Search results for "ISOTOPE"

showing 10 items of 2232 documents

Access to Gamma-ray Spectroscopy of Neutron-Rich sdfp Shell Nuclei

2000

γ-rays in neutron-rich sdfp shell nuclei, produced in deep-inelastic processes during collisions of 37Cl and 40Ar ions on 208Pb and of 48Ca ions on 48Ca, have been studied using large Ge multidetector arrays. Candidates for new yrast states in heavy argon and sulfur isotopes have been identified.

ArgonMaterials scienceYrastNuclear TheoryShell (structure)chemistry.chemical_elementCoulomb excitationIsotopes of sulfurIonchemistryPhysics::Plasma PhysicsNeutronGamma spectroscopyAtomic physicsNuclear Experiment
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Dental calculus is not equivalent to bone collagen for isotope analysis: a comparison between carbon and nitrogen stable isotope analysis of bulk den…

2014

Palaeodietary reconstruction using the carbon and nitrogen isotope values of bone and dentine collagen is a well-established method and the biochemical processes involved are well known. Researchers have recently explored using bulk samples of dental calculus as a substitute for bone and dentine collagen in dietary analyses, because calculus can be sampled without causing damage to the teeth, and may be useful in situations where more destructive analyses are not possible, or where collagen is poorly preserved. Several questions remain about the use of bulk calculus as a source of carbon and nitrogen isotope data, however. It is not yet clear how much of an individual¿s life span dental cal…

Arqueologia medievalArcheologyBone collagenIsotopeChemistryStable isotope ratioCalculus (dental)educationMineralogychemistry.chemical_elementmedicine.diseaseNitrogenIsotopes of nitrogenstomatognathic diseasesmedicineCalculusCarbonIsotope analysisJournal of Archaeological Science
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Retention of Pb isotopes in glass surfaces for retrospective assessment of radon exposure

2006

Abstract In recent years there has been increasing interest in radio-epidemiological techniques to retrospectively measure the radon dose exposure by determining the activity of 210Pb, the longest-lived 222Rn progeny, in glass surface layers. In this study the diffusion of 39 keV 209Pb+ ions implanted into glass using the IGISOL facility has been studied under conditions that mimic the recoil implantation of 210Pb from 222Rn. The resulting depth distributions of 209Pb were then measured after heat treatment in vacuum at different temperatures by a sputter erosion technique. The diffusion coefficient could be described by an Arrhenius equation D = D0exp(−H/kT) where D 0 = 0.30 - 0.24 + 1.14 …

Arrhenius equationNuclear and High Energy PhysicsIsotopeAnnealing (metallurgy)Radiochemistrychemistry.chemical_elementRadon01 natural sciences030218 nuclear medicine & medical imagingRadon exposureIon03 medical and health sciencessymbols.namesake0302 clinical medicineRecoilchemistrySputtering0103 physical sciencessymbols010306 general physicsInstrumentationNuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms
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JAK3/STAT5/6 Pathway Alterations Are Associated with Immune Deviation in CD8+ T Cells in Renal Cell Carcinoma Patients

2010

To investigate the molecular mechanisms underlying altered T cell response in renal cell carcinoma (RCC) patients, we compared autologous and allogeneic CD8(+) T cell responses against RCC line from RCC patients and their HLA-matched donors, using mixed lymphocyte/tumor cell cultures (MLTCs). In addition, we analyzed the expression of molecules associated with cell cycle regulation. Autologous MLTC responder CD8(+) T cells showed cytotoxic activity against RCC cell lines; however the analysis of the distribution of CD8(+) T-cell subsets revealed that allogenic counterparts mediate superior antitumor efficacy. In RCC patients, a decreased proliferative response to tumor, associated with defe…

Article SubjectCell Survivallcsh:Biotechnologylcsh:MedicineEnzyme-Linked Immunosorbent AssayE2F4 Transcription FactorCD8-Positive T-Lymphocytesurologic and male genital diseaseslcsh:TP248.13-248.65Chromium IsotopesSTAT5 Transcription FactorTumor Cells CulturedHumansCarcinoma Renal CellInhibitor of Differentiation Protein 2Microscopy Confocallcsh:RCell CycleIntracellular Signaling Peptides and ProteinsJanus Kinase 3Flow Cytometryfemale genital diseases and pregnancy complicationsKidney NeoplasmsGene Expression Regulation NeoplasticCase-Control StudiesLymphocyte Culture Test MixedSTAT6 Transcription FactorCyclin-Dependent Kinase Inhibitor p27Research ArticleSignal TransductionJournal of Biomedicine and Biotechnology
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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
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Climate signals in carbon and oxygen isotope ratios of Pinus cembra tree‐ring cellulose from the Călimani Mountains, Romania

2020

Abstract We analyze annually resolved tree-ring stable carbon (I´13C) and oxygen (I´18O) isotopic chronologies from Swiss stone pine (Pinus cembra L.) in Romania. The chronologies cover the period between 1876 and 2012 and integrate data from four individual trees from the Calimani Mts in the eastern Carpathians where climatic records are scarce and starts only from 1961. Calibration trials show that the I´13C values correlate with local April-May relative humidity and with regional to larger scale (European) summer precipitation. I´18O correlates significantly with local relative humidity, cloud cover, maximum temperature, as well as European scale drought conditions. In all cases, the cli…

Atmospheric Science010504 meteorology & atmospheric sciencesδ13Cδ18OPinus cembra15. Life on land010502 geochemistry & geophysics01 natural sciencesIsotopes of oxygenfood.foodMediterranean seafood13. Climate actionClimatologyDendrochronologyEnvironmental sciencePrecipitationPhysical geographyPressure system0105 earth and related environmental sciencesInternational Journal of Climatology
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Interannual variability of Greenland winter precipitation sources: 2. Effects of North Atlantic Oscillation variability on stable isotopes in precipi…

2008

[1] A new Lagrangian moisture source diagnostic is applied to identify the atmospheric conditions relevant for the fractionation of stable water isotopes during evaporation over the ocean and subsequent transport to Greenland. Northern Hemisphere winter months with positive and negative North Atlantic Oscillation (NAO) index are studied on the basis of ERA-40 reanalysis data. Diagnosed moisture transport conditions are supplied to a Rayleigh-type isotope fractionation model to derive estimates for the isotopic composition of stable isotopes in winter precipitation on the Greenland plateau for the two NAO phases. Because of changes in atmospheric circulation, moisture source locations for pr…

Atmospheric Science010504 meteorology & atmospheric sciencesδ18O0207 environmental engineeringSoil ScienceGreenland ice sheet02 engineering and technologyAquatic ScienceOceanography01 natural sciencesIsotope fractionationIce coreGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)020701 environmental engineering[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface ProcessesWater Science and Technology[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereEcologyStable isotope ratioNorthern HemispherePaleontologyForestrySea surface temperatureGeophysics13. Climate actionSpace and Planetary ScienceNorth Atlantic oscillationClimatologyEnvironmental science
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δ13C variations in tree rings as an indication of severe changes in the urban air quality

2002

Abstract Annual growth rings sampled from three free-standing trees (Platanus hybrida sp.), grew in the metropolitan area of Palermo (Italy) and covering a 118 years time span (1880–1998), have been studied for their 13C/12C carbon isotope ratios. It has been found that the 13C/12C tree ring record, during the study time interval, decreased of −3.6‰, from −26.4‰ in 1880 to −30‰ in 1998. Such a progressive depletion has been attributed to the addition of anthropogenic 13C depleted carbon dioxide to the local atmosphere. The observed 13C/12C decrease has been used to infer some possible pathways of atmospheric CO2 change in the study urban area.

Atmospheric ScienceAir pollutionMineralogyUrban environmentAtmospheric sciencesmedicine.disease_causeAtmospherechemistry.chemical_compoundmedicineDendrochronologyEnvironmental geochemistryAir quality indexGeneral Environmental Scienceδ13Cbiologybiology.organism_classificationStable carbon isotopeSettore GEO/08 - Geochimica E VulcanologiaPlatanuschemistryCarbon dioxideIsotopes of carbonCarbon dioxideEnvironmental scienceDendrochemistryTree ring
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Paleoceanography of the Late Cretaceous northwestern Tethys Ocean: Seasonal upwelling or steady thermocline?

2020

In this study we attempted to assess whether seasonal upwelling or a steady thermocline persisted at the western margin of the Tethys Ocean during the late Turonian-early Coniacian interval. For this scope, we employed novel and published stable oxygen isotope (δ18O) data of various organisms (bivalves, bivalves, brachiopods, fish and belemnites). New seasonally resolved temperature estimates were based on the δ18O record of sequentially sampled inoceramid (Inoceramus sp.) and rudist (Hippurites resectus) shells from the Scaglia Rossa and Gosau deposits of northern Italy and western Austria, respectively. Diagenetic screening was performed using reflected light, cathodoluminescence (CL), sc…

Atmospheric ScienceComposite Particles010504 meteorology & atmospheric sciencesMarine and Aquatic SciencesOxygen IsotopesOceanography010502 geochemistry & geophysics01 natural sciencesIsotopesClimatologyCretaceous PeriodMultidisciplinarybiologyPhysicsStable IsotopesQRTemperatureEukaryotaGeologyCretaceousOceanographyPhysical SciencesMedicineMesozoic EraSeasonsPaleotemperatureGeologyResearch ArticleShallow WaterInoceramusBivalvesAtomsWater massScienceOceans and SeasPaleoenvironmentsPaleoceanographyAnimalsPaleoclimatologyParticle PhysicsOcean Temperature0105 earth and related environmental sciencesOrganismsPaleontologyWaterBiology and Life SciencesGeologic TimeMolluscsTethys Oceanbiology.organism_classificationInvertebratesBivalviaWaves and shallow waterEarth SciencesUpwellingHydrologyZoologyThermoclinePLOS ONE
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Lagrangian simulations of stable isotopes in water vapor: An evaluation of nonequilibrium fractionation in the Craig-Gordon model

2009

[1] The Craig-Gordon model is the basis for the parameterization of water isotope fractionation during evaporation from the ocean in many atmospheric isotope models. Its exact formulation (e.g., with respect to the nonequilibrium fractionation factor k) is mainly based on theoretical considerations and not very well constrained by observations. This study addresses this issue by combining a recently developed Lagrangian moisture source analysis with a Craig-Gordon fractionation parameterization for the identified evaporation events in order to model isotope ratios in water vapor. This technique is applied to 45 measurement days of isotopes in water vapor at Rehovot (Israel) during the years…

Atmospheric ScienceEcologyMeteorologyStable isotope ratioEvaporationPaleontologySoil ScienceNon-equilibrium thermodynamicsThermodynamicsForestryAquatic ScienceOceanographyWind speedGeophysicsIsotope fractionationDeuteriumSpace and Planetary ScienceGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Environmental scienceParametrizationPhysics::Atmospheric and Oceanic PhysicsWater vaporEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research
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