Burduhos Nergis Dumitru Doru, Vizureanu Petrica, Sandu Andrei Victor, Burduhos Nergis Diana Petronela, Bejinariu Costica
Faculty of Materials Science and Engineering, Gheorghe Asachi Technical University of Iasi, 700050 Iasi, Romania.
Materials Science and Engineering Section, Technical Sciences Academy of Romania, Dacia Blvd 26, 030167 Bucharest, Romania.
Materials (Basel). 2021 Dec 28;15(1):202. doi: 10.3390/ma15010202.
Coal ash-based geopolymers with mine tailings addition activated with phosphate acid were synthesized for the first time at room temperature. In addition, three types of aluminosilicate sources were used as single raw materials or in a 1/1 wt. ratio to obtain five types of geopolymers activated with HPO. The thermal behaviour of the obtained geopolymers was studied between room temperature and 600 °C by Thermogravimetry-Differential Thermal Analysis (TG-DTA) and the phase composition after 28 days of curing at room temperature was analysed by X-ray diffraction (XRD). During heating, the acid-activated geopolymers exhibited similar behaviour to alkali-activated geopolymers. All of the samples showed endothermic peaks up to 300 °C due to water evaporation, while the samples with mine tailings showed two significant exothermic peaks above 400 °C due to oxidation reactions. The phase analysis confirmed the dissolution of the aluminosilicate sources in the presence of HPO by significant changes in the XRD patterns of the raw materials and by the broadening of the peaks because of typically amorphous silicophosphate (Si-P), aluminophosphate (Al-P) or silico-alumino-phosphate (Si-Al-P) formation. The phases resulted from geopolymerisation are berlinite (AlPO), brushite (CaHPO∙2HO), anhydrite (CaSO) or ettringite as AFt and AFm phases.
首次在室温下合成了添加尾矿并用磷酸活化的煤灰基地质聚合物。此外,使用三种类型的铝硅酸盐源作为单一原料或以1/1重量比使用,以获得五种用HPO活化的地质聚合物。通过热重-差热分析(TG-DTA)研究了所得地质聚合物在室温至600℃之间的热行为,并通过X射线衍射(XRD)分析了室温下养护28天后的相组成。在加热过程中,酸活化地质聚合物表现出与碱活化地质聚合物相似的行为。由于水蒸发,所有样品在300℃以下均出现吸热峰,而含有尾矿的样品在400℃以上由于氧化反应出现两个明显的放热峰。相分析通过原料XRD图谱的显著变化以及由于典型的无定形硅磷酸盐(Si-P)、铝磷酸盐(Al-P)或硅铝磷酸盐(Si-Al-P)形成导致的峰变宽,证实了铝硅酸盐源在HPO存在下的溶解。地质聚合产生的相为白硅钙石(AlPO)、透钙磷石(CaHPO∙2HO)、硬石膏(CaSO)或作为AFt和AFm相的钙矾石。