Literature DB >> 28059547

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

Ching-Yao Lai1, Zhong Zheng1,2, Emilie Dressaire3, Guy Z Ramon4, Herbert E Huppert2,5, Howard A Stone1.   

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.

Year:  2016        PMID: 28059547     DOI: 10.1103/PhysRevLett.117.268001

Source DB:  PubMed          Journal:  Phys Rev Lett        ISSN: 0031-9007            Impact factor:   9.161


  2 in total

1.  Foam-driven fracture.

Authors:  Ching-Yao Lai; Bhargav Rallabandi; Antonio Perazzo; Zhong Zheng; Samuel E Smiddy; Howard A Stone
Journal:  Proc Natl Acad Sci U S A       Date:  2018-07-26       Impact factor: 11.205

2.  Hydraulic transmissivity inferred from ice-sheet relaxation following Greenland supraglacial lake drainages.

Authors:  Ching-Yao Lai; Laura A Stevens; Danielle L Chase; Timothy T Creyts; Mark D Behn; Sarah B Das; Howard A Stone
Journal:  Nat Commun       Date:  2021-06-25       Impact factor: 14.919

  2 in total

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