3.1. Validation of the Fluid Flow Obtained by the Mathematical Model with Experimental Measurements
To ensure the robustness of the mathematical model for predicting the fluid flow field, a first validation was performed using the experimental data reported by Dong-Yuan Sheng [
20]. Our modeling strategy consisted of meshing, turbulence model selection, and spatial discretization strategy. We compared our refined model’s results with the best-known experimental benchmark for tundishes [
20,
21]. The mathematical model described before was used to simulate the reported results of an experimental physical model of a single-strand tundish, without flow modifiers [
20], by changing the appropriate boundary conditions and geometry. This tundish geometry was selected because it represents a well-documented and simplified reference case, allowing for the assessment of the model’s performance under controlled conditions. Although it differs from the main geometry of this study, it serves as a useful preliminary step to verify the numerical setup and turbulence model before applying them to the more complex case. Still, this first validation has the purpose of warranting our model’s capacity to describe the flow field of any tundish accurately. Sheng et al. [
20] performed CFD simulations of the experimental results shown in
Figure 5a. They used different modeling parameters, such as mesh size and turbulence model. Their modeling results show that predicted flow patterns in the tundish can vary considerably, even for simple single-phase flow, by changing a single modeling parameter. This highlights the risk of error associated with selecting a defined modeling practice without reliable experimental results for parameter fine-tuning. Following this strategy, we adjusted the mesh size and selected the turbulence model. The following turbulence models are available in Fluent:
k-
ε, k-ω, and Large Eddy Simulation (LES), among others. LES is computationally expensive for modeling the whole tundish. Therefore, we selected the realizable
k-
ε turbulence model. It provided
profile results very close to the experimental reference and comparable to the best case selected by Sheng et al. [
20].
Figure 5 compares the experimental velocity vectors and the turbulence intensity (
) contours against our predictions from this work’s mathematical model. Turbulence intensity is calculated using Equation (22) and is defined in the paper as the ratio of fluctuating velocity to instantaneous velocity. Vectors represent the velocities, and the model predicts the same velocities in the entering jet region, in both
Figure 5a,b, for both experimental and theoretical results. When the jet impinges on the tundish bottom, it changes direction and spreads along all the directions. In the measurement longitudinal plane, one part of the jet moves laterally to the left of the jet, ascending through the wall and being redirected, forming a recirculation loop (with high turbulence characterized by a high
, given by the color contour plot) and a descending diagonal flow to the right of the jet. Meanwhile, at the right side of the jet at the bottom wall, part of the fluid moves to the tundish exit, but part of it interacts with the diagonal flow and forms a high-turbulence recirculation region near the bottom center of the tundish. Part of the fluid ascends and forms a high-turbulence region near the tundish free surface. As we can see, the velocity vectors and the Tu contours show reasonable qualitative and quantitative agreement between experimental measurements and simulated results from our mathematical model.
The axial profile of the experimental [
20] time-averaged velocity (
) at x/L = 0.5 is compared with the predicted profile from the developed model in
Figure 6. The mathematical model accurately predicts the measured velocity profile with a mean relative error of 20.77 ± 20.73%. This confirms the robustness of the model to calculate tundish fluid flow. Near the free surface, small discrepancies exist between predictions and measurements. Near the bottom wall, even smaller discrepancies are observed. These results suggest that deformation of the free surface needs to be accounted for in the next model version. The current model uses a flat, fixed free surface to reduce computational cost and avoid multiphase methods like VOF. While this limits how we capture dynamic surface effects, validation shows that the model still gives reasonably accurate predictions without a deformable surface. Additionally, treatment of the walls should be fine-tuned by improving the description of the laminar-to-turbulent connection. Currently, the standard wall functions are used, but it may be necessary to consider alternative wall functions or set specific values for shear stresses or wall surface roughness.
Once our model’s mathematical approach, including the turbulence model and the discretization, was validated, we proceeded to simulate the fluid flow within the tundish shown in
Figure 3. The purpose was to obtain the operating velocity fields in the planes indicated in
Figure 3 and compare them with the experimental results obtained by PIV.
Figure 7 and
Figure 8 present the tundish velocity vector fields, without flow modifiers, for three longitudinal and two transverse planes, respectively. These planes are described in
Figure 3 and
Table 3. On the left side, experimental velocity measurements obtained using PIV are presented; on the right side, the calculated velocity vectors derived from the mathematical model are presented. In general terms, the mathematical model properly captures the qualitative behavior of the fluid flow measured by PIV in the physical model (
Figure 7 and
Figure 8), considering that the experimental measurements show some fluctuations and errors due to the optical nature of the PIV measurements and the appearance of some physical interferences and optical aberrations. For instance, the mathematical model results exhibit perfect symmetric behavior due to the assumption of symmetric planes, whereas the experimental measurements reveal some asymmetries resulting from the inherent experimental error. Additionally, the mathematical model’s predicted velocity magnitude is overestimated in certain regions, particularly due to the numerical simulation’s inaccurate representation of the wall interaction with the fluid at the bottom wall.
In
Figure 7a, the measured and predicted velocity vector fields are shown at the middle longitudinal plane (xy) of the tundish (plane 1, xy at z = 0). We can see that in both physical and mathematical models, the jet is located just at the exit of the shroud. The jet impinges on the tundish bottom and is then redirected radially in all directions. In
Figure 7a, the jet is redirected to the tundish exit; however, part of the flow ascends through the wall and is then redirected diagonally to the water jet, generating a recirculation loop. On the other hand, in
Figure 8a (plane 4, middle transversal plane yz at x = 0), the flow field indicates that the water is redirected to the lateral wall, then ascends through the wall and generates a recirculation that reincorporates the flow into the jet. In both the measured and calculated flow fields, the recirculation loops in measurement planes 1 and 4 (see
Figure 3) are qualitatively similar; the numerical model accurately predicts the path that the liquid follows within the tundish. The main difference lies in the quantitative value of the magnitude of the velocity vectors. The numerical simulation predicts higher velocities in general. Experimentally, the effect of the static walls on the fluid velocity is greater, slowing down the water flow as it approaches the bottom and lateral walls.
Due to the tridimensional nature of the fluid flow inside the tundish, we decided to measure the fluid dynamics of the physical model with PIV in additional measurement planes (planes 2, 3, and 5 in
Figure 3), to carry out a more rigorous validation of the fluid flow predicted by the mathematical model. In
Figure 7b (plane 2, xy at z = 0.6m), in general terms, it shows a projection of
Figure 7a, as we can see the main movement of the water flow is the same due to the jet after interacting with the tundish bottom wall, but with a lower-velocity magnitude. In
Figure 7b, the water at the bottom flows towards the lateral wall and then rises, generating a diagonal circulation loop similar to that in
Figure 7a. However, there is no perceptible interaction with the tundish exit in this case. Due to the distance to the jet, a decrease in velocity magnitude in this plane is perceptible compared with the middle plane presented in
Figure 7a. As in the middle plane, there is greater interaction with the walls in the measured velocities in comparison with those calculated by the simulation. In plane 3 (xy plane at z = 0.12 m),
Figure 7c, as the flow approaches the tundish wall, we measure and simulate a diagonally ascending flow from the center of the tundish to the higher region of the lateral wall. This plane is interesting because the measurement showed higher velocities and was in an opposite direction from the flow patterns measured in the other two longitudinal planes (
Figure 7a,b). This behavior is explained by considering the three-dimensional nature of the flow. Plane 3 shows an ascending movement of the water in the circulation loop, as shown in
Figure 8a. The numerical model (
Figure 7c) accurately captures the measurement’s qualitative and quantitative behavior. With a high-velocity ascending flow in a diagonal direction, some of the vectors are directed towards the tundish surface, and part of them interact with the wall, forming a circulation loop near the free surface.
Figure 8b (transverse plane yz at x = 0.44 m) shows a flow field with completely different behavior compared to
Figure 8a. The jet radial movement is not perceptible in this transversal plane located away from the fluid inlet; however, circulation loops are captured in both the physical and the numerical models, and the position and magnitude of the loops are similar in both cases. These circulation loops are not generated due to the interaction of the jet movement in this plane; in this case, they are caused by the projections of the three-dimensional circulation loops shown in the middle planes (measurement planes 1 and 4 in
Figure 3). As is presented in
Table 4, the relative error in the mean velocity magnitudes increases (15–68%) as the measurement plane moves from the symmetry (water inlet longitudinal plane) and moves closer to the walls (planes 1–3, see
Figure 3). In the transversal planes (planes 4 and 5, see
Figure 3), the overprediction of the velocity magnitude by the numerical simulation is even higher (93–139%). These discrepancies suggest limitations in the turbulence model used. The system under study exhibits both high- and low-velocity regions, making it difficult for the available RANS turbulence models to accurately capture the full range of flow behavior in all planes, especially the secondary flow patterns. The increased errors near the walls may suggest additional issues with the wall function implementation. In addition, the assumption of a flat free surface is preventing the model from properly dissipating energy through the surface deformation and wave motion, as occurs in reality, contributing to the deviation between numerical and experimental results.
In summary, the mathematical model is capable of predicting the flow pattern in agreement with the measured flow fields, although the comparison of the predictions against the PIV experimental measurement indicates some model limitations and areas of opportunity to improve it. The main need is to improve the model’s capability to capture the water/wall interactions and also the deformable free surface.
3.2. Validation of the Predicted Mixing by the Mathematical Model with PLIF Measurements
To verify the accuracy of the mathematical model in calculating mixing inside the tundish, PLIF measurements were compared with the simulation results of Rhodamine mixing behavior.
Figure 9 presents the instantaneous concentration contours measured using PLIF (left) and numerically simulated (right) at different times after the tracer was pulsed injected.
Figure 9a shows the instantaneous concentration contours at 0.25 s. In both cases, the tracer follows the flow pattern depicted in
Figure 7a. After injection, the Rhodamine is transported by the water jet to the tundish bottom. The mathematical model indicates that the tracer has already reached the bottom, whereas the experimental measurement suggests that the tracer is approaching the tundish bottom.
After two seconds from injection (
Figure 7b), most of the tracer is moving as a high-concentration fluid package, transported by convection, following the flow pattern presented in plane 1 (
Figure 7a). The experimental concentration contour shows more tracer displacement, practically reaching the tundish exit, and with a very low quantity of tracer in the jet region. At the same time, the mathematical model predicts that part of the tracer is still on the jet, showing a gradient of concentration from the jet end to the tundish exit. The PLIF measurement also shows some lateral dispersion of the tracer due to the turbulent diffusion in the jet surroundings. On the other hand, the mathematical model predicts a slight lateral dispersion due to turbulent diffusion near the main tracer package. Both convective and turbulent diffusion species transport mechanisms are underestimated in the mathematical model relative to the PLIF measurements.
Figure 9c shows that after 3 s, in both the measured and the simulated concentration contours, part of the tracer is leaving the tundish, while a region of high concentration of Rhodamine can be observed near the shroud. This region is due to the three-dimensional nature of the tundish flow, as part of the tracer follows the flow pattern presented in plane 4 (
Figure 8a) and is recirculated, hence being visible on measurement plane 1 (see
Figure 3). The concentration in the experimental measurement is higher and exhibits a larger and more chaotic lateral dispersion, which reinforces the notion that the mathematical model underestimates the species transport mechanisms.
Figure 9d shows that after 20 s, the tracer is more evenly distributed inside the tundish with a region with zero concentration at the water jet. The mathematical model predicts a concentration gradient from the jet to the lateral wall. However, the experimental measurement shows two bands of high concentration at the surface and the bottom of the tundish. This phenomenon is attributed to an error due to the optical nature of the PLIF technique, specifically the luminosity gradient in the laser sheet [
17]. Regardless of this, the concentration values in both models are nearly the same, from 2 to 3.5 ppt. After 30 and 50 s (
Figure 9e,f), the tracer is more evenly distributed in the tundish, and the concentration is decreasing to about 3 ppt and 2.5 ppt, respectively. The gradient of concentration due to the PLIF non-homogeneous illumination is still visible. Finally, at 150 s (
Figure 9g), the concentration of rhodamine inside the tundish is negligible in both the experimental measurements and the mathematical model, with values below 1.5 ppt. The values of mean concentration at every time are presented at
Table 5.
Table 5 shows that, except at 0.25 s and 150 s, the errors of the numerical model are generally moderate (most around 20%). At 0.25 s, the large error likely results from the actual injection point being just before the inlet, causing the solute to enter the tundish after a brief travel and pre-mixing, instead of a true pulse at the precise inlet. At 150 s, the solute is highly diluted, and the error, which is relative to the measured values, increases as the rhodamine concentration decreases to a measured value below 1 ppt.
Nevertheless, we still think the mathematical model predicts reasonably well the fluid flow of the tundish (see
Figure 7 and
Figure 8), and the mixing of the Rhodamine is also properly captured by the model (see
Figure 9) according to the PIV and PLIF measurements. The transport of the tracer by convection following the flow pattern of the tundish is qualitatively well calculated by the numerical model, as well as the description of the lateral dispersion due to the turbulent diffusion. However, the use of PLIF measurements through instantaneous concentration contours to validate the tracer distribution predicted by the model presents some areas of opportunity to quantitatively improve the calculation of species transport mechanisms in the mathematical model, mainly the turbulent diffusion that has a greater significance in the physical model than in the mathematical model, but also the convective transport of the tracer, which is slightly underestimated in the mathematical model.
To quantify the effect of the mass transport mechanisms on the mixing inside the tundish, the instantaneous convection and instantaneous turbulent diffusion mass transfer flux were calculated with the formulation described in [
22].
To further investigate the mass transfer physics,
Figure 10 presents the comparison of experimental and numerical simulated instantaneous (at time of 2 s after tracer injection) convective flux, turbulent diffusion flux, and the ratio between both mass transfer mechanisms (
) calculated as (Equation (23)):
where
and
are the instantaneous convective flux and instantaneous turbulent diffusive flux, respectively.
Figure 10a,b present a similar distribution of the instantaneous mass transfer mechanisms, where a high convective and turbulent diffusive flux at the jet and at the lateral region after the tracer impinges with the tundish bottom, presenting high flux values at the regions where the tracer concentration is high (see
Figure 9b). In both experimental and simulated flux results, the convective flux (
Figure 10a) presents a higher value compared with the turbulent diffusive flux (
Figure 10b).
Table 6 presents the mean value of the mass transfer fluxes in measurement plane 1 (see
Figure 3). The mean convection flux is 21% and 57% higher compared with the turbulent diffusion flux (only considering the mean value of the mechanism in the plane) for experimental and numerical simulation, respectively. We can also observe that the numerical simulation yields significantly lower values in both mass fluxes, with the experiment presenting 3.6 times and 4.7 times more convection and turbulent diffusion mass flux, respectively.
To explore the difference between the numerical values of the fluxes, the local ratio between both fluxes was calculated (see
Figure 10c). Notably, the local mass flux ratio is higher in the numerical simulation (mean value 1.21) than in the experimental measurement (mean value 0.51; see
Table 6). This suggests that the model does not accurately represent the relationship between velocity and turbulence, likely due to the turbulence model. However, in qualitative terms, the flux ratio is similar: in most of the tundish, convection dominates mass transport, whereas just above the bottom, turbulent diffusion dominates. Specifically, after the jet impinges on the bottom, part of the tracer is transported to the tundish exit by convection. Subsequently, a region above this forms a layer where turbulent diffusion becomes the dominant mechanism.