Abstract
Interaction of metallic gold with (Na, K)Cl salt melts was investigated by the weight-loss method at 700–1000°C using silica glass ampoules. Interaction was not detected in hermetic evacuated ampoules over the whole temperature interval and even after the addition of 5 wt % Na2SO4 as a possible oxidizer to the salt. Gold solubility increased sharply in open ampoules, but this was accompanied by the evaporation of salt melt and, possibly, AuCl x . The limiting gold solubility in the salt melt at 860°C was estimated as 1 wt % or 10000 ppm. The model of gold transport in a gas phase during magmatic degassing invokes shallow gold extraction by salt melt, melt evaporation, and removal of precipitated metallic particles by the gas phase.
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Original Russian Text © K.I. Shmulovich, P.G. Bukhtiyarov, E.S. Persikov, 2016, published in Geokhimiya, 2016, No. 11, pp. 1015–1024.
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Shmulovich, K.I., Bukhtiyarov, P.G. & Persikov, E.S. Gold transport during magmatic degassing: Model experiments. Geochem. Int. 54, 979–988 (2016). https://doi.org/10.1134/S0016702916090093
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DOI: https://doi.org/10.1134/S0016702916090093