On
the basis of lifetime cancer risks, lead-210 (210Pb) and
polonium-210 (210Po) ≥ 1.0 and 0.7 pCi/L
(picocuries per liter), respectively, in drinking-water supplies may
pose human-health concerns. 210Pb and 210Po
were detected at concentrations greater than these thresholds at 3.7
and 1.5%, respectively, of filtered untreated groundwater samples
from 1263 public-supply wells in 19 principal aquifers across the
United States. Nationally, 72% of samples with radon-222 (222Rn) concentrations > 4000 pCi/L had 210Pb ≥
1.0
pCi/L. 210Pb is mobilized by alpha recoil associated with
the decay of 222Rn and short-lived progeny. 210Pb concentrations ≥ 1.0 pCi/L occurred most frequently where
acidic groundwaters inhibited 210Pb readsorption (felsic-crystalline
rocks) and where reducing alkaline conditions favored dissolution
of iron–manganese- (Fe–Mn-) oxyhydroxides (which adsorb 210Pb) and formation of lead–carbonate complexes (enhancing
lead (Pb) mobility). 210Po concentrations ≥ 0.7
pCi/L occurred almost exclusively in confined Coastal Plain aquifers
where old (low percent-modern carbon-14) groundwaters were reducing,
with high pH (>7.5) and high sodium/chloride (Na/Cl) ratios resulting
from cation exchange. In high-pH environments, aqueous polonium (Po)
is poorly sorbed, occurring as dihydrogen polonate (H2PoO3(aq)) or, under strongly reducing conditions, as a hydrogen-polonide
anion (HPo–). Fe–Mn- and sulfate-reduction
and cation-exchange processes may mobilize polonium from mineral surfaces.
Po2+ occurrence in low-to-neutral-pH waters is attenuated
by adsorption.