Search results for "calcite"

showing 10 items of 191 documents

Substrate templating guides the photoinduced reaction of C60on calcite

2014

cited By 7; International audience; A substrate-guided photochemical reaction of C60 fullerenes on calcite, a bulk insulator, investigated by non-contact atomic force microscopy is presented. The success of the covalent linkage is evident from a shortening of the intermolecular distances, which is clearly expressed by the disappearance of the moiré pattern. Furthermore, UV/Vis spectroscopy and mass spectrometry measurements carried out on thick films demonstrate the ability of our setup for initiating the photoinduced reaction. The irradiation of C60 results in well-oriented covalently linked domains. The orientation of these domains is dictated by the lattice dimensions of the underlying c…

Fullerenescanning probe microscopysurface chemistry02 engineering and technologyMicroscopy Atomic Force010402 general chemistry01 natural sciencesChemical reaction530CatalysisCalcium CarbonateScanning probe microscopychemistry.chemical_compoundSpectroscopyCalcite[PHYS]Physics [physics]Spectrum AnalysisIntermolecular forcefullerenesGeneral Chemistrycovalent networksself-assemblyPhotochemical Processes021001 nanoscience & nanotechnology0104 chemical sciencesCrystallographychemistryChemical physicsCovalent bondSelf-assembly0210 nano-technology
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Authigenic phase formation and microbial activity control Zr, Hf, and rare earth element distributions in deep-sea brine sediments

2014

Abstract. Sediments collected from hypersaline and anoxic deep-sea basins in the eastern Mediterranean (Thetis, Kryos, Medee, and Tyro) were characterised in terms of their mineralogical composition, the distributions of rare earth elements (REE), Zr, and Hf and their content of microbial DNA. We identified two major mineralogical fractions: one fraction of detritic origin was composed of quartz, gypsum, and low-Mg calcite bioclasts (with 0 < Mg < 0.07%) and another fraction of authigenic origin constituted of halite, dolomite, high-Mg calcite (with a Mg content of up to 22%) and rare bischofite and showed a textural evidence of microbial assemblages. We found that in the Medee and Ty…

Gypsum010504 meteorology & atmospheric sciencesSettore AGR/13 - Chimica AgrariaGeochemistrylcsh:LifeMineralogy[SDU.STU]Sciences of the Universe [physics]/Earth Sciencesengineering.material010502 geochemistry & geophysics01 natural sciencesDeep seachemistry.chemical_compoundlcsh:QH540-549.5Settore CHIM/01 - Chimica AnaliticaQuartzEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesgeochemistryCalciteRare-earth elementlcsh:QE1-996.5AuthigenicAnoxic watersSettore GEO/08 - Geochimica E Vulcanologialcsh:Geologylcsh:QH501-531chemistryengineeringCarbonatelcsh:EcologyGeology
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Laminated carbonate deposits in Roman aqueducts: Origin, processes and implications

2013

Carbonate deposits in Roman aqueducts of Patara and Aspendos (southern Turkey) were studied to analyse the nature of their regular layering. Optical microscopy and electron-backscattered diffraction results show an alternation of dense, coarsely crystalline, translucent laminae composed of bundles and fans of elongate calcite crystals with their c-axes parallel to the long axis, and porous, fine-grained laminae with crystals at near-random orientation. The ?18O and ?13C data show a strong cyclicity and anti-correlation, whereby high and low ?18O values correspond to dense columnar and porous fine-grained laminae, respectively. Geochemical analyses show similar cyclic changes in carbonate co…

Hydraulic structurescrystal structureTurkeyaqueductcarbon isotopeδ18OStratigraphyRoman aqueductMineralogyisotopic compositionsediment chemistryAqueductMuglaOptical microscopyBioactivityIsotopes of oxygenClimate modelschemistry.chemical_compoundCalcareous sinterIsotopesSinteringstable isotopeMagnesiumoxygen isotopeLaminatingCarbonate depositsAnalytical geochemistryPataraCalcareous sinterLayeringStable isotopesCalciteClimatologyTrace elementsMass spectrometryCalciteWatertrace elementGeologyLamination (geology)Electromagnetic inductionchemistryTufaCarbonateCarbonationcarbonate sedimentDepositsGeologyCrystal orientation
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A geochemical survey of the telese hypothermal spring, southern Italy: Sulfate anomalies induced by crustal deformation

2002

This study deals with a chemical survey (major ions and Li+, F–, Br–, and ) on water samples collected from April 1998 to April 1999, from the Telese thermal spring, southern Italy, in order to investigate possible variations in the chemical composition of the spring. Water samples are of the calcium bicarbonate type, with small fluctuations in outlet temperature (20.05 ± 0.23°C), pH (6.23 ± 0.16), and TDS (2415 ± 35 mg/l). The concentrations of major ions stayed nearly constant, except for . All analyzed waters are saturated or oversaturated relative to calcite and dolomite. The higher saturation indices of the water samples relative to calcite and dolomite observed during the summer of 19…

HydrologyCalcitegeographygeography.geographical_feature_categoryDolomiteGeochemistryAquiferchemistry.chemical_compoundchemistryCalcium bicarbonateSpring (hydrology)General Earth and Planetary SciencesSulfateSaturation (chemistry)Chemical compositionGeologyGeneral Environmental Science
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Modelling fractionation of stable isotopes in stalagmites

2009

Abstract High resolution δ13C and δ18O profiles recorded in precisely dated speleothems are widely used proxies for the climate of the past. Both δ13C and δ18O depend on several climate related effects including meteorological processes, processes occurring in the soil zone above the cave and isotope fractionation processes occurring in the solution layer on the stalagmite surface. Here we model the latter using a stalagmite isotope and growth model and determine the relationship between the stable isotope values in speleothem calcite and cave parameters, such as temperature, drip interval, water p CO 2 and a mixing coefficient describing mixing processes between the solution layer and the …

HydrologyCalcitegeographygeography.geographical_feature_categoryIsotopeStable isotope ratioδ18OSpeleothemMineralogyStalagmiteFractionationchemistry.chemical_compoundIsotope fractionationchemistryGeochemistry and PetrologyGeologyGeochimica et Cosmochimica Acta
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Modelling the cement-latex interactions : experimental and simulation approach : Consequences on the rheological propertiec

2014

Latex is used in industrial mortars to improve the material properties. This behaviour is obviously related to the interactions between cement phases and latex which are still not understood. In this frame, the aim of the present work is to understand the role of latexes in mortar in particular how the various latex characteristics, such as the latex chemistry surface, or the latex size, influence the characteristics of this complex granular system. The major issue concerns the reactivity of the cement: indeed, several parameters are modified during cement hydration which governs the development of the paste mechanical properties. Consequently in order to avoid side effects due to cement hy…

LatexSimulation numériqueCalciteNumerical simulationsAdsorptionRheologyRhéologieC-S-H[PHYS.PHYS.PHYS-CHEM-PH] Physics [physics]/Physics [physics]/Chemical Physics [physics.chem-ph]
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Protein-induced, previously unidentified twin form of calcite.

2007

Using single-crystal x-ray diffraction, we found a formerly unknown twin form in calcite crystals grown from solution to which a mollusc shell-derived 17-kDa protein, Caspartin, was added. This intracrystalline protein was extracted from the calcitic prisms of the Pinna nobilis shells. The observed twin form is characterized by the twinning plane of the (108)-type, which is in addition to the known four twin laws of calcite identified during 150 years of investigations. The established twin forms in calcite have twinning planes of the (001)-, (012)-, (104)-, and (018)-types. Our discovery provides additional evidence on the crucial role of biological macromolecules in biomineralization.

MESH : Calcium Carbonatetwinning02 engineering and technology010402 general chemistry01 natural sciencesMESH : Proteinschemistry.chemical_compoundMESH: Proteinscalcium carbonate[SDV.IB.BIO]Life Sciences [q-bio]/Bioengineering/BiomaterialsCalciteMultidisciplinarybiologycrystal growthProteins021001 nanoscience & nanotechnologybiology.organism_classificationbiomineralization[ SDV.IB.BIO ] Life Sciences [q-bio]/Bioengineering/Biomaterials0104 chemical sciencesCrystallographyCalcium carbonateMESH: Calcium Carbonatechemistryx-ray diffractionPhysical Sciences0210 nano-technologyCrystal twinningPinna nobilisBiomineralization
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Caspartin and calprismin, two proteins of the shell calcitic prisms of the Mediterranean fan mussel Pinna nobilis.

2005

We used the combination of preparative electrophoresis and immunological detection to isolate two new proteins from the shell calcitic prisms of Pinna nobilis, the Mediterranean fan mussel. The amino acid composition of these proteins was determined. Both proteins are soluble, intracrystalline, and acidic. The 38-kDa protein is glycosylated; the 17-kDa one is not. Ala, Asx, Thr, and Pro represent the dominant residues of the 38-kDa protein, named calprismin. An N-terminal sequence was obtained from calprismin. This sequence, which comprises a pattern of 4 cysteine residues, is not related to any known protein. The second protein, named caspartin, exhibits an unusual amino acid composition, …

MESH : Molecular Sequence DataMESH : Calcium CarbonateMESH: BivalviaMESH: ElectrophoresisMESH: Amino Acid Sequence01 natural sciencesBiochemistrychemistry.chemical_compoundMESH : BivalviaMESH: AnimalsMESH: CrystallizationCalciteImmunoassay0303 health sciencesbiologyMESH : Amino Acid SequenceImmunogold labellingMESH : ImmunoassayBiochemistryMESH: Calcium CarbonateMESH : CrystallizationCrystallizationMESH: ImmunoassayElectrophoresisAmino Acid Sequence;Animals;Bivalvia;Calcium Carbonate;Crystallization;Electrophoresis;Glycoproteins;Immunoassay;Molecular Sequence DataMolecular Sequence DataMESH: Glycoproteins010402 general chemistryCalcium CarbonateBiomaterials03 medical and health sciencesAnimalsAmino Acid Sequence[SDV.IB.BIO]Life Sciences [q-bio]/Bioengineering/BiomaterialsMolecular Biology030304 developmental biologyGlycoproteinsAntiserumMESH: Molecular Sequence DataMESH : ElectrophoresisCell BiologyMussel[ SDV.IB.BIO ] Life Sciences [q-bio]/Bioengineering/Biomaterialsbiology.organism_classificationMESH : Glycoproteins0104 chemical sciencesBivalvia[SDV.IB.BIO] Life Sciences [q-bio]/Bioengineering/BiomaterialsCalcium carbonatechemistryPolyclonal antibodiesbiology.proteinBiomatériauxMESH : AnimalsPinna nobilisCysteine
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Resolving Point Defects in the Hydration Structure of Calcite (10.4) with Three-Dimensional Atomic Force Microscopy

2018

It seems natural to assume that defects at mineral surfaces critically influence interfacial processes such as the dissolution and growth of minerals in water. The experimental verification of this claim, however, is challenging and requires real-space methods with utmost spatial resolution, such as atomic force microscopy (AFM). While defects at mineral-water interfaces have been resolved in 2D AFM images before, the perturbation of the surrounding hydration structure has not yet been analyzed experimentally. In this Letter, we demonstrate that point defects on the most stable and naturally abundant calcite (10.4) surface can be resolved using high-resolution 3D AFM-even within the fifth h…

Materials scienceField (physics)General Physics and Astronomy02 engineering and technology53001 natural sciences114 Physical sciencesDEFLECTION SENSORMolecular dynamicschemistry.chemical_compoundDISSOLUTION0103 physical sciencesWATERFIELD010306 general physicsImage resolutionDissolutionCalciteMineralResolution (electron density)021001 nanoscience & nanotechnologyCrystallographic defectSIMULATIONSchemistryRESOLUTIONChemical physicsMOLECULAR-DYNAMICS0210 nano-technology
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Biocalcite, a multifunctional inorganic polymer: Building block for calcareous sponge spicules and bioseed for the synthesis of calcium phosphate-bas…

2014

Calcium carbonate is the material that builds up the spicules of the calcareous sponges. Recent results revealed that the calcium carbonate/biocalcite-based spicular skeleton of these animals is formed through an enzymatic mechanism, such as the skeleton of the siliceous sponges, evolutionarily the oldest animals that consist of biosilica. The enzyme that mediates the calcium carbonate deposition has been identified as a carbonic anhydrase (CA) and has been cloned from the calcareous sponge species Sycon raphanus. Calcium carbonate deposits are also found in vertebrate bones besides the main constituent, calcium phosphate/hydroxyapatite (HA). Evidence has been presented that during the init…

Materials scienceGeneral Physics and Astronomychemistry.chemical_elementMineralogyReview02 engineering and technologyCalciumlcsh:Chemical technologybonelcsh:Technologysponge03 medical and health scienceschemistry.chemical_compoundVateriteNanotechnologylcsh:TP1-1185General Materials SciencebiocalciteSycon raphanusElectrical and Electronic Engineeringlcsh:Sciencebone formation030304 developmental biologycalcareous spiculesCalcite0303 health sciencesbiologyCalcareous spongelcsh:T021001 nanoscience & nanotechnologybiology.organism_classificationlcsh:QC1-999NanoscienceSpongeCalcium carbonatechemistryChemical engineeringlcsh:Q0210 nano-technologybioprintingCalcareouslcsh:PhysicsBeilstein Journal of Nanotechnology
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