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Geometry of elastic hydrofracturing by injection of an over pressured non-Newtonian Fluid

dc.contributor.authorJ Chavez-Alvarez, E Soto
dc.contributor.authorB Barrientos, C Mares
dc.contributor.authorM Cerca
dc.date.accessioned2009-10-19T21:13:32Z
dc.date.available2009-10-19T21:13:32Z
dc.date.issued2009-10-19T21:13:32Z
dc.description.abstractThe nucleation and propagation of hydrofractures by injection of over pressured fluids in an elastic and isotropic medium are studied experimentally. Non-Newtonian fluids are injected inside a gelatine whose mechanical properties are assumed isotropic at the experimental strain rates. Linear elastic theory predicts that plastic deformation associated to breakage of gelatin bonds is limited to a small zone ahead of the tip of the propagating fracture and that propagation will be maintained while the fluid pressure exceeds the normal stress to the fracture walls (Ch\'avez-\'Alvarez,2008) (i.e., the minimum compressive stress), resulting in a single mode I fracture geometry. However, we observed the propagation of fractures type II and III as well as nucleation of secondary fractures, with oblique to perpendicular trajectories with respect to the initial fracture. Experimental evidence shows that the fracture shape depends on the viscoelastic properties of gelatine coupled with the strain rate achieved by fracture propagtion.en_US
dc.description.sponsorshipConacyt. DGEP, DGAPA, UNAMen_US
dc.identifier.urihttps://hdl.handle.net/1813/14122
dc.language.isoen_USen_US
dc.titleGeometry of elastic hydrofracturing by injection of an over pressured non-Newtonian Fluiden_US
dc.typevideo/moving imageen_US

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