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首页> 外文期刊>Advances in Materials Physics and Chemistry >Physico-Chemical and Mineralogical Characterization of Two Clay Materials of the Far North Region of Cameroon (Makabaye, Maroua)
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Physico-Chemical and Mineralogical Characterization of Two Clay Materials of the Far North Region of Cameroon (Makabaye, Maroua)

机译:喀麦隆最北部地区的两种粘土材料的理化和矿物学表征(马鲁巴,马鲁阿)

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摘要

To contribute to the valorization of local materials, the physico-chemical and mineralogical characterization of two clay materials MJ and MN collected in the Mayo Tsanaga river which crosses the Makabaye district of Maroua (Cameroon) was carried out. For this purpose, various methods of characterization have been used, namely granulometric analysis, Atterberg limits, X-ray fluorescence spectrometry and X-ray diffraction. It is apparent from the granulometry that the clay materials studied titrate 33.77% of clays for MJ against 44.13% for MN. The plasticity indices Ip with values Ip_(MJ) = 19.27% and Ip_(MN) = 23.4% place the materials in the plastic domain and offer them the possibility to being shaped into objects. The chemical composition of the MJ and MN materials reveals that the silicon oxide SiO_2, the aluminumoxide Al_2O_3 and iron oxide Fe_2O_3 are their main constituents. The X-ray diffraction of the MJ and MN materials shows that they consist mainly of quartz with associated kaolinite, illite, montmorillonite, perlialite, dickite, nacrite, amesite, albite, brookite and anorthite. In addition to these, 2/1 minerals such as muscovite, nontronite, glauconite, and phlogopite are also identified in the MJ material. The peaks of sanidine, microcline and gismondine are also found in the MN material. The materials being rich in clay minerals 2/1 can be valorized in the adsorption and the absorption of the oils and greases and in the waterproofing of the grounds. The presence of quartz, kaolinite and illite is undoubtedly favorable for the manufacture of ceramic products in terracotta. These products will be obtained at a relatively lower temperature due to illite, feldspars and iron minerals that provide vitrification during firing by forming eutectics. The aluminosilicate amorphous phases contained in the studied materials can be exploited to produce geopolymer cements and concretes.
机译:为了促进当地材料的增值,对穿过马鲁阿(喀麦隆)马卡巴耶地区的梅奥·察纳加河中收集的两种黏土材料MJ和MN进行了物理化学和矿物学表征。为了这个目的,已经使用了各种表征方法,即粒度分析,阿特伯格极限,X射线荧光光谱法和X射线衍射。从粒度分析中可以明显看出,所研究的粘土材料滴定了MJ的粘土含量为33.77%,而MN为44.13%。具有Ip_(MJ)= 19.27%和Ip_(MN)= 23.4%值的可塑性指数Ip将材料置于塑性域中,并为它们提供了成型为物体的可能性。 MJ和MN材料的化学成分表明,氧化硅SiO_2,氧化铝Al_2O_3和氧化铁Fe_2O_3是它们的主要成分。 MJ和MN材料的X射线衍射表明,它们主要由石英以及相关的高岭石,伊利石,蒙脱土,珍珠岩,珍珠岩,珍珠岩,铁矾石,钠长石,板钛矿和钙长石组成。除了这些之外,MJ材料中还鉴定出2/1矿物,例如白云母,绿脱石,青石和金云母。在MN材料中也发现了Sanidine,microcline和gismondine的峰。富含粘土矿物2/1的材料在油和油脂的吸附和吸收以及地面防水方面可以发挥作用。石英,高岭石和伊利石的存在无疑有利于兵马俑中陶瓷产品的生产。由于伊利石,长石和铁矿物质在煅烧过程中通过形成共晶而提供玻璃化作用,因此将在相对较低的温度下获得这些产品。所研究材料中所含的铝硅酸盐无定形相可用于生产地聚合物水泥和混凝土。

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