Groundwater–surface water connectivity in a chain-of-ponds semiarid river |
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Authors: | Sébastien Lamontagne Jason Kirby Caroline Johnston |
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Institution: | CSIRO Land & Water, Waite Campus, Adelaide, South Australia, Australia |
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Abstract: | Semiarid rivers are often characterized by chains of small pools connected by riffles and wet meadows. The pools can be maintained by wet season surface runoff, groundwater discharge, or some combination thereof. Using synoptic surveys for several environmental tracers (δD and δ18O of H2O, specific electrical conductance at 25°C EC], chloride and 222Rn), we evaluated the groundwater—surface water connectivity of the Light River (South Australia) along an 8 km section in the vicinity of a proposed mining development. In all three surveys (representing spring, summer and winter conditions), the pools were maintained by regional groundwater discharge based on an elevated surface water EC (9–12 dS m?1) similar to regional groundwater, elevated radon-222 activities (0.09–3.0 Bq L?1) and low rainfall. Most pools were perennial, either because they directly received groundwater discharge or, indirectly, had an inflow originating from upstream groundwater-fed pools. The elevated salinity of regional groundwater is a key factor for the maintenance of perennial pools in the Light River because the potential for baseflow depletion by groundwater pumping is more limited. |
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Keywords: | chain-of-ponds connectivity environmental tracers groundwater-surface water interactions radon semiarid |
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