J4 ›› 2011, Vol. 41 ›› Issue (4): 1040-1047.

Previous Articles     Next Articles

Characteristic Comparison of Hydrocarbon Generation Kinetics Under Open-Closed Systems with Constant Heating Rates and Its Significance

LI Ting-ting1,WANG Min1|2,LU Shuang-fang1,TIAN Shan-si1,CHEN Guo-hui1,HAN Lu3   

  1. 1.College of Earth Sciences, Northeast Petroleum University, Daqing163318, Heilongjiang,China;
    2.Key Laboratory of Tectonics and Petroleum Resources (China University of Key Laboratory of Geosciences), Ministry of Eduction, Hubei Province, Wuhan430074, China;
    3.College of Horticulture Science and Technology|Hebei Normal University of Science and Technology, Qinhuangdao066004, Hebei|China
  • Received:2010-10-27 Online:2011-07-26 Published:2011-07-26

Abstract:

In order to reveal the difference of hydrocarbon generation kinetics characteristics and its geologic application under different experiment conditions, two thermal simulation apparatus (open and closed systems) are employed to pyrolyze coal sample from Songliao basin. According to the relationship between experimental product yields and temperature, the kinetic models of the oil/gas generated from organic matter are calibrated. Then the kinetic parameters obtained from two experimental systems are extrapolated under the experimental heating rate and the geological heating rate, the results show that the TR (transformation ratio) increasing rate of the gas generation under closed system is slower than that under open system, the reason is that the coal sample pyrolysis to gas under open system is mainly primary cracking, but under closed system it is a common result of primary and secondary cracking. For further application, the hydrocarbon generation threshold is calculated, which combined the burial-thermal history of Xujiaweizi and the kinetic parameters obtained from two experimental systems. And the extrapolation result shows that the calculated geological time (115 Ma) corresponding to the threshold from open system is earlier than the geological time corresponding to the actual threshold (110 Ma), and the calculated geological time (92 Ma) corresponding to the threshold from closed system is later than the geological time corresponding to the actual threshold.

Key words: open system, closed system, hydrocarbon generation kinetics, hydrocarbon generation threshold, Xujiaweizi

CLC Number: 

  • P618.13
[1] Gao Bo, Pan Zhejun, Liu Lianjie, Li Lingling, Hong Shuxin, Pan Huifang, Zhang Bo. Comprehensive Evaluation on the Effectiveness of Conglomerate Reservoir in Shahezi Formation of Xujiaweizi Fault Depression, Songliao Basin [J]. Journal of Jilin University(Earth Science Edition), 2025, 55(1): 31-45.
[2] Zhou Xiang, Li Shaohu. Diagenesis in Sequence Stratigraphical Framework: A Case Study on Shahezi Formation in Xujiaweizi Fault Depression [J]. Journal of Jilin University(Earth Science Edition), 2022, 52(6): 1800-1812.
[3] Zhang Dazhi, Chu Lilan, Zhou Xiang, Wang Xiaolian, Li Xin. Diagenesis and Diagenesis Facies of Tight Gas Reservoir of Shahezi Formation, in Xujiaweizi Fault Depression of North Songliao Basin [J]. Journal of Jilin University(Earth Science Edition), 2021, 51(1): 22-34.
[4] Chen Shumin,Jiang Chuanjin,Liu Li,Chu Lilan,Pei Mingbo. Fracture Formation Mechanism of Volcanic Rocks in Xujiaweizi Fault Depression of Songliao Basin [J]. Journal of Jilin University(Earth Science Edition), 2014, 44(6): 1816-1826.
[5] Meng Fanchao, Liu Jiaqi,Cui Yan. Petrogenesis and Crypto-Explosive Mechanism of Trachyte in Yingcheng Formation of Xujiawei Fault Depression, Songliao Basin, NE China [J]. Journal of Jilin University(Earth Science Edition), 2013, 43(3): 704-715.
[6] FU Guang, HU Ming, HAN Ying. Controlling of Faults to Gas Accumulation of Volcanic Rock in Depression Basin: An Example from Xujiaweizi Depression of Songliao Basin [J]. J4, 2012, 42(1): 1-8.
[7] FU Guang, ZANG Feng-zhi. Favorable Geological Conditions for Formation of Xushen Large Gas Field [J]. J4, 2011, 41(1): 12-20.
[8] QI Jing-shun, LI Guang-wei, SUN Li-dong, XIE Hao, LIU Qiang-min. The Research on Sequence Stratigraphy and Sedimentary Facies of the Member 4 of Yingcheng Formation in Xujiaweizi Depression [J]. J4, 2009, 39(6): 983-990.
[9] FU Guang, PANG Lei. Quantitative Study on Formation Conditions of Different Reserves Abundance of Gas Reservoirs in Xujiaweizi Depression [J]. J4, 2009, 39(6): 976-982.
[10] XU Dan, FU Xiao-fei, LV Yan-fang, FU Guang, HU Ming. Cap-Rock Characteristic and Sealing Ability Evaluation of Deep Xujiaweizi Fault Depression [J]. J4, 2009, 39(5): 773-780.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] Wu Yuankun, Liu Chenglin, Yu Chunyong.. Main Controlling Factors and Accumulation Mode of Deep Oil in Shuangcheng Fault Depression of Songliao Basin[J]. Journal of Jilin University(Earth Science Edition), 2024, 54(5): 1443 -1456 .
[2] Ma Rong, Shi Jiansheng, Liu Jichao. Application of Artificial Endocrine Network Model in Studying of Hydrogeology Parameter[J]. Journal of Jilin University(Earth Science Edition), 2013, 43(3): 914 -921 .
[3] Li Ning, Wang Chengwen. Formation and Evolution of Jiamusi-Mongolia Block and Contact Relationship of Late Paleozoic Strata in Northeast China and Adjacent Region[J]. Journal of Jilin University(Earth Science Edition), 2017, 47(5): 1331 -1340 .
[4] HU Da-qian, CHU Feng-you, YAO Jie. The Mineral Composition and Element Geochimestry of CoEnriched Crust from the YJA Sea Mount in the Central Pacific Ocean[J]. J4, 2006, 36(01): 32 -0037 .
[5] JIANG Xue, CHENG Ri-hui, YU Min-feng. Climate and Tectonic Controls on the Rift Stratigraphy:Analysis of Zscape Model and its Application in the BeianFaulting Depression of the Songliao Basin[J]. J4, 2006, 36(01): 54 -0059 .
[6] LI Chun-bai,ZHANG Xin-tao,LIU Li,REN Yan-guang,MENG Peng. The Thermal Fluid Activities and Their Modification on Volcaniclastic Rock in Budate Group-An Example from the Beier Sag of Hailaer Basin[J]. J4, 2006, 36(02): 221 -0226 .
[7] Meng Xiangang, Bo Wanju, Liu Zhiguang, LiuYong, Chang Liu, Li Chaozhu, Wang Ziping. Activity in the Middle East of Bayan Har Block with Lushan MS 7.0 Earthquake[J]. Journal of Jilin University(Earth Science Edition), 2014, 44(5): 1705 -1711 .
[8] Chen Huanqing, Liang Shuxian, Shu Zhirui, Deng Xiaojuan, Peng Shouchang. Characteristics of Conglomerate Reservoir Architecture of Alluvial Fan and Its Controlling Effects to Reservoir Development:Taking Alluvial Fan Reservoir in Some Area of Northwest Margin of Junggar Basin as an Example[J]. Journal of Jilin University(Earth Science Edition), 2015, 45(1): 13 -24 .
[9] JIA Dacheng, XING Lixin, PAN Jun, M. J. van Bergen, H. van Roermund. Geochemical Characteristics of the AluminumEnriched Spinels in Xenoliths from the Upper Mantle Shear Belt in Yitong,Northeastern China[J]. J4, 2006, 36(04): 497 -502 .
[10] XIE Zhong-lei, YANG Bai-ling, BAO Guo-zhang,DONG De-ming. Fractionation and Its Affecting Factors of Nickel in Tea Garden Soils[J]. J4, 2006, 36(04): 599 -604 .