Title of article :
Characterization and cycling of atmospheric mercury along the central US Gulf Coast
Author/Authors :
Mark A. Engle، نويسنده , , Michael T. Tate، نويسنده , , David P. Krabbenhoft، نويسنده , , Allan Kolker، نويسنده , , Mark L. Olson، نويسنده , , Eric S. Edgerton، نويسنده , , John F. DeWild، نويسنده , , Ann K. McPherson، نويسنده ,
Issue Information :
روزنامه با شماره پیاپی سال 2000
Pages :
19
From page :
419
To page :
437
Abstract :
Concentrations of atmospheric Hg species, elemental Hg (Hgring operator), reactive gaseous Hg (RGM), and fine particulate Hg (Hg-PM2.5) were measured at a coastal site near Weeks Bay, Alabama from April to August, 2005 and January to May, 2006. Mean concentrations of the species were 1.6 ± 0.3 ng m−3, 4.0 ± 7.5 pg m−3 and 2.7 ± 3.4 pg m−3, respectively. A strong diel pattern was observed for RGM (midday maximum concentrations were up to 92.7 pg m−3), but not for Hgring operator or Hg-PM2.5. Elevated RGM concentrations (>25 pg m−3) in April and May of 2005 correlated with elevated average daytime O3 concentrations (>55 ppbv) and high light intensity (>500 W m−2). These conditions generally corresponded with mixed continental-Gulf and exclusively continental air mass trajectories. Generally lower, but still elevated, RGM peaks observed in August, 2005 and January–March, 2006 correlated significantly (p < 0.05) with peaks in SO2 concentration and corresponded to periods of high light intensity and lower average daytime O3 concentrations. During these times air masses were dominated by trajectories that originated over the continent. Elevated RGM concentrations likely resulted from photochemical oxidation of Hgring operator by atmospheric oxidants. This process may have been enhanced in and by the near-shore environment relative to inland sites. The marine boundary layer itself was not found to be a significant source of RGM.
Journal title :
Applied Geochemistry
Serial Year :
2000
Journal title :
Applied Geochemistry
Record number :
740861
Link To Document :
بازگشت