地下水中过量 234U 形成的数学模型

I. V. Tokarev
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引用次数: 0

摘要

天然水中铀-234 的过量(234U/234U 1 与平衡值 1 的活度比)与全球气候的变化相关,在温暖时期增加,在寒冷时期减少。在地下水中发现了 234U/234U 10 的飓风失衡。根据数学模型,这种反常现象是含水层在地质上长期处于冰冻状态以及随后地冰融化形成 "复活 "水的结果。存在于永久冻土岩石中的非冻结膜水分对 234U 过量飓风的形成起了决定性作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Mathematical modeling of the excessive 234U formation in groundwater
Excess of uranium-234 in natural water (ratio 234U/234U 1 in comparison to the equilibrium value as 1 by activity) correlates with global climate variations, increasing during warm and decreasing during cold periods. The hurricane disequilibrium of 234U/234U 10 are found in groundwater. Based on mathematical models, it is shown that such anomalies are the result of a geologically long stay of aquifers in a frozen state in the past and the subsequent melting of ground ice with the formation of “revived” water. Non-freezing film moisture present in permafrost rocks make a decisive contribution to the formation of hurricane 234U excess.
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