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The Physico-Mechanical Characteristics of the Clays in and After Doping With Metal Oxide Al2O3 in the Region of Fez (Morocco)

机译:菲斯地区金属氧化物Al 2 O 3 中掺杂后的黏土的物理力学特性

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Miocene marl is one of the widespread geological substrates in Fez vicinity (Central Morocco). In this study we proceed by a physicochemical characterization of the marl after doping with metal oxides, by various analytical techniques, namely the X-ray fluorescence, the mineralogical analysis, and dielectric property. The doping of these marl was conducted by solid oxides of Al2O3 at different percentages (5%, 10% and 15%). The results of chemical analysis showed the Al2O3 increase during doping. So, the mineralogical analysis of doped clays shows peaks' increases for kaolin. The marl doped acquired the property of their good electrical conductor compared to crass marl.
机译:中新世泥灰岩是非斯附近(摩洛哥中部)广泛的地质基质之一。在这项研究中,我们通过各种分析技术,即X射线荧光,矿物学分析和介电性能,对金属氧化物掺杂后的泥灰石进行了物理化学表征。这些灰泥的掺杂是通过Al 2 O 3 的固体氧化物以不同的百分比(5%,10%和15%)进行的。化学分析结果表明,掺杂过程中Al 2 O 3 的增加。因此,掺杂粘土的矿物学分析表明高岭土的峰增加。相比于黄铜渣,掺杂的石灰获得了其良好电导体的性能。

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