构成蒙脱石群的矿物

Khandamov Davron Abdikadirovich, Djumaniyazova Malokhat Rihsiyevna, Tursunova Dilnozakhon Isroiljon Qizi
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引用次数: 0

摘要

含规则结构物质的粘土是自然界中最常用的水净化无机吸附剂。吸附剂属于可膨胀结构地层矿物类型,包括蒙脱土和蛭石,它们构成膨润土粘土的基础。膨润土是一种粘土,主要由蒙脱土属的矿物组成,有时被称为石皂。纳夫巴赫碱性膨润土矿床位于乌兹别克斯坦共和国纳沃伊州纳夫巴赫地区。该矿床目前探明储量714.26万吨以上。蒙脱土主要是各种化合物和水净化最有效的吸附剂。蒙脱土的表面积为450 m2/g,蛭石的表面积为450-500 m2/g[1]。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Minerals That Make Up the Montmorillonite Group
Clays containing materials of regular structure are the most common inorganic sorbents for water purification in nature. Sorbents belonging to the type of expandable structural stratum minerals include montmorillonite and vermiculite, which form the basis of bentonite clays. Bentonites are clays which compose mainly of minerals belonging to the group of montmorillonite and sometimes called stonesoap. Navbahor alkaline bentonite deposit is located in Navbahr district of Navoi region of Uzbekistan Republic. The current proven reserves of the deposit are more than 7142.6 thousand tons. Montmorillonite is mainly the most effective adsorbent for various compounds and water purification. The surface area of montmorillonite is 450 m2/g, and vermiculite is 450-500 m2/g [1].
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