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Modeling Flow and Transport in Fractured Crystalline Rock using the Discrete Fracture Network Concept

Published online by Cambridge University Press:  26 February 2011

Björn Dverstorp ,
Wille Nordqvist  and
Johan Andersson
Björn Dverstorp
Affiliation:
Hydraulics Engineering, The Royal Institute of Technology, S-100 44 Stockholm, Sweden
Wille Nordqvist
Affiliation:
Hydraulics Engineering, The Royal Institute of Technology, S-100 44 Stockholm, Sweden
Johan Andersson
Affiliation:
Hydraulics Engineering, The Royal Institute of Technology, S-100 44 Stockholm, Sweden
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Abstract

The conductive properties of fractured crystalline rock vary considerably in space, which implies that the flow is very unevenly distributed in space. The large variability raises doubts on modeling the flow with a large scale continuum model. Modeling flow in fractured crystalline rock in a network of discrete fractures provides an increased understanding of the character of the rock heterogeneity. Compared to a continuum model discrete models introduce new parameters such as statistical distributions for fracture orientation, radii, density and transmissivity that need to be estimated. By analyzing the migration experiment in the Stripa research mine in Sweden it is demonstrated how to calibrate and eventually validate a discrete model on field data. The flow analysis shows that the flow distribution on the drift roof and in two out of three vertical boreholes can be modelled with the same discrete model. The properties of the third borehole differ substantially. Initial attempts of analyzing the tracer experiment are also described.

Type
Research Article
Information
MRS Online Proceedings Library (OPL) , Volume 127: Symposium BERLIN – Scientific Basis for Nuclear Waste Management XII , 1988 , 787
Copyright
Copyright © Materials Research Society 1989

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References

REFERENCES

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