Villalobos Mario, Cheney Marcos A, Alcaraz-Cienfuegos Jorge
Grupo de Bio-Geoquímica Ambiental, Universidad Nacional Autónoma de México, Coyoacán, 04510 DF, Mexico.
J Colloid Interface Sci. 2009 Aug 15;336(2):412-22. doi: 10.1016/j.jcis.2009.04.052. Epub 2009 May 3.
The model described in this investigation explains the variable macroscopic surface reactivity of different goethite preparations when adsorption data are normalized by surface area, especially the high reactivity of low specific surface area goethites. A simplified model of crystalline face distributions for each of the goethite preparations, in combination with experimental maximum chromate adsorption values previously determined, allowed a crystallographic site-density analysis that would explain the latter values. In addition, a surface complexation modeling approach was coupled to the previous model and provided individual affinity constants for proton and ion binding for singly, doubly, and triply coordinated surface sites. The proposed microscopic model is able to accurately describe the macroscopic adsorption behavior of protons, carbonate, chromate, and lead(II) ions on three goethites of specific surface areas of 50, 70, and 94 m(2)/g, using the same affinity constants. The model results indicate that the surface of high specific surface area nanoparticulate goethites may be described mostly as a combination of (1 0 1) and (0 0 1) faces, with reactive singly and triply coordinated surface oxygen sites; while the model for low specific surface area goethites requires, in addition to one of the above faces, a variable but high degree of (0 1 0)/(2 1 0) faces containing high surface densities of reactive singly and doubly coordinated oxygen groups. The model is potentially very useful and may be applied to any goethite provided its maximum ion adsorption capacity and proton charging behavior are known.
本研究中描述的模型解释了在通过表面积对吸附数据进行归一化时,不同针铁矿制剂的宏观表面反应性差异,特别是低比表面积针铁矿的高反应性。结合先前测定的实验最大铬酸盐吸附值,对每种针铁矿制剂的晶面分布进行简化模型,从而进行晶体学位点密度分析,以解释后者的值。此外,将表面络合建模方法与先前的模型相结合,给出了单配位、双配位和三配位表面位点的质子和离子结合的个体亲和常数。所提出的微观模型能够使用相同的亲和常数,准确描述质子、碳酸盐、铬酸盐和铅(II)离子在比表面积分别为50、70和94 m²/g的三种针铁矿上的宏观吸附行为。模型结果表明,高比表面积纳米颗粒针铁矿的表面主要可描述为(1 0 1)面和(0 0 1)面的组合,具有反应性的单配位和三配位表面氧位点;而低比表面积针铁矿的模型除了上述其中一个面外,还需要一定程度的(0 1 0)/(2 1 0)面,这些面上含有高表面密度的反应性单配位和双配位氧基团。该模型可能非常有用,只要知道其最大离子吸附容量和质子充电行为,就可应用于任何针铁矿。