Ramli Mohd Izrul Izwan, Salleh Mohd Arif Anuar Mohd, Abdullah Mohd Mustafa Al Bakri, Aziz Ikmal Hakem, Ying Tan Chi, Shahedan Noor Fifinatasha, Kockelmann Winfried, Fedrigo Anna, Sandu Andrei Victor, Vizureanu Petrica, Chaiprapa Jitrin, Burduhos Nergis Dumitru Doru
Faculty of Chemical Engineering Technology, Universiti Malaysia Perlis (UniMAP), Perlis 02600, Malaysia.
Geopolymer & Green Technology, Center of Excellence (CEGeoGTech), Universiti Malaysia Perlis (UniMAP), Perlis 02600, Malaysia.
Materials (Basel). 2022 Apr 5;15(7):2667. doi: 10.3390/ma15072667.
Geopolymer materials are used as construction materials due to their lower carbon dioxide (CO) emissions compared with conventional cementitious materials. An example of a geopolymer material is alkali-activated kaolin, which is a viable alternative for producing high-strength ceramics. Producing high-performing kaolin ceramics using the conventional method requires a high processing temperature (over 1200 °C). However, properties such as pore size and distribution are affected at high sintering temperatures. Therefore, knowledge regarding the sintering process and related pore structures on alkali-activated kaolin geopolymer ceramic is crucial for optimizing the properties of the aforementioned materials. Pore size was analyzed using neutron tomography, while pore distribution was observed using synchrotron micro-XRF. This study elucidated the pore structure of alkali-activated kaolin at various sintering temperatures. The experiments showed the presence of open pores and closed pores in alkali-activated kaolin geopolymer ceramic samples. The distributions of the main elements within the geopolymer ceramic edifice were found with Si and Al maps, allowing for the identification of the kaolin geopolymer. The results also confirmed that increasing the sintering temperature to 1100 °C resulted in the alkali-activated kaolin geopolymer ceramic samples having large pores, with an average size of ~80 µm and a layered porosity distribution.
与传统胶凝材料相比,地质聚合物材料因其较低的二氧化碳(CO)排放量而被用作建筑材料。地质聚合物材料的一个例子是碱激活高岭土,它是生产高强度陶瓷的一种可行替代材料。使用传统方法生产高性能高岭土陶瓷需要较高的加工温度(超过1200°C)。然而,在高烧结温度下,诸如孔径和分布等性能会受到影响。因此,了解碱激活高岭土地质聚合物陶瓷的烧结过程及相关孔隙结构对于优化上述材料的性能至关重要。使用中子断层扫描分析孔径,同时使用同步加速器微X射线荧光观察孔隙分布。本研究阐明了碱激活高岭土在不同烧结温度下的孔隙结构。实验表明,碱激活高岭土地质聚合物陶瓷样品中存在开孔和闭孔。通过硅和铝图谱发现了地质聚合物陶瓷结构体中主要元素的分布,从而能够识别高岭土地质聚合物。结果还证实,将烧结温度提高到1100°C会导致碱激活高岭土地质聚合物陶瓷样品出现大孔,平均尺寸约为80 µm,且具有层状孔隙率分布。