25℃和大气压下Ag-Au-Se-Te体系的热力学平衡

IF 0.8 4区 化学 Q4 CHEMISTRY, PHYSICAL
O. V. Eremin, G. A. Yurgenson, E. S. Epova
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引用次数: 0

摘要

Ag-Au-Se-Te体系中矿物的标准吉布斯形成能是用加性元素贡献来计算的。在25℃和常压下,用选择程序(PC)计算了一摩尔贵金属和可变硫含量的初始状态下所考虑的系统的热力学平衡。模拟结果表明,银比金更积极地参与矿物组成。在一定浓度的硒和碲下,贵金属不会产生天然形式。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Thermodynamic Equilibria in the Ag–Au–Se–Te System at 25°C and Atmospheric Pressure

Standard Gibbs energies of formation for minerals of the Ag–Au–Se–Te system are calculated using additive elemental contributions. Thermodynamic equilibria of the considered system in the initial state of one mole of noble metals and variable chalcogen contents at 25°C and atmospheric pressure are calculated using the Selector program compleх (PC). Results from modeling show that silver participates more actively than gold in the composition of the minerals. Noble metals do not produce native forms at certain concentrations of selenium and tellurium.

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来源期刊
CiteScore
1.20
自引率
14.30%
发文量
376
审稿时长
5.1 months
期刊介绍: Russian Journal of Physical Chemistry A. Focus on Chemistry (Zhurnal Fizicheskoi Khimii), founded in 1930, offers a comprehensive review of theoretical and experimental research from the Russian Academy of Sciences, leading research and academic centers from Russia and from all over the world. Articles are devoted to chemical thermodynamics and thermochemistry, biophysical chemistry, photochemistry and magnetochemistry, materials structure, quantum chemistry, physical chemistry of nanomaterials and solutions, surface phenomena and adsorption, and methods and techniques of physicochemical studies.
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