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Topology, connectivity and percolation in fracture networks

Topology, connectivity and percolation in fracture networks
Topology, connectivity and percolation in fracture networks

The connectivity of a fracture network depends on both its geometry and topology, which may be characterized in terms of the types of nodes and branches in the system. A number of dimensionless parameters (dimensionless intensity (P22, B22), connections per line (CL) and connections per branch (CB), are used to characterize and assess network connectivity based on well-established lattice and continuum percolation models. These models result in networks with only I- and X-nodes, whereas most natural fracture networks have many Y-nodes. A simple scheme to transform IX systems into IYX systems is developed that allows the expected value of dimensionless branch intensity (B22C) at the percolation threshold to be derived for any network topology. The method is used to assess if a network is likely to be connected or not, and demonstrated by analysing the development of a network of desiccation cracks.

0191-8141
167-177
Sanderson, David J.
5653bc11-b905-4985-8c16-c655b2170ba9
Nixon, Casey W.
757fe329-f10f-4744-a28e-0ccc92217554
Sanderson, David J.
5653bc11-b905-4985-8c16-c655b2170ba9
Nixon, Casey W.
757fe329-f10f-4744-a28e-0ccc92217554

Sanderson, David J. and Nixon, Casey W. (2018) Topology, connectivity and percolation in fracture networks. Journal of Structural Geology, 115, 167-177. (doi:10.1016/j.jsg.2018.07.011).

Record type: Article

Abstract

The connectivity of a fracture network depends on both its geometry and topology, which may be characterized in terms of the types of nodes and branches in the system. A number of dimensionless parameters (dimensionless intensity (P22, B22), connections per line (CL) and connections per branch (CB), are used to characterize and assess network connectivity based on well-established lattice and continuum percolation models. These models result in networks with only I- and X-nodes, whereas most natural fracture networks have many Y-nodes. A simple scheme to transform IX systems into IYX systems is developed that allows the expected value of dimensionless branch intensity (B22C) at the percolation threshold to be derived for any network topology. The method is used to assess if a network is likely to be connected or not, and demonstrated by analysing the development of a network of desiccation cracks.

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More information

Accepted/In Press date: 17 July 2018
e-pub ahead of print date: 29 July 2018
Published date: 1 October 2018

Identifiers

Local EPrints ID: 425795
URI: http://eprints.soton.ac.uk/id/eprint/425795
ISSN: 0191-8141
PURE UUID: 95cde36a-cc07-437b-931a-f8ae24f45f30
ORCID for David J. Sanderson: ORCID iD orcid.org/0000-0002-2144-3527

Catalogue record

Date deposited: 02 Nov 2018 17:30
Last modified: 18 Mar 2024 03:09

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Contributors

Author: Casey W. Nixon

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