聚合物
硅酸盐
傅里叶变换红外光谱
硅酸钠
衰减全反射
粉煤灰
材料科学
单体
沸石
溶胶凝胶
氢氧化物
微观结构
化学工程
化学
矿物学
无机化学
有机化学
冶金
催化作用
复合材料
纳米技术
聚合物
工程类
作者
Catherine A. Rees,John L. Provis,Grant C. Lukey,J.S.J. van Deventer
出处
期刊:Langmuir
[American Chemical Society]
日期:2007-06-23
卷期号:23 (15): 8170-8179
被引量:423
摘要
Structural changes in fly ash geopolymers activated with different sodium hydroxide and silicate concentrations are investigated using attenuated total reflectance Fourier transform infrared (ATR-FTIR) spectroscopy over a period of 200 days. A strong correlation is found between the concentration of silicate monomer in the activating solution and the position of the main Si-O-T stretching band in the FTIR spectrum, which gives an indication of the relative changes in the gel Si/Al ratio. The FTIR spectra of geopolymer samples with activating solution concentrations of up to 1.2 M SiO2 indicate that an Al-rich gel forms before the final gel composition is reached. The time required for the system to reach a steady gel composition depends on the silicate activating solution concentration and speciation. Geopolymers activated with solutions containing predominantly high-order silicate species rapidly reach a steady gel composition without first forming an Al-rich gel. A minimum silicate monomer concentration of approximately 0.6 M is required to shift the geopolymer synthesis mechanism from hydroxide activation to silicate activation. Silicate speciation in the activating solutions also affects zeolite formation and geopolymer microstructures, with a more homogeneous microstructure and less zeolite formation observed at a higher SiO2 content.
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