Search results for "Organic matter"

showing 10 items of 577 documents

Relationships between soil water repellency and microbial community composition under different plant species in a Mediterranean semiarid forest

2014

Abstract Soil water repellency (SWR) can influence many hydrological soil properties, including water infiltration, uneven moisture distribution or water retention. In the current study we investigated how variable SWR persistence in the field is related to the soil microbial community under different plant species (P. halepensis, Q. rotundifolia, C. albidus and R. officinalis) in a Mediterranean forest. The soil microbial community was determined through phospholipid fatty acids (PLFA). The relationships between microbiological community structure and the soil properties pH, Glomalin Related Soil Protein (GRSP) and soil organic matter (SOM) content were also studied. Different statistical …

BiohydrologyMediterranean climatesoil hydrophobicityTA Engineering (General). Civil engineering (General)Phospholipids fatty acidsActinobacteriaBotanymedicinebiohydrologyGlomalin Related Soil ProteinWater Science and TechnologyFluid Flow and Transfer Processesglomalin related soil proteinbiologyphospholipids fatty acidsMechanical EngineeringSoil organic matterCommunity structureactinobacteriaMicrobial community structureHydraulic engineeringbiology.organism_classificationWater retentionActinobacteriaGlomalinMicrobial population biologyAgronomymicrobial community structureSoil waterbiology.proteinEnvironmental sciencemedicine.symptomTC1-978Soil hydrophobicity
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Soil carbon quality and nitrogen fertilization structure bacterial communities with predictable responses of major bacterial phyla

2014

Abstract Agricultural practices affect the soil ecosystem in multiple ways and the soil microbial communities represent an integrated and dynamic measure of soil status. Our aim was to test whether the soil bacterial community and the relative abundance of major bacterial phyla responded predictably to long-term organic amendments representing different carbon qualities (peat and straw) in combination with nitrogen fertilization levels and if certain bacterial groups were indicative of specific treatments. We hypothesized that the long-term treatments had created distinctly different ecological niches for soil bacteria, suitable for either fast-growing copiotrophic bacteria, or slow-growing…

Biomass (ecology)EcologybiologyEcologySoil organic matterSoil biology[SDV]Life Sciences [q-bio]Soil ScienceBiological indicatorsSoil carbonStrawbiology.organism_classificationAgricultural and Biological Sciences (miscellaneous)Nitrogen fertilizationAgronomySoil statusLong-term experimentMicrobial community[SDE]Environmental Sciences[SDV.BV]Life Sciences [q-bio]/Vegetal BiologyGemmatimonadetesEcosystemOrganic amendmentAcidobacteria
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Soil microbial activity and functional diversity in primeval beech forests

2015

Virgin forests are unique ecosystems, which can be used as etalon for basic biocoenotic investigation. Soil microorganisms are very sensitive reagents on influence of biotical factors, and at the same time are the active producers of phytotoxic and phytostimulating exometabolites. Studies of soil microbiota were conducted in virgin beech forests of Shyrokoluzhansky massif of the Carpathian Biosphere Reserve. It was found the ratio and the number of different ecological-trophic groups of soil microorganisms changes with altitude. So the number of ammonificators with increasing of altitude above sea level was reduced. The soil at altitude of 1,100 meters above sea level was characterized by m…

Biotopegeographygeography.geographical_feature_categorybiologyEcologyMicroorganismSoil organic matterbiology.organism_classificationOld-growth forestAltitudeAgronomyMicrobial ecologyEcosystemBeechJournal of Earth Science and Engineering
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In situ polymerization of soil organic matter by oxidative biomimetic catalysis

2017

Abstract Background Agricultural practices that enhance organic matter content in soil can play a central role in sequestering soil organic carbon (SOC) and reducing greenhouse gases emissions. Methods We used a water-soluble iron-porphyrin to catalyze directly in situ oxidative polymerization of soil organic matter in the presence of H2O2 oxidant, with the aim to enhance OC stabilization, and, consequently, reduce CO2 emissions from soil. The occurred SOC stabilization was assessed by monitoring soil aggregate stability, OC distribution in water-soluble aggregates, soil respiration, and extraction yields of humic and fulvic acids. Results Soil treatment with H2O2 and iron-porphyrin increas…

CO2 emissions Soil carbon sequestrate Soil organic matter Soil respiration Oxidative biomimetic catalysisSettore AGR/13 - Chimica Agraria010501 environmental sciencesCO2 emissions01 natural sciencesBiochemistrycomplex mixturesSoil respirationlcsh:AgricultureOrganic matter0105 earth and related environmental scienceschemistry.chemical_classificationSoil organic matterSoil organic matterlcsh:SSoil chemistry04 agricultural and veterinary sciencesSoil carbonMineralization (soil science)Soil respirationOxidative biomimetic catalysischemistryPolymerizationEnvironmental chemistrySoil water040103 agronomy & agriculture0401 agriculture forestry and fisheriesSoil carbon sequestrationAgronomy and Crop ScienceFood ScienceBiotechnologySettore AGR/16 - Microbiologia AgrariaChemical and Biological Technologies in Agriculture
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Small scale secondary CaCO3 accumulations in selected sections of the European loess belt. Morphological forms and potential for paleoenvironmental r…

1997

Eighteen important Quaternary loess paleosoil sites have been studied across the European loess belt. They included approximately 50 buried soils, the over and/or underlying loess and the present-day surface soils (where possible). From the numerous types of secondary CaCO3 accumulations recognized, only the small scale accumulations are discussed in this paper, including calcified root cells, CaCO3 hypocoatings, needle-fiber calcite, powdery calcite coatings, earthworm biospheroliths, and calcite pseudomorphs on gypsum. Most of the features studied are found in the rhizosphere microecosystem. Each of these features showed a unique relationship with organic matter, micro-organism and plant …

Calcitechemistry.chemical_classificationGypsumMoistureSoil ScienceSoil scienceengineering.materialPaleosolchemistry.chemical_compoundchemistryLoessSoil waterLeaching (pedology)engineeringOrganic matterGeologyGeoderma
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Impact of changing forest management on soil organic matter in low mountain acid media

2002

The impacts of changes in vegetation cover from native deciduous forest to Douglas fir ( Pseudotsuga menziesii Franco) and of human activity on soil organic matter (SOM) characteristics were studied in two low mountain areas of east-central France. No striking difference in soil type (Dystric Cambisol) was found between the two sites. Humus-rich horizons were of the “Dysmull” and “Moder” types, regardless of the nature of the bedrock. Contrary to a common affirmation concerning other coniferous species, Douglas fir had no negative effect on soil pH and humification degree of SOM, with respect to the native beech vegetation. Pruning and partial clearing slightly improved humification, espect…

CambisolSoil seriesSoil organic matterEnvironmental scienceSoil scienceSoil classificationForestryVegetationPlant litterSoil typeHumus
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Isotope ratios of nonexchangeable hydrogen in soils from different climate zones

2010

Abstract The fractionation of H isotopes in global precipitation leads to a continuous decrease in 2 H concentrations of precipitation with increasing latitude, altitude and continentality. Thus, the local precipitation, soil and ground water used by plants for photosynthesis or consumed during neoformation of pedogenic clay minerals often have a spatially diagnostic δ 2 H value. We hypothesize that the δ 2 H value of isotopically nonexchangeable H in bulk soil (composed of C-bonded H in soil organic matter (SOM) and the nonexchangeable fraction of O-bonded H in pedogenic clay minerals) is correlated with the mean δ 2 H value of local precipitation water at the place and time of biomass pro…

CambisolTopsoilPedogenesisSoil testSoil organic matterSoil waterBulk soilSoil ScienceSoil scienceClay mineralsGeologyGeoderma
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Short-term response of the Ca cycle of a montane forest in Ecuador to low experimental CaCl2 additions

2013

The tropical montane forests of the E Andean cordillera in Ecuador receive episodic Sahara-dust inputs particularly increasing Ca deposition. We added CaCl2 to isolate the effect of Ca deposition by Sahara dust to tropical montane forest from the simultaneously occurring pH effect. We examined components of the Ca cycle at four control plots and four plots with added Ca (2 x 5kg ha(-1) Ca annually as CaCl2) in a random arrangement. Between August 2007 and December 2009 (four applications of Ca), we determined Ca concentrations and fluxes in litter leachate, mineral soil solution (0.15 and 0.30 m depths), throughfall, and fine litterfall and Al concentrations and speciation in soil solutions…

Canopy010504 meteorology & atmospheric sciencesSoil SciencePlant ScienceCalcium cycleAl ratio [Molar Ca]01 natural sciencesDissolved organic carbonBotanyGraffenrieda emarginata TrianaOrganic matter0105 earth and related environmental scienceschemistry.chemical_classificationAl speciationBiomass (ecology)Stem diameter growthTropical montane forest04 agricultural and veterinary sciences15. Life on landPlant litterThroughfallchemistryEnvironmental chemistry040103 agronomy & agricultureLitter0401 agriculture forestry and fisheriesDeposition (chemistry)
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Microstructure-specific carbon isotopic signatures of organic matter from ∼3.5 Ga cherts of the Pilbara Craton support a biologic origin.

2016

21 pages; International audience; The ∼3.5 Ga Dresser Formation from the North Pole Dome of the Pilbara Craton (Western Australia) contains some of the oldest evidence for life on Earth. Here, we present a detailed study of microstructure-specific carbon isotopic composition of organic matter (OM) preserved in Dresser Formation bedded cherts and hydrothermal chert vein using in situ Secondary-Ion Mass Spectrometry (SIMS). The OM in these rocks occurs mainly as clots that, together with minor fine OM layers and laminae, are considered primary textures formed prior to host rock lithification. Other than rare OM-rich stylolites, no evidence was found for later OM migration beyond the micromete…

Carbon isotope ratio010504 meteorology & atmospheric sciencesMetamorphic rockPilbara CratonMineralogy010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesMicrofossilsPilbara cratonGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryDresser FormationOrganic matterLithificationAnkerite0105 earth and related environmental scienceschemistry.chemical_classificationδ13CGeology15. Life on land[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistrychemistry13. Climate actionStylolite[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyOrganic matterVein (geology)SIMSGeology
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Sequestration of organomettalic compounds by synthetic and naturally occuring polycarboxylate ligands. Binding of monomethylmercury(II) by polyacryli…

2007

The sequestering capacity of synthetic and naturally occurring polycarboxylate ligands towards mono- methylmercury(II) was evaluated by stability quantitative data on the interaction of CH3Hgþ with different molecular weight synthetic polyacrylates (2 and 20 kDa average M.wt) and alginate (70– 100 kDa) extracted from brown algae Macrocystis pyrifera. The influence of ionic medium was evaluated by measurements on the CH3Hgþ-polyacrylate systems in NaNO3 medium at different ionic strengths (0.10, 0.25, 0.50 and 0.75mol Lÿ1), and a Debye–Hu¨ ckel type equation was used for the dependence of complex formation constants on ionic strength. Measurements on the CH3Hgþ - alginate system were carried…

Chemical Health and SafetybiologyChemistryHealth Toxicology and MutagenesisComplex formationIonic bondingmonomethylmercury; sequestration by organic matter; polyacrylic and alginic acidsToxicologybiology.organism_classificationBrown algaemonomethylmercuryBinding abilityType equationpolyacrylic and alginic acidsmonomethylmercury sequestration by organic matter polyacrylic and alginic acids speciation equilibrium analysis complex species formationIonic strengthOrganic chemistrySettore CHIM/01 - Chimica Analiticasequestration by organic matterNuclear chemistryGroup 2 organometallic chemistry
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