石英
流体包裹体
多孔性
煅烧
矿物学
浸出(土壤学)
气泡
材料科学
地质学
复合材料
化学
催化作用
生物化学
并行计算
计算机科学
土壤科学
土壤水分
作者
Shoujing Wang,Deshui Yu,Chi Ma,Fushuai Wei,Haiqi Zhang
出处
期刊:Minerals
[MDPI AG]
日期:2024-08-01
卷期号:14 (8): 794-794
被引量:10
摘要
A purification process including flotation separation, acid leaching, calcination, and water quenching was conducted to obtain high-purity quartz sand. The surface morphology of the quartz after flotation separation, acid leaching, calcination, and water quenching reveals that the cracks, pits, and cavities on the quartz surface can be deepened and enlarged, and the more fluid inclusions, the greater the number and openness of cracks, pits, and cavities. The specific surface area is positively correlated with the number of cracks, pits, and cavities, the opacity of quartz glass, and the number of bubbles in quartz glass. The results of Raman spectroscopy analysis reveal that the bubbles in quartz glass are composed of nitrogen, which excludes the possibility of bubble formation in quartz glass caused by the gas composition (i.e., H2O) of unburst fluid inclusions in quartz sand. The formation of bubbles in quartz glass is more likely to be related to a high specific surface area and porosity, which increase the surface adsorption performance of quartz and contribute to the adsorption of more gas. The presented results suggest that using these methods to reduce the content of fluid inclusions in quartz cannot effectively solve the problem of bubbles in quartz glass, and using quartz raw materials with no or minor fluid inclusions is still the key to ensuring the quality of quartz products.
科研通智能强力驱动
Strongly Powered by AbleSci AI