阿尔泰共和国乌拉甘斯基地区阿克塔什汞矿床地区积雪成分特征

V. Malov, M. Gustaitis, I. N. Myagkaya, B. Saryg-ool, O. N. Surkov, E. Lazareva
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引用次数: 0

摘要

注:阿克塔什汞矿床区域积雪成分为Ca-Mg-HCO 3型和ca - mg - so4hco 3型。雪中含有大量的固体颗粒(19.2 ~ 1031.1 mg / L),是雪矿化的主要来源。境内积雪中汞的总含量与采样地点有很强的相关性,变化幅度为3个数量级(0.05 ~ 16 μg / L),积雪中汞的主要形式是以胶体组分溶解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
FEATURES OF THE SNOW COVER COMPOSITION IN THE AKTASH MERCURY DEPOSIT REGION (ULAGANSKY DISTRICT, ALTAI REPUBLIC)
ANNOTATION: The snow composition of the region in the Aktash mercury deposit is Ca-Mg-HCO 3 and Ca-Mg-SO 4 HCO 3 type. Total dissolved solids varies from 12.5 to 35.5 mg / L. Snow contains large amount of solid particles (19.2-1031.1 mg / L) that are the main source of snow mineralization. The total content of mercury in snow of the territory strongly depends on the sampling place and varies by 3 orders of magnitude (0.05-16 μg / L). The predominant Hg form in snow is dissolved with colloids fraction.
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