S. Bortnikova, N. Yurkevich, A. Devyatova, S. S. Volynkin
{"title":"VAPOR-GAS TRANSFER OF CHEMICAL ELEMENTS UNDER LOW-TEMPERATURE CONDITIONS (FIELD AND LABORATORY EXPERIMENTS)","authors":"S. Bortnikova, N. Yurkevich, A. Devyatova, S. S. Volynkin","doi":"10.31554/978-5-7925-0584-1-2020-22-25","DOIUrl":null,"url":null,"abstract":": The article presents the results of a study of the elemental composition of condensates collected at the Ursk sulfide waste heaps (Kemerovo region). The composition of the vapor-gas phase under ambient conditions was compared with the composition obtained in laboratory experiments by heating the waste material to 60°C. Element con-centrations in condensates collected at the waste heaps significantly exceed background values. In the adjacent territory at a distance of 100 and 200 m the metal content does not reach the background. In the condensates of laboratory experiments, many chemical elements were determined, including Au, Zr, Cs, U, Tl. A high positive correlation between the compositions of condensates and the compositions of aqueous extracts extracted from parallel samples was established. This suggests that the sources of elements in condensed gas-vapor streams are secondary sulfates formed during the oxidation of sulfides. The most mobile elements during transport in the vapor – gas phase are alkaline (Li, Cs, Na, K), alkaline earth (Ca, Sr), chalcofilic metals Hg, Zn, Cu, and metalloids As, Sb, Se.","PeriodicalId":208191,"journal":{"name":"WATER-ROCK INTERACTION: GEOLOGICAL EVOLUTION","volume":"76 2 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"WATER-ROCK INTERACTION: GEOLOGICAL EVOLUTION","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.31554/978-5-7925-0584-1-2020-22-25","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
: The article presents the results of a study of the elemental composition of condensates collected at the Ursk sulfide waste heaps (Kemerovo region). The composition of the vapor-gas phase under ambient conditions was compared with the composition obtained in laboratory experiments by heating the waste material to 60°C. Element con-centrations in condensates collected at the waste heaps significantly exceed background values. In the adjacent territory at a distance of 100 and 200 m the metal content does not reach the background. In the condensates of laboratory experiments, many chemical elements were determined, including Au, Zr, Cs, U, Tl. A high positive correlation between the compositions of condensates and the compositions of aqueous extracts extracted from parallel samples was established. This suggests that the sources of elements in condensed gas-vapor streams are secondary sulfates formed during the oxidation of sulfides. The most mobile elements during transport in the vapor – gas phase are alkaline (Li, Cs, Na, K), alkaline earth (Ca, Sr), chalcofilic metals Hg, Zn, Cu, and metalloids As, Sb, Se.