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Jiang Feng, Du Jianguo, Wang Wanchun, Cao Zhenglin. The Study on High-Pressure-High-Temperature Aqueous PyrolysisⅠ. Influence of temperature and pressure on maturation of organic matter[J]. Acta Sedimentologica Sinica, 1998, 16(3): 153-155,160.
Citation: Jiang Feng, Du Jianguo, Wang Wanchun, Cao Zhenglin. The Study on High-Pressure-High-Temperature Aqueous PyrolysisⅠ. Influence of temperature and pressure on maturation of organic matter[J]. Acta Sedimentologica Sinica, 1998, 16(3): 153-155,160.

The Study on High-Pressure-High-Temperature Aqueous PyrolysisⅠ. Influence of temperature and pressure on maturation of organic matter

  • Received Date: 1990-01-24
  • Rev Recd Date: 1998-03-31
  • Publish Date: 1998-12-10
  • Immature organic matter(peat) were pyrolysized at temperatures ranging from 200℃ to 400℃ under high pressure ranging from 0.1 to 2 GPa in a closed system. As the index of maturation, vitrinite reflectance (Ro) of samples was measured. The results display that Ro value of samples tends to rise when temperature increases under constant pressure and the Ro value decreases when pressure increases under constant pressure. These results indicate that pressure is one of factors that influence the maturation of organic matter as important as temperature do, and the pressure can retard the thermal evolution of organic matter. The function of pressure has its interior kinetic principle. The role of pressure in organic maturation process of organic matter can't benig nored as suggested by results of experiment and fact of Geology. It has important theoretical and practical significance on studying the function and influence of pressure by means of pyrolysis
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    [10] .Schaefer R G. Determination of gross kinetic prarameters for petroleum formation from Jurassic source rocks of different maturity levels by means of laboratory experiments. Org. Geochem., 1990, 16(1~3): 115~120
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    [13] .范善发, 周中毅, 韩林木等. 压力以盆地深部有机质演化的影响. 第五届全国有机地球化学会议论文摘要汇编, 1992. 256~257
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  • Received:  1990-01-24
  • Revised:  1998-03-31
  • Published:  1998-12-10

The Study on High-Pressure-High-Temperature Aqueous PyrolysisⅠ. Influence of temperature and pressure on maturation of organic matter

Abstract: Immature organic matter(peat) were pyrolysized at temperatures ranging from 200℃ to 400℃ under high pressure ranging from 0.1 to 2 GPa in a closed system. As the index of maturation, vitrinite reflectance (Ro) of samples was measured. The results display that Ro value of samples tends to rise when temperature increases under constant pressure and the Ro value decreases when pressure increases under constant pressure. These results indicate that pressure is one of factors that influence the maturation of organic matter as important as temperature do, and the pressure can retard the thermal evolution of organic matter. The function of pressure has its interior kinetic principle. The role of pressure in organic maturation process of organic matter can't benig nored as suggested by results of experiment and fact of Geology. It has important theoretical and practical significance on studying the function and influence of pressure by means of pyrolysis

Jiang Feng, Du Jianguo, Wang Wanchun, Cao Zhenglin. The Study on High-Pressure-High-Temperature Aqueous PyrolysisⅠ. Influence of temperature and pressure on maturation of organic matter[J]. Acta Sedimentologica Sinica, 1998, 16(3): 153-155,160.
Citation: Jiang Feng, Du Jianguo, Wang Wanchun, Cao Zhenglin. The Study on High-Pressure-High-Temperature Aqueous PyrolysisⅠ. Influence of temperature and pressure on maturation of organic matter[J]. Acta Sedimentologica Sinica, 1998, 16(3): 153-155,160.
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