CALL FOR PROPOSALS:

ORGANIZERS

  • Harvey Thorleifson, Chair
    Minnesota Geological Survey
  • Carrie Jennings, Vice Chair
    Minnesota Geological Survey
  • David Bush, Technical Program Chair
    University of West Georgia
  • Jim Miller, Field Trip Chair
    University of Minnesota Duluth
  • Curtis M. Hudak, Sponsorship Chair
    Foth Infrastructure & Environment, LLC

 

Paper No. 7
Presentation Time: 3:30 PM

EVALUATING ROAD SALT PERSISTENCE IN A WETLAND


QUINN, John J.1, VAN LONKHUYZEN, Robert A.1 and KAMIYA, Mark A.2, (1)Argonne National Laboratory, Environmental Science Sivision, 9700 S. Cass Avenue, EVS- 240, Argonne, IL 60439, (2)Environment, Safety, and Health, Argonne National Laboratory, 9700 S. Cass, Argonne, IL 60439, quinnj@anl.gov

Deicing of highways, roads, and parking lots can contribute large amounts of chloride to watersheds. The seasonal presence of salt in aquatic systems relative to the spring growth period is a critical factor for understanding the potential effect on the ecology. At longer time scales, it is important to understand whether the watershed flushes the chloride or accumulates it from year to year.

To evaluate the changing chloride concentrations in a watershed, we have monitored a wetland system in northeast Illinois since 2005 by collecting continuous (hourly) specific conductivity readings at key stations, supplemented by occasional hand measurements at many additional locations. The wetlands receive runoff from parking lots, road, forested areas, and a highway cloverleaf. In addition to the conductivity measurements, water samples were collected at various times and locations corresponding to a wide range of conductivity measurements and analyzed for chloride content. These were strongly correlated to the conductivity values and allowed the numerous conductivity readings to serve as surrogates for chloride concentration.

The study demonstrated the value of numerous, quick, and inexpensive continuous and manual water conductivity measurements for assessing the road salt load of waters entering, exiting, and retained within the wetland basin. The data demonstrated that the chloride concentrations at individual measurement stations fluctuate wildly throughout the year, with large increases during the salting season, and sudden, but brief, decreases resulting from winter, spring, or summer rain. The datalso show also show that winter salting has a prolonged effect on the chloride concentrations in the wetland, as chloride concentrations had an overall downward trend during the spring growth season and summer, yet remained above background levels until July. Such observations are significant in evaluating the effects of the salt on the wetland ecology, but they would not have been possible with a traditional water sampling program.

Meeting Home page GSA Home Page