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›› 2016, Vol. 39 ›› Issue (6): 1230-1237.

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Application of environmental isotopes to identify recharge sources of groundwater in Mulei mining area, Xinjiang

WEI Wen1, YANG Zhen-jing1, BAI Ming2, CHEN Zong-yu1   

  1. 1 Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, Hebei, China;
    2 The Second Hydrology and Engineering Geology Section of Xinjiang Bureau of Geology and Mineral Resources, Changji 831100, Xinjiang, China
  • Received:2016-06-18 Revised:2016-08-28

Abstract: The coal resources are considerable rich in Mulei region, Xinjiang, China. However, the development of the local coal resources is seriously limited because of the shortage and uneven distribution of water resources. In addition, the water gushing in coal mining process is one of the major threats to the mining safety. Therefore, this paper aims to identify the groundwater recharge sources in Mulei mining area, which is significant for the safety guarantee in mining operations and water suppling. Thirty-three water samples were collected from precipitation, surface water and groundwater in the study area, and by using stable isotopes analysis, water chemistry measurement, radioactive tritium and carbon-14 dating method, the recharge sources were identified and the flow pattern of groundwater was delineated in Mulei mining area, Xinjiang. Oxygen-18 components of the Quaternary unconfined groundwater in the two sides of the boundary line from Dahongliu valley to the middle part of Mingsha mountain had different characteristics; the δ18O value of groundwater varied from -14.8‰ to -12.8‰ with mean value of -13.9‰ in the west side, and varied from -17.3‰ to 15.4‰ with mean value of -16.1‰ in the east side. This two mean values of δ18O were 3.2‰ and 5.4‰ lower respectively, than the weighted average δ18O value of precipitation in Urumqi, indicating that the main recharge source of groundwater in the central area was originated from the higher elevated mountain precipitation, and the recharge elevation was about 1 700-2 300 meters. The low δ18O value of the Tertiary confined groundwater and the carbon-14 dating results show that the groundwater was recharged under the Late Pleistocene cold climates. Moreover, there was a certain relationship among the Jurassic pore fissure water, the bedrock fissure water and the modern unconfined groundwater; the flow pattern is probably that the bedrock fissure water infiltrated fast into underground through the piedmont permeable layer after seeped from the mountain-pass, and then recharged the fissure water and the Tertiary or Jurassic fissure water. This study is significant for guiding the safety exploitation of mining and security of water supply in Mulei mining area.

Key words: environmental isotopes, groundwater, recharge sources

CLC Number: 

  • P641.8