This has resulted in salinization of this region’s lakes, streams and groundwater downslope from roadways, according to research by Dan Kelting, executive director of the Adirondack Watershed Institute and a professor at Paul Smith’s College. Nearly 7 million tons of salt have been dropped on Adirondack roads since 1980, he says.

“We all do benefit from its use in making roads clear, and drivable in some cases,” Kelting said in a presentation at the Cantwell Room in the Saranac Lake Free Library on Thursday, “but there are some negative consequences and effects that we should all be aware of.”

He put these into three categories: the potential environmental costs, property and infrastructure costs, and hazards to human health.

But not all roads are salted equally. Kelting and the institute in its research broke the 10,555 lane miles in the Adirondacks into the 2,830 state Department of Transportation-maintained miles, and the 7,725 locally maintained miles.

Dan Kelting, executive director of the Adirondack Watershed Institute and a professor at Paul Smith’s College, points to a projected map showing where people’s wells that tested for high sodium and chloride levels due to salt dumped on nearby roads. Kelting gave this presentation Thursday at the Saranac Lake Free Library’s Cantwell Room. (Enterprise photo — Jesse Adcock)

On an annual basis this entire network receives just under 192,700 tons of road salt, Kelting said. This can be split into about 80,000 tons on municipal and county roads and more than 110,000 tons on state roads.

“The local road network receives on average just over 10 tons of salt per lane mile,” Kelting said, while “the state road network receives over 37 tons of salt per lane mile. … The jargon would be that they’re maintained at the highest level of service.”

State roads have the highest speed limits and handle the most traffic. The state uses 2.5 times more salt than municipalities to try and keep these roads clean, despite managing a quarter of the total lane miles, Kelting said.

Local roads are salted according to a municipality’s own preference, Kelting said — often they are just plowed and sanded. Though this sand does contain 3 to 8 percent salt, it contributes less to runoff and regional salinization.

The Adirondacks have low chloride concentration, Kelting said — this means little chloride is released from rocks when they weather.

“So our natural chloride levels in our lakes are very, very low, less than 1 part per million,” Kelting said. “When we compare that to the concentration in lakes and watersheds with paved roads, it’s 14 times higher.”

The highest chloride concentration Kelting said the institute found in a lake was around 50 parts per million. Some of the streams they sampled were double and triple that. He said the reason for the difference is that lakes have many different sources — benefiting from dilution by tributaries that don’t have salted roads near them.

More than half of the total length of streams in the Adirondacks have been affected, he said.

What about groundwater? In 2012, Kelting, the institute and partner organizations ran a survey seeking 500 well owners in the Adirondacks. In the end, they got 489, mailing them test kits to return with water samples from their wells.

The state of New York provides “guidance” values for the amount of sodium and chlorine that should be in well water, but regulations for municipal water.

“So I live in the village of Saranac Lake; I’m on municipal water,” Kelting said. “We’re on what’s called regulatory thresholds. But if you are on your own water, there are no regulatory thresholds. It is just a guidance.”

Water above 20 ppm for sodium is a potential health risk for people with heart disease or any other health condition that requires a low-sodium diet, Kelting said. For chloride, the state provides a guidance value of 250 ppm.

“Once you get above 250 ppm, you have serious problems with corrosion in your pipes,” Kelting said. “So you’ll have serious problems with your hot water heater, dishwasher — appliances that run water. So you’re probably going to be investing in water treatment systems to use it.”

From the test kits Kelting got back, he found that among well systems that were not downslope of state or local roads, none exceeded the guidance values for chloride and sodium.

For wells downslope of local roads, 20 percent exceeded the guidance values for sodium, and 3 percent exceeded the chloride guidance value.

For wells downslope of state roads, 64 percent exceeded the guidance values for sodium, and 29 percent exceeded the chloride guidance value.

However, in small hamlets like Gabriels that have high-traffic state roads running through, the values he got back were higher. In Gabriels, 87 percent of wells tested downslope of state roads exceeded the guidance values for sodium.

“We see this same phenomenon in Lake Clear, in Indian Lake, in Keene Valley, where we see these hamlets with the state road networks in them and lots of and lots of wells with high sodium and chloride concentrations,” Kelting said.

So what’s to be done? Kelting suggested that maybe we don’t need to drive so fast immediately following a weather event. Maintaining roads for a 55 mph speed during or right after a snowstorm has heavy consequences for the environment and our drinking water.

Another option would be to create more municipal water districts, like Saranac Lake’s, to stop Adirondack residents from drinking potentially salinized water. Municipalities and the DOT could also put salt on the roads more effectively, and therefore use less, by dropping it at slower speeds or using liquid brine solutions.

“So what if we do nothing?” Kelting said. “If we continue to load more salt in our watersheds, we’ll continue to load more salt in our lakes. So we’ll continue to see these concentrations go up.”

If you want to get involved with Kelting’s research and are a well owner, contact him at dkelting@paulsmiths.edu to have your water tested.