Elsevier

Ceramics International

Volume 40, Issue 4, May 2014, Pages 5129-5136
Ceramics International

Mullitization process of andalusite concentrates – Role of natural inclusions

https://doi.org/10.1016/j.ceramint.2013.10.036Get rights and content

Abstract

In the article the results of investigations into the mullitization process of two andalusite concentrates are presented. XRD, XRF and ICP investigations revealed nearly identical phase and chemical composition of both concentrates. However, the andalusites considerably differ in the rate of the mullitization process. XPS and LM investigations revealed that the factors responsible for mullitization include not only the content of mineral inclusions and grain size distribution but also impurities dispersion and the content of naturally occurring carbon in andalusite grains.

Introduction

Andalusite Al2SiO5 crystallizes in an orthorhombic system in Pnnm space group. It occurs in a form of euhedral, pseudotetragonal columnar crystals, characterized by good fissility, parallel to plane (110) and slightly poorer along plane (100) [1], [2]. Theoretically, its chemical composition contains 62.93% of Al2O3 and 37.07% of SiO2, but in nature it occurs with various impurities, for example carbon-rich andalusite. When carbon is specifically located in a form of a cross visible in the crystal along (001) plane, it is known as chiastolite [3].

The biggest deposits of mined andalusite are metamorphogenic (primary) deposits, related to plutonism. Another extensively exploited type are supergenic (secondary), elluvial and alluvial deposits. The above mentioned types of deposits may differ in their age of mineralization. The term “mineralization” is understood as a process of andalusite formation from rocks which are rich in aluminum and poor in silica, referred to as metapellits, in the conditions of contact metamorphism of igneous intrusions [4].

The interest in andalusite is related to the fact that it is a useful raw material to be applied in the ceramic industry, including high-temperature applications (refractory materials). The usefulness of the mineral in question results mainly from its properties such as low thermal conductivity (the lowest in the group of silimanite minerals) [5], a possibility of using andalusite in a raw state for ceramic mixes, both in fine and coarse fractions, as well as its relatively low price [6], [7], [8]. From the point of view of refractory applications, an extremely important phenomenon is thermally activated transformation of andalusite into mullite. Mullite Al6Si2O13 is a phase characterized by high melting point and good thermo-mechanical properties, resistance to chemical corrosion and thermal shocks [9]. As a formality, it should be added that the mullitization process is accompanied by a release of amorphous phase rich in SiO2 [10]. It is assumed that the process of andalusite mullitization is a diffusion assisted phase transformation with silica dissolution [6], [11]. The andalusite mullitization process was investigated by many authors and in various experiments a high number of results were obtained for the process temperature (1100–1480 °C) [12], [13], [14], [15], [16]. In general, on the basis of literature review, it can be stated that transition temperature and kinetics depend on the grain size distribution and the degree of raw andalusite material purification [15], [17], [18]. Undoubtedly, the type and content of impurities that accompany andalusite are important. Impurities can be related to the genesis of the deposit [19].

It is worth emphasizing that in the analysis of andalusite transition into mullite the attention was focused mainly on the total content of impurities related to mineral inclusions, while the manner of their distribution was ignored. Neither discussed the role of carbon naturally occurring in andalusite grains as a factor which might influence the mullitization process. In this article we would like to discuss both above mentioned issues. In order to do that, we analyzed 2 andalusite concentrates differing considerably in their susceptibility to mullitization but having a very similar chemical composition as well as grain size distribution.

In search of factors that are evidently different for both above quoted andalusites, several experimental techniques were applied: optical light microscopy LM, X-ray fluorescence spectrometry XRF, X-ray diffraction XRD, plasma emission spectrometry ICP and X-ray photoelectron spectroscopy XPS.

The aim of this article is to enrich the discussion on factors which may play a significant role in the process of andalusite phase transformation into mullite, which is of great practical importance.

Section snippets

Investigated andalusite concentrates

Commercial concentrates of andalusite from two separate deposits, differing in their genesis and mineralization age, were used as a research material: the elluvial deposit from the Republic of South Africa, hereinafter referred to as andalusite A, and the autochthonous deposit from France, hereinafter referred to as andalusite B. Admittedly, andalusite A comes from a secondary, elluvial deposit but its primary mineralization is related to igneous granite intrusion of Bushveld complex, which

Characteristics of the raw materials

As mentioned in the introduction, andalusites A and B considerably differ in their susceptibility to mullitization. The results of degree of conversion αB determined at 1350 °C, 1400 °C and 1450 °C are presented in a form of αB=f(t) dependence in Fig. 1. Transformation of andalusite B is evidently slower – lower values αB are reached for the same periods of transformation compared to andalusite A. Kinetic measurements of the mullitization process were carried out for powdered samples with grain

Summary

In the article the results concerning two types of andalusite – andalusite A, originating from the secondary (elluvial) deposit, and andalusite B, from the primary (autochthonous) deposit – have been presented. XRD, XRF and ICP investigations revealed a very similar phase and chemical composition of both samples. However, the andalusites considerably differed in the rate of the mullitization process. A possible explanation of this problem was provided by investigations conducted by XPS and LM.

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