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Zhang Tongwei, Wang Xianbin, Chen Jianfa. The Chromat Fractional Effect of Vertical Oil一gas Microleapage[J]. Acta Sedimentologica Sinica, 1994, 12(4): 110-117.
Citation: Zhang Tongwei, Wang Xianbin, Chen Jianfa. The Chromat Fractional Effect of Vertical Oil一gas Microleapage[J]. Acta Sedimentologica Sinica, 1994, 12(4): 110-117.

The Chromat Fractional Effect of Vertical Oil一gas Microleapage

  • Received Date: 1993-11-10
  • Publish Date: 1994-12-10
  • Ordos basin is a large sedimentary basin in the eastern China. In the inner of the basin,faults donut develop and strata are flat(the angle of inclination is less than one degree),so the possibility that oil and gas can migrate along faults should be ruled out, and then oll and gas microleapage through the fractures and pores in strata should be main form for oil and gas vertical migration. A deep gas-producing well, which is located in the central ancient rift in the inner of the basin,is chosen for study. According to the characteristics of the vertical evolution of organic matter and the change of acidolysis hydrocarbon compositions in different clastic rock layers from the deep well, the chromatographic fractional effect of vertical oil-gas microleapage has been discussed. Owing to the chemical and physical difference among methane and its homologes in mass number,molecular diameter, and the solubility in water, etc.,methane and i-butane preferentially migrate to heavier hydrocarbon and n- butane,respectively. Because the concentation of organic matter is low and the amount of hydrocarbon generated in situ is accordingly little in the two sections which range from 0 to 1020m and 3080m to 3560m in depth,so the above chromatographic effect can be recorded. 1. In the section from 0 to 1020m depth, the result shows that the ratios of C1/C2+,C1/Ctal, and iC4/nC4, of acidolysis hydrocarbon gases in sandstone are less than those in mudstone. It mainly results from the chromatographic fractional effect, i. e.,methane and i-butane are relativeiy easier to go through poorly permeabie mudstone barrier bed than heavier hydrocarbon and n- butane respectively. 2. In the section from 3080m to 3560m depth,the maturity of organic matter is in condensate to high mature stage,the composition of gas generated by such matter should be increasingly drier and therefore the ratios of C1/C2+,C1/Ctal,tend to rise with depth. However, the change of the ratios shows a controversial tendency and an obvious inconsistence with the composition characteristics of gas generated by thermolization,suggesting that methane preferentially migrates to heavier hydrocarbon. In addition,the changing characteristics of C1/C2+,C1/Ctal and C2/C3 ratios of the acidolysis hydrocarbon in the layers rich in organic matter ( the depth from 1020m to 3080m),which decreases firstly and increases consequently with depth,is controlled by the generation of hydrocarbon in situ and hence the chromatographic fractional effect is concealed.
  • [1] A. Mackenize ,D. Leythaeuser and R. Schaefer, expulsion of petroleum hydrocarbons from shale rocks. Nature, 1983,301:506~509.
    [2] D. l.eythaeuser, A. Mackenzie and R. Schaefer et al.,1984. A novel approe由for recognition and quantification of hydrocarbon migration effects in shale-sandstone sequences. AAPG,68(2):196~219.
    [3] D. Leythaeuser,R.,Schaefer and H. Pooch. Diffusion of light hydrocarbon in subsurface sedimentary rocks, AAPG, 1983.67(6):889-895.
    [4] 赵重远等,含油气盆地地质学研究进展.西北大学出版社,西安:1993.321~328.
    [5] 高瑞琪等,石油地质实验手册,黑龙江科技出版社,哈尔滨.1992,
    [6] 郊立言等,生油岩热解快速定量评价,科学出版社,北京:1986.44~45.
    [7] J. K. Whelan, J. W. Farrington and M. E. Tarafa, Maturity of organic matter and migration of hydrocarbons in two Alaskan North Slop wells. Organic Geochemistry,1986.10:207~219.
    [8] E. M. Galimov, Sources and mechanisms of formation of gaseous hydrocarbons in sedimentary racks, Chemical Geology, 1988. 71(1/3) :77~95.
    [9] 徐永昌,沈平,天然气成因新模式一I.多阶连续、主阶定名,中国科学((B辑).1993.23(7);751·755,
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  • Received:  1993-11-10
  • Published:  1994-12-10

The Chromat Fractional Effect of Vertical Oil一gas Microleapage

Abstract: Ordos basin is a large sedimentary basin in the eastern China. In the inner of the basin,faults donut develop and strata are flat(the angle of inclination is less than one degree),so the possibility that oil and gas can migrate along faults should be ruled out, and then oll and gas microleapage through the fractures and pores in strata should be main form for oil and gas vertical migration. A deep gas-producing well, which is located in the central ancient rift in the inner of the basin,is chosen for study. According to the characteristics of the vertical evolution of organic matter and the change of acidolysis hydrocarbon compositions in different clastic rock layers from the deep well, the chromatographic fractional effect of vertical oil-gas microleapage has been discussed. Owing to the chemical and physical difference among methane and its homologes in mass number,molecular diameter, and the solubility in water, etc.,methane and i-butane preferentially migrate to heavier hydrocarbon and n- butane,respectively. Because the concentation of organic matter is low and the amount of hydrocarbon generated in situ is accordingly little in the two sections which range from 0 to 1020m and 3080m to 3560m in depth,so the above chromatographic effect can be recorded. 1. In the section from 0 to 1020m depth, the result shows that the ratios of C1/C2+,C1/Ctal, and iC4/nC4, of acidolysis hydrocarbon gases in sandstone are less than those in mudstone. It mainly results from the chromatographic fractional effect, i. e.,methane and i-butane are relativeiy easier to go through poorly permeabie mudstone barrier bed than heavier hydrocarbon and n- butane respectively. 2. In the section from 3080m to 3560m depth,the maturity of organic matter is in condensate to high mature stage,the composition of gas generated by such matter should be increasingly drier and therefore the ratios of C1/C2+,C1/Ctal,tend to rise with depth. However, the change of the ratios shows a controversial tendency and an obvious inconsistence with the composition characteristics of gas generated by thermolization,suggesting that methane preferentially migrates to heavier hydrocarbon. In addition,the changing characteristics of C1/C2+,C1/Ctal and C2/C3 ratios of the acidolysis hydrocarbon in the layers rich in organic matter ( the depth from 1020m to 3080m),which decreases firstly and increases consequently with depth,is controlled by the generation of hydrocarbon in situ and hence the chromatographic fractional effect is concealed.

Zhang Tongwei, Wang Xianbin, Chen Jianfa. The Chromat Fractional Effect of Vertical Oil一gas Microleapage[J]. Acta Sedimentologica Sinica, 1994, 12(4): 110-117.
Citation: Zhang Tongwei, Wang Xianbin, Chen Jianfa. The Chromat Fractional Effect of Vertical Oil一gas Microleapage[J]. Acta Sedimentologica Sinica, 1994, 12(4): 110-117.
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