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Strontium isotopic geochemistry of the Changjiang estua-rine waters: Implications for water-sediment interaction
作者姓名:王中良  刘丛强  韩贵琳  徐志方
作者单位:WANG Zhongliang LIU CongqiangHAN Guilin & XU ZhifangState Key Laboratory of Environmental Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences,Guiyang 550002,China;Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100101,China
基金项目:This research was supported jointly by the Outstanding Young Scientists Foundation (Grant No.49625304),the Ministry of Science and Technology of China (Grant No. 95-pre-39). Special thank go to Professor Qiao Guangsheng for his assistance in Sr isotopi
摘    要:The Sr concentrations and 87Sr/86Sr ratios have been measured for the Changjiang es-tuarine waters with a main purpose to understand physical and chemical processes at the estuary. The result shows that the Changjiang River water has higher Sr concentration (150 ng/g) and lower 87Sr86Sr ratio (0.7105) when compared with the average values (0.7119 for 87Sr/86Sr and 78ppb for Sr, respectively) of large world rivers. In the mixing process, no simple mixing of two end-members has been found according to the variations of Sr concentration and isotope ratios. There is an abrupt rise of Sr isotope ratios at the salinity about 1 mg/g during river-sea water mixing at the estuary. This abrupt rise of Sr isotope ratios is mostly ascribed to the strong water-sediment interaction, because there exists the same rise of suspended particulate materials due to energetic resuspension of bottom sediments.


Strontium isotopic geochemistry of the Changjiang estua-rine waters: Implications for water-sediment interaction
WANG Zhongliang,LIU CongqiangHAN Guilin,& XU ZhifangState Key Laboratory of Environmental Geochemistry.Strontium isotopic geochemistry of the Changjiang estua-rine waters: Implications for water-sediment interaction[J].Science in China(Technological Sciences),2001(Z1).
Authors:WANG Zhongliang  LIU CongqiangHAN Guilin  & XU ZhifangState Key Laboratory of Environmental Geochemistry
Affiliation:WANG Zhongliang LIU CongqiangHAN Guilin & XU ZhifangState Key Laboratory of Environmental Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences,Guiyang 550002,China,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100101,China
Abstract:The Sr concentrations and 87Sr/86Sr ratios have been measured for the Changjiang es-tuarine waters with a main purpose to understand physical and chemical processes at the estuary. The result shows that the Changjiang River water has higher Sr concentration (150 ng/g) and lower 87Sr86Sr ratio (0.7105) when compared with the average values (0.7119 for 87Sr/86Sr and 78ppb for Sr, respectively) of large world rivers. In the mixing process, no simple mixing of two end-members has been found according to the variations of Sr concentration and isotope ratios. There is an abrupt rise of Sr isotope ratios at the salinity about 1 mg/g during river-sea water mixing at the estuary. This abrupt rise of Sr isotope ratios is mostly ascribed to the strong water-sediment interaction, because there exists the same rise of suspended particulate materials due to energetic resuspension of bottom sediments.
Keywords:87Sr/86Sr  Changjiang estuary  mixing  water-sediment interaction  
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