Articles | Volume 22, issue 2
https://doi.org/10.5194/hess-22-1629-2018
https://doi.org/10.5194/hess-22-1629-2018
Research article
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02 Mar 2018
Research article | Highlight paper |  | 02 Mar 2018

Using hydraulic head, chloride and electrical conductivity data to distinguish between mountain-front and mountain-block recharge to basin aquifers

Etienne Bresciani, Roger H. Cranswick, Eddie W. Banks, Jordi Batlle-Aguilar, Peter G. Cook, and Okke Batelaan

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Revised manuscript not accepted

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Cited articles

Allison, G. B., Gee, G. W., and Tyler, S. W.: Vadose-zone techniques for estimating groundwater recharge in arid and semiarid regions, Soil Sci. Soc. Am. J., 58, 6–14, 1994. 
Anderson, T. W.: Electrical-analog analysis of the hydrologic system, Tucson basin, southeastern Arizona, Geological Survey Water-Supply Paper 1939C, 1972. 
Baird, D. J.: Groundwater recharge and flow mechanisms in a perturbed, buried aquifer system: Northern Adelaide Plains, South Australia, PhD thesis, Flinders University, Adelaide, South Australia, 345 pp., 2010. 
Batlle-Aguilar, J., Banks, E. W., Batelaan, O., Kipfer, R., Brennwald, M. S., and Cook, P. G.: Groundwater residence time and aquifer recharge in multilayered, semi-confined and faulted aquifer systems using environmental tracers, J. Hydrol., 546, 150–165, 2017. 
Bense, V. F., Gleeson, T., Loveless, S. E., Bour, O., and Scibek, J.: Fault zone hydrogeology, Earth-Sci. Rev., 127, 171–192, 2013. 
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Short summary
This article tackles the problem of finding the origin of groundwater in basin aquifers adjacent to mountains. In particular, we aim to determine whether the recharge occurs predominantly through stream infiltration along the mountain front or through subsurface flow from the mountain. To this end, we discuss the use of routinely measured variables: hydraulic head, chloride and electrical conductivity. A case study from Australia demonstrates the approach.