锂同位素测速法在察尔汗水动态中的应用  

Application of the Method for Determination of the Velocity by Lithium Isotopes in Water Regime Investigation in Chaerhan

作　　者：肖应凯[1] 刘卫国[1] 王蕴慧[1] 祁海平[1] 周引民[1] 

机构地区：[1]中国科学院青海盐湖研究所,西宁810008

出　　处：《盐湖研究》1999年第4期1-8,共8页Journal of Salt Lake Research

摘　　要：采用锂同位素示踪技术，对察尔汗首采区采卤过程中晶间卤水的流向、流速和流量进行了测定。研究的初步结果表明，锂同位素示踪技术在地下水动态的研究中具有较好的应用前景。The direction,velocity and capacity of brine flowing through a well have been measured using lithium isotopic trace and isotopic dilution mass spectrometry.The perliminary results show that the technology of isotopic trace of lithium can be used in water regime investigation of groundwater.\;

关 键 词：锂同位素 水动态 地下水 钾 镁 盐矿床 盐湖 

分 类 号：P641.3[天文地球—地质矿产勘探] P641.464[天文地球—地质学]