Search results for "Mine"

showing 10 items of 20410 documents

Hydroxylamine released by nitrifying microorganisms is a precursor for HONO emission from drying soils

2018

AbstractNitrous acid (HONO) is an important precursor of the hydroxyl radical (OH), the atmosphere´s primary oxidant. An unknown strong daytime source of HONO is required to explain measurements in ambient air. Emissions from soils are one of the potential sources. Ammonia-oxidizing bacteria (AOB) have been identified as possible producers of these HONO soil emissions. However, the mechanisms for production and release of HONO in soils are not fully understood. In this study, we used a dynamic soil-chamber system to provide direct evidence that gaseous emissions from nitrifying pure cultures contain hydroxylamine (NH2OH), which is subsequently converted to HONO in a heterogeneous reaction w…

010504 meteorology & atmospheric sciencesMicroorganismScienceHeterotrophNitrous AcidHydroxylamine010501 environmental sciences01 natural sciencesArticlechemistry.chemical_compoundSoilHydroxylamineAmmoniaSoil Microbiology0105 earth and related environmental sciencesNitrous acidMultidisciplinarybiologyBacteriaAtmosphereHydroxyl RadicalQRbiology.organism_classificationArchaeaNitrificationchemistryNitrifying bacteriaEnvironmental chemistryMedicineHydroxyl radicalNitrificationGasesSoil microbiologyOxidation-ReductionScientific Reports
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Long-term stability of alpha particle damage in natural zircon

2005

Abstract We report the first discovery of radiation damage haloes generated by alpha particles in zircon. Proterozoic zircon crystals from a potassium-rich leucogranite from the Adirondack Mountains, New York State, have interior regions that are generally low in actinide elements (UO 2  + ThO 2  ≤ 0.02 wt.%) but show a remarkable pattern of heterogeneous metamictisation. The degree of radiation damage in these regions is not uniformly low, as would be expected if it corresponded to the observed actinide distribution patterns and age of the crystals. Rather, radiation damage is significantly increased in the outermost micro-areas of the low-actinide regions. The additional radiation damage …

010504 meteorology & atmospheric sciencesMineralogyGeologyAlpha particleengineering.material010502 geochemistry & geophysics01 natural sciencesCrystallographic defectMolecular physicsLeucograniteMetamictizationGeochemistry and PetrologyRadiation damageengineeringFrenkel defectBiotiteGeology0105 earth and related environmental sciencesZirconChemical Geology
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Hydrochemical mercury distribution and air-sea exchange over the submarine hydrothermal vents off-shore Panarea Island (Aeolian arc, Tyrrhenian Sea)

2017

Abstract There is a growing concern about the mercury (Hg) vented from submarine hydrothermal fluids to the marine surrounding and exchange of dissolved gaseous mercury (DGM) between the sea surface and the atmosphere. A geochemical survey of thermal waters collected from submarine vents at Panarea Island (Aeolian Islands, southern Italy) was carried out in 2015 (15–17th June and 17–18th November), in order to investigate the concentration of Hg species in hydrothermal fluids and the vertical distribution in the overlying water column close to the submarine exhalative area. Specific sampling methods were employed by Scuba divers at five submarine vents located along the main regional tecton…

010504 meteorology & atmospheric sciencesMineralogychemistry.chemical_element010501 environmental sciencesOceanographyAir-sea exchange01 natural sciencesHydrothermal circulationWater columnEnvironmental ChemistryHydrothermal fluidMercury evasion0105 earth and related environmental sciencesWater Science and TechnologySubmarineGeneral ChemistryDissolved gaseous mercuryDilutionMercury (element)Hydrothermal fluidschemistryEnvironmental chemistryAeolian processesSeawaterDissolved gaseous mercury; Mercury evasion; Air-sea exchange; Hydrothermal fluids; Panarea IslandPanarea IslandGeologyHydrothermal ventMarine Chemistry
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Sr/Ca and Mg/Ca ratios of ontogenetically old, long-lived bivalve shells (Arctica islandica) and their function as paleotemperature proxies

2011

International audience; The Sr/Ca and Mg/Ca ratios of many biogenic skeletons provide useful paleotemperature estimates. As yet however, it has remained largely impossible to obtain such information from bivalve shells. In the present study, metal-to-calcium values in the hinge plate (aragonite, outer shell layer) of four ontogenetically old (85 to 374 year-old) specimens of the long-lived bivalve, Arctica islandica, were measured on a LA-ICP-MS. The shells were collected alive in 1868, 1986 and 2003 from three different localities around Iceland. With increasing ontogenetic age and decreasing growth rate, a distinct trend toward increasing Sr/Ca (max. 5.17 mmol/mol) and Mg/Ca values (max. …

010504 meteorology & atmospheric sciencesOntogenySea surface temperatureLongevityZoologyMineralogyAmbient waterengineering.materialSignificant negative correlation010502 geochemistry & geophysicsOceanography01 natural sciencesMetal-to-calcium ratioMole14. Life underwaterGrowth rateBivalve shellArctica islandicaEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesVital effectbiologyAragonitePaleontologybiology.organism_classificationBivalve shell[SDE]Environmental Sciencesengineering
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Activity-composition relations for the calculation of partial melting equilibria in metabasic rocks

2020

A set of thermodynamic models is presented that, for the first time, allows partial melting equilibria to be calculated for metabasic rocks. The models consist of new activity–composition relations combined with end-member thermodynamic properties from the Holland & Powell dataset, version 6. They allow for forward modelling in the system Na (Formula presented.) O–CaO–K (Formula presented.) O–FeO–MgO–Al (Formula presented.) O (Formula presented.) –SiO (Formula presented.) –H (Formula presented.) O–TiO (Formula presented.) –Fe (Formula presented.) O (Formula presented.). In particular, new activity–composition relations are presented for silicate melt of broadly trondhjemitic–tonalitic compo…

010504 meteorology & atmospheric sciencesPartial meltingMineralogyThermodynamicsGeologyComposition (combinatorics)010502 geochemistry & geophysics01 natural sciencesSilicatechemistry.chemical_compoundchemistryGeochemistry and PetrologyTetrahedronGeologyMixing (physics)0105 earth and related environmental sciencesSolid solutionJournal of Metamorphic Geology
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Acoustic properties of ancient shallow-marine carbonates: effects of depositional environments and diagenetic processes (Middle Jurassic, Paris Basin…

2010

17 pages; International audience; Examination of petrophysical properties (acoustic velocity, porosity, permeability, and density) and petrographical characteristics (texture, facies composition, and diagenesis) of more than 250 core plugs from the Middle Jurassic carbonates of the eastern Paris Basin provides insights into the parameters controlling acoustic velocities in relatively low-porosity carbonate rocks ({Phi} < 20%). The pore-type observations reveal distinct acoustic velocities in samples with intergranular macropores and samples with micropores in subhedral micrite, such that velocities in microporous mudstone–wackestone (lagoonal) deposits are greater than in macroporous grains…

010504 meteorology & atmospheric sciencesPetrophysicsCompaction[SDU.STU.PE]Sciences of the Universe [physics]/Earth Sciences/PetrographyMineralogyGeology010502 geochemistry & geophysicsCementation (geology)[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesDiagenesisGrainstone[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyFaciesMarlCarbonate rockGeology0105 earth and related environmental sciences[ SDU.STU.PE ] Sciences of the Universe [physics]/Earth Sciences/Petrography
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Secondary minerals from salt caves in the Atacama Desert (Chile): a hyperarid and hypersaline environment with potential analogies to the Martian sub…

2017

Over the past 15 years several expeditions by French, American and especially Italian cavers have unveiled over 50 caves in the Cordillera de la Sal (Atacama Desert, Northern Chile). Many of these caves contain a variety of speleothems and minerals, some of which have rarely been observed within karst systems. Most of the secondary deposits in these caves are composed of halite, but also other halide, carbonate, sulphate, nitrate, phosphate, and silicate minerals have been found. Among the sixteen cave mineral species recognized, atacamite, darapskite, blödite, leonite, anhydrite, and especially antarcticite are worth mentioning. In one of the samples an unknown Ca-Sr-bearing chloride miner…

010504 meteorology & atmospheric sciencesQH301-705.5Settore GEO/04 - Geografia Fisica E GeomorfologiaEarth scienceSalt (chemistry)martian010502 geochemistry & geophysics01 natural sciencesAstrobiologyatacamaCaveminerogenesisMinerogenesiBiology (General)Hyperaridity0105 earth and related environmental sciencesEarth-Surface Processescave mineralschemistry.chemical_classificationMartianQE1-996.5Settore GEO/06 - Mineralogiageographygeography.geographical_feature_categoryDesert (philosophy)Mars analoguesMars analogueCave mineralGeologysalt cavescave minerals atacama martianchemistrySalt cavecave minerals salt caves hyperaridity minerogenesis Mars analoguesGeologyInternational Journal of Speleology
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Reactive oxygen species formed in aqueous mixtures of secondary organic aerosols and mineral dust influencing cloud chemistry and public health in th…

2017

Mineral dust and secondary organic aerosols (SOA) account for a major fraction of atmospheric particulate matter, affecting climate, air quality and public health. How mineral dust interacts with SOA to influence cloud chemistry and public health, however, is not well understood. Here, we investigated the formation of reactive oxygen species (ROS), which are key species of atmospheric and physiological chemistry, in aqueous mixtures of SOA and mineral dust by applying electron paramagnetic resonance (EPR) spectrometry in combination with a spin-trapping technique, liquid chromatography-tandem mass spectrometry (LC-MS/MS), and a kinetic model. We found that substantial amounts of ROS includi…

010504 meteorology & atmospheric sciencesRadicalInorganic chemistry010501 environmental sciencesMineral dustbehavioral disciplines and activities01 natural scienceschemistry.chemical_compoundKaolinitePhysical and Theoretical ChemistryIsoprene0105 earth and related environmental sciencesAerosolsAir PollutantsMineralsAqueous solutionAtmosphereWaterParticulatesDecompositionDeposition (aerosol physics)chemistryEnvironmental chemistryParticulate MatterPublic HealthReactive Oxygen SpeciesFaraday Discussions
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Validation of a novel Multi-Gas sensor for volcanic HCl alongside H2S and SO2 at Mt. Etna

2017

Erratum to: Bull Volcanol (2017) 79: 36DOI 10.1007/s00445-017-1114-zDuring the steps of corrections, the publisher inadvertently changed the author affiliations so that they were no longer correct. The correct information is given below. The publisher regrets this mistake.; International audience; Volcanic gas emission measurements inform predictions of hazard and atmospheric impacts. For these measurements, Multi-Gas sensors provide low-cost in situ monitoring of gas composition but to date have lacked the ability to detect halogens. Here, two Multi-Gas instruments characterized passive outgassing emissions from Mt. Etna’s (Italy) three summit craters, Voragine (VOR), North-east Crater (NE…

010504 meteorology & atmospheric sciencesResponse modelPoison controlMineralogyOpen-system volcanic degassing010502 geochemistry & geophysics01 natural sciencesElectronic noseImpact craterGeochemistry and PetrologyCalibrationGas compositionVolcanic outgassing0105 earth and related environmental sciencesMulti-Gas instrumentgeographygeography.geographical_feature_categoryE-noseOutgassingVolcano13. Climate action[SDU]Sciences of the Universe [physics]HalogenMagmaChlorineGeology
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Phlogopite-pargasite coexistence in an oxygen reduced spinel-peridotite ambient

2021

AbstractThe occurrence of phlogopite and amphibole in mantle ultramafic rocks is widely accepted as the modal effect of metasomatism in the upper mantle. However, their simultaneous formation during metasomatic events and the related sub-solidus equilibrium with the peridotite has not been extensively studied. In this work, we discuss the geochemical conditions at which the pargasite-phlogopite assemblage becomes stable, through the investigation of two mantle xenoliths from Mount Leura (Victoria State, Australia) that bear phlogopite and the phlogopite + amphibole (pargasite) pair disseminated in a harzburgite matrix. Combining a mineralogical study and thermodynamic modelling, we predict …

010504 meteorology & atmospheric sciencesSciencephlogopiteGeochemistryengineering.materialamphibole010502 geochemistry & geophysics01 natural sciencesArticleMantle (geology)NOupper mantleMineral redox bufferUltramafic rockgeothermMetasomatismGeneralAmphibolePetrology0105 earth and related environmental sciencesPeridotitemodelMultidisciplinarymetasomatismphlogopite-pargasiteChemistrygeotherm; model; mantle xenoliths;PargasiteQRMineralogymantle xenolithsGeochemistryphlogopite; amphibole; metasomatism; upper mantleengineeringPhlogopiteMedicinemantle xenolithScientific Reports
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