Groundwater protection zones in fractured-rock aquifers are delineated with a hybrid method that combines discrete fracture network (DFN) models and equivalent continuum models. The method, known as the Statistical Continuum Method (SCM), relies on statistics of movement of particles in a local-scale DFN followed by the use of those statistics to mimic movement in a catchment-scale continuum model. Because the method is based in a Monte-Carlo procedure, it is possible to delineate probability contours for protection zones. The method is implemented in a catchment-scale synthetic case study that uses MODFLOW as the continuum groundwater flow model. Reverse particle tracking is conducted and the locations of the particles at time t are used to create probability contours of the t-isochrone protection zone. The computational needs for upscaling from local to regional scale are not heavy and probability contours of protection zones can be easily computed.
Rishi ParasharDonald M. Reeves
Peter G. CookA.J. LoveNeville I. RobinsonCraig T. Simmons