Karst aquifer evolution in fractured rocks
We study the large-scale evolution and flow in a fractured karst aquifer by means of a newly developed numerical method. A karst aquifer is discretized into a set of irregularly spaced nodal points, which are connected to their set of natural neighbors to simulate a network of interconnected conduits in two dimensions. The conduits are allowed to enlarge by solutional widening. The geometric flexibility of this method, along with a simplified model for the dissolution kinetics within the system...[Show more]
|Collections||ANU Research Publications|
|Source:||Water Resources Research|
Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.