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. Author manuscript; available in PMC: 2017 Sep 27.
Published in final edited form as: Water Resour Res. 2016 May 1;52(5):3324–3349. doi: 10.1002/2015WR018224

Figure 7.

Figure 7

Water stable isotopic (δ2H and δ18O) composition of groundwater and its relationship to the global meteoric water line (GMWL) of Craig [1961]. For comparison, Dhaka precipitation and its average [Stute et al., 2007] are also displayed. Note that the high-3H samples (yellow fill) plot mostly to the right of the GMWL.