Influence of pore-throat characteristics and displacement parameters of 3D digital cores on seepage and displacement capability: A case study of tight oil reservoir of Chang 8 reservoir group in Fuxian area, Ordos Basin
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摘要:目的
鄂尔多斯盆地长 8 段为典型特低孔、特低渗致密砂岩储层,微观孔喉非均质性强、水驱剩余油分布规律复杂;现有数字岩心渗流研究多单独剖析孔隙结构或单一驱替条件,缺少孔喉本征参数与驱替工况协同作用的定量表征体系。厘清微观孔喉结构、驱替参数共同控制下的渗流驱替演化机理,可为富县地区致密油高效注水开发提供微观理论支撑。
方法以鄂尔多斯盆地富县延长组长 8 致密砂岩储层为研究载体,选取 2 块代表性岩心开展显微 CT 扫描,通过灰度增强、非局部均值滤波、阈值二值化完成切片预处理,依托最大球算法重构三维孔隙网络;开展 REV 单元尺度校验后对孔隙网格粗化、几何缺陷修复,采用 N-S 方程组耦合 Cahn–Hilliard 相场法搭建微观渗流数值模型,分别开展单相水渗流、油水两相水驱油瞬态仿真;设置多梯度驱动压力、油水粘度比两组控制变量,定量对比 YP1、YP2 两类差异化孔喉岩心的渗流与驱替响应规律,系统揭示孔喉结构、驱替参数对渗流驱替效率的协同控制机制。
结果单相渗流条件下,流体流速、压差集中于细小喉道形成应力集中带,孔隙腔体内流速、压力波动微弱;YP1 样品具备大孔隙、细喉道、强微观非均质特征,驱替演化曲线分段陡变,若要达到与 YP2 同等剩余油饱和度,所需驱动压力显著更高;两类岩心渗透率均随驱动压力增大呈递减趋势,低压区间渗透率保持稳定。细小喉道与复杂孔喉网络产生的应力集中易造成流体封堵、驱替停滞;喉道半径、孔喉非均质性直接控制水驱推进速度与平面波及范围,连通孔隙的体积占比决定有效可动用储集空间规模,孤立微小孔隙易形成永久剩余油滞留区。定量模拟结果显示:喉道半径<8 μm 占比高的 YP1 岩心,提高驱动压力可大幅提升驱替效率;喉道整体偏大的 YP2 样品升压增效幅度微弱;孔隙半径>18 μm 占比高、优势渗流通道发育岩心,降低油水粘度比可拓宽波及范围、改善驱替效果;以微小孔隙为主的岩心,减小粘度比会增大渗流阻力,驱替效率出现衰减。
结论综合孔喉本征属性与人为驱替工况的耦合响应规律,建立了区分孔隙、喉道两类主控因素的微观驱替定量认识,可为鄂尔多斯盆地富县长 8 致密油储层注水参数优化、剩余油精准预测提供微观数值理论依据。
Abstract:ObjectiveThe Chang 8 member of the Yanchang Formation in the Ordos Basin is a typical ultra-low-porosity and ultra-low-permeability tight sandstone reservoir characterized by severe microscopic pore-throat heterogeneity and complex distribution patterns of residual oil after water flooding. Existing studies utilizing digital core simulation mostly focus on the independent characterization of pore structure or single displacement condition, and few quantitative investigations have systematically revealed the synergistic effects of intrinsic pore-throat properties and displacement conditions. A comprehensive quantitative understanding of seepage and displacement evolution mechanism under the joint control of microscopic pore-throat structure and displacement parameters can provide a microscopic theoretical basis for efficient water-flooding development of tight oil in Fuxian area, Ordos Basin.
MethodsIn this study, the tight sandstone reservoir in the Chang 8 member of the Yanchang Formation in Fuxian area, Ordos Basin was selected as the study object. Two representative tight sandstone core samples (labeled YP1 and YP2) were collected and scanned by micro-CT scan with a spatial resolution of 1 μm. A series of image preprocessing procedures, including grayscale enhancement, non-local mean filtering, and threshold binarization, were performed to eliminate instrument noise, and the maximal ball algorithm was adopted to reconstruct 3D pore-throat network. Representative elementary volume (REV) analysis was carried out to confirm the stable core calculation unit with a side length of 350 μm. Subsequently, grid coarsening and geometric defect repair were conducted to reduce computational cost. A microscopic seepage numerical model coupling Navier-Stokes (N-S) equations with the Cahn–Hilliard (C-H) phase-field method was established to simulate single-phase water seepage and transient oil-water two-phase displacement separately. Two sets of controlled variables—multiple gradient driving pressures (0.001-500 MPa) and eight groups of oil-water viscosity ratios (0.06-3.00)—were designed to quantitatively compare the seepage and displacement response patterns of YP1 and YP2 with distinct pore-throat configurations.
ResultsUnder single-phase seepage conditions, fluid velocity and differential pressure were concentrated within narrow throats to form high stress concentration zones, while fluid velocity and pressure fluctuated slightly inside large pore cavities. Sample YP1 was characterized by large pores, small throats, and strong microscopic heterogeneity, and its displacement evolution curves showed segmented steep changes. To achieve the same residual oil saturation as YP2, YP1 required remarkably higher driving pressure. For both samples, the calculated absolute permeability declined continuously as driving pressure increased, while permeability remained stable in the low-pressure range. Stress concentration generated by small throats and intricate pore-throat networks easily caused fluid blockage and displacement stagnation. Throat radius and pore-throat heterogeneity directly controlled the advancing speed and sweep range of water flooding, while the volume fraction of connected pores determined the scale of effectively mobilizable pore space and ultimately controlled final displacement efficiency. Isolated micropores were prone to forming permanent residual oil retention zones. Quantitative simulation results showed that, for cores with a high proportion of throats smaller than 8 μm, increasing driving pressure could greatly improve displacement efficiency, whereas cores dominated by large throats showed limited efficiency improvement after increasing pressure. For samples with abundant pores larger than 18 μm and well-developed preferential seepage channels, reducing the oil-water viscosity ratio could expand the sweep range and improve displacement performance. In contrast, reservoirs dominated by micropores showed higher seepage resistance and lower displacement efficiency when the viscosity ratio decreased. The simulated permeability values (0.32–0.75×10−3 μm2) were consistent with laboratory core measurements, which verified the reliability of the established simulation model.
ConclusionThis study distinguishes the respective controlling effects of pores and throats on microscopic oil-water displacement and clarifies their coupling response patterns under different water-flooding parameters. The quantitative relationships among pore-throat configuration, driving pressure, and viscosity ratio can provide a basis for optimizing water-flooding parameters and predicting residual oil for Chang 8 tight oil reservoirs in Fuxian area, Ordos Basin. Unlike previous single-factor simulation studies, this study establishes a complete quantitative evaluation framework considering the joint influence of intrinsic pore-throat properties and artificial displacement conditions, which offers new microscopic insights for the efficient exploitation of analogous tight sandstone reservoirs worldwide.
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表 1 样品孔喉结构参数及对比
Table 1. Pore-throat structural parameters and comparison of samples
样品编号 孔隙 喉道 非均质性 孤立孔隙
数量占比/%连通孔隙
体积占比/%连通孔隙半径/μm
(主流外高占比/%)数量连通率/% 体积连通率/% 半径/μm(主流
外高占比/%)迂曲度 逐层面孔率
标准差YP1 97.60 85.64 >18(54) 2.40 91.78 <8(83) 2.62 0.028 YP2 97.43 72.67 <18(58) 2.57 76.23 >8(58) 1.58 0.015 对比 YP1>YP2 YP1<YP2 YP1<YP2 表 2 不同出入口压差下渗流模拟绝对渗透率
Table 2. Absolute permeability obtained from seepage simulations under different inlet-outlet pressure differences
样品编号 驱动压
力/MPa体积流量
Q/(m3·s−1)流动横截
面积A/m2入口压力
p1/Pa出口压力
p2/Pa渗透率
K/10−3 μm2YP1 0.1 2.52×10−11 2.81×10−9 9.81×104 3.34 0.32 0.25 6.28×10−11 2.81×10−9 2.45×105 8.39 0.32 0.5 1.25×10−10 2.81×10−9 4.91×105 1.20×10 0.32 0.8 1.99×10−10 2.81×10−9 7.85×105 2.72×10 0.32 1 2.47×10−10 2.81×10−9 9.81×105 3.43×10 0.32 10 2.17×10−9 2.81×10−9 9.76×106 4.23×102 0.74 50 8.95×10−9 2.81×10−9 4.84×107 4.19×103 0.62 100 1.61×10−8 2.81×10−9 9.63×107 1.30×104 0.55 500 5.90×10−8 2.81×10−9 4.76×108 1.79×105 0.41 YP2 0.001 9.11×10−13 4.40×10−9 9.87×102 7.45 0.75 0.025 2.27×10−11 4.40×10−9 2.47×104 1.90×102 0.74 0.05 4.52×10−11 4.40×10−9 4.94×104 3.85×102 0.74 0.1 8.94×10−11 4.40×10−9 9.87×104 7.93×102 0.73 0.25 2.17×10−10 4.40×10−9 2.47×105 2.13×103 0.71 0.5 4.16×10−10 4.40×10−9 4.93×105 4.73×103 0.68 0.8 6.29×10−10 4.40×10−9 7.88×105 8.44×103 0.65 1 7.58×10−10 4.40×10−9 9.84×105 1.12×104 0.63 10 5.44×10−9 4.40×10−9 9.71×106 2.76×105 0.46 50 2.03×10−8 4.40×10−9 4.77×107 2.71×106 0.36 100 3.57×10−8 4.40×10−9 9.45×107 7.14×106 0.33 500 1.24×10−7 4.40×10−9 4.60×108 6.37×107 0.25 -
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