“…41 The results from the TVA spill confirmed that boron can be a sensitive indicator for metals leaching from CCRs, with boron content up to 1600 μg/L in downstream porewater in ash covered sediments, relative to the upstream and uncontaminated river water with boron of 6−9 μg/L (Figure 2). 9,29 Results from surface water at a site covered with spilled ash and limited water exchange (known henceforth as the Cove) 9,29 yielded low δ Sr variations in watersheds in the US 42,43 show that most of the southeastern, south, and central watersheds in the coterminous U.S. have a similar isotopic range that would mask the difference between CCR-impacted and naturally occurring background waters. Yet in other areas of the northeastern, northern, and western U.S., the isotopic ratios are either higher (e.g., northeastern U.S., Minnesota, southern Appalachian range) or lower (e.g., Southern Texas, Oregon) that would allow a clear distinction between CCRimpacted water and natural background.…”