Abstract

The present work reports the effect of carbonate addition to iron rich kaolinite on the phase transformation during firing. Mineralogical, thermal (including DTA-TGA and dilatometric) and physico-mechanical analyses were performed on fired product made from a mixture of kaolinite and 8% by mass of dolomite. The firing temperatures used are 920°C, 1050°C, 1150°C, 1200°C and 1250°C. The major mineral phases formed during firing are mullite, cristobalite and hematite associated to gehlenite and anorthite at temperature >1150°C. Their presence induces increased densification of the product that results in an increased in the flexural strength up to 1150°C. Beyond this temperature, increase glassy phase formation together with hematite development, induce a decrease of the flexural strength as well as the porosity and water adsorption. The SEM observations show that primary mullite is formed as from 1150°C. The EDS analysis from SEM is coherent with the chemical and the mineralogical analyses from XRD. The overall analyses indicate that the addition of dolomite at 8% by mass is favorable to vitreous ceramic formation as from 1050°C.

Highlights

  • A mineral material, upon thermal treatment, undergoes chemical and structural modification

  • The overall analyses indicate that the addition of dolomite at 8% by mass is favorable to vitreous ceramic formation as from 1050 ̊C

  • This study evaluates the influence of carbonate addition to kaolinitic clay from Bimbo in the elaboration of fired products

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Summary

Introduction

A mineral material, upon thermal treatment, undergoes chemical and structural modification. These mineralogical transformations are influenced by the chemical composition, the initial mineralogical composition; the particles size, the firing temperature, the heating rate and the soaking time [1] [2] [3]. The phase transformation of clay containing calcite is subject of many reported studies [4]-[9]. For clayey material with low iron impurities (Fe < 5%), about 50% SiO2, 15% Al2O3 and 10% carbonate, the new phases formed are gehlénite, wollastonite, anorthite, cordierite, larnite, périclase, akermamite, forstérite, spinell and monticellite

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