Martínez-Martínez Sergio, Bouguermouh Karima, Bouzidi Nedjima, Mahtout Laila, Sánchez-Soto Pedro J, Pérez-Villarejo Luis
Department of Mechanical & Mining Engineering, Linares Higher Polytechnic School, University of Jaén, Cinturón Sur s/n, 23700 Linares, Spain.
Center for Advanced Studies in Earth Sciences, Energy and Environment (CEACTEMA), University of Jaén, Campus "Las Lagunillas", 23071 Jaén, Spain.
Materials (Basel). 2024 Apr 16;17(8):1839. doi: 10.3390/ma17081839.
In the present work, the development of geopolymeric materials with Na or K based on industrial kaolin samples, with variable kaolinite content and alkaline silicates, is studied. XRF, XRD, FTIR and SEM-EDS have been used as characterization techniques. Three ceramic kaolin samples, two from Algeria and one from Charente (France), have been considered. In particular, chemical and mineralogical characterization revealed elements distinct of Si and Al, and the content of pure kaolinite and secondary minerals. Metakaolinite was obtained by grinding and sieving raw kaolin at 80 μm and then by thermal activation at 750 °C for 1 h. This metakaolinite has been used as a base raw material to obtain geopolymers, using for this purpose different formulations of alkaline silicates with NaOH or KOH and variable Si/K molar ratios. The formation of geopolymeric materials by hydroxylation and polycondensation characterized with different Si/Al molar ratios, depending on the original metakaolinite content, has been demonstrated. Sodium carbonates have been detected by XRD and FTIR, and confirmed by SEM-EDS, in two of these geopolymer materials being products of NaOH carbonation.
在本研究中,基于工业高岭土样品,研究了含钠或钾的地质聚合物材料的开发,这些样品具有可变的高岭石含量和碱性硅酸盐。X射线荧光光谱法(XRF)、X射线衍射法(XRD)、傅里叶变换红外光谱法(FTIR)和扫描电子显微镜-能谱仪(SEM-EDS)已被用作表征技术。考虑了三种陶瓷高岭土样品,两种来自阿尔及利亚,一种来自法国夏朗德省。特别是,化学和矿物学表征揭示了硅和铝以外的元素,以及纯高岭石和次生矿物的含量。偏高岭土是通过将原始高岭土研磨并筛分为80μm,然后在750℃下热活化1小时而获得的。这种偏高岭土已被用作基础原料来制备地质聚合物,为此使用了不同配方的含氢氧化钠或氢氧化钾的碱性硅酸盐以及可变的硅/钾摩尔比。已经证明,根据原始偏高岭土含量,通过具有不同硅/铝摩尔比的羟基化和缩聚反应形成地质聚合物材料。通过XRD和FTIR检测到碳酸钠,并通过SEM-EDS得到证实,在其中两种地质聚合物材料中,碳酸钠是氢氧化钠碳酸化的产物。