单 位：
塔里木大学水利与建筑工程学院;塔里木大学水利与建筑工程学院华北水利水电学院塔里木大学植物科学学院
摘 要：
皮墨垦区位于塔克拉玛干沙漠边缘,是南疆典型的荒漠绿洲,生态极其脆弱。针对该绿洲土壤次生盐渍化发生严重的现状,通过对项目区地下水埋深及地下水矿化度的连续监测,以期研究探讨垦区的地下水盐动态变化规律及水化学特征。初步表明:垦区地下水埋深和矿化度均存在时间和空间上的变化,地下水水化学类型也具有明显的时空分布特征。
译 名：
Dynamic Changes of Water and Salt and It's Chemical Analysis of Groundwater in 224 Farm of Pimo Reclamation Regions
作 者：
XIAO Rang1,SUN Jian1,YE Han-chun1,ZHANG Yong-ling1,ZHENG De-ming2(1.College of Water Resources and Architectural Engineering,Tarim University,Alaer 843300,Xinjiang,China; 2.College of Plant Science and Technology,Tarim University,Alare 843300,Xinjiang,China)
关键词：
Pimo reclamation regions;dynamic of water and salt;groundwater chemistry;groundwater
摘 要：
Because of locating on the edge of the taklamakan desert,Pimo reclamation region is one of the typical dry-desert areas,its ecological environment is frailty.According to a year monitor data of water and salt in Pimo reclamation regions,the dynamic changes of water and salt and chemical characteristics was discussed.The results indicated that Changes of groundwater depth and mineralization existed temporal and spatial rule,meanwhile,so was the chemical characteristics of groundwater.
