2007
DOI: 10.1016/j.ceramint.2006.03.016
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Phase changes of ceramic whiteware slip-casting bodies studied by XRD and FTIR

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Cited by 25 publications
(9 citation statements)
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“…01-089-1471 corresponding to anorthite feldspar or calcium aluminum silicate. These results are consistent with the XRD peak pattern results, as previously reported by Lavat et al 25 The XRD peak patterns of the porcelain clay powder and commercial ceramic hand mold are similar to the XRD peak patterns of stoneware clay powder and stoneware hand mold: mullite or aluminosilicate (Al 2 O 3 .SiO 2 ) and alumina corresponding to the JCPDS file nos. 00-081-0026 and 01-075-1865; silica corresponding Figure 8.…”
Section: Characteristics Of Plaster and Stoneware Hand Moldssupporting
confidence: 92%
“…01-089-1471 corresponding to anorthite feldspar or calcium aluminum silicate. These results are consistent with the XRD peak pattern results, as previously reported by Lavat et al 25 The XRD peak patterns of the porcelain clay powder and commercial ceramic hand mold are similar to the XRD peak patterns of stoneware clay powder and stoneware hand mold: mullite or aluminosilicate (Al 2 O 3 .SiO 2 ) and alumina corresponding to the JCPDS file nos. 00-081-0026 and 01-075-1865; silica corresponding Figure 8.…”
Section: Characteristics Of Plaster and Stoneware Hand Moldssupporting
confidence: 92%
“…18 Illite and muscovite may be characterized by the OH-stretching around 3620 cm -1 , accompanied by the broad absorption at 3400 cm -1 . 16 The peaks in the range 815 and 746 cm -1 indicate the presence of Si-O-Al where Al is in tetrahedral co-ordination supporting the earlier observation of the possible presence of sericite/muscovite minerals. The peaks in the range 539 and 477 cm -1 are due to octahedral AlO 6 sheet vibrations.…”
Section: Characterization Of Pyrophyllitesupporting
confidence: 74%
“…15 The peak at 1120 cm -1 can be assigned to Al-OH vibration. 16 This band is formed by the vibrations of oxygen, common to tetrahedron and octahedron, and the Si-O vibration that is perpendicular to the silicate layers. 17 The peak at 950 cm -1 may be attributed to Al-OH vibrations.…”
Section: Characterization Of Pyrophyllitementioning
confidence: 99%
“…The absorption peaks at 459, 778 and 798 cm -1 correspond to the vibration of non-bridging oxygen (Si-O-). The peaks at 778 and 798 cm -1 correspond also to the vibration of non-bridging oxygen (Si-O-) associated with K + , and the peaks 700, 1081 and 1169 cm -1 correspond to the vibration of bridging oxygen (Si-O-Si) while the peak at 544 cm -1 corresponds to the vibration of (Si-O-Al) for the sample sintered at 1160 °C for 2 h [43][44][45][46]; this peak may belong to the mullite phase. The sharp spitted band corresponding to (Si-O-Si) is a diagnosis to identify quartz.…”
Section: Resultsmentioning
confidence: 99%