SHI Wei, TANG Shuheng, LI Zhongcheng, ZHANG Songhang. Hydrogen-oxygen isotope characteristics of produced water from coal reservoir of Shanxi Formation in Qinshui basin[J]. COAL GEOLOGY & EXPLORATION, 2017, 45(2): 62-68. DOI: 10.3969/j.issn.1001-1986.2017.02.011
Citation: SHI Wei, TANG Shuheng, LI Zhongcheng, ZHANG Songhang. Hydrogen-oxygen isotope characteristics of produced water from coal reservoir of Shanxi Formation in Qinshui basin[J]. COAL GEOLOGY & EXPLORATION, 2017, 45(2): 62-68. DOI: 10.3969/j.issn.1001-1986.2017.02.011

Hydrogen-oxygen isotope characteristics of produced water from coal reservoir of Shanxi Formation in Qinshui basin

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National Science and Technology Major Project(2011ZX05034-003)

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  • Received Date: March 08, 2016
  • Published Date: April 24, 2017
  • To study the groundwater runoff and water chemistry characteristics of the primary minable seam No.3 of coal reservoir in Shanxi Formation in the southern block of Shizhuang, southern Qinshui basin, this paper collected water samples from coalbed methane wells in the south of Shizhuang block. The characteristics of ion concentration and hydrogen-oxygen isotope are determined to analyze the distribution characteristics of ion concentration and isotope. The results show that the produced water from seam No.3 was supplied from atmospheric precipitation and was also characterized by 18O and D drift. δD and δ18O which increased from the east to the west, presented a positive correlation with ion concentration, which was consistent with the characteristics of the transition from runoff area to residence area in the study area. δD and δ18O can be used as effective exploration tool in judging the runoff conditions and evaluating exploration target.
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