(535a) Roadway Deicing: A Pinch of Salt

Authors: 
Chatterjee, R. - Presenter, University of Illinois at Chicago
Beysens, D., PMMH
Anand, S., University of Illinois at Chicago
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Rukmava Rukmava 2 12 2019-04-13T03:27:00Z 2019-04-13T03:27:00Z 1 255 1457 Microsoft 12 3 1709 16.00

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text-align:center;line-height:normal;mso-layout-grid-align:none;text-autospace:
none"> font-family:" arial>Roadway Deicing: A Pinch of Salt

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justify;line-height:normal;mso-layout-grid-align:none;text-autospace:none">Ice formation on roads
can have profound effects leading to car accidents. With approximately 70% of
U.S. roads being located in snowy regions, each winter >22 million tons of
salt is sprinkled on U.S. roads to keep them drivable. These road salts corrode
infrastructure and have detrimental effects on the environment. Inspired by the
semi-permeable biological membranes found in nature (e.g. our kidneys), we aim
to coat road salt within a polymer membrane which will maintain its deicing
functionality but prevent the environmental salt release. For this purpose, we have studied the
fundamentals of phase change of water to ice in the presence of a hygroscopic
material (such as salt), the resulting source-sink interactions between salt,
water, and water vapor and eventually develop scaling laws that govern the
deicing performance of a rock salt. We also have determined the freezing delay
potential of a number of other commonly used salts, subjected to different
environmental conditions. This methodical investigation is expected to
facilitate in choosing which salt performs best in a particular frigid outdoor
environment. The very fact that road salts are subjected to a myriad of
environmental conditions during their application in the winter season,
understanding the underlying physics that dictate their deicing performance is
crucial for efficiently salting roads by being beneficial for both
transportation safety and environmental sustainability.

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normal;mso-layout-grid-align:none;text-autospace:none"> 12.0pt;font-family:" arial>                                                                                       
Figure 1. Region of inhibited condensation around a sodium chloride salt
crystal chilled to -15°C