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首页> 外文期刊>Oceanology >Hydrochemical and Atmochemical Mercury Dispersion Zones over Hydrothermal Vents of the Submarine Piip Volcano In the Bering Sea
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Hydrochemical and Atmochemical Mercury Dispersion Zones over Hydrothermal Vents of the Submarine Piip Volcano In the Bering Sea

机译:白令海海底Piip火山热液喷口的水化学和大气化学汞弥散区

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摘要

Signs of mercury input and dispersion in the water mass and the atmosphere over the submarine Piip Volcano have been revealed. The mercury from hydrothermal vents has been found to release mostly as a component of hydrothermal-gas bubbles rising through the water mass to the sea's surface. The mercury's dispersion and the seawater's enrichment with it is a consequence of the partial dissolution of the gas bubbles. The atmochemical dispersion zone is represented by an area of higher mercury concentration with two maximums shifted in the direction of the wind (northeastward) from the northern and southern peak of the volcano.
机译:已经发现了潜艇Piip火山上水团和大气中汞的输入和扩散迹象。已经发现,来自热液喷口的汞主要作为热液气泡的成分释放出来,这些气泡通过水团上升到海面。汞的分散和海水的富集是气泡部分溶解的结果。大气化学物扩散区以汞含量较高的区域表示,其中两个最大值从火山的北峰和南峰沿风向(向东)移动。

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