地理科学

地理科学 ›› 2000, Vol. 20 ›› Issue (3): 236-240.doi: 10.13249/j.cnki.sgs.2000.03.236

• 论文 • 上一篇    下一篇

我国河水主要离子组成与区域自然条件的关系

张利田1, 陈静生2   

  1. 1. 中山大学城市与资源规划系, 广东广州510275;
    2. 北京大学城市与环境学系, 北京100871
  • 收稿日期:1999-05-25 修回日期:1999-10-08 出版日期:2000-05-20 发布日期:2000-05-20
  • 基金资助:
    广东省自然科学基金项目(994112)资助.

The Relationship Between the Composition of the Major Ion of River of China and Regional Natural Factors

ZHANG Li-tian1, CHEN Jing-sheng2   

  1. 1. Department of City Rsources Planning, Zhongshan Universisty, Guangzhou, Guangdong 510275;
    2. Department of Urban & Environmental Sciences, Peking University, Beijing 100871
  • Received:1999-05-25 Revised:1999-10-08 Online:2000-05-20 Published:2000-05-20

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42

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被引次数

80

摘要： 对我国四大水系-长江、黄河、松花江和珠江50年代末至80年代中期河水中主要离子含量与流域降水量、区域地质岩性等自然条件进行了统计研究.研究表明:区域地质岩性对河水离子含量和组成有显著影响;河水离子总量与相应区域的降水量存在显著负相关关系.

Abstract: According to major ion content data of the Yangtze River, Yellow River, Songhua River and Preal River systems from 1959 to 1985, regional rainfall data and lithology data, the relationship between the characteristics of major ion chemistry and natural factors such as regional climate and lithology has been analyzed through statistics methods. The conclusions reached are as follows. The ion content of river water and the composition of river water are remarkably controlled by rational rock dissolution. The total ion contents of river water are remarkably negatively correlated with regional rainfall.

中图分类号: 

  • X143