Search results for "H2S"

showing 10 items of 12 documents

Thermomineral waters of Greece: geochemical characterization

2020

75 °C). In terms of pH most results vary from 5.5 to 823 °C) ii) warm (23 40 °C) iii) thermal (40 75 °C) and iv) hyperthermal (&gtfew springs show either very low pH (&lt10) proposing serpentinization processes. Regarding TDS concentrations collected waters can be subdivided into low salinity (up to 1.5 g/L) brackish (up to 20 g/L) and saline (up to 43 g/L). The medium high salinities can be justified by mixing with sea water and/or strong waterrock interaction processes. Isotope composition of O and H ranges from 12.7 to +2.7 ‰ SMOW and from 91 to +12 ‰ SMOW respectively and is generally comprised between the Global Meteoric Water Line and the East Mediterranean Meteoric Water Line. Only few water samples show a positive shift for δ18O possibly related to high temperature waterrock interaction processes. Carbon dioxide (18 997000 μmol/mol) or N2 (1100 989000 μmol/mol) or CH4 (&ltMany geothermal areas of Greece are located in regions affected by Miocene or Quaternary volcanism and in continental basins characterised by elevated heat flow. Moreover the majority of them is found along the coast as well as in islands of the Aegean Sea and thus thermal water is often brackish to saline due to marine intrusion into costal aquifer. In the present study almost 300 thermal and cold mineral water samples were collected along the Hellenic territory with their physicochemical parameters (temperature pH electrical conductivity and Eh) and the amount of bicarbonates (titration with 0.1N HCl) being determined in situ. Additionally gases found either in free or dissolved phase were sampled. Both water and gas samples were analysed at the INGVPa laboratories for major ions (Ion Chromatography) silica (Inductively Coupled Plasma Optical Emission Spectrometry) chemical composition of free and dissolved gases (Gas Chromatography) water isotopes (O and H) and carbon and helium isotopes of free and dissolved gases (Mass Spectrometry). The temperature of the investigated waters ranges from 6.5 to 98°C pH from 1.96 to 11.98 whilst Total Dissolved Solids (TDS) from 0.06 to 43 g/L. Based on the temperature parameter waters can be divided into four groups: i) cold (&lt0.5 913000 μmol/mol) are the prevailing gas species found in the studied sites. The δ13CCO2 values ranged from 20.1 to +8.5 ‰ whilst the isotope ratio of He from 0.21 to 6.71 R/RA.4) suggesting interaction with H2Srich gases or very high pH values (&gtSettore GEO/08 - Geochimica E Vulcanologia
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ZrO2 Acting as a Redox Catalyst

2016

Surface defects are discussed and reviewed with regards to the use of ZrO2 in applications involving interactions with CO, H2, CH4, CO2, water and hydrocarbons. Studies of catalytic partial oxidation of methane reveal that part of the surface lattice oxygen in terraces can be removed by methane at high temperatures (e.g. 900 °C). The reaction proceeds via a surface confined redox mechanism. The studies presented here also highlight that defects play a decisive role in the water–gas-shift reaction, since the reaction is likely carried out via OH groups present at defect sites, which are regenerated by dissociating water. Hydroxyl chemistry on ZrO2 is briefly reviewed related to the studies p…

Chemistry(all)Tar oxidationInorganic chemistryHydroxyl groups02 engineering and technology010402 general chemistry01 natural sciencesRedoxCatalysisMethaneDissociation (chemistry)CatalysisRedoxHSchemistry.chemical_compoundAdsorptionZrO2Partial oxidationbiologyH2SCPOMActive siteGeneral ChemistryZrO021001 nanoscience & nanotechnology0104 chemical scienceschemistrybiology.proteinDensity functional theory0210 nano-technologyWGSTopics in Catalysis
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Direct Methane Oxidation on La1-xSrxCr1-yFeyO3-δ perovskite-type oxides as Potential Anode for Intermediate Temperature Solid Oxide Fuel Cells

2016

Abstract La1−xSrxCr1−yFeyO3−δ (x = 0, 0.1, 0.15, 0.2; y = 0, 0.3, 0.5) perovskite-type oxide powders were synthesized by solution combustion synthesis and characterized by X-ray diffraction, X-ray photoelectron spectroscopy and H2-temperature programmed reduction. Selected compositions were studied by CH4-temperature programmed reduction in the absence and in the presence of H2S. Temperature programmed oxidation and structural characterizations were performed in order to discriminate the nature of residual deposits on the catalyst surface. The study about reduction in different methane-based mixture revealed that total and partial methane oxidation occurred in the range ∼450–1000 °C indepen…

Doped-LaCrO3; IT-SOFC; Direct methane oxidation; H2SInorganic chemistryOxide02 engineering and technology010402 general chemistry01 natural sciencesCatalysisMethaneCatalysischemistry.chemical_compoundX-ray photoelectron spectroscopyGeneral Environmental SciencePerovskite (structure)Range (particle radiation)IT-SOFCChemistryH2SProcess Chemistry and Technologydirect methane oxidation021001 nanoscience & nanotechnologydoped-LaCrO30104 chemical sciencesAnodedoped-LaCrO3; IT-SOFC; direct methane oxidation; H2SSettore CHIM/03 - Chimica Generale E InorganicaAnaerobic oxidation of methane0210 nano-technology
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A new fluorescent "turn-on" chemodosimeter for the detection of hydrogen sulfide in water and living cells

2013

[EN] A new fluorescent turn-on probe for the selective detection of hydrogen sulfide in water and living cells based on a 8-hydroxyquinoline fluorophore functionalized with a 2,6-dinitrophenyl ether moiety has been developed.

FluorophoreReagentsChemosensorsH2SGeneral Chemical EngineeringHydrogen sulfideQUIMICA INORGANICAAnionThiolysisEtherGeneral ChemistryPhotochemistryProbeFluorescenceTurn (biochemistry)chemistry.chemical_compoundQUIMICA ORGANICAThiolysischemistryReagentMoiety
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Kompleksy manganu(III) z czterodonorowymi zasadami Schiffa

2008

H2salenmangan(III)absorpcyjna spektroskopia elektronowaiminy
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A new geochemical approach to estimate the distribution of air pollutants from natural and anthropogenic sources: examples from Solfatara Crater (Cam…

2015

Volcanic and geothermal systems significantly contribute to the input of volatile contaminants, such as mercury and hydrogen sulfide, into the atmosphere. Mercury has a strong environmental impact. In the atmosphere the prevalent elemental form is Hg0 (~98 %), whose main physical-chemical features are: high volatility, low solubility and chemical inertness. Hydrogen sulfide (H2S), one of the most abundant gas compounds in volcanic fluids, is highly poisoning and corrosive and unpleasantly smells of rotten eggs. Measurements of Hg0 and H2S concentrations in air are commonly performed by means of passive samplers. However, real-time measurements, coupled with monitoring of local atmospheric c…

Hg H2S pollution Solfatara Campi Flegrei Mt. Amiata
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Sulfuric Acid Caves of Italy: An Overview

2016

ItalyH2SSettore GEO/04 - Geografia Fisica E GeomorfologiaSAS caveGypsum
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Sulfidation Mechanism of Pure and Cu-Doped ZnO Nanoparticles at Moderate Temperature: TEM and In Situ XRD Studies

2012

International audience; Sulfidation mechanism of pure and Cu-doped ZnO nanoparticles (Cu0.03Zn0.97O and Cu0.06Zn0.94O) at 250 and 350 degrees C was studied by transmission electron microscopy (TEM) and in situ synchrotron XRD. For nondoped ZnO, we observed by TEM that partial reaction with H2S is accompanied by the formation of voids at the ZnO/ZnS interface. This phenomenon (known as the Kirkendall effect) confirms that sulfidation of nanosized ZnO by gaseous H2S proceeds via the outward growth of ZnS: Zn2+ and O2- are transferred to the external (ZnS/gas) surface, where zinc is combined with sulfur and oxygen reacts with protons yielding H2O. During sulfidation of Cu-doped ZnO, the caviti…

Materials scienceKirkendall effectHydrogen sulfideSulfidationNANOTUBESchemistry.chemical_element02 engineering and technologyZincHYDROGEN-SULFIDE010402 general chemistry01 natural sciencesOxygenchemistry.chemical_compoundSORBENTSPhysical and Theoretical ChemistryZINC-OXIDEKINETICSDESULFURIZATIONMetallurgy021001 nanoscience & nanotechnologySulfurREACTIVITY0104 chemical sciencesSurfaces Coatings and FilmsElectronic Optical and Magnetic MaterialsFlue-gas desulfurizationGeneral EnergychemistryChemical engineeringTransmission electron microscopyH2S REMOVAL0210 nano-technologyGAS STREAMS
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Hydrogen sulfide measurements in air by passive/diffusive samplers and high-frequency analyzer: A critical comparison

2016

In this study, hydrogen sulfide (H2S) measurements in air carried out using (a) passive/diffusive samplers (Radiello® traps) and (b) a high-frequency (60 s) real-time analyzer (Thermo® 450i) were compared in order to evaluate advantages and limitations of the two techniques. Four different sites in urban environments (Florence, Italy) and two volcanic areas characterized by intense degassing of H2S-rich fluids (Campi Flegrei and Vulcano Island, Italy) were selected for such measurements. The concentrations of H2S generally varied over 5 orders of magnitude (from 101e103 mg/m3), the H2S values measured with the Radiello® traps (H2SR) being significantly higher than the average values measure…

PollutionSpectrum analyzerAir quality monitoring010504 meteorology & atmospheric sciencesOrders of magnitude (temperature)media_common.quotation_subjectHydrogen sulfideActive analyzersAnalytical chemistryPassive/diffusive samplers010501 environmental sciencesHydrogen sulphide01 natural sciencesAir quality monitoringchemistry.chemical_compoundGeochemistry and PetrologyEnvironmental Chemistry0105 earth and related environmental sciencesmedia_commongeographygeography.geographical_feature_categoryHydrogen sulfideGaseous contaminantsPollutionPassive/diffusive samplerchemistryVolcanoEnvironmental chemistryGaseous contaminantH2S in airActive analyzerApplied Geochemistry
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Oб определении внутримолекулярной потенциальной функции многоатомной молекулы H2S

2008

In modern molecular physics, there are two basic methods of determining the intramolecular potential function of polyatomic molecules. The first method is ab initio calculations and the second is the so-called semi-empirical method in which the Hamiltonian parameters are varied by direct construction of the Hamiltonian matrix. In the present work, the second approach is discussed on the example of the XY2 three-atomic molecule of the C2v symmetry. On the one hand, it is extremely simple for implementation, and on the other hand, it considerably extends the capability of application of the traditional semi-empirical methods. The approach suggested involves two aspects that make it advantageo…

XY2 three-atomic molecule of C2v symmetry -H2S[PHYS.QPHY]Physics [physics]/Quantum Physics [quant-ph][ PHYS.QPHY ] Physics [physics]/Quantum Physics [quant-ph]Intramolecular potential function[PHYS.QPHY] Physics [physics]/Quantum Physics [quant-ph]
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