尼日利亚ondo州ifon ose地方政府辖区omialafara粘土矿床的物化和矿物学性质评价

E. Irabor, T.E. Anaun
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引用次数: 0

摘要

采用标准方法对尼日利亚Ondo州Ifon Ose地方政府区的Omialafara粘土矿床的物理化学和矿物学性质进行了评价。研究结果表明,该矿床由层状硅酸盐矿物组成,包括丽沙石铝、斜长石铁、海泡石铁、新富石;其他的是石英、针铁矿,甚至还有一种非常罕见的碳氢化合物矿物。粘土矿物溶胀性好,塑性中等,收缩率超出推荐范围,耐热性好,表观孔隙率在推荐范围内。其耐火度低于1200oC。粘土矿物矿床的性质反映了粘土和非矿物组成的综合特征,这使得它适合在1200℃的极限工作温度下的各种应用。粘土矿物矿床的有色性质是由有色粘土矿物和针铁矿的存在共同造成的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
EVALUATION OF THE PHYSICO-CHEMICAL AND MINERALOGICAL PROPERTIES OF A CLAY MINERAL DEPOSIT IN OMIALAFARA IN IFON OSE LOCAL GOVERNMENT AREA IN ONDO STATE , NIGERIA
The physico-chemical and mineralogical properties of a clay mineral deposit in Omialafara in Ifon Ose Local Government Area in Ondo State, Nigeria was evaluated using standard methods. The results of the study revealed that the deposit consisted of phyllosilicate minerals- lizardite aluminian, clinochlore feroanB, sepiolite ferrian , neotocite; others were quartz, goethite and evenkite a very rare hydrocarbon mineral. The clay minerals exhibited good swelling property, medium plasticity, shrinkage in excess of recommended range, good thermal resistance and the apparent porosity was within the recommended limit. It had refractoriness below 1200oC. The properties of the clay mineral deposit was a reflection of the combined characteristics of both the clay and non-mineral composition which recommends it for a variety of applications subject to a limiting working temperature of 1200oC. The coloured nature of the clay mineral deposit was accounted for by a combination of the presence of the coloured clay minerals and goethite.  
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