Abstract
Sea water samples, still hot from volcanic emanations were taken in a bay of Nishinoshima-Shinto Island just after volcanic activity had ceased and were analysed for borate-B, fluoride-F and bromide-Br. The hot water is considered to be formed by the conservative mixing of volcanic emanations with sea water, and the emanations containedCl, B, F andBr in the ratio of 1∶1.84×10−3∶0.474×10−3∶6.47×10−3 by weight.
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