砷酸盐
亚砷酸盐
针铁矿
傅里叶变换红外光谱
化学
砷
吸附
红外光谱学
无机化学
氢键
核化学
萃取(化学)
分子
物理化学
有机化学
化学工程
工程类
作者
Xiaohua Sun,Harvey E. Doner
出处
期刊:Soil Science
[Ovid Technologies (Wolters Kluwer)]
日期:1996-12-01
卷期号:161 (12): 865-872
被引量:321
标识
DOI:10.1097/00010694-199612000-00006
摘要
The bonding structures of arsenite (As(III)) and arsenate (As(V)) on goethite (α-FeOOH) were studied by Transmission-Fourier Transform Infrared (T-FTIR) and Attenuated Total Reflectance-FTIR (ATR-FTIR) spectroscopy. ATR-FTIR spectra of deuterated goethite showed three bands of OD stretch, corresponding to singly, doubly, and triply coordinated OH hydroxyls on the goethite surface. Both FTIR modes provided similar structural information for arsenic adsorption. Most arsenate and arsenite oxyanions replaced two singly coordinated surface OH groups (A-type) to form binuclear bridging complexes Fe-O-AsO(OH)-O-Fe and Fe-O-As(OH)-O-Fe. However, their effects on doubly (C-type) and triply (B-type) coordinated surface OH groups are different. As(III) mainly reacted with C-type OH groups, whereas As(V) reacted with B-type OH groups. These reactions may be attributed to hydrogen-bonding and/or chemical bonding. Finally, we applied a sequential extraction method to evaluate the fractions with different bonding strengths. Relatively strong chemical extraction was necessary to remove 75 to 80% of adsorbed arsenite or arsenate from goethite. The strong retention of As(III) and As(V) is most likely caused by the formation of binuclear complexes with goethite.
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