Search results for "C mineralisation"

showing 4 items of 4 documents

Agricultural management affects the response of soil bacterial community structure and respiration to water-stress

2013

International audience; Soil microorganisms are responsible for organic matter decomposition processes that regulate soil carbon storage and mineralisation to CO2. Climate change is predicted to increase the frequency of drought events, with uncertain consequences for soil microbial communities. In this study we tested the hypothesis that agricultural management used to enhance soil carbon stocks would increase the stability of microbial community structure and activity in response to water-stress. Soil was sampled from a long-term field trial with three soil carbon management systems and was used in a laboratory study of the effect of a dry wet cycle on organic C mineralisation and microbi…

Agricultural land use010504 meteorology & atmospheric sciencesSoil biodiversity[SDV]Life Sciences [q-bio]Soil biologySoil Science01 natural sciencesMicrobiologyDrying-rewettingFUNCTIONAL STABILITYSoil retrogression and degradation[SDV.BV]Life Sciences [q-bio]/Vegetal BiologyOrganic matterGlobal changeNITROGEN MINERALIZATION0105 earth and related environmental sciences2. Zero hungerchemistry.chemical_classificationC mineralisationCLIMATE-CHANGEMICROBIAL COMMUNITYEcologySoil organic matterLAND-USE CHANGE04 agricultural and veterinary sciencesSoil carbonRESILIENCE15. Life on landDRYING-REWETTING FREQUENCYORGANIC-MATTERAgronomychemistryMicrobial population biology13. Climate action[SDE]Environmental Sciences040103 agronomy & agricultureBacterial community structure0401 agriculture forestry and fisheriesEnvironmental scienceCATABOLIC DIVERSITYCARBON STOCKSMicrocosmStabilitySoil Biology and Biochemistry
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Long‐Term Tillage and Cropping System Effects on Chemical and Biochemical Characteristics of Soil Organic Matter in a Mediterranean Semiarid Environm…

2015

Several studies have reported how tillage and cropping systems affect quantity, quality, and distribution of soil organic matter (SOM) along the profile. However, the effect of soil management on the chemical structure of SOM and on its hydrophobic and hydrophilic components has been little investigated. In this work, the long-term (19 years) effects of two cropping systems (wheat monoculture and wheat/faba bean rotation) and three tillage managements (conventional, reduced, and no tillage) on some chemical characteristics of SOM and their relationships with labile carbon (C) pools were evaluated. Soil samples were taken from the topsoil (0–15 cm) of a Chromic Haploxerert (central Sicily, I…

C mineralisationDRIFTSettore AGR/13 - Chimica Agrariaaromaticitymicrobial biomass ChydrophobicitySettore AGR/02 - Agronomia E Coltivazioni Erbacee
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Dynamics of carbon pools in a soil covered with different forest tree species after controlled heating and wetting

2012

Fire-induced soil heating deeply affects soil organic C pools and their dynamics. The objective of this study was to investigate, in a soil covered with different forest tree species (Eucalyptus camaldulensis, E. occidentalis, Pinus halepensis, and Cupressus sempervirens), the effect of controlled heating on C pools and C mineralization dynamics. Soil samples were heated under controlled condition in laboratory (160 and 380°C) and then wetted with distilled or sea water to simulate the extinction of wildfires. Soil organic C pools react to heating in different way depending on forest tree species. Total organic C was almost halved following the heating of soils at 380°C. Soil covered with P…

Settore AGR/13 - Chimica Agrariaforest soil C pools C mineralisation soil heating sea water
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Effect of temperature on soil microbial structure and fractionation during C mineralisation

2008

International audience; Microbial carbon mineralization in soils leads to the production of different gaseous or dissolved components that have environmental impacts. Our study deals with the influence of soil temperature on the production of gaseous and dissolved carbon components during carbon mineralization in forest soils in France. After an incubation of soil samples for 42 days at 4 different temperatures, we determined both size and 13C isotopic signature of dissolved organic carbon and CO2 pools. We also characterised the soil microbial community structure (PLFA profiles). While temperature clearly increases the CO2 production, a low decrease of the dissolved organic carbon pool was…

[SDV] Life Sciences [q-bio][SDE] Environmental SciencesC mineralisationeffect of temperature[SDV]Life Sciences [q-bio][SDE]Environmental Sciencesfractionationsoil microbial structurecomplex mixtures
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