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含氢地下水,即氢浓度增高的水(超过36爱曼),系矿水的一种,它可用于矿泉医疗。假如对地下水中氢的底数浓度和异常浓度的形成条件有正确的概念,那么这种水也能作为寻找放射性矿床的普查标志。促成地下水氢的富集的基本因素之一是被地下水冲洗的岩石中镭的绝对含量。但是,目前对岩石中放射性元素分布规律的知识尚很有限。尼柯诺夫认为,近十年来总趋势是:过去采用过的岩石中放射性元素含量值是下降,而且接近岩浆岩和沉积岩的平均值。从尼柯諾夫文章中借用的、并经维诺格拉多夫的资料加以补充的表l
Hydrogen-containing groundwater, which is an increase in the concentration of hydrogen (more than 36 amman), is a type of mineral water that can be used in mineral springs. This water can also serve as a census marker for radioactive mineral deposits provided that there is a correct concept of formation of base and concentration of hydrogen in groundwater. One of the basic factors contributing to the enrichment of groundwater hydrogen is the absolute content of radium in rocks washed by groundwater. However, the current knowledge of the distribution of radioactive elements in rocks is limited. Nikonov believes that the general trend in the last decade is that the radioactive element content of the rocks used in the past is decreasing and is close to the average of magmatic rocks and sedimentary rocks. Table l borrowed from Nikonov’s article and supplemented by Vinogradov’s material