西南石油大学学报(自然科学版) ›› 2019, Vol. 41 ›› Issue (1): 1-17.DOI: 10.11885/j.issn.1674-5086.2018.01.01.01

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Mechanism of Complex Modes of the Pore Structure of Sandstone/Conglomerate Reservoirs

YIN Senlin1, CHEN Gongyang1, CHEN Yukun2, WU Xiaojun2   

  1. 1. Institute of Mud Logging Technology and Engineering, Yangtze University, Jingzhou, Hubei 434023, China;
    2. Research Institute of Exploration and Development, Xinjiang Oilfield Company, CNPC, Karamay, Xinjiang 834000, China
  • Received:2018-01-01 Online:2019-02-10 Published:2019-02-10

Abstract: The formation mechanism of complex modes of the pore structure of sandstone/conglomerate reservoirs is still unclear. Thus, this study investigated the difference mechanisms of lithofacies classification, pore structure modes, and displacement efficiencies based on experimental data of 325 core examples through mercury intrusion porosimetry, cast thin sections, scanning electron microscopy, and X-ray computed tomography. The results reveal that, taking both oil field exploitation and utility into consideration, lithofacies of sandstone/conglomerate reservoirs can be classified to 3 primary categories, 7 secondary categories, and 13 tertiary categories. They have different pore structure modal characteristics and relatively great variance in their efficiency of displacement by water injection. Single-mode rock particles are mostly coarse sandstones with highly developed and relatively well inter-connected pores in a network structure. The displacement by water injection is mainly via connected networks, resulting in higher efficiency. Dual-mode rock particles are composed of two classes of particles:conglomerates and medium-coarse sandstones. They have relatively developed and moderately inter-connected pores in a sparse network structure. The displacement, here, is mainly via star-shaped connected networks, with ordinary efficiency. Complexmode rock particles consist of three types of particles:conglomerates, medium-coarse sandstones, and silt or mud. Their pores are moderately developed and relatively poorly inter-connected with a star-shaped networking structure. The water injectiondriven displacement is mostly scattered over local high-permeability zones, resulting in poor overall efficiency. The same lithofacies typically show different pore structure modes while different lithofacies can have identical structure modes. Differential transformation due to particle configuration and diagenesis leads to different pore structure modes for identical lithofacies; while sorting, rounding, and arrangement of particles result in identical pore structure modes for different lithofacies.

Key words: sandstone/conglomerate reservoir, pore structure, complex mode, alluvial fan, lithofacies, displacement efficiency

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