Soils are vital for supporting food security and other ecosystem services. Climate change can affect soil functions both directly and indirectly. Direct effects include temperature, precipitation, and moisture regime changes. Indirect effects include those that are induced by adaptations such as irrigation, crop rotation changes, and tillage practices. Although extensive knowledge is available on the direct effects, an understanding of the indirect effects of agricultural adaptation options is less complete. A review of 20 agricultural adaptation case\uffe2\uff80\uff90studies across Europe was conducted to assess implications to soil threats and soil functions and the link to the Sustainable Development Goals (SDGs). The major findings are as follows: (a) adaptation options reflect local conditions; (b) reduced soil erosion threats and increased soil organic carbon are expected, although compaction may increase in some areas; (c) most adaptation options are anticipated to improve the soil functions of food and biomass production, soil organic carbon storage, and storing, filtering, transforming, and recycling capacities, whereas possible implications for soil biodiversity are largely unknown; and (d) the linkage between soil functions and the SDGs implies improvements to SDG 2 (achieving food security and promoting sustainable agriculture) and SDG 13 (taking action on climate change), whereas the relationship to SDG 15 (using terrestrial ecosystems sustainably) is largely unknown. The conclusion is drawn that agricultural adaptation options, even when focused on increasing yields, have the potential to outweigh the negative direct effects of climate change on soil degradation in many European regions.
", "keywords": ["sol", "[SDE.MCG]Environmental Sciences/Global Changes", "Sustainable Development Goals", "Sustainable development goals", "regional case studies", "adaptation", "Soil degradation", "01 natural sciences", "service \u00e9cosyst\u00e9mique", "630", "333", "soil", "12. Responsible consumption", "soil degradation", "Regional case-studies", "Agrucultural adaption", "DPSIR", "11. Sustainability", "regional case-studies", "Agricultural adaptation; DPSIR; Regional case-studies; Soil degradation; Sustainable Development Goals; Environmental Chemistry; Development3304 Education; 2300; Soil Science", "Climate change", "Research Articles", "0105 earth and related environmental sciences", "2. Zero hunger", "VDP::Landbruks- og Fiskerifag: 900", "agricultural adaptation", "15. Life on land", "6. Clean water", "services \u00e9cosyst\u00e9miques", "13. Climate action"]}, "links": [{"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1002/ldr.3006"}, {"href": "https://doi.org/10.1002/ldr.3006"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Land%20Degradation%20%26amp%3B%20Development", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1002/ldr.3006", "name": "item", "description": "10.1002/ldr.3006", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1002/ldr.3006"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-05-30T00:00:00Z"}}, {"id": "10.1007/s11104-011-0870-3", "type": "Feature", "geometry": null, "properties": {"updated": "2026-10-06T16:15:09Z", "type": "Journal Article", "created": "2011-07-05", "title": "Biochar Adsorbed Ammonia Is Bioavailable", "description": "Biochar is produced as a by-product of the low temperature pyrolysis of biomass during bioenergy extraction and its incorporation into soil is of global interest as a potential carbon sequestration tool. Biochar influences soil nitrogen transformations and its capacity to take up ammonia is well recognized. Anthropogenic emissions of ammonia need to be mitigated due to negative environmental impacts and economic losses. Here we use an isotope of nitrogen to show that ammonia-N adsorbed by biochar is stable in ambient air, but readily bioavailable when placed in the soil. When biochars, containing adsorbed 15N labelled ammonia, were incorporated into soil the 15N recovery by roots averaged 6.8% but ranged from 26.1% to 10.9% in leaf tissue due to differing biochar properties with plant 15N recovery greater when acidic biochars were used to capture ammonia. Recovery of 15N as total soil nitrogen (organic+inorganic) ranged from 45% to 29% of 15N applied. We provide a proof of concept for a synergistic mitigation option where anthropogenic ammonia emissions could be captured using biochar, and made bioavailable in soils, thus leading to nitrogen capture by crops, while simultaneously sequestering carbon in soils.", "keywords": ["ryegrass", "550", "ANZSRC::31 Biological sciences", "ANZSRC::0703 Crop and Pasture Production", "ANZSRC::050301 Carbon Sequestration Science", "ANZSRC::30 Agricultural", "04 agricultural and veterinary sciences", "540", "ammonia", "01 natural sciences", "7. Clean energy", "nitrogen", "veterinary and food sciences", "13. Climate action", "ANZSRC::0503 Soil Sciences", "ANZSRC::41 Environmental sciences", "0401 agriculture", " forestry", " and fisheries", "biochar", "ANZSRC::070304 Crop and Pasture Biomass and Bioproducts", "N stable isotope", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1007/s11104-011-0870-3"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Plant%20and%20Soil", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s11104-011-0870-3", "name": "item", "description": "10.1007/s11104-011-0870-3", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s11104-011-0870-3"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2011-07-06T00:00:00Z"}}, {"id": "699cce7b36d2cdfbbf190e86cca42533", "type": "Feature", "geometry": null, "properties": {"updated": "2026-10-06T16:24:09Z", "type": "Report", "title": "Multi-modelling predictions show high uncertainty of required carbon input changes to reach a 4 parts per thousand target", "description": "Soils store vast amounts of carbon (C) on land, and increasing soil organic carbon (SOC) stocks in already managed soils such as croplands may be one way to remove C from the atmosphere, thereby limiting subsequent warming. The main objective of this study was to estimate the amount of additional C input needed to annually increase SOC stocks by 4%(0) at 16 long-term agricultural experiments in Europe, including exogenous organic matter (EOM) additions. We used an ensemble of six SOC models and ran them under two configurations: (1) with default parametrization and (2) with parameters calibrated site-by-site to fit the evolution of SOC stocks in the control treatments (without EOM). We compared model simulations and analysed the factors generating variability across models. The calibrated ensemble was able to reproduce the SOC stock evolution in the unfertilised control treatments. We found that, on average, the experimental sites needed an additional 1.5 +/- 1.2 Mg C ha(-)(1) year(-1) to increase SOC stocks by 4%(0) per year over 30 years, compared to the C input in the control treatments (multi-model median +/- median standard deviation across sites). That is, a 119% increase compared to the control. While mean annual temperature, initial SOC stocks and initial C input had a significant effect on the variability of the predicted C input in the default configuration (i.e., the relative standard deviation of the predicted C input from the mean), only water-related variables (i.e., mean annual precipitation and potential evapotranspiration) explained the divergence between models when calibrated. Our work highlights the challenge of increasing SOC stocks in agriculture and accentuates the need to increasingly lean on multi-model ensembles when predicting SOC stock trends and related processes. To increase the reliability of SOC models under future climate change, we suggest model developers to better constrain the effect of water-related variables on SOC decomposition.", "keywords": ["2. Zero hunger", "13. Climate action", "Soil Science", "15. Life on land", "551"], "contacts": [{"organization": "Bruni, Elisa, Chenu, Claire, Abramoff, Rose Z., Baldoni, Guido, Barkusky, Dietmar, Clivot, Hugues, Huang, Yuanyuan, K\u00e4tterer, Thomas, Pikula, Dorota, Virto, Inigo, Guenet, Bertrand,", "roles": ["creator"]}]}, "links": [{"href": "https://pub.epsilon.slu.se/31490/1/bruni-e-et-al-20230810.pdf"}, {"href": "https://doi.org/699cce7b36d2cdfbbf190e86cca42533"}, {"rel": "self", "type": "application/geo+json", "title": "699cce7b36d2cdfbbf190e86cca42533", "name": "item", "description": "699cce7b36d2cdfbbf190e86cca42533", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/699cce7b36d2cdfbbf190e86cca42533"}, {"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": "10.1016/j.apsoil.2016.05.018", "type": "Feature", "geometry": null, "properties": {"updated": "2026-10-06T16:15:42Z", "type": "Journal Article", "created": "2016-06-11", "title": "Interactive Effects Of Precipitation Manipulation And Nitrogen Addition On Soil Properties In California Grassland And Shrubland", "description": "Abstract Soil microbial communities and pools of carbon (C) and nitrogen (N) play an important role in ecosystem responses to precipitation variability and N deposition. In southern California, ecosystem vulnerability to these environmental change drivers may differ for grassland versus shrubland vegetation types. We hypothesized that (1) these vegetation types would differ in their responses to precipitation and N manipulation; (2) reduced precipitation (\u201cdrought treatment\u201d) would have a negative effect on soil microbial abundance and alter microbial community composition, (3) these changes would be associated with reductions in soil C and N pools, (4) N addition would increase microbial abundance as well as soil C and N pools, and (5) combined drought and N deposition would have offsetting effects on soil properties. We tested these hypotheses at the Loma Ridge Global Change Experiment in southern California. Across vegetation types, we found that microbial biomass based on phospholipid fatty acids declined with drought and N addition. Microbial composition differed more strongly by vegetation type than with environmental change treatments. Added precipitation had little effect on microbial biomass but reduced labile C and N pools; these reductions were mitigated by N addition. Drought reduced labile forms of soil C and N, whereas N addition increased labile soil C pools and all soil N pools. Negative effects of drought and N addition were additive for microbial biomass, which could inhibit soil C cycling if both of these environmental changes occur together. Drought interacted with N addition to significantly increase the most labile N pool under the drought\u00a0+\u00a0N treatment, which suggests a build-up of available N under these conditions. These results imply that multiple environmental changes may combine non-additively to affect below-ground microorganisms and soil C and N pools, which may have important consequences for ecosystem services such as productivity, biodiversity, and soil quality in Mediterranean climate regimes of North America.", "keywords": ["Veterinary and Food Sciences", "Soil Science", "Microbial communities", "Shrubland", "veterinary and food sciences", "Carbon and nitrogen cycle", "11. Sustainability", "Global change", "2. Zero hunger", "Agricultural", "Drought", "Agricultural and Veterinary Sciences", "Ecology", "Forestry Sciences", "Agronomy & Agriculture", "04 agricultural and veterinary sciences", "Biological Sciences", "15. Life on land", "Grassland", "Agricultural and Biological Sciences (miscellaneous)", "6. Clean water", "Environmental sciences", "Biological sciences", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "Environmental Sciences"]}, "links": [{"href": "https://escholarship.org/content/qt1p4898qc/qt1p4898qc.pdf"}, {"href": "https://doi.org/10.1016/j.apsoil.2016.05.018"}, {"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.2016.05.018", "name": "item", "description": "10.1016/j.apsoil.2016.05.018", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.apsoil.2016.05.018"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2016-11-01T00:00:00Z"}}, {"id": "10.1016/j.geoderma.2009.12.023", "type": "Feature", "geometry": null, "properties": {"updated": "2026-10-06T16:16:16Z", "type": "Journal Article", "created": "2010-01-19", "title": "Responses Of Soil Respiration To N Fertilization In A Loamy Soil Under Maize Cultivation", "description": "Abstract To understand the effects of nitrogen fertilization on soil respiration in an intensively cultivated fluvo-aquic loamy soil, a field experiment was conducted in the Fengqiu State Key Agro-Ecological Experimental Station, Henan province, China. The experiment consisted of five treatments: unplanted and N-unfertilized soil (CK0), unplanted soil treated with 150\u00a0kg N\u00a0ha \u2212\u00a01 (CKNL), maize ( Zea mays L.) planted and N-unfertilized soil (N0), and planted soils fertilized with 150\u00a0kg N\u00a0ha \u2212\u00a01 (NL) and 250\u00a0kg N\u00a0ha \u2212\u00a01 (NH). Soil CO 2 efflux during the maize growth season was significantly affected by soil temperature and also by soil moisture when the opposite effect of soil moisture below and above the optimum values was distinguished. There was a significant interdependence between soil temperature and soil moisture in the effect on soil CO 2 efflux in the presence of maize plants. A logarithm transformed regression equation including soil temperature ( T ) and soil moisture ( W ) was developed as y \u00a0=\u00a0 a \u00a0+\u00a0 bT log( W ). This equation accounted for 60\u201371% of the seasonal variation in soil CO 2 efflux, which better depicted soil CO 2 efflux than did a regression equation with soil temperature alone in the maize planted soils. Cumulative soil CO 2 emissions in the CK0 and CKNL treatments were estimated as 229\u00a0\u00b1\u00a012 and 245\u00a0\u00b1\u00a017\u00a0g C\u00a0m \u2212\u00a02 , respectively during the experimental period and the application of N fertilizer slightly increased soil basal respiration by 6.5% through enhancing microbial biomass. In contrast, cumulative seasonal soil CO 2 emissions were 7.4% lower in the NL (461\u00a0\u00b1\u00a033\u00a0g C\u00a0m \u2212\u00a02 ) and NH (462\u00a0\u00b1\u00a013\u00a0g C\u00a0m \u2212\u00a02 ) treatments than in the N0 treatment (498\u00a0\u00b1\u00a032\u00a0g C\u00a0m \u2212\u00a02 ), indicating that N fertilization marginally significantly depressed soil respiration ( p \u00a0=\u00a00.06). N application rates, however, did not exhibit any effects. Our results suggest that the effects of N fertilization on soil respiration mainly depended on the concentration of easily decomposed organic carbon in soil and N fertilization possibly reduced soil respiration in the planted soils when N released from the decomposition of native soil organic carbon roughly met the demand for maize growth.", "keywords": ["Environmental sciences", "2. Zero hunger", "Biological sciences", "Agricultural", "veterinary and food sciences", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "Soil sciences not elsewhere classified", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.geoderma.2009.12.023"}, {"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.2009.12.023", "name": "item", "description": "10.1016/j.geoderma.2009.12.023", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.geoderma.2009.12.023"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2010-03-01T00:00:00Z"}}, {"id": "10.1016/j.geoderma.2010.05.013", "type": "Feature", "geometry": null, "properties": {"updated": "2026-10-06T16:16:16Z", "type": "Journal Article", "created": "2010-07-01", "title": "Impact Of Biochar Amendments On The Quality Of A Typical Midwestern Agricultural Soil", "description": "Abstract Biochar, a co-product of thermochemical conversion of lignocellulosic materials into advanced biofuels, may be used as a soil amendment to enhance the sustainability of biomass harvesting. We investigated the impact of biochar amendments (0, 5, 10, and 20\u00a0g-biochar\u00a0kg\u2212\u00a01 soil) on the quality of a Clarion soil (Mesic Typic Hapludolls), collected (0\u201315\u00a0cm) in Boone County, Iowa. Repacked soil columns were incubated for 500\u00a0days at 25\u00a0\u00b0C and 80% relative humidity. On week 12, 5\u00a0g of dried and ground swine manure was incorporated into the upper 3\u00a0cm of soil for half of the columns. Once each week, all columns were leached with 200\u00a0mL of 0.001\u00a0M CaCl2. Soil bulk density increased with time for all columns and was significantly lower for biochar amended soils relative to the un-amended soils. The biochar amended soils retained more water at gravity drained equilibrium (up to 15%), had greater water retention at \u2212\u00a01 and \u22125\u00a0bars soil water matric potential, (13 and 10% greater, respectively), larger specific surface areas (up to 18%), higher cation exchange capacities (up to 20%), and pH values (up to 1 pH unit) relative to the un-amended controls. No effect of biochar on saturated hydraulic conductivity was detected. The biochar amendments significantly increased total N (up to 7%), organic C (up to 69%), and Mehlich III extractable P, K, Mg and Ca but had no effect on Mehlich III extractable S, Cu, and Zn. The results indicate that biochar amendments have the potential to substantially improve the quality and fertility status of Midwestern agricultural soils.", "keywords": ["2. Zero hunger", "Soil Science", "Agriculture", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "Soil quality", "630", "333", "6. Clean water", "Manure", "Black carbon", "Geochemistry", "Charcoal", "0401 agriculture", " forestry", " and fisheries", "biochar", "0105 earth and related environmental sciences"], "contacts": [{"organization": "Laird, David, Fleming, Pierce, Davis, Dedrick, Horton, Robert, Karlen, Douglas, Wang, Baiqun,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1016/j.geoderma.2010.05.013"}, {"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.2010.05.013", "name": "item", "description": "10.1016/j.geoderma.2010.05.013", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.geoderma.2010.05.013"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2010-09-01T00:00:00Z"}}, {"id": "10.1016/j.geoderma.2013.08.003", "type": "Feature", "geometry": null, "properties": {"updated": "2026-10-06T16:16:17Z", "type": "Journal Article", "created": "2013-09-20", "title": "The Effects Of N And P Additions On Microbial N Transformations And Biomass On Saline-Alkaline Grassland Of Loess Plateau Of Northern China", "description": "AbstractMicrobial nutrient transformation plays an important role in regulating nitrogen (N) and phosphorus (P) cycling in terrestrial ecosystems. Soil N and P contents also control microbial nutrient transformations. However, there is still dispute on how N and P additions affect microbial activity and N transformations. A field experiment was conducted to examine the effects of N and P on microbial N transformations and biomass in saline-alkaline grassland in Loess Plateau of northern China during growing season in 2009. N was added at a rate of 10gNm\u22122 y\u22121 in the form of NH4NO3. P was added at a rate of 5g P m\u22122 y\u22121 in the form of P2O5\u2212. We measured the in situ net ammonification rate (Ramm), and nitrification rate (Rnit) once a month from May to October; we also measured potential soil microbial biomass carbon (MBC), nitrogen (MBN), and potential microbial respiration (MR) once a month in laboratory.ResultsDuring the whole growing seasons, P addition significantly stimulated soil inorganic N pool, soil extractable C, soil extractable N pool, Rmin, and the metabolic quotient (qCO2) from the estimates of microbial respiration and microbial biomass carbon, and there was no effect on peak aboveground biomass, MBC, MBN and MR during the whole growing seasons in 2009. N addition significantly increased peak aboveground biomass, inorganic N pool, Rmin, MBN, MR, and qCO2, decreased soil extractable C and the ratio of MBC/MBN, and there was no effect on soil extractable N and MBC during the growing season in 2009. P addition increased the soil net N mineralization rate and N addition not only increased the soil net N mineralization rate but also increased microbial biomass N. We observed that P induced a decreased soil inorganic N pool, but N addition directly increased soil inorganic N pool, how to balance the quantity of N and P additions in agriculture system is an important technique in agriculture harvest in the future in Loess Plateau of Northern China.", "keywords": ["2. Zero hunger", "4. Education", "Microbial biomass", "N mineralization", "Soil Science", "04 agricultural and veterinary sciences", "15. Life on land", "Nitrification", "01 natural sciences", "6. Clean water", "Microbial respiration", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "Saline\u2013alkaline soil", "0105 earth and related environmental sciences"], "contacts": [{"organization": "Zhu Feng, Dong Kuanhu, Zhao Xiang, Wang Changhui,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1016/j.geoderma.2013.08.003"}, {"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.2013.08.003", "name": "item", "description": "10.1016/j.geoderma.2013.08.003", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.geoderma.2013.08.003"}, {"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": "ftslunivuppsala:oai:pub.epsilon.slu.se:34892", "type": "Feature", "geometry": null, "properties": {"updated": "2026-10-06T16:26:47Z", "type": "Report", "title": "When and why microbial-explicit soil organic carbon models can be unstable", "description": "Microbial-explicit soil organic carbon (SOC) cycling models are increasingly being recognized for their advantages over linear models in describing SOC dynamics. These models are known to exhibit oscillations, but it is not clear when they yield stable vs. unstable equilibrium points (EPs) - i.e., EPs that exist analytically but are not stable in relation to small perturbations and cannot be reached by transient simulations. The occurrence of such unstable EPs can lead to unexpected model behavior in transient simulations or unrealistic predictions of steady-state soil organic carbon (SOC) stocks. Here, we ask when and why unstable EPs can occur in an archetypal microbial-explicit model (representing SOC, dissolved OC (DOC), microbial biomass, and extracellular enzymes) and some simplified versions of it. Further, if a model formulation allows for physically meaningful but unstable EPs, can we find constraints in the model parameters (i.e., environmental conditions and microbial traits) that ensure stability of the EPs? We use analytical, numerical, and descriptive tools to answer these questions. We found that instability can occur when the resupply of a growth substrate (DOC) is (via a positive feedback loop) dependent on its abundance. We identified a conservative, sufficient condition in terms of model parameters to ensure the stability of EPs. Principally, three distinct strategies can avoid instability: (1) neglecting explicit DOC dynamics, (2) biomass-independent uptake rate, or (3) correlation between parameter values to obey the stability criterion. While the first two approaches simplify some mechanistic processes, the third approach points to the interactive effects of environmental conditions and parameters describing microbial physiology, highlighting the relevance of basic ecological principles for the avoidance of unrealistic (i.e., unstable) simulation outcomes. These insights can help to improve the applicability of microbial-explicit models, aid our understanding of the dynamics of these models, and highlight the relation between mathematical requirements and (in silico) microbial ecology.", "keywords": ["550", "Soil Science"], "contacts": [{"organization": "Ghersheen, Samia", "roles": ["creator"]}]}, "links": [{"href": "https://pub.epsilon.slu.se/34892/1/schwarz-e-et-al-20240828.pdf"}, {"href": "https://doi.org/ftslunivuppsala:oai:pub.epsilon.slu.se:34892"}, {"rel": "self", "type": "application/geo+json", "title": "ftslunivuppsala:oai:pub.epsilon.slu.se:34892", "name": "item", "description": "ftslunivuppsala:oai:pub.epsilon.slu.se:34892", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/ftslunivuppsala:oai:pub.epsilon.slu.se:34892"}, {"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.eti.2023.103229", "type": "Feature", "geometry": null, "properties": {"updated": "2026-10-06T16:16:04Z", "type": "Journal Article", "created": "2023-06-02", "title": "Modeling biochar-soil depth dependency on fecal coliform straining under subsurface drip irrigation", "description": "Funding Information: This work was supported by Shahrekord University, Iran. N. Sepehrnia is funded by a Marie Sk\u0142odowska-Curie Individual Fellowship, United Kingdom under the grant agreement No. 101026287. We acknowledge University of Aberdeen, UK for supporting this project. ; Peer reviewed", "keywords": ["GE", "Soil Science", "610", "Plant Science", "04 agricultural and veterinary sciences", "01 natural sciences", "6. Clean water", "510", "Biochar", "Maximum allowable depletion", "0401 agriculture", " forestry", " and fisheries", "Mathematical modeling", "Irrigation strategy", "HYDRUS", "Soil bacteria contamination", "GE Environmental Sciences", "General Environmental Science", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.eti.2023.103229"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Environmental%20Technology%20%26amp%3B%20Innovation", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.eti.2023.103229", "name": "item", "description": "10.1016/j.eti.2023.103229", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.eti.2023.103229"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-08-01T00:00:00Z"}}, {"id": "10.1002/ldr.3080", "type": "Feature", "geometry": null, "properties": {"updated": "2026-10-06T16:14:34Z", "type": "Journal Article", "created": "2018-07-04", "title": "A framework for scaling sustainable land management options", "description": "AbstractImprovements in land use and management are needed at a global scale to tackle interconnected global challenges of population growth, poverty, migration, climate change, biodiversity loss, and degrading land and water resources. There are hundreds of technical options for improving the sustainability of land management and preventing or reversing degradation, but there are many sociocultural, institutional, economic, and policy barriers hindering their adoption at large scale. To tackle this challenge, the Dryland Systems Program of the Consultative Group for International Agricultural Research and the UN Convention to Combat Desertification convened an expert group to consider barriers and incentives to scaling technologies, processes, policies, or institutional arrangements. The group reviewed existing frameworks for scaling sustainable land management (SLM) interventions across a range of contexts and identified eight critical actions for success: (a) plan iteratively; (b) consistently fund; (c) select SLM options for scaling based on best available evidence; (d) identify and engage with stakeholders at all scales; (e) build capacity for scaling; (f) foster institutional leadership and policy change to support scaling; (g) achieve early benefits and incentives for as many stakeholders as possible; and (h) monitor, evaluate, and communicate. Incentives for scaling were identified for the private sector, farmers and their communities, and policy makers. Based on these findings, a new action framework for scaling is presented that analyses the contexts where specific SLM interventions can be scaled, so that SLM options can be screened and adapted to these contexts, piloted and disseminated. The framework can help countries achieve land degradation neutrality.70%) in OC and total nitrogen (TN). Soil microbial respiration (SMR) also decreased significantly, following deforestation. Carbon, and N contents and population of fungi were significantly higher in all hillslope positions of the FO than the DEF. Changes in soil quality attributes were not significant in different slope positions of FO, which might be related to the stability of forest landscape. Effect of different slope positions on soil quality attributes was more pronounced in the DEF. The SH and BS were found as the most susceptible positions to erosion in DEF. Soils of the FO were mainly classified as Alfisols and Mollisols with evidences for clay illuviation compared to the weakly developed Inceptisols formed in the DEF. Micromorphological investigations revealed that the FO soils had strong granular and crumb microstructure with a high porosity indicating the presence of high amount of organic matter. The high microbial and faunal activity was confirmed through the presence of excremental pedofeatures in the topsoil of the FO. Lower organic matter and consequently microbial activity in the topsoil of the DEF have resulted in the massive microstructure with little porosity.", "keywords": ["2. Zero hunger", "Soil Science", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land", "551", "630"]}, "links": [{"href": "https://doi.org/10.1016/j.agee.2009.06.017"}, {"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.2009.06.017", "name": "item", "description": "10.1016/j.agee.2009.06.017", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.agee.2009.06.017"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2009-12-01T00:00:00Z"}}, {"id": "10.1002/ldr.2293", "type": "Feature", "geometry": null, "properties": {"updated": "2026-10-06T16:14:34Z", "type": "Journal Article", "created": "2014-05-22", "title": "Long-Term Tillage And Cropping System Effects On Chemical And Biochemical Characteristics Of Soil Organic Matter In A Mediterranean Semiarid Environment", "description": "Abstract
Several studies have reported how tillage and cropping systems affect quantity, quality, and distribution of soil organic matter (SOM) along the profile. However, the effect of soil management on the chemical structure of SOM and on its hydrophobic and hydrophilic components has been little investigated. In this work, the long\uffe2\uff80\uff90term (19\uffe2\uff80\uff89years) effects of two cropping systems (wheat monoculture and wheat/faba bean rotation) and three tillage managements (conventional, reduced, and no tillage) on some chemical characteristics of SOM and their relationships with labile carbon (C) pools were evaluated. Soil samples were taken from the topsoil (0\uffe2\uff80\uff9315\uffe2\uff80\uff89cm) of a Chromic Haploxerert (central Sicily, Italy). After 19\uffe2\uff80\uff89years of different tillage and cropping systems management, total organic C significantly differed among treatments with the labile organic C pools showing the greater amount in no till and in wheat/faba bean plots. Hydrophobic and hydrophilic components of SOM, determined by diffuse reflectance infrared Fourier transform spectroscopy, were mainly affected by cropping system, whereas aromatic components of SOM by tillage. Soil organic matter components and characteristics showed significant correlations with the soil biochemical parameters, confirming the expected synergism between chemical and biochemical properties. This study demonstrated that (i) no tillage and crop rotation improve the chemical and biochemical properties of SOM of Vertisols under semiarid environment; and (ii) tillage management and cropping systems have affected, after 19\uffe2\uff80\uff89years, more the chemical and biochemical properties of SOM than its quantity. Copyright \uffc2\uffa9 2014 John Wiley & Sons, Ltd.
", "keywords": ["2. Zero hunger", "3303 Development", "Soil Science", "04 agricultural and veterinary sciences", "15. Life on land", "Development", "6. Clean water", "2300 General Environmental Science", "10122 Institute of Geography", "13. Climate action", "2304 Environmental Chemistry", "Environmental Chemistry", "0401 agriculture", " forestry", " and fisheries", "910 Geography & travel", "1111 Soil Science", "General Environmental Science"]}, "links": [{"href": "https://doi.org/10.1002/ldr.2293"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Land%20Degradation%20%26amp%3B%20Development", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1002/ldr.2293", "name": "item", "description": "10.1002/ldr.2293", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1002/ldr.2293"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2014-06-11T00:00:00Z"}}, {"id": "10.1002/ece3.10086", "type": "Feature", "geometry": null, "properties": {"updated": "2026-10-06T16:14:29Z", "type": "Journal Article", "created": "2023-05-18", "title": "Fire severity as a key determinant of aboveground and belowground biological community recovery in managed even\u2010aged boreal forests", "description": "Abstract
Changes in fire regime of boreal forests in response to climate warming are expected to impact postfire recovery. However, quantitative data on how managed forests sustain and recover from recent fire disturbance are limited.
Two years after a large wildfire in managed even\uffe2\uff80\uff90aged boreal forests in Sweden, we investigated how recovery of aboveground and belowground communities, that is, understory vegetation and soil microbial and faunal communities, responded to variation in the severity of soil (i.e., consumption of soil organic matter) and canopy fires (i.e., tree mortality).
While fire overall enhanced diversity of understory vegetation through colonization of fire adapted plant species, it reduced the abundance and diversity of soil biota. We observed contrasting effects of tree\uffe2\uff80\uff90 and soil\uffe2\uff80\uff90related fire severity on survival and recovery of understory vegetation and soil biological communities. Severe fires that killed overstory Pinus sylvestris promoted a successional stage dominated by the mosses Ceratodon purpureus and Polytrichum juniperinum, but reduced regeneration of tree seedlings and disfavored the ericaceous dwarf\uffe2\uff80\uff90shrub Vaccinium vitis\uffe2\uff80\uff90idaea and the grass Deschampsia flexuosa. Moreover, high tree mortality from fire reduced fungal biomass and changed fungal community composition, in particular that of ectomycorrhizal fungi, and reduced the fungivorous soil Oribatida. In contrast, soil\uffe2\uff80\uff90related fire severity had little impact on vegetation composition, fungal communities, and soil animals. Bacterial communities responded to both tree\uffe2\uff80\uff90 and soil\uffe2\uff80\uff90related fire severity.
Synthesis: Our results 2\uffe2\uff80\uff89years postfire suggest that a change in fire regime from a historically low\uffe2\uff80\uff90severity ground fire regime, with fires that mainly burns into the soil organic layer, to a stand\uffe2\uff80\uff90replacing fire regime with a high degree of tree mortality, as may be expected with climate change, is likely to impact the short\uffe2\uff80\uff90term recovery of stand structure and above\uffe2\uff80\uff90 and belowground species composition of even\uffe2\uff80\uff90aged P.\uffe2\uff80\uff89sylvestris boreal forests.
tocm.tif), one for each layer; format is GeoTIFF, compatible with\u00a0convert_geotiff, a commandline utility for converting data from GeoTIFF to geogrid format used by WRF; 16 tiles, 8 for each layer, each covering 90 degrees by 90 degrees (SoilType_depthThe relationship between the spatial variability of soil multifunctionality (i.e., the capacity of soils to conduct multiple functions; SVM) and major climatic drivers, such as temperature and aridity, has never been assessed globally in terrestrial ecosystems. We surveyed 236 dryland ecosystems from six continents to evaluate the relative importance of aridity and mean annual temperature, and of other abiotic (e.g., texture) and biotic (e.g., plant cover) variables as drivers of SVM, calculated as the averaged coefficient of variation for multiple soil variables linked to nutrient stocks and cycling. We found that increases in temperature and aridity were globally correlated to increases in SVM. Some of these climatic effects on SVM were direct, but others were indirectly driven through reductions in the number of vegetation patches and increases in soil sand content. The predictive capacity of our structural equation\uffc2\uffa0modelling was clearly higher for the spatial variability of N\uffe2\uff80\uff90 than for C\uffe2\uff80\uff90 and P\uffe2\uff80\uff90related soil variables. In the case of N cycling, the effects of temperature and aridity were both direct and indirect via changes in soil properties. For C and P, the effect of climate was mainly indirect via changes in plant attributes. These results suggest that future changes in climate may decouple the spatial availability of these elements for plants and microbes in dryland soils. Our findings significantly advance our understanding of the patterns and mechanisms driving SVM in drylands across the globe, which is critical for predicting changes in ecosystem functioning in response to climate change.A calcareous and clayey xeric Chromic Haploxerept of a long\uffe2\uff80\uff90term experimental site in Sicily (Italy) was sampled (0\uffe2\uff80\uff9315\uffe2\uff80\uff89cm depth) under different land use management and cropping systems (CSs) to study their effect on soil aggregate stability and organic carbon (SOC). The experimental site had three tillage managements (no till [NT], dual\uffe2\uff80\uff90layer [DL] and conventional tillage [CT]) and two CSs (durum wheat monocropping [W] and durum wheat/faba bean rotation [WB]). The annually sequestered SOC with W was 2\uffc2\uffb775\uffe2\uff80\uff90times higher than with WB. SOC concentrations were also higher. Both NT and CT management systems were the most effective in SOC sequestration whereas with DL system no C was sequestered. The differences in SOC concentrations between NT and CT were surprisingly small. Cumulative C input of all cropping and tillage systems and the annually sequestered SOC indicated that a steady state occurred at a sequestration rate of 7\uffc2\uffb74\uffe2\uff80\uff89Mg\uffe2\uff80\uff89C\uffe2\uff80\uff89ha\uffe2\uff88\uff921\uffe2\uff80\uff89y\uffe2\uff88\uff921. Independent of the CSs, most of the SOC was stored in the silt and clay fraction. This fraction had a high N content which is typical for organic matter interacting with minerals. Macroaggregates (>250\uffe2\uff80\uff89\uffc2\uffb5m) and large microaggregates (75\uffe2\uff80\uff93250\uffe2\uff80\uff89\uffc2\uffb5m) were influenced by the treatments whereas the finest fractions were not. DL reduced the SOC in macroaggregates while NT and CT gave rise to higher SOC contents. In Mediterranean areas with Vertisols, agricultural strategies aimed at increasing the SOC contents should probably consider enhancing the proportion of coarser soil fractions so that, in the short\uffe2\uff80\uff90term, organic C can be accumulated. Copyright \uffc2\uffa9 2010 John Wiley & Sons, Ltd.
", "keywords": ["2300 General Environmental Science", "2. Zero hunger", "10122 Institute of Geography", "3303 Development", "2304 Environmental Chemistry", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "910 Geography & travel", "15. Life on land", "1111 Soil Science"]}, "links": [{"href": "https://doi.org/10.1002/ldr.1055"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Land%20Degradation%20%26amp%3B%20Development", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1002/ldr.1055", "name": "item", "description": "10.1002/ldr.1055", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1002/ldr.1055"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2010-10-14T00:00:00Z"}}, {"id": "10.1111/ejss.13455", "type": "Feature", "geometry": null, "properties": {"updated": "2026-10-06T16:17:59Z", "type": "Journal Article", "created": "2024-03-11", "title": "Interactions between soil structure dynamics, hydrological processes, and organic matter cycling: A new soil\u2010crop model", "description": "AbstractThe structure of soil is critical for the ecosystem services it provides since it regulates many key soil processes, including water, air and solute movement, root growth and the activity of soil biota. Soil structure is dynamic, driven by external factors such as land management and climate and mediated by a wide range of biological agents and physical processes operating at strongly contrasting time\uffe2\uff80\uff90scales, from seconds (e.g., tillage) to many decades (e.g., faunal activity and soil aggregation). In this respect, positive feedbacks in the soil\uffe2\uff80\uff93plant system may lead in the longer term to soil physical degradation or to the recovery of structurally poor soils. As far as we are aware, no existing soil\uffe2\uff80\uff90crop model can account for such processes. In this paper, we describe a new soil\uffe2\uff80\uff90crop model (USSF, Uppsala model of Soil Structure and Function) that accounts for the effects of soil structure dynamics on water and organic matter cycling at the soil profile scale. Soil structure dynamics are expressed as time\uffe2\uff80\uff90varying physical (bulk density, porosity) and hydraulic properties (water retention, hydraulic conductivity) responding to the activity of biological agents (i.e., earthworms, plant roots) and physical processes (i.e., tillage, soil swell\uffe2\uff80\uff90shrink) at seasonal to decadal time\uffe2\uff80\uff90scales. In this first application of the model, we present the results of 30\uffe2\uff80\uff90year scenario simulations that illustrate the potential role and importance of soil structure dynamics for the soil water balance, carbon storage in soil, root growth, and winter wheat yields on two soils (loam and clay) in the climate of central Sweden. A sensitivity analysis was also performed for these two scenarios using the Morris method of elementary effects, which revealed that the most sensitive parameters controlling soil structure dynamics in the USSF model are those determining aggregation induced by organic matter turnover and swell/shrink. We suggest that the USSF model is a promising new tool to investigate a wide range of processes and phenomena triggered by land use and climate change. Results from this study show that feedback in the soil\uffe2\uff80\uff90crop system mediated by the dynamics of soil physical and hydraulic properties are potentially of central importance for long\uffe2\uff80\uff90term predictions of soil water balance, crop production, and carbon sequestration under global change.Conservation agriculture practices have been proposed as a set of techniques for improving soil structure properties and related ecosystem services. This study compared conservation agriculture (CA) practices (no\uffe2\uff80\uff90tillage, cover crop and residue retention) and conventional intensive tillage system in order to evaluate their effects on total porosity, pore size distribution, pore architecture and morphology. The experiment was set up in 2010 on four farms of the low\uffe2\uff80\uff90lying Veneto Region plain characterized by silty soils. Almost hundred soil samples were collected in 2015 at four depths down to 50\uffe2\uff80\uff90cm layer and investigated for porosity from micrometre (0\uffc2\uffb70074\uffc2\uffa0\uffce\uffbcm) to macrometre (2\uffc2\uffb75\uffc2\uffa0mm) by coupling mercury intrusion porosimetry and X\uffe2\uff80\uff90ray computed microtomography (\uffce\uffbcCT). Indices of soil morphology and architecture were derived by analysing 3D images and mercury intrusion porosimetry pore size curves. Results suggested that silty soils of Veneto plain are microstructured because much (82%) of the porosity ranged between 0\uffc2\uffb70074 and 30\uffc2\uffa0\uffce\uffbcm. CA practices positively influenced the ultramicroporosity class (0\uffc2\uffb71\uffe2\uff80\uff935\uffc2\uffa0\uffce\uffbcm) (1\uffc2\uffb786E\uffe2\uff80\uff9001 vs 1\uffc2\uffb767E\uffe2\uff80\uff9001\uffc2\uffa0\uffce\uffbcm3\uffc2\uffa0\uffce\uffbcm\uffe2\uff88\uff923) that is strictly linked to soil organic carbon stabilization while no effects were observed in X\uffe2\uff80\uff90ray \uffce\uffbcCT porosity domain (> 26\uffc2\uffa0\uffce\uffbcm). Silty soils of Veneto plain showed a slow reaction to CA because of the poor aggregate stability and low soil organic carbon. However, the positive response of the ultramicropore fraction indicates that a virtuous cycle was initiated between soil organic carbon and porosity, hopefully leading to well\uffe2\uff80\uff90developed macropore systems and, in turn, enhanced soil functions and ecosystem services. Copyright \uffc2\uffa9 2017 John Wiley & Sons, Ltd.
", "keywords": ["2. Zero hunger", "Conservation agriculture; Mercury intrusion porosimetry; Pore morphology and architecture; Pore size distribution; X-ray computed microtomography; Environmental Chemistry; Development3304 Education; 2300; Soil Science", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land"]}, "links": [{"href": "https://doi.org/10.1002/ldr.2726"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Land%20Degradation%20%26amp%3B%20Development", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1002/ldr.2726", "name": "item", "description": "10.1002/ldr.2726", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1002/ldr.2726"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-05-12T00:00:00Z"}}, {"id": "10.1016/j.agee.2015.02.001", "type": "Feature", "geometry": null, "properties": {"updated": "2026-10-06T16:15:31Z", "type": "Journal Article", "created": "2015-02-14", "title": "Surface Organic Carbon Enrichment To Explain Greater Co2 Emissions From Short-Term No-Tilled Soils", "description": "The impact of agricultural practices on CO2 emissions from soils needs to be understood and quantified to enhance ecosystem functions, especially the ability of soils to sequester atmospheric carbon (C), while enhancing food and biomass production. The objective of this study was to assess CO2 emissions in the soil surface following tillage abandonment and to investigate some of the underlying soil physical, chemical and biological controls. Maize (Zea mays) was planted under conventional tillage (T) and no-tillage (NT), both without crop residues under smallholder farming conditions in Potshini, South Africa. Intact top-soil (0\u20130.05 m) core samples (N = 54) from three 5 \u00d7 15 m2 plots per treatment were collected two years after conversion of T to NT to evaluate the short-term CO2 emissions. Depending on the treatment, cores were left intact, compacted by 5 and 10 or had surface crusts removed. They were incubated for 20 days with measurements of CO2 fluxes twice a day during the first three days and once a day thereafter. Soil organic C (SOC) content, soil bulk density (\u03c1b), aggregate stability, soil organic matter quality, and microbial biomass and its activity were evaluated at the onset of the incubation. CO2 emissions were 22% lower under NT compared with T with CO2 emissions of 0.9 \u00b1 0.10 vs 1.1 \u00b1 0.10 mg C\u2013CO2 gC\u22121 day\u22121 under NT and T, respectively, suggesting greater SOC protection under NT. However, there were greater total CO2 emissions per unit of surface by 9% under NT compared to T (1.15 \u00b1 0.03 vs 1.05 \u00b1 0.04 g C\u2013CO2 m\u22122 day\u22121). SOC protection significantly increased with the increase in soil bulk density (r = 0.89) and aggregate stability (from 1.7 \u00b1 0.25 mm to 2.3 \u00b1 0.31, r = 0.50), and to the decrease in microbial biomass and its activity (r = \u22120.59 and \u22120.57, respectively). In contrast, the greater NT CO2 emissions per m2 were explained by top-soil enrichment in SOC by 48% (from 12.4 \u00b1 0.2 to 19.1 \u00b1 0.4 g kg\u22121, r = 0.59). These results on the soil controls of tillage impact on CO2 emissions are expected to inform on the required shifts in agricultural practices for enhancing C sequestration in soils. In the context of the study, any mechanism favoring aggregate stability and promoting SOC allocation deep in the soil profile rather than in the top-soil would greatly diminish soil CO2 outputs and thus stimulate C sequestration.", "keywords": ["550", "non travail du sol", "ma\u00efs", "No-tillage", "no-tillage", "[SDU.STU]Sciences of the Universe [physics]/Earth Sciences", "Soil Science", "maize", "7. Clean energy", "630", "Sciences de la Terre", "dioxyde de carbone", "non labour", "Climate change", "propri\u00e9t\u00e9 du sol", "2. Zero hunger", "changement climatique", "carbon dioxide", "04 agricultural and veterinary sciences", "15. Life on land", "No-tillage;Carbon dioxide;Climate change;Maize;Small holders;Africa", "6. Clean water", "Maize", "climate change", "Small holders", "Carbon dioxide", "13. Climate action", "\u00e9mission d'azote", "Africa", "8. Economic growth", "[SDU.STU] Sciences of the Universe [physics]/Earth Sciences", "Earth Sciences", "0401 agriculture", " forestry", " and fisheries", "afrique du sud", "small holders", "azote du sol"]}, "links": [{"href": "https://doi.org/10.1016/j.agee.2015.02.001"}, {"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.2015.02.001", "name": "item", "description": "10.1016/j.agee.2015.02.001", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.agee.2015.02.001"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2015-05-01T00:00:00Z"}}, {"id": "10.1007%2fs00374-010-0497-1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-10-06T16:14:37Z", "type": "Journal Article", "created": "2010-09-03", "title": "Crop Residues And Fertilizer Nitrogen Influence Residue Decomposition And Nitrous Oxide Emission From A Vertisol", "description": "Crop residues with high C/N ratio immobilize N released during decomposition in soil, thus reducing N losses through leaching, denitrification, and nitrous oxide (N2O) emission. A laboratory incubation experiment was conducted for 84\u00a0days under controlled conditions (24\u00b0C and moisture content 55% of water-holding capacity) to study the influence of sugarcane, maize, sorghum, cotton and lucerne residues, and mineral N addition, on N mineralization\u2013immobilization and N2O emission. Residues were added at the rate of 3\u00a0t C ha\u22121 to soil with, and without, 150\u00a0kg urea N\u00a0ha\u22121. The addition of sugarcane, maize, and sorghum residues without N fertilizer resulted in a significant immobilization of soil N. Amended soil had significantly (P\u2009<\u20090.05) lower NO 3 \u2212 \u2013N, which reached minimum values of 2.8\u00a0mg\u00a0N kg\u22121 for sugarcane (at day\u00a028), 10.3\u00a0mg\u00a0N kg\u22121 for maize (day\u00a07), and 5.9\u00a0mg\u00a0N kg\u22121 for sorghum (day\u00a07), compared to 22.7\u00a0mg\u00a0N kg\u22121 for the unamended soil (day\u00a07). During 84\u00a0days of incubation, the total mineral N in the residues\u2009+\u2009N treatments were decreased by 45\u00a0mg\u00a0N kg\u22121 in sugarcane, 34\u00a0mg\u00a0kg\u22121 in maize, 29\u00a0mg\u00a0kg\u22121 in sorghum, and 16\u00a0mg\u00a0kg\u22121 in cotton amended soil compared to soil\u2009+\u2009N fertilizer, although soil NO 3 \u2212 \u2013N increased by 7\u00a0mg\u00a0kg\u22121 in lucerne amended soil. The addition of residues also significantly increased amended soil microbial biomass C and N. Maximum emissions of N2O from crop residue amended soils occurred in the first 4\u20135\u00a0days of incubation. Overall, after 84\u00a0days of incubation, the cumulative N2O emission was 25% lower with cotton\u2009+\u2009N fertilizer, compared to soil\u2009+\u2009N fertilizer. The cumulative N2O emission was significantly and positively correlated with NO 3 \u2212 \u2013N (r\u2009=\u20090.92, P\u2009<\u20090.01) and total mineral N (r\u2009=\u20090.93, P\u2009<\u20090.01) after 84\u00a0days of incubation, and had a weak but significant positive correlation with cumulative CO2 in the first 3 and 5\u00a0days of incubation (r\u2009=\u20090.59, P\u2009<\u20090.05).", "keywords": ["2. Zero hunger", "Crop residues", "Nitrous oxide", "571", "2404 Microbiology", "Vertisol", "04 agricultural and veterinary sciences", "15. Life on land", "630", "6. Clean water", "Mineral N", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "1102 Agronomy and Crop Science", "1111 Soil Science", "Fertilizer N"], "contacts": [{"organization": "Muhammad, W, Vaughan, SM, Dalal, RC, Menzies, NW,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1007%2fs00374-010-0497-1"}, {"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%2fs00374-010-0497-1", "name": "item", "description": "10.1007%2fs00374-010-0497-1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007%2fs00374-010-0497-1"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2010-09-04T00:00:00Z"}}, {"id": "10.1007/978-94-011-3252-7_20", "type": "Feature", "geometry": null, "properties": {"updated": "2026-10-06T16:14:38Z", "type": "Journal Article", "created": "2006-04-09", "title": "Changes In Soil Properties And Site Productivity Caused By Red Alder", "description": "Red alder (Alnus rubra Bong.) is well recognized as an effective host plant for the symbiotic fixation of N. While this fixation process leads to the rapid accumulation of N within the ecosystem, it also enhances nutrient accumulation in biomass and soil organic matter and increases nitrification and cation leaching. We hypothesized that changes in soil properties resulting from these processes would decrease site productivity for second rotation red alder. Adjacent stands of 55 yr old alder and Douglas fir (Pseudotsuga menziesii [Mirb.] Franco) were studied at the Thompson Research Center on the Cedar River Watershed in western Washington, USA. The presence of red alder caused the following soil changes: decreased soil solution pH, increased CEC, increased exchangeable acidity accompanied by a decreased soil pH and base saturation. This decreased soil and soil solution pH resulted in increased Al concentration in the soil solution and on exchange sites as well as decreased P availability. To determine the effect of these changes on the productivity of the 2nd rotation alder forest, a species conversion experiment was initiated 5 yr ago. Results from this conversion study clearly indicated that the first rotation red alder forest has caused a relative decrease in the productivity of the second rotation red alder plantation. Compared to the growth of red alder on the former Douglas fir site, the second rotation red alder on the former red alder site exhibited 33% less height growth and 75% less aboveground biomass accumulation after 5 yr. Future research will focus on identifying those factors causing this lower productivity including P availability, soil acidity and Al toxicity, cation availability, and competition with other vegetation.", "keywords": ["site productivity", "soil properties", "changes", "Soil Science", "0401 agriculture", " forestry", " and fisheries", "red alder", "04 agricultural and veterinary sciences", "15. Life on land", "Forest Sciences", "Environmental Sciences"]}, "links": [{"href": "https://doi.org/10.1007/978-94-011-3252-7_20"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Water%2C%20Air%2C%20and%20Soil%20Pollution", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/978-94-011-3252-7_20", "name": "item", "description": "10.1007/978-94-011-3252-7_20", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/978-94-011-3252-7_20"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "1990-03-01T00:00:00Z"}}, {"id": "10.1016/j.agee.2007.08.005", "type": "Feature", "geometry": null, "properties": {"updated": "2026-10-06T16:15:26Z", "type": "Journal Article", "created": "2007-09-22", "title": "Cattle Manure And Grass Residues As Liming Materials In A Semi-Subsistence Farming System", "description": "Abstract A field experiment was conducted on an acid soil in a semi-subsistence farming area of KwaZulu-Natal, South Africa to investigate the possibility of using organic amendments as liming materials within a minimum tillage (strip cultivation) system to produce maize. Amendments (cattle manure, grass residues and dolomitic lime) were incorporated to a depth of 20\u00a0cm in bands 15\u00a0cm wide down plant rows at rates of 10 and 20\u00a0t\u00a0ha \u22121 (in the amended area) for organic materials and 2.5 and 5.0\u00a0t\u00a0ha \u22121 for lime. The remainder of the field remained untilled. Additions of cattle manure rapidly increased soil pH, and concentrations of exchangeable K, Ca and Mg and extractable P were also greatly elevated. Grass residue additions increased pH progressively and increased exchangeable K and Mg and those of dolomitic lime increased pH, exchangeable Ca and Mg. Addition of each of the amendments decreased concentrations of exchangeable Al; the effect was greatest for animal manure after 6 weeks and for lime and grass residues at harvest. At harvest, addition of all three amendments had significantly reduced concentrations of both phytotoxic monomeric and total Al in soil solution. The system not only resulted in an increase in pH and extractable nutrients in row soil compared to that in the inter-row but also an increase in the size and activity of the soil microbial community. Maize yields were increased by additions of amendments under both unfertilised and fertilised conditions and yields were generally greatest at the higher rate of addition. Under unfertilised conditions, cattle manure treatments gave the greatest yields. Fertiliser additions increased yields greatly particularly in the control, grass residue and lime treatments. It was concluded that the strip tillage system used is a practicable way of applying high rates of organic materials to soils, that cattle manure has a rapid liming effect as well as being a nutrient source and that grass residues from rangeland decompose slowly and, therefore, have a slow liming effect.", "keywords": ["0106 biological sciences", "2. Zero hunger", "Soil acidity", "Lime", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "630", "Strip tillage", "050304 Soil Chemistry (excl. Carbon Sequestration Science)", "0401 agriculture", " forestry", " and fisheries", "0503 Soil Sciences", "CX", "9614 Soils", "Organic amendments"]}, "links": [{"href": "https://doi.org/10.1016/j.agee.2007.08.005"}, {"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.2007.08.005", "name": "item", "description": "10.1016/j.agee.2007.08.005", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.agee.2007.08.005"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2008-03-01T00:00:00Z"}}, {"id": "10.1016/j.eja.2020.126198", "type": "Feature", "geometry": null, "properties": {"updated": "2026-10-06T16:15:58Z", "type": "Journal Article", "created": "2020-11-27", "title": "Soil management in semi-arid vineyards: Combined effects of organic mulching and no-tillage under different water regimes", "description": "Optimizing water use in vineyards is crucial for ensuring the sustainability of viticulture in semi-arid regions, and this may be achieved by minimizing direct water evaporation from the soil through the use of mulching. In this context, the current study aimed at assessing the combined effects of the vine-row application of an organic mulch (vine prunings) and no-tillage under two water regimes on soil properties, plant water and nutritional status, yield and must composition of grapevine (Vitis vinifera L.) cv. Bobal grown under semi-arid conditions. For this purpose, a field experiment in a split-plot design was carried out for three years (2016\u20132018) in a mature Bobal vineyard located in Eastern Spain. Two soil management strategies (tillage and organic mulching with no-tillage) were assessed under two water regimes (rainfed and deficit drip irrigation) with four replications per combination. Vine responses were determined by measuring midday stem water potential, leaf nutrient concentrations, pruning weight, yield components and grape composition. Soil properties were assessed at the end of the experiment. Mulching and no-tillage positively affected vine water status under both water regimes, resulting in reductions in grape phenolic composition. Interactive effects of both water regime and soil management on water use efficiency were found. Regardless of soil management practice, irrigation increased yield and pruning weight when compared to rainfed conditions. Soil management had slight effects on vine nutritional status. At the end of the experiment, soil compaction increased and infiltration decreased as a consequence of mulching and no-tillage. Organic mulch and no-tillage improved vine water status, however, considering the final soil surface compaction and low water infiltration rate, longer-term studies are necessary to assess the sustainability of combining both practices.", "keywords": ["2. Zero hunger", "0106 biological sciences", "Soil management", "sustainable viticulture", "04 agricultural and veterinary sciences", "15. Life on land", "F06 Irrigation", "01 natural sciences", "6. Clean water", "P11 Drainage", "Vitis vinifera L.", "Water relations", "Vitis vinifera", "Drip irrigation", "P30 Soil science and management", "0401 agriculture", " forestry", " and fisheries", "Sustainable viticulture"]}, "links": [{"href": "https://doi.org/10.1016/j.eja.2020.126198"}, {"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.2020.126198", "name": "item", "description": "10.1016/j.eja.2020.126198", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.eja.2020.126198"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-02-01T00:00:00Z"}}, {"id": "10.1007/s00248-018-1305-y", "type": "Feature", "geometry": null, "properties": {"updated": "2026-10-06T16:14:44Z", "type": "Journal Article", "created": "2018-12-08", "title": "Soil Type and Cyanobacteria Species Influence the Macromolecular and Chemical Characteristics of the Polysaccharidic Matrix in Induced Biocrusts", "description": "Inoculation of soils with cyanobacteria is proposed as a sustainable biotechnological technique for restoration of degraded areas in drylands due to the important role that cyanobacteria and their exopolysaccharides (EPS) play in the environment. So far, few studies have analyzed the macromolecular and chemical characteristics of the polysaccharidic matrix in induced cyanobacterial biocrusts and the scarce existing studies have mainly focused on sandy soil textures. However, the characteristics of the cyanobacterial polysaccharidic matrix may greatly depend on soil type. The objective of this study was to examine the macromolecular distribution and monosaccharidic composition of the polysaccharidic matrix induced by inoculation of two cyanobacterial species common in arid environments, Phormidium ambiguum (non N-fixing) and Scytonema javanicum (N-fixing) in different soil types. S. javanicum promoted a higher release in the soil of the more soluble and less condensed EPS fraction (i.e., the loosely bound EPS fraction, LB-EPS), while P. ambiguum showed a higher release of the less soluble and more condensed EPS fraction (i.e., the tightly bound EPS fraction, TB-EPS). LB-EPSs were mainly composed of low MW molecules (<\u200950\u00a0kDa), while TB-EPSs were mainly composed of high MW molecules (1100-2000\u00a0kDa). The two EPS fractions showed a complex monosaccharidic composition (from 11 to 12 different types of monosaccharides), with glucose as the most abundant monosaccharide, in particular in the poorer soils characterized by lower organic C contents. In more C-rich soils, high abundances of galactose, mannose, and xylose were also found. Low abundance of uronic acids and hydrophobic monosaccharides, such as fucose and rhamnose, was found in the EPS extracted from the inoculated soils. Our results point to the influence of soil type on the macromolecular distribution and monosaccharide composition of the polysaccharidic matrix in induced biocrusts, which is likely to affect biocrust development and their role in soil structure and nutrient cycling in restored dryland soils.", "keywords": ["0301 basic medicine", "2. Zero hunger", "0303 health sciences", "Cyanobacteria inoculation", "Tightly bound EPS", "Polysaccharides", " Bacterial", "Biological soil crust; Cyanobacteria inoculation; Loosely bound EPS; Molecular weight; Monosaccharide composition; Tightly bound EPS; Ecology; Evolution; Behavior and Systematics; Ecology; Soil Science", "Biological soil crust", "Monosaccharide composition", "15. Life on land", "Cyanobacteria", "Molecular weight", "Biological soil crust; Cyanobacteria inoculation; Loosely bound EPS; Molecular weight; Monosaccharide composition; Tightly bound EPS; Ecology", " Evolution", " Behavior and Systematics; Ecology; Soil Science", "Soil", "03 medical and health sciences", "13. Climate action", "Loosely bound EPS", "Desert Climate", "Soil Microbiology"]}, "links": [{"href": "https://iris.unive.it/bitstream/10278/5089943/1/s00248-018-1305-y.pdf"}, {"href": "http://link.springer.com/content/pdf/10.1007/s00248-018-1305-y.pdf"}, {"href": "https://doi.org/10.1007/s00248-018-1305-y"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Microbial%20Ecology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s00248-018-1305-y", "name": "item", "description": "10.1007/s00248-018-1305-y", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s00248-018-1305-y"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-12-08T00:00:00Z"}}, {"id": "10.1007/s00271-005-0026-4", "type": "Feature", "geometry": null, "properties": {"updated": "2026-10-06T16:14:45Z", "type": "Journal Article", "created": "2006-01-04", "title": "Comparison Of Irrigation Strategies For Surface-Irrigated Corn In West Central Nebraska", "description": "Many farmers in West Central Nebraska have limited irrigation water supplies, and need to produce crops with less water. This study evaluated the impact of four water management strategies on grain yield of surface-irrigated corn (Zea mays L.) at North Platte, Nebraska. Treatments included: (1) no irrigation (DRYLAND), (2) one irrigation prior to tassel formation (EARLY), (3) one irrigation during the silk stage (LATE), and (4) irrigation following farmer\u2019s practices (FARMER). The study included three wet years (1992, 1993, and 1996) and 2 years with average annual rainfall for the area (1994 and 1995). Significant yield differences among treatments, and a yield response to irrigation, were only observed during the 2 years with average rainfall. During all years, the FARMER treatment was over-irrigated and resulted in considerable water losses by runoff and deep percolation. Grain yield response to irrigation during the three wet years was insignificant among the treatments, but significant during the dry years. The results of this study suggest that inducing stress is not a good strategy for increasing crop water productivity (yield per unit ETd) for corn and point out the need to minimize irrigation water losses and improve irrigation scheduling.", "keywords": ["2. Zero hunger", "0106 biological sciences", "571", "Soil Science", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "6. Clean water", "2312 Water Science and Technology", "0401 agriculture", " forestry", " and fisheries", "1102 Agronomy and Crop Science", "Agronomy and Crop Science", "1111 Soil Science", "Water Science and Technology"], "contacts": [{"organization": "Payero, Jose O., Klocke, Norman L., Schneekloth, Joel P., Davison, Don R.,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1007/s00271-005-0026-4"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Irrigation%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s00271-005-0026-4", "name": "item", "description": "10.1007/s00271-005-0026-4", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s00271-005-0026-4"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2006-01-05T00:00:00Z"}}, {"id": "10.1111/ejss.13570", "type": "Feature", "geometry": null, "properties": {"updated": "2026-10-06T16:17:59Z", "type": "Journal Article", "created": "2024-09-17", "title": "Five decades' experience of long\u2010term soil monitoring, and key design principles, to assist the EU soil health mission", "description": "AbstractThe European Union has a long\uffe2\uff80\uff90term objective to achieve healthy soils by 2050. The European Commission has proposed a Directive of the European Parliament and of the Council on Soil Monitoring and Resilience (Soil Monitoring Law, SML), the first stage of which is to focus on setting up a soil monitoring framework and assessing soils throughout the EU. Situated in NW Europe, the UK has substantial experience in soil monitoring over the last half century which may usefully contribute to this wider EU effort. A set of overarching principles have and continue to guide design of national soil monitoring and may prove helpful as other European countries embark on similar monitoring programmes. Therefore, we present the principles of design from five decades of national soil monitoring. The monitoring discussed is based on a stratified\uffe2\uff80\uff90random design, has matured in support of policy questions, and operates over space and time scales relevant to the SML. The UK Centre for Ecology & Hydrology (UKCEH) Countryside Surveys (CS) of Great Britain and Northern Ireland,\uffc2\uffa0Welsh Government, Environment and Rural Affairs Monitoring and Modelling Programme (ERAMMP) and the England Ecosystem Survey (EES) monitoring programme are national programmes currently operating in the UK. Some important lessons learnt include: adopting a question\uffe2\uff80\uff90based approach; having a clear robust statistical design for the purpose; selecting indicators that address policy and underlying scientific questions; and selecting indicators that can detect change and use robust and well\uffe2\uff80\uff90tested methodologies across a wide range of soil and land use types, remaining valid over long time scales, supporting thinking long\uffe2\uff80\uff90term. Technical lessons learned include the proven cost effectiveness of a stratified\uffe2\uff80\uff90random design including replication, while adopting a common stratification layer of stable environmental attributes aids comparability between monitoring programmes. Common protocols are vital for future intercomparisons, but a full ecosystem approach that includes co\uffe2\uff80\uff90located soil and vegetation samples for interpreting a co\uffe2\uff80\uff90evolving system has proved hugely advantageous. UK monitoring programmes offer a range of experience that may prove valuable to future soil monitoring design to address the major societal challenges of our time, such as maintaining food production and addressing climate change and biodiversity loss.Phosphorus (P) is one of the most important elements for soil biology and biogeochemistry worldwide. Yet, despite decades of research, important uncertainties persist about the drivers and changes in soil P forms during long-term soil formation. Here, we analyzed topsoils from nine globally distributed retrogressive soil chronosequences aiming to evaluate the relative contribution of key environmental factors (that is, soil age, substrate origin, climate, soil attributes, and vegetation) in explaining the long-term dynamics of primary, occluded, non-occluded, organic, and total P across different terrestrial ecosystems. We found that, rather than soil age, substrate origin was the main driver controlling the fate of different P fractions across contrasting environmental conditions. Moreover, our findings suggest that temporal patterns governing the long-term dynamics of different P forms as soils develop are not consistent among soil chronosequences, which is a result of contrasting environmental conditions, especially substrate origin. We further showed that topsoil total P was the greatest at intermediate soil development stage across the globe. Lastly, our results showed that P fractions were highly correlated with multiple surrogates of ecosystem services, such as carbon sequestration, plant productivity, and biodiversity. Together, our work provides new insights into the natural history of P availability, and further highlights that substrate origin, rather than soil age, is essential to predict changes in P availability in response to physical perturbation and climate change.Quantifying the upper limit of stable soil carbon storage is essential for guiding policies to increase soil carbon storage. One pool of carbon considered particularly stable across climate zones and soil types is formed when dissolved organic carbon sorbs to minerals. We quantified, for the first time, the potential of mineral soils to sorb additional dissolved organic carbon (DOC) for six soil orders. We compiled 402 laboratory sorption experiments to estimate the additional DOC sorption potential, that is the potential of excess DOC sorption in addition to the existing background level already sorbed in each soil sample. We estimated this potential using gridded climate and soil geochemical variables within a machine learning model. We find that mid- and low-latitude soils and subsoils have a greater capacity to store DOC by sorption compared to high-latitude soils and topsoils. The global additional DOC sorption potential for six soil orders is estimated to be 107 $$ pm$$ \uffc2\uffb1 13 Pg C to 1\uffc2\uffa0m depth. If this potential was realized, it would represent a 7% increase in the existing total carbon stock.Establishing parkland agroforestry on currently treeless cropland in the West African Sahel may help mitigate climate change. To evaluate its potential, we used climatically suitable ranges for parklands for 19 climate scenarios, derived by ecological niche modeling, for estimating potential carbon stocks in parkland and treeless cropland. A biocarbon business model was used to evaluate profitability of hypothetical Terrestrial Carbon Projects (TCPs), across a range of farm sizes, farm numbers, carbon prices and benefit sharing mechanisms. Using climate analogues, we explored potential climate change trajectories for selected locations. If mature parklands covered their maximum range, carbon stocks in Sahelian productive land would be about 1,284\uffc2\uffa0Tg, compared to 725\uffc2\uffa0Tg in a treeless scenario. Due to slow increase rates of total system carbon by 0.4\uffc2\uffa0Mg\uffc2\uffa0C\uffc2\uffa0ha\uffe2\uff88\uff921 a\uffe2\uff88\uff921, most TCPs at carbon prices that seem realistic today were not feasible, or required the participation of large numbers of farmers. For small farms, few TCP scenarios were feasible, and low Net Present Values for farmers made it unlikely that carbon payments would motivate many to participate in TCPs, unless additional benefits were provided. Climate analogue locations indicated an uncertain climate trajectory for the Sahel, but most scenarios projected increasing aridity and reduced suitability for parklands. The potentially severe impacts of climate change on Sahelian ecosystems and the uncertain profitability of TCPs make the Sahel highly risky for carbon investments. Given the likelihood of degrading environmental conditions, the search for appropriate adaptation strategies should take precedence over promoting mitigation activities.
", "keywords": ["Carbon sequestration", "Carbon accounting", "Atmospheric Science", "Adaptation to Climate Change in Agriculture", "Economics", "Profitability index", "7. Clean energy", "01 natural sciences", "agroforestry", "Agricultural and Biological Sciences", "Climate change mitigation", "Range (aeronautics)", "Rangeland Degradation", "Natural resource economics", "Soil water", "11. Sustainability", "Rangeland Degradation and Pastoral Livelihoods", "Carbon fibers", "Climate change", "Business", "agriculture", "2. Zero hunger", "Global and Planetary Change", "Ecology", "Life Sciences", "Composite number", "04 agricultural and veterinary sciences", "Soil carbon", "Physical Sciences", "Composite material", "Atmospheric carbon cycle", "Management", " Monitoring", " Policy and Law", "Greenhouse gas", "Environmental science", "Global Forest Transition", "Agroforestry", "climate", "Biology", "Ecology", " Evolution", " Behavior and Systematics", "Ecosystem", "0105 earth and related environmental sciences", "Soil science", "15. Life on land", "carbon sequestration", "Materials science", "Carbon dioxide", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "0401 agriculture", " forestry", " and fisheries", "Drivers and Impacts of Tropical Deforestation", "Finance"]}, "links": [{"href": "https://doi.org/10.1007/s10584-012-0438-0"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Climatic%20Change", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s10584-012-0438-0", "name": "item", "description": "10.1007/s10584-012-0438-0", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s10584-012-0438-0"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2012-03-28T00:00:00Z"}}, {"id": "10.1007/s10661-023-11079-y", "type": "Feature", "geometry": null, "properties": {"updated": "2026-10-06T16:15:02Z", "type": "Journal Article", "created": "2023-03-25", "title": "Evaluating the impacts of sustainable land management practices on water quality in an agricultural catchment in Lower Austria using SWAT", "description": "AbstractManaging agricultural watersheds in an environmentally friendly manner necessitate the strategic implementation of well-targeted sustainable land management (SLM) practices that limit soil and nonpoint source pollution losses and translocation. Watershed-scale SLM-scenario modeling has the potential to identify efficient and effective management strategies from the field to the integrated landscape level. In a case study targeting a 66-hectare watershed in Petzenkirchen, Lower Austria, the Soil and Water Assessment Tool (SWAT) was utilized to evaluate a variety of locally adoptable SLM practices. SWAT was calibrated and validated (monthly) at the catchment outlet for flow, sediment, nitrate-nitrogen (NO3\uffe2\uff80\uff93N), ammonium nitrogen (NH4\uffe2\uff80\uff93N), and mineralized phosphorus (PO4\uffe2\uff80\uff93P) using SWATplusR. Considering the locally existing agricultural practices and socioeconomic and environmental factors of the research area, four conservation practices were evaluated: baseline scenario, contour farming (CF), winter cover crops (CC), and a combination of no-till and cover crops (NT\uffe2\uff80\uff89+\uffe2\uff80\uff89CC). The NT\uffe2\uff80\uff89+\uffe2\uff80\uff89CC SLM practice was found to be the most effective soil conservation practice in reducing soil loss by around 80%, whereas CF obtained the best results for decreasing the nutrient loads of NO3\uffe2\uff80\uff93N and PO4\uffe2\uff80\uff93P by 11% and 35%, respectively. The findings of this study imply that the setup SWAT model can serve the context-specific performance assessment and eventual promotion of SLM interventions that mitigate on-site land degradation and the consequential off-site environmental pollution resulting from agricultural nonpoint sources.