The level of salty compounds in the Monongahela River south of Pittsburgh spiked above acceptable limits in late 2008 - not a health risk, according to federal and state regulators, but drinking water drawn from the river tasted like mud.
Environmentalists blamed the contamination on Marcellus Shale gas-drilling discharges. Natural-gas drillers pointed to other sources in the historically stressed river: pollutants from coal mines and other industrial discharges.
Which source was to blame didn't really matter. What mattered was that the Monongahela's elevated levels of total dissolved solids - salty compounds known as TDS that can't be removed by conventional treatment - set off alarms, a clarion that Pennsylvania's streams would be unable to assimilate the huge volumes of wastewater expected with the coming Marcellus Shale boom, then in its infancy.