Groundwater Isotope Characteristics Analysis of Wuhai

Article Preview

Abstract:

By the field investigation on BaYinTaohai of WuHai,this article found that ,although this town locates in the northwest arid areas with little rain and big evaporation, the groundwater is abundant. Many artesian wells and springs are founded in this place. Through the analysis of the isotope characteristics of the groundwater in the study area, It is concluded that the shallow groundwater of south Wuhai recharge from local precipitation,while deep confined water recharge from allogenic water with isotope dilution.

You might also be interested in these eBooks

Info:

Periodical:

Advanced Materials Research (Volumes 955-959)

Pages:

3185-3189

Citation:

Online since:

June 2014

Export:

Price:

Permissions CCC:

Permissions PLS:

Сopyright:

© 2014 Trans Tech Publications Ltd. All Rights Reserved

Share:

Citation:

* - Corresponding Author

[1] Xuchun ZHAO,Chenghai WANG,Yongsheng ZHANG,Huan JIANG. 2007. Application Comparison And Research of Two Kinds of Grade Indices of Drought Analysis In Wuhai Area[J]. JOURNAL OF THE METEOROLOGICAL SCIENCES, 27(1): 162-168(in Chinese).

Google Scholar

[2] Fangqiang SUN, 2010. Research on groundwater circulation and environment effect of Dusitu river in Ordos Basin. [D]. Chang'an University. (in Chinese ).

Google Scholar

[3] Guangcai HOU, Xiaosi SU, Xueyu LIN, Futian LIU, Shuping YI, Weihong DONG, Fakang YU, Yuncheng YANG, Dong WANG. 2007. Environmental Isotopic Composition of Natural Water in Ordos Cretaceous Groundwater Basin and Its Significance for Hydrological Cycle[J]. Journal of Jilin University(Earth Science Edition), 37(2): 255-260(in Chinese).

Google Scholar

[4] Guangcai HOU, Xueyu LIN, Xiaosi SU, Xiaoyong WANG, Jie LIU. 2006. Groundwater System in Ordos Cretaceous Artisan Basin (CAB)[J]. Journal of Jilin University(Earth Science Edition), 36(3): 391-398(in Chinese ).

Google Scholar

[5] Shaohua MA, RuiYANG, Airong MA, Chunming SUI, Guang LI. 2012. Storage and distribution of Karst groundwater of the West Table Mountain. RESOURCES[J], (4): 120-123(in Chinese ).

Google Scholar

[6] Chen J, Liu X, Wang C, et al. Isotopic constraints on the origin of groundwater in the Ordos Basin of northern China[J]. Environmental Earth Sciences, 2012, 66(2): 505-517.

DOI: 10.1007/s12665-011-1259-6

Google Scholar

[7] Clark I D, Fritz P. Environmental isotopes in hydrogeology[M]. CRC press, (1997).

Google Scholar

[8] Jiang SUN. 2013. The mechanism of moisture movement in the unsaturated zones of the Ordos Deserts. [D]. Hohai University. (in Chinese ).

Google Scholar

[9] Hui QIAN, Yan DOU Xijian, LI, Bingchao YANG, Zhenhong ZHAO. 2007. Changes of δ18O and δD along Dousitu River and its indication of river water evaporation[J]. HYDROGEOLOGY&ENGINEERING GEOLOGY, 2007, 34(1): 107-112. (in Chinese).

DOI: 10.1007/s10498-007-9011-2

Google Scholar