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

新疆叶尔羌河流域地下水同位素特征及其补给来源分析
引用本文:武倩倩 任加国 许,模.新疆叶尔羌河流域地下水同位素特征及其补给来源分析[J].中国地质,2008,35(2):331-336.
作者姓名:武倩倩 任加国 许  
作者单位:1. 山东科技大学,山东,青岛,266510
2. 成都理工大学,四川,成都,610059
摘    要:笔者以新疆叶尔羌河流域为例,在研究区水文地质调查的基础上,根据不同区域、不同深度D、~(18)O和T值的变化分析地下水补给来源.解决了传统研究方法很难解决的问题.为干旱地区地下水起源及空间分布规律研究提供了新思路。研究结果表明:(1)研究区地下水不是来自大气降水的直接入渗,而是地表水渗漏补给。(2)流域分为两个独立的地下水循环系统,分别接受叶尔羌河与提孜那甫河河水补给。(3)潜水和承压水的起源相同,属统一的地下水系统。(4)地下水径流表现为倾斜平原区径流强烈,地下水以水平运动为主;细土平原区地下水径流迟缓,地下水以垂直蒸发运动为主.径流方向与地表水流向密切相关。

关 键 词:叶尔羌河流域  环境同位素  地下水  水循环
文章编号:1000-3657(2008)02-0331-06
修稿时间:2007年10月9日

Isotope features and supply sources of groundwater in the Yarkant River drainage area, Xinjiang
WU Qian-qian,REN Jia-guo,XU Mo.Isotope features and supply sources of groundwater in the Yarkant River drainage area, Xinjiang[J].Chinese Geology,2008,35(2):331-336.
Authors:WU Qian-qian  REN Jia-guo  XU Mo
Abstract:On the basis of hydrogeological investigation of the Yarkant River drainage area,Xinjiang,the authors analyze the sources of groundwater recharge according to the variations of D,~(18)O and T values in different regions and at different depths,solve the problem that is difficult to solve with the traditional research approach and provide a new idea for the study of the origin and spatial distribution of groundwater in arid areas.The results indicate that:(1)the groundwater is not derived from direct infiltration of precipitation but from seepage recharge of surface water;(2)there are two independent groundwater circulation systems which receive the waters of the Yarkant River and Tiznap River respectively;(3)the origins of phreatic water and confined water are the same,belonging to a unified groundwater system;and(4)in the sloping plain area the groundwater runoff is strong and groundwater movement is mostly horizontal,while in the fine soil plain area,the groundwater runoff is sluggish with vertical evaporative movement predominating and the runoff direction is closely related to the flow direction of surface water.
Keywords:Yarkant River drainage area  environmental isotope  groundwater  water cycle
本文献已被 CNKI 维普 万方数据 等数据库收录!
点击此处可从《中国地质》浏览原始摘要信息
点击此处可从《中国地质》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