4.5 Article

Modeling Turbulent Hydraulic Fracture Near a Free Surface

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ASME
DOI: 10.1115/1.4005879

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  1. National Science Foundation OPP [ANT-0739444]
  2. United States Geological Survey
  3. Office of Polar Programs (OPP)
  4. Directorate For Geosciences [0739444] Funding Source: National Science Foundation

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Motivated by observations of the subglacial drainage of water, we consider a hydraulic fracture problem in which the crack grows parallel to a free surface, subject to fully turbulent fluid flow. Using a hybrid Chebyshev/series-minimization numerical approach, we solve for the pressure profile, crack opening displacement, and crack growth rate for a crack that begins relatively short but eventually becomes long compared with the distance to the free surface. We plot nondimensionalized results for a variety of different times, corresponding with different fracture lengths, and find substantial differences when free-surface effects are important. [DOI: 10.1115/1.4005879]

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