Quantifying the effects of grazing on soil organic carbon (SOC) decomposition is of crucial importance for understanding soil C dynamics. However, less attention has been paid to the pool\uffe2\uff80\uff90specific SOC decomposition and the underlying factors associated with each C pool, representing critical knowledge gaps on soil C dynamics. In this study, we applied a state\uffe2\uff80\uff90of\uffe2\uff80\uff90the\uffe2\uff80\uff90art Bayesian data assimilation technique to re\uffe2\uff80\uff90analyze previous soil incubation data to examine how herbivores influenced the fraction and cumulative respiration of labile and recalcitrant soil C pools from seven edaphically diverse sites in Yellowstone National Park, whereas those variables were not explored in the earlier study. Our results showed that grazing significantly increased cumulative respiration from both labile and recalcitrant C pools. Greater cumulative respiration from the labile C pool was related to grazers increasing labile C pool fractions, while higher cumulative respiration from the recalcitrant C pool was associated with grazers accelerating the decomposition rate of the recalcitrant C pool. Cumulative respiration from both labile and recalcitrant C pools was positively correlated with shoot biomass, soil gravimetric moisture, and soil C and nitrogen content. Our results underscore how knowledge of pool\uffe2\uff80\uff90specific SOC decomposition can provide a better mechanistic understanding of soil C dynamics along topo\uffe2\uff80\uff90edaphic gradients in grazed grassland.Conversion of arable land (maize) to pasture will affect the soil organic matter (SOM) content. Changes in the SOM content were studied using a size- and density-fractionation method and C-13 analysis. Twenty-six years of maize cropping had resulted in a depletion of carbon stored in the macro-organic fractions (>150 mu m) and an increase in the 250 mu m), light (b.d. 150 mu m) and light (b.d. 150 mu m; b.d. >1.13 g cm(-3)) in the 0- to 20-cm layer was still 40-50% lower than in the continuous pasture plots. Average half-life times calculated from C-13 analyses ranged from 7 years in the light fractions to 56 years in heavy fractions. Fractionation results and C-13 data indicated that mechanical disturbance (plowing) during maize cropping had resulted in vertical displacement of dispersed soil carbon from the 0- to 20-cm layer down to 60-80 cm. Conversion of arable land to pasture, therefore, not only causes a regeneration of the soil carbon content, it also reduces the risk of contaminant transport by dispersed soil carbon.
", "keywords": ["land use change", "DECOMPOSITION", "2. Zero hunger", "C-13 analyses", "04 agricultural and veterinary sciences", "15. Life on land", "maize", "Maize", "C-13 NATURAL-ABUNDANCE", "CULTIVATION", "pasture", "13C analyses", "VERTISOLS", "SIZE", "SYSTEMS", "Pasture", "0401 agriculture", " forestry", " and fisheries", "Organic matter", "Fractionation", "fractionation", "Land use change", "CARBON TURNOVER", "FRACTIONS", "organic matter", "STORAGE"], "contacts": [{"organization": "R\u00f6mkens, P.F.A.M., van der Plicht, J., Hassink, J.,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1007/s003740050494"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biology%20and%20Fertility%20of%20Soils", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s003740050494", "name": "item", "description": "10.1007/s003740050494", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s003740050494"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "1999-01-01T00:00:00Z"}}, {"id": "10.1007/s003740050493", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:14:41Z", "type": "Journal Article", "created": "2002-08-25", "title": "The Climex Soil-Heating Experiment: Soil Response After 2 Years Of Treatment", "description": "Most model predictions concerning the response of boreal forest ecosystems to climate change are inferred from small-scale experiments on artificial, simplified systems. Whole-ecosystem experiments designed to validate these models are scarce. We experimentally manipulated a small forested catchment in southern Norway by increasing soil temperature (+3 \u00b0C in summer to +5 \u00b0C in winter) using heating cables installed at 1 cm depth in the litter layer. Especially nitrification in the 0 to 10-cm soil layer increased as a result of the climate manipulation. Betula litter, produced after exposing trees for 2 years to ambient and elevated CO2 in greenhouses, was incubated for 1 year in the manipulated catchment. Exposure to elevated CO2 did not affect the C/N ratio or decomposition of the Betula litter, but lignin content decreased by 10%. We found no effect of elevated temperature on litter decomposition, probably due to desiccation of the litter. The heating cables caused a permanent increase in soil temperature in this soil layer, but when soils were dry, the temperature difference between control and heated plots decreased with increasing distance from the cables. When soils were wet, no gradients in temperature increase occurred.", "keywords": ["Climate warming", "Decomposition", "Nitrogen mineralization", "Whole catchment manipulation", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land", "Soil heating", "01 natural sciences", "0105 earth and related environmental sciences"], "contacts": [{"organization": "Verburg, P.S.J., van Loon, W.K.P., L\u00fckewille, A.,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1007/s003740050493"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biology%20and%20Fertility%20of%20Soils", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s003740050493", "name": "item", "description": "10.1007/s003740050493", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s003740050493"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "1999-01-01T00:00:00Z"}}, {"id": "10.1007/s10021-004-0218-4", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:14:47Z", "type": "Journal Article", "created": "2004-08-21", "title": "Climate Change Affects Carbon Allocation To The Soil In Shrublands", "description": "Climate change may affect ecosystem functioning through increased temperatures or changes in precipitation patterns. Temperature and water availability are important drivers for ecosystem processes such as photosynthesis, carbon translocation, and organic matter decomposition. These climate changes may affect the supply of carbon and energy to the soil microbial population and subsequently alter decomposition and mineralization, important ecosystem processes in carbon and nutrient cycling. In this study, carried out within the cross-European research project CLIMOOR, the effect of climate change, resulting from imposed manipulations, on carbon dynamics in shrubland ecosystems was examined. We performed a 14C-labeling experiment to probe changes in net carbon uptake and allocation to the roots and soil compartments as affected by a higher temperature during the year and a drought period in the growing season. Differences in climate, soil, and plant characteristics resulted in a gradient in the severity of the drought effects on net carbon uptake by plants with the impact being most severe in Spain, followed by Denmark, with the UK showing few negative effects at significance levels of p \u2264 0.10. Drought clearly reduced carbon flow from the roots to the soil compartments. The fraction of the 14C fixed by the plants and allocated into the soluble carbon fraction in the soil and to soil microbial biomass in Denmark and the UK decreased by more than 60%. The effects of warming were not significant, but, as with the drought treatment, a negative effect on carbon allocation to soil microbial biomass was found. The changes in carbon allocation to soil microbial biomass at the northern sites in this study indicate that soil microbial biomass is a sensitive, early indicator of drought- or temperature-initiated changes in these shrubland ecosystems. The reduced supply of substrate to the soil and the response of the soil microbial biomass may help to explain the observed acclimation of CO2 exchange in other ecosystems.", "keywords": ["2. Zero hunger", "0106 biological sciences", "decomposition", "photosynthesis", "temperature", "translocation", "plant", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "6. Clean water", "dioxide", "calluna-vulgaris", "13. Climate action", "lolium-perenne", "0401 agriculture", " forestry", " and fisheries", "rhizosphere", "respiration"]}, "links": [{"href": "https://doi.org/10.1007/s10021-004-0218-4"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Ecosystems", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s10021-004-0218-4", "name": "item", "description": "10.1007/s10021-004-0218-4", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s10021-004-0218-4"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2004-08-06T00:00:00Z"}}, {"id": "10.1007/s10021-004-0259-8", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:14:47Z", "type": "Journal Article", "created": "2005-07-11", "title": "The Influence Of Nutrient Availability On Soil Organic Matter Turnover Estimated By Incubations And Radiocarbon Modeling", "description": "We investigated the decomposability of soil organic matter (SOM) along a chronosequence of rainforest sites in Hawaii that form a natural fertility gradient and at two long-term fertilization experiments. To estimate turnover times and pool sizes of organic matter, we used two independent methods: (1) long-term incubations and (2) a three-box soil model constrained by radiocarbon measurements. Turnover times of slow-pool SOM (the intermediate pool between active and passive pools) calculated from incubations ranged from 6 to 20 y in the O horizon and were roughly half as fast in the A horizon. The radiocarbon-based model yielded a similar pattern but slower turnover times. The calculation of the 14C turnover times is sensitive to the lag time between photosynthesis and incorporation of organic C into SOM in a given horizon. By either method, turnover times at the different sites varied two- or threefold in soils with the same climate and vegetation community. Turnover times were fastest at the sites of highest soil fertility and were correlated with litter decay rates and primary productivity. However, experimental fertilization at the two least-fertile sites had only a small and inconsistent effect on turnover, with N slowing turnover and P slightly speeding it at one site. These results support studies of litter decomposition in suggesting that while plant productivity can respond rapidly to nutrient additions, decomposition may respond much more slowly to added nutrients.", "keywords": ["tropical forest", "decomposition", "Ecology", "microbial biomass", "carbon", "C-14", "04 agricultural and veterinary sciences", "Biological Sciences", "15. Life on land", "nitrogen", "0401 agriculture", " forestry", " and fisheries", "phosphorus", "Zoology", "Environmental Sciences"]}, "links": [{"href": "https://escholarship.org/content/qt9186j2fw/qt9186j2fw.pdf"}, {"href": "https://doi.org/10.1007/s10021-004-0259-8"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Ecosystems", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s10021-004-0259-8", "name": "item", "description": "10.1007/s10021-004-0259-8", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s10021-004-0259-8"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2005-06-01T00:00:00Z"}}, {"id": "10.1007/s10021-007-9104-1", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:14:47Z", "type": "Journal Article", "created": "2007-11-16", "title": "Nutrient Addition Prompts Rapid Destabilization Of Organic Matter In An Arctic Tundra Ecosystem", "description": "Nutrient availability in the arctic is expected to increase in the next century due to accelerated decomposition associated with warming and, to a lesser extent, increased nitrogen deposition. To explore how changes in nutrient availability affect ecosystem carbon (C) cycling, we used radiocarbon to quantify changes in belowground C dynamics associated with long-term fertilization of graminoid-dominated tussock tundra at Toolik Lake, Alaska. Since 1981, yearly fertilization with nitrogen (N) and phosphorus (P) has resulted in a shift to shrub-dominated vegetation. These combined changes have altered the quantity and quality of litter inputs, the vertical distribution and dynamics of fine roots, and the decomposition rate of soil organic C. The loss of C from the deep organic and mineral soil has more than offset the C accumulation in the litter and upper organic soil horizons. In the litter and upper organic horizons, radiocarbon measurements show that increased inputs resulted in overall C accumulation, despite being offset by increased decomposition in some soil pools. To reconcile radiocarbon observations in the deeper organic and mineral soil layers, where most of the ecosystem C loss occurred, both a decrease in input of new root material and a dramatic increase of decomposition rates in centuries-old soil C pools were required. Therefore, with future increases in nutrient availability, we may expect substantial losses of C which took centuries to accumulate.", "keywords": ["tundra", "decomposition", "Ecology", "carbon dynamics", "04 agricultural and veterinary sciences", "Biological Sciences", "15. Life on land", "01 natural sciences", "nitrogen", "13. Climate action", "radiocarbon", "0401 agriculture", " forestry", " and fisheries", "phosphorus", "Environmental Sciences", "0105 earth and related environmental sciences"], "contacts": [{"organization": "Nowinski, Nicole S, Trumbore, Susan E, Schuur, Edward AG, Mack, Michelle C, Shaver, Gaius R,", "roles": ["creator"]}]}, "links": [{"href": "https://escholarship.org/content/qt9p9291hz/qt9p9291hz.pdf"}, {"href": "https://doi.org/10.1007/s10021-007-9104-1"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Ecosystems", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s10021-007-9104-1", "name": "item", "description": "10.1007/s10021-007-9104-1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s10021-007-9104-1"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2007-11-17T00:00:00Z"}}, {"id": "10.1007/s10533-015-0157-5", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:14:57Z", "type": "Journal Article", "created": "2015-11-14", "title": "Chronic Nitrogen Fertilization And Carbon Sequestration In Grassland Soils: Evidence Of A Microbial Enzyme Link", "description": "Chronic nitrogen (N) fertilization can greatly affect soil carbon (C) sequestration by altering biochemical interactions between plant detritus and soil microbes. In lignin-rich forest soils, chronic N additions tend to increase soil C content partly by decreasing the activity of lignin-degrading enzymes. In cellulose-rich grassland soils it is not clear whether cellulose-degrading enzymes are also inhibited by N additions and what consequences this might have on changes in soil C content. Here we address whether chronic N fertilization has affected (1) the C content of light versus heavier soil fractions, and (2) the activity of four extracellular enzymes including the C-acquiring enzyme \u03b2-1,4-glucosidase (BG; necessary for cellulose hydrolysis). We found that 19\u00a0years of chronic N-only addition to permanent grassland have significantly increased soil C sequestration in heavy but not in light soil density fractions, and this C accrual was associated with a significant increase (and not decrease) of BG activity. Chronic N fertilization may increase BG activity because greater N availability reduces root C:N ratios thus increasing microbial demand for C, which is met by C inputs from enhanced root C pools in N-only fertilized soils. However, BG activity and total root mass strongly decreased in high pH soils under the application of lime (i.e. CaCO3), which reduced the ability of these organo-mineral soils to gain more C per units of N added. Our study is the first to show a potential \u2018enzyme link\u2019 between (1) long-term additions of inorganic N to grassland soils, and (2) the greater C content of organo-mineral soil fractions. Our new hypothesis is that the \u2018enzyme link\u2019 occurs because (a) BG activity is stimulated by increased microbial C demand relative to N under chronic fertilization, and (b) increased BG activity causes more C from roots and from microbial metabolites to accumulate and stabilize into organo-mineral C fractions. We suggest that any combination of management practices that can influence the BG \u2018enzyme link\u2019 will have far reaching implications for long-term C sequestration in grassland soils.", "keywords": ["DECOMPOSITION", "DYNAMICS", "570", "\u03b2-1", "4-Glucosidase", "/dk/atira/pure/subjectarea/asjc/2300/2304", "NUTRIENT RELEASE", "Environmental Sciences & Ecology", "Root C:N ratio", "Extracellular enzyme activity", "LITTER DECAY", "FOREST ECOSYSTEMS", "0399 Other Chemical Sciences", "0402 Geochemistry", "Environmental Chemistry", "Geosciences", " Multidisciplinary", "beta-1", "4-Glucosidase", "Earth-Surface Processes", "Water Science and Technology", "2. Zero hunger", "Multidisciplinary", "Science & Technology", "/dk/atira/pure/subjectarea/asjc/1900/1904", "Geology", "sequestration", "Agronomy & Agriculture", "04 agricultural and veterinary sciences", "15. Life on land", "Soil carbon", "N DEPOSITION", "ORGANIC-MATTER", "PHOSPHORUS", "Fertilization", "Physical Sciences", "N ratio [Root C]", "0401 agriculture", " forestry", " and fisheries", "Soil carbon sequestration", "Liming", "TURNOVER", "Life Sciences & Biomedicine", "Geosciences", "/dk/atira/pure/subjectarea/asjc/2300/2312", "Environmental Sciences", "RESPONSES"]}, "links": [{"href": "https://doi.org/10.1007/s10533-015-0157-5"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biogeochemistry", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s10533-015-0157-5", "name": "item", "description": "10.1007/s10533-015-0157-5", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s10533-015-0157-5"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2015-11-14T00:00:00Z"}}, {"id": "10.1007/s10533-012-9808-y", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:14:57Z", "type": "Journal Article", "created": "2012-10-31", "title": "Earthworms, Litter And Soil Carbon In A Northern Hardwood Forest", "description": "The important role of soil carbon (C) in the global C cycle has stimulated interest in better understanding the mechanisms regulating soil C storage and its stabilization. Exotic earthworm invasion of northern forest soils in North America can affect soil C pools, and we examined their effects on these mechanisms by adding 13C labeled leaf litter to adjacent northern hardwood forests with and without earthworms. Two types of labeled litter were produced, one with the 13C more concentrated in structural (S) components and the other in non-structural (NS) components, to evaluate the role of biochemical differences in soil C stabilization. Earthworm invasions have reduced soil C storage in the upper 20\u00a0cm of the soil profile by 37\u00a0%, mostly by eliminating surface organic horizons. Despite rapid mixing of litter into mineral soil and its incorporation into aggregates, mineral soil C has not increased in the presence of earthworms. Incorporation of litter C into soil and microbial biomass was not affected by biochemical differences between S versus NS labeled litter although NS litter C was assimilated more readily into earthworm biomass and S litter C into fungal hyphae. Apparently, the net effect of earthworm mixing of litter and forest floor C into mineral soil, plus stabilization of that C in aggregates, is counterbalanced by earthworm bioturbation and possible priming effects. Our results support recent arguments that biochemical recalcitrance is not a major contributor to the stabilization of soil C.", "keywords": ["IMPACTS", "Decomposition", "STABILIZATION", "Multidisciplinary", "biomass", "MICROBIAL BIOMASS", "INVASION", "Microbial biomass", "TEMPERATE", "04 agricultural and veterinary sciences", "SEQUESTRATION", "15. Life on land", "Fungal hyphae", "Aggregation", "Microbial", "Sugar maple", "FORESTS", "DISSOLVED ORGANIC-MATTER", "PATTERNS", "0401 agriculture", " forestry", " and fisheries", "USA", "Environmental Sciences", "Geosciences", "Isotope labeling", "CENTRAL NEW-YORK"]}, "links": [{"href": "https://doi.org/10.1007/s10533-012-9808-y"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biogeochemistry", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s10533-012-9808-y", "name": "item", "description": "10.1007/s10533-012-9808-y", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s10533-012-9808-y"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2012-11-01T00:00:00Z"}}, {"id": "10.1007/s10533-015-0159-3", "type": "Feature", "geometry": null, "properties": {"license": "Closed Access", "updated": "2026-04-04T16:14:57Z", "type": "Journal Article", "created": "2015-12-17", "title": "Mediation Of Soil C Decomposition By Arbuscular Mycorrizhal Fungi In Grass Rhizospheres Under Elevated Co2", "description": "Arbuscular mycorrhizal (AMF) function has mostly been studied from the plant perspective, but there is a shortage of empirical assessments of their ecosystem level impacts on soil carbon (C). Our understanding of the role of AMF on C processing belowground has been restricted mostly to fresh plant residues, not stabilized soil organic matter. The mechanisms by which elevated CO2 (eCO2) alter soil C remain an open question but AMF likely play a role via C and nutrients, which could in turn, be plant species dependent. We assessed AMF as mediators of C processing in the rhizosphere of two grasses under eCO2. We exposed a C4 and a C3 grass to a combination of ambient and eCO2 with and without modification of the AMF communities and using stable isotopes quantified the respiration of native soil C (as rhizosphere priming), its contribution to dissolved and microbial C and the final remaining C pool. The AMF treatment impacted soil C respiration under the C3-plant and only under eCO2. eCO2 suppressed decomposition (negative priming) but this effect disappeared when the AMF community was reduced. In contrast to studies of fresh plant residues suggesting that AMF can enhance C loss, our observations indicate that AMF may promote C storage in the soil organic matter pool. Results support that AMF can mediate the effect of eCO2 on soil C in the rhizosphere of some plant species, a potential mechanism explaining variation in impacts of eCO2 on soil C storage and C balances across species and ecosystems.", "keywords": ["vesicular-arbuscular mycorrhizas", "580", "2. Zero hunger", "grasses", "13. Climate action", "XXXXXX - Unknown", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land", "rhizosphere", "biodegradation"]}, "links": [{"href": "https://doi.org/10.1007/s10533-015-0159-3"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biogeochemistry", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s10533-015-0159-3", "name": "item", "description": "10.1007/s10533-015-0159-3", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s10533-015-0159-3"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2015-12-17T00:00:00Z"}}, {"id": "10.5061/dryad.c2fqz61cf", "type": "Feature", "geometry": null, "properties": {"license": "unspecified", "updated": "2026-04-04T16:21:56Z", "type": "Dataset", "title": "Oxygen availability regulates the quality of soil dissolved organic matter by mediating microbial metabolism and iron oxidation", "description": "Dissolved organic matter (DOM) plays a vital role in biogeochemical processes and in determining the responses of soil organic matter (SOM) to global change. Although the quantity of soil DOM has been inventoried across diverse spatio-temporal scales, the underlying mechanisms accounting for variability in DOM dynamics remain unclear, especially in upland ecosystems. Here, a gradient of SOM storage across twelve croplands in northeast China was used to understand links between DOM dynamics, microbial metabolism, and abiotic conditions. We assessed the composition, biodegradability and key biodegradable components of DOM. In addition, SOM and mineral-associated organic matter (MAOM) composition, soil enzyme activities, oxygen availability, soil texture, iron (Fe), Fe-bound organic matter and nutrient concentrations were quantified to clarify the drivers of DOM quality (composition and biodegradability). The proportion of biodegradable DOM increased exponentially with decreasing initial DOM concentration due to larger fractions of depolymerized DOM that was rich in small-molecular phenols and proteinaceous components. Unexpectedly, the composition of DOM was decoupled from that of SOM or MAOM, but significantly related to enzymatic properties. These results indicate that microbial metabolism exhibited a dominant role in DOM generation. As DOM concentration declined, increased soil oxygen availability regulated DOM composition and enhanced its biodegradability mainly through mediating microbial metabolism and Fe oxidation. The oxygen-induced oxidation of Fe(II) to Fe(III) removed complex DOM compounds with large molecular weight. Moreover, increased oxygen availability stimulated oxidase-catalyzed depolymerization of aromatic substances, and promoted production of protein-like DOM components due to lower enzymatic C/N acquisition ratio. As global changes in temperature and moisture will have large impacts on soil oxygen availability, the role of oxygen in regulating DOM dynamics highlights the importance of integrating soil oxygen supply with microbial metabolism and Fe redox status to improve model predictions of soil carbon under climate change.", "keywords": ["2. Zero hunger", "soil organic carbon", "iron cycling", "13. Climate action", "FOS: Agricultural sciences", "Biodegradation", "oxygen availability", "enzymatic stoichiometry", "15. Life on land", "dissolved organic matter", "6. Clean water"], "contacts": [{"organization": "Li, Ye, Chen, Zengming, Chen, Ji, Castellano, Michael J., Ye, Chenglong, Zhang, Nan, Miao, Yuncai, Zheng, Huijie, Li, Junjie, Ding, Weixin,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5061/dryad.c2fqz61cf"}, {"rel": "self", "type": "application/geo+json", "title": "10.5061/dryad.c2fqz61cf", "name": "item", "description": "10.5061/dryad.c2fqz61cf", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5061/dryad.c2fqz61cf"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-10-23T00:00:00Z"}}, {"id": "10.1016/j.agee.2011.06.015", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:15:33Z", "type": "Journal Article", "created": "2011-07-29", "title": "Short Term Effects Of Bioenergy By-Products On Soil C And N Dynamics, Nutrient Availability And Biochemical Properties", "description": "Abstract The shift towards a biobased economy will probably trigger the application of bioenergy by-products to the soil as either amendments or fertilizers. However, limited research has been done to determine how this will influence C and N dynamics and soil functioning. The aim of this work was to investigate the effects of different bioenergy by-products on C and N mineralisation, nutrient availability and microbial content and activity of amended soil and compare them to other more commonly used organic amendments. Two agricultural soils were amended (0.5% w/w) with four different bioenergy by-products (anaerobic digestate, rapeseed meal, bioethanol residue, biochar) and three other commonly used organic amendments (sewage sludge and two composts) and incubated at 20\u00a0\u00b0C in the laboratory for 30 days. During incubation, soil CO2 and N2O evolution were measured every 4\u00a0h by an automatic chromatographic system. After 2, 7 and 30 days of incubation, soil samples were analysed for K2SO4\u2013extractable C, N, NO3\u2212, NH4+ and P, microbial biomass C and three enzymatic activities (\u03b2-glucosidase, alkaline phosphatase and leucine aminopeptidase). Soil amendment led to a general increase in soil respiration, available N and P and microbial content and activity, but with remarkably different dynamics and values. Particularly, rapeseed meal and the bioethanol by-product led to N2O emissions and the greatest increases in soil respiration, N availability and enzymatic activity compared with the other amendments. The exception was represented by biochar that did not cause any significant variation with respect to the control, but promoted C accumulation. According to their impact on soil biochemical properties, the materials can be ranked as follows: rapeseed meal, bioethanol residue\u00a0>\u00a0anaerobic digestate, sewage sludge\u00a0>\u00a0composts\u00a0>\u00a0biochar. For each measured parameter, soil properties did not affect the response pattern found for the different treatments, but modified the magnitude of the response. In particular, soil respiration and enzymatic activity were higher in the slightly acidic soil, while greater values of available P were found in the alkaline soil. This study clearly indicates that the impact on GHG emissions and soil functioning of bioenergy by-products needs to be taken into account for a correct life cycle assessment of the bioenergy chain. Moreover, when properly managed, they may represent an effective alternative to usual amendments to improve the quality and nutrient balance of amended soils.", "keywords": ["2. Zero hunger", "crop residues", "decomposition", "microbial biomass", "carbon", "enzyme-activities", "04 agricultural and veterinary sciences", "15. Life on land", "composts", "7. Clean energy", "6. Clean water", "12. Responsible consumption", "organic amendments", "13. Climate action", "nitrous-oxide emission", "0401 agriculture", " forestry", " and fisheries", "mineralization", "management"], "contacts": [{"organization": "Galvez, A., Sinicco, T., Cayuela, M.L, Mingorance, M.D., Fornasier, F., Mondini, C.,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1016/j.agee.2011.06.015"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Agriculture%2C%20Ecosystems%20%26amp%3B%20Environment", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.agee.2011.06.015", "name": "item", "description": "10.1016/j.agee.2011.06.015", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.agee.2011.06.015"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2012-10-01T00:00:00Z"}}, {"id": "10.1016/j.agee.2013.10.022", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:15:35Z", "type": "Journal Article", "created": "2013-11-16", "title": "Uncropped Field Margins To Mitigate Soil Carbon Losses In Agricultural Landscapes", "description": "Fil: D'acunto, Luciana. Consejo Nacional de Investigaciones Cientificas y Tecnicas. Oficina de Coordinacion Administrativa Parque Centenario. Instituto de Investigaciones Fisiologicas y Ecologicas Vinculadas a la Agricultura; Argentina", "keywords": ["2. Zero hunger", "0106 biological sciences", "Decomposition", "13. Climate action", "Field Margins", "https://purl.org/becyt/ford/4.1", "0401 agriculture", " forestry", " and fisheries", "Agricultural Intensification", "https://purl.org/becyt/ford/4", "Pampas", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences"], "contacts": [{"organization": "D'acunto, Luciana, Semmartin, Mar\u00eda Gisela, Ghersa, Claudio Marco,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1016/j.agee.2013.10.022"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Agriculture%2C%20Ecosystems%20%26amp%3B%20Environment", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.agee.2013.10.022", "name": "item", "description": "10.1016/j.agee.2013.10.022", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.agee.2013.10.022"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2014-01-01T00:00:00Z"}}, {"id": "10.1016/j.apsoil.2009.03.003", "type": "Feature", "geometry": null, "properties": {"license": "Closed Access", "updated": "2026-04-04T16:15:47Z", "type": "Journal Article", "created": "2009-04-30", "title": "Soil Priming By Sugar And Leaf-Litter Substrates: A Link To Microbial Groups", "description": "The impact of elevated CO2 on leaf-litter and root exudate production may alter soil carbon storage capacities for the future. In particular when so-called \u2018priming effects\u2019, the counterintuitive loss of soil carbon following input of organic carbon substrates, are taken into consideration. Here we investigate the dynamics of priming effects and ask whether the source of primed carbon is microbial biomass or soil organic matter and whether specific microbial groups, as identified by phospholipid fatty acid (PLFA) biomarkers, may be important in causing them. We measured \u03b413C within soil CO2 efflux and PLFA biomarkers following C3 soil priming effects caused by additions of C4 sugar-cane sucrose and maize (Zea mays L.) leaf-litter chopped and ground. All additions caused an initial pulse of priming effect CO2 and a later pulse of substrate-derived CO2, showing that priming effects can be induced rapidly following changes in substrate supply. Priming effects persisted over 32 days and led to a loss of soil carbon, with an increase in soil carbon decomposition of 169% following sucrose addition, 44% following chopped maize and 67% following ground maize additions. An increased concentration of soil-derived carbon within specific PLFA biomarkers provided evidence that a source of the primed carbon was soil organic matter. Certain Gram negative bacteria, identified by PLFA biomarkers (16:1\u03c95, 16:1\u03c97), showed increased uptake of soil carbon for both sucrose and maize treatments and may be directly linked to priming effects. Our study provides evidence that substrate carbon inputs to soil induce rapid changes in specific microbial groups, which in turn increase soil carbon metabolism.", "keywords": ["priming effect", "2. Zero hunger", "decomposition", "leaf-litter", "13. Climate action", "PLFA", "stable isotopes", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "soil carbon", "15. Life on land", "6. Clean water"], "contacts": [{"organization": "Nottingham, Andrew T., Griffiths, Howard, Chamberlain, Paul M., Stott, Andrew W., Tanner, Edmund V. J.,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1016/j.apsoil.2009.03.003"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Applied%20Soil%20Ecology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.apsoil.2009.03.003", "name": "item", "description": "10.1016/j.apsoil.2009.03.003", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.apsoil.2009.03.003"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2009-07-01T00:00:00Z"}}, {"id": "10.1016/j.apsoil.2010.09.006", "type": "Feature", "geometry": null, "properties": {"license": "Closed Access", "updated": "2026-04-04T16:15:47Z", "type": "Journal Article", "created": "2010-10-15", "title": "Is There A Linear Relationship Between Priming Effect Intensity And The Amount Of Organic Matter Input?", "description": "C-labeling abstract Inputs of fresh organic matter (FOM) are known to affect the rate of soil organic matter (SOM) mineral- ization. SOM mineralization can be accelerated or decelerated by FOM inputs. This phenomenon, known as the Priming effect (PE), may largely influence the carbon (C) storage capacity of soils. However, the link between PE intensity and FOM inputs is not clearly understood. Indeed, almost all the studies about PE used only one FOM amount which is generally largely below the amount of FOM observed in field conditions. In our study, we incubated soil amended with three levels of 13 C-labeled straw as FOM and a control without FOM amendment for 80 days. The three levels used were in the same range as the natural FOM inputs observed on our sampling site. Various levels of mineral nitrogen were added within each level of straw supply so that the final input C:N ratios ranged among 44, 30 and 20. CO2 and i 13 C-CO2 were measured during the experiment allowing us to distinguish the FOM respired CO2 from the SOM respired CO2. We observed that PE intensity did not increase linearly with increasing FOM additions. Moreover, decreasing the input C:N ratios did not systematically affect PE intensity probably because of shifts in the microbial characteristics such as their C:N ratio or their assimilation yields. These results suggest that PE is a saturating function of FOM inputs that is only weakly influenced by initial N availability. Our results may be explained (i) by the existence of a limited SOM pool subject to PE (ii) or by the occurrence of two simultaneous and antagonistic mechanisms: an increase of the total active microbial biomass accel- erating SOM mineralization (i.e. a positive PE) and a preferential substrate utilization of FOM over SOM decreasing SOM mineralization (i.e. a negative PE). Finally, irrespective of the mechanisms implied, our results suggest that the importance of positive PE relatively to the amount of FOM may decrease when FOM inputs increase, which is favorable to carbon sequestration in soils. Indeed, in the case of the lower amount of FOM, the PE corresponded to 6.25% of the total amount of CO2 mineralized at the end of the experiment while, for the higher amount of FOM, the PE corresponded to 5% of the total amount of CO2 mineralized at the end of the experiment.", "keywords": ["DECOMPOSITION", "2. Zero hunger", "330", "[SDV]Life Sciences [q-bio]", "Soil organic matter mineralization", "Straw", "(13)C-labeling", "04 agricultural and veterinary sciences", "15. Life on land", "630", "6. Clean water", "MECHANISMS", "GLUCOSE", "CARBON", "SOIL", "NITROGEN", "MODEL", "[SDV] Life Sciences [q-bio]", "Carbon storage", "SUBSTRATE", "0401 agriculture", " forestry", " and fisheries", "Priming effect", "MINERALIZATION", "ROOTS"]}, "links": [{"href": "https://doi.org/10.1016/j.apsoil.2010.09.006"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Applied%20Soil%20Ecology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.apsoil.2010.09.006", "name": "item", "description": "10.1016/j.apsoil.2010.09.006", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.apsoil.2010.09.006"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2010-11-01T00:00:00Z"}}, {"id": "10.1016/j.biortech.2018.04.095", "type": "Feature", "geometry": null, "properties": {"license": "Closed Access", "updated": "2026-04-04T16:15:54Z", "type": "Journal Article", "created": "2018-04-25", "title": "Performance of a biotrickling filter for the anaerobic utilization of gas-phase methanol coupled to thiosulphate reduction and resource recovery through volatile fatty acids production", "description": "The anaerobic removal of continuously fed gas-phase methanol (2.5-30\u202fg/m3.h) and the reduction of step-fed thiosulphate (1000\u202fmg/L) was investigated in a biotrickling filter (BTF) operated for 123\u202fd at an empty bed residence time (EBRT) of 4.6 and 2.3\u202fmin. The BTF performance during steady step-feed and special operational phases like intermittent liquid trickling in 6 and 24\u202fh cycles and operation without pH regulation were evaluated. Performance of the BTF was not affected and nearly 100% removal of gas-phase methanol was achieved with an ECmax of 21\u202fg/m3.h. Besides, >99% thiosulphate reduction was achieved, in all the phases of operation. The production of sulphate, H2S and volatile fatty acids (VFA) was monitored and a maximum of 2500\u202fmg/L of acetate, 200\u202fmg/L of propionate, 150\u202fmg/L of isovalerate and 100\u202fmg/L isobutyrate was produced.", "keywords": ["Biodegradation", " Environmental", "Bioreactors", "Methanol", "Thiosulfates", "0211 other engineering and technologies", "02 engineering and technology", "Fatty Acids", " Volatile", "01 natural sciences", "Filtration", "6. Clean water", "0105 earth and related environmental sciences"], "contacts": [{"organization": "Eregowda, Tejaswini, Matanhike, Luck, Rene, Eldon R., Lens, Piet N.L.,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1016/j.biortech.2018.04.095"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Bioresource%20Technology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.biortech.2018.04.095", "name": "item", "description": "10.1016/j.biortech.2018.04.095", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.biortech.2018.04.095"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-09-01T00:00:00Z"}}, {"id": "10.1016/j.chemosphere.2019.02.158", "type": "Feature", "geometry": null, "properties": {"license": "Closed Access", "updated": "2026-04-04T16:16:00Z", "type": "Journal Article", "created": "2019-02-25", "title": "Bioreduction of selenate in an anaerobic biotrickling filter using methanol as electron donor", "description": "The anaerobic bioreduction of selenate, fed in step (up to 60\u202fmg.L-1) or continuous (\u223c7\u202fmg.L-1) trickling mode, in the presence of gas-phase methanol (4.3-50\u202fg\u202fm-3.h-1) was evaluated in a biotrickling filter (BTF). During the 48\u202fd of step-feed and 41\u202fd of continuous-feed operations, average selenate removal efficiencies (RE)\u202f>\u202f90% and \u223c68% was achieved, corresponding to a selenate reduction rate of, respectively, 7.3 and 4.5\u202fmg.L-1.d-1. During the entire period of BTF operation, 65.6% of the total Se fed as SeO42- was recovered. Concerning gas-phase methanol, the maximum elimination capacity (ECmax) was 46.4\u202fg\u202fm-3.h-1, with a RE\u202f>\u202f80%. Methanol was mainly utilized for acetogenesis and converted to volatile fatty acids (VFA) in the liquid-phase. Up to 5000\u202fmg.L-1 of methanol and 800\u202fmg.L-1 of acetate accumulated in the trickling liquid of the BTF.", "keywords": ["Bacteria", "Sewage", "Methanol", "0211 other engineering and technologies", "02 engineering and technology", "Selenic Acid", "Fatty Acids", " Volatile", "Archaea", "01 natural sciences", "6. Clean water", "Biodegradation", " Environmental", "Bioreactors", "Oxidation-Reduction", "Filtration", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.chemosphere.2019.02.158"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Chemosphere", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.chemosphere.2019.02.158", "name": "item", "description": "10.1016/j.chemosphere.2019.02.158", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.chemosphere.2019.02.158"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-06-01T00:00:00Z"}}, {"id": "10.1016/j.earscirev.2018.05.017", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:16:03Z", "type": "Journal Article", "created": "2018-06-02", "title": "Advances in the determination of humification degree in peat since : Applications in geochemical and paleoenvironmental studies", "description": "Peer reviewed", "keywords": ["2. Zero hunger", "Decomposition", "Organic matter decay", "13. Climate action", "Bog", "Bogs; C cycle; Decomposition; H/C; Organic matter decay; Earth and Planetary Sciences (all)", "H/C", "C cycle; Decomposition; Organic matter decay; Bogs", " H/C", "C cycle", "15. Life on land", "Earth and Planetary Sciences (all)", "01 natural sciences", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://cris.unibo.it/bitstream/11585/690169/5/POSTPRINT%20690169.pdf"}, {"href": "https://doi.org/10.1016/j.earscirev.2018.05.017"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Earth-Science%20Reviews", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.earscirev.2018.05.017", "name": "item", "description": "10.1016/j.earscirev.2018.05.017", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.earscirev.2018.05.017"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-10-01T00:00:00Z"}}, {"id": "10.1016/j.eja.2013.02.005", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:16:07Z", "type": "Journal Article", "created": "2013-03-16", "title": "Managing Tephrosia Mulch And Fertilizer To Enhance Coffee Productivity On Smallholder Farms In The Eastern African Highlands", "description": "Abstract In Maraba, Southwest Rwanda, coffee productivity is constrained by poor soil fertility and lack of organic mulch. We investigated the potential to produce mulch by growing Tephrosia vogelii either intercropped with smallholder coffee or in arable fields outside the coffee, and the effect of the mulch on coffee yields over two years. Two accessions of T. vogelii (ex. Gisagara, Rwanda and ex. Kisumu, Kenya) were grown for six months both within and outside smallholder coffee fields in the first year. Experimental blocks were replicated across eight smallholder farms, only a single replicate per farm due to the small farm sizes. The accession from Rwanda (T. vogelii ex. Gisagara) grew more vigorously in all experiments. Soils within the coffee fields were more fertile those outside the coffee fields, presumably due to farmers\u2019 long-term management with mulch. Tephrosia grew less well in the fields outside coffee, producing only 0.6\u20130.7\u00a0Mg\u00a0ha\u22121 of biomass and adding (in kg\u00a0ha\u22121) 19 N, 1 P and 6 K in the mulch. By contrast, Tephrosia intercropped with coffee, produced 1.4\u20131.9\u00a0Mg\u00a0ha\u22121 of biomass and added (in kg\u00a0ha\u22121) 42\u201357 N, 3 P and 13\u201316 K in the mulch. Coffee yields were increased significantly by 400\u2013500\u00a0kg\u00a0ha\u22121 only in the treatments where Tephrosia was intercropped with coffee. Soil analysis and a missing-nutrient pot experiment showed that the poor growth of Tephrosia in the fields outside coffee was due to soil acidity (aluminium toxicity) combined with deficiencies of P, K and Ca. In the second year, the treatments in fields outside coffee were discontinued, and in the coffee intercrops, two Tephrosia accessions were grown in treatments with and without NPK fertilizer. Tephrosia grew well and produced between 2.5 and 3.8\u00a0Mg\u00a0ha\u22121 biomass for the two accessions when interplanted within coffee fields, adding 103\u2013150\u00a0kg\u00a0N\u00a0ha\u22121, 5\u20139\u00a0kg\u00a0P\u00a0ha\u22121 and 24\u201338\u00a0kg\u00a0K\u00a0ha\u22121. Tephrosia mulch increased yields of coffee by 400\u00a0kg\u00a0ha\u22121. Combined use of NPK\u00a0+\u00a0Tephrosia mulch increased Tephrosia biomass production and in turn yielded an additional 300\u2013700\u00a0kg\u00a0ha\u22121 of coffee. Over the two years, this was equivalent to a 23\u201336% increase in coffee yield using Tephrosia intercropping alone and a further 25\u201342% increase in coffee yield when NPK fertilizer was also added. Agronomic efficiency (AE) of nutrients added were 30% greater when the Tephrosia mulch was grown in situ and the two cultivars of Tephrosia did not differ in AE. The AE of Tephrosia mulch was 87% that of NPK fertilizer, reflecting the rapid mineralization of Tephrosia mulch. There was a synergistic effect of Tephrosia mulch on the efficiency with which NPK fertilizer was used by coffee. The increase in coffee yields was positively related to the amount of nutrients added in the Tephrosia biomass. Tephrosia intercropping required 30 man-days\u00a0ha\u22121 less than current farmer management due to reduced labour required for weeding, and benefit\u2013cost ratios ranged between 3.4 and 5.5. The Tephrosia-coffee intercropping system offers great potential for agroecological intensification for smallholder farmers in the East African highlands.", "keywords": ["2. Zero hunger", "decomposition", "variability", "tephrosia", "coffee", "nitrogen release", "western kenya", "resource-allocation", "cropping systems", "04 agricultural and veterinary sciences", "smallholder farmer", "15. Life on land", "improved fallows", "bukoba district", "0401 agriculture", " forestry", " and fisheries", "cover crops", "intercropping", "management"]}, "links": [{"href": "https://doi.org/10.1016/j.eja.2013.02.005"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/European%20Journal%20of%20Agronomy", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.eja.2013.02.005", "name": "item", "description": "10.1016/j.eja.2013.02.005", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.eja.2013.02.005"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2013-07-01T00:00:00Z"}}, {"id": "10.1890/08-0172.1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:20:19Z", "type": "Journal Article", "created": "2009-09-17", "title": "Effects Of Warming And Altered Precipitation On Plant And Nutrient Dynamics Of A New England Salt Marsh", "description": "Salt marsh structure and function, and consequently ability to support a range of species and to provide ecosystem services, may be affected by climate change. To better understand how salt marshes will respond to warming and associated shifts in precipitation, we conducted a manipulative experiment in a tidal salt marsh in Massachusetts, USA. We exposed two plant communities (one dominated by Spartina patens\uffe2\uff80\uff93Distichlis spicata and one dominated by short form Spartina alterniflora) to five climate manipulations: warming via passive open\uffe2\uff80\uff90topped chambers, doubled precipitation, warming and doubled precipitation, extreme drought via rainout shelter, and ambient conditions. Modest daytime warming increased total aboveground biomass of the S. alterniflora community (24%), but not the S. patens\uffe2\uff80\uff93D. spicata community. Warming also increased maximum stem heights of S. alterniflora (8%), S. patens (8%), and D. spicata (15%). Decomposition was marginally accelerated by warming in the S. alterniflora community. Drought markedly increased total biomass of the S. alterniflora community (53%) and live S. patens (69%), perhaps by alleviating waterlogging of sediments. Decomposition was accelerated by increased precipitation and slowed by drought, particularly in the S. patens\uffe2\uff80\uff93D. spicata community. Flowering phenology responded minimally to the treatments, and pore water salinity, sulfide, ammonium, and phosphate concentrations showed no treatment effects in either plant community. Our results suggest that these salt marsh communities may be resilient to modest amounts of warming and large changes in precipitation. If production increases under climate change, marshes will have a greater ability to keep pace with sea\uffe2\uff80\uff90level rise, although an increase in decomposition could offset this. As long as marshes are not inundated by flooding due to sea\uffe2\uff80\uff90level rise, increases in aboveground biomass and stem heights suggest that marshes may continue to export carbon and nutrients to coastal waters and may be able to increase their carbon storage capability by increasing plant growth under future climate conditions.
", "keywords": ["Greenhouse Effect", "0106 biological sciences", "570", "Spartina patens", "Time Factors", "open-topped chamber", "Light", "Rain", "Plant Development", "Distichlis spicata", "Sodium Chloride", "01 natural sciences", "Spartina alterniflora", "Distichlis spicata;", "Spartina alterniflora;", "0105 earth and related environmental sciences", "2. Zero hunger", "decomposition", "Temperature", "Water", "nutrient cycling", "15. Life on land", "6. Clean water", "Circadian Rhythm", "salt marsh", "climate change", "Massachusetts", "13. Climate action", "Wetlands", "altered precipitation", "ecosystem services"]}, "links": [{"href": "https://doi.org/10.1890/08-0172.1"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Ecological%20Applications", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1890/08-0172.1", "name": "item", "description": "10.1890/08-0172.1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1890/08-0172.1"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2009-10-01T00:00:00Z"}}, {"id": "10.1016/j.fcr.2012.07.014", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:16:17Z", "type": "Journal Article", "created": "2012-08-09", "title": "Maize\u2013Grain Legume Intercropping Is An Attractive Option For Ecological Intensification That Reduces Climatic Risk For Smallholder Farmers In Central Mozambique", "description": "Abstract Many farmers in central Mozambique intercrop maize with grain legumes as a means to improve food security and income. The objective of this study was to understand the farming system, and to evaluate the suitability of maize\u2013legume intercropping to alleviate the biophysical and socio-economic constraints faced by smallholder farmers in Ruaca and Vunduzi villages, central Mozambique. To achieve this we characterised the farming systems and measured grain yields, rainfall infiltration, economic returns and acceptability of maize\u2013legume intercrops under different N and P application rates. Two intercropping strategies were tested: (a) an additive design of within-row intercropping in which legume was intercropped with alternating hills of maize within the same row; maize plant population was the same as sole crop maize, and (b) a substitutive design with distinct alternating rows of maize and legume (local practice). Fertiliser treatments imposed on all treatments were: (i) no fertiliser, (ii) 20\u00a0kg\u00a0P\u00a0ha \u22121 , (iii) 20\u00a0kg\u00a0P\u00a0ha \u22121 \u00a0+\u00a030\u00a0kg\u00a0N\u00a0ha \u22121 , and (iv) 20\u00a0kg\u00a0P\u00a0ha \u22121 \u00a0+\u00a060\u00a0kg\u00a0N\u00a0ha \u22121 . Intercrops were relatively more productive than the corresponding sole crops; land equivalent ratios (LER) for within-row intercropping ranged between 1.1 and 2.4, and between 1.0 and 1.9 for distinct-row intercropping. Average maize yield penalty for intercropping maize and pigeonpea in the within-row was small (8%) compared with 50% in the distinct-row design; average (season\u00a0\u00d7\u00a0fertiliser) sole maize yield was 3.2\u00a0t\u00a0ha \u22121 . Intercropping maize and cowpea in within-row led to maize yield loss of only 6%, whereas distinct-row intercropping reduced maize yield by 25% from 2.1\u00a0t\u00a0ha \u22121 of sole maize (season\u00a0\u00d7\u00a0fertiliser). Cowpea yield was less affected by intercropping: sole cowpea had an average yield of 0.9\u00a0t\u00a0ha \u22121 , distinct-row intercropping (0.8\u00a0t\u00a0ha \u22121 ) and the within-row intercropping yielded 0.9\u00a0t\u00a0ha \u22121 . Legumes were comparatively less affected by the long dry spells which were prevalent during the study period. Response to N and P fertiliser was weak due to poor rainfall distribution. In the third season, maize in rotation with pigeonpea and without N fertiliser application yielded 5.6\u00a0t\u00a0ha \u22121 , eight times more than continuous maize which was severely infested by striga ( Striga asiatica ) and yielded only 0.7\u00a0t\u00a0ha \u22121 . Rainfall infiltration increased from 6\u00a0mm\u00a0h \u22121 to 22\u00a0mm\u00a0h \u22121 with long-term maize\u2013legume intercropping due to a combination of good quality biomass production which provided mulch combined with no tillage. Intercropping maize and pigeonpea was profitable with a rate of return of at least 343% over sole maize cropping. Farmers preferred the within-row maize\u2013legume intercropping with an acceptability score of 84% because of good yields for both maize and legume. Intercropping increased the labour required for weeding by 36% compared with the sole crops. Farmers in Ruaca faced labour constraints due to extensification thus maize\u2013pigeonpea intercropping may improve productivity and help reduce the area cultivated. In Vunduzi, land limitation was a major problem and intensification through legumes is amongst the few feasible options to increase both production and productivity. The late maturity of pigeonpea means that free-grazing of cattle has to be delayed, which allows farmers to retain crop residues in the fields as mulch if they choose to; this allows the use of no-tillage practises. We conclude that maize\u2013legume intercropping has potential to: (a) reduce the risk of crop failure, (b) improve productivity and income, and (c) increase food security in vulnerable production systems, and is a feasible entry point to ecological intensification.", "keywords": ["0106 biological sciences", "F08 - Syst\u00e8mes et modes de culture", "rendement des cultures", "agro\u00e9cologie", "petite exploitation agricole", "extensification", "nitrogen-fixation", "01 natural sciences", "7. Clean energy", "630", "analyse \u00e9conomique", "l\u00e9gume sec", "http://aims.fao.org/aos/agrovoc/c_6214", "striga", "syst\u00e8me de culture", "intensification", "2. Zero hunger", "http://aims.fao.org/aos/agrovoc/c_10967", "soil fertility", "1. No poverty", "facteur climatique", "04 agricultural and veterinary sciences", "Sorghum bicolor", "resource capture", "http://aims.fao.org/aos/agrovoc/c_92381", "rentabilit\u00e9", "conservation agriculture", "http://aims.fao.org/aos/agrovoc/c_8504", "s\u00e9curit\u00e9 alimentaire", "http://aims.fao.org/aos/agrovoc/c_13199", "E16 - \u00c9conomie de la production", "Vigna unguiculata", "crop-rotation", "http://aims.fao.org/aos/agrovoc/c_29554", "Cenchrus americanus", "Zea mays", "http://aims.fao.org/aos/agrovoc/c_7247", "http://aims.fao.org/aos/agrovoc/c_10176", "Life Science", "decomposition", "15. Life on land", "yield", "Maize", "cowpea", "http://aims.fao.org/aos/agrovoc/c_3351", "http://aims.fao.org/aos/agrovoc/c_33484", "http://aims.fao.org/aos/agrovoc/c_33485", "systems", "http://aims.fao.org/aos/agrovoc/c_3910", "0401 agriculture", " forestry", " and fisheries", "http://aims.fao.org/aos/agrovoc/c_2469", "culture intercalaire", "http://aims.fao.org/aos/agrovoc/c_1971", "http://aims.fao.org/aos/agrovoc/c_4964", "http://aims.fao.org/aos/agrovoc/c_8247", "http://aims.fao.org/aos/agrovoc/c_7113"]}, "links": [{"href": "https://doi.org/10.1016/j.fcr.2012.07.014"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Field%20Crops%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.fcr.2012.07.014", "name": "item", "description": "10.1016/j.fcr.2012.07.014", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.fcr.2012.07.014"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2012-09-01T00:00:00Z"}}, {"id": "10.1016/j.foreco.2005.05.030", "type": "Feature", "geometry": null, "properties": {"license": "Closed Access", "updated": "2026-04-04T16:16:21Z", "type": "Journal Article", "created": "2005-06-28", "title": "Carbon And Nitrogen Pools In Chinese Fir And Evergreen Broadleaved Forests And Changes Associated With Felling And Burning In Mid-Subtropical China", "description": "Abstract A Chinese fir forest ( Cunninghamia lanceolata , CL) and a secondary evergreen broadleaved forest (BF) located in Fujian Province, south-eastern China, were examined before clear-cutting to compare their ecosystem carbon and nitrogen pools (above- and below-ground tree, understorey vegetation and forest floor biomass\u00a0+\u00a00\u2013100\u00a0cm mineral soil layer). The ecosystem pools of C and N in the CL before clear-cutting were 257\u00a0Mg\u00a0ha \u22121 and 8605\u00a0kg\u00a0ha \u22121 , respectively. The corresponding values for the BF were 336\u00a0Mg\u00a0ha \u22121 of C and 10,248\u00a0kg\u00a0ha \u22121 of N. For the two forests, most of the C was in the trees, whereas most of the N pool was in the soil. C and N pools in understorey vegetation and forest floor were small in the two forests (about 2% of ecosystem pools). During clear-cutting, 117\u00a0Mg\u00a0ha \u22121 \u00a0C and 307\u00a0kg\u00a0ha \u22121 \u00a0N in stem wood with bark and coarse branches (>2\u00a0cm) were removed from the CL compared to 159\u00a0Mg\u00a0ha \u22121 \u00a0C and 741\u00a0kg\u00a0ha \u22121 \u00a0N from the BF. Two days after slash burning, C removal from logging residues (including forest floor material) was estimated at 10\u00a0Mg\u00a0ha \u22121 for CL and 23\u00a0Mg\u00a0ha \u22121 for BF, and N removal was 233 and 490\u00a0kg\u00a0ha \u22121 in the CL and BF, respectively. Compared with the pre-burn levels in the CL, contents of topsoil organic C and total N 2 days after burning were reduced by 17 and 19%, respectively. In the BF, the corresponding proportions were 27% (C) and 25% (N). Our results indicate that clear-cutting and slash burning had caused marked short-term changes in ecosystem C and N in the two forests. How long these changes will persist needs further study.", "keywords": ["NATURAL FOREST", "DECOMPOSITION", "DYNAMICS", "0106 biological sciences", "15. Life on land", "01 natural sciences", "333", "TREE PLANTATIONS", "CHEMISTRY", "ECOSYSTEMS", "MANAGEMENT", "MIXED FOREST", "SOIL CARBON", "STORAGE"]}, "links": [{"href": "https://doi.org/10.1016/j.foreco.2005.05.030"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Forest%20Ecology%20and%20Management", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.foreco.2005.05.030", "name": "item", "description": "10.1016/j.foreco.2005.05.030", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.foreco.2005.05.030"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2005-09-01T00:00:00Z"}}, {"id": "10.1016/j.foreco.2008.05.007", "type": "Feature", "geometry": null, "properties": {"license": "Restricted", "updated": "2026-04-04T16:16:23Z", "type": "Journal Article", "created": "2008-06-19", "title": "Effect Of Tree Species On Carbon Stocks In Forest Floor And Mineral Soil And Implications For Soil Carbon Inventories", "description": "Forest soil organic carbon (SOC) and forest floor carbon (FFC) stocks are highly variable. The sampling effort required to assess SOC and FFC stocks is therefore large, resulting in limited sampling and poor estimates of the size, spatial distribution, and changes in SOC and FFC stocks in many countries. Forest SOC and FFC stocks are influenced by tree species. Therefore, quantification of the effect of tree species on carbon stocks combined with spatial information on tree species distribution could improve insight into the spatial distribution of forest carbon stocks. We present a study on the effect of tree species on FFC and SOC stock for a forest in the Netherlands and evaluate how this information could be used for inventory improvement. We assessed FFC and SOC stocks in stands of beech (Fagus sylvatica), Douglas fir (Pseudotsuga menziesii), Scots pine (Pinus sylvestris), oak (Quercus robur) and larch (Larix kaempferi). FFC and SOC stocks differed between a number of species. FFC stocks varied between 11.1 Mg C ha-1 (beech) and 29.6 Mg C ha-1 (larch). SOC stocks varied between 53.3 Mg C ha-1 (beech) and 97.1 Mg C ha-1 (larch). At managed locations, carbon stocks were lower than at unmanaged locations. The Dutch carbon inventory currently overestimates FFC stocks. Differences in carbon stocks between conifer and broadleaf forests were significant enough to consider them relevant for the Dutch system for carbon inventory.
", "keywords": ["0106 biological sciences", "land-use history", "01 natural sciences", "mitigation", "greenhouse gases", "Carbon stock", "Forest floor", "forest ecology", "SDG 15 - Life on Land", "forests", "decomposition", "species composition", "transformation", "carbon dioxide", "belgium", "04 agricultural and veterinary sciences", "15. Life on land", "Management", "impact", "0401 agriculture", " forestry", " and fisheries", "spatial variability", "europe", "Mineral soil", "management", "pine", "Tree species"]}, "links": [{"href": "https://doi.org/10.1016/j.foreco.2008.05.007"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Forest%20Ecology%20and%20Management", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.foreco.2008.05.007", "name": "item", "description": "10.1016/j.foreco.2008.05.007", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.foreco.2008.05.007"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2008-07-01T00:00:00Z"}}, {"id": "10.1016/j.geoderma.2004.02.014", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:16:29Z", "type": "Journal Article", "created": "2004-04-10", "title": "Conversion Of Grassy Cerrado Into Riparian Forest And Its Impact On Soil Organic Matter Dynamics In An Oxisol From Southeast Brazil", "description": "Abstract The purpose of this study was to evaluate possible changes in soil organic matter (SOM) dynamics after establishing riparian forests on soils previously under Brazilian savannah (\u201ccerrado\u201d). We selected a site with a homogeneous Typic Acric Red\u2013Yellow Latosol (Anionic Acrustox). Part of this site was maintained under native vegetation (grassy cerrado C 4 -dominated), and part was planted with riparian species (C 3 ) in 1992. Litter and soil samples were collected and analysed (total organic carbon, total nitrogen, \u03b4 13 C isotopic analysis, and SOM density fractionation). Due to the predominance of grasses, carbon input was mainly below ground in cerrado. In such a soil, the decomposition process was more efficient, and much C and N were transferred to the heavy fraction. When forest was planted, there was a change from belowground to aboveground litter input (largely superficial), leading to higher C and N stocks in the light and lower stocks in the heavy fraction (resulting in lower stocks for bulk soil). The introduction of the C 3 vegetation decreased the soil \u03b4 13 C signature. It has occurred particularly in the topsoil (0\u20135 cm) due to the deposition of C 3 litter on the soil surface. At the same time, the presence of cerrado-remaining C below 5 cm maintained higher \u03b4 13 C values in this layer. During the 8 years after forest plantation, the input mode influenced both the \u03b4 13 C distribution with depth, and the C replacement: between 0 and 2.5 cm, nearly 50% of cerrado-derived C was replaced by forest-derived C, while below 5 cm, replacement was around 20%. The relatively rapid C dynamics in this Oxisol (27% replacement in the top 20 cm after 8 years of forest plantation) shows that, under tropical conditions, significant changes may occur in a short period of time.", "keywords": ["delta-c-13", "decomposition", "c-13 natural-abundance", "particle-size fractions", "turnover", "0401 agriculture", " forestry", " and fisheries", "vegetation changes", "04 agricultural and veterinary sciences", "15. Life on land", "stable carbon isotope", "density fractions", "ratios", "nitrogen"], "contacts": [{"organization": "de Alcantara, F.A., Buurman, P., Furtini Neto, A.E., Curi, N., Roscoe, R.,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1016/j.geoderma.2004.02.014"}, {"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.2004.02.014", "name": "item", "description": "10.1016/j.geoderma.2004.02.014", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.geoderma.2004.02.014"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2004-12-01T00:00:00Z"}}, {"id": "10.1016/j.geoderma.2019.114009", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:16:34Z", "type": "Journal Article", "created": "2019-11-12", "title": "Predicting glyphosate sorption across New Zealand pastoral soils using basic soil properties or Vis\u2013NIR spectroscopy", "description": "Glyphosate [N-(phosphonomethyl) glycine] is the active ingredient in Roundup, which is the most used herbicide around the world. It is a non-selective herbicide with carboxyl, amino, and phosphonate functional groups, and it has a strong affinity to the soil mineral fraction. Sorption plays a major role for the fate and transport of glyphosate in the environment. The sorption coefficient (Kd) of glyphosate, and hence its mobility, varies greatly among different soil types. Determining Kd is laborious and requires the use of wet chemistry. In this study, we aimed to estimate Kd using basic soil properties, and visible near-infrared spectroscopy (vis\u2013NIRS). The latter method is fast, requires no chemicals, and several soil properties can be estimated from the same spectrum. The data set included 68 topsoil samples collected across the South Island of New Zealand, with clay and organic carbon (OC) contents ranging from 0.001 to 0.520 kg kg\u22121 and 0.021 to 0.217 kg kg\u22121, respectively. The Kd was determined with batch equilibration sorption experiments and ranged from 13 to 3810 L kg\u22121. The visible near-infrared spectra were obtained from 400 to 2500 nm. Multiple linear regression was used to correlate Kd to oxalate extractable aluminium and phosphorous and pH, which resulted in an R2 of 0.89 and an RMSE of 259.59 L kg\u22121. Further, interval partial least squares regression with ten-fold cross-validation was used to predict Kd by vis\u2013NIRS, and an R2 of 0.93 and an RMSECV of 207.58 L kg\u22121 were obtained. Thus, these results show that both basic soil properties and vis\u2013NIRS can predict the variation in Kd across these samples with high accuracy and hence, that glyphosate sorption to a soil can be determined with vis\u2013NIRS.
", "keywords": ["2. Zero hunger", "ADSORPTION", "NEAR-INFRARED SPECTROSCOPY", "04 agricultural and veterinary sciences", "DEGRADATION", "15. Life on land", "WATER REPELLENCY", "FIELD-SCALE", "REFLECTANCE SPECTROSCOPY", "MOBILITY", "FACILITATED TRANSPORT", "CONTAMINANTS", "0401 agriculture", " forestry", " and fisheries", "COEFFICIENT"]}, "links": [{"href": "https://doi.org/10.1016/j.geoderma.2019.114009"}, {"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.2019.114009", "name": "item", "description": "10.1016/j.geoderma.2019.114009", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.geoderma.2019.114009"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-02-01T00:00:00Z"}}, {"id": "10.1016/j.geoderma.2015.03.024", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:16:33Z", "type": "Journal Article", "created": "2015-04-08", "title": "Decomposition Of Beech (Fagus Sylvatica) And Pine (Pinus Nigra) Litter Along An Alpine Elevation Gradient: Decay And Nutrient Release", "description": "Litter decomposition is an important process for cycling of nutrients in terrestrial ecosystems. The objective of this study was to evaluate direct and indirect effects of climate on litter decomposition along an altitudinal gradient in a temperate Alpine region. Foliar litter of European beech (Fagus sylvatica) and Black pine (Pinus nigra) was incubated in litterbags during two years in the Hochschwab massif of the Northern Limestone Alps of Austria. Eight incubation sites were selected following an altitudinal/climatic transect from 1900 to 900\u00a0m\u00a0asl. The average remaining mass after two years of decomposition amounted to 54% (beech) and 50% (pine). Net release of N, P, Na, Al, Fe and Mn was higher in pine than in beech litter due to high immobilization (retention) rates of beech litter. However, pine litter retained more Ca than beech litter. Altitude retarded decay (mass loss and associated C release) in beech litter during the first year only but had a longer lasting effect on decaying pine litter. Altitude comprises a suite of highly auto-correlated characteristics (climate, vegetation, litter, soil chemistry, soil microbiology, snow cover) that influence litter decomposition. Hence, decay and nutrient release of incubated litter is difficult to predict by altitude, except during the early stage of decomposition, which seemed to be controlled by climate. Reciprocal litter transplant along the elevation gradient yielded even relatively higher decay of pine litter on beech forest sites after a two-year adaptation period of the microbial community.", "keywords": ["Pinus nigra", "0106 biological sciences", "Decomposition", "Fagus sylvatica", "Soil Science", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "Article", "Climosequence", "13. Climate action", "Elevation gradient", "0401 agriculture", " forestry", " and fisheries", "Litterbag"]}, "links": [{"href": "https://doi.org/10.1016/j.geoderma.2015.03.024"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Geoderma", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.geoderma.2015.03.024", "name": "item", "description": "10.1016/j.geoderma.2015.03.024", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.geoderma.2015.03.024"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2015-08-01T00:00:00Z"}}, {"id": "10.1016/j.geoderma.2016.02.010", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:16:34Z", "type": "Journal Article", "created": "2016-02-19", "title": "Potential Of Grassland Rehabilitation Through High Density-Short Duration Grazing To Sequester Atmospheric Carbon", "description": "According to the World Resources Institute (2000), a relative increase of carbon (C) stocks in world soils by 0.4% per year would be sufficient to compensate all anthropogenic greenhouse gas emissions. Several land management practices such as the suppression of tillage in agroecosystems and livestock exclusion in grasslands had initially been thought to store more carbon into the soil, but recent research puts this into question. In a context where finding effective C sequestration methods is urgent, the main objective of this study was to assess the ability of an innovative grassland management practice based on high density and short duration (HDSD) grazing to sequester atmospheric C into soils. The study was performed in a degraded communal rangeland in South Africa where soil organic C (SOC) depletion ranged from 5 to 95% depending on the degradation level, which varied from non-degraded (ND; with grass above ground coverage, Cov of 100%), degraded (D1; 50 < Cov < 75%), D2 (25 < Cov < 50%) and HD (highly degraded: Cov < 5%). The ability of HDSD (1200 cows ha\u2212 1 for 3 days a year) to replenish SOC stocks was compared to four commonly used strategies: (1) livestock exclosure (E); (2) livestock exclosure with topsoil tillage (ET); (3) livestock exclosure with NPK fertilization (2:3:3, 22 at 0.2 t ha\u2212 1) (EF); (4) annual burning (AB); all treatments being compared to traditional free grazing control. A total of 540 soil samples were collected in the 0\u20130.05 m soil layer for all treatments and degradation intensities. After two years, topsoil SOC stocks were significantly increased under EF and HDSD, by an average of 33.4 \u00b1 0.5 and 12.4 \u00b1 2.1 g C m2 y\u2212 1, respectively. In contrast, AB reduced SOC stocks by 3.6 \u00b1 3.0 g C m2 y\u2212 1, while the impact of E and ET was not significant at P < 0.05. HDSD replenished SOC stocks the most at D1 and D2 (6.7 and 7.4% y\u2212 1) and this was explained by grass recovery, i.e. a significant increase in soil surface coverage by grass and grass production. HDSD is cost-effective, and thus has great potential to be widely adopted by smallholder farmers.", "keywords": ["2. Zero hunger", "[PHYS.PHYS.PHYS-GEO-PH] Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]", "Rehabilitation", "Sequestration", "[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]", "04 agricultural and veterinary sciences", "15. Life on land", "Grassland", "01 natural sciences", "630", "Degradation", "Grazing", "13. Climate action", "Others", "Climate change", "0401 agriculture", " forestry", " and fisheries", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.geoderma.2016.02.010"}, {"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.2016.02.010", "name": "item", "description": "10.1016/j.geoderma.2016.02.010", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.geoderma.2016.02.010"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2016-06-01T00:00:00Z"}}, {"id": "10.1016/j.jcs.2019.102829", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:16:42Z", "type": "Journal Article", "created": "2019-09-06", "title": "Morpho-densitometric traits for quinoa (Chenopodium quinoa Willd.) seed phenotyping by two X-ray micro-CT scanning approaches", "description": "Recent studies are increasingly focusing on quinoa (Chenopodium quinoa) as a high-quality protein-rich food source and, in general, on seed quality. This latter is a complex trait difficult to characterize with standard measurements or analyses. X-ray micro-CT allows to visualise the internal structure of small objects and has been already used in seed research, mostly for maize kernel characterization. To date this technique has not yet been applied to study quinoa seeds, despite the increasing interest for their nutritional properties. The aim of this work was to explore the use of X-ray microtomography to provide new traits improving the seed phenotyping of quinoa. Two different scanning approaches have been compared: one based on the simultaneous scanning of multiple seeds (30) at lower resolution (20 ?m voxel size) and one based on the scanning of a single seed at higher resolution (2 ?m voxel size). Such approaches were tested on a study case consisting of four different quinoa genotypes. Among the measured morpho-densitometric parameters, the embryo volume and weight ratios (derived from bulk and single seed scanning, respectively) showed high positive correlation with the total protein content, while the thickest fraction of the pericarp was the best correlated with the presence of saponins.", "keywords": ["Fitomejoramiento", "2. Zero hunger", "0301 basic medicine", "0303 health sciences", "Evaluaci\u00f3n", "Rayos-X", "Seed quality", "Semillas", "Variaci\u00f3n gen\u00e9tica", "Quinua", "Per\u00fa", "03 medical and health sciences", "https://purl.org/pe-repo/ocde/ford#2.11.01", "Quinoa", "Radiaci\u00f3n", "3D image analysis", "X-ray micro-CT", "Chenopodium quinoa", "Fenotipos"]}, "links": [{"href": "https://iris.cnr.it/bitstream/20.500.14243/386031/1/prod_406462-doc_142170.pdf"}, {"href": "https://iris.cnr.it/bitstream/20.500.14243/386031/2/prod_406462-doc_142171.pdf"}, {"href": "https://iris.cnr.it/bitstream/20.500.14243/386031/4/prod_406462-doc_147996.pdf"}, {"href": "https://doi.org/10.1016/j.jcs.2019.102829"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Cereal%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.jcs.2019.102829", "name": "item", "description": "10.1016/j.jcs.2019.102829", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.jcs.2019.102829"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-11-01T00:00:00Z"}}, {"id": "10.1016/j.jhazmat.2018.12.062", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:16:45Z", "type": "Journal Article", "created": "2018-12-18", "title": "H2S removal and microbial community composition in an anoxic biotrickling filter under autotrophic and mixotrophic conditions", "description": "Removal of H2S from gas streams using NO3--containing synthetic wastewater was investigated in an anoxic biotrickling filter (BTF) at feed N/S ratios of 1.2-1.7\u2009mol mol-1 with an empty bed residence time of 3.5\u2009min and a hydraulic retention time of 115\u2009min. During 108 days of operation under autotrophic conditions, the BTF showed a maximum elimination capacity (EC) of 19.2\u2009g S m-3\u2009h-1 and H2S removal efficiency (RE) >99%. When the BTF was operated under mixotrophic conditions by adding organic carbon (10.2\u2009g acetate m-3\u2009h-1) to the synthetic wastewater, the H2S EC decreased from 16.4 to 13.1\u2009g S m-3\u2009h-1, while the NO3- EC increased from 9.9 to 11.1\u2009g NO3--N m-3\u2009h-1, respectively. Thiobacillus sp. (98-100% similarity) was the only sulfur-oxidizing nitrate-reducing bacterium detected in the BTF biofilm, while the increased abundance of heterotrophic denitrifiers, i.e. Brevundimonas sp. and Rhodocyclales, increased the N/S ratio during BTF operation. Residence time distribution tests showed that biomass accumulation during BTF operation reduced gas and liquid retention times by 17.1% and 83.5%, respectively.", "keywords": ["570", "Air Pollutants", "Nitrates", "550", "Bacteria", "Microbiota", "116 Chemical sciences", "116", "Waste Disposal", " Fluid", "01 natural sciences", "6. Clean water", "Bioreactors", "Denitrification", "Hydrogen Sulfide", "Filtration", "Water Pollutants", " Chemical", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.jhazmat.2018.12.062"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Hazardous%20Materials", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.jhazmat.2018.12.062", "name": "item", "description": "10.1016/j.jhazmat.2018.12.062", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.jhazmat.2018.12.062"}, {"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": "10.57745/KAMGHR", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:24:39Z", "type": "Dataset", "title": "The effects of earthworm species on organic matter transformations and soil microbial communities are only partially related to their bioturbation activity", "description": "This dataset was acquired to investigate the effects of earthworm species on soil bioturbation, biogeochemical transformations of soil organic matter, and soil microbial communities under controlled conditions. Six earthworm species (Lumbricus terrestris, Allolobophora chlorotica, Octolasion cyaneum, Octodrilus complanatus, Aporrectodea caliginosa meridionalis and Microscolex dubius) were incubated in soil cores with soil and alfalfa litter for 6 weeks, at 16 \u00b0C. The soil is a silty loam sampled in an agricultural plot in Estr\u00e9es-Mons, northern France. Two series of soil cores were performed, including controls (3 with litter and without earthworm, 3 without litter and without earthworm per series). At the end of the incubation period, the entire cores were scanned using a medical scanner for bioturbation measurements. All images were processed the same way to compute the number of macropores (set of connected voxels), the volume of burrows (sum of all the macropore volume), the vertical barycentre of the burrow system (the centre of mass of the burrow system when only the vertical dimension is taken into account), the diameter (assessed as the median of the diameter of all vertical pores with a circularity 0.8) and burrow system continuity (number of burrows whose vertical length was higher than 30% of the depth of the soil core). In cores with earthworms, the soil was sampled from three different compartments: surface casts, the drilosphere (i.e., soil surrounding burrows, up to 4 mm from the burrow walls), and surrounding bulk soil. In control cores without earthworms, the soil was sampled from three different depths: surface (0-2 cm from the soil surface), middle (8-12 cm) and bottom (18-22 cm). Biogeochemical measurements, performed on the different soil compartments, included : soil humidity, dissolved organic carbon (C), total C, total nitrogen (N), mineral N, organic N contents, C to N ratio, nitrate (NO3-) and ammonium (NH4+) contents at the time if sampling and after 8 days in incubation at 20\u00b0C, carbon dioxide (CO2) fluxes measured with Isotope-ratio mass spectrometry (IRMS) method after 46, 91, 136, and 181 hours of microcosm incubation at 20\u00b0C, CO2 fluxes measured with sodium hydroxide (NaOH) traps after 46, 94, 142, and 190 hours of microcosm incubation at 20\u00b0C. Microbiological measurements, performed on the different soil compartments, included: total DNA concentration in soil, 16S rRNA copy number, 18S rRNA copy number, bacterial operational taxonomic unit (OUT) composition, and Shannon index, calculated on bacterial OTU. This work was supported by the the AgroEcoSystem Division of INRAE through the funding of the \u201cGloWorms\u201d project.", "keywords": ["Earth and Environmental Science", "Decomposition", "Agricultural Sciences", "Nitrogen", "Life Sciences", "Agriculture", " Forestry", " Horticulture", " Aquaculture", "Carbon", "Soil", "Earth and Environmental Sciences", "Earthworm", "Agriculture", " Forestry", " Horticulture", " Aquaculture and Veterinary Medicine", "mineralization", "Environmental Research", "Natural Sciences", "Agriculture", " Forestry", " Horticulture", "Geosciences"], "contacts": [{"organization": "Lashermes, Gwena\u00eblle, Vion-Guibert, Luna, Capowiez, Yvan, Alavoine, Gonzague, Delfosse, Olivier, Hedde, Micka\u00ebl, Marsden, Claire,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.57745/KAMGHR"}, {"rel": "self", "type": "application/geo+json", "title": "10.57745/KAMGHR", "name": "item", "description": "10.57745/KAMGHR", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.57745/KAMGHR"}, {"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": "10.1016/j.scitotenv.2013.03.090", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:16:55Z", "type": "Journal Article", "created": "2013-04-24", "title": "Microbial Utilisation Of Biochar-Derived Carbon", "description": "Whilst largely considered an inert material, biochar has been documented to contain a small yet significant fraction of microbially available labile organic carbon (C). Biochar addition to soil has also been reported to alter soil microbial community structure, and to both stimulate and retard the decomposition of native soil organic matter (SOM). We conducted a short-term incubation experiment using two (13)C-labelled biochars produced from wheat or eucalypt shoots, which were incorporated in an aridic arenosol to examine the fate of the labile fraction of biochar-C through the microbial community. This was achieved using compound specific isotopic analysis (CSIA) of phospholipid fatty acids (PLFAs). A proportion of the biologically-available fraction of both biochars was rapidly (within three days) utilised by gram positive bacteria. There was a sharp peak in CO2 evolution shortly after biochar addition, resulting from rapid turnover of labile C components in biochars and through positive priming of native SOM. Our results demonstrate that this CO2 evolution was at least partially microbially mediated, and that biochar application to soil can cause significant and rapid changes in the soil microbial community; likely due to addition of labile C and increases in soil pH.", "keywords": ["Carbon sequestration", "[SDE] Environmental Sciences", "Carbon Sequestration", "Chromatography", " Gas", "Magnetic Resonance Spectroscopy", "550", "short term", "[SDV]Life Sciences [q-bio]", "growth", "black carbon", "Char", "01 natural sciences", "630", "Mass Spectrometry", "c 13 plfa", "Black carbon", "soil organic matter", "Soil Pollutants", "mineralization", "Organic carbon", "Phospholipids", "Soil Microbiology", "char", "0105 earth and related environmental sciences", "2. Zero hunger", "Carbon Isotopes", "decomposition", "wheat straw", "biomass", "organic carbon", "Fatty Acids", "Western Australia", "04 agricultural and veterinary sciences", "Carbon Dioxide", "15. Life on land", "540", "pyrolysis", "forest soil", "carbon sequestration", "Carbon", "[SDV] Life Sciences [q-bio]", "Charcoal", "[SDE]Environmental Sciences", "0401 agriculture", " forestry", " and fisheries", "community structure", "\u00b9\u00b3C-PLFA", "Pyrolysis"]}, "links": [{"href": "https://doi.org/10.1016/j.scitotenv.2013.03.090"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Science%20of%20The%20Total%20Environment", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.scitotenv.2013.03.090", "name": "item", "description": "10.1016/j.scitotenv.2013.03.090", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.scitotenv.2013.03.090"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2013-11-01T00:00:00Z"}}, {"id": "10.1016/j.soilbio.2009.12.011", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:17:07Z", "type": "Journal Article", "created": "2010-01-02", "title": "Impacts Of Extreme Winter Warming Events On Litter Decomposition In A Sub-Arctic Heathland", "description": "Arctic climate change is expected to lead to a greater frequency of extreme winter warming events. During these events, temperatures rapidly increase to well above 0 degrees C for a number of days, which can lead to snow melt at the landscape scale, loss of insulating snow cover and warming of soils. However, upon return of cold ambient temperatures, soils can freeze deeper and may experience more freeze-thaw cycles due to the absence of a buffering snow layer. Such loss of snow cover and changes in soil temperatures may be critical for litter decomposition since a stable soil microclimate during winter (facilitated by snow cover) allows activity of soil organisms. Indeed, a substantial part of fresh litter decomposition may occur in winter. However, the impacts of extreme winter warming events on soil processes such as decomposition have never before been investigated. With this study we quantify the impacts of winter warming events on fresh litter decomposition using field simulations and lab studies. Winter warming events were simulated in sub-Arctic heathland using infrared heating lamps and soil warming cables during March (typically the period of maximum snow depth) in three consecutive years of 2007, 2008, and 2009. During the winters of 2008 and 2009, simulations were also run in January (typically a period of shallow snow cover) on separate plots. The lab study included soil cores with and without fresh litter subjected to winter-warming simulations in climate chambers. Litter decomposition of common plant species was unaffected by winter warming events simulated either in the lab (litter of Betula pubescens ssp. czerepanovii), or field (litter of Vaccinium vitis-idaea, and B. pubescens ssp. czerepanovii) with the exception of Vaccinium myrtillus (a common deciduous dwarf shrub) that showed less mass loss in response to winter warming events. Soil CO2 efflux measured in the lab study was (as expected) highly responsive to winter warming events but surprisingly fresh litter decomposition was not. Most fresh litter mass loss in the lab occurred during the first 3-4 weeks (simulating the period after litter fall). In contrast to past understanding, this suggests that winter decomposition of fresh litter is almost nonexistent and observations of substantial mass loss across the cold season seen here and in other studies may result from leaching in autumn, prior to the onset of 'true' winter. Further, our findings surprisingly suggest that extreme winter warming events do not affect fresh litter decomposition. Crown Copyright (c) 2009 Published by Elsevier Ltd. All rights reserved.", "keywords": ["Betula pubescens ssp czerepanovii", "Decomposition", "Extreme weather", "04 agricultural and veterinary sciences", "15. Life on land", "Winter warming event", "V. myrtillus", "Arctic", "13. Climate action", "Snow", "SDG 13 - Climate Action", "Climate change", "0401 agriculture", " forestry", " and fisheries", "Vaccinium vitis-idaea", "Freeze-thaw"]}, "links": [{"href": "https://doi.org/10.1016/j.soilbio.2009.12.011"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20Biology%20and%20Biochemistry", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.soilbio.2009.12.011", "name": "item", "description": "10.1016/j.soilbio.2009.12.011", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.soilbio.2009.12.011"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2010-04-01T00:00:00Z"}}, {"id": "10.1016/j.scitotenv.2018.05.063", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:16:57Z", "type": "Journal Article", "created": "2018-05-14", "title": "Retention soil filter as post-treatment step to remove micropollutants from sewage treatment plant effluent", "description": "Retention soil filters (RSFs) are a specific form of vertical flow constructed wetlands for the treatment of rain water and/or wastewater. We have tested 3 pilot RSFs to investigate removal of dissolved organic carbon (DOC) and 14 different organic micropollutants (OMPs) from the effluent of a large scale sewage treatment plant (STP). Two of them were operated as conventional RSF with material (sand with CaCO3 and organic matter) from two different full-scale RSFs. The third pilot RSF contained filter material (sand with CaCO3) with additional biochar in the upper layer (0-10\u202fcm) and granulated activated carbon (GAC) in the lower layer (60-90\u202fcm). The filters were planted with Phragmites australis. The RSFs were operated and monitored for 3\u202fyears, and water samples were taken regularly at inflow, outflows and in 3 depths within the filters. In total 523 samples were taken. In the conventional RSF, best median removal was detected for galaxolide, diclofenac 4-hydroxy, metoprolol and clarithromycin (75-79%). No removal was seen for sulfamethoxazole and carbamazepine. The DOC and OMP removal in the conventional RSFs was best in the upper layer with highest organic matter content, increased in time over the three years of operation and also with extended contact time. In the effluent of the RSF with GAC, 10 out of the 14 OMPs could not be detected; 4 OMPs were detected, but only metformin with removal\u202f<\u202f80%, thus showing a more efficient removal than the conventional RSF. A decrease in DOC removal was detected in the GAC layer (>88% to 60%) over the 2.5\u202fyears of operation. Biochar was most effective in OMP removal in the first operational year. It can be concluded that the increasing removal efficiency of the conventional RSF material - also present in the RSF with biochar and GAC - might mitigate the reduced efficiency of the sorbent additives biochar and GAC. This enables to extend the operational lifetime of the filters with acceptable removal rates. Finally, our study demonstrates that an RSF with GAC shows an enhanced removal of OMPs, which is a suitable post-treatment step for STPs.", "keywords": ["Constructed wetlands", "Granular activated carbon", "Sewage", "Wastewater treatment", "Waste Disposal", " Fluid", "01 natural sciences", "6. Clean water", "Water Purification", "Post-treatment step", "Soil", "Charcoal", "Micropollutants", "Retention soil filter", "Filtration", "Water Pollutants", " Chemical", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.scitotenv.2018.05.063"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Science%20of%20The%20Total%20Environment", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.scitotenv.2018.05.063", "name": "item", "description": "10.1016/j.scitotenv.2018.05.063", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.scitotenv.2018.05.063"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-10-01T00:00:00Z"}}, {"id": "10.1016/j.scitotenv.2019.03.176", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:16:58Z", "type": "Journal Article", "created": "2019-03-13", "title": "Effect of digestate application on microbial respiration and bacterial communities' diversity during bioremediation of weathered petroleum hydrocarbons contaminated soils", "description": "Digestate is an organic by-product of biogas production via anaerobic digestion processes and has a great potential as soil fertilizer due to concentrated nutrients. In this study, we examined digestate as a potential nutrient and microbial seeding for bioremediation of weathered (aged) petroleum hydrocarbon contaminated soils. We analysed 6 different treatments in microcosm using two industrial soils having different textures: a clay rich soil and a sandy soil. After 30\u202fdays of incubation, the highest total petroleum hydrocarbons (TPH) removal was observed in microcosms containing digestate together with bulking agent (17.8% and 12.7% higher than control in clay rich soil and sandy soil, respectively) or digestate together with immobilized bacteria (13.4% and 9% higher than control in clay rich soil and sandy soil, respectively). After digestate application microbial respiration was enhanced in sandy soil and inhibited in clay rich soil due to aggregates formation. After bulking agent addition to clay rich soil aggregates size was reduced and oxygen uptake was improved. Application of digestate to soil resulted in the development of distinct microbial groups in amended and non-amended soils. Genera containing species able to degrade TPH like Acinetobacter and Mycobacterium were abundant in digestate and in soil amended with digestate. Quantification of alkB genes, encoding alkane monoxygenase, revealed high concentration of these genes in digestate bacterial community. After application of digestate, the level of alkB genes significantly increased in soils and remained high until the end of the treatment. The study revealed great potential of digestate as a nutrient and bacteria source for soil bioremediation.", "keywords": ["[SDE] Environmental Sciences", "TPH removal", "550", "Soil remediation", "0211 other engineering and technologies", "alkB genes; Organic fertilizers; qPCR; Soil remediation; TPH removal; Biodegradation", " Environmental; Environmental Restoration and Remediation; Hydrocarbons; Petroleum; Petroleum Pollution; Soil; Soil Pollutants; Soil Microbiology", "02 engineering and technology", "01 natural sciences", "7. Clean energy", "630", "Organic fertilizers", "Environmental", "Soil", "alkB genes", "Soil Pollutants", "Petroleum Pollution", "Environmental Restoration and Remediation", "Soil Microbiology", "0105 earth and related environmental sciences", "2. Zero hunger", "[SDE.IE]Environmental Sciences/Environmental Engineering", "15. Life on land", "Hydrocarbons", "6. Clean water", "qPCR", "Biodegradation", " Environmental", "Petroleum", "[SDE]Environmental Sciences", "Biodegradation", "[SDE.IE] Environmental Sciences/Environmental Engineering"]}, "links": [{"href": "https://doi.org/10.1016/j.scitotenv.2019.03.176"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Science%20of%20The%20Total%20Environment", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.scitotenv.2019.03.176", "name": "item", "description": "10.1016/j.scitotenv.2019.03.176", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.scitotenv.2019.03.176"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-06-01T00:00:00Z"}}, {"id": "10.1016/j.soilbio.2010.03.026", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:17:07Z", "type": "Journal Article", "created": "2010-04-14", "title": "Nitrogen Alters Carbon Dynamics During Early Succession In Boreal Forest", "description": "Boreal forests are an important source of wood products, and fertilizers could be used to improve forest yields, especially in nutrient poor regions of the boreal zone. With climate change, fire frequencies may increase, resulting in a larger fraction of the boreal landscape present in early-successional stages. Since most fertilization studies have focused on mature boreal forests, the response of burned boreal ecosystems to increased nutrient availability is unclear. Therefore, we used a nitrogen (N) fertilization experiment to test how C cycling in a recently-burned boreal ecosystem would respond to increased N availability. We hypothesized that fertilization would increase rates of decomposition, soil respiration, and the activity of extracellular enzymes involved in C cycling, thereby reducing soil C stocks. In line with our hypothesis, litter mass loss increased significantly and activities of cellulose- and chitin-degrading enzymes increased by 45\u201361% with N addition. We also observed a significant decline in C concentrations in the organic soil horizon from 19.5 \u00b1 0.7% to 13.5 \u00b1 0.6%, and there was a trend toward lower total soil C stocks in the fertilized plots. Contrary to our hypothesis, mean soil respiration over three growing seasons declined by 31% from 78.3 \u00b1 6.5 mg CO2\u2013C m\u22122 h\u22121 to 54.4 \u00b1 4.1 mg CO2\u2013C m\u22122 h\u22121. These changes occurred despite a 2.5-fold increase in aboveground net primary productivity with N, and were accompanied by significant shifts in the structure of the fungal community, which was dominated by Ascomycota. Our results show that the C cycle in early-successional boreal ecosystems is highly responsive to N addition. Fertilization results in an initial loss of soil C followed by depletion of soil C substrates and development of a distinct and active fungal community. Total microbial biomass declines and respiration rates do not keep pace with plant inputs. These patterns suggest that N fertilization could transiently reduce but then increase ecosystem C storage in boreal regions experiencing more frequent fires.", "keywords": ["0106 biological sciences", "Decomposition", "Extracellular enzyme", "Agricultural and Veterinary Sciences", "Fungi", "Agronomy & Agriculture", "Soil respiration", "04 agricultural and veterinary sciences", "Biological Sciences", "15. Life on land", "Fire", "Soil carbon", "01 natural sciences", "Nitrogen fertilization", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "Boreal forest", "Succession", "Alaska", "Environmental Sciences"]}, "links": [{"href": "https://escholarship.org/content/qt4z375574/qt4z375574.pdf"}, {"href": "https://doi.org/10.1016/j.soilbio.2010.03.026"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20Biology%20and%20Biochemistry", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.soilbio.2010.03.026", "name": "item", "description": "10.1016/j.soilbio.2010.03.026", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.soilbio.2010.03.026"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2010-07-01T00:00:00Z"}}, {"id": "10.1016/j.soilbio.2010.07.011", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:17:07Z", "type": "Journal Article", "created": "2010-07-28", "title": "Resistance Of Microbial And Soil Properties To Warming Treatment Seven Years After Boreal Fire", "description": "Boreal forests store a large fraction of global terrestrial carbon and are susceptible to environmental change, particularly rising temperatures and increased fire frequency. These changes have the potential to drive positive feedbacks between climate warming and the boreal carbon cycle. Because few studies have examined the warming response of boreal ecosystems recovering from fire, we established a greenhouse warming experiment near Delta Junction, Alaska, seven years after a 1999 wildfire. We hypothesized that experimental warming would increase soil CO2 efflux, stimulate nutrient mineralization, and alter the composition and function of soil fungal communities. Although our treatment resulted in 1.20 \u00b0C soil warming, we found little support for our hypothesis. Only the activities of cellulose- and chitin-degrading enzymes increased significantly by 15% and 35%, respectively, and there were no changes in soil fungal communities. Warming resulted in drier soils, but the corresponding change in soil water potential was probably not sufficient to limit microbial activity. Rather, the warming response of this soil may be constrained by depletion of labile carbon substrates resulting from combustion and elevated soil temperatures in the years after the 1999 fire. We conclude that positive feedbacks between warming and the microbial release of soil carbon are weak in boreal ecosystems lacking permafrost. Since permafrost-free soils underlie 45\u201360% of the boreal zone, our results should be useful for modeling the warming response during recovery from fire in a large fraction of the boreal forest.", "keywords": ["0301 basic medicine", "Decomposition", "0303 health sciences", "Extracellular enzyme", "Agricultural and Veterinary Sciences", "Fungi", "Agronomy & Agriculture", "Soil respiration", "Biological Sciences", "15. Life on land", "Fire", "Soil carbon", "Climate Action", "03 medical and health sciences", "13. Climate action", "Boreal forest", "Warming", "Succession", "Alaska", "Environmental Sciences"]}, "links": [{"href": "https://escholarship.org/content/qt2zk6k6ms/qt2zk6k6ms.pdf"}, {"href": "https://doi.org/10.1016/j.soilbio.2010.07.011"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20Biology%20and%20Biochemistry", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.soilbio.2010.07.011", "name": "item", "description": "10.1016/j.soilbio.2010.07.011", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.soilbio.2010.07.011"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2010-10-01T00:00:00Z"}}, {"id": "10.1016/j.soilbio.2014.11.003", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:17:12Z", "type": "Journal Article", "created": "2014-11-17", "title": "Short- And Long-Term Effects Of Nutrient Enrichment On Microbial Exoenzyme Activity In Mangrove Peat", "description": "Abstract Mangroves receive increasing quantities of nutrients as a result of coastal development, which could lead to significant changes in carbon sequestration and soil subsidence. We hypothesised that mangrove-produced tannins induce a nitrogen (N) limitation on microbial decomposition even when plant growth is limited by phosphorus (P). As a result, increased N influx would lead to a net loss of sequestered carbon negating the ability to compensate for sea level rise in P-limited mangroves. To examine this, we quantified the short- and long-term effects of N and P enrichment on microbial biomass and decomposition-related enzyme activities in a Rhizophora mangle-dominated mangrove, which had been subjected to fertilisation treatments for a period of fifteen years. We compared microbial biomass, elemental stoichiometry and potential enzyme activity in dwarf and fringe-type R. mangle-dominated sites, where primary production is limited by P or N depending on the proximity to open water. Even in P-limited mangroves, microbial activity was N-limited as indicated by stoichiometry and an increase in enzymic activity upon N amendment. Nevertheless, microbial biomass increased upon field additions of P, indicating that the carbon supply played even a larger role. Furthermore, we found that P amendment suppressed phenol oxidase activity, while N amendment did not. The possible differential nutrient limitations of microbial decomposers versus primary producers implies that the direction of the effect of eutrophication on carbon sequestration is nutrient-specific. In addition, this study shows that phenol oxidase activities in this system decrease through P, possibly strengthening the enzymic latch effect of mangrove tannins. Furthermore, it is argued that the often used division between N-harvesting, P-harvesting, and carbon-harvesting exoenzymes needs to be reconsidered.", "keywords": ["Rhizophora", "Decomposition", "Peat", "Differential nutrient limitation", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "Microbial activity", "Microbial elemental stoichiometry", "13. Climate action", "international", "Taverne", "11. Sustainability", "Mangroves", "0401 agriculture", " forestry", " and fisheries", "SDG 14 - Life Below Water", "SOC", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.soilbio.2014.11.003"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20Biology%20and%20Biochemistry", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.soilbio.2014.11.003", "name": "item", "description": "10.1016/j.soilbio.2014.11.003", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.soilbio.2014.11.003"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2015-02-01T00:00:00Z"}}, {"id": "10.1016/j.soilbio.2015.11.018", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:17:13Z", "type": "Journal Article", "created": "2016-01-08", "title": "Peat Origin And Land Use Effects On Microbial Activity, Respiration Dynamics And Exo-Enzyme Activities In Drained Peat Soils In The Netherlands", "description": "This study assessed the risk of decomposition-driven soil subsidence in drained peat soils in the Netherlands, contrasting in peat origin and current land use. In a full factorial design, fen peat and bog peat were sampled from sites in use for nature conservation and for dairy farming, which contrast in history of drainage and fertilisation. In these four peat types, which frequently occur in the Netherlands, the microbial activity and respiration dynamics were studied in samples from superficial oxic peat layers by measuring Substrate Induced Respiration (SIR) and Substrate Induced Growth Response (SIGR). Total and active microbial biomass, microbial growth potential and potential exo-enzyme activities were determined in unamended samples and after nitrogen and/or glucose amendments.It has been hypothesized that greater production of total nonstructural carbohydrates (TNC) in foliage grown under elevated atmospheric carbon dioxide (CO2) will result in higher concentrations of defensive compounds in tree leaf litter, possibly leading to reduced rates of decomposition and nutrient cycling in forest ecosystems of the future. To evaluate the effects of elevated atmospheric CO2on litter chemistry and decomposition, we performed a 111 day laboratory incubation with leaf litter of trembling aspen (Populus tremuloidesMichaux) produced at 36\uffe2\uff80\uff83Pa and 56\uffe2\uff80\uff83Pa CO2and two levels of soil nitrogen (N) availability. Decomposition was quantified as microbially respired CO2and dissolved organic carbon (DOC) in soil solution, and concentrations of nonstructural carbohydrates, N, carbon (C), and condensed tannins were monitored throughout the incubation. Growth under elevated atmospheric CO2did not significantly affect initial litter concentrations of TNC, N, or condensed tannins. Rates of decomposition, measured as both microbially respired CO2and DOC did not differ between litter produced under ambient and elevated CO2. Total C lost from the samples was 38\uffe2\uff80\uff83mg\uffe2\uff80\uff83g\uffe2\uff88\uff921litter as respired CO2and 138\uffe2\uff80\uff83mg\uffe2\uff80\uff83g\uffe2\uff88\uff921litter as DOC, suggesting short\uffe2\uff80\uff90term pulses of dissolved C in soil solution are important components of the terrestrial C cycle. We conclude that litter chemistry and decomposition in trembling aspen are minimally affected by growth under higher concentrations of CO2.
", "keywords": ["Ecology and Evolutionary Biology", "carbohydrates", "Quaking aspen", "forest-soil", "litter-plant", "nitrogen", "nitrogen-", "Microlysimeter", "soil-chemistry", "cycling-", "populus-tremuloides", "Geology and Earth Sciences", "Soil Carbon", "Microbiology of soils", "Carbon cycle", "04 agricultural and veterinary sciences", "GLOBAL-ECOLOGY", "chemical-composition", "Organic-matter", "soil-solution", "nutrient-availability", "Tannin", "leaf-litter", "Science", "decomposition-", "Nutrient enrichment", "Carbohydrates", "carbohydrates-", "respiration-", "carbon-dioxide-enrichment", "Nitrogen in soil", "michigan-", "carbon sinks", "C", "Nutrient budget of forests", "Litter", "Populus tremuloides", "Global Change", "tannins-", "Decomposition", "forest-litter", "Foliage", "Carbon dioxide effects on forest litter", "Climatic changes", "15. Life on land", "carbon-nitrogen-ratio", "Forest litter decomposition", "N Ratio", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "microbial-activities", "nitrogen-content"]}, "links": [{"href": "https://doi.org/10.1046/j.1365-2486.2001.00388.x"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Change%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1046/j.1365-2486.2001.00388.x", "name": "item", "description": "10.1046/j.1365-2486.2001.00388.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1046/j.1365-2486.2001.00388.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2001-01-01T00:00:00Z"}}, {"id": "10.1021/acs.est.0c06687", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:17:36Z", "type": "Journal Article", "created": "2021-02-10", "title": "Microbial Interactions Drive the Complete Catabolism of the Antibiotic Sulfamethoxazole in Activated Sludge Microbiomes", "description": "Microbial communities are believed to outperform monocultures in the complete catabolism of organic pollutants via reduced metabolic burden and increased robustness to environmental challenges; however, the interaction mechanism in functional microbiomes remains poorly understood. Here, three functionally differentiated activated sludge microbiomes (S1: complete catabolism of sulfamethoxazole (SMX); S2: complete catabolism of the phenyl part of SMX ([phenyl]-SMX) with stable accumulation of its heterocyclic product 3-amino-5-methylisoxazole (3A5MI); A: complete catabolism of 3A5MI rather than [phenyl]-SMX) were enriched. Combining time-series cultivation-independent microbial community analysis, DNA-stable isotope probing, molecular ecological network analysis, and cultivation-dependent function verification, we identified key players involved in the SMX degradation process. Paenarthrobacter and Nocardioides were primary degraders for the initial cleavage of the sulfonamide functional group (-C-S-N- bond) and 3A5MI degradation, respectively. Complete catabolism of SMX was achieved by their cross-feeding. The co-culture of Nocardioides, Acidovorax, and Sphingobium demonstrated that the nondegraders Acidovorax and Sphingobium were involved in the enhancement of 3A5MI degradation. Moreover, we unraveled the internal labor division patterns and connections among the active members centered on the two primary degraders. Overall, the proposed methodology is promisingly applicable and would help generate mechanistic, predictive, and operational understanding of the collaborative biodegradation of various contaminants. This study provides useful information for synthetic activated sludge microbiomes with optimized environmental functions.", "keywords": ["Sulfamethoxazole", "Physiology", "Science Policy", "analysis", "0211 other engineering and technologies", "02 engineering and technology", "Microbiology", "Environmental Sciences not elsewhere classified", "heterocyclic product 3-", "11. Sustainability", "Activated Sludge Microbiomes Microb.", "Acidovorax", "SMX degradation process", "Molecular Biology", "cultivation-dependent function veri.", "phenyl", "Ecology", "Sewage", "Microbiota", "catabolism", "Nocardioide", "Computational Biology", "Cell Biology", "6. Clean water", "Sphingobium", "Anti-Bacterial Agents", "sludge microbiomes", "Infectious Diseases", "Complete", "Biodegradation", " Environmental", "Microbial Interactions Drive", "degrader", "Microbial Interactions", "labor division patterns", "5MI degradation", "Water Pollutants", " Chemical", "Developmental Biology", "Biological Sciences not elsewhere classified"]}, "links": [{"href": "https://pubs.acs.org/doi/pdf/10.1021/acs.est.0c06687"}, {"href": "https://doi.org/10.1021/acs.est.0c06687"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Environmental%20Science%20%26amp%3B%20Technology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1021/acs.est.0c06687", "name": "item", "description": "10.1021/acs.est.0c06687", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1021/acs.est.0c06687"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-02-10T00:00:00Z"}}, {"id": "10.1021/acs.est.4c10664", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:17:37Z", "type": "Journal Article", "created": "2025-04-18", "title": "An Analytical Workflow to Quantify Biodegradable Polyesters in Soils and Its Application to Incubation Experiments", "description": "Open AccessSoil biodegradable polyesters are designed to undergo to microbial utilization in aerobic soils, forming carbon dioxide and microbial biomass. These polyesters are thus viable substitutes for conventional, persistent polymers (e.g., polyethylene) in specific applications for which the transfer of some of the polymers into the soil is inevitable. While polymer biodegradability is often assessed in laboratory incubations using respirometric analysis of formed CO2, approaches to accurately quantify biodegradable polyesters in soils and to track their mass loss in field incubations over time remain missing. This study first introduces an analytical workflow combining Soxhlet extraction with proton nuclear magnetic resonance spectroscopy for the accurate, high-throughput, and chemically selective quantification of eight commercially important biodegradable polyesters (i.e., poly(butylene adipate-co-terephthalate), polylactic acid, poly(3-hydroxybutyrate-co-3-hydroxyhexanoate), poly(3-hydroxybutyrate-co-3-hydroxyvalerate), polycaprolactone, polybutylene adipate, polybutylene azelate, and polybutylene succinate), and the nonbiodegradable polymer polystyrene, in six soils spanning a range of types and physicochemical properties. This work introduces an effective sample deployment-retrieval approach that, combined with the analytical method, allows the biodegradation of poly(butylene adipate-co-terephthalate) and polylactic acid from a biodegradable mulch film in three agricultural soils to be monitored. In combination, the two parts of this work lay the foundation to accurately quantify and monitor biodegradable polymers in soils.", "keywords": ["Soxhlet extraction", "Soxhlet extraction; biodegradable polymer; biodegradation; soil; H-1-NMR; mulch film", "biodegradable polymer", "biodegradation", "H-1-NMR", "mulch film", "soil"], "contacts": [{"organization": "Mattia Cerri, Flora Wille, Silvan Arn, Thomas D. Bucheli, Franco Widmer, Rhayn Werz, Kristopher McNeill, Alessandro Manfrin, Michael Sander,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1021/acs.est.4c10664"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Environmental%20Science%20%26amp%3B%20Technology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1021/acs.est.4c10664", "name": "item", "description": "10.1021/acs.est.4c10664", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1021/acs.est.4c10664"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-04-18T00:00:00Z"}}, {"id": "10.1023/a:1009728007279", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:17:42Z", "type": "Journal Article", "created": "2002-12-22", "title": "Nutrient Imitations In An Extant And Drained Poor Fen: Implications For Restoration", "description": "In a species-rich poor fen (Caricetum nigrae) and a species-poor drained fen, the difference in nutrient limitation of the vegetation was assessed in a full-factorial fertilization experiment with N, P and K. The results were compared to the nutrient ratios of plant material and to chemical analysis of the topsoil. A rewetting experiment with intact sods was carried out in the glasshouse and the results are discussed in view of restoration prospects of drained and degraded peatlands. In the undrained poor fen the above-ground biomass yield was N-limited while the vegetation of the drained fen was K-limited. Experimental rewetting of intact turf samples, taken in the drained site, did not change the biomass yield or the type of nutrient limitation. It was concluded that mire systems which have been subjected to prolonged drainage are inclined to pronounced K-deficiency, probably due to washing out of potassium and harvesting the standing crop. This may hamper restoration projects in degraded peat areas where nature conservation tries to restore species-rich vegetation types with a high nature value.
", "keywords": ["0106 biological sciences", "DECOMPOSITION", "restoration", "fen", "rewetting", "N-MINERALIZATION", "VEGETATION RESPONSE", "Caricetum nigrae", "potassium limitation", "04 agricultural and veterinary sciences", "WET MEADOWS", "15. Life on land", "01 natural sciences", "wetland", "SOIL", "DEFICIENCY", "ORGANIC-MATTER", "STANDS", "PHOSPHORUS", "fertilization", "nutrients", "ECOSYSTEMS", "0401 agriculture", " forestry", " and fisheries", "drainage"], "contacts": [{"organization": "van Duren, I.C., Boeye, Dirk, Grootjans, A.P.,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1023/a:1009728007279"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Plant%20Ecology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1023/a:1009728007279", "name": "item", "description": "10.1023/a:1009728007279", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1023/a:1009728007279"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "1997-11-01T00:00:00Z"}}, {"id": "10.1023/a:1009838618133", "type": "Feature", "geometry": null, "properties": {"license": "Closed Access", "updated": "2026-04-04T16:17:43Z", "type": "Journal Article", "description": "The decomposition of oilseed rape residues of differentquality and its effects on the mineral N dynamics of the soil in the period between crops were studied in situ. The residues studied were obtained by growing an oilseed rape crop at two levels of N fertilisation, 0 and 270 kg N ha\u22121. The study was carried out using two types of experiment: \ufb01eld plots and cylinders \ufb01lled with disturbed soil and inserted into the soil. The decomposition of the residues was followed using an approach involving the dynamics of both carbon and nitrogen, the parameters measured being the CO2 emitted from the soil, the soil mineral N content, the C present in soluble form or in the form of microbial biomass, and the C and N present in the form of plant residues. The two residues studied, of similar biochemical composition, and differing only in their N content, were rapidly mineralised: approximately 50% of the carbon in the residues was decomposed during the \ufb01rst two months following incorporation into the soil. The carbon mineralised in the form of CO2 was largely related to the C present in the residues, no relationship having been found with the C present in soluble form or in the form of microbial biomass. Calculation of net N mineralisation from the residues using a model of mineralisation and leaching has provided evidence of an immobilisation phase for soil mineral N, during the \ufb01rst steps of residues decomposition. Labelling the high-N residues with 15N has moreover enabled us to demonstrate the low availability of the organic N from this residue, 20.8% of the organic N being mineralised in the course of 18 months of experimentation. Eventually, only the highest-N content residue resulted in a mineral N surplus in the soil, equivalent to 9 kg N ha\u22121, by comparison with the control soil. Finally, this study has provided good evidence of the complementarity between the two experimental methods. The cylinders of disturbed soil gave a precise measurement of the decomposition of the residues, especially by means of monitoring soil respiration. The \ufb01eld plots were used to monitor the dynamics of soil mineral N which were calculated with the aid of a mathematical model of mineralisation and leaching of nitrogen in the presence and absence of residues.", "keywords": ["[SDV.SA.AGRO] Life Sciences [q-bio]/Agricultural sciences/Agronomy", "[SDE] Environmental Sciences", "decomposition", "Agronomie", "[SDV.SA.AGRO]Life Sciences [q-bio]/Agricultural sciences/Agronomy", "Brassica napus L.", "[SDV.SA.SDS]Life Sciences [q-bio]/Agricultural sciences/Soil study", "N immobilisation", "630", "modelling", "Brassica napus L", "[SDE]Environmental Sciences", "N mineralisation", "Teneur en eau du sol", "plant residues", "[SDV.SA.SDS] Life Sciences [q-bio]/Agricultural sciences/Soil study"]}, "links": [{"href": "https://doi.org/10.1023/a:1009838618133"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nutrient%20Cycling%20in%20Agroecosystems", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1023/a:1009838618133", "name": "item", "description": "10.1023/a:1009838618133", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1023/a:1009838618133"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2000-01-01T00:00:00Z"}}, {"id": "10.1029/2003gb002127", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:17:48Z", "type": "Journal Article", "created": "2004-03-15", "title": "More New Carbon In The Mineral Soil Of A Poplar Plantation Under Free Air Carbon Enrichment (Popface): Cause Of Increased Priming Effect?", "description": "In order to establish suitability of forest ecosystems for long\uffe2\uff80\uff90term storage of C, it is necessary to characterize the effects of predicted increased atmospheric CO2 levels on the pools and fluxes of C within these systems. Since most C held in terrestrial ecosystems is in the soil, we assessed the influence of Free Air Carbon Enrichment (FACE) treatment on the total soil C content (Ctotal) and incorporation of litter derived C (Cnew) into soil organic matter (SOM) in a fast growing poplar plantation. Cnew was estimated by the C3/C4 stable isotope method. Ctotal contents increased under control and FACE respectively by 12 and 3%, i.e., 484 and 107 gC/m2, while 704 and 926 gC/m2 of new carbon was sequestered under control and FACE during the experiment. We conclude that FACE suppressed the increase of Ctotal and simultaneously increased Cnew. We hypothesize that these opposite effects may be caused by a priming effect of the newly incorporated litter, where priming effect is defined as the stimulation of SOM decomposition caused by the addition of labile substrates.
", "keywords": ["mechanisms", "decomposition", "turnover", "terrestrial ecosystems", "04 agricultural and veterinary sciences", "15. Life on land", "system", "storage", "forest", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "organic-matter", "elevated atmospheric co2", "feedbacks"]}, "links": [{"href": "https://doi.org/10.1029/2003gb002127"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Biogeochemical%20Cycles", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1029/2003gb002127", "name": "item", "description": "10.1029/2003gb002127", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1029/2003gb002127"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2004-03-01T00:00:00Z"}}, {"id": "10.1029/95gb02148", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:17:52Z", "type": "Journal Article", "created": "2004-02-04", "title": "Belowground Cycling Of Carbon In Forests And Pastures Of Eastern Amazonia", "description": "Forests in seasonally dry areas of eastern Amazonia near Paragominas, Par\uffc3\uffa1, Brazil, maintain an evergreen forest canopy through an extended dry season by taking up soil water through deep (>1 m) roots. Belowground allocation of C in these deep\uffe2\uff80\uff90rooting forests is very large (1900 g C m\uffe2\uff88\uff922 yr\uffe2\uff88\uff921) relative to litterfall (460 g C m\uffe2\uff88\uff922 yr\uffe2\uff88\uff921). The presence of live roots drives an active carbon cycle deeper than l m in the soil. Although bulk C concentrations and 14C contents of soil organic matter at >l\uffe2\uff80\uff90m depths are low, estimates of turnover from fine\uffe2\uff80\uff90root inputs, CO2 production, and the 14C content of CO2 produced at depth show that up to 15% of the carbon inventory in the deep soil has turnover times of decades or less. Thus the amount of fast\uffe2\uff80\uff90cycling soil carbon between 1 and 8\uffe2\uff80\uff90m depths (2\uffe2\uff80\uff933 kg C m\uffe2\uff88\uff922, out of 17\uffe2\uff80\uff9318 kg C m\uffe2\uff88\uff922) is significant compared to the amount present in the upper meter of soil (3\uffe2\uff80\uff934 kg C m\uffe2\uff88\uff922 out of 10\uffe2\uff80\uff9311 kg C m\uffe2\uff88\uff922). A model of belowground carbon cycling derived from measurements of carbon stocks and fluxes, and constrained using carbon isotopes, is used to predict C fluxes associated with conversion of deep\uffe2\uff80\uff90rooting forests to pasture and subsequent pasture management. The relative proportions and turnover times of active (including detrital plant material; 1\uffe2\uff80\uff933 year turnover), slow (decadal and shorter turnover), and passive (centennial to millennial turnover) soil organic matter pools are determined by depth for the forest soil, using constraints from measurements of C stocks, fluxes, and isotopic content. Reduced carbon inputs to the soil in degraded pastures, which are less productive than the forests they replace, lead to a reduction in soil carbon inventory and \uffce\uff9414C, in accord with observations. Managed pastures, which have been fertilized with phosphorous and planted with more productive grasses, show increases in C and 14C over forest values. Carbon inventory increases in the upper meter of managed pasture soils are partially offset by predicted carbon losses due to death and decomposition of fine forest roots at depths >1 m in the soil. The major adjustments in soil carbon inventory in response to land management changes occur within the first decade after conversion. Carbon isotopes are shown to be more sensitive indicators of recent accumulation or loss of soil organic matter than direct measurement of soil C inventories.
", "keywords": ["cycling", "decomposition", "model", "rooting", "carbon", "belowground carbon cycling", "carbon cycling", "04 agricultural and veterinary sciences", "South America", "15. Life on land", "Poaceae", "soil", "pasture", "forest", "Amazonia", "soil organic matter", "death", "tropical soil", "0401 agriculture", " forestry", " and fisheries", "phosphorus", "Brazil", "organic matter"]}, "links": [{"href": "https://escholarship.org/content/qt1zb7d8kx/qt1zb7d8kx.pdf"}, {"href": "https://doi.org/10.1029/95gb02148"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Biogeochemical%20Cycles", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1029/95gb02148", "name": "item", "description": "10.1029/95gb02148", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1029/95gb02148"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "1995-12-01T00:00:00Z"}}, {"id": "10.1038/s41561-020-0612-3", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:17:59Z", "type": "Journal Article", "created": "2020-07-27", "title": "Persistence of soil organic carbon caused by functional complexity", "description": "Soil organic carbon management has the potential to aid climate change mitigation through drawdown of atmospheric carbon dioxide. To be effective, such management must account for processes influencing carbon storage and re-emission at different space and time scales. Achieving this requires a conceptual advance in our understanding to link carbon dynamics from the scales at which processes occur to the scales at which decisions are made. Here, we propose that soil carbon persistence can be understood through the lens of decomposers as a result of functional complexity derived from the interplay between spatial and temporal variation of molecular diversity and composition. For example, co-location alone can determine whether a molecule is decomposed, with rapid changes in moisture leading to transport of organic matter and constraining the fitness of the microbial community, while greater molecular diversity may increase the metabolic demand of, and thus potentially limit, decomposition. This conceptual shift accounts for emergent behaviour of the microbial community and would enable soil carbon changes to be predicted without invoking recalcitrant carbon forms that have not been observed experimentally. Functional complexity as a driver of soil carbon persistence suggests soil management should be based on constant care rather than one-time action to lock away carbon in soils.", "keywords": ["[SDE] Environmental Sciences", "DECOMPOSITION", "2. Zero hunger", "106022 Mikrobiologie", "[SDE.MCG]Environmental Sciences/Global Changes", "UNCERTAINTY", "04 agricultural and veterinary sciences", "INPUTS", "15. Life on land", "TRANSPORT", "MODEL", "[SDE.MCG] Environmental Sciences/Global Changes", "106026 \u00d6kosystemforschung", "13. Climate action", "SDG 13 \u2013 Ma\u00dfnahmen zum Klimaschutz", "[SDE]Environmental Sciences", "SDG 13 - Climate Action", "Meteorology & Atmospheric Sciences", "106022 Microbiology", "GROWTH", "0401 agriculture", " forestry", " and fisheries", "TURNOVER", "PLANT", "106026 Ecosystem research", "MATTER"]}, "links": [{"href": "http://www.nature.com/articles/s41561-020-0612-3.pdf"}, {"href": "https://escholarship.org/content/qt84n3398c/qt84n3398c.pdf"}, {"href": "https://doi.org/10.1038/s41561-020-0612-3"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature%20Geoscience", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s41561-020-0612-3", "name": "item", "description": "10.1038/s41561-020-0612-3", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41561-020-0612-3"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-07-27T00:00:00Z"}}, {"id": "10.1046/j.1365-2486.1997.d01-133.x", "type": "Feature", "geometry": null, "properties": {"license": "Restricted", "updated": "2026-04-04T16:18:07Z", "type": "Journal Article", "created": "2003-11-02", "title": "Elevated Atmospheric Co2 Affects Decomposition Of Festuca Vivipara (L) Sm Litter And Roots In Experiments Simulating Environmental Change In Two Contrasting Arctic Ecosystems", "description": "Mass loss, together with nitrogen and carbon loss, from above\uffe2\uff80\uff90ground material and roots of Festuca vivipara were followed for 13 months in a high Arctic polar semi\uffe2\uff80\uff90desert and a low Arctic tree\uffe2\uff80\uff90line dwarf shrub heath. Festuca vivipara for the study was obtained from plants cultivated at two different CO2 concentrations (350 and 500 \uffce\uffbcL L\uffe2\uff80\uff931) in controlled environment chambers in the UK. Each of the four resource types (shoots or roots from plants grown in elevated or ambient CO2 concentrations) was subsequently placed in an experiment simulating aspects of environmental change in each Arctic ecosystem. Air, litter and soil temperatures were increased using open\uffe2\uff80\uff90topped polythene tents at both sites, and a 58% increase in summer precipitation was simulated at the high Arctic site.
Mass loss was greatest at the low Arctic site, and from the shoot material, rather than the roots. Shoots grown under an elevated CO2 concentration decomposed more slowly at the high Arctic site, and more quickly at the low Arctic one, than shoots grown at ambient CO2. After 13 months, greater amounts of C and N remained in above\uffe2\uff80\uff90ground litter from plants grown under elevated, rather than ambient, CO2 at the polar semi\uffe2\uff80\uff90desert site, although lower amounts of C remained in elevated CO2 litter at the low Arctic ecosystem. In the high Arctic, roots grown in the 500 \uffce\uffbcL L\uffe2\uff80\uff931 CO2 concentration decomposed significantly more slowly than below\uffe2\uff80\uff90ground material derived from the ambient CO2 chambers. Elevated CO2 concentrations significantly increased the inital C:N ratio, % soluble carbohydrates and \uffce\uffb1\uffe2\uff80\uff90cellulose content, and significantly decreased the inital N content, of the above\uffe2\uff80\uff90ground material compared to that derived from the ambient treatment. Initially, the C:N ratio and percentage N were similar in both sets of roots derived from the two different CO2 treatments, but soluble carbohydrate and \uffce\uffb1\uffe2\uff80\uff90cellulose concentrations were higher, and percentage lignin lower, in the elevated CO2 treatments.The tent treatments significantly retarded shoot decomposition in both ecosystems, probably because of lower litter bag moisture contents, although the additional precipitation treatment had no effect on mass loss from the above\uffe2\uff80\uff90ground material. The results suggest that neither additional summer precipitation (up to 58%), nor soil temperature increase of 1 \uffc2\uffb0C, which may occur by the end of the next century as an effect of a predicted 4 \uffc2\uffb0C rise in air temperature, had an appreciable effect on root decomposition in the short term in a high Arctic soil. However, at the low Arctic site, greater root decomposition, and a lower pool of root N remaining, were observed where soil temperature was increased by 2 \uffc2\uffb0C in response to a 4 \uffc2\uffb0C rise in air temperature. These results suggest that decomposition below\uffe2\uff80\uff90ground in this ecosystem would increase as an effect of predicted climate change. These data also show that there is a difference in the initial results of decomposition processes between the two Arctic ecosystems in response to simulated environmental change.
", "keywords": ["0106 biological sciences", "Decomposition", "Litter quality", "Nitrogen", "Grass", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "Carbon", "Arctic", "13. Climate action", "Soil temperature", "0401 agriculture", " forestry", " and fisheries", "Elevated CO2", "Soil moisture"]}, "links": [{"href": "https://doi.org/10.1046/j.1365-2486.1997.d01-133.x"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Change%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1046/j.1365-2486.1997.d01-133.x", "name": "item", "description": "10.1046/j.1365-2486.1997.d01-133.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1046/j.1365-2486.1997.d01-133.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "1997-02-01T00:00:00Z"}}], "links": [{"rel": "self", "type": "application/geo+json", "title": "This document as GeoJSON", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?facets=true&soil_functions=decomposition&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?facets=true&soil_functions=decomposition&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?facets=true&soil_functions=decomposition&", "hreflang": "en-US"}, {"rel": "next", "type": "application/geo+json", "title": "items (next)", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?facets=true&soil_functions=decomposition&offset=50", "hreflang": "en-US"}], "numberMatched": 123, "numberReturned": 50, "distributedFeatures": [], "timeStamp": "2026-04-04T17:43:18.210695Z"}