Low-molecular-weight
organic acids such as oxalate, which are ubiquitous in the environment,
can control the solubility and bioavailability of toxic metals such
as Pb in soils and water by influencing complexation and precipitation
reactions. Here, we investigated Pb solubility in relation to Pb-oxalate
precipitation at pH 5.0 in the absence and presence of calcium (Ca),
a common cation in environmental matrices. At Pb mole fractions less
than 0.10, sequestration of Pb into Ca oxalate to form a solid solution
substantially lowered Pb solubility relative to that of pure Pb oxalate
to an extent inversely proportional to the Pb mole fraction. Small
Pb/Ca solid–solution distribution coefficients at these low
mole ratios was largely attributed to the stronger complexation of
Pb compared to Ca with oxalate to form soluble metal-oxalate complexes,
which in turn limited Pb incorporation into the Ca-oxalate crystal
lattice. Characterization of the Pb/Ca-oxalate coprecipitates by X-ray
diffraction, optical microscopy, and Fourier transform infrared spectroscopy
revealed that the whewellite (Ca-oxalate monohydrate) structure was
destabilized by substitution of small amounts of Pb into the lattice,
and thus, the formation of the Ca-oxalate dihydrate (weddellite) was
favored over the monohydrate. At Pb mole fractions above 0.20, discrete
crystallites of Pb oxalate were identified. These new findings imply
that Pb/Ca-oxalate coprecipitates in the presence of Ca could reduce
the solubility of Pb in Pb-contaminated acid soils.