dc.description.abstract | Unconventional reservoir systems are heterogeneous, thinly layered, and often
exhibit strongly contrasting properties between layers. In addition, the interfaces
between layers vary in strength (friction and cohesion) and, when weak, they provide
preferential directions to rock failure and fluid flow. Traditional rock mechanics
modeling for hydraulic fracturing, wellbore stability, stress prediction, and other
petroleum-related applications assume homogeneous rocks and welded interfaces. This
assumption is hard to reconcile with the strongly layered texture and varied layer
composition observed in unconventional rocks.
Using the finite element method (FEM), we investigated the consequences of the
presence of rock layers and weak interfaces on three different subjects: 1) formation
shear stress development, shear slip at interfaces, and wellbore stability; 2) hydraulic
fracture height growth; and 3) casing shear impairment.
For the first scenario in this work, three different layered rock models were
simulated and compared: laterally-homogeneous, laterally-heterogeneous, and strongly
laterally-heterogeneous. Results show that localized shear stresses develop along
interfaces between layers with contrasting properties and along the wellbore walls. It
was also seen that rock shear and slip, along interfaces between layers, may occur when
the planes of weakness are pressurized (e.g., during hydraulic fracturing).
In the second scenario, we used a range of tensile strength and fluid flow
properties at the interfaces between layers, to investigate their impact on vertical
propagation of hydraulic fracture. The results show a systematic decrease in fracture
height and fracturing fluid efficiency with increasing interface hydraulic conductivity
and/or decreasing interface strength. We also propose that fluid viscosity has a strong
influence on fluid efficiency as well as fracture height growth.
In the third scenario, finite-element simulations were also conducted in a casing-cement-
formation system to evaluate casing curvature and plastic deformation caused by
formation shear movement occurring with slippage along the weak interface between
two distinct rock layers. The results indicate that the abrupt curvature change and the
plastic deformation along the casing are generated near the slip surface. We also observe
that casing shear at the peak temperature during a single thermal cycle of cyclic steam
stimulation induces higher casing plastic deformations. | en |