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Geologically controlling factors on coal bed methane (CBM) productivity in Liulin

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Journal of Coal Science and Engineering (China)

Abstract

It is of great significance to forecast high yield of CBM wells and analyze dynamic production by having an overall study on the characteristics of the produced CBM and determining the main factors influencing the productivity of CBM. With the test report and the related geological parameters of a single well, methods of combining the productivity data and typical production curves were used to analyze different geological factors and how to influence the capacity of a single layer. Then, the paper proposed a new understanding about capacity characteristics of the study area and geological control factors: First, the Shanxi formation production capacity characteristics was divided into two-stages, showing signs of gas and gas breakthrough for 100 days. Second, two parameters, which include potential of gas production and gas production capacity, were better than the single parameter, such as gas content, coal thickness, and penetration to analyze affecting factors of single well production. Finally, comprehensive analysis concluded that the ratio of critical desorption pressure to reservoir pressure has greater influence on the production of vertical CBM wells. Besides, the potential of gas production capacity has greater impact at stage of showing gas signs; the coal reservoir pressure and gas production capacity have greater impact at stage of gas breakthrough for 100 days. Thus, to seek the coal bed methane with high ratio of critical desorption pressure to reservoir pressure and high yield of gas will be important guarantee to the success of the coal bed methane exploration and development.

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Correspondence to Li-jun Gao.

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Supported by the National Science and Technology Major Project of the Ministry of Science and Technology of China (2008ZX05034-001, 2011ZX05062-01)

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Gao, Lj., Tang, Dz., Xu, H. et al. Geologically controlling factors on coal bed methane (CBM) productivity in Liulin. J Coal Sci Eng China 18, 362–367 (2012). https://doi.org/10.1007/s12404-012-0405-4

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  • DOI: https://doi.org/10.1007/s12404-012-0405-4

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