Volume 45 Issue 2
Apr.  2017
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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
shu

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

  • 1. MOE Key Lab of Marine Reservoir Evolution and Hydrocarbon Enrichment Mechanism, China University of Geosciences(Beijing), Beijing 100083, China;

  • 2. MOLR Key Lab of Shale Gas Resources Survey and Strategic Evaluation, China University of Geosciences(Beijing), Beijing 100083, China;

  • 3. China United Coalbed Methane Corporation Ltd., Beijing 100011, China

Funds: 

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

More Information
  • Received Date: March 08, 2016
  • Published Date: April 24, 2017
    Graphical Abstract
    • Abstract
  • 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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    • References (22)
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