Abstract

Several different approaches have been developed to model the specific characteristics of karst aquifers, taking account of their inherent complex spatial and temporal heterogeneities. This paper sets out the development of a semidistributed modelling approach for applications in an Irish karst context using urban drainage software. The models have proven to be very useful for different studies, with examples given for the ecohydrology of ephemeral karst lakes, extreme groundwater-flood alleviation, karst network investigation, submarine groundwater discharge, and quantification of different recharge and flow components. The limitations of the approach are also highlighted, in particular not being able to simulate diffuse infiltration and flow paths explicitly across the groundwater catchment. Hence, a more distributed, finite-difference modelling approach using MODFLOW Unstructured Grid (USG) with the newly developed Connected Linear Network (CLN) process is then compared against the semidistributed approach on the same karst catchment. Whilst it has proven difficult to achieve the same levels of model performance in simulating the spring flows in the distributed model compared to the semidistributed model, the ability to interrogate the flow paths at any point on the three-dimensional aquifer is demonstrated, which can give new insights into flows (and potential contaminant transport) through such complex systems. The influence of the proximity of highly transmissive conduits on the flow dynamics through the much-lower transmissive matrix cells in which the network is embedded has been particularly investigated.

Highlights

  • Karst aquifers host some of the most important drinking water resources across the world with roughly one quarter of the global population estimated to be relying on the supply of freshwater from these aquifer types (Ford and Williams 2007)

  • The simulated spring results from the models were compared to the spring discharge data across 2018/2019: for the full 18 months for the semidistributed model and for three periods shaded in grey, totalling 9 months, for the distributed MODFLOW model

  • The models have proven to be very useful for different applications with examples given for the ecohydrology of ephemeral karst lakes, extreme groundwater flood alleviation, karst network investigations, submarine groundwater discharge and quantification of different recharge and flow components

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Summary

Introduction

Karst aquifers host some of the most important drinking water resources across the world with roughly one quarter of the global population estimated to be relying on the supply of freshwater from these aquifer types (Ford and Williams 2007). Karst systems are complex systems to unravel, being highly heterogeneous geological formations characterised by multi-scale temporal and spatial hydrological behaviour. They contain a mix of primary (matrix), secondary (tectonic) and tertiary (dissolution) porosity with several orders of magnitude between the associated permeabilities (White and White 2005). Fractures and bedding planes provide the framework for the karstification processes during which ongoing dissolution develops a conduit network. Such aquifers are often characterized by a hierarchical drainage system

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