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Theoretical Investigation of the Transition from Spontaneous to Forced Imbibition

机译:从自发转变为强制吸收的理论调查

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Spontaneous and forced imbibition are recognized as important recovery mechanisms in naturally fractured reservoirs as the capillary force controls the movement of the fluid between the matrix and the fracture. For unconventional reservoirs, imbibition is also important as the capillary pressure is more dominant in these tighter formations, and the theoretical understanding of the flow mechanism for the imbibition process will benefit the understanding of important multiphase flow phenomenons like water blocking. In this paper, a new semi-analytic method is presented to examine the interaction between spontaneous and forced imbibition and to quantitatively represent the transient imbibition process. The methodology solves the partial differential equation of unsteady state immiscible, incompressible flow with arbitrary saturation- dependent functions using the normalized water flux concept, which is very identical to the fractional flow terminology used in traditional Buckley-Leverett analysis. The result gives a universal inherent relationship between time, normalized water flux, saturation profile and the ratio between co-current and total flux. The current analysis also develops a novel stability envelope outside of which the flow becomes unstable due to strong capillary forces, and the characteristic dimensionless parameter shown in the envelope is derived from the intrinsic properties of the rock and fluid system and can describe the relative magnitude of capillary and viscous forces at the continuum scale. This dimensionless parameter is consistently applicable in both capillary dominated and viscous dominated flow conditions.
机译:由于毛细管力控制在基质和骨折之间的流体的运动中,自发性和强制的吸收被认为是自然裂缝储层中的重要回收机制。对于非传统的储层,吸收也是重要的,因为在这些更紧的地层中毛细管压力更大,并且对吸入过程的流动机制的理论理解将有利于对水阻滞等重要的多相流动现象的理解。在本文中,提出了一种新的半分析方法,以检查自发性和强制吸收之间的相互作用,并定量代表瞬态吸入过程。该方法解决了不可稳定状态的局部微分方程不混溶,使用归一化水通量概念与任意饱和依赖性功能的不可压缩流量,这与传统的Buckley-Leverett分析中使用的分数流动术语非常相同。结果在时间,归一化水通量,饱和度,饱和度曲线和电流和总通量之间的比率之间提供了通用的固有关系。目前的分析还在其中开发出一种新的稳定性封套,其中流动由于强烈的毛细力而变得不稳定,并且封套中所示的特征无量纲参数源自岩石和流体系统的内在特性,并且可以描述相对幅度连续尺度毛细管和粘性力。该无量纲参数一致适用于毛细管主导和粘性主导的流动条件。

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