地理科学 ›› 1993, Vol. 13 ›› Issue (3): 273-278,296.doi: 10.13249/j.cnki.sgs.1993.03.273

• 研究报道 • 上一篇    下一篇

海南岛雨水、河水、地下水氢氧稳定同位素特征及其关系

陈静生, 王忠   

  1. 北京大学环境科学中心 北京 100871
  • 收稿日期:1993-01-01 出版日期:1993-05-20 发布日期:1993-05-20
  • 基金资助:
    国家自然科学基金

A STUDY ON STABLE ISOTOPES OF HYDROGEN AND OXYGEN IN RAIN WATER, RIVER WATER AND GROUNDWATER FROM HAINAN ISLAND OF CHINA

Chen Jingsheng, Wang Zhong   

  1. The Centre for Environmental Studies, Peking University, Belling 100871
  • Received:1993-01-01 Online:1993-05-20 Published:1993-05-20

摘要: 通过海南岛若干地点1990年夏季雨水、河水及地下水氢氧稳定同位索的测定,探讨了其与大陆降水同位素的比较,及岛内水的同位素分布特征,并试图应用同位素方法探讨岛上若干地点雨水、河水、地下水之间的相互关系。

Abstract: This paper deals with the stable isotopes of hydrogen and oxygen in rain water, river water and groundwater from Hainan Island of China. Water samples were collected in summer season of 1990. Results show: 1. The δD values of rain water samples from Hainan Island are much lower than δD values which were obtained by extrapolation from the distrbution tendency of δD values in rain water of the mainland China. The elope of the meteoric water line in Hainan Island is also much lower than that in the mainland China. 2. The δD and δ18O contentes of rain water, river water, and groundwater in eastern and southern areas are little higher than those in western and northern areas. The δD and δ18O contents in rain water, river water and groundwater decrease from low altitude to high altitude. The similarity of δD and δ18O of distribution of contentes in rain water, river water and groundwater, indicates the co-genesis of rain water, river water and groundwater in Hainan Island. 3. Data calculated by the isotope mixture equation showthat after each rain period the recharge of rain into streams is much higher than the recharge of rain into groudwater. This fact may lead to the shortage of groundwater resource in Hainan Island.