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Unified theory of global flow and squirt flow in cracked porous media

机译:裂隙多孔介质中全球流动和喷射流的统一理论

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Approximations for frequency-dependent and complex-valued effective stiffness tensors of cracked porous media (saturated with a single fluid) are developed on the basis of an inclusion-based model (the T-matrix approach to rock physics) and a unified treatment of the global-flow and squirt-flow mechanisms. Essentially, this study corrects an inconsistency or error related to fluid-mass conservation in an existing expression for the t-matrix (wave-induced deformation) of a communicating cavity, a cavity that is isolated with respect to stress propagation (through the solid matrix) but that can exchange fluid mass with other cavities because of global and/or local pressure gradients associated with passage of a long viscoelastic wave. An earlier demonstration of Gassmann consistency remains valid because the new theory of global flow and squirt flow (which also takes into account solid mechanical effects of stress interaction by us-ing products of communicating t-matrices associated with two-point correlation functions of ellipsoidal symmetry) only differs from an earlier version by a correction term that goes to zero in the low-frequency limit. If the unified model is applied to the special case of a model involving a single set of spheroidal cavities (having the same aspect ratio and orientation), the results become identical with those obtained using a special theory of global flow that predicts that at zero frequency the cavities will behave as though they are isolated with respect to wave-induced fluid flow (in accordance with Gassmann’s formulas) and that at high frequencies, they will behave as though they are dry. Our theory predicts that there will be a continuous transition from a global-flow-dominated system (characterized by a negative velocity dispersion) to a squirt-flow-dominated system (characterized by a positive velocity dispersion) if one begins with a single set of cavities and then introduces a distribution of shapes and/or orientations that gradually becomes wider (more realistic).Read More: http://library.seg.org/doi/abs/10.1190/1.3078404
机译:在基于夹杂物的模型(岩石物理学的T矩阵方法)和对岩石的统一处理的基础上,开发了开裂的多孔介质(饱和了一种流体)的频率相关和复数值有效刚度张量的近似值。全局流和喷流机制。本质上,这项研究纠正了连通腔的t矩阵(波动引起的变形)的现有表达式中与流体质量守恒相关的不一致或错误,该腔相对于应力传播(通过固体基质)是隔离的),但由于与长粘弹性波通过有关的整体和/或局部压力梯度,可以与其他空腔交换流体质量。 Gassmann一致性的早期证明仍然有效,因为新的整体流动和喷流理论(还考虑了通过与椭圆对称的两点相关函数相关的连通t矩阵的乘积来考虑应力相互作用的固体机械效应)。 )与早期版本的区别仅在于修正项,该修正项在低频范围内变为零。如果将统一模型应用于包含单个球体腔(具有相同的长宽比和方向)的模型的特殊情况,则结果将与使用特殊的整体流动理论(在零频率时预测该结果)获得的结果相同。空腔的行为就好像它们相对于波引起的流体流是隔离的(根据加斯曼公式),并且在高频下,它们的表现就好像它们是干的。我们的理论预测,如果从一组单一的方程组开始,则将从整体流动为主的系统(以负速度色散为特征)到喷水流动为主的系统(以正速度色散为特征)连续过渡。空腔,然后引入形状和/或方向的分布,并逐渐变得更宽(更真实)。阅读更多:http://library.seg.org/doi/abs/10.1190/1.3078404

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    Jakobsen, M.; Chapman, Mark;

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  • 年度 2009
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