Surface structure of Amur region high grade native gold

М. Радомский, S. Radomskiy, V. Radomskaya
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Abstract

The purpose of the research is to study the surface structure of high grade gold. The subject of research is gold ore fields in the Amur region. The object of the study is samples of native high grade gold grains from these fields. The study uses the methods of thermodynamics and X-ray electron microscopy. The study results in revealing a multilayer structure of the surface of high grade minerals of the Amur region native gold with the following levels: a boundary layer with zero oxidation degree Au0 in the form of yellow metallic gold; an oxide layer with the oxidation degree Au+1 in the form of purple Au2O; an oxide layer with the oxidation degree Au+3 in the form of a yellow-brown Au2O3; a hydrated oxide layer with the oxidation degree Au+3 in the form of a red-yellow-brown Au(OH)3. The methods of electron microscopy have allowed to identify external surface structures – dense oxide layers of the form of Au2O3 and loose hydrated layers of the form of Au(OH)3, whereas the inner layers of metallic and monovalent gold are not visible. Important thermodynamic characteristics of the presented levels are the values of standard oxidation-reduction potentials (E°), which determine their physicochemical properties: for metallic gold E° = +1.68 V; for the oxide layer with the oxidation degree Au+1 in the form of Au2O – E° = +0.32 V; for the oxide layer with the oxidation degree Au+3 in the form of Au2O3 – E° = +1.36 V; for the hydrated oxide layer with the oxidation degree Au+3 in the form of Au(OH)3 – E° = +0.7 V. The results of the conducted studies indicate that the surface structure has several layers that lower the oxidation-reduction potential, which explains the generation and formation of migratory forms of gold in humid hypergene conditions of natural environment.
黑龙江地区高品位原生金的表面结构
本研究的目的是研究高品位金的表面结构。本文的研究对象是阿穆尔河地区的金矿田。研究对象是这些矿区的原生高品位金颗粒样品。研究采用了热力学和x射线电子显微镜的方法。研究结果揭示了阿穆尔河地区原生金高品位矿物表面的多层结构,其层次为:以黄色金属金形式存在的零氧化度Au0的边界层;氧化度为Au+1的氧化层,呈紫色Au2O;氧化度为Au+3的氧化层以黄棕色Au2O3的形式存在;氧化度为Au+3的水合氧化层,呈红黄褐色Au(OH)3的形式。电子显微镜的方法已经允许识别外部表面结构- Au2O3形式的致密氧化层和Au(OH)3形式的松散水合层,而金属和单价金的内层是不可见的。标准氧化还原电位(E°)的值决定了它们的物理化学性质:对于金属金E°= +1.68 V;氧化度为Au+1的氧化层形式为Au2O - E°= +0.32 V;氧化度为Au+3的氧化层形式为Au2O3 - E°= +1.36 V;对于氧化度为Au+3的水合氧化层,形式为Au(OH)3 - E°= +0.7 V。研究结果表明,表面结构具有多层结构,降低了氧化还原电位,这解释了金在自然环境湿润的高生条件下迁移形式的产生和形成。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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