Gas generation from coal: taking Jurassic coal in the Minhe Basin as an example

Abstract The gas generation features of coals at different maturities were studied by the anhydrous pyrolysis of Jurassic coal from the Minhe Basin in sealed gold tubes at 50 MPa. The gas component yields (C1, C2, C3, i-C4, n-C4, i-C5, n-C5, and CO2); the δ 13C of C1, C2, C3, and CO2; and the mass o...

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Main Authors: Deliang Fu, Guosheng Xu, Li Ma, Fu Yang, Dan He, Zhonghui Duan, Yu Ma
Format: Article
Language:English
Published: SpringerOpen 2020-04-01
Series:International Journal of Coal Science & Technology
Subjects:
Online Access:https://doi.org/10.1007/s40789-020-00318-z
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spelling doaj-9d1035da6a8140eeac84616b717073ae2021-04-25T11:29:27ZengSpringerOpenInternational Journal of Coal Science & Technology2095-82932198-78232020-04-017361162210.1007/s40789-020-00318-zGas generation from coal: taking Jurassic coal in the Minhe Basin as an exampleDeliang Fu0Guosheng Xu1Li Ma2Fu Yang3Dan He4Zhonghui Duan5Yu Ma6Key Laboratory of Coal Exploration and Comprehensive Utilization, Ministry of Nature and Resources, Shaanxi Coal Geology Group Co., Ltd.College of Energy, Chengdu University of TechnologyKey Laboratory of Coal Exploration and Comprehensive Utilization, Ministry of Nature and Resources, Shaanxi Coal Geology Group Co., Ltd.Key Laboratory of Coal Exploration and Comprehensive Utilization, Ministry of Nature and Resources, Shaanxi Coal Geology Group Co., Ltd.Key Laboratory of Coal Exploration and Comprehensive Utilization, Ministry of Nature and Resources, Shaanxi Coal Geology Group Co., Ltd.Key Laboratory of Coal Exploration and Comprehensive Utilization, Ministry of Nature and Resources, Shaanxi Coal Geology Group Co., Ltd.Ningxia Institute of Geological SurveyAbstract The gas generation features of coals at different maturities were studied by the anhydrous pyrolysis of Jurassic coal from the Minhe Basin in sealed gold tubes at 50 MPa. The gas component yields (C1, C2, C3, i-C4, n-C4, i-C5, n-C5, and CO2); the δ 13C of C1, C2, C3, and CO2; and the mass of the liquid hydrocarbons (C6+) were measured. On the basis of these data, the stage changes of δ 13C1, δ 13C2, δ 13C3, and δ 13CO2 were calculated. The diagrams of δ 13C1–δ 13C2 vs ln (C1/C2) and δ 13C2–δ 13C1 vs δ 13C3–δ 13C2 were used to evaluate the gas generation features of the coal maturity stages. At the high maturity evolution stage (T > 527.6 °C at 2 °C/h), the stage change of δ 13C1 and the CH4 yield are much higher than that of CO2, suggesting that high maturity coal could still generate methane. When T < 455 °C, CO2 is generated by breaking bonds between carbons and heteroatoms. The reaction between different sources of coke and water may be the reason for the complicated stage change in $$\delta^{{{13}}} {\text{C}}_{{{\text{CO}}_{{2}} }}$$ δ 13 C CO 2 when the temperature was higher than 455 °C. With increasing pyrolysis temperature, δ 13C1–δ 13C2 vs ln (C1/C2) has four evolution stages corresponding to the early stage of breaking bonds between carbon and hetero atoms, the later stage of breaking bonds between carbon and hetero atoms, the cracking of C6+ and coal demethylation, and the cracking of C2–5. The δ 13C2–δ 13C1 vs δ 13C3–δ 13C2 has three evolution stages corresponding to the breaking bonds between carbon and hetero atoms, demethylation and cracking of C6+, and cracking of C2–5.https://doi.org/10.1007/s40789-020-00318-zJurassic coalPyrolysisGas generationδ 13CStage evolution
collection DOAJ
language English
format Article
sources DOAJ
author Deliang Fu
Guosheng Xu
Li Ma
Fu Yang
Dan He
Zhonghui Duan
Yu Ma
spellingShingle Deliang Fu
Guosheng Xu
Li Ma
Fu Yang
Dan He
Zhonghui Duan
Yu Ma
Gas generation from coal: taking Jurassic coal in the Minhe Basin as an example
International Journal of Coal Science & Technology
Jurassic coal
Pyrolysis
Gas generation
δ 13C
Stage evolution
author_facet Deliang Fu
Guosheng Xu
Li Ma
Fu Yang
Dan He
Zhonghui Duan
Yu Ma
author_sort Deliang Fu
title Gas generation from coal: taking Jurassic coal in the Minhe Basin as an example
title_short Gas generation from coal: taking Jurassic coal in the Minhe Basin as an example
title_full Gas generation from coal: taking Jurassic coal in the Minhe Basin as an example
title_fullStr Gas generation from coal: taking Jurassic coal in the Minhe Basin as an example
title_full_unstemmed Gas generation from coal: taking Jurassic coal in the Minhe Basin as an example
title_sort gas generation from coal: taking jurassic coal in the minhe basin as an example
publisher SpringerOpen
series International Journal of Coal Science & Technology
issn 2095-8293
2198-7823
publishDate 2020-04-01
description Abstract The gas generation features of coals at different maturities were studied by the anhydrous pyrolysis of Jurassic coal from the Minhe Basin in sealed gold tubes at 50 MPa. The gas component yields (C1, C2, C3, i-C4, n-C4, i-C5, n-C5, and CO2); the δ 13C of C1, C2, C3, and CO2; and the mass of the liquid hydrocarbons (C6+) were measured. On the basis of these data, the stage changes of δ 13C1, δ 13C2, δ 13C3, and δ 13CO2 were calculated. The diagrams of δ 13C1–δ 13C2 vs ln (C1/C2) and δ 13C2–δ 13C1 vs δ 13C3–δ 13C2 were used to evaluate the gas generation features of the coal maturity stages. At the high maturity evolution stage (T > 527.6 °C at 2 °C/h), the stage change of δ 13C1 and the CH4 yield are much higher than that of CO2, suggesting that high maturity coal could still generate methane. When T < 455 °C, CO2 is generated by breaking bonds between carbons and heteroatoms. The reaction between different sources of coke and water may be the reason for the complicated stage change in $$\delta^{{{13}}} {\text{C}}_{{{\text{CO}}_{{2}} }}$$ δ 13 C CO 2 when the temperature was higher than 455 °C. With increasing pyrolysis temperature, δ 13C1–δ 13C2 vs ln (C1/C2) has four evolution stages corresponding to the early stage of breaking bonds between carbon and hetero atoms, the later stage of breaking bonds between carbon and hetero atoms, the cracking of C6+ and coal demethylation, and the cracking of C2–5. The δ 13C2–δ 13C1 vs δ 13C3–δ 13C2 has three evolution stages corresponding to the breaking bonds between carbon and hetero atoms, demethylation and cracking of C6+, and cracking of C2–5.
topic Jurassic coal
Pyrolysis
Gas generation
δ 13C
Stage evolution
url https://doi.org/10.1007/s40789-020-00318-z
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