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膨润土的酸化脱色机理研究
引用本文:王世杰 陈丰. 膨润土的酸化脱色机理研究[J]. 矿物学报, 1993, 13(4): 325-330
作者姓名:王世杰 陈丰
作者单位:中国科学院地球化学研究所,中国科学院地球化学研究所 贵阳 550002,贵阳 550002
摘    要:
通过对广西田东钙基膨润土的酸化脱色实验研究,表明活性土的脱色能力是其表面积和酸化作用中浸取出的铝离子量的函数;在钙蒙脱石晶体结构处于彻底破坏前的临界点,膨润土具有最大的脱色能力和比表面积。

关 键 词:膨润土 矿物油 植物油 脱色 酸化

A STUDY ON THE MECHANISM OF ACIDATION AND DECOLORIZATION OF BENTONITE
Wang Shijie,Chen Feng Institute of Geochemistry,Academia Sinica,Guiyang. A STUDY ON THE MECHANISM OF ACIDATION AND DECOLORIZATION OF BENTONITE[J]. Acta Mineralogica Sinica, 1993, 13(4): 325-330
Authors:Wang Shijie  Chen Feng Institute of Geochemistry  Academia Sinica  Guiyang
Affiliation:Wang Shijie,Chen Feng Institute of Geochemistry,Academia Sinica,Guiyang,550002
Abstract:
The decoloring ability of Ca-bentonite from Tiandong, Guangxi, which was obtained byacidation of bentonite, has been determined as a function of its surface area and amount of alumi-num cations removed from the octahedra of montmorillonite. During the acid curing, the greatestdecoloring ability and surface area of bentonite were achieved at the crystal structure collapse'scritical point of Ca-montmorillonite.
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