铁酸盐
蒙脱石
高岭石
吸附
氮气
矿物学
化学
化学工程
材料科学
无机化学
物理化学
有机化学
工程类
作者
R. Celis,J. Cornejo,M.C. Hermosı́n
出处
期刊:Clay Minerals
[Cambridge University Press]
日期:1998-09-01
卷期号:33 (3): 395-407
被引量:29
标识
DOI:10.1180/000985598545705
摘要
Abstract Kaolinite-ferrihydrite and montmorillonite-ferrihydrite associations were prepared following a procedure based on the Russell method for the synthesis of ferrihydrite and the texture of the clay-ferrihydrite complexes was studied using different techniques. The textural properties of kaolinite were little affected by the Fe association, showing only a slight increase in the specific surface area measured by nitrogen adsorption and a decrease in the largest pores (>10 µm), as measured by mercury porosimetry. In contrast, the nitrogen specific surface area of the montmorillonite complexes was much higher than that of the clay without Fe and the pore structure depended on the amounts of Fe in the complexes. Application of the fractal approach to nitrogen adsorption data indicated that the surface roughness (microporosity) was greater for the complexes prepared from diluted Fe(III) solutions, in agreement with the information obtained from classical interpretation of the adsorption isotherms (shape of the isotherms and t-plots).
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