EVOLUTION OF METHANE FROM DEEP SOURCE AND ORIGIN OF CARBON DIOXIDE

LIU Bin

doi:10.11781/sysydz198902167

Volume 11 Issue 2

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LIU Bin. EVOLUTION OF METHANE FROM DEEP SOURCE AND ORIGIN OF CARBON DIOXIDE[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1989, 11(2): 167-176. doi: 10.11781/sysydz198902167

Citation:

LIU Bin. EVOLUTION OF METHANE FROM DEEP SOURCE AND ORIGIN OF CARBON DIOXIDE[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1989, 11(2): 167-176. doi: 10.11781/sysydz198902167

LIU Bin. EVOLUTION OF METHANE FROM DEEP SOURCE AND ORIGIN OF CARBON DIOXIDE[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1989, 11(2): 167-176. doi: 10.11781/sysydz198902167

Citation:

LIU Bin. EVOLUTION OF METHANE FROM DEEP SOURCE AND ORIGIN OF CARBON DIOXIDE[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1989, 11(2): 167-176. doi: 10.11781/sysydz198902167

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EVOLUTION OF METHANE FROM DEEP SOURCE AND ORIGIN OF CARBON DIOXIDE

doi: 10.11781/sysydz198902167

LIU Bin

Central Laboratory of Petroleum Geology, Ministry of Geology and Mineral Resources

Publish Date: 1989-04-25

Abstract

Abstract

Considering the equilibrium system of CH₄-H₂O-CO₂ and the reaction of methane with CaSO₄(gypsum)in water for example,with the viewpoint of statistical thermodynamics and chemical thermodynamic equilibrium,the conditions and direction of the reaction are studied,as a result,the rela-tion of equilibrium constant and temperature-pressure are inferred.Besides,the neccessary conditions for the preservation and destruction of methane gas under different burial depths and for the generation of carbon dioxide are discussed.It is proposed that the acidity of sedimentary environment,or the pH value,is an important factor which acts in conjunction with temperature in the hydrolysis of carbonate rocks.

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References

[1]	傅献彩等,1979,物理化学,人民教育出版社,1979年修订本.
[2]	唐有祺,1979,统计力学及其在物理化学中的应用,科学出版社.
[3]	叶大纶,1981,实用无机物热力学数据手册,冶金工业出版社.

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EVOLUTION OF METHANE FROM DEEP SOURCE AND ORIGIN OF CARBON DIOXIDE

doi: 10.11781/sysydz198902167

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EVOLUTION OF METHANE FROM DEEP SOURCE AND ORIGIN OF CARBON DIOXIDE

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