首页 | 本学科首页   官方微博 | 高级检索  
     检索      

罗布泊盐湖晶间卤水运动特征及其动力学分析
引用本文:焦鹏程,刘成林,王弭力,陈永志,王新民.罗布泊盐湖晶间卤水运动特征及其动力学分析[J].地球学报,2003,24(3):255-260.
作者姓名:焦鹏程  刘成林  王弭力  陈永志  王新民
作者单位:中国地质科学院水文地质环境地质研究所,河北正定,050803;中国地质科学院矿产资源研究所,北京,100037; 北京大学城市与环境学系,北京,100871;中国地质科学院矿产资源研究所,北京,100037;中国地质科学院矿产资源研究所,北京,100037;新疆地质矿产局第三地质大队,新疆库尔勒,841000
基金项目:国土资源部科技项目(编号:992025),国家科技攻关305项目(编号:96-915-08-05),地质调查项目(编号:DKD2002002)
摘    要:根据地下水运动的一般规律,阐述了罗布泊盐湖钙芒硝储卤层及富钾卤水的特性,并讨论了该卤水层的变化特性。在罗布泊干盐湖区采用^14C测年技术、人工放射性同位素技术和化学示踪技术,研究晶间卤水循环速率、卤水渗流方向及渗透流速与实际流速,揭示罗布泊盐湖晶间卤水处于缓慢的流动及交替状态。探讨了新构造活动、古气候变化、地层静压力作用、深部地层水及大气降水补给作用等因素对罗布泊盐湖晶间卤水运动的控制和影响,提出了晶间卤水的运动模式。

关 键 词:罗布泊盐湖    晶间卤水    水运动

Characteristics and Dynamic Analysis of Inter-Crystal Brine Movement in the Lop Nur Salt Lake
JIAO Peng-cheng,LIU Cheng-lin,WANG Mi-er,CHEN Yong-zhi and WANG Xin-min.Characteristics and Dynamic Analysis of Inter-Crystal Brine Movement in the Lop Nur Salt Lake[J].Acta Geoscientia Sinica,2003,24(3):255-260.
Authors:JIAO Peng-cheng  LIU Cheng-lin  WANG Mi-er  CHEN Yong-zhi and WANG Xin-min
Institution:Institute of Hydrogeology and Environmental Geology, CAGS, Zhengding, Hebei 050803;Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037; Department of Municipality and Environmental Sciences, Peking University, Beijing 100871;Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037;Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037;No.3 Geological Party, Xinjiang Bureau of Geology and Mineral Resourses, Karla, Xinjiang, 841000
Abstract:Based on general movement regularity of underground water, this paper describes in detail physical characteristics of brine aquifers and dynamic properties of brine movement as well as their variation in Luobei depression lying in the northeast of Lop Nur, Xinjiang. With such means as 14C-dating, I 131 technique and chemical tracing technique, the authors studied the rate of circulation, the flowing direction, the vadose velocity and the actual flowing velocity of inter-crystal brine in Luobei playa, thus revealing the chronic flowing and exchange state of the inter-crystal brine. In addition, it is shown that various factors such as neotectonic activity, paleoclimate change, hydrostatic pressure of strata, oilfield water and precipitated water have exerted controlling influence on the movement of inter-crystal brine. Finally, a model of inter-crystal brine is suggested.
Keywords:Lop Nur salt lake  inter-crystal brine  movement of underground water
本文献已被 万方数据 等数据库收录!
点击此处可从《地球学报》浏览原始摘要信息
点击此处可从《地球学报》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号