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dc.contributor.advisorGhassemi, Ahmad
dc.creatorSerajian, Vahid
dc.date.accessioned2011-10-21T22:04:00Z
dc.date.accessioned2011-10-25T14:38:21Z
dc.date.available2011-10-21T22:04:00Z
dc.date.available2011-10-25T14:38:21Z
dc.date.created2011-08
dc.date.issued2011-10-21
dc.date.submittedAugust 2011
dc.identifier.urihttps://hdl.handle.net/1969.1/ETD-TAMU-2011-08-10125
dc.description.abstractHydraulic fracturing of transverse isotropic reservoirs is of major interest for reservoir stimulation and in-situ stress estimation. Rock fabric anisotropy not only causes in-situ stress anisotropy, but also affects fracture initiation from the wellbore. In this study a semi-analytical method is used to investigate these effects with particular reference to shale stimulation. Using simplifying assumptions, equations are derived for stress distribution around the wellbore's walls. The model is then used to study the fracture initiation pressure variations with anisotropy. A sensitivity analysis is carried out on the impact of Young's modulus and Poisson's ration, on the fracture initiation pressure. The results are useful in designing hydraulic fractures and also can be used to develop information about in-situ rock properties using failure pressure values observed in the field. Finally, mechanical and permeability anisotropy are measured using Pulse Permeameter and triaxial tests on Pierre shale.en
dc.format.mimetypeapplication/pdf
dc.language.isoen_US
dc.subjectfracture initiationen
dc.subjectfracturing pressureen
dc.subjecttransverse isotropyen
dc.subjectwellbore failureen
dc.subjectshaleen
dc.titleA Study of Hydraulic Fracturing Initiation in Transversely Isotropic Rocksen
dc.typeThesisen
thesis.degree.departmentPetroleum Engineeringen
thesis.degree.disciplinePetroleum Engineeringen
thesis.degree.grantorTexas A&M Universityen
thesis.degree.nameMaster of Scienceen
thesis.degree.levelMastersen
dc.contributor.committeeMemberHolditch, Stephen A.
dc.contributor.committeeMemberDuan, Benchun
dc.type.genrethesisen
dc.type.materialtexten


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