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 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.


Introduction
Mullite is an aluminosilicate with the nominal composition 3Al 2 O 3 ·2SiO 2 (72 wt. % Al 2 O 3 and 28 wt. % SiO 2 ), one of the most common crystalline phases in ceramics [1][2][3][4][5][6]. It is the only stable crystalline phase in the binary Al 2 O 3 -SiO 2 system with a high melting point (1830 • C) at normal pressure [1,2]. High-mullite content materials show excellent properties, such as good chemical and thermal stability, stability in oxidative atmospheres, high-temperature strength, creep resistance, high resistance to thermal shock, low density (3.17 g/cm 3 ), low expansion coefficient (~4.5 × 10 −6 K −1 ), very high transmittance in the mid-Infrared range and retention of mechanical properties at elevated temperatures. Consequently, due to their outstanding properties, they are important as structural advanced materials for high-temperature engineering applications, being one of the most important refractory ceramic materials, as well as electronical, catalytical (substrate) and In the present work, a large deposit of albite sands in south Spain produced by alteration from intrusive rocks is considered [57]. It has been observed that the mining wastes of this deposit are concentrated under the storage in air of the raw materials. These solid wastes can be considered a product collected after washing the albite sands under the effects of rainwater. They contain a fine fraction of the raw materials which is discharged. The objectives of this work are to study these wastes and to investigate the firing properties and the formation of mullite. It should be noted that this kind of waste has been not studied until now. Therefore, it could be of interest for the valorization of these wastes as ceramic raw materials.

Materials and Methods
An in situ examination of several samples of this albite deposit was performed. The selection was based on the residue after wet sieving using a 0.063 mm sieve and 100 g of each sample. The sample name was assigned as follows: F for feldspar; Na for the chemical symbol of sodium (sodium feldspar, albite); the number, 1, 2, etc., indicates the number of samples studied; and B is for basic examination.
After a previous wet sieving, FNa-1B was a sample without residue using the 0.063 mm sieve. A second sample, FNa-2B, was a sample with an estimation of residue of 3 wt. %. Sample FNa-3B was a sample with a higher amount of residue, after wet sieving, with an estimation of~10 wt. %. Sample FNa-4B was a sample with the highest amount of residue after wet sieving, with an estimation of~30 wt. %. Finally, the sample designated FNa-5B was a sample with~10 wt. % of residue after wet sieving, similar to sample FNa-3B, but the visual examination indicated that iron oxides were present at a high relative proportion. Therefore, it was discarded. This simple screening procedure was of great interest to select only two samples for further examination and characterization at the laboratory: FNa-3B and FNa-4B. Then, when fractions were obtained using several sieves at the laboratory, the capital letter "B" was changed to "M" to indicate "Mullite precursor". Two samples were obtained by wet sieving under 0.063 mm: FNa-3M and FNa-4M. They were wet sieved in batches of 1 kg each to pass 63 µm and the resultant wet powders were air dried overnight and dried at 110 • C for 24 h (samples designated FNa-3M and FNa-4M).
The chemical analysis of all the samples was performed by X-ray fluorescence analysis (XRF) using ground powders prepared as pressed pellets using boric acid. The equipment was a Siemens SRS-3000 (Siemens AG, Munich, Germany) sequential XRF spectrometer with an Rh standard X-ray tube.
The mineralogical analysis of the samples was performed by X-ray powder diffraction (XRD). Samples were ground in an agate mortar. They were scanned in random preparations using an X-ray diffractometer, Siemens, D-501 model (Siemens AG, Munich, Germany), at 40 kV and 20 mA, with Ni-filtered CuKα radiation and a graphite monochromator. The mineralogical composition of the samples was determined using the methods proposed by Schultz [58] and Biscaye [59]. These methods were applied in previous investigations by several authors [60][61][62][63][64]. From the X-ray diagnostic peaks of each crystalline mineral phase, the peak areas were measured. Several sources of errors that influence the shape of XRD diagrams, for instance, the orientation of layer silicates, the background and grinding of the samples, were avoided. The error expected in this estimation was ±5% according to the X-ray profile selected for the determination. Mineral phases at a low relative proportion were indicated as <5 %.
Particle size distribution of the samples after wet sieving was determined by sedimentation based on Stokes' law using the method of Andreasen following the experimental set up of the Spanish group of kaolins [65].
Test bars were prepared in a plaster of Paris molds. Dextrin (5 wt. %) was mixed with the samples to increase the plasticity of the powders as an additive to prepare these bars. After drying at 110 • C in an oven, the green test bars were subjected to dilatometric analysis using a Malkin BCRA (Malkin and Company Ltd., Stoke-on-Trent, UK) dilatometer in air, at a heating rate of 6 • C/min. After firing at 1000 • C for 1 min, test bars were also subjected to further dilatometric analysis. Differential thermal analysis (DTA) and thermogravimetric (TG) analysis were carried out simultaneously using a Rigaku Thermal Analyzer, PTC-10A model (Rigaku Corporation, Tokyo, Japan), with the data processor DPS-1. Ground samples (40 mg) using an agate mortar were packed in a platinum crucible and thermally treated in flowing air from 20 to 1200 • C (Pt/Pt-Rh 13% thermocouples) at a heating rate of 12 • C·min −1 .Cylindrical pellets for determination of ceramic properties were prepared by uniaxial dry pressing of the powders using~5 wt. % of distilled water, at 40 MPa. The pellets were air dried for 4 h and then treated at 60 • C for 4 h using an oven. They were heated in air to selected temperatures, in the range 1000-1350 • C at 50 • C intervals, with 2 h of soaking time, and then furnace cooled. An electric laboratory furnace with SiC heating elements was used at a heating rate of 6 • C/min. Linear firing shrinkage was obtained by measuring the length of the samples before and after the firing treatments using a caliper with a precision of ±0.01 mm. The weight loss after firing (%) was determined as the mass loss between drying at 110 • C and firing at several temperatures. Water absorption, bulk density and apparent or open porosity of the heated cylindrical pellets were measured by the Archimedes immersion technique, using distilled water, saturation for 24 h and boiling in distilled water for 2 h. All the measurements were performed in triplicate. A portion of the heated samples was also ground and examined by XRD.
Microstructures of the fired samples at 1200 • C were examined on fresh fractures by scanning electron microscopy (SEM) after coating with a thin layer of gold by sputtering. The equipment was a JEOL microscope, model JSM-5400 (JEOL Ltd., Tokyo, Japan). The samples were examined after previous etching for 10 min in 20% HF aqueous solution. Table 1 shows the chemical analysis by XRF of the raw samples (FNa-3B and FNa-4B) and samples wet sieved to pass 63 µm (FNa-3M and FNa-4B). All these samples present a high content of SiO 2 (>60 wt. %), associated with the albite present and possible quartz, being in the range 62.0-72.5 wt. %. The Al 2 O 3 content is medium, being in the range 18.7-25.1 wt. %, and associated with combined silicates. The content of Na 2 O must correspond to albite present in the samples, with variable content in the range 3.09-5.44 wt. %. The rest of the elements are not relevant. The iron content in the samples is relatively low, with a minimum value of 0.37 wt. % in the sample FNa-4M and a maximum value in the sample FNa-3B. Finally, it should be noted that the values of weight loss after heating at 1000 • C (named "loss on ignition" = LOI) are in the range 1.08-4.45 wt. %. This is an indication of other mineralogical components present in the samples, besides albite and quartz. Both of these minerals do not present any weight loss after heating when they are pure [53]. Then, assuming that all the weight loss is associated with kaolinite, an estimation of the kaolinite content is presented in Table 1. This estimation was performed on the basis of the 13.9 mass % of structural water for pure kaolinite [28]. From these results, it can be observed that the sample with the higher kaolinite content is FNa-4M with 32 wt. % of kaolinite, and the lower content (~8 wt. %) is found for sample FNa-3B.   Table 1), relicts of muscovite mica and possibly calcium-sodium feldspars. The kaolinite identified in these samples is of low crystallinity because broad X-ray peaks are observed, in accordance with previous results [57]. It has been verified by XRD that if the albite content increases, the content of quartz decreases. In this sense, some raw materials of the same deposit with a low albite content could be considered as Na feldspar sands. However, it should be noted that the boundary from feldspathic sand to silica sand varies from country to country [49].   Table 1), relicts of muscovite mica and possibly calcium-sodium feldspars. The kaolinite identified in these samples is of low crystallinity because broad X-ray peaks are observed, in accordance with previous results [57]. It has been verified by XRD that if the albite content increases, the content of quartz decreases. In this sense, some raw materials of the same deposit with a low albite content could be considered as Na feldspar sands. However, it should be noted that the boundary from feldspathic sand to silica sand varies from country to country [49].

Particle Size Analysis of Samples by Wet Sieving
The particle size analysis of raw samples and samples by wet sieving (Figure 2a

Particle Size Analysis of Samples by Wet Sieving
The particle size analysis of raw samples and samples by wet sieving (Figure 2a This result is in connection with the presence of variable amounts of kaolinite in the raw albite samples (Figure 1). In fact, as observed in Table 1, the samples FNa-3M and FNa-4M show the higher percentages of LOI, with this result being associated with the presence of kaolinite.
Minerals 2021, 11, 232 6 of 15 this fraction (Figure 2c) indicates percentages of 10-20 wt. % of the fraction lower than 2 µm. This result is in connection with the presence of variable amounts of kaolinite in the raw albite samples (Figure 1). In fact, as observed in Table 1, the samples FNa-3M and FNa-4M show the higher percentages of LOI, with this result being associated with the presence of kaolinite.

Thermal Analysis of Samples
Figures 3 and 4 show the thermal analysis results of selected samples. Figure 3 shows the thermal dilatation curves for both green and fired (1000 • C) samples. The profiles of all the samples are very similar. A continuous linear expansion from room temperature with a change in the slope at 550 to 600 • C associated with the α to β quartz phase transition can be seen in the samples [52][53][54]66]. Above 600 • C, the linear expansion is continued, although the values are lower than at the starting of these run tests. The dilatometry curves for the test bars fired at 1000 • C show the quartz phase transition, being of lower intensity as expected in the case of the fraction <63 µm.

Thermal Analysis of Samples
Figures 3 and 4 show the thermal analysis results of selected samples. Figure 3 shows the thermal dilatation curves for both green and fired (1000 °C) samples. The profiles of all the samples are very similar. A continuous linear expansion from room temperature with a change in the slope at 550 to 600 °C associated with the α to β quartz phase transition can be seen in the samples [52][53][54]66]. Above 600 °C, the linear expansion is continued, although the values are lower than at the starting of these run tests. The dilatometry curves for the test bars fired at 1000 °C show the quartz phase transition, being of lower intensity as expected in the case of the fraction <63 µm.  The above results are in relation to the DTA-TG diagrams (Figure 4). It should be noted that pure albite does not show weight loss by TG and the DTA trace without any  Figures 3 and 4 show the thermal analysis results of selected samples. Figure 3 shows the thermal dilatation curves for both green and fired (1000 °C) samples. The profiles of all the samples are very similar. A continuous linear expansion from room temperature with a change in the slope at 550 to 600 °C associated with the α to β quartz phase transition can be seen in the samples [52][53][54]66]. Above 600 °C, the linear expansion is continued, although the values are lower than at the starting of these run tests. The dilatometry curves for the test bars fired at 1000 °C show the quartz phase transition, being of lower intensity as expected in the case of the fraction <63 µm.  The above results are in relation to the DTA-TG diagrams (Figure 4). It should be noted that pure albite does not show weight loss by TG and the DTA trace without any presence of kaolinite. In fact, this sample contains the higher percentage of kaolinite, as shown Figure 1 and Table 1 (with an estimation of~32 wt. %). The profile is characteristic with a broad endothermic DTA effect at 530 • C, with the main weight loss observed by TG, associated with the dehydroxylation of this silicate with loss of structural OH groups and formation of "metakaolinite" [5,13,[16][17][18][22][23][24][25][26]. There is also a slight change in the slope of the DTA curve at 570 • C associated with the α to β thermal phase transformation of quartz [52,54,66]. This thermal change was more evident by dilatometry (Figure 3).

Thermal Analysis of Samples
There is a small DTA exothermic effect centered at~300 • C. This effect could be associated with the presence of amorphous components, such as allophane or even iron oxy-hydroxide gels. At this point in time, the presence of both components is not clear, and it would need more experimental work. Allophane of the chemical composition Al 2 O 3 (SiO 2 ) x nH 2 O with x = 1.3-2 and n = 2.5-3 is an amorphous component originated by weathering or the hydrothermal alteration product of volcanic glass and feldspars [67,68]. The presence of allophane in this feldspar deposit is possible. Therefore, the "loss on ignition" associated with kaolinite (see Table 1) would be modified to perform the estimation of the kaolinite content. On the other hand, the mass loss determined by TG is small (~0.37 wt. %) when this DTA effect is observed. In a previous paper concerning the characterization of a waste washing solid product of mining granitic tin-bearing sands [46], a similar effect was observed by DTA at 350 • C. It was associated with the presence of amorphous iron oxide gels (Fe 2 O 3 obtained by chemical analysis was 5.13 wt. %). The DTA profile of this solid product was typical of a kaolinitic sample. It should be noted that Romero-Gómez et al. [69] studied the thermal transformation of limonite, a mixture of FeO(OH)nH 2 O and α-FeO(OH) or goethite. When this mineral is heated, a thermal transformation with weight loss is produced at~300 • C, originating Fe 2 O 3 (haematite).
The further decrease in mass loss observed by TG (Figure 4) could be associated with the loss of the last structural OH groups present in kaolinite. They would need higher temperatures to be completely eliminated from the structure of "amorphous metakaolinite" originated by the kaolinite thermal decomposition [13]. Estimation of kaolinite in this sample is~32 wt. % ( Table 1). The total weight loss by TG is 4.55 wt. %, in agreement with the LOI value (4.45 wt. %) presented in Table 1 for this sample.
The characteristic exothermic sharp DTA effect at~970 • C is associated with the decomposition of metakaolinite previously formed by heating [5,13,[16][17][18]26,27,47]. This effect has been attributed to the formation of either mullite nuclei or a transient aluminatype spinel (γ-Al 2 O 3 solid solution) or both because at DTA heating rates, both mullite and spinel have the possibility of forming concurrently [5]. Finally, from 1000 to 1200 • C, a progressive decrease in the DTA endothermal signal can be observed. It is associated with the progressive formation of the liquid phase from the albite present, with a shrinkage effect of the sample by sintering, with diminution of the thermal contact between the sample and crucible. It should be noted that under the dynamic heating conditions (12 • C/min) using the DTA furnace up to 1200 • C and subsequent cooling in the furnace, the product of this treatment appeared sintered. The treated sample was easily separated from the crucible. Table 2 shows the ceramic properties of the fired sample FNa-4M (for sample FNa-3M, they were similar) from 1000 to 1350 • C. The progressive shrinkage of the fired sample up to a value of 10% at 1200 • C can be observed, which then decreased from this temperature. The water absorption changes from 22.80% at 1000 • C to minimum values (0.03-0.07 %) at 1200-1250 • C. The apparent or open porosity follows a similar trend. The bulk density values increase from 1.62 at 1000 • C to a maximum value of 2.38 g/cm 3 at 1200 • C. Linear firing shrinkage and bulk density were maximized by firing the sample at 1200 • C for 2 h. To illustrate this thermal evolution, Figure 5 shows a graphical plot of the variation in linear shrinkage and water absorption, both as a function of the firing temperature. Two parameters are of interest concerning the densification and sintering of the samples if the vitrification or range curves are considered [70], as follows: the vitrification temperature (Tv), or the temperature at which the apparent or open porosity becomes almost zero, and the temperature of the maximum of the apparent density (Td). In this particular case, it is found that Tv = 1200 • C = Td.    in linear shrinkage and water absorption, both as a function of the firing temperature. Two parameters are of interest concerning the densification and sintering of the samples if the vitrification or range curves are considered [70], as follows: the vitrification temperature (Tv), or the temperature at which the apparent or open porosity becomes almost zero, and the temperature of the maximum of the apparent density (Td). In this particular case, it is found that Tv = 1200 °C = Td.   Figure 6 shows the XRD diagrams of the sample FNa-4M after thermal treatments in the range 1000-1200 °C for 2 h. Quartz, albite and the formation of mullite can be detected at 1100 °C, with detection of several characteristic X-ray patterns, which increases in intensity as the firing temperature increases. An abrupt change is observed from 1150 to 1200 °C, with disappearance of all the albite X-ray peaks associated with the melting of this phase. At 1200 °C, quartz and mullite are the crystalline phases present in the fired sample besides the presence of the vitreous phase according to the increased hump of the XRD diagram. This result is in connection with the thermal evolution of the sample presented in Table 2 and Figure 5 and the previous DTA results (Figure 4). In fact, the equilibrium phase diagram SiO2-Al2O3-Na2O [71] indicates that the melting of albite  Figure 6 shows the XRD diagrams of the sample FNa-4M after thermal treatments in the range 1000-1200 • C for 2 h. Quartz, albite and the formation of mullite can be detected at 1100 • C, with detection of several characteristic X-ray patterns, which increases in intensity as the firing temperature increases. An abrupt change is observed from 1150 to 1200 • C, with disappearance of all the albite X-ray peaks associated with the melting of this phase. At 1200 • C, quartz and mullite are the crystalline phases present in the fired sample besides the presence of the vitreous phase according to the increased hump of the XRD diagram. This result is in connection with the thermal evolution of the sample presented in Table 2 and Figure 5 and the previous DTA results (Figure 4). In fact, the equilibrium phase diagram SiO 2 -Al 2 O 3 -Na 2 O [71] indicates that the melting of albite (Na 2 O·Al 2 O 3 ·6SiO 2 ) is at 1118 • C. The melting of Na feldspar was reported in the temperature range 1118-1160 • C [66]. Besides this, the Na feldspar composition of porcelain bodies exhibited the maximum densification at 1171 • C [50] and the eutectic in the system albite-quartz has been found at 1060 • C [72]. Celik [73] reported a melting point of 1170 • C. In the same sense, Martin-Marquez et al. [51] reported a complete melting of feldspars (microcline and albite) used in the preparation of porcelain stoneware at 1200 • C. cording to Dondi [49], the primary function of feldspathic fluxes is to melt during firing, thus providing a liquid phase that is responsible for viscous flow sintering and partial vitrification. It is clear that the presence of the Na-rich phase in the fired samples studied in this paper accelerates the vitrification process due to its fluxing effect. Furthermore, the amorphous silica produced during metakaolinite decomposition, being larger in this sample (kaolinite content ~32 wt. %, see Table 1), can also give rise to a vitreous phase formation. Finally, the SEM observation of the sample FNa-4M fired at 1200 °C ( Figure 7) shows a compacted microstructure with mullite crystals, which originated from kaolinite present in the sample (estimated at an amount of ~32 wt. %, see Table 1), showing needle shapes of small sizes, besides relicts of the glassy phase and quartz crystals, as expected from On the other hand, Bernardo et al. [74] mentioned that alkali feldspar crystals (tectosilicates by the formula M·AlSi 3 O 8 , where M = Na or K, like albite) are known to provide excellent glasses but are unable to crystallize in practical periods of time. However, according to Dondi [49], the primary function of feldspathic fluxes is to melt during firing, thus providing a liquid phase that is responsible for viscous flow sintering and partial vitrification. It is clear that the presence of the Na-rich phase in the fired samples studied in this paper accelerates the vitrification process due to its fluxing effect. Furthermore, the amorphous silica produced during metakaolinite decomposition, being larger in this sample (kaolinite content~32 wt. %, see Table 1), can also give rise to a vitreous phase formation.

XRD and SEM of Fired FNa-4M Sample
Finally, the SEM observation of the sample FNa-4M fired at 1200 • C ( Figure 7) shows a compacted microstructure with mullite crystals, which originated from kaolinite present in the sample (estimated at an amount of~32 wt. %, see Table 1), showing needle shapes of small sizes, besides relicts of the glassy phase and quartz crystals, as expected from previous XRD results ( Figure 6) when albite has disappeared. These findings are in agreement with previous SEM results of the literature concerning studies on vitreous bodies and porcelain stoneware [16,[50][51][52]54]. previous XRD results ( Figure 6) when albite has disappeared. These findings are in agreement with previous SEM results of the literature concerning studies on vitreous bodies and porcelain stoneware [16,[50][51][52]54]. According to all these results, it can be mentioned that the amount of and variations in the wastes are a function of the raw albite with quartz processed at the deposit. At this time, the authors do not have access to any statistical data of production. The proprietary of the deposit has not revealed information concerning the production of albite sands, amount of mining wastes, cost of the mining products and other details. At the beginning, the interest of this research was focused on the finer fraction, where it was assumed that kaolin and kaolinized minerals, precursors of mullite, could be found. Then, the results of particle size analysis ( Figure 2) indicated that variations of 11-31 wt. % in the fraction lower than 63 µm could be obtained. The clay fraction (lower than 2 µm), where kaolin minerals are present, is proportional to these contents, as demonstrated by the results obtained by sedimentation analysis (Figure 2c). The question is, therefore, as follows: why is this process the solution? A first solution was to consider the wastes of albite sand processing as mullite precursors, focusing on the size fractions lower than 63 µm, particularly "the clay fraction". Therefore, the product would be considered of added value as compared to albite and even quartz.
It was already mentioned that this kind of waste from an albite deposit has not been studied until now. The present paper is a preliminary report concerning several samples of this deposit. The formation of mullite was demonstrated in these samples by thermal treatment from 1100 °C ( Figure 6). Furthermore, the microstructure developed by firing the selected fraction of this waste showed mullite crystals with the characteristic needle shape (Figure 7). Taking into account the precedent literature reports as mentioned in the Introduction section, the firing product (1200 °C) could be very interesting for advanced According to all these results, it can be mentioned that the amount of and variations in the wastes are a function of the raw albite with quartz processed at the deposit. At this time, the authors do not have access to any statistical data of production. The proprietary of the deposit has not revealed information concerning the production of albite sands, amount of mining wastes, cost of the mining products and other details. At the beginning, the interest of this research was focused on the finer fraction, where it was assumed that kaolin and kaolinized minerals, precursors of mullite, could be found. Then, the results of particle size analysis ( Figure 2) indicated that variations of 11-31 wt. % in the fraction lower than 63 µm could be obtained. The clay fraction (lower than 2 µm), where kaolin minerals are present, is proportional to these contents, as demonstrated by the results obtained by sedimentation analysis (Figure 2c). The question is, therefore, as follows: why is this process the solution? A first solution was to consider the wastes of albite sand processing as mullite precursors, focusing on the size fractions lower than 63 µm, particularly "the clay fraction". Therefore, the product would be considered of added value as compared to albite and even quartz.
It was already mentioned that this kind of waste from an albite deposit has not been studied until now. The present paper is a preliminary report concerning several samples of this deposit. The formation of mullite was demonstrated in these samples by thermal treatment from 1100 • C ( Figure 6). Furthermore, the microstructure developed by firing the selected fraction of this waste showed mullite crystals with the characteristic needle shape (Figure 7). Taking into account the precedent literature reports as mentioned in the Introduction section, the firing product (1200 • C) could be very interesting for advanced materials based on mullite. However, the content of elements distinct from silica and alumina (3Al 2 O 3 ·2SiO 2 , composition of mullite), as found by XRF analysis (Table 1), favored the formation of the vitreous phase, and besides this, the microstructure contains crystalline quartz. The vitreous phase is responsible for the sintering of the samples at temperatures that are relatively low (1200 • C). Therefore, vitreous mullite ceramic bodies containing quartz, with the above microstructure, were the main finding according to the results of the present report. A future research work, under a contract with the proprietary of the albite deposit, will be performed for a wider and deeper study with new experimental findings and additional results. Consequently, a more complete study will be performed.

Conclusions
In this study, two representative samples of mining wastes of an albite deposit were examined. The content of albite was found by XRD in the range 40-65 wt. %, with 25-40 wt. % of quartz and accessory minerals, mainly kaolinite. The kaolinite content was of interest to produce mullite by firing. The XRD results agree with the high content of silica and alumina determined by XRF, with Na 2 O contents in the range 3.09-5.44 wt. % associated with albite in the samples, variable contents of silica and alumina, low weight loss in the range 1-4.5 wt. % and low iron contents (<1 wt. %).
The particle size analysis by wet sieving indicated: (a) variable percentages of fractions lower than 2000 µm, (b) percentages of 11-31 wt. % in the percentages of particles <63 µm and (c) percentages of 10-20 wt. % of fractions <2 µm. In the finest fractions, kaolinite is concentrated, with an estimated amount of~8-32 wt. %. The dilatometry curves showed the quartz phase transition, with a lower intensity of the profiles in the case of the fraction <63 µm. Thermal analysis by DTA-TG allowed observing the kaolinitic character of this fine fraction, with a progressive effect of liquid formation and sintering mainly associated with the albite present.
The ceramic properties of fired samples (1000-1350 • C) showed progressive shrinkage by the thermal sintering effect, with water absorption and open porosity almost at zero at 1200-1250 • C. Thus, fully densified vitrified materials by firing treatments can be obtained, being characterized by a nice white color because the iron content is very low. At 1200 • C, the apparent density reached a maximum value of 2.38 g/cm 3 . As a result of this behavior, it was found that Tv = 1200 • C = Td. The main change in the phase evolution was observed by XRD from 1150 to 1200 • C, with the disappearance of albite by melting in accordance with previous studies, the predictions of the phase diagram SiO 2 -Al 2 O 3 -Na 2 O and the binary system albite-quartz. The development of mullite crystals was evidenced by XRD. At 1200 • C, quartz and mullite were found in the fired material besides the presence of the vitreous phase, as detected by XRD, and the needle shape of mullite crystals observed by SEM. These findings will be of interest when kaolinite wastes are used for the preparation of vitrified mullite ceramics. Further studies on this subject will be considered taking into account the present results.