Three-Dimensional Network Model for Coupling~of~Fracture and Mass Transport in Quasi-Brittle Geomaterials
arXiv:1510.05184 · doi:10.3390/ma9090782
Abstract
Dual three-dimensional networks of structural and transport elements were combined to model the effect of fracture on mass transport in quasi-brittle geomaterials. Element connectivity of the structural network, representing elasticity and fracture, was defined by the Delaunay tessellation of a random set of points. The connectivity of transport elements within the transport network was defined by the Voronoi tessellation of the same set of points. A new discretisation strategy for domain boundaries was developed to apply boundary conditions for the coupled analyses. The properties of transport elements were chosen to evolve with the crack opening values of neighbouring structural elements. Through benchmark comparisons involving non-stationary transport and fracture, the proposed dual network approach was shown to be objective with respect to element size and orientation.
References in corpus (1)
Cited by in corpus (6)
- Multiphysics Lattice Discrete Particle Modeling (M-LDPM) for the Simulation of Shale Fracture Permeability
- Homogenization of discrete mesoscale model of concrete for coupled mass transport and mechanics by asymptotic expansion
- Homogenization of discrete diffusion models by asymptotic expansion
- Adaptive discretization refinement for discrete models of coupled mechanics and mass transport in concrete
- Macroscopic stress, couple stress and flux tensors derived through energetic equivalence from microscopic continuous and discrete heterogeneous finite representative volumes
- Initiation of fluid-induced fracture in a thick-walled hollow permeable sphere