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Surface structure of Amur region high grade native gold
Author(s) -
С. М. Радомский,
В. И. Радомская
Publication year - 2021
Publication title -
nauki o zemle i nedropolʹzovanie
Language(s) - English
Resource type - Journals
eISSN - 2686-7931
pISSN - 2686-9993
DOI - 10.21285/2686-9993-2021-44-1-39-47
Subject(s) - oxide , metal , degree (music) , layer (electronics) , chemistry , materials science , crystallography , nanotechnology , metallurgy , physics , acoustics
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 Au 2 O; an oxide layer with the oxidation degree Au +3 in the form of a yellow-brown Au 2 O 3 ; 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 Au 2 O 3 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 Au 2 O – E° = +0.32 V; for the oxide layer with the oxidation degree Au +3 in the form of Au 2 O 3 – 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.

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