3.1. Specific Surface Area, Characteristic Particle Size, and Morphological Change of Molybdenum Tailings at Different Grinding Times
Table 5 shows the specific surface area test results of the molybdenum tailings with different grinding times.
Table 6 shows the characteristic particle size of the molybdenum tailings with different grinding times.
It can be seen from
Table 5 that the particle size of the molybdenum tailings decreases continuously during the grinding process between 15 and 60 min. When the grinding process reaches 60 min, the specific surface area reaches 934.2 m
2/kg; however, after 60 min, the specific surface area decreases, which may be caused by agglomeration between particles during the grinding process.
It can be observed from
Table 5 and
Table 6 that during the grinding process, the molybdenum tailings are micronized due to external grinding action, whereas the fine particles will agglomerate with each other due to surface adsorption. At the initial stage of grinding, due to the large particles and the small surface energy of the powder, the particles do not agglomerate through mutual attraction. With the prolongation of the grinding time, the particles are continuously refined, and the surface free energy of the particles increases. When grinding exceeds a certain duration, and due to the increase in the surface energy of the powder, the fine particles agglomerate due to surface adsorption [
8]. Determining whether the agglomeration phenomenon will affect the continuous increase of the specific surface area can be accomplished by measuring the particle size distribution of the sample using a laser particle size analyzer. If the individual particles of the sample are clustered at the nanometer level, they will not be dispersed by ultrasound and ethanol, and a contradiction phenomenon will occur, which is that the fineness of the sample will continue to increase. However, the particle size distribution test showed that the sample particles became larger instead.
The composition of tailings is complex, the hardness and wear resistance of the various mineral components are different, and the material after grinding does not show a normal distribution. During the initial stage of grinding, the particle size of the minerals was reduced. As grinding continued, the submicron particles of the molybdenum tailings increased significantly. As the particle size decreased, the corresponding specific surface area increased, which is consistent with the test results shown in
Table 5. Because this study uses molybdenum tailings to prepare a tailing cementitious material, the national standard requires that the specific surface area of 42.5 ordinary Portland cement should not be less than 300 m
2/kg, and the activity of the molybdenum tailings should be low. When replacing cement with concrete cementitious material, the specific surface area of the molybdenum tailings must be greater than that of ordinary Portland cement. When the grinding time is too long, the grinding cost will increase.
In general, when molybdenum tailings are not milled, the reaction under normal temperature and pressure without a catalyst is slow or difficult. However, after mechanical grinding, the ability of molybdenum tailings to participate in the reaction can be enhanced, and the mechanical properties of the products are improved.
With the reduction of the particle size of the ground molybdenum tailing powder, its specific surface area and surface atom number increase sharply. Additionally, the surface atom coordination is insufficient, resulting in a large number of suspended and unsaturated bonds, which creates a thermodynamically unstable state, i.e., these surfaces have high activity and easily combine with other atoms.
Figure 2 shows the FESEM photos of molybdenum tailings after various grinding durations at 5K× magnification. After grinding for 15 min, most molybdenum tailing particles are long strips and irregular polygonal blocks, with sharp edges and corners. As the grinding duration increases, the size of the tailing particles continues to decrease, and the edges and corners become smooth. At less than 1 μm, the number of ultrafine particles increases. When the grinding time is 60 min, the elongated particles with edges and corners disappear, and many round particles appear. When the grinding time is more than 75 min, the tailing particles exhibit obvious agglomeration.
Based on the above experimental results, the grinding time of molybdenum tailings in the follow-up test was set at 60 min.
3.4. SEM Analyses of the Paste Mixtures
SEM was employed to characterize the morphology of the hydration products and the microstructure of the hardened specimens at different ages. The surface microstructures of the fractured surface and inner pores of the paste specimens aged for 3, 7, and 28 days are presented in
Figure 4. As shown in this figure, the amount of needle-like phases on the surface of the pores in the paste specimens increased with the increase in the curing age. Further magnification of
Figure 4(b1) is given in
Figure 4(b2), where the needle-like phase corresponds to AFt crystals.
Figure 4(a1,a2) display the presence of several unhydrated molybdenum tailing particles on the broken surface of the paste specimens at the curing age of three days. The comparison of
Figure 4(b1) with
Figure 4(c1) revealed the formation of more needle-like AFt with the increase in curing age. As shown in
Figure 4(c2), the molybdenum tailing particles were coated well with the amorphous C-S-H gel at the curing age of 28 days, resulting in a denser microstructure. Therefore, the amount of AFt and C-S-H gel in the paste specimens increased with the increase in the curing age, resulting in a denser microstructure that contributes to strength enhancement.
3.5. FTIR
Figure 5 shows the FTIR spectra of the hydrated neat cementitious material specimens mixed with ground molybdenum tailings, gypsum, and Ca(OH)
2 when cured for 3, 7, and 28 days. The IR spectrum of the dry mixture is also shown as a comparison. As shown in
Figure 5, the absorption band between 3800 and 3000 cm
−1 indicates the stretching vibration of O-H bonds in the different phases of the system. The prominent absorption bands of ~3640 cm
−1 indicate that the O-H bonds in Ca(OH)
2 became weaker and nearly disappeared at the curing age of 28 days [
10,
11,
12,
13]. This suggests that the hydration reaction consumed most of the Ca(OH)
2 when the curing age was prolonged to 28 days.
Similar absorption peaks were also observed at 3428, 3424, and 3424 cm−1 in the IR spectra of the specimens cured for 3, 7, and 28 days, respectively. These peaks are the overlaps of the O-H bonds attached to silica and the O-H bonds in ettringite. Interestingly, the wave numbers of the peaks increased from the dry mixture specimen to the specimens cured for three days. This increase indicates that the average bonding energy of the O-H bonds increased continuously from the dry mixture specimen to the specimens cured for three days. It also suggests that the average abstraction forces between the cations in the system and the O-H bonds became increasingly weaker. The combined water in the newly formed ettringite and C-S-H gels was generally less strongly bound to the cations than in well-crystallized silicate minerals. This property resulted in a higher bonding energy of the O-H bonds in the newly formed ettringite and C-S-H gels. Conversely, the increasingly prominent absorption bands between 3800 and 3000 cm−1 indicate the occurrence of a hydrating reaction that progressed with the increase in the curing age. This deduction coincides well with the results obtained from the XRD and SEM analyses.
An absorption band of ~1651 cm−1, which is a characteristic of the bending vibration of the O-H bonds of structural or crystallized water, occurred in the spectra of the specimens cured for three days. This peak was mainly due to the newly formed ettringite. Similar absorption peaks also occurred at 1643 and 1644 cm−1 in the IR spectra of specimens cured for 7 and 28 days, respectively. The absorption peak appeared in the 3-, 7-, and 28-day specimens, but not in the dry mixture specimen. This finding indicates that ettringite was generated during the hydration reaction.
Another prominent absorption peak occurred at 1445 cm
−1 [
10,
14] due to the original calcite mineral in the molybdenum tailings. This peak is a characteristic of the stretching vibration of CO
32− in the IR spectrum of the dry mixture. Similar absorption peaks also occurred at 1434, 1435, and 1435 cm
−1 in the IR spectra of the specimens cured for 3, 7, and 28 days, respectively. Thus, the peaks became slightly more prominent with the increasing curing age; however, the wavenumbers did not change significantly. This observation suggests that new calcite minerals were formed during the curing process by combining with the carbon dioxide in the atmosphere.
The absorption band of ~1089 cm
−1 is a characteristic of the asymmetric stretching vibration of the S-O bands in the IR spectrum of the dry mixture [
15] and is typically due to the original gypsum mineral. The moderately wide range and lack of sharpness of this peak reflect the lower crystalline or multiphase character of gypsum. Similar absorption peaks also occurred at 1092, 1093, and 1093 cm
−1 in the IR spectra of the specimens cured for 3, 7, and 28 days, respectively. This finding suggests that the peaks became more prominent and their sharpness increased with the increasing curing age; however, the wavenumbers did not change significantly. These changes indicate that the SO
42− ions were transformed from the gypsum minerals to the ettringite minerals, which are normally well crystallized.
The absorption band at ~876 cm
−1 characterizes the asymmetric stretching vibration of the Al-O bands in various minerals [
16]. This absorption band became increasingly sharper from the dry mixture to the specimens cured for 3 to 7 to 28 days. This observation indicates that the Al-O bands increased continuously in one well-crystallized mineral, while the Al-O bands in the other minerals disappeared. The above XRD and SEM analyses suggest that the concentration of Al-O bands was mainly caused by the crystallization of ettringite.
The last noticeable absorption band is located at ~464 cm
−1 and characterizes the asymmetric bending vibration of Si-O-Si bands in various complicated silicate minerals and typically in C-S-H gels [
17,
18]. This absorption band became increasingly sharper from the dry mixture to the specimens cured for 3 to 7 to 28 days. This finding suggests that the total amount of C-S-H gel increased continuously, while other silicate minerals were being consumed.