3.1. Effect of water cement ratio on frost heaving stress
The trends in low-temperature frost heaving stress for grout materials with different water-cement ratios under freeze-thaw cycling conditions, as depicted in
Figure 3a, demonstrate that as the grout materials transition from room temperature to a 5 °C low-temperature curing phase, frost heaving stress rapidly decreases and remains stable. This behavior can be attributed to the volumetric contraction of the grout material when it shifts from room temperature to a lower temperature, resulting in a reduction and stabilization of frost heaving stress. The graph reveals that all grout materials, regardless of water-cement ratio, exhibit initially high frost heaving stress during the first cycle. Grout materials with lower water-cement ratios experience a substantial reduction in frost heaving stress and enter a negative stress pattern (the frost heaving stress after freezing is less than that after thawing) after a limited number of freeze-thaw cycles. Specifically, for water-cement ratios of 0.24, 0.26, 0.28, and 0.30, the duration of frost heaving is 1, 2, 3, and 4 cycles, respectively. However, with a water-cement ratio of 0.32, the grout material consistently maintains high frost heaving stress and an extended duration of frost heaving, even retaining relatively high frost heaving stress during the 6th freeze-thaw cycle. The trends in setting time and free water content variations in the grout material (as depicted in
Figure 3c) demonstrate a significant correlation between both setting time and free water content at different stages of freeze-thaw cycles with the water-cement ratio.
Additionally, there is a positive relationship between the free water content at various stages of freeze-thaw cycles and the frost heaving pressure, with higher free water content associated with greater frost heaving stress. Notably, when the free water content in the grout material falls below the critical threshold (approximately 11.5%), the stress mode transitions to a negative stress pattern. These observations can be explained by several primary factors. As the water-cement ratio increases, the spacing between solid particles in the grout material widens, the setting rate slows down, and defects in hydration products become more prominent. Consequently, this leads to extended setting times and increased free water content in the grout material. Under the influence of freeze-thaw cycles, both the initial cycle maximum frost heaving stress (σ
1-max) and the duration of frost heaving cycles (T
d) exhibit an increasing trend. However,
Figure 3d also reveals that as the water-cement ratio decreases, the fluidity of the grout material declines, particularly with a significant decrease in the 30-minute fluidity. When the water-cement ratio reaches 0.26, both the 30-minute standard fluidity and low-temperature fluidity of the grout material exceed 30 seconds, making it difficult to carry out normal grouting construction.
Moreover, the results also indicate a clear downward trend in both the standard strength of the grout materials and the compressive strength after freeze-thaw cycles (as
Figure 3e shows) with an increasing water-cement ratio. However, the decrease in compressive strength after freeze-thaw cycles is more pronounced compared to the standard compressive strength. Notably, when the water-cement ratio reaches 0.32, there is a significant drop in compressive strength after freeze-thaw cycles, with the residual compressive strength falling to less than one-third of the standard strength.
Figure 3f provides insight into the composition of the final hydration products of the grout materials, which predominantly consist of a significant amount of calcium hydroxide(CH), a certain quantity of ettringite, C-S-H, and a small amount of mullite. Increasing the water-cement ratio does not lead to the formation of new crystalline phases in these hydration products, and except for a slight decrease in the intensity of the C-S-H peak, there are minimal changes in other crystalline phases. Additionally,
Figure 3g reveals optical and SEM images after freeze-thaw cycles, showing the emergence of numerous micro and macro cracks in the hydration products of the grout materials. As the water-cement ratio increases, both the number and width of these cracks intensify, serving as a primary reason for the accelerated decline in compressive strength after freeze-thaw cycles. Furthermore, the frost heaving stress curve indicates that the residual frost heaving stress in the grout material is slightly higher than the initial stress and cannot fully return to the initial stress level. This effect is particularly pronounced when the water-cement ratio reaches 0.32, and as freeze-thaw cycles progress, the residual frost heaving stress exhibits a linear growth trend, closely related to cracking in the grout material induced by freeze-thaw cycles.
Figure 3.
Effect of water cement ratio on frost heaving stress.
Figure 3.
Effect of water cement ratio on frost heaving stress.
Figure 4 demonstrate 2 characteristic patterns of frost heaving stress: the freeze-expansion/thaw-shrink pattern (FETS pattern, as
Figure 4a shows) and the freeze-shrink/thaw-expansion pattern (FSTE pattern, as
Figure 4b shows). In the FETS pattern, during the initial freezing phase, frost heaving stress undergoes a brief linear decrease followed by a rapid linear increase until it peaks. It then transitions into a slow, nonlinear growth before gradually declining linearly until the freezing process concludes. During the melting phase, frost heaving stress experiences a transient logarithmic increase followed by a rapid linear decrease. After reaching its peak, it transitions into a slow increase until the melting process concludes. Analyzing the temperature fluctuations in the environmental chamber and specimen surface (as shown in
Figure 2d), these patterns are primarily a result of the grout material’s gradual linear contraction due to rapid cooling from 5 °C, causing a brief linear decrease in frost heaving stress. Upon reaching the freezing point, the coupled effect of free water freezing expansion and grout material shrinkage leads to near-linear growth in frost heaving stress. Once the pipe temperature stabilizes, the nearly complete crystallization of free water results in a slowed, nonlinear growth in frost heaving stress. Upon reaching its peak, the continued freezing induces slight shrinkage in the grout material, accompanied by a linear decrease in frost heaving stress. As the environmental temperature rises, rapid melting of ice crystals leads to gradual volume recovery in the grout material, resulting in a rapid linear decrease in frost heaving stress. Upon returning to normal temperature, accelerated hydration reactions in the grout material cause slight volume expansion and a minor increase in pipeline stress.
Figure 4.
Two characteristic frost heaving stress patterns.
Figure 4.
Two characteristic frost heaving stress patterns.
The distinctive features of the FSTE pattern can be outlined as follows: during the freezing process, the frost heaving stress undergoes a two-stage rapid reduction. The first stage is characterized by a linear decrease, followed by a second stage of nonlinear reduction, reaching a peak and maintaining stability until the freezing process concludes. Once the thawing process begins, the frost heaving stress exhibits a three-stage rapid increase. The first stage involves linear growth, followed by a second stage of nonlinear growth, and finally, a third stage of linear growth persists until the end of the thawing process. The primary rationale behind this model can be explained as follows: when the free water content in the grout material decreases to the frost expansion threshold, the grout material gradually contracts as it cools, resulting in a linear decrease in frost heaving pressure. When the ambient temperature drops below the freezing point of free water, the coupling of the expansion caused by the freezing of free water and the contraction due to the cooling of the grout material leads to nonlinear volume contraction, accompanied by a corresponding decrease in frost heaving stress. Once the temperature stabilizes, the volume of the grout material remains constant, and the expansion pressure also remains stable until the freezing process’s conclusion. Upon the initiation of the warming process, the grout material containing ice expands linearly as the temperature rises, resulting in a linear increase in frost heaving stress. Once the temperature surpasses the freezing point, the coupling of the contraction induced by the melting of free water and the expansion due to the warming of the grout material leads to nonlinear expansion (accompanied by a corresponding nonlinear increase in frost heaving stress). After the complete melting of free water, the grout material expands linearly as the temperature continues to rise, accompanied by a corresponding linear increase in frost heaving stress.
3.2. Effect of calcium formate on frost heaving stress
As
Figure 5a illustrates, the addition of calcium formate can effectively reduce the initial maximum frost heaving stress of the grout material and shorten the duration of frost heaving cycles (Td). When the calcium formate content is at or below 0.3%, the first and second frost-thaw cycles exhibit a typical FETS pattern, while the third frost-thaw cycle follows a typical freezing-shrinking-frosting pattern. However, when the calcium formate content reaches 0.4%, only the initial low-temperature frost heaving stress curve adheres to the freezing-shrinking pattern. The second low-temperature frost heaving stress curve remains stable with frost heaving stress approaching zero, and subsequent frost-thaw cycles adopt a typical FSTE pattern, with frost heaving stress becoming negative stress pattern.
From
Figure 5b and
Figure 5c, it is apparent that the incorporation of calcium formate into the grout material effectively reduces both ambient and low-temperature setting times. Notably, it significantly shortens the initial setting time of the grout material. Additionally, it has a moderating effect on the free water content within the grout material, with setting time and free water content gradually decreasing as the calcium formate content increases. As shown in
Figure 5d, an increase in calcium formate content leads to a slight reduction in the initial flowability of the grout material, with a substantial decline observed at the 30-minute mark. Importantly, when the calcium formate content reaches 3%, the 30-minute low-temperature flowability consistently exceeds 30 seconds. In
Figure 5e, it is demonstrated that increasing calcium formate content results in gradual improvements in both the standard and low-temperature compressive strength of the grout material. The standard compressive strength reaches its peak at 2% calcium formate content, while the freeze-thaw cycle compressive strength peaks at 3% calcium formate content. Analyzing the XRD spectra of the grout material after freeze-thaw cycling in
Figure 3f, it becomes apparent that the addition of calcium formate leads to a significant increase in the crystalline phases of C-S-H and ettringite, with no new crystalline phases formed. Furthermore, as shown in
Figure 5g, an increase in calcium formate content corresponds to a reduction in the quantity, width, and damaged areas of internal cracks within the grout material. This signifies a notable attenuation of freeze-thaw damage, which is a direct consequence of the enhanced compressive strength observed with higher calcium formate content. These phenomena primarily result from the introduction of calcium formate, which raises the concentration of Ca
2+ ions in the liquid phase, accelerating the dissolution rate of C-S-H. Simultaneously, a substantial quantity of HCOO
- is introduced, and due to its faster diffusion rate compared to Ca
2+, HCOO- penetrates the hydration layers of C
3S and C
2S, speeding up the precipitation of Ca(OH)
2 and the decomposition of calcium silicate [
25]. This, in turn, promotes the formation of C-S-H and ettringite. Furthermore, HCOO
- can chemically react to further cross-link adjacent silicate groups, facilitating the formation of C-S-H gel [
26,
27]. The combined effect of the high concentration of Ca
2+ and HCOO
- accelerates the participation of free water in hydration reactions, enhances early strength development, and reduces the susceptibility of the grout material to freezing.
Figure 5.
Effect of calcium formate on frost heaving stress.
Figure 5.
Effect of calcium formate on frost heaving stress.
3.3. Effect of sulphoaluminate cement on frost heaving stress
The incorporation of sulphoaluminate cement(SAC), as depicted in
Figure 6a, is observed to effectively reduce the frost heaving duration of the grout material. Following the initial cycle, all specimens transitioned from a frost heaving-shrinking mode to a freezing-shrinking-frosting mode. The maximum frost heaving stress during the first cycle exhibited a decreasing trend with increasing SAC content. In
Figure 6b, it is evident that the addition of SAC in the grout material significantly shortens the setting time, with a gradual reduction in setting time corresponding to higher levels of cement addition.
Figure 6c illustrates a comparison of free water content during various cycles, it becomes apparent that the incorporation of SAC into the grout material also leads to a significant reduction in free water content during each cycling period. After the initial freeze-thaw cycle, the free water content in all dosage levels of the grout material decreases to the frost heaving threshold or below. Additionally,
Figure 6d reveals a slight enhancement in initial fluidity with increasing SAC content. However, at SAC content equal to or exceeding 10%, the fluidity drastically declines after 30 minutes at low temperatures, exceeding 30 seconds. Due to the loss of plasticity, grout materials lose their flowability, rendering them unsuitable for grouting applications.
Figure 6.
Effect of sulphoaluminate cement on frost heaving stress.
Figure 6.
Effect of sulphoaluminate cement on frost heaving stress.
The primary factor contributing to the aforementioned phenomena is the incorporation of SAC into the grout material, which introduces a significant quantity of anhydrous calcium sulfoaluminate. This compound rapidly consumes a substantial portion of free water, promoting the rapid hydration of the grout material and the production of a considerable amount of ettringite. As a consequence, early strength development in the grout material is accelerated. In the later stages of hydration, both types of cement mutually facilitate the formation of denser hydrated compounds, resulting in improved mechanical strength [
28,
29]. Additionally, the rapid hydration reaction of SAC generates a substantial amount of heat [
29], which can expedite the rate of hydration reactions in the grout material, particularly when the ambient temperature returns to normal.
3.4. Effect of air-entraining agents on frost heaving stress
Figure 7a depicts the changing pattern of frost heaving stress in air-entrained grout materials under low-temperature conditions. The graph unequivocally illustrates that the addition of air-entraining agents results in a notable decrease in both the the initial cycle maximum frost heaving stress (σ
1-max) and the duration of frost heaving cycles (T
d) in the grout material. The frost heaving stress model exhibits distinct the FETS pattern and the FSTE pattern. Specifically, when the air-entraining agent content is 0.05%, the initial maximum frost heaving stress measures 2.50kN, and the frost heaving cycle occurs three times. With a progressive increase in the air-entraining agent content, the initial maximum frost heaving stress experiences a gradual and substantial reduction, accompanied by a decrease in the frost heaving cycle. For instance, at an air-entraining agent content of 0.20%, the initial maximum frost heaving stress diminishes to a mere 0.05kN, and the frost heaving cycle occurs only once.
By comparing the experimental results of free water content at various stages (as
Figure 7b shows) and the setting time of grout materials (as
Figure 7c shows), it becomes evident that the inclusion of an air-entraining agent does not exert a significant influence on these parameters. Additionally,
Figure 7d illustrates that the impact of the air-entraining agent on grout materials is relatively minor, with flowability showing a trend of initial reduction followed by an increase as the agent dosage increases. As depicted in
Figure 7e, the introduction of an air-entraining agent gradually diminishes the mechanical strength of the materials under standard curing conditions. However, under freeze-thaw cycling conditions, a moderate amount of air-entraining agent can enhance the mechanical strength of the grout materials to a certain extent. Nonetheless, when the dosage of the air-entraining agent surpasses 0.2%, the compressive strength of the grout materials experiences rapid deterioration during freeze-thaw cycling.
Figure 7f reveals that the air-entraining agent has no discernible impact on the crystalline phase composition of hydration products in grout materials, with minimal changes in the content of CH, C-S-H, and ettringite. However, examination of macro/microscopic images of grout materials (as
Figure 7g shows) demonstrates a significant influence of the air-entraining agent on the macrostructure of the hydration products. With an increase in the air-entraining agent dosage, the formation of macroscopically visible closed air voids within the grout materials increases, while macroscopic damage areas, macroscopic cracks, and the number and width of microscopic cracks decrease. This phenomenon can be primarily attributed to the introduction of a substantial volume of structurally stable, fine, and persistent bubbles by the air-entraining agent in the grout materials. These bubbles serve to mitigate the volume expansion occurring during free water crystallization, alleviate freeze-thaw pressures, and reduce structural damage, thereby mitigating the adverse effects of freeze-thaw cycling on the structure and strength of grout materials [
30,
31,
32,
33,
34].
Figure 7.
Effect of air-entraining agents on frost heaving stress.
Figure 7.
Effect of air-entraining agents on frost heaving stress.
3.5. Effect of carbamide on frost heaving stress
The trend of frost heaving stress variation in carbamide-added grout materials under low-temperature conditions is depicted in
Figure 8a. The graph clearly illustrates that the addition of carbamide significantly reduces frost heaving stress during the freeze-thaw cycles. At a carbamide content of 0.1%, the change in frost heaving stress under low-temperature freeze-thaw cycles follows a pattern similar to the typical FETS pattern. However, with the introduction of carbamide, the initial frost heaving stress in the grout material increases slowly during the early freezing stages, reaching a minimal value, and experiences rapid attenuation during the early melting phases. As the carbamide content further increases, the heterogeneity in frost heaving stress during the grout material’s freezing stages intensifies. The first maximum frost heaving stress gradually grows, and the duration of frost heaving extends. When the carbamide content surpasses 0.2%, the initial frost heaving stress exhibits a linear growth pattern, reaching peak upon the first freezing termination. It continues to follow the frost-expansion even after three consecutive freeze-thaw cycles, and the frost-thaw stress difference diminishes with the elongation of the freeze-thaw cycles. From
Figure 8b and
Figure 8c, it is evident that incorporating carbamide into the grout material does not accelerate the setting time or reduce free water content. On the contrary, the addition of carbamide leads to an increase in both setting time and free water content as the carbamide content rises. The results of flowability tests for carbamide-added grout materials (
Figure 8d) show a slight improvement in flowability after the addition of carbamide, although the overall impact is relatively minor.
As illustrated in
Figure 8e, the standard compressive strength of the grout material shows a marginal increase with the introduction of carbamide. The peak compressive strength is reached at a carbamide content of 1.5%. However, under the influence of freeze-thaw cycles, the compressive strength reaches its maximum at a carbamide content of 0.5%, gradually declining as the carbamide content continues to rise. From the XRD patterns in
Figure 8f), it is evident that the hydration products within the grout material undergo some changes with the incorporation of carbamide. The peak intensity of C-S-H exhibits a moderate increase with increasing carbamide content, and new product phases appear around 2θ=56°.
Figure 8g provides macroscopic and microscopic images of the grout material, indicating that the addition of a small quantity of carbamide results in a reduction in both the number and width of macro and micro cracks, as well as a decrease in the level of damage. However, as the carbamide content increases further, the number and width of cracks expand, and the degree of damage intensifies. Simultaneously, the inclusion of carbamide within the grout material leads to the formation of visible macroscopic closed pores.
Figure 8.
Effect of carbamide on frost heaving stress.
Figure 8.
Effect of carbamide on frost heaving stress.
In contrast to the above characteristic patterns, the introduction of carbamide led to a distinctive alteration in frost heaving stress, characterized by two heteromorphosis patterns: linear growth pattern (LG pattern, as shown in
Figure 9a) and non-linear growth pattern (NLG pattern, as illustrated in
Figure 9b). The NLG pattern closely resembled the freeze-thaw expansion-shrinkage model. Its distinctive features were as follows: during the initial freezing phase, frost heaving stress displayed a noticeable linear decrease until reaching a nadir, followed by a rapid non-linear growth until it peaked. Subsequently, the stress exhibited a gradual decline until the freezing process concluded. During the thawing stage, frost heaving stress rapidly decreased in a linear manner initially, transforming into a slow linear growth until the thawing process concluded. These patterns were correlated with the temperature fluctuations in the environmental chamber and the surface temperature of the pipeline, as depicted in
Figure 2d. The primary reasons for these patterns were as follows: the grout material experienced rapid cooling, causing contraction and resulting in continuous linear reduction of frost heaving stress. When the temperature of the grout material dropped below freezing, the combination of freezing expansion of free water and the grout material’s contraction due to freezing led to non-linear continuous growth of frost heaving stress, reaching its peak after complete crystallization of free water. Subsequently, due to continuous freezing of the grout material, volume contraction occurred until the freezing stage ended. As the temperature rose, rapid melting of ice crystals ensued, gradually restoring the grout material’s volume. carbamide facilitated faster ice crystal melting, leading to a swift linear decline in frost heaving stress. After complete ice crystal melting, the material underwent accelerated hydration reactions, causing volume expansion and resulting in slow linear growth of frost heaving stress.
Figure 9.
Two heteromorphosis frost heaving stress patterns.
Figure 9.
Two heteromorphosis frost heaving stress patterns.
The characteristics of the LG pattern are as follows: at the beginning of the freezing process, there is a noticeable linear decrease in frost heaving stress, succeeded by a rapid linear increase until the freezing process concludes. During the thawing process, frost heaving stress experiences an extremely rapid linear decline, reaching a peak before transitioning into a slow linear increase until the thawing process concludes. These patterns are observed in conjunction with the temperature variation curves of the environmental chamber and pipeline surface (as shown in
Figure 8d). The primary factors driving this behavior include the grout material’s gradual rapid cooling from 5℃, leading to contraction and a distinct linear decrease in frost heaving stress. As the grout material’s temperature drops below freezing, frost heaving occurs due to the expansion caused by the freezing of free water, combined with the grout material’s freezing-induced contraction. The intensification of the freezing process results in a continuous linear increase in frost heaving stress until the freezing stage concludes. This phenomenon is attributed to the high carbamide content, which delays setting time, increases free water content, lowers the freezing point of free water, and decelerates free water crystallization. Upon warming, ice crystals melt rapidly, leading to gradual volume recovery of the grout material and a swift linear decrease in frost heaving stress. Once the ice crystals within the grout material completely melt, resulting in the lowest volume contraction, frost heaving stress peaks. Subsequently, accelerated hydration reactions due to complete thawing and self-heating result in slow volume expansion, leading to a gradual linear increase in frost heaving stress.
3.6. Effect of compound agents on frost heaving stress
As demonstrated in the preceding five sections of this paper, it is evident that reducing the water-to-cement ratio or incorporating additives like calcium formate and sulfoaluminate cement can partially reduce the frost heaving stress and frost heaving duration of grout materials under freeze-thaw cycling conditions. However, due to their distinct mechanisms of action, achieving the desired comprehensive performance for grout materials in construction remains challenging. Therefore, in this section, we adopt a combined approach involving calcium formate, sulfoaluminate cement, carbamide, and air-entraining agents to enhance grout materials. Detailed experimental results are presented in the subsequent sections.
Figure 10a illustrates the variation trend of frost heaving stress in grout materials containing composite additives under low-temperature conditions. The graph clearly demonstrates that the incorporation of composite additives effectively reduces both the initial cycle maximum frost heaving stress (σ
1-max) and the duration of frost heaving cycles (T
d) in the grout material. With lower admixture content, the grout material exhibits a frost heaving pattern only during the initial freeze-thaw cycle. However, the maximum frost heaving stress during this cycle significantly diminishes compared to the blank sample, accompanied by a distinct deformation in its stress pattern. When the composite additive content reaches 9.9%, the grout material experiences no frost heaving stress during the initial freeze-thaw cycle.
Figure 10b,c reveal that the introduction of composite additives leads to effective reductions in low-temperature setting time and free water content in the grout material, owing to the combined effects of calcium formate and sulfoaluminate cement. At composite additive contents of 9.9% and 13.2%, the co-action of carbamide and air-entraining agents transforms the frost heaving stress pattern into a freeze-shrink-thaw mode, even when the free water content in the grout material exceeds the critical moisture level before the initial freeze-thaw cycle.
Figure 10d shows that the incorporation of composite additives also diminishes the flowability of the grout material. When the content reaches 13.2%, the 30-minute low-temperature flowability slightly exceeds 30 seconds, but the grout material in this state still complies with the requirements for grouting construction.
Figure 10e indicates that the addition of composite additives results in a gradual increase in the standard compressive strength of the grout material, with a substantial improvement in compressive strength after freeze-thaw cycles. At a composite additive content of 9.9%, the residual strength after freeze-thaw cycles exceeds 85%. From the XRD spectra of hydration products in
Figure 10f, it can be observed that with an increase in composite additive content, the content of ettringite and C-S-H in the grout material’s hydration products significantly increases, while the content of calcium hydroxide (CH) decreases. Additionally, as the composite additive content rises, new phase products (around 2θ=56°) also form in the hydration products.
Figure 10g reveals that under the influence of freeze-thaw cycles, an increase in composite additive content leads to a reduction in macroscopic/microscopic cracks within the grout material, decreased structural damage, and an increase in the number of macroscopic pores. In summary, compared to other singly modified grout materials, composite additives demonstrate superior freeze resistance even at lower contents due to the combined effects of calcium formate, sulfoaluminate cement for early strength and rapid setting, air-entraining agents for freeze-thaw resistance, and carbamide for reducing the crystallization point of ice. At a content of 9.9%, composite additives can already exhibit a negative frost heaving stress pattern during the initial freeze-thaw cycle.
Figure 10.
Effect of composite additives on frost heaving stress.
Figure 10.
Effect of composite additives on frost heaving stress.