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鲁南两城地区水的铀同位素研究及其应用
引用本文:赵树森,吴爱民.鲁南两城地区水的铀同位素研究及其应用[J].岩石学报,1994,10(2):202-210.
作者姓名:赵树森  吴爱民
作者单位:中国科学院地质研究所,山东地矿局第三水文及工程地质队
摘    要:用天然水溶液中234U与238U之间的放射性不平衡研究的方法,对鲁南两城地区30组水样地表水和地下水铀同位素组分进行了实测。结果表明,本区地下水有三个来源:深部喀斯特岩溶水、浅部孔隙水和地表水。水的铀同位素组分稳定,并应用混合比例计算了地下水资源量,其结果与常规方法计算结果完全一致。

关 键 词:铀同位素,地表水,地下水,山东

A STUDY AND ITS APPLACATION OF URANIUM ISOTOPE IN UNDERGROUND AND SURFACE WATER FROM LIANGCHENG AREA,SUOTHERN SHANDONG PROVINCE
Zhao Shusen,Liu Minglin and Qiao Guangsheng.A STUDY AND ITS APPLACATION OF URANIUM ISOTOPE IN UNDERGROUND AND SURFACE WATER FROM LIANGCHENG AREA,SUOTHERN SHANDONG PROVINCE[J].Acta Petrologica Sinica,1994,10(2):202-210.
Authors:Zhao Shusen  Liu Minglin and Qiao Guangsheng
Abstract:Determination of uranium isotope contents has been made by the method of radioactive disequilibrium between 234U and 238U for the surface and underground water from Liangcheng region of southern Shandong Province, and the results of 30 water samples analyses are presented.These results show that the underground water has three sources, namely deep karst, shallow porous and surface waters. The uranium isotopic compositions of water are quite stable, and the mixing ratio of water body has been used to evaluate the amount of water resource in considered area.The results of calculation is of the same with those obtained by other regular method.
Keywords:Uranium isotope  Underground water  Surface water  Shandong provingce
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