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Abstract
DOI:10.1306/1063815CA53234
Fractured Continuum Approach to Stochastic Permeability Modeling
S. A. McKenna,1 P. C. Reeves2
1Sandia National Laboratories, Albuquerque, New Mexico, U.S.A.
2Sandia National Laboratories, Albuquerque, New Mexico, U.S.A.
ACKNOWLEDGMENTS
Funding for this work was provided by the Japanese Nuclear Cycle Development Institute. This chapter was improved through reviews by Steve Carle, Eileen Poeter, Norm Warpinski, and two anonymous reviewers. The original draft of this chapter was completed and sent to the editors in November 1999. Sandia is a multiprogram laboratory operated by Sandia Corporation, a Lockheed Martin Company, for the U.S. Department of Energy's National Nuclear Security Administration under contract DE-AC04-94AL85000.
ABSTRACT
A new kind of fracture-permeability model called the fractured continuum model (FCM) is presented that incorporates the advantages of discrete fracture network models and the processing speed of effective continuum representations of fracture permeability. Observations of fracture orientation, length, frequency, and transmissivity from boreholes and outcrops are used as input to the FCM approach. Geostatistical realizations of fracture connectivity, represented by the coordination number of a local percolation network, and fracture frequency are combined with object-based simulations of high- and low-permeability classes in the model domain. At each location, these three spatially variable properties are combined into an effective grid-block
permeability using an approximation based on the effective medium theory. The resulting realizations of fracture permeability, containing greater than 106 elements, are used as input to a single-phase flow model. A parallel computer platform coupled with a unique groundwater flow code is used to efficiently solve steady-state pressure fields on multiple realizations. The ability to solve many realizations in a short amount of time allows for the evaluation of the effects of two different conceptual models of fracture permeability on particle traveltimes.
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