The
Kirkwood–Cohansey aquifer in southern New Jersey is
an important source of drinking-water supplies, but the availability
of the resource is limited in some areas by high concentrations of
radium, a potential carcinogen at elevated concentrations. Radium
(226Ra plus 228Ra) concentrations from a network
of 25 drinking-water wells showed a statistically significant increase
over a decadal time scale (p < 0.05), with a median
increase of 0.35 picocuries per liter. Increases in Ra are correlated
with road-salt application rates, and we hypothesize that the correlation
is causal. Geochemical processes associated with road-salt applications
that can mobilize Ra into solution include competition by excess sodium
for sorption sites and formation of chloride complexes (RaCl+ and RaCl2). The largest increases in Ra were in groundwater
with low pH (≤5), which is an indirect surrogate for low cation-sorption
capacity. Correlations with other potential anthropogenic causes for
the increase in Ra were not observed, further suggesting a road-salt
effect. Given the significant increase in Ra concentrations in this
drinking-water source, the known carcinogenic risks from Ra, the direct
link to road-salt application, and the likelihood for continued increases,
additional monitoring is necessary in areas with similar hydrogeologic
and geochemical settings.