carbonates were observed, they were subject to  acid-fumigation prior to dry combustion (Harris et al., 2001). Only 25  samples were analyzed for carbonates and 13 of those had carbonate  concentrations above the detection limit. There were 218 samples for SOM,  but only 2016 for TOC and TN because two samples were accidently  discarded.", "keywords": ["2. Zero hunger", "Alfalfa", "FOS: Agricultural sciences", "15. Life on land", "Total nitrogen", "Zea mays", "soil", "Tillage", "Maize", "soil organic carbon", "loss on ignition", "corn", "crop rotation", "Wisconsin", "soil organic matter", "manure", "Soil texture", "drainage", "Medicago sativa"], "contacts": [{"organization": "Ruark, Matt, Richardson, Greg, Radatz, Timothy, Radatz, Amber, Cooley, Eric, Augarten, Abigail,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5061/dryad.9w0vt4bk0"}, {"rel": "self", "type": "application/geo+json", "title": "10.5061/dryad.9w0vt4bk0", "name": "item", "description": "10.5061/dryad.9w0vt4bk0", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5061/dryad.9w0vt4bk0"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-02-02T00:00:00Z"}}, {"id": "e8c9167a-4e29-44c2-8972-c8c2a3c3d86d", "type": "Feature", "geometry": {"type": "Polygon", "coordinates": [[[5.81, 47.26], [5.81, 54.76], [15.77, 54.76], [15.77, 47.26], [5.81, 47.26]]]}, "properties": {"themes": [{"concepts": [{"id": "farming"}], "scheme": "https://standards.iso.org/iso/19139/resources/gmxCodelists.xml#MD_TopicCategoryCode"}, {"concepts": [{"id": "Soil"}, {"id": "precision agriculture"}, {"id": "remote sensing"}, {"id": "sensors"}, {"id": "clay"}, {"id": "soil organic carbon"}, {"id": "soil organic matter"}, {"id": "machine learning"}, {"id": "regression analysis"}, {"id": "soil chemistry"}], "scheme": "AGROVOC Multilingual agricultural thesaurus"}, {"concepts": [{"id": "opendata"}, {"id": "Digital Soil Mapping"}, {"id": "pH"}], "scheme": "Individual"}, {"concepts": [{"id": "Boden"}], "scheme": "GEMET - INSPIRE themes, version 1.0"}, {"concepts": [{"id": "Brazil"}, {"id": "Sao Paulo"}, {"id": "Bahia"}, {"id": "Goias"}, {"id": "Mato Grosso"}, {"id": "Mato Grosso do Sul"}, {"id": "Santa Catarina"}, {"id": "Germany"}, {"id": "Brandenburg"}, {"id": "North Rhine-Westphalia"}, {"id": "Saxony-Anhalt"}, {"id": "Mecklenburg-Western Pomerania"}, {"id": "China"}, {"id": "Hubei"}, {"id": "Japan"}, {"id": "Saitama Prefecture"}, {"id": "Sweden"}, {"id": "Sk\u00e5ne L\u00e4n"}, {"id": "Uppsala L\u00e4n"}, {"id": "Switzerland"}, {"id": "Canton of Vaud"}, {"id": "USA"}, {"id": "Wisconsin"}, {"id": "Hungary"}, {"id": "Pest County"}, {"id": "Czechia"}, {"id": "South Moravia"}, {"id": "France"}, {"id": "Occitania"}], "scheme": "individual"}], "rights": "Restrictions applied to assure the protection of privacy or intellectual property, and any special restrictions or limitations or warnings on using the resource or metadata. Reports, articles, papers, scientific and non - scientific works of any form, including tables, maps, or any other kind of output, in printed or electronic form, based in whole or in part on the data supplied, must contain an acknowledgement of the form: \"Data reused from the BonaRes Data Centre www.bonares.de. This data were created as part of the ZALF Datenerfassung's research activities.\" Although every care has been taken in preparing and testing the data, the ZALF Datenerfassung and the BonaRes Data Centre cannot guarantee that the data are correct; neither does the ZALF Datenerfassung and the BonaRes Data Centre accept any liability whatsoever for any error, missing data or omission in the data, or for any loss or damage arising from its use. The ZALF Datenerfassung and BonaRes Data Centre will not be responsible for any direct or indirect use which might be made of the data.", "updated": "2025-02-26", "type": "Dataset", "created": "2025-02-24", "language": "eng", "title": "Precision Liming Soil Datasets (LimeSoDa)", "description": "Precision Liming Soil Datasets (LimeSoDa) is a collection of 31 datasets from a field- and farm-scale soil mapping context. These datasets are \"ready-to-use\" for modeling purposes, as they include target soil properties and features in a tidy tabular format. Three target soil properties are present in every dataset: (1) soil organic matter (SOM) or soil organic carbon (SOC), (2) pH, and (3) clay content, while the features for modeling are dataset-specific. The primary goal of `LimeSoDa` is to enable more reliable benchmarking of machine learning methods in digital soil mapping and pedometrics. All the associated materials and data from LimeSoDa can be downloaded in this data repository. However, for a more in-depth analysis, we refer to the published paper \"LimeSoDa: A Dataset Collection for Benchmarking of Machine Learning Regressors in Digital Soil Mapping\" by Schmidinger et al. 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