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Experimental and Modeling Investigation of Fracture Initiation from Open-Hole Horizontal Wells in Permeable Formations

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Abstract

To investigate the evolution of hydraulic fractures in open-hole horizontal wells, a comprehensive experimental and analytical modeling investigation of fluid-driven fracture initiation in open-hole horizontal wells is presented in this paper. A large triaxial experimental system and a three-dimensional (3D) micro-computed tomography (micro-CT) imaging setup were used to simulate and investigate hydraulic fractures similar to those produced in field tests. We used an 8-mm-diameter and 100-mm-long hollow cylinder as a borehole within a 115 mm × 115 mm × 93 mm cement sample. The samples were first loaded in three orthogonal directions at different confining pressures to reproduce in situ reservoir conditions. Subsequently, a viscous fluid used in field operations with a viscosity of 60 mPa·s was injected into the borehole at 9 cc min−1. During the tests, the injection pressure and rate were monitored. Then, the fracture morphologies were detected by 3D micro-CT scanning. The fracture initiation pressure increases as the wellbore orientation rotates toward the minimum principal stress direction. The 3D images demonstrated that an induced hydraulic fracture first extends along the horizontal wellbore and then turns to align with the preferred fracture plane. An analytical model considering the fluid penetration effect, which is represented by the injection rate, rock permeability and fluid viscosity, was also developed to predict the fracture initiation pressure in open holes in permeable formations. The modeling results of the initiation pressure and the fracture position and orientation fit well with the experimental results. During the stimulation of a permeable formation, some of the fracturing fluid being injected into the wellbore flows from the wellbore into the surrounding formation. The infiltrating fracturing fluid increases the formation pore pressure, causing a compressive circumferential stress around the borehole. This mechanism reduces the fracture initiation pressure. The initiation pressure decreases with the rock permeability and injection rate but increases with the fracturing fluid viscosity. This result is important for petroleum engineering applications, because nearly all reservoirs are permeable to fracturing fluids, and the limitations of previous models preclude them from drawing the same conclusions.

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Abbreviations

BDP:

Breakdown pressure

c :

Compressibility coefficient of the fracturing fluid

Ei :

Exponential integral

FIP:

Fracture initiation pressure

h :

Interval of the open hole

k :

Permeability of the rock

p :

Pore pressure around the wellbore

p p :

Virgin formation pore pressure

p w :

Wellbore pressure

\({\bar {p}_{R\left( t \right)}}\) :

Average pressure

q :

Constant injection rate of fracturing fluid

q 0 :

Injection rate

r :

Radial distance from the center of the wellbore

R(t):

Disturbed radius caused by the fluid penetration

r w :

Wellbore radius

t :

Duration of the fluid injection period

t i :

Pumping time

α :

Biot’s coefficient

β :

Azimuth angle

γ :

Fracture initiation angle

θ :

Wellbore circumferential angle

ψ :

Deviation angle

η :

Conductivity coefficient

φ :

Porosity

µ :

Viscosity

ν :

Poisson’s ratio

σ 1 :

Maximum principal stress

σ 2 :

Intermediate principal stress

σ 3 :

Minimum principal stress

σ f :

Rock effective strength

σ H :

Maximum horizontal principal stress

σ h :

Minimum horizontal principal stress

σ t :

Tensile strength of the rock material

σ v :

Vertical stress

\({\sigma _{xx}},{\sigma _{yy}},{\sigma _{zz}}\) :

Normal stresses in a Cartesian coordinate system

\({\tau _{xy}},{\tau _{xz}},{\tau _{yz}}\) :

Shear stress in a Cartesian coordinate system

\({\sigma _r},{\sigma _z},{\sigma _\theta }\) :

Normal stresses in a cylindrical coordinate system

\({\tau _{rz}},{\tau _{r\theta }},{\tau _{\theta z}}\) :

Shear stresses in a cylindrical coordinate system

Ox, Oy, Oz :

Three axes in a Cartesian coordinate system

(r, θ, z):

Point coordinates in a cylindrical coordinate system

(x, y, z):

Point coordinates in a normal coordinate system

(x 1, y 1, z 1):

Specific point coordinates in a normal coordinate system

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Acknowledgements

This research was supported by the National Key Research and Development Plan of China (Grant no. 2018YFB0605602), Natural Science Foundation of China (Grant nos. 51504203; 51525404; and 51374178), National Key Research and Development Program of China (Grant no. 2017ZX05037-004) and China Scholarship Council (CSC Grant no. 201508515130). Special funding was provided by the Central Government of China for the development of local colleges and universities from the National First-level Discipline in the Oil and Gas Engineering Project (Project no. 20150727) and the Scientific Research Starting Project of Southwest Petroleum University (Project no. 2014QHZ004). Additionally, project szjj2015-020 was supported by the Open Research Subject of Key Laboratory of Fluid Power Machinery and the Ministry of Education. Thanks are owed to the CSC for providing support to the first author of this paper to conduct research at the University of Calgary, Alberta, Canada. Special thanks are extended to Mr. Sou Ma for his contribution to the experimental work. This research was also supported by the NSERC/AIEES/Foundation CMG and AITF Chairs.

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Zeng, F., Yang, B., Guo, J. et al. Experimental and Modeling Investigation of Fracture Initiation from Open-Hole Horizontal Wells in Permeable Formations. Rock Mech Rock Eng 52, 1133–1148 (2019). https://doi.org/10.1007/s00603-018-1623-x

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