磁铁矿
铜
赤铁矿
拉曼光谱
退火(玻璃)
氧化铁
大气温度范围
氧化物
氧化铜
材料科学
冶金
无机化学
化学
化学工程
矿物学
分析化学(期刊)
环境化学
气象学
工程类
物理
光学
作者
F. Pérez-Robles,Francisco Javier García Rodríguez,S. Jiménez‐Sandoval,J. González‐Hernández
标识
DOI:10.1002/(sici)1097-4555(199912)30:12<1099::aid-jrs490>3.0.co;2-0
摘要
The structure of heat-treated sol–gel-made SiO2 samples containing copper or iron in various amounts was studied using Raman spectroscopy and x-ray diffraction. The treatments were in air in the temperature range 200–800 °C. Copper and iron concentrations were in the range 7–55 wt%. It was found that in the samples containing copper, the metal is mainly dissolved in the SiO2 network when the thermal treatment is at low temperatures. For higher annealing temperatures, first a copper silicate is formed and then most of the copper forms cupric oxide particles at temperatures of about 800 °C. In samples containing iron, the formation of particles with nanometric size of the γ-Fe2O3 (maghemite) phase is observed after annealing at 500 °C. At 800 °C the maghemite phase is transformed into the stable hematite (α-Fe2O3) phase. Copyright © 1999 John Wiley & Sons, Ltd.
科研通智能强力驱动
Strongly Powered by AbleSci AI