Influence of Size Reduction of Fly Ash Particles by Grinding on the Chemical Properties of Geopolymers

Chemical properties of geopolymers were evaluated from the reduction of fly ash particle size by grinding. X-ray diffraction determined that at early curing ages new crystalline phases appear in the matrix of the geopolymer and they remain for 28 days, with increases in intensities up to 60%. In Fourier transform infrared spectroscopy, displacements were identified in the main band of the geopolymers at higher wavenumbers, attributed to the greater rigidity in the structures of the aluminosilicate gel due to the increase of the reaction products in the geopolymers obtained through fly ashsubjected to previous grinding, which is observable in the geopolymers matrix. Results indicate that the reduction of fly ash particle size by grinding has an influence on the chemical properties of geopolymers.


Introduction
Current research by the scientific-technical community looks for alternative solutions to problems related to energy consumption and CO 2 emissions.
Global infrastructure demands require massive concrete and cement production, causing a significant negative environmental impact since its production is responsible for 5-7% of global anthropogenic CO 2 emissions [1][2][3].In addition, Portland cement production releases about 0.8 tons of carbon dioxide for every ton of clinker produced [4].This represents a considerable fraction of total CO 2 emissions.For this reason, it is important to propose alternative solutions with second-generation materials, remains of other productive cycles (waste), which reduce the environmental impact and avoid the use of new reserves.Therefore, the perspective for the future is to allow the adaptation of new materials pertaining to concrete and Portland cement, but from a new perspective of durability, as well as economic and social sustainability.
Fly ash (FA), metakaolin, and silica fume have been used as additions in the cement industries and as pozzolanic materials that improve the physical, chemical, and mechanical properties of concrete [5][6][7][8].In the last years, FA with high silica and aluminum content (Class F, ASTM C618 [9]) has made important advances in the search for new applications [10][11][12].Currently, the annual production of fly ash worldwide is estimated to be around 700 million tons [13,14].These achievements are aimed at the development of binding materials due to their wide range of possible potential applications [15][16][17].Alkaline cements, also called geopolymers, are obtained through a chemical process between fly ash and an alkaline solution at temperatures below 100 • C.This reaction results in the dissolution of reactive phases of aluminosilicates.With the progress of the reaction, water is gradually removed, and the tetrahedral groups of SiO 4 and AlO 4 form the polymeric precursors [18][19][20].
According to various studies, the physicochemical properties of geopolymers depend mainly on the Si/Al, Na/Al ratios and water content [21,22].Often, these ratios are investigated indirectly, for example, by varying the activation ratio and curing conditions [23][24][25].The chemical composition in mass is largely related to the kinetics of the geopolymer matrix; therefore, FA reactivity and the geopolymers chemical behavior depend specifically on the particle sizes and surface area [26,27].The activation of these materials is also promoted by mechanical means, such as grinding, where results that favor geopolymerization are obtained at low curing temperatures.Through FT-IR it is demonstrated that FA with finer particles produce high reactivity indexes in the geopolymers and, therefore, an increase in the reaction product of the alkaline aluminosilicate amorphous gel.This produces an increase in compressive strength [28,29].
On the other hand, the use of X-ray diffraction (XRD) allows us to observe the formation of new phases which are characteristics of the FA geopolymerization process, such as semicrystalline and polycrystalline phases of inorganic polymers (especially zeolites) [30,31].
In this work, the influence of three different particle sizes of Mexican FA were comparatively studied in the physicochemical behavior of the geopolymers, using XRD, FT-IR, and SEM.

Materials
FA from José López Portillo coal-fired power plant, located in Coahuila, México, was used; its chemical composition determined by X-ray fluorescence is shown in Table 1, classifying it as a Class F fly ash (FA-1) (ASTM C618 [9]).The FA was subjected to mechanical grinding using a ball mill for periods of one hour until the highest percentage of material was passed through #200 and #325 sieves, and average particle sizes of ≤74 µm (FA-2) and ≤45 µm (FA-3) were obtained, respectively.

Characterization of FA
The distribution of FA particles is shown in Figure 1; it can be observed that 92% of the particles in sample FA-3 are smaller than 45 µm, while FA-1 and FA-2 have a higher percentage of particles with a size greater than 45 µm with 55% and 60%, respectively.It can also be observed that FA-1 contains particle sizes greater than 100 µm (30%).The specific surface area obtained by Brunauer-Emmett-Teller method (BET) of FA-1, FA-2, and FA-3 is shown in Table 2.

Sample Specific Surface Area (m 2 /kg)
FA-1 975 FA-2 1107 FA-3 1371 The identification of phases obtained by XRD show that the main compounds in FA-1, FA-2, and FA-3 are the mullite (Al6Si2O13) and quartz (SiO2), respectively (Figure 2a).Shown in the diffractograms are their primary peaks at 16.3 and 26.7° 2θ, in addition to an amorphous phase between 17° and 30° of 2θ, which is characteristic of this type of material [33].The XRD patterns indicated no apparent change in the mineralogy and peak intensities in the milled samples [28].In Figure 2b the FT-IR spectra of FA-1, FA-2, and FA-3 are shown, in which no band shifts or significant changes of FA-1 are observed respect to FA-2 and FA-3, presenting bands at 560, 792 and 1092 cm −1 attributed to symmetric stretching (Al-O-Si), symmetric stretching vibrations (Si-O-Si), and asymmetric stretching vibrations (Si-O-Si and Al-O-Si), respectively.Moreover, the bands in the regions of 1630 and 3437 cm −1 are attributable to stretching and deformation vibrations of O-H and H-O-H groups [33,34].For this, only FA-1 was chosen as a reference for comparison with the FT-IR spectra of the different geopolymers (Figure 4. The transmittance spectra of FA-1 and the different )  The identification of phases obtained by XRD show that the main compounds in FA-1, FA-2, and FA-3 are the mullite (Al 6 Si 2 O 13 ) and quartz (SiO 2 ), respectively (Figure 2a).Shown in the diffractograms are their primary peaks at 16.3 and 26.7 • 2θ, in addition to an amorphous phase between 17 • and 30 • of 2θ, which is characteristic of this type of material [33].The XRD patterns indicated no apparent change in the mineralogy and peak intensities in the milled samples [28].The identification of phases obtained by XRD show that the main compounds in FA-1, FA-2, and FA-3 are the mullite (Al6Si2O13) and quartz (SiO2), respectively (Figure 2a).Shown in the diffractograms are their primary peaks at 16.3 and 26.7° 2θ, in addition to an amorphous phase between 17° and 30° of 2θ, which is characteristic of this type of material [33].The XRD patterns indicated no apparent change in the mineralogy and peak intensities in the milled samples [28].In Figure 2b the FT-IR spectra of FA-1, FA-2, and FA-3 are shown, in which no band shifts or significant changes of FA-1 are observed respect to FA-2 and FA-3, presenting bands at 560, 792 and 1092 cm −1 attributed to symmetric stretching (Al-O-Si), symmetric stretching vibrations (Si-O-Si), and asymmetric stretching vibrations (Si-O-Si and Al-O-Si), respectively.Moreover, the bands in the regions of 1630 and 3437 cm −1 are attributable to stretching and deformation vibrations of O-H and H-O-H groups [33,34].For this, only FA-1 was chosen as a reference for comparison with the FT-IR spectra of the different geopolymers (Figure 4. The transmittance spectra of FA-1 and the different ) In Figure 2b the FT-IR spectra of FA-1, FA-2, and FA-3 are shown, in which no band shifts or significant changes of FA-1 are observed respect to FA-2 and FA-3, presenting bands at 560, 792 and 1092 cm −1 attributed to symmetric stretching (Al-O-Si), symmetric stretching vibrations (Si-O-Si), and asymmetric stretching vibrations (Si-O-Si and Al-O-Si), respectively.Moreover, the bands in the regions of 1630 and 3437 cm −1 are attributable to stretching and deformation vibrations of O-H and H-O-H groups [33,34].For this, only FA-1 was chosen as a reference for comparison with the FT-IR spectra of the different geopolymers (Figure 4 The transmittance spectra of FA-1 and the different geopolymers over the range of 1350-850 cm −1 were subjected to a deconvolution analysis using the Gaussian peak shape method).

XRD and FT-IR Analysis
The XRD of the geopolymers show a similarity in the intensity of the peaks produced by the present crystalline phases, in relation to each type of geopolymer, highlighting quartz as the most intense peak, present at 2θ = 27 • , attributed to the natural structure of the FA.The main crystalline phases of FA depend on the combustion process carried out in the coal plants; however, the crystal structures present in FA (Class F) coincide with the results of other investigations [35,36].
However, the reduction of particle size through mechanical grinding is the variable that causes a change in the XRD of the geopolymers, which is attributed, on the one hand, to the increase of the specific surface area, expanding the contact area with the alkaline activator, which promotes an increase in the reactivity of the FA.It was also observed that the mechanical grinding affected the microstructure of the FA and mainly causes a weakening in the vitreous chemical bonds of Si-O or Al-O, besides the fact that it accelerates the dissolution of these bonds, shortening the equilibrium time, gelation, and structuring of the new crystalline phases and of the different reaction products, specifically the hydrated sodium aluminosilicate gel (N-A-S-H), which is known as the reaction product that gives the mechanical properties to the geopolymer.
In Figure 3, the characteristic crystalline phases that were already present in the FA did not suffer any change with respect to the activated samples, because sodium hydroxide did not cause alterations in these phases due to the strong binding energies, which oscillate between 360 and 380 kcal/mol (five times stronger than the vitreous phase) [37], through which the alkalinity of the solution is capable of dissolving the bonds of the amorphous phase of this starting material.geopolymers over the range of 1350-850 cm −1 were subjected to a deconvolution analysis using the Gaussian peak shape method.

XRD and FT-IR Analysis
The XRD of the geopolymers show a similarity in the intensity of the peaks produced by the present crystalline phases, in relation to each type of geopolymer, highlighting quartz as the most intense peak, present at 2θ = 27°, attributed to the natural structure of the FA.The main crystalline phases of FA depend on the combustion process carried out in the coal plants; however, the crystal structures present in FA (Class F) coincide with the results of other investigations [35,36].
However, the reduction of particle size through mechanical grinding is the variable that causes a change in the XRD of the geopolymers, which is attributed, on the one hand, to the increase of the specific surface area, expanding the contact area with the alkaline activator, which promotes an increase in the reactivity of the FA.It was also observed that the mechanical grinding affected the microstructure of the FA and mainly causes a weakening in the vitreous chemical bonds of Si-O or Al-O, besides the fact that it accelerates the dissolution of these bonds, shortening the equilibrium time, gelation, and structuring of the new crystalline phases and of the different reaction products, specifically the hydrated sodium aluminosilicate gel (N-A-S-H), which is known as the reaction product that gives the mechanical properties to the geopolymer.
In Figure 3, the characteristic crystalline phases that were already present in the FA did not suffer any change with respect to the activated samples, because sodium hydroxide did not cause alterations in these phases due to the strong binding energies, which oscillate between 360 and 380 kcal/mol (five times stronger than the vitreous phase) [37], through which the alkalinity of the solution is capable of dissolving the bonds of the amorphous phase of this starting material.A semicrystalline gel is produced in the geopolymers pastes, which is characteristic in these materials and is displayed in the range of 2θ between 20° and 40°.In addition, scattered peaks appear at different intensities, located between 5° and 50° in 2θ [38].These results are consistent with those shown in the infrared spectra (Figure 4) that identify small bands located between 560 cm −1 and 792 cm −1 , where the first can be attributed to the vibration of Al-O-Si bonds contained in the mullite and the second to Si-O-Si bonds included in the quartz [39,40].Considering that these bands A semicrystalline gel is produced in the geopolymers pastes, which is characteristic in these materials and is displayed in the range of 2θ between 20 • and 40 • .In addition, scattered peaks appear at different intensities, located between 5 • and 50 • in 2θ [38].These results are consistent with those shown in the infrared spectra (Figure 4) that identify small bands located between 560 cm −1 and 792 cm −1 , where the first can be attributed to the vibration of Al-O-Si bonds contained in the mullite and the second to Si-O-Si bonds included in the quartz [39,40].Considering that these bands are maintained for each of the spectra of the activated materials (the sets G1, G2, and G3), it is confirmed that these crystalline phases are not modified and, therefore, the signals come from the crystals of the FA.Regarding the curing age at early ages, the sets G1 and G2 remain constant.However, set G3 presents an increase in its intensity, and this behavior remains for 14 and 28 days, indicating the development of polymerization of the material.This process reveals evolutions in the crystalline phases, determining the influence that the particle sizes of the FA have on the reactivity of the geopolymers.are maintained for each of the spectra of the activated materials (the sets G1, G2, and G3), it is confirmed that these crystalline phases are not modified and, therefore, the signals come from the crystals of the FA.Regarding the curing age at early ages, the sets G1 and G2 remain constant.However, set G3 presents an increase in its intensity, and this behavior remains for 14 and 28 days, indicating the development of polymerization of the material.This process reveals evolutions in the crystalline phases, determining the influence that the particle sizes of the FA have on the reactivity of the geopolymers.As curing time passes, there is a decrease in the halo of the amorphous phase (Figure 3) located between 20° and 40° of 2θ due to its dissolution, which promotes the formation of new products and allows for the occurrence of the specific phases of the geopolymers.
In Figure 5, it is shown how faujasite and type Y-zeolite acquire intensities with similar tendencies.The largest ones are concentrated in G3-14 and G3-28, and are up to 50% more intense than those in group G1, which can be attributed to a greater development of crystallinity in its phases [41], mainly due to a greater reactivity of the FA, because of the increase of the specific surface area induced by the reduction of particle size by grinding, which causes the weakening of Si-O and Al-O bonds and thus promotes the incorporation of soluble Si and Al in the crystalline chain.As curing time passes, there is a decrease in the halo of the amorphous phase (Figure 3) located between 20 • and 40 • of 2θ due to its dissolution, which promotes the formation of new products and allows for the occurrence of the specific phases of the geopolymers.
In Figure 5, it is shown how faujasite and type Y-zeolite acquire intensities with similar tendencies.The largest ones are concentrated in G3-14 and G3-28, and are up to 50% more intense than those in group G1, which can be attributed to a greater development of crystallinity in its phases [41], mainly due to a greater reactivity of the FA, because of the increase of the specific surface area induced by the reduction of particle size by grinding, which causes the weakening of Si-O and Al-O bonds and thus promotes the incorporation of soluble Si and Al in the crystalline chain.
The band at 3437 cm −1 is derived from the O-H stretching present in the FA.In the same way, this band appears wider in the geopolymeric samples due to the overlapping of signals, originating from the contribution of hydroxyl systems of the alkaline activator to the chemical structure of G1, G2, and G3.On the other hand, the free water present in the FA shows a low transmittance at 1630 cm −1 .This is attributed to the low contained humidity; however, in G1, G2, and G3 a more intense band appeared at 1655 cm −1 due to the presence of physically bound water (H-O-H), which was produced by the hydrolysis that occurs from the specific equilibrium process of aluminates and silicates until the final polymerization of the geopolymer.
In Figure 5, it is shown how faujasite and type Y-zeolite acquire intensities with similar tendencies.The largest ones are concentrated in G3-14 and G3-28, and are up to 50% more intense than those in group G1, which can be attributed to a greater development of crystallinity in its phases [41], mainly due to a greater reactivity of the FA, because of the increase of the specific surface area induced by the reduction of particle size by grinding, which causes the weakening of Si-O and Al-O bonds and thus promotes the incorporation of soluble Si and Al in the crystalline chain.The intensification of the band at 1428 cm −1 is attributed to the C-O bonds present in NaCO 3 (Figure 3c) produced by the reaction of free NaOH in the geopolymers with CO 2 from the environment.
At 1092 cm −1 , a band corresponding to the FA-1 spectrum is observed and there is a shift towards lower wavenumber, in the 1000 and 1016 cm −1 range, attributed to the asymmetric stretching of the Si-O-Si and Al-O-Si bonds present in the semicrystalline gel of the specimens.The presence of this band is considered the most important, since it provides information related to the development and polymerization of the alkali-activated FA [23,38,42].
Spectra deconvolutions were performed (Figures 6-8) which show these shifts of the evolution of the bands that characterize these activated materials.The assignment of bands is proposed in Table 3.The band at 3437 cm −1 is derived from the O-H stretching present in the FA.In the same way, this band appears wider in the geopolymeric samples due to the overlapping of signals, originating from the contribution of hydroxyl systems of the alkaline activator to the chemical structure of G1, G2, and G3.On the other hand, the free water present in the FA shows a low transmittance at 1630 cm −1 .This is attributed to the low contained humidity; however, in G1, G2, and G3 a more intense band appeared at 1655 cm −1 due to the presence of physically bound water (H-O-H), which was produced by the hydrolysis that occurs from the specific equilibrium process of aluminates and silicates until the final polymerization of the geopolymer.
The intensification of the band at 1428 cm −1 is attributed to the C-O bonds present in NaCO3 (Figure 3c) produced by the reaction of free NaOH in the geopolymers with CO2 from the environment.
At 1092 cm −1 , a band corresponding to the FA-1 spectrum is observed and there is a shift towards lower wavenumber, in the 1000 and 1016 cm −1 range, attributed to the asymmetric stretching of the Si-O-Si and Al-O-Si bonds present in the semicrystalline gel of the specimens.The presence of this band is considered the most important, since it provides information related to the development and polymerization of the alkali-activated FA [23,38,42].
Spectra deconvolutions were performed (Figures 6-8) which show these shifts of the evolution of the bands that characterize these activated materials.The assignment of bands is proposed in Table 3.      Table 3. Characteristic IR vibrational bands of geopolymers [43].The spectra deconvolution allows us to observe the shift and the displacement of the bands of FA-1 towards lower wavenumbers with more precision, as well as to establish the changes that occur in the material during polymerization and ascertain with greater certainty that the FA was activated and a geopolymer is obtained.In the spectra analyzed by this method, it can be seen that the curing time is a factor that determines the process, but that the particle size from the first days of curing influences the polymerization process to a greater extent through the activation of the FA.The width of the blue band is wide because of the diversity of vibrations Si-O and Al-O produced by the amorphous molecule of the reaction product [44,45].

Band (cm
The vibrations of the bonds attributed to the vitreous phase of the FA-1 of origin, when activated, transform and vibrations at lower wavenumbers are observed, which is characteristic of the formation of the gel product of the polymerization of the activated material.
It can be observed that the green band cedes almost all of its color towards the darker blue; however, sets G1 and samples G2-7 and G2-14 continue showing small green areas, indicating the continued vibration of the amorphous material, which suggests that it is still present in some Table 3. Characteristic IR vibrational bands of geopolymers [43].The spectra deconvolution allows us to observe the shift and the displacement of the bands of FA-1 towards lower wavenumbers with more precision, as well as to establish the changes that occur in the material during polymerization and ascertain with greater certainty that the FA was activated and a geopolymer is obtained.In the spectra analyzed by this method, it can be seen that the curing time is a factor that determines the process, but that the particle size from the first days of curing influences the polymerization process to a greater extent through the activation of the FA.The width of the blue band is wide because of the diversity of vibrations Si-O and Al-O produced by the amorphous molecule of the reaction product [44,45].

Band (cm
The vibrations of the bonds attributed to the vitreous phase of the FA-1 of origin, when activated, transform and vibrations at lower wavenumbers are observed, which is characteristic of the formation of the gel product of the polymerization of the activated material. It can be observed that the green band cedes almost all of its color towards the darker blue; however, sets G1 and samples G2-7 and G2-14 continue showing small green areas, indicating the continued vibration of the amorphous material, which suggests that it is still present in some geopolymers (see Figures 6-8).The change of color or the change of phase (the amorphous phase of FA-1 to the semicrystalline phase of geopolymers) is derived from the precipitation of Si and Al reactive bonds in the original FA with NaOH.The FA contains a higher percentage of Si 4+ than Al 3+ and, together with the reactivity of the same and the increase in the curing time, Si 4+ bonds are gradually integrated into the environment of the aluminosilicate gel, so Si 4+ begin to occupy the spaces of Al 3+ [46].This causes displacements to higher wavenumbers, due to the higher Si-O bond strength (80 kcal/mol) with respect to the Al-O bond strength (60 kcal/mol) [47], moving from 1002.5 cm −1 at the lowest end (G1-7) to 1015.26 cm −1 at the highest end (G3-28).With this information (1026 cm −1 -1002 cm −1 = 100%), Figure 9 attempts to relate the highest wavenumber with the geopolymerization of the specimens.It can be seen that the set G3 has the highest displacements, with percentages greater than 60% in relation to the extremes.In this list, G2-14 and G2-28 are integrated with 60% and 66%, respectively.Samples that were obtained through FA without milling or sifting show percentages below 30%.As previously mentioned, the specific surface area of the FA plays a more important role in relation to the curing time, since after 14 days sets G-2 and G-3 show a high or acceptable geopolymerization.The band that appears in a violet color in FA-1 disappears for the samples of the geopolymers.This behavior indicates that the Si-O and Al-O vibrations become part of the color blue or the crystalline phase, represented by the color red.The vibrations of the bonds found in the phases of the mullite or quartz for the FA are identified in the red band.However, this band widens considerably in the geopolymers, which is caused by the formation of new zeolitic phases.

Microstructure
Figure 10 shows the morphologies, structures, and phases of the geopolymers with a curing time of 28 days, which is when significant changes and differences between the samples are observed.The NaOH produces the phase dissolution of the FA, and forms reaction products with a homogeneous and compact matrix that does not occur in the starting material, the main characteristic of which is its spherical shape (Figure 10a) [48].In the micrographs corresponding to the geopolymers, cavities left between the reaction products can be observed, which are mostly gels formed by long chains of silicates and aluminates balanced by the sodium ions of the NaOH used as The band that appears in a violet color in FA-1 disappears for the samples of the geopolymers.This behavior indicates that the Si-O and Al-O vibrations become part of the color blue or the crystalline phase, represented by the color red.The vibrations of the bonds found in the phases of the mullite or quartz for the FA are identified in the red band.However, this band widens considerably in the geopolymers, which is caused by the formation of new zeolitic phases.

Microstructure
Figure 10 shows the morphologies, structures, and phases of the geopolymers with a curing time of 28 days, which is when significant changes and differences between the samples are observed.The NaOH produces the phase dissolution of the FA, and forms reaction products with a homogeneous and compact matrix that does not occur in the starting material, the main characteristic of which is its spherical shape (Figure 10a) [48].In the micrographs corresponding to the geopolymers, cavities left between the reaction products can be observed, which are mostly gels formed by long chains of silicates and aluminates balanced by the sodium ions of the NaOH used as solution.These results consistent with other investigations [49,50].The new structures are a consequence of alkaline attack and thermal curing during the process of obtaining the geopolymers [51].

Conclusions
1.The reduction of fly ash particle size by grinding allows a greater dissolution in the alkaline activation of the raw material.2. Deconvolutions show the displacement of the bands with greater precision, and in the same way establish whether the activation process was carried out and elucidate the evolution of how the bonds are restructured over time.3. A smaller particle size requires less time to produce crystalline structures and gels that provide stability to the geopolymers, as well as more homogeneity in the matrix and more rigid bonds.Likewise, through these images it is also possible to observe the evolution of the reaction products with different particle sizes of FA-1.
In Figure 10b there are fewer crystalline phases and a heterogeneous matrix without defined structures which is related to a low crystallinity; as the particle size decreases (Figure 10c,d), the number of crystalline products increases and is consistent with zeolitic structures attributed to the faujasite and type Y-zeolite.These structures are present in the sets G1, G2, and G3, but with higher intensity in G3 (Figure 5) inside an amorphous matrix attributed to the formation of gels in the activation and geopolymerization process [51].
This influence on the achievement of the reaction products is observed in the displacement of the bands of the FT-IR spectra and in the creation of new crystalline phases that also appear in XRD.

1.
The reduction of fly ash particle size by grinding allows a greater dissolution in the alkaline activation of the raw material.

2.
Deconvolutions show the displacement of the bands with greater precision, and in the same way establish whether the activation process was carried out and elucidate the evolution of how the bonds are restructured over time.

3.
A smaller particle size requires less time to produce crystalline structures and gels that provide stability to the geopolymers, as well as more homogeneity in the matrix and more rigid bonds.

Figure 4 .
Figure 4. FT-IR spectra of FA-1 and obtained geopolymers at different curing days.

Figure 4 .
Figure 4. FT-IR spectra of FA-1 and obtained geopolymers at different curing days.

Figure 5 .Figure 5 .
Figure 5. Intensities ratio of faujasite and type Y-zeolite phases obtained by X-ray diffraction.
stretching (Si-O-Si and Al-O-Si) 1150-1200 Asymmetric stretching (Si-O-Si) 1050-1150 Asymmetric stretching of amorphous phase (Si-O-Si and Al-O-Si) 980-1030 Asymmetric stretching of N-A-S-H gel (Si-O-Si and Al-O-Si) Appl.Sci.2018, 8, x FOR PEER REVIEW 8 of 11 plays a more important role in relation to the curing time, since after 14 days sets G-2 and G-3 show a high or acceptable geopolymerization.

Table 1 .
Chemical composition of fly ash.