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A Sub-Milliwatt Graphene-Based Thermal Conductivity Detector for On-Site Gas Analysis. [PDF]
Sium FS +7 more
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Multiobjective optimization of natural convection and entropy generation in a porous wavy cavity with a heated star-shaped obstacle using a hybrid nanofluid. [PDF]
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On thermal regime of nanoparticles in synthesis flame
Chemical Physics Letters, 2021Flame Synthesis conditions significantly affect nanoparticles properties. Understanding thermal regime in flames can be very useful for tuning nanoparticles with specific properties. In this work, information on thermal status is obtained through the analysis of light emission from nanoparticles during synthesis and under an external laser irradiation.
De Iuliis S, Dondè R, Altman I
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Icarus, 1990
Models for the thermal evolution of Venus are constructed numerically. The mantle is proposed to consist of two independently convecting layers (upper and lower mantles); the floating crust keeps the temperature of the upper surface of the convecting mantle near 1200°C and the core may solidify at temperatures below the liquidus.
V.S. Solomatov, V.N. Zharkov
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Models for the thermal evolution of Venus are constructed numerically. The mantle is proposed to consist of two independently convecting layers (upper and lower mantles); the floating crust keeps the temperature of the upper surface of the convecting mantle near 1200°C and the core may solidify at temperatures below the liquidus.
V.S. Solomatov, V.N. Zharkov
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Thermal regimes of anisotropic-thermoelement thermal converters
Journal of Engineering Physics and Thermophysics, 2000A computational procedure is developed for the thermal regime of anisotropic-thermoelement thermal converters of cavity and plane types used to investigate heat fluxes and energy parameters of radiation. Heat losses from different elements of the thermal-converter structure are analyzed and the parameters of a battery of anisotropic thermoelements are ...
I. M. Pilat +4 more
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2010
Pyrometamorphism related to intrusion of mafic magma and the burning of organic material is expected to result in anisotropic thermal expansion and associated positive volume changes in contact rocks due to reaction and melting of the mineral phases. Columnar jointing, cracking and dilation are typical of the structures developed. Temperature variation
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Pyrometamorphism related to intrusion of mafic magma and the burning of organic material is expected to result in anisotropic thermal expansion and associated positive volume changes in contact rocks due to reaction and melting of the mineral phases. Columnar jointing, cracking and dilation are typical of the structures developed. Temperature variation
openaire +1 more source

