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Laboratory study of Fracturing Fluid Migration due to Spontaneous Imbibition in Fractured Tight Formations

机译:骨折紧密地层自发性吸收引起的压裂液迁移的实验室研究

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During hydraulic fracturing operations in low permeability formations, spontaneous imbibition of fracturing fluid into the rock matrix may be responsible for having a significant impact on the retention of water-based fracturing fluids in the neighborhood of the induced fracture. This may consequently affect the post-frac productivity of the well. However, there is lack of direct quantitative and visual evidence of the extent of retention, evolution of the resulting imbibing fluid front, and how they relate to potential productivity hindrance. In this paper, laboratory experiments have been carefully designed to represent the vicinity of a hydraulic fracture. The evolution of fracturing fluid leak-off is monitored as a function of space and time using X-ray computed tomography (CT). The X-ray CT imaging technique allows us to map saturations at controlled time intervals to monitor the migration of fracturing fluid into the reservoir formation. It is generally expected for low permeability formations to show strong capillary forces due to their small characteristic pore radii, but this driving mechanism is in competition with the low permeability and spatial heterogeneities found in tight gas sands. The relevance of capillarity as a driver of fluid migration and retention in a tight gas sand sample is interpreted visually, quantified and compared with high permeability Berea sandstone in our experiments. It is seen that although these formations demonstrate strong capillarity, the effect can be suppressed by the low permeability of the formation and the heterogeneous nature of the sample. However, saturation values attained during imbibition experiments are comparable to those previously obtained for high permeability samples, which can have significant implications in terms of phase mobilities in the neighborhood of induced fractures. Results from this investigation are expected to provide fundamental insight regarding critical variables affecting the retention and migration of water-based fracturing fluids in the neighborhood of hydraulic fractures, and consequently on the post-frac productivity of the well.
机译:在低渗透性形成的液压压裂操作期间,将压裂液进入岩石基质的自发性吸收可能是对诱导骨折附近的水性压裂液具有显着影响的原因。因此,这可能会影响井的近距离生产率。然而,缺乏直接的定量和视觉证据的保持程度,由此产生的吸收流体前部的演变,以及它们如何与潜在的生产率障碍有关。在本文中,经验丰富的实验室实验以代表液压骨折附近。使用X射线计算机断层扫描(CT)被监测压裂液泄漏的进化作为空间和时间的函数。 X射线CT成像技术允许我们以受控时间间隔映射饱和,以监测压裂流体进入贮存器形成的迁移。通常,由于它们的小特征孔径,通常对低渗透性形成显示出强烈的毛细管力,但是这种驱动机制在竞争中,在紧密气体砂中发现的低渗透性和空间异质性。在目视,量化和在我们的实验中,在视觉上,量化和比较了毛细血管作为流体迁移和保留在紧密气砂样中的驾驶员的相关性。可以看出,尽管这些形成表明了强烈的毛细血管,但是通过形成的低渗透性和样品的异质性质可以抑制效果。然而,在吸收实验期间获得的饱和度值与先前获得的高渗透性样本的饱和值相当,这可以对诱导骨折附近的相迁移率具有显着影响。预计这项调查的结果将为影响水力骨折附近的水性压裂液保留和迁移的关键变量提供基本洞察力,从而对井的后近距离生产率。

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