Search results for "melting"

showing 10 items of 238 documents

Combustion synthesis of MoSi2 and MoSi2–Mo5Si3 composites: Multilayer modeling and control of the microstructure

2010

International audience; In this work, we present a multilayer modeling for the formation of molybdenum silicides in the exothermic reaction between Mo and Si under the influence of a temperature pulse. The heating rate can either be a well-controlled ramp or be generated spontaneously by the propagation of a combustion synthesis front. The model addresses the specific situation above the melting point of silicon and describes the solid–liquid reaction taking place in a single representative particle of molybdenum surrounded by the melt of silicon. We obtain a set of kinetic equations for the propagation of the interfaces between the different layers (Mo/Mo5Si3 and Mo5Si3/MoSi2) in the solid…

Exothermic reactionMaterials scienceSiliconSelf-propagating high-temperature synthesischemistry.chemical_element02 engineering and technologyCombustion01 natural sciences7. Clean energy[PHYS.PHYS.PHYS-CHEM-PH] Physics [physics]/Physics [physics]/Chemical Physics [physics.chem-ph]Powder metallurgy0103 physical sciencesMolybdenum silicidesMaterials ChemistryComposite material010302 applied physicsMechanical EngineeringModelingMetals and Alloys021001 nanoscience & nanotechnologyMicrostructure[ PHYS.PHYS.PHYS-CHEM-PH ] Physics [physics]/Physics [physics]/Chemical Physics [physics.chem-ph]KineticsSolid–liquid reactionschemistryMechanics of MaterialsMolybdenumMelting pointParticle[PHYS.PHYS.PHYS-CHEM-PH]Physics [physics]/Physics [physics]/Chemical Physics [physics.chem-ph]0210 nano-technologySelf-propagating high-temperature synthesisJournal of Alloys and Compounds
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Field and petrographic evidence for partial melting of TTG gneisses from the central region of the mainland Lewisian complex, NW Scotland

2013

The central region of the mainland Lewisian complex is dominated by granulite-facies tonalite–trondhjemite–granodiorite (TTG) gneisses that are highly depleted in some mobile trace elements (Cs, Rb, Th and U) relative to amphibolite-facies TTG gneisses elsewhere in the Lewisian complex and to the average composition of TTG gneisses worldwide. Over almost half a century of research there has been vigorous debate as to the origin of this depletion, in particular with respect to the role of partial melting and melt loss. Here we provide field and petrographic evidence that TTG gneisses across the central region partially melted during granulite-facies (Badcallian) metamorphism. Partial melting…

FelsicPartial meltingGeochemistryengineeringMetamorphismPlagioclaseGeologyengineering.materialMigmatiteGeologyGneissLewisian complexHornblendeJournal of the Geological Society
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Homogeneous freezing of single sulfuric and nitric acid solution drops levitated in an acoustic trap

2009

Abstract The freezing temperatures of single supercooled drops of binary and ternary sulfuric and nitric acid solutions were measured while varying the acid concentration. An acoustic levitator was used which allows to freely suspend single solution drops in air without electrical charges thereby avoiding any electrical influences which may affect the freezing process. The drops of typically 500 µm in radius were monitored by a video camera during cooling cycles down to − 85 °C to simulate the upper tropospheric and stratospheric temperature range. The present data confirm that liquid solution droplets can be supercooled far below the equilibrium melting point by approximately 35 °C. They f…

Flash freezingAtmospheric ScienceMaterials scienceThermodynamicsSulfuric acidRadiuslaw.inventionchemistry.chemical_compoundchemistrylawNitric acidMelting pointIce nucleusSupercoolingTernary operationAtmospheric Research
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Ab Initio Phase Diagram of Chromium to 2.5 TPa

2022

Chromium possesses remarkable physical properties such as hardness and corrosion resistance. Chromium is also a very important geophysical material as it is assumed that lighter Cr isotopes were dissolved in the Earth’s molten core during the planet’s formation, which makes Cr one of the main constituents of the Earth’s core. Unfortunately, Cr has remained one of the least studied 3d transition metals. In a very recent combined experimental and theoretical study (Anzellini et al., Scientific Reports, 2022), the equation of state and melting curve of chromium were studied to 150 GPa, and it was determined that the ambient body-centered cubic (bcc) phase of crystalline Cr re…

Fluid Flow and Transfer ProcessesProcess Chemistry and TechnologyGeneral EngineeringFísicaGeneral Materials ScienceQuímicaquantum molecular dynamics; melting curve; solid–solid phase transition boundary; equation of state; multi-phase materialsInstrumentationMaterialsComputer Science Applications
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Confined growth of carbon nanoforms in one-dimension by fusion of anthracene rings inside the pores of MCM-41

2014

We report a simple two-step procedure that uses anthracene, a cheap polyaromatic hydrocarbon with low melting point, as a molecular precursor to produce carbon nanoforms (CNFs). First, we describe the chemical synthesis of graphite from the fusion of anthracene rings at relatively low temperature (520 °C) followed by cyclodehydrogenation. Next, we extend this protocol to the synthesis of CNFs by confining the molecular precursor in a mesoporous host like MCM-41. The confined environment favors one-dimensional growth of CNFs with sizes controlled by the pores of the mesoporous host.

FusionAnthraceneMaterials scienceLow melting pointchemistry.chemical_elementNanotechnologyChemical synthesischemistry.chemical_compoundChemical engineeringchemistryMCM-41General Materials ScienceGraphiteMesoporous materialCarbonNanoscale
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Structural transitions and melting of copper clusters

1993

Molecular dynamics is used to study the melting and structural transitions of small copper clusters. The melting temperature is found to be proportional to the average coordination number. Small icosahedral clusters melt at slightly higher temperatures than the cubic structures. Small cuboctahedral clusters are not stable but transform via a nondiffusive transition to icosahedral structure.

FusionMolecular dynamicsMaterials scienceTransition metalchemistryChemical physicsIcosahedral symmetryCondensed Matter::SuperconductivityMelting temperatureCoordination numberchemistry.chemical_elementCopperAtomic and Molecular Physics and OpticsZeitschrift f�r Physik D Atoms, Molecules and Clusters
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New constraints on granulite facies metamorphism and melt production in the Lewisian Complex, northwest Scotland

2018

The research carried out for this study was part of YF's Master Thesis at the Institute of Geoscience, Johannes Gutenberg University, Mainz, which provided the funding for fieldwork and laboratory analyses. TJ acknowledges support from Open Fund GPMR210704 from the State Key Lab for Geological Processes and Mineral Resources, China University of Geosciences, Wuhan. In this study we investigate the metamorphic history of the Assynt and Gruinard blocks of the Archaean Lewisian Complex, northwest Scotland, which are considered by some to represent discrete crustal terranes. For samples of mafic and intermediate rocks, phase diagrams were constructed in the Na2O-CaO‐K2O‐FeO‐MgO‐Al2O3-SiO2-H2O-T…

GE010504 meteorology & atmospheric sciencesArcheanEarth sciencePartial meltingNDASMetamorphismPseudosectionThermocalcGeologyArchaeanPartial melting010502 geochemistry & geophysicsGranulite01 natural sciencesMineral resource classificationLewisian complexQE GeologyMafic phase equilibraGeochemistry and PetrologyFaciesQEGeology0105 earth and related environmental sciencesGE Environmental Sciences
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Quaternary ammonium polyiodides as ionic liquid/soft solid electrolytes in dye-sensitized solar cells

2007

Abstract Four new quaternary ammonium iodides, (Me 2 Pe 2 N)I, (Me 2 Hex 2 N)I, (Et 2 Pe 2 N)I and (Et 2 Hex 2 N)I, were synthesized and studied as electrolytes in dye-sensitized solar cells. All compounds were solids at room temperature. Influence of varying amounts of elemental iodine and the effect of tert -butylpyridine (TBP) on the performance of the cell was also studied. Addition of iodine lowered the melting points of the resulting polyiodides. From the ammonium iodides only (Me 2 Hex 2 N)I:I 2 (10:1) was liquid at the room temperature and the others were soft solids. Under illumination from a halogen lamp source at 10 mW cm −2 intensity, the highest power conversion efficiency of 2…

General Chemical EngineeringInorganic chemistryGeneral Physics and Astronomychemistry.chemical_elementGeneral ChemistryElectrolyteIodinechemistry.chemical_compoundPolyiodideDye-sensitized solar cellchemistryIonic liquidMelting pointFast ion conductorAmmoniumJournal of Photochemistry and Photobiology A: Chemistry
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Is the Crucible Reproducible? Reconciling Melting Experiments with Thermodynamic Calculations

2011

Experimental studies and thermodynamic modelling have advanced our understanding of partial melting in the crust and have provided a frame-work for the interpretation of migmatites, residual granulites and granites. Each approach has advantages and pitfalls, and each is more appropriate than the other for investigating particular aspects of the melting process. A comparison of these two approaches may be useful because, together, they potentially give more information. A comparison of a small number of experiments with model calculations using equivalent bulk compositions shows important consistencies between the results, especially regarding the overall topologies of key melting equilibria…

Geochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Partial meltingMineralogyThermodynamicsCrucibleResidualTopology (chemistry)GeologyElements
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Anatectic amphibole and restitic garnet in Variscan migmatite from NE Sardinia, Italy: insights into partial melting from mineral trace elements

2014

We report results of a laser-ICP-MS investigation of trace element contents in the main constituent minerals of an amphibole-bearing migmatite from the Variscan orogen in northeastern Sardinia. The migmatite is associated with migmatised orthogneiss and Al-silicate-bearing pelitic migmatites. The protolith of the amphibole-bearing migmatite was a mid-Ordovician igneous rock of intermediate composition characterised by a biotite + plagioclase + quartz assemblage. The migmatite consists of mesosomes and tonalitic (or, less frequently, granodioritic) leucosomes, characterised by amphibole crystals (potassian ferropargasite) up to 2 cm in size. The tonalitic leucosomes are made up of quartz, pl…

Geochemistry and PetrologyGeochemistryPartial meltingengineeringPlagioclaseMaficengineering.materialMigmatiteAnatexisProtolithAmphiboleGeologyZirconEuropean Journal of Mineralogy
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