Geofluids / 2017 / Article / Fig 5

Research Article

Palaeohydrogeology and Transport Parameters Derived from 4He and Cl Profiles in Aquitard Pore Waters in a Large Multilayer Aquifer System, Central Australia

Figure 5

Time taken to reach steady state solute transport in model 4 from continuous high concentrations throughout the profile for (a) chloride and (b) 4He concentration; the chloride concentration was then increased in the upper aquifer in model 5 giving the profiles for (c) chloride and (d) 4He concentration.