{"type": "FeatureCollection", "features": [{"id": "10.1016/j.scitotenv.2016.03.243", "type": "Feature", "geometry": null, "properties": {"license": "Restricted", "updated": "2026-06-24T16:17:26Z", "type": "Journal Article", "created": "2016-05-02", "title": "Fire-Induced Pine Woodland To Shrubland Transitions In Southern Europe May Promote Shifts In Soil Fertility", "description": "Since the mid of the last century, fire recurrence has increased in the Iberian Peninsula and in the overall Mediterranean basin due to changes in land use and climate. The warmer and drier climate projected for this region will further increase the risk of wildfire occurrence and recurrence. Although the impact of wildfires on soil nutrient content in this region has been extensively studied, still few works have assessed this impact on the basis of fire recurrence. This study assesses the changes in soil organic C and nutrient status of mineral soils in two Southern European areas, V\u00e1rzea (Northern Portugal) and Valencia (Eastern Spain), affected by different levels of fire recurrence and where short fire intervals have promoted a transition from pine woodlands to shrublands. At the short-term (<1year), the amount of soil organic matter was higher in burned than in unburned soils while its quality (represented as labile to total organic matter) was actually lower. In any case, total and labile soil organic matter showed decreasing trends with increasing fire recurrence (one to four fires). At the long-term (>5years), a decline in overall soil fertility with fire recurrence was also observed, with a drop between pine woodlands (one fire) and shrublands (two and three fires), particularly in the soil microsites between shrubs. Our results suggest that the current trend of increasing fire recurrence in Southern Europe may result in losses or alterations of soil organic matter, particularly when fire promotes a transition from pine woodland to shrubland. The results also point to labile organic matter fractions in the intershrub spaces as potential early warning indicators for shifts in soil fertility in response to fire recurrence.", "keywords": ["2. Zero hunger", "550", "Microsite", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "Early warning indicators", "Soil quality", "13. Climate action", "Fire frequency", "Sudden shift", "0401 agriculture", " forestry", " and fisheries", "Mediterranean region", "Mineral soil", "Pinus spp. woodlands", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1016/j.scitotenv.2016.03.243"}, {"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.2016.03.243", "name": "item", "description": "10.1016/j.scitotenv.2016.03.243", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.scitotenv.2016.03.243"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2016-12-01T00:00:00Z"}}, {"id": "10.1016/j.soilbio.2010.07.011", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:17:36Z", "type": "Journal Article", "created": "2010-07-28", "title": "Resistance Of Microbial And Soil Properties To Warming Treatment Seven Years After Boreal Fire", "description": "Boreal forests store a large fraction of global terrestrial carbon and are susceptible to environmental change, particularly rising temperatures and increased fire frequency. These changes have the potential to drive positive feedbacks between climate warming and the boreal carbon cycle. Because few studies have examined the warming response of boreal ecosystems recovering from fire, we established a greenhouse warming experiment near Delta Junction, Alaska, seven years after a 1999 wildfire. We hypothesized that experimental warming would increase soil CO2 efflux, stimulate nutrient mineralization, and alter the composition and function of soil fungal communities. Although our treatment resulted in 1.20 \u00b0C soil warming, we found little support for our hypothesis. Only the activities of cellulose- and chitin-degrading enzymes increased significantly by 15% and 35%, respectively, and there were no changes in soil fungal communities. Warming resulted in drier soils, but the corresponding change in soil water potential was probably not sufficient to limit microbial activity. Rather, the warming response of this soil may be constrained by depletion of labile carbon substrates resulting from combustion and elevated soil temperatures in the years after the 1999 fire. We conclude that positive feedbacks between warming and the microbial release of soil carbon are weak in boreal ecosystems lacking permafrost. Since permafrost-free soils underlie 45\u201360% of the boreal zone, our results should be useful for modeling the warming response during recovery from fire in a large fraction of the boreal forest.", "keywords": ["0301 basic medicine", "Decomposition", "0303 health sciences", "Extracellular enzyme", "Agricultural and Veterinary Sciences", "Fungi", "Agronomy & Agriculture", "Soil respiration", "Biological Sciences", "15. Life on land", "Fire", "Soil carbon", "Climate Action", "03 medical and health sciences", "13. Climate action", "Boreal forest", "Warming", "Succession", "Alaska", "Environmental Sciences"]}, "links": [{"href": "https://escholarship.org/content/qt2zk6k6ms/qt2zk6k6ms.pdf"}, {"href": "https://doi.org/10.1016/j.soilbio.2010.07.011"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20Biology%20and%20Biochemistry", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.soilbio.2010.07.011", "name": "item", "description": "10.1016/j.soilbio.2010.07.011", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.soilbio.2010.07.011"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2010-10-01T00:00:00Z"}}, {"id": "10.1016/j.soilbio.2012.02.021", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:17:37Z", "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": "10.1029/2017JD027827", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:15Z", "type": "Journal Article", "created": "2018-04-26", "title": "Fine Particle Emissions From Tropical Peat Fires Decrease Rapidly With Time Since Ignition", "description": "Abstract<p>Southeast Asia experiences frequent fires in fuel\uffe2\uff80\uff90rich tropical peatlands, leading to extreme episodes of regional haze with high concentrations of fine particulate matter (PM2.5) impacting human health. In a study published recently, the first field measurements of PM2.5 emission factors for tropical peat fires showed larger emissions than from other fuel types. Here we report even higher PM2.5 emission factors, measured at newly ignited peat fires in Malaysia, suggesting that current estimates of fine particulate emissions from peat fires may be underestimated by a factor of 3 or more. In addition, we use both field and laboratory measurements of burning peat to provide the first mechanistic explanation for the high variability in PM2.5 emission factors, demonstrating that buildup of a surface ash layer causes the emissions of PM2.5 to decrease as the peat fire progresses. This finding implies that peat fires are more hazardous (in terms of aerosol emissions) when first ignited than when still burning many days later. Varying emission factors for PM2.5 also have implications for our ability to correctly model the climate and air quality impacts downwind of the peat fires. For modelers able to implement a time\uffe2\uff80\uff90varying emission factor, we recommend an emission factor for PM2.5 from newly ignited tropical peat fires of 58\uffc2\uffa0g of PM2.5 per kilogram of dry fuel consumed (g/kg), reducing exponentially at a rate of 9%/day. If the age of the fire is unknown or only a single value may be used, we recommend an average value of 24\uffc2\uffa0g/kg.</p>", "keywords": ["5", "550", "TRACE GASES", "PM2", "PM2.5", "Social and Behavioral Sciences", "01 natural sciences", "TRANSFORM INFRARED-SPECTROSCOPY", "INDONESIA", "CARBON", "SDG 3 - Good Health and Well-being", "11. Sustainability", "Medicine and Health Sciences", "Meteorology & Atmospheric Sciences", "AUSTRALIAN VEGETATION FIRES", "Research Articles", "0105 earth and related environmental sciences", "Science & Technology", "GE", "emissions", "AIR-POLLUTION", "15. Life on land", "FOREST", "FIELD-MEASUREMENTS", "DERIVATION", "13. Climate action", "Physical Sciences", "PREMATURE MORTALITY", "peat", "FoR 0401 (Atmospheric Sciences)", "FoR 0502 (Environmental Science and Management)", "fire"]}, "links": [{"href": "https://researchonline.ljmu.ac.uk/id/eprint/9303/1/Fine%20Particle%20Emissions%20From%20Tropical%20Peat%20Fires%20Decrease%20Rapidly%20With%20Time%20Since%20Ignition..pdf"}, {"href": "https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2017JD027827"}, {"href": "https://doi.org/10.1029/2017JD027827"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Geophysical%20Research%3A%20Atmospheres", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1029/2017JD027827", "name": "item", "description": "10.1029/2017JD027827", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1029/2017JD027827"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-05-16T00:00:00Z"}}, {"id": "10.1029/2019gb006393", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:15Z", "type": "Journal Article", "created": "2020-02-07", "title": "Sources of Uncertainty in Regional and Global Terrestrial CO 2 Exchange Estimates", "description": "<p>The Global Carbon Budget 2018 (GCB2018) estimated by the atmospheric CO  growth rate, fossil fuel emissions, and modeled (bottom\uffe2\uff80\uff90up) land and ocean fluxes cannot be fully closed, leading to a \uffe2\uff80\uff9cbudget imbalance,\uffe2\uff80\uff9d highlighting uncertainties in GCB components. However, no systematic analysis has been performed on which regions or processes contribute to this term. To obtain deeper insight on the sources of uncertainty in global and regional carbon budgets, we analyzed differences in Net Biome Productivity (NBP) for all possible combinations of bottom\uffe2\uff80\uff90up and top\uffe2\uff80\uff90down data sets in GCB2018: (i) 16 dynamic global vegetation models (DGVMs), and (ii) 5 atmospheric inversions that match the atmospheric CO  growth rate. We find that the global mismatch between the two ensembles matches well the GCB2018 budget imbalance, with Brazil, Southeast Asia, and Oceania as the largest contributors. Differences between DGVMs dominate global mismatches, while at regional scale differences between inversions contribute the most to uncertainty. At both global and regional scales, disagreement on NBP interannual variability between the two approaches explains a large fraction of differences. We attribute this mismatch to distinct responses to El\uffc2\uffa0Ni\uffc3\uffb1o\uffe2\uff80\uff93Southern Oscillation variability between DGVMs and inversions and to uncertainties in land use change emissions, especially in South America and Southeast Asia. We identify key needs to reduce uncertainty in carbon budgets: reducing uncertainty in atmospheric inversions (e.g., through more observations in the tropics) and in land use change fluxes, including more land use processes and evaluating land use transitions (e.g., using high\uffe2\uff80\uff90resolution remote\uffe2\uff80\uff90sensing), and, finally, improving tropical hydroecological processes and fire representation within DGVMs.</p>", "keywords": ["[SDE] Environmental Sciences", "FLUXES", "550", "BURNED AREA PRODUCT", "atmospheric inversions", "01 natural sciences", "Environnement et pollution", "DATA ASSIMILATION", "Ph\u00e9nom\u00e8nes atmosph\u00e9riques", "PLANT FUNCTIONAL TYPES", "global carbon budget", "carbon cycle", "ATMOSPHERIC CO2", "0105 earth and related environmental sciences", "LAND-COVER CHANGE", "FOSSIL-FUEL", "VEGETATION MODEL ORCHIDEE", "15. Life on land", "ddc:910", "CARBON-DIOXIDE EMISSIONS", "13. Climate action", "[SDE]Environmental Sciences", "dynamic global vegetation models", "contr\u00f4le de la pollution", "Technologie de l'environnement", "INCORPORATING SPITFIRE"]}, "links": [{"href": "https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2019GB006393"}, {"href": "https://doi.org/10.1029/2019gb006393"}, {"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": "10.1029/2019gb006393", "name": "item", "description": "10.1029/2019gb006393", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1029/2019gb006393"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-02-01T00:00:00Z"}}, {"id": "10.1029/2022gb007489", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:18:16Z", "type": "Journal Article", "created": "2022-11-09", "title": "Mineral Soils Are an Important Intermediate Storage Pool of Black Carbon in Fennoscandian Boreal Forests", "description": "Abstract<p>Approximately 40% of earth's carbon (C) stored in land vegetation and soil is within the boreal region. This large C pool is subjected to substantial removals and transformations during periodic wildfire. Fire\uffe2\uff80\uff90altered C, commonly known as pyrogenic carbon (PyC), plays a significant role in forest ecosystem functioning and composes a considerable fraction of C transport to limnic and oceanic sediments. While PyC stores are beginning to be quantified globally, knowledge is lacking regarding the drivers of their production and transport across ecosystems. This study used the chemo\uffe2\uff80\uff90thermal oxidation at 375\uffc2\uffb0C (CTO\uffe2\uff80\uff90375) method to isolate a particularly refractory subset of PyC compounds, here called black carbon (BC), finding an average increase of 11.6\uffc2\uffa0g BC m\uffe2\uff88\uff922 at 1\uffc2\uffa0year postfire in 50 separate wildfires occurring in Sweden during 2018. These increases could not be linked to proposed drivers, however BC storage in 50 additional nearby unburnt soils related strongly to soil mass while its proportion of the larger C pool related negatively to soil C:N. Fire approximately doubled BC stocks in the mineral layer but had no significant effect on BC in the organic layer where it was likely produced. Suppressed decomposition rates and low heating during fire in mineral subsoil relative to upper layers suggests potential removals of the doubled mineral layer BC are more likely transported out of the soil system than degraded in situ. Therefore, mineral soils are suggested to be an important storage pool for BC that can buffer short\uffe2\uff80\uff90term (production in fire) and long\uffe2\uff80\uff90term (cross\uffe2\uff80\uff90ecosystem transport) BC cycling.</p", "keywords": ["Ekologi", "Ecology", "mineral soil", "Soil Science", "Geokemi", "15. Life on land", "black carbon", "Markvetenskap", "01 natural sciences", "pyrogenic carbon", "fire severity", "Geochemistry", "13. Climate action", "carbon cycle", "boreal wildfire", "Research Article", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1029/2022gb007489"}, {"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": "10.1029/2022gb007489", "name": "item", "description": "10.1029/2022gb007489", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1029/2022gb007489"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-11-01T00:00:00Z"}}, {"id": "10.1038/35040544", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:18Z", "type": "Journal Article", "created": "2002-07-26", "title": "Elevated Co2 Increases Productivity And Invasive Species Success In An Arid Ecosystem", "description": "Arid ecosystems, which occupy about 20% of the earth's terrestrial surface area, have been predicted to be one of the most responsive ecosystem types to elevated atmospheric CO2 and associated global climate change. Here we show, using free-air CO2 enrichment (FACE) technology in an intact Mojave Desert ecosystem, that new shoot production of a dominant perennial shrub is doubled by a 50% increase in atmospheric CO2 concentration in a high rainfall year. However, elevated CO2 does not enhance production in a drought year. We also found that above-ground production and seed rain of an invasive annual grass increases more at elevated CO2 than in several species of native annuals. Consequently, elevated CO2 might enhance the long-term success and dominance of exotic annual grasses in the region. This shift in species composition in favour of exotic annual grasses, driven by global change, has the potential to accelerate the fire cycle, reduce biodiversity and alter ecosystem function in the deserts of western North America.", "keywords": ["0106 biological sciences", "Fire cycle", "Environmental Indicators and Impact Assessment", "Invasive species", "Mojave desert", "Water availability", "Free-air CO2 enrichment (FACE)", "Plant Biology", "04 agricultural and veterinary sciences", "Carbon Dioxide", "Plants", "15. Life on land", "Poaceae", "01 natural sciences", "13. Climate action", "Climate change", "0401 agriculture", " forestry", " and fisheries", "Elevated CO2", "Grasses", "Desert Climate", "Rosales", "Ecosystem", "Nevada"]}, "links": [{"href": "https://doi.org/10.1038/35040544"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/35040544", "name": "item", "description": "10.1038/35040544", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/35040544"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2000-11-01T00:00:00Z"}}, {"id": "10.1038/nature24668", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:19Z", "type": "Journal Article", "created": "2017-12-08", "title": "Fire frequency drives decadal changes in soil carbon and nitrogen and ecosystem productivity", "description": "Fire frequency is changing globally and is projected to affect the global carbon cycle and climate. However, uncertainty about how ecosystems respond to decadal changes in fire frequency makes it difficult to predict the effects of altered fire regimes on the carbon cycle; for instance, we do not fully understand the long-term effects of fire on soil carbon and nutrient storage, or whether fire-driven nutrient losses limit plant productivity. Here we analyse data from 48 sites in savanna grasslands, broadleaf forests and needleleaf forests spanning up to 65 years, during which time the frequency of fires was altered at each site. We find that frequently burned plots experienced a decline in surface soil carbon and nitrogen that was non-saturating through time, having 36 per cent (\u00b113 per cent) less carbon and 38 per cent (\u00b116 per cent) less nitrogen after 64 years than plots that were protected from fire. Fire-driven carbon and nitrogen losses were substantial in savanna grasslands and broadleaf forests, but not in temperate and boreal needleleaf forests. We also observe comparable soil carbon and nitrogen losses in an independent field dataset and in dynamic model simulations of global vegetation. The model study predicts that the long-term losses of soil nitrogen that result from more frequent burning may in turn decrease the carbon that is sequestered by net primary productivity by about 20 per cent of the total carbon that is emitted from burning biomass over the same period. Furthermore, we estimate that the effects of changes in fire frequency on ecosystem carbon storage may be 30 per cent too low if they do not include multidecadal changes in soil carbon, especially in drier savanna grasslands. Future changes in fire frequency may shift ecosystem carbon storage by changing soil carbon pools and nitrogen limitations on plant growth, altering the carbon sink capacity of frequently burning savanna grasslands and broadleaf forests.", "keywords": ["2. Zero hunger", "Carbon Sequestration", "Time Factors", "Nitrogen", "carbon", "Geographic Mapping", "Phosphorus", "15. Life on land", "Grassland", "01 natural sciences", "nitrogen", "Carbon", "Wildfires", "Soil", "Spatio-Temporal Analysis", "13. Climate action", "XXXXXX - Unknown", "Potassium", "carbon cycle (biogeochemistry)", "Calcium", "ecosystems", "soils", "fire", "Ecosystem", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1038/nature24668"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/nature24668", "name": "item", "description": "10.1038/nature24668", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/nature24668"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-12-11T00:00:00Z"}}, {"id": "10.1038/s41558-025-02356-4", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:18:24Z", "type": "Journal Article", "created": "2025-06-13", "title": "Future climate-driven fires may boost ocean productivity in the iron-limited North Atlantic", "description": "Rapid shifts in fire regimes affect the carbon cycle by releasing carbon and nutrients such as iron (Fe), potentially enhancing marine productivity and carbon export. Here we use fire emission projections and Earth system models to examine how climate-driven changes in fire emissions may alter soluble Fe (SFe) deposition and productivity. By century\u2019s end, climate change could increase Fe emissions from fires by 1.7\u20131.8 times beyond projections considering only direct human influences. Model projections show rising SFe deposition in Northern Hemisphere high latitudes under increasing socio-economic activity, potentially boosting the impact of SFe deposition on productivity in the Fe-limited North Atlantic by up to 20% annually (40% in summer), assuming stable macronutrient levels. However, declining macronutrient availability may shrink Fe-limited areas, where climate-driven fires could offset productivity losses by 7\u20138%. In the Southern Ocean, fossil fuel emissions primarily control SFe deposition, as reductions in anthropogenic fires counterbalance climate-driven increases.", "keywords": ["Fire emissions", "\u00c0rees tem\u00e0tiques de la UPC::Desenvolupament hum\u00e0 i sostenible::Degradaci\u00f3 ambiental::Canvi clim\u00e0tic", "Climate change", "Carbon cycle", "Iron (Fe)", "Article"]}, "links": [{"href": "https://doi.org/10.1038/s41558-025-02356-4"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature%20Climate%20Change", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s41558-025-02356-4", "name": "item", "description": "10.1038/s41558-025-02356-4", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41558-025-02356-4"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-06-13T00:00:00Z"}}, {"id": "10.1038/s41467-023-42597-5", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:18:23Z", "type": "Journal Article", "created": "2023-10-26", "title": "Wildfire precursors show complementary predictability in different timescales", "description": "Abstract<p>In most of the world, conditions conducive to wildfires are becoming more prevalent. Net carbon emissions from wildfires contribute to a positive climate feedback that needs to be monitored, quantified, and predicted. Here we use a causal inference approach to evaluate the influence of top-down weather and bottom-up fuel precursors on wildfires. The top-down dominance on wildfires is more widespread than bottom-up dominance, accounting for 73.3% and 26.7% of regions, respectively. The top-down precursors dominate in the tropical rainforests, mid-latitudes, and eastern Siberian boreal forests. The bottom-up precursors dominate in North American and European boreal forests, and African and Australian savannahs. Our study identifies areas where wildfires are governed by fuel conditions and hence where fuel management practices may be more effective. Moreover, our study also highlights that top-down and bottom-up precursors show complementary wildfire predictability across timescales. Seasonal or interannual predictions are feasible in regions where bottom-up precursors dominate.</p", "keywords": ["CLIMATE-CHANGE", "WEATHER", "13. Climate action", "FORESTS", "Earth and Environmental Sciences", "Science", "Q", "15. Life on land", "DRIVEN", "ENSO", "FIRE", "Article", "info:eu-repo/classification/ddc/500"]}, "links": [{"href": "https://www.nature.com/articles/s41467-023-42597-5.pdf"}, {"href": "https://doi.org/10.1038/s41467-023-42597-5"}, {"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/s41467-023-42597-5", "name": "item", "description": "10.1038/s41467-023-42597-5", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41467-023-42597-5"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-10-26T00:00:00Z"}}, {"id": "10.1038/s41559-024-02630-2", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:24Z", "type": "Journal Article", "created": "2025-03-24", "title": "Overwintering fires can occur in both peatlands and upland forests with varying ecological impacts", "description": "Climate warming is increasing the prevalence of overwintering 'zombie' fires, which are expected to occur primarily in peatlands, undermining carbon storage through deep burning of organic soils. We visited overwintering fires in Northwest Territories, Canada, and Interior Alaska, United States, and present field measurements of where overwintering fires are burning in the landscape and their impact on combustion severity and forest regeneration. Combustion severity hotspots did not generate overwintering, but peat and woody biomass smouldering both supported overwintering, leading to wintertime smouldering in both treed peatlands and upland forests. These findings create challenges for fire managers and uncertainty about carbon emissions, but forest regeneration was not compromised.", "keywords": ["Northwest Territories", "Soil", "Climate Change", "Seasons", "Forests", "Alaska", "Fires", "Wildfires"], "contacts": [{"organization": "Jennifer L. Baltzer, Xanthe J. Walker, Sander Veraverbeke, Thomas D. Hessilt, Raquel Alfaro-Sanchez, Max J. van Gerrevink, Michelle C. Mack, Emily L. Ogden, Richard Olsen, Rebecca C. Scholten, Merritt R. Turetsky,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1038/s41559-024-02630-2"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature%20Ecology%20%26amp%3B%20Evolution", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s41559-024-02630-2", "name": "item", "description": "10.1038/s41559-024-02630-2", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41559-024-02630-2"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-03-24T00:00:00Z"}}, {"id": "10.1038/s41561-024-01505-2", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:25Z", "type": "Journal Article", "created": "2024-09-02", "title": "Spatial variability in Arctic\u2013boreal fire regimes influenced by environmental and human factors", "description": "Abstract<p>Wildfire activity in Arctic and boreal regions is rapidly increasing, with severe consequences for climate and human health. Regional long-term variations in fire frequency and intensity characterize fire regimes. The spatial variability in Arctic\uffe2\uff80\uff93boreal fire regimes and their environmental and anthropogenic drivers, however, remain poorly understood. Here we present a fire tracking system to map the sub-daily evolution of all circumpolar Arctic\uffe2\uff80\uff93boreal fires between 2012 and 2023 using 375\uffe2\uff80\uff89m Visible Infrared Imaging Radiometer Suite active fire detections and the resulting dataset of the ignition time, location, size, duration, spread and intensity of individual fires. We use this dataset to classify the Arctic\uffe2\uff80\uff93boreal biomes into seven distinct \uffe2\uff80\uff98pyroregions\uffe2\uff80\uff99 with unique climatic and geographic environments. We find that these pyroregions exhibit varying responses to environmental drivers, with boreal North America, eastern Siberia and northern tundra regions showing the highest sensitivity to climate and lightning density. In addition, anthropogenic factors play an important role in influencing fire number and size, interacting with other factors. Understanding the spatial variability of fire regimes and its interconnected drivers in the Arctic\uffe2\uff80\uff93boreal domain is important for improving future predictions of fire activity and identifying areas at risk for extreme events.</p", "keywords": ["Environmental impact", "Fire ecology", "Natural hazards", "Boreal ecology", "Biogeochemistry", "Article"]}, "links": [{"href": "https://www.nature.com/articles/s41561-024-01505-2.pdf"}, {"href": "https://escholarship.org/content/qt7370v7qr/qt7370v7qr.pdf"}, {"href": "https://doi.org/10.1038/s41561-024-01505-2"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature%20Geoscience", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s41561-024-01505-2", "name": "item", "description": "10.1038/s41561-024-01505-2", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41561-024-01505-2"}, {"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": "10.1038/srep03829", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:28Z", "type": "Journal Article", "created": "2014-01-23", "title": "Rapid Recovery Of Soil Bacterial Communities After Wildfire In A Chinese Boreal Forest", "description": "Abstract<p>Fires affect hundreds of millions of hectares annually. Above-ground community composition and diversity after fire have been studied extensively, but effects of fire on soil bacterial communities remain largely unexamined despite the central role of bacteria in ecosystem recovery and functioning. We investigated responses of bacterial community to forest fire in the Greater Khingan Mountains, China, using tagged pyrosequencing. Fire altered soil bacterial community composition substantially and high-intensity fire significantly decreased bacterial diversity 1-year-after-burn site. Bacterial community composition and diversity returned to similar levels as observed in controls (no fire) after 11 years. The understory vegetation community typically takes 20\uffe2\uff80\uff93100 years to reach pre-fire states in boreal forest, so our results suggest that soil bacteria could recover much faster than plant communities. Finally, soil bacterial community composition significantly co-varied with soil pH, moisture content, NH4+ content and carbon/nitrogen ratio (P &lt; 0.05 in all cases) in wildfire-perturbed soils, suggesting that fire could indirectly affect bacterial communities by altering soil edaphic properties.</p>", "keywords": ["DNA", " Bacterial", "China", "Bacteria", "Nitrogen", "Biodiversity", "04 agricultural and veterinary sciences", "15. Life on land", "Article", "Carbon", "Fires", "13. Climate action", "RNA", " Ribosomal", " 16S", "0401 agriculture", " forestry", " and fisheries", "Biomass", "Soil Microbiology"]}, "links": [{"href": "https://doi.org/10.1038/srep03829"}, {"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/srep03829", "name": "item", "description": "10.1038/srep03829", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/srep03829"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2014-01-23T00:00:00Z"}}, {"id": "10.1046/j.1365-2389.2000.00310.x", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:18:32Z", "type": "Journal Article", "created": "2003-03-11", "title": "Changes In Organic Matter, Nitrogen, Phosphorus And Cations In Soil As A Result Of Fire And Water Erosion In A Mediterranean Landscape", "description": "Summary<p>Fire affects large parts of the dry Mediterranean shrubland, resulting in erosion and losses of plant nutrients. We have attempted to measure these effects experimentally on a calcareous hillside representative of such shrubland. Experimental fires were made on plots (4\uffe2\uff80\uff83m \uffc3\uff97 20\uffe2\uff80\uff83m) in which the fuel was controlled to obtain two different fire intensities giving means of soil surface temperature of 439\uffc2\uffb0C and 232\uffc2\uffb0C with temperatures exceeding 100\uffc2\uffb0C lasting for 36\uffe2\uff80\uff83min and 17\uffe2\uff80\uff83min. The immediate and subsequent changes induced by fire on the soil's organic matter content and other soil chemical properties were evaluated, together with the impact of water erosion.</p><p>Seven erosive rain events, which occurred after the experimental fires (from August 1995 to December 1996), were selected, and on them runoff and sediment produced from each plot were measured. The sediments collected were weighed and analysed. Taking into account the variations induced by fire on the soil properties and their losses by water erosion, estimates of the net inputs and outputs of the soil system were made. Results show that the greatest losses of both soil and nutrients took place in the 4\uffe2\uff80\uff83months immediately after the fire. Plots affected by the most intense fire showed greater losses of soil (4077\uffe2\uff80\uff83kg\uffe2\uff80\uff83ha\uffe2\uff88\uff921) than those with moderate fire intensity (3280\uffe2\uff80\uff83kg\uffe2\uff80\uff83ha\uffe2\uff88\uff921). The unburned plots produced the least sediment (72.8\uffe2\uff80\uff83kg\uffe2\uff80\uff83ha\uffe2\uff88\uff921). Organic matter and nutrient losses by water erosion were related to the degree of fire intensity. However, the largest losses of N\uffe2\uff80\uff90NH4+ and N\uffe2\uff80\uff90NO3\uffe2\uff80\uff93 by water erosion corresponded to the moderate fire (8.1 and 7.5\uffe2\uff80\uff83mg\uffe2\uff80\uff83N\uffe2\uff80\uff83m\uffe2\uff88\uff922, respectively).</p>", "keywords": ["13. Climate action", "Parameters", "Infiltration", "0401 agriculture", " forestry", " and fisheries", "Vegetation fires", "04 agricultural and veterinary sciences", "15. Life on land"]}, "links": [{"href": "https://doi.org/10.1046/j.1365-2389.2000.00310.x"}, {"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": "10.1046/j.1365-2389.2000.00310.x", "name": "item", "description": "10.1046/j.1365-2389.2000.00310.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1046/j.1365-2389.2000.00310.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2000-06-01T00:00:00Z"}}, {"id": "10.1071/WF16198", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:38Z", "type": "Journal Article", "created": "2017-10-31", "title": "Downward spread of smouldering peat fire: the role of moisture, density and oxygen supply", "description": "<p>Smouldering fires in peatland are different from the flames in wildland fires. Smouldering peat fire is slow, low-temperature and more persistent, releasing large amounts of smoke into the atmosphere. In this work, we experimentally and computationally investigate the vertical downward spread of smouldering fire in a column of 30cm-tall moss peat under variable moisture content (MC) and bulk density. The measured downward spread rate decreases with depth and wet bulk density, and is ~1cmh\uffe2\uff88\uff921 equivalent to a carbon emission flux of 200 tonnesday\uffe2\uff88\uff921ha\uffe2\uff88\uff921. We observe that downward spread increases as MC increases substantially at least inside the range from 10 to 70%, which is not intuitive and goes against the trend observed for the horizontal spread in the same peat. We also conduct one-dimensional computational simulations to successfully reproduce the experimental observations. The analysis shows that the spread rate increases with MC and decreases with density because smouldering spread is controlled by the oxygen supply. The volume of the porous peat expands when absorbing water, which reduces the density of organic matter and decreases the heat release rate. This shows that the widely assumed conclusion that the spread rate of wildfire decreases with MC is not universal when applied to smouldering fires.</p>", "keywords": ["WILDFIRES", "Science & Technology", "0602 Ecology", "fire spread rate", "Forestry", "BURN", "in-depth spread", "624", "15. Life on land", "01 natural sciences", "7. Clean energy", "BIOMASS", "modelling", "COMBUSTION", "IGNITION", "13. Climate action", "DEPTH", "carbon emission", "0705 Forestry Sciences", "peatland", "ORGANIC SOILS", "0502 Environmental Science And Management", "Life Sciences & Biomedicine", "KINETICS", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://www.publish.csiro.au/WF/pdf/WF16198"}, {"href": "https://doi.org/10.1071/WF16198"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/International%20Journal%20of%20Wildland%20Fire", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1071/WF16198", "name": "item", "description": "10.1071/WF16198", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1071/WF16198"}, {"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": "10.1071/mu13028", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:40Z", "type": "Journal Article", "created": "2015-02-02", "title": "Avian Responses To Varying Intensity Of Cattle Production In Spartina Densiflora Saltmarshes Of South-Eastern South America", "description": "Saltmarshes of Spartina densiflora in south-eastern South America have been modified by anthropogenic activities, mainly production of livestock. We examined the effect of the intensity of cattle production on the structure of saltmarsh vegetation and the effect of these changes to vegetation on the richness, composition and size of the avian populations and the abundance of nests. The levels of cattle production were based on the combined intensity of prescribed burning and cattle grazing, classed as: (1) High grazing \u2013 High burning (HH), (2) Low grazing \u2013 Low burning (LL) and (3) No grazing \u2013 No burning (NN). Cattle production altered the vegetation structure of saltmarshes and indirectly modified the richness, composition and size of their avian populations and the abundance of nests. Saltmarshes with either LL or NN production levels were inhabited by tall grassland specialists and generalists and by species specialised to live in a mosaic of short and tall grassland patches. Conversely, saltmarshes with HH production levels were inhabited by short-grassland specialists. That avian species diversity does not differ between S. densiflora saltmarsh subject to low or no human impacts has several potential interpretations, which are discussed. These findings have implications for management of grasslands to maintain avian diversity.", "keywords": ["0106 biological sciences", "2. Zero hunger", "Grassland Birds", "https://purl.org/becyt/ford/1.6", "Argentina", "Cattle Grazing", "Conservation", "Pampas", "15. Life on land", "Fire", "https://purl.org/becyt/ford/1", "01 natural sciences"], "contacts": [{"organization": "Cardoni, Daniel Augusto, Isacch, Juan Pablo, Iribarne, Oscar Osvaldo,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1071/mu13028"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Emu%20-%20Austral%20Ornithology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1071/mu13028", "name": "item", "description": "10.1071/mu13028", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1071/mu13028"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2015-03-01T00:00:00Z"}}, {"id": "10.1071/wf10120", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:44Z", "type": "Journal Article", "created": "2011-10-16", "title": "Soil N2o Emissions In A Mediterranean Shrubland Disturbed By Experimental Fires", "description": "<p>In the present work, post-burning soil N2O fluxes and related microbial processes were investigated in a Mediterranean shrubland subjected to experimental fires. Nine plots were selected, of which three were used as controls, three were burned with low-intensity fire and three with higher intensity fire. N2O fluxes, soil humidity and temperature were measured starting 2 days before burning and for 1 year after fire. Potential net nitrification, denitrification enzyme activity, mineral N and organic C were measured from soil samples collected periodically after burning. Cumulative data indicate a doubling of N2O production in burned plots over 1 year. Burned plots showed an increase of frequency of hot spots of N2O production. A slight detrimental effect of fire on the analysed biological activities was detected only immediately after burning. After 3 months, both potential net nitrification and denitrification enzyme activity had mostly recovered and potential net nitrification further increased over control levels in the following months. Fire seemed to induce a change in the main source of N2O, which in control plots was represented by heterotrophic activity (50\uffe2\uff80\uff9375%), whereas in burned plots it was mostly of autotrophic origin, most probably due to the significant increase of soil NH4+ after burning.</p>", "keywords": ["2. Zero hunger", "Nitrous oxide", "denitrification; fire intensity; nitrification; soil nitrogen;", "13. Climate action", "Nitrous oxide; soil; fire", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land", "fire", "soil"]}, "links": [{"href": "https://doi.org/10.1071/wf10120"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/International%20Journal%20of%20Wildland%20Fire", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1071/wf10120", "name": "item", "description": "10.1071/wf10120", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1071/wf10120"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2011-01-01T00:00:00Z"}}, {"id": "10.1071/wf17084", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:44Z", "type": "Journal Article", "created": "2018-05-21", "title": "Review of emissions from smouldering peat fires and their contribution to regional haze episodes", "description": "<p>  Smouldering peat fires, the largest fires on Earth in terms of fuel consumption, are reported in six continents and are responsible for regional haze episodes. Haze is the large-scale accumulation of smoke at low altitudes in the atmosphere. It decreases air quality, disrupts transportation and causes health emergencies. Research on peat emissions and haze is modest at best and many key aspects remain poorly understood. Here, we compile an up-to-date inter-study of peat fire emission factors (EFs) found in the literature both from laboratory and from field studies. Tropical peat fires yield larger EFs for the prominent organic compounds than boreal and temperate peat fires, possibly due to the higher fuel carbon content (56.0 vs 44.2%). In contrast, tropical peat fires present slightly lower EFs for particulate matter with diameter \uffe2\uff89\uffa42.5\uffe2\uff80\uff89\uffce\uffbcm (PM2.5) for unknown reasons but are probably related to combustion dynamics. An analysis of the modified combustion efficiency, a parameter widely used for determining the combustion regime of wildfires, shows it is partially misunderstood and highly sensitive to unknown field variables. This is the first review of the literature on smouldering peat emissions. Our integration of the existing literature allows the identification of existing gaps in knowledge and is expected to accelerate progress towards mitigation strategies. </p>", "keywords": ["emission factor", "550", "TRACE GASES", "CENTRAL KALIMANTAN", "01 natural sciences", "7. Clean energy", "TRANSFORM INFRARED-SPECTROSCOPY", "2015 EL-NINO", "CROP RESIDUE", "COMBUSTION", "11. Sustainability", "CHEMICAL-CHARACTERIZATION", "0105 earth and related environmental sciences", "Science & Technology", "0602 Ecology", "Forestry", "AIR-POLLUTION", "15. Life on land", "FIELD-MEASUREMENTS", "modified combustion efficiency", "FOREST-FIRES", "smoke", "13. Climate action", "FLIGHT MASS-SPECTROMETRY", "0705 Forestry Sciences", "wildfires", "0502 Environmental Science And Management", "Life Sciences & Biomedicine", "BIOMASS-BURNING EMISSIONS", "BROWN CARBON"]}, "links": [{"href": "https://www.publish.csiro.au/WF/pdf/WF17084"}, {"href": "https://doi.org/10.1071/wf17084"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/International%20Journal%20of%20Wildland%20Fire", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1071/wf17084", "name": "item", "description": "10.1071/wf17084", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1071/wf17084"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-01-01T00:00:00Z"}}, {"id": "10.1071/wf20117", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:44Z", "type": "Journal Article", "created": "2021-03-08", "title": "Laboratory study on the suppression of smouldering peat wildfires: effects of flow rate and wetting agent", "description": "<p>The application of water, or water mixed with suppressants, to combat wildfires is one of the most common firefighting methods but is rarely studied for smouldering peat wildfire, which is the largest type of fire worldwide in term of fuel consumption. We performed experiments by spraying suppressant to the top of a burning peat sample inside a reactor. A plant-based wetting agent suppressant was mixed with water at three concentrations: 0% (pure water), 1% (low concentration), and 5% (high concentration), and delivered with varying flowrates. The results showed that suppression time decreased non-linearly with flow rate. The average suppression time for the low-concentration solution was 39% lower than with just water, while the high-concentration solution reduced suppression time by 26%. The volume of fluid that contributes to the suppression of peat in our experiments is fairly constant at 5.7\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff892.1\uffe2\uff80\uff89L kg\uffe2\uff88\uff921 peat despite changes in flow rate and suppressant concentration. This constant volume suggests that suppression time is the duration needed to flood the peat layer and that the suppressant acts thermally and not chemically. The results provide a better understanding of the suppression mechanism of peat fires and can improve firefighting and mitigation strategies.</p>", "keywords": ["wetting", "Science & Technology", "550", "experiment", "smouldering", "0602 Ecology", "firefighting", "Forestry", "02 engineering and technology", "suppression", "15. Life on land", "7. Clean energy", "01 natural sciences", "6. Clean water", "0201 civil engineering", "mitigation", "13. Climate action", "0705 Forestry Sciences", "peatland", "0502 Environmental Science and Management", "Life Sciences & Biomedicine", "fire", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1071/wf20117"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/International%20Journal%20of%20Wildland%20Fire", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1071/wf20117", "name": "item", "description": "10.1071/wf20117", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1071/wf20117"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-03-09T00:00:00Z"}}, {"id": "10.1111/gcb.70179", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:19:24Z", "type": "Journal Article", "created": "2025-04-07", "title": "Lightning Impacts on Global Forest and Carbon Dynamics: Current Understanding and Knowledge Gaps", "description": "Lightning is a fundamental Earth system process that influences the world's major forest biomes and their carbon storage through two primary pathways. Lightning is the major cause of boreal forest fires, while lightning strikes kill patches of trees in tropical forests. We summarized the current understanding of these processes and identified knowledge gaps.", "keywords": ["carbon", "tropical", "Forests", "Lightning", "Carbon", "Carbon Cycle", "Trees", "forest", "Perspective", "boreal", "tree mortality", "Life Science", "lightning", "fire"], "contacts": [{"organization": "Sander Veraverbeke, Thomas A. J. Janssen, Esther Brambleby, Matt Jones, Bianca Zoletto, Masha T. van der Sande,", "roles": ["creator"]}]}, "links": [{"href": "https://ueaeprints.uea.ac.uk/id/eprint/99058/1/Veraverbeke_etal_2025_GlobalChangeBiology.pdf"}, {"href": "https://doi.org/10.1111/gcb.70179"}, {"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.70179", "name": "item", "description": "10.1111/gcb.70179", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcb.70179"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-04-01T00:00:00Z"}}, {"id": "10.1111/gcb.70247", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:19:24Z", "type": "Journal Article", "created": "2025-05-23", "title": "Carbon Emissions From Fires in Eastern Siberian Larch Forests", "description": "ABSTRACT<p>Siberian boreal forests have experienced increases in fire extent and intensity in recent years, which may threaten their role as carbon (C) sinks. Larch forests (Larix spp.) cover approximately 2.6 million km2 across Siberia, yet little is known about the magnitude and drivers of carbon combustion in these ecosystems. To address the paucity of field\uffe2\uff80\uff90based estimates of fuel load and consumption in Siberian larch forests, we sampled 41 burned plots, one to two years after fire, in Cajander larch (Larix cajanderi) forests in the Republic of Sakha (Yakutia), Russia. We estimated pre\uffe2\uff80\uff90fire carbon stocks and combustion with the objective of identifying the main drivers of carbon emissions. Pre\uffe2\uff80\uff90fire aboveground (trees and woody debris) and belowground carbon stocks at our study plots were 3.12\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff891.26\uffe2\uff80\uff89kg C m\uffe2\uff88\uff922 (mean\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff89standard deviation) and 3.50\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff890.93\uffe2\uff80\uff89kg C m\uffe2\uff88\uff922. We found that combustion averaged 3.20\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff890.75\uffe2\uff80\uff89kg C m\uffe2\uff88\uff922, of which 78% (2.49\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff890.56\uffe2\uff80\uff89kg C m\uffe2\uff88\uff922) stemmed from organic soil layers. These results suggest that severe fires in Cajander larch forests can result in combustion rates comparable to those observed in North American boreal forests and exceeding those previously reported for other forest types and burning conditions in Siberia. Carbon combustion was driven by both fire weather conditions and landscape variables, with pre\uffe2\uff80\uff90fire organic soil depth being the strongest predictor across our plots. Our study highlights the need to better account for Siberian larch forest fires and their impact on the carbon balance, especially given the expected climate\uffe2\uff80\uff90induced increase in fire extent and severity in this region.</p", "keywords": ["Larix cajanderi", "[SDU.OCEAN] Sciences of the Universe [physics]/Ocean", " Atmosphere", "eastern Siberia", "boreal forest carbon combustion climate change eastern Siberia fire severity larch forests Larix cajanderi", "Larix", "Forests", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "larch forests", "Fires", "Carbon", "Wildfires", "Siberia", "climate change", "fire severity", "carbon combustion", "boreal forest", "Research Article"], "contacts": [{"organization": "Delcourt, Clement, Rogers, Brendan, Akhmetzyanov, Linar, Izbicki, Brian, Scholten, Rebecca, Shestakova, Tatiana, van Wees, Dave, Mack, Michelle, Sass\u2010klaassen, Ute, Veraverbeke, Sander,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1111/gcb.70247"}, {"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.70247", "name": "item", "description": "10.1111/gcb.70247", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcb.70247"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-05-01T00:00:00Z"}}, {"id": "10.1098/rstb.2012.0102", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:19:07Z", "type": "Journal Article", "created": "2012-10-08", "title": "Impact Of Grazing Intensity On Seasonal Variations In Soil Organic Carbon And Soil Co2 Efflux In Two Semiarid Grasslands In Southern Botswana", "description": "<p>             Biological soil crusts (BSCs) are an important source of organic carbon, and affect a range of ecosystem functions in arid and semiarid environments. Yet the impact of grazing disturbance on crust properties and soil CO             2             efflux remain poorly studied, particularly in African ecosystems. The effects of burial under wind-blown sand, disaggregation and removal of BSCs on seasonal variations in soil CO             2             efflux, soil organic carbon, chlorophyll             a             and scytonemin were investigated at two sites in the Kalahari of southern Botswana. Field experiments were employed to isolate CO             2             efflux originating from BSCs in order to estimate the C exchange within the crust. Organic carbon was not evenly distributed through the soil profile but concentrated in the BSC. Soil CO             2             efflux was higher in Kalahari Sand than in calcrete soils, but rates varied significantly with seasonal changes in moisture and temperature. BSCs at both sites were a small net sink of C to the soil. Soil CO             2             efflux was significantly higher in sand soils where the BSC was removed, and on calcrete where the BSC was buried under sand. The BSC removal and burial under sand also significantly reduced chlorophyll             a             , organic carbon and scytonemin             .             Disaggregation of the soil crust, however, led to increases in chlorophyll             a             and organic carbon. The data confirm the importance of BSCs for C cycling in drylands and indicate intensive grazing, which destroys BSCs through trampling and burial, will adversely affect C sequestration and storage. Managed grazing, where soil surfaces are only lightly disturbed, would help maintain a positive carbon balance in African drylands.           </p>", "keywords": ["Chlorophyll", "2. Zero hunger", "Conservation of Natural Resources", "Botswana", "Indoles", "Chlorophyll A", "Temperature", "Water", "04 agricultural and veterinary sciences", "Carbon Dioxide", "15. Life on land", "Poaceae", "Carbon", "Fires", "Carbon Cycle", "Soil", "Phenols", "13. Climate action", "Animals", "0401 agriculture", " forestry", " and fisheries", "Herbivory", "Seasons", "Desert Climate", "Ecosystem", "Soil Microbiology"], "contacts": [{"organization": "Andrew D. Thomas", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1098/rstb.2012.0102"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Philosophical%20Transactions%20of%20the%20Royal%20Society%20B%3A%20Biological%20Sciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1098/rstb.2012.0102", "name": "item", "description": "10.1098/rstb.2012.0102", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1098/rstb.2012.0102"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2012-11-19T00:00:00Z"}}, {"id": "10.1098/rstb.2017.0302", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:19:07Z", "type": "Journal Article", "created": "2018-10-08", "title": "Tropical land carbon cycle responses to 2015/16 El Ni\u00f1o as recorded by atmospheric greenhouse gas and remote sensing data", "description": "<p>             The outstanding tropical land climate characteristic over the past decades is rapid warming, with no significant large-scale precipitation trends. This warming is expected to continue but the effects on tropical vegetation are unknown. El Ni\uffc3\uffb1o-related heat peaks may provide a test bed for a future hotter world. Here we analyse tropical land carbon cycle responses to the 2015/16 El Ni\uffc3\uffb1o heat and drought anomalies using an atmospheric transport inversion. Based on the global atmospheric CO             2             and fossil fuel emission records, we find no obvious signs of anomalously large carbon release compared with earlier El Ni\uffc3\uffb1o events, suggesting resilience of tropical vegetation. We find roughly equal net carbon release anomalies from Amazonia and tropical Africa, approximately 0.5 PgC each, and smaller carbon release anomalies from tropical East Asia and southern Africa. Atmospheric CO anomalies reveal substantial fire carbon release from tropical East Asia peaking in October 2015 while fires contribute only a minor amount to the Amazonian carbon flux anomaly. Anomalously large Amazonian carbon flux release is consistent with downregulation of primary productivity during peak negative near-surface water anomaly (October 2015 to March 2016) as diagnosed by solar-induced fluorescence. Finally, we find an unexpected anomalous positive flux to the atmosphere from tropical Africa early in 2016, coincident with substantial CO release.           </p>           <p>This article is part of a discussion meeting issue \uffe2\uff80\uff98The impact of the 2015/2016 El Ni\uffc3\uffb1o on the terrestrial tropical carbon cycle: patterns, mechanisms and implications\uffe2\uff80\uff99.</p>", "keywords": ["Life Sciences & Biomedicine - Other Topics", "FLUX", "0301 basic medicine", "Hot Temperature", "550", "551", "global warming", "01 natural sciences", "Carbon Cycle", "Greenhouse Gases", "03 medical and health sciences", "[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/Climatology", "CHEMICAL-TRANSPORT MODEL", "carbon cycle", "INVERSION", "Biology", "TEMPERATURE", "11 Medical and Health Sciences", "0105 earth and related environmental sciences", "tropical forests", "El Nino-Southern Oscillation", "Evolutionary Biology", "Tropical Climate", "Science & Technology", "Atmosphere", "PHOTOSYNTHESIS", "EQUATORIAL PACIFIC", "Articles", "06 Biological Sciences", "15. Life on land", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "6. Clean water", "Droughts", "[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology", "13. Climate action", "PRECIPITATION", "Remote Sensing Technology", "INDUCED CHLOROPHYLL FLUORESCENCE", "CO2", "[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces", "SENSITIVITY", "environment", "Life Sciences & Biomedicine", "fire"]}, "links": [{"href": "https://eprints.whiterose.ac.uk/135234/8/Tropical%20land%20carbon%20cycle%20responses%20to%202015/16%20El%20Ni%C3%B1o%20as%20recorded%20by%20atmospheric%20greenhouse%20gas%20and%20remote%20sensing%20data.pdf"}, {"href": "https://royalsocietypublishing.org/doi/pdf/10.1098/rstb.2017.0302"}, {"href": "https://doi.org/10.1098/rstb.2017.0302"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Philosophical%20Transactions%20of%20the%20Royal%20Society%20B%3A%20Biological%20Sciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1098/rstb.2017.0302", "name": "item", "description": "10.1098/rstb.2017.0302", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1098/rstb.2017.0302"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-10-08T00:00:00Z"}}, {"id": "10.1111/ejss.13290", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:19:18Z", "type": "Journal Article", "created": "2022-07-25", "title": "Post\u2010fire recovery of soil microbial functions is promoted by plant growth", "description": "Abstract<p>Forest fires can alter the biological properties of soils. There is increasing evidence that fires cause a shift in soil microbial communities, which play a central role in forest carbon and nutrient cycling. In this study, we evaluate the effect of soil heating on soil microbial functions. We hypothesised that fire reduces the catabolic functional diversity of soil, and that post\uffe2\uff80\uff90fire plant growth enhances its recovery. To test this, we experimentally heated a forest soil at 200\uffc2\uffb0C (T200) or 450\uffc2\uffb0C (T450). Heated and unheated soils were then incubated in tubs with or without live grass (Lolium perenne L.). We determined the functional profiles by measuring the substrate\uffe2\uff80\uff90induced respiration (SIR) using the Microresp\uffe2\uff84\uffa2 technique and analysed nutrient availability at the end of the incubation. At both temperatures, soil heating altered the respiration responses to substrate additions and the catabolic functional diversity of soils. Functional diversity was initially reduced in T200 soils but recovered at the end of the incubation. In contrast, T450 soils initially maintained the catabolic functional diversity, but decreased at the end of the incubation. Heating\uffe2\uff80\uff90induced nutrient availability stimulated the growth of grass, which in turn increased the response to several substrates and increased the functional diversity to values similar to the unheated controls. Our results suggest that fire\uffe2\uff80\uff90driven alteration of soil microbial communities has consequences at a functional level, and that the recovery of plant communities enhances the recovery of soil microbial functions.</p>Highlights<p> <p>Soil experimental heating altered microbial functions and reduced soil functional diversity.</p> <p>Soil heating also increased nutrient availability, enhancing plant growth.</p> <p>Growth of plants promoted the recovery of soil functional diversity.</p> <p>Post\uffe2\uff80\uff90fire recovery of functional diversity may be related to the recovery of photosynthetic tissues.</p> </p", "keywords": ["2. Zero hunger", "soil heating", "soil microbial functions", "Incendis forestals", "Forest fires", "Aboveground biomass", "04 agricultural and veterinary sciences", "15. Life on land", "Soil microbial functions", "catabolic functional diversity", "substrate-induced respiration", "S\u00f2ls", "13. Climate action", "forest fires", "Substrate-induced respiration", "Soils", "0401 agriculture", " forestry", " and fisheries", "Catabolic functional diversity", "Forest soils", "aboveground biomass", "Soil heating", "S\u00f2ls forestals"]}, "links": [{"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1111/ejss.13290"}, {"href": "https://doi.org/10.1111/ejss.13290"}, {"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.13290", "name": "item", "description": "10.1111/ejss.13290", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/ejss.13290"}, {"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": "10.1111/j.1365-2486.2007.01406.x", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:19:29Z", "type": "Journal Article", "created": "2007-08-28", "title": "The Legacy Of Harvest And Fire On Ecosystem Carbon Storage In A North Temperate Forest", "description": "Abstract<p>Forest harvesting and wildfire were widespread in the upper Great Lakes region of North America during the early 20th century. We examined how long this legacy of disturbance constrains forest carbon (C) storage rates by quantifying C pools and fluxes after harvest and fire in a mixed deciduous forest chronosequence in northern lower Michigan, USA. Study plots ranged in age from 6 to 68 years and were created following experimental clear\uffe2\uff80\uff90cut harvesting and fire disturbance. Annual C storage was estimated biometrically from measurements of wood, leaf, fine root, and woody debris mass, mass losses to herbivory, soil C content, and soil respiration. Maximum annual C storage in stands that were disturbed by harvest and fire twice was 26% less than a reference stand receiving the same disturbance only once. The mechanism for this reduction in annual C storage was a long\uffe2\uff80\uff90lasting decrease in site quality that endured over the 62\uffe2\uff80\uff90year timeframe examined. However, during regrowth the harvested and burned forest rapidly became a net C sink, storing 0.53\uffe2\uff80\uff83Mg\uffe2\uff80\uff83C\uffe2\uff80\uff83ha\uffe2\uff88\uff921\uffe2\uff80\uff83yr\uffe2\uff88\uff921after 6 years. Maximum net ecosystem production (1.35\uffe2\uff80\uff83Mg\uffe2\uff80\uff83C\uffe2\uff80\uff83ha\uffe2\uff88\uff921\uffe2\uff80\uff83yr\uffe2\uff88\uff921) and annual C increment (0.95\uffe2\uff80\uff83Mg\uffe2\uff80\uff83C\uffe2\uff80\uff83ha\uffe2\uff88\uff921\uffe2\uff80\uff83yr\uffe2\uff88\uff921) were recorded in the 24\uffe2\uff80\uff90 and 50\uffe2\uff80\uff90year\uffe2\uff80\uff90old stands, respectively. Net primary production averaged 5.19\uffe2\uff80\uff83Mg\uffe2\uff80\uff83C\uffe2\uff80\uff83ha\uffe2\uff88\uff921\uffe2\uff80\uff83yr\uffe2\uff88\uff921in experimental stands, increasing by &lt; 10% from 6 to 50 years. Soil heterotrophic respiration was more variable across stand ages, ranging from 3.85\uffe2\uff80\uff83Mg\uffe2\uff80\uff83C\uffe2\uff80\uff83ha\uffe2\uff88\uff921\uffe2\uff80\uff83yr\uffe2\uff88\uff921in the 6\uffe2\uff80\uff90year\uffe2\uff80\uff90old stand to 4.56\uffe2\uff80\uff83Mg\uffe2\uff80\uff83C\uffe2\uff80\uff83ha\uffe2\uff88\uff921\uffe2\uff80\uff83yr\uffe2\uff88\uff921in the 68\uffe2\uff80\uff90year\uffe2\uff80\uff90old stand. These results suggest that harvesting and fire disturbances broadly distributed across the region decades ago caused changes in site quality and successional status that continue to limit forest C storage rates.</p>", "keywords": ["disturbance", "570", "aspen", "net primary production", "net ecosystem production", "carbon storage", "15. Life on land", "01 natural sciences", "logging", "630", "succession", "northern hardwoods", "Biology", "fire", "legacy effects", "0105 earth and related environmental sciences"], "contacts": [{"organization": "Katherine H. Harrold, Christoph S. Vogel, Peter S. Curtis, Christopher M. Gough, Kristen George,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1111/j.1365-2486.2007.01406.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.1365-2486.2007.01406.x", "name": "item", "description": "10.1111/j.1365-2486.2007.01406.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/j.1365-2486.2007.01406.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2007-07-17T00:00:00Z"}}, {"id": "10.1371/journal.pone.0020105", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:20:07Z", "type": "Journal Article", "created": "2011-06-17", "title": "Global Change Could Amplify Fire Effects On Soil Greenhouse Gas Emissions", "description": "Open AccessBackground  Little is known about the combined impacts of global environmental changes and ecological disturbances on ecosystem functioning, even though such combined impacts might play critical roles in shaping ecosystem processes that can in turn feed back to climate change, such as soil emissions of greenhouse gases.    Methodology/Principal Findings  We took advantage of an accidental, low-severity wildfire that burned part of a long-term global change experiment to investigate the interactive effects of a fire disturbance and increases in CO2 concentration, precipitation and nitrogen supply on soil nitrous oxide (N2O) emissions in a grassland ecosystem. We examined the responses of soil N2O emissions, as well as the responses of the two main microbial processes contributing to soil N2O production \u2013 nitrification and denitrification \u2013 and of their main drivers. We show that the fire disturbance greatly increased soil N2O emissions over a three-year period, and that elevated CO2 and enhanced nitrogen supply amplified fire effects on soil N2O emissions: emissions increased by a factor of two with fire alone and by a factor of six under the combined influence of fire, elevated CO2 and nitrogen. We also provide evidence that this response was caused by increased microbial denitrification, resulting from increased soil moisture and soil carbon and nitrogen availability in the burned and fertilized plots.    Conclusions/Significance  Our results indicate that the combined effects of fire and global environmental changes can exceed their effects in isolation, thereby creating unexpected feedbacks to soil greenhouse gas emissions. These findings highlight the need to further explore the impacts of ecological disturbances on ecosystem functioning in the context of global change if we wish to be able to model future soil greenhouse gas emissions with greater confidence.", "keywords": ["Greenhouse Effect", "effet de serre", "sol", "Internationality", "Time Factors", "550", "Nitrogen", "QH301 Biology", "Science", "Nitrous Oxide", "incendie", "Fires", "12. Responsible consumption", "Soil", "dioxyde de carbone", "11. Sustainability", "Chemical Precipitation", "Soil Microbiology", "azote", "2. Zero hunger", "Q", "R", "04 agricultural and veterinary sciences", "Carbon Dioxide", "15. Life on land", "\u00e9mission", "[SDE.BE] Environmental Sciences/Biodiversity and Ecology", "pr\u00e9cipitation atmosph\u00e9rique", "13. Climate action", "Denitrification", "Medicine", "0401 agriculture", " forestry", " and fisheries", "[SDE.BE]Environmental Sciences/Biodiversity and Ecology", "GE Environmental Sciences", "Research Article"]}, "links": [{"href": "https://hal.science/halsde-00723483/file/2011_Niboyet_Plosone_1.pdf"}, {"href": "https://openknowledge.nau.edu/id/eprint/1706/7/Niboyet_A_etal_2011_Global_change_amplify_fire%281%29.pdf"}, {"href": "https://doi.org/10.1371/journal.pone.0020105"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/PLoS%20ONE", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1371/journal.pone.0020105", "name": "item", "description": "10.1371/journal.pone.0020105", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1371/journal.pone.0020105"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2011-06-08T00:00:00Z"}}, {"id": "10.1111/j.1365-2486.2012.02732.x", "type": "Feature", "geometry": null, "properties": {"license": "Closed Access", "updated": "2026-06-24T16:19:33Z", "type": "Journal Article", "created": "2012-05-11", "title": "Long-Term Nitrogen Additions Increase Likelihood Of Climate Stress And Affect Recovery From Wildfire In A Lowland Heath", "description": "Abstract<p>Increases in the emissions and associated atmospheric deposition of nitrogen (N) have the potential to cause significant changes to the structure and function of N\uffe2\uff80\uff90limited ecosystems. Here, we present the results of a long\uffe2\uff80\uff90term (13\uffc2\uffa0year) experiment assessing the impacts of N addition (30\uffc2\uffa0kg\uffc2\uffa0ha\uffe2\uff88\uff921\uffc2\uffa0yr\uffe2\uff88\uff921) on a UK lowland heathland under a wide range of environmental conditions, including the occurrence of prolonged natural drought episodes and a severe summer fire. Our findings indicate that elevated N deposition results in large, persistent effects on Calluna growth, phenology and chemistry, severe suppression of understorey lichen flora and changes in soil biogeochemistry. Growing season rainfall was found to be a strong driver of inter\uffe2\uff80\uff90annual variation in Calluna growth and, although interactions between N and rainfall for shoot growth were not significant until the later phase of the experiment, N addition exacerbated the extent of drought injury to Calluna shoots following naturally occurring droughts in 2003 and 2009. Following a severe wildfire at the experimental site in 2006, heathland regeneration dynamics were significantly affected by N, with a greater abundance of pioneering moss species and suppression of the lichen flora in plots receiving N additions. Significant interactions between climate and N were also apparent post fire, with the characteristic stimulation in Calluna growth in +N plots suppressed during dry years. Carbon (C) and N budgets demonstrate large increases in both above\uffe2\uff80\uff90 and below\uffe2\uff80\uff90ground stocks of these elements in N\uffe2\uff80\uff90treated plots prior to the fire, despite higher levels of soil microbial activity and organic matter turnover. Although much of the organic material was removed during the fire, pre\uffe2\uff80\uff90existing treatment differences were still evident following the burn. Post fire accumulation of below\uffe2\uff80\uff90ground C and N stocks was increased rapidly in N\uffe2\uff80\uff90treated plots, highlighting the role of N deposition in ecosystem C sequestration.</p>", "keywords": ["2. Zero hunger", "550", "droughts", "04 agricultural and veterinary sciences", "15. Life on land", "nitrogen", "bushfires", "6. Clean water", "climatic changes", "eutrophication", "13. Climate action", "wildfires", "0401 agriculture", " forestry", " and fisheries", "ecosystems"]}, "links": [{"href": "https://doi.org/10.1111/j.1365-2486.2012.02732.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.1365-2486.2012.02732.x", "name": "item", "description": "10.1111/j.1365-2486.2012.02732.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/j.1365-2486.2012.02732.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2012-06-27T00:00:00Z"}}, {"id": "10.1111/j.1757-1707.2012.01181.x", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:19:43Z", "type": "Journal Article", "created": "2012-05-24", "title": "Assessing The Potential Of Wildfires As A Sustainable Bioenergy Opportunity", "description": "Abstract<p>As the environmental and economic consequences of fossil\uffe2\uff80\uff90fuel use become clear, land is increasingly targeted as a source of bioenergy. We explore the potential for generating electricity from biomass vulnerable to fires as an ecologic and socioeconomic opportunity that can reduce the risk of greenhouse gas generation from wildfires and help to create incentives to preserve natural and seminatural vegetation and prevent its conversion to agriculture, including biofuel crops. On the basis of a global analysis of the energy generation and spatial distribution of fires, we show that between 2003 and 2010, global fires consumed ~8300\uffc2\uffa0\uffc2\uffb1\uffc2\uffa0592\uffc2\uffa0PJ\uffc2\uffa0yr\uffe2\uff88\uff921 of energy, equivalent to ~36\uffe2\uff80\uff9344% of the global electricity consumption in 2008 and &gt;100% national consumption in 57 countries. Forests/woodlands, cultivated areas, shrublands, and grasslands contributed 53%, 19%, 16%, and 3.5% of the global energy released by fires. Although many agroecological, socioeconomic, and engineering challenges need to be overcome before diverting the energy lost in fires into more useable forms, done cautiously it could reconcile habitat preservation with economic yields in natural systems.</p>", "keywords": ["2. Zero hunger", "Dry Forests", "15. Life on land", "Fire Radiative Energy", "7. Clean energy", "01 natural sciences", "12. Responsible consumption", "Bioelectricity", "https://purl.org/becyt/ford/2.7", "13. Climate action", "11. Sustainability", "Biomass Burning", "https://purl.org/becyt/ford/2", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1111/j.1757-1707.2012.01181.x"}, {"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/j.1757-1707.2012.01181.x", "name": "item", "description": "10.1111/j.1757-1707.2012.01181.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/j.1757-1707.2012.01181.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2012-05-24T00:00:00Z"}}, {"id": "10.1111/nph.12409", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:19:44Z", "type": "Journal Article", "created": "2013-07-22", "title": "Fire, Hurricane And Carbon Dioxide: Effects On Net Primary Production Of A Subtropical Woodland", "description": "Summary<p>   <p>Disturbance affects most terrestrial ecosystems and has the potential to shape their responses to chronic environmental change.</p>  <p>Scrub\uffe2\uff80\uff90oak vegetation regenerating from fire disturbance in subtropical Florida was exposed to experimentally elevated carbon dioxide (CO2) concentration (+350\uffc2\uffa0\uffce\uffbcl\uffc2\uffa0l\uffe2\uff88\uff921) using open\uffe2\uff80\uff90top chambers for 11\uffc2\uffa0yr, punctuated by hurricane disturbance in year 8. Here, we report the effects of elevated CO2 on aboveground and belowground net primary productivity (NPP) and nitrogen (N) cycling during this experiment.</p>  <p>The stimulation of NPP and N uptake by elevated CO2 peaked within 2\uffc2\uffa0yr after disturbance by fire and hurricane, when soil nutrient availability was high. The stimulation subsequently declined and disappeared, coincident with low soil nutrient availability and with a CO2\uffe2\uff80\uff90induced reduction in the N concentration of oak stems.</p>  <p>These findings show that strong growth responses to elevated CO2 can be transient, are consistent with a progressively limited response to elevated CO2 interrupted by disturbance, and illustrate the importance of biogeochemical responses to extreme events in modulating ecosystem responses to global environmental change.</p>  </p>", "keywords": ["0106 biological sciences", "NITROGEN-USE EFFICIENCY", "Scrub oak ecosystem", "01 natural sciences", "Trees", "Quercus", "Soil", "nitrogen cycling", "oak woodland", "ECOSYSTEMS", "Global environmental change", "Biomass", "ROOT BIOMASS", "disturbance", "Florida scrub", "elevated CO2", "Elevated atmospheric CO2", "Plant Stems", "Cyclonic Storms", "Aboveground biomass", "FOREST PRODUCTIVITY", "Hurricane", "04 agricultural and veterinary sciences", "Nitrogen Cycle", "Fire", "Soil carbon", "LONG-TERM EXPOSURE", "Net primary productivity", "Long term exposure", "Florida", "Elevated CO2", "fire", "FLORIDA SCRUB", "ABOVEGROUND BIOMASS", "Nitrogen cycling", "TERRESTRIAL", "Oak woodland", "ELEVATED ATMOSPHERIC CO2", "Elevated CO 2", "Nitrogen", "hurricane", "Forest productivity", "Fires", "Terrestrial ecosystems", "SCRUB-OAK ECOSYSTEM", "Net primary productivity (NPP)", "Ecosystem", "Nitrogen use efficiency", "Atmosphere", "net primary productivity (NPP)", "Root biomass", "Plant Sciences", "global environmental change", "Disturbance", "Carbon Dioxide", "15. Life on land", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "SOIL CARBON"]}, "links": [{"href": "https://digitalcommons.odu.edu/context/biology_fac_pubs/article/1266/viewcontent/Day2013FireHurricaneandCarbonDioxideOCR.pdf"}, {"href": "https://doi.org/10.1111/nph.12409"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/New%20Phytologist", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/nph.12409", "name": "item", "description": "10.1111/nph.12409", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/nph.12409"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2013-07-22T00:00:00Z"}}, {"id": "10.1126/science.1082709", "type": "Feature", "geometry": null, "properties": {"license": "unspecified", "updated": "2026-06-24T16:19:49Z", "type": "Journal Article", "created": "2003-05-08", "title": "Long-Term Effects Of Wildfire On Ecosystem Properties Across An Island Area Gradient", "description": "<p>Boreal forest soils play an important role in the global carbon cycle by functioning as a large terrestrial carbon sink or source, and the alteration of fire regime through global change phenomena may influence this role. We studied a system of forested lake islands in the boreal zone of Sweden for which fire frequency increases with increasing island size. Large islands supported higher plant productivity and litter decomposition rates than did smaller ones, and, with increasing time since fire, litter decomposition rates were suppressed sooner than was ecosystem productivity. This contributes to greater carbon storage with increasing time since fire; for every century without a major fire, an additional 0.5 kilograms per square meter of carbon becomes stored in the humus.</p>", "keywords": ["Sweden", "0106 biological sciences", "Geography", "Light", "Plant Development", "Carbon Dioxide", "15. Life on land", "01 natural sciences", "Carbon", "Fires", "Trees", "Soil", "13. Climate action", "Biomass", "Ecosystem", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1126/science.1082709"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1126/science.1082709", "name": "item", "description": "10.1126/science.1082709", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1126/science.1082709"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2003-05-09T00:00:00Z"}}, {"id": "10.1126/science.1128834", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:19:49Z", "type": "Journal Article", "created": "2006-07-07", "title": "Warming And Earlier Spring Increase Western Us Forest Wildfire Activity", "description": "<p>Western United States forest wildfire activity is widely thought to have increased in recent decades, yet neither the extent of recent changes nor the degree to which climate may be driving regional changes in wildfire has been systematically documented. Much of the public and scientific discussion of changes in western United States wildfire has focused instead on the effects of 19th- and 20th-century land-use history. We compiled a comprehensive database of large wildfires in western United States forests since 1970 and compared it with hydroclimatic and land-surface data. Here, we show that large wildfire activity increased suddenly and markedly in the mid-1980s, with higher large-wildfire frequency, longer wildfire durations, and longer wildfire seasons. The greatest increases occurred in mid-elevation, Northern Rockies forests, where land-use histories have relatively little effect on fire risks and are strongly associated with increased spring and summer temperatures and an earlier spring snowmelt.</p>", "keywords": ["13. Climate action", "Climate change", "Forest Biology", "Wildfire", "15. Life on land", "Forest Sciences", "01 natural sciences", "333", "United States", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1126/science.1128834"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1126/science.1128834", "name": "item", "description": "10.1126/science.1128834", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1126/science.1128834"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2006-08-18T00:00:00Z"}}, {"id": "10.1126/science.1132075", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:19:49Z", "type": "Journal Article", "created": "2006-11-16", "title": "The Impact Of Boreal Forest Fire On Climate Warming", "description": "<p>We report measurements and analysis of a boreal forest fire, integrating the effects of greenhouse gases, aerosols, black carbon deposition on snow and sea ice, and postfire changes in surface albedo. The net effect of all agents was to increase radiative forcing during the first year (34 \uffc3\uff82\uffc2\uffb1 31 Watts per square meter of burned area), but to decrease radiative forcing when averaged over an 80-year fire cycle (\uffc3\uffa2&#128;&#147;2.3 \uffc3\uff82\uffc2\uffb1 2.2 Watts per square meter) because multidecadal increases in surface albedo had a larger impact than fire-emitted greenhouse gases. This result implies that future increases in boreal fire may not accelerate climate warming.</p>", "keywords": ["Greenhouse Effect", "330", "13. Climate action", "15. Life on land", "01 natural sciences", "Ecosystem", "Fires", "Trees", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://authors.library.caltech.edu/51883/7/Randerson.SOM.pdf"}, {"href": "https://escholarship.org/content/qt2t07n8d3/qt2t07n8d3.pdf"}, {"href": "https://escholarship.org/content/qt54g6g1ns/qt54g6g1ns.pdf"}, {"href": "https://doi.org/10.1126/science.1132075"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1126/science.1132075", "name": "item", "description": "10.1126/science.1132075", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1126/science.1132075"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2006-11-17T00:00:00Z"}}, {"id": "10.1126/science.aal4108", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:19:49Z", "type": "Journal Article", "created": "2017-07-12", "title": "A Human-Driven Decline In Global Burned Area", "description": "Burn less, baby, burn less           <p>             Humans have, and always have had, a major impact on wildfire activity, which is expected to increase in our warming world. Andela             et al.             use satellite data to show that, unexpectedly, global burned area declined by \uffe2\uff88\uffbc25% over the past 18 years, despite the influence of climate. The decrease has been largest in savannas and grasslands because of agricultural expansion and intensification. The decline of burned area has consequences for predictions of future changes to the atmosphere, vegetation, and the terrestrial carbon sink.           </p>           <p>             Science             , this issue p.             1356           </p>", "keywords": ["[SDE] Environmental Sciences", "Satellite Imagery", "Carbon Sequestration", "Conservation of Natural Resources", "550", "General Science & Technology", "Climate", "Veterinary and Food Sciences", "Fires", "Theoretical", "Models", "11. Sustainability", "Human Activities", "SDG 2 - Zero Hunger", "Ecosystem", "Agricultural", "info:eu-repo/classification/ddc/550", "ddc:550", "Forestry Sciences", "Agriculture", "Models", " Theoretical", "15. Life on land", "Earth sciences", "13. Climate action", "Ecological Applications", "[SDE]Environmental Sciences", "Environmental Sciences"]}, "links": [{"href": "https://escholarship.org/content/qt6v95t473/qt6v95t473.pdf"}, {"href": "https://escholarship.org/content/qt6b42q71s/qt6b42q71s.pdf"}, {"href": "https://doi.org/10.1126/science.aal4108"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1126/science.aal4108", "name": "item", "description": "10.1126/science.aal4108", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1126/science.aal4108"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-06-30T00:00:00Z"}}, {"id": "10.1128/aem.01355-07", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:19:50Z", "type": "Journal Article", "created": "2007-11-17", "title": "Effects Of Wildfire And Harvest Disturbances On Forest Soil Bacterial Communities", "description": "ABSTRACT           <p>             Wildfires and harvesting are important disturbances to forest ecosystems, but their effects on soil microbial communities are not well characterized and have not previously been compared directly. This study was conducted at sites with similar soil, climatic, and other properties in a spruce-dominated boreal forest near Chisholm, Alberta, Canada. Soil microbial communities were assessed following four treatments: control, harvest, burn, and burn plus timber salvage (burn-salvage). Burn treatments were at sites affected by a large wildfire in May 2001, and the communities were sampled 1 year after the fire. Microbial biomass carbon decreased 18%, 74%, and 53% in the harvest, burn, and burn-salvage treatments, respectively. Microbial biomass nitrogen decreased 25% in the harvest treatment, but increased in the burn treatments, probably because of microbial assimilation of the increased amounts of available NH             4             +             and NO             3             \uffe2\uff88\uff92             due to burning. Bacterial community composition was analyzed by nonparametric ordination of molecular fingerprint data of 119 samples from both ribosomal intergenic spacer analysis (RISA) and rRNA gene denaturing gradient gel electrophoresis. On the basis of multiresponse permutation procedures, community composition was significantly different among all treatments, with the greatest differences between the two burned treatments versus the two unburned treatments. The sequencing of DNA bands from RISA fingerprints revealed distinct distributions of bacterial divisions among the treatments.             Gamma             - and             Alphaproteobacteria             were highly characteristic of the unburned treatments, while             Betaproteobacteria             and members of             Bacillus             were highly characteristic of the burned treatments. Wildfire had distinct and more pronounced effects on the soil microbial community than did harvesting.           </p>", "keywords": ["DNA", " Bacterial", "Electrophoresis", "0301 basic medicine", "0303 health sciences", "Bacteria", "Molecular Sequence Data", "Biodiversity", "Sequence Analysis", " DNA", "15. Life on land", "Nucleic Acid Denaturation", "DNA", " Ribosomal", "Fires", "6. Clean water", "Alberta", "Trees", "03 medical and health sciences", "13. Climate action", "DNA", " Ribosomal Spacer", "Biomass", "Soil Microbiology"], "contacts": [{"organization": "B.E. Kishchuk, William W. Mohn, Nancy R. Smith,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1128/aem.01355-07"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Applied%20and%20Environmental%20Microbiology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1128/aem.01355-07", "name": "item", "description": "10.1128/aem.01355-07", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1128/aem.01355-07"}, {"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": "10.1128/aem.71.5.2713-2722.2005", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:19:50Z", "type": "Journal Article", "created": "2005-05-03", "title": "Changes In Nitrogen-Fixing And Ammonia-Oxidizing Bacterial Communities In Soil Of A Mixed Conifer Forest After Wildfire", "description": "ABSTRACT           <p>             This study was undertaken to examine the effects of forest fire on two important groups of N-cycling bacteria in soil, the nitrogen-fixing and ammonia-oxidizing bacteria. Sequence and terminal restriction fragment length polymorphism (T-RFLP) analysis of             nifH             and             amoA             PCR amplicons was performed on DNA samples from unburned, moderately burned, and severely burned soils of a mixed conifer forest. PCR results indicated that the soil biomass and proportion of nitrogen-fixing and ammonia-oxidizing species was less in soil from the fire-impacted sites than from the unburned sites. The number of dominant             nifH             sequence types was greater in fire-impacted soils, and             nifH             sequences that were most closely related to those from the spore-forming taxa             Clostridium             and             Paenibacillus             were more abundant in the burned soils. In T-RFLP patterns of the ammonia-oxidizing community, terminal restriction fragments (TRFs) representing             amoA             cluster 1, 2, or 4             Nitrosospira             spp. were dominant (80 to 90%) in unburned soils, while TRFs representing             amoA             cluster 3A             Nitrosospira             spp. dominated (65 to 95%) in fire-impacted soils. The dominance of             amoA             cluster 3A             Nitrosospira             spp. sequence types was positively correlated with soil pH (5.6 to 7.5) and NH             3             -N levels (0.002 to 0.976 ppm), both of which were higher in burned soils. The decreased microbial biomass and shift in nitrogen-fixing and ammonia-oxidizing communities were still evident in fire-impacted soils collected 14 months after the fire.           </p>", "keywords": ["2. Zero hunger", "0301 basic medicine", "0303 health sciences", "Bacteria", "Base Sequence", "Molecular Sequence Data", "15. Life on land", "Polymerase Chain Reaction", "Fires", "Trees", "Soil", "03 medical and health sciences", "Ammonia", "Nitrogen Fixation", "Oxidoreductases", "Oxidation-Reduction", "Polymorphism", " Restriction Fragment Length", "Soil Microbiology"], "contacts": [{"organization": "Chris M. Yeager, Diana E. Northup, Susan M. Barns, Cheryl R. Kuske, Christy C. Grow,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1128/aem.71.5.2713-2722.2005"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Applied%20and%20Environmental%20Microbiology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1128/aem.71.5.2713-2722.2005", "name": "item", "description": "10.1128/aem.71.5.2713-2722.2005", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1128/aem.71.5.2713-2722.2005"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2005-05-01T00:00:00Z"}}, {"id": "10.5194/essd-16-3601-2024", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:22:28Z", "type": "Journal Article", "created": "2024-08-13", "title": "State of Wildfires 2023\u20132024", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Abstract. Climate\u00a0change contributes to the increased frequency and intensity of wildfires globally, with significant impacts on society and the environment. However, our understanding of the global distribution of extreme fires remains skewed, primarily influenced by media coverage and regionalised research efforts. This inaugural State of Wildfires report systematically analyses fire activity worldwide, identifying extreme events from the March 2023\u2013February 2024 fire season. We assess the causes, predictability, and attribution of these events to climate change and land use and forecast future risks under different climate scenarios. During the 2023\u20132024 fire season, 3.9\u00d7106\u2009km2 burned globally, slightly below the average of previous seasons, but fire carbon (C) emissions were 16\u2009% above average, totalling 2.4\u2009Pg\u2009C. Global fire C emissions were increased by record emissions in Canadian boreal forests (over 9 times the average) and reduced by low emissions from African savannahs. Notable events included record-breaking fire extent and emissions in Canada, the largest recorded wildfire in the European Union (Greece), drought-driven fires in western Amazonia and northern parts of South America, and deadly fires in Hawaii (100 deaths) and Chile (131 deaths). Over 232\u2009000 people were evacuated in Canada alone, highlighting the severity of human impact. Our analyses revealed that multiple drivers were needed to cause areas of extreme fire activity. In Canada and Greece, a combination of high fire weather and an abundance of dry fuels increased the probability of fires, whereas burned area anomalies were weaker in regions with lower fuel loads and higher direct suppression, particularly in Canada. Fire weather prediction in Canada showed a mild anomalous signal 1 to 2 months in advance, whereas events in Greece and Amazonia had shorter predictability horizons. Attribution analyses indicated that modelled anomalies in burned area were up to 40\u2009%, 18\u2009%, and 50\u2009% higher due to climate change in Canada, Greece, and western Amazonia during the 2023\u20132024 fire season, respectively. Meanwhile, the probability of extreme fire seasons of these magnitudes has increased significantly due to anthropogenic climate change, with a 2.9\u20133.6-fold increase in likelihood of high fire weather in Canada and a 20.0\u201328.5-fold increase in Amazonia. By the end of the century, events of similar magnitude to 2023 in Canada are projected to occur 6.3\u201310.8 times more frequently under a medium\u2013high emission scenario (SSP370). This report represents our first annual effort to catalogue extreme wildfire events, explain their occurrence, and predict future risks. By consolidating state-of-the-art wildfire science and delivering key insights relevant to policymakers, disaster management services, firefighting agencies, and land managers, we aim to enhance society's resilience to wildfires and promote advances in preparedness, mitigation, and adaptation. New datasets presented in this work are available from https://doi.org/10.5281/zenodo.11400539 (Jones et al., 2024) and https://doi.org/10.5281/zenodo.11420742 (Kelley et al., 2024a).                     </p></article>", "keywords": ["QE1-996.5", "info:eu-repo/classification/ddc/550", "550", "Geology", "15. Life on land", "7. Clean energy", "wildfire", "[SDU] Sciences of the Universe [physics]", "Environmental sciences", "climate change", "[SDU]Sciences of the Universe [physics]", "13. Climate action", "11. Sustainability", "Life Science", "GE1-350"]}, "links": [{"href": "https://ueaeprints.uea.ac.uk/id/eprint/96389/1/essd_16_3601_2024.pdf"}, {"href": "https://essd.copernicus.org/articles/16/3601/2024/essd-16-3601-2024.pdf"}, {"href": "https://doi.org/10.5194/essd-16-3601-2024"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Earth%20System%20Science%20Data", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.5194/essd-16-3601-2024", "name": "item", "description": "10.5194/essd-16-3601-2024", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5194/essd-16-3601-2024"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-08-14T00:00:00Z"}}, {"id": "10.1371/journal.pone.0001299", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:20:07Z", "type": "Journal Article", "created": "2007-12-11", "title": "Increased Litterfall In Tropical Forests Boosts The Transfer Of Soil Co2 To The Atmosphere", "description": "Open AccessLa production de liti\u00e8re a\u00e9rienne dans les for\u00eats est susceptible d'augmenter en raison des concentrations \u00e9lev\u00e9es de dioxyde de carbone atmosph\u00e9rique (CO(2)), de la hausse des temp\u00e9ratures et du changement des r\u00e9gimes de pr\u00e9cipitations. Comme les chutes de liti\u00e8re repr\u00e9sentent un flux majeur de carbone de la v\u00e9g\u00e9tation vers le sol, les changements dans les apports de liti\u00e8re sont susceptibles d'avoir des cons\u00e9quences de grande port\u00e9e sur la dynamique du carbone du sol. De telles perturbations du bilan carbone peuvent \u00eatre particuli\u00e8rement importantes sous les tropiques, car les for\u00eats tropicales stockent pr\u00e8s de 30\u00a0% du carbone mondial du sol, ce qui en fait une composante essentielle du cycle mondial du carbone\u00a0; n\u00e9anmoins, les effets de l'augmentation de la production de liti\u00e8re a\u00e9rienne sur la dynamique du carbone souterrain sont mal compris. Nous avons utilis\u00e9 des traitements mensuels \u00e0 long terme et \u00e0 grande \u00e9chelle d'enl\u00e8vement et d'ajout de liti\u00e8re dans une for\u00eat tropicale de plaine pour \u00e9valuer les cons\u00e9quences de l'augmentation des chutes de liti\u00e8re sur la production souterraine de CO(2). Au cours de la deuxi\u00e8me \u00e0 la cinqui\u00e8me ann\u00e9e de traitement, l'ajout de liti\u00e8re a augment\u00e9 la respiration du sol plus que l'enl\u00e8vement de la liti\u00e8re ne l'a diminu\u00e9\u00a0; la respiration du sol \u00e9tait en moyenne 20\u00a0% plus faible dans l'enl\u00e8vement de la liti\u00e8re et 43\u00a0% plus \u00e9lev\u00e9e dans le traitement d'ajout de liti\u00e8re par rapport aux t\u00e9moins, mais l'ajout de liti\u00e8re n'a pas modifi\u00e9 la biomasse microbienne. Nous avons pr\u00e9dit une augmentation de 9% de la respiration du sol dans les parcelles d'ajout de liti\u00e8re, bas\u00e9e sur la diminution de 20% des parcelles d'enl\u00e8vement de la liti\u00e8re et une r\u00e9duction de 11% due \u00e0 une biomasse racinaire fine plus faible dans les parcelles d'ajout de liti\u00e8re. L'augmentation mesur\u00e9e de 43\u00a0% de la respiration du sol \u00e9tait donc 34\u00a0% plus \u00e9lev\u00e9e que pr\u00e9vu et il est possible que ce CO \u00ab\u00a0suppl\u00e9mentaire\u00a0\u00bb (2) soit le r\u00e9sultat d'effets d'amor\u00e7age, c'est-\u00e0-dire la stimulation de la d\u00e9composition de la mati\u00e8re organique du sol plus ancienne par l'ajout de mati\u00e8re organique fra\u00eeche. Nos r\u00e9sultats montrent que l'augmentation de la production de liti\u00e8re a\u00e9rienne en raison du changement global a le potentiel de provoquer des pertes consid\u00e9rables de carbone du sol dans l'atmosph\u00e8re dans les for\u00eats tropicales.", "keywords": ["570", "Atmospheric sciences", "Science", "Atmosphere (unit)", "Soil Science", "Carbon Loss", "630", "Environmental science", "Plant litter", "Trees", "Agricultural and Biological Sciences", "Impact of Climate Change on Forest Wildfires", "Soil", "Meteorology", "Litter", "Biomass", "Biology", "Ecosystem", "2. Zero hunger", "Tropical Climate", "Global and Planetary Change", "Ecology", "Geography", "Atmosphere", "Global Forest Drought Response and Climate Change", "Q", "R", "Temperature", "Tropics", "Water", "Life Sciences", "Geology", "FOS: Earth and related environmental sciences", "04 agricultural and veterinary sciences", "Carbon Dioxide", "15. Life on land", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "Physical Sciences", "Medicine", "0401 agriculture", " forestry", " and fisheries", "Seasons", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems", "Research Article"]}, "links": [{"href": "http://oro.open.ac.uk/36464/1/Sayer%20et%20al%202007.pdf"}, {"href": "https://eprints.lancs.ac.uk/id/eprint/69199/1/journal.pone.0001299.pdf"}, {"href": "https://doi.org/10.1371/journal.pone.0001299"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/PLoS%20ONE", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1371/journal.pone.0001299", "name": "item", "description": "10.1371/journal.pone.0001299", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1371/journal.pone.0001299"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2007-12-12T00:00:00Z"}}, {"id": "10.1371/journal.pone.0150256", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:20:10Z", "type": "Journal Article", "created": "2016-02-26", "title": "Management Impacts On Carbon Dynamics In A Sierra Nevada Mixed Conifer Forest", "description": "Forest ecosystems can act as sinks of carbon and thus mitigate anthropogenic carbon emissions. When forests are actively managed, treatments can alter forests carbon dynamics, reducing their sink strength and switching them from sinks to sources of carbon. These effects are generally characterized by fast temporal dynamics. Hence this study monitored for over a decade the impacts of management practices commonly used to reduce fire hazards on the carbon dynamics of mixed-conifer forests in the Sierra Nevada, California, USA. Soil CO2 efflux, carbon pools (i.e. soil carbon, litter, fine roots, tree biomass), and radial tree growth were compared among un-manipulated controls, prescribed fire, thinning, thinning followed by fire, and two clear-cut harvested sites. Soil CO2 efflux was reduced by both fire and harvesting (ca. 15%). Soil carbon content (upper 15 cm) was not significantly changed by harvest or fire treatments. Fine root biomass was reduced by clear-cut harvest (60-70%) but not by fire, and the litter layer was reduced 80% by clear-cut harvest and 40% by fire. Thinning effects on tree growth and biomass were concentrated in the first year after treatments, whereas fire effects persisted over the seven-year post-treatment period. Over this period, tree radial growth was increased (25%) by thinning and reduced (12%) by fire. After seven years, tree biomass returned to pre-treatment levels in both fire and thinning treatments; however, biomass and productivity decreased 30%-40% compared to controls when thinning was combined with fire. The clear-cut treatment had the strongest impact, reducing ecosystem carbon stocks and delaying the capacity for carbon uptake. We conclude that post-treatment carbon dynamics and ecosystem recovery time varied with intensity and type of treatments. Consequently, management practices can be selected to minimize ecosystem carbon losses while increasing future carbon uptake, resilience to high severity fire, and climate related stresses.", "keywords": ["0106 biological sciences", "570", "550", "Life on Land", "General Science & Technology", "Science", "Veterinary and Food Sciences", "Forests", "01 natural sciences", "California", "Fires", "Carbon Cycle", "Soil", "Biomass", "Ecosystem", "0105 earth and related environmental sciences", "Agricultural", "Forestry Sciences", "Q", "R", "Forestry", "Biological Sciences", "Carbon Dioxide", "15. Life on land", "Climate Action", "Tracheophyta", "13. Climate action", "Ecological Applications", "Medicine", "Environmental Sciences", "Research Article"]}, "links": [{"href": "https://escholarship.org/content/qt1xc0j927/qt1xc0j927.pdf"}, {"href": "https://doi.org/10.1371/journal.pone.0150256"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/PLOS%20ONE", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1371/journal.pone.0150256", "name": "item", "description": "10.1371/journal.pone.0150256", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1371/journal.pone.0150256"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2016-02-26T00:00:00Z"}}, {"id": "10.1594/pangaea.967653", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:20:27Z", "type": "Dataset", "title": "Arctic-boreal fire atlas: 12-hourly perimeters of individual fires in the Arctic-boreal domain from 2012 to 2023", "description": "Open AccessData is provided per calendar year. Each year's directory contains a subdirectory 'Snapshot' with 12-hourly fire perimeters (all active fire perimeters of a time step) and active fire lines (files ending on *_FL.gpkg), and a subdirectory 'NFP' with text files containing the original active fire location information associated with each fire at each time step. The two additional folders 'final_perims' and 'ignitions' contain annual summary vector files of all ignitions and final perimeters. The attributes of all types of outputs (snapshots, new fire pixel files, final perimeters and ignitions) are described in detail in the provided pdf.", "keywords": ["History", "Arctic Report Card 2024", "fire behaviour", "Binary Object", "Binary Object (File Size)", "fire ignitions", "Humanities", "DATE/TIME", "Arctic", "fire history", "Fire mapping", "File content", "DATE TIME", "boreal forest", "fire regimes", "Tundra", "Binary Object File Size", "fire"], "contacts": [{"organization": "Scholten, Rebecca, Chen, Yang, Veraverbeke, Sander, Randerson, James,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1594/pangaea.967653"}, {"rel": "self", "type": "application/geo+json", "title": "10.1594/pangaea.967653", "name": "item", "description": "10.1594/pangaea.967653", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1594/pangaea.967653"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-01-01T00:00:00Z"}}, {"id": "10.1594/pangaea.939352", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:20:27Z", "type": "Dataset", "title": "Global fraction of lightning fires and burned area from lightning", "description": "This dataset contains the global fraction of lightning fires and burned area from lightning, and associated uncertainties, at 0.5 degree resolution. The dataset is representative for contemporary fire regimes (between 2001 and 2020). The dataset is based on a statistical model with three geospatial predictor variables: the seasonal correlation between lightning and burned area, the seasonal correlation between fire weather and burned area, and the fraction of low impact land. These variables are derivatives from remote sensing products. The statistical model was calibrated and validated with fire cause reference data from seven different parts of the world: USA including Alaska, Canada, Portugal, southern France, Yakutia (Russia), Victoria (Australia) and Tasmania (Australia). The statistical model explained 53 % of the variability in the reference data for the fraction of lightning fires, and 39 % for the burned area from lightning. All other relevant datasets from the study, processed to 0.5 degree resolution, are also provided. These include burned land, seasonal correlation between lightning and burned area, seasonal correlation between fire weather and burned area, low impact land, fire cause reference data, intact forests, fire-related forest loss, carbon combustion and future lightning projections.", "keywords": ["13. Climate action", "Earth System Research", "15. Life on land", "global", "lightning", "burned area", "fire"], "contacts": [{"organization": "Janssen, Thomas, Jones, Matthew W, Finney, Declan, van der Werf, Guido R, van Wees, Dave, Xu, Wenxuan, Veraverbeke, Sander,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1594/pangaea.939352"}, {"rel": "self", "type": "application/geo+json", "title": "10.1594/pangaea.939352", "name": "item", "description": "10.1594/pangaea.939352", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1594/pangaea.939352"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-01-01T00:00:00Z"}}, {"id": "10.3389/fmicb.2022.824813", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:21:26Z", "type": "Journal Article", "created": "2022-04-28", "title": "Microbial Community-Level Physiological Profiles and Genetic Prokaryotic Structure of Burned Soils Under Mediterranean Sclerophyll Forests in Central Chile", "description": "<p>Forest fires alter soil microbial communities that are essential to support ecosystem recovery following land burning. These alterations have different responses according to soil abiotic pre- and post-fire conditions and fire severity, among others, and tend to decrease along vegetation recovery over time. Thus, understanding the effects of fires on microbial soil communities is critical to evaluate ecosystem resilience and restoration strategies in fire-prone ecosystems. We studied the state of community-level physiological profiles (CLPPs) and the prokaryotic community structure of rhizosphere and bulk soils from two fire-affected sclerophyll forests (one surveyed 17 months and the other 33 months after fire occurrence) in the Mediterranean climate zone of central Chile. Increases in catabolic activity (by average well color development of CLPPs), especially in the rhizosphere as compared with the bulk soil, were observed in the most recently affected site only. Legacy of land burning was still clearly shaping soil prokaryote community structure, as shown by quantitative PCR (qPCR) and Illumina MiSeq sequencing of the V4 region of the 16S rRNA gene, particularly in the most recent fire-affected site. The qPCR copy numbers and alpha diversity indexes (Shannon and Pielou\uffe2\uff80\uff99s evenness) of sequencing data decreased in burned soils at both locations. Beta diversity analyses showed dissimilarity of prokaryote communities at both study sites according to fire occurrence, and NO3\uffe2\uff80\uff93 was the common variable explaining community changes for both of them. Acidobacteria and Rokubacteria phyla significantly decreased in burned soils at both locations, while Firmicutes and Actinobacteria increased. These findings provide a better understanding of the resilience of soil prokaryote communities and their physiological conditions in Mediterranean forests of central Chile following different time periods after fire, conditions that likely influence the ecological processes taking place during recovery of fire-affected ecosystems.</p", "keywords": ["Biolog EcoPlates", "13. Climate action", "rhizosphere; bacteria; Biolog EcoPlates; ecosystem recovery; wildfires", "wildfires", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "ecosystem recovery", "15. Life on land", "rhizosphere", "bacteria", "Microbiology", "QR1-502"]}, "links": [{"href": "https://doi.org/10.3389/fmicb.2022.824813"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Frontiers%20in%20Microbiology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3389/fmicb.2022.824813", "name": "item", "description": "10.3389/fmicb.2022.824813", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3389/fmicb.2022.824813"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-04-28T00:00:00Z"}}, {"id": "10.17221/9/2008-swr", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:20:31Z", "type": "Journal Article", "created": "2018-02-11", "title": "The Impact Of Windthrow And Fire Disturbances On Selected Soil Properties In The Tatra National Park", "description": ": In November 2004, forest stands in the Tatra National Park (TANAP) were affected by windthrow and in July 2005, the wildfire broke out on a part of the affected area. The objective of this study is to evaluate the impact of the windthrow and fire disturbances on soil microbial activity. Basal and potential soil respiration, N-mineralisation, catalase activity, soil microbial biomass, and cellulase activity were measured in soil samples taken from the A-horizon (depth of 0-10 cm) along 100 m transects established on 4 plots (reference site, burnt, non-extracted, and extracted sites) in October 2006. Some soil microbial characteristics exhibited a high spatial variability, especially microbial biomass and N-mineralisation. Significant differences in soil microbial characteristics (especially basal soil respiration and catalase activity) between plots were found. Generally, the highest microbial activity was revealed on the plot affected by fire. Soil microbial activity was similar on the extracted and non-extracted sites.", "keywords": ["0106 biological sciences", "windthrow", "S", "0401 agriculture", " forestry", " and fisheries", "Agriculture", "04 agricultural and veterinary sciences", "forest soil", "microbial activity", "01 natural sciences", "wildfire", "spruce stands"]}, "links": [{"href": "https://doi.org/10.17221/9/2008-swr"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20and%20Water%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.17221/9/2008-swr", "name": "item", "description": "10.17221/9/2008-swr", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.17221/9/2008-swr"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2008-12-31T00:00:00Z"}}, {"id": "10.18710/FJWV6X", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:20:34Z", "type": "Dataset", "title": "Replication Data for: Spatial variation in amount of carbon in boreal forest surface soil \u2013 the role of historical fires, hydro-topography, and contemporary vegetation", "description": "This dataset contains data on soil C and N stocks (from soil samples), charcoal weight, historical fire frequencies, year of last fire, bottom layer vegetation cover, topography, and woody cover from Trillemarka Nature reserve.", "keywords": ["Earth and Environmental Science", "History", "Humanities", "Hydro-topography", "Hydro topography", "13. Climate action", "Earth and Environmental Sciences", "Organic surface carbon stocks", "15. Life on land", "Forest fire history", "Environmental Research", "Natural Sciences", "Geosciences"], "contacts": [{"organization": "Haukenes, Vilde L., \u00c5sg\u00e5rd, Lisa, Asplund, Johan, Nybakken, Line, Rolstad, J\u00f8rund, Storaunet, Ken Olaf, Ohlson, Mikael,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.18710/FJWV6X"}, {"rel": "self", "type": "application/geo+json", "title": "10.18710/FJWV6X", "name": "item", "description": "10.18710/FJWV6X", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.18710/FJWV6X"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-01-01T00:00:00Z"}}, {"id": "10.18739/a2cv4bt4j", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:20:34Z", "type": "Dataset", "title": "Arctic-boreal fire atlas: 12-hourly perimeters of individual fires in the Arctic-boreal domain from 2012 to 2023", "description": "Open AccessData is provided per calendar year. Each year's directory contains a subdirectory 'Snapshot' with 12-hourly fire perimeters (all active fire perimeters of a time step) and active fire lines (files ending on *_FL.gpkg), and a subdirectory 'NFP' with text files containing the original active fire location information associated with each fire at each time step. The two additional folders 'final_perims' and 'ignitions' contain annual summary vector files of all ignitions and final perimeters. The attributes of all types of outputs (snapshots, new fire pixel files, final perimeters and ignitions) are described in detail in the provided pdf.", "keywords": ["History", "Arctic Report Card 2024", "fire behaviour", "Binary Object", "Binary Object (File Size)", "fire ignitions", "Humanities", "DATE/TIME", "Arctic", "fire history", "Fire mapping", "File content", "DATE TIME", "boreal forest", "fire regimes", "Tundra", "Binary Object File Size", "fire"], "contacts": [{"organization": "Scholten, Rebecca, Chen, Yang, Veraverbeke, Sander, Randerson, James,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.18739/a2cv4bt4j"}, {"rel": "self", "type": "application/geo+json", "title": "10.18739/a2cv4bt4j", "name": "item", "description": "10.18739/a2cv4bt4j", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.18739/a2cv4bt4j"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-01-01T00:00:00Z"}}, {"id": "10.1890/03-5133", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:20:35Z", "type": "Journal Article", "created": "2007-06-06", "title": "Relationships Among Fires, Fungi, And Soil Dynamics In Alaskan Boreal Forests", "description": "Fires are critical pathways of carbon loss from boreal forest soils, whereas microbial communities form equally critical controls over carbon accumulation between fires. We used a chronosequence in Alaska to test Read's hypothesis that arbuscular my- corrhizal fungi should dominate ecosystems with low accumulation of surface litter, and ectomycorrhizal fungi should proliferate where organic horizons are well-developed. This pattern is expected because ectomycorrhizal fungi display a greater capacity to mineralize organic compounds than do arbuscular mycorrhizal fungi. The sites were located in upland forests near Delta Junction, Alaska, and represent stages at 3, 15, 45, and 80 years following fire. Soil organic matter accumulated 2.8-fold over time. Fire did not noticeably reduce the abundance of arbuscular mycorrhizal fungi. In contrast, ectomycorrhizal colonization re- quired up to 15 years to return to pre-fire levels. As a result, dominant mycorrhizal groups shifted from arbuscular to ectomycorrhizal fungi as succession progressed. Bacterial func- tional diversity was greatest in the oldest sites. Altogether, microbes that can mineralize organic compounds (i.e., ectomycorrhizae and bacteria) recovered more slowly than those that cannot (i.e., arbuscular mycorrhizae). Potential net N mineralization and standing pools of ammonium-N were relatively low in the youngest site. In addition, glomalin stocks were positively correlated with arbuscular mycorrhizal hyphal length, peaking early in the chron- osequence. Our results indicate that microbial succession may influence soil carbon and nitrogen dynamics in the first several years following fire, by augmenting carbon storage in glomalin while inhibiting mineralization of organic compounds.", "keywords": ["external hyphae", "soil carbon and nitrogen", "biolog", "04 agricultural and veterinary sciences", "15. Life on land", "chronosequence", "fire and soil microbes", "succession", "Alaskan boreal forest", "mycorrhizal fungi", "organic material", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "mineralization", "microbial community", "glomalin"]}, "links": [{"href": "https://escholarship.org/content/qt3wc775gm/qt3wc775gm.pdf"}, {"href": "https://doi.org/10.1890/03-5133"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Ecological%20Applications", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1890/03-5133", "name": "item", "description": "10.1890/03-5133", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1890/03-5133"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2004-12-01T00:00:00Z"}}, {"id": "10.1890/06-1187.1", "type": "Feature", "geometry": null, "properties": {"license": "Closed Access", "updated": "2026-06-24T16:20:36Z", "type": "Journal Article", "created": "2007-07-19", "title": "Soil Responses To Management, Increased Precipitation, And Added Nitrogen In Ponderosa Pine Forests", "description": "Forest management, climatic change, and atmospheric N deposition can affect soil biogeochemistry, but their combined effects are not well understood. We examined the effects of water and N amendments and forest thinning and burning on soil N pools and fluxes in ponderosa pine forests near Flagstaff, Arizona (USA). Using a 15N-depleted fertilizer, we also documented the distribution of added N into soil N pools. Because thinning and burning can increase soil water content and N availability, we hypothesized that these changes would alleviate water and N limitation of soil processes, causing smaller responses to added N and water in the restored stand. We found little support for this hypothesis. Responses of fine root biomass, potential net N mineralization, and the soil microbial N to water and N amendments were mostly unaffected by stand management. Most of the soil processes we examined were limited by N and water, and the increased N and soil water availability caused by forest restoration was insufficient to alleviate these limitations. For example, N addition caused a larger increase in potential net nitrification in the restored stand, and at a given level of soil N availability, N addition had a larger effect on soil microbial N in the restored stand. Possibly, forest restoration increased the availability of some other limiting resource, amplifying responses to added N and water. Tracer N recoveries in roots and in the forest floor were lower in the restored stand. Natural abundance delta15N of labile soil N pools were higher in the restored stand, consistent with a more open N cycle. We conclude that thinning and burning open up the N cycle, at least in the short-term, and that these changes are amplified by enhanced precipitation and N additions. Our results suggest that thinning and burning in ponderosa pine forests will not increase their resistance to changes in soil N dynamics resulting from increased atmospheric N deposition or increased precipitation due to climatic change. Restoration plans should consider the potential impact on long-term forest productivity of greater N losses from a more open N cycle, especially during the period immediately after thinning and burning.", "keywords": ["Time Factors", "Nitrogen", "Climate", "Arizona", "Water", "04 agricultural and veterinary sciences", "15. Life on land", "Fires", "Pinus ponderosa", "Soil", "13. Climate action", "Chemical Precipitation", "0401 agriculture", " forestry", " and fisheries", "Ecosystem", "Nitrites"]}, "links": [{"href": "https://doi.org/10.1890/06-1187.1"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Ecological%20Applications", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1890/06-1187.1", "name": "item", "description": "10.1890/06-1187.1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1890/06-1187.1"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2007-07-01T00:00:00Z"}}, {"id": "10.1890/07-1767.1", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:20:36Z", "type": "Journal Article", "created": "2009-02-25", "title": "Impacts Of Fire And Fire Surrogate Treatments On Forest Soil Properties: A Meta-Analytical Approach", "description": "<p>The soils underlying the 12 Fire and Fire Surrogates Network include six soil orders and &gt;50 named soil series. Across the network, pretreatment soils varied from 3.7 to 7.1 in pH, and exhibited ranges of twofold in bulk density, fourfold in soil organic C (SOC) content, 10\uffe2\uff80\uff90fold in total inorganic N (TIN), and 200\uffe2\uff80\uff931000\uffe2\uff80\uff90fold in extractable Ca and K. Nonmetric multidimensional (NMS) ordination of pretreatment soil conditions arrayed the FFS sites along gradients of pH/base cation status, net N transformation rates, bulk density, and SOC. At the network scale, mineral soil exposure was significantly greater in fire\uffe2\uff80\uff90only (mean of 9.2%) and mechanical + fire (5.0%) treatments than in the controls (1.5%) during the first posttreatment year, and this persisted through the later sampling year (second through fourth year, depending on site) in the fire\uffe2\uff80\uff90only treatment (fire 4.1%, control 1.1%). Bulk density was not affected significantly at the network scale. TIN concentrations during the first posttreatment year increased after all three manipulative treatments, but this effect did not persist to the later sampling year. Neither SOC content nor soil C:N ratio was affected by any of the treatments at the network scale. At the individual site scale, the combined mechanical + fire treatment produced more significant site \uffc3\uff97 treatment \uffc3\uff97 year effects than did the fire\uffe2\uff80\uff90only or mechanical\uffe2\uff80\uff90only treatments, though in most cases even the statistically significant differences produced by the manipulative treatments were modest in magnitude. Ordination of first\uffe2\uff80\uff90year standardized effect sizes produced no discernable separation of the three manipulative treatments but did separate the three sites with the greatest fire severity (based on proportional fuel consumption) from the majority of the network sites, with changes in pH, TIN, SOC content, and soil C:N ratio correlating most strongly with this separation. Ordination of the effect sizes from the later sampling year produced somewhat clearer separation of treatments than did the first\uffe2\uff80\uff90year ordination, though fewer sites were represented in this second ordination. Overall, the network\uffe2\uff80\uff90wide effects of the FFS treatments on soil properties appear to have been modest and transient.</p>", "keywords": ["0106 biological sciences", "Conservation of Natural Resources", "Forestry", "04 agricultural and veterinary sciences", "Hydrogen-Ion Concentration", "15. Life on land", "01 natural sciences", "Carbon", "Fires", "6. Clean water", "Trees", "Soil", "0401 agriculture", " forestry", " and fisheries", "Seasons"], "contacts": [{"organization": "Jianjun Huang, Ralph E. J. Boerner, Stephen C. Hart,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1890/07-1767.1"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Ecological%20Applications", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1890/07-1767.1", "name": "item", "description": "10.1890/07-1767.1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1890/07-1767.1"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2009-03-01T00:00:00Z"}}, {"id": "10.1890/08-0501.1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:20:36Z", "type": "Journal Article", "created": "2009-03-18", "title": "Forest Fuel Reduction Alters Fire Severity And Long-Term Carbon Storage In Three Pacific Northwest Ecosystems", "description": "<p>Two forest management objectives being debated in the context of federally managed landscapes in the U.S. Pacific Northwest involve a perceived trade\uffe2\uff80\uff90off between fire restoration and carbon sequestration. The former strategy would reduce fuel (and therefore C) that has accumulated through a century of fire suppression and exclusion which has led to extreme fire risk in some areas. The latter strategy would manage forests for enhanced C sequestration as a method of reducing atmospheric CO2and associated threats from global climate change. We explored the trade\uffe2\uff80\uff90off between these two strategies by employing a forest ecosystem simulation model, STANDCARB, to examine the effects of fuel reduction on fire severity and the resulting long\uffe2\uff80\uff90term C dynamics among three Pacific Northwest ecosystems: the east Cascades ponderosa pine forests, the west Cascades western hemlock\uffe2\uff80\uff93Douglas\uffe2\uff80\uff90fir forests, and the Coast Range western hemlock\uffe2\uff80\uff93Sitka spruce forests. Our simulations indicate that fuel reduction treatments in these ecosystems consistently reduced fire severity. However, reducing the fraction by which C is lost in a wildfire requires the removal of a much greater amount of C, since most of the C stored in forest biomass (stem wood, branches, coarse woody debris) remains unconsumed even by high\uffe2\uff80\uff90severity wildfires. For this reason, all of the fuel reduction treatments simulated for the west Cascades and Coast Range ecosystems as well as most of the treatments simulated for the east Cascades resulted in a reduced mean stand C storage. One suggested method of compensating for such losses in C storage is to utilize C harvested in fuel reduction treatments as biofuels. Our analysis indicates that this will not be an effective strategy in the west Cascades and Coast Range over the next 100 years. We suggest that forest management plans aimed solely at ameliorating increases in atmospheric CO2should forgo fuel reduction treatments in these ecosystems, with the possible exception of some east Cascades ponderosa pine stands with uncharacteristic levels of understory fuel accumulation. Balancing a demand for maximal landscape C storage with the demand for reduced wildfire severity will likely require treatments to be applied strategically throughout the landscape rather than indiscriminately treating all stands.</p>", "keywords": ["Greenhouse Effect", "0106 biological sciences", "Bioelectric Energy Sources", "Forestry", "Carbon Dioxide", "15. Life on land", "16. Peace & justice", "Models", " Biological", "01 natural sciences", "7. Clean energy", "Carbon", "Fires", "Pseudotsuga", "Pinus ponderosa", "Oregon", "13. Climate action", "Computer Simulation", "Picea", "Ecosystem", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1890/08-0501.1"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Ecological%20Applications", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1890/08-0501.1", "name": "item", "description": "10.1890/08-0501.1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1890/08-0501.1"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2009-04-01T00:00:00Z"}}, {"id": "10.1890/09-0934.1", "type": "Feature", "geometry": null, "properties": {"license": "Closed Access", "updated": "2026-06-24T16:20:37Z", "type": "Journal Article", "created": "2010-04-09", "title": "Carbon And Water Fluxes From Ponderosa Pine Forests Disturbed By Wildfire And Thinning", "description": "<p>Disturbances alter ecosystem carbon dynamics, often by reducing carbon uptake and stocks. We compared the impact of two types of disturbances that represent the most likely future conditions of currently dense ponderosa pine forests of the southwestern United States: (1) high\uffe2\uff80\uff90intensity fire and (2) thinning, designed to reduce fire intensity. High\uffe2\uff80\uff90severity fire had a larger impact on ecosystem carbon uptake and storage than thinning. Total ecosystem carbon was 42% lower at the intensely burned site, 10 years after burning, than at the undisturbed site. Eddy covariance measurements over two years showed that the burned site was a net annual source of carbon to the atmosphere whereas the undisturbed site was a sink. Net primary production (NPP), evapotranspiration (ET), and water use efficiency were lower at the burned site than at the undisturbed site. In contrast, thinning decreased total ecosystem carbon by 18%, and changed the site from a carbon sink to a source in the first post\uffe2\uff80\uff90treatment year. Thinning also decreased ET, reduced the limitation of drought on carbon uptake during summer, and did not change water use efficiency. Both disturbances reduced ecosystem carbon uptake by decreasing gross primary production (55% by burning, 30% by thinning) more than total ecosystem respiration (TER; 33\uffe2\uff80\uff9347% by burning, 18% by thinning), and increased the contribution of soil carbon dioxide efflux to TER. The relationship between TER and temperature was not affected by either disturbance. Efforts to accurately estimate regional carbon budgets should consider impacts on carbon dynamics of both large disturbances, such as high\uffe2\uff80\uff90intensity fire, and the partial disturbance of thinning that is often used to prevent intense burning. Our results show that thinned forests of ponderosa pine in the southwestern United States are a desirable alternative to intensively burned forests to maintain carbon stocks and primary production.</p>", "keywords": ["Biometry", "QH301 Biology", "Cell Respiration", "Arizona", "Water", "Forestry", "Plant Transpiration", "Carbon Dioxide", "15. Life on land", "01 natural sciences", "Carbon", "Fires", "6. Clean water", "Pinus ponderosa", "Soil", "13. Climate action", "Biomass", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1890/09-0934.1"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Ecological%20Applications", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1890/09-0934.1", "name": "item", "description": "10.1890/09-0934.1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1890/09-0934.1"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2010-04-01T00:00:00Z"}}, {"id": "10.1890/10-0660.1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:20:37Z", "type": "Journal Article", "created": "2011-06-10", "title": "Fire effects on temperate forest soil C and N storage", "description": "Temperate forest soils store globally significant amounts of carbon (C) and nitrogen (N). Understanding how soil pools of these two elements change in response to disturbance and management is critical to maintaining ecosystem services such as forest productivity, greenhouse gas mitigation, and water resource protection. Fire is one of the principal disturbances acting on forest soil C and N storage and is also the subject of enormous management efforts. In the present article, we use meta-analysis to quantify fire effects on temperate forest soil C and N storage. Across a combined total of 468 soil C and N response ratios from 57 publications (concentrations and pool sizes), fire had significant overall effects on soil C (-26%) and soil N (-22%). The impacts of fire on forest floors were significantly different from its effects on mineral soils. Fires reduced forest floor C and N storage (pool sizes only) by an average of 59% and 50%, respectively, but the concentrations of these two elements did not change. Prescribed fires caused smaller reductions in forest floor C and N storage (-46% and -35%) than wildfires (-67% and -69%), and the presence of hardwoods also mitigated fire impacts. Burned forest floors recovered their C and N pools in an average of 128 and 103 years, respectively. Among mineral soils, there were no significant changes in C or N storage, but C and N concentrations declined significantly (-11% and -12%, respectively). Mineral soil C and N concentrations were significantly affected by fire type, with no change following prescribed burns, but significant reductions in response to wildfires. Geographic variation in fire effects on mineral soil C and N storage underscores the need for region-specific fire management plans, and the role of fire type in mediating C and N shifts (especially in the forest floor) indicates that averting wildfires through prescribed burning is desirable from a soils perspective.", "keywords": ["0106 biological sciences", "Nitrogen", "Science", "soil nitrogen", "Ecology and Evolutionary Biology", "forest management", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "Carbon", "Fires", "Trees", "meta-analysis", "Soil", "carbon sinks", "13. Climate action", "temperate forests", "0401 agriculture", " forestry", " and fisheries", "soil carbon", "fire", "Ecosystem"], "contacts": [{"organization": "Lucas E. Nave, Lucas E. Nave, Eric D. Vance, Christopher W. Swanston, Peter S. Curtis,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1890/10-0660.1"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Ecological%20Applications", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1890/10-0660.1", "name": "item", "description": "10.1890/10-0660.1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1890/10-0660.1"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2011-06-01T00:00:00Z"}}], "links": [{"rel": "self", "type": "application/geo+json", "title": "This document as GeoJSON", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=Fire&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=Fire&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=Fire&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=Fire&offset=100", "hreflang": "en-US"}], "numberMatched": 251, "numberReturned": 50, "distributedFeatures": [], "timeStamp": "2026-06-25T00:15:30.477200Z"}