Geofluids / 2017 / Article / Fig 2

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 2

δ18O and δ2H in pore water, groundwater, and drilling fluid samples. Error bars represent the possible isotopic equilibrium fractionation difference for samples with less than 3 g water adapted from Hendry et al. [50]. The black line represents the local meteoric water line (LMWL), δ2H = 7.2δ18O + 5.7, from Alice Springs.