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Genesis of Sr Isotopes in Groundwater of Hebei Plain
Authors:Ye Ping  Zhou Aiguo  Liu Cunfu  Cai Hesheng  Gan Yiqun  Li Xiaoqian  Jin Qinsheng
Institution:1. School of Environmental Studies, China University of Geosciences, Wuhan 430074, China
2. Central Southern China Electric Power Design Institute, Wuhan 430071, China
Abstract:To analyze the genesis of Sr isotopes in groundwater of Hebei plain, time-accumulative effect of 87Sr/86Sr ratio was studied. It is shown that 87Sr/86Sr ratio increases with the increasing age and depth of groundwater and has a positive correlation to 4Heece and a negative correlation to δ18O and δD. The groundwater is divided into three groups to discuss the relation between 87Sr/86Sr ratio and Sr2+ content:
></figure> moderate Sr<sup>2+</sup> content and higher <sup>87</sup>Sr/<sup>86</sup>Sr ratio (water I); <figure class=></figure> lower Sr<sup>2+</sup> content and higher <sup>87</sup>Sr/<sup>86</sup>Sr ratio (water II); and <figure class=></figure> higher Sr<sup>2+</sup> content and lower <sup>87</sup>Sr/<sup>86</sup>Sr ratio (water III), that is hot water. On the basis of integrated analysis, it was considered that <figure class=></figure> the radiogenic Sr in the Quaternary groundwater (Q<sub>4</sub>-Q<sub>1</sub>) originates from weathering of silicate rich in Na and Rb, mainly from plagioclase; <figure class=></figure> the radiogenic Sr of hot water in Huanghua port is attributed to carbonate dissolution, with lower <sup>87</sup>Sr/<sup>86</sup>Sr ratio and higher Sr/Na ratio; <figure class=></figure> the recharge area is laterally recharged by the groundwater flowing through igneous and metamorphic rocks, with moderate <sup>87</sup>Sr/<sup>86</sup>Sr ratio. However, the formation mechanism of Sr isotopes in Tertiary groundwater needs further studies.</td>
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Keywords:strontium  87Sr/86Sr  groundwater  Hebei plain  
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