Search results for "ORGANIC MATTER"

showing 10 items of 577 documents

Biogeochemical Cycle of Silica in an Apolyhaline Interdunal Holocene Lake (Chad, N'Guigmi Region, Niger)

1999

During the Holocene, the apolyhaline conditions in interdunal ephemeral lakes in the Lake Chad region led to various diagenetic processes, which resulted in: (a) clay authigenesis, (b) organic matter lithification (plants and cyanobacterial mats), (c) precipitation of sodium silicate (magadiite, kenyaite, zeolite), and (d) chert neoformation. Each step in this diagenetic process involves silica, which can be highly mobile under such conditions. Therefore, the paleoenvironmental variations can be investigated using the Si cycle.http://link.springer. de/link/service/journals/00114/bibs/9086010/90860475.htm</HEA

chemistry.chemical_classificationBiogeochemical cycleEcologyEphemeral keyGeochemistrySodium silicateGeneral MedicineDiagenesischemistry.chemical_compoundchemistryOrganic matterPrecipitationLithificationEcology Evolution Behavior and SystematicsHoloceneGeologyNaturwissenschaften
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Stable Cu isotope fractionation in soils during oxic weathering and podzolization

2011

Abstract Copper stable isotope ratios are fractionated during various biogeochemical processes and may trace the fate of Cu during long-term pedogenetic processes. We assessed the effects of oxic weathering (formation of Cambisols) and podzolization on Cu isotope ratios (δ65Cu). Two Cambisols (oxic weathered soils without strong vertical translocations of soil constituents) and two Podzols (soils showing vertical translocation of organic matter, Fe and Al) were analyzed for Cu concentrations, partitioning of Cu in seven fractions of a sequential extraction and δ65Cu values in bulk soil. Cu concentrations in the studied soils were low (1.4–27.6 μg g−1) and Cu was mainly associated with stron…

chemistry.chemical_classificationBiogeochemical cycleIsotope fractionationGeochemistry and PetrologyChemistryStable isotope ratioEnvironmental chemistrySoil waterBulk soilOrganic matterWeatheringPodzolGeochimica et Cosmochimica Acta
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Accumulation of metals and changes in composition of freshwater lake organic sediments during the Holocene

2020

Abstract The distribution of metals in the strata of sediments deposited in the freshwater environment formed during the Holocene in the territory of Latvia has been studied rather insufficiently. Considering the large volume of accumulated organic matter in sediments, studies on the content of metallic elements in sediments can help to determine the peculiarities of the metal accumulation process in limnic systems and the biogeochemical cycling of metals. Lake Pilvelis, which is located in the eastern part of Latvia (the northern part of Europe), was selected as the main study site. Lake Pilvelis is a small lake of a glacial origin, and >90% of its depression is filled with organic-rich se…

chemistry.chemical_classificationBiogeochemical cycleMineral010504 meteorology & atmospheric sciencesGeochemistrySedimentGeologySapropel010502 geochemistry & geophysics01 natural scienceschemistryGeochemistry and PetrologySedimentary rockOrganic matterGlacial periodHoloceneGeology0105 earth and related environmental sciencesChemical Geology
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Effect of wastewater management on phosphorus content and sedimentary fractionation in Mediterranean saline lakes

2019

The La Mancha Húmeda Biosphere Reserve is the largest wetland district in the Iberian Peninsula, containing many temporary saline lakes undergoing different anthropogenic pressures. Eleven of these lakes were selected to assess phosphorus (P) burial, fractionation and mobilization in their sediments. Wastewater inputs, wherever they occurred, favored accumulation of all P sedimentary fractions, which took place mainly via precipitation with divalent cations (i.e. calcium or magnesium) and as buried organic matter, both representing relatively occluded P forms, although they can also be involved in P release. P immobilization would be partially restrained in the volcanic lakes of the region,…

chemistry.chemical_classificationBiogeochemical cyclegeographyEnvironmental Engineeringgeography.geographical_feature_category010504 meteorology & atmospheric sciencesPhosphorusfood and beverageschemistry.chemical_elementBiogeochemistryWetland010501 environmental sciences01 natural sciencesPollutionchemistryWastewaterEnvironmental chemistryEnvironmental ChemistryEnvironmental scienceOrganic matterWater pollutionEutrophicationWaste Management and Disposal0105 earth and related environmental sciencesScience of The Total Environment
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Soil microbial and microfaunal communities and organic matter quality in reindeer winter and summer ranges in Finnish subarctic mountain birch forests

2008

Abstract Reindeer husbandry has significant influences on the aboveground plant communities and the structure of the mountain birch forests in the Fennoscandian subarctic. We investigated how the reindeer-mediated aboveground changes affect soil microbial and microfaunal communities and enzymatic activities. We hypothesized that in areas with intensive summer browsing by reindeer, the carbon flow to belowground is reduced, but the carbon substances are more readily degradable. This is likely to influence both the abundance and the trophic structure of microbial and microfaunal communities. However, despite large differences in the vegetation, the reindeer ranges did not differ in the amount…

chemistry.chemical_classificationBiomass (ecology)EcologyEcologySoil biologySoil organic matterSoil SciencePlant communitySoil carbonAgricultural and Biological Sciences (miscellaneous)Subarctic climatechemistryAgronomyEnvironmental scienceOrganic matterTrophic levelApplied Soil Ecology
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Responses of microbial-feeding nematodes to organic matter distribution and predation in experimental soil habitat

2001

Abstract Soils are spatially heterogeneous environments, a condition which is likely to affect the structure and function of soil food webs. To study the influence of soil organic matter distribution on decomposer food webs, we established microcosms that contained either: (1) large patches of initially sterile humus-litter mixture placed within sterile sand matrix (creating a large-patch habitat; LPH); or (2) blend of sand and humus-litter mixture (creating a small-patch habitat; SPH). Ten species of bacteria and ten species of fungi, and two bacterial-feeding ( Acrobeloides tricornis , Caenorhabditis elegans ) and two fungal-feeding ( Aphelenchus avenae , Aphelenchoides sp.) nematodes wer…

chemistry.chemical_classificationBiomass (ecology)EcologySoil biologySoil organic matterSoil ScienceBiologyMicrobiologyFood webchemistrySoil food webOrganic matterTrophic levelApex predatorSoil Biology and Biochemistry
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Microscale magnesium distribution in shell of the Mediterranean mussel Mytilus galloprovincialis: An example of multiple factors controlling Mg/Ca in…

2019

Abstract Since magnesium concentration (Mg/Ca) in biogenic calcite is considered to reflect water temperature during precipitation, the magnesium-to‑calcium ratio has been examined as a proxy for water temperature in paleoclimate research, although factors other than temperature may also influence Mg/Ca in biogenic calcite, thereby introducing a potential bias in the relationship between Mg/Ca and temperature observed in inorganic systems. To better understand factors controlling Mg incorporation into the calcitic shells of bivalves, the distribution of Mg in the Mediterranean mussel Mytilus galloprovincialis was studied, being compared with ambient sea surface temperature (SST), shell grow…

chemistry.chemical_classificationCalciteMediterranean mussel010504 meteorology & atmospheric sciencesbiologyMagnesiumchemistry.chemical_elementGeology010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesMytiluschemistry.chemical_compoundSea surface temperaturechemistryGeochemistry and PetrologyEnvironmental chemistryOrganic matterGrowth rateMicroscale chemistryGeology0105 earth and related environmental sciencesChemical Geology
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Microbial origin for pedogenic micrite associated with a carbonate paleosol (Champagne, France)

1999

Abstract Micro-rods have been observed in indurated carbonate horizons (30 cm thick) that overlie a periglacial chalk formation, in contact with the present-day soil (Champagne, France). They are numerous in the upper part of the hardened layers. Variations in micro-rod morphologies are related to progressive biomineralization of organic matter, transforming purely organic rods into calcite. Mineralized rods undergo diagenesis and their arrangement evolves from a random mesh fabric to recrystallized micritic platelets to microsparite. Two types of organic micro-rods have been observed: bacilliform and thread-like bacteria. Mineralogically, micro-rods are low-magnesian calcite. Crystallograp…

chemistry.chemical_classificationCalcitegenetic structuresMicriteStratigraphyMineralogyGeologyPaleosolDiagenesischemistry.chemical_compoundPedogenesischemistryCarbonateOrganic mattersense organsGeologyBiomineralizationSedimentary Geology
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Effects of organic matter complexation on partitioning of transition metals into calcite: Cave-analogue crystal growth experiments

2022

We highlight the potential for first row transition metals to carry paleohydrological signals in speleothems, and argue that these metals constitute valuable proxies for climate reconstructions. Metal availability to speleothems is hypothesised to be restricted by organic complexation, which strongly limits the free ion activity of transition metals (Co2+, Ni2+ and Cu2+) in dripwater, thereby creating a kinetic overprint on metal concentrations and isotope ratios in speleothem calcite. This study presents the results of the first cave-analogue experiments of transition metal partitioning into calcite in the absence and presence of organic ligands. The Geological Microclimate (GeoMic) system…

chemistry.chemical_classificationCalcitegeographyAqueous solutiongeography.geographical_feature_categoryInorganic chemistryNitrilotriacetic acidSpeleothemF800Metalchemistry.chemical_compoundchemistryTransition metalGeochemistry and Petrologyvisual_artvisual_art.visual_art_mediumOrganic matterChelation
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Soil water repellency assessment in olive groves in Southern and Eastern Spain

2016

Soil water repellency (SWR) has been reported under different soils, land uses and regions of the world, particularly in forest land and after wildfires, yet the understanding of this variable in agricultural lands is still rather limited. This study presents the characterization from field-based measurements of SWR in four contrasted olive groves (Olea europaea L.) in Spain in terms of different environmental conditions and management: abandoned and commercial farms under permanent cover crop, conventional tillage and herbicide use. The main objectives were [1] to evaluate the potential occurrence, intensity and persistence of soil water repellency in different types of olive groves and [2…

chemistry.chemical_classificationCanopyConventional tillage010504 meteorology & atmospheric sciencesOliveSoil water repellency04 agricultural and veterinary sciences01 natural sciencesAgronomychemistryDry seasonSoil water040103 agronomy & agriculture0401 agriculture forestry and fisheriesEnvironmental scienceOrganic matterOrganic matterOrchardHydrologyCover cropWater content0105 earth and related environmental sciencesEarth-Surface ProcessesCrop management
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