Groundwater residence time and aquifer recharge in multilayered, semi-confined and faulted aquifer systems using environmental tracers

Author:

Batlle-Aguilar Jordi,Banks Eddie W.,Batelaan Okke,Kipfer Rolf,Brennwald Matthias S.,Cook Peter G.

Funder

Australian Research Council

National Water Commission

Goyder Institute for Water Research

Publisher

Elsevier BV

Subject

Water Science and Technology

Reference76 articles.

1. Inert gases in groundwater from the Bunter Sandstone of England as indicators of age and palaeoclimatic trends;Andrews;J. Hydrol.,1979

2. Baird, D.J., 2010. Groundwater recharge and flow mechanisms in a perturbed, buried aquifer system: Northern Adelaide Plains, South Australia. School of Chemistry, Physics and Earth Sciences: 238.

3. Fault zone hydrogeology;Bense;Earth Sci. Rev.,2013

4. Faults as conduit-barrier systems to fluid flow in siliciclastic sedimentary aquifers;Bense;Water Resour. Res.,2006

5. Thermal anomalies indicate preferential flow along faults in unconsolidated sedimentary aquifers;Bense;Geophys. Res. Lett.,2008

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