2006
DOI: 10.1134/s0036024406070132
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A Mössbauer spectroscopy study of the transformation of iron compounds in clay materials

Abstract: Palabras Clave: Activación térmica de arcillas, Material cementante suplementario, Geología de arcillas, Atmósfera y temperatura de calcinación, Desempeño de arcillas en morteros, Machine learning, Analítica de datos, Random forest, Big data.

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Cited by 6 publications
(6 citation statements)
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“…Their presence could not be determined by XRD in our nano-/microscale separate, because the sample was purposely chosen in such a way that it visually exhibited as small amounts as possible of such contamination. However, their presence cannot also be excluded and could be correlated to the high Fe contents found from the SEM-EDX measurements, beside the Fe substitute in montmorillonite [62].…”
Section: Summary Discussionmentioning
confidence: 99%
“…Their presence could not be determined by XRD in our nano-/microscale separate, because the sample was purposely chosen in such a way that it visually exhibited as small amounts as possible of such contamination. However, their presence cannot also be excluded and could be correlated to the high Fe contents found from the SEM-EDX measurements, beside the Fe substitute in montmorillonite [62].…”
Section: Summary Discussionmentioning
confidence: 99%
“…Clay materials can contain up to 15 wt. % of iron oxide phases, and contents above 5% Fe 2 O 3 promote a reddish or pinkish colour of raw and calcined clays [121][122][123]. Cement producers may avoid selling cement with a colour different from the traditional grey, mainly for marketing purposes [95,120].…”
Section: Colour Controlmentioning
confidence: 99%
“…Iron oxide is the primary colorant in the clay materials. Most clay materials contain more than 5% Fe 2 O 3 , mainly as impurities which strongly influence the reddish color of clays [15,16]. This can affect their industrial application, in fine ceramic, paper, pigment industries, and civil construction [18].…”
Section: The Role Of Iron In Claysmentioning
confidence: 99%
“…In a low oxygen environment, hematite is reduced to form magnetite, which can be stable even at temperatures close to 300 °C [27][28][29] (see Fig. 1) For temperatures above 650°C, regardless the presence of oxygen, the main iron phase formed is magnetite [16,22,28,30].…”
Section: Color Control During Clay Calcinationmentioning
confidence: 99%
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