River-aquifer interactions in a semi-arid environment stressed by groundwater abstraction

• Published in: Hydrological processes 2013-03, Vol.27 (7), p.1072-1085
• Main Authors: McCallum, Andrew M., Andersen, Martin S., Giambastiani, Beatrice M. S., Kelly, Bryce F. J., Ian Acworth, R.
• Format: Article
• Language: English
• Subjects: conjunctive water management; river-aquifer interactions; semi-arid; stream depletion
• ISSN: 0885-6087; 1099-1085
• DOI: 10.1002/hyp.9229

Rivers and aquifers are, in many cases, a connected resource and as such the interactions between them need to be understood and quantified for the resource to be managed appropriately. The objective of this paper is to advance the understanding of river–aquifer interactions processes in semi‐arid environments stressed by groundwater ion. This is performed using data from a specific catchment where records of precipitation, evapotranspiration, river flow, groundwater levels and groundwater ion are analysed using basic statistics, hydrograph analysis and a simple mathematical model to determine the processes causing the spatial and temporal changes in river–aquifer interactions. This combined approach provides a novel but simple methodology to analyse river–aquifer interactions, which can be applied to catchments worldwide. The analysis revealed that the groundwater levels have declined (~ 3 m) since the onset of groundwater ion. The decline is predominantly due to the ion rather than climatic changes (r = 0.84 for the relationship between groundwater ion and groundwater levels; r = 0.92 for the relationship between decline in groundwater levels and magnitude of seasonal drawdown). It is then demonstrated that, since the onset of ion, the river has changed from being gaining to losing during low‐flow periods, defined as periods with flow less than 0.5, 1.0 or 1.5 GL/day (1 GL/day = 1 × 106 m3/day). If defined as  10 years) between the onset of groundwater ion and the changeover from gaining to losing conditions. Finally, a relationship between the groundwater gradient towards the river and the river flow at low‐flow is demonstrated. The results have important implications for water management as well as water ecology and quality. Copyright © 2012 John Wiley & Sons, Ltd.