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Chromate and oxalate adsorption on goethite. 1. Calibration of surface complexation models

Journal Article · · Environmental Science and Technology; (United States)
DOI:https://doi.org/10.1021/es00036a004· OSTI ID:7234411
;  [1]
  1. Oregon Graduate Inst. of Science and Technology, Beaverton, OR (United States)
Adsorption of chromate and oxalate on [alpha]-FeOOH was quantified for single-adsorbate systems as a function of pH, ionic strength and adsorbate and adsorbent concentrations. The comprehensive data base was used to calibrate and compare two surface complexation models. Both anions exhibited Langmuir-type adsorption with maximum adsorption densities ([Gamma][sub max]) of 2.2 (oxalate) and 2.4 [mu]mol/m[sup 2] (chromate). Increasing ionic strength diminished the adsorption of both anions. However, the background electrolyte affected oxalate adsorption more than chromate adsorption, reflecting a higher intrinsic affinity of chromate for the goethite surface. Measured proton/anion adsorption stoichiometry ratios (r[sub H]) ranged from 0.3 to 1.1, increased with pH, but showed little dependence on surface concentration of adsorbates. The diffuse layer model (DLM) and triple-layer model (TLM) reproduced all major adsorption features with a single set of constants for each model, but more surface species were required for the DLM. Another difference between models arose in the computation of r[sub H]: DLM-calculated values were closer to the experimental values. 49 refs., 7 figs., 4 tabs.
DOE Contract Number:
FG06-89ER60845
OSTI ID:
7234411
Journal Information:
Environmental Science and Technology; (United States), Journal Name: Environmental Science and Technology; (United States) Vol. 26:12; ISSN ESTHAG; ISSN 0013-936X
Country of Publication:
United States
Language:
English