针铁矿
硫酸盐
化学
斯沃特曼矿
吸附
无机化学
离子强度
傅里叶变换红外光谱
衰减全反射
红外光谱学
离子键合
分析化学(期刊)
化学工程
色谱法
水溶液
离子
物理化学
有机化学
工程类
作者
Derek Peak,Robert Ford,Donald L. Sparks
标识
DOI:10.1006/jcis.1999.6405
摘要
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.
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