Missana T, Alonso U, García-Gutiérrez M
CIEMAT, Departamento de Medioambiente Avenida Complutense 22, 28040 Madrid, Spain.
J Colloid Interface Sci. 2009 Jun 15;334(2):132-8. doi: 10.1016/j.jcis.2009.02.059. Epub 2009 Apr 8.
This study provides a large set of experimental selenite sorption data for pure smectite and illite. Similar sorption behavior existed in both clays: linear within a large range of the Se concentrations investigated (from 1x10(-10) to 1x10(-3) M); and independent of ionic strength. Selenite sorption was also analysed in the illite/smectite system with the clays mixed in two different proportions, as follows: (a) 30% illite-70% smectite and (b) 43% illite-57% smectite. The objective of the study was to provide the simplest model possible to fit the experimental data, a model also capable of describing selenite sorption in binary illite/smectite clay systems. Selenite sorption data, separately obtained in the single mineral systems, were modeled using both a one- and a two-site non-electrostatic model that took into account the formation of two complexes at the edge sites of the clay. Although the use of a two-site model slightly improved the fit of data at a pH below 4, the simpler one-site model reproduced satisfactorily all the sorption data from pH 3 to 8. The complexation constants obtained by fitting sorption data of the individual minerals were incorporated into a model to predict the adsorption of selenium in the illite/smectite mixtures; the model's predictions were consistent with the experimental adsorption data.
本研究提供了大量关于纯蒙脱石和伊利石对亚硒酸盐吸附的实验数据。两种黏土存在相似的吸附行为:在所研究的较大亚硒酸盐浓度范围内(从1×10⁻¹⁰到1×10⁻³ M)呈线性关系;且与离子强度无关。还对伊利石/蒙脱石体系中两种不同比例混合的黏土进行了亚硒酸盐吸附分析,如下:(a) 30%伊利石 - 70%蒙脱石和(b) 43%伊利石 - 57%蒙脱石。本研究的目的是提供一个尽可能简单的模型来拟合实验数据,该模型还应能够描述二元伊利石/蒙脱石黏土体系中的亚硒酸盐吸附。在单一矿物体系中分别获得的亚硒酸盐吸附数据,使用考虑了黏土边缘位点形成两种络合物的单点位和双点位非静电模型进行建模。尽管在pH值低于4时使用双点位模型能稍微改善数据拟合,但更简单的单点位模型在pH值3到8范围内令人满意地再现了所有吸附数据。通过拟合各矿物吸附数据得到的络合常数被纳入一个模型,以预测伊利石/蒙脱石混合物中硒的吸附;该模型的预测结果与实验吸附数据一致。