Experimentally determined parameters of the invariant quasi-binary eutectic reaction L → (Al) + Al8CeCu4 (610 ☌, 14 wt.% Cu and 7 wt.% Ce) were essentially different from those published earlier. It was determined that about 17 wt.% Cu dissolves in Al4Ce the existence of the Al4CeCu phase was not confirmed. Construction of isothermal section of the phase diagram of the YCuSn ternary system at 673 K in the whole concentration range, using X-ray diffraction and EPM analyses. The potential of the model to compute the activities in the case of multicomponent slags was demonstrated. It was shown that Al4Ce (Al11Ce3), Al8CeCu4 and Al2Cu were in equilibrium with the aluminum solid solution (Al). Liquidus and solidus surfaces, three isothermal cross-sections (540, 590 and 200 ☌) and five vertical cross-sections were constructed. Phases and invariant reactions were identified. The structural model used in this work has been extended to predict other properties, such as molar volume, phase diagrams, sulphide capacity and all the thermodynamic properties of binary and ternary silicate systems. n of ZnO FFe 6O 7 in roasting of sulphide ores. Here we develop a deficient ternary metal sulfide (CdIn2S4) photoanode, and its PEC performance is significantly enhanced by introducing surface sulfur vacancies, achieving a photocurrent density. To conclude, the model proposed in this study links melt composition, structure and thermodynamic properties. In ironcopper sulphide ores, umberof ternary phases and also solid solutions of FeS in Cu 6S may form during roasting. The phase relations of the ternary system Bi-Te-S at 500 and 400C were made study by Yusa. Differentsulphide may form solid solutions and even complex sulphides. Аннотация: The phase diagram of the Al-Ce-Cu system in the aluminum-rich corner (concentrations up to 35 wt.% Cu and up to 16 wt.% Ce) was studied. Phase diagram for Bi 2 Te 3-Bi 2 S 3 join in the Bi-Te-S system above 450C (modified after Yusa 19797)).Местоположение издательства: Netherlands A phase diagram in physical chemistry, engineering, mineralogy, and materials science is a type of chart used to show conditions at which thermodynamically distinct phases (such as solid, liquid or gaseous states) occur and coexist at equilibrium.
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