All Days 2012
DOI: 10.2118/159262-ms
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Laboratory Testing and Numerical Modelling of Fracture Propagation from Deviated Wells in Poorly Consolidated Formations

Abstract: This paper presents the results of an integrated laboratory and numerical modelling study on the effect of wellbore deviation and wellbore azimuth on fracture propagation in poorly consolidated sandstone formations. The goal of this project was to develop an understanding of how fractures would transition from single planar fractures to non-planar transverse fractures for fields in the deep-water Gulf of Mexico.The foundation of this work was over 40 fracturing laboratory tests to measure fracture propagation … Show more

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Cited by 18 publications
(12 citation statements)
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“…As the value of K II /K I becomes large enough, the shear sliding becomes the dominant mode of the fracture growth. us, according to the proposed theoretical model, for the model shown in Figure 1(a), the fracture will twist more during its growth under higher stress anisotropy coefficient conditions, which is same as the experimental results obtained by Ispas et al [35]. is is what hydraulic fracturing engineers have been trying to alleviate or avoid.…”
Section: Effect Of Stress Anisotropy Coefficientsupporting
confidence: 80%
“…As the value of K II /K I becomes large enough, the shear sliding becomes the dominant mode of the fracture growth. us, according to the proposed theoretical model, for the model shown in Figure 1(a), the fracture will twist more during its growth under higher stress anisotropy coefficient conditions, which is same as the experimental results obtained by Ispas et al [35]. is is what hydraulic fracturing engineers have been trying to alleviate or avoid.…”
Section: Effect Of Stress Anisotropy Coefficientsupporting
confidence: 80%
“…[10] Laboratory experiments of fluid injection under triaxial conditions have been conducted in sand and in mixtures of sand and silica flour [Khodaverdian and McElfresh, 2000;Chang, 2004;Bohloli and de Pater, 2006;Bezuijen et al, 2006;Dong and de Pater, 2008;Zhou et al, 2010;Golovin et al, 2010Golovin et al, , 2011Germanovich et al, 2012;Hurt and Germanovich, 2012;Ispas et al, 2012] and in clay [Murdoch, 1993b[Murdoch, , 1993cBolton et al, 1994;Au et al, 2003;Soga et al, 2004]. While the experiments in clay have mostly produced opening mode tensile fractures, the phenomena in sand are much more complex due to the coupling of fluid infiltration and grain displacements.…”
Section: Background and Experimental Motivationmentioning
confidence: 99%
“…The auxiliary HF will likely propagate the tip of the shear-activated NF plane, which tends to create new interconnected fractures. Transverse fractures are likely to be created due to shear failure in the Marcellus shale (Aimene and Nairn 2014), and in weak and poorly consolidated sandstones (Ispas et al 2012).…”
Section: Nf Reactivationmentioning
confidence: 99%