Hydrogeochemical Evolution of Groundwater in the Dusit-Yanchi Watery System, North of the Ordos Basin

Author

Yan, Dou ; Hui, Qian ; Guangcai, Hou ; Lihe, Yin ; Xiaoyong, Wang

Volume

2

fYear

2009

fDate

16-18 Oct. 2009

Firstpage

609

Lastpage

612

Abstract

With the development of energy base in Ordos basin, the deficiency of groundwater becomes serious. Therefore, the hydrogeochemical evolution of groundwater is studied, which is in the Dusit-Yanchi watery system. Some results are obtained. The quality of groundwater in Dusit river system is better, and in the aquifer, the main water-rock action is the solution of gypsum, fluorite, and siderite, and the precipitation of calcite and dolomite.

Keywords

geochemistry; groundwater; minerals; precipitation (physical chemistry); rocks; solvation; water quality; Dusit-Yanchi water system; Ordos basin; aquifer; calcite precipitation; dolomite precipitation; fluorite solution; groundwater deficiency; groundwater hydrogeochemical evolution; groundwater quality; gypsum solution; siderite solution; water-rock action; Fault location; Geology; Humidity; Lakes; Mineral resources; Natural gas; Permeability; Rivers; Temperature; Water resources; hydrogeochemistry; saturation index (SI); water type;

fLanguage

English

Publisher

ieee

Conference_Titel

Energy and Environment Technology, 2009. ICEET '09. International Conference on

Conference_Location

Guilin, Guangxi

Print_ISBN

978-0-7695-3819-8

Type

conf

DOI

10.1109/ICEET.2009.385

Filename

5364092