Improved understanding of groundwater flow in complex superficial deposits using three-dimensional geological-framework and groundwater models: an example from Glasgow, Scotland (UK)

• Published in: Hydrogeology journal Vol. 23; no. 3; pp. 493 - 506
• Main Authors: Turner, R. J., Mansour, M. M., Dearden, R., Ó Dochartaigh, B. É., Hughes, A. G.
• Format: Journal Article
• Language: English
• Published: Berlin/Heidelberg Springer Berlin Heidelberg 01-05-2015; Springer Nature B.V
• Subjects: Aquatic Pollution; Deposition; Earth and Environmental Science; Earth Sciences; Environmental stress; Geology; Geophysics/Geodesy; Ground-water flow; Groundwater; Groundwater data; Groundwater flow; Groundwater levels; Groundwater recharge; Hydrogeology; Hydrology/Water Resources; Modelling; Quaternary; Rivers; Three dimensional; Three dimensional models; Valleys; Waste Water Technology; Water Management; Water Pollution Control; Water Quality/Water Pollution; Glasgow Scotland; United Kingdom > UK; Scotland; British Isles, Scotland, Glasgow; British Isles, Scotland; 3D geological modelling; Superficial deposits; Conceptual modelling; Urban groundwater; UK
• ISSN: 1431-2174; 1435-0157
• DOI: 10.1007/s10040-014-1207-0

Groundwater models are useful in improving knowledge of groundwater flow processes, both for testing existing hypotheses of how specific systems behave and predicting the response to various environmental stresses. The recent advent of highly detailed three-dimensional (3D) geological-framework models provides the most accurate representation of the subsurface. This type of modelling has been used to develop conceptual understanding of groundwater in the complex Quaternary deposits of Glasgow, Scotland (UK). Delineating the 3D geometry of the lithostratigraphical units has allowed the most detailed conceptualisation of the likely groundwater flow regime yet attempted for these superficial deposits. Recharge and groundwater flow models have been developed in order to test this conceptual understanding. Results indicate that the direction of groundwater flow is predominantly convergent through the permeable, relatively thick Quaternary deposits of the Clyde valley towards the River Clyde, which runs through Glasgow, with some indication of down-valley flow. A separate nearby system with thick and potentially permeable Quaternary deposits, the Proto-Kelvin Valley, may also be a significant conveyor of groundwater towards the River Clyde, although the absence of local data makes any conclusions conjectural. To improve the robustness of the current model there is a need for an overall increase in good quality groundwater-level data, particularly outside central Glasgow. A prototype groundwater-monitoring network for part of Glasgow is an encouraging development in this regard. This would allow the development of a time-variant groundwater model which could be used to study future modelling scenarios.