赤铁矿
球体
粒径
傅里叶变换红外光谱
材料科学
谱线
粒子(生态学)
分子物理学
吸收(声学)
声子
椭球体
凝聚态物理
光学
化学
物理
矿物学
复合材料
量子力学
海洋学
物理化学
天文
地质学
作者
Li Wang,Atsushi Muramatsu,Tadao Sugimoto
标识
DOI:10.1016/s0927-7757(97)00102-7
摘要
Abstract The FTIR spectra of well-defined hematite (α-Fe2O3) particles varying in size, shape and internal structure have systematically been analyzed. It has been found that the absorption peak frequencies of the pseudocubic particles are located between the corresponding theoretical peak frequencies of spheres and cubes and shift to lower frequencies as particle size increases, corresponding approximately with the Mie theory. However, the basic spectrum pattern was determined by the morphology of the particles. The observation of ellipsoids with various aspect ratios revealed some essential discrepancies in the peak frequency between experiment and the theory on the surface phonon modes in small particles, even if the particles were completely dispersed in the medium. The internal structure mainly affects the peak width, which increases with the decreasing subcrystal size. Finally, the effects of aggregation on the IR spectrum are discussed.
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