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Scaling of capillary, gravity and viscous forces affecting flow morphology in unsaturated porous media

机译:影响非饱和多孔介质中流动形态的毛细管力,重力和粘性力的缩放

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摘要

Interplay between capillary, gravity and viscous forces in unsaturated porous media gives rise to a range of complex flow phenomena affecting morphology, stability and dynamics of wetting and drainage fronts. Similar average phase contents may result in significantly different fluid distribution and patterns affecting macroscopic transport properties of the unsaturated medium. The formulation of general force balance within simplified pore spaces yields scaling relationships for motion of liquid elements in which gravitational force in excess of capillary pinning force scales linearly with viscous force. Displacement fluid front morphology is described using dimensionless force ratios expressed as Bond and Capillary numbers. The concise representations of a wide range of flow regimes with scaling relations, and predictive capabilities of front morphology based on dimensionless numbers lend support to certain generalizations. Considering available experimental data, we are able to define conditions for onset of unstable and intermittent flows leading to enhanced liquid and gas entrapment. These results provide a basis for delineation of a tentative value of Bo ~ 0.05 as an upper limit of applicability of the Richards equation (at pore to sample scales) and related continuum-based flow models.
机译:在不饱和多孔介质中的毛细作用,重力作用和粘性力之间的相互作用导致一系列复杂的流动现象,这些现象影响了润湿和排水前沿的形态,稳定性和动力学。相似的平均相含量可能导致明显不同的流体分布和模式,从而影响不饱和介质的宏观传输特性。在简化的孔隙空间内一般力平衡的表述产生了液体元素运动的比例关系,其中超过毛细管钉扎力的重力与粘性力成线性比例关系。使用表示为键和毛细管数的无量纲力比来描述驱替液的前部形态。具有比例关系的各种流动状态的简洁表示,以及基于无量纲数的前部形态预测能力,为某些概括提供了支持。考虑到可用的实验数据,我们能够为不稳定和间歇性流动的发生定义条件,从而导致更多的液体和气体截留。这些结果为划定Bo〜0.05的暂定值提供了基础,该值是Richards方程(在孔隙到样品尺度上)和相关的基于连续介质的流动模型的适用性上限。

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