Search results for "Trace element"

showing 10 items of 321 documents

The aqueduct of Gerasa – Intra-annual palaeoenvironmental data from Roman Jordan using carbonate deposits

2021

Abstract Calcium carbonate (CaCO3) deposits from Roman aqueducts are an innovative archive to obtain local high-resolution palaeoenvironmental and archaeological data in interdisciplinary studies. Deposits from one of the aqueducts of the Roman city of Gerasa provide a record of 59 years during the 1st to 3rd centuries CE, divided into three sequences separated by plaster layers. Annual carbonate layers show an alternation of sparite, formed in winter, and micrite, formed in summer. Brown bands at the base of many sparite layers probably correspond to large rainstorms in early winter. A fine lamination present in the brown bands may be diurnal in origin. Stable isotope and trace element dat…

Calcite010506 paleontologygeographygeography.geographical_feature_categoryMicriteGeochemistryTrace elementPaleontologyAquiferAqueduct010502 geochemistry & geophysicsOceanography01 natural scienceschemistry.chemical_compoundCalcium carbonatechemistrySpring (hydrology)CarbonateEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Accurate trace element analysis of speleothems and biogenic calcium carbonates by LA-ICP-MS

2012

The high spatial resolution of laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) microanalysis of speleothems and biogenic calcium carbonates makes it possible to improve our understanding of past climatic conditions. However, there are analytical problems associated with this method, such as molecular interferences, elemental fractionation, and mass-load-dependent matrix effects, when using NIST silicate reference glasses for calibration. Our study with a sector-field ICP-MS shows that many masses are affected by interferences, such as 24Mg+ by 48Ca++ or 31P+ by 15N16O+. Elemental fractionation and mass-load-dependent matrix effects have been detected for both 213 and…

CalciteAragoniteAnalytical chemistryTrace elementGeologyFractionationengineering.materialMicroanalysisSilicatechemistry.chemical_compoundCalcium carbonatechemistryGeochemistry and PetrologyengineeringGeologyRefractory (planetary science)Chemical Geology
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An overview of the geochemical characteristics of oceanic carbonatites: New insights from Fuerteventura carbonatites (Canary islands)

2021

The occurrence of carbonatites in oceanic settings is very rare if compared with their continental counterpart, having been reported only in Cape Verde and Canary Islands. This paper provides an overview of the main geochemical characteristics of oceanic carbonatites, around which many debates still exist regarding their petrogenesis. We present new data on trace elements in minerals and whole-rock, together with the first noble gases isotopic study (He, Ne, Ar) in apatite, calcite, and clinopyroxene from Fuerteventura carbonatites (Canary Islands). Trace elements show a similar trend as Cape Verde carbonatites, almost tracing the same patterns on multi-element and REE abundance diagrams. 3…

CalciteCape Verdelcsh:Mineralogylcsh:QE351-399.2010504 meteorology & atmospheric sciencesCape Verde Fuerteventura Noble gases isotopes Oceanic carbonatites Trace elementsnoble gases isotopesGeochemistrytrace elementsGeology010502 geochemistry & geophysicsGeotechnical Engineering and Engineering Geology01 natural sciencesLithospheric mantleMantle (geology)Cape verdeFuerteventurachemistry.chemical_compoundchemistryCarbonatiteoceanic carbonatitesGeology0105 earth and related environmental sciencesPetrogenesis
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Calcite Mg and Sr partition coefficients in cave environments: Implications for interpreting prior calcite precipitation in speleothems

2020

Abstract Trace element to Ca ratios in speleothems have emerged as important proxies that reflect local environmental conditions. However, interpretations of speleothem trace element records can be challenging due to various processes. Positive correlations between speleothem Mg/Ca and Sr/Ca have often been interpreted to reflect prior calcite precipitation (PCP), a process potentially modulated by rainfall variability. For quantitative interpretation of PCP, the distribution coefficients for Mg and Sr (DMg and DSr) are required. Here, we use ten cave monitoring calcite and drip water datasets to investigate the influence of temperature and drip water and calcite Mg/Ca and Sr/Ca ratios on s…

CalciteDolostonegeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesChemistryTrace elementSpeleothemMineralogy010502 geochemistry & geophysicsPositive correlation01 natural sciencesPartition coefficientchemistry.chemical_compoundCaveGeochemistry and PetrologyPrecipitation0105 earth and related environmental sciencesGeochimica et Cosmochimica Acta
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Investigation of manganese in salt- and freshwater pearls

2001

Abstract The trace element distribution in natural and cultured pearls is analysed by micro-PIXE, cathodoluminescence (CL) microscopy and spectroscopy and electron spin resonance (ESR) spectroscopy to develop a new method to distinguish cultured from natural pearls. These different kinds of pearls can be identified by their manganese content and its distribution in aragonite and calcite structure, respectively. Manganese content of natural freshwater pearls from Persian Gulf was compared to that of natural freshwater pearls from the Mississippi river (USA). Moreover manganese content of tissue-graft freshwater pearls from Chansu (China) was compared to that of natural freshwater pearls from…

CalciteNuclear and High Energy PhysicsMicro pixeAragoniteTrace elementchemistry.chemical_elementMineralogyManganeseengineering.materialchemistry.chemical_compoundchemistryEnvironmental chemistryengineeringInstrumentationNuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms
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Determination of aragonite trace element distribution coefficients from speleothem calcite–aragonite transitions.

2016

The processes that govern the incorporation of (trace) elements into speleothems can often be linked to environmental changes. Although element incorporation into speleothem calcite is now reasonably well understood, current knowledge regarding trace element variability in speleothem aragonite is very limited. Of particular interest is whether trace element distribution coefficients are above or below one in order to assess the extent to which prior aragonite precipitation has affected speleothem aragonite trace element records. This study uses nine calcite-to-aragonite transitions in seven speleothems from diverse environmental settings to derive the first quantitative estimates of the dis…

Calcitegeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesAragoniteTrace elementMineralogySpeleothemF700StalagmiteF800engineering.materialF600010502 geochemistry & geophysics01 natural sciencesF900chemistry.chemical_compoundchemistryGeochemistry and PetrologyengineeringGrowth rateNegative correlationGeology0105 earth and related environmental sciences
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Validated fast procedure for trace element determination in basil powder

2011

Abstract An inductively coupled plasma optical emission spectroscopic (ICP-OES) method has been developed and fully validated for trace element determination in basil samples. The method involves the previous sample digestion, under pressure, with a mixture of HNO 3 , HCl and H 2 O 2 inside a microwave oven, 42 elements were studied and 33 elements (Al, As, Ba, Ca, Cr, Co, Cu, Fe, Pb, Li, Mg, Mn, Mo, Ni, K, Se, Na, Sr, Tl, Ti, V, Zn, Sc, Y, La, Ce, Nd, Tb, Ho, Er, Tm, Yb, Lu) were determined quantitatively in basil leaves obtained from Morocco and Spain. The method provided recovery percentages from 89% to 113% for spiked concentrations at mg kg −1 and μg kg −1 . Accurate results were found…

Certified reference materialsChemistryInductively coupled plasma atomic emission spectroscopyMicrowave ovenAnalytical chemistryTrace elementGeneral MedicineOptical emission spectroscopyInductively coupled plasmaSpectroscopyChemical compositionFood ScienceAnalytical ChemistryFood Chemistry
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Nature-Inspired Effects of Naturally Occurring Trace Element-Doped Hydroxyapatite Combined with Surface Interactions of Mineral-Apatite Single Crysta…

2022

Innovative engineering design for biologically active hydroxyapatites requires enhancing both mechanical and physical properties, along with biocompatibility, by doping with appropriate chemical elements. Herein, the purpose of this investigation was to evaluate and elucidate the model of naturally occurring hydroxyapatite and the effects of doped trace elements on the function of normal human fibroblasts, representing the main cells of connective tissues. The substrates applied (geological apatites with hexagonal prismatic crystal habit originated from Slyudyanka, Lake Baikal, Russia (GAp) and from Imilchil, The Atlas Mountains, Morocco (YAp)) were prepared from mineral natural apatite wit…

Chemical Phenomenahydroxyapatite; mineral apatite single crystals; FTIR; SEM-EDXS; X-ray diffraction; fibroblast cell culture; cell–surface interactionsQH301-705.5Cell SurvivalBiocompatible MaterialsCatalysisArticleInorganic Chemistryfibroblast cell cultureApatitesHumansBiology (General)Physical and Theoretical ChemistryQD1-999Molecular BiologySpectroscopyCell ProliferationMineralsSpectrum AnalysisOrganic Chemistryhydroxyapatitecell–surface interactionsGeneral MedicineFibroblastsComputer Science ApplicationsX-ray diffractionTrace ElementsChemistryDurapatiteFTIRSEM-EDXSmineral apatite single crystalsInternational Journal of Molecular Sciences
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Geochemical characteristics of waters in mineralised area of Peloritani Mountains (Sicily, Italy)

2009

Abstract This paper presents the results of a study on the geochemistry of waters circulating in the mineralised area of the south-eastern sector of Mt. Peloritani (north-eastern Sicily, Italy), aimed at basic understanding of the geochemical processes influencing their chemical composition. Chemico-physical parameters and data on 26 major and minor chemical elements are reported for 103 water samples. Water chemistry is mainly dominated by dissolution of carbonates and hydrolysis of aluminosilicate minerals. Total dissolved salts (TDS) range from 80 to 1398 mg/L. All the waters exhibit E H characteristic of an oxygenated environment. Excluding two samples, which show very high H + activity…

ChemistryDolomiteCarbonate mineralsGeochemistryTrace elementWeatheringPollutionSettore GEO/08 - Geochimica E Vulcanologiachemistry.chemical_compoundmineralised area trace elements hydrogeochemistryGeochemistry and PetrologyEnvironmental ChemistryKaoliniteCarbonateClay mineralsChemical compositionApplied Geochemistry
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Determination of mineral and trace element concentrations in pine needles by ICP-OES: evaluation of different sample pre-treatment methods

2008

In the present study, the determination of mineral and trace elements (Al, B, Ca, Cu, Fe, K, Mg, Mn, Na, P and Zn) from pine needles using three sample pre-treatment methods followed by inductively coupled plasma optical emission spectrometry, was examined. Sample pre-treatment methods tested were microwave digestion, ultrasound-assisted digestion and dry ashing. The new ultrasound-assisted digestion method was optimised by the analysis of the standard reference material (SRM) 1575a (pine needles) sample. The speed of dry ashing method was significantly increased by ultrasound dissolution after ashing. All the ICP-OES measurements were performed in robust plasma conditions which were tested…

ChemistryHealth Toxicology and MutagenesisPublic Health Environmental and Occupational HealthAnalytical chemistryTrace elementSoil SciencePollutionAnalytical ChemistryDigestion (alchemy)AshingInductively coupled plasma atomic emission spectroscopyEnvironmental ChemistryMicrowave digestionInductively coupled plasmaWaste Management and DisposalDissolutionMicrowaveWater Science and TechnologyInternational Journal of Environmental Analytical Chemistry
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