{"title":"赤塔tpp-1排土场入渗效应区水中硅迁移形式(热力学评价)","authors":"L. Zamana, L. I. Usmanova","doi":"10.31554/978-5-7925-0584-1-2020-227-230","DOIUrl":null,"url":null,"abstract":": As a result of thermodynamic calculations using the HydroGeo 32 program, the possible forms of the presence of dissolved silicon in the waters of the settling tank of the Chita TPP-1 hydraulic ash dump and groundwater in the zone of its influence due to infiltration losses are determined. At Si concentrations of 2.1–17.8 mg/L, of the avail-able forms in the program, (HSi 2 O 6 ) 3 – is predominant, the contents of H 4 SiO 4 and SiO 2 following it are 6–8 orders of magnitude lower. The minimum calculated concentrations ( n 10 –21 mg/L) were obtained for (Si 2 O 5 ) 2 – and (SiO 4 ) 4– ions at pH 7.20.","PeriodicalId":208191,"journal":{"name":"WATER-ROCK INTERACTION: GEOLOGICAL EVOLUTION","volume":"19 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"FORMS OF SILICON MIGRATION IN WATERS IN THE ZONE OF INFILTRATION EFFECT OF THE CHITA TPP-1 ASH DUMP (THERMODYNAMIC ASSESSMENT)\",\"authors\":\"L. Zamana, L. I. Usmanova\",\"doi\":\"10.31554/978-5-7925-0584-1-2020-227-230\",\"DOIUrl\":null,\"url\":null,\"abstract\":\": As a result of thermodynamic calculations using the HydroGeo 32 program, the possible forms of the presence of dissolved silicon in the waters of the settling tank of the Chita TPP-1 hydraulic ash dump and groundwater in the zone of its influence due to infiltration losses are determined. At Si concentrations of 2.1–17.8 mg/L, of the avail-able forms in the program, (HSi 2 O 6 ) 3 – is predominant, the contents of H 4 SiO 4 and SiO 2 following it are 6–8 orders of magnitude lower. The minimum calculated concentrations ( n 10 –21 mg/L) were obtained for (Si 2 O 5 ) 2 – and (SiO 4 ) 4– ions at pH 7.20.\",\"PeriodicalId\":208191,\"journal\":{\"name\":\"WATER-ROCK INTERACTION: GEOLOGICAL EVOLUTION\",\"volume\":\"19 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/10.31554/978-5-7925-0584-1-2020-227-230\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"WATER-ROCK INTERACTION: GEOLOGICAL EVOLUTION","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.31554/978-5-7925-0584-1-2020-227-230","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
FORMS OF SILICON MIGRATION IN WATERS IN THE ZONE OF INFILTRATION EFFECT OF THE CHITA TPP-1 ASH DUMP (THERMODYNAMIC ASSESSMENT)
: As a result of thermodynamic calculations using the HydroGeo 32 program, the possible forms of the presence of dissolved silicon in the waters of the settling tank of the Chita TPP-1 hydraulic ash dump and groundwater in the zone of its influence due to infiltration losses are determined. At Si concentrations of 2.1–17.8 mg/L, of the avail-able forms in the program, (HSi 2 O 6 ) 3 – is predominant, the contents of H 4 SiO 4 and SiO 2 following it are 6–8 orders of magnitude lower. The minimum calculated concentrations ( n 10 –21 mg/L) were obtained for (Si 2 O 5 ) 2 – and (SiO 4 ) 4– ions at pH 7.20.