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Volume 24 Issue 6
Dec 2013
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Journal of Earth Science  > 2013  >  24(6): 891-902.
Shufang Wang, Zhonghe Pang, Jiurong Liu, Pei Lin, Sida Liu, Ming Yin. Origin and Evolution Characteristics of Geothermal Water in the Niutuozhen Geothermal Field, North China Plain. Journal of Earth Science, 2013, 24(6): 891-902. doi: 10.1007/s12583-013-0390-6
Citation: Shufang Wang, Zhonghe Pang, Jiurong Liu, Pei Lin, Sida Liu, Ming Yin. Origin and Evolution Characteristics of Geothermal Water in the Niutuozhen Geothermal Field, North China Plain. Journal of Earth Science, 2013, 24(6): 891-902. doi: 10.1007/s12583-013-0390-6
shu

Origin and Evolution Characteristics of Geothermal Water in the Niutuozhen Geothermal Field, North China Plain

doi: 10.1007/s12583-013-0390-6
  • 1.

    Key Laboratory of Engineering Geomechanics, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China

  • 2.

    Graduate University of Chinese Academy of Sciences, Beijing 100049, China

  • 3.

    Beijing Institute of Hydrogeology and Engineering Geology, Beijing 100195, China

  • 4.

    School of Water Resources and Environment, China University of Geosciences, Beijing 100083, China

  • 5.

    China Institute of Geo-Environment Monitoring, Beijing 100081, China

Funds:

the National Basic Research Program of China 2010CB428806

Beijing Municipal Science and Technology Project D07050601510000

More Information
  • Corresponding author: Shufang Wang, shufangwang111@163.com
  • Received Date: 14 Jun 2013
  • Accepted Date: 22 Oct 2013
  • Publish Date: 01 Dec 2013
    Abstract
  • Statistical study of analyses of water from 43 samples from geothermal wells, three groundwater wells, and one sample of local rainwater along with rainwater data from the Global Network of Isotopes in Precipitation has been used to identify the origin and evolution of geothermal water in the Niutuozhen (牛驼镇) geothermal field and estimate the renewability rate of its geothermal resource. The results show that the geothermal waters of the Jixianian Wumishanian dolomite reservoir and the Ordovician limestone reservoir are of Cl-Na type, the geothermal water of the Pliocene Minghuazhen (明化镇) Formation sandstone reservoir are Cl-Na type and HCO3-Na type and the groundwater of the Quaternary aquifer is HCO3-Na and HCO3-Na·Mg·Ca type. A linear relationship between silica concentration and temperature indicates that higher temperature probably enhances concentration of silica in Jixianian geothermal water. δ18O shift in Wumishanian geothermal water averaged 1.57‰, and was less than 1‰ in the other geothermal waters. The minimum and maximum 14C ages of Wumishanian geothermal water are 17 000 and 33 000 years from north to the south of the Niutuozhen geothermal field. Geothermal water and Quaternary groundwater belong to different groundwater systems with no hydraulic connections. Although the geothermal field receives some recharge from the Yanshan and Taihang mountains outside the northern and western boundaries of the geothermal field respectively, the renewability rate of geothermal water is on the scale of 10 000 years.

     

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