The Recognition on the Source of Shaizhudong Spring in the Central of Weibei, Shaanxi Province, China

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Abstract:

Shaizhudong spring is the largest karst spring in the central of north of the Weihe River, Shaanxi Province, China. A lot of studies have been done for investigating the recharge source of it. The most common understanding was that the leakage of Jinghe was the main recharge source for Shaizhudong Spring which is the concentrated discharge point of hidden karst system in the catchment area of Shaizhudong Spring. However, with the method of hydrogen and oxygen isotopes, and combining the condition of hydro-geochemistry and karst hydro-geology, we have different opinions on the recharge source of Shaizhudong Spring. This study shows the result that the recharge of Shaizhudong Spring is given priority by karst groundwater which is outside the southwest of the Shaizhudong Spring area.

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Periodical:

Advanced Materials Research (Volumes 1073-1076)

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1651-1655

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December 2014

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© 2015 Trans Tech Publications Ltd. All Rights Reserved

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[1] Geological survey of Shaanxi province. The center of Shaanxi Weibei karst groundwater investigation report [R]. 1999-(2002).

Google Scholar

[2] Shi Jian, Liang Yongping, Wong Jing. The study on evaluation and exploitation of groundwater in the Loess Plateau hidden karst region of western Weibei [J]. Chinese karst, 2002, 21 (1): 44-50.

Google Scholar

[3] Lin Pingxuan, Li Feng, Huang Weixing. The application of water isotope in distinguishing components of the karst groundwater – as Shuaizhudong spring region for example [J]. Shaanxi geology, 2003, 21(1): 67-71.

Google Scholar

[4] Ma Zhiyuan, Qian Hui. Environmental isotope geohydrology [M]. Shaanxi Xi'an: Shaanxi science and technology publication, (2004).

Google Scholar

[5] Chen Zongyu, Qi Jixiang, zhang zhaoji etc. The application of isotope hydrogeology method in typical northern basin [M]. Science Publication, 2010. 06.

Google Scholar

[6] Yin Guan etc. The evolution of groundwater deuterium excess parameter [J]. Mineral rock geochemistry bulletin, 2001, 20 (4): 409-411.

Google Scholar

[7] Ma Zhiyuan, Qian Hui, Huang Jianxun etc. The evidence of environmental isotope hydrogeochemistry about relationships among aquifers of southern Guanzhong basin [J]. Journal of Earth Sciences and environment. 2006, 28(2): 69-74.

Google Scholar

[8] Lin Liangjun, Wang Jinsheng. The karst water isotope and hydrochemical analysis of Jinshan valley region [J]. Engineering Survey, 2004, (No. 4): 27-30.

Google Scholar

[9] Zhang Jianghua, Liang Yongping. The application of sulfur isotope technology in northern karst water survey [J]. China karst, 2009, 28 (3): 235-241.

Google Scholar