Cj. Ottley et Rm. Harrison, ATMOSPHERIC DRY DEPOSITION FLUX OF METALLIC SPECIES TO THE NORTH-SEA, Atmospheric environment. Part B, Urban atmosphere, 27(5), 1993, pp. 685-695
Air sampling on a series of 10 research cruises on the North Sea (sout
h of 56-degrees-N) has yielded detailed spatial distributions of atmos
pheric metal concentrations, Al, Ca, Cd, Cu, Fe, Mg, Na, Pb and Zn whi
ch closely parallel the results of earlier published models. Air mass
back trajectory analysis demonstrates the strong influence which sourc
e region may have upon the elemental composition of the North Sea atmo
sphere. A cascade impactor designed to collect efficiently large as we
ll as small aerosol has produced detailed size distributions from whic
h mass weighted deposition velocity estimates have been produced (Al,
0.33; Cd, 0.24, Cu, 0.44; Fe, 0.30; Pb, 0. 1 3; Zn, 0.30 cm s-1) enabl
ing estimates for the dry deposition flux to the study area to be made
. Extrapolation of these data to the whole of the North Sea yields dry
deposition flux estimates (Cd, 33; Cu, 350, Pb, 370; Zn, 2640 tonnes
yr-1) which are in some instances substantially lower than those previ
ously reported, but nevertheless represent a significant pathway for m
etallic species to enter this marine environment. The size distributio
ns show the clear dominance that large aerosol has upon the overall dr
y deposition flux. Flux estimates are thus highly sensitive to the sam
pling of this large aerosol component, and to assumptions made regardi
ng the sea surface as a source of giant trace metal-enriched particles
which act only as a means of recycling marine metals.