Gradient (2013)

“Overall, there is no scientific basis for significant upward migration of HF fluid or brine from formations in sedimentary basins. Even if upward migration from a target formation to potable aquifer were hypothetically possible, the rate of migration would be extremely slow and the resulting dilution of the fluids would be very large…Given the overall implausibility and very high dilution factor, this exposure pathway does not pose a threat to drinking water resources.”