nerc.ac.uk

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

Turner, R.J.; Mansour, M.M.; Dearden, R.; O Dochartaigh, B.E.; Hughes, A.G.. 2015 Improved understanding of groundwater flow in complex superficial deposits using three-dimensional geological-framework and groundwater models: an example from Glasgow, Scotland (UK). Hydrogeology Journal, 23 (3). 493-506. https://doi.org/10.1007/s10040-014-1207-0

Before downloading, please read NORA policies.
[img]
Preview
Text (Open Access Paper)
art%3A10.1007%2Fs10040-014-1207-0.pdf - Published Version
Available under License Creative Commons Attribution.

Download (5MB) | Preview

Abstract/Summary

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.

Item Type: Publication - Article
Digital Object Identifier (DOI): https://doi.org/10.1007/s10040-014-1207-0
ISSN: 1431-2174
Additional Keywords: GroundwaterBGS, Groundwater, Groundwater modelling, UKGEOS_Glasgow
Date made live: 22 Dec 2014 15:11 +0 (UTC)
URI: https://nora.nerc.ac.uk/id/eprint/509154

Actions (login required)

View Item View Item

Document Downloads

Downloads for past 30 days

Downloads per month over past year

More statistics for this item...