Publication Date:
2015-06-04
Description:
Chloride (Cl – ), stable isotope ratios of water (δ 18 O and δ 2 H), sulfur hexafluoride (SF 6 ), tritium ( 3 H), carbon-14 ( 14 C), noble gases ( 4 He, Ne and Ar) and hydrometry were used to characterise groundwater-surface water interactions, in particular infiltration rates, for the Lower Namoi River (New South Wales, Australia). The study period (four sampling campaigns between November 2009 and November 2011) represented the end of a decade-long drought followed by several high-flow events. The hydrometry showed that the river was generally losing to the alluvium, except when storm-derived floodwaves in the river channel generated bank recharge – discharge cycles. Using 3 H/ 14 C-derived estimates of groundwater mean residence times along the transect, infiltration rates ranged from 0.6 – 5 m year −1 . However, when using the peak transition age (a more realistic estimate of travel time in highly dispersive environments), the range in infiltration rate was larger (4 – 270 m year −1 ). Both river water (highest δ 2 H, δ 18 O, SF 6 , 3 H and 14 C) and an older groundwater source (lowest δ 2 H, δ 18 O, SF 6 , 3 H, 14 C and highest 4 He) were found in the riparian zone. This old groundwater end-member may represent leakage from an underlying confined aquifer (Great Artesian Basin). Environmental tracers may be used to estimate infiltration rates in this riparian environment but the presence of multiple sources of water and a high dispersion induced by frequent variations in the water table complicates their interpretation. This article is protected by copyright. All rights reserved.
Print ISSN:
0043-1397
Electronic ISSN:
1944-7973
Topics:
Architecture, Civil Engineering, Surveying
,
Geography
