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致密岩心带压渗吸规律实验研究

江昀 许国庆 石阳 余玥 王天一 曾星航 郑伟

江昀, 许国庆, 石阳, 余玥, 王天一, 曾星航, 郑伟. 致密岩心带压渗吸规律实验研究[J]. 石油实验地质, 2021, 43(1): 144-153. doi: 10.11781/sysydz202101144
引用本文: 江昀, 许国庆, 石阳, 余玥, 王天一, 曾星航, 郑伟. 致密岩心带压渗吸规律实验研究[J]. 石油实验地质, 2021, 43(1): 144-153. doi: 10.11781/sysydz202101144
JIANG Yun, XU Guoqing, SHI Yang, YU Yue, WANG Tianyi, ZENG Xinghang, ZHENG Wei. Forced imbibition in tight sandstone cores[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2021, 43(1): 144-153. doi: 10.11781/sysydz202101144
Citation: JIANG Yun, XU Guoqing, SHI Yang, YU Yue, WANG Tianyi, ZENG Xinghang, ZHENG Wei. Forced imbibition in tight sandstone cores[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2021, 43(1): 144-153. doi: 10.11781/sysydz202101144

致密岩心带压渗吸规律实验研究

doi: 10.11781/sysydz202101144
基金项目: 

国家科技重大专项“致密油储层高效体积改造技术” 2016ZX05046-004

详细信息
    作者简介:

    江昀(1990-), 男, 博士, 工程师, 从事非常规储层改造基础理论研究。E-mail: jiangyun119@petrochina.com.cn

    通讯作者:

    石阳(1983-), 男, 高级工程师, 从事油气藏改造与保护。E-mail: shy312@petrochina.com.cn

  • 中图分类号: TE311

Forced imbibition in tight sandstone cores

  • 摘要: 致密油藏体积改造压后闷井过程中发生的渗吸置换,通常在压差(基质外部流体压力与孔隙压力之差)作用下进行,但渗吸置换物理模拟却通常在常压下进行(即自发渗吸),带压条件下的渗吸置换特征尚未提及。为研究压差作用下的渗吸置换(即带压渗吸)规律,首先,建立基于低场核磁共振测试技术的带压渗吸实验方法;其次,分析自发/带压渗吸的异同;最后,建立带压渗吸无因次时间模型。结果表明,质量分数为96.76%~97.25%的油相集中分布于纳米孔(1 ms ≤ T2 ≤ 100 ms)内,纳米孔是主要储集空间;相比于自发渗吸,带压渗吸置换效率大幅提升是由强化的渗吸作用和压实作用共同造成的;岩心尺度建立的带压渗吸无因次时间模型可行,为确定油藏尺度压后闷井时间提供了新思路。

     

  • 图  1  压后闷井过程中两相渗流区域示意

    Figure  1.  Schematic diagram for two-phase flow regions during shut-in period

    图  2  渗吸作用主导的两相渗流区内压差作用下逆向渗吸示意

    Figure  2.  Counter-current imbibition under forced pressure in two-phase seepage zone dominated by imbibition

    图  3  自发/带压渗吸实验装置示意

    Figure  3.  Schematic diagram of experimental devices for spontaneous imbition/forced imbition

    图  4  高压压汞测试中孔隙直径分布结果(a) 和低场核磁共振T2谱(b)

    Figure  4.  Pore size distribution of core samples (a) and T2 by Low-field nuclear magnetic resonance (b) in high pressure mercury injection

    图  5  自发/带压渗吸置换效率随时间(a)和时间平方根(b)变化关系曲线

    Figure  5.  Oil recovery for SI/FI vs. imbibition time (a) and its square root (b)

    图  6  有效孔隙半径随有效应力变化关系曲线

    Figure  6.  Effective pore radius vs. net confining stress

    图  7  自发渗吸T2谱及孔隙油相分布(a) 和选定时间节点测定的T2谱渗吸实验前后纳米孔隙内油相分布(b)

    Figure  7.  T2 distribution during SI and corresponding frequency of oil distribution in pores at selected time intervals (a) and frequency of oil distribution in nanopores before and after SI (b)

    图  8  带压渗吸T2谱及孔隙油相分布(a-d) 和选定时间节点测定的T2谱渗吸实验前后纳米孔隙内油相分布(e-h)

    Figure  8.  T2 distribution during FI and corresponding frequency of oil distribution in pores at selected time intervals (a-d) and frequency of oil distribution in nanopores before and after FI (e-h)

    图  9  渗吸置换效率随无因次时间变化关系曲线

    Figure  9.  Oil recovery as a function of dimensionless time

    表  1  带压渗吸实验岩心样品物性参数

    Table  1.   Petrophysical properties of tight core samples for forced imbibition experiment

    类别 编号 深度/m 直径/cm 长度/cm 渗透率/(10-3 μm2) 孔隙度/%
    高压压汞 A11 2 179.7 2.51 1.76 0.034 10.54
    A12 2 179.9 2.53 1.71 0.030 9.71
    A13 2 180.4 2.53 1.70 0.048 12.53
    A14 2 180.6 2.53 1.72 0.031 8.79
    A15 2 180.6 2.53 1.71 0.049 11.32
    自发/带压渗吸 A21 2 179.7 2.51 5.21 0.034 10.54
    A22 2 179.9 2.53 5.26 0.030 9.71
    A23 2 180.4 2.53 4.96 0.048 12.53
    A24 2 180.6 2.53 5.23 0.031 8.79
    A25 2 180.6 2.53 4.60 0.049 11.32
    接触角 B11 2 176.6 2.53 1.35 0.048 12.37
    B12 2 177.6 2.53 1.28 0.057 10.69
    B13 2 178.4 2.53 1.32 0.023 8.42
    含油量标定 B21 2 176.6 2.53 3.62 0.048 12.37
    B22 2 177.6 2.53 3.66 0.057 10.69
    B23 2 178.4 2.53 3.61 0.023 8.42
    脉冲衰减 C1 2 179.2 2.51 3.24 0.026 10.25
    C2 2 180.5 2.52 3.21 0.015 7.57
    C3 2 180.8 2.52 3.27 0.037 10.67
    C4 2 180.7 2.53 3.51 0.014 7.36
    下载: 导出CSV

    表  2  带压渗吸实验流体样品物性参数(20 ℃, 1 atm)

    Table  2.   Physical properties of fluid samples for forced imbibition experiment

    流体类型 密度/(g·cm-3) 黏度/(mPa·s) 界面张力/(mN·m-1)
    煤油 0.83 2.53 26.82
    氘水 1.09 1.25 72.75
    下载: 导出CSV

    表  3  平均值法表面弛豫率计算结果

    Table  3.   Calculation results of surface relaxation by average method

    岩心编号 T2LM/ms Rp/nm ρ/(μm·s-1)
    A21 3.11 34.2 2.75
    A22 5.49 78.2 3.56
    A23 2.08 58.5 7.02
    A24 1.29 55.3 10.68
    A25 3.20 81.4 6.37
    下载: 导出CSV

    表  4  基于低场核磁T2值的孔隙类型分类

    Table  4.   Pore size classification based on T2 value by low-field nuclear magnetic resonance

    T2/ms 孔隙直径/nm 孔隙类型
    0.1~100 1~1 000 纳米孔
    ≥100 ≥1 000 微孔/中孔
    下载: 导出CSV

    表  5  气体滑脱因子与平均孔隙半径计算结果

    Table  5.   Gas slippage factor and average pore radius

    岩心编号 有效应力/MPa 克氏渗透率/(10-3μm2) 气体滑脱因子/MPa 有效孔隙半径/μm
    C1 2.5 0.016 0 0.34 0.53
    5.0 0.007 8 0.59 0.31
    10.0 0.002 0 1.42 0.13
    15.0 0.001 0 3.22 0.06
    C2 2.5 0.009 5 0.60 0.30
    5.0 0.008 1 0.80 0.23
    10.0 0.001 6 1.45 0.13
    15.0 0.000 6 1.81 0.10
    C3 2.5 0.018 0 0.38 0.48
    5.0 0.004 1 1.29 0.14
    10.0 0.002 1 1.90 0.10
    15.0 0.001 1 2.02 0.09
    C4 2.5 0.009 2 0.56 0.33
    5.0 0.004 2 1.23 0.15
    10.0 0.003 6 1.99 0.09
    15.0 0.001 1 4.35 0.05
    下载: 导出CSV
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  • 收稿日期:  2020-06-19
  • 修回日期:  2020-10-10
  • 刊出日期:  2021-01-28

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