The results have been categorized into three sections The first section deals with the extent of mixing and velocity profiles in a swirling steam injection into cross-flowing water along two orthogonal planes. In the second section, the effect of mixing on the stability of the flow domain is reported and discussed. In the third section, we discuss the effect of scaling of the vertical trajectory of the swirling steam jet on the mixing under all operating conditions. It should be noted that the measured results for the temperature and velocity have been supported by the CFD outcomes wherever necessary.
3.1. The Extent of Mixing and the Velocity Profiles for Swirling Steam Injection into Cross-Flowing Water
The steam was injected into the cross-flowing water at 1 bar of gauge pressure initially, at varying rpm ranging from 60–300 rpm. The water was injected at the same 1 bar of gauge pressure; the manual valve was used to adjust the pressure inside the flow vessel. Measurements were obtained by using the LM35 temperature sensors [
12] mounted on the plane sheet. It should be noted that all LM35 temperature sensors were mounted on the plane sheet in such a way that their measurement faces were flush with the surface of the plane sheet. The corresponding time-averaged temperature measurements for the time duration (i.e., 5 min) recorded by each of the LM35 temperature sensors are shown by the color contours on each sensor in
Figure 3.
The color contours inside each circle show the rounded-off, time-averaged value of the temperature recorded by the respective LM35 temperature sensor. As the flow vessel was heavily wrapped with Teflon and sponge tape, on an adiabatic basis, the theoretical equilibrium temperature of the resultant mixture of steam and water at the varying inlet pressure, neglecting friction losses and height differences, was given by Equations (3)–(6), as follows,
where
is the mass flowrate (kg/s) of water,
is the mass flowrate (kg/s) of steam,
is the temperature of water at the inlet (°C),
is the temperature of steam at the inlet (°C),
is the inlet pressure of steam or water (Pa),
is the outlet pressure of steam or water (Pa),
represents steam or water,
is volumetric flowrate (m
3/s), and
is the universal gas constant (J/mol.K). Based on these estimations, the adiabatic equilibrium temperature at varying operating conditions ranged from 57.5 to 74.5 °C. So, the average temperature value recorded by each of the LM35 temperature sensors, which was within the given temperature range at the respective operating conditions, provided the information related to the extent of mixing as well as the area patches on the plane sheet that inhibited proper mixing between the swirling steam and cross-flowing water. In other words, the color contours belong to the temperature ranges that showed the extent of mixing of the swirling steam and water in terms of area inhibiting the mixing phenomenon. A Matlab-based code written for color recognition and pixel counting [
19] was used to recognize different colors based on their RGB intensity as well as to estimate the area based on their colors. It should be noted that the experimental values of the average temperature recorded by each LM35 sensor constructed a 2D plane sheet having different color patches based on the difference in the average temperature values. The experimental values were compared/supported by using the computational fluid dynamic (CFD) studies, in which the direct contact condensation (DCC) model [
20] was applied to our previous steam–water studies [
12,
21,
22]. The associated boundary conditions for the CFD study are given in
Table 2. A total mesh number of 4.89 million along the two orthogonal planes provided grid independence at all operating conditions. The perfect mixing zones based on the experimental as well as theoretical studies at the initial conditions (i.e., P
steam = 1 bar, P
water = 1 bar, and rpm = 60) can be seen in
Figure 4a. Perfect mixing is outlined by the even distribution of steam bubbles across the cross-flowing water, and even distribution of steam is reduced. It should be noted that the experimental measurements were placed in an overlapping configuration over the CFD-based profiles after equating the aspect ratios of the two figures (one figure contains experimental profiles, and other contains CFD profiles) showing the orthogonal planes. A clear difference existed between the theoretical and experimental values of the temperature profiles. A possible reason for this difference may be the spatial resolution of the temperature sensors on the plane of symmetry as well as vertical planes while acquiring the experimental data, as the distance between two adjacent LM35 temperature sensors left a void region between them. This region may have contained some meaningful data regarding mixing that was not acquired within the allowed time due to limitations in the data acquisition system used in the present experiment.
Contrarily, in simulation studies, no region was left without characterization. It should also be noted that in the CFD studies, a number of suppositions led to regular nature profiles, whereas in the experimental studies, there were myriad hidden factors that were not incorporated into the CFD studies, including the non-uniformity of the flow profiles in connection with the surface of the plane of symmetry, the effect of the wake profile and insertion of the surrounding cold water inside the leeward section. It should be noted that, in the experimental profiles, regions inhibiting perfect mixing have been shown only, whereas in the CFD profiles, such area patches have been shown by a dotted square around a portion in the legend. The corresponding area patches have been shown by color contours in the CFD profile along the vertical and horizontal planes.
The variation in the area patches inhibiting the perfect mixing of swirling steam inside the cross-flowing water under the varying operating conditions on an experimental as well as theoretical basis is shown by the bar charts in
Figure 4b. The centralized dark region is the maximized mixing area, whereas the zones surrounding this represent inhibited mixing areas shown by the color, which is lightened as it is displaced away from the center of the steam pipe’s exit. It was found that the rotational speed of the propeller, as well as the inlet pressure of the and water, contributed to a rise in the area under the influence of approximate perfect mixing. With an increase in rotational speed from 60 to 300 RPM in steps of 60 RPM, the percentage increase in the area under the influence of perfect mixing ranged from 13 to 25% on an experimental basis and 15 to 38% on a theoretical basis. Overall, by varying the operating conditions from P
steam, P
water = 1 bar each and RPM = 60 to P
steam = 3 bars, P
water = 1 bar and RPM = 300, a 97% (on experimental basis) and 85% (on theoretical basis) increase in the area was estimated, which was under the influence of perfect adiabatic mixing. In the experimental study, a higher percentage of rise in the area under the influence of perfect mixing than in the CFD study was noted. However, in fact, there was a tendency toward narrowing the difference between experimental and CFD results within a fixed aspect ratio plane. The experimental results shown in
Figure 4b are reproducible with varying errors depending upon the accurateness of the experimental setups. In the present setup, the errors shown in
Figure 4b ranged from 4 to 7%. The velocity variations were measured using the 20 HFA sensors, of which 13 were oriented in the horizontal direction with respect to the plane sheet and seven were mounted in the vertical direction with respect to the plane sheet. For characterizing the fluid region based on the velocity distribution across the plane of symmetry as well as a vertical plane, the velocity data were recorded by using the HFA sensors along the plane of symmetry as well as vertical plane. The amplitudes of the velocity fluctuations were computed using a fast Fourier transform (FFT). As the data were acquired for the whole length of the plane sheet, only the time-averaged amplitudes at an axial distance of 1 cm along the axial direction over the plane sheet were plotted symbolically with the similar experimental and CFD aspect ratio-based temperature profiles, as shown in
Figure 5. The actual values of the amplitudes can be seen in the legend in
Figure 5. Here, two important observations were made. First, the time-averaged amplitudes of the velocity profiles had higher values in the crossing regions than the mainstream velocity, whereas the water/steam mixed region was directed toward the windward side, and the velocities were toward the leeward side of the swirling steam duct. A possible reason for this behavior is that the swirling steam jet may provide a virtual cover over the exit of the duct, which leads to bending of the mainstream flow. This lead toward an accelerated flow within this region, which contributes to an increase in the velocity of the swirling steam–water mixture in these regions. These regions are depicted by Regions R1 and R2 in
Figure 5. Another observation was that when the duct was raised above the surface of the plane sheet to a height of h ≈ d/2, the velocity amplitudes initially had lower values than the values of the velocity amplitudes in the mainstream region area, as well as compared to the regions R1 and R2 on the plane of symmetry, but afterward, these amplitude values restored their strength, starting from a distance of 2.3 r ≈ 4.0 cm up to 3.6 r ≈ 6.3 cm. This led to the amplitudes being reduced to the end of the plane sheet. A possible reason for the velocity amplitude decrease followed by an increasing trend is due to the deflection of the streamlines with the body of the duct inhibiting the propeller, and this was raised to the height of h ≈ d/2. After the deflection zone, the streamlines converged toward the wake region, thus giving rise to the amplitudes of the velocity fluctuations.
It was observed that in all given hydrodynamic operating conditions, there were multiple mixing zones that inhibited the extent of good mixing. These mixing zones prevailed over different sizes of area patches, which in the present research project were measured by using color recognition and pixel-counting Matlab-based code. It was observed that in each phase of experimentation, there was a virtual cover based on the void fraction of the swirling steam spread and the surroundings of the duct inhibiting the propeller. The area stretch of this virtual cover was defined based on the colored pixels recorded on an experimental and theoretical CFD basis. The area of this virtual cover had a weak relationship with the total area of the region inhibiting the perfect mixing. The area of such a virtual cover under all hydrodynamic operating conditions is shown in
Figure 6.
The relationship of the area of virtual cover with the area of perfect mixing can be represented by an analytical relation, as shown in Equation (7).
where,
is the area of the virtual cover,
= 0.875 cm,
is experimentally or CFD based,
is the area under the influence of perfect mixing (either experimentally or theoretically based), and
is the power factor (~1.03). With increasing inlet pressure of steam, it was observed that along the plane of symmetry, a proportional rise to the area under the influence of virtual cover resulted. Also, it was observed that with increasing RPM, the area along the plane of symmetry showed a decreasing trend. This may be attributed to the effect of vertical lift acting on the swirling steam jet. In addition, close similarity was observed between the experimental and CFD studies, under operating conditions (P
steam = 2 bars, P
water = 1 bar), in terms of the total area of the virtual cover surrounding the exit of the duct, which may be associated with the higher degree of vertical lift action by the swirling steam on the cross-flowing water.
3.2. Effect of Mixing on the Stability of Swirling Steam–Water Cross-Flows
Swirling steam was injected into cross-flowing water. It was found that the swirling steam mixed with the cross-flowing water, which resulted in the formation of multiple regions surrounding the swirling steam, and the flow phenomena within these regions tended to be complex. However, before discussing the effect of the mixing on the stability in the flow domain, there is a need to discuss some norms from the cited literature, based on which the analysis of the flow domain for its stability can become easier task.
The radius of curvature was taken as positive when the jet was bending outward or upward and considered negative when the jet was bending inward or downward [
2]. Thus, based on this observation, the plane of symmetry around the swirling steam jet exit was divided into four regions, as shown in
Figure 7a. In addition, the stability of the flow domain could be defined based on the velocity variation trends inside the fluid domain. If the velocity decreases in the direction of the radius of curvature, it shows that the flow domain tends towards instability. But when the velocity increases in the direction of the radius of curvature, then the flow domain tends toward stability in that region [
2]. The area at the exit of the duct was divided into small area elements dA/dx, as shown in
Figure 7b. The dotted arrows indicate the radius of curvature, whereas the dotted circles indicate acceleration, dissipation and retardation.
On the plane of symmetry, the behavior of the velocity profiles seems strongly dependent on this small area dA/dx variation across the exit of the steam duct. It was observed that the value of the dA/dx shifted from positive to negative across the duct exit. This imparts an effect on the velocity profiles along the plane of symmetry, which can be realized upon the distribution of the perfect mixing zones, as shown in
Figure 5. Under all operating conditions initially, this gradient of area element, where blocking the cross-stream flow resulted in deacceleration, subsequently diverted it along the radial direction on both sides of the duct and accelerated it in the downward direction around the jet, eventually dissipating in the far-off fluid domain along the axial direction, as shown in
Figure 5. The stability plot based on the experimental data across the plane of symmetry is shown in
Figure 7c.
It was observed that the stability profiles follow the criteria set for the flow stability in the cited literature [
2], where the accelerating flows in the direction of the radius of curvature contribute to a stable flow, and the retarding flows contribute to the flow instabilities. It should also be noted that the flow stability had similar values in the surroundings of the steam jet exit duct as well as in the downstream part of the flow domain across the plane sheet. S ≈ (∂V/∂x)/(∂U/∂y) provides a measure of the rotational intensity of the steam swirl. Relatively smaller values of dA/dx point toward an unstable region, and larger values point toward an unstable uniform region.
The rotational intensity of the swirl is determined by determining the strength of the swirl, which is defined as the ratio of the axial flux of angular momentum to the axial flux of axial momentum. The rotational intensity of the swirl, S, is expressed mathematically as,
where
is the axial flux of linear momentum,
is the axial flux of angular momentum, R is the radius of the pipe through which the steam was injected, and
and
are the axial and tangential velocities.
The first two protrusions around the swirling steam exit duct may be attributed to the bending over the mainstream of water due to the virtual cover around the swirling steam jet exit duct where the flow accelerates. Another contribution may be due to the velocity fluctuations that are due to the inception and collapse of the steam bubbles, as shown in
Figure 7c. The last two protrusions are due to the contribution of the inward bending of the surrounding fluids; thus, after the wake region, the inward flow contributes to the velocity of the flow, which provides more stable flow within the regions, as shown by
Figure 7c. The flow in the leeward region was found to be more stable, which indicates the dominant role of the inward deflecting flow on the flow stability. The stability had a higher value on the left side than the right-hand side in the leeward section. The possible reason may be the head-on collision of the steam wave accompanied by the swirler fin. This results in more blockage by the virtual cover on the left-hand side than the right-hand side within the vicinity of the nozzle, which eventually converges with surrounding water at higher speed on the left-hand side of the leeward section than the right-hand side.
On the right-hand side, the fin almost supports the flowing water direction; thus, the two protrusions are large enough but have comparable sizes. The presence of flow instabilities is essential for the proper mixing of the two fluids if these interact with each other in such a manner that one fluid exerts a shearing effect upon the other one. The mixing will occur under the effect of a highly time-driven sequence of small-scale instabilities, whose strength depends on the structure of the shear layers. For this reason, on the plane of symmetry, the stability has lower values in the regions where the shear layers act in a more dominant way, thus generating retardation due to the blockage by the swirling steam in the adjacent windward quadrants, and their curvatures have positive values (
Figure 7b). The downstream area and surroundings of the swirling steam jet in the duct showed no protrusions; thus, regions with unstable flow domains, due to the highly time-driven sequence of small-scale instabilities, promote proper mixing [
2]. Overall, the total flow patches under the influence of stability protrusions, fulfilling all hydrodynamic conditions, can be seen in
Figure 7d. The experimental results shown in
Figure 7d are reproducible with varying errors depending upon the accuracy of the experimental setup. In the present setup, the errors in
Figure 7d range from 3 to 8%.
With increasing RPM at fixed operating inlet pressure, a decreasing trend toward instability occurred in the fluid domain across the plane sheet, and hence, a growing tendency toward proper mixing, which was governed and influenced dominantly by the small-scale instabilities, whereas overall, the variations in operating conditions had more than twice the effect on the area under the influence of these stability protrusions. Thus, an overall rise in inlet pressure contributed to improper mixing, whereas a rise in the RPM contributed to proper mixing.
3.3. Effect of Spatial Scaling of Swirling Steam Trajectory on Mixing in Cross-Flows
The swirling steam was injected into the cross-flowing water at varying inlet steam gauge pressures in the range of 1–3 bars and at a constant inlet gauge pressure of 1 bar of water. To examine the effect of the mixing on the spatial scaling of the swirling steam trajectory inside the cross-flowing water along the horizontal and vertical planes, the velocity data gathered by the HFA sensors were analyzed. It should be noted that in the current phase of experimentation, we had a total of 60 million data points (spatial resolution ~50 mm), which were collected for each sensor along the horizontal as well as vertical directions. The jet trajectory along the horizontal and vertical planes was based on the windward and leeward jet trajectory lines, as shown in
Figure 8a. It should be noted that the windward and leeward boundaries were drawn based on the time-averaged velocity values at 0.5 cm each. In previous studies [
2], different scaling methods were adopted, with the majority of the time scaling relying on the parameters stated as rd and r
2d (
, d is the diameter of the steam duct exit).
In the present case, the jet trajectory was scaled by using the same methodology as adopted in the cited literature [
2,
3,
5,
11,
23], first by calculating the height at which the jet remained vertical and after that point deflected to the right-hand direction. If it is considered that the steam exit has a diameter, d, and height, h, to the point that it remains vertical, the pressure gradient can be computed using the relation expressed as,
The vertical momentum flux in the present case can be given as,
Now the deflection of the steam jet under the influence of the cross-flowing water can be valid if the vertically acting momentum flux is comparable to the pressure gradient along the axial direction. This condition is given by the relation,
where
(in the present case ≈ 0.017) is the constant of proportionality. Now, if the velocity of the steam jet has been presented in terms of the effective diameter
, which is the diameter of the jet, density of steam jet
, and time-averaged velocity of the steam jet
the relation is given as,
Now, in the present case, where an effective diameter
has been calculated as
1–1.09, under all operating conditions, the effective diameter allows us to compare the jet trajectories under all operating conditions having the same values of
but different velocities. Simplifying Equations (11) and (12) results in the following,
Thus, from Equation (13), it is inferred that when the value of r is raised (in the present case by raising the inlet pressure of steam) on the right-hand side, the value of
will be raised also, to satisfy Equation (13), and thus, on physical grounds, the swirling steam jet will deflect to the right-hand side after gaining some penetration/vertical lift, which is denoted by
. It was observed that the rise in the RPM (60–300) contributed to the rise in the vertical penetration of the jet (15–19%). The penetration depth bears a relationship [
6] with the hydraulic diameter of the steam duct exit as well as with the ratio r, expressed as,
In our case, this condition was approximately satisfied with the value of
when it is lower than the value of
at RPM = 60 and 120 and Psteam, Pwater = 1 bar each. For higher values, the relation is given as,
This condition was approximately satisfied under the rest of the operating conditions (RPM = 180–300, P
steam = 2 and 3 bars, and P
water = 1 bar). By parameterizing the axis using the same scaling technique as proposed in the cited literature [
6], i.e., scaling of the axial and radial axes by rd = rd
steam (d
steam =
, the velocity distribution was obtained along the vertical plane, as shown in
Figure 8b. Using the scaled axis, the vertical trajectories of the velocities were collapsed into a tick strip composed of the velocity trajectories of the vertical jet along the vertical plane at all operating conditions, as shown in
Figure 8c. As the values of the proportionality constant,
and the penetration depth
were obtained from experiments. Upon further adjustment, i.e., scaling by r
2d with the corrected value of r, i.e.,
= 0.16–0.31 (for all operating conditions) for the vertical steam jet trajectory scaling, the velocity profiles collapsed nearer to each other, as shown in
Figure 8d. It was observed that the amended value of r is well suited for scaling the vertical trajectories of the swirling steam jet in cross-flowing water.
The scaling imparts a proportional effect on the calculated area under the effect of the perfect mixing. Although the vertical swirling impingement of the steam jet tried to recover the pressure loss at the steam duct exit with the help of the swirler, after the onset of the impingement, an irrecoverable loss of pressure, and hence, the kinetic energy inside the cross-flowing water, was observed [
6,
24]. It was observed that, based on the velocity points that represent the regions for perfect mixing, the scaling of the vertical trajectories of the swirling steam jets under all operating conditions merged the regions of perfect mixing to some extent. Thus, it was observed that by scaling the trajectories along the vertical plane, the area under the influence of perfect mixing was reduced to around 3–4.7% under all operating conditions. This method could be helpful for a number of flow-related studies involved in chemical and environmental fluid mechanics, where a large area needs to be studied. As in the environmental engineering domain, we can compare the different injection mechanisms of the brine from desalination plants inside flowing water reservoirs as the improper mixing of the brine, resulting in higher salinity near the brine exit into the flowing water [
5]. Thus, our observed flow domain size, as well as characterization requirements, would be reduced to inlet pressure/velocity of the brine and the resulting area under the influence of perfect mixing only, whereas in such cases, the discerning factor would be the relative concentration of salts inside the domain under observation.