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Volume 41 Issue 2
Jul.  2022
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Article Navigation >  CARSOLOGICA SINICA  > 2022  >  41(2): 174-182
TANG Chunlei, LIANG Yongping, JIN Hua, SHEN Haoyong, ZHAO Chunhong, WANG Zhiheng, XIE Hao, ZHAO Yi, WANG Shina. Niangziguan spring group in Shanxi Province and its water source[J]. CARSOLOGICA SINICA, 2022, 41(2): 174-182. doi: 10.11932/karst20220201
Citation: TANG Chunlei, LIANG Yongping, JIN Hua, SHEN Haoyong, ZHAO Chunhong, WANG Zhiheng, XIE Hao, ZHAO Yi, WANG Shina. Niangziguan spring group in Shanxi Province and its water source[J]. CARSOLOGICA SINICA, 2022, 41(2): 174-182. doi: 10.11932/karst20220201
shu

Niangziguan spring group in Shanxi Province and its water source

doi: 10.11932/karst20220201
  • 1.

    Taiyuan University of Technology, Taiyuan, Shanxi 030024, China

  • 2.

    Institute of Karst Geology, CAGS/ Key Laboratory of Karst Dynamics, MNR & GZAR, Guilin, Guangxi 541004, China

  • 3.

    International Research Center on Karst under the Auspices of UNESCO, Guilin, Guangxi 541004, China

  • 4.

    Guangxi Karst Resources and Environment Research Center of Engineering Technology, Guilin, Guangxi 541004, China

  • 5.

    Land and Resources Exploration Center of Hebei Bureau of Geology and Mineral Resources Exploration, Shijiazhuang, Hebei 050081, China

  • Received Date: 2021-04-06
    Abstract
  • As a main natural discharge point of karst groundwater, Niangziguan spring group consists of 11 springs and is located in Niangziguan town, Yangquan City, Shanxi Province. It is distributed on the floodplain and terrace of the Taohe river, the Wenhe river and the Mianhe river, with an exposed elevation of 360 m to 392 m. Among these springs, Chengjia spring is the highest and Jinqu spring is the lowest. The annual average flow of spring group is 9.48 m3·s−1 and the flow differences of springs are large, among which the difference of Wulong spring is the largest. Niangziguan spring group is the largest karst spring in northern China, with a catchment area of 7,436 km2. Previous studies believe that karst water in the spring area flows from north, west and south to Niangziguan area, and the chert mass or strip dolomite of lower Ordovicianin Niangziguan area relatively rises to the aquifuge, and is eroded and exposed by the Taohe River, which makes the karst groundwater overflow to the surface and form a spring group. The main aquifer is made up of gypsum-bearing carbonate rock of middle Ordovician. However, because Niangziguan springs are not from the same source, their hydrochemistry and isotope are different. Therefore, it is necessary to study the source of Niangziguan spring group. This study is conducted with the methods of hydrochemistry, isotope and hydrogeological section, and is concluded that there are two aquifers and three subsystems in Niangziguan spring area. The aquifer consists of middle Ordovician limestone aquifer and middle upper Cambrian dolomite one. Subsystem distribution is comprised of Ordovician karst water system in the west, and Ordovician karst water system and middle upper Cambrian karst water system both in the East. Chengxi spring and Chengjia spring are exposed on the marl of lower Majiagou formation of middle Ordovician, and their aquifers consist of fissure and fissure water of Middle Ordovician limestone. Because the marl of lower Majiagou formation is uplifted in this region, the surface spring-the eastern Ordovician karst water system-is formed. Mainly supplied by the water-bearing formation of middle upper Cambrian, Podi spring, Wulong spring, Shibanmo spring, Shuiliandong spring and Weizeguan spring are pressure-bearing ascending springs and belong to the middle upper Cambrian karst water system in the east.

     

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