Mining Wastes of an Albite Deposit as Raw Materials for Vitrified Mullite Ceramics

In this work, an examination of mining wastes of an albite deposit in south Spain was carried out using X-ray Fluorescence (XRF), X-ray diffraction (XRD), particle size analysis, thermo-dilatometry and Differential Thermal Analysis (DTA) and Thermogravimetric (TG) analysis, followed by the determina...

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Main Authors: Sánchez-Soto, Pedro J., Garzón, Eduardo, Pérez-Villarejo, Luis, Angelopoulos, George N., Eliche-Quesada, Dolores
Format: info:eu-repo/semantics/article
Language:English
Published: MDPI 2021
Subjects:
Online Access:http://hdl.handle.net/10835/10043
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author Sánchez-Soto, Pedro J.
Garzón, Eduardo
Pérez-Villarejo, Luis
Angelopoulos, George N.
Eliche-Quesada, Dolores
author_facet Sánchez-Soto, Pedro J.
Garzón, Eduardo
Pérez-Villarejo, Luis
Angelopoulos, George N.
Eliche-Quesada, Dolores
author_sort Sánchez-Soto, Pedro J.
collection DSpace
description In this work, an examination of mining wastes of an albite deposit in south Spain was carried out using X-ray Fluorescence (XRF), X-ray diffraction (XRD), particle size analysis, thermo-dilatometry and Differential Thermal Analysis (DTA) and Thermogravimetric (TG) analysis, followed by the determination of the main ceramic properties. The albite content in two selected samples was high (65–40 wt. %), accompanied by quartz (25–40 wt. %) and other minor minerals identified by XRD, mainly kaolinite, in agreement with the high content of silica and alumina determined by XRF. The content of Na2O was in the range 5.44–3.09 wt. %, being associated with albite. The iron content was very low (<0.75 wt. %). The kaolinite content in the waste was estimated from ~8 to 32 wt. %. The particle size analysis indicated values of 11–31 wt. % of particles <63 µm. The ceramic properties of fired samples (1000–1350 °C) showed progressive shrinkage by the thermal effect, with water absorption and open porosity almost at zero at 1200–1250 °C. At 1200 °C, the bulk density reached a maximum value of 2.38 g/cm3. An abrupt change in the phase evolution by XRD was found from 1150 to 1200 °C, with the disappearance of albite by melting in accordance with the predictions of the phase diagram SiO2-Al2O3-Na2O and the system albite-quartz. These fired materials contained as main crystalline phases quartz and mullite. Quartz was present in the raw samples and mullite was formed by decomposition of kaolinite. The observation of mullite forming needle-shape crystals was revealed by Scanning Electron Microscopy (SEM). The formation of fully densified and vitrified mullite materials by firing treatments was demonstrated.
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spelling oai:repositorio.ual.es:10835-100432023-04-12T19:29:41Z Mining Wastes of an Albite Deposit as Raw Materials for Vitrified Mullite Ceramics Sánchez-Soto, Pedro J. Garzón, Eduardo Pérez-Villarejo, Luis Angelopoulos, George N. Eliche-Quesada, Dolores waste mining albite quartz kaolinite mullite vitrified sintering In this work, an examination of mining wastes of an albite deposit in south Spain was carried out using X-ray Fluorescence (XRF), X-ray diffraction (XRD), particle size analysis, thermo-dilatometry and Differential Thermal Analysis (DTA) and Thermogravimetric (TG) analysis, followed by the determination of the main ceramic properties. The albite content in two selected samples was high (65–40 wt. %), accompanied by quartz (25–40 wt. %) and other minor minerals identified by XRD, mainly kaolinite, in agreement with the high content of silica and alumina determined by XRF. The content of Na2O was in the range 5.44–3.09 wt. %, being associated with albite. The iron content was very low (<0.75 wt. %). The kaolinite content in the waste was estimated from ~8 to 32 wt. %. The particle size analysis indicated values of 11–31 wt. % of particles <63 µm. The ceramic properties of fired samples (1000–1350 °C) showed progressive shrinkage by the thermal effect, with water absorption and open porosity almost at zero at 1200–1250 °C. At 1200 °C, the bulk density reached a maximum value of 2.38 g/cm3. An abrupt change in the phase evolution by XRD was found from 1150 to 1200 °C, with the disappearance of albite by melting in accordance with the predictions of the phase diagram SiO2-Al2O3-Na2O and the system albite-quartz. These fired materials contained as main crystalline phases quartz and mullite. Quartz was present in the raw samples and mullite was formed by decomposition of kaolinite. The observation of mullite forming needle-shape crystals was revealed by Scanning Electron Microscopy (SEM). The formation of fully densified and vitrified mullite materials by firing treatments was demonstrated. 2021-03-04T08:23:13Z 2021-03-04T08:23:13Z 2021-02-25 info:eu-repo/semantics/article 2075-163X http://hdl.handle.net/10835/10043 en https://www.mdpi.com/2075-163X/11/3/232 Attribution-NonCommercial-NoDerivatives 4.0 Internacional http://creativecommons.org/licenses/by-nc-nd/4.0/ info:eu-repo/semantics/openAccess MDPI
spellingShingle waste mining
albite
quartz
kaolinite
mullite
vitrified
sintering
Sánchez-Soto, Pedro J.
Garzón, Eduardo
Pérez-Villarejo, Luis
Angelopoulos, George N.
Eliche-Quesada, Dolores
Mining Wastes of an Albite Deposit as Raw Materials for Vitrified Mullite Ceramics
title Mining Wastes of an Albite Deposit as Raw Materials for Vitrified Mullite Ceramics
title_full Mining Wastes of an Albite Deposit as Raw Materials for Vitrified Mullite Ceramics
title_fullStr Mining Wastes of an Albite Deposit as Raw Materials for Vitrified Mullite Ceramics
title_full_unstemmed Mining Wastes of an Albite Deposit as Raw Materials for Vitrified Mullite Ceramics
title_short Mining Wastes of an Albite Deposit as Raw Materials for Vitrified Mullite Ceramics
title_sort mining wastes of an albite deposit as raw materials for vitrified mullite ceramics
topic waste mining
albite
quartz
kaolinite
mullite
vitrified
sintering
url http://hdl.handle.net/10835/10043
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