非均质裂隙渗流场研究中的水化学方法  

Hydrochemical Methods for Study Water Flow in Heterogenous Featured Aquifers

作　　者：陈友媛[1] 惠二青[1] 郑西来[1] 邱汉学[1] 

机构地区：[1]青岛海洋大学地球科学学院,青岛266003

出　　处：《青岛海洋大学学报（自然科学版）》2002年第5期757-762,共6页Journal of Ocean University of Qingdao

摘　　要：采用水化学分析、氢氧同位素示踪和氯离子质量平衡法相结合的手段 ,对非洲博茨瓦纳的帕拉匹水源地的地下水资源进行分析。结果表明该水源地有 2层水化学类型不同的含水层 ,即茨瓦蓬和鲁村纳 2个含水层 ,而且地下水主要在裂隙网络中运动。氢氧同位素示踪说明茨瓦蓬含水层的地下水主要来源于未受强烈蒸发的大气降水补给 ,用氯离子质量平衡法计算大气降水补给每年约 17mm。In this paper the combination of the hydrochemical analyses,environmental isotope ( δ 2 H and δ 18 O) and chloride mass balance method, to analyze groundwater resources in Palapye wellfield, Botswana, is reported. The result indicates that there are two types of different hydrochemical aquifers. One is Tswapong aquifer, and the other is Lostane aquifer. Groundwater mainly flows in featured connectivity web. Hydrogen and oxygen isotope show that groundwater in Tswapong aquifer is mainly from precipitation. Groundwater recharge rate is estimated at 17mm/a by using chloride mass balance method.

关 键 词：非均质裂隙渗流场 水化学 帕拉匹水源地 氯离子 质量平衡法 氢同位素 氧同位素 

分 类 号：P342[天文地球—水文科学]