Search results for "CHIMIE DU SOL"

showing 2 items of 2 documents

Les phénols de la lignine et le 13C, traceurs de l'origine des matières organiques du sol

2001

Abstract In spodosols of Gascony (France), conversion of maritime pine stands into maize cropping leads to an incorporation of maize organic matter, which changed the isotopic (δ13C) and phenolic signature in A and L horizons of soil. Hydrolysis of phenol lignin in forests and cultivated soils showed the predominance of vanillic units under forest and the early but moderate incorporation of cinnamic acids. Incorporation of syringic units appeared higher, related to a large maize production of stable syringic phenols. Syringic units represented a long-term marker of maize inputs in soils, whereas vanillic units revealed the degradation of forest organic matter.

[SDE] Environmental SciencesCHIMIE DU SOL[SDV]Life Sciences [q-bio]SOL CULTIVEOcean Engineering010501 environmental sciences01 natural scienceschemistry.chemical_compoundBotanyLigninZONE FORESTIEREOrganic matterMARQUEUR MOLECULAIREPhenolsComputingMilieux_MISCELLANEOUSEcology Evolution Behavior and Systematics0105 earth and related environmental sciences2. Zero hungerchemistry.chemical_classificationTotal organic carbonδ13CChemistryPIN MARITIME04 agricultural and veterinary sciences15. Life on landCARBONEPodzolLANDES DE GASCOGNE[SDV] Life Sciences [q-bio]MAIS[SDE]Environmental SciencesSoil water040103 agronomy & agriculture0401 agriculture forestry and fisheriesSoil horizonLIGNINECOMPOSE PHENOLIQUE
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In situ Mössbauer spectroscopy: Evidence for green rust (fougerite) in a gleysol and its mineralogical transformations with time and depth

2005

Abstract A miniaturized Mossbauer spectrometer, adapted to the Earth’s conditions from the instrument developed for Mars space missions, has been used for the first time to study in situ variations with depth and transformations with time of iron minerals in a gleysol. The instrument is set into a PVC tube and can be moved up and down precisely (±1 mm) at the desired depth. Mossbauer spectra were obtained from 15 to 106 cm depth and repeated exactly at the same point at different times to follow mineralogical transformations with time. X-ray diffraction (XRD) and selective extraction techniques were performed on soil samples. The piezometric level of the water table was measured and the com…

P33 - Chimie et physique du solSoil test[SDV]Life Sciences [q-bio]Instrument de mesureAnalytical chemistryStructural formulaSol hydromorphe010501 environmental sciencesengineering.material010502 geochemistry & geophysicsFougèrite01 natural sciencesChimie du solhttp://aims.fao.org/aos/agrovoc/c_25315Geochemistry and PetrologyMössbauer spectroscopyhttp://aims.fao.org/aos/agrovoc/c_12457ComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesChemistryhttp://aims.fao.org/aos/agrovoc/c_7161FerMINERALOGIEGleysolGEOCHIMIE13. Climate action[SDE]Environmental SciencesSoil waterengineeringSoil horizonhttp://aims.fao.org/aos/agrovoc/c_3950Gleysolhttp://aims.fao.org/aos/agrovoc/c_3276Solid solutionGeochimica et Cosmochimica Acta
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