3.4.1. Pore structures
MIP results of AAC and hardened aerated concrete (HAC-5) were shown in Fig. 9. Cumulative pore volume increased with the increase of MCS content in AAC, and the cumulative pore volume of the HAC-5 is less than the final AAC-5. The pore size of AAC-1 is mainly distributed around 50 nm, and it increased with the increase of MCS. The pore size of AAC-1 is mainly distributed at about 50 nm, and the pore size increases with the increase of MCS. The pore size of AAC-4 and AAC-5 is mainly distributed at about 100 nm, and the pore size of HAC-5 is mainly distributed at about 100 nm and 3000 nm. The porosity and pore distribution of AAC and HAC-5 calculated through MIP datas in Fig. 9 are shown in Fig. 10. Porosity of AAC increased from 62.9–63.4%, 63.6%, 63.7% and 63.9%, respectively, with the increase of MCS content from 0–25%, 50%, 75% and 100%. Air voids (above 10000 nm) and mesopores (10–50 nm) content decreased while macropores (50-10000 nm) increased in this case. In summary, the increase of MCS in AAC increased the macropores and porosity of AAC, which is consistent with the test results of physical properties. The increase of porosity will increase the thermal conductivity of AAC and decrease the mechanical properties. After HAC-5 was cured in autoclave (216°C, 2 MPa) for 8 hours to form AAC-5, the porosity increased from 57.9% (HAC-5) to 63.9% (AAC-5), air voids and macropores content decreased while mesopores increased. The results show that in the process of high-pressure curing, the hydrated products fill the large pores of the matrix, which refine the pores of the matrix, and the matrix also forms additional pores due to hydration reaction.
3.4.2. Mineral compositions
XRD patterns of AAC and HAC-5 were shown in Fig. 11. Tobermorite, quartz, katoite, anhydrite and calcite are the main minerals in AAC. MCS has no effect on the mineral phase types of AAC. The amount and crystallinity of tobermorite have a significant impact on all aspects of AAC properties (Matsui et al. 2011; Isu et al. 1995; Mostafa 2005), which is the most important crystallization product of AAC. It can be seen from Fig. 11 (b) that the crystallinity of tobermorite in AAC-5 is high, that is, AAC-5 sample has good physical and mechanical properties and thermal conductivity. The characteristic diffraction peaks of AAC-1 and AAC-5 mineral phases are consistent, as shown in Fig. 11(a). The main mineral phases of hac-5 are quartz, kuzelite, ettringite and portland. Quartz is the mineral phase of fly ash, and kuzelite, ettringite and portland are formed by hydration reaction in the early stage of HAC. At 216 ℃ and 2MPa, after autoclave curing for 8 hours, the characteristic peaks of kuzelite, ettringite and portland mineral phases in HAC-5 disappeared, and the characteristic peaks of tobermorite, katoite, anhydrite and calcite appeared. This is because under high pressure conditions, AFt, C-S-H gel, gypsum and silicate hydration products in HAC-5 react in autoclave reaction, and finally convert to tobermorite, katoite and anhydrite. During the formation of tobermorite, katoite and anhydrite in the system, heat will be released, new pores will be generated in the matrix and the porosity of the matrix will be improved. This is consistent with MIP results.
TG and DTG curves of AAC-5 and HAC-5 are shown in Fig. 12. In HAC-5 the main weight loss is located at about 100°C (C-S-H gels dehydrated), 120°C (AFt dehydrated) and 450°C (Ca(OH)2 dehydroxylated) (Luo et al. 2019; Luo et al. 2020), respectively. As shown in Fig. 12(b), the main weight loss of AAC-5 is at about 50–300 ℃ (the loss of adsorbed water and bound water) (Cai et al. 2021), 100–350°C (tobermorite dehydrated) and 850°C (exothermic transformation of tobermorite into β- wollastonite), 400°C (katoite decomposed) (Jiang et al. 2021), 750°C (calcite decomposed). Under high pressure conditions, AFt, C-S-H gel, gypsum and silicate hydration products in HAC-5 react in autoclave reaction, and finally convert to tobermorite, katoite and anhydrite. The results are consistent with the XRD results.
Figure 13 shows the morphology of HAC-5 (a, c) and AAC-5 (b, d). There were a small amount of dense plate products (A), gelatinous (B), needle-stick (C), bamboo leaf (D), regular hexagonal shape (E), filamentous (F) and irregular block (G) products in the samples. EDS data of the labeled area in Fig. 13 are shown in Table 3. In HAC-5, the gelatinous and filamentous products containing Ca, Si and Al can be identified as C-S-H, the dense plate products can be identified as Ca(OH)2, the needle-stick products can be identified as AFt. HAC-5 was mainly composed of C-S-H gel, AFt and Ca(OH)2. In AAC-5, the bamboo leaf products can be identified as tobermorite, the regular hexagonal shape products can be identified as CaCO3, the irregular block products can be identified as katoite. At 216 ℃ and 2MPa, after autoclave curing for 8 hours, AAC-5 was mainly composed of tobermorite, CaCO3, and katoite. This is because under high pressure conditions, AFt, C-S-H gel, gypsum and silicate hydration products in HAC-5 react in autoclave reaction, and finally convert to tobermorite and katoite. SEM and EDS data were consistent with TG and XRD results.
Table 3
EDS datas of red areas in SEM images
Area | Element, Atomic % |
O | Mg | Al | Si | Ca | S |
A | 62.87 | 0.60 | 0.48 | 2.24 | 33.81 | - |
B | 55.04 | 0.51 | 0.31 | 15.31 | 28.83 | - |
C | 62.84 | 0.31 | 7.50 | 0.45 | 26.30 | 2.60 |
D | 53.79 | - | 4.05 | 20.94 | 21.12 | - |
E | 74.26 | 0.02 | 0.01 | 0.09 | 25.62 | - |
F | 78.37 | - | 0.99 | 4.80 | 15.84 | 0.01 |
G | 75.23 | 0.02 | 6.05 | 3.15 | 14.2 | 1.35 |