Overall dry deposition velocities of several elements were determined by di
viding measured fluxes by measured airborne concentrations in different par
ticle size ranges, The dry deposition measurements were made with a smooth
surrogate surface on an automated dry deposition sampler (Eagle II) and the
ambient particle concentrations were measured with a dichotomous sampler.
These long-term measurements were made in Chicago, IL, South Haven, MI, and
Sleeping Bear Dunes, MI, from December 1993 through October 1995 as part o
f the Lake Michigan Mass Balance Study. In general, the dry deposition flux
es of elements were highly correlated with coarse particle concentrations,
slightly less well correlated with total particle concentrations, and least
well correlated with tine particle concentrations. The calculated overall
dry deposition Velocities obtained using coarse particle concentrations var
ied from approximately 12 cms(-1) for Mg in Chicago to 0.2 cms(-1) for some
primarily anthropogenic metals at the more remote sites. The velocities ca
lculated using total particle concentrations were slightly lower. The crust
al elements (Mg, Al, and Mn) had higher deposition velocities than anthropo
genic elements (V, Cr, Cu, Zn, Mo, Ba and Pb). For crustal elements, overal
l dry deposition velocities were higher in Chicago than at the other sites.
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