Features of hydrogeochemistry of natural waters the tracts of the Kastropol (southern coast of the Crimean peninsula)

A. Maksimova
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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.
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克里米亚半岛南岸卡斯特罗波尔天然水域水文地球化学特征
本文介绍了卡斯特罗波尔天然水域的水文地球化学综合研究。研究水体主要以HCO -Ca和HCO - mg -Ca组成为特征,总矿化度在220 ~ 2306 mg/dm之间,硅含量在0.78 ~ 6.08之间。环境的地球化学参数变化范围从还原到氧化,Eh在-146,6 ~ +275,9 mV之间;pH值为7,4至8,5,O值为1,80至7,73 mg/dm。根据Ca/Na、Ca/Mg和Si/Na关系不同的地球化学系数,将天然水体划分为两个地球化学类群。B、Br、I、Re、Au在水中聚集。Li, B, Sr, Re和Au在溶液中有很强的迁移能力。根据水体重金属污染指标,确定了Partizanskoye村井水富集程度较高。
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