地理科学

地理科学 ›› 1996, Vol. 16 ›› Issue (3): 224-231.doi: 10.13249/j.cnki.sgs.1996.03.224

• 论文 • 上一篇    下一篇

潍河下游地区海咸水入侵动态系统分析

陈鸿汉1, 张永祥2, 王新民3, 任仲宇4   

  1. 1. 中国矿业大学北京研究生部, 北京100083;
    2. 南京大学, 南京210008;
    3. 长春地质学院, 长春130026;
    4. 建设部城市地下水资源研究中心, 北京100007
  • 收稿日期:1995-06-18 修回日期:1995-09-11 出版日期:1996-05-20 发布日期:1996-05-20

ANALYSIS OF SEA-SALT WATER INTRUSION DYNAMIC SYSTEM IN THE LOWER REACHES OF THE WEIHE RIVER

Chen Honghan1, Zhang Yongxiang2, Wang Xinmin3, Ren Zhongyu4   

  1. 1. China Mining university, Beijing 100083;
    2. Department of the Earth Sciences, NanJing University, Nanjing 210008;
    3. Department of Hydrogeology and Engineering geology, Changchun College of Geology, Changchun 130026;
    4. Ground water Resources Research Center, Ministry of Construction, Beijing 100007
  • Received:1995-06-18 Revised:1995-09-11 Online:1996-05-20 Published:1996-05-20

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9 | 2

摘要： 以潍河下游为研究区,采用趋势面分析等数理统计方法对海咸水入侵历史、现状及其发展规律进行定量研究,指出产生海咸水入侵的根本原因是由于过量开采地下淡水资源,必须科学控制地下淡水资源开采量,以防治海咸水入侵

Abstract: In this thesis, with the method of trend system analysis, the history, present status, development law and hydro chemical characteristics of sea-salt water intrusion are systematically and quantitatively researched in the lower reaches of the Weihe River. The result indicates that the over exploitation of fresh water resources is the basic reason of sea-salt water intrusion, and the hydro-chemical dynamics is the important factor. The exploitation of fresh water resource must be scientifically controlled, in order to prevent and govern the sea-salt water inrtusion.