Search results for "Organic carbon"

showing 10 items of 319 documents

Assessment of Organic Carbon Sequestration from Romanian Degraded Soils: Livada Forest Plantation Case Study

2022

To analyse the capacity of a soil to sequester organic carbon and the impact that deforestation and reforestation can have on its physical and chemical properties, specific laboratory analyses are necessary. According to a standard methodology, a number of 16 samples were taken from two different depths (0–10 cm, 10–20 cm) and from two different areas (degraded area and forest area) to identify if the type of land use and sampling depth are the key factors in changing the obtained values and also to prove the hypothesis according to which forest lands may have a higher carbon sequestration capacity. The highest value of soil organic carbon was identified in the forest area at a …

Atmospheric ScienceEnvironmental Science (miscellaneous)afforestation; organic carbon; water holding capacity; degraded soils; pHAtmosphere
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Composition and diurnal variability of the natural Amazonian aerosol

2003

As part of the Large-Scale Biosphere-Atmosphere Experiment in Amazonia (LBA)-Cooperative LBA Airborne Regional Experiment (CLAIRE) 2001 campaign, separate day and nighttime aerosol samples were collected in July 2001 at a ground-based site in Amazonia, Brazil, in order to examine the composition and temporal variability of the natural “background” aerosol. A combination of analytical techniques was used to characterize the elemental and ionic composition of the aerosol. Major particle types larger than ∼0.5 μm were identified by electron and light microscopy. Both the coarse and fine aerosol were found to consist primarily of organic matter (∼70 and 80% by mass, respectively), with the coar…

Atmospheric Sciencefood.ingredientSoil ScienceMineralogyAquatic ScienceOceanographychemistry.chemical_compoundfoodGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Organic matterSulfateEarth-Surface ProcessesWater Science and Technologychemistry.chemical_classificationTotal organic carbonEcologySea saltPaleontologyForestryParticulatesAerosolGeophysicschemistrySpace and Planetary ScienceEnvironmental chemistryParticleBioaerosolJournal of Geophysical Research: Atmospheres
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Organosulfates in atmospheric aerosol: synthesis and quantitative analysis of pm<sub>2.5</sub> from xi'an, northwestern c…

2018

Abstract. The sources, formation mechanism and amount of organosulfates (OS) in atmospheric aerosol are not yet well understood, partly due to the lack of authentic standards for quantification. In this study, we report an improved robust procedure for the synthesis of organosulfates with different functional groups. Nine authentic organosulfate standards were synthesized and four standards (benzyl sulfate, phenyl sulfate, glycolic acid sulfate, and hydroxyacetone sulfate) were used to quantify their ambient concentrations. The authentic standards and ambient aerosol samples were analyzed using an optimized ultra performance liquid chromatography–electrospray ionization-tandem mass spectrom…

Atmospheric Scienceparticulate organosulfates010504 meteorology & atmospheric sciences010501 environmental sciences01 natural scienceschemistry.chemical_compoundambient aerosolhaze eventsSulfateGlycolic acid0105 earth and related environmental sciencesDetection limitTotal organic carbondicarboxylic-acidsHydroxyacetonemass-spectrometryAerosolaromatic organosulfateschemistryEnvironmental chemistrychemical-compositionarctic aerosolsisopreneQuantitative analysis (chemistry)secondary organic aerosolOrganosulfate
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Differenziazione e quantificazione dei carbonati litogenici e pedogenici di Gypsisuoli forestali attraverso l'analisi isotopica

2004

Gli autori riferiscono sui tipi e sui modelli di genesi dei carbonati dei suoli, attraverso l’uso degli isotopi del 13C. Lo studio è stato condotto in un’area dell’interno collinare argilloso siciliano, su suoli che evolvono sui depositi evaporitici della Serie Gessoso-Solfifera. Sono stati scelti cinque pedon su litotipi calcarei e non. I pedon sono stati descritti in campo e campionati secondo la sequenza degli orizzonti genetici; sui campioni di suolo sono state eseguite le seguenti analisi: tessitura, reazione, conducibilità elettrica, gesso, carbonio organico ed inorganico. Inoltre, parallelamente sono state eseguite le analisi isotopiche del carbonio organico ed inorganico. I risultat…

Authors report on forms and soil carbonate formation models as detected by 13C isotopes. This study was carried out in a clayey hilly area of central Sicily where soils have developed on evaporitic deposits of “Gessoso-Solfifera” Formation. Four pedons were selected both on calcareous and no calcareous lithotypes. Pedons were described in field and sampled according to sequence of genetic horizons. Soil samples were analyzed to investigate the following properties: particle size distribution reaction electrical conductivity gypsum organic and inorganic carbon. Moreover isotopic analyses were performed on organic and inorganic carbon. Results allow us to describe the complex relationships between biotic and abiotic soil components. In addition models of calcic horizon formation and their implication in soil classification were defined.Settore AGR/13 - Chimica Agraria
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Consequence of litter removal on pedogenesis: A case study in Bachs and Irchel (Switzerland)

2016

In forests, soils contain at least twice as much carbon than plants that mostly grow in the upper layers. Litter at the interface between soils and the atmosphere regulates a variety of biogeochemical cycles, which are important for both plants and soils and have possible implications for other environmental components. We have compared leachates collected during an incubation experiment on: a) beech and oak leaves; b) organic subhorizons OLn, OLv, OF, and mineral A horizon; c) treated with litter removal (and untreated) plots, to assess the changes in the chemical composition of the litter layers and leachates during weathering and their influence on the underlying horizons. . Two differen…

Biogeochemical cycle010504 meteorology & atmospheric sciencesChemistryNitrogenSettore AGR/13 - Chimica AgrariaBiomassSoil ScienceLuvisol04 agricultural and veterinary sciencesPlant litter01 natural sciencesPodzol13C CPMAS NMRSUVAPedogenesisSettore AGR/14 - PedologiaEnvironmental chemistryDissolved organic carbonBotanySoil water040103 agronomy & agricultureLitter0401 agriculture forestry and fisheriesPodzol0105 earth and related environmental sciences
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Dust inputs and bacteria influence dissolved organic matter in clear alpine lakes.

2011

6 páginas, 4 figuras.

Biogeochemical cycle010504 meteorology & atmospheric sciencesUltraviolet RaysDrainage basinAir MicrobiologyGeneral Physics and AstronomyFresh Water010501 environmental sciences01 natural sciencesGeneral Biochemistry Genetics and Molecular BiologyArticleDissolved organic carbonEcosystemOrganic ChemicalsEcosystem0105 earth and related environmental sciencesgeographyMultidisciplinarygeography.geographical_feature_categoryBacteriaEcologyAquatic ecosystemAirTemperatureBiogeochemistryDustGeneral Chemistry15. Life on land6. Clean waterDeposition (aerosol physics)Solubility13. Climate actionEnvironmental chemistryEnvironmental scienceEcosystem ecologyNature communications
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Storage and release of fossil organic carbon related to weathering of sedimentary rocks

2007

International audience; The biogeochemical carbon cycle, which plays an undeniable role in global climate change, is defined both by the size of carbon reservoirs (such as the atmosphere, biomass, soil and bedrock) and the exchange between them of various mineral and organic carbon forms. Among these carbon forms, fossil organic carbon (FOC) (i.e., the ancient organic matter stored in sedimentary rocks) is widely observed in modern environments but is not included in the supergene carbon budget. Using a digitized map of the world and an existing model of CO2 consumption associated with rock weathering, we establish the global distribution of FOC stored in the first meter of sedimentary rock…

Biogeochemical cycle010504 meteorology & atmospheric sciencesglobal carbon cyclemajor river basinsEarth science[SDE.MCG]Environmental Sciences/Global ChangesWeatheringSoil science010502 geochemistry & geophysics01 natural sciencesCarbon cycleGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryEarth and Planetary Sciences (miscellaneous)Organic matter91.67.-y0105 earth and related environmental sciencesfossil organic carbon fluxTotal organic carbonchemistry.chemical_classificationgeographygeography.geographical_feature_categoryspatial distributionBedrockSoil carbon15. Life on land[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistry[ SDE.MCG ] Environmental Sciences/Global ChangesGeophysicschemistry13. Climate actionSpace and Planetary Scienceweatheringfossil organic carbon storageSedimentary rockGeology
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Impact of hydrologically driven hillslope erosion and landslide occurrence on soil organic carbon dynamics in tropical watersheds

2016

The dynamics of soil organic carbon (SOC) in tropical forests play an important role in the global carbon (C) cycle. Past attempts to quantify the net C exchange with the atmosphere in regional and global budgets do not systematically account for dynamic feedbacks among linked hydrological, geomorphological, and biogeochemical processes, which control the fate of SOC. Here we quantify effects of geomorphic perturbations on SOC oxidation and accumulation in two adjacent wet tropical forest watersheds underlain by contrasting lithology (volcaniclastic rock and quartz diorite) in the Luquillo Critical Zone Observatory. This study uses the spatially-explicit and physically-based model of SOC dy…

Biogeochemical cycleEnvironmental Engineering010504 meteorology & atmospheric sciencesTropical forestsLithologyLife on Land0208 environmental biotechnologyTRIBS02 engineering and technologyCoupled processesStructural basin01 natural sciencesCivil EngineeringPhysical Geography and Environmental GeoscienceTropical forestLandscape0105 earth and related environmental sciencesWater Science and TechnologyHydrologySoil organic carbonSettore ICAR/02 - Costruzioni Idrauliche E Marittime E IdrologiaLandslideSoil carbonCoupled processe020801 environmental engineeringDioriteDenudationErosionApplied EconomicsErosionCoupled processes; Erosion; Landscape; Soil organic carbon; TRIBS; Tropical forests; Water Science and TechnologyGeology
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2016

Rivers carry large amounts of dissolved organic matter (DOM) to the oceans thereby connecting terrestrial and marine element cycles. Photo-degradation in conjunction with microbial turnover is considered a major pathway by which terrigenous DOM is decomposed. To reveal globally relevant patterns behind this process, we performed photo-degradation experiments and year-long bio-assays on DOM from ten of the largest world rivers that collectively account for more than one-third of the fresh water discharge to the global ocean. We furthermore tested the hypothesis that the terrigenous component in deep ocean DOM may be far higher than biomarker studies suggest, because of the selective photoche…

Biogeochemical cyclegeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesTerrigenous sedimentEcologyDrainage basinVegetation15. Life on land010501 environmental sciences01 natural sciencesDeep sea6. Clean waterGrassland13. Climate actionEnvironmental chemistryDissolved organic carbonGeneral Earth and Planetary SciencesEnvironmental science14. Life underwaterRelative species abundance0105 earth and related environmental sciencesFrontiers in Earth Science
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Batch Test Evaluation of Four Organic Substrates Suitable for Biological Groundwater Denitrification

2014

Nitrates pollution represents nowadays a serious issue related to the quality of groundwater; continuous growth of industrial-scale agricultures lead to an increase of nitrates content in groundwater in the last years. Several technologies have been validated as capable to promote in situ biological nitrates remediation, such as permeable reactive barriers (PRB), biotrench, biobarriers etc. These technologies are all characterised by the use of organic substrate that act as a slow release carbon source. In free dissolved oxygen absence, such organic carbon is further oxidised, by heterotrophic bacteria naturally present in soil, in compliance to anoxic metabolism by using nitrates bound oxy…

Biological groundwater Denitrificationlcsh:Computer engineering. Computer hardwareSettore ICAR/03 - Ingegneria Sanitaria-AmbientaleOrganic carbon source.lcsh:TP155-156lcsh:TK7885-7895Batch testlcsh:Chemical engineeringChemical Engineering Transactions
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