{"type": "FeatureCollection", "features": [{"id": "10.1016/j.soilbio.2021.108466", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-20T16:16:14Z", "type": "Journal Article", "created": "2021-11-03", "title": "Improved global-scale predictions of soil carbon stocks with Millennial Version 2", "description": "Abstract   Soil carbon (C) models are used to predict C sequestration responses to climate and land use change. Yet, the soil models embedded in Earth system models typically do not represent processes that reflect our current understanding of soil C cycling, such as microbial decomposition, mineral association, and aggregation. Rather, they rely on conceptual pools with turnover times that are fit to bulk C stocks and/or fluxes. As measurements of soil fractions become increasingly available, it is necessary for soil C models to represent these measurable quantities so that model processes can be evaluated more accurately. Here we present Version 2 (V2) of the Millennial model, a soil model developed to simulate C pools that can be measured by extraction or fractionation, including particulate organic C, mineral-associated organic C, aggregate C, microbial biomass, and low molecular weight C. Model processes have been updated to reflect the current understanding of mineral-association, temperature sensitivity and reaction kinetics, and different model structures were tested within an open-source framework. We evaluated the ability of Millennial V2 to simulate total soil organic C (SOC), as well as the mineral-associated and particulate fractions, using three independent data sets of soil fractionation measurements spanning a range of climate and geochemistry in Australia (N\u00a0=\u00a0495), Europe (N\u00a0=\u00a0175), and across the globe (N\u00a0=\u00a0659). When using all the data together (N\u00a0=\u00a01329), the Millennial V2 model predicted SOC (RMSE\u00a0=\u00a03.3\u00a0kg\u00a0C m\u22122, AIC\u00a0=\u00a0675,      R   i  n   2     \u00a0=\u00a00.31,      R   o  u  t   2     \u00a0=\u00a00.26) better than the widely-used first-order decomposition model Century (RMSE\u00a0=\u00a03.4\u00a0kg\u00a0C m\u22122, AIC\u00a0=\u00a0696,      R   i  n   2     \u00a0=\u00a00.21,      R   o  u  t   2     \u00a0=\u00a00.18) across sites, despite the fact that Millennial V2 has an increase in process complexity and number of parameters compared to Century. Millennial V2 also reproduced the observed fraction of C in MAOM and larger particle size fractions for most latitudes and biomes, and allows for a more detailed understanding of the pools and processes that affect model performance. It is important to note that this study evaluates the spatial variation in C stock only, and that the temporal dynamics of Millennial V2 remain to be tested. The Millennial V2 model updates the conceptual Century model pools and processes and represents our current understanding of the roles that microbial activity, mineral association and aggregation play in soil C sequestration.", "keywords": ["2. Zero hunger", "[SDU.OCEAN]Sciences of the Universe [physics]/Ocean", "550", "Mineral association", "Atmosphere", "Soil organic carbon stocks", "[SDU.OCEAN] Sciences of the Universe [physics]/Ocean", " Atmosphere", "15. Life on land", "551", "Microbial decomposition", "01 natural sciences", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "13. Climate action", "Soil carbon modeling", "[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces", "environment", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.soilbio.2021.108466"}, {"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.2021.108466", "name": "item", "description": "10.1016/j.soilbio.2021.108466", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.soilbio.2021.108466"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-01-01T00:00:00Z"}}, {"id": "10.1080/0020739X.2023.2254314", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-20T16:17:05Z", "type": "Journal Article", "created": "2023-09-15", "title": "An optimal control problem for resource utilisation by microorganisms", "description": "Decomposition of organic matter controls the flow of carbon and nutrients in terrestrial and aquatic ecosystems. Several kinetic laws have been proposed to describe decomposition rates, but they neglect adaptation of the microbial decomposer to environmental conditions. Here we formalise decomposition as an optimal control problem by assuming that microorganisms regulate the uptake rate of a substrate to maximise their growth over the period of decomposition. The result is an optimal control problem consisting of two differential equations and auxiliary conditions that determine the optimal value of the control variable (the uptake rate), the remaining substrate at any given time, and the optimal completion time. This problem serves as a case study to illustrate the solution of differential equations and optimal control problems for students in undergraduate courses. The mathematical analysis of the problem requires rewriting the differential equations in reverse time along with the solution of a nonhomogeneous linear first order differential equation. We then return to modelling with some biologically motivated questions about how the parameters of the model representing environmental conditions and microbial functional traits affect the outcome. Finally, we discuss alternative ways to use the material with students.", "keywords": ["0301 basic medicine", "03 medical and health sciences", "Annan matematik", "05 social sciences", "resource utilisation", "Didactics", "microbial decomposition", "Didaktik", "Other Mathematics", "0503 education", "6. Clean water", "Optimal control"]}, "links": [{"href": "https://www.tandfonline.com/doi/pdf/10.1080/0020739X.2023.2254314"}, {"href": "https://doi.org/10.1080/0020739X.2023.2254314"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/International%20Journal%20of%20Mathematical%20Education%20in%20Science%20and%20Technology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1080/0020739X.2023.2254314", "name": "item", "description": "10.1080/0020739X.2023.2254314", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1080/0020739X.2023.2254314"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-09-15T00:00:00Z"}}, {"id": "10.1080/0020739x.2023.2254314", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-20T16:17:05Z", "type": "Journal Article", "created": "2023-09-15", "title": "An optimal control problem for resource utilisation by microorganisms", "description": "Decomposition of organic matter controls the flow of carbon and nutrients in terrestrial and aquatic ecosystems. Several kinetic laws have been proposed to describe decomposition rates, but they neglect adaptation of the microbial decomposer to environmental conditions. Here we formalise decomposition as an optimal control problem by assuming that microorganisms regulate the uptake rate of a substrate to maximise their growth over the period of decomposition. The result is an optimal control problem consisting of two differential equations and auxiliary conditions that determine the optimal value of the control variable (the uptake rate), the remaining substrate at any given time, and the optimal completion time. This problem serves as a case study to illustrate the solution of differential equations and optimal control problems for students in undergraduate courses. The mathematical analysis of the problem requires rewriting the differential equations in reverse time along with the solution of a nonhomogeneous linear first order differential equation. We then return to modelling with some biologically motivated questions about how the parameters of the model representing environmental conditions and microbial functional traits affect the outcome. Finally, we discuss alternative ways to use the material with students.", "keywords": ["0301 basic medicine", "03 medical and health sciences", "Annan matematik", "05 social sciences", "resource utilisation", "Didactics", "microbial decomposition", "Didaktik", "Other Mathematics", "0503 education", "6. Clean water", "Optimal control"]}, "links": [{"href": "https://www.tandfonline.com/doi/pdf/10.1080/0020739X.2023.2254314"}, {"href": "https://doi.org/10.1080/0020739x.2023.2254314"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/International%20Journal%20of%20Mathematical%20Education%20in%20Science%20and%20Technology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1080/0020739x.2023.2254314", "name": "item", "description": "10.1080/0020739x.2023.2254314", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1080/0020739x.2023.2254314"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-09-15T00:00:00Z"}}, {"id": "10.1111/ejss.12487", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-20T16:17:27Z", "type": "Journal Article", "created": "2017-10-27", "title": "Plant exudates may stabilize or weaken soil depending on species, origin and time", "description": "Summary<p>We hypothesized that plant exudates could either gel or disperse soil depending on their chemical characteristics. Barley (Hordeum vulgare L. cv. Optic) and maize (Zea mays L. cv. Freya) root exudates were collected using an aerated hydroponic method and compared with chia (Salvia hispanica L.) seed exudate, a commonly used root exudate analogue. Sandy loam soil was passed through a 500\uffe2\uff80\uff90\uffce\uffbcm mesh and treated with each exudate at a concentration of 4.6 mg exudate g\uffe2\uff88\uff921 dry soil. Two sets of soil samples were prepared. One set of treated soil samples was maintained at 4\uffc2\uffb0C to suppress microbial processes. To characterize the effect of decomposition, the second set of samples was incubated at 16\uffc2\uffb0C for 2 weeks at \uffe2\uff88\uff9230 kPa matric potential. Gas chromatography\uffe2\uff80\uff93mass spectrometry (GC\uffe2\uff80\uff93MS) analysis of the exudates showed that barley had the largest organic acid content and chia the largest content of sugars (polysaccharide\uffe2\uff80\uff90derived or free), and maize was in between barley and chia. Yield stress of amended soil samples was measured by an oscillatory strain sweep test with a cone plate rheometer. When microbial decomposition was suppressed at 4\uffc2\uffb0C, yield stress increased 20\uffe2\uff80\uff90fold for chia seed exudate and twofold for maize root exudate compared with the control, whereas for barley root exudate decreased to half. The yield stress after 2 weeks of incubation compared with soil with suppressed microbial decomposition increased by 85% for barley root exudate, but for chia and maize it decreased by 87 and 54%, respectively. Barley root exudation might therefore disperse soil and this could facilitate nutrient release. The maize root and chia seed exudates gelled soil, which could create a more stable soil structure around roots or seeds.</p>Highlights<p>  <p>Rheological measurements quantified physical behaviour of plant exudates and effect on soil stabilization.</p> <p>Barley root exudates dispersed soil, which could release nutrients and carbon.</p> <p>Maize root and chia seed exudates had a stabilizing effect on soil.</p> <p>Physical engineering of soil in contact with plant roots depends on the nature and origin of exudates.</p>  </p", "keywords": ["construction", "0301 basic medicine", "EP/M020355/1", "seed exudate", "QH301 Biology", "610", "root exudate", "630", "QH301", "03 medical and health sciences", "DIMR 646809", "microbial decompisition", "Physical Processes and Function", "NE/L00237/1", "2. Zero hunger", "soil gelling", "BB/J000868/1", "Civil_env_eng", "Natural Environment Research Council (NERC)", "04 agricultural and veterinary sciences", "15. Life on land", "6. Clean water", "yield stress", "BB/J011460/1", "BB/L026058/1", "Engineering and Physical Sciences Research Council (EPSRC)", "soil dispersion", "viscosity", "Biotechnology and Biological Sciences Research Council (BBSRC)", "0401 agriculture", " forestry", " and fisheries", "microbial decomposition", "yeild stress", "European Research Council"]}, "links": [{"href": "https://repository.uwl.ac.uk/id/eprint/4980/1/Naveed_et_al-2017-European_Journal_of_Soil_Science.pdf"}, {"href": "https://eprints.soton.ac.uk/414238/1/EJSS_submitted_Manuscript.pdf"}, {"href": "http://onlinelibrary.wiley.com/wol1/doi/10.1111/ejss.12487/fullpdf"}, {"href": "https://doi.org/10.1111/ejss.12487"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/European%20Journal%20of%20Soil%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/ejss.12487", "name": "item", "description": "10.1111/ejss.12487", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/ejss.12487"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-10-27T00:00:00Z"}}, {"id": "10.1111/gcb.17153", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-20T16:17:31Z", "type": "Journal Article", "created": "2024-01-22", "title": "Carbon sequestration in the subsoil and the time required to stabilize carbon for climate change mitigation", "description": "Abstract<p>Soils store large quantities of carbon in the subsoil (below 0.2\uffe2\uff80\uff89m depth) that is generally old and believed to be stabilized over centuries to millennia, which suggests that subsoil carbon sequestration (CS) can be used as a strategy for climate change mitigation. In this article, we review the main biophysical processes that contribute to carbon storage in subsoil and the main mathematical models used to represent these processes. Our guiding objective is to review whether a process understanding of soil carbon movement in the vertical profile can help us to assess carbon storage and persistence at timescales relevant for climate change mitigation. Bioturbation, liquid phase transport, belowground carbon inputs, mineral association, and microbial activity are the main processes contributing to the formation of soil carbon profiles, and these processes are represented in models using the diffusion\uffe2\uff80\uff93advection\uffe2\uff80\uff93reaction paradigm. Based on simulation examples and measurements from carbon and radiocarbon profiles across biomes, we found that advective and diffusive transport may only play a secondary role in the formation of soil carbon profiles. The difference between vertical root inputs and decomposition seems to play a primary role in determining the shape of carbon change with depth. Using the transit time of carbon to assess the timescales of carbon storage of new inputs, we show that only small quantities of new carbon inputs travel through the profile and can be stabilized for time horizons longer than 50\uffe2\uff80\uff89years, implying that activities that promote CS in the subsoil must take into consideration the very small quantities that can be stabilized in the long term.</p", "keywords": ["Carbon Sequestration", "Climate Change", "transit time", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "diffusion\u2013advection\u2013reaction", "Carbon", "climate change mitigation", "Soil", "soil carbon sequestration", "13. Climate action", "radiocarbon", "0401 agriculture", " forestry", " and fisheries", "climate change mitigation; diffusion\u2013advection\u2013reaction; microbial decomposition; organic matter stabilization; radiocarbon; soil carbon sequestration; transit time", "microbial decomposition", "Ecosystem", "0105 earth and related environmental sciences", "organic matter stabilization"]}, "links": [{"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.17153"}, {"href": "https://doi.org/10.1111/gcb.17153"}, {"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": "10.1111/gcb.17153", "name": "item", "description": "10.1111/gcb.17153", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcb.17153"}, {"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": "3210439835", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-20T16:22:53Z", "type": "Journal Article", "created": "2021-11-03", "title": "Improved global-scale predictions of soil carbon stocks with Millennial Version 2", "description": "Abstract   Soil carbon (C) models are used to predict C sequestration responses to climate and land use change. Yet, the soil models embedded in Earth system models typically do not represent processes that reflect our current understanding of soil C cycling, such as microbial decomposition, mineral association, and aggregation. Rather, they rely on conceptual pools with turnover times that are fit to bulk C stocks and/or fluxes. As measurements of soil fractions become increasingly available, it is necessary for soil C models to represent these measurable quantities so that model processes can be evaluated more accurately. Here we present Version 2 (V2) of the Millennial model, a soil model developed to simulate C pools that can be measured by extraction or fractionation, including particulate organic C, mineral-associated organic C, aggregate C, microbial biomass, and low molecular weight C. Model processes have been updated to reflect the current understanding of mineral-association, temperature sensitivity and reaction kinetics, and different model structures were tested within an open-source framework. We evaluated the ability of Millennial V2 to simulate total soil organic C (SOC), as well as the mineral-associated and particulate fractions, using three independent data sets of soil fractionation measurements spanning a range of climate and geochemistry in Australia (N\u00a0=\u00a0495), Europe (N\u00a0=\u00a0175), and across the globe (N\u00a0=\u00a0659). When using all the data together (N\u00a0=\u00a01329), the Millennial V2 model predicted SOC (RMSE\u00a0=\u00a03.3\u00a0kg\u00a0C m\u22122, AIC\u00a0=\u00a0675,      R   i  n   2     \u00a0=\u00a00.31,      R   o  u  t   2     \u00a0=\u00a00.26) better than the widely-used first-order decomposition model Century (RMSE\u00a0=\u00a03.4\u00a0kg\u00a0C m\u22122, AIC\u00a0=\u00a0696,      R   i  n   2     \u00a0=\u00a00.21,      R   o  u  t   2     \u00a0=\u00a00.18) across sites, despite the fact that Millennial V2 has an increase in process complexity and number of parameters compared to Century. Millennial V2 also reproduced the observed fraction of C in MAOM and larger particle size fractions for most latitudes and biomes, and allows for a more detailed understanding of the pools and processes that affect model performance. It is important to note that this study evaluates the spatial variation in C stock only, and that the temporal dynamics of Millennial V2 remain to be tested. The Millennial V2 model updates the conceptual Century model pools and processes and represents our current understanding of the roles that microbial activity, mineral association and aggregation play in soil C sequestration.", "keywords": ["2. Zero hunger", "[SDU.OCEAN]Sciences of the Universe [physics]/Ocean", "550", "Mineral association", "Atmosphere", "Soil organic carbon stocks", "[SDU.OCEAN] Sciences of the Universe [physics]/Ocean", " Atmosphere", "15. Life on land", "551", "Microbial decomposition", "01 natural sciences", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "13. Climate action", "Soil carbon modeling", "[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces", "environment", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/3210439835"}, {"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": "3210439835", "name": "item", "description": "3210439835", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/3210439835"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-01-01T00:00:00Z"}}, {"id": "10.5061/dryad.r7sqv9shh", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-20T16:19:32Z", "type": "Dataset", "title": "Imprint of tree species mycorrhizal association on microbial-mediated enzyme activity and stoichiometry", "description": "unspecified1. Understanding the effects of tree species and their mycorrhizal  association on soil processes is critical for predicting the ecosystem  consequences of species shifts owing to global change and forest  management decisions. While it is well established that forests dominated  by different mycorrhizal types can vary in how they cycle carbon (C),  nitrogen (N) and phosphorus (P), the degree to which these patterns are  driven by microbial-mediated enzyme activity (EA) and ecoenzymatic  stoichiometry (ES) remain elusive. 2. Here, we synthesized the effects of  mycorrhizal association on seven soil enzymes involved in microbial C, N  and P acquisition and ES using data from 56 peer-reviewed papers. 3. We  found that relative to soil in ectomycorrhizal (EcM) trees, soil in  arbuscular mycorrhizal (AM) trees exhibited greater activity of some C  acquisition enzymes (e.g., beta-glucosidase; BG) and higher ecoenzymatic  ratios of BG/NAG (N-acetyl-glucosaminidase) and BG/AP (acid phosphatase).  These results supported that AM trees had rapid C and nutrient turnover  rates, inorganic nutrient economics and high soil microbial C limitation.  We also found evidence for an organic nutrient economy and greater soil  microbial demand for nutrients in EcM trees compared to AM trees. In  addition, the effect of mycorrhizal association on the activity of certain  soil enzymes and enzymatic stoichiometry (i.e., BG and BG/NAG ratio)  appeared to be associated with the differences in soil pH, phylogenetic  group (i.e., conifers and broadleaves) and leaf habit (i.e., evergreen and  deciduous) between AM and EcM trees. 4. The results from the global  meta-analysis suggested that soil EA and ES appear to play critical roles  in shaping the differences in the nutrient economy between AM and EcM tree  species, but leaf morphology and soil conditions should be considered in  evaluations of soil processes in forests of different mycorrhizal  associations. Given that most of the studies in the database were from the  temperate and subtropical regions, further research in other biomes is  needed to elucidate the underlying mechanisms driving the mycorrhizal  effect at the global scale.", "keywords": ["meta-analysis", "soil enzyme activity", "13. Climate action", "Nutrient economics", "FOS: Earth and related environmental sciences", "15. Life on land", "microbial decomposition", "substrate quality"], "contacts": [{"organization": "Zheng, Haifeng, Phillips, Richard, Rousk, Johannes, Yue, Kai, Schmidt, Inger Kappel, Wang, Senhao, Peng, Yan, Vesterdal, Lars,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5061/dryad.r7sqv9shh"}, {"rel": "self", "type": "application/geo+json", "title": "10.5061/dryad.r7sqv9shh", "name": "item", "description": "10.5061/dryad.r7sqv9shh", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5061/dryad.r7sqv9shh"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-02-28T00:00:00Z"}}, {"id": "20.500.11850/655486", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-20T16:22:15Z", "type": "Journal Article", "created": "2024-01-22", "title": "Carbon sequestration in the subsoil and the time required to stabilize carbon for climate change mitigation", "description": "Abstract<p>Soils store large quantities of carbon in the subsoil (below 0.2\uffe2\uff80\uff89m depth) that is generally old and believed to be stabilized over centuries to millennia, which suggests that subsoil carbon sequestration (CS) can be used as a strategy for climate change mitigation. In this article, we review the main biophysical processes that contribute to carbon storage in subsoil and the main mathematical models used to represent these processes. Our guiding objective is to review whether a process understanding of soil carbon movement in the vertical profile can help us to assess carbon storage and persistence at timescales relevant for climate change mitigation. Bioturbation, liquid phase transport, belowground carbon inputs, mineral association, and microbial activity are the main processes contributing to the formation of soil carbon profiles, and these processes are represented in models using the diffusion\uffe2\uff80\uff93advection\uffe2\uff80\uff93reaction paradigm. Based on simulation examples and measurements from carbon and radiocarbon profiles across biomes, we found that advective and diffusive transport may only play a secondary role in the formation of soil carbon profiles. The difference between vertical root inputs and decomposition seems to play a primary role in determining the shape of carbon change with depth. Using the transit time of carbon to assess the timescales of carbon storage of new inputs, we show that only small quantities of new carbon inputs travel through the profile and can be stabilized for time horizons longer than 50\uffe2\uff80\uff89years, implying that activities that promote CS in the subsoil must take into consideration the very small quantities that can be stabilized in the long term.</p", "keywords": ["Carbon Sequestration", "Climate Change", "transit time", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "diffusion\u2013advection\u2013reaction", "Carbon", "climate change mitigation", "Soil", "soil carbon sequestration", "13. Climate action", "radiocarbon", "0401 agriculture", " forestry", " and fisheries", "climate change mitigation; diffusion\u2013advection\u2013reaction; microbial decomposition; organic matter stabilization; radiocarbon; soil carbon sequestration; transit time", "microbial decomposition", "Ecosystem", "0105 earth and related environmental sciences", "organic matter stabilization"]}, "links": [{"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.17153"}, {"href": "https://doi.org/20.500.11850/655486"}, {"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": "20.500.11850/655486", "name": "item", "description": "20.500.11850/655486", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/20.500.11850/655486"}, {"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": "2164/9551", "type": "Feature", "geometry": null, "properties": {"updated": "2026-09-20T16:22:24Z", "type": "Journal Article", "created": "2017-10-27", "title": "Plant exudates may stabilize or weaken soil depending on species, origin and time", "description": "Summary                                                             <p>                       We hypothesized that plant exudates could either gel or disperse soil depending on their chemical characteristics. Barley (                       Hordeum vulgare                       L. cv. Optic) and maize (                       Zea mays                       L. cv. Freya) root exudates were collected using an aerated hydroponic method and compared with chia (                       Salvia hispanica                       L.) seed exudate, a commonly used root exudate analogue. Sandy loam soil was passed through a 500                       \uffe2\uff80\uff90                       \uffce\uffbcm mesh and treated with each exudate at a concentration of 4.6 mg exudate g                       \uffe2\uff88\uff921                       dry soil. Two sets of soil samples were prepared. One set of treated soil samples was maintained at 4\uffc2\uffb0C to suppress microbial processes. To characterize the effect of decomposition, the second set of samples was incubated at 16\uffc2\uffb0C for 2 weeks at \uffe2\uff88\uff9230 kPa matric potential. Gas chromatography\uffe2\uff80\uff93mass spectrometry (                       GC                       \uffe2\uff80\uff93                       MS                       ) analysis of the exudates showed that barley had the largest organic acid content and chia the largest content of sugars (polysaccharide\uffe2\uff80\uff90derived or free), and maize was in between barley and chia. Yield stress of amended soil samples was measured by an oscillatory strain sweep test with a cone plate rheometer. When microbial decomposition was suppressed at 4\uffc2\uffb0C, yield stress increased 20\uffe2\uff80\uff90fold for chia seed exudate and twofold for maize root exudate compared with the control, whereas for barley root exudate decreased to half. The yield stress after 2 weeks of incubation compared with soil with suppressed microbial decomposition increased by 85% for barley root exudate, but for chia and maize it decreased by 87 and 54%, respectively. Barley root exudation might therefore disperse soil and this could facilitate nutrient release. The maize root and chia seed exudates gelled soil, which could create a more stable soil structure around roots or seeds.                     </p>                                                           Highlights                     <p>                                                                           <p>Rheological measurements quantified physical behaviour of plant exudates and effect on soil stabilization.</p>                                                                             <p>Barley root exudates dispersed soil, which could release nutrients and carbon.</p>                                                                             <p>Maize root and chia seed exudates had a stabilizing effect on soil.</p>                                                                             <p>Physical engineering of soil in contact with plant roots depends on the nature and origin of exudates.</p>                                                                     </p>", "keywords": ["construction", "0301 basic medicine", "EP/M020355/1", "seed exudate", "QH301 Biology", "610", "root exudate", "630", "QH301", "03 medical and health sciences", "DIMR 646809", "microbial decompisition", "Physical Processes and Function", "NE/L00237/1", "2. Zero hunger", "soil gelling", "BB/J000868/1", "Civil_env_eng", "Natural Environment Research Council (NERC)", "04 agricultural and veterinary sciences", "15. Life on land", "6. Clean water", "yield stress", "BB/J011460/1", "BB/L026058/1", "Engineering and Physical Sciences Research Council (EPSRC)", "soil dispersion", "viscosity", "Biotechnology and Biological Sciences Research Council (BBSRC)", "0401 agriculture", " forestry", " and fisheries", "microbial decomposition", "yeild stress", "European Research Council"]}, "links": [{"href": "https://repository.uwl.ac.uk/id/eprint/4980/1/Naveed_et_al-2017-European_Journal_of_Soil_Science.pdf"}, {"href": "https://eprints.soton.ac.uk/414238/1/EJSS_submitted_Manuscript.pdf"}, {"href": "http://onlinelibrary.wiley.com/wol1/doi/10.1111/ejss.12487/fullpdf"}, {"href": "https://doi.org/2164/9551"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/European%20Journal%20of%20Soil%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "2164/9551", "name": "item", "description": "2164/9551", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2164/9551"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-10-27T00:00:00Z"}}, {"id": "bebbe78b-b2d7-4ad8-9ca1-5d650d052dfe", "type": "Feature", "geometry": {"type": "Polygon", "coordinates": [[[8.5, 49.81], [8.5, 53.25], [11.46, 53.25], [11.46, 49.81], [8.5, 49.81]]]}, "properties": {"themes": [{"concepts": [{"id": "farming"}], "scheme": "https://standards.iso.org/iso/19139/resources/gmxCodelists.xml#MD_TopicCategoryCode"}, {"concepts": [{"id": "Soil"}, {"id": "forest soils"}, {"id": "subsoil"}, {"id": "carbon cycle"}, {"id": "dissolved organic carbon"}, {"id": "soil organic carbon"}, {"id": "soil respiration"}, {"id": "soil transport processes"}, {"id": "temperate forests"}, {"id": "forest litter"}, {"id": "soil sorption"}, {"id": "desorption"}, {"id": "carbon mineralization"}], "scheme": "AGROVOC Multilingual agricultural thesaurus"}, {"concepts": [{"id": "carbon storage"}, {"id": "carbon retention"}, {"id": "microbial decomposition"}, {"id": "sorption isotherms"}, {"id": "opendata"}], "scheme": "Individual"}, {"concepts": [{"id": "Boden"}, {"id": "Gel\u00f6ster organischer Kohlenstoff"}, {"id": "Bodenprofil"}, {"id": "Organische Substanz"}, {"id": "Kohlenstoffkreislauf"}], "scheme": "GEMET - Concepts, version 2.4"}, {"concepts": [{"id": "Boden"}], "scheme": "GEMET - INSPIRE themes, version 1.0"}], "rights": "Restrictions applied to assure the protection of privacy or intellectual property, and any special restrictions or limitations or warnings on using the resource or metadata. Reports, articles, papers, scientific and non - scientific works of any form, including tables, maps, or any other kind of output, in printed or electronic form, based in whole or in part on the data supplied, must contain an acknowledgement of the form: \"Data reused from the BonaRes Data Centre www.bonares.de. This data were created as part of the SUBSOM's research activities.\"\n\nAlthough every care has been taken in preparing and testing the data, the SUBSOM and  the BonaRes Data Centre cannot guarantee that the data are correct; neither does the SUBSOM and the BonaRes Data Centre accept any liability whatsoever for any error, missing data or omission in the data, or for any loss or damage arising from its use. The SUBSOM and BonaRes Data Centre will not be responsible for any direct or indirect use which might be made of the data.", "updated": "2021-01-21", "type": "Dataset", "created": "2020-11-09", "language": "eng", "title": "Grinderwald soil monitoring - Soil organic carbon", "description": "This dataset includes soil OC data derived from soil cores taken at the sites from the DOC and CO2 monitoring at November 2016. Data derived from Liebmann et al. (2020) and were modified in this manuscript.\nThe dataset is a part of a larger data collection. The parent dataset is accessible via: https://doi.org/10.20387/bonares-rmtx-ttaj \n\nResearch domain: Soil Sciences\n\nResearch question: This dataset and all connected research data aim at evaluating temperate forest subsoils as potential future C-sinks.\n\nLiterature: Liebmann, P., Wordell-Dietrich, P., Kalbitz, K., Mikutta, R., Kalks, F., Don, A., Woche, S. K., Dsilva, L. R., and Guggenberger, G.: Relevance of aboveground litter for soil organic matter formation \u2013 a soil profile perspective, Biogeosciences, 17, 3099\u20133113, https://doi.org/10.5194/bg-17-3099-2020, 2020.", "formats": [{"name": "CSV"}], "keywords": ["Soil", "forest soils", "subsoil", "carbon cycle", "dissolved organic carbon", "soil organic carbon", "soil respiration", "soil transport processes", "temperate forests", "forest litter", "soil sorption", "desorption", "carbon mineralization", "carbon storage", "carbon retention", "microbial decomposition", "sorption isotherms", "opendata", "Boden", "Gel\u00f6ster organischer Kohlenstoff", "Bodenprofil", "Organische Substanz", "Kohlenstoffkreislauf", "Boden"], "contacts": [{"name": "Patrick Liebmann", "organization": "Leibniz Universit\u00e4t Hannover", "position": null, "roles": ["author"], "phones": [{"value": "+49 5117623671"}], "emails": [{"value": "liebmann@ifbk.uni-hannover.de"}], "addresses": [{"deliveryPoint": ["Herrenh\u00e4user Strasse 2"], "city": "Hannover", "administrativeArea": "Lower Saxony", "postalCode": "30419", "country": "Germany"}], "links": [{"href": {"url": "www.ORCID.org", "protocol": null, "protocol_url": "", "name": "0000-0002-0204-5857", "name_url": "", "description": "ORCID", "description_url": "", "applicationprofile": null, "applicationprofile_url": "", "function": null}}]}, {"name": "Timo Leinemann", "organization": "Leibniz Universit\u00e4t Hannover", "position": null, "roles": ["author"], "phones": [{"value": null}], "emails": [{"value": "timoleinemann@gmx.de"}], "addresses": [{"deliveryPoint": ["Herrenh\u00e4user Strasse 2"], "city": "Hannover", "administrativeArea": "Lower Saxony", "postalCode": "30419", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Patrick Wordell-Dietrich", "organization": "Technische Universit\u00e4t Dresden", "position": null, "roles": ["author"], "phones": [{"value": "+49 35146331391"}], "emails": [{"value": "patrick.wordell-dietrich@tu-dresden.de"}], "addresses": [{"deliveryPoint": ["Pienner Strasse 19"], "city": "Tharandt", "administrativeArea": "Saxony", "postalCode": "01737", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Sebastian Preusser", "organization": "Universit\u00e4t Hohenheim", "position": null, "roles": ["author"], "phones": [{"value": "+49 71145924065"}], "emails": [{"value": "s.preusser@uni-hohenheim.de"}], "addresses": [{"deliveryPoint": ["Emil-Wolff-Stra\u00dfe 27"], "city": "Stuttgart-Hohenheim", "administrativeArea": "Baden-Wuerttemberg", "postalCode": "70599", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Robert Mikutta", "organization": "Martin Luther University Halle-Wittenberg", "position": null, "roles": ["author"], "phones": [{"value": "+49 3455522530"}], "emails": [{"value": "robert.mikutta@landw.uni-halle.de"}], "addresses": [{"deliveryPoint": ["Von-Seckendorff-Platz 3"], "city": "Halle (Saale)", "administrativeArea": "Saxony-Anhalt", "postalCode": "06210", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Karsten Kalbitz", "organization": "Technische Universit\u00e4t Dresden", "position": null, "roles": ["author"], "phones": [{"value": "+49 35146331379"}], "emails": [{"value": "karsten.kalbitz@tu-dresden.de"}], "addresses": [{"deliveryPoint": ["Pienner Strasse 19"], "city": "Tharandt", "administrativeArea": "Saxony", "postalCode": "01737", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Axel Don", "organization": "Th\u00fcnen Institute of Climate-Smart Agriculture", "position": null, "roles": ["author"], "phones": [{"value": "+49 5315962641"}], "emails": [{"value": "axel.don@thuenen.de"}], "addresses": [{"deliveryPoint": ["Bundesallee 65"], "city": "Braunschweig", "administrativeArea": "Lower Saxony", "postalCode": "38116", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Ellen Kandeler", "organization": "Universit\u00e4t Hohenheim", "position": null, "roles": ["author"], "phones": [{"value": "+49 71145924220"}], "emails": [{"value": "kandeler@uni-hohenheim.de"}], "addresses": [{"deliveryPoint": ["Emil-Wolff-Stra\u00dfe 27"], "city": "Stuttgart-Hohenheim", "administrativeArea": "Baden-Wuerttemberg", "postalCode": "70599", "country": "Germany"}], "links": [{"href": null}]}, {"name": "J\u00f6rg Bachmann", "organization": "Leibniz Universit\u00e4t Hannover", "position": null, "roles": ["author"], "phones": [{"value": "+49 5117623672"}], "emails": [{"value": "bachmann@ifbk.uni-hannover.de"}], "addresses": [{"deliveryPoint": ["Herrenh\u00e4user Strasse 2"], "city": "Hannover", "administrativeArea": "Lower Saxony", "postalCode": "30419", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Bernd Marschner", "organization": "Ruhr-University Bochum", "position": null, "roles": ["author"], "phones": [{"value": "+49 2343222108"}], "emails": [{"value": "bernd.marschner@rub.de"}], "addresses": [{"deliveryPoint": ["Universit\u00e4tsstra\u00dfe 150"], "city": "Bochum", "administrativeArea": "North Rhine-Westphalia", "postalCode": "44801", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Frank Schaarschmidt", "organization": "Leibniz Universit\u00e4t Hannover", "position": null, "roles": ["author"], "phones": [{"value": "+49 5117625821"}], "emails": [{"value": "schaarschmidt@cell.uni-hannover.de"}], "addresses": [{"deliveryPoint": ["Herrenh\u00e4user Strasse 2"], "city": "Hannover", "administrativeArea": "Lower Saxony", "postalCode": "30419", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Georg Guggenberger", "organization": "Leibniz Universit\u00e4t Hannover", "position": null, "roles": ["author"], "phones": [{"value": "+49 5117622623"}], "emails": [{"value": "guggenberger@ifbk.uni-hannover.de"}], "addresses": [{"deliveryPoint": ["Herrenh\u00e4user Strasse 2"], "city": "Hannover", "administrativeArea": "Lower Saxony", "postalCode": "30419", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Georg Guggenberger", "organization": "Leibniz Universit\u00e4t Hannover", "position": null, "roles": ["projectLeader"], "phones": [{"value": "+49 5117622623"}], "emails": [{"value": "guggenberger@ifbk.uni-hannover.de"}], "addresses": [{"deliveryPoint": ["Herrenh\u00e4user Strasse 2"], "city": "Hannover", "administrativeArea": "Lower Saxony", "postalCode": "30419", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Karsten Kalbitz", "organization": "Technische Universit\u00e4t Dresden", "position": null, "roles": ["projectLeader"], "phones": [{"value": "+49 35146331379"}], "emails": [{"value": "karsten.kalbitz@tu-dresden.de"}], "addresses": [{"deliveryPoint": ["Pienner Strasse 19"], "city": "Tharandt", "administrativeArea": "Saxony", "postalCode": "01737", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Robert Mikutta", "organization": "Martin Luther University Halle-Wittenberg", "position": null, "roles": ["projectLeader"], "phones": [{"value": "+49 3455522530"}], "emails": [{"value": "robert.mikutta@landw.uni-halle.de"}], "addresses": [{"deliveryPoint": ["Von-Seckendorff-Platz 3"], "city": "Halle (Saale)", "administrativeArea": "Saxony-Anhalt", "postalCode": "06210", "country": "Germany"}], "links": [{"href": null}]}, {"name": "BonaRes Data Centre", "organization": "Leibniz Centre for Agricultural Landscape Research (ZALF)", "position": "Research Platform 'Data Analysis & Simulation' - WG Geodata", "roles": ["publisher"], "phones": [{"value": "+49 33432 82 171"}], "emails": [{"value": "bonares-datenzentrum@zalf.de"}], "addresses": [{"deliveryPoint": ["Eberswalder Strasse 84"], "city": "M\u00fcncheberg", "administrativeArea": "Brandenburg", "postalCode": "15374", "country": "Germany"}], "links": [{"href": null}]}, {"organization": "Th\u00fcnen Institute of Climate-Smart Agriculture;Ruhr-University Bochum;Martin Luther University Halle-Wittenberg;Technische Universit\u00e4t Dresden;Universit\u00e4t Hohenheim;Leibniz Universit\u00e4t Hannover", "roles": ["contributor"]}]}, "links": [{"href": "https://maps.bonares.de/mapapps/resources/apps/bonares/index.html?lang=en&mid=bebbe78b-b2d7-4ad8-9ca1-5d650d052dfe", "rel": "download"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/4d9f666c-7022-418d-822b-3d1b9c2726e0", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "bebbe78b-b2d7-4ad8-9ca1-5d650d052dfe", "name": "item", "description": "bebbe78b-b2d7-4ad8-9ca1-5d650d052dfe", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/bebbe78b-b2d7-4ad8-9ca1-5d650d052dfe"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-01-21T00:00:00Z"}}, {"id": "de0ec281-9f57-44a5-b78e-5c60672d73fe", "type": "Feature", "geometry": {"type": "Polygon", "coordinates": [[[8.5, 49.81], [8.5, 53.25], [11.46, 53.25], [11.46, 49.81], [8.5, 49.81]]]}, "properties": {"themes": [{"concepts": [{"id": "farming"}], "scheme": "https://standards.iso.org/iso/19139/resources/gmxCodelists.xml#MD_TopicCategoryCode"}, {"concepts": [{"id": "Soil"}, {"id": "forest soils"}, {"id": "subsoil"}, {"id": "carbon cycle"}, {"id": "dissolved organic carbon"}, {"id": "soil respiration"}, {"id": "soil transport processes"}, {"id": "temperate forests"}, {"id": "forest litter"}, {"id": "soil sorption"}, {"id": "desorption"}, {"id": "carbon mineralization"}], "scheme": "AGROVOC Multilingual agricultural thesaurus"}, {"concepts": [{"id": "carbon storage"}, {"id": "carbon retention"}, {"id": "microbial decomposition"}, {"id": "sorption isotherms"}, {"id": "initial mass approach"}, {"id": "opendata"}], "scheme": "Individual"}, {"concepts": [{"id": "Boden"}, {"id": "Gel\u00f6ster organischer Kohlenstoff"}, {"id": "Bodenprofil"}, {"id": "Organische Substanz"}, {"id": "Kohlenstoffkreislauf"}], "scheme": "GEMET - Concepts, version 2.4"}, {"concepts": [{"id": "Boden"}], "scheme": "GEMET - INSPIRE themes, version 1.0"}], "rights": "Restrictions applied to assure the protection of privacy or intellectual property, and any special restrictions or limitations or warnings on using the resource or metadata. Reports, articles, papers, scientific and non - scientific works of any form, including tables, maps, or any other kind of output, in printed or electronic form, based in whole or in part on the data supplied, must contain an acknowledgement of the form: \"Data reused from the BonaRes Data Centre www.bonares.de. This data were created as part of the SUBSOM's research activities.\"\n\nAlthough every care has been taken in preparing and testing the data, the SUBSOM and  the BonaRes Data Centre cannot guarantee that the data are correct; neither does the SUBSOM and the BonaRes Data Centre accept any liability whatsoever for any error, missing data or omission in the data, or for any loss or damage arising from its use. The SUBSOM and BonaRes Data Centre will not be responsible for any direct or indirect use which might be made of the data.", "updated": "2021-01-21", "type": "Dataset", "created": "2020-11-09", "language": "eng", "title": "Grinderwald / R\u00fcdershausen / Eberg\u00f6tzen \u2013 Sorption isotherms", "description": "This dataset includes laboratory batch sorption experiments with soil from all three study sites and soil depths down to 100 cm. DOC solutions with different concentrations between 1-400 ppm DOC were used in order to generate sorption isotherms.\nThe dataset is a part of a larger data collection. The parent dataset is accessible via: https://doi.org/10.20387/bonares-rmtx-ttaj \n\nResearch domain: Soil Sciences\n\nResearch question: This dataset and all connected research data aim at evaluating temperate forest subsoils as potential future C-sinks.", "formats": [{"name": "CSV"}], "keywords": ["Soil", "forest soils", "subsoil", "carbon cycle", "dissolved organic carbon", "soil respiration", "soil transport processes", "temperate forests", "forest litter", "soil sorption", "desorption", "carbon mineralization", "carbon storage", "carbon retention", "microbial decomposition", "sorption isotherms", "initial mass approach", "opendata", "Boden", "Gel\u00f6ster organischer Kohlenstoff", "Bodenprofil", "Organische Substanz", "Kohlenstoffkreislauf", "Boden"], "contacts": [{"name": "Patrick Liebmann", "organization": "Leibniz Universit\u00e4t Hannover", "position": null, "roles": ["author"], "phones": [{"value": "+49 5117623671"}], "emails": [{"value": "liebmann@ifbk.uni-hannover.de"}], "addresses": [{"deliveryPoint": ["Herrenh\u00e4user Strasse 2"], "city": "Hannover", "administrativeArea": "Lower Saxony", "postalCode": "30419", "country": "Germany"}], "links": [{"href": {"url": "www.ORCID.org", "protocol": null, "protocol_url": "", "name": "0000-0002-0204-5857", "name_url": "", "description": "ORCID", "description_url": "", "applicationprofile": null, "applicationprofile_url": "", "function": null}}]}, {"name": "Timo Leinemann", "organization": "Leibniz Universit\u00e4t Hannover", "position": null, "roles": ["author"], "phones": [{"value": null}], "emails": [{"value": "timoleinemann@gmx.de"}], "addresses": [{"deliveryPoint": ["Herrenh\u00e4user Strasse 2"], "city": "Hannover", "administrativeArea": "Lower Saxony", "postalCode": "30419", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Patrick Wordell-Dietrich", "organization": "Technische Universit\u00e4t Dresden", "position": null, "roles": ["author"], "phones": [{"value": "+49 35146331391"}], "emails": [{"value": "patrick.wordell-dietrich@tu-dresden.de"}], "addresses": [{"deliveryPoint": ["Pienner Strasse 19"], "city": "Tharandt", "administrativeArea": "Saxony", "postalCode": "01737", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Sebastian Preusser", "organization": "Universit\u00e4t Hohenheim", "position": null, "roles": ["author"], "phones": [{"value": "+49 71145924065"}], "emails": [{"value": "s.preusser@uni-hohenheim.de"}], "addresses": [{"deliveryPoint": ["Emil-Wolff-Stra\u00dfe 27"], "city": "Stuttgart-Hohenheim", "administrativeArea": "Baden-Wuerttemberg", "postalCode": "70599", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Robert Mikutta", "organization": "Martin Luther University Halle-Wittenberg", "position": null, "roles": ["author"], "phones": [{"value": "+49 3455522530"}], "emails": [{"value": "robert.mikutta@landw.uni-halle.de"}], "addresses": [{"deliveryPoint": ["Von-Seckendorff-Platz 3"], "city": "Halle (Saale)", "administrativeArea": "Saxony-Anhalt", "postalCode": "06210", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Karsten Kalbitz", "organization": "Technische Universit\u00e4t Dresden", "position": null, "roles": ["author"], "phones": [{"value": "+49 35146331379"}], "emails": [{"value": "karsten.kalbitz@tu-dresden.de"}], "addresses": [{"deliveryPoint": ["Pienner Strasse 19"], "city": "Tharandt", "administrativeArea": "Saxony", "postalCode": "01737", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Axel Don", "organization": "Th\u00fcnen Institute of Climate-Smart Agriculture", "position": null, "roles": ["author"], "phones": [{"value": "+49 5315962641"}], "emails": [{"value": "axel.don@thuenen.de"}], "addresses": [{"deliveryPoint": ["Bundesallee 65"], "city": "Braunschweig", "administrativeArea": "Lower Saxony", "postalCode": "38116", "country": "Germany"}], "links": [{"href": null}]}, {"name": "Ellen Kandeler", "organization": "Universit\u00e4t Hohenheim", 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Reports, articles, papers, scientific and non - scientific works of any form, including tables, maps, or any other kind of output, in printed or electronic form, based in whole or in part on the data supplied, must contain an acknowledgement of the form: \"Data reused from the BonaRes Data Centre www.bonares.de. This data were created as part of the SUBSOM's research activities.\"\n\nAlthough every care has been taken in preparing and testing the data, the SUBSOM and  the BonaRes Data Centre cannot guarantee that the data are correct; neither does the SUBSOM and the BonaRes Data Centre accept any liability whatsoever for any error, missing data or omission in the data, or for any loss or damage arising from its use. The SUBSOM and BonaRes Data Centre will not be responsible for any direct or indirect use which might be made of the data.", "updated": "2021-01-21", "type": "Dataset", "created": "2020-11-09", "language": "eng", "title": "Grinderwald soil monitoring - CO2 flux and production", "description": "This dataset includes data from a CO2 monitoring conducted in the Grinderwald research forest at the same sites as the DOC monitoring from January 2015 until end of October 2016 at the soil surface and in three depth compartments (10-30, 30-50, and 50-90 cm soil depth). Data derive from Wordell-Dietrich et al. (2019) and were modified for this manuscript.\nThe dataset is a part of a larger data collection. The parent dataset is accessible via: https://doi.org/10.20387/bonares-rmtx-ttaj\n\nResearch domain: Soil Sciences\n\nResearch question: This dataset and all connected research data aim at evaluating temperate forest subsoils as potential future C-sinks.\n\nLiterature: Wordell-Dietrich, P., Don, A., Wotte, A., Rethemeyer, J., Bachmann, J., Helfrich, M., Kirfel, K., and Leuschner, C.: Vertical partitioning of CO2 production in a Dystric Cambisol, Biogeosciences Discuss., https://doi.org/10.5194/bg-2019-143, in review, 2019.", "formats": [{"name": "CSV"}], "keywords": ["Soil", "forest soils", "subsoil", "carbon cycle", "dissolved organic carbon", "soil organic carbon", "soil respiration", "soil transport processes", "temperate forests", "forest litter", "soil sorption", "desorption", "carbon mineralization", "carbon storage", "carbon retention", "microbial decomposition", "sorption isotherms", "opendata", "Boden", "Gel\u00f6ster organischer Kohlenstoff", "Bodenprofil", "Organische 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Reports, articles, papers, scientific and non - scientific works of any form, including tables, maps, or any other kind of output, in printed or electronic form, based in whole or in part on the data supplied, must contain an acknowledgement of the form: \"Data reused from the BonaRes Data Centre www.bonares.de. This data were created as part of the SUBSOM's research activities.\"\n\nAlthough every care has been taken in preparing and testing the data, the SUBSOM and  the BonaRes Data Centre cannot guarantee that the data are correct; neither does the SUBSOM and the BonaRes Data Centre accept any liability whatsoever for any error, missing data or omission in the data, or for any loss or damage arising from its use. The SUBSOM and BonaRes Data Centre will not be responsible for any direct or indirect use which might be made of the data.", "updated": "2021-01-21", "type": "Dataset", "created": "2020-11-09", "language": "eng", "title": "Grinderwald / R\u00fcdershausen / Eberg\u00f6tzen - Batch sorption and desorption experiments", "description": "This dataset includes laboratory batch sorption and desorption experiments with soil from all three study sites and soil depths down to 100 cm. Sorption experiments were conducted with 13C-labelled DOM solution and desorption experiments with ionic background solution.\nThe dataset is a part of a larger data collection. 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Reports, articles, papers, scientific and non - scientific works of any form, including tables, maps, or any other kind of output, in printed or electronic form, based in whole or in part on the data supplied, must contain an acknowledgement of the form: \"Data reused from the BonaRes Data Centre www.bonares.de. This data were created as part of the SUBSOM's research activities.\"\n\nAlthough every care has been taken in preparing and testing the data, the SUBSOM and  the BonaRes Data Centre cannot guarantee that the data are correct; neither does the SUBSOM and the BonaRes Data Centre accept any liability whatsoever for any error, missing data or omission in the data, or for any loss or damage arising from its use. 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Reports, articles, papers, scientific and non - scientific works of any form, including tables, maps, or any other kind of output, in printed or electronic form, based in whole or in part on the data supplied, must contain an acknowledgement of the form: \"Data reused from the BonaRes Data Centre www.bonares.de. This data were created as part of the SUBSOM's research activities.\"\n\nAlthough every care has been taken in preparing and testing the data, the SUBSOM and  the BonaRes Data Centre cannot guarantee that the data are correct; neither does the SUBSOM and the BonaRes Data Centre accept any liability whatsoever for any error, missing data or omission in the data, or for any loss or damage arising from its use. 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Reports, articles, papers, scientific and non - scientific works of any form, including tables, maps, or any other kind of output, in printed or electronic form, based in whole or in part on the data supplied, must contain an acknowledgement of the form: \"Data reused from the BonaRes Data Centre www.bonares.de. This data were created as part of the SUBSOM's research activities.\"\n\nAlthough every care has been taken in preparing and testing the data, the SUBSOM and  the BonaRes Data Centre cannot guarantee that the data are correct; neither does the SUBSOM and the BonaRes Data Centre accept any liability whatsoever for any error, missing data or omission in the data, or for any loss or damage arising from its use. The SUBSOM and BonaRes Data Centre will not be responsible for any direct or indirect use which might be made of the data.", "updated": "2021-01-21", "type": "Dataset", "created": "2020-11-09", "language": "eng", "title": "Grinderwald - Mineral field incubation", "description": "This dataset includes data from a two-year field incubation of C-coated and 13C-labelled minerals (goethite and vermiculite) in the Grinderwald research forest in close vicinity to the DOC and CO2 monitoring sites. Minerals were buried in three soil depths down to 150 cm in May 2016 and removed in May 2018.\nThe dataset is a part of a larger data collection. 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Reports, articles, papers, scientific and non - scientific works of any form, including tables, maps, or any other kind of output, in printed or electronic form, based in whole or in part on the data supplied, must contain an acknowledgement of the form: \"Data reused from the BonaRes Data Centre www.bonares.de. This data were created as part of the SUBSOM's research activities.\"\n\nAlthough every care has been taken in preparing and testing the data, the SUBSOM and  the BonaRes Data Centre cannot guarantee that the data are correct; neither does the SUBSOM and the BonaRes Data Centre accept any liability whatsoever for any error, missing data or omission in the data, or for any loss or damage arising from its use. The SUBSOM and BonaRes Data Centre will not be responsible for any direct or indirect use which might be made of the data.", "updated": "2021-01-20", "type": "Dataset", "created": "2020-11-09", "language": "eng", "title": "Basic information of three beech forest sites in Lower Saxony (GER), part of the research unit SubSOM", "description": "This dataset includes general information about the sites used in our study. Our main investigations were done in the Grinderwald research forest by conducting a litter manipulation experiment with 13C-enriched beech litter combined with DOC and CO2 monitoring from February 2015 until November 2016, and soil core sampling. The monitoring was complemented by burial of 13C-coated minerals (goethite and vermiculite) with subsequent field incubation for two years (May 2016 \u2013 May 2018) and laboratory batch sorption and desorption experiments. The latter was additionally done with soil from two beech forest sites (R\u00fcdershausen and Eberg\u00f6tzen) with varying parent material, texture, and pedogenic oxides. 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