{"type": "FeatureCollection", "features": [{"id": "10.1016/j.pedobi.2010.03.002", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-05-01T16:16:40Z", "type": "Journal Article", "created": "2010-04-05", "title": "Earthworm Impacts On Soil Organic Matter And Fertilizer Dynamics In Tropical Hillside Agroecosystems Of Honduras", "description": "Abstract   Earthworms are important processors of soil organic matter (SOM) and nutrient turnover in terrestrial ecosystems. In agroecosystems, they are often seen as beneficial organisms to crop growth and are actively promoted by farmers and extension agents, yet their contribution to agroecosystem services is uncertain and depends largely on management. The Quesungual slash-and-mulch agroforestry system (QSMAS) of western Honduras has been proposed as a viable alternative to traditional slash-and-burn (SB) practices and has been shown to increase earthworm populations, yet the effect of earthworms on soil fertility and SOM in QSMAS is poorly understood. This study examined the role of Pontoscolex corethrurus in QSMAS by comparing their influence on aggregate-associated SOM and fertilizer dynamics with their effects under SB and secondary forest in a replicated field trial. Both the fertilized QSMAS and SB treatments had plots receiving additions of inorganic 15N and P, as well as plots with no inorganic N additions. Earthworm populations were manipulated in field microcosms at the beginning of the rainy season within each management treatment via additions of P. corethrurus or complete removal of existing earthworm populations. Microcosms were destructively sampled at harvest of Zea mays and soils were wet-sieved (using 53, 250 and 2000\u00a0\u03bcm mesh sizes) to isolate different aggregate size fractions, which were analyzed for total C, N and 15N. The effects of management system were smaller than expected, likely due to disturbance associated with the microcosm installation. Contrary to our hypothesis that earthworms would stabilize organic matter in soil aggregates, P. corethrurus decreased total soil C by 3% in the surface layer (0\u201315\u00a0cm), predominantly through a decrease in the C concentration of macroaggregates (>250\u00a0\u03bcm) and a corresponding depletion of C in coarse particulate organic matter occluded within macroaggregates. Earthworms also decreased bulk density by over 4%, but had no effect on aggregate size distribution. Within the two fertilized treatments, the QSMAS appeared to retain slightly more fertilizer derived N in smaller aggregate fractions (", "keywords": ["2. Zero hunger", "agroecosystems", "materia organica del suelo", "aplicacion de abonos", "04 agricultural and veterinary sciences", "15. Life on land", "nitrogen", "6. Clean water", "oligochaeta", "fertilization", "soil organic matter", "agroecosistemas", "0401 agriculture", " forestry", " and fisheries", "honduras"]}, "links": [{"href": "https://doi.org/10.1016/j.pedobi.2010.03.002"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Pedobiologia", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.pedobi.2010.03.002", "name": "item", "description": "10.1016/j.pedobi.2010.03.002", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.pedobi.2010.03.002"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2010-08-01T00:00:00Z"}}, {"id": "10.1016/j.pedobi.2024.150977", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-05-01T16:16:40Z", "type": "Journal Article", "created": "2024-07-10", "title": "Precise method to measure fungal and bacterial necromass using high pressure liquid chromatography with fluorescence detector adjusted to inorganic, organic and peat soils", "description": "Soil organic matter is the dominant pool of carbon (C) in terrestrial ecosystems. Recent advances in understanding of the mechanisms of C stabilization in the soil emphasize microbes as the main drivers. Special attention is placed on the accumulation of bacterial and fungal necromasses. This calls for development of fast and reliable methods to estimate microbial necromass in a various type of soils, including peat soils. Here we provide precise method to measure fungal and bacterial necromasses with high-pressure liquid chromatography-fluorescence detector (HPLC-FLD) and its comparison with gas chromatography method. Purity of the chromatographic peaks was confirmed with mass spectrometry. The HPLC-FLD method provides reliable results for mineral, organic and highly organic peat soils. ; 2024", "keywords": ["570", "soil organic matter", "amino sugars", "carbon stabilization"]}, "links": [{"href": "https://doi.org/10.1016/j.pedobi.2024.150977"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Pedobiologia", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.pedobi.2024.150977", "name": "item", "description": "10.1016/j.pedobi.2024.150977", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.pedobi.2024.150977"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-09-01T00:00:00Z"}}, {"id": "10.1016/j.scitotenv.2014.02.103", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:16:45Z", "type": "Journal Article", "created": "2014-03-19", "title": "Carbon Dioxide Emissions From Semi-Arid Soils Amended With Biochar Alone Or Combined With Mineral And Organic Fertilizers", "description": "Semi-arid soils cover a significant area of Earth's land surface and typically contain large amounts of inorganic C. Determining the effects of biochar additions on CO2 emissions from semi-arid soils is therefore essential for evaluating the potential of biochar as a climate change mitigation strategy. Here, we measured the CO2 that evolved from semi-arid calcareous soils amended with biochar at rates of 0 and 20tha(-1) in a full factorial combination with three different fertilizers (mineral fertilizer, municipal solid waste compost, and sewage sludge) applied at four rates (equivalent to 0, 75, 150, and 225kg potentially available Nha(-1)) during 182 days of aerobic incubation. A double exponential model, which describes cumulative CO2 emissions from two active soil C compartments with different turnover rates (one relatively stable and the other more labile), was found to fit very well all the experimental datasets. In general, the organic fertilizers increased the size and decomposition rate of the stable and labile soil C pools. In contrast, biochar addition had no effects on any of the double exponential model parameters and did not interact with the effects ascribed to the type and rate of fertilizer. After 182 days of incubation, soil organic and microbial biomass C contents tended to increase with increasing the application rates of organic fertilizer, especially of compost, whereas increasing the rate of mineral fertilizer tended to suppress microbial biomass. Biochar was found to increase both organic and inorganic C contents in soil and not to interact with the effects of type and rate of fertilizer on C fractions. As a whole, our results suggest that the use of biochar as enhancer of semi-arid soils, either alone or combined with mineral and organic fertilizers, is unlikely to increase abiotic and biotic soil CO2 emissions.", "keywords": ["Bioqu\u00edmica", "Mineral fertilizer", "Carbonates", "Waste Disposal", " Fluid", "01 natural sciences", "7. Clean energy", "12. Responsible consumption", "Soil", "Inorganic C", "11. Sustainability", "Fertilizers", "Environmental Restoration and Remediation", "0105 earth and related environmental sciences", "2. Zero hunger", "Soil organic matter", "Air Pollutants", "Minerals", "Agriculture", "04 agricultural and veterinary sciences", "Carbon Dioxide", "15. Life on land", "6. Clean water", "Biochar", "13. Climate action", "Charcoal", "0401 agriculture", " forestry", " and fisheries", "Organic amendment"]}, "links": [{"href": "https://doi.org/10.1016/j.scitotenv.2014.02.103"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Science%20of%20The%20Total%20Environment", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.scitotenv.2014.02.103", "name": "item", "description": "10.1016/j.scitotenv.2014.02.103", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.scitotenv.2014.02.103"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2014-06-01T00:00:00Z"}}, {"id": "10.1016/j.scitotenv.2020.137852", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-05-01T16:16:47Z", "type": "Journal Article", "created": "2020-03-13", "title": "Restoration of soil quality using biochar and brown coal waste: A review", "description": "Soils in intensively farmed areas of the world are prone to degradation. Amendment of such soils with organic waste materials attempts to restore soil quality. Organic amendments are heterogeneous media, which are a source of soil organic matter (SOM) and maintain or restore chemical, physical, biological and ecological functionality. More specifically, an increase in SOM can influence the soil microclimate, microbial community structure, biomass turnover and mineralisation of nutrients. The search is on-going for locally sourced alternatives as many forms may be costly or geographically limiting. The present review focuses on a heterogeneous group of amendments i.e. biochar and brown coal waste (BCW). Both biochar (made from a variety of feedstocks at various temperatures) and BCW (mined extensively) are options that have worldwide applicability. These materials have very high C contents and soil stability, therefore can be used for long-term C sequestration to abate greenhouse gas emissions and as conditioners to improve soil quality. However, biochar is costly for large-scale applications and BCW may have inherently high moisture and pollutant contents. Future studies should focus on the long-term application of these amendments and determine the physicochemical properties of the soil, bioavailability of soil contaminants, diversity of soil communities and productivity of selected crops. Furthermore, the development of in situ technologies to lower production and processing costs of biochar and BCW would improve their economic feasibility for large-scale application.", "keywords": ["2. Zero hunger", "Soil organic matter", "Brown coal waste", "Quality indicators", "04 agricultural and veterinary sciences", "15. Life on land", "Soil quality", "6. Clean water", "12. Responsible consumption", "Biochar", "Greenhouse Gases", "Soil", "13. Climate action", "Charcoal", "0401 agriculture", " forestry", " and fisheries"]}, "links": [{"href": "https://eprints.whiterose.ac.uk/158976/1/1-s2.0-S0048969720313644-main.pdf"}, {"href": "https://doi.org/10.1016/j.scitotenv.2020.137852"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Science%20of%20The%20Total%20Environment", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.scitotenv.2020.137852", "name": "item", "description": "10.1016/j.scitotenv.2020.137852", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.scitotenv.2020.137852"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-06-01T00:00:00Z"}}, {"id": "10.1016/j.scitotenv.2022.156952", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:16:48Z", "type": "Journal Article", "created": "2022-06-22", "title": "Integrated organic and inorganic fertilization and reduced irrigation altered prokaryotic microbial community and diversity in different compartments of wheat root zone contributing to improved nitrogen uptake and wheat yield", "description": "Open AccessThe effect of long-term water and integrated fertilization on prokaryotic microorganisms and their regulation for crop nutrient uptake remains unknown. Therefore, the impact of soil water and integrated fertilization after eight years on prokaryotic microbial communities in different compartments of root zone and their association with wheat nitrogen (N) absorption and yield were investigated. The results showed that compared with fertilization treatments (F), water regimes (W) more drastically modulated the prokaryotic microbial community structure and diversity in bulk soil, rhizosphere and endosphere. The increase of irrigation improved the prokaryotic diversity in the rhizosphere and endosphere while decreased the diversity in the bulk soil. Application of organic fertilizers significantly improved soil organic matter (SOM) and nutrient contents, increased rhizosphere and endophytic prokaryotic microbial diversity, and elevated the relative abundance of aerobic ammonia oxidation and nitrification-related functional microorganisms in rhizosphere and endosphere. Increasing irrigation elevated the relative abundance of functional microorganisms related to aerobic ammonia oxidation and nitrification in the rhizosphere and endosphere. Soil water content (SWC) and NH4+-N as well as NO3\u2212-N were key predictors of prokaryotic microbial community composition under W and F treatments, respectively. Appropriate application of irrigation and organic fertilizers increased the relative abundance of some beneficial bacteria such as Flavobacterium. Water and fertilization treatments regulated the prokaryotic microbial communities of bulk soil, rhizosphere and endosphere by altering SWC and SOM, and provided evidence for the modulation of prokaryotic microorganisms to promote nitrogen uptake and wheat yield under long-term irrigation and fertilization. Conclusively, the addition of organic manure (50 %) with inorganic fertilizers (50 %) and reduced amount of irrigation (pre-sowing and jointing-period irrigation) decreased the application amount of chemical fertilizers and water, while increased SOM and nutrient content, improved prokaryotic diversity, and changed prokaryotic microbial community structure in the wheat root zone, resulting in enhanced nutrient uptake and wheat yield.", "keywords": ["0106 biological sciences", "Yield", "Microorganism", "Microbial population biology", "Nitrogen", "Soil Science", "Organic chemistry", "Plant Science", "01 natural sciences", "Environmental science", "Agricultural and Biological Sciences", "Soil", "Symbiotic Nitrogen Fixation in Legumes", "Soil water", "Genetics", "Fertilizers", "Biology", "Irrigation", "Soil Microbiology", "Triticum", "2. Zero hunger", "Soil organic matter", "Soil Fertility", "Physicochemical factors", "Ecology", "Bacteria", "Microbiota", "Marine Microbial Diversity and Biogeography", "Water", "Life Sciences", "04 agricultural and veterinary sciences", "15. Life on land", "Nitrification", "Agronomy", "6. Clean water", "Chemistry", "Human fertilization", "13. Climate action", "Fertilization", "FOS: Biological sciences", "Environmental Science", "Physical Sciences", "Rhizosphere", "Bulk soil", "0401 agriculture", " forestry", " and fisheries", "Prokaryotic microorganisms", "Endosphere", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems", "Nutrient"]}, "links": [{"href": "https://doi.org/10.1016/j.scitotenv.2022.156952"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Science%20of%20The%20Total%20Environment", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.scitotenv.2022.156952", "name": "item", "description": "10.1016/j.scitotenv.2022.156952", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.scitotenv.2022.156952"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-10-01T00:00:00Z"}}, {"id": "10.1016/j.soilbio.2004.04.031", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-05-01T16:16:50Z", "type": "Journal Article", "created": "2004-06-24", "title": "Long-Term Soil Organic Carbon Dynamics In A Subhumid Tropical Climate: 13c Data In Mixed C3/C4 Cropping And Modeling With Rothc", "description": "Abstract   Scanty information on long-term soil organic carbon (SOC) dynamics hampers validation of SOC models in the tropics. We observed SOC content changes in a 16-year continuously cropped agroforestry experiment in Ibadan, south-western Nigeria. SOC levels declined in all treatments. The decline was most pronounced in the no-tree control treatments with continuous maize and cowpea cropping, where SOC levels dropped from the initial 15.4 to 7.3\u20138.0\u00a0Mg\u00a0C\u00a0ha\u22121 in the 0\u201312 cm topsoil in 16 years. In the two continuously cropped alley cropping (AC) systems, one with Leucaena leucocephala and one with Senna siamea trees, SOC levels dropped to 10.7\u201313.2\u00a0Mg\u00a0C\u00a0ha\u22121. Compared to the no-tree control treatments, an annual application of an additional 8.5\u00a0Mg\u00a0ha\u22121 (dry matter) of plant residues, mainly tree prunings, led to an extra 3.5\u00a0Mg\u00a0C\u00a0ha\u22121 (\u223c0.2% C) in the 0\u201312 cm top soil after 11 years, and 4.1\u00a0Mg\u00a0C\u00a0ha\u22121 after 16 years. The addition of NPK fertilizer had little effect on the quantities of above-ground plant residues returned to the soil, and there was no evidence that the fertilizer affected the rate of SOC decomposition. The fact that both C3 and C4 plants returned organic matter to the soil in all cropping systems, but in contrasting proportions, led to clear contrasts in the 13C abundance in the SOC. This 13C information, together with the measured SOC contents, was used to test the ROTHC model. Decomposition was very fast, illustrated by the fact that we had to double all decomposition rate constants in the model in order to simulate the measured contrasts in SOC contents and \u03b413C between the AC treatments and the no-tree controls. We hypothesized (1) that the pruning materials from the legume trees and/or the extra rhizodeposition from the tree roots in the AC treatments accelerated the decomposition of the SOC present at the start of the experiment (true C-priming), and/or (2) that the physical protection of microbial biomass and metabolites by the clay fraction on this site, having a sandy top soil in which clay minerals are mainly of the 1:1 type, is lower than assumed by the model.", "keywords": ["alley cropping", "2. Zero hunger", "leucaena leucocephala", "senna siamea", "soil organic matter", "microbiology", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land", "tropics"]}, "links": [{"href": "https://doi.org/10.1016/j.soilbio.2004.04.031"}, {"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.2004.04.031", "name": "item", "description": "10.1016/j.soilbio.2004.04.031", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.soilbio.2004.04.031"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2004-11-01T00:00:00Z"}}, {"id": "10.1016/j.soilbio.2012.02.021", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:16:57Z", "type": "Journal Article", "created": "2012-03-08", "title": "Biodegradability Of Organic Matter In Fire-Affected Mineral Soils Of Southern Spain", "description": "Open AccessIncorporated into the soil, naturally formed pyrogenic organic matter (PyOM) is considered as highly recalcitrant, but direct estimation of PyOM decomposition rates are scarce. With this aim in mind, we subjected organic matter (OM) of fire-affected and unaffected soils to biochemical degradation under laboratory conditions and monitored CO2 production over a period of seven months. The soils derived from the Sierra de Aznalc\u00f3llar, Southern Spain, and were sampled 4 weeks and 5 years after a severe fire. Virtual fractionation of the solid-state 13C nuclear magnetic resonance (NMR) spectra of the fire-affected soils into fire-unaffected soil organic matter (SOM) and PyOM yielded charcoal C contributions of 30 to 50% to the total organic C (Corg) of the sample. Fitting the respiration data with a double exponential decay model revealed a fast carbon flush during the first three weeks of the experiment. Solid-state 13C NMR spectroscopy evidenced the contribution of aromatic moieties of the PyOM to this initial carbon release and to the biosynthesis of new microbial biomass. Considering the loss of microbiologically easily available fresh litter by wildfires, this relatively labile PyOM fraction may contribute to a fast recovery of a fire-affected site. The input of PyOM resulted in an increase of the mean residence time (MRT) of the slow OM pool of the soil by a factor of 3-4 to approximately 40 years. Assuming that under field conditions, the microbial activity corresponds to approximately 10% of the value observed under optimal laboratory conditions, MRTs of 500-600 years were estimated for the slow PyOM pool. The fact that these times are only 5-6 times longer than those calculated for fire-unaffected SOM rises doubts about the presumed big influence of PyOM as an additional C-sink in soils. On the other hand, although being small the difference in turnover rates is evident and has some major implication with respect to long-term alteration of the chemical composition of OM in fire-affected soils. In case of a reduced input of fresh litter, the preferential degradation of fire-unaffected SOM yields in a selective preservation of PyOM. To what extent this can alter soil properties, has still to be elucidated. In cultivated soils rarely affected by fire or with low charcoal input after burning of harvest, the impact of PyOM accumulation may be of minor importance. On the other hand, for soils regularly amended with high amounts of biochar or subjected to frequent natural or prescribed burnings, it may be an important factor.", "keywords": ["Respiration experiments", "Biochar", "Soil organic matter turnover", "Forest fires", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "Solid-state NMR spectroscopy", "04 agricultural and veterinary sciences", "Virtual fractionation of SOM", "15. Life on land", "Pyrogenic organic matter"]}, "links": [{"href": "https://doi.org/10.1016/j.soilbio.2012.02.021"}, {"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.2012.02.021", "name": "item", "description": "10.1016/j.soilbio.2012.02.021", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.soilbio.2012.02.021"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2013-01-01T00:00:00Z"}}, {"id": "10.1016/j.soilbio.2012.02.037", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-05-01T16:16:57Z", "type": "Journal Article", "created": "2012-03-28", "title": "The Effect Of Earthworms On Carbon Storage And Soil Organic Matter Composition In Tropical Soil Amended With Compost And Vermicompost", "description": "The use of organic matter (OM) amendments is widespread in tropical countries and may be beneficial for soil carbon storage. Interactions between earthworms and OM amendments in tropical soils are largely unknown. The aim of this study was to investigate the effect of bioturbation on the quantity and chemical composition of OM in soil amended with compost and vermicompost. Our approach included comparison of soil samples amended with compost, vermicompost or chemical fertilizers in the presence or absence of earthworms during a one-year greenhouse experiment. The soils were submitted to a regular cultivation cycle. After one year, we analysed bulk samples for soil OM elemental composition and characterised its lignin and non-cellulosic carbohydrate components. Our results showed a decrease of the carbon and nitrogen content in soil amended with chemical fertilizers. Vermicompost amendment led to unchanged OC content, whereas the compost amendment increased the soils OC content compared to initial soil. The addition of earthworms reduced OC and N content in soils with organic amendments. This is in contrast to soil amended with mineral fertilizer only, where the presence of earthworms did not have any effect. Bioturbation influenced the lignin signature of the soils, and to a lesser extent the non-cellulosic carbohydrate signature. In conclusion, compost amendment combined with bioturbation influenced the quality and quantity of SOM and as result carbon storage and its biogeochemical cycling in tropical soils. Implications for soil fertility remain to be elucidated.", "keywords": ["2. Zero hunger", "Soil organic matter", "Compost", "04 agricultural and veterinary sciences", "15. Life on land", "630", "333", "6. Clean water", "13. Climate action", "Earthworms", "0401 agriculture", " forestry", " and fisheries", "Tropical soil", "Vermicompost"]}, "links": [{"href": "https://doi.org/10.1016/j.soilbio.2012.02.037"}, {"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.2012.02.037", "name": "item", "description": "10.1016/j.soilbio.2012.02.037", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.soilbio.2012.02.037"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2012-07-01T00:00:00Z"}}, {"id": "10.1016/j.soilbio.2012.07.026", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:16:57Z", "type": "Journal Article", "created": "2012-08-17", "title": "Physical, Chemical, And Biochemical Mechanisms Of Soil Organic Matter Stabilization Under Conservation Tillage Systems: A Central Role For Microbes And Microbial By-Products In C Sequestration", "description": "Open AccessPeer reviewed", "keywords": ["2. Zero hunger", "Aggregates", "Soil organic matter", "No-tillage", "Microbial biomass", "Organo-mineral complexes", "04 agricultural and veterinary sciences", "15. Life on land", "12. Responsible consumption", "C sequestrartion", "NMR spectroscopy", "0401 agriculture", " forestry", " and fisheries", "Conservation tillage"]}, "links": [{"href": "https://doi.org/10.1016/j.soilbio.2012.07.026"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20Biology%20and%20Biochemistry", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.soilbio.2012.07.026", "name": "item", "description": "10.1016/j.soilbio.2012.07.026", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.soilbio.2012.07.026"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2013-02-01T00:00:00Z"}}, {"id": "10.1016/j.soilbio.2016.10.016", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:17:00Z", "type": "Journal Article", "created": "2016-11-01", "title": "Repeated Application Of Organic Waste Affects Soil Organic Matter Composition: Evidence From Thermal Analysis, Ftir-Pas, Amino Sugars And Lignin Biomarkers", "description": "Land application of organic waste is an important alternative to landfilling and incineration because it helps restore soil fertility and has environmental and agronomic benefits. These benefits may be related to the biochemical composition of the waste, which can result in the accumulation of different types of carbon compounds in soil. The objective of this study was to identify and characterise changes in soil organic matter (SOM) composition after repeated applications of organic waste. Soil from the CRUCIAL field experiment in Denmark was sampled after 12 years of annual application of household waste compost, cattle manure and sewage sludge, and was compared to a control treatment that had received NPK fertilisation. Soils were characterised using CO2-evolved gas analysis (CO2-EGA) during ramped thermal analysis, mid-infrared photoacoustic spectroscopy (FTIR-PAS) and analysis of amino-sugar and lignin phenols. SOM from the compost and cattle manure treatments had greater thermal stability than the sludge and NPK treatments, which was consistent with the thermal stability of the applied wastes. Compost-amended soils and manure-amended soils also had a greater lignin content with a lower degree of oxidation and a greater contribution of bacterial amino sugars relative to fungal amino sugars compared to soils from the NPK treatment. The high soil C accumulation rate combined with low amino sugar C in SOM from the compost treatment suggested less stimulation of microbial activity, while the cattle manure seemed to result in both microbial stimulation and accumulation of thermally stable forms of C. FTIR-PAS revealed greater C=O vibration of carboxylic groups and amides in sludge and NPK treatments, indicating more oxidised SOM and the presence of proteins. Taken together, these results show that there was accumulation in soil of different C compounds for the different types of applied organic waste, which appeared to be related to the degree to which microbial activity was stimulated and the type of microbial communities applied with the wastes or associated with the decomposition of applied wastes. This in turn may have important effects on ecosystem functioning and long-term soil C storage.", "keywords": ["MIRS", "2. Zero hunger", "Soil organic matter", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land", "CO-EGA", "6. Clean water", "Elemental analyses", "Organic amendments", "Photoacoustic spectroscopy", "12. Responsible consumption"]}, "links": [{"href": "https://doi.org/10.1016/j.soilbio.2016.10.016"}, {"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.2016.10.016", "name": "item", "description": "10.1016/j.soilbio.2016.10.016", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.soilbio.2016.10.016"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-01-01T00:00:00Z"}}, {"id": "10.1016/j.still.2004.02.012", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:17:04Z", "type": "Journal Article", "created": "2004-04-09", "title": "Effects Of Compost, Mycorrhiza, Manure And Fertilizer On Some Physical Properties Of A Chromoxerert Soil", "description": "Abstract   Addition of organic materials of various origins to soil has been one of the most common rehabilitation practices to improve soil physical properties. Mycorrhiza has been known to play a significant role in forming stable soil aggregates. In this study, a 5-year field experiment was conducted to explore the role of mycorrhizal inoculation and organic fertilizers on the alteration of physical properties of a semi-arid Mediterranean soil (Entic Chromoxerert, Arik clay-loam soil). From 1995 to 1999, wheat ( Triticum aestivum  L.), pepper ( Capsicum annuum  L.), maize ( Zea mays  L.) and wheat were sequentially planted with one of five fertilizers: (1) control, (2) inorganic (160\u201326\u201383\u00a0kg N\u2013P\u2013K\u00a0ha \u22121 ), (3) compost at 25\u00a0t\u00a0ha \u22121 , (4) farm manure at 25\u00a0t\u00a0ha \u22121  and (5) mycorrhiza-inoculated compost at 10\u00a0t\u00a0ha \u22121 . Soil physical properties were significantly affected by organic fertilizers. For soil depths of 0\u201315 and 15\u201330\u00a0cm, mean weight diameter (MWD) was highest under the manure treatment while total porosity and saturated hydraulic conductivity were highest under the compost treatment. For a soil depth of 0\u201315\u00a0cm, the compost and manure-treated plots significantly decreased soil bulk density and increased soil organic matter concentration compared with other treatments. Compost and manure treatments increased available water content (AWC) of soils by 86 and 56%, respectively. The effect of inorganic fertilizer treatment on most soil physical properties was insignificant ( P >0.05) compared with the control. Mycorrhizal inoculation+compost was more effective in improving soil physical properties than the inorganic treatment. Organic fertilizer sources were shown to have major positive effects on soil physical properties.", "keywords": ["2. Zero hunger", "Soil organic matter", "Mineral fertilization", "Soil physical properties", "Compost", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "6. Clean water", "Manure", "Soil aggregation", "0401 agriculture", " forestry", " and fisheries", "Mycorrhiza", "0105 earth and related environmental sciences"], "contacts": [{"organization": "Celik I., Ortas I., Kilic S.,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1016/j.still.2004.02.012"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20and%20Tillage%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.still.2004.02.012", "name": "item", "description": "10.1016/j.still.2004.02.012", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.still.2004.02.012"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], 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\u0644\u0644\u062a\u0631\u0628\u0629 \u0627\u0644\u0645\u0639\u062f\u0646\u064a\u0629 C \u0639\u0646 \u0637\u0631\u064a\u0642 \u062a\u0643\u0648\u064a\u0646 OM \u0627\u0644\u0645\u0631\u062a\u0628\u0637 \u0628\u0627\u0644\u0645\u0639\u0627\u062f\u0646 \u0648\u062a\u0645\u0639\u062f\u0646 \u0645\u064a\u0643\u0631\u0648\u0628\u064a \u0623\u0643\u0628\u0631 \u0644\u0640 SOM \u0645\u0639 \u0627\u0631\u062a\u0641\u0627\u0639 \u0627\u0644\u0637\u0644\u0628 \u0639\u0644\u0649 \u0627\u0644\u0645\u0648\u0627\u0631\u062f \u0627\u0644\u0645\u064a\u0643\u0631\u0648\u0628\u064a\u0629. \u062a\u0634\u064a\u0631 \u0627\u0644\u0646\u062a\u0627\u0626\u062c \u0625\u0644\u0649 \u0623\u0646 EA \u0628\u0648\u0633\u0627\u0637\u0629 \u0623\u0646\u0648\u0627\u0639 \u0627\u0644\u0623\u0634\u062c\u0627\u0631\u060c \u0648\u0627\u0644\u062d\u062f \u0645\u0646 \u0627\u0644\u0645\u0648\u0627\u0631\u062f \u0627\u0644\u0645\u064a\u0643\u0631\u0648\u0628\u064a\u0629 \u0648\u062a\u0643\u0648\u064a\u0646 \u0627\u0644\u0645\u062c\u062a\u0645\u0639 \u0627\u0644\u0645\u064a\u0643\u0631\u0648\u0628\u064a \u0647\u064a \u0645\u062d\u0631\u0643\u0627\u062a \u0645\u0647\u0645\u0629 \u0644\u0644\u0645\u062e\u0632\u0648\u0646\u0627\u062a \u0648\u0627\u0644\u062a\u0648\u0632\u064a\u0639 \u0627\u0644\u0631\u0623\u0633\u064a \u0644\u0645\u062e\u0632\u0648\u0646 \u0627\u0644\u0643\u0631\u0628\u0648\u0646 \u0627\u0644\u0639\u0636\u0648\u064a \u0641\u064a \u0627\u0644\u062a\u0631\u0628\u0629 \u0628\u064a\u0646 \u0623\u0646\u0648\u0627\u0639 \u0627\u0644\u0623\u0634\u062c\u0627\u0631 \u0648\u0628\u064a\u0646 \u0646\u0648\u0639\u064a\u0646 \u0645\u0646 \u0627\u0644\u062c\u0630\u0648\u0631 \u0627\u0644\u0641\u0637\u0631\u064a\u0629 \u0627\u0644\u0645\u0631\u062a\u0628\u0637\u0629 \u0628\u0647\u0627.", "keywords": ["Biomass (ecology)", "Microbial population biology", "Fagus sylvatica", "Soil Science", "Plant Science", "Plant litter", "Agricultural and Biological Sciences", "Mycorrhizal Fungi and Plant Interactions", "Soil water", "Genetics", "Monoculture", "Forest floor", "Saproxylic Insect Ecology and Forest Management", "Biology", "Beech", "Soil organic matter", "Soil Fertility", "Ecology", "Bacteria", "Picea abies", "Botany", "Life Sciences", "04 agricultural and veterinary sciences", "Soil carbon", "Agronomy", "Insect Science", "FOS: Biological sciences", "0401 agriculture", " forestry", " and fisheries", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems", "Nutrient"]}, "links": [{"href": "https://doi.org/10.1016/j.soilbio.2022.108754"}, {"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.2022.108754", "name": "item", "description": "10.1016/j.soilbio.2022.108754", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.soilbio.2022.108754"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-09-01T00:00:00Z"}}, {"id": "10.1016/j.still.2010.12.006", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:17:09Z", "type": "Journal Article", "created": "2011-01-18", "title": "Organic Carbon And Total Nitrogen Stocks In A Vertisol Following 40 Years Of No-Tillage, Crop Residue Retention And Nitrogen Fertilisation", "description": "Abstract   Conservation agricultural practices such as no-till (NT) and crop residue retention (CRR), and nutrient application, increases soil organic C (SOC) and are considered effective measures of C sequestration in soil. However, long-term effects of individual components of conservation agriculture and their interactions on SOC are rarely evaluated; as a result, conflicting findings of these practices on SOC are reported in the literature. We measured SOC and soil total N in a balanced factorial experiment, conducted on a Vertisol, consisting of tillage practices (conventional mechanical tillage, CT; and no-tillage, NT), crop residue management (crop residue burned, CRB; and crop residue retained, CRR) and N fertiliser application (no N, 30\u00a0kg\u00a0N\u00a0ha \u22121 \u00a0year \u22121 ; and 90\u00a0kg\u00a0N\u00a0ha \u22121 \u00a0year \u22121 ). The site, in a semiarid subtropical region, was cropped with wheat ( Triticum aestivum  L.) except for 3 years of barley ( Hordeum vulgare  L.), for 40 years using conservation practices.  In general, tillage effects on SOC and soil total N were small. Crop residue and N fertiliser interactively increased SOC and total N stocks at 0\u20130.1\u00a0m depth and cumulative stocks at 0\u20130.2\u00a0m and 0\u20130.3\u00a0m depths; that is, CRR increased SOC and soil total N only when N fertiliser was applied, and fertilisation increased SOC and soil total N only under CRR treatment. Depletion of \u03b4 13 C values in CRR treatments and \u03b4 15 N values in N treatments strongly indicated the contribution of crop residue (and root biomass) and N fertiliser to soil organic matter in this Vertisol. From this study and previous findings from this site, it appears, however, the effects of crop residue retention and N fertiliser occurred in early years, and did not continually increase SOC and total soil N with increasing period of conservation practices.", "keywords": ["2. Zero hunger", "Soil organic matter", "Agricultural", "Nitrogen", "1904 Earth-Surface Processes", "No-till", "04 agricultural and veterinary sciences", "15. Life on land", "Carbon", "630", "Land capability and soil productivity", "Environmental sciences", "Biological sciences", "veterinary and food sciences", "0401 agriculture", " forestry", " and fisheries", "1102 Agronomy and Crop Science", "1111 Soil Science"]}, "links": [{"href": "https://doi.org/10.1016/j.still.2010.12.006"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20and%20Tillage%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.still.2010.12.006", "name": "item", "description": "10.1016/j.still.2010.12.006", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.still.2010.12.006"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2011-04-01T00:00:00Z"}}, {"id": "10.1016/j.still.2003.08.007", "type": "Feature", "geometry": null, "properties": {"license": "Closed Access", "updated": "2026-05-01T16:17:03Z", "type": "Journal Article", "created": "2004-01-27", "title": "Change In Carbon And Nitrogen Stocks In Soil Under 13 Years Of Conventional Or Zero Tillage In Southern Brazil", "description": "The objective of this study was to determine in a long-term experiment (13 years) the effect of three different crop rotations (R1: wheat (Triticum aestivum)\u2013soybean (Glycine max), R2: wheat\u2013soybean\u2013vetch (Vicia villosa)\u2013maize (Zea mays), and R3: wheat\u2013soybean\u2013oat (Avena sativa)\u2013soybean\u2013vetch\u2013maize) under zero tillage (ZT) and conventional tillage (CT) on the stocks of soil organic matter (SOM) in a clayey Oxisol soil of Passo Fundo, Rio Grande do Sul. At the end of 13 years, soil samples were taken to a depth of 100 cm, and analysed for bulk density, chemical composition and 13 C natural abundance. Under a continuous sequence of wheat (winter) and soybean (summer) the stock of soil organic C to 100 cm depth under ZT (168 Mg ha \u22121 ) was not significantly different (LSD at P = 0.05 of 11 Mg ha \u22121 ) to that under CT (168 Mg ha \u22121 ). However, in the rotations with vetch planted as a winter green-manure crop (R2 and R3), soil C stocks were approximately 17 Mg ha \u22121 higher under ZT than under CT. Between 46 and 68% of this difference occurred at 30\u201385 cm depth. The 13 C abundance data indicated that under ZT the decomposition of the original native SOM was not affected by the different composition of crops in the different rotations, but under CT the rotations R2 and R3, which included vetch and maize, stimulated the decay of the original native SOM compared to the continuous wheat/soybean sequence (R1). It appears that the contribution of N2 fixation by the leguminous green manure (vetch) in the cropping system was the principal factor responsible for the observed C accumulation in the soil under ZT, and that most accumulated C was derived from crop roots. \u00a9 2003 Elsevier B.V. All rights reserved.", "keywords": ["Carbon sequestration", "Soil nutrients", "2. Zero hunger", "Soil management", "Soil organic matter", "Carbon-13", "Green manure crops", "Agriculture", "04 agricultural and veterinary sciences", "15. Life on land", "Crop rotations", "01 natural sciences", "Soil quality", "Zero tillage", "Soil", "0401 agriculture", " forestry", " and fisheries", "Field Scale", "Conservation tillage", "Tillage methods", "Brazil", "0105 earth and related environmental sciences"], "contacts": [{"organization": "Sisti, C. P. J., dos Santos, H. P., Kohhann, R., Alves, B. J. R., Urquiaga, S., Boddey, R. M.,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1016/j.still.2003.08.007"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20and%20Tillage%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.still.2003.08.007", "name": "item", "description": "10.1016/j.still.2003.08.007", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.still.2003.08.007"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2004-03-01T00:00:00Z"}}, {"id": "10.1016/j.still.2004.03.006", "type": "Feature", "geometry": null, "properties": {"license": "Closed Access", "updated": "2026-05-01T16:17:04Z", "type": "Journal Article", "created": "2004-08-10", "title": "No Tillage And Crop Rotation Effects On Soil Aggregation And Organic Carbon In A Rhodic Ferralsol From Southern Brazil", "description": "Abstract   In Brazil, no tillage (NT) is a soil conservation practice now widely adopted by farmers, including smallholders. The effect of NT and conventional tillage (disc ploughing followed by two light disc harrowings, CT) was investigated on the aggregation properties of a clayey Rhodic Ferralsol from southern Brazil under different crop rotations. The same soil type under secondary forest was used as reference. Macro- and microaggregate classes were separated by wet sieving using a series of eight sieves (8, 4, 2, 1, 0.5, 0.25, 0.125, 0.053\u00a0mm) at four sampling layers (0\u20135, 5\u201310, 10\u201320, 20\u201330\u00a0cm). The soil in general had high structural stability. At 0\u20135\u00a0cm, meanweight diameter (MWD, 11.1\u00a0mm) and total organic C in macroaggregates (TOC, 39\u00a0g\u00a0kg \u22121  soil) were highest for the forest soil. Soil under NT had a more similar distribution of aggregate size classes and TOC to the forest soil than CT. The most pronounced difference between tillage systems was observed in the surface soil layer (0\u20135\u00a0cm). In this layer, NT had higher aggregate stability (AS NT : 96%; AS CT : 89%), had higher values of aggregate size distribution (MWD NT : 7.9\u00a0mm, MWD CT : 4.3\u00a0mm), and had on average 28% greater TOC in all aggregate size classes than CT. Soil under NT had greater TOC in macroaggregates (NT: 22\u00a0g\u00a0kg \u22121 ; CT: 13\u00a0g\u00a0kg \u22121 ). Crop rotation did not have a significant effect on soil aggregate distribution and TOC. By increasing macroaggregation NT increased organic carbon accumulation in soil.", "keywords": ["Carbon sequestration", "2. Zero hunger", "Soil organic matter", "Soil", "Subtropical climate", "Subtropics", "Forest soil", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land", "Field Scale", "Conservation tillage", "Soil aggregate distribution"]}, "links": [{"href": "https://doi.org/10.1016/j.still.2004.03.006"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20and%20Tillage%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.still.2004.03.006", "name": "item", "description": "10.1016/j.still.2004.03.006", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.still.2004.03.006"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2005-01-01T00:00:00Z"}}, {"id": "10.1016/j.still.2006.07.001", "type": "Feature", "geometry": null, "properties": {"license": "Restricted", "updated": "2026-05-01T16:17:05Z", "type": "Journal Article", "created": "2006-08-18", "title": "Tillage And Fertility Management Effects On Soil Organic Matter And Sorghum Yield In Semi-Arid West Africa", "description": "Whether it is traditional, modern or \u2018\u2018sustainable\u2019\u2019 agriculture, soil organic matter plays a key role in sustaining crop production and in preventing land degradation. A field experiment was conducted on a Ferric Lixisol at Gampela (Burkina Faso) in 2000 and 2001 to carried out the effects of tillage, fertilisation and their interaction on soil organic carbon (SOC) (0\u201310 cm), crop performance and microbial activities. Maize straw or sheep dung were applied separately or combined with urea in a till or no-till systems and compared with urea only and a control treatment. Sampling was done each year at 2 months after sowing and at harvest. SOC was increased in the tillage treatments in 2000 by 35% but only with 18% in 2001 suggesting reduced carbon accumulation in the absence of organic and mineral restitution. Ploughing in maize straw under conditions of N deficiency led to a drastic decrease in SOC due microbial priming effect that, was not observed when ploughing in sheep dung. In no-till system, losses, organic amendment N concentration and the soil N status determined the impact on SOC and crop productivity. The negative effect on SOC in the tillage treatment with maize straw (4.1 g kg \ufffd 1 ) was less when maize straw was combined with urea (6.2 g kg \ufffd 1 ). It is concluded that in semi-arid West Africa, without both organic resource and N inputs, soil organic matter \u2018\u2018pays\u2019\u2019 for crop N nutrition. Increasing SOC accumulation while improving crop yield may be conflicting under low-input agricultural systems in semi-arid West Africa. Therefore, optimum soil organic carbon and crop performance results from a judicious combination of organic resources and inorganic N mediated by microbial activity. # 2006 Elsevier B.V. All rights reserved.", "keywords": ["sustainable land-use", "Soil nutrients", "2. Zero hunger", "Soil management", "Soil organic matter", "microbial biomass", "Crop performance", "carbon", "dynamics", "04 agricultural and veterinary sciences", "15. Life on land", "Soil carbon", "Tillage", "Manure", "biocidal treatments", "13. Climate action", "Fertilization", "0401 agriculture", " forestry", " and fisheries", "Fertilizers", "Field Scale", "metabolism", "Conservation tillage", "Organic amendments"]}, "links": [{"href": "https://doi.org/10.1016/j.still.2006.07.001"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20and%20Tillage%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.still.2006.07.001", "name": "item", "description": "10.1016/j.still.2006.07.001", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.still.2006.07.001"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2007-05-01T00:00:00Z"}}, {"id": "10.1016/j.still.2006.08.006", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:17:06Z", "type": "Journal Article", "created": "2006-09-27", "title": "Long-Term Impact Of Reduced Tillage And Residue Management On Soil Carbon Stabilization: Implications For Conservation Agriculture On Contrasting Soils", "description": "Residue retention and reduced tillage are both conservation agricultural management options that may enhance soil organic carbon (SOC) stabilization in tropical soils. Therefore, we evaluated the effects of long-term tillage and residue management on SOC dynamics in a Chromic Luvisol (red clay soil) and Areni-Gleyic Luvisol (sandy soil) in Zimbabwe. At the time of sampling the soils had been under conventional tillage (CT), mulch ripping (MR), clean ripping (CR) and tied ridging (TR) for 9 years. Soil was fully dispersed and separated into 212\u20132000 mm (coarse sand), 53\u2013212 mm (fine sand), 20\u201353 mm (coarse silt), 5\u201320 mm (fine silt) and 0\u20135 mm (clay) size fractions. The whole soil and size fractions were analyzed for C content. Conventional tillage treatments had the least amount of SOC, with 14.9 mg C g \ufffd 1 soil and 4.2 mg C g \ufffd 1 soil for the red clay and sandy soils, respectively. The highest SOC content was 6.8 mg C g \ufffd 1 soil in the sandy soil under MR, whereas for the red clay soil, TR had the highest SOC content of 20.4 mg C g \ufffd 1 soil. Organic C in the size fractions increased with decreasing size of the fractions. In both soils, the smallest response to management was observed in the clay size fractions, confirming that this size fraction is the most stable. The coarse sand-size fraction was most responsive to management in the sandy soil where MR had 42% more organic C than CR, suggesting that SOC contents of this fraction are predominantly controlled by amounts of C input. In contrast, the fine sand fraction was the most responsive fraction in the red clay soil with a 66% greater C content in the TR than CT. This result suggests that tillage disturbance is the dominant factor reducing C stabilization in a clayey soil, probably by reducing C stabilization within microaggregates. In conclusion, developing viable conservation agriculture practices to optimize SOC contents and long-term agroecosystem sustainability should prioritize the maintenance of C inputs (e.g. residue retention) to coarse textured soils, but should focus on the reduction of SOC decomposition (e.g. through reduced tillage) in fine textured soils. # 2006 Elsevier B.V. All rights reserved.", "keywords": ["organic-matter dynamics", "Soil management", "Conservation agriculture", "Residue management", "no-tillage", "continuous cultivation", "sudano-sahelian conditions", "loam soil", "Tropical agroecosystems", "Tillage", "Agricultural ecosystems", "conventional-tillage", "Field Scale", "Conservation tillage", "2. Zero hunger", "Tropical zones", "Soil organic matter", "microbial biomass", "Particulate organic matter (pom)", "Soil organic carbon", "04 agricultural and veterinary sciences", "15. Life on land", "6. Clean water", "crop residue", "fractions", "0401 agriculture", " forestry", " and fisheries", "manure application"]}, "links": [{"href": "https://doi.org/10.1016/j.still.2006.08.006"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20and%20Tillage%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.still.2006.08.006", "name": "item", "description": "10.1016/j.still.2006.08.006", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.still.2006.08.006"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2007-06-01T00:00:00Z"}}, {"id": "10.1016/j.still.2008.09.003", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:17:07Z", "type": "Journal Article", "created": "2008-11-08", "title": "Stratification Ratio Of Soil Organic Matter Pools As An Indicator Of Carbon Sequestration In A Tillage Chronosequence On A Brazilian Oxisol", "description": "Abstract   Long-term no-tillage (NT) leads to profile stratification of soil organic matter (SOM) pools, and the soil organic carbon (SOC) stratification ratio (SR) is an indicator of soil quality. The objective of this report is to assess the feasibility of using SOC-SR as an index for estimating SOC sequestration in NT soils. The effect of a plow tillage (PT) and NT chronosequence on the SR of SOM pools was assessed in an Oxisol in Southern Brazil (50\u00b023\u2032W and 24\u00b036\u2032S). The chronosequence consisted of six sites: (i) native field (NF); (ii) PT of the native field (PNF-1) involving conversion of natural vegetation to cropland; (iii) NT for 10 years (NT-10); (iv) NT for 20 years (NT-20); (v) NT for 22 years (NT-22); (vi) conventional tillage for 22 years (CT-22). Soil samples were collected from four depths (0\u20135\u00a0cm; 5\u201310\u00a0cm; 10\u201320\u00a0cm; 20\u201340\u00a0cm layer) and soil parameters comprised by SOM pools [i.e., C, N, S, particulate organic C (POC), particulate N (PN), stable C (SC) and stable N (SN), microbial biomass C (MBC) and microbial biomass N (MBN), basal respiration (BR), dissolved organic C (DOC), total polysaccharides (TP) and labile polysaccharides (LP)] were measured. In undisturbed NF soil, the SR of all parameters increased with increase in soil depth. In contrast, the SR decreased in PT, and the SOM was uniformly distributed in the soil profile. All NT treatments restored the SR, and were characterized with higher values of all measured parameters compared to NF. The SR for SOC ranged from 1.12 to 1.51 for CT-22 compared with 1.64\u20132.61 SR for NT surface and sub-soil layers, respectively. The SR for POC and PN were higher than those for stable C and N. However, SR for the biological pools (e.g., MBC, MBN and BR) were the highest and strongly correlated with the rate of SOC sequestration. An increase in SR of SOC was also positively correlated with the rate and amount of SOC sequestered. Regression analyses indicated a strong correlation between SR of SOC and all parameters monitored in this study. The data showed that the SR of SOC is an efficient indicator of C sequestration in long-term NT management.", "keywords": ["Carbon sequestration", "2. Zero hunger", "Soil organic matter", "Chronosequence", "No-till", "Black oats", "04 agricultural and veterinary sciences", "15. Life on land", "Soil fertility", "Stratification ratio", "Soil quality", "Lupine", "6. Clean water", "Tillage", "Soil erosion", "0401 agriculture", " forestry", " and fisheries", "Som pools", "Oxisols", "Field Scale", "Conservation tillage"]}, "links": [{"href": "https://doi.org/10.1016/j.still.2008.09.003"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20and%20Tillage%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.still.2008.09.003", "name": "item", "description": "10.1016/j.still.2008.09.003", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.still.2008.09.003"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2009-04-01T00:00:00Z"}}, {"id": "10.1016/j.still.2006.10.001", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-05-01T16:17:06Z", "type": "Journal Article", "created": "2006-11-14", "title": "Depth Distribution Of Soil Organic C And N After Long-Term Soybean Cropping In Texas", "description": "Abstract   Crop management practices have potential to enhance subsoil C and N sequestration in the southern U.S., but effects may vary with tillage regime and cropping sequence. The objective of this study was to determine the impacts of tillage and soybean cropping sequence on the depth distribution of soil organic C (SOC), dissolved organic C (DOC), and total N after 20 years of treatment imposition for a silty clay loam soil in central Texas. A continuous soybean monoculture, a wheat\u2013soybean doublecrop, and a sorghum\u2013wheat\u2013soybean rotation were established under both conventional (CT) and no tillage (NT). Soil was sampled after soybean harvest and sectioned into 0\u20135, 5\u201315, 15\u201330, 30\u201355, 55\u201380, and 80\u2013105\u00a0cm depth intervals. Both tillage and cropping intensity influenced C and N dynamics in surface and subsurface soils. No tillage increased SOC, DOC, and total N compared to CT to a 30\u00a0cm depth for continuous soybean, but to 55\u00a0cm depths for the more intensive sorghum\u2013wheat\u2013soybean rotation and wheat\u2013soybean doublecrop. Averaged from 0 to 105\u00a0cm, NT increased SOC, DOC, and total N by 32, 22, and 34%, respectively, compared to CT. Intensive cropping increased SOC and total N at depths to 55\u00a0cm compared to continuous soybean, regardless of tillage regime. Continuous soybean had significantly lower SOC (5.3\u00a0g\u00a0kg \u22121 ) than sorghum\u2013wheat\u2013soybean (6.4\u00a0g\u00a0kg \u22121 ) and wheat\u2013soybean (6.1\u00a0g\u00a0kg \u22121 ), and 19% lower total N than other cropping sequences. Dissolved organic C was also significantly higher for sorghum\u2013wheat\u2013soybean (139\u00a0mg\u00a0C\u00a0kg \u22121 ) than wheat\u2013soybean (92\u00a0mg\u00a0C\u00a0kg \u22121 ) and continuous soybean (100\u00a0mg\u00a0C\u00a0kg \u22121 ). The depth distribution of SOC, DOC, and total N indicated treatment effects below the maximum tillage depth (25\u00a0cm), suggesting that roots, or translocation of dissolved organic matter from surface soils, contributed to higher soil organic matter levels under NT than CT in subsurface soils. High-intensity cropping sequences, coupled with NT, resulted in the highest soil organic matter levels, demonstrating potential for C and N sequestration for subsurface soils in the southern U.S.", "keywords": ["Carbon sequestration", "2. Zero hunger", "Dissolved organic C", "Soil organic matter", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land", "6. Clean water", "Tillage"], "contacts": [{"organization": "International Arctic Research Center Koyukuk Drive, P.O. Box 757340, Fairbanks, AK 99775-7340, Unites States ( host institution ), Dou, Fugen ( author ), Wright, Alan L. ( author ), Hons, Frank M. ( author ),", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1016/j.still.2006.10.001"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20and%20Tillage%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.still.2006.10.001", "name": "item", "description": "10.1016/j.still.2006.10.001", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.still.2006.10.001"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2007-06-01T00:00:00Z"}}, {"id": "10.1016/j.still.2006.11.005", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-05-01T16:17:06Z", "type": "Journal Article", "created": "2007-01-04", "title": "Tillage Effect On C Stocks Of A Clayey Oxisol Under A Soybean-Based Crop Rotation In The Brazilian Cerrado Region", "description": "Abstract   A large area (180\u00a0Mha) of central Brazil is occupied by a savanna biome known as the Cerrado. Annual rainfall in this region varies from 1200 to 2000\u00a0mm, although there is a long (\u223c5 month) dry season with almost no rain. This region is regarded by Brazilians as their agricultural frontier and there is a steady growth in the area dedicated to permanent cropping in the region, which today is estimated to occupy 14\u00a0Mha. Owing to the dearth of long-term experiments, the impact of continuous cropping on soil carbon stocks remains unclear. The objective of this study was to evaluate the effects of different tillage systems (zero till (ZT) and conventional tillage (CT)) on the change in soil carbon stocks over a 20-year period of the same crop sequence compared to that under a neighbouring area of native vegetation (NV). Only approximately 10\u00a0Mg\u00a0ha\u22121 of soil carbon in the 0\u2013100\u00a0cm depth interval was lost under continuous ZT. However, under CT systems losses were greater (up to 30\u00a0Mg\u00a0C\u00a0ha\u22121) when the mouldboard plough was used and/or tillage was performed twice a year. We did not have access to instrumentation to accurately assess soil charcoal but the C/N data and peroxide and dichromate oxidative techniques suggested that \u223c40% of soil C was in this form. The 13C natural abundance of soil profiles indicated that residues of crops (maize) and the spontaneous annual fallow of Brachiaria spp. resulted in integration of significant C4 residues to a depth of at least 40\u00a0cm. It would appear that zero tillage, which is already widely adopted in the Cerrado region of Brazil, will have only a small negative long-term impact on soil C stocks, but ploughing, especially more than once a year, will lead to considerably larger soil C losses.", "keywords": ["2. Zero hunger", "Soil organic matter", "04 agricultural and veterinary sciences", "15. Life on land", "Cerrado region", "Zero tillage", "Charcoal", "Disc plough", "Mouldboard plough", "0401 agriculture", " forestry", " and fisheries", "Soil carbon accumulation", "13C", "Soybean", "Brazil"]}, "links": [{"href": "https://doi.org/10.1016/j.still.2006.11.005"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20and%20Tillage%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.still.2006.11.005", "name": "item", "description": "10.1016/j.still.2006.11.005", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.still.2006.11.005"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2007-09-01T00:00:00Z"}}, {"id": "10.1016/j.still.2006.12.002", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:17:06Z", "type": "Journal Article", "created": "2007-02-07", "title": "Determinants Of Annual Fluxes Of Co2 And N2o In Long-Term No-Tillage And Conventional Tillage Systems In Northern France", "description": "The greenhouse gases CO2 andN2O emissions were quantified in a long-term experiment in northern France, in which no-till (NT)and conventional tillage (CT) had been differentiated during 32 years in plots under a maize\u2013wheat rotation. Continuous CO2 andperiodical N2O soil emission measurements were performed during two periods: under maize cultivation (April 2003\u2013July 2003) and during the fallow period after wheat harvest (August 2003\u2013March 2004). In order to document the dynamics and importance of these emissions, soil organicCand mineral N, residue decomposition, soil potential forCO2 emission and climatic dataweremeasured.CO2 emissions were significantly larger in NTon 53% and in CTon 6% of the days. From April to July 2003 and from November 2003 to March 2004, the cumulated CO2 emissions did not differ significantly between CT and NT. However, the cumulated CO2 emissions from August to November 2003 were considerably larger for NT than for CT. Over the entire 331 days of measurement, CT and NT emitted 3160 269 and 4064 138 kgCO2-C ha-1, respectively.The differences in CO2 emissions in the two tillage systems resulted from the soil climatic conditions and the amounts and location of crop residues and SOM. A large proportion of the CO2 emissions in NTover the entiremeasurement period was probably due to the decomposition of old weathered residues.NTtended to emit more N2O than CT over the entiremeasurement period.However differences were statistically significant in only half of the cases due to important variability. N2O emissions were generally less than 5 g N ha-1 day-1, except for a few dates where emission increased up to 21 g N ha-1 day-1. These N2O fluxes represented 0.80, 0.15 and 1.32 0.52 kg N2O-N ha-1 year-1 for CT and NT, respectively. Depending on the periods, a large part of the N2O emissions occurred was probably induced by nitrification, since soil conditions were not favorable for denitrification. Finally, for the period ofmeasurement after 32 years of tillage treatments, theNTsystem emitted more greenhouses gases (CO2 and N2O) to the atmosphere on an annual basis than the CT system.", "keywords": ["[SDV.SA.AGRO] Life Sciences [q-bio]/Agricultural sciences/Agronomy", "2. Zero hunger", "Soil organic matter", "571", "Crop residues", "[SDV.SA.AGRO]Life Sciences [q-bio]/Agricultural sciences/Agronomy", "04 agricultural and veterinary sciences", "[SDV.SA.SDS]Life Sciences [q-bio]/Agricultural sciences/Soil study", "15. Life on land", "Soil tillage", "N2O emission", "12. Responsible consumption", "13. Climate action", "CO2 emission", "0401 agriculture", " forestry", " and fisheries", "Effect of climatic conditions", "[SDV.SA.SDS] Life Sciences [q-bio]/Agricultural sciences/Soil study"]}, "links": [{"href": "https://doi.org/10.1016/j.still.2006.12.002"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20and%20Tillage%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.still.2006.12.002", "name": "item", "description": "10.1016/j.still.2006.12.002", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.still.2006.12.002"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2007-09-01T00:00:00Z"}}, {"id": "10.1016/j.still.2008.11.007", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:17:07Z", "type": "Journal Article", "created": "2009-01-08", "title": "Soil Organic Carbon And Fertility Interactions Affected By A Tillage Chronosequence In A Brazilian Oxisol", "description": "Abstract   No-till (NT) adoption is an essential tool for development of sustainable agricultural systems, and how NT affects the soil organic C (SOC) dynamics is a key component of these systems. The effect of a plow tillage (PT) and NT age chronosequence on SOC concentration and interactions with soil fertility were assessed in a variable charge Oxisol, located in the South Center quadrant of Parana State, Brazil (50\u00b023\u2019W and 24\u00b036'S). The chronosequence consisted of the following six sites: (i) native field (NF); (ii) PT of the native field (PNF-1) involving conversion of natural vegetation to cropland; (iii) NT for 10 years (NT-10); (iv) NT for 20 years (NT-20); (v) NT for 22 years (NT-22); and (vi) conventional tillage for 22 years (CT-22) involving PT with one disking after summer harvest and one after winter harvest to 20\u00a0cm depth plus two harrow disking. Soil samples were collected from five depths (0\u20132.5; 2.5\u20135; 5\u201310; 10\u201320; and 20\u201340\u00a0cm) and SOC, pH (in H 2 O and KCl), \u0394pH, potential acidity, exchangeable bases, and cation exchangeable capacity (CEC) were measured. An increase in SOC concentration positively affected the pH, the negative charge and the CEC and negatively impacted potential acidity. Regression analyses indicated a close relationship between the SOC concentration and other parameters measured in this study. The regression fitted between SOC concentration and CEC showed a close relationship. There was an increase in negative charge and CEC with increase in SOC concentration: CEC increased by 0.37\u00a0cmol c \u00a0kg \u22121  for every g of C\u00a0kg \u22121  soil. The ratio of ECEC:SOC was 0.23\u00a0cmol c \u00a0kg \u22121  for NF and increased to 0.49\u00a0cmol c \u00a0kg \u22121  for NT-22. The rates of P and K for 0\u201310\u00a0cm depth increased by 9.66\u00a0kg\u00a0ha \u22121 \u00a0yr \u22121  and 17.93\u00a0kg\u00a0ha \u22121 \u00a0yr \u22121 , respectively, with NF as a base line. The data presented support the conclusion that long-term NT is a useful strategy for improving fertility of soils with variable charge.", "keywords": ["2. Zero hunger", "Soil management", "Soil organic matter", "Root depth", "Crop residues", "Cation exchange capacity (CEC)", "Conservation agriculture", "Chronosequence", "Acidity", "Sustainable agriculture", "No-till", "Soil ph", "04 agricultural and veterinary sciences", "15. Life on land", "Soil fertility", "Soil quality", "Tillage", "Variable charge", "Soil analysis", "0401 agriculture", " forestry", " and fisheries", "Oxisols", "Field Scale"]}, "links": [{"href": "https://doi.org/10.1016/j.still.2008.11.007"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20and%20Tillage%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.still.2008.11.007", "name": "item", "description": "10.1016/j.still.2008.11.007", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.still.2008.11.007"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2009-06-01T00:00:00Z"}}, {"id": "10.1016/j.still.2009.04.006", "type": "Feature", "geometry": null, "properties": {"license": "Closed Access", "updated": "2026-05-01T16:17:08Z", "type": "Journal Article", "created": "2009-05-24", "title": "Earthworm Populations And Growth Rates Related To Long-Term Crop Residue And Tillage Management", "description": "Conventional tillage creates soil physical conditions that may restrict earthworm movement and accelerate crop residue decomposition, thus reducing the food supply for earthworms. These negative impacts may be alleviated by retaining crop residues in agroecosystems. The objective of this study was to determine the effects of various tillage and crop residue management practices on earthworm populations in the field and earthworm growth under controlled conditions. Population assessments were conducted at two long-term (15+ years) experimental sites in Quebec, Canada with three tillage systems: moldboard plow/disk harrow (CT), chisel plow or disk harrow (RT) and no tillage (NT), as well as two levels of crop residue inputs (high and low). Earthworm growth was assessed in intact soil cores from both sites. In the field, earthworm populations and biomass were greater with long-term NT than CT and RT practices, but not affected by crop residue management. Laboratory growth rates of Aporrectodea turgida (Eisen) in intact soil cores were affected by tillage and residue inputs, and were positively correlated with the soil organic C pool, suggesting that tillage and residue management practices that increase the soil organic C pool provide more organic substrates for earthworm growth. The highest earthworm growth rates were in soils from RT plots with high residue input, which differed from the response of earthworm populations to tillage and residue management treatments in the field. Our results suggest that tillage-induced disturbance probably has a greater impact than food availability on earthworm populations in cool, humid agroecosystems.", "keywords": ["2. Zero hunger", "Soil management", "Soil organic matter", "Aporrectodea turgida", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "Crop residue input", "Agricultural ecosystems", "Tillage system", "Growth rates", "Earthworms", "0401 agriculture", " forestry", " and fisheries", "Field Scale", "Temperate zones", "Conservation tillage", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.still.2009.04.006"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20and%20Tillage%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.still.2009.04.006", "name": "item", "description": "10.1016/j.still.2009.04.006", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.still.2009.04.006"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2009-07-01T00:00:00Z"}}, {"id": "10.1016/j.still.2011.04.007", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-05-01T16:17:09Z", "type": "Journal Article", "created": "2011-05-21", "title": "Long-Term Effect Of Tillage, Rotation And Nitrogen Fertiliser On Soil Quality In A Mediterranean Vertisol", "description": "Studies of the impacts of the interactions of soil agricultural practices on soil quality could assist with assessment of better management to establish sustainable crop production system. The main objective was to determine the long-term effects of tillage system, crop rotation and N fertilisation on soil total N and organic C (SOC), labile fractions of organic matter (water soluble carbon, WSC, and active carbon, AC), nitrate content, and soil enzymatic activities (dehydrogenase (DHA), \u03b2-glucosidase (Glu) and alkaline phosphatase (AP)) at four different soil depths (0\u20135, 5\u201310, 10\u201330 and 30\u201350 cm), in a Mediterranean dryland Vertisol in SW Spain. Tillage systems were conventional tillage (CT) and no tillage (NT). Crop rotations were wheat\u2013sunflower (WS), wheat\u2013chickpea (WC), wheat\u2013faba bean (WFb), wheat\u2013fallow (WF) and continuous wheat (WW). Nitrogen fertiliser rates were 0, 50 and 150 kg N ha\u22121. The different crop rotation systems had a great influence in soil C and N fractions and enzymatic activities. In general, the SOC, total N, WSC, and \u03b2-glucosidase contents were higher in the no tillage system than in conventional tillage system in the wheat\u2013wheat and in the wheat\u2013faba bean rotations at upper layer (0\u20135 cm), while the lowest ones were obtained in the wheat\u2013fallow rotation in both tillage systems. Carbon and N fractions, calculated by volumetric soil, showed an increase with depth in both tillage systems and in all crop rotations, which could be related to the increase of soil bulk density and soil mass with depth. The highest N fertiliser rate increased most of soil variables, especially nitrate content at deeper layers, thereby precautions should be taken with long-term N fertilisation to avoid leaching of nitrates below the tillage layer. With the exception of wheat\u2013fallow rotation, slightly greater grain and above-ground biomass yields were obtained for wheat in NT, especially at 150 kg N ha\u22121. Combination of NT with any biannual rotation except fallow could be an adequate sustainable management in order to improve soil quality of Vertisols, under our conditions.", "keywords": ["2. Zero hunger", "Soil organic matter", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "Soil enzymatic activities", "15. Life on land", "Rainfed agriculture", "Conservation tillage", "6. Clean water", "12. Responsible consumption"]}, "links": [{"href": "https://doi.org/10.1016/j.still.2011.04.007"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20and%20Tillage%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.still.2011.04.007", "name": "item", "description": "10.1016/j.still.2011.04.007", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.still.2011.04.007"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2011-08-01T00:00:00Z"}}, {"id": "10.1016/j.still.2011.05.001", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-05-01T16:17:09Z", "type": "Journal Article", "created": "2011-06-24", "title": "Long-Term Effect Of Tillage, Nitrogen Fertilization And Cover Crops On Soil Organic Carbon And Total Nitrogen Content", "description": "Abstract   No-tillage, N fertilization and cover crops are known to play an important role in conserving or increasing SOC and STN but the effects of their interactions are less known.  In order to evaluate the single and combined effects of these techniques on SOC and STN content under Mediterranean climate, a long term experiment started in 1993 on a loam soil (Typic Xerofluvent) in Central Italy.  The experimental variants are: conventional tillage (CT) and no-tillage (NT), four N fertilization rates (N0, N1, N2 and N3) and four soil cover crop (CC) types (C \u2013 no cover crop; NL \u2013 non-legume CC; LNL \u2013 low nitrogen supply legume CC, and HNL \u2013 high nitrogen supply legume CC).  The nitrogen fertilization rates (N0, N1, N2 and N3) were: 0, 100, 200, 300\u00a0kg\u00a0N\u00a0ha \u22121  for maize ( Zea mays,  L.); 0, 60, 120,180\u00a0kg\u00a0N\u00a0a \u22121  for durum wheat ( Triticum durum   Desf. ); 0, 50, 100, 150\u00a0kg\u00a0N\u00a0ha \u22121  for sunflower ( Helianthus annuus  L.).  From 1993 to 2008, under the NT system the SOC and STN content in the top 30\u00a0cm soil depth increased by 0.61 and 0.04\u00a0Mg\u00a0ha \u22121 \u00a0year \u22121  respectively. In the same period, the SOC and STN content under the CT system decreased by a rate of 0.06 and 0.04\u00a0Mg\u00a0ha \u22121 \u00a0year \u22121  respectively.  During the experimental period, N1, N2 and N3 increased the SOC content in the 0\u201330\u00a0cm soil layer at a rate of 0.14, 0.45 and 0.49\u00a0Mg\u00a0ha \u22121 \u00a0year \u22121 . Only the higher N fertilization levels (N2 and N3) increased STN content, at a rate of 0.03 and 0.05\u00a0Mg\u00a0ha \u22121 \u00a0year \u22121 .  NL, LNL and HNL cover crops increased SOC content by 0.17, 0.41 and 0.43\u00a0Mg\u00a0C\u00a0ha \u22121 \u00a0year \u22121  and \u22120.01, +0.01 and +0.02\u00a0Mg\u00a0N\u00a0ha \u22121 \u00a0year \u22121 .  Significant interactions among treatments were evident only in the case of the N fertilization by tillage system interaction on SOC and STN concentration in the 0\u201310\u00a0cm soil depth in 2008.  The observed SOC and STN variations were correlated to C returned to the soil as crop residues, aboveground cover crop biomass and weeds (C input).  We conclude that, under our Mediterranean climate, it is easier to conserve or increase SOC and STN by adopting NT than CT. To reach this objective, the CT system requires higher N fertilization rates and introduction of highly productive cover crops.", "keywords": ["2. Zero hunger", "Soil organic matter", "Farm/Enterprise Scale Field Scale", "Soil organic carbon", "Soil carbon input", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "Mediterranean climate", "15. Life on land", "fertilization; no-tillage; cover crop", "Conservation tillage"]}, "links": [{"href": "https://www.iris.sssup.it/bitstream/11382/338180/2/Mazzoncini%20et%20al.%20%282011%29_STILL.pdf"}, {"href": "https://doi.org/10.1016/j.still.2011.05.001"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20and%20Tillage%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.still.2011.05.001", "name": "item", "description": "10.1016/j.still.2011.05.001", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.still.2011.05.001"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2011-08-01T00:00:00Z"}}, {"id": "10.1016/j.still.2011.10.012", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:17:09Z", "type": "Journal Article", "created": "2011-11-17", "title": "No Tillage In Rainfed Aragon (Ne Spain): Effect On Organic Carbon In The Soil Surface Horizon", "description": "Open AccessThis research was supported by the Comisi\u00f3n Interministerial de Ciencia y Tecnolog\u00eda of Spain (Grants AGL2010-22050-CO3-02/AGR and AGL2007-66320-C02-02/AGR) and the European Union (FEDER Funds). N. Blanco-Moure was awarded with a PhD fellowship (FPI Program) by the Spanish Ministry of Science and Innovation.", "keywords": ["2. Zero hunger", "Soil organic matter", "On-farm research", "Crop residues", "Soil organic matter;", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "Dryland cereal farming", "15. Life on land", "Conservation tillage"]}, "links": [{"href": "https://doi.org/10.1016/j.still.2011.10.012"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20and%20Tillage%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.still.2011.10.012", "name": "item", "description": "10.1016/j.still.2011.10.012", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.still.2011.10.012"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2012-01-01T00:00:00Z"}}, {"id": "10.1016/j.still.2013.02.008", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:17:10Z", "type": "Journal Article", "created": "2013-03-19", "title": "Cover Crops And No-Till Effects On Physical Fractions Of Soil Organic Matter", "description": "Brazilian Agricultural Research Corporation (EMBRAPA) Rice and Beans Research Center, Santo Antonio de Goias, GO", "keywords": ["land use change", "Soil management", "Aggregates", "Millet", "fallow", "grass", "Cultivation", "Soil pollution", "soil depth", "Crops", "cover crop", "Plants (botany)", "soil organic matter", "Organic compounds", "soil quality", "zero tillage", "Agricultural machinery", "soil aggregate", "Panicum maximum", "2. Zero hunger", "soil surface", "rice", "Brachiaria brizantha", "Biological materials", "04 agricultural and veterinary sciences", "Biogeochemistry", "15. Life on land", "sustainability", "Agronomy", "Brachiaria ruziziensis", "13. Climate action", "Soils", "conservation tillage", "0401 agriculture", " forestry", " and fisheries", "total organic carbon", "plowing"]}, "links": [{"href": "https://doi.org/10.1016/j.still.2013.02.008"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20and%20Tillage%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.still.2013.02.008", "name": "item", "description": "10.1016/j.still.2013.02.008", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.still.2013.02.008"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2013-06-01T00:00:00Z"}}, {"id": "10.1023/a:1006128401073", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:17:26Z", "type": "Journal Article", "created": "2002-12-22", "description": "In cropping systems with limited amounts of external inputs, the soil organic matter pool (SOM) may contribute significantly to plant nutrition. The impact of organic inputs on total SOM and particulate organic matter (POM) N contents as affected by soil type and the relationships between sources of N and maize N uptake were assessed for a set of alley cropping trials in the West- African moist savanna. The trials were established in Niaouli (Benin Republic), in Glidji, Amoutchou, and Sarakawa (Togo), and in Bouake and Ferkessedougou (Cote d\u2018 Ivoire). The total soil N content, averaged over all treatments and years, varied between 324 and 1140 mg N kg\u22121 soil. The POM-N content varied between 50 and 160 mg N kg\u22121 soil. The average proportion of soil N belonging to the POM pool ranged between 9% and 29%. This was significantly related to the annual N inputs from maize stover and prunings, when averaged over the different alley cropping treatments. The trial \u2018age\u2018 also appeared to be related to the impact of the different treatments on the POM-N content. The Ferkessedougou soil contained a relatively higher proportion of total soil N in the POM pool because of its relatively high silt and clay content, compared to the other sites. The relative change in POM-N content between 1996 and the initial sampling was about twice the relative change in total soil N content. This suggests that N incorporated in the POM is relatively labile, compared to N incorporated in the other SOM fractions. Maize N uptake was related to the amount of add pruning-N (partial r2 of 27%), the rainfall during the growing season (partial r2 of 17%), the POM-N content (partial r2 of 14%), and to a lesser degree to the POM N concentration (partial r2 of 5%), the fertilizer N addition rate (partial r2 of 3%), and the silt and clay content of the soil (partial r2 of 3%). The POM-N content was shown to be influenced by organic matter additions and soil characteristics and to contribute significantly to maize N supply. This pool may be an important indicator for the soil fertility status of savanna soils.", "keywords": ["alley cropping", "2. Zero hunger", "senna siamea", "albie lebbeck", "cropping systems", "04 agricultural and veterinary sciences", "particle size", "15. Life on land", "01 natural sciences", "6. Clean water", "gliricidia sepium", "leucaena leucocephala", "soil organic matter", "0401 agriculture", " forestry", " and fisheries", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1023/a:1006128401073"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Agroforestry%20Systems", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1023/a:1006128401073", "name": "item", "description": "10.1023/a:1006128401073", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1023/a:1006128401073"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "1998-09-01T00:00:00Z"}}, {"id": "10.1023/a:1010310300067", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-05-01T16:17:28Z", "type": "Journal Article", "created": "2002-12-23", "description": "Planted tree or shrub fallows can help increase the fertility of degraded tropical soils. We investigated the effects of planted fallows of Indigofera (IND), Calliandra (CAL), and Tithonia (TTH); a natural, unmanaged fallow (NAT); and a maize/bean rotation (ROT) on the dynamics and partitioning of soil organic matter (SOM) and phosphorus (P). One year after treatment, samples were collected from a fine-textured volcanic-ash soil (Oxic Dystropept) of a mid-altitude hillside in southwestern Colombia. The SOM in the sand-size fraction (150\u20132000 \u03bcm) was subdivided into light (LL), intermediate (LM), and heavy (LH) fractions. Total soil P was also fractionated into inorganic (Pi) and organic (Po). Of the planted fallows, TTH most increased and NAT least increased plant-available Pi and Po. The amounts of C, N, and P in the LL and LM fractions of SOM followed the order, TTH>CAL>NAT>ROT>IND and CAL>TTH>IND>NAT>ROT, respectively. Total amounts of N, P, K, Ca, and Mg in the soil were significantly (P < 0.05) highest under TTH and lowest under NAT. The fallow and ROT systems did not affect the C/N, C/P, and N/P ratios in the soil but significantly did so in the LL and LM fractions of SOM. Significant correlations indicated that the P content in the LL and LM fractions of SOM may help determine the amounts of NaHCO3-extractable Pi and Po, which may therefore serve as sensitive indicators of `readily available' and `readily mineralizable' soil P pools, respectively, in the volcanic-ash soils of the Andes.", "keywords": ["2. Zero hunger", "rotaci\u00f3n de cultivos", "soil chemicophysical properties", "soil fertility", "materia org\u00e1nica del suelo", "calliandra calothyrsus", "04 agricultural and veterinary sciences", "rotational cropping", "fertilidad del suelo", "15. Life on land", "fallow systems", "indigofera constricta", "sistemas con barbecho", "soil organic matter", "tithonia diversifolia", "propiedades f\u00edsico - qu\u00edmicas suelo", "0401 agriculture", " forestry", " and fisheries", "phosphorus"]}, "links": [{"href": "https://doi.org/10.1023/a:1010310300067"}, {"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": "10.1023/a:1010310300067", "name": "item", "description": "10.1023/a:1010310300067", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1023/a:1010310300067"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2001-04-01T00:00:00Z"}}, {"id": "10.1029/2007gb003168", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:17:33Z", "type": "Journal Article", "created": "2009-04-03", "title": "Grazing Effects On Belowground C And N Stocks Along A Network Of Cattle Exclosures In Temperate And Subtropical Grasslands Of South America", "description": "<p>We evaluated the effects of grazing on C and N belowground pools by comparing 15 grazing\uffe2\uff80\uff90exclosure pairs across the R\uffc3\uffado de la Plata grasslands of Uruguay and Argentina. We measured C and N pools of belowground biomass, particulate organic matter (POM), and the mineral associated organic matter (MAOM) in the top meter of the soil. Grazing exclusion in the R\uffc3\uffado de la Plata grasslands promoted (1) decreased belowground biomass stocks across all sites, (2) increased soil organic carbon (SOC) and soil organic nitrogen (SON) stocks in upland soils, and (3) decreased stocks in shallow and lowland soils. In all cases, SOC and SON variations were largely derived by changes in MAOM stocks that maintained their C:N ratios unchanged. In contrast, stocks of the labile POM fractions changed little, but C:N ratios of these fractions decreased after grazing removal. We hypothesize that changes in soil organic matter (SOM) contents between grazed and ungrazed stands result from the balance between changes in belowground N allocation patterns (root N retention hypothesis) and the ability of the soil to retain the extra N available after the exclusion of herbivores and the cessation of volatilization and leaching from urine and dung patches (N loss hypothesis). On the basis of our results we suggest that the relative importance of these two cooccurring mechanisms will shape grazing effects on SOM stocks, depending on soil properties, including texture, pH and soil depth, and vegetation type, particularly allocation patterns and C:N ratios of different plant species.</p>", "keywords": ["2. Zero hunger", "ARGENTINA", "GRAZING", "AGRICULTURE", "SOIL SCIENCES", "SOIL ORGANIC MATTER", "RANGE MANAGEMENT", "04 agricultural and veterinary sciences", "15. Life on land", "carbono", "pastoreo", "nitrogeno", "13. Climate action", "URUGUAY", "gradientes", "https://purl.org/becyt/ford/4.1", "0401 agriculture", " forestry", " and fisheries", "https://purl.org/becyt/ford/4", "GRASSLANDS", "AGROCHEMICALS"]}, "links": [{"href": "https://doi.org/10.1029/2007gb003168"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Biogeochemical%20Cycles", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1029/2007gb003168", "name": "item", "description": "10.1029/2007gb003168", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1029/2007gb003168"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2009-04-04T00:00:00Z"}}, {"id": "10.1029/95gb02148", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:17:36Z", "type": "Journal Article", "created": "2004-02-04", "title": "Belowground Cycling Of Carbon In Forests And Pastures Of Eastern Amazonia", "description": "<p>Forests in seasonally dry areas of eastern Amazonia near Paragominas, Par\uffc3\uffa1, Brazil, maintain an evergreen forest canopy through an extended dry season by taking up soil water through deep (&gt;1 m) roots. Belowground allocation of C in these deep\uffe2\uff80\uff90rooting forests is very large (1900 g C m\uffe2\uff88\uff922 yr\uffe2\uff88\uff921) relative to litterfall (460 g C m\uffe2\uff88\uff922 yr\uffe2\uff88\uff921). The presence of live roots drives an active carbon cycle deeper than l m in the soil. Although bulk C concentrations and 14C contents of soil organic matter at &gt;l\uffe2\uff80\uff90m depths are low, estimates of turnover from fine\uffe2\uff80\uff90root inputs, CO2 production, and the 14C content of CO2 produced at depth show that up to 15% of the carbon inventory in the deep soil has turnover times of decades or less. Thus the amount of fast\uffe2\uff80\uff90cycling soil carbon between 1 and 8\uffe2\uff80\uff90m depths (2\uffe2\uff80\uff933 kg C m\uffe2\uff88\uff922, out of 17\uffe2\uff80\uff9318 kg C m\uffe2\uff88\uff922) is significant compared to the amount present in the upper meter of soil (3\uffe2\uff80\uff934 kg C m\uffe2\uff88\uff922 out of 10\uffe2\uff80\uff9311 kg C m\uffe2\uff88\uff922). A model of belowground carbon cycling derived from measurements of carbon stocks and fluxes, and constrained using carbon isotopes, is used to predict C fluxes associated with conversion of deep\uffe2\uff80\uff90rooting forests to pasture and subsequent pasture management. The relative proportions and turnover times of active (including detrital plant material; 1\uffe2\uff80\uff933 year turnover), slow (decadal and shorter turnover), and passive (centennial to millennial turnover) soil organic matter pools are determined by depth for the forest soil, using constraints from measurements of C stocks, fluxes, and isotopic content. Reduced carbon inputs to the soil in degraded pastures, which are less productive than the forests they replace, lead to a reduction in soil carbon inventory and \uffce\uff9414C, in accord with observations. Managed pastures, which have been fertilized with phosphorous and planted with more productive grasses, show increases in C and 14C over forest values. Carbon inventory increases in the upper meter of managed pasture soils are partially offset by predicted carbon losses due to death and decomposition of fine forest roots at depths &gt;1 m in the soil. The major adjustments in soil carbon inventory in response to land management changes occur within the first decade after conversion. Carbon isotopes are shown to be more sensitive indicators of recent accumulation or loss of soil organic matter than direct measurement of soil C inventories.</p>", "keywords": ["cycling", "decomposition", "model", "rooting", "carbon", "belowground carbon cycling", "carbon cycling", "04 agricultural and veterinary sciences", "South America", "15. Life on land", "Poaceae", "soil", "pasture", "forest", "Amazonia", "soil organic matter", "death", "tropical soil", "0401 agriculture", " forestry", " and fisheries", "phosphorus", "Brazil", "organic matter"]}, "links": [{"href": "https://escholarship.org/content/qt1zb7d8kx/qt1zb7d8kx.pdf"}, {"href": "https://doi.org/10.1029/95gb02148"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Biogeochemical%20Cycles", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1029/95gb02148", "name": "item", "description": "10.1029/95gb02148", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1029/95gb02148"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "1995-12-01T00:00:00Z"}}, {"id": "10.1038/s41467-022-31540-9", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:17:41Z", "type": "Journal Article", "created": "2022-07-01", "title": "Global stocks and capacity of mineral-associated soil organic carbon", "description": "Abstract<p>Soil is the largest terrestrial reservoir of organic carbon and is central for climate change mitigation and carbon-climate feedbacks. Chemical and physical associations of soil carbon with minerals play a critical role in carbon storage, but the amount and global capacity for storage in this form remain unquantified. Here, we produce spatially-resolved global estimates of mineral-associated organic carbon stocks and carbon-storage capacity by analyzing 1144 globally-distributed soil profiles. We show that current stocks total 899 Pg C to a depth of 1\uffe2\uff80\uff89m in non-permafrost mineral soils. Although this constitutes 66% and 70% of soil carbon in surface and deeper layers, respectively, it is only 42% and 21% of the mineralogical capacity. Regions under agricultural management and deeper soil layers show the largest undersaturation of mineral-associated carbon. Critically, the degree of undersaturation indicates sequestration efficiency over years to decades. We show that, across 103 carbon-accrual measurements spanning management interventions globally, soils furthest from their mineralogical capacity are more effective at accruing carbon; sequestration rates average 3-times higher in soils at one tenth of their capacity compared to soils at one half of their capacity. Our findings provide insights into the world\uffe2\uff80\uff99s soils, their capacity to store carbon, and priority regions and actions for soil carbon management.</p", "keywords": ["Carbon sequestration", "550", "Permafrost", "/704/106/47/4113", "Carbon Dynamics in Peatland Ecosystems", "Digital Soil Mapping Techniques", "Oceanography", "01 natural sciences", "Agricultural and Biological Sciences", "Soil", "Soil water", "Carbon fibers", "Climate change", "2. Zero hunger", "Minerals", "Ecology", "Forestry Sciences", "Q", "Total organic carbon", "article", "Life Sciences", "Composite number", "Geology", "Agriculture", "/704/106/694/682", "Soil carbon", "Chemistry", "/704/47/4113", "CESD-Soil Quality", "Physical Sciences", "Environmental chemistry", "Engineering sciences. Technology", "Composite material", "/141", "Carbon Sequestration", "Environmental Engineering", "Life on Land", "Science", "[SDU.STU]Sciences of the Universe [physics]/Earth Sciences", "Veterinary and Food Sciences", "Soil Science", "/704/106/694/1108", "Environmental science", "Article", "Digital Soil Mapping", "[SDU] Sciences of the Universe [physics]", "Global Soil Information", "Soil Carbon Sequestration", "Biology", "0105 earth and related environmental sciences", "Soil science", "Agricultural", "Soil organic matter", "FOS: Environmental engineering", "Soil Properties", "FOS: Earth and related environmental sciences", "15. Life on land", "Materials science", "Carbon", "Carbon dioxide", "[SDU]Sciences of the Universe [physics]", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "[SDU.STU] Sciences of the Universe [physics]/Earth Sciences", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems", "/119", "Climate Change Impacts and Adaptation", "Environmental Sciences"]}, "links": [{"href": "https://www.nature.com/articles/s41467-022-31540-9.pdf"}, {"href": "https://escholarship.org/content/qt2vm0b30s/qt2vm0b30s.pdf"}, {"href": "https://doi.org/10.1038/s41467-022-31540-9"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature%20Communications", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s41467-022-31540-9", "name": "item", "description": "10.1038/s41467-022-31540-9", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41467-022-31540-9"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-07-01T00:00:00Z"}}, {"id": "10.1038/s41467-019-11993-1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:17:40Z", "type": "Journal Article", "created": "2019-09-04", "title": "Plant roots increase both decomposition and stable organic matter formation in boreal forest soil", "description": "Abstract<p>Boreal forests are ecosystems with low nitrogen (N) availability that store globally significant amounts of carbon (C), mainly in plant biomass and soil organic matter (SOM). Although crucial for future climate change predictions, the mechanisms controlling boreal C and N pools are not well understood. Here, using a three-year field experiment, we compare SOM decomposition and stabilization in the presence of roots, with exclusion of roots but presence of fungal hyphae and with exclusion of both roots and fungal hyphae. Roots accelerate SOM decomposition compared to the root exclusion treatments, but also promote a different soil N economy with higher concentrations of organic soil N compared to inorganic soil N accompanied with the build-up of stable SOM-N. In contrast, root exclusion leads to an inorganic soil N economy (i.e., high level of inorganic N) with reduced stable SOM-N build-up. Based on our findings, we provide a framework on how plant roots affect SOM decomposition and stabilization.</p>", "keywords": ["roots", "0106 biological sciences", "330", "Nitrogen", "Science", "ta1171", "Hyphae", "Models", " Biological", "Plant Roots", "01 natural sciences", "Article", "LITTER DECOMPOSITION", "Soil", "POLYPHENOLS", "CARBON SEQUESTRATION", "soil organic matter", "Taiga", "SDG 13 - Climate Action", "SUGAR MAPLE", "Biomass", "Organic Chemicals", "forest ecology", "106026 Ecosystem research", "Ecosystem", "Soil Microbiology", "TANNINS", "2. Zero hunger", "106022 Mikrobiologie", "ECTOMYCORRHIZAL FUNGI", "MYCORRHIZA", "Q", "ta1182", "Forestry", "04 agricultural and veterinary sciences", "Plants", "15. Life on land", "Carbon", "Environmental sciences", "NITROGEN", "Boreal forests", "106026 \u00d6kosystemforschung", "13. Climate action", "SDG 13 \u2013 Ma\u00dfnahmen zum Klimaschutz", "106022 Microbiology", "ta1181", "0401 agriculture", " forestry", " and fisheries", "COMMUNITIES", "STORAGE"]}, "links": [{"href": "https://www.nature.com/articles/s41467-019-11993-1.pdf"}, {"href": "https://doi.org/10.1038/s41467-019-11993-1"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature%20Communications", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s41467-019-11993-1", "name": "item", "description": "10.1038/s41467-019-11993-1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41467-019-11993-1"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-09-04T00:00:00Z"}}, {"id": "10.1038/s43247-022-00523-5", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:17:46Z", "type": "Journal Article", "created": "2022-08-18", "title": "Ecoenzymatic stoichiometry reveals widespread soil phosphorus limitation to microbial metabolism across Chinese forests", "description": "Abstract<p>Forest soils contain a large amount of organic carbon and contribute to terrestrial carbon sequestration. However, we still have a poor understanding of what nutrients limit soil microbial metabolism that drives soil carbon release across the range of boreal to tropical forests. Here we used ecoenzymatic stoichiometry methods to investigate the patterns of microbial nutrient limitations within soil profiles (organic, eluvial and parent material horizons) across 181 forest sites throughout China. Results show that, in 80% of these forests, soil microbes were limited by phosphorus availability. Microbial phosphorus limitation increased with soil depth and from boreal to tropical forests as ecosystems become wetter, warmer, more productive, and is affected by anthropogenic nitrogen deposition. We also observed an unexpected shift in the latitudinal pattern of microbial phosphorus limitation with the lowest phosphorus limitation in the warm temperate zone (41-42\uffc2\uffb0N). Our study highlights the importance of soil phosphorus limitation to restoring forests and predicting their carbon sinks.</p", "keywords": ["0301 basic medicine", "Biogeochemical Cycling of Nutrients in Aquatic Ecosystems", "Nitrogen", "Soil Science", "Organic chemistry", "Carbon Dynamics in Peatland Ecosystems", "Nitrogen cycle", "Environmental science", "Nutrient cycle", "Agricultural and Biological Sciences", "03 medical and health sciences", "Terrestrial ecosystem", "XXXXXX - Unknown", "Taiga", "Soil water", "Environmental Chemistry", "GE1-350", "Biology", "Ecosystem", "Soil science", "2. Zero hunger", "QE1-996.5", "Soil organic matter", "Ecology", "Life Sciences", "Geology", "Phosphorus", "Carbon cycle", "04 agricultural and veterinary sciences", "15. Life on land", "Soil carbon", "Environmental sciences", "Temperate climate", "Chemistry", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "Physical Sciences", "0401 agriculture", " forestry", " and fisheries", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems", "Ecosystem Functioning", "Nutrient"]}, "links": [{"href": "https://doi.org/10.1038/s43247-022-00523-5"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Communications%20Earth%20%26amp%3B%20Environment", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s43247-022-00523-5", "name": "item", "description": "10.1038/s43247-022-00523-5", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s43247-022-00523-5"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-08-18T00:00:00Z"}}, {"id": "10.1111/gcb.15496", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:41Z", "type": "Journal Article", "created": "2020-12-20", "title": "Topsoil organic matter build\u2010up in glacier forelands around the world", "description": "Abstract<p>Since the last glacial maximum, soil formation related to ice\uffe2\uff80\uff90cover shrinkage has been one major sink of carbon accumulating as soil organic matter (SOM), a phenomenon accelerated by the ongoing global warming. In recently deglacierized forelands, processes of SOM accumulation, including those that control carbon and nitrogen sequestration rates and biogeochemical stability of newly sequestered carbon, remain poorly understood. Here, we investigate the build\uffe2\uff80\uff90up of SOM during the initial stages (up to 410\uffc2\uffa0years) of topsoil development in 10 glacier forelands distributed on four continents. We test whether the net accumulation of SOM on glacier forelands (i) depends on the time since deglacierization and local climatic conditions (temperature and precipitation); (ii) is accompanied by a decrease in its stability and (iii) is mostly due to an increasing contribution of organic matter from plant origin. We measured total SOM concentration (carbon, nitrogen), its relative hydrogen/oxygen enrichment, stable isotopic (13C, 15N) and carbon functional groups (C\uffe2\uff80\uff90H, C=O, C=C) compositions, and its distribution in carbon pools of different thermal stability. We show that SOM content increases with time and is faster on forelands experiencing warmer climates. The build\uffe2\uff80\uff90up of SOM pools shows consistent trends across the studied soil chronosequences. During the first decades of soil development, the low amount of SOM is dominated by a thermally stable carbon pool with a small and highly thermolabile pool. The stability of SOM decreases with soil age at all sites, indicating that SOM storage is dominated by the accumulation of labile SOM during the first centuries of soil development, and suggesting plant carbon inputs to soil (SOM depleted in nitrogen, enriched in hydrogen and in aromatic carbon). Our findings highlight the potential vulnerability of SOM stocks from proglacial areas to decomposition and suggest that their durability largely depends on the relative contribution of carbon inputs from plants.</p>", "keywords": ["[SDV.BID.SPT]Life Sciences [q-bio]/Biodiversity/Systematics", "550", "Nitrogen", "Chronosequence", "551", "01 natural sciences", "[SDV.BV.BOT] Life Sciences [q-bio]/Vegetal Biology/Botanics", "Soil", "soil organic matter", "carbon stability; chronosequence; climate sensitivity; soil organic matter; topsoil development; Carbon; Nitrogen; Temperature; Ice Cover; Soil", "[SDV.BID.SPT] Life Sciences [q-bio]/Biodiversity/Systematics", " Phylogenetics and taxonomy", "[SDV.EE.ECO] Life Sciences [q-bio]/Ecology", " environment/Ecosystems", "Ice Cover", "topsoil development", "Carbon stability", "0105 earth and related environmental sciences", "2. Zero hunger", "Soil organic matter", "Temperature", "Phylogenetics and taxonomy", "04 agricultural and veterinary sciences", "[SDV.BV.BOT]Life Sciences [q-bio]/Vegetal Biology/Botanics", "15. Life on land", "Climate sensitivity", "Primary Research Articles", "Carbon", "chronosequence", "[SDE.BE] Environmental Sciences/Biodiversity and Ecology", "13. Climate action", "[SDV.EE.ECO]Life Sciences [q-bio]/Ecology", "[SDE]Environmental Sciences", "Topsoil development", "climate sensitivity", "carbon stability; chronosequence; climate sensitivity; soil organic matter; topsoil development;", "0401 agriculture", " forestry", " and fisheries", "[SDE.BE]Environmental Sciences/Biodiversity and Ecology", "environment/Ecosystems", "carbon stability"]}, "links": [{"href": "https://air.unimi.it/bitstream/2434/851691/2/khedim%202021%20submitted.pdf"}, {"href": "https://air.unimi.it/bitstream/2434/851691/3/khedim%202021%20Global%20Change%20Biol.pdf"}, {"href": "https://boa.unimib.it/bitstream/10281/300214/2/10281-300214_VoR.pdf"}, {"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.15496"}, {"href": "https://doi.org/10.1111/gcb.15496"}, {"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.15496", "name": "item", "description": "10.1111/gcb.15496", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcb.15496"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-01-16T00:00:00Z"}}, {"id": "10.1038/srep08280", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:17:47Z", "type": "Journal Article", "created": "2015-02-06", "title": "Convergence Of Soil Nitrogen Isotopes Across Global Climate Gradients", "description": "Abstract<p>Quantifying global patterns of terrestrial nitrogen (N) cycling is central to predicting future patterns of primary productivity, carbon sequestration, nutrient fluxes to aquatic systems and climate forcing. With limited direct measures of soil N cycling at the global scale, syntheses of the 15N:14N ratio of soil organic matter across climate gradients provide key insights into understanding global patterns of N cycling. In synthesizing data from over 6000 soil samples, we show strong global relationships among soil N isotopes, mean annual temperature (MAT), mean annual precipitation (MAP) and the concentrations of organic carbon and clay in soil. In both hot ecosystems and dry ecosystems, soil organic matter was more enriched in 15N than in corresponding cold ecosystems or wet ecosystems. Below a MAT of 9.8\uffc2\uffb0C, soil \uffce\uffb415N was invariant with MAT. At the global scale, soil organic C concentrations also declined with increasing MAT and decreasing MAP. After standardizing for variation among mineral soils in soil C and clay concentrations, soil \uffce\uffb415N showed no consistent trends across global climate and latitudinal gradients. Our analyses could place new constraints on interpretations of patterns of ecosystem N cycling and global budgets of gaseous N loss.</p>", "keywords": ["N-15 Natural-Abundance", "550", "Ecosystem ecology", "TROPICAL FORESTS", "Organic chemistry", "Suelo", "Nitrogen cycle", "01 natural sciences", "Nutrient cycle", "cycle de l'azote", "CARBON", "Agricultural and Biological Sciences", "Soil", "Terrestrial ecosystem", "Isotopes", "https://purl.org/becyt/ford/1.6", "Soil water", "SDG 13 - Climate Action", "N-15 NATURAL-ABUNDANCE", "Climate change", "croisement de donn\u00e9es", "Milieux et Changements globaux", "SDG 15 \u2013 Leben an Land", "Global change", "SDG 15 - Life on Land", "2. Zero hunger", "106022 Mikrobiologie", "Climatic Factors", "Tropical Forests", "Ecology", "Geography", "Nitr\u00f3geno", "Nutrient Cycling", "FRACTIONATION", "Litter Decomposition", "ECOSYSTEM ECOLOGY", "Life Sciences", "ecosystem ecology", "Cycling", "Forestry", "Is\u00f3topos", "Carbon cycle", "04 agricultural and veterinary sciences", "Nitrogen Cycle", "Soil carbon", "6. Clean water", "Organic-Matter", "Earth and Planetary Sciences", "ORGANIC-MATTER", "Chemistry", "PRECIPITATION", "SDG 13 \u2013 Ma\u00dfnahmen zum Klimaschutz", "Physical Sciences", "106022 Microbiology", "carbone du sol", "Stable Isotope Analysis of Groundwater and Precipitation", "Ecosystem Functioning", "570", "STABLE ISOTOPE", "Biogeochemical Cycling of Nutrients in Aquatic Ecosystems", "Stable isotope analysis", "Nitrogen", "[SDE.MCG]Environmental Sciences/Global Changes", "Soil Science", "stable isotope analysis;ecosystem ecology", "Article", "Environmental science", "LITTER DECOMPOSITION", "sol min\u00e9ral", "INORGANIC NITROGEN", "Geochemistry and Petrology", "stable isotope analysis", "Carbono", "Environmental Chemistry", "Factores Clim\u00e1ticos", "https://purl.org/becyt/ford/1", "Biology", "Ecosystem", "0105 earth and related environmental sciences", "Soil science", "Soil organic matter", "Soil Fertility", "climat", "AVAILABILITY", "Nitrogen Dynamics", "15. Life on land", "Carbon", "Inorganic", "NITROGEN", "MODEL", "[SDE.MCG] Environmental Sciences/Global Changes", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "PATTERNS", "0401 agriculture", " forestry", " and fisheries", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems"]}, "links": [{"href": "https://scholars.unh.edu/context/faculty_pubs/article/1042/viewcontent/srep08280.pdf"}, {"href": "https://edoc.unibas.ch/37215/1/srep08280.pdf"}, {"href": "https://doi.org/10.1038/srep08280"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Scientific%20Reports", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/srep08280", "name": "item", "description": "10.1038/srep08280", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/srep08280"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2015-02-06T00:00:00Z"}}, {"id": "10.1046/j.1365-2486.2003.00598.x", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-05-01T16:17:52Z", "type": "Journal Article", "created": "2003-05-06", "title": "Soil Organic Matter Biochemistry And Potential Susceptibility To Climatic Change Across The Forest-Tundra Ecotone In The Fennoscandian Mountains", "description": "Abstract<p>We studied soil organic carbon (C) chemistry at the mountain birch forest\uffe2\uff80\uff90tundra ecotone in three regions of the Fennoscandian mountain range with comparable vegetation cover but contrasting degrees of continentality and latitude. The aim of the study was to identify functional compound classes and their relationships to decomposition and spatial variation across the ecotone and latitudinal gradient. Solid\uffe2\uff80\uff90state 13C nuclear magnetic resonance (CPMAS 13C NMR) was used to identify seven functional groups of soil organic C: alkyls, N\uffe2\uff80\uff90alkyls, O\uffe2\uff80\uff90alkyls, acetals, aromatics, phenolics and carboxyls. N\uffe2\uff80\uff90alkyls, O\uffe2\uff80\uff90alkyls and acetals are generally considered labile substrates for a large number of saprotrophic fungi and bacteria, whilst phenolics and aromatics are mainly decomposed by lignolytic organisms and contribute to the formation of soil organic matter together with aliphatic alkyls and carboxyls. All soils contained a similar proportional distribution of functional groups, although relatively high amounts of N\uffe2\uff80\uff90alkyls, O\uffe2\uff80\uff90alkyls and acetals were present in comparison to earlier published studies, suggesting that large amounts of soil C were potentially vulnerable to microbial degradation. Soil organic matter composition was different at the most southerly site (Dovrefjell, Norway), compared with the two more northerly sites (Abisko, Sweden, and Joatka, Norway), with higher concentrations of aromatics and phenolics, as well as pronounced differences in alkyl concentrations between forest and tundra soils. Clear differences between mountain birch forest and tundra heath soil was noted, with generally higher concentrations of labile carbon present in tundra soils. We conclude that, although mesic soils around the forest\uffe2\uff80\uff90tundra ecotone in Fennoscandia are a potential source of C to the atmosphere in a changing environment, the response is likely to vary between comparable ecosystems in relation to latitude and continentality as well as soil properties especially soil nitrogen content and pH.</p>", "keywords": ["570", "decomposition", "550", "Fennoscandia", "Mass Import - autoclassified (may be erroneous)", "04 agricultural and veterinary sciences", "910", "15. Life on land", "Chemistry", "Soil", "ecotone", "13. Climate action", "soil organic matter", "CPMAS 13C NMR", "Climate change", "0401 agriculture", " forestry", " and fisheries"]}, "links": [{"href": "https://doi.org/10.1046/j.1365-2486.2003.00598.x"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Change%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1046/j.1365-2486.2003.00598.x", "name": "item", "description": "10.1046/j.1365-2486.2003.00598.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1046/j.1365-2486.2003.00598.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2003-05-01T00:00:00Z"}}, {"id": "10.1071/sr07106", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:17:59Z", "type": "Journal Article", "created": "2008-12-02", "title": "Traffic And Tillage Effects On Wheat Production On The Loess Plateau Of China: 1. Crop Yield And Som", "description": "<p>Challenges for dryland farming on the Loess Plateau of China are continuous nutrient loss, low soil organic matter and crop yield, and soil degradation. Controlled traffic, combined with zero or minimum tillage and residue cover, has been proposed to improve soil structure and crop yield. From 1998 to 2006, we conducted a field experiment comparing soil organic matter and wheat productivity between controlled traffic and conventional tillage farming systems. The field experiment was conducted using 2 controlled traffic treatments (zero tillage with residue cover and no compaction, shallow tillage with residue cover and no compaction) and a conventional tillage treatment. Results showed that controlled traffic treatments significantly increased soil organic matter and microbial biomass in the 0\uffe2\uff80\uff930.30\uffe2\uff80\uff89m soil profile. Controlled traffic with zero tillage significantly increased total N in the 0\uffe2\uff80\uff930.05\uffe2\uff80\uff89m soil profile. The mean yield over 8 years of controlled traffic treatments was &gt;10% greater than that of conventional tillage. Controlled traffic farming appears to be a solution to the cropping problems faced on the Loess Plateau of China.</p>", "keywords": ["2. Zero hunger", "Soil organic matter", "Controlled traffic", "Wheat yield", "13. Climate action", "2304 Environmental Chemistry", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land", "1111 Soil Science", "630", "6. Clean water"]}, "links": [{"href": "https://doi.org/10.1071/sr07106"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1071/sr07106", "name": "item", "description": "10.1071/sr07106", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1071/sr07106"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2008-01-01T00:00:00Z"}}, {"id": "10.1071/sr21268", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:01Z", "type": "Journal Article", "created": "2022-01-18", "title": "Lessons from a landmark 1991 article on soil structure: distinct precedence of non-destructive assessment and benefits of fresh perspectives in soil research", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>In 1991, at the launch of a national symposium devoted to soil structure, the Australian Society of Soil Science invited Professor John Letey to deliver a keynote address, which was later published in the society\u2019s journal. In his lecture, he shared the outcome of his reflexion about what the assessment of soil structure should amount to, in order to produce useful insight into the functioning of soils. His viewpoint was that the focus should be put on the openings present in the structure, rather than on the chunks of material resulting from its mechanical dismantlement. In the present article, we provide some historical background for Letey\u2019s analysis, and try to explain why it took a number of years for the paradigm shift that he advocated to begin to occur. Over the last decade, his perspective that soil structure needs to be characterised via non-destructive methods appears to have gained significant momentum, which is likely to increase further in the near future, as we take advantage of recent technological advances. Other valuable lessons that one can derive from Letey\u2019s pioneering article relate to the extreme value for everyone, even neophytes, to constantly ask questions about where research on given topics is heading, what its goals are, and whether the methods that are used at a certain time are optimal.</p></article>", "keywords": ["570", "soil image analysis", "soil microorganisms", "[SDE.MCG]Environmental Sciences/Global Changes", "Soil measuring", "earthworms", "micromorphology", "Aggregate stability", "Soil functions", "01 natural sciences", "630", "Soil fauna", "soil organic matter", "Earthworms", "Micromorphology", "Computed tomography", "aggregate stability", "0105 earth and related environmental sciences", "soil measuring", "2. Zero hunger", "Soil organic matter", "computed tomography", "04 agricultural and veterinary sciences", "soil functions", "15. Life on land", "[SDE.MCG] Environmental Sciences/Global Changes", "Soil image analysis", "0401 agriculture", " forestry", " and fisheries", "soil fauna", "earthworms; micromorphology", "Soil microorganisms"]}, "links": [{"href": "https://doi.org/10.1071/sr21268"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1071/sr21268", "name": "item", "description": "10.1071/sr21268", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1071/sr21268"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-01-19T00:00:00Z"}}, {"id": "10.2174/1874331501307010022", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:20:27Z", "type": "Journal Article", "created": "2013-02-13", "description": "It is expected that the agricultural intensification occurred in recent decades in the Argentine Rolling Pampa significantly alters the SOM reserves. Therefore, it is necessary to identify soil organic carbon (C) and nitrogen (N) fractions to understand the functionality and stabilization of these reserves. Our objectives were to study the NT effect in two crop rotations, corn-double cropped wheat/soybean (MWS) and double cropped wheat/soybean (WS) on: 1) SOM and its particle size and biological fractions contents, 2) C and N stubble biomass and 3) some soil properties in order to explain the SOM differences found. The larger biomass residue remaining on the soil surface under NT promoted higher aggregate stability and lower soil temperature and pH. At 0-5 cm soil depth, NT exhibited higher C and N contents, for both uncomplexed and intimately associated to the mineral components fractions. However, the results indicated variations in the SOM protection according to the rotation: in MWS the high aggregate stability showed better physical protection, while in WS the greater cation exchange capacity and the lower value of N released by anaerobic incubation would indicate the presence of transformed SOM. At 5-20 cm soil depth, only in WS, C microbial biomass was higher with a low metabolic rate, indicating again the presence of highly decomposed SOM. The results obtained in WS under NT would indicate the possibility of achieving slower recycled of the SOM.", "keywords": ["Rotaci\u00f3n de Cultivos", "[SDE] Environmental Sciences", "soil organic matter fractions", "Plant Soil Relations", "Propiedades F\u00edsico-qu\u00edmicas Suelo", "Residuos de Cosechas", "Nitrogen", "[SDV]Life Sciences [q-bio]", "Crop Residues", "Conventional Tillage", "Materia Org\u00e1nica", "Labranza Convencional", "630", "Regi\u00f3n Pampa Ondulada", "no tillage;crop rotations;soil organic matter fractions", "Crop Rotation", "no tillage", "crop rotations", "Carbono", "[SDV.BV]Life Sciences [q-bio]/Vegetal Biology", "[SDV.BV] Life Sciences [q-bio]/Vegetal Biology", "Zero Tillage", "2. Zero hunger", "Nitr\u00f3geno", "Soil Biology", "04 agricultural and veterinary sciences", "15. Life on land", "Relaciones Planta Selo", "Carbon", "[SDV] Life Sciences [q-bio]", "Organic Matter", "[SDE]Environmental Sciences", "0401 agriculture", " forestry", " and fisheries", "Soil Organic Matter Fractions", "Biolog\u00eda del Suelo", "Fracciones de la Materia Org\u00e1nica", "Cero-labranza"], "contacts": [{"organization": "Irizar, A, Andriulo, Adrian Enrique, Mary, Bruno, B.,", "roles": ["creator"]}]}, "links": [{"href": "https://hal.inrae.fr/hal-02642900/file/2013_Irizar_Open%20Agriculture%20Journal_1.pdf"}, {"href": "https://doi.org/10.2174/1874331501307010022"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/The%20Open%20Agriculture%20Journal", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.2174/1874331501307010022", "name": "item", "description": "10.2174/1874331501307010022", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.2174/1874331501307010022"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2013-02-08T00:00:00Z"}}, {"id": "10.1080/00103624.2013.790406", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:05Z", "type": "Journal Article", "created": "2013-04-16", "title": "Influence Of Soil Management And Crop Rotation On Physical Properties In A Long-Term Experiment In Parana, Brazil", "description": "This work aims to evaluate the soil physical properties affected by cover crop rotation and soil management in a long-term experiment in southern Brazil. The experiment was established in 1986, with treatments combining six winter treatments and two tillage systems (conventional and no tillage). Bulk density, porosity, aggregate-size class distribution, and organic carbon content of the aggregates were determined at six depths. Bulk density was not affected by tillage systems and winter treatments. The soil disturbance by plowing enhanced the macroporosity, decreased the microporosity, and promoted the formation of smaller aggregate size, in comparison to no tillage. Apart from the soil management, all winter species increased the greater aggregate-size classes, mean weight diameter, geometric mean diameter, and aggregate stability index compared to the fallow treatments. At the no-till treatments, the greater part of sequestered carbon into the soil was stored into the lower and bigger soil aggregates.", "keywords": ["STABILIZATION", "[SDV]Life Sciences [q-bio]", "cover crop", "AGGREGATE", "PARTICULATE", "ORGANIC-MATTER DYNAMICS", "630", "CARBON", "soil organic matter", "Farm nutrient management", "CONSERVATION TILLAGE", "Conservation tillage", "2. Zero hunger", "CULTIVATED SOILS", "04 agricultural and veterinary sciences", "15. Life on land", "sustainability", "Soil tillage", "6. Clean water", "[SDV] Life Sciences [q-bio]", "Crop combinations and interactions", "subtropical soil", "0401 agriculture", " forestry", " and fisheries", "NO-TILLAGE", "CONVENTIONAL-TILLAGE", "FRACTIONS"]}, "links": [{"href": "https://doi.org/10.1080/00103624.2013.790406"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Communications%20in%20Soil%20Science%20and%20Plant%20Analysis", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1080/00103624.2013.790406", "name": "item", "description": "10.1080/00103624.2013.790406", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1080/00103624.2013.790406"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2013-07-20T00:00:00Z"}}, {"id": "10.1088/1748-9326/ab239c", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:17Z", "type": "Journal Article", "created": "2019-05-30", "title": "Global soil acidification impacts on belowground processes", "description": "Abstract                <p>With continuous nitrogen (N) enrichment and sulfur (S) deposition, soil acidification has accelerated and become a global environmental issue. However, a full understanding of the general pattern of ecosystem belowground processes in response to soil acidification due to the impacting factors remains elusive. We conducted a meta-analysis of soil acidification impacts on belowground functions using 304 observations from 49 independent studies, mainly including soil cations, soil nutrient, respiration, root and microbial biomass. Our results show that acid addition significantly reduced soil pH by 0.24 on average, with less pH decrease in forest than non-forest ecosystems. The response ratio of soil pH was positively correlated with site precipitation and temperature, but negatively with initial soil pH. Soil base cations (Ca2+, Mg2+, Na+) decreased while non-base cations (Al3+, Fe3+) increased with soil acidification. Soil respiration, fine root biomass, microbial biomass carbon and nitrogen were significantly reduced by 14.7%, 19.1%, 9.6% and 12.1%, respectively, under acid addition. These indicate that soil carbon processes are sensitive to soil acidification. Overall, our meta-analysis suggests a strong negative impact of soil acidification on belowground functions, with the potential to suppress soil carbon emission. It also arouses our attention to the toxic effects of soil ions on terrestrial ecosystems.</p>", "keywords": ["Biomass (ecology)", "Organic chemistry", "Soil pH", "soil respiration", "Environmental technology. Sanitary engineering", "Agricultural and Biological Sciences", "Engineering", "Terrestrial ecosystem", "Soil water", "Climate change", "GE1-350", "TD1-1066", "Ecology", "Physics", "Soil Water Retention", "Ocean acidification", "Q", "Life Sciences", "Soil respiration", "04 agricultural and veterinary sciences", "Soil carbon", "6. Clean water", "Chemistry", "Physical Sciences", "Environmental chemistry", "soil cations", "microbes", "Mechanics and Transport in Unsaturated Soils", "Nitrogen", "Science", "QC1-999", "Materials Science", "Soil Science", "Thermal Effects on Soil", "Environmental science", "Biomaterials", "soil pH", "acid deposition", "Soil Carbon Sequestration", "Biology", "Soil acidification", "Ecosystem", "Civil and Structural Engineering", "Applications of Clay Nanotubes in Various Fields", "Soil science", "Soil organic matter", "Soil Fertility", "15. Life on land", "Soil biodiversity", "Agronomy", "meta-analysis", "Environmental sciences", "Soil Hydraulic Properties", "13. Climate action", "FOS: Biological sciences", "Bulk soil", "0401 agriculture", " forestry", " and fisheries", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems", "Nutrient"]}, "links": [{"href": "https://doi.org/10.1088/1748-9326/ab239c"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Environmental%20Research%20Letters", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1088/1748-9326/ab239c", "name": "item", "description": "10.1088/1748-9326/ab239c", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1088/1748-9326/ab239c"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-07-01T00:00:00Z"}}, {"id": "10.1093/nsr/nwab120", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:21Z", "type": "Journal Article", "created": "2021-06-29", "title": "Significant loss of soil inorganic carbon at the continental scale", "description": "Abstract                <p>Widespread soil acidification due to atmospheric acid deposition and agricultural fertilization may greatly accelerate soil carbonate dissolution and CO2 release. However, to date, few studies have addressed these processes. Here, we use meta-analysis and nationwide-survey datasets to investigate changes in soil inorganic carbon (SIC) stocks in China. We observe an overall decrease in SIC stocks in topsoil (0\uffe2\uff80\uff9330\uffc2\uffa0cm) (11.33\uffc2\uffa0g C m\uffe2\uff80\uff932 yr\uffe2\uff80\uff931) from the 1980s to the 2010s. Total SIC stocks have decreased by \uffe2\uff88\uffbc8.99\uffc2\uffa0\uffc2\uffb1\uffc2\uffa02.24% (1.37\uffc2\uffa0\uffc2\uffb1\uffc2\uffa00.37\uffc2\uffa0Pg C). The average SIC losses across China (0.046 Pg C yr\uffe2\uff80\uff931) and in cropland (0.016 Pg C yr\uffe2\uff80\uff931) account for \uffe2\uff88\uffbc17.6%\uffe2\uff80\uff9324.0% of the terrestrial C sink and 57.1% of the soil organic carbon sink in cropland, respectively. Nitrogen deposition and climate change have profound influences on SIC cycling. We estimate that \uffe2\uff88\uffbc19.12%\uffe2\uff80\uff9319.47% of SIC stocks will be further lost by 2100. The consumption of SIC may offset a large portion of global efforts aimed at ecosystem carbon sequestration, which emphasizes the importance of achieving a better understanding of the indirect coupling mechanisms of nitrogen and carbon cycling and of effective countermeasures to minimize SIC loss.</p", "keywords": ["Carbon sequestration", "Cartography", "China", "Mechanics and Transport in Unsaturated Soils", "Carbonate", "Nitrogen", "Soil Science", "Organic chemistry", "Carbon Dynamics in Peatland Ecosystems", "soil inorganic carbon stocks", "Soil pH", "Environmental science", "Carbon sink", "Agricultural and Biological Sciences", "carbonate", "Engineering", "Soil water", "Soil Carbon Sequestration", "Biology", "global change", "Ecosystem", "Soil acidification", "Civil and Structural Engineering", "Soil science", "2. Zero hunger", "Soil organic matter", "Soil Fertility", "Ecology", "Geography", "Soil Water Retention", "Life Sciences", "Cycling", "Forestry", "Carbon cycle", "04 agricultural and veterinary sciences", "15. Life on land", "Topsoil", "Soil carbon", "Chemistry", "Sink (geography)", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "Physical Sciences", "Environmental chemistry", "0401 agriculture", " forestry", " and fisheries", "soil acidification", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems", "Research Article"]}, "links": [{"href": "https://doi.org/10.1093/nsr/nwab120"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/National%20Science%20Review", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1093/nsr/nwab120", "name": "item", "description": "10.1093/nsr/nwab120", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1093/nsr/nwab120"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-07-02T00:00:00Z"}}, {"id": "10.1098/rsta.2023.0139", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:26Z", "type": "Journal Article", "created": "2023-10-10", "title": "Relating mineral\u2013organic matter stabilization mechanisms to carbon quality and age distributions using ramped thermal analysis", "description": "<p>             Organic carbon (OC) association with soil minerals stabilizes OC on timescales reflecting the strength of mineral\uffe2\uff80\uff93C interactions. We applied ramped thermal oxidation to subsoil B horizons with different mineral\uffe2\uff80\uff93C associations to separate OC according to increasing temperature of oxidation, i.e. thermal activation energy. Generally, OC released at lower temperatures was richer in bioavailable forms like polysaccharides, while OC released at higher temperatures was more aromatic. Organic carbon associated with pedogenic oxides was released at lower temperatures and had a narrow range of             14             C content. By contrast, N-rich compounds were released at higher temperatures from samples with 2\uffe2\uff80\uff89:\uffe2\uff80\uff891 clays and short-range ordered (SRO) amorphous minerals. Temperatures of release overlapped for SRO minerals and crystalline oxides, although the mean age of OC released was older for the SRO. In soils with more mixed mineralogy, the added presence of older OC released at temperatures greater than 450\uffc2\uffb0C from clays resulted in a broader distribution of OC ages within the sample, especially for soils rich in 2\uffe2\uff80\uff89:\uffe2\uff80\uff891 layer expandable clays such as smectite. While pedogenic setting affects mineral stability and absolute OC age, mineralogy controls the structure of OC age distribution within a sample, which may provide insight into model structures and OC dynamics under changing conditions.           </p>           <p>This article is part of the Theo Murphy meeting issue \uffe2\uff80\uff98Radiocarbon in the Anthropocene\uffe2\uff80\uff99.</p", "keywords": ["soil minerals", "Soil organic matter", "550", "py-GC/MS", "Articles", "Py-GC/MS", "Radiocarbon", "mineral-associated organic matter", "13. Climate action", "soil organic matter", "radiocarbon", "Mineral-associated organic matter", "radiocarbon; soil organic matter; mineral-associated organic matter; Py-GC/MS; Soil minerals", "Soil minerals"]}, "links": [{"href": "https://escholarship.org/content/qt17101110/qt17101110.pdf"}, {"href": "https://doi.org/10.1098/rsta.2023.0139"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Philosophical%20Transactions%20of%20the%20Royal%20Society%20A%3A%20Mathematical%2C%20Physical%20and%20Engineering%20Sciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1098/rsta.2023.0139", "name": "item", "description": "10.1098/rsta.2023.0139", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1098/rsta.2023.0139"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-10-09T00:00:00Z"}}, {"id": "10.1111/ejss.13532", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-05-01T16:18:38Z", "type": "Journal Article", "created": "2024-07-05", "title": "Role of cover crop roots in soil organic carbon accrual\u2014A review", "description": "Abstract                   <p>Appropriate cover crop (CC) management is an important tool for the improvement of soil carbon stock; however, the relationships between carbon accumulation and CC root traits remain unclear. A literature review was performed to identify the extent and focus of recent research and to answer questions about the role of root traits of CCs in soil C accumulation with regard to species selection, mixture composition and agronomic management. The findings based on the analysis of 69 publications show that a range of root traits such as root biomass, architecture, depth of rooting, root chemical composition, as well as quantity and quality of rhizodeposition, can contribute to soil structure formation and C accumulation. These traits are usually species specific, and it seems that appropriate species combinations in the mixtures can offer the highest potential for optimization of C stock across various environments. However, there has been twice as much recent research on roots of CC monocultures than on mixtures, with little attention paid to agronomic aspects such as plant spatial arrangement or soil tillage in relation to CC root development. Considerations of real management under field conditions could be beneficial in providing greater accuracy of estimation of the contribution of CCs in increasing the SOC stock in croplands.</p", "keywords": ["2. Zero hunger", "agronomy", "EJPSOIL", "soil organic matter", "catch crops", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "root architecture", "15. Life on land", "01 natural sciences", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1111/ejss.13532"}, {"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.13532", "name": "item", "description": "10.1111/ejss.13532", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/ejss.13532"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-07-01T00:00:00Z"}}, {"id": "10.1111/gcb.14815", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:41Z", "type": "Journal Article", "created": "2019-08-30", "title": "How to measure, report and verify soil carbon change to realize the potential of soil carbon sequestration for atmospheric greenhouse gas removal", "description": "Abstract<p>There is growing international interest in better managing soils to increase soil organic carbon (SOC) content to contribute to climate change mitigation, to enhance resilience to climate change and to underpin food security, through initiatives such as international \uffe2\uff80\uff984p1000\uffe2\uff80\uff99 initiative and the FAO's Global assessment of SOC sequestration potential (GSOCseq) programme. Since SOC content of soils cannot be easily measured, a key barrier to implementing programmes to increase SOC at large scale, is the need for credible and reliable measurement/monitoring, reporting and verification (MRV) platforms, both for national reporting and for emissions trading. Without such platforms, investments could be considered risky. In this paper, we review methods and challenges of measuring SOC change directly in soils, before examining some recent novel developments that show promise for quantifying SOC. We describe how repeat soil surveys are used to estimate changes in SOC over time, and how long\uffe2\uff80\uff90term experiments and space\uffe2\uff80\uff90for\uffe2\uff80\uff90time substitution sites can serve as sources of knowledge and can be used to test models, and as potential benchmark sites in global frameworks to estimate SOC change. We briefly consider models that can be used to simulate and project change in SOC and examine the MRV platforms for SOC change already in use in various countries/regions. In the final section, we bring together the various components described in this review, to describe a new vision for a global framework for MRV of SOC change, to support national and international initiatives seeking to effect change in the way we manage our soils.</p>", "keywords": ["[SDE] Environmental Sciences", "550", "BULK-DENSITY", "QH301 Biology", "Climate", "[SDV]Life Sciences [q-bio]", "NEW-ZEALAND", "630", "Soil", "NE/M021327/1", "11. Sustainability", "SDG 13 - Climate Action", "AGRICULTURAL SOILS", "SDG 15 - Life on Land", "General Environmental Science", "agriculture", "2. Zero hunger", "Global and Planetary Change", "reporting", "Measurement", "Ecology", "IN-SITU", "Agricultura", "NE/P019455/1", "carbono org\u00e1nico del suelo", "Agriculture", "LAND-USE CHANGE", "04 agricultural and veterinary sciences", "[SDV] Life Sciences [q-bio]", "climate change", "Sustainability", "[SDE]Environmental Sciences", "Carbon Sequestration", "DIFFUSE-REFLECTANCE SPECTROSCOPY", "LONG-TERM EXPERIMENTS", "330", "Monitoring", "STOCK CHANGES", "MRV", "secuestro de carbon", "12. Responsible consumption", "QH301", "Greenhouse Gases", "ORGANIC-CARBON", "soil organic matter", "greenhouse gases", "Invited Research Reviews", "Environmental Chemistry", "774378", "SDG 2 - Zero Hunger", "European Commission", "resilience", "Climate Solutions", "Soil organic matter", "Soil organic carbon", "Natural Environment Research Council (NERC)", "Verification", "food security", "15. Life on land", "carbon sequestration", "Sustainable Agriculture", "Carbon", "EDDY-COVARIANCE", "soil organic carbon", "monitoring", "Reporting", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "measurement", "verification"]}, "links": [{"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.14815"}, {"href": "https://scholarworks.uvm.edu/context/rsfac/article/1079/viewcontent/Lini2019b.pdf"}, {"href": "https://doi.org/10.1111/gcb.14815"}, {"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.14815", "name": "item", "description": "10.1111/gcb.14815", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcb.14815"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-10-06T00:00:00Z"}}, {"id": "10.1111/gcb.70430", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-05-01T16:18:43Z", "type": "Journal Article", "created": "2025-08-19", "title": "Forest Topsoil Organic Carbon Declines Under Ash Dieback", "description": "ABSTRACT<p>Tree diseases are increasingly affecting woodland ecosystems across the world. However, the impact of these diseases upon the soil, and in particular soil carbon, is still poorly understood. Here we present the results of a field survey of ~100 woodlands across Great Britain measured in 1971, 2001 and 2022 and evaluate the fifty\uffe2\uff80\uff90year trend in topsoil (0\uffe2\uff80\uff9315\uffe2\uff80\uff89cm) carbon based upon measurements of soil organic matter (SOM) and the impact of Hymenoscyphus fraxineus (ash dieback). To better represent the full SOM distribution, including the extremely high SOM measurements, we adopt a Beta mixture modelling approach within a Bayesian framework. Across all woodlands, comprising ~1,500 plots per survey, average SOM remained constant across the fifty\uffe2\uff80\uff90year time series. However, the 311 plots with ash dieback had lower SOM in the most recent survey compared to the 328 plots with ash trees present but no dieback recorded, due to a slight decline in SOM under ash dieback. This resulted in plots with ash dieback having a modelled mean SOM of 12.2% compared to 13.4% in plots without ash dieback, a difference of 1.23 percentage points (95% CI 0.25\uffe2\uff80\uff932.21). Ash dieback was more likely to be recorded in plots that had higher soil pH pre\uffe2\uff80\uff90ash dieback invasion, but the decline in SOM under ash dieback was not explained by changes in soil pH or changes in the ground flora composition. Converting our results to soil C and extrapolating for broadleaved woodland across the entirety of Great Britain, the total amount of topsoil carbon lost to date due to ash dieback could be 6 MtCO2 (\uffc2\uffb1\uffe2\uff80\uff894\uffe2\uff80\uff89s.d.). Our results show the importance of understanding the impacts of tree disease when considering current and future woodland carbon dynamics.</p", "keywords": ["loss on ignition", "soil pH", "soil organic matter", "Fraxinus excelsior", "Hymenoscyphus fraxineus", "tree disease", "woodland", "Research Article"]}, "links": [{"href": "https://doi.org/10.1111/gcb.70430"}, {"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.70430", "name": "item", "description": "10.1111/gcb.70430", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcb.70430"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-08-01T00:00:00Z"}}, {"id": "10.1111/gcbb.12158", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-05-01T16:18:44Z", "type": "Journal Article", "created": "2014-02-05", "title": "Effect Of Physical Weathering On The Carbon Sequestration Potential Of Biochars And Hydrochars In Soil", "description": "Abstract<p>Physical weathering can modify the stability of biochar after field exposure. The aim of our study was to determine the potential carbon sequestration of the two chars at different timescales. We investigated the modification in composition and stability resulting from physical weathering of two different chars produced (i) at low temperature (250\uffc2\uffa0\uffc2\uffb0C) by hydrothermal carbonization (HTC); and (ii) at high temperature (1200\uffc2\uffa0\uffc2\uffb0C) by gasification (GS) using contrasting feedstocks. Physical weathering of HTC and GS placed on a water permeable canvas was performed through successive wetting/drying and freezing/thawing cycles. Carbon loss was assessed by mass balance. Chemical stability of the remaining material was evaluated as resistance to acid dichromate oxidation, and biological stability was assessed during laboratory incubation. Moreover, we assessed modification in potential priming effects due to physical weathering. Physical weathering induced a carbon loss ranging between 10 and 40% of the total C mass depending on the feedstock. This C loss is most probably related to leaching of small particulate and dissolved compounds. GS produced from maize silage showed the highest C loss. The chemical stability of HTC and GS was unaffected by physical weathering. In contrast, physical weathering strongly increased the biological stability of HTC and GS char produced from maize silage. After physical weathering, the half\uffe2\uff80\uff90life (t1/2) of GS was doubled but only slight increase was noted for those of HTC. During the first weeks of incubation, HTC addition to soil stimulated native soil organic matter (SOM) mineralization (positive priming effect), while the GS addition led to protection of the native SOM against biologic degradation (negative priming effect). Physical weathering led to reduction in these priming effects. Model extrapolations based on our data showed that decadal C sequestration potential of GS and HTC is globally equivalent when all losses including those due to priming and physical weathering were taken into account. However, at century scale only GS may have the potential to increase soil C storage.</p>", "keywords": ["priming effect", "[SDE] Environmental Sciences", "2. Zero hunger", "[SDV]Life Sciences [q-bio]", "aging", "gasification", "HTC", "04 agricultural and veterinary sciences", "15. Life on land", "carbon sequestration", "01 natural sciences", "630", "hydrothermal carbonization", "[SDV] Life Sciences [q-bio]", "13. Climate action", "soil organic matter", "[SDE]Environmental Sciences", "weathering", "0401 agriculture", " forestry", " and fisheries", "chemical oxidation", "biochar", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1111/gcbb.12158"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/GCB%20Bioenergy", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/gcbb.12158", "name": "item", "description": "10.1111/gcbb.12158", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcbb.12158"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2014-02-05T00:00:00Z"}}, {"id": "10.1111/j.1365-2486.2005.01001.x", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-05-01T16:18:48Z", "type": "Journal Article", "created": "2005-08-19", "title": "Soil Organic Matter And Litter Chemistry Response To Experimental N Deposition In Northern Temperate Deciduous Forest Ecosystems", "description": "Abstract<p>The effects of atmospheric nitrogen (N) deposition on organic matter decomposition vary with the biochemical characteristics of plant litter. At the ecosystem\uffe2\uff80\uff90scale, net effects are difficult to predict because various soil organic matter (SOM) fractions may respond differentially. We investigated the relationship between SOM chemistry and microbial activity in three northern deciduous forest ecosystems that have been subjected to experimental N addition for 2 years. Extractable dissolved organic carbon (DOC), DOC aromaticity, C\uffe2\uff80\uff83:\uffe2\uff80\uff83N ratio, and functional group distribution, measured by Fourier transform infrared spectra (FTIR), were analyzed for litter and SOM. The largest biochemical changes were found in the sugar maple\uffe2\uff80\uff93basswood (SMBW) and black oak\uffe2\uff80\uff93white oak (BOWO) ecosystems. SMBW litter from the N addition treatment had less aromaticity, higher C\uffe2\uff80\uff83:\uffe2\uff80\uff83N ratios, and lower saturated carbon, lower carbonyl carbon, and higher carboxylates than controls; BOWO litter showed opposite trends, except for carbonyl and carboxylate contents. Litter from the sugar maple\uffe2\uff80\uff93red oak (SMRO) ecosystem had a lower C\uffe2\uff80\uff83:\uffe2\uff80\uff83N ratio, but no change in DOC aromaticity. For SOM, the C\uffe2\uff80\uff83:\uffe2\uff80\uff83N ratio increased with N addition in SMBW and SMRO ecosystems, but decreased in BOWO; N addition did not affect the aromaticity of DOC extracted from mineral soil. All ecosystems showed increases in extractable DOC from both litter and soil in response to N treatment. The biochemical changes are consistent with the divergent microbial responses observed in these systems. Extracellular oxidative enzyme activity has declined in the BOWO and SMRO ecosystems while activity in the SMBW ecosystem, particularly in the litter horizon, has increased. In all systems, enzyme activities associated with the hydrolysis and oxidation of polysaccharides have increased. At the ecosystem scale, the biochemical characteristics of the dominant litter appear to modulate the effects of N deposition on organic matter dynamics.</p>", "keywords": ["Litter Chemistry", "Geology and Earth Sciences", "13. Climate action", "Soil Organic Matter", "Science", "Ecology and Evolutionary Biology", "0401 agriculture", " forestry", " and fisheries", "Nitrogen Deposition", "04 agricultural and veterinary sciences", "15. Life on land", "Dissolved Organic Matter", "Extracellular Enzyme Activity"]}, "links": [{"href": "https://doi.org/10.1111/j.1365-2486.2005.01001.x"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Change%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/j.1365-2486.2005.01001.x", "name": "item", "description": "10.1111/j.1365-2486.2005.01001.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/j.1365-2486.2005.01001.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2005-07-19T00:00:00Z"}}, {"id": "10.1111/j.1365-2486.2005.001058.x", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-05-01T16:18:47Z", "type": "Journal Article", "created": "2005-11-28", "title": "Effects Of Experimental Drought On Soil Respiration And Radiocarbon Efflux From A Temperate Forest Soil", "description": "Abstract<p>Soil moisture affects microbial decay of SOM and rhizosphere respiration (RR) in temperate forest soils, but isolating the response of soil respiration (SR) to summer drought and subsequent wetting is difficult because moisture changes are often confounded with temperature variation. We distinguished between temperature and moisture effects by simulation of prolonged soil droughts in a mixed deciduous forest at the Harvard Forest, Massachusetts. Roofs constructed over triplicate 5 \uffc3\uff97 5\uffe2\uff80\uff83m2plots excluded throughfall water during the summers of 2001 (168\uffe2\uff80\uff83mm) and 2002 (344\uffe2\uff80\uff83mm), while adjacent control plots received ambient throughfall and the same natural temperature regime. In 2003, throughfall was not excluded to assess the response of SR under natural weather conditions after two prolonged summer droughts. Throughfall exclusion significantly decreased mean SR rate by 53\uffe2\uff80\uff83mg\uffe2\uff80\uff83C\uffe2\uff80\uff83m\uffe2\uff88\uff922\uffe2\uff80\uff83h\uffe2\uff88\uff921over 84 days in 2001, and by 68\uffe2\uff80\uff83mg\uffe2\uff80\uff83C\uffe2\uff80\uff83m\uffe2\uff88\uff922\uffe2\uff80\uff83h\uffe2\uff88\uff921over 126 days in 2002, representing 10\uffe2\uff80\uff9330% of annual SR in this forest and 35\uffe2\uff80\uff9375% of annual net ecosystem exchange (NEE) of C. The differences in SR were best explained by differences in gravimetric water content in the Oi horizon (r2=0.69) and the Oe/Oa horizon (r2=0.60). Volumetric water content of the A horizon was not significantly affected by throughfall exclusion. The radiocarbon signature of soil CO2efflux and of CO2respired during incubations of O horizon, A horizon and living roots allowed partitioning of SR into contributions from young C substrate (including RR) and from decomposition of older SOM. RR (root respiration and microbial respiration of young substrates in the rhizosphere) made up 43\uffe2\uff80\uff9371% of the total C respired in the control plots and 41\uffe2\uff80\uff9380% in the exclusion plots, and tended to increase with drought. An exception to this trend was an interesting increase in CO2efflux of radiocarbon\uffe2\uff80\uff90rich substrates during a period of abundant growth of mushrooms.</p><p>Our results suggest that prolonged summer droughts decrease primarily heterotrophic respiration in the O horizon, which could cause increases in the storage of soil organic carbon in this forest. However, the C stored during two summers of simulated drought was only partly released as increased respiration during the following summer of natural throughfall. We do not know if this soil C sink during drought is transient or long lasting. In any case, differential decomposition of the O horizon caused by interannual variation of precipitation probably contributes significantly to observed interannual variation of NEE in temperate forests.</p>", "keywords": ["Ecology", "04 agricultural and veterinary sciences", "Biological Sciences", "15. Life on land", "soil respiration", "6. Clean water", "soil drought", "heterotrophic respiration", "rhizosphere respiration", "13. Climate action", "soil organic matter", "temperate forest", "radiocarbon", "0401 agriculture", " forestry", " and fisheries", "soil wetting", "soil moisture", "Q(10)", "Environmental Sciences"]}, "links": [{"href": "https://escholarship.org/content/qt3mk9v58k/qt3mk9v58k.pdf"}, {"href": "https://doi.org/10.1111/j.1365-2486.2005.001058.x"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Change%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/j.1365-2486.2005.001058.x", "name": "item", "description": "10.1111/j.1365-2486.2005.001058.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/j.1365-2486.2005.001058.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2005-11-28T00:00:00Z"}}], "links": [{"rel": "self", "type": "application/geo+json", "title": "This document as GeoJSON", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=Soil+organic+matter&offset=50&f=json", "hreflang": "en-US"}, {"rel": "alternate", "type": "text/html", "title": "This document as HTML", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=Soil+organic+matter&offset=50&f=html", "hreflang": "en-US"}, {"rel": "collection", "type": "application/json", "title": "Collection URL", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main", "hreflang": "en-US"}, {"type": "application/geo+json", "rel": "prev", "title": "items (prev)", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=Soil+organic+matter&offset=0", "hreflang": "en-US"}, {"rel": "next", "type": "application/geo+json", "title": "items (next)", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=Soil+organic+matter&offset=100", "hreflang": "en-US"}], "numberMatched": 241, "numberReturned": 50, "distributedFeatures": [], "timeStamp": "2026-05-01T20:19:21.305968Z"}