3.1 DSC analysis
Figure 1 showed the DSC graph of parent glasses with different Al2O3/SiO2 at heating rate of 10 ℃/min. Table 2 showed the specific characteristic temperature values for A1-A5, where Tg was the glass transition temperature, Tc1 was the first crystallization temperature, and Tc2 was the second crystallization temperature. In Fig. 1, there were two obvious exothermic peaks within the range of 780–900 ℃, among which the first crystal peak shape of A1 parent glass was relatively flat.
Table 2
Characteristic temperature of glasses with different Al2O3/SiO2 in DSC.
| Tg(℃) | Tc1(℃) | Tc2(℃) |
A1 | 613.7 | 851.8 | 900.8 |
A2 | 594.7 | 799.0 | 878.8 |
A3 | 568.8 | 790.8 | 887.1 |
A4 | 413.1 | 783.7 | 886.2 |
A5 | 565.2 | 783.5 | 886.0 |
The DSC curve of the base glasses showed that the peak of Tc1 became sharp and moved towards low temperature gradually for A1-A5, while Tc2 showed a trend of moving towards high temperature for A2-A5. While the charge of Al3+ is less than that of Si4+, and the self-diffusion coefficient of Al3+ is higher than that of Si4+[15]. Therefore, the higher Al2O3 content in the glasses was more conducive to particle diffusion in the crystallization process, which reduced Tc1 for A1-A5[15]; then the crystal phase was precipitated on the surface of the glass particle, which increased the viscosity of the glasses, hindered the further diffusion of the particle, and led to the rise of Tc2[16]. The first crystallization peak of the A1 glass was not obvious and the Tc2 was high, which may be related to the high SiO2 content in the A1 glass, as Si4+ can gather the network, increase the viscosity of the glass, hinder the diffusion of particles inside the glass, and increase the crystallization temperature[17]. Figure 1 and Table 2 showed that Tg decreased first from A1 to A5 (reached the minimum in A4) and then increased, which indicated that the thermal stability of glasses deduced first and then rose with the increase of Al2O3/SiO2. The thermal stability of glasses is closely related to the network structure of glass[18], which also indicated that the network polymerization degree of glasses showed a trend of first decreasing and then increasing in series A glasses. In this experiment, according to the DSC curve (Fig. 1), in order to ensure that the crystallization process of each sample was fully carried out, the sintering temperature of the sample was set at 890 ℃ and the holding time was 1.5 h.
3.2 Crystal phase analysis
The XRD graph of glass-ceramics with different Al2O3/SiO2 was illustrated in Fig. 2. It shows that the peaks of A1-A5 glass-ceramics were basically the same. The analysis by Jade 6.5 indicated that the crystal phase of A series glass-ceramics was composed of the main crystal phase gehlenite(Ca2(Al(AlSi)O7,PDF#74-1607), the secondary crystal phase diopside(CaMgSi2O6༌PDF#74-1607) and hyalophane (K.6Ba.4Al1.42Si2.58O8༌PDF#72-1497). Figure 2 also showed that the diffraction peak intensity of the main crystal phase increased while that of the secondary crystal phase decreased gradually for A1-A5.
It means that the content of gehlenite in the glass-ceramics increased while diopside and hyalophane decreased with the increase of Al2O3/SiO2. The degree of polymerization of anionic groups is different between the primary phase (gehlenite) and the secondary phase (diopside and hyalophane). The reaction process is as follows:
2Ca2+ + Al3+ + (AlSiO7)7− → Ca2Al(AlSi)O7
Ca2+ + Mg2+ + (Si2O6)4− → CaMgSi2O6
0.6K+ + 0.4Ba2+ + (Al1.42Si2.58O8)1.42− → K.6Ba.4Al1.42Si2.58O8
The Si(Al)/O ratio of anion group [AlSiO7] is smaller than that of [Si2O6] and [Al1.42Si2.58O8], indicating a lower degree of polymerization of [AlSiO7][19, 20]. In terms of element composition, Al3+ directly participated in the formation of the main crystal phase gehlenite, therefore, the increase of Al2O3 content was conducive to the precipitation of gehlenite. As a network intermediate, Al3+ can not only replace Si4+ to participate in the glass network and crystal phase constitution with [AlO4], but also destroy the glass network structure in the form of [AlO6][7, 8]. On the one hand, with the increase of Al2O3/SiO2, Si4+ in the glass decreased and Al3+ increased, [AlO6] played a role in breaking the glass network, reducing the degree of polymerization of glass network and facilitating the precipitation of gehlenite with low degree of anionic polymerization; on the other hand, the increase of Al2O3 rose the number of Al3+ substituted for Si4+ in the glass network, which was conducive to the formation of [AlSiO7] and promoted the precipitation of gehlenite. On account of the large amount of precipitation of gehlenite, Si4+ content in the glasses was decreased, which led to the reduction of the anion group of the secondary crystal phase and reduced the precipitation of diopside and hyalophane.
The SEM graph was showed in Fig. 3. It illustrated that there were a large number of strip or gridded crystals, and the XRD analysis results showed that the crystal phase was gehlenite; a few clusters of granular crystals were seen in A1-A3, which were speculated to be diopside based on the XRD results. In the A4 and A5 samples, no other crystal phases were found, which was mainly attributed to the high precipitation of gehlenite and the low precipitation of secondary phase. In the SEM graph of A1, there were more holes left by HF solution erosion. With the increase of Al2O3/SiO2, the holes decreased gradually, indicating that the increase of crystal evolution led to the decrease of glass phase for A1-A5. When the Al2O3/SiO2 increased to 0.34 (A4), it was seen that the growth of crystal grains was united and arranged in a certain direction, and the defect area without crystal phase existed; when the Al2O3/SiO2 ratio continued to increase to 0.39 (A5), the crystal grains continued to grow into long strips, and the long strips growing in different directions were interspersed and nested together.
3.3 FTIR analysis
FTIR is a common method used to test the internal structure of glass and glass-ceramics. Figure 4 was the FTIR of the base glasses with different Al2O3/SiO2 at 400 cm− 1-1400 cm− 1. In Fig. 4, the shape of vibration absorption peak of A1-A5 parent glasses was substantially the same. There were mainly three wide vibration absorption bands, which were in the range of 400–600 cm− 1, 600–800 cm− 1 and 800–1200 cm− 1 respectively. The irregular arrangement of ions (ion clusters) in the glasses and the existence of non-bridging oxygen bonds made the angle and length of Si-O bond change, which made the infrared vibration absorption peak shift to a certain extent and become gentle and broad[21, 22].
In the infrared vibration spectra of glasses, the vibration absorption band in the range of 400–600 cm− 1 was attributed to the bending vibration of Si–O–Si, Si–O–Al, O–Si–O and O–Al–O[23, 24].
The absorption peak in the range of 600–800 cm− 1 was the symmetric stretching vibration of Si–O–Al, which was mainly attributed to the stretching vibration of the [AlO4] and stretching vibration of the bridge oxygen bond in the glass network structure[11]. From A1 to A5, the vibration absorption peak near 720 cm− 1 showed a small shift towards low wavenumbers, and the absorption intensity was enhanced, indicating that the Si–O–Al bond with lower vibration frequency in the glass network increased[23]. This was due to the fact that with the increase of Al2O3/SiO2, more and more Al3+ replaced Si4+ to form tetrahedron and entered into the glass network, forming Si–O–Al bond with [SiO4].
The absorption vibration peak in the range of 800–1200 cm− 1 was mainly related to the [SiO4], which was attributed to the asymmetric stretching vibration of Si–O–Si, the symmetric stretching vibration and asymmetric stretching vibration of O–Si–O, the absorption was strong and broad, which was caused by the superposition of different peaks[25–27]. The vibration absorption peak in the range of 800–1200 cm− 1 can be decomposed into stretching vibration of silicon-oxygen tetrahedron with different degree of polymerization by Gaussian function (Fig. 5), whose symbol is Qn, where n is the number of bridging oxygen (Ob) in the silicon-oxygen tetrahedron (n = 0,1,2,3,4,5)[19, 28]. Figure 5 was the Gaussian deconvolution diagram of the infrared vibration absorption peak at the range of 800–1200 cm− 1 of the series A glasses, and table 3 was the specific peak values of each Qn. The results of Fig. 5 and Table 3 showed that the vibration absorption peaks of A1-A5 glasses at 800–1200 cm− 1 were all decomposed into 5 vibration absorption peaks corresponding to Q0, Q1, Q2, Q3 and Q4 respectively. Moreover, the peak positions of Qn were relatively similar for each sample of series A glasses, indicating that the network structure of the base glass did not change significantly with the increase of Al2O3/SiO2.
Figure 6 was the variation distribution chart of peak position of Qn for A1-A5, which indicated that the peak position of Qn was firstly shifted to direction of the low wavenumbers and then to the high wavenumbers, among which the peak position of Qn reached the lowest when the Al2O3/SiO2 was 0.34 (A4). The vibration absorption peak of Qn is closely related to the glass network[29]. When the glass network tends to be close, the vibration peak is shifted to the direction of high wavenumbers; on the contrary, when the glass network structure tends to be loose, the vibration peak moves to the direction of low wavenumbers[29]. The curve in Fig. 6 illustrated that the glass network structure tended to be loose with the increase of Al2O3/SiO2 from 0.19 to 0.34; subsequently, the glass network structure tended to be close with the Al2O3/SiO2 continues to increase from 0.34 to 0.39.
Table 3
Wavenumbers of Qn in glasses with different Al2O3/SiO2.
| | A1 | A2 | A3 | A4 | A5 |
Wavenumbers (cm− 1) | Q0 | 849.7 | 847.2 | 847.1 | 844.1 | 844.1 |
Q1 | 894.6 | 890.6 | 889.0 | 883.5 | 886.2 |
Q2 | 970.2 | 962.4 | 956.6 | 948.4 | 959.6 |
Q3 | 1069.5 | 1061.6 | 1054.5 | 1049.2 | 1060.9 |
Q4 | 1144.7 | 1140.1 | 1136.5 | 1132.2 | 1135.9 |
The infrared vibration absorption spectra of the glass-ceramics sintered at 890 ℃ was showed in Fig. 7. It indicated that the peak range of the glass-ceramics sample was roughly the same as that of the base glasses (Fig. 4), which was still divided into three vibration absorption bands, however, there were some sharp absorption peaks which were not found in the infrared vibration absorption spectra of the base glasses. This was mainly attributed to the generation of crystal phase, which made the originally covered absorption peaks appear[21, 23]. The position and shape of the infrared absorption peaks of A1-A5 were basically the same, indicating that the crystal phase of glass-ceramics with different Al2O3/SiO2 were basically the same, and the XRD analysis also proves this conclusion.
In the range of 400-600cm− 1, the vibration absorption peak at 470 cm− 1 was divided into two absorption peaks: 472 cm− 1 and 424 cm− 1. The peak at 472 cm− 1 was attributed to the bending vibration of Si–O–Si in the residual glass phase and diopside phase (a small amount of hyalophane), the peak at 424 cm− 1 was attributed to the bending vibration of Si–O–Al bond in gehlenite[24, 30]. The intensity of the vibration absorption peak at 424 cm− 1 gradually increased for A1-A5, which indicated that the content of gehlenite increased in glass ceramics with the increase of Al2O3/SiO2. There were two vibration absorption peaks at 544 cm− 1 and 579 cm− 1, which were not found in the base glasses in Fig. 4. This was due to the coupling effect between the bending vibration of O-Si-O in the crystal phase and the stretching vibration of Ca–O[24, 27]. In the range of 600–800 cm− 1, in addition to the vibration absorption peak near 714 cm− 1(base glasses also had the same vibration absorption peak), two new vibration absorption peaks appeared at 682 cm− 1 and 630 cm− 1. The peak at 714 cm− 1 and 682 cm− 1 were attributed to the symmetric stretching vibration of Si–O–Si and the stretching vibration of Si–O–Al respectively; the peak at 630 cm− 1 was related to the stretching vibration of Al–O in the aluminum-oxygen tetrahedron[22, 27, 30]. In the range of 800–1200 cm− 1, the vibration absorption peak near 1000 cm− 1 split into 1028 cm− 1, 985 cm− 1 and 939 cm− 1 due to crystal phase precipitation, which were associated with the stretching vibration of Si–O in [SiO4] (asymmetric stretching vibration of Si–O–Si, symmetric stretching vibration and asymmetric stretching vibration of O–Si–O)[22, 26, 27].
3.4 27Al NMR analysis
To further study the coordination of Al3+ in glass, the 27Al MAS NMR spectra were used to investigate the glass structure, as shown in Fig. 8, there was an obvious wide peak in the range of -25-100 ppm. In aluminosilicate system, Al3+ has three coordination modes: [AlO4], [AlO5], [AlO6]. Therefore[31, 32], 27Al NMR spectra were deconvoluted by Gaussian function, and the results were shown in Fig. 9 and Fig. 10.
The results in Fig. 9 showed that the 27Al NMR spectra deconvolution of series A glasses were similar, which was consisted of three distinct peaks [AlO4], [AlO5] and [AlO6], in which the area % of [AlOn] (n = 4, 5, 6) was related to its content[7, 9, 10]. In Fig. 10, the area % of [AlO6] first increased and then decreased for A2-A5, and reached the maximum in A4 (the Al2O3/SiO2 was 0.34); on the contrary, the area % of [AlO5] and [AlO4] first decreased and then increased, and reached the minimum in A4. The area % of [AlO6] in A1 glass was relatively large, while area % of [AlO5] and [AlO4] were relatively small, which may be related to the small Al2O3/SiO2 in A1. The high SiO2 content in the glass made the glass network densified, at the same time, the low Al2O3 content made it difficult for Al3+ to replace Si4+ in glass network, hence, more Al3+ existed in [AlO6] for A1.
3.5 Physical and mechanical properties analysis
The physical and mechanical properties of glass-ceramics with different Al2O3/SiO2 were showed in Fig. 11; (a), (b) and (c) were the volume density, the bending strength and the microhardness respectively.
The results of Fig. 8 showed that the volume density of the glass-ceramics was between 2.735–2.770 g/cm3, the bending strength was between 95–120 MPa and the microhardness was between 540–610 Hv. Meanwhile, with the increase of Al2O3/SiO2, the volume density, bending strength and microhardness of glass-ceramics all decreased first (reached the minimum in A4, the Al2O3/SiO2 was 0.34) and then increased. The physical and mechanical properties of glass-ceramics are closely connected to the crystal phase, the glass phase and the combination among them[33, 34]. According to the previous analysis, with the Al2O3/SiO2 gradually raising from 0.19 to 0.34, the precipitation of main crystal phase gehlenite (Ca2(Al(AlSi)O7)) increased, while the precipitation of secondary crystal phase decreased, and the remaining glass phase in the glass-ceramics also decreased. With the precipitation and growth of crystal phase, the internal stress of the glass-ceramics rose, and the decrease of liquid phase content was harmful to the sintering process, which led to the insufficient connection between crystal phase and led to more holes and defects in the glass-ceramics. At the same time, more Al3+ destroyed the glass network structure with [AlO6], making the microstructure of the glasses tend to be loose. These results combined to reduce the physical properties (volume density, bending strength, microhardness) of the glass-ceramics with the increase of Al2O3/SiO2 from 0.19–0.34 (A1-A4). With the further increase of Al2O3/SiO2 from 0.34 to 0.39, the proportion of [AlO4] in the glass network increased, which was beneficial to strengthen the glass network and make the structure tend to be dense. Meanwhile, the crystal phase in the glass-ceramics was further precipitated and grown, and the long strip crystal phase was interspersed with each other, which made the bonding between the crystal phase more complex and compact, thus increasing the density, bending strength and microhardness.