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针铁矿上硫酸盐键合机制的原位衰减全反射傅里叶变换红外光谱研究

An in Situ ATR-FTIR Investigation of Sulfate Bonding Mechanisms on Goethite.

作者信息

Peak D, Ford RG, Sparks DL

机构信息

Department of Plant and Soil Sciences, University of Delaware, 149 Townsend Hall, Newark, Delaware, 19717-1303

出版信息

J Colloid Interface Sci. 1999 Oct 1;218(1):289-299. doi: 10.1006/jcis.1999.6405.

Abstract

The mechanism of sulfate adsorption on goethite was investigated in situ using attenuated total reflectance Fourier transform infrared (ATR-FTIR) spectroscopy. Sulfate adsorption was investigated at ionic strengths between 0.005 and 0.1 M, reactant concentrations between 5 and 500 µM, and pH values between 3.5 and 9.0. It was determined that sulfate forms both outer-sphere and inner-sphere surface complexes on goethite at pH less than 6. At pH values greater than 6, sulfate adsorbs on goethite only as an outer-sphere complex. The relative amount of outer-sphere sulfate surface complexation increased with decreasing ionic strength. The spectrum of sulfate adsorbed on goethite was also compared to the infrared spectrum of synthetic schwertmannite, an iron(III) oxy-hydroxy-sulfate. It was determined that in situ spectra of both schwertmannite and adsorbed sulfate are quite similar, suggesting that a continuum of outer- and inner-sphere sulfate occurs in both cases. Copyright 1999 Academic Press.

摘要

利用衰减全反射傅里叶变换红外光谱(ATR-FTIR)原位研究了针铁矿对硫酸盐的吸附机制。在离子强度为0.005至0.1 M、反应物浓度为5至500 μM以及pH值为3.5至9.0的条件下研究了硫酸盐吸附情况。结果表明,在pH小于6时,硫酸盐在针铁矿上形成外层和内层表面络合物。在pH值大于6时,硫酸盐仅以外层络合物形式吸附在针铁矿上。外层硫酸盐表面络合的相对量随离子强度降低而增加。还将吸附在针铁矿上的硫酸盐光谱与合成施韦特曼石(一种铁(III)羟基硫酸盐)的红外光谱进行了比较。结果表明,施韦特曼石和吸附硫酸盐的原位光谱非常相似,表明在这两种情况下都存在外层和内层硫酸盐的连续体。版权所有1999年学术出版社。

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