1998
DOI: 10.1016/s0992-4361(99)80017-4
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Lattice vibration spectra. Part XCV. Infrared spectroscopic studies on the iron oxide hydroxides goethite (α), akaganéite (β), lepidocrocite (γ), and feroxyhite (δ)

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Cited by 181 publications
(104 citation statements)
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“…41,43,45 Also, the studied materials demonstrate bands at 3450, 3000-2800, 1620, and 1380 cm -1 in the region of 600-4000 cm -1 . The bands at 3450 and 1620 cm -1 result from bending vibrations of hydrogen-bonded hydroxyl groups and physically adsorbed water on the surface of the samples, respectively.…”
Section: Description Of the Studied Samplesmentioning
confidence: 72%
“…41,43,45 Also, the studied materials demonstrate bands at 3450, 3000-2800, 1620, and 1380 cm -1 in the region of 600-4000 cm -1 . The bands at 3450 and 1620 cm -1 result from bending vibrations of hydrogen-bonded hydroxyl groups and physically adsorbed water on the surface of the samples, respectively.…”
Section: Description Of the Studied Samplesmentioning
confidence: 72%
“…as a wide absorption band with a maximum at 3158 stretching vibrations of H-O bonds [13]. Additionally, the spectrum of this sample contains weaker absorption bands with ν 1053, 1137 and 1160 cm −1 , which can be attributed to the stretching vibrations of (SO 4 ) 2− ions [14].…”
Section: Fig 2 the Average Crystal Size D (Nm) Of Phases Formed Inmentioning
confidence: 79%
“…Four main absorption peaks are observed at approximately 1142, 1023, 750, and 583 cm À1 , which is characteristic of the bonding structure in -FeOOH. [20][21][22] The absorption band at approximately 1142 cm À1 is assigned to the in-plane Fe-O-H bending vibration, and it is shifted to a À1 is observed in Fig. 5(c), which is caused by Fe-O-Si bending vibration.…”
Section: Infrared Spectramentioning
confidence: 97%