摘要
通过对巴仑马海钾矿区地下水的补给、径流、排泄条件分析,说明在均衡计算时段内,地下水处于正均衡,地下水质大部分地段出现淡化现象。通过钾矿区主要盐份的均衡概算,说明主要盐份还处于积累中,成矿作用仍在继续。
Through the analyses of conditions of groundwater recharge, runoff, drainage in Balunmahai potash mine area, it was accounted that the underwater was in positive balance, and the underwater in a majority of area was desalted during the calculation of balance. Through the balance budgetary estimation of main salt components, it was accounted that main salt components were still in accumulation, the mineralization was still in continuation.
出处
《化工矿物与加工》
CAS
北大核心
2006年第7期5-7,24,共4页
Industrial Minerals & Processing
关键词
地下水
水盐均衡
概算
groundwater
salt and water balance
budgetary estimation