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Geochemically alkaline snowpack in northern Utah mountains in spring of 1982
Abstract Cores from the 1982 spring snowpack in the Wasatch Mountains exhibited low concentrations of , thus tending to discount the impact of West Coast NOx sources on the Rocky Mountains. SO4 = concentrations, presumably originating from the Salt Lake City/Provo metropolitan area, were higher (420 to 2340 μg 1−1), but the associated acid was effectively titrated by alkaline dust, resulting in pH's ranging from 5.89 to 6.77.
Geochemically alkaline snowpack in northern Utah mountains in spring of 1982
Abstract Cores from the 1982 spring snowpack in the Wasatch Mountains exhibited low concentrations of , thus tending to discount the impact of West Coast NOx sources on the Rocky Mountains. SO4 = concentrations, presumably originating from the Salt Lake City/Provo metropolitan area, were higher (420 to 2340 μg 1−1), but the associated acid was effectively titrated by alkaline dust, resulting in pH's ranging from 5.89 to 6.77.
Geochemically alkaline snowpack in northern Utah mountains in spring of 1982
Messer, Jay J. (author)
Atmospheric Environment ; 17 ; 1051-1054
1983-01-01
4 pages
Article (Journal)
Electronic Resource
English
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