2012
DOI: 10.1180/claymin.2012.047.4.08
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Mineralogical and physico-chemical characterizations of clay from Keur Saër (Senegal)

Abstract: There is interest in exploiting and developing natural resources, particularly deposits of natural clays. Senegal has several clay mineral deposits for which chemical and mineralogical compositions have been little studied. Some of these natural materials are nowadays used in pottery and ceramics. To extend applications, a better basic knowledge is required and, for this objective, the raw clay and separated <2 μm clay fraction from Keur Saër (Senegal) were subjected to chemical and mineralogical studies. S… Show more

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Cited by 5 publications
(4 citation statements)
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“…Figure depicts the FTIR spectra of NC and different CAPB-NC samples. The absorption band at 3697 cm –1 is assigned to combined in-phase and out-of-phase stretching frequency of hydroxyl groups of kaolinite. , Bands around 3438 and 1625 cm –1 are attributed to adsorbed water stretching and bending vibration, respectively . The bands at 2970 and 2920 cm –1 are attributed to the asymmetric stretching vibration of C–C in the alkyl chain, while the bands at 2856 and 1390 cm –1 are attributed to the symmetric stretching and bending mode, respectively, of the same group. , The intense band at 1045 cm –1 with a shoulder at 1090 cm –1 is ascribed to perpendicular stretching vibrations of the Si–O–Si group, while the bands at 685 and 468 cm –1 are the bending mode of the same group. ,, Absorption bands at 920 and 534 cm –1 are ascribed to Al­(IV)–OH and Si–O–Al­(VI) stretching vibrations, respectively.…”
Section: Resultsmentioning
confidence: 99%
See 1 more Smart Citation
“…Figure depicts the FTIR spectra of NC and different CAPB-NC samples. The absorption band at 3697 cm –1 is assigned to combined in-phase and out-of-phase stretching frequency of hydroxyl groups of kaolinite. , Bands around 3438 and 1625 cm –1 are attributed to adsorbed water stretching and bending vibration, respectively . The bands at 2970 and 2920 cm –1 are attributed to the asymmetric stretching vibration of C–C in the alkyl chain, while the bands at 2856 and 1390 cm –1 are attributed to the symmetric stretching and bending mode, respectively, of the same group. , The intense band at 1045 cm –1 with a shoulder at 1090 cm –1 is ascribed to perpendicular stretching vibrations of the Si–O–Si group, while the bands at 685 and 468 cm –1 are the bending mode of the same group. ,, Absorption bands at 920 and 534 cm –1 are ascribed to Al­(IV)–OH and Si–O–Al­(VI) stretching vibrations, respectively.…”
Section: Resultsmentioning
confidence: 99%
“…The absorption band at 3697 cm −1 is assigned to combined in-phase and out-of-phase stretching frequency of hydroxyl groups of kaolinite. 26,38 Bands around 3438 and 1625 cm −1 are attributed to adsorbed water stretching and bending vibration, respectively. 26 The bands at 2970 and 2920 cm −1 are attributed to the asymmetric stretching vibration of C−C in the alkyl chain, while the bands at 2856 and 1390 cm −1 are attributed to the symmetric stretching and bending mode, respectively, of the same group.…”
Section: ■ Results and Discussionmentioning
confidence: 99%
“…In the course of a general program aimed at the study of natural clay minerals and their applications (Bouna et al, 2010(Bouna et al, , 2011Mbaye et al, 2012), this paper reports the characteristics and properties of a natural clay from the Mako area in the southeastern part of Senegal. The clay fraction and organically modified derivatives were also investigated.…”
mentioning
confidence: 99%
“…However, an obvious increase in the relative intensities of the absorption in the OH stretching region of organoclays between 3696 cm −1 -3425 cm −1 can be observed. The weak and sharp bands at 3696 cm −1 and 3420 cm −1 were assigned to the stretching vibrations of the surface and inner hydroxyl groups in kaolinite, respectively [48][49][50][51]. The former of two poorly resolved bands at 3530 cm −1 was assigned to the structural OH−stretching mode in largely disordered glauconite, while the later one at 3425 cm −1 was attributed to the OH−stretching of the interlayer and adsorbed water [49,50].…”
Section: Ft-ir Measurementsmentioning
confidence: 99%