2017
DOI: 10.1016/j.jafrearsci.2016.10.007
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Diagnosis of the heating effect on the electrical resistivity of Ouargla (Algeria) dunes sand using XRD patterns and FTIR spectra

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Cited by 10 publications
(6 citation statements)
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“…e., S1, S2, S3, S4, and S5) are shown in Fig.2. They revealed similar characteristic bands mainly in the fingerprint region, where we distinguished characteristic absorption bands of silica at 459, 692, 779, 794, 1080, 1170, and 1878 cm −1 , corresponding to symmetric stretching and bending vibration of Si-O and Si-O-Si bond(Mechri et al 2017;Kumar and Rajkumar 2020). Moreover, double absorption bands at 794 and 779 cm −1 in all the spectra confirmed the presence of α-quartz.…”
mentioning
confidence: 67%
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“…e., S1, S2, S3, S4, and S5) are shown in Fig.2. They revealed similar characteristic bands mainly in the fingerprint region, where we distinguished characteristic absorption bands of silica at 459, 692, 779, 794, 1080, 1170, and 1878 cm −1 , corresponding to symmetric stretching and bending vibration of Si-O and Si-O-Si bond(Mechri et al 2017;Kumar and Rajkumar 2020). Moreover, double absorption bands at 794 and 779 cm −1 in all the spectra confirmed the presence of α-quartz.…”
mentioning
confidence: 67%
“…Those natural materials are not being well exploited because of the lack of sufficient and rigorous studies on the mineralogy, microscopic, and systematic physicochemical characterizations of aeolian sand deposits for their potential use in several applications. Numerous studies have been carried out to valorize the abundantly available aeolian sands from Algeria (Abdelhak et al 2014;Kheloufi et al 2017;Mechri et al 2017;Mahdadi et al 2017;Beddiaf et al 2017;Hassani et al 2019). Moreover, Guettala et al (2010), Mezghiche (2011), andBrahim et al (2017) extensively studied the possibility of using dune sand powder as addition to Portland cement.…”
Section: Introductionmentioning
confidence: 99%
“…Similarly, another study investigated dunes sand in Ouargla, Algeria. The study also demonstrated the FTIR peak identification [ 63 ]. The peaks that match are found in the following frequencies, the wideband between 1100–1250 cm -1 due to the quartz in the dunes sand and the peak at 1607 cm -1 due to gypsum.…”
Section: Resultsmentioning
confidence: 98%
“…The 1607 and 1744 cm -1 is due to carboxylic acid C = O stretch and the broad and strong band were situated at 2900–2800 cm -1 , which is attributed to the C-H aldehyde. Wide bands that are visible at 1100–1250 cm -1 are attributed to the quartz in the sand [ 63 ].…”
Section: Resultsmentioning
confidence: 99%
“…e X-ray diffractograms of the sand before and after adsorption shows almost the same appearance and reveal the existence of several characteristic peaks of quartz and calcite [25,26]. For unsaturated sand, these two elements have a codominance indicated by the major peaks corresponding to the position 2θ, 27.7°and 29.7°, respectively [27][28][29][30][31]. Whereas for saturated sand, quartz predominates over calcite with the appearance of two unidentified peaks at 2θ, 43.41°and 51.08°, which can be attributed to the effluent components of the tannery.…”
Section: X-ray Diffractionmentioning
confidence: 99%