Journal of Jilin University(Earth Science Edition) ›› 2021, Vol. 51 ›› Issue (1): 35-51.doi: 10.13278/j.cnki.jjuese.20190272

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Fluid Mobility and Its Influencing Factors of Tight Sandstone Reservoirs in China

Wu Meng1,2, Qin Yong1, Wang Xiaoqing3, Li Guozhang1, Zhu Chao1, Zhu Shifei2   

  1. 1. Key Laboratory of CBM Resource and Reservoir Formation Process, Ministry of Education, Xuzhou 221008, Jiangsu, China;
    2. Jiangsu Mineral Resources and Geological Design and Research Institute, Xuzhou 221006, Jiangsu, China;
    3. College of Resources and Environment, Henan Polytechnic University, Jiaozuo 454000, Henan, China
  • Received:2019-12-16 Published:2021-02-02
  • Supported by:
    Supported by the National Science and Technology Major Project of China(2016ZX050660104) and the National Natural Science Foundation of China(42002193)

Abstract: Fluid mobility of tight sandstone reservoirs is of great significance for oil and gas development, prediction,and evaluation. According to relevant domestic achievements in the past ten years, the fluidity parameters, test methods, distribution characteristics,and influencing factors of tight reservoirs were analyzed. It is found that the T2 value of tight sandstone reservoirs is 0.540-41.600 ms, the porosity of the movable fluid is 0.12%-14.35%, the saturation of the movable fluid is 2.16%-90.30%, the lower limit of the pore throat radius of movable fluids in tight reservoirs is 0.013-0.110 μm, the lower limit of pore-throat radius of high pressure mercury injection, nuclear magnetic resonance,and constant velocity mercury injection are 0.037 5 μm, 0.070 0-0.200 0 μm,and 0.120 0 μm respectively, and the water film thickness is 0.05-1.00 μm. Ⅲ-Ⅳ reservoirs are the main types of tight sandstone reservoirs. Statistical analysis shows that the mobile flow saturation of tight reservoirs is low, which is measured by nuclear magnetic resonance and constant velocity mercury injection. The water film thickness is the main factor affecting fluid seepage in tight sandstone reservoirs. The saturation of movable fluid of low-rank coal seams is the highest, the second is that of tight sandstone reservoirs, and the lowest is that of shale reservoirs. The movable fluid porosity of tight sandstone reservoirs is 10 times more than that of shale reservoirs and low-rank coal seams. The movable fluids in sandstone reservoirs exist in pores and throats, and are controlled by these pores and throats. Tight sandstone has a concentrated throat distribution and poor effective pore development, and most of the pores are micropores with a throat diameter less than 1.000 μm. The more concentrated the throat radius, the larger the effective throat radius, and the more favorable the seepage of the reservoir fluid. Lower sandstone permeability (<2×10-3 μm2) leads to faster decay of movable fluid parameters; and higher permeability (>2×10-3 μm2) leads to slower rise of movable fluid parameters. The throat radius is the main factor controlling fluid mobility of tight reservoirs.

Key words: tight sandstone, fluid mobility, micropore structure, wettability, pore-throat radius

CLC Number: 

  • TE122.221
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