2019
DOI: 10.1051/e3sconf/20199805004
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Transfer of chemical elements in vapor-gas streams at the dehydration of secondary sulfates

Abstract: The elemental composition of vapor-gas streams obtained during heating of secondary hydrous sulfates are presented. Samples of abundant sulfate intergrowth were collected at the Belovo waste heaps and heated at 60ºC in experiments to collect condensates of the releasing vapor-gas streams. A wide spectrum of major and trace elements was determined in the condensate. Chemical elements can be absorbed by the water vapor and migrate with this phase during the dehydration of hydrous sulfates. To determine the mecha… Show more

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Cited by 2 publications
(1 citation statement)
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“…The concentrations of elements in condensates from solids increased depending on the oxidation state of the tailings matter, and there is a direct correlation with the amount of water-soluble species of elements [34]. It was shown that secondary sulfates forming on tailings surfaces can be a significant source of chemical elements because of their volatilization and transport by vapor-gas flows [34][35][36]. The investigation of sulfates and hydrated sulfate minerals plays a key role in the interpretation of the hydrochemical history of anthropogenic toxic tailings (and rock dumps) [36][37][38][39][40][41].…”
Section: Introductionmentioning
confidence: 99%
“…The concentrations of elements in condensates from solids increased depending on the oxidation state of the tailings matter, and there is a direct correlation with the amount of water-soluble species of elements [34]. It was shown that secondary sulfates forming on tailings surfaces can be a significant source of chemical elements because of their volatilization and transport by vapor-gas flows [34][35][36]. The investigation of sulfates and hydrated sulfate minerals plays a key role in the interpretation of the hydrochemical history of anthropogenic toxic tailings (and rock dumps) [36][37][38][39][40][41].…”
Section: Introductionmentioning
confidence: 99%