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Quantitavive analysis and FT-IR study of clay raw materials and thermal treated bricks

Juan A. G Carrió 1Izabela C A. Dutra 1Mauro C. Terence 1Rosane Toledo 2Denise R. Santos 2Edmar V. Mota 2

1. Presbyterian University Mackenzie (UPM), Rua da Consolação 930, Sao Paulo 01302-907, Brazil
2. Universidade Estadual do Norte Fluminense Darcy Ribeiro (UENF), Ave. Alberto Lamego 2000, Campos do Goytacazes 28013-600, Brazil

Abstract

In this work we present results on the structutural properties of clay deposits localized in northern Rio de Janeiro sate in Brazil, where this kind of soil is abundant and used for production of ceramics, maily brics and roof tiles. The soil samples were dried, grounded and passed through a sieve with nominal aperture of 840 μm. The resulting homogeneus powder was very representative of the natural soil, which presents 95% particles with grain sizes below 50 μm. This powder was extruded in order to obtain bricks with average dimensions of 100 X 20 X 10 mm. The bricks were dried in air at room temperature during one week and subsequently at 110 oC during 24 hours. Thereafter the bricks were submitted to a slow firing process in a furnace of high heat capacity. The temperature was slowly raised up to 600 oC and kept constant during 60 minutes in order to avoid cracks owing to a quartz phase transition that occurs at 575 oC. Then the temperature was increased to a firing temperature Tf, and kept at this value during 180 min. Subsequently the sample was cooled at a controlled rate of 1.5 oC/min. Similar procedures were applied for preparing bricks with Tf = 300, 400, 500, 600, 700, 800, 900, 950, 1000, 1050, 1100 and 1200 oC. Powder difraction data were collectes from the treated brick with a conventional diffractometer Seifert URD65. The experimental conditions were 3o ≤ 2θ ≤ 75o,  Δ2θ = 0,02o and counting time 3 s. A granulometric study of untreated samples was performed and alowed a quantitative analyse of three different fractions by the Rietveld method using the refinement program GSAS. Samples from differents soil depths treated at 1200 oC were also quantitatively analyzed and showed small differents in their compositions of cristobalite, mullite and hematite. The effect of the thermal treatment in the clay structural properties was also analyzed by FT-IR spectroscopy. In the IR region of 780 cm-1 to 1010 cm-1 were detected different peaks of silicates in dependence of the temperature Tf.

References:

1. Toledo R., Dos Santos D.R., Faria Júnior, R.T., Carrio J.G., Auler L.T., Vargas H.. Gas release during clay firing and evolution of the ceramic poperties. Appl. Clay Sci., Amsterdam, 27, 3-4, 151-157, 2004. 

2. Dos Santos D.R., Toledo R., Faria Júnior, R.T., Carrio J.G., Silva M.C., Auler L.T., Vargas H., Evolved gas analysis of clay materials. Rev. Sci. Instrum., Melville, 74, 1, 663-666, 2003.

3. A.C. Larson, R.B. Von Dreele, Los Alamos National Laboratory. Los Alamos, EUA. Copyright, 1985–2000, The Regents of the University of California, 2001.

Acknowledgments: Mackpesquisa, CAPES, FAPERJ

 

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Related papers

Presentation: Poster at 11th European Powder Diffraction Conference, Poster session, by Juan A. G Carrió
See On-line Journal of 11th European Powder Diffraction Conference

Submitted: 2008-04-29 21:07
Revised:   2009-06-07 00:48