Irreversible Sorption of Contaminants During Ferrihydrite Transformation
- Sandia National Laboratories
A better understanding of the fraction of contaminants irreversibly sorbed by minerals is necessary to effectively quantify bioavailability. Ferrihydrite, a poorly crystalline iron oxide, is a natural sink for sorbed contaminants. Contaminants may be sorbed/occluded as ferrihydrite precipitates in natural waters or as it ages and transforms to more crystalline iron oxides such as goethite or hematite. Laboratory studies indicate that Cd, Co, Cr, Cu, Ni, Np, Pb, Sr, U, and Zn are irreversibly sorbed to some extent during the aging and transformation of synthetic ferrihydrite. Barium, Ra and Sr are known to sorb on ferrihydrite in the pH range of 6 to 10 and sorb more strongly at pH values above its zero point of charge (pH> 8). We will review recent literature on metal retardation, including our laboratory and modeling investigation of Ba (as an analogue for Ra) and Sr adsorption/resorption, during ferrihydrite transformation to more crystalline iron oxides. Four ferrihydrite suspensions were aged at pH 12 and 50 °C with or without Ba in 0.01 M KN03 for 68 h or in 0.17 M KN03 for 3424 h. Two ferrihydrite suspensions were aged with and without Sr at pH 8 in 0.1 M KN03 at 70°C. Barium or Sr sorption, or resorption, was measured by periodically centrifuging suspension subsamples, filtering, and analyzing the filtrate for Ba or Sr. Solid subsamples were extracted with 0.2 M ammonium oxalate (pH 3 in the dark) and with 6 M HCl to determine the Fe and Ba or Sr attributed to ferrihydrite (or adsorbed on the goethite/hematite stiace) and the total Fe and Ba or Sr content, respectively. Barium or Sr occluded in goethite/hematite was determined by the difference between the total Ba or Sr and the oxalate extractable Ba or Sr. The percent transformation of ferrihydrite to goethite/hematite was estimated from the ratio of oxalate and HC1 extractable Fe. All Ba was retained in the precipitates for at least 20 h. Resorption of Ba reached a maximum of 7 to 8% of the Ba2+ added for samples aged in 0.01 and 0.17 M KN03 after 68 and 90 h of aging, respectively. About 3% of the Ba2+ added was readsorbed from 90 to 3424 h of aging in 0.17 M KN03. The amount of Ba sorbed by ferrihydrite or adsorbed on goethite (oxalate-extractable) decreased from 70 to 40% of the Ba2+ added after 68 h in 0.01 M KNO3 and from 80 to 20% of the Ba2+ added after 400 h in 0.17 M KN03. The Ba occluded in goethite (HCl-extractable) in 0.01 M KN03 increased rapidly to 30% of the Ba2+ added in the first 0.4 h and then to 50% of the Ba2+ added after 68 h. In 0.17 M KN03, Ba occluded in goethite increased from 60% of the Ba2+ added by 68 h and to 75% of the Ba2+ added after 3424 h. After 68 h at 70°C, ferrihydrite transformation was 99% compIete and was slightly inhibited with Sr present during the first few hours. Occlusion of Sr in ferrihydrite or Sr reversibly adsorbed decreased from 96 to 4o/0 after 86 h. Occlusion of Sr in hematite/goethite increased from 4 to 40% after 68 h. Resorption of Sr increased from 0.2 to 50% after 68 h. At least 90% of the Ba and 25% of the Sr added to the ferrihydrite suspensions were retained by the iron oxides during the aging periods in this study. At least 75% of the Ba and 15% of the Sr were irreversibly sorbed during ferrihydrite transfomnation to goethite and/or hematite.
- Research Organization:
- Sandia National Laboratories (SNL), Albuquerque, NM, and Livermore, CA
- Sponsoring Organization:
- USDOE
- DOE Contract Number:
- AC04-94AL85000
- OSTI ID:
- 7261
- Report Number(s):
- SAND99-1275C; ON: DE00007261
- Country of Publication:
- United States
- Language:
- English
Similar Records
Influence of sorbate-sorbent interactions on the crystallization kinetics of nickel- and lead-ferrihydrite coprecipitates
Thermally induced release of adsorbed Pb upon aging ferrihydrite and soil oxides