Journal of Jilin University(Earth Science Edition) ›› 2015, Vol. 45 ›› Issue (5): 1502-1514.doi: 10.13278/j.cnki.jjuese.201505205

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Characters of Hydrogen and Oxygen Stable Isotope of Different Water Bodies in Huainan Coal Mining Area

Zhang Lei1,2, Qin Xiaoguang1, Liu Jiaqi1, Mu Yan1, An Shikai3, Lu Chunhui3, Chen Yongchun3   

  1. 1. Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;
    2. College of Earth Science, University of Chinese Academy of Sciences, Beijing 100049, China;
    3. National Engineering Laboratory for Protection of Coal Mine Eco-Environment, Coal Mining National Engineering Technology Research Institute, Huainan 232001, Anhui, China
  • Received:2014-12-07 Published:2015-09-26

Abstract:

Huainan is an important energy base in Eastern China with a large coal mining subsidence area due to the underground mining. Groundwater aquifers may be broken by the subsidence cracks to become a critical source of subsidence area water. It means that the water cycle system may be damaged due to coal mining. To resolve this geological hazards, establishing "plain reservoir" was suggested by using coal mining subsidence areas. The "plain reservoir" may also solve water shortage during drought year. However, how to evaluate the potential water sources of the "plain reservoirs" is still an issue; and a stable water supply is another question as it is essential for "plain reservoirs". In order to find out whether the subsidence cracks have broken the groundwater system and whether groundwater is a stable source of the subsidence area water, we analyzed the water sources of subsidence areas. We collected 23 water samples from wells, rivers, rainfalls, wetlands and subsidence areas in Huainan mining area in dry and rainy seasons, and compared with the deep groundwater. The composition of hydrogen and oxygen stable isotope is used to trace the source of water. The results show that the atmospheric precipitation is the main water source of subsidence areas. Deep groundwater is not a stable water source to "plain reservoirs"; although groundwater systems are broken by subsidence cracks at present, and surface water filters down and mixes with the deep groundwater.

Key words: Huaibei plain, coal mining subsidence area, source of water, hydrogen and oxygen stable isotope

CLC Number: 

  • P641.6

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