4.3 Article

Implications of geological conditions on gas content and geochemistry of deep coalbed methane reservoirs from the Panji Deep Area in the Huainan Coalfield, China

Journal

Publisher

ELSEVIER SCI LTD
DOI: 10.1016/j.jngse.2020.103712

Keywords

Geological conditions; Deep coalbed methane reservoirs; Gas content and geochemistry; Panji deep area; Huainan coalfield

Funding

  1. National Natural Science Foundation of China [U1810201, 41572125]
  2. National Science and Technology Major Project of China [2016ZX05007-003]
  3. Public Projects of Anhui Province [2013-3-18, 2015-g-29]
  4. Fundamental Research Funds for the Central Universities [2020YJMT02]
  5. Study on identification technologyof thin limestone in Huainan and Huaibei areas [2020xhx029]
  6. Teachers' application ability development workstation project of Suzhou University (Professional Workstation) [2018XJYY07]
  7. Suzhou University [2019jb20]

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This study reveals the implications of geological conditions on deep coalbed methane reservoirs, finding that factors such as burial depth, effective thickness of overlying strata, and gas pressure significantly impact gas content and geochemistry.
The objective of this study is to reveal the implications of geological conditions on gas content and geochemistry of deep coalbed methane (CBM) reservoirs. It is of great practical significances to improve the theory and technology for deep CBM development. In this work, the gas content and geochemistry of selected samples were obtained by canister desorption method, gas chromatography (GC) and GC-Mass Spectrometry (GC-MS). On the basis of geological conditions, the Panji Deep Area was confirmed as a mining block of high gas content, high ground stress and reservoir temperature, multiple sets of coal seams, and complex mining conditions. Deep-buried coals from No.13-1 and No.11-2 coal seams are generally low-mineral bituminous coals, which show similar coal rank (R-o,(max) = 0.71%-0.85%) but vary in maceral and chemical components. In addition, the estimated total gas contents of No.13-1 and No.11-2 coal seams are 9.58-23.59 m(3)/t and 9.46-13.72 m(3)/t, respectively. Notably, the growth rate of total gas content exhibits two different stages and shows a logarithmic correlation with reservoir temperature, effective thickness of overlying strata, burial depth and gas pressure. The carbon isotopic value of methane (delta C-13(1)) of No.13-1 coal seam varies from -45.09 parts per thousand to -39.23 parts per thousand (average, -41.90 parts per thousand), and that for No.11-2 coal seam ranges from -44.92 parts per thousand to -38.45 parts per thousand (average, -41.90 parts per thousand). delta C-13(1) is unrelated with R-o,R-max but is positively correlated with burial depth and effective thickness of overlying strata, this indicates that delta C-13(1) value becomes heavier as burial depth increases, which may be related to the desorption-diffusion-migration effect caused by deeper burial depth and in-situ stress exertion. Moreover, delta C-13(1) shows a positive linear correlation with total gas content, it is inferred that delta C-13(1) has a correlation with the control factors of total gas content.

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