2016
DOI: 10.15446/esrj.v20n4.61633
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The pilot appraisal of acid fracturing of coalbed methane reservoir in southeast Qinshui Basin, China

Abstract: The reserves of Coalbed Methane (CBM) in Qinshui Basin are quite promising, but the outputs from CBM wells are quite small even after massive hydraulic fracturing. Herein the fracture system with #3 and #15 coal seams in Qinshui basin was analyzed, and it was found that both of the macro-scale fractures and micro-scale fractures are filled with clay and carbonate minerals, which explains the low productivity of CBM wells after conventional hydraulic fracturing. Acid fracturing has long been an effective method… Show more

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Cited by 10 publications
(5 citation statements)
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“…By measuring hydrogen sulfide and pyrite δ 34 S abundances, Liu et al demonstrated that the δ 34 S of mine produced by BSR was commonly negative and even reached −50‰. In contrast, the δ 34 S of mine produced by thermal sulfate reduction (TSR) was commonly greater than +10‰, which is similar to the δ 34 S of sulfides in the field. , Liu et al and Machel found that anaerobic environments with the temperature of 60–80 °C had an effect on the type of sulfate-reducing bacteria (SRB) present. , Yan et al and Jiang et al noted that the ash index can indicate the trend of the reducing capacity for sedimentary environments hosting coal seams containing hydrogen sulfide. , After Deng et al used the acid–base index of the coal, the salinity index, and the retention index to determine the hydrodynamic condition of the coal’s formation, their studies further revealed the effects of the reducing sedimentary environment on the formation of hydrogen sulfide . Fu et al studied the excess sulfur in the Zaozhuang Bayi coal mine, China, and reached the conclusion that magmatic heat led to abnormal enrichment of hydrogen sulfide…”
Section: Introductionmentioning
confidence: 99%
“…By measuring hydrogen sulfide and pyrite δ 34 S abundances, Liu et al demonstrated that the δ 34 S of mine produced by BSR was commonly negative and even reached −50‰. In contrast, the δ 34 S of mine produced by thermal sulfate reduction (TSR) was commonly greater than +10‰, which is similar to the δ 34 S of sulfides in the field. , Liu et al and Machel found that anaerobic environments with the temperature of 60–80 °C had an effect on the type of sulfate-reducing bacteria (SRB) present. , Yan et al and Jiang et al noted that the ash index can indicate the trend of the reducing capacity for sedimentary environments hosting coal seams containing hydrogen sulfide. , After Deng et al used the acid–base index of the coal, the salinity index, and the retention index to determine the hydrodynamic condition of the coal’s formation, their studies further revealed the effects of the reducing sedimentary environment on the formation of hydrogen sulfide . Fu et al studied the excess sulfur in the Zaozhuang Bayi coal mine, China, and reached the conclusion that magmatic heat led to abnormal enrichment of hydrogen sulfide…”
Section: Introductionmentioning
confidence: 99%
“…Therefore, the permeability of coal reservoirs is the key parameter that dominates gas and water migration [3]. Most coal reservoirs in China are characterized by low permeability (~0.001-~0.1 mD), which has largely restricted coal seam degassing processes, especially when the mining moves towards deeper depths [4][5][6][7]. In order to guarantee safe mining and CBM production, the reservoir permeability should be further improved to increase the efficiency of coalbed methane extraction.…”
Section: Introductionmentioning
confidence: 99%
“…The length and width of the fracture network can be estimated by analyzing the MS locations. 31,32 And the characteristic of MS responses to the evolution of hydraulic pressure (HP) is significant, which can reveal the fracture occurrence mechanism. 31,32 And the characteristic of MS responses to the evolution of hydraulic pressure (HP) is significant, which can reveal the fracture occurrence mechanism.…”
Section: Introductionmentioning
confidence: 99%
“…30 A number of application tests of MS monitoring for subsurface HF have been performed to estimate the stimulated area. 31,32 And the characteristic of MS responses to the evolution of hydraulic pressure (HP) is significant, which can reveal the fracture occurrence mechanism. 33 However, the mechanism of MS responses to HF is rarely expressed in the complicated subsurface field.…”
Section: Introductionmentioning
confidence: 99%