Ceramic behaviour of five Chilean clays which can be used in the manufacture of ceramic tile bodies
Introduction
It is well known that industrial clays have a complex mineralogical composition, which makes rather difficult the study of mineral phases present in the raw material. Paste contraction occurs while grains are approaching each other. Each particle in the body is separated by water film at the initial stages of drying (Jeridi et al., 2008). The water film becomes thinner until the “critical point”, at which the rate of drying and shrinkage sharply change (Dondi et al., 2002), and the particles come into contact occupying the open space left by the released water. Shrinkage tends to increase as vacuum volume rises, and this seems to explain partially why shrinkage is lower when pressing load increases (Jeridi et al., 2008). During the firing process a series of transformations occur, which will be decisive to achieve the final properties of the ceramic products (González-García et al., 1990, Jordan et al., 1999). Through the ceramic process, once the crystalline structures of minerals exceed their stability limits, they are partially decomposed while simultaneously others are being formed. The destruction of the pre-existing structure does not occur instantaneously (Jordan et al., 1999). The knowledge of the origin, diagenesis and physicochemical composition of the clays is essential when sketching out suitable compositions required for ceramic production (Sanfeliu and Jordan 2009).
The relationship between the mineralogy of the raw materials and the phase changes taking place during their sintering under different conditions have been examined (Daskshama et al., 1992, Jordan et al., 1999, Jordan et al., 1999). Between 900 and 1000 °C a sintering process takes place, which consists in the aggregate compaction of particles. This process is not complete, so the ceramic tile bodies are still quite porous. Towards 1000 °C the larger pores are seen to increase (between 1 and 10 μm). This phenomenon coincides with the destruction of illites, chlorites and their re-crystallisation into quartz and spinel principally (Jordan et al., 2008).
Ceramics industry in Chile starts between 1950 and 1960 as a result of the optimistic and positive attitude of a country, which has made great effort to implement a small industry located around Santiago de Chile. The continuous improvement of the initial modest facilities using primitive methods of manufacture has been the result of joint efforts of various companies and factories that together implemented new and improved manufacturing techniques. These enabled producing from the clay gres stoneware to the most advanced ceramic products for varied uses.
There is no previous study about these non exploited clay deposits in the region and it is the first time that the applicability of these clays as raw materials for ceramic industry has been tested. The main objective of this paper is the study of the chemical–mineralogical compositions and technological behaviour that allows the evaluation of the applicability of the clay deposits studied.
Section snippets
Materials and methods
Five deposits of Chilean clays which can be used in the formulation of ceramic pastes were selected (Fig. 1). The clays come from San Vicente de Tagua-Tagua (SVTT), Litueche (L) in the VI Region of Chile, and Las Compañías – Río Elqui (LC), La Herradura – Coquimbo (LH) and Monte Patria – Coquimbo (MP) from the IV Region of Chile.
The Tagua-Tagua basin in Chile (VI Region) was studied by Varela, 1976, Nuñez et al., 1994. The Formation “Laguna de Taguatagua” had a lagoon origin and it was form
Mineralogy
The mineralogical compositions of samples differ considerably (Table 1). SVTT bulk samples consisted mainly of albite and quartz, and contain K-feldspars, hematite, kaolinite and chlorite in minor amounts. Illite/muscovite, kaolinite and palygorskite were the dominant phases in SVTT clay fraction. Other components found in lesser quantities in this fraction were quartz and albite.
In LC bulk samples albite, quartz and chlorite were the dominant phases; tremolite, hematites and kaolinite were
Conclusions
All the studied clays seem to be easily adaptable to a correct dry pressing ceramic process. In particular, illite–kaolinite-rich samples (LH) and kaolinite-rich samples (L) show the best ceramic behaviour due to their firing behaviour. In mixtures with samples LH and MP the amount of carbonates should not exceed 10% to avoid excess porosity caused by strong decarbonation reactions. In contrast, samples SVTT are more suitable for the production of fast firing vitreous pieces. L samples present
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