Acq. Ladeira et al., Mechanism of anion retention from EXAFS and density functional calculations: Arsenic (V) adsorbed on gibbsite, GEOCH COS A, 65(8), 2001, pp. 1211-1217
X-ray absorption fine structure spectroscopy and density functional calcula
tions were used to determine the structural model of arsenic surface comple
x on gibbsite mineral. The structural environment of arsenic at the solid s
urface may determine its potential for remobilization and stability. Data w
ere collected for arsenate adsorbed on gibbsite surface at pH 5.5. The X-ra
y absorption fine structure spectroscopy results showed that As(V) forms an
inner sphere bidentate binuclear complex on the surface of Al oxyhydroxyl
octaedra. Quantitative results showed an average interatomic As(V)-Al dista
nce of 3.19 +/- 0.05 Angstrom and a coordination number of 1.3 +/- 1.0 atom
s. Four different adsorption sites in which arsenate can interact with gibb
site have been studied using density functional calculations, i.e., bidenta
te binuclear complex, bidentate mononuclear complex, monodentate mononuclea
r complex, and monodentate binuclear complex. The density functional calcul
ations confirm that the most stable structure predicted for As(V)-gibbsite
system is the bidentate-binuclear complex. Copyright (C) 2001 Elsevier Scie
nce Ltd.