Evolution Characteristic and Implication of Coalbed Methane Desorption Stages Division for Tectonically Deformed Coals
Abstract This paper discusses the evolution characteristic and implication of coalbed methane (CBM) desorption stages division with the tectonic deformation degree based on the $ CH_{4} $ isothermal adsorption/desorption experiments and desorption efficiency for the primary coal and tectonically def...
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| Autor*in: |
Zhou, Dan [verfasserIn] |
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E-Artikel |
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| Sprache: |
Englisch |
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2022 |
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| Schlagwörter: |
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| Anmerkung: |
© The Author(s), under exclusive licence to Springer Nature B.V. 2022 |
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| Übergeordnetes Werk: |
Enthalten in: Transport in porous media - Dordrecht [u.a.] : Springer Science + Business Media B.V, 1986, 141(2022), 3 vom: 19. Jan., Seite 713-736 |
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| Übergeordnetes Werk: |
volume:141 ; year:2022 ; number:3 ; day:19 ; month:01 ; pages:713-736 |
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| DOI / URN: |
10.1007/s11242-022-01744-0 |
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SPR046373993 |
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| 520 | |a Abstract This paper discusses the evolution characteristic and implication of coalbed methane (CBM) desorption stages division with the tectonic deformation degree based on the $ CH_{4} $ isothermal adsorption/desorption experiments and desorption efficiency for the primary coal and tectonically deformed coals (TDCs). The results show the pressure drops for the three desorption stages divided contributing to the CBM productivity increase with the tectonic deformation degree. This evolution characteristic indicates the CBM productivity of the strong brittle and ductile deformation TDCs is greater than that of the primary coal and weak brittle deformation TDCs, while the actual productivity is prohibited by the special reservoir properties of low strength, low permeability, and stimulation difficulty. This study demonstrates the two reservoir stimulation methods of the staged hydraulic fracturing of horizontal well in roof strata and the double string screen pipe completion and flushing of horizontal well can be considered adaptive for the strong brittle and ductile deformation TDCs reservoirs. Also, the special water drainage and depressurization management need to be adopted in different TDCs reservoirs. The reasonable flow pressure for CBM production can be estimated by the evolution characteristics of the three key pressures and desorption stages division with the tectonic deformation degree. In summary, this study is of great significance for achieving high and stable CBM production in TDCs reservoirs. Article HighlightsThe evolution characteristic of CBM desorption stages division for TDCs was analyzed.The CBM productivity for the different types of TDCs was revealed.The implications of this study on CBM production for TDCs were discussed. | ||
| 650 | 4 | |a Coalbed methane |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Desorption efficiency |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Desorption stages division |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Tectonically deformed coal |7 (dpeaa)DE-He213 | |
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| 700 | 1 | |a Song, Yu |4 aut | |
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| 700 | 1 | |a Zhang, Zhen |4 aut | |
| 700 | 1 | |a Liu, Gaofeng |0 (orcid)0000-0002-9340-9029 |4 aut | |
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10.1007/s11242-022-01744-0 doi (DE-627)SPR046373993 (SPR)s11242-022-01744-0-e DE-627 ger DE-627 rakwb eng Zhou, Dan verfasserin aut Evolution Characteristic and Implication of Coalbed Methane Desorption Stages Division for Tectonically Deformed Coals 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer Nature B.V. 2022 Abstract This paper discusses the evolution characteristic and implication of coalbed methane (CBM) desorption stages division with the tectonic deformation degree based on the $ CH_{4} $ isothermal adsorption/desorption experiments and desorption efficiency for the primary coal and tectonically deformed coals (TDCs). The results show the pressure drops for the three desorption stages divided contributing to the CBM productivity increase with the tectonic deformation degree. This evolution characteristic indicates the CBM productivity of the strong brittle and ductile deformation TDCs is greater than that of the primary coal and weak brittle deformation TDCs, while the actual productivity is prohibited by the special reservoir properties of low strength, low permeability, and stimulation difficulty. This study demonstrates the two reservoir stimulation methods of the staged hydraulic fracturing of horizontal well in roof strata and the double string screen pipe completion and flushing of horizontal well can be considered adaptive for the strong brittle and ductile deformation TDCs reservoirs. Also, the special water drainage and depressurization management need to be adopted in different TDCs reservoirs. The reasonable flow pressure for CBM production can be estimated by the evolution characteristics of the three key pressures and desorption stages division with the tectonic deformation degree. In summary, this study is of great significance for achieving high and stable CBM production in TDCs reservoirs. Article HighlightsThe evolution characteristic of CBM desorption stages division for TDCs was analyzed.The CBM productivity for the different types of TDCs was revealed.The implications of this study on CBM production for TDCs were discussed. Coalbed methane (dpeaa)DE-He213 Desorption efficiency (dpeaa)DE-He213 Desorption stages division (dpeaa)DE-He213 Tectonically deformed coal (dpeaa)DE-He213 Wu, Caifang aut Song, Yu aut Xian, Baoan aut Gao, Bin aut Zhang, Zhen aut Liu, Gaofeng (orcid)0000-0002-9340-9029 aut Enthalten in Transport in porous media Dordrecht [u.a.] : Springer Science + Business Media B.V, 1986 141(2022), 3 vom: 19. Jan., Seite 713-736 (DE-627)269017720 (DE-600)1473676-7 1573-1634 nnns volume:141 year:2022 number:3 day:19 month:01 pages:713-736 https://dx.doi.org/10.1007/s11242-022-01744-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 141 2022 3 19 01 713-736 |
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10.1007/s11242-022-01744-0 doi (DE-627)SPR046373993 (SPR)s11242-022-01744-0-e DE-627 ger DE-627 rakwb eng Zhou, Dan verfasserin aut Evolution Characteristic and Implication of Coalbed Methane Desorption Stages Division for Tectonically Deformed Coals 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer Nature B.V. 2022 Abstract This paper discusses the evolution characteristic and implication of coalbed methane (CBM) desorption stages division with the tectonic deformation degree based on the $ CH_{4} $ isothermal adsorption/desorption experiments and desorption efficiency for the primary coal and tectonically deformed coals (TDCs). The results show the pressure drops for the three desorption stages divided contributing to the CBM productivity increase with the tectonic deformation degree. This evolution characteristic indicates the CBM productivity of the strong brittle and ductile deformation TDCs is greater than that of the primary coal and weak brittle deformation TDCs, while the actual productivity is prohibited by the special reservoir properties of low strength, low permeability, and stimulation difficulty. This study demonstrates the two reservoir stimulation methods of the staged hydraulic fracturing of horizontal well in roof strata and the double string screen pipe completion and flushing of horizontal well can be considered adaptive for the strong brittle and ductile deformation TDCs reservoirs. Also, the special water drainage and depressurization management need to be adopted in different TDCs reservoirs. The reasonable flow pressure for CBM production can be estimated by the evolution characteristics of the three key pressures and desorption stages division with the tectonic deformation degree. In summary, this study is of great significance for achieving high and stable CBM production in TDCs reservoirs. Article HighlightsThe evolution characteristic of CBM desorption stages division for TDCs was analyzed.The CBM productivity for the different types of TDCs was revealed.The implications of this study on CBM production for TDCs were discussed. Coalbed methane (dpeaa)DE-He213 Desorption efficiency (dpeaa)DE-He213 Desorption stages division (dpeaa)DE-He213 Tectonically deformed coal (dpeaa)DE-He213 Wu, Caifang aut Song, Yu aut Xian, Baoan aut Gao, Bin aut Zhang, Zhen aut Liu, Gaofeng (orcid)0000-0002-9340-9029 aut Enthalten in Transport in porous media Dordrecht [u.a.] : Springer Science + Business Media B.V, 1986 141(2022), 3 vom: 19. Jan., Seite 713-736 (DE-627)269017720 (DE-600)1473676-7 1573-1634 nnns volume:141 year:2022 number:3 day:19 month:01 pages:713-736 https://dx.doi.org/10.1007/s11242-022-01744-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 141 2022 3 19 01 713-736 |
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10.1007/s11242-022-01744-0 doi (DE-627)SPR046373993 (SPR)s11242-022-01744-0-e DE-627 ger DE-627 rakwb eng Zhou, Dan verfasserin aut Evolution Characteristic and Implication of Coalbed Methane Desorption Stages Division for Tectonically Deformed Coals 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer Nature B.V. 2022 Abstract This paper discusses the evolution characteristic and implication of coalbed methane (CBM) desorption stages division with the tectonic deformation degree based on the $ CH_{4} $ isothermal adsorption/desorption experiments and desorption efficiency for the primary coal and tectonically deformed coals (TDCs). The results show the pressure drops for the three desorption stages divided contributing to the CBM productivity increase with the tectonic deformation degree. This evolution characteristic indicates the CBM productivity of the strong brittle and ductile deformation TDCs is greater than that of the primary coal and weak brittle deformation TDCs, while the actual productivity is prohibited by the special reservoir properties of low strength, low permeability, and stimulation difficulty. This study demonstrates the two reservoir stimulation methods of the staged hydraulic fracturing of horizontal well in roof strata and the double string screen pipe completion and flushing of horizontal well can be considered adaptive for the strong brittle and ductile deformation TDCs reservoirs. Also, the special water drainage and depressurization management need to be adopted in different TDCs reservoirs. The reasonable flow pressure for CBM production can be estimated by the evolution characteristics of the three key pressures and desorption stages division with the tectonic deformation degree. In summary, this study is of great significance for achieving high and stable CBM production in TDCs reservoirs. Article HighlightsThe evolution characteristic of CBM desorption stages division for TDCs was analyzed.The CBM productivity for the different types of TDCs was revealed.The implications of this study on CBM production for TDCs were discussed. Coalbed methane (dpeaa)DE-He213 Desorption efficiency (dpeaa)DE-He213 Desorption stages division (dpeaa)DE-He213 Tectonically deformed coal (dpeaa)DE-He213 Wu, Caifang aut Song, Yu aut Xian, Baoan aut Gao, Bin aut Zhang, Zhen aut Liu, Gaofeng (orcid)0000-0002-9340-9029 aut Enthalten in Transport in porous media Dordrecht [u.a.] : Springer Science + Business Media B.V, 1986 141(2022), 3 vom: 19. Jan., Seite 713-736 (DE-627)269017720 (DE-600)1473676-7 1573-1634 nnns volume:141 year:2022 number:3 day:19 month:01 pages:713-736 https://dx.doi.org/10.1007/s11242-022-01744-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 141 2022 3 19 01 713-736 |
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10.1007/s11242-022-01744-0 doi (DE-627)SPR046373993 (SPR)s11242-022-01744-0-e DE-627 ger DE-627 rakwb eng Zhou, Dan verfasserin aut Evolution Characteristic and Implication of Coalbed Methane Desorption Stages Division for Tectonically Deformed Coals 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer Nature B.V. 2022 Abstract This paper discusses the evolution characteristic and implication of coalbed methane (CBM) desorption stages division with the tectonic deformation degree based on the $ CH_{4} $ isothermal adsorption/desorption experiments and desorption efficiency for the primary coal and tectonically deformed coals (TDCs). The results show the pressure drops for the three desorption stages divided contributing to the CBM productivity increase with the tectonic deformation degree. This evolution characteristic indicates the CBM productivity of the strong brittle and ductile deformation TDCs is greater than that of the primary coal and weak brittle deformation TDCs, while the actual productivity is prohibited by the special reservoir properties of low strength, low permeability, and stimulation difficulty. This study demonstrates the two reservoir stimulation methods of the staged hydraulic fracturing of horizontal well in roof strata and the double string screen pipe completion and flushing of horizontal well can be considered adaptive for the strong brittle and ductile deformation TDCs reservoirs. Also, the special water drainage and depressurization management need to be adopted in different TDCs reservoirs. The reasonable flow pressure for CBM production can be estimated by the evolution characteristics of the three key pressures and desorption stages division with the tectonic deformation degree. In summary, this study is of great significance for achieving high and stable CBM production in TDCs reservoirs. Article HighlightsThe evolution characteristic of CBM desorption stages division for TDCs was analyzed.The CBM productivity for the different types of TDCs was revealed.The implications of this study on CBM production for TDCs were discussed. Coalbed methane (dpeaa)DE-He213 Desorption efficiency (dpeaa)DE-He213 Desorption stages division (dpeaa)DE-He213 Tectonically deformed coal (dpeaa)DE-He213 Wu, Caifang aut Song, Yu aut Xian, Baoan aut Gao, Bin aut Zhang, Zhen aut Liu, Gaofeng (orcid)0000-0002-9340-9029 aut Enthalten in Transport in porous media Dordrecht [u.a.] : Springer Science + Business Media B.V, 1986 141(2022), 3 vom: 19. Jan., Seite 713-736 (DE-627)269017720 (DE-600)1473676-7 1573-1634 nnns volume:141 year:2022 number:3 day:19 month:01 pages:713-736 https://dx.doi.org/10.1007/s11242-022-01744-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 141 2022 3 19 01 713-736 |
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10.1007/s11242-022-01744-0 doi (DE-627)SPR046373993 (SPR)s11242-022-01744-0-e DE-627 ger DE-627 rakwb eng Zhou, Dan verfasserin aut Evolution Characteristic and Implication of Coalbed Methane Desorption Stages Division for Tectonically Deformed Coals 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer Nature B.V. 2022 Abstract This paper discusses the evolution characteristic and implication of coalbed methane (CBM) desorption stages division with the tectonic deformation degree based on the $ CH_{4} $ isothermal adsorption/desorption experiments and desorption efficiency for the primary coal and tectonically deformed coals (TDCs). The results show the pressure drops for the three desorption stages divided contributing to the CBM productivity increase with the tectonic deformation degree. This evolution characteristic indicates the CBM productivity of the strong brittle and ductile deformation TDCs is greater than that of the primary coal and weak brittle deformation TDCs, while the actual productivity is prohibited by the special reservoir properties of low strength, low permeability, and stimulation difficulty. This study demonstrates the two reservoir stimulation methods of the staged hydraulic fracturing of horizontal well in roof strata and the double string screen pipe completion and flushing of horizontal well can be considered adaptive for the strong brittle and ductile deformation TDCs reservoirs. Also, the special water drainage and depressurization management need to be adopted in different TDCs reservoirs. The reasonable flow pressure for CBM production can be estimated by the evolution characteristics of the three key pressures and desorption stages division with the tectonic deformation degree. In summary, this study is of great significance for achieving high and stable CBM production in TDCs reservoirs. Article HighlightsThe evolution characteristic of CBM desorption stages division for TDCs was analyzed.The CBM productivity for the different types of TDCs was revealed.The implications of this study on CBM production for TDCs were discussed. Coalbed methane (dpeaa)DE-He213 Desorption efficiency (dpeaa)DE-He213 Desorption stages division (dpeaa)DE-He213 Tectonically deformed coal (dpeaa)DE-He213 Wu, Caifang aut Song, Yu aut Xian, Baoan aut Gao, Bin aut Zhang, Zhen aut Liu, Gaofeng (orcid)0000-0002-9340-9029 aut Enthalten in Transport in porous media Dordrecht [u.a.] : Springer Science + Business Media B.V, 1986 141(2022), 3 vom: 19. Jan., Seite 713-736 (DE-627)269017720 (DE-600)1473676-7 1573-1634 nnns volume:141 year:2022 number:3 day:19 month:01 pages:713-736 https://dx.doi.org/10.1007/s11242-022-01744-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 141 2022 3 19 01 713-736 |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR046373993</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230507121904.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">220303s2022 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s11242-022-01744-0</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR046373993</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s11242-022-01744-0-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Zhou, Dan</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Evolution Characteristic and Implication of Coalbed Methane Desorption Stages Division for Tectonically Deformed Coals</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2022</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© The Author(s), under exclusive licence to Springer Nature B.V. 2022</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract This paper discusses the evolution characteristic and implication of coalbed methane (CBM) desorption stages division with the tectonic deformation degree based on the $ CH_{4} $ isothermal adsorption/desorption experiments and desorption efficiency for the primary coal and tectonically deformed coals (TDCs). The results show the pressure drops for the three desorption stages divided contributing to the CBM productivity increase with the tectonic deformation degree. This evolution characteristic indicates the CBM productivity of the strong brittle and ductile deformation TDCs is greater than that of the primary coal and weak brittle deformation TDCs, while the actual productivity is prohibited by the special reservoir properties of low strength, low permeability, and stimulation difficulty. This study demonstrates the two reservoir stimulation methods of the staged hydraulic fracturing of horizontal well in roof strata and the double string screen pipe completion and flushing of horizontal well can be considered adaptive for the strong brittle and ductile deformation TDCs reservoirs. Also, the special water drainage and depressurization management need to be adopted in different TDCs reservoirs. The reasonable flow pressure for CBM production can be estimated by the evolution characteristics of the three key pressures and desorption stages division with the tectonic deformation degree. In summary, this study is of great significance for achieving high and stable CBM production in TDCs reservoirs. Article HighlightsThe evolution characteristic of CBM desorption stages division for TDCs was analyzed.The CBM productivity for the different types of TDCs was revealed.The implications of this study on CBM production for TDCs were discussed.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Coalbed methane</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Desorption efficiency</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Desorption stages division</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Tectonically deformed coal</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wu, Caifang</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Song, Yu</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Xian, Baoan</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Gao, Bin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zhang, Zhen</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Liu, Gaofeng</subfield><subfield code="0">(orcid)0000-0002-9340-9029</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Transport in porous media</subfield><subfield code="d">Dordrecht [u.a.] : Springer Science + Business Media B.V, 1986</subfield><subfield code="g">141(2022), 3 vom: 19. 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Evolution Characteristic and Implication of Coalbed Methane Desorption Stages Division for Tectonically Deformed Coals Coalbed methane (dpeaa)DE-He213 Desorption efficiency (dpeaa)DE-He213 Desorption stages division (dpeaa)DE-He213 Tectonically deformed coal (dpeaa)DE-He213 |
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Evolution Characteristic and Implication of Coalbed Methane Desorption Stages Division for Tectonically Deformed Coals |
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evolution characteristic and implication of coalbed methane desorption stages division for tectonically deformed coals |
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Evolution Characteristic and Implication of Coalbed Methane Desorption Stages Division for Tectonically Deformed Coals |
| abstract |
Abstract This paper discusses the evolution characteristic and implication of coalbed methane (CBM) desorption stages division with the tectonic deformation degree based on the $ CH_{4} $ isothermal adsorption/desorption experiments and desorption efficiency for the primary coal and tectonically deformed coals (TDCs). The results show the pressure drops for the three desorption stages divided contributing to the CBM productivity increase with the tectonic deformation degree. This evolution characteristic indicates the CBM productivity of the strong brittle and ductile deformation TDCs is greater than that of the primary coal and weak brittle deformation TDCs, while the actual productivity is prohibited by the special reservoir properties of low strength, low permeability, and stimulation difficulty. This study demonstrates the two reservoir stimulation methods of the staged hydraulic fracturing of horizontal well in roof strata and the double string screen pipe completion and flushing of horizontal well can be considered adaptive for the strong brittle and ductile deformation TDCs reservoirs. Also, the special water drainage and depressurization management need to be adopted in different TDCs reservoirs. The reasonable flow pressure for CBM production can be estimated by the evolution characteristics of the three key pressures and desorption stages division with the tectonic deformation degree. In summary, this study is of great significance for achieving high and stable CBM production in TDCs reservoirs. Article HighlightsThe evolution characteristic of CBM desorption stages division for TDCs was analyzed.The CBM productivity for the different types of TDCs was revealed.The implications of this study on CBM production for TDCs were discussed. © The Author(s), under exclusive licence to Springer Nature B.V. 2022 |
| abstractGer |
Abstract This paper discusses the evolution characteristic and implication of coalbed methane (CBM) desorption stages division with the tectonic deformation degree based on the $ CH_{4} $ isothermal adsorption/desorption experiments and desorption efficiency for the primary coal and tectonically deformed coals (TDCs). The results show the pressure drops for the three desorption stages divided contributing to the CBM productivity increase with the tectonic deformation degree. This evolution characteristic indicates the CBM productivity of the strong brittle and ductile deformation TDCs is greater than that of the primary coal and weak brittle deformation TDCs, while the actual productivity is prohibited by the special reservoir properties of low strength, low permeability, and stimulation difficulty. This study demonstrates the two reservoir stimulation methods of the staged hydraulic fracturing of horizontal well in roof strata and the double string screen pipe completion and flushing of horizontal well can be considered adaptive for the strong brittle and ductile deformation TDCs reservoirs. Also, the special water drainage and depressurization management need to be adopted in different TDCs reservoirs. The reasonable flow pressure for CBM production can be estimated by the evolution characteristics of the three key pressures and desorption stages division with the tectonic deformation degree. In summary, this study is of great significance for achieving high and stable CBM production in TDCs reservoirs. Article HighlightsThe evolution characteristic of CBM desorption stages division for TDCs was analyzed.The CBM productivity for the different types of TDCs was revealed.The implications of this study on CBM production for TDCs were discussed. © The Author(s), under exclusive licence to Springer Nature B.V. 2022 |
| abstract_unstemmed |
Abstract This paper discusses the evolution characteristic and implication of coalbed methane (CBM) desorption stages division with the tectonic deformation degree based on the $ CH_{4} $ isothermal adsorption/desorption experiments and desorption efficiency for the primary coal and tectonically deformed coals (TDCs). The results show the pressure drops for the three desorption stages divided contributing to the CBM productivity increase with the tectonic deformation degree. This evolution characteristic indicates the CBM productivity of the strong brittle and ductile deformation TDCs is greater than that of the primary coal and weak brittle deformation TDCs, while the actual productivity is prohibited by the special reservoir properties of low strength, low permeability, and stimulation difficulty. This study demonstrates the two reservoir stimulation methods of the staged hydraulic fracturing of horizontal well in roof strata and the double string screen pipe completion and flushing of horizontal well can be considered adaptive for the strong brittle and ductile deformation TDCs reservoirs. Also, the special water drainage and depressurization management need to be adopted in different TDCs reservoirs. The reasonable flow pressure for CBM production can be estimated by the evolution characteristics of the three key pressures and desorption stages division with the tectonic deformation degree. In summary, this study is of great significance for achieving high and stable CBM production in TDCs reservoirs. Article HighlightsThe evolution characteristic of CBM desorption stages division for TDCs was analyzed.The CBM productivity for the different types of TDCs was revealed.The implications of this study on CBM production for TDCs were discussed. © The Author(s), under exclusive licence to Springer Nature B.V. 2022 |
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Evolution Characteristic and Implication of Coalbed Methane Desorption Stages Division for Tectonically Deformed Coals |
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Wu, Caifang Song, Yu Xian, Baoan Gao, Bin Zhang, Zhen Liu, Gaofeng |
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| score |
7.3976994 |