2022
DOI: 10.1016/j.jhazmat.2021.127657
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Solid phase characterization and transformation of illite mineral with gas-phase ammonia treatment

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Cited by 12 publications
(3 citation statements)
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“…The loading spectrum of GCM is illustrated in figure 4 and encompasses the following FTIR spectral bands: two stretching bands associated with structural hydroxyl groups (3691 and 3619 cm -1 ), a band corresponding to Si-O stretching (987 cm -1 ), deformation bands related to Al-Al-OH vibration (987 cm -1 ), and deformation bands associated with Al-O-Si in-plane vibration (797 cm -1 ) (Ashour and Tony, 2020).The bands observed at 3619 cm -1 , 987 cm -1 , and 797 cm -1 are attributed to illite, similar results were found in the study reported by Oumar et al in 2022. The bands at 1638 and 1634 cm -1 in the loading spectra are indicative of carbonates present as impurities in the sample (Di Pietro et al, 2022). The presence of carbonates in this sample is minimal; hence, the intensity of the band in the IR spectra is very weak.…”
Section: Ftir Analysismentioning
confidence: 93%
“…The loading spectrum of GCM is illustrated in figure 4 and encompasses the following FTIR spectral bands: two stretching bands associated with structural hydroxyl groups (3691 and 3619 cm -1 ), a band corresponding to Si-O stretching (987 cm -1 ), deformation bands related to Al-Al-OH vibration (987 cm -1 ), and deformation bands associated with Al-O-Si in-plane vibration (797 cm -1 ) (Ashour and Tony, 2020).The bands observed at 3619 cm -1 , 987 cm -1 , and 797 cm -1 are attributed to illite, similar results were found in the study reported by Oumar et al in 2022. The bands at 1638 and 1634 cm -1 in the loading spectra are indicative of carbonates present as impurities in the sample (Di Pietro et al, 2022). The presence of carbonates in this sample is minimal; hence, the intensity of the band in the IR spectra is very weak.…”
Section: Ftir Analysismentioning
confidence: 93%
“…However, in these experimental samples, the infrared signals at 800, 777, and 747 cm −1 (Figure 4) show faint but sensible variations that would be interest to OH bending vibrations/interactions with cations, thus pointing to possible leeching processes. The 1000 and 900 cm −1 bands, related to Si-O-Si stretching and Al-Al-OH bending [28], can be tentatively attributed to structural modification of the illite clays or muscovite with possibly consequent cation losses.…”
Section: Diffusion Experimentsmentioning
confidence: 93%
“…The properties of illite are no swelling, adequate plasticity and workability, and change in color from grey to red and black depending on the amount of ion oxides calcite, and pyrite, as well as the process of firing. This type of clay is common in the Mediterranean area [36,37]. (iii) Smectite: This involves several minerals, including montmorillonite ((Na, Ca) 0 .…”
Section: Claymentioning
confidence: 99%