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流体驱动裂纹的弹性松弛及由此产生的回流

Elastic Relaxation of Fluid-Driven Cracks and the Resulting Backflow.

作者信息

Lai Ching-Yao, Zheng Zhong, Dressaire Emilie, Ramon Guy Z, Huppert Herbert E, Stone Howard A

机构信息

Department of Mechanical and Aerospace Engineering, Princeton University, Princeton, New Jersey 08544, USA.

Institute of Theoretical Geophysics, Department of Applied Mathematics and Theoretical Physics, University of Cambridge, Cambridge CB3 0WA, United Kingdom.

出版信息

Phys Rev Lett. 2016 Dec 23;117(26):268001. doi: 10.1103/PhysRevLett.117.268001.

Abstract

Cracks filled with fluid propagation when the pressurized fluid is injected into the crack. Subsequently, when the fluid inlet is exposed to a lower pressure, the fluid flows backwards (backflow) and the crack closes due to the elastic relaxation of the solid. Here we study the dynamics of the crack closure during the backflow. We find that the crack radius remains constant and the fluid volume in the crack decreases with time in a power-law manner at late times. The balance between the viscous stresses in the fluid and elastic stresses in the fluid and the elastic stresses in the solid yields a scaling law that agrees with the experimental results for different fluid viscosities, Young's moduli of the solid, and initial radii of the cracks. Furthermore, we visualize the time-dependent crack shapes, and the convergence to a universal dimensionless shape demonstrates the self-similarity of the crack shapes during the backflow process.

摘要

当向裂缝中注入加压流体时,充满流体的裂缝会扩展。随后,当流体入口处压力降低时,流体会倒流,并且由于固体的弹性松弛,裂缝会闭合。在此,我们研究倒流过程中裂缝闭合的动力学。我们发现,裂缝半径保持恒定,并且在后期裂缝中的流体体积随时间呈幂律方式减小。流体中的粘性应力与流体中的弹性应力以及固体中的弹性应力之间的平衡产生了一个标度律,该标度律与不同流体粘度、固体杨氏模量和裂缝初始半径的实验结果相符。此外,我们可视化了随时间变化的裂缝形状,并且收敛到一个通用的无量纲形状证明了倒流过程中裂缝形状的自相似性。

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