奥克拉粘土的矿物学、物理化学和形态特征

N. Salahudeen, Aminat Oluwafisayo Abodunrin
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引用次数: 1

摘要

当地粘土矿物开采自尼日利亚江户州Etsako地方政府区Okpella镇。利用x射线衍射分析仪对粘土进行了矿物学表征。用x射线荧光分析仪对粘土进行了化学表征,并用pH计对粘土进行了pH分析。矿物学分析表明,粘土主要为白云岩矿物,白云岩含量达72%。杂质含量为18%方解石、4.1%石榴石、5%方解石和1%生石灰。粘土的pH值分析表明,粘土呈酸性,平均pH值为3.9。1:1、1:2、1:4、1:8和1:10样品的pH值分别为3.61、3.85、3.85、4.05和4.09。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Mineralogical, Physicochemical and Morphological Characterization of Okpella Clay
Abstract Local clay mineral was mined from Okpella Town, Etsako Local Government Area of Edo State, Nigeria. Mineralogical characterization of the clay was carried out using X-ray diffraction analyzer. Chemical characterization of the clay was carried out using X-ray fluorescence analyzer and the pH analysis of the clay was carried out using pH meter. The mineralogical analysis revealed that the clay was majorly a dolomite mineral having 72% dolomite. The impurities present are 18% cristobalite, 4.1% garnet, 5% calcite and 1% quicklime. The pH analysis of the clay revealed that the clay was acidic having average pH value of 3.9. The pH determined for the 1:1, 1:2, 1:4, 1:8 and 1:10 samples were 3.61, 3.85, 3.85, 4.05 and 4.09, respectively.
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