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首页> 外文期刊>Russian journal of Pacific geology >Hydrochemistry and genesis of thermal waters of the Goryachii Klyuch spring in Primorskii Krai (Far East of Russia)
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Hydrochemistry and genesis of thermal waters of the Goryachii Klyuch spring in Primorskii Krai (Far East of Russia)

机译:俄罗斯滨海边疆区戈里阿奇克留奇温泉的水化学和成因

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摘要

This report presents original data on the hydrochemical, isotope, and microbiological composition of nitric thermal waters of the Goryachii Klyuch spring (Primorskii Krai). The first-performed year-round surveys of the conditions of the spring water and the environment have shown that the ground waters heated over 30A degrees C in fractured siliceous Upper-Permian rocks suffered no significant seasonal variations in their temperature and discharge during a year, and the slight seasonal variations in the chemical composition of the waters were caused by the interactions in the water-rock system. The isotope studies (delta O-18, delta H-2, and H-3) have shown that the thermal waters were of atmospheric genesis and with a long-term circulation period of > 50 years. The processes of the transition of elements to the solution were decelerated at the absence of soluble rocks and aggressive gases, which caused the low mineralization of the waters. The water temperature was determined by the depth of their circulation amounting to 1-2 km. It was found that the processes of the carbon and nitrogen cycles involving microorganisms were the most intense in the thermal waters.
机译:该报告提供了关于Goryachii Klyuch春季(Primorskii Krai)的硝酸热水的水化学,同位素和微生物组成的原始数据。首次对泉水和环境条件进行了全年的调查,结果表明,断裂的硅质上二叠统岩石中加热到30A摄氏度以上的地下水在一年中温度和流量没有明显的季节性变化,水-化学系统中的相互作用引起水化学成分的轻微季节性变化。同位素研究(δO-18,δH-2和H-3)表明,温泉水是大气成因的,长期循环期大于50年。在没有可溶性岩石和侵蚀性气体的情况下,元素向溶液过渡的过程减速,这导致水的矿化度低。水温由它们的1-2 km的循环深度决定。发现在热水中涉及微生物的碳和氮循环过程最强烈。

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