{"title":"Features of hydrogeochemistry of natural waters the tracts of the Kastropol (southern coast of the Crimean peninsula)","authors":"A. Maksimova","doi":"10.33764/2618-981x-2022-2-1-223-232","DOIUrl":null,"url":null,"abstract":"This paper presents comprehensive hydrogeochemical studies of the natural waters the tracts of the Kastropol. The studied waters are mainly characterized by HCO Ca and HCO Mg-Ca composition with total mineralization, which varies from 220 to 2306 mg/dm and silicon content from 0,78 to 6,08. The geochemical parameters of the environment vary from the reductive to oxidative setting with Eh from -146,6 to +275,9 mV; pH from 7,4 to 8,5, and O from 1,80 to 7,73 mg/dm. Natural waters were divided into two geochemical groups by geochemical coefficients that differ from each other in their relations Ca/Na, Ca/Mg and Si/Na. B, Br, I, Re и Au accumulate in the waters. Li, B, Sr, Re and Au have a very strong migration ability in solution. According to the indices of water pollution with heavy metals, a high degree of enrichment of the waters of wells in the Partizanskoye village was established.","PeriodicalId":13672,"journal":{"name":"Interexpo GEO-Siberia","volume":"23 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2022-05-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Interexpo GEO-Siberia","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.33764/2618-981x-2022-2-1-223-232","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
This paper presents comprehensive hydrogeochemical studies of the natural waters the tracts of the Kastropol. The studied waters are mainly characterized by HCO Ca and HCO Mg-Ca composition with total mineralization, which varies from 220 to 2306 mg/dm and silicon content from 0,78 to 6,08. The geochemical parameters of the environment vary from the reductive to oxidative setting with Eh from -146,6 to +275,9 mV; pH from 7,4 to 8,5, and O from 1,80 to 7,73 mg/dm. Natural waters were divided into two geochemical groups by geochemical coefficients that differ from each other in their relations Ca/Na, Ca/Mg and Si/Na. B, Br, I, Re и Au accumulate in the waters. Li, B, Sr, Re and Au have a very strong migration ability in solution. According to the indices of water pollution with heavy metals, a high degree of enrichment of the waters of wells in the Partizanskoye village was established.