Search results for "DIOXIDE"

showing 10 items of 1250 documents

Soil carbon and soil physical properties under land use change in a protected area of Sicily

2010

This work investigated the role of land cover and land use change as a soil’s ability to store carbon and reduce carbon dioxide emission in a Mediterranean area. Using both historic records and land cover crop maps we estimated the effect of land cover change on the carbon stock from 1972 to 2008 in a natural reserve (Grotta di S. Ninfa) in the West of Sicily. Five paired sites in different soil types were selected and five land use classes (arable land, vineyard, olivegrove, gariga, eucalyptus afforestation) were analyzed. We studied the effect of land use on soil organic carbon (SOC) content in bulk soil and 1000-2000 m, 500-1000 m, 250-500 m, 63-250 m, 25-63 m and <25 m size fractions. F…

Carbon Dioxide EmissionLand Use changeSoil Organic Carbon.
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Geochemistry of fluids and CO2 output in the southern Apennine (Italy): Preliminary results for cold and thermal waters

2020

Carbon Dioxide Earth Degassing Tectonics Appenine
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Fluid geochemistry and CO2 output in the southern Apennine (Italy): Preliminary results

2019

Carbon Dioxide Earth Degassing Tectonics Appenine
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Origin and significance of the production of carbon dioxide during the ozonization of 13C-labeled D-glucose at different pH values.

2001

Abstract [1- 13 C], [2- 13 C] and [6- 13 C] d -glucose were, respectively, ozonized in a semi-batch reactor in acidic and basic conditions. The composition of the gas phase was evaluated by on-line mass spectrometry measurements. The quantitative and isotopic analyses of the carbon dioxide formed during ozonization are presented and discussed. The data, correlated with previous literature results, clearly show that at pH 2.5 the production of carbon dioxide from C-6 and C-1 carbon atoms is nearly equivalent. Conversely, at higher pH values, CO 2 is released with a greater selectivity from the reducing end. The importance of the decarboxylation reaction in the formation of by-products with f…

Carbon IsotopesOzoneDecarboxylationOrganic ChemistryInorganic chemistrychemistry.chemical_elementGeneral MedicineCarbon DioxideHydrogen-Ion ConcentrationBiochemistryMass SpectrometryAnalytical Chemistrychemistry.chemical_compoundGlucoseOzonechemistryTotal inorganic carbonD-GlucoseCarbon dioxideOrganic chemistrySelectivityCarbonElectrochemical reduction of carbon dioxideCarbohydrate research
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Reversible coordination of dioxygen by tripodal tetraamine copper complexes incorporated in a porous silica framework.

2010

The present study reports the synthesis and rational design of porous structured materials by using a templating method. A tetraethoxysilylated tripodal tetraamine (TREN) was covalently incorporated in a silica framework with a double imprint: A surfactant template and a metal ion imprint. The presence of a cationic surfactant (CTAB) endowed the material with a high porosity, and the tripodal or square-pyramidal topology of the ligand was preserved thanks to the use of the silylated Cu(II) complex. After removal of the surfactant and de-metalation, the incorporated tetraamine was quantitatively complexed by CuCl(2) and the material has shown after thermal activation that a reversible bindin…

Carbon MonoxideSilicon dioxideLigandNitrogenMetal ions in aqueous solutionOrganic ChemistryInorganic chemistryCationic polymerizationElectron Spin Resonance Spectroscopychemistry.chemical_elementGeneral ChemistrySilicon DioxideCopperCatalysisAdductOxygenchemistry.chemical_compoundchemistryCoordination ComplexesTripodal ligandPolymer chemistryReactivity (chemistry)AminesPorosityCopperChemistry (Weinheim an der Bergstrasse, Germany)
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Microtomographic Quantification of Hydraulic Clay Mineral Displacement Effects During a CO2 Sequestration Experiment with Saline Aquifer Sandstone

2013

We combined a noninvasive tomographic imaging technique with an invasive open-system core-flooding experiment and compared the results of the pre- and postflooded states of an experimental sandstone core sample from an ongoing field trial for carbon dioxide geosequestration. For the experiment, a rock core sample of 80 mL volume was taken from the 629 m Stuttgart Formation storage domain of a saline sandstone aquifer at the CCS research pilot plant Ketzin, Germany. Supercritical carbon dioxide and synthetical brine were injected under in situ reservoir p/T-conditions at an average flow rate of 0.1 mL/min for 256 h. X-ray computed microtomographic imaging was carried out before and after the…

Carbon SequestrationGeological PhenomenaSalinitySupercritical carbon dioxideTomographic reconstructionMineralogyCore sample550 - Earth sciencesX-Ray MicrotomographyGeneral ChemistryCarbon DioxideCarbon sequestrationPermeabilitySedimentary depositional environmentBriningClayEnvironmental ChemistryAluminum SilicatesSaltsClay mineralsPorosityGroundwaterPorosityGeologyEnvironmental Science &amp; Technology
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Comparative biochemistry of CO2 fixation and the evolution of autotrophy

1999

Carbon dioxide fixation is a polyphyletic trait that has evolved in widely separated prokaryotic branches. The three principal CO2-assimilation pathways are (i) the reductive pentose-phosphate cycle, i. e. the Calvin-Benson cycle; (ii) the reductive citric acid (or Arnon) cycle; and (iii) the net synthesis of acetyl-CoA from CO/CO2, or Wood pathway. Sequence analysis and the comparative biochemistry of these routes suggest that all of them were shaped to a considerable extent by the evolutionary recruitment of enzymes. Molecular phylogenetic trees show that the Calvin-Benson cycle was a relatively late development in the (eu)bacterial branch, suggesting that some form(s) of carbon assimilat…

Carbon dioxide assimilationArnon cycleCalvin-Benson cycle; Arnon cycle; Wood pathway; Semi-enzymatic synthesis; Carbon dioxide assimilationCalvin-Benson cycle:CIENCIAS DE LA VIDA::Microbiología [UNESCO]Wood pathwaySemi-enzymatic synthesisUNESCO::CIENCIAS DE LA VIDA::Microbiología
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Response of Central European SST to atmospheric pCO2 forcing during the Oligocene – A combined proxy data and numerical climate model approach

2016

CO2-induced global warming will affect seasonal to decadal temperature patterns. Expected changes will be particularly strong in extratropical regions where temperatures will increase at faster rates than at lower latitudes. Despite that, it is still poorly constrained how precisely short-term climate dynamics will change in a generally warmer world, particularly in nearshore surface waters in the extratropics, i.e., the ecologically most productive regions of the ocean on which many human societies depend. Specifically, a detailed knowledge of the relationship between pCO2 and seasonal SST is crucial to understand interactions between the ocean and the atmosphere. In the present investigat…

Carbon dioxide in Earth's atmosphere010504 meteorology & atmospheric sciencesδ18OGlobal warmingPaleontology010502 geochemistry & geophysicsOceanography01 natural sciencesLatitudeAtmosphereSea surface temperature13. Climate actionSclerochronologyClimatologyClimate model14. Life underwaterEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Exposure to moderate concentrations of tropospheric ozone impairs tree stomatal response to carbon dioxide.

2011

With rising concentrations of both atmospheric carbon dioxide (CO(2)) and tropospheric ozone (O(3)), it is important to better understand the interacting effects of these two trace gases on plant physiology affecting land-atmosphere gas exchange. We investigated the effect of growth under elevated CO(2) and O(3), singly and in combination, on the primary short-term stomatal response to CO(2) concentration in paper birch at the Aspen FACE experiment. Leaves from trees grown in elevated CO(2) and/or O(3) exhibited weaker short-term responses of stomatal conductance to both an increase and a decrease in CO(2) concentration from current ambient level. The impairement of the stomatal CO(2) respo…

Carbon dioxide in Earth's atmosphereStomatal conductanceAir PollutantsOzoneHealth Toxicology and MutagenesisGrowing seasonPlant physiologyGeneral MedicineCarbon DioxideToxicologyPollutionTrace gasTreesPlant Leaveschemistry.chemical_compoundOzonechemistryStress PhysiologicalEnvironmental chemistryCarbon dioxideBotanyPlant StomataEnvironmental scienceTropospheric ozoneBetulaEnvironmental pollution (Barking, Essex : 1987)
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2012

Abstract. Global change forces ecosystems to adapt to elevated atmospheric concentrations of carbon dioxide (CO2). We understand that carbonyl sulfide (COS), a trace gas which is involved in building up the stratospheric sulfate aerosol layer, is taken up by vegetation with the same triad of the enzymes which are metabolizing CO2, i.e. ribulose-1,5-bisphosphate carboxylase/oxygenase (Rubisco), phosphoenolpyruvate carboxylase (PEP-Co) and carbonic anhydrase (CA). Therefore, we discuss a physiological/biochemical acclimation of these enzymes affecting the sink strength of vegetation for COS. We investigated the acclimation of two European tree species, Fagus sylvatica and Quercus ilex, grown …

Carbon dioxide in Earth's atmospherebiologyRuBisCOchemistry.chemical_elementAcclimatizationSulfurTrace gaschemistry.chemical_compoundchemistryEnvironmental chemistryCarbon dioxidebiology.proteinPhosphoenolpyruvate carboxylaseEcology Evolution Behavior and SystematicsEarth-Surface ProcessesCarbonyl sulfideBiogeosciences
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