Date(s) - 05/11/2017
11:00 am - 1:30 pm
Rock Bottom Brewery
Categories No Categories
Assessing Microseismicity Derived Fracture Distributions Utilizing Scanlines and Topological Approaches for Reservoir Model Development
By: Dr. Ted Urbancic – Chief Technology Officer of ESG Solutions
Hydraulic fracture stimulations generally result in microseismicity that is associated with the activation of pre-existing fractures or in the generation of new fractures. Typically, the event distribution provides a sense of where fracturing is occurring and the extent of fracturing away from the treatment zone. However, by utilizing a multi-array multi-well distribution of sensors, a more complete descriptive image of the individual fractures can be obtained, including the type of failure (eg., tensile, shear, or shear-tensile), fracture azimuth and dip, as well as the relative dimensions (assuming a penny-shaped crack). These fractures define the discrete fracture network that has been activated because of the stimulation program.
These data offer a unique approach to characterizing the rock mass fracture state. One approach we have considered is the adaptation of traditional scanlines utilized in rock mechanics applications. Scanlines are an effective systematic approach that considers the location and number of discontinuities that intersect the scanline. To effectively apply this approach to microseismic data, consideration had to be made of the event location errors for placement along scanlines perpendicular to the treatment zone at points of perforation. Much like setting a scanline at a rock face, additional quantifiable estimates of fracture curvature and roughness were defined. Additional estimates of discontinuity aperture were obtained based on the calculated tensile component of failure and corrections for angular differences between fractures obliquely oriented to scanlines. Further information can be gleaned on the fracture state through considering a topological approach to fracture characterization, where fractures are either considered as isolated, branching off from other fractures or crossing other fractures. By plotting the population of fractures in this rubric, the percolation properties of the reservoir post stimulation may be assessed.
Utilizing these approaches, we define the relative uniformity of rock mass structure with similar fracturing properties. As well, we characterize the degree of uniformity with position from the perforation intervals. Our observations suggest that a change in fracture spacing and type is indicative of changes in rock mass response to the stimulation and can therefore be used to classify the varying fracture state of the reservoir. Data from these analyses provide further constraint or input on the development of geomechanical and reservoir models.