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Development of ceramic floor tile compositions
based on quartzite and granite sludges
P. Torres, R.S. Manjate, S. Quaresma, H.R. Fernandes, J.M.F. Ferreira ∗
Department of Ceramics and Glass Engineering, CICECO, University of Aveiro, 3810-193 Aveiro, Portugal
Received 17 November 2006; received in revised form 15 February 2007; accepted 23 February 2007
Abstract
In the present work, industrial sludges derived from cutting and polishing natural stones (granite and quartzite) were characterised in terms of
particles size distribution, chemical and mineralogical composition, and thermal behaviour and their potential to be incorporated as main components
in red-clay-based stoneware tiles was evaluated. High levels (60–70 wt.%) of incorporation were attempted aiming at designing new formulations
intended to be less expensive and possess better final properties (lower water absorption and higher flexural strength) in comparison to an industrial
reference body used in the production of rustic tiles by extrusion, characterised 8–9% water absorption and a flexural strength of 17–18 MPa.
Extruded rods of different formulations were produced and fired at 1100 ◦ C, 1125 ◦ C, 1150 ◦ C and 1200 ◦ C. The experimental results showed that
all the new formulations performed better with the most significant improvements being obtained with incorporation of granite sludge. Flexural
strength values more than triplicate and water absorption decreased by more than one order of magnitude in comparison to the reference paste.
The new products fulfil the requirements of the ISO 13006 standard, group BIa (porcelain tiles).
© 2007 Elsevier Ltd. All rights reserved.
Keyword: Recycling
1. Introduction
The natural rock extraction and transformation industry represents an important field in world’s economy. Rock production
increased from 1.80 × 106 tonnes/year in the 1920s decade to
81.25 × 106 tonnes/year in 2004 and it is expected to reach
450 × 106 tonnes/year in 2025. During the same period of about
80 years, the world’s production of granite increased from
0.175 × 106 tonnes/year to 33 × 106 tonnes/year.1 According to
2005 statistics,1 Portugal is one the world’s biggest natural rock
producers (10th position, 2.45 × 106 tonnes, 2004) and exporters
(8th position, 1.15 × 106 tonnes, 2004), positioned in the 3rd
position among European countries.
According to INETI report,2 the transformation of the
extracted ornamental rock origins residues produced during
sawing, cutting and polishing processes. In the case of granite
transformation industry, it is estimated about 25% of rejected
material during sawing process and about 15 wt.% during
∗
Corresponding author. Tel.: +351 234 370242; fax: +351 234 425300.
E-mail address: jmf@cv.ua.pt (J.M.F. Ferreira).
cutting and polishing and about 1% during finishing process. According to this report, the transformation process of
granite produces about 0.1 m3 of mud for each ton of processed rock. The transformation industry of industrial rocks,
as quartzite, involving less processing steps, produces about 1%
residues.2
Land filling is the actual main destination for rock residues.
The disposal of inert sludges puts serious environmental and
health concerns, creating necrotic conditions for flora and fauna
while, after drying, fine particles can be deposited in the lungs of
mammals via breath. On the other hand, considering that some
natural raw materials used in traditional ceramic industry derive
from the decomposition of the rocks, a somewhat similar mineralogical composition between both should be expected. This
means that these inexpensive residues can be regarded as good
substitutes for the costly raw materials, therefore preserving
the mineral resources, solving environmental problems, while
lowering the production costs.3
Prior literature reports show that this approach has been
already attempted with different degrees of success in the production of several kinds of building ceramic products. In 1999,
Vieira et al.4 used recovery wastes from primary rock industry
0955-2219/$ – see front matter © 2007 Elsevier Ltd. All rights reserved.
doi:10.1016/j.jeurceramsoc.2007.02.217
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to produce tiles and flooring by pressing and sintering in the
interval 1150–1170 ◦ C obtaining water absorption values lower
than 0.5%. Two years later, Hernandéz-Crespo et al.5 used ash of
municipal solid wastes and two different granite sawing residues
to fabricate porcelainized stoneware showing properties similar to conventional material. Granite and marble industry rejects
were used by Mothé et al.6 and Acchar et al.7 to produce ceramic
material. Monteiro and co-workers8 evaluated the effect of granite powder waste incorporation in a red ceramic body: ceramic
formulations comprising from 0 to 40 wt.% granite waste were
prepared and sintered in an industrial furnace at 970 ◦ C. The
results showed that granite incorporation in red clay formulations can improve extrusion process, facilitate drying stage and
decrease water absorption of final product. In 2005, Menezes
et al.9 studied the incorporation of granite sawing wastes up
to 35% in ceramic bricks and tiles compositions. The results
showed that ceramic compositions with additions of granite
wastes could be used to produce wall and floor tiles, which
after firing at 1200 ◦ C exhibited water absorption values lower
than 3%.
This work is focused on the valorisation of wastes derived
from cut and polishing of ornamental rocks of granite and
quartzite through its incorporation as alternative raw materials in
stoneware formulations for floor and wall tiles production. The
final properties were evaluated through several types of characterization tests in order to choose the best formulations. The
main goal was to achieve a formulation with a residues content as high as possible without sacrificing the final properties
of the products, preferentially with some improvements of its
physical or aesthetical properties10–12 in comparison to a reference commercial paste used by Ceralfa (Oliveira do Bairro,
Portugal) in the production of rustic ceramic tiles by extrusion.
The reference paste, intended to be replaced by a new suitable
formulation, exhibited high water absorption values (8–9%) and
poor bending strength (17–18 MPa).
2. Materials and experimental procedure
The starting raw materials for the new formulations were a red
clay (RC) supplied by Argilacentro (Pombal, Portugal), a granite
sludge (GS) from Incoveca (Viseu, Portugal), and a quartzite
sludge (Qz) supplied by Piçarra & Ribeiro (Aveiro, Portugal).
For comparison purposes, a red paste (CF) being already used
by Ceralfa (Oliveira do Bairro, Portugal) for the production of
rustic floor and wall tiles was also used. The details of the CF
composition were not disclosed, but it included fine red clay rich
in smectites, which make the past sensitive to drying, coarse low
grade clay, and a fraction of milled tiles that were rejected after
firing.
The granite sludge was received as filter-pressing wet cakes
containing about 25% humidity and residues of metallic shot
used in the cutting operation, as well as residual abrasives from
polishing. In order to remove the coarser grains of metallic shot,
the wet sludge was dispersed in water and passed through a sieve
of 500 m. The resultant suspension was kept under agitation
while most of the remaining iron particles were removed by
magnetic bars. The most part of the water of the suspension
was decantated and the remaining part was vaporized in a
ventilated oven at 110 ◦ C. Finally, the dried sludge was disaggregated in a hammers-mill and passed through a 500 m
sieve.
The sludge Qz was received as fine and “clean” material
with about 20% humidity and then dried in a ventilated oven
at 110 ◦ C, milled in a hammers-mill and finally passed through
a 500 m sieve. The clay RC was dried at 70 ◦ C to avoid the rupture of smectites’ structure. After manual removing the organic
impurities of larger dimensions, it was milled and sieved as
described above for the sludges.
The densities of the dried powders were determined by the
water picnometer method. Particle size distribution of the raw
materials was measured using a light scattering instrument
(Coulter LS 230, UK, Fraunhofer optical model). Chemical
composition of the sludge’s was determined through X-Ray
Fluorescence Analysis (X-Ray Spectrometer, PW1400, Philips,
Nederland). The mineralogical characterization and the identification of the crystalline phases was performed through
a X-Ray Diffractometer (XRD, Rigaku GeigerflexD/Mac, C
Series, Cu Ka radiation, Japan) and complemented with Differential (DTA) and Gravimetrical (TG) Thermal Analyses (Labsys
Setaram TG–DTA/DSC, France, heating rate 5◦ /min, 1 atm
flowing N2).
The tested compositions are presented in Table 1. Batches
of ∼6 kg were mixed with water (∼16–19 wt.%) and homogenized using a mixer. The extruded cylinders (Ø ∼10 mm, length
120 mm) were obtained according to industrial standards (laboratory extruder NR Burton on Trent, Rawdon Ltd., Moira, UK),
dried (room temperature – 24 h, 110 ◦ C – 24 h), and fired at
1100 ◦ C, 1125 ◦ C, 1150 ◦ C and 1200 ◦ C.
The bulk density of the fired samples was determined
through the Archimedes’ method with Hg-immersion. Shimadzu
machine (Trapezium 2, Japan, 0.5 mm/min displacement) was
used to perform three-point bending strength evaluation. The
presenting results are the average of more than 10 tested cylinders.
Water absorption was measured according to the ISOstandard 10545-3, i.e. weight gain of dried pellets after
immersion into boiling water for 2 h, cooling for 3 h and sweeping of their surface with a wet towel.13
Finally, the surface fracture of samples was observed by
Scanning Electron Microscopy (SEM, Hitachi S-4100, 25 kV
acceleration voltage, Tokyo, Japan).
Table 1
Tested compositions (in wt.%)
Compositions
RC
CF
RC
1
2
3
4
5
6
7
100
30
35
40
30
35
40
30
Qz
Reference paste
–
70
65
60
–
–
–
35
GS
–
–
–
–
70
65
60
35
Please cite this article in press as: Torres, P. et al., Development of ceramic floor tile compositions based on quartzite and granite sludges, J.
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3
3. Results and discussion
Table 2
Mineral phases
3.1. Characterization of raw materials
Compositions
Mineral phases
RC
GS
Qz
Quartz, kaolinite, muscovite
Quartz, kaolinite, illite, muscovite, microcline, albite, calcite
Quartz, muscovite, clinochlore, microcline
The starting raw materials presented the following values of
density: 2.67 g/cm3 for the RC, which is typical for red clays
(2.60–2.70 g/cm3 ) and 2.77 g/cm3 and 2.70 g/cm3 , for granite
and quartzite sludges, respectively.
Fig. 1(a) and (b) shows, respectively, the differential and
cumulative particle size distributions of RC, GS and Qz, after
having passed through a 500 m sieve. It can be observed that
100% of the sieved materials have maximum particle sizes
below 100 m. RC clay exhibits particle size values lower than
40 m, which is accompanied by a bimodal Gaussian distribution centred in 11 and 25 m. GS presents a wider particle size
distribution range, with an average particle size of 18 m while
Qz shows a bimodal Gaussian distribution centred in 15 m and
in 70 m. The percentage of clay minerals (particles with sizes
<2 m), is about 21 vol.% for RC, 23 vol.% for Qz and 17 vol.%
for GS. The silt fractions (particles with sizes between 2 and
60 m, are about 79 vol.% for RC, 80 vol.% for Qz and 78 vol.%
for GS. The sand fraction (particles larger than 60 m) is only
presented in GS, in a relatively small amount of about 4 vol.%.
As a reference, it is known that the rustic ceramic stoneware
formulations usually contain particles with maximum size of
around 500 m. Therefore, from the granulometry point of view,
it becomes obvious that these residues can be directly incorporated in stoneware tile formulations, avoiding any kind of
further milling process. This enables to lower the energy costs
associated with milling, permitting simultaneously to reduce the
processing time as well as to save time dispended with equipment
maintenance.
Fig. 1. Particle-size distribution of the raw materials.
Table 2 shows the mineral phases present in raw materials that have been identified by XRD. RC consists mostly
of kaolinite [Al2 Si2 O5 (OH)4 ], quartz [SiO2 ] and muscovite
[KAlSi3 O10 (OH)2 ]; Qz is composed of quartz, muscovite, and
also of clinochlore [(Mg,Fe)6 (Si,Al)4 O10 (OH)8 ] and microcline
[KAlSi3 O8 ], which is feldspar materials. Feldspar minerals are
typical fluxing agents, lowering the temperature required to form
a vitreous phase that promotes densification. In the GS the following crystalline phases could be identified: quartz, kaolinite,
illite, muscovite, feldspatic minerals such as microcline and
albite [Na(AlSi3 O8 )] and, some traces of calcite [CaCO3 ], probably derived from the polishing equipment or from any marble
rock contamination in the cutting industrial unit. All the minerals detected in GS and QZ sludge’s are usually present in the
raw materials employed for the manufacture of the traditional
ceramics, making feasible the incorporation of these sludges in
rustic stoneware products.
The results of thermal analysis (DTA and TG) of the raw
materials tested in this work are shown in Fig. 2(a) and
(b), respectively. The DTA/TG behaviour of RC is typical of
kaolinitic/illitic clays, which is consistent with the presence of
kaolinite and muscovite.14 At about 120 ◦ C, an endothermic
Fig. 2. Thermal analysis curves, DTA (a) and TG (b), of RC, Qz and GS.
Please cite this article in press as: Torres, P. et al., Development of ceramic floor tile compositions based on quartzite and granite sludges, J.
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Table 3
Chemical composition of the raw materials (wt.%)
Oxide
Red clay (RC)
Granite sludge (GS)
Quartzite (Qz)
SiO2
Al2 O3
Fe2 O3
CaO
MgO
Na2 O
K2 O
TiO2
MnO
P2 O5
LoI
60.27
20.11
7.53
0.15
0.76
0.19
2.10
1.14
0.07
0.18
6.40
67.09
13.73
2.26
4.16
0.81
3.50
4.62
0.24
0.04
0.28
3.00
68.48
14.93
4.68
0.11
0.78
0.31
2.94
1.08
0.07
0.21
5.50
peak occurs due to the release of adsorbed water, accompanied
by 2% weight loss. Between 200 ◦ C and 470 ◦ C, there is a weight
loss of 1%, due to the decomposition of organic matter, which
is translated in the DTA curve by a broad exothermic band.
This is then followed by an endothermic peak centred at 520 ◦ C,
attributed to the desidroxhilation of kaolinite, with 4% weight
loss. At 980 ◦ C, an exothermic peak of low intensity corresponding to the mullite nucleation is observed. The total weight loss
of RC clay is about 7%.
The DTA/TG curves of Qz are very similar to those of RC, differing mostly in peaks intensity (lower). The peaks also appear
centred at temperatures that are slightly different. The total
weight loss for this sludge is about 6%. The DTA curves of
Qz and GS show low intensity endothermic peaks at 570 ◦ C,
which are associated to the quartz transformation.15 Besides this
peak, GS also shows a main endothermic peak centred at 740 ◦ C,
which is consistent with the presence of illite–muscovite-like
minerals and calcium carbonate detected by XRD, the decomposition of which originates a weight loss of 1%.14 A low intensity
endothermic band observed in the temperatures range of about
860–900 ◦ C can also be attributed to the calcite decomposition,
while a slight exothermic peak appearing at 975 ◦ C is due to the
nucleation of mullite. The total weight loss of GS sludge is 3%.
The data of chemical composition and loss on ignition of the
raw materials are presented in Table 3. It can be observed that
SiO2 is the predominant oxide, followed by Al2 O3 . GS has a high
total content (10.38%) of fluxing oxides (K2 O + Na2 O + Fe2 O3 ),
being more prone to form larger amounts of a glassy phase upon
sintering. Qz presents a lower total amount (7.93%) of fluxing
oxides, being therefore expected to confer to the pastes a higher
refractoriness in comparison to QS. All the raw materials used
contain appreciable amounts of F2 O3 , and besides its fluxing
role, it also confers to the fired products the characteristic reddish
colour.
Fig. 3. Comparison of water adsorption values and its dependence on sintering
temperature for all the samples presented in Table 1, after firing for 1 h. The
horizontal dashed lines are the limits stipulated for the ISO 13006 standard
groups: (a) BIa, (b) BIb and (c) BIIa.
the glass former oxides (SiO2 or Al2 O3 ) and the modifier oxides
like K2 O and Na2 O (excellent fluxing agents). It is also a function of the ratio between these last ones. The main difference
between these two fluxing agents is that, while K2 O forms eutectics at low temperatures, Na2 O has a more pronounced effect on
decreasing the viscosity.17
Figs. 3–5 present the results of technological properties of the
samples from different formulations as a function of the sintering temperatures. Fig. 3 shows that water absorption decreases
for every composition with the increase of sintering temperature, except for formulations comprising GS (4, 5, 6, and 7)
sintered at 1200 ◦ C, the values of which increase suggesting
over-firing phenomena. It is clear that the samples made of
Fig. 4. Density of the samples after firing at different temperatures for 1 h.
3.2. Technological characterization of the formulated
products
As referred above, the formation a liquid phase during sintering is essential to promote densification. Depending on the liquid
viscosity, it tends to fulfil the cavities of the ceramic body, reducing its porosity.16 The viscosity is a function of the ratio between
Fig. 5. Bending strength of samples sintered at 1150 ◦ C for 1 h. The horizontal
dashed lines are the limits stipulated for the ISO 13006 standard groups: (a) BIa,
(b) BIb and (c) BIIa.
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reference paste are the ones that exhibit the higher water absorption values after firing at the two higher temperatures (1150 ◦ C
and 1200 ◦ C). When sintering is carried out at the two lower temperatures (1100 ◦ C and 1125 ◦ C) at which the quartzite sludge
still behaves mostly like an inert filler, the samples of formulations 1, 2 and 3 exhibit a higher water absorption capacity in
comparison to the reference paste. Fig. 3 also reveals that, except
at the lowest sintering temperature, the samples made of red clay
RC present water absorption values that are systematically lower
in comparison to those of reference paste, suggesting a better
sintering behaviour. The water absorption capacity is a property directly related with the type of microstructure developed
during sintering. It can be therefore regarded as a simple way
to predict the technological properties of the final products. At
1150 ◦ C, the compositions 4, 5, 6 and 7 present water absorption
values corresponding to those of stoneware pressed pavements
classified by the international standard ISO 13006 as belonging
to the group BIa. The accentuated decrease of water absorption
observed with the introduction of GS reflects the effects of its
higher total amount of fluxing agents (Fe2 O3 , K2 O and Na2 O)
contributing to a more extensive formation of liquid phase and to
a significant reduction of porosity. The samples of formulations
1, 2 and 3 sintered at 1200 ◦ C present water absorption values
that permit to classify them according to the ISO 13006 group
BIIa.18
The evolution of the apparent density of each formulation
with sintering temperature is presented in Fig. 4. Apparent density permits to evaluate the sintering status of the material and
anticipates the microstructure of the final product. The apparent
density of the reference paste, clay RC, and of the formulations 1, 2 and 3 tend to systematically increase with sintering
temperature increasing, in good agreement with the observed
water absorption values Fig. 3. On the other hand, formulations
4, 5, 6, and 7 comprising GS reached maximum density values at 1125 ◦ C, followed by a slight decrease at 1150 ◦ C and a
more clear decreasing trend as the sintering temperature further
increased to 1200 ◦ C. Crossing this information with Fig. 3, the
simultaneous decrease of apparent density and water absorption
values observed for formulations comprising GS when sintering temperature increases from 1125 ◦ C to 1150 ◦ C, can suggest
contradictory results. However, these results can be explained
by the formation of closed porosity that turns samples impermeable to water, contributing for the decrease of water absorption
values. Moreover, some phases with lower density such as mullite and glassy phase can occur at 1150 ◦ C, contributing to the
decrease of apparent density values. At 1200 ◦ C, the significant
decrease of density is mainly the result of over-firing phenomena.
Fig. 5 compares the results of three-point bending strength
of all the samples sintered at 1150 ◦ C. It is interesting to note
that the reference paste CF is the one that presents the lowest
values of mechanical properties. The measured data of water
absorption and flexural strength are in close agreement to the
results indicated by the supplier, but do not fit even the less
demanding standard BIIa ISO 13006 for stoneware products (see
Figs. 3 and 5). A slight apparent decreasing trend is observed
among the formulations 1–3 containing Qz sludge. This
5
Fig. 6. XRD spectra of formulation 2 before and after firing at different temperatures for 1 h.
decreasing trend was not expected since the RC weight ratio
increases from 30 to 40% from the formulation 1 to 3, although
it shows some consistence with the measured values of water
absorption. The formulations containing GS (4, 5, 6, and 7) are
significantly stronger in comparison to the other compositions.
The measured values are well above the minimum values stipulated for group BIa of the ISO standard 13006, which is directed
to the porcelain tiles made by dry-powder pressing, whereby
water absorption must be less than 0.5% and three point bend-
Fig. 7. XRD spectra of formulation 5 before and after firing at different temperatures for 1 h.
Fig. 8. XRD spectra of formulation 7 before and after firing at different temperatures for 1 h.
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Fig. 9. SEM photomicrographs of fracture surfaces of samples of formulation 2 sintered at different temperatures: (a) 1100 ◦ C; (b) 1150 ◦ C; (c) 1200 ◦ C.
Fig. 10. SEM photomicrographs of fracture surfaces of samples of formulations 5 and 7 sintered at the three different indicated temperatures of 1100 ◦ C, 1125 ◦ C,
and 1150 ◦ C.
ing strength higher than 35 MPa.18 Moreover, a clear increasing
trend is observed with the RC weight ratio increasing from 30%
to 40% (formulations 4, 5, and 6), as expected. The replacement
of half of the GS in the formulation 4 by an equivalent amount
of Qz sludge (formulation 7) resulted in a decrease of flexural strength of about 7% and an increase of water absorption.
Therefore, it is possible to conclude that the results of mechanical properties are in accordance with the values obtained for
water absorption and density, showing that formulations comprising granite sludge present higher mechanical resistance and
the corresponding lower water absorption and higher density
values.
Figs. 6–8 present the X-ray spectra of the compositions 2, 5
and 7 before and after sintering at 1000 ◦ C, 1150 ◦ C and 1200 ◦ C.
It can be observed that kaolinite and muscovite existing in the
green bodies disappeared after firing at 1100 ◦ C, while mullite
and hematite appeared as new crystalline phases. The intensity
of the peaks corresponding to the fluxing minerals (microcline
and albite) tends to diminish as the temperature increases, while
quartz is gradually dissolved in the vitreous phase. As expected,
the intensity of the quartz peaks is stronger in the formulations 2
and 7, more refractory and richer in Qz sludge. Fig. 9 shows SEM
images of fracture surfaces of samples of formulation 2 sintering at 1000 ◦ C, 1150 ◦ C and 1200 ◦ C, while Fig. 10 shows SEM
images of fracture surfaces of samples of formulations 5 and 7
sintering at 1000 ◦ C, 1125 ◦ C and 1150 ◦ C. For all compositions
tested, a porosity reduction as sintering temperature increases is
clearly observed, which is associated with the increased amount
of the vitreous phase and the concomitant densification process.
The densification process occurs at higher temperatures in the
case of composition 2, and at lower temperatures in the case
of composition 5, with composition 7 showing an intermediate behaviour, as expected. The morphology of the pores is still
irregular at 1100 ◦ C and then evolves to a spherical shape as sintering temperature increases. Spherical pores are usually formed
in matrices rich in a vitreous phase. These results suggest that
the amount of liquid phase formed within the temperature range
of 1125–1150 ◦ C shall be enough to promote a good level of
densification, especially in the case of compositions containing granite sludge. This hypothesis is supported by the water
absorption results (Fig. 3) and apparent density (Fig. 4).
4. Conclusions
The results presented and discussed along this report enable
the following conclusions to be drawn:
1. As has been postulated, the inexpensive granite and quartzite
sludges proved to be good substitutes for costly raw materials,
therefore preserving the mineral resources, solving environmental problems, while lowering the production costs.
2. Being constituted mainly by very thin particles (φ < 100 m),
these residues can be directly incorporated in industrial
compositions, avoiding energy costs related with milling processes, as well as with the maintenance and erosion of the
milling equipment.
3. This work proves that much better final properties of the
ceramic body could be achieved with simple formulations
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involving just 30–40 wt.% of a plastic clay of suitable chemical and mineralogical compositions and 70–60 wt.% of one
of the tested sludges or their mixtures, and that depositing
this kind of residues in landfill is a big environmental and
economic mistake.
4. Granite sludge has a high content of total fluxing oxides
that favour the maturation of the ceramic body at lower
sintering temperatures, being a good substitute for feldspar
in stoneware tile products that satisfy the most demanding
requirements of the group BIa of the ISO 13006 standard.
5. The incorporation of quartzite residues allows to obtain semiporous ceramic bodies with water absorption values between
3.5% and 4.7%, within the range BII (3–6%) of the standard
ISO 13006.
6. A combination of granite and quartzite residues enables to
obtain ceramic stoneware bodies satisfying the requirements
of the group BIb of the ISO 13006 standard.
Acknowledgement
The financial support of CICECO is grateful acknowledged.
References
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Please cite this article in press as: Torres, P. et al., Development of ceramic floor tile compositions based on quartzite and granite sludges, J.
Eur. Ceram. Soc. (2007), doi:10.1016/j.jeurceramsoc.2007.02.217