Kp. Raven et al., ARSENITE AND ARSENATE ADSORPTION ON FERRIHYDRITE - KINETICS, EQUILIBRIUM, AND ADSORPTION ENVELOPES, Environmental science & technology, 32(3), 1998, pp. 344-349
Because of its toxicity, arsenic is of considerable environmental conc
ern. Its solubility in natural systems is strongly influenced by adsor
ption at iron oxide surfaces. The objective of this study was to compa
re the adsorption behavior of arsenite and arsenate on ferrihydrite, u
nder carefully controlled conditions, with regard to adsorption kineti
cs, adsorption isotherms, and the influence of pH on adsorption. The a
dsorption reactions were relatively fast, with the reactions almost co
mpleted within the first few hours. At relatively high As concentratio
ns, arsenite reacted faster than arsenate with the ferrihydrite, i.e.,
equilibrium was achieved sooner, but arsenate adsorption was faster a
t low As concentrations and low pH. Adsorption maxima of approximately
0.60 (0.58) and 0.25 (0.16) mol(As), mol(Fe)(-1) were achieved for ar
senite and arsenate, respectively, at pH 4.6 (pH 9.2 in parentheses).
The high arsenite retention, which precludes its retention entirely as
surface adsorbed species, indicates the likelihood that ferrihydrite
was transformed to a ferric arsenite phase, although this possibility
has yet to be confirmed by spectroscopic studies. The general trend at
initial arsenic concentrations greater than or equal to 0.27 mol(As)
kg(-1) ferrihydrite within the pH range of 4-9 was increasing arsenite
adsorption and decreasing arsenate adsorption with increasing pH. At
initial As concentrations of 0.27-0.80 mol(As), kg(-1) ferrihydrite, t
he adsorption envelopes crossed at approximately pH 6-7.5, i.e., adsor
bed arsenate concentrations were relatively greater than adsorbed arse
nite concentrations at lower pH values whereas adsorbed arsenite was g
reater at higher pH. At the highest initial arsenic concentration of 1
3.3 mol(As) kg(-1) ferrihydrite, a distinct adsorption maximum was obs
erved for arsenite adsorption at approximately pH 9.0, which correspon
ds closely to the first pK(a) (9.2) of H3AsO30, whereas there was a co
ntinuous drop in arsenate adsorption with increasing pH from 3 to 11.