Effect of Geological Layer Properties on Hydraulic-Fracture Initiation and Propagation: An Experimental Study

Abstract

Summary Hydraulic-fracture initiation and propagation in the presence of multiple layers with different mechanical and flow properties are investigated experimentally using a novel fracturing cell. Mixtures of plaster, clay, and hydrostone are used to cast sheet-like and porous test specimens in layers with different configurations and properties. The layered specimens are hydraulically fractured under varying far-field differential stress. Fracture growth is recorded using a high-resolution digital camera. Key frames are subsequently analyzed using digital image correlation (DIC) to reveal microcracks, measure strains, and show other features such as shear-failure events that are difficult to detect with the naked eye. The problem of a hydraulic fracture induced in a soft layer bounded by harder layers is considered. We demonstrate numerous laboratory experiments that reveal a clear tendency for induced fractures to avoid harder bounding layers. This is seen as fracture deflection or kinking away from the harder layers, fracture curving between the harder bounding layers, and fracture tilt from the maximum far-field stress direction. These observations appear to be more pronounced as the contrast in Young's modulus and fracture toughness between the layers increases and/or the far-field differential stress decreases. Moreover, when a fracture is induced in a relatively thin layer, the fracture avoids the harder bounding layers by starting and propagating parallel to the bounding interfaces. Fracture propagation parallel to the bounding layers is also observed in relatively wide layers when the far-field stress is isotropic or very low. A fracture approaching a dipping, harder layer tends to curve away from the hard layer by kinking toward the high side of the interface. Nonplanar fracture trajectories are observed even in homogeneous materials when the far-field differential stress is relatively low. Furthermore, various other fracture behaviors in layered specimens are demonstrated and discussed, such as fracture offsetting at material interfaces, fracture branching and complex fracture trajectories, and shear failure of weakly bonded interfaces.

Hydraulic fracturing behavior of shale–sandstone interbedded structure under true triaxial stress conditions: A comprehensive experimental analysis

“…When the hydraulic fracture attempts to extend from the sandstone layer to the shale layer, it tends to deflect or avoid the shale layer, resulting in termination or activation at the shale–sandstone interface. Previous research on fracture propagation inside layered formations with varying lithologies has attributed this phenomenon to differences in the elastic modulus 27,28 …”

“…Previous research on fracture propagation inside layered formations with varying lithologies has attributed this phenomenon to differences in the elastic modulus. 27,28…”

A Numerical Study of Hydraulic Fracture Propagation Geometry in a Layered Shale Reservoir

“…Permeable layer 4 Geofluids and the effective stresses can be expressed by Equation (10), and the effective stresses govern the deformation and failure of the rock.…”

“…Many studies have investigated the effect of elastic modulus on hydraulic fracture behaviors by using numerical or experimental methods. However, these studies all focus on the hydraulic propagation path, and few studies have studied the influence of modulus contrast in different layers on the hydraulic fracture geometry [10,21,23,25,38]. To better understand the impact of multilayered systems on fracture propagation geometry, the impact of modulus contrasts on fracture propagation geometry has been investigated using the following specimens and strategies.…”

“…Teufel et al [9] carried out laboratory experiments in which three-layer rock specimens were hydraulically fractured under a uniaxial compression stress state and demonstrated that two distinct geologic conditions could inhibit or contain hydraulic fracture growth in layered rock. Altammar et al [10] performed an experimental study in layered specimens that directly observed fracture growth near the material interface. The results provide fundamental insights on fracture propagation behavior in heterogeneous porous media.…”