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![After [128] Schematic form of the principal thermodynamic parameters through a phase transformation at Tc. Column I = first order; column II =second order; column III = λ transformation with a small first order break at Tc ; column IV = λ transformation with no first order break. G = free energy, H = enthalpy, S = entropy, ηl = long range order parameter ηs= short range order parameter describing precursor ordering above Tc; CP = specific heat; Ik = integrated intensity of a superlattice reflection. D = disordered state, O= ordered state. LRO = long range order, SRO = short range order. Volume is not shown, but must be continuous or discontinuous in some manner analogous to H and S](profile/Artur-Benisek/publication/360362552/figure/fig4/AS:1156923588116481@1652843486680/After-128-Schematic-form-of-the-principal-thermodynamic-parameters-through-a-phase.png)
After [128] Schematic form of the principal thermodynamic parameters through a phase transformation at Tc. Column I = first order; column II =second order; column III = λ transformation with a small first order break at Tc ; column IV = λ transformation with no first order break. G = free energy, H = enthalpy, S = entropy, ηl = long range order parameter ηs= short range order parameter describing precursor ordering above Tc; CP = specific heat; Ik = integrated intensity of a superlattice reflection. D = disordered state, O= ordered state. LRO = long range order, SRO = short range order. Volume is not shown, but must be continuous or discontinuous in some manner analogous to H and S
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![Figure 4 Bronzite [93], data and ideal cP calculated for ideal composition.](profile/Artur-Benisek/publication/360362552/figure/fig2/AS:1156923588120582@1652843486647/Bronzite-93-data-and-ideal-cP-calculated-for-ideal-composition_Q320.jpg)
![Figure 5 Bronzite [93], low T, data and ideal cP calculated for the...](profile/Artur-Benisek/publication/360362552/figure/fig3/AS:1156923588120583@1652843486665/Bronzite-93-low-T-data-and-ideal-cP-calculated-for-the-ideal-composition-The-Fs_Q320.jpg)
We provide detailed background, theoretical and practical, on the specific heat of minerals and mixtures thereof, ‘astro-materials’, as well as background information on common minerals and other relevant solid substances found on the surfaces of solar system bodies. Furthermore, we demonstrate how to use specific heat and composition data for luna...
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![Bronzite [92], low T, data, and ideal cP calculated for the ideal...](publication/362408990/figure/fig5/AS:11431281089396808@1665540178042/Bronzite-92-low-T-data-and-ideal-cP-calculated-for-the-ideal-composition-The-Fs_Q320.jpg)
We provide detailed background, theoretical and practical, on the specific heat of minerals and mixtures thereof, 'astro-materials,' as well as background information on common minerals and other relevant solid substances found on the surfaces of solar system bodies. Furthermore, we demonstrate how to use specific heat and composition data for luna...
The authors carried out petrographic, mineralogical, and chemical analyses (bulk chemical composition and microanalyses of mineral chemical composition) of NWA 4446 carbonaceous chondrite. NWA 4446 chondrite is classified as CV3, S2, W2. This meteorite is a rock fragment most likely from one of the C-type asteroids orbiting the Sun in the outer par...
