4.6 Article

Riveraquifer interactions in a semi-arid environment stressed by groundwater abstraction

Journal

HYDROLOGICAL PROCESSES
Volume 27, Issue 7, Pages 1072-1085

Publisher

WILEY
DOI: 10.1002/hyp.9229

Keywords

riveraquifer interactions; stream depletion; semi-arid; conjunctive water management

Funding

  1. Cotton Catchment Communities CRC
  2. National Centre for Groundwater Research and Training, an Australian Government initiative
  3. Australian Research Council
  4. National Water Commission

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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 riveraquifer interactions processes in semi-arid environments stressed by groundwater abstraction. This is performed using data from a specific catchment where records of precipitation, evapotranspiration, river flow, groundwater levels and groundwater abstraction are analysed using basic statistics, hydrograph analysis and a simple mathematical model to determine the processes causing the spatial and temporal changes in riveraquifer interactions. This combined approach provides a novel but simple methodology to analyse riveraquifer interactions, which can be applied to catchments worldwide. The analysis revealed that the groundwater levels have declined (similar to 3m) since the onset of groundwater abstraction. The decline is predominantly due to the abstraction rather than climatic changes (r=0.84 for the relationship between groundwater abstraction 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 abstraction, 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 1.5GL/day (1GL/day=1x106m3/day). If defined as<1.0GL/day, low-flow periods constitute approximately 65% of the river flows; the periods where the river is losing at low-flow conditions are thus significant. Importantly, there was a significant delay (>10 years) between the onset of groundwater abstraction 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 (c) 2012 John Wiley & Sons, Ltd.

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