3.2.1. Kinetic Model of PC Hydration
Park et al. [
12,
13] presented a kinetics model for the hydration reaction of PC to simulate the temperature distribution inside the concrete structures. The reaction coefficient of the initial dormant period, k
d, the effective diffusion coefficient of the water in the hydration product, D
e, and the coefficient of the reaction rate of the cement, k
r, were considered in this model. These coefficients determine the rate of the mass transport through the initial shell layer, the rate of the chemical reaction process, and the rate of the diffusion-controlled process in the hydration of PC. In the model, PC particles are assumed to be spherical, and the surface is surrounded by the hydration product. External water diffuses through the surface of the hydration products and reacts with the unhydrated PC particles to form a new hydration product (C-S-H gel). The main hydration model for PC is shown in Equation (7).
where α
c represent the reaction degree of PC; v represents the stoichiometric ratio by mass of water to PC; w
g represents the amount of physically bound water in hydrated cement, which typically ranges from 0.15 to 0.19; and ρ
c is the density of the PC. The values of v and w
g depend on the compound compositions of PC. In this study, fixed values of v = 0.25 and w
g = 0.15 were assumed, as referenced in [
17]. In Equation (8), C
wfree denotes the amount of capillary water at the exterior of hydration products, which is expressed as a function of hydration degree as follows:
where W
cap and W
0 are the content of the capillary water in hydrating concrete and the content of water in the concrete mixture; the terms (v + w
g) α
c P
c and 0.25 α
F P
F are the mass of capillary water consumed by PC hydration and FA reaction, respectively; the value of (v + w
g) = 0.4 represents the total chemically and physically bound water from PC hydration; the value of 0.25 represents the chemically bound water (=0.1 g/g FA) and gel water (=0.15 g/g FA), noting that it is assumed in Ref. [
16] that 0.25 g free water is needed for total reaction of 1 g of FA; P
c and P
F are the mass fractions of PC content and FA content in the mix proportion; and α
c and α
F are the degree of hydration of PC and the reaction degree of FA, respectively.
If an FA reaction (α
F) is not included in the analysis, the term 0.25 α
F P
F in Equation (8) will be equal to zero. However, this term will be used when analyzing the interactions between PC and FA reactions. In Equation (7), the PC particles were assumed to be spherical with uniform sizes and an average radius of r
c0 that can be obtained using the following equation [
10]:
where BF
c is the Blaine fineness (cm
2/g) and ρ
c is the density of PC.
The term S
w/S
0 in Equation (7) was first proposed by Navi and Pignat [
22,
23,
24,
25] to describes the decrease in the contact area between PC particles and ambient capillary. S
w is the effective contact surface area between the cement particles and capillary water. S
0 is the total surface area when the hydration products develop unconstrained, S
0 = 4πR
c2. The surface of the PC particles has enough water at the start of the hydration process for hydration to continue. The PC particles gradually develop as the hydration progresses and the contact areas between free water and hydration products depend on the volumes of hydration products. As the contact area between PC particles and the surrounding water decreases, the hydration rate drops because of the growing interconnections among particles. This effect was incorporated by Park et al. [
13] through the S
w/S
0 term.
The effective surface area between the free water and PC particle is shown in Equations (10a)–(10c). Equation (10a) accounts for the hydration products surrounding individual PC particles that are not in contact with each other, while Equation (10b) considers the hydration products around the particles that are in contact with each other. As the particles grow further, (10c) would apply.
where R
c represents the radius of the PC particle, including the outer hydration products, and is expressed as a function of the degree of hydration, α
c, and the rate of volume growth (the volume ratio between hydration products and the reacted PC), RVG. In Equation (11), the RVG was assumed to have a constant value of 2.0 [
13].
In this model, the PC paste is represented as spherical cement particles surrounded by water. Park et al. [
12] modeled the PC paste as a unit cell consisting of the unhydrated PC grains, gel, and capillary pores. The particles are dispersed in the water without making contact with one another. As illustrated in
Figure 3, the geometry of each particle and the surrounding water is formulated within a cubic unit cell, where the entire hydration process occurs. The length of the cube unit cell (l
c), the average radius of a PC particle (r
c0), the PC density, and the w/c ratio are related in Equation (12) as follows:
As mentioned previously, the model is represented by a single equation with three coefficients (k
d, D
e, and k
r). The reaction coefficient, k
d, describes the initial dormant period, during which an impermeable layer forms and subsequently breaks down. The hydration rate slows due to the formation of this layer but accelerates once the layer is disrupted. In this model, k
d is assumed to be a function of the degree of hydration.
where B and C are the rates of formation and breakdown of the initial impermeable layer, respectively. The term D
e in Equation (7) denotes the rate of PC hydration during the diffusion-controlled phase and is expressed in terms of the degree of hydration, Equation (14), where D
e0 is the initial diffusion coefficient.
The effect of curing temperature on the reaction coefficients is modeled according to Arrhenius’s law, as outlined in Equation (15) [
10].
where β
B, β
C, β
De and E
r/R denote temperature sensitivity coefficients, while B
20, C
20, D
e20, and k
r20 represent the respective values of B, C, D
e0, and k
r at T
r = 20 °C (293 K). The four parameters (B
20, C
20, D
e20, and k
r20) are related to the mineral components of PC [
17]. Wang showed that the B
20, C
20, D
e20, and k
r20 have a relationship with (C
3S + C
3A), C
3S, C
2S, and C
3S, respectively [
17]. These relationships are used in this study.
According to Park et al. [
13] and Maruyama [
14], the temperature sensitivity coefficients can be roughly regarded as constants for different PCs. Based on experimental data from various ATRs, Wang [
17] proposed the following values: β
B = β
C = 1000, β
De = 7500, and E
r/R = 5400. These values have been used in the analysis of this study.
3.2.2. FA Reaction Model
FA are silicate-based materials that react with Ca(OH)
2 produced by the hydration of PC to form cementitious hydration products such as C-S-H and C-S-A-H [
26]. Ca(OH)
2 plays a major role in the reaction of low-calcium materials such as FA in PC + FA blended binder systems, as it will consume Ca(OH)
2 to form additional C-S-H. The available amount of Ca(OH)
2 directly affects the dissolution rate of FA; this phenomenon has been reported in the literature. Wang and Lee [
16] revised the original shrinking-core model to determine the reaction of FA. Similarly to the PC hydration model, the FA reaction is expressed through a single equation involving three key coefficients (k
dF, D
eF, k
rF). In this analysis, both the PC hydration and FA reaction models are integrated to examine the interaction and overall reaction mechanism in PC + FA systems. The main FA reaction model is shown in Equation (17):
where
represents the reaction degree of FA; P
F is the mass of the FA in the mix proportion;
is the density of FA; mC
CH is the stoichiometric ratio of the mass of Ca(OH)
2 to FA, and it can be calculated using Equation (19b); and r
F0 is the radius of the FA particle.
is the mass of the Ca(OH)
2 in a unit volume of hydrating PC + FA blends and can be established as follows:
where the first term is for the hydration of PC and the second term is for the FA reaction; the terms (mP
CH·P
c·α
c) and (mC
CH·P
F·α
F) in Equation (18) are the mass of Ca(OH)
2 produced from PC hydration and the mass of Ca(OH)
2 consumed by the FA reaction, respectively; and the two factors in Equation (18), mP
CH and mC
CH, are the produced mass of Ca(OH)
2 from 1 g of hydrated PC and the consumed mass of Ca(OH)
2 by 1 g of reacted FA, respectively, and they can be calculated as Equations (19a) and (19b).
Here, P
C3S, P
C2S, and P
C4AF denote the weight fractions of the mineral phases C
3S, C
2S, and C
4AF in PC, respectively; P
FA is the mass fraction of fly ash in total cementitious materials. It is evident that the evolution of Ca(OH)
2 mass in the system depends on these two factors (mP
CH and mC
CH). The values in Equation (19a) were calculated based on the known stoichiometry of PC chemical reactions, as proposed in the literature. Wang [
27] derived Equation (19b) empirically by fitting Ca(OH)
2 consumption data reported by Lam et al. [
28], who studied cement–fly ash pastes across various water/binder ratios (0.19, 0.24, 0.30, and 0.50) and replacement levels (25%, 45%, and 55%). Lam et al.’s study is one of the few that provides both the degree of hydration and detailed Ca(OH)
2 consumption at various ages. Based on these data, Wang estimated the mass of Ca(OH)
2 consumed per one gram of reacted fly ash (mC
CH), values equal to 0.67, 0.53, and 0.46 for 25%, 45%, and 55% replacement, respectively. These values were then regressed against the corresponding replacement ratios P
FA = 0.25, 0.45, and 0.55, resulting in the linear form of Equation (19b).
As is well acknowledged, FA in blended PC reacts with Ca(OH)2, produced by the PC hydration reaction. Therefore, this study used the capillary water content calculated using Equation (8) and the Ca(OH)2 content calculated using Equation (18) in the hydrating system to consider the interactions between the reaction of PC and the reaction of FA.
To provide a chemically grounded alternative to Wang’s empirical model, this study developed a modified version of Equation (19b). The revised equation incorporates an expression based on the stoichiometric Ca(OH)
2 consumption of reactive silica and alumina in FA:
The terms (SiO
2)
active and (Al
2O
3)
active represent the active (reactive) fractions of silica and alumina in FA. Although these reactive components can be determined experimentally, this study estimated the reactive part of SiO
2 and Al
2O
3 based on the literature [
29]. The reactive fractions of SiO
2 and Al
2O
3 were estimated assuming 50% amorphous content based on the literature values for Class F fly ash [
29]. The constants 1.357 and 2.18 correspond to the molar ratios of Ca(OH)
2 consumed per mole of reactive SiO
2 and Al
2O
3, respectively, derived based on the pozzolanic reaction stoichiometry. For all the Class F fly ash used during this study, the amorphous value was assumed as 50% to calculate the weight fractions of (SiO
2)
active and (Al
2O
3)
active. The intercept value (0.845) was retained from Wang’s original model, representing the Ca(OH)
2 yield from full hydration of pure PC when there is no fly ash used. When Equation (19c) was applied, plotting mC
CH versus P
FA yielded a linear correlation similar to Wang’s [
27] model, highlighting the improved predictive capability of the stoichiometric model, which now depends on the chemical composition of the fly ash.
Similarly to the PC hydration model, the reaction rate coefficient in the dormant period, k
dF, the initial diffusion coefficient, D
eF, the reaction rate coefficient, k
rF, and the influence of the temperature on the FA reaction are described using Arrhenius’s law, as shown in Equations (20), (21) and (22a)–(22d).
where the β
BF = 6000 (K), β
CF = 6000 (K), β
DeF = 10,000 (K), and E
rF/R = 10,000 (K) are temperature sensitivity coefficients and B
F20, C
F20, D
eF20, and k
rF20 are the values of B
F, C
F, D
e0F, and k
rF at T
r = 20 °C (293 K).
3.2.3. Heat of Hydration
The heat from PC hydration and FA reaction can be obtained using the following Equation (23):
where H
c is ultimate heat of hydration of PC and can be calculated using Equation (24); H
1, H
2, H
3, H
4, H
5, H
6, and H
7 are the maximum heats of hydration of the individual mineral compounds in PC (J/g); P
C3S, P
C2S, P
C3A, P
C4AF, P
SO3, P
freeCaO, and P
MgO are the mass proportions for each chemical compound (%) of PC (the maximum heats of hydration of major mineral compounds in PC used in this analysis are shown in
Table 1); and H
F is the ultimate heat of reaction of FA.
Limited data is available for the ultimate heat of reaction of FA. Kichi and Maekawa [
30] reported a value of 209.0 J/g for a specific FA with 8.8 wt.% of CaO. Han et al. [
31] suggest a value of 285.0 J/g for their FA, obtained by analyzing the results for the heat of hydration of PC blended with FA. Waller [
32] proposed values for heat of reactions for the FA from experimental measurements where five different FAs were tested with Ca(OH)
2, and values of 522.0, 556.0, 569.0, 533.0, and 626.0 J/g were found (average = 560.0 J/g). Based on the thorough experiments carried out by [
32], it appears that these results are the most reliable to be used for FA; hence, H
F is assumed as 560.0 J/g.
The incremental temperature rise in one time step under adiabatic conditions can be determined between the ratio of the heat released and the specific heat (J/g °C) of SCMs as follows:
where the
is the mass density, while C
p(t) is the specific heat capacity of the hydrating concrete, which typically varies based on the degree of hydration of the cementitious materials and the temperature of the concrete. Water has an exceptionally high specific heat. The binding of water in hydration products reduces the specific heat of composite concrete [
2,
4,
33,
34]. In this study, the specific heat capacity of hydrating concrete can be calculated as the sum of the individual component of concrete as follows:
where W
c, W
F, W
S, W
A, and W
W are the mass of PC, FA, sand, coarse aggregate, and water per unit volume of concrete (kg/m
3). The specific heat of PC, FA, sand, coarse aggregate, chemically bound water, and water (C
c, C
F, C
S, C
A, C
cbm, and C
W) were assumed to be 740, 720, 710, 840, 2200, and 4184 (J/kg K), respectively.
The W
cbm in Equation (26) is the chemically bound water and can be determined using Equation (27). In the reaction of FA, the chemically bound water, gel water, and consumed Ca(OH)
2 per 1 g reacted FA were assumed to be 0.10 g, 0.15 g, 1.00 g, respectively [
35]. Therefore, the mass of chemically bound water in the reaction of FA is 0.1 g/g FA, and 0.25 g/g can be used to obtain the mass of chemically bound water in the cement reaction. As shown in Equation (27), both PC hydration and FA reaction contribute to chemically bound water.
The adiabatic temperature can be calculated with Equation (28):
The hydration model calculations were verified with experimental results conducted by Chen et al. [
4]. An ordinary PC (D-4) mix and a 30% fly ash (D-10) mix were chosen from [
4] to compare with the kinetic model described above. The concrete’s placement temperatures were 24 °C and 27 °C, respectively. The chemical compositions of the D-4 and D-10 concrete mixes are provided in
Table 2. The calculated Bogue compositions (mass fractions) for PC (D-10) are C
3S, C
2S, C
3A, and C
4AF are 57.63%, 14.41%, 7.68%, and 10.59%, respectively. Control coefficients for the hydration model are calculated based on the mass fractions of the major clinker phases of PC and given in
Table 3. The calibrated control coefficients of the FA reaction model used in this study were adopted from [
17] as a reference. The model was then calibrated using the experimental data of the available FAs, where similar coefficients (except DeF
20) were obtained (
Table 4). The mix designs and the measured properties of the D-4 and D-10 concrete mixes are given in
Table 5 and
Table 6, respectively. The FA reaction model was calibrated using isothermal heat data from a 70% PC + 30% FA mix (w/b = 0.5, cured at 23 °C), prepared using the same PC and FA materials for both the D-10 case and the case of this study. The ATR tests were conducted using different mix proportions: 70% PC + 30% FA for D-10 and 67% PC + 33% FA for this study. However, the isothermal calibration mix was identical in both cases. As a result, the same DeF
20 value was obtained for both cases. This consistency confirms that when the same materials and curing conditions are used in the isothermal test, the calibrated DeF
20 remains valid across different mix proportions used in subsequent ATR analyses.
It should be noted that the kinetic coefficients (kdF, DeF, krF) adopted from the literature may vary depending on the reactivity of individual fly ashes. Variations in amorphous content and fineness can influence diffusion and reaction rates. Based on comparisons with multiple published datasets, the uncertainty associated with parameter transferability is estimated to be within ±5–10%, which is acceptable for practical ATR prediction accuracy.
The kinetic model was programmed using MATLAB R2018a (MathWorks, Natick, MA, USA), with a time step of 0.2 h. Prior to simulating the ATR behavior of both the PC (D-4) and PC + FA (D-10) mixes, the isothermal heat of hydration was calculated using the model. The reaction of FA was determined using Equation (23). Constant FA parameters were established by calibrating the model against experimental isothermal hydration heat results. For each FA, one mixture was used for calibration, as shown in
Figure 4. These parameters remained constant regardless of FA/PC replacement level, w/b ratio, or temperature. In Equation (24), a fixed value of 1.0% was assumed for
for all the PC, and the heat contribution from P
MgO was considered negligible heat contribution during the first seven days.
A reasonably good agreement between the model predictions and experimental results was obtained, as shown in
Figure 4a, enabling ATR simulations of these mixes. This experimental testing was conducted using the TAM Air isothermal calorimeter (TA Instruments), following ASTM C1679 standard procedures. This instrument, equipped with eight parallel twin measurement channels, was used to investigate the hydration kinetics. For comparison, the heat of hydration of 100% PC in the D-10 mix was also calculated and included in
Figure 4a, alongside that of the D-4 mix. Although D-10 and D-4 differ in chemical and physical properties and were both cured at 23 °C, they exhibited nearly identical heat evolution behavior under their respective conditions.
Additionally, experimental heat of hydration was measured for the 70% PC + 30% FA mix of this study at different curing temperatures (23 °C, 33 °C, and 43 °C) under isothermal conditions. The corresponding model-predicted heats of hydration were also calculated and presented in
Figure 4b.
Figure 5a shows a parameter study of PC + FA concrete for the D-10 mix (30 wt.% FA) in adiabatic conditions. The individual reaction degrees of PC and FA concretes are shown in
Figure 5a. Based on these individual reaction degrees, the heat contributions from PC hydration and FA reaction were calculated.
Figure 5b shows the respective heat contributions, where their sum represents the total heat of hydration. As expected, the heat released from PC hydration is significantly higher than that of the FA reaction. The heat contributions from the FA reaction reached about 50.0 J/g after 7 days (about 21% of the total heat), which reflects the slow short-term pozzolanic reaction of FA, constituting 30% of the total cementitious materials.
It is observed that the degree of reaction of FA in D-10 is slightly higher than that reported for FA in this study mix shown in
Figure 5c,d. Similarly, the degree of hydration of cement in D-10 proceeds slightly faster, particularly within the first 24 h, which can be attributed to the higher curing temperature (27 °C for D-10 versus 21 °C in this study mix). When applying Equation (24), it becomes evident that the chemical composition of the cement also influences the total heat of hydration: D-10 generates 288.4 J/g at 168 h, compared to 275.2 J/g for the cement used in the present study mix. Furthermore, the calculated maximum heat of hydration of cement (H
C) using Equation (24) yielded values of 448.0 J/g for the PC in D-10 and 435.0 J/g for the PC in the present study mix.
For comparison,
Figure 5e includes the individual reaction degrees of PC and FA based on a mix reported in Wang’s study [
17], in which the mix design comprised 75% PC and 25% FA, cured at a temperature of 20 °C. Notably, the water/binder (w/b) ratio used in Wang’s mix was very low (0.25), which significantly influenced the reaction kinetics. As a result, the reaction degrees of both PC and FA, as well as the total heat evolution, were much lower than those observed in the D-10 mix and in the current study mix. The heat generated at 168 h in Wang’s mix was 177.4 J/g, while the calculated maximum heat of hydration of cement (H
C), based on Equation (24), was 447.6 J/g. The analysis of all three mixes is presented together in
Figure 5 to highlight the influence of curing conditions and mix design parameters.
The lower ATR observed in [
17] is attributed to the reduced internal moisture availability in low w/b mixes (0.25). Insufficient capillary water limits the diffusion of ions and restricts the hydration of both PC and FA, resulting in slower reaction rates and lower total heat evolution compared to mixes with moderate w/b ratios.
The analytical and experimental results are compared in
Figure 6. The results demonstrate a close alignment between the model’s predictions and experimental observations.
Figure 6a shows the comparison between analytical and experimental results for the 100% PC (D-4) case, and
Figure 6b shows the results for the 70% PC + 30% FA (D-10) case. Besides the analytical and test data for the 70PC + 30FA case in
Figure 6b, the analytical results for 100PC (100% PC—no FA) for D-10 PC, along with 70% of that 100PC, are plotted to explain FA contribution in the ATR. The analysis results in
Figure 6b show that without FA (100PC case), the ATR reached 70.5 °C. With 30 wt.% FA replacement, the ATR of 70PC + 30FA case decreased to 65.1 °C. The ATR of the 70% of 100PC is 57.5 °C at 200 h. The contribution of FA can be explained by the 7.6 °C difference between the curves of 30% FA and 70% of 100PC. In general, replacing 30 wt.% of the PC with FA decreased the ATR to approximately 8% of the D-10 100PC mix (without FA), which is a positive result. The close match between the model predictions and experimental data supports the reliability of the multi-scale model. This suggests that the model is capable of simulating the ATR for both ordinary PC and FA mixes with reasonable accuracy.
A sensitivity analysis of the proposed method was performed by varying the DeF
20 with three different values (3 × 10
−15, 9 × 10
−15, and 15 × 10
−15 cm
2/h), and comparing with the experimental data of the D-10 mix (70% PC + 30% FA) with a w/b ratio of 0.496 and cured at 27 °C, shown in
Figure 6b. The results in
Figure 7 display the adiabatic temperature rise (ATR). As shown in the figure, varying DeF
20 affected the ATR. At 200 h, the corresponding ATR values were 62.6 °C, 65.1 °C, and 66.5 °C for those different DeF
20 values, respectively. In this simulation, DeF
20 was the only parameter altered, while all other input parameters remained constant (as shown in
Table 4). This demonstrates that DeF
20 has a significant influence on the fly ash reaction rate. As its value increases, the reaction accelerates, leading to a higher heat release and a greater temperature rise. It is reasonable to see a benefit for future application; when simulating the ATR of a PC + FA mix is of interest with a typical Class F fly ash where the chemical composition of the fly ash is similar to those used in the cases of D-10 and this study, DeF
20 can be assumed a constant of 9 × 10
−15 cm
2/h.