含皂石膨润土覆岩细粉的结构改性

A. Ayzenshtadt, E. Korolev, M. Malygina, T. Drozdyuk, M. Frolova
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引用次数: 0

摘要

研究了高分散皂矿粉体机械分散后结构改性过程的动力学规律。作为表征矿物晶格重构的信息标准,采用了粉体在不同磨矿时间比表面的变化以及在810 ~ 820°С温度范围内的放热热效应(焓变)。经测定,含皂石物料在机械研磨超过20分钟的过程中,皂石发生强烈的改性,其结构发生变化,导致蛇纹石的形成。在优化实验样品的结构变化时,传统的用粉体比表面来评价原料机械研磨过程的准则并不是一个足够的信息参数。这一过程的主要参数是焓因子,它表征了结构改性的热效应。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Structural modification of fine powders of overburden rocks of saponite-containing bentonite clay
The kinetic regularities of the process of structural modification of highly dispersed powders of saponite-containing material after mechanical dispersion have been studied. As information criteria characterizing the restructuring of the crystal lattice of minerals, changes are used that occur with the specific surface of powders at different grinding times and the exothermic thermal effect (enthalpy change) in the temperature range of 810 – 820 °С. It has been determined that during mechanical grinding of a saponite-containing material for more than 20 minutes, intensive modification of saponite occurs, associated with its structural changes, leading to the formation of serpentine. It has been established that the traditionally used criterion for evaluating the process of mechanical grinding of raw materials by the specific surface of the powder in this case is not a sufficient information parameter when optimizing structural changes in experimental samples. The dominant parameter of this process is the enthalpy factor, which characterizes the thermal effect of the structural modification.
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