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Atmochemical mercury dispersion aureoles over active geologic structures of the northern Sea of Japan

机译:日本北海活跃地质结构上的大气化学汞弥散金

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摘要

In the autumn of 2010, contrasting dispersion aureoles of atomic mercury were revealed in the northern Sea of Japan, in the vicinity of the Vityaz' and Alpatov Rises. Based on the elimination method, the assumption is made that the aureoles resulted from the supply of mercury from hydrothermal or water-gas bottom sources through the sea water column, either in gas bubbles or as a result of diffusion and turbulent mixing. It is inferred that gas-mercury measurements can be used in geological research in sea water areas. (C) 2014, V.S. Sobolev IGM, Siberian Branch of the RAS. Published by Elsevier B.V. All rights reserved.
机译:2010年秋天,在日本北部海中Vityaz'和Alpatov Rises附近发现了对比鲜明的原子汞分散金黄色。根据消除方法,可以假设,由于气泡是由气泡或扩散和湍流混合作用而产生的,因此,金黄色的原子是通过热水塔或水煤气塔底源通过海水塔供应的汞产生的。可以推断,气汞测量可用于海水区域的地质研究。 (C)2014,V.S. Sobolev IGM,RAS的西伯利亚分公司。由Elsevier B.V.发布。保留所有权利。

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