The
dynamics of trace metals at mineral surfaces influence their
fate and bioaccessibility in the environment. Trace metals on iron
(oxyhydr)oxide surfaces display adsorption–desorption hysteresis,
suggesting entrapment after aging. However, desorption experiments
may perturb the coordination environment of adsorbed metals, the distribution
of labile Fe(III), and mineral aggregation properties, influencing
the interpretation of labile metal fractions. In this study, we investigated
irreversible binding of nickel, zinc, and cadmium to goethite after
aging times of 2–120 days using isotope exchange. Dissolved
and adsorbed metal pools exchange rapidly, with half times <90
min, but all metals display a solid-associated fraction inaccessible
to isotope exchange. The size of this nonlabile pool is the largest
for nickel, with the smallest ionic radius, and the smallest for cadmium,
with the largest ionic radius. Spectroscopy and extractions suggest
that the irreversibly bound metals are incorporated in the goethite
structure. Rapid exchange of labile solid-associated metals with solution
demonstrates that adsorbed metals can sustain the dissolved pool in
response to biological uptake or fluid flow. Trace metal fractions
that irreversibly bind following adsorption provide a contaminant
sequestration pathway, limit the availability of micronutrients, and
record metal isotope signatures of environmental processes.