The bedding plane
formed by sedimentation makes shale anisotropic.
To clarify the influence of bedding on the hydraulic fracturing of
shale, the fracture characteristics of bedding shale were first clarified
by conducting a hydraulic fracturing experiment on large-scale shale
samples with different bedding angles. Subsequently, combined with
the experimental results, based on the theory of elasticity, a new
fracture initiation criterion for shale hydraulic fracturing considering
its anisotropic characteristics was established. The influence of
the bedding angle on the hydraulic fracture initiation pressure and
initiation angle was analyzed. The results showed that the pump pressure
curve during hydraulic fracturing can be divided into four stages:
continuous pressurization, internal pressure drop, internal pressure
attenuation, and internal pressure equilibrium stage. Corresponding
to the four stages of the pump pressure curve, the evolution of hydraulic
fracture has four processes: microfracture development, fracture initiation,
fracture propagation, and fracture network equilibrium process. When
the direction of the maximum principal stress is perpendicular to
the bedding, a complex fracture network is easily formed. Depending
on whether the bedding plane is open or not, the modes of interaction
between the hydraulic fractures and bedding plane could be divided
into eight types. Hydraulic fractures initiate in two ways: from the
matrix and from natural fractures. During fracturing, with the increase
in the bedding angle, the initiation pressure decreases gradually
and the initiation angle decreases first and then increases. The knowledge
gained in this study can provide data and theoretical support for
drilling direction design and fracture pressure evaluation in the
field of hydraulic fracturing.