CALL FOR PROPOSALS:

ORGANIZERS

  • Harvey Thorleifson, Chair
    Minnesota Geological Survey
  • Carrie Jennings, Vice Chair
    Minnesota Geological Survey
  • David Bush, Technical Program Chair
    University of West Georgia
  • Jim Miller, Field Trip Chair
    University of Minnesota Duluth
  • Curtis M. Hudak, Sponsorship Chair
    Foth Infrastructure & Environment, LLC

 

Paper No. 4
Presentation Time: 2:20 PM

COMPETITIVE ADSORPTION OF ARSENATE AND PHOSPHATE AT THE FERRIC HYDROXIDE-WATER INTERFACE


NEUPANE, Ghanashyam and DONAHOE, Rona J., Department of Geological Sciences, University of Alabama, 201 7th Ave, Room 2003 Bevill Building, Tuscaloosa, AL 35487-0338, gneupane@ua.edu

Single and competitive adsorption of arsenate (As(V)) and phosphate (Pi) on ferric hydroxide were investigated using adsorption isotherms, adsorption envelopes, surface complexation modeling, adsorption kinetics, and As K-edge EXAFS spectroscopy. This research was aimed at evaluating the selectivity and mechanism of As(V) and Pi adsorption on ferric hydroxide. Adsorption isotherms at pH 4, 8, and 11 were constructed for both oxyanions with initial concentrations of 0.07 mM to 6.67 mM in single as well as competitive settings. The empirical results indicated that the adsorption of these oxyanions on ferric hydroxide is largely controlled by pH, generally decreasing with increasing pH. The triple layer model simulations using bidentate surface complexes slightly under-predicted adsorption at lower and upper pH regions, and over-predicted adsorption in the intermediate pH range. Kinetic experiments showed early rapid, followed by slower, adsorption/desorption of As(V) and Pi at the ferric hydroxide-water interface. During competitive adsorption experiments, As(V) was preferentially adsorbed over Pi. The As K-edge EXAFS spectra showed that the corner-sharing bidentate binuclear complex is the major surface complex of As(V) on ferric hydroxide. Similarly, the edge-sharing bidentate mononuclear complex of As(V) was also identified in all samples at pH 4, and in samples where both As(V) and Pi were loaded at pH 8. It was found that the presence of Pi enhanced the formation of As(V) bidentate mononuclear surface complexes, more at pH 8 than at pH 4. Adsorption isotherms, envelopes, kinetics, and As K-edge EXAFS analysis suggest that the adsorption preference of As(V) is related to its ability to form edge-sharing bidentate complex at higher surface coverage and in the presence of Pi. Arsenate was found to compete with Pi for adsorption at the corner sharing sites, in addition to possibly noncompetitive edge-sharing sites, thereby resulting in greater uptake of As(V) than Pi during competitive adsorption. The research findings indicate that both As(V) and Pi compete for adsorption on ferric hydroxide and each showed a capacity to desorb the other. Therefore, excessive input of Pi to contaminated soils and sediments due to the overuse of fertilizers could release As through competitive desorption.
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