XRD analysis of the hydration and carbonation reaction
Fig. 2 shows the XRD patterns of LFS samples (< 38 μm) hydrated and carbonated at different temperatures and of LFS samples of different particle sizes after reaction at 20 ℃. The results confirm that LFS is an alkaline solid waste material composed mainly of silicate minerals, such as CS, C2S, and C3S, with additional amounts of calcium hydroxide Ca(OH)2 and anorthite (CaAl2Si2O8). After the hydration and carbonation reaction processes, the diffraction peaks of the calcium silicate phases were decreased or even disappeared. Simultaneously, three diffraction peaks appeared at around 2θ = 28.5°, 31.2°, and 61.2°, which were assigned to C-S-H gel 16-19, indicating that the calcium silicate phases formed C-S-H gel during the hydration and carbonation reaction. As C2S and C3S are known to undergo hydration reactions20, C2S and C3S present on the surface of LFS particles can undergo hydration to form C-S-H gel in the early stage of the reaction. As the reaction progresses, the C-S-H gel releases Ca2+ to maintain the required alkaline environment21, resulting in decalcification of the C-S-H gel. CO2 gas was continuously passed through the solution to generate H2CO3 of weak acidity, which is extremely unstable and rapidly ionize in solution to generate HCO3- and CO32-. The free Ca2+ in the solution combines with CO32- to form stable CaCO3. C-S-H gel will eventually provide more Ca2+ than the present Ca(OH)2 when cement paste is exposed to high concentrations of CO222, Finally, Ca2+ in CaCO3 mainly originates from the hydration product C-S-H gel, and since the presence of moisture is a necessary condition to initiate the carbonation reaction23, 24, hydration will occur before the carbonation reaction. The XRD spectra in Fig. 2 indicate the formation of large amounts of CaCO3 in the reaction at different temperatures or different LFS particle sizes, indicating that the main product after carbonation was CaCO3. As CS cannot undergo a hydration reaction11, 25, 26, the CS present on the surface of LFS particles does not form C-S-H gel in the early stage of the reaction, but instead directly combines with CO32- in solution to form CaCO3. In addition, the diffraction peaks for CaAl2Si2O8) did not change significantly following the hydration and carbonation reaction, indicating that the anorthite structure was relatively stable and did not participate in the reaction process, which is consistent with the results observed by Ashraf27. With the increase in reaction temperature, the CaCO3 diffraction peaks gradually decrease, which may be due to faster movement of CO2 molecules and expansion of the volume, resulting in an increase in the distance between the molecules of CO2 and H2O, weakening the intermolecular forces and hindering the generation of CO32-28. In addition, the increase in temperature also causes the solubility of CO2 to gradually decrease29, which ultimately leads to a reduction in carbonation efficiency. With the decrease in particle size, the diffraction peaks of the calcium silicate phases and Ca(OH)2 gradually decrease, which might be explained by the simultaneously increasing surface area enhancing the contact area between particles and the solution which is conducive for the rate of the occurring reactions. However, a considerable amount of calcium silicates and Ca(OH)2 did not participate in the hydration and carbonation reaction at the largest particle size of LFS, resulting in an incomplete reaction.
TG-DTG analysis of the hydration and carbonation reaction
Table 2. Changes in mineral phase composition determined by TG and RIR at different hydration and carbonation reaction temperatures or particle sizes
Carbonation periods
|
Uncarbonated
|
20 °C
|
40 °C
|
60 °C
|
80 °C
|
96-180 μm
|
48-96 μm
|
38-48 μm
|
<38 μm
|
TG(%)
|
CaCO3
|
-
1.9
-
-
|
24.7
|
25.1
|
24.6
|
18.0
|
1.0
|
20.0
|
21.8
|
24.7
|
Total
|
35.2
|
35.2
|
34.4
|
27.3
|
2.1
|
29.2
|
32.9
|
35.2
|
RIR(%)
|
CaCO3
|
23.0
|
22.9
|
23.1
|
23.3
|
6.3
|
18.0
|
19.2
|
23.0
|
C2S, C3S
|
26.0
|
32.5
|
34.8
|
52.6
|
64.4
|
32.4
|
26.0
|
26.0
|
Fig. 3 shows the TG-DTG diagram of LFS after hydration and carbonation under different reaction temperatures or when different particle sizes were used. The mass losses are divided into three temperature ranges of 100-300 °C, 300-500 °C, and 500-850 °C, which are attributed to the dehydration of C-S-H gel and Ca-deficient C-S-H gel, the dehydration of Ca(OH)2, and the decarbonization of CaCO330, respectively. In the case of dry weight, the mass loss over the entire temperature range is referred to as the total mass loss. The mass of CaCO3 can be obtained from the CO2 content generated by CaCO3 decarbonization31. The weight-loss peak appearing in the range of 300-500 °C prior to the hydration and carbonation reaction may be caused by the formation of Ca(OH)2 due to the combination of calcium-based components of LFS with atmospheric water under natural conditions. Two weight-loss peaks appeared in the range of 100 -300 °C and 500-850 °C after the hydration and carbonation reactions.
Table 2 lists the results of CaCO3 and t otal mass loss measured by TG at different reaction temperatures or when different particle sizes were used, showing that the mass of CaCO3 decreases with the increase in temperature or in particle size. The content of CaCO3, C2S, and C3S was calculated by adopting the reference intensity ratio (RIR) method. Results show that, as the temperature decreases, the content of C2S and C3S reduces, indicating that increasing amounts of C2S and C3S participated in the hydration reaction stage and that, under the effect of carbonation, C-S-H gel continuously participates in the carbonation reaction stage further promoting the hydration reaction, while a reaction temperature of 20 °C is more advantageous to the occurrence of the carbonation reaction. With the increase in particle size, the content of C2S and C3S increase, possibly because C2S and C3S in LFS require longer leaching channels to participate in the hydration reaction. Furthermore, this also negatively affects the later carbonation reaction, that is, increasing particle size is not conducive to the further occurrence of the carbonation reaction.
SEM-EDS analysis of the hydration and carbonation reaction
Table 3. Elemental content of EDS areas (%)
Samples
|
C
|
O
|
Al
|
Si
|
Ca
|
20 °C
|
17.3
|
57.8
|
8.3
|
2.3
|
14.3
|
40 °C
|
21.7
|
56.7
|
6.0
|
1.1
|
14.6
|
60 °C
|
30.5
|
47.8
|
3.1
|
0.7
|
18.0
|
80 °C
|
15.7
|
55.1
|
5.3
|
1.0
|
23.0
|
96-180 μm
|
7.2
|
54.6
|
11.4
|
2.0
|
25.8
|
48-96 μm
|
7.7
|
56.0
|
7.6
|
1.0
|
23.3
|
38-48 μm
|
12.7
|
55.7
|
5.8
|
3.1
|
22.8
|
<38 μm
|
17.3
|
57.8
|
8.3
|
2.3
|
14.3
|
Fig. 4 shows the SEM images of LFS following hydration and carbonation at different temperatures and when using samples of different particle sizes, Fig. 5 shows the schematic diagram of the microstructure mechanism of hydration and carbonation of a slag particle, and Table 3 lists the average elemental content of these areas according to energy-dispersive X-ray spectroscopy (EDS). As shown in Fig. 4, after hydration and carbonation, a large amount of C-S-H gel was formed with rough surfaces and a coagulated or fibrous form (indicated by the red area in Fig 4), as well as CaCO3 crystals such as calcite with a cubic structure (indicated by the blue area in Fig 4) 32, 33. As the reaction temperature increases, more voids are visible in the structure. As the particle size of the LFS increases, the amount of calcite gradually decreases, and the LFS surface is covered by C-S-H gel and Ca-deficient C-S-H gel (indicated by the green area in Fig 4). When the particle size is 96-180 μm, the hydration product Ca(OH)2 is present in the form of hexagonal flakes (indicated by the yellow area in Fig 4). These results could be attributed to the cementitious properties of C2S and C3S, which cause a hydration reaction to form C-S-H gel and Ca(OH)2. During carbonation, the C-S-H gel is decalcified to form Ca-deficient C-S-H gel and CaCO3. Furthermore, Ca(OH)2 directly reacts with CO32- in solution to form CaCO3. As illustrated in Figure. 5, the carbonation products CaCO3 and Ca-deficient C-S-H gel adhere to the surface of the reaction phase, and the entire structure becomes dense and thus inhibits the diffusion of Ca2+ into the solution, which eventually prevents the further progress of the reactions. According to the results in Table 3, the reaction products are mainly composed of C, O, Al, Si, and Ca. The content of Ca gradually increases with the increase in temperature or particle size, indicating that the decalcification degree of the C-S-H gel gradually decreases, and that the concentration of Ca2+ ions leached into solution decreases, further reducing the formation of CaCO3. As a result, increasing temperature or particle size is detrimental to the hydration and carbonation reaction.
Microstructure of the cementitious substances in the hydration and carbonation reaction
Table 4. Range of 29Si NMR chemical shifts of Qn structural units in silicate
Types
|
Chemical shift/ppm
|
Q0
|
﹣68—﹣76
|
Q1
|
﹣76—﹣82
|
Q2
|
﹣82—﹣88
|
Q3
|
﹣88—﹣98
|
Q4
|
﹣98—﹣129
|
Table 4 shows the 29Si NMR chemical shift range of Qn structural units in silicates34, while Fig. 6 shows the 29Si NMR spectra following hydration and carbonation of LFS at different temperatures or when using different LFS particle sizes. In NMR analysis, Q0 represents an isolated SiO4 tetrahedra, Q1 often appears at the end group of a straight chain, Q2 mostly appears as a middle group of a straight chain, Q3 has a double-stranded polymer structure or a layered structure, and Q4 represents a SiO4 tetrahedra connected to four SiO4 tetrahedra, in a three-dimensional network structure35. As shown in Fig. 6, the main peak of uncarbonated LFS is Q0, with a few Q1 peaks appearing around -79 ppm, which may be due to the formation of C-S-H gel by C2S and C3S hydration under natural conditions. After the hydration and carbonation reactions, Q2, Q3, and Q4 peaks are present.
Table 5. Results of 29Si NMR spectra deconvolution following LFS hydration and carbonation at different reaction temperatures or particle sizes
Samples
|
Unhydrated
|
C-S-H gel
|
|
Ca- deficient gel
|
Ld
|
H(%)
|
Pol
|
Q0(%)
|
Q1(%)
|
Q2(%)
|
|
Q3(%)
|
Q4(%)
|
Uncarbonated
|
93.8
|
6.2
|
-
|
|
-
|
-
|
0
|
6.2
|
0
|
20 °C
|
-
|
7
|
-
|
|
20.3
|
72.7
|
13
|
100
|
0.9
|
40 °C
|
6.7
|
-
|
18.1
|
|
51.4
|
23.8
|
4
|
93.3
|
0.8
|
60 °C
|
6.4
|
-
|
26.3
|
|
40.5
|
26.8
|
3
|
93.6
|
0.7
|
80 °C
|
46.8
|
-
|
26.9
|
|
-
|
26.3
|
1
|
53.2
|
0.5
|
96-180 μm
|
85.2
|
-
|
9.1
|
|
-
|
5.7
|
0.6
|
14.8
|
0.4
|
48-96 μm
|
-
|
48.6
|
-
|
|
46.6
|
4.8
|
1.1
|
100
|
0.5
|
38-48 μm
|
-
|
25.8
|
16.8
|
|
21.1
|
36.3
|
1.3
|
100
|
0.6
|
<38 μm
|
-
|
7
|
-
|
|
20.3
|
72.7
|
13
|
100
|
0.9
|
Table 5 lists the calculated deconvolution results from 29Si NMR analysis. No Q3 and Q4 peaks are present before the hydration and carbonation reactions, indicating that it is more difficult to complete the C2S and C3S hydration and carbonation reaction under natural conditions. After the hydration and carbonation reactions, the content of Q0 gradually decreases or even disappears, and the Q2 peak appears, indicating that at this point C2S and C3S begin to participate in the reaction under the action of the hydration reaction, resulting in the formation of C-S-H gel with longer chain lengths. Since the Si atom radius is smaller than the Ca atom radius, the bond length of the Si-O bond is shorter than that of the Ca-O bond, resulting in the bond energy of the Si-O bond being greater than that of the Ca-O bond. Furthermore, Si has weak non-metal properties, making it difficult to form ions alone in compounds. Therefore, as the reaction time increases, the Ca-O bonds in the C-S-H gel gradually break under the action of the carbonation reaction, and the decalcification of the C-S-H gel results in Ca2+ combining with CO32- in solution to form CaCO3. After decalcification, the C-S-H gel is negatively charged due to the loss of Ca2+. To maintain the charge balance, H+ in solution is adsorbed by the C-S-H gel and combines with the broken Si-O- to form -Si-OH via protonation, which subsequently undergoes a condensation reaction with the adjacent -Si-OH. This condensation increases the mean silicate chain length and forms bridges between neighboring regions, thus pulling them closer together and causing shrinkage. This results in the formation of the Q3 and Q4 structures of Ca-deficient C-S-H gel with longer chain lengths and a higher degree of polymerization. CS is composed of chains of SiO4 tetrahedra (Q2), which can directly form CaCO3 during the carbonation process11, 36. Equations (1), (2), and (3) are used to express the degree of decalcification (Ld), the degree of polymerization (Pol) of the C-S-H gel, and the degree of hydration (H) of C2S and C3S, respectively5, 37, as follows:

While H reflects the degree of C2S and C3S hydration, Ld reflects the degree of separation of Ca2+ in the C-S-H gel, Pol reflects the degree of re-polymerization of the SiO4 tetrahedra after decalcification of the C-S-H gel. According to the results in Table 5, the ratio of Ca-deficient C-S-H gel to the remaining C-S-H gel did not change significantly in the temperature range of 40-80 °C and at particle sizes from 38 μm to 180 μm, and the decalcification degree of C-S-H gel remained low. When the reaction conditions included a temperature of 20 °C and LFS particle sizes of <38 μm, Ld was significantly increased to 13, indicating that more Ca2+ leached into solution, leading to more carbonation in the rapid carbonation phase. Fig. 7 shows H and Pol at different reaction temperatures and different particle sizes, indicating that, as the reaction temperature increases, both parameters exhibit a decreasing trend. This may occur as the reaction products cover the reaction phase surface, preventing further contact between water and the reaction phase, which ultimately inhibits the process of hydration. Furthermore, increasing the reaction temperature reduces the solubility of CO2, thereby inhibiting the carbonation reaction. The observed trend in Pol was negatively correlated with the particle size, and the reason for this analysis may be that with the decrease in particle size, the -Si-OH groups in Ca-deficient C-S-H connect more easily with adjacent Si-OH groups to form bridges and thus polymerize, thereby accelerating the carbonation reaction; released Ca2+ combines with CO32- in solution to form CaCO3, which will lead to a decrease in Ca2+ concentration; according to Kurdowski's theory, a low concentration of Ca will accelerate the hydration reaction of C2S and C3S and generate more C-S-H gel and Ca-deficient C-S-H gel to participate in the carbonation reaction. Therefore, the carbonation reaction promotes the hydration reaction.