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Article

A Block Triple-Relaxation-Time Lattice Boltzmann Method for Solid–Liquid Phase Change Problem

1
School of Mathematics and Statistics, Hunan First Normal University, Changsha 410205, China
2
School of Physics and Electronic Science, Changsha University of Science and Technology, Changsha 410114, China
3
School of Mathematics and Statistics, Changsha University of Science and Technology, Changsha 410114, China
*
Author to whom correspondence should be addressed.
Mathematics 2024, 12(12), 1815; https://doi.org/10.3390/math12121815
Submission received: 18 May 2024 / Revised: 1 June 2024 / Accepted: 7 June 2024 / Published: 11 June 2024
(This article belongs to the Special Issue Computational Fluid Dynamics of Heat Transfer and Applications)

Abstract

:
This study introduces a block triple-relaxation-time (B-TriRT) lattice Boltzmann model designed specifically for simulating melting phenomena within a rectangular cavity subject to intense heating from below, characterized by high Rayleigh ( R a ) numbers ( R a = 10 8 ). Through benchmark testing, it is demonstrated that the proposed B-TriRT approach markedly mitigates numerical diffusion along the phase interface. Furthermore, an examination of the heated region’s placement is conducted, revealing its significant impact on the rate of melting. Notably, findings suggest that optimal melting occurs most rapidly when the heated region is positioned centrally within the cavity.

1. Introduction

The study of thermal flow problems involving phase changes holds paramount importance for both academic inquiry and practical engineering applications. Phase change processes entail intricate thermodynamic phenomena, presenting numerous academic challenges. Among these, the solid–liquid phase change problem stands out due to its widespread occurrence in various engineering domains. Applications such as latent heat thermal energy storage [1,2], battery thermal management [3,4], etc., all play significant roles in modern industry [5].
The investigation of melting phenomena within rectangular enclosures has been the subject of numerous analytical, numerical, and experimental inquiries. Notably, Chen et al. [6] devised a solid–liquid phase change model tailored to simulate phase changes within porous media. Chiappini [7] introduced a hybrid LB-FV methodology to address phase change material dynamics and showcased its versatility across various scenarios. Additionally, the thermal characteristics of phase change materials, encompassing solidification and melting processes, were computationally elucidated through a multi-physics solver. Rui et al. [8] explored natural-convection-induced melting within square cavities, developing an enthalpy-based lattice Boltzmann model integrated with the pseudo-potential lattice Boltzmann approach to accurately delineate solid–liquid interfaces. Chen and Shu et al. [9] advanced a phase-field-simplified lattice Boltzmann method specifically tailored for modeling solid–liquid phase transitions within homogeneous materials. This approach adeptly captures intricate geometries and flow dynamics encountered in such systems. Furthermore, Han et al. [10] conducted an investigation into enhancing the melting performance of composite phase change materials reconstructed via the QSGS method. Their study involved a detailed analysis and comparison of melting front evolution and transient temperature responses between composite and pure phase change materials, offering valuable insights into their thermal behavior.
However, investigations into the melting behavior of phase change materials (PCMs) subjected to bottom heating are notably lacking. It is widely recognized that when heated from below, the heat transfer dynamics resemble classical Rayleigh–Bénard convection, potentially inducing turbulent thermal convection at elevated Rayleigh numbers [11]. A comprehensive comprehension of the intricate transport mechanisms within thermal convective flows necessitates robust experimental and computational methodologies. Over the past three decades, the lattice Boltzmann method (LBM) has emerged as a prominent numerical technique and serves as a formidable tool for computational fluid dynamics and heat transfer analyses [12,13,14,15,16,17]. Moreover, LBM offers a potent approach for solving nonlinear partial differential equations [18,19], encompassing the Navier–Stokes equation, convection–diffusion equation [20], phase field equation [21], and Nernst–Planck equation [22], among others [23]. While numerous LBM models have been proposed for solid–liquid phase change phenomena, the single-relaxation-time (SRT) model remains prevalent [24]. Despite its numerical efficiency, the SRT model often exhibits instability in high-Rayleigh-number scenarios and suffers from numerical diffusion across phase interfaces, as highlighted by Huang. Although Huang [25] mitigated this issue using the multiple-relaxation-time (MRT) model, determining the free relaxation parameters proves cumbersome. In the subsequent discourse, Liu et al. [26] introduce a cascaded LBM tailored for investigating solid–liquid phase change heat transfer. Comparative evaluations with the MRT method demonstrate the superior numerical stability of the cascaded lattice Boltzmann method, which is attributed to enhanced Galilean invariance. Additionally, a novel enthalpy-based immersed boundary-lattice Boltzmann model is proposed for addressing solid–liquid phase change challenges within porous media under local thermal non-equilibrium conditions in reference [27]. Notably, recent advancements include the introduction of a simple yet efficient MRT-LBM for modeling anisotropic liquid–solid phase transitions [28].
In this work, we present a block triple-relaxation-time (B-TriRT) model to solve the phase change problem that has fewer relaxation parameters to be determined than the MRT model and can also reduce the numerical diffusion. The rest of this paper is organized as follows. In Section 2, the B-TriRT LBM is developed for the solid–liquid phase change problem. Section 3 presents the numerical diffusion analysis of the B-TriRT LBM for solid–liquid phase transition. Several numerical experiments, including one-phase melting by conduction and melting in a cavity heated locally from below, are carried out in Section 4. At last, some conclusions are summarized in Section 5.

2. The Block Triple-Relaxation-Time Lattice Boltzmann Model

The governing equations of the solid–liquid phase change problem consist of the incompressible Navier–Stokes (N-S) equations and the energy conservation equation, which have the following form:
· u = 0 ,
u t + · uu = p + · ( ν u ) + F ,
H t + · ( C p T u ) = 1 ρ 0 · ( κ T ) ,
where u , p and ν are the velocity, pressure and kinematic viscosity, respectively. F is the external force; according to the Boussinesq approximation, it can be given by
F = g β ( T T r e f ) ,
where g is the gravitational acceleration vector, β is the thermal expansion coefficient, and T and T r e f are the temperature and reference temperature, respectively. C p , κ , ρ 0 are the specific heat, thermal conductivity and referenced density, respectively. H = C p T + f l L is the total enthalpy, with f l , L representing the liquid fraction and latent heat.
To improve the numerical stability of LBM, the B-TriRT LBM [29,30] is employed for the governing Equations (1)–(3). In the B-TriRT model for the incompressible N-S equations, the evolution of the distribution function is given by
f i ( x + c i Δ t , t + Δ t ) = f i ( x , t ) k ¯ 0 f i n e q ( x , t ) ( k ¯ 1 k ¯ 0 ) ω i c i · M f 1 n e q ( x , t ) c s 2 ( k ¯ 2 k ¯ 0 ) ω i ( c i c i c s 2 I ) : M f 2 n e q ( x , t ) 2 c s 4 + ( 1 k ¯ 1 2 ) ω i c i · F c s 2 + ( 1 k ¯ 2 2 ) ω i ( c i c i c s 2 I ) : ( uF + Fu ) 2 c s 4 ,
where f i ( x , t ) is the discrete distribution function for a particle with velocity c i at time t and position x , and k ¯ 0 , k ¯ 1 , k ¯ 2 are dimensionless relaxation parameters, M f 1 n e q ( x , t ) = j c j f j n e q , M f 2 n e q ( x , t ) = j c j c j f j n e q are the first-order and second-order moment of non-equilibrium distribution function, with f j n e q = f j f j e q . The term f i e q ( x , t ) is the equilibrium distribution function, which is defined as
f i e q ( x , t ) = λ i p + ω i [ c i · u c s 2 + uu : ( c i c i c s 2 I ) 2 ε c s 4 ] ,
where λ 0 = ( ω 0 1 ) / c s 2 , λ i = ω i / c s 2 ( i 0 ) , ω i are the weight coefficients. For the two-dimensional case considered here, the popular D2Q9 model is employed; then, the weight coefficients can be give by ω 0 = 4 / 9 , ω i = 1 / 9 ( i = 1 4 ) , ω i = 1 / 36 ( i = 5 8 ) , respectively.
The macroscopic velocity u and the hydrodynamic pressure p are computed by
u = i c i f i + Δ t 2 F ,
p = c s 2 1 ω 0 ( i 0 f i ω 0 | u | 2 2 c s 2 ) .
Through the multi-scale Chapman–Enskog analysis, the incompressible N-S Equations (1) and (2) can be recovered by the above B-TriRT model with
1 k ¯ 2 = τ f = ν c s 2 Δ t + 1 2 ,
where τ f represents the dimensionless relaxation time. In addition, to balance the numerical stability and efficiency in the numerical simulation, we can enforce k ¯ 0 = k ¯ 1 = k ¯ 2 .
The evolution equation of the B-TriRT model for the energy conservation Equation (3) is
g i ( x + c i Δ t , t + Δ t ) = g i ( x , t ) k 0 g i n e q ( x , t ) ( k 1 k 0 ) ω i c i · M g 1 n e q ( x , t ) c s 2 ( k 2 k 0 ) ω i ( c i c i c s 2 I ) : M g 2 n e q ( x , t ) 2 c s 4 ,
where g i ( x , t ) is the discrete distribution function for the total enthalpy. The terms k 0 , k 1 , k 2 are dimensionless relaxation parameters, and M g 1 n e q ( x , t ) = j c j g j n e q , M g 2 n e q ( x , t ) = j c j c j g j n e q are the first-order and second-order moment of the non-equilibrium part of g j , with g j n e q = g j g j e q .
In addition, the equilibrium distribution function g i e q is defined by
g i e q = H C p T + ω i C p T , i = 0 , ω i C p T 1 + c i · u c s 2 , i 0 .
The total enthalpy is calculated by
H = i g i ( x , t ) .
In order to recover the energy Equation (3), the dimensionless relaxation time k 1 should satisfy the following equation.
1 k 1 = κ ρ 0 C p c s 2 Δ t + 0.5 = α c s 2 Δ t + 0.5 ,
where α is the thermal diffusivity. As pointed out in ref. [25], the traditional total-enthalpy-based thermal LBM is usually accompanied by numerical diffusion across the phase interface. To address such a drawback, Huang et al. [25] proposed an improved MRT model to reduce the numerical diffusion. In the present work, we also derive a relational expression to reduce the numerical diffusion as
1 k 1 2 k 2 2 = 0 .
By adopting the relational expression, the solid phase can be precisely kept at the melting temperature and the phase interface can be exactly restricted in one lattice spacing, i.e., the numerical diffusion across the phase interface can be thoroughly eliminated, which will be confirmed in the next section.

3. Numerical Diffusion Analysis of the B-TriRT LB Model for Solid–Liquid Phase Transition

In this section, we delve into the possible numerical diffusion phenomena at the phase interface in solid–liquid phase transition problems, and we analyze the B-TriRT LB model proposed in this work. Therefore, we will derive a relaxation parameter relationship to eliminate numerical diffusion. Without loss of generality, the one-dimensional isothermal phase transition (melting) problem is considered, where the phase transition temperature is a constant temperature T m and the solid phase remains at the initial temperature T m . Figure 1 provides a schematic diagram of the macroscopic quantities ( H , f l , T ) near the solid–liquid interface x point at time t, where the x point is the phase transition interface point, the x + 1 point is the solid-phase point, and the x 1 point is the liquid-phase point.
According to the evolution equation Equation (10), the distribution function of point x + 1 at time t + δ t is
g i ( x + 1 , t + Δ t ) = g i ( x , t ) k 0 g i n e q ( x , t ) ( k 1 k 0 ) ω i c i · i c i ( g i ( x , t ) g i e q ( x , t ) ) c s 2 ( k 2 k 0 ) ω i ( c i c i c s 2 I ) : i c i c i ( g i ( x , t ) g i e q ( x , t ) ) 2 c s 4 ,
Then, the evolution equation is divided into the following three categories as
g i ( x + c i δ t , t + δ t ) = g i ( x , t + δ t ) , i = 0 , 2 , 4 ; g i ( x + c i δ t , t + δ t ) = g i ( x + c δ t , t + δ t ) , i = 1 , 5 , 8 ; g i ( x + c i δ t , t + δ t ) = g i ( x c δ t , t + δ t ) , i = 3 , 6 , 7 .
Furthermore, by summing up the distribution functions in the 0 , 2 , 4 directions, 1 , 5 , 8 directions and 3 , 6 , 7 directions, respectively. We can obtain
g 0 ( x , t + δ t ) + g 2 ( x , t + δ t ) + g 4 ( x , t + δ t ) = g 0 ( x , t ) + g 2 ( x , t ) + g 4 ( x , t ) k 0 [ g 0 ( x , t ) + g 2 ( x , t ) + g 4 ( x , t ) ( g 0 e q ( x , t ) + g 2 e q ( x , t ) + g 4 e q ( x , t ) ) ] ( k 0 k 2 ) [ g 1 ( x , t ) + g 5 ( x , t ) + g 8 ( x , t ) ( g 1 e q ( x , t ) + g 5 e q ( x , t ) + g 8 e q ( x , t ) ) ] ( k 0 k 2 ) [ g 3 ( x , t ) + g 6 ( x , t ) + g 7 ( x , t ) ( g 3 e q ( x , t ) + g 6 e q ( x , t ) + g 7 e q ( x , t ) ) ]
g 1 ( x + c δ t , t + δ t ) + g 5 ( x + c δ t , t + δ t ) + g 8 ( x + c δ t , t + δ t ) = g 1 ( x , t ) + g 5 ( x , t ) + g 8 ( x , t ) ( k 1 2 + k 2 2 ) [ g 1 ( x , t ) + g 5 ( x , t ) + g 8 ( x , t ) ( g 1 e q ( x , t ) + g 5 e q ( x , t ) + g 8 e q ( x , t ) ) ] ( k 2 2 k 1 2 ) [ g 3 ( x , t ) + g 6 ( x , t ) + g 7 ( x , t ) ( g 3 e q ( x , t ) + g 6 e q ( x , t ) + g 7 e q ( x , t ) ) ]
g 3 ( x c δ t , t + δ t ) + g 6 ( x c δ t , t + δ t ) + g 7 ( x c δ t , t + δ t ) = g 3 ( x , t ) + g 6 ( x , t ) + g 7 ( x , t ) ( k 2 2 k 1 2 ) [ g 1 ( x , t ) + g 5 ( x , t ) + g 8 ( x , t ) ( g 1 e q ( x , t ) + g 5 e q ( x , t ) + g 8 e q ( x , t ) ) ] ( k 1 2 + k 2 2 ) [ g 3 ( x , t ) + g 6 ( x , t ) + g 7 ( x , t ) ( g 3 e q ( x , t ) + g 6 e q ( x , t ) + g 7 e q ( x , t ) ) ] .
Since x , t are arbitrary values and have generality, we make x in Equation (19) equal to x + c δ t and t equal to t δ t . Therefore, Equation (19) can be written as
g 3 ( x , t ) + g 6 ( x , t ) + g 7 ( x , t ) = g 3 ( x + c δ t , t δ t ) + g 6 ( x + c δ t , t δ t ) + g 7 ( x + c δ t , t δ t ) ( k 2 2 k 1 2 ) [ g 1 ( x + c δ t , t δ t ) + g 5 ( x + c δ t , t δ t ) + g 8 ( x + c δ t , t δ t ) ( g 1 e q ( x + c δ t , t δ t ) + g 5 e q ( x + c δ t , t δ t ) + g 8 e q ( x + c δ t , t δ t ) ) ] ( k 1 2 + k 2 2 ) [ g 3 ( x + c δ t , t δ t ) + g 6 ( x + c δ t , t δ t ) + g 7 ( x + c δ t , t δ t ) ( g 3 e q ( x + c δ t , t δ t ) + g 6 e q ( x + c δ t , t δ t ) + g 7 e q ( x + c δ t , t δ t ) ) ] .
When the point x is the phase transition interface point, x + 1 is the solid-phase point and x 1 is the liquid-phase point; since the temperature at the solid-phase point remains constant, the corresponding distribution function should equal the value of its equilibrium distribution function. Therefore, from Equation (20), it can be obtained that
g 3 ( x , t ) + g 6 ( x , t ) + g 7 ( x , t ) = g 3 e q ( x + c δ t , t δ t ) + g 6 e q ( x + c δ t , t δ t ) + g 7 e q ( x + c δ t , t δ t ) .
Assuming that at time t a certain point is a solid-phase point, then at time t 1 , that point must also be a solid-phase point. Meanwhile, due to the constant temperature of the solid-phase point, the equilibrium distribution functions corresponding to the two moments are also identical. Therefore, Equation (21) can be written as
g 3 ( x , t ) + g 6 ( x , t ) + g 7 ( x , t ) = g 3 e q ( x + c δ t , t ) + g 6 e q ( x + c δ t , t ) + g 7 e q ( x + c δ t , t ) .
Then, substituting Equation (22) into Equation (18) yields
g 1 ( x + c δ t , t + δ t ) + g 5 ( x + c δ t , t + δ t ) + g 8 ( x + c δ t , t + δ t ) = g 1 e q ( x , t ) + g 5 e q ( x , t ) + g 8 e q ( x , t ) + ( 1 k 1 2 k 2 2 ) [ g 1 ( x , t ) + g 5 ( x , t ) + g 8 ( x , t ) ( g 1 e q ( x , t ) + g 5 e q ( x , t ) + g 8 e q ( x , t ) ) ] ( k 2 2 k 1 2 ) [ g 3 e q ( x + c δ t , t ) + g 6 e q ( x + c δ t , t ) + g 7 e q ( x + c δ t , t ) ( g 3 e q ( x , t ) + g 6 e q ( x , t ) + g 7 e q ( x , t ) ) ] .
Since the temperature at the phase transition point remains constant, the corresponding equilibrium distribution function also does not change. Therefore, the above equation can be written as
g 1 ( x + c δ t , t + δ t ) + g 5 ( x + c δ t , t + δ t ) + g 8 ( x + c δ t , t + δ t ) = g 1 e q ( x , t ) + g 5 e q ( x , t ) + g 8 e q ( x , t ) + ( 1 k 1 2 k 2 2 ) [ g 1 ( x , t ) + g 5 ( x , t ) + g 8 ( x , t ) ( g 1 e q ( x , t ) + g 5 e q ( x , t ) + g 8 e q ( x , t ) ) ] .
In order for the solid-phase point ( x + c δ t ) to remain inactive, the distribution functions in the directions of 1 , 5 , 8 must satisfy [25]
g 1 ( x + c δ t , t ) + g 5 ( x + c δ t , t ) + g 8 ( x + c δ t , t ) = g 1 e q ( x , t ) + g 5 e q ( x , t ) + g 8 e q ( x , t ) ,
Therefore, the relaxation parameters k 1 and k 2 should be
1 k 1 2 k 2 2 = 0 .
At this point, the numerical diffusion at the interface can be completely eliminated.

4. Numerical Results

4.1. One-Phase Melting by Conduction

We first consider one-phase conduction melting as a benchmark problem to validate the present B-TriRT model’s ability to reduce numerical diffusion across the phase interface. Initially, the phase change material is solid uniformly and the temperature is set to be T m . At time t > 0 , a constant temperature T h ( T h > T m ) is imposed on the left wall (i.e., x = 0 ); then, the phase change material begins to melt. For this problem, the analytical solution of the temperature is given by [25]
T ( x , t ) = T h ( T h T m ) e r f x 2 α t e r f ( κ ) , 0 < x < X i ( t ) , T m , x > X i ( t ) ,
where e r f ( x ) = 2 π 0 x e η 2 d η is the error function, and the position of the phase interface can be determined as
X i ( t ) = 2 κ α t , S t e e x p ( κ 2 ) e r f ( κ ) = κ π .
In the present simulations, the dimensionless parameters and thermophysical properties are set as T h = 1 , T m = 0 , S t e = 0.01 , α = 1 / 6 , and the computational parameters of present model are given by Δ x = 1 / 100 , c = 1.0 . In addition, the time step Δ t is calculated by the relationship Δ t = α / [ c s 2 ( 1 / k 1 0.5 ) ] , with k 1 being set as 0.1 , 0.5 , 1.0 , 1.5 and 2.0 , respectively. The temperature distributions at t = 25 of the SRT model and the present B-TriRT model for different k 1 values are illustrated in Figure 2. It can be seen from Figure 2a that for the SRT model, the temperature distributions deviate from the analytical solutions when k 1 1 . The results show that the solid phase has been activated before it starts melting, which can be explained by the numerical diffusion [25]. However, for the present B-TriRT model, the temperature distributions agree well with the analytical solutions, and the temperatures of the solid phase stay at T m . The results indicate that the numerical diffusion across the phase interface can be dramatically reduced when employing the present B-TriRT model. On the other hand, as discussed in ref. [25], the numerical diffusion will cause the phase interface width to exceed one lattice spacing. To verify this point clearly, the liquid fraction distributions at t = 25 are captured by the SRT model and the present B-TriRT model with different k 1 values, and the results are shown in Figure 3. The results indicate that the phase interface width obtained from the SRT model is always larger than one lattice spacing. However, the phase interface width obtained by the present B-TriRT model is exactly one lattice spacing. From the above results and discussions, it can be concluded that the present B-TriRT model can be exploited to reduce the numerical diffusion across the phase interface in the solid–liquid phase change problem.

4.2. Melting in a Cavity Heated Locally from Below

In this section, melting in a cavity heated locally from below is investigated. As shown in Figure 4, the problem consists of a cubical cavity with length L = 1.0 that is filled with PCM at the initial temperature T m , and the cavity is heated locally with temperature T h from below. The width of the heated region is set to D = 0.5 L , and the distance from the left wall to the center of heated region (C) is varied in the range of 0.25 C 0.5 . For the walls of the cavity, non-slip adiabatic boundary conditions (i.e., T / n = 0 , ( u , v ) = ( 0 , 0 ) , where n is the normal vector of walls) are applied.
In the present investigation, we consider the influence of C on the melting process, and we plot the liquid fraction variation for different cases in Figure 5, where T h = 1 , T m = 0 , R a = 10 8 , P r = 6.2 , S t e = 0.125 , c = 1.0 , Δ x = 1 / 512 . As shown in Figure 5, when the distance C is changed from 0.25L to 0.5L, the full melting time is decreased. The results indicate that the melting rate can be increased through changing the heated region from the sides to the middle region. The reason can be interpreted by a symmetry argument. The average distance between the PCM and the heated region is minimized when the heated region is centered, which allows faster melting. Furthermore, the instantaneous flow and temperature structures and the contours of the flow field are presented in Figure 6 and Figure 7. From these figures, it can be observed that the flow in the melt region is nearly chaotic, with a thin thermal boundary layer. In addition, the interface area in the case of C = 0.5L is larger than the interface area in the cases of C = 0.25 L and C = 0.375 L , which leads to a larger melting rate at C = 0.5 L .

5. Conclusions

In this study, a B-TriRT model was developed to address the solid–liquid phase change problem. Through considering a one-dimensional isothermal phase transition problem, a relaxation parameter relationship was derived that can mitigate numerical diffusion across the phase interface significantly. The numerical experiment of one-phase melting by conduction confirmed that the numerical diffusion across the phase interface can be dramatically reduced by the present B-TriRT model. Furthermore, we examined the effects of the heated region’s location on the melting process at high Rayleigh numbers. The results indicate that positioning the heated region at the center of the bottom wall facilitates earlier complete melting.

Author Contributions

Methodology, formal analysis, investigation and writing—original draft preparation, X.Y.; supervision and methodology, Z.C.; conceptualization, supervision, review and editing and funding acquisition, Y.Z. All authors have read and agreed to the published version of the manuscript.

Funding

This work is supported by the National Natural Science Foundation of China (grant No. 12302373 and 12372286) and the Natural Science Foundation of Hunan Province, China (grant No. 2022JJ40466).

Data Availability Statement

The computed data can be provided by the corresponding author on request.

Conflicts of Interest

The authors declare no conflicts of interest.

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Figure 1. Schematic diagram of macroscopic quantities ( H , f l , T ) near point x at the solid–liquid interface at time t.
Figure 1. Schematic diagram of macroscopic quantities ( H , f l , T ) near point x at the solid–liquid interface at time t.
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Figure 2. Comparisons of temperature distributions between SRT model (a) and B-TriRT model (b) for different k 1 values.
Figure 2. Comparisons of temperature distributions between SRT model (a) and B-TriRT model (b) for different k 1 values.
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Figure 3. Comparisons of liquid fraction distributions between SRT model (a) and B-TriRT model (b) for different k 1 values.
Figure 3. Comparisons of liquid fraction distributions between SRT model (a) and B-TriRT model (b) for different k 1 values.
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Figure 4. Schematic illustration of the physical domain.
Figure 4. Schematic illustration of the physical domain.
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Figure 5. The variation of fractions for different cases at different F o values.
Figure 5. The variation of fractions for different cases at different F o values.
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Figure 6. The streamlines and contours of the temperatures for the different cases at different F o values. ((ad): C = 0.25 L , (eh): C = 0.375 L and (il): C = 0.5 L ; (a,e,i): F o = 0.1 , (b,f,j): F o = 0.2 , (c,g,k): F o = 0.3 and (d,h,l): F o = 0.4 ). The phase interface is marked by the red line.
Figure 6. The streamlines and contours of the temperatures for the different cases at different F o values. ((ad): C = 0.25 L , (eh): C = 0.375 L and (il): C = 0.5 L ; (a,e,i): F o = 0.1 , (b,f,j): F o = 0.2 , (c,g,k): F o = 0.3 and (d,h,l): F o = 0.4 ). The phase interface is marked by the red line.
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Figure 7. The contours of the velocities at different F o values. ((ad): C = 0.25 L , (eh): C = 0.375 L and (il): C = 0.5 L ; (a,e,i): F o = 0.1 , (b,f,j): F o = 0.2 , (c,g,k): F o = 0.3 and (d,h,l): F o = 0.4 ).
Figure 7. The contours of the velocities at different F o values. ((ad): C = 0.25 L , (eh): C = 0.375 L and (il): C = 0.5 L ; (a,e,i): F o = 0.1 , (b,f,j): F o = 0.2 , (c,g,k): F o = 0.3 and (d,h,l): F o = 0.4 ).
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Yang, X.; Chen, Z.; Zhao, Y. A Block Triple-Relaxation-Time Lattice Boltzmann Method for Solid–Liquid Phase Change Problem. Mathematics 2024, 12, 1815. https://doi.org/10.3390/math12121815

AMA Style

Yang X, Chen Z, Zhao Y. A Block Triple-Relaxation-Time Lattice Boltzmann Method for Solid–Liquid Phase Change Problem. Mathematics. 2024; 12(12):1815. https://doi.org/10.3390/math12121815

Chicago/Turabian Style

Yang, Xuguang, Zhenyu Chen, and Yong Zhao. 2024. "A Block Triple-Relaxation-Time Lattice Boltzmann Method for Solid–Liquid Phase Change Problem" Mathematics 12, no. 12: 1815. https://doi.org/10.3390/math12121815

APA Style

Yang, X., Chen, Z., & Zhao, Y. (2024). A Block Triple-Relaxation-Time Lattice Boltzmann Method for Solid–Liquid Phase Change Problem. Mathematics, 12(12), 1815. https://doi.org/10.3390/math12121815

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