3.1. Chemical Analysis, Mineralogical Phases and Particle Size Distribution
Each residue used in this study was characterized to confirm the function it can perform in the compositions of the newly designed geopolymer mortars.
Table 1 shows that the SiO
2 and Al
2O
3 contents detected in the RCF and RCG were 52.5 wt% and 53.5 wt%, respectively. For geopolymeric systems to function, SiO
2 and Al
2O
3 must be present as they tend to form aluminosilicates, which significantly impact the mechanical and microstructural properties [
29,
30]. As expected, SiO
2, Al
2O
3, Fe
2O
3 and CaO contents were detected in the RG. The presence of Fe
2O
3 and CaO contents is related to the chemical composition of the granite, as well as the addition of grit and calcium oxide, which are often used as a lubricant and abrasive in the industrial process of cutting/sawing this material [
31]. SiO
2 and Al
2O
3 values in the RG were 49.4 wt% and 18.5 wt%, respectively.
The mineralogical analysis of the RCF, RCG and RG is shown in
Figure 1a–c. The mica (JCPDS 83-1808), feldspar (JCPDS 83-1808) and quartz (JCPDS 46-1045) phases were detected in the RG (
Figure 1a), indicating that they come from granitic rocks [
32]. The calcite (JCPDS 47-1743) and dolomite (JCPDS: 89-5862) phases were also detected in the RG and are related to the limestone used as a lubricant and alkalinizer of the environment during the sawing process. Mica, kaolinite (JCPDS 78-2110) and quartz were the mineralogical phases identified in RCF and RCGs; see
Figure 1b,c. The presence of the kaolinite phase (Si
2O
5Al
2(OH)
4) is essential for the geopolymerization reaction since it can be a source of metakaolin (Si
2O
5Al
2O
2) through a dehydroxylation reaction (Si
2O
5Al
2(OH)
4 → Si
2O
5Al
2O
2 + 2H
2O) [
33]. Therefore, to form metakaolin, the RCF was calcined at 650 °C for 2 h. This new calcined material was called fine calcined kaolin waste (RCFC). As expected, the diffractogram of the RCFC (
Figure 1d) is characteristic of an amorphous material and kaolinite peaks were not detected, indicating the efficiency of calcination. The presence of amorphous metakaolin favors pozzolanic activity in mortars with the potential to influence the decrease in porosity and increase mechanical strength and durability [
34,
35,
36].
The following experimental results were obtained considering RCFC since this would be the source of metakaolin for the mortar compositions investigated in this work. Particle size distribution curves (cumulative and frequency) of RCFC, RCG and RG are shown in
Figure 2a,
Figure 2b and
Figure 2c, respectively. The RCFC presented a bimodal frequency curve with all particles with sizes smaller than 12.3 µm, with D
90 = 12.3 µm, D
50 = 3.3 µm and D
10 = 0.8 µm. The RCG also showed a bimodal frequency curve with particles smaller than 48.2 µm, with D
90 = 48.2 µm, D
50 = 10.3 µm and D
10 = 1.2 µm. The RG showed particle sizes smaller than 28.7 µm, with D
90, D
50 and D
10 equal to 28.7 µm, 7.9 µm and 1.1 µm, respectively. Comparatively, RCG and RG showed a wider curve profile, with more considerable variation in particle size than RCFCs.
Table 4 shows the percentage of accumulated mass for different particle size ranges and their respective mean diameters for RCFC, RCG and RG. Approximately 32% of the RCFC particles were smaller than 2 μm, while the RCG and RG were only 17.8% and 19.1%, respectively. The fraction of particles of the RCFC comprising sizes between 2 µm and 20 µm was 66.2%, while for the RCG and RG, they were 44.0% and 62.0%, respectively. The RG had the highest fraction of particles with sizes above 20 µm, followed by the RG (18.9%) and RCFC (2.2%). The identification of the metakaolin in the RCFC (see
Figure 1d), plus the relatively fine granulometry, justifies the use of this residue as a precursor of the geopolymer reaction. On the other hand, the use of RCG and RG as an aggregate is primarily justified by their relatively larger granulometry.
3.2. Design of Mortar Compositions Containing RCFC, RCG and RG
The water/binder factor (W
exp (%)) necessary for each mortar composition suggested by the experimental design to reach the consistency index (260 mm [
37]) is listed in
Table 5. Mortar composition 1 required more water to achieve the desired consistency index (W
exp = 52.0%). Still, as it only contains RCFC, it is uninteresting in terms of the suggested application of RCFC, RG and RCG. For mortar composition 10, less water was needed to achieve the consistency index. However, the absence of the RCFC in this mixture might have an adverse effect on its mechanical characteristics. In actuality, the function of RCFC is to serve as a source of metakaolin, a substance that aids in the geopolymerization reaction (see
Figure 1d) [
34,
36,
38]. Since all the residues examined in this paper contribute to the mortar composition numbers 4, 5, 6 and 7, they are intriguing from a sustainable perspective. For the consistency index, the W
exp (%) values for mortar compositions 4, 5, 6 and 7 were 35.5%, 32.5%, 35.0%, and 43.0%, respectively. It is feasible to deduce from an investigation of the compositions of mortars 4, 5, 6 and 7 that the values of W
exp% rise with the amount of RCFC residue.
The linear, quadratic, cubic and special cubic mathematical models were adjusted to the experimental data shown in
Table 5. The most representative and predictive mathematical adjustments were chosen based on three criteria: (I) presenting
p-values lower than 0.05, (II) presenting an F
test greater than 5 (F
test > 5) and (III) higher R
2 values.
Table 6 summarizes the results of the mathematical adjustments performed. From the viewpoint of criterion (I), no mathematical adjustment showed
p-values above 0.05. The cubic model was disregarded because it presented an F
test value below 5. Both adjustments performed with the linear, quadratic and special cubic models presented F
test values > 5; however, the special cubic model was considered more representative and predictive because it had a higher R
2 value (0.93). In this sense, Equation (1) represents the dependence on the amount of water necessary for the mortar compositions to reach the consistency index. In this equation, the coefficients a, b and c correspond to the percentages of the RCFC, RG and RCG, respectively. All coefficients were statistically significant at the 95% confidence level.
The 3D response surface plot and its corresponding projection, derived from the mathematical fit using the special cubic model (see Equation (1)), are presented in
Figure 3a,b. The trend observed in
Table 5 was confirmed; mortar compositions with higher proportions of RCFCs required more water to achieve a consistency index of 260 mm. This behavior is attributed to the smaller average particle diameter of RCFC (5.0 µm, as shown in
Table 4) compared to the other residues, resulting in a larger surface area. Generally, mortar compositions containing at least 60% RCFC required over 40% water by volume to reach the desired consistency. Conversely, the lowest water volumes (>35%) were necessary for mortar compositions containing over 65% RG. It is known that higher water content tends to reduce mechanical strength. This introduces an interesting element to the study, as the mortar compositions requiring the highest water content to reach the target consistency are those with a greater RCFC proportion, which is critical for the geopolymerization reaction.
3.3. Influence of Different Curing Conditions on SCS
The influence of curing conditions (A, B, C, D and E; see
Table 3) and alkaline activation (NaOH) on SCS values was evaluated for mortar compositions suggested by the experimental design, see
Table 7.
The linear, quadratic, cubic and special cubic mathematical models were also fitted to the data shown in
Table 8, and the most representative and predictive fits were also chosen according to
p-values below 0.05, F
test values above 5 and higher R
2 values. For some cure conditions (C, D and E), it was not possible to adjust all mathematical models. For cure condition A, the special cubic model was not considered predictive since the
p-value was above 0.05. Considering an F
test > 5 and higher R
2 values, we conclude that the cubic model is more predictive for mortar compositions cured under conditions A and D while the special cubic model is more predictive for mortar compositions cured under conditions B, C and E. The equations describing the most predictive fit for cures A, B, C, D, and E are listed in
Table 9.
The effect of curing conditions on SCS values in mortar compositions containing RCFC, RCG and RG is shown in the 3D response surface plots; see
Figure 4a–e. Such graphs were constructed from the equations shown in
Table 9. From the viewpoint of composition, regardless of the curing conditions used, the highest SCS values were observed for mortars containing higher levels of RCFC. As shown in
Figure 1d, the RCFC is a source of metakaolin, which, due to factors such as a high specific surface, a high chemical reactivity and being a source of aluminosilicate, plays a key role in increasing the geopolymerization reaction kinetics [
29,
30,
39]. From the perspective of curing conditions, the highest SCS values were observed for mortar compositions kept under curing conditions A and B (>7 MPa and >6 MPa, respectively). These curing conditions have, typically, a pre-curing stage of 72 h at room temperature, and only then are they cured for 72 h at different temperatures, that is, 60 °C and 100 °C for curing conditions A and B, respectively. The pre-curing step at room temperature, due to the availability of water, allowed for a more pronounced dissolution of Si
4+ and Al
3+ ions, increasing the Si/Al ratio. The Si/Al ratio is one of the factors that affect the SCS of geopolymers [
40,
41,
42]. Furthermore, water molecules and available OH
- ions are also consumed in the first step of geopolymerization [
43,
44].
Comparatively, mortar compositions cured under conditions C and D (
Figure 4c,d) showed lower SCS values than those maintained under curing conditions A and B (
Figure 4a,b). As commented on before, this occurred due to the absence of a pre-cure step at room temperature, which decreased the concentration of Si
4+ and Al
3+ ions available for the polymerization reaction. Besides that, the fact that the samples were taken directly to the oven at a temperature above room temperature (60 °C and 100 °C for curing conditions C and D, respectively) contributed significantly to the decrease in humidity and, therefore, in the water amount and, thus, the OH
- ions available for the geopolymerization reaction. The lowest SCS values (<1.1 MPa) were measured from mortar compositions cured for 240 h at room temperature (cure E). Here, again, the absence of a curing step above room temperature appears to have significantly influenced the kinetics of the geopolymerization reaction. In fact, in studies [
5,
6,
7,
14,
45,
46], regarding the influence of temperature and curing time on the strength of geopolymers, it was found that curing at room temperature is not feasible due to the long time required for the beginning of the geopolymerization reaction to occur.