The physical and chemical phenomena responsible for the atmospheric co
rrosion of lead are presented. Corrosion layer formation, morphology,
and chemical makeup are discussed in the context of lead containing mi
nerals and other crystalline structures that thermodynamics and kineti
cs suggest are likely to be present. Formation pathways for the minera
ls most often reported to be present in lead corrosion layers are show
n in schematic diagrams. Lead is quite reactive to common atmospheric
gases, outdoor exposures typically producing anglesite (PbSO4) and/or
cerussite (PbCO3) and indoor exposures often producing lead carboxylat
es. The presence of these species is shown to be a natural consequence
of the thin aqueous layer chemistry that obtains on lead in humid env
ironments. The primary atmospheric agents responsible for degradation
of lead are SO2, CO2, and carboxylic acids. Comprehensive kinetic simu
lations of the corrosion process are desirable, but await more extensi
ve laboratory determinations of the rates of dissolution, precipitatio
n, and transformation of lead containing chemical species.