Environmental Science & Technology · 1998 · 127 citations · 15 references
AgricultureChemistrySoil SciencesEnvironmental ChemistryInorganic ChemistrySoil ChemistryChelation In SoilsHeavy Metal ContaminationIron HydroxidesIron OxidesMetal ToxicityTrace Element ChemistryHeavy Metal MobilityMetal LeachingMetal MobilityMetal Speciation In SoilMetal Toxicity In SoilSoil Iron OxidesSoil Metal MobilitySoil Metal Retention
Coprecipitates of heavy metals in iron oxides are possible long-term sinks that could limit metal mobility and toxicity in soils. To test the efficacy of this process to maintain low metal solubilities, rapid and slow simultaneous titrations of Cd 2+, Cu 2+, Pb 2+, and Zn 2+ were conducted in the presence of Fe 3+ by titration with KOH to pH 6 in order to form coprecipitates having concentrations of 100 mg kg - 1 Cd 2+, 1500 mg kg - 1 Cu 2+, 500 or 1500 mg kg - 1 Pb 2+, and 3000 mg kg - 1 Zn 2+ . The final soluble concentrations of Cd 2+ (0.28 and 0.16 μM), Zn 2+ (8.4 μM), Cu 2+ (0.60 μM), and Pb 2+ (<5 nM) after aging the coprecipitates for long periods, as measured by voltammetry, corresponded to 28 and 59%, 58%, 94%, and 100% removal from solution by the coprecipitate, respectively. Soluble Cd 2+ and Zn 2+ were virtually unaffected by the pH changes induced by aging, whereas Cu 2+ solubility tended to increase as aging decreased pH. The solubility values (pMetal) of Cu 2+ and Zn 2+ coprecipitates with Fe 3+ indicate solubilities intermediate between that expected from metal (hydr)oxides precipitation and surface adsorption, whereas Cd 2+ solubility (pCd) indicated solubility lower than that expected from precipitation or adsorption.
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