Search results for " petrology"

showing 10 items of 1353 documents

Uranyl sorption onto birnessite: A surface complexation modeling and EXAFS study

2014

This work investigates the mechanism of the uranyl interaction with birnessite, one of the most common layer-type MnO2 mineral at the Earth's surface, by coupling macroscopic (surface complexation experiments) and microscopic (EXAFS measurements) approaches. The sorption of uranyl on synthetic hexagonal birnessite, the low-pH birnessite form, was studied under various conditions of pH (3–6), electrolyte backgrounds (0.1 M NaClO4, NaNO3 and Na2CO3), and solid/liquid ratios (from 0.27 to 4.5 g/L). Sorption isotherms exhibit a complex form indicative of at least two types of sorption sites. EXAFS data reveal the presence of two equatorial O shells at ca. 2.32 Å and 2.46 Å for all the samples, …

birnessiteUBirnessiteDenticityExtended X-ray absorption fine structureInorganic chemistryGeologySorptionElectrolyteUranylEXAFSchemistry.chemical_compoundMontmorilloniteOctahedronchemistryGeochemistry and Petrology[PHYS.PHYS.PHYS-CHEM-PH]Physics [physics]/Physics [physics]/Chemical Physics [physics.chem-ph][CHIM.RADIO]Chemical Sciences/Radiochemistry
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Magma and volatile supply to post-collapse volcanism and block resurgence in Siwi caldera (Tanna Island, Vanuatu arc)

2011

Siwi caldera, in the Vanuatu arc (Tanna island), is a rare volcanic complex where both persistent eruptive activity (Yasur volcano) and rapid block resurgence (Yenkahe horst) can be investigated simultaneously during a post-caldera stage. Here we provide new constraints on the feeding system of this volcanic complex, based on a detailed study of the petrology, geochemistry and volatile content of Yasur-Siwi bulk-rocks and melt inclusions, combined with measurements of the chemical composition and mass fluxes of Yasur volcanic gases. Major and trace element analyses of Yasur-Siwi volcanic rocks, together with literature data for other volcanic centers, point to a single magmatic series and p…

blockEarth scienceAndesiteYasur magmatic degassingvolcano thermal budgetVanuatu arcGeochemistryPyroclastic rockVolcanologyVolcanismmelt inclusionsBlock (meteorology)volatilesGeophysicsGeochemistry and PetrologyresurgentMagma[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyCalderagas fluxes[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentYasurGeologyMelt inclusions
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Uptake of actinides by calcium silicate hydrate (C-S-H) phases

2018

Abstract The sorption of actinides (Th, U – Am) was studied in dependence of the solid-to-liquid (S/L) ratio (0.5–20.0 g/L) and the calcium-to-silicon (C:S) ratio. The C:S ratio was varied between 1.80 and 0.70 to simulate the changing composition of the C-S-H phases during cement degradation from high to low C:S ratios. The decrease of the calcium content in the C-S-H phases by time is accompanied by a decrease in pH in the corresponding suspensions from 12.6 to 10.2. X-ray photoelectron spectroscopy (XPS) of the C-S-H phases showed an increasing depletion of Ca on the surface with increasing C:S ratio in comparison to the composition of the solid phase as a whole. The sorption experiments…

cementTechnology02 engineering and technology010501 environmental sciences01 natural sciencesRedoxAmchemistry.chemical_compoundX-ray photoelectron spectroscopyGeochemistry and PetrologyOxidation statePhase (matter)Environmental ChemistryThCalcium silicate hydrateSpectroscopy0105 earth and related environmental sciencesUactinideshigh-energy resolution X-ray absorption near-edge structure (HR-XANES)SorptionX-ray photoelectron spectroscopy (XPS)Pu021001 nanoscience & nanotechnologyPollutionNpC-S-Hchemistryradioactive wasteSorptionAbsorption (chemistry)0210 nano-technologyddc:600Nuclear chemistry
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Comparative high-resolution chemostratigraphy of the Bonarelli Level from the reference Bottaccione section (Umbria-Marche Apennines) and from an equ…

2006

The Bonarelli Level (BL) from the upper Cenomanian portion of the reference Bottaccione section (central Italy) is characterized by the presence of black shales containing high TOC concentrations (up to 17%) and amounts of CaCO3 near to zero. In the absence of carbonate and, consequently, of relative carbon- and oxygen-isotopic data, the elemental geochemistry revealed to be a very useful tool to obtain information about the palaeoclimatic and palaeoceanographic evolution of the Tethys Ocean during the OAE2. Based on several geochemical proxies (Rb, V, Ni, Cr, Si, Ba), the BL is interpreted as a high-productivity event driven by increasingly warm and humid climatic conditions promoting an a…

chemistry.chemical_classification010506 paleontologyCretaceous Umbria–Marche Apennines Sicily Corg-rich deposits Bonarelli Level Geochemical proxies PalaeoceanographyGeology15. Life on land010502 geochemistry & geophysicsTethys Ocean01 natural sciencesCretaceousSeafloor spreadingDeposition (geology)chemistry.chemical_compoundPaleontologychemistry13. Climate actionGeochemistry and PetrologyChemostratigraphy[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyCarbonateOrganic matterCenomanianGeology0105 earth and related environmental sciences
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Palladium(II) sequestration by phytate in aqueous solution. Speciation analysis and ionic medium effects.

2010

Environmental context.In the last 20 years, the demand for palladium and other platinum-group elements has intensified, causing a significant increase in their concentration in the environment, with particular accumulation in urban areas. Knowledge about Pd2+ speciation in aqueous media is fundamental for the understanding of its biological and environmental activity in contaminated areas. Phytic acid appears to be a good sequestering agent towards Pd2+ under various conditions, indicating its potential use in the remediation of contaminated sites. Abstract. Palladium(II) speciation in the presence of phytate (Phy12–) was studied by H+ ion selective electrode (ISE) potentiometry at 25°C in…

chemistry.chemical_classificationAqueous solutionMetal ions in aqueous solutionInorganic chemistryFluorescence spectrometrychemistry.chemical_elementcomplexes stability constantsPhytateIon selective electrodeDivalentMetalchemistryComplexesGeochemistry and PetrologyChemistry (miscellaneous)Ionic strengthvisual_artvisual_art.visual_art_mediumEnvironmental ChemistrySettore CHIM/01 - Chimica AnaliticaStability constantsComplexes; Stability constants; Phytate; PalladiumPalladiumPalladium
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Development of a Matrix-Matched Sphalerite Reference Material (MUL-ZnS-1) for Calibration of In Situ Trace Element Measurements by Laser Ablation-Ind…

2016

Sphalerite (ZnS) is an abundant ore mineral and an important carrier of elements such as Ge, Ga and In used in high-technology applications. In situ measurements of trace elements in natural sphalerite samples using LA-ICP-MS are hampered by a lack of homogenous matrix-matched sulfide reference materials available for calibration. The preparation of the MUL-ZnS1 calibration material containing the trace elements V, Cr, Mn, Co, Ni, Cu, Ga, Ge, As, Se, Mo, Ag, Cd, In, Sn, Sb, Tl and Pb besides Zn, Fe and S is reported. Commercially available ZnS, FeS, CdS products were used as the major components, whereas the trace elements were added by doping with single-element ICP-MS standard solutions a…

chemistry.chemical_classificationArgonLaser ablationMaterials scienceSulfide010401 analytical chemistryAnalytical chemistryTrace elementchemistry.chemical_elementGeologyElectron microprobeengineering.material010502 geochemistry & geophysics01 natural sciences0104 chemical sciencesSphaleritechemistryGeochemistry and PetrologyengineeringInductively coupled plasma mass spectrometryPowder mixture0105 earth and related environmental sciencesGeostandards and Geoanalytical Research
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Composition, crystallization conditions and genesis of sulfide-saturated parental melts of olivine-phyric rocks from Kamchatsky Mys (Kamchatka, Russi…

2020

Highlights • Parental melts of sulfide-bearing KM rocks have near primary MORB-like composition. • Crystallization of these S-saturated melts occurred in near-surface conditions. • Extensive fractionation and crustal assimilation are not the causes of S-saturation. • S content in melts can be restored by accounting for daughter sulfide globules. Abstract Sulfide liquids that immiscibly separate from silicate melts in different magmatic processes accumulate chalcophile metals and may represent important sources of the metals in Earth's crust for the formation of ore deposits. Sulfide phases commonly found in some primitive mid-ocean ridge basalts (MORB) may support the occurrence of sulfide …

chemistry.chemical_classificationBasaltOlivine010504 meteorology & atmospheric sciencesSulfideGeochemistrychemistry.chemical_elementGeologyengineering.material010502 geochemistry & geophysics01 natural sciencesSulfurSilicateMantle (geology)chemistry.chemical_compoundchemistry13. Climate actionGeochemistry and PetrologyengineeringPhenocrystGeology0105 earth and related environmental sciencesMelt inclusionsLithos
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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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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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