Road Salt use on the Edgewood Campus
Monica Zillner

Introduction

Methods

Results

Discussion 

Link to Full Report (pdf)

Link to Slide Show on Salt Movement Through Watershed (pdf)

Introduction

Road salt is used to melt ice and snow in parking lots, on roads, and on sidewalks. Chloride levels in Lake Wingra have risen since use of road salt began being used as a de-icer. Before salting, levels were below 10 mg/L. Since salt practices have been instituted, levels often surpass 75 mg/L, particularly after the spring snowmelt (WRM Workshop, 1999).

 

Road salt moves through the watershed by drying and being transported by wind, running downhill, infiltrating soil and groundwater, or may be sprayed or splashed onto vegetation along salting areas. Road salt negatively affects the health of the watershed, including its vegetation and drinking water. Edgewood contributes to the chloride levels in Lake Wingra through use of road salt on campus parking lots and sidewalks. The sidewalks are salted by College staff and the parking lots by a private contractor. To determine if Edgewood uses more road salt than necessary to de-ice, I collected road salt that remained after melting of snow and ice from Edgewood parking lots and sidewalks.

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Methods

Figure 1. Map with labeled sampling sites. ¤ represents parking lots. represents sidewalks.

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Results 

Figure 2. Result of Samples. The average salt/meter2 indicates the amount of excess road salt.

Sample Date

Sidewalks

g/m2

Parking Lots

g/m2

12/1/2008

180.6 g

45.0 g

12/6/2008

102.8 g

127.8 g

2/27/2009

105.4 g

 

 Average g/m2

129.6  g

86 g

Figure 3. Comparison of excess road salt on sidewalks and parking lots.

Figure 4. Comparison of the estimated total annual salt use on Edgewood Campus, road salt used to de-ice, and excess amounts of road salt.


Figure 5. Comparison of ton of road salt per acre that the City of Madison and Edgewood Campus use.

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Discussion 

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