T67 Unconventional Energy Resources: Advances and Evolution in Tight Reservoir Assessment and Production (Posters)
Sunday, 22 October 2017
9:00 AM - 5:30 PM
Halls 4EF
NEW STOCHASTIC ASSESSMENT OF FRACTURE INTERCONNECTIVITY AND IMPLICATION FOR HYDRAULIC FRACTURING OPTIMIZATION FOR UNCONVENTIONAL FRACTURED RESERVOIRS
Paper number: T67-12
Program: Technical Sessions
Time: 9:00 AM – 5:30 PM
Authors
Abstract
We have developed a workflow for stochastic assessment of the interconnectivity of fracture network based on discrete fracture network (DFN) modeling and 3-D fracture permeability characterization. Fracture networks are realized and visualized using the stochastic distributions of fracture properties (size, orientation, spacing, aperture, etc.) as measured from field investigations, well logs, and/or core data. Fracture permeability is characterized with a 3-D full permeability tensor technique to account for the geometry of each individual fracture. Three typical scenarios of fracture systems have been analyzed for detailed fracture interconnectivity assessment. For a fracture system with moderately to highly concentrated fractures, the interconnectivity of fractures is generally low, which indicates that the hydraulic fracturing will be most effective only if the hydraulic fracture is perpendicular to the mean direction of the fracture system. A DFN model with randomized fracture orientations could yield high fracture interconnectivity with no preferred direction. Modeling of fracture interconnectivity indicates that there exists no preferred direction for hydraulic fracturing to be most effective.
The proposed method has been applied to the Devonian Chattanooga Shale in Alabama. Two fracture sets have been identified and modeled into a DFN model. Hydraulic pathway analysis indicates that hydraulic fracturing can be equally effective for hydrocarbon fluid/gas exploration as long as its orientation is not aligned with that of the regional system fractures.
Geological Society of America Abstracts with Programs. Vol. 49, No. 6
doi: 10.1130/abs/2017AM-306348
© Copyright 2017 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.