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Volume 34 Issue 5
Oct.  2015
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Article Navigation >  CARSOLOGICA SINICA  > 2015  >  34(5): 486-494
LIU Meng-jiao, WANG Yong, ZHANG Yao-hua, LI Guo. Variation characteristics of stable isotopes in different water bodies in Southwestern China monsoon area——A case study of Beibei District,Chongqing[J]. CARSOLOGICA SINICA, 2015, 34(5): 486-494. doi: 10.11932/karst20150509
Citation: LIU Meng-jiao, WANG Yong, ZHANG Yao-hua, LI Guo. Variation characteristics of stable isotopes in different water bodies in Southwestern China monsoon area——A case study of Beibei District,Chongqing[J]. CARSOLOGICA SINICA, 2015, 34(5): 486-494. doi: 10.11932/karst20150509
shu

Variation characteristics of stable isotopes in different water bodies in Southwestern China monsoon area——A case study of Beibei District,Chongqing

doi: 10.11932/karst20150509

  • School of Geographical Sciences,Southwest University

  • Publish Date: 2015-10-25
    Abstract
  • The hydrogen and oxygen isotopes of precipitation water in Beibei District of Chongqing and water in Longtanzi reservoir in upper stream Maanxi were investigated during a hydrologic year (2014) ,to explore the relationship of δD and δ18O between precipitation and the reservoir water.It was found that the correlation between δD and δ18O in the precipitation is extremely significant, namely, δD=8.82δ18O+18.97,r=0.99,n=101,P<0.01.The slope and intercept of local meteoric water line are both greater than the global meteoric water line and China meteoric water line. The result suggested that southwest monsoon and southeast monsoon have alternative influence on local precipitation;(2) Both δD Dandδ18O values in rain water exhibited significant seasonal variations, having lower values in summer and higher ones in winter;(3)The δ value and precipitation as well as temperature assumed negative correlation. The precipitation amount effect of the δD and δ18O in the precipitation was very profound, which concealed the temperature effect;(4)The δD and δ18O in reservoir had a great correlation and they fell near the global meteoric water line and local meteoric water line. In addition, the excess deuterium (d) in the reservoir water and in the precipitation showed very similar patterns. The result indicated that the precipitation recharged the reservoir. However, the variety range of the δD and δ18O from reservoir was far less than precipitation. The result suggested that the reservoir was not only recharged by precipitation, but also by soil water and groundwater.

     

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