Search results for "CARBONATE"

showing 10 items of 920 documents

Micro-Raman spectroscopy of pigments contained in different calcium carbonate polymorphs from freshwater cultured pearls

2008

The metastable calcium carbonate polymorph vaterite has recently been found to occur commonly in freshwater cultured pearls from Japan and China. Organic pigment molecules in these vaterite regions of freshwater cultured pearls were analysed by resonance and near-resonance micro-Raman spectroscopy, in single spectra and in mapping modes and are compared with their aragonitic counterparts. Four different excitation wavelengths (487.9, 514.5, 532.2 and 632.8 nm) were used, resulting in differential increase of resolution for the pigments. Although vaterite areas were always lightly coloured (light yellow, light brown or white), ten different pigments were identified and a single colour is for…

AragoniteMineralogyengineering.materialConjugated systemResonance (chemistry)Crystallographysymbols.namesakechemistry.chemical_compoundPigmentCalcium carbonatechemistryVateritevisual_artengineeringsymbolsvisual_art.visual_art_mediumGeneral Materials ScienceRaman spectroscopySpectroscopySpectroscopyJournal of Raman Spectroscopy
researchProduct

Carbonates from the ancient world's longest aqueduct:A testament of Byzantine water management

2021

The fourth‐ and fifth‐century aqueduct system of Constantinople is, at 426 km, the longest water supply line of the ancient world. Carbonate deposits in the aqueduct system provide an archive of both archaeological developments and palaeo‐environmental conditions during the depositional period. The 246‐km‐long aqueduct line from the fourth century used springs from a small aquifer, whereas a 180‐km‐long fifth‐century extension to the west tapped a larger aquifer. Although historical records testify at least 700 years of aqueduct activity, carbonate deposits in the aqueduct system display less than 27 years of operation. This implies that the entire system must have been cleaned of carbonate…

Archeology552.5business.industrywater supplyRoman aqueductWater supplyAqueductAncient history930 History of ancient world550 Geowissenschaftenchemistry.chemical_compoundcarbonate930 Alte Geschichtechemistry550 Earth sciencesEarth and Planetary Sciences (miscellaneous)CarbonateByzantineConstantinoplebusinessGeologyByzantine architecture
researchProduct

1200 years of decadal-scale variability of Mediterranean vegetation and climate at Pantelleria Island, Italy.

2013

A new sedimentary sequence from Lago di Venere on Pantelleria Island, located in the Strait of Sicily between Tunisia and Sicily was recovered. The lake is located in the coastal infra-Mediterranean vegetation belt at 2 m a.s.l. Pollen, charcoal and sedimentological analyses are used to explore linkages among vegetation, fire and climate at a decadal scale over the past 1200 years. A dry period from ad 800 to 1000 that corresponds to the 'Medieval Warm Period' (WMP) is inferred from sedimentological analysis. The high content of carbonate recorded in this period suggests a dry phase, when the ratio of evaporation/precipitation was high. During this period the island was dominated by thermop…

ArcheologyInstitut für Erd- und UmweltwissenschaftenSettore AGR/05 - Assestamento Forestale E Selvicoltura'Little Ice Age' (LIA)'Medieval Warm Period' (MWP)Climate changePinus pinasterQuercus pubescenschemistry.chemical_compoundcentral Mediterraneancentral Mediterranean fire history ‘Little Ice Age’ (LIA) ‘Medieval Warm Period’ (MWP) Pinus pinaster Quercus ilex Quercus pubescens vegetation historyddc:550Precipitationvegetation historyEarth-Surface ProcessesGlobal and Planetary ChangeEcologybiologyEcologyPaleontologySedimentPlant communityVegetationbiology.organism_classificationQuercus ilexfire historychemistryQuercus pubescensPeriod (geology)CarbonateInstitut für GeowissenschaftenPhysical geographyGeology
researchProduct

Fragmentation of polycarbonate macroinitiators in solution and in the bulk state

1990

The diphenylethane initiator 3,4-diethyl-3,4-(p-methoxyphenyl)-hexane (T–OCH3) was synthesized. By cocondensation of bisphenol A or C and the bisphenol derivative (“T”) of T–OCH3 with phosgene, polycarbonate macroinitiators PC(TxA1-x) and PC(TxC1-x) with different compositions x were made. The thermal fragmentation of T–OCH3 and the copolycarbonates was investigated with and without a radical scavenger both in solution and in the bulk state. The primary dissociation of T–OCH3 is a monomolecular Arrhenius process with a characteristic temperature of T* (τ = 1h) = 140°C (τ: average life time of the intact molecule). When the radicals are not intercepted, the dissociation is excessively revert…

Arrhenius equationPolymers and PlasticsChemistryRadicalActivation energyCondensed Matter PhysicsDissociation (chemistry)symbols.namesakeFragmentation (mass spectrometry)visual_artPolymer chemistryMaterials Chemistryvisual_art.visual_art_mediumsymbolsPhysical and Theoretical ChemistryPolycarbonateRadical disproportionationGlass transitionJournal of Polymer Science Part B: Polymer Physics
researchProduct

Inverted responses of the carbon cycle to orbital forcing in Mesozoic peri‐platform marginal basins: implications for astrochronology

2020

International audience; Astrochronology depends on the faithful record of insolation forcing in climatic proxies, including the carbon isotope composition measured on bulk carbonates (δ13Ccarb). In marginal basins close to carbonate platforms, the source of carbonate is varied, which can impact the record of the astronomical cycles in the δ13Ccarb signal. We compare here the δ13Ccarb values together with detrital and weathering proxies before and during a crisis in the platform carbonate production (Weissert event, Valanginian, ~135 Ma) to document how a change in the carbonate source can affect the record of the orbital forcing by the carbon isotope system. The level of burial diagenesis w…

Astrochronology010506 paleontologyAtmospheric ScienceOrbital forcingGeochemistryPaleontologyWeatheringStructural basin010502 geochemistry & geophysicsOceanography01 natural sciencesDiagenesisCarbon cyclechemistry.chemical_compoundchemistry13. Climate action[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryMarlCarbonateGeology0105 earth and related environmental sciences
researchProduct

Astrochronology of the Valanginian stage from GSSP candidates and hypostratotype.

2013

Valanginian; Astrochronology; Gamma-ray spectrometry; Weissert event; Paraná-Etendeka; International audience; The Valanginian Stage currently displays no radiometric age, which severely hampers palaeoceanographic reconstructions for this time interval. An astrochronology of the Valanginian Stage using the stable 405-kyr eccentricity cycle was performed on biostratigraphically well-calibrated standard sections from the Vocontian Basin (southeastern France). High-resolution gamma-ray spectrometry signals were obtained from orbitally driven marl-limestone alternations from five sections in the basin, and they display the same long-term trends. The spectral analyses present the pervasive recor…

Astrochronology010506 paleontologyCarbonate platformmedia_common.quotation_subjectLarge igneous province010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesGlobal Boundary Stratotype Section and PointPaleontology13. Climate actionStage (stratigraphy)[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyPrecessionRadiometric datingEccentricity (behavior)Geology0105 earth and related environmental sciencesmedia_common
researchProduct

Relief and calcium from gypsum as key factors for net inorganic carbon accumulation in soils of a semiarid Mediterranean environment

2021

Abstract In semiarid environments, the total inorganic carbon (TIC) in soil may contribute to the total carbon (C) pool more than the total organic C pool (TOC), thus playing a key role in storing atmospheric CO2. However, due to the different origin pathways of soil carbonates, not all of the TIC pool can be accounted for CO2 sequestration. Indeed, the inorganic C can be accounted for a net sink of CO2 only when calcium (Ca2+) forming carbonates originate from non-carbonate minerals (atmogenic inorganic C, AIC). The aim of this study carried out in a gypsiferous area is to investigate the dissolution of Ca2+ that comes from gypsum (CaSO4·2H2O) in the formation of soil atmogenic carbonates …

Atmogenic inorganic CGypsumSoil testSoil Sciencechemistry.chemical_element010501 environmental sciencesCarbon sequestrationengineering.material01 natural scienceschemistry.chemical_compoundEucalyptus camaldulensiTotal inorganic carbon0105 earth and related environmental sciencesToposequenceSoil carbonate04 agricultural and veterinary sciencesStrontium isotope ratiochemistryEnvironmental chemistrySoil water040103 agronomy & agricultureengineering0401 agriculture forestry and fisheriesCarbonateEnvironmental scienceSink (computing)CarbonGypsiferous soilGeoderma
researchProduct

Lithologic composition of the Earth's continental surfaces derived from a new digital map emphasizing riverine material transfer

2005

[1] A new digital map of the lithology of the continental surfaces is proposed in vector mode (n ≈ 8300, reaggregated at 0.5° × 0.5° resolution) for 15 rock types (plus water and ice) targeted to surficial Earth system analysis (chemical weathering, land erosion, carbon cycling, sediment formation, riverine fluxes, aquifer typology, coastal erosion). These types include acid (0.98% at global scale) and basic (5.75%) volcanics, acid (7.23%) and basic (0.20%) plutonics, Precambrian basement (11.52%) and metamorphic rocks (4.07%), consolidated siliciclastic rocks (16.28%), mixed sedimentary (7.75%), carbonates (10.40%), semi- to un-consolidated sedimentary rocks (10.05%), alluvial deposits (15…

Atmospheric ScienceGlobal and Planetary Changegeographygeography.geographical_feature_categoryEvaporiteLithologyGeochemistryVolcanic rockPrecambrianBasement (geology)Environmental ChemistryCarbonate rockSiliciclasticSedimentary rockGeomorphologyGeologyGeneral Environmental ScienceGlobal Biogeochemical Cycles
researchProduct

Worldwide distribution of continental rock lithology: Implications for the atmospheric/soil CO2uptake by continental weathering and alkalinity river …

2003

[1] The silicate rock weathering followed by the formation of carbonate rocks in the ocean, transfers CO2 from the atmosphere to the lithosphere. This CO2 uptake plays a major role in the regulation of atmospheric CO2 concentrations at the geologic timescale and is mainly controlled by the chemical properties of rocks. This leads us to develop the first world lithological map with a grid resolution of 1° × 1°. This paper analyzes the spatial distribution of the six main rock types by latitude, continents, and ocean drainage basins and for 49 large river basins. Coupling our digital map with the GEM-CO2 model, we have also calculated the amount of atmospheric/soil CO2 consumed by rock weathe…

Atmospheric ScienceGlobal and Planetary Changegeographygeography.geographical_feature_categorySoil production functionLithologyGeochemistryWeatheringVolcanic rockIgneous rockClastic rockEnvironmental ChemistryCarbonate rockSedimentary rockGeomorphologyGeologyGeneral Environmental ScienceGlobal Biogeochemical Cycles
researchProduct

Composition and mixing state of the urban background aerosol in the Rhein-Main area (Germany)

2007

Abstract Size-resolved aerosol particle samples in the size range 0.1–10 μm aerodynamic diameter were collected in the years 2003 and 2004 at an urban background station in Mainz, Germany. Size, morphology, chemical composition and mixing state of more than 5400 individual particles of 7 selected sampling days were analyzed in detail by scanning electron microscopy and energy-dispersive X-ray microanalysis. In addition, transmission electron microscopy, aerosol mass spectrometry and atomic force microscopy were applied to obtain detailed information about the mixing state of the particles. The fine particle fraction (diameter 1 μm diameter) is strongly dependant on air mass history with var…

Atmospheric Sciencefood.ingredientChemistrySea saltAnalytical chemistrymedicine.disease_causeSootAerosolchemistry.chemical_compoundfoodUltrafine particleParticle-size distributionmedicineCarbonateParticleAerosol mass spectrometryGeneral Environmental ScienceAtmospheric Environment
researchProduct