Arsenite sorption and co-precipitation with calcite

被引:130
作者
Roman-Ross, G.
Cuello, G. J.
Turrillas, X.
Fernandez-Martinez, A.
Charlet, L.
机构
[1] Univ Girona, Fac Sci, Dept Chem, Girona 17071, Spain
[2] Inst Max Von Laue Paul Langevin, F-38042 Grenoble 9, France
[3] CSIC, Eduardo Torroja Inst Construct Sci, Madrid 28033, Spain
[4] Univ Grenoble 1, Environm Geochem Grp, LGIT, IRIGM, F-38041 Grenoble 9, France
关键词
calcite; arsenite; adsorption; co-precipitation;
D O I
10.1016/j.chemgeo.2006.04.007
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Sorption of As(III) by calcite was investigated as a function of As(III) concentration, time and pH. The sorption isotherm, i.e. the log Gamma(As(III)) vs. log [AS(OH)(3)degrees/As-sat] plot is S-shaped and has been modelled on an extended version of the surface precipitation model [Farley, K.J., Dzombak, D.A., Morel, F.F.M., 1985. A surface precipitation model for the sorption of cations on metal oxides. Journal of Colloid and Interface Science 106 (227-242); Wersin, R, Charlet, L., Kathein, R., Stumm, W, 1989. From adsorption to precipitation: sorption of Mn2+ to FeCO3(s). Geochimica et Cosmochimica Acta 53, 2787-2796]. At low concentrations, As(OH)(3)degrees is adsorbed by complexation to surface Ca surface sites, as previously described by the X-ray standing wave technique [Cheng, L.W., Fenter, P., Sturchio, N.C., Zhong, Z., Bedzyk, M.J., 1999. X-ray standing wave study of arsenite incorporation at the calcite surface. Geochimica et Cosmochimica Acta 63 (19-20), 3153-3157]. The inflexion point of the isotherm, where As(OH)(3)degrees is limited by the amount of surface sites (S-T), yields 6 sites nm(-2) in good agreement with crystallographic data. Beyond this value, the amount of sorbed arsenic increases linearly with solution concentration, up to the saturation of arsenic with respect to the precipitation of CaHAsO3(s). The solid solutions formed in this concentration range were examined by X-ray and neutron diffraction. The doped calcite lattice parameters increase with arsenic content while c/a ratio remains constant. Our results made on bulk calcite on the atomic displacement of As atoms along [0001] direction extend those published by Cheng et a]. [Cheng, L.W., Fenter, P., Sturchio, N.C., Zhong, Z., Bedzyk, M.J., 1999. X-ray standing wave study of arsenite incorporation at the calcite surface. Geochimica et Cosmochimica Acta 63 (19-20), 3153-3157] on calcite surface. This study provides a molecular-level explanation for why As(III) is trapped by calcite in industrial treatments. (c) 2006 Elsevier B.V All rights reserved.
引用
收藏
页码:328 / 336
页数:9
相关论文
共 39 条
[11]   Remobilization of arsenic from buried wastes at an industrial site: mineralogical and geochemical control [J].
Juillot, F ;
Ildefonse, P ;
Morin, G ;
Calas, G ;
de Kersabiec, AM ;
Benedetti, M .
APPLIED GEOCHEMISTRY, 1999, 14 (08) :1031-1048
[12]  
Kinniburgh D.G., 2001, British Geological Survey Technical Report WC/00/19
[13]   Efficient iterative schemes for ab initio total-energy calculations using a plane-wave basis set [J].
Kresse, G ;
Furthmuller, J .
PHYSICAL REVIEW B, 1996, 54 (16) :11169-11186
[14]  
KRESSE G, 1999, VASP
[15]  
Langmuir D., 1997, AQUEOUS ENV GEOCHEMI
[16]   X-RAY STUDY OF THE ELECTRON-DENSITY IN CALCITE, CACO3 [J].
MASLEN, EN ;
STRELTSOV, VA ;
STRELTSOVA, NR .
ACTA CRYSTALLOGRAPHICA SECTION B-STRUCTURAL SCIENCE, 1993, 49 :636-641
[17]  
MIHALKOVIC M, 2004, PHYS REV B
[18]  
Plant JA, 2005, TREATISE ON GEOCHEMISTRY, VOL 9: ENVIRONMENTAL GEOCHEMISTRY, P17
[20]   Thermodynamic properties and stoichiometry of As(III) hydroxide complexes at hydrothermal conditions [J].
Pokrovski, G ;
Gout, R ;
Schott, J ;
Zotov, A ;
Harrichoury, JC .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1996, 60 (05) :737-749