In situ infrared speciation of absorbed carbonate on aluminum and iron oxide

被引:245
作者
Su, CM [1 ]
Suarez, DL [1 ]
机构
[1] ARS, USDA, US Salin Lab, Riverside, CA 92507 USA
关键词
attenuated total reflectance Fourier transform infrared; carbonate adsorption; electrophoretic mobility; infrared; point of zero charge; point of zero net proton charge; x-ray diffraction;
D O I
10.1346/CCMN.1997.0450605
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Surface adsorption mechanisms of dissolved inorganic carbon species on soil minerals are not well understood. Traditional infrared (IR) study of adsorbed species of inorganic carbon using air-dried samples may not reveal true species in the solid/water interface in suspension. The purpose of this study was to obtain information on interfacial carbonate speciation between solid and aqueous phases. The interaction of bicarbonate and carbonate ions with X-ray amorphous (am) Al and Fe oxides, gibbsite (gamma-Al(OH)(3)) and goethite ((alpha-FeOOH) was examined by electrophoresis and in sitar attenuated total reflectance Fourier transform infrared (ATR-FTIR) spectroscopy. The presence of carbonate lowered the electrophoretic mobility and decreased the point of zero charge (PZC) of all minerals, implying specific adsorption. Inner-sphere complexation of bicarbonate and carbonate was supported by a lowering in the anion sym metry due to the interaction with Al and Fe oxide surfaces. Only complexed monodentate carbonate was identified in am-Al(OH)(3)/aqueous solution at pH 4.1-7.8 when the solid was reacted with either NaHCO3 or Na2CO3 solutions. Am-Al(OH)(3) was transformed to a crystalline sodium aluminum hydroxy carbonate, dawsonite [NaAl(CO3)(OH)(2)], and bayerite (alpha-Al(OH)(3)) after reacting with 1.0 M NB2CO3 for 24 h. Gibbsite adsorbed much less carbonate than am-Al(OH)(3) such that adsorbed carbonate on gibbsite gave weal; IR absorption. It is probable that monodentate carbonate is also the complexed species on gibbsite. Evidence suggesting the presence of both surface complexed bicarbonate and carbonate species in the interfacial region of am-Fe(OH)(3) in suspension and the dependence of their relative distribution on solution pH is shown. Only monodentate carbonate was found in the interfacial region of goethite in 1.0 M NaHCO3. A ligand exchange reaction was proposed to describe the interaction of bicarbonate and carbonate with the surface functional groups of Al and Fe oxides.
引用
收藏
页码:814 / 825
页数:12
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