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Geoscience ›› 2017, Vol. 31 ›› Issue (01): 158-166.

• Petroleum Geology • Previous Articles     Next Articles

Temperature Monitoring Results for Gas Hydrate Borehole DK-9 and Thickness of Gas Hydrate Stability Zone in the Qilian Mountains Permafrost

WANG Chaoqun1,2(), DING Yingying2, HU Daogong1(), QI Bangshen1, ZHANG Yaoling1, TAO Tao1, WU Huanhuan1   

  1. 1. Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
    2. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
  • Received:2016-09-21 Revised:2016-12-02 Online:2017-02-10 Published:2017-03-16

Abstract:

Gas hydrate was discovered in 2008 in the Sanlutian coalfield, Qilian Mountain permafrost, Northwest China. This discovery was first successfully sampled by drilling in mid-low-latitudes mountain permafrost, and was a breakthrough in gas hydrate exploration in onshore regions of China. Temperature monitoring for gas hydrate scientific borehole DK-9, one of boreholes in the Sanlutian coalfield in which gas hydrate was discovered, yielded steady ground temperature data for both in and beneath permafrost layer for one year. The results suggest that the thickness of permafrost in the Sanlutian coalfield is about 160 m and that the geothermal gradient is 1.38 ℃/100 m in the permafrost layer and 4.85 ℃/100 m below the permafrost layer. Analysis of the gas hydrate stability conditions indicate that the permafrost conditions and gas components are favorable for gas hydrate formation, and the maximum depth of the gas hydrate stability zone(GHSZ)in the Sanlutian coalfield is 510-617 m.

Key words: gas hydrate, geothermal gradient, gas hydrate stability zone, Qilian Mountain

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