Search results for "13. Climate action"

showing 10 items of 2386 documents

Integrative analysis of the mineralogical and chemical composition of modern microbialites from ten Mexican lakes: What do we learn about their forma…

2021

International audience; Interpreting the environmental conditions under which ancient microbialites formed relies upon comparisons with modern analogues. This is why we need a detailed reference framework relating the chemical and mineralogical compositions of modern microbialites to the physical and chemical parameters prevailing in the environments where they form. Here, we measured the chemical, including major and trace elements, and mineralogical composition of microbialites from ten Mexican lakes as well as the chemical composition of the surrounding waters. Saturation states of lakes with different mineral phases were systematically determined and correlations between solution and so…

(Mg-)calcite010504 meteorology & atmospheric sciencesREE+YDolomiteGeochemistryalkalinityengineering.material010502 geochemistry & geophysics01 natural sciencesaragonitechemistry.chemical_compoundmonohydrocalciteGeochemistry and Petrologyhydromagnesite0105 earth and related environmental sciencesCalciteAragoniteTrace elementmicrobialitesAuthigenic6. Clean waterDiagenesisMonohydrocalcitecrater lakechemistry13. Climate actionkerolite[SDE]Environmental SciencesengineeringCarbonate
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The influence of decision-making in tree ring-based climate reconstructions.

2021

Tree-ring chronologies underpin the majority of annually-resolved reconstructions of Common Era climate. However, they are derived using different datasets and techniques, the ramifications of which have hitherto been little explored. Here, we report the results of a double-blind experiment that yielded 15 Northern Hemisphere summer temperature reconstructions from a common network of regional tree-ring width datasets. Taken together as an ensemble, the Common Era reconstruction mean correlates with instrumental temperatures from 1794–2016 CE at 0.79 (p < 0.001), reveals summer cooling in the years following large volcanic eruptions, and exhibits strong warming since the 1980s. Differing in…

/141/704/106/694010506 paleontology010504 meteorology & atmospheric sciencesScienceGeneral Physics and AstronomyClimate changePalaeoclimate01 natural sciencesArticleGeneral Biochemistry Genetics and Molecular BiologyPaleoclimatologySDG 13 - Climate ActionDendrochronologyddc:550Climate change[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment0105 earth and related environmental sciencesResearch dataddc:333.7-333.913 Climate ActionClimate change; Palaeoclimate; Research dataGEMultidisciplinaryQNorthern HemisphereDASGeneral ChemistryResearch data/706/648/697Geography13. Climate actionClimatology/704/106/413GE Environmental Sciences
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2021

Atomic layer deposition (ALD) technology has unlocked new ways of manipulating the growth of inorganic materials. The fine control at the atomic level allowed by ALD technology creates the perfect conditions for the inclusion of new cationic or anionic elements of the already-known materials. Consequently, novel material characteristics may arise with new functions for applications. This is especially relevant for inorganic luminescent materials where slight changes in the vicinity of the luminescent centers may originate new emission properties. Here, we studied the luminescent properties of CaS:Eu by introducing europium with oxygen ions by ALD, resulting in a novel CaS:EuO thin film. We …

010302 applied physicsPhotoluminescenceMaterials sciencebusiness.industryDopingchemistry.chemical_elementPhosphor02 engineering and technology021001 nanoscience & nanotechnology7. Clean energy01 natural sciencesIonAtomic layer depositionchemistry13. Climate action0103 physical sciencesOptoelectronicsGeneral Materials ScienceThin film0210 nano-technologybusinessLuminescenceEuropiumMaterials
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Radiation hardness studies of CdTe and for the SIXS particle detector on-board the BepiColombo spacecraft

2009

Abstract We report of the radiation hardness measurements that were performed in the developing work of a particle detector on-board ESA's forthcoming BepiColombo spacecraft. Two different high- Z semiconductor compounds, cadmium telluride (CdTe) and mercuric iodide (HgI 2 ), were irradiated with 22 MeV protons in four steps to attain the estimated total dose of 10 12 p / cm 2 for the mission time. The performance of the detectors was studied before and after every irradiation with radioactive 55 Fe source Mn K α 5.9 keV emission line. We studied the impact of the proton beam exposure on detector leakage current, energy resolution and charge collection efficiency (CCE). Also the reconstruct…

010302 applied physicsPhysicsNuclear and High Energy PhysicsProton010308 nuclear & particles physicsbusiness.industryDetector7. Clean energy01 natural sciencesCadmium telluride photovoltaicsParticle detectorSemiconductor detectorSemiconductor13. Climate action0103 physical sciencesOptoelectronicsIrradiationbusinessInstrumentationRadiation hardeningNuclear Instruments and Methods in Physics Research Section A: Accelerators, Spectrometers, Detectors and Associated Equipment
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Introduction to the special issue on molecular spectroscopy, atmospheric composition and climate change

2018

International audience

010304 chemical physicsClimate changeMolecular spectroscopy010402 general chemistryAtmospheric sciences01 natural sciencesAtomic and Molecular Physics and Optics0104 chemical sciences[CHIM.THEO]Chemical Sciences/Theoretical and/or physical chemistryAtmospheric composition13. Climate action0103 physical sciencesEnvironmental sciencePhysical and Theoretical ChemistryComputingMilieux_MISCELLANEOUSSpectroscopyJournal of Molecular Spectroscopy
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Heterogeneous Interactions between Gas-Phase Pyruvic Acid and Hydroxylated Silica Surfaces: A Combined Experimental and Theoretical Study

2019

The adsorption of gas-phase pyruvic acid (CH3COCOOH) on hydroxylated silica particles has been investigated at 296 K using transmission Fourier transform infrared (FTIR) spectroscopy and theoretical simulations. Under dry conditions (<1% relative humidity, RH), both the trans-cis (Tc) and trans-trans (Tt) pyruvic acid conformers are observed on the surface as well as the (hydrogen bonded) pyruvic acid dimer. The detailed surface interactions were further understood through ab initio molecular dynamics simulations. Under higher relative humidity conditions (above 10% RH), adsorbed water competes for surface adsorption sites. Adsorbed water is also observed to change the relative populations …

010304 chemical physicsHydrogenChemistryDimerInorganic chemistrychemistry.chemical_element010402 general chemistry01 natural sciences0104 chemical scienceschemistry.chemical_compoundAdsorption13. Climate action0103 physical sciencesRelative humidityPyruvic acid[PHYS.PHYS.PHYS-CHEM-PH]Physics [physics]/Physics [physics]/Chemical Physics [physics.chem-ph]Physical and Theoretical ChemistryFourier transform infrared spectroscopySpectroscopyConformational isomerismComputingMilieux_MISCELLANEOUS
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Tetracationic and Tetraanionic Manganese Porphyrins: Electrochemical and Spectroelectrochemical Characterization

2017

International audience; The electrochemistry and spectroelectrochemistry of four tetrapositively charged and two tetranegatively charged porphyrins were characterized in two nonaqueous solvents (dimethyl sulfoxide and N,N-dimethylformamide) containing 0.1 M tetra-n-butylammonium perchlorate. The tetrapositively charged compounds are represented by the tetrapyridylporphyrins [TRPyPM]4+(X-)4, where R is a methyl or [2-[2-(2-methoxy)ethoxy]ethoxy]ethyl group, M = MnIIII, MnIIICl, CuII, or PdII, and X = I- or Cl-. The tetranegatively charged porphyrins are represented by the tetrasulfonato derivatives [TPPSMn(OAc)]4-(NH4+)4 and [TArPSMn(OAc)]4-(NH4+)4, where Ar = 4-O-[2-[2-(2-methoxy)ethoxy]eth…

010405 organic chemistryDimethyl sulfoxidechemistry.chemical_element[ CHIM.INOR ] Chemical Sciences/Inorganic chemistryManganese[CHIM.INOR]Chemical Sciences/Inorganic chemistry010402 general chemistryElectrochemistryPhotochemistry01 natural sciencesMedicinal chemistry0104 chemical sciencesInorganic Chemistrychemistry.chemical_compoundPerchloratechemistry13. Climate actionAlkoxy groupPyridiniumEthyl groupPhysical and Theoretical Chemistry
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Theoretical investigation of the spin crossover transition states of the addition of methane to a series of Group 6 metallocenes using minimum energy…

2016

International audience; Density functional calculations are reported on the addition of methane to Group 6 metallocenes, M(η-C5H5)2 (M), M(CH2(η-C5H4)2) (a-M) and M(η-C5Me5)2 (M*) where M = Mo and W. Full geometry optimisations were carried out on the singlet and triplet 16 electron complexes, 1[M] and 3[M], the η2-methane complexes, 1[M(η2-CH4)], and the hydridomethyl adducts, 1[M(CH3)(H)]. The triplet state for [M] was found to be more stable for all six metallocenes, the difference being least in the case of the ansa-bridged system. Formation of the hydridomethyl complexes was exoenergetic for all tungsten systems and for a-Mo, the other two Mo systems being endoenergetic. Minumum energy…

010405 organic chemistrychemistry.chemical_elementGeneral ChemistryElectronTungsten010402 general chemistry7. Clean energy01 natural sciencesTransition stateMethane0104 chemical sciencesAdduct[CHIM.THEO]Chemical Sciences/Theoretical and/or physical chemistrychemistry.chemical_compoundchemistry13. Climate actionSpin crossoverComputational chemistryPhysical chemistry[CHIM.COOR]Chemical Sciences/Coordination chemistrySinglet stateTriplet stateJOURNAL OF THE CHEMICAL SOCIETY-DALTON TRANSACTIONS
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A trajectory-based classification of ERA-Interim ice clouds in the region of the North Atlantic storm track

2016

A two-type classification of ice clouds (cirrus) is introduced, based on the liquid and ice water content, LWC and IWC, along air parcel backward trajectories from the clouds. In situ cirrus has no LWC along the trajectory segment containing IWC; it forms via nucleation from the gas phase. In contrast, liquid-origin cirrus has both LWC and IWC along their backward trajectories; it forms via lifting from the lower troposphere and freezing of mixed-phase clouds. This classification is applied to 12 years of ERA-Interim ice clouds in the North Atlantic region. Between 400 and 500 hPa more than 50% are liquid-origin cirrus, whereas this frequency decreases strongly with altitude (<10% at 200 hP…

010504 meteorology & atmospheric sciences010501 environmental sciencesFluid parcelAtmospheric sciences01 natural sciencesIce waterGas phaseTroposphereGeophysicsAltitude13. Climate actionGeneral Earth and Planetary SciencesCirrusStorm trackTrajectory (fluid mechanics)Geology0105 earth and related environmental sciencesGeophysical Research Letters
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Surface sediment dynamics along the shore of Hammamet Gulf (Tunisia, southern Mediterranean)

2016

International audience; In the summer of 2015 the authors analysed grain size and surface sediment composition through high spatial resolution from samples taken at 53 stations along the Hammamet coast (southern Mediterranean Sea). The Acoustic Doppler Current Profiler deployed in this study showed that the surface current flows toward the north-east, parallel to the coast at a maximum speed along the main axis of about 5.9 cm s−1. Near the bottom the current flows toward the north-west at a maximum speed of 2.2 cm s−1. The tide plays a relatively small role in water circulation in Hammamet Gulf. Spatial distribution of particle size, along with speed and current direction analysis, furnish…

010504 meteorology & atmospheric sciences010501 environmental sciencesSpatial distribution01 natural sciences[ SDE ] Environmental SciencesMediterranean seaAcoustic Doppler current profilerCurrents14. Life underwaterGeomorphology0105 earth and related environmental sciencesEarth-Surface ProcessesShoregeographyMineralsgeography.geographical_feature_categorySedimentGeologyParticle sizeSediment dynamicsHammamet GulfSwellCurrent (stream)Oceanography13. Climate action[SDE]Environmental SciencesSubmarine pipelineGeology
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