The chemical composition of aerosols and precipitation collected over Sardi
nia primarily reflect Saharan and European inputs. European background aero
sols in Sardinia show a 3- to 25-fold decrease in EFcrust values for Cd, Zn
, Pb, and Cr compared with coastal stations in the Western Mediterranean. P
artitioning of total atmospheric deposition between soluble and insoluble p
hases shows that Al, Si, Fe and Pb originating from the atmosphere are most
ly in an insoluble form. For Ca, Cd and Cr metals, the dissolved fraction r
epresents 50-90% of the total input. Aerosol dissolution experiments perfor
med at particle concentrations ranging from 3 to 300 mg l(-1) show that Cd
and Pb have low solubilities at high mass particle concentrations. The solu
bility of Pb increases with EFcrust values and the finest grain-size of the
aerosols (<1 mu m), and is also affected by pH. Dissolution of Al and Fe d
ecreases significantly from 30% (13% for Fe) at aerosol loads lower than 5
mg l(-1) to less than 1% for both metals at total aerosol concentrations gr
eater than 100 mg l(-1). The fluxes (dry + wet) of metals in Sardinia show
that similar to 30% of the Cd and Pb to more than 80% of the Fe and Al come
from the Sahara. (C) 1999 Elsevier Science Ltd. All rights reserved.