2012
DOI: 10.1590/s1516-14392012005000144
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Zeolite A synthesis employing a brazilian coal ash as the silicon and aluminum source and its applications in adsorption and pigment formulation

Abstract: Zeolite A was synthesized using the coal ash from Siderópolis/RS -Brazil. The synthesis was based on a standard IZA synthesis using coal ash as the Si and Al source. XRF analysis showed that the coal ash has a Si/Al ratio of 1.52, which is close to the Si/Al ratio required to produce zeolite A (1.0). The synthesized materials were analyzed by XRD, SEM and N 2 adsorption. More crystalline materials were obtained during synthesis when an additional treatment was applied at a temperature of 353 K at the dissoluti… Show more

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Cited by 29 publications
(19 citation statements)
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“…XRD results for commercial zeolite samples showed similar patterns as those obtained with the joint committee of powder diffraction standard powder diffraction database file and previous studies (Treacy and Higgins 2007;Teber et al 2010). Peaks typical of zeolite type A were found at 2θ = 7.1°, 10.1°, 22.4°, and 27.1° (Sharma et al 2012;Bieseki et al 2013). XRD results for zeolite type A showed the existence of feldspar in the zeolite structure due to the appearance of XRD peaks at 2θ = 16.2° and 34.3° (Zheng et al 2012).…”
Section: Resultssupporting
confidence: 80%
See 1 more Smart Citation
“…XRD results for commercial zeolite samples showed similar patterns as those obtained with the joint committee of powder diffraction standard powder diffraction database file and previous studies (Treacy and Higgins 2007;Teber et al 2010). Peaks typical of zeolite type A were found at 2θ = 7.1°, 10.1°, 22.4°, and 27.1° (Sharma et al 2012;Bieseki et al 2013). XRD results for zeolite type A showed the existence of feldspar in the zeolite structure due to the appearance of XRD peaks at 2θ = 16.2° and 34.3° (Zheng et al 2012).…”
Section: Resultssupporting
confidence: 80%
“…XRD results for zeolite type A showed the existence of feldspar in the zeolite structure due to the appearance of XRD peaks at 2θ = 16.2° and 34.3° (Zheng et al 2012). The reflections at 2θ = 20.8° and 26.6° in faujasite (Y) and mordenite zeolite showed a large quantity of quartz and a smaller amount of feldspar compared to zeolite type A (Szostak 1998;Mohamed et al 2005;Bieseki et al 2013). High-intensity M-CLZ peaks were found at 2θ = 10.8°, 22.7°, 24.5°, and 30.3°, which correspond to the existence of clinoptilolite zeolite in the sample (Muir et al 2016).…”
Section: Resultsmentioning
confidence: 99%
“…In all samples, typical cubical structure, that may belong to zeolite A or zeolite X, were observed (Figure 6a). 23,55,56 The presence of zeolite X was also observed by XRD analysis ( Figure S1), but in very low levels. For the second zeolite product investigated, SEM images (Figure 6b) illustrate first stage of zeolite Na-P1 formation over a partially activated CFA spheres.…”
Section: Zeolite Characterization Identification and Purity Of Zeolitmentioning
confidence: 79%
“…The low solubility of these minerals in NaOH and likely saturation of the reactive medium with Si and Al explain this behavior. According to Bieseki et al, 42 the original quartz present in the coal ash did not react during zeolite formation. The chemical composition of zeolites Na-P1 and 4A obtained in process A are shown in Figure 3 (also see Table S2).…”
Section: Zeolite Characterizationmentioning
confidence: 94%