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Water Isotopic-Geochemical Composition in the Trekhtsvetnoe Meromictic Lake on the White Sea Coast

机译:白海沿岸Trekhtsvetnoe微生物湖中的水同位素地球化学组成

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摘要

The isotopic features of Lake Trekhtsvetnoe in the White Sea coast area were studied in 2012-2015 in both winter and summer. Lake Trekhtsvetnoe is a water body, separating from the sea, with constant vertical stratification throughout the observation period. Its isotopic, hydrophysical, and biological characteristics have been studied. By the isotopic profile of lake water body, three zones can be identified in the lake: (1) 0-1 m: mixolimnion zone with delta O-18 varying from -12 to -11.1 parts per thousand; (2) 1.0-3.0 m: zone with transitional properties with delta O-18 varying from -11.1 to -5.5 parts per thousand; (3) 3.0-7.6 m: monimolimnion zone with highest values of delta O-18-from -5.5 to -4.7 parts per thousand.
机译:在2012-2015年的冬季和夏季,研究了白海沿岸地区Trekhtsvetnoe湖的同位素特征。 Trekhtsvetnoe湖是一个水体,与海分离,在整个观测期内具有恒定的垂直分层。已经对其同位素,水物理和生物学特性进行了研究。根据湖泊水体的同位素分布,可在湖泊中识别出三个区域:(1)0-1 m:δO-18含量在-12至-11.1千分之一之间的混合寡聚带; (2)1.0-3.0 m:具有过渡特性的区域,δO-18范围从-11.1到-5.5千分之几; (3)3.0-7.6 m:δO-18最高值的单imolimnion区域--5.5至-4.7千分之几。

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