3.2. Rheology of Geopolymer Coatings
The plastic viscosity and yield stress are indicative of the slurry's rheological characteristics, reflecting its ability to resist flow under external shear forces[
31,
32,
33].
Figure 5a depicts the shear stress‒shear rate (τ-γ) curve for the alkaline activator. At a shear rate of 0 s
-1, the shear stress is likewise 0 s
-1. Subsequently, the shear stress of the alkaline activator increases linearly with the shear rate, suggesting Newtonian fluid behavior[
12].
Figure 5b presents the shear stress‒shear rate (τ-γ) and dynamic viscosity-shear rate (η-γ) curves of GPC-D0-0.5. The upward trend of the shear stress demonstrated shear-thinning behavior, while the downward trend was approximately a straight line, exhibiting a linear increase with increasing shear rate. The dynamic viscosity of the geopolymer coating decreases rapidly at low shear rates (γ ≤ 20 s
-1) and then remains constant. Therefore, the freshly mixed geopolymer coating slurry behaves as a pseudoplastic fluid with shear-thinning characteristics. An appropriate mathematical model is crucial for quantifying the rheological parameters of a slurry. The data from the downcurve of the shear stress‒shear rate curve were selected for rheological analysis[
34], and the geopolymer coating adheres to the typical Bingham model (Eq. 1)[
35]:
where τ is the shear stress (Pa), τ
0 is the yield stress (Pa), η
0 is the plastic viscosity (Pa·s), and γ is the shear rate (s
-1).
Figure 6 illustrates the influence of diatomite on the rheology of the geopolymer coatings. All the samples exhibit shear-thinning behavior, as shown in
Figure 6a. As the diatomite concentration increases, the viscosity of the geopolymer coating initially rises and then declines. At high shear rates (γ≥ 20 s
-1), the viscosity stabilizes due to internal gel structure rupture. The Bingham model (Eq. 1) was employed to fit the shear stress‒shear rate curve of the geopolymer coating, with the fitting results depicted in
Figure 6b and summarized in
Table 3. A high correlation coefficient (R
2≥0.98) between shear stress and shear rate for the geopolymer coating suggests that the yield stress and plastic viscosity can adequately describe its rheological behavior.
Figure 7 illustrates the impact of diatomite and its concentration on the rheological properties of geopolymer coatings using rheological fitting curves. With an increase in diatomite concentration, the rheological parameters of the geopolymer coatings initially rise, followed by a subsequent decrease. Notably, at a diatomite concentration of 1.1%, there was a significant increase in the rheological parameters of the geopolymer coatings. Comparative analysis between GPC-D0-0.5 and GPC-D1.1-0.5 revealed remarkable increases of 420.5% and 41.9%, respectively, in yield stress and plastic viscosity. Diatomite notably surpasses slag and fly ash in specific surface area, with values of 4000 m
2/kg, 425 m
2/kg, and 350 m
2/kg, respectively, and demonstrates heightened water adsorption capabilities due to its larger specific surface area[
36,
37]. This reduces the free water content within the geopolymer coating slurry, attenuating the lubricating effect of water, increasing the frictional resistance of solid particles, and consequently reducing the slurry's flowability[
38]. However, the disc-like configuration of diatomite engenders a mesh structure between particles in the geopolymer coating slurry, augmenting the overall viscosity of the mixture. The elevated yield stress of GPC-D1.1-0.5 results in heightened resistance to gravitational forces, coupled with elevated viscosity at lower shear rates, showcasing exemplary sag resistance. Nonetheless, with an excessive concentration of diatomite (wt.%>1.1%), the yield stress and plastic viscosity of the geopolymer coatings exhibit a decreasing trend. The smooth, non-angular morphology of diatomite particles reduces interparticle friction, enhancing the coating's flowability and reducing rheological parameters, thereby diminishing sag resistance.
Thixotropy, another common parameter for characterizing the rheological performance of coatings, is determined by the hysteresis loop area formed in the shear rate-shear stress rheological curve during the upstroke and downstroke[
38]. In
Figure 7, the hysteresis loop area is observed to increase and then decrease with increasing diatomite concentration. Integrating the aforementioned rheological performance test results,
Figure 8 presents a model illustrating the internal structural variations in geopolymer coatings at different diatomite concentrations during the upstroke and downstroke phases. Based on the shear rate-shear stress rheological curve, in GPC-D0-0.5, as the shear rate gradually increases, unhydrated precursor particles are uniformly dispersed in the slurry. When the shear rate decreases, the collision time between these precursor particles increases, generating a minimal flocculation structure and thereby forming a small hysteresis loop. The introduction of diatomite alters the internal structure of the geopolymer coating, creating a multiscale network structure of diatomite-precursors, precursor-precursors, and diatomite-diatomite. As the shear rate increases, the network structure is disrupted; however, as the shear rate gradually decreases, the partially disrupted network structure rearranges, reverting to a state similar to that during the upstroke. At a diatomite concentration of 1.1%, the reduced free water in the geopolymer coating slurry leads to an increased collision frequency of particles, resulting in an augmented hysteresis loop area. Conversely, at a diatomite concentration of 2.0%, the rheological properties of GPC-D2.0-0.5 deteriorate. As the shear rate increases, diatomite aggregates are less prone to dispersion, precursor particles are enveloped, and a limited structure is disrupted. During a decrease in shear rate, aggregated diatomite particles compress each other, arranging themselves in the slurry in a specific pattern. The energy required for the slurry to restore flow is lower than that for GPC-D1.1-0.5, resulting in a reduction in the hysteresis loop area.
Based on the rheological tests mentioned above,
Figure 9 illustrates the sag resistance of geopolymer coatings applied to vertical substrates. Compared to GPC-D0-0.5, the addition of diatomite significantly boosts the yield stress of geopolymer coatings, thus enhancing sag resistance. Within the coating thickness range of 400 to 500 μm, the sag resistance of geopolymer coatings fluctuates depending on the concentration of diatomite, initially increasing before decreasing. Specifically, GPC-D1.1-0.5 and GPC-D1.4-0.5 demonstrated moderate sag resistance in comparison to the remaining samples. In this thickness range, the yield stress of the coating surpasses gravitational stress, effectively preventing sagging and ensuring the stability and uniformity of the coating. Even with a coating thickness of 600 μm, GPC-D1.1-0.5 maintains exceptional sag resistance, whereas GPC-D1.4-0.5 displays a noticeable edge effect. As layer thickness and diatomite concentration increase, the coating progressively flows, taking on a "curtain" or "teardrop" shape. In this range of thickness, gravitational stress exceeds yield stress, causing an uneven distribution of the coating and significantly affecting its uniform coverage and protective performance on concrete.
3.3. Water Retention Capacity and Setting Time Tests
Figure 10 shows the results of the water retention capacity and setting time tests for freshly mixed geopolymer coating slurries. Through centrifugation, the volume of free water in freshly mixed geopolymer coating slurries with the same mass was obtained, as shown in
Figure 10a. As diatomite concentration increases, the volume of free water in the geopolymer coating system decreases gradually. The weight loss of free water follows a similar trend, as depicted in
Figure 10b. For the geopolymer coating with a diatomite concentration of 1.1%, the weight loss at 60 minutes was 2.21%, a reduction of 54.8% compared to that of GPC-D0-0.5. However, at a diatomite concentration of 2.0%, the weight loss was only 0.33%, significantly lower than the blank group's loss of 4.89%. The unique hollow and porous structure of diatomite can absorb free water in the geopolymer system and store it inside the particles, greatly enhancing the water retention performance and slowing the early-stage water loss during geopolymer coating hydration. However, during the 30-50 minute interval, geopolymer coatings containing diatomite experience rapid weight loss, with GPC-D0.8-0.5 exhibiting a mass loss rate of 1.08% within this range. This difference may be attributed to diatomite participating in the hydration reaction of the geopolymer, leading to the dissolution of amorphous SiO
2 and the disruption of the internal pore structure of diatomite, thereby reducing the water retention performance[
39] and disrupting the internal pore structure of diatomite, thereby reducing the water retention performance.
The water retention capability of diatomite also enhanced the setting and drying times of the geopolymer coatings.
Figure 10c demonstrates the changes in setting time for geopolymer coatings with varying diatomite concentrations. The initial and final setting times for GPC-D0-0.5 were 22 minutes and 30 minutes, respectively. A shorter setting time can adversely impact the practical utility of geopolymer coatings, potentially constraining their deployment in real-world engineering scenarios[
40,
41]. With increasing in diatomite concentration, both the initial and final setting times of the geopolymer coatings significantly increase. When the diatomite concentration was 1.1%, the initial and final setting times of the geopolymer coatings increased to 46 min and 58 min, respectively. With further increases in diatomite concentration, the setting time stabilizes.
The drying time also influences the practical engineering of geopolymer coatings[
1,
42]. The drying time of geopolymer coatings is influenced by both environmental factors, such as temperature, humidity, and ventilation, and the reaction rate of the raw materials used in the coating. In this study, we rigorously controlled for the impact of environmental factors on drying time, eliminating their consideration.
Figure 10c shows the results of the geopolymer coating drying time tests. The diatomite particles envelop the surface of precursor particles, reducing the contact between water molecules and slag-fly ash particles and thereby slowing the hydration rate of slag and fly ash. As the diatomite concentration increases, the hydration rate decreases, resulting in prolonged surface drying and overall drying times for the coating.
3.4. Mechanical Properties of Geopolymer Coatings
The bonding strength and surface hardness, crucial performance indicators for coatings, effectively reflect the protective effect of geopolymer coatings on concrete structures. The interfacial bonding between geopolymer coatings and concrete arises from physicochemical interactions at the contact surfaces between phases[
43,
44,
45,
46,
47].
Figure 11a illustrates the bond strength of geopolymer coatings with varying diatomite concentrations at curing ages of 3 days, 7 days, and 28 days. The incorporation of diatomite significantly enhances the bond strength of geopolymer coatings, showing an initial increase followed by a decrease with rising diatomite concentration. Furthermore, during the 3-7 days curing period, the bonding strength of GPC-D1.1-0.5 showed the most rapid increase, reaching 106.09% of the blank group's value. However, concentrations of diatomite exceeding 1.1% had a detrimental effect on the development of bond strength in the geopolymer coatings. At 28 days, GPC-D2.0-0.5 exhibited a bonding strength of only 1.85 MPa, a 21.9% reduction compared to that of GPC-D1.1-0.5.
Figure 11b shows the surface hardness test results for the geopolymer coatings. At 12 hours, the surface hardness of the geopolymer coatings with added diatomite was lower than that of the blank group. However, after curing for 1 days, the trend in the change in surface hardness aligns with that in bond strength. The surface hardness of geopolymer coatings with diatomite concentrations of 0.8%, 1.1%, and 1.4% surpasses that of the blank group. After 28 days of curing, GPC-D1.1-0.5 exhibited the highest surface hardness at 9 H, surpassing the other experimental groups and the blank group. Combining the bond strength test results, the addition of 1.1% diatomite yields the optimal enhancement in the mechanical properties of geopolymer coatings.
Due to the numerous internal pores in geopolymer coatings, diatomite can act as a fine aggregate filler[
26]. Initially, due to its higher water absorption, an increase in diatomite concentration results in higher adsorption of free water, thereby slowing down the progress of geopolymer hydration reactions[
48]. This delay resulted in the surface hardness of the geopolymer coatings with added diatomite being lower than that of the blank group. As the curing age increases, diatomite participates in the alkali-activated secondary hydration reaction[
39], generating additional C-(A)-S-H gel phases and interconnecting internally into a cohesive structure, thereby enhancing the mechanical properties in the later stages of hydration.
3.5. The Enhancement Mechanism and Reaction Process of Diatomite
The microscopic morphological changes in diatomite during the geopolymer hydration reaction of GPC-D1.1-0.5 are illustrated in
Figure 12. In the initial stages of the hydration reaction, the slag and fly ash particles within the geopolymer coating amalgamate with diatomite particles via face-to-face contact, forming aggregates. The interconnected porous structure of diatomite persists, offering a substantial internal surface area. After 5 minutes of the hydration reaction, diatomite particles undergo expansion due to water absorption. This stage results in a reduction in the free water content within the geopolymer coating system, leading to enhanced rheological properties. After 10 minutes of the hydration reaction, the surface structure of diatomite starts to erode under alkaline conditions, with internal active substances engaging in the geopolymer hydration reaction alongside mineral powder and fly ash particles. This leads to an increase in the content of C-(A)-S-H gel phases. In comparison to the early stages of hydration, the interactions between particles within the aggregate structure intensify significantly, resulting in a denser gel phase structure. By 12 hours, the structure of diatomite undergoes complete disruption, and by 1 day, it fully reacts and integrates into the geopolymer gel phase network.
The isothermal calorimetry method provides as an effective means to elucidate the various reaction stages in the geopolymerization process.
Figure 13 illustrates the heat evolution of geopolymer coatings with varying diatomite concentrations. As shown in
Figure 13a, the exothermic rate curve of the geopolymer coatings displayed five stages analogous to the hydration process of cement, including the initial hydration stage, the induction period, the acceleration period, the deceleration stage and the steady-state period[
49]. Sagging in geopolymer coatings primarily occurs during the initial hydration stage. During the early stages of initial hydration, the GPC-D0-0.5 sample displayed the first peak (Ⅰ) at 0.15 hours, primarily due to the combined effects of early wetting and dissolution. The second peak (Ⅱ) emerges at 0.73 hours, coinciding with the setting time test results, indicating that GPC-D0-0.5 reaches the initial setting at this point. This peak results from further dissolution and polymerization of geopolymer materials, marking the initiation of the induction stage of geopolymer coating hydration. During the early stages of initial hydration, the heat release rates of GPC-D0.8-0.5 and GPC-D1.1-0.5 are 10.52% and 11.03%, respectively, higher than those of the blank group. This suggests that the inclusion of a small quantity of diatomite can facilitate the wetting and dissolution of active substances during the initial stages of geopolymer material hydration, thereby augmenting the formation of the C-(A)-S-H gel phase within the geopolymer coating. These hydrated gel phase structures tend to aggregate under van der Waals forces and electrostatic forces, resulting in an increase in the yield stress, plastic viscosity, and thixotropy of the geopolymer coating, thus enhancing its sag resistance.
Concurrently, the incorporation of diatomite prolonged the occurrence time of peaks Ⅰ and Ⅱ. However, with diatomite concentration surpassing 1.1%, the occurrence time of peaks Ⅰ and Ⅱ decreased even further. At this juncture, diatomite absorbs a significant amount of free water within the geopolymer material, thereby retarding the dissolution rate of active substances in the initial stages of hydration. Inadequate wetting and dissolution of slag and fly ash particles lead to reduced formation of C-(A)-S-H gel phases and diminished sag resistance. The heat release rate of GPC-D2.0-0.5 reached its peak at 0.32 hours, reaching 16.35%, which was significantly greater than that of the other samples. Combining the SEM and water retention capacity results, at this stage, the porous structure of diatomite begins to break down, releasing a substantial amount of absorbed free water into the geopolymer material [
50], thereby accelerating the wetting and dissolution of slag and fly ash particles.
In the acceleration phase of hydration, due to the polymerization and hardening of the geopolymer coating, GPC-D0-0.5 manifested a third peak (Ⅲ) around 33 hours. With the inclusion of diatomite, peak Ⅲ emerged roughly 15.5 hours earlier than in the control group. Additionally, the total heat release results (
Figure 13b) suggest that incorporating diatomite increases the hydration heat released by the geopolymer coating. Geopolymer coatings containing 1.1% and 2.0% diatomite exhibit almost identical total heat release curves in the first 17.5 hours, representing increases of 66.95% and 66.68%, respectively, compared to GPC-D0-0.5. GPC-D1.1-0.5 demonstrated a 59.18% increase in total heat release at 70 hours compared to GPC-D0-0.5. The main reason for this phenomenon is the participation of a significant amount of active SiO
2 from diatomite in the secondary hydration reaction, increasing the quantity of hydration products. Simultaneously, the internal silica provides additional nucleation sites[
51], accelerating the polymerization of silicon and aluminum monomers in the middle of geopolymer hydration.
To further investigate the structural evolution and development patterns of the gel phase in geopolymer coatings with diatomite, we utilized the DTG curves and mass loss obtained through thermogravimetric analysis, as depicted in
Figure 14.
Figure 14a shows the DTG curves and mass loss test results of the geopolymer coatings at the initial setting time for the different diatomite concentrations. A primary peak appears in the range of 25-200 °C and is attributed to the dehydration of the C-(A)-S-H gel that formed during the geopolymerization process. According to the DTG curve, the thermal stability of the geopolymer coatings in this temperature range can be divided into two intervals. The first interval, with a mass loss primarily below 100 °C, is mainly attributed to the evaporation of free water within the gel structure of the geopolymer material[
52]. The second interval, within 100-200 °C, represents the mass loss of bound water within the gel structure[
53]. Compared to those of GPC-D0-0.5, the geopolymer coatings with 1.1% and 2.0% diatomite exhibit increases of 84.63% and 85.78%, respectively, in terms of the mass loss of free water and increases of 78.41% and 28.19%, respectively, in terms of the mass loss of bound water. The increase in free water loss corroborates the enhancement in the water retention capability of the geopolymer coatings due to diatomite, consistent with the results of the tests mentioned in section 3.3. An increase in the mass loss of bound water indicates an increase in the quantity of hydration products within the coating. Simultaneously,
Figure 14a
2 indicates that with increasing diatomite content, the maximum weight loss temperature of the geopolymer coatings first increases and then decreases. GPC-D1.1-0.5 achieved a maximum weight loss temperature of 80.53 °C, surpassing the other groups. During the heating process of geopolymer materials, the increased content of the gel phase and its more complex, disordered, and denser structure enhance thermal stability. This results in an elevated saturation vapor pressure of water, consequently raising the temperature at which weight loss occurs for the samples[
52,
54]. Therefore, in the early stages of hydration, GPC-D1.1-0.5 exhibited increased disorder in the internal structure of the gel phase, augmented rheological parameters, and enhanced resistance to sagging.
Figure 14b and c depict the DTG curves and mass loss of GPC-D0-0.5 and GPC-D1.1-0.5 at 1, 3, 7, and 28 days. During the same curing period, the geopolymer coating with 1.1% diatomite exhibited greater weight loss than its counterpart without diatomite as the temperature rose from 25 °C to 900 °C. With the extension of curing time, an increase in mass loss within the range of 25-200 °C is observed, accompanied by a slight shift of the maximum weight loss temperature toward higher temperatures. This further confirms that the inclusion of diatomite facilitated and contributed to the polymerization reaction, elucidating the enhancement in the mechanical properties of the geopolymer coatings.