Measurements of A1, Pb, 21øpb, and 21øpo in precipitation and aerosol were used to estimate wet and dry components of the atmospheric flux at a semiremote site in northern Wisconsin. Wet deposition was primarily responsible for removing airborne Pb, 21øpb, and 2•øpo, while dry deposition was also important for A1. Although Pb and 2•øpb both exhibited a wet/total ratio of about 0.8, precipitation washout ratios for Pb and 2•øpb suggested that 2•øpb was washed from the atmosphere with greater efficiency than was Pb. This phenomenon was also illustrated by comparing the weighted mean annual specific activity in precipitation (976 pCi 21øpb mg -• Pb) and in aerosol (476 pCi 21øpb mg -• Pb) at this site between June 1979 and June 1980. By consideration of the apparent differential precipitation washout of Pb and 2•øpb, a reasonable estimate of the atmospheric flux of Pb was obtained by using the mean Pb/2• øPb ratio in aerosol and the 21Opb flux. The atmospheric flux to northern Wisconsin was estimated to be 0.8 #g crn -2 yr -• for Pb and 0.70 pCi cm -2 yr -• for 2•øpb. INTRODUCTION Despite convincing evidence that the atmosphere is the principal source of lead to the oceans [Duce et al., 1976; Patterson et al., 1976; Schaule and Patterson, 1981; Settle and Patterson, 1982] and many freshwater lakes [Winchester and Nifon•?, 1971; Gatz, 1975; Eisenreich, 1980; Talbot, 1981], surprisingly few data have been reported on wet and dry deposition of Pb and the naturally occurring radionuclide 2'øpb (t,/z = 22.3 years) to surface waters. In most cases the atmospheric fluxes of Pb and •"øPb have been inferred from their accumulation rates in sediments. Although this sometimes provides an adequate time-averaged record of lead deposition for chronological and historical input purposes, the specific aspects of the atmospheric input are not revealed. Furthermore, sedimentation regimes and postdepositional processes may redistribute the lead, making such natural repositories unreliable indicators of the actual lead flux. It is therefore highly desirable to conduct atmospheric sampling to estimate atmospheric input to the system. In conjunction with our studies of lead transport within lake systems (R. W. Talbot and A. W. Andren, unpublished manuscript, 1982), it was also of particular interest to us to explore the relationships between Pb and 2•øpb in both precipitation and aerosol over a period of 1 year. These measurements have been used to assess the relative contributions of wet and dry fallout to the total atmospheric deposition of Pb and 2 • Opb ' The specific activity (picocuries of 2• Opb per milligram of Pb) and the ratios Pb/A1 and 2•øPb/A1 have been employed to evaluate the potential for using 2•øpb as a natural geochemical tracer of Pb at sites removed from direct urban influence. SAMPLE COLLECTION Atmospheric sampling was conducted at a site within the Northern Highlands State Forest of north central Wisconsin (Vilas County). The site (46ø3'N, 89ø39'W) is about 80 km southeast of Lake Superior and 190 km west of the no...