In the current study, the evidence of the generation of hydrodynamic instabilities as well as their propagation was found by recording temperature profiles across the steam jet using the device developed as shown above. This was achieved by determining the influence of steam’s inlet pressure and temperature of water in the vessel on the temperature variation on axial profiles and radial profiles obtained across the steam’s jet.
3.1 Axial Temperature Profiles
As stated above nearly 60,000 temperature readings were obtained along the vertical axis of the steam jet to look at the generation of hydrodynamic instabilities and their influence on the interface involving supersonic steam jet and the surrounding water.
Influence of Water Temperature & Steam Inlet Pressure: Axial temperature measurements presented in Figure 5 were obtained with the steam’s inlet pressure varying within 1.5 – 3.0 bars, whereas, the temperature of the water in the tank ranged from 30oC to 60oC. The temperature profile obtained at 30oC shows that the temperature reduces along the axis, however, in the region close to the nozzle’s exit, the profile reveals independence from the temperature of the surrounding water [14], [15], [16], [17]. When the water temperature in the column increased, the nature of the temperature profile along the axis developed highly fluctuating. This was possibly due to the overturning motions being formed at the interface that involved entrapping water from the region in the neighbourhood of the interface [18]. Further, at low water temperature in the vessel, the condensation rate is higher, which causes the minimal instabilities across the steam-water interface because of the sub-cooling. Higher condensation rate provides a calming function to reduce the instabilities at the interface. Another interesting outcome from the Figure. 5 is that with increase in the steam inlet pressure, axial temperature profile seems more continuous at low temperature of the water in the column, which reveals the importance of the influence of temperature of water in the vessel on the variations of temperature within the steam jet.
At a higher temperature of the water in the column, the axial temperature profiles showed strong fluctuations [14][17] particularly when the temperature of water raised from 45oC to 60oC. Such observations were evident due to the higher steam jet’s velocity than the water in its surroundings that generated KH instabilities across the interface. Due to an increase in steam pressure, an increase in the amplitude owing to the fluctuations in temperature was observed, which hinted to an increase in the growth of these instabilities at the interface, thus resulting in an increased entrapment of water (i.e. ~20 - 30 mm). Therefore, with an increase in steam’s inlet pressure and water temperature in the vessel, the penetration length and the width of the jet also increased that has been in accordance to the earlier measurements [14-15,19-20]. Since, an under disbursed nozzle [15] was used for steam injection here. Thus, the pressure at the nozzle’s exit should be larger than the pressure being exerted backwards. In accordance with the compressible flow theory [21] an expansion wave occurs for the present case at the nozzle’s exit because of the pressure difference between the nozzle’s exit and backpressure. With an increase in steam’s inlet pressure, the nozzle steam rate increases, along with an increase in exit pressure and Mach number. Increase in pressure at the nozzle’s exit also raises, it’s gap over the backpressure, which triggers the steam jet to expand explosively, this results towards a reduced pressure as well as the temperature, outside of the nozzle’s exit, which can be seen in the temperature profiles in the Figure. 5.
Occurrence of hydrodynamic instabilities due to unstable interface:
With the help of Figure. 5 an attempt is made here to determine the effect of pressure of steam injection and change in temperature of the surrounding water in a column on the interface between the steam and water. Here, the reasons have been elaborated relating to the existence of fluctuations in temperature obtained along the centerline of the steam jet, which is ascribed as the KH instabilities. Even such instabilities have appeared at steam’s inlet pressure of 1.5 bars, signifying the velocity difference as the lowest possible between the steam and the water. The instabilities propagate along axial centreline. The temperature profiles, found at steam’s pressure of 1.5 bars against a range of water’s temperature in the column, particularly temperature greater than 45oC, are shown in a magnified view in Figure 6. It is apparent from the Figure that when the temperature of water in the column raises with even maintaining the inlet pressure constant, the jet becomes unsteady [20,22] as evident from the very fluctuating temperature profiles as exhibited by the regions 1, 2 and 3 corresponding to the higher water temperatures of 50, 55 and 60oC respectively in the vessel.
Whilst steering the sensors from the front of the jet to the nozzle’s exit along the centerline, it was found, at first there were minimal variations in the temperature contours at nearly 50 mm farther from the nozzle’s exit. Nearly all the temperature profiles show elevated fluctuations being emerged at a distance varying between 20 mm and 40 mm, which depended upon the temperature of water in the column. At higher sub-cooling, i.e. 30oC it was found that the fluctuations existed at a distance within the vicinity of the nozzle exit. Also, the amplitudes associated with the fluctuations appeared in case of water temperature of 30oC were smaller than those obtained for temperatures higher than 45oC. The spontaneous appearance of fluctuations was mainly due to the high sub-cooling; in this case, the penetration distance of the jet was small. Thus, the surface area accessible for the heat transfer as well as mass transfer from steam to water was small as well. The fluctuations across the interface occurred owing to the gradient of velocities within this region, subsequently these fluctuations propagated to the centerline of the jet. Due to the increase in water temperature, the distance, where the fluctuations occurred, increased in addition to the increase in fluctuations’ amplitude. Also, fluctuations shifted to the right, as seen in Figure. 6, exhibiting a dislocation of the interface away from the nozzle’s exit to the water region. These fluctuations may be ascribed as condensation oscillation (CO) as reported by Arinobu, 1980 [23]; Aya & Nariai, 1991 [24]; Chun et al., 1996 [22]; Yan et al., 2010 [20] which occurred at low mass flux with rise in water temperature in the vessel, thus giving rise to the instability at the interface of the steam jet and water [25]. Formation of these fluctuations along the axial axis of the jet at the temperature of the water in the vessel greater than 45oC may contribute to increase the shear across the interface, which caused KH instabilities. It is well known that at elevated values of inlet pressure, the flow rates and the Mach number of the steam leaving the nozzle may increase, which may induce additional momentum into the water layers in the neighbourhood of steam jet, which may provide added intensity to the KH Instabilities. These instabilities consequently grew into eddies that acted to entrain the water by the steam at its interface [18], which gave rise to fluctuations that propagated towards the mid, along the centerline (r= 0) of the jet. Moreover, in case of higher condensation interface between the steam and water. Here, the reasons have been elaborated relating to the existence of fluctuations in temperature obtained along the centerline of the steam jet, which are ascribed as the KH instabilities. Even such instabilities have appeared at steam’s inlet pressure of 1.5 bars, signifying the velocity difference as the lowest possible between the steam and the water. The instabilities propagate along the axial centerline. The temperature profiles, found at steam’s pressure of 1.5 bars against a range of water’s temperature in the column, particularly temperature greater than 45oC, are shown in a magnified view in Figure 6. It is apparent from the Figure that when the temperature of water in the column raises with even maintaining the inlet pressure constant, the jet becomes unsteady [20,22] as evident from the very fluctuating temperature profiles as exhibited by the regions 1, 2 and 3 corresponding to the higher water temperatures of 50, 55 and 60oC respectively in the vessel.
Whilst steering the sensors from the front of the jet to the nozzle’s exit along the centerline, it was found, at first there were minimal variations in the temperature contours at nearly 50 mm farther from the nozzle’s exit. Nearly all the temperature profiles show elevated fluctuations being emerged at a distance varying between 20 mm and 40 mm, which depended upon the temperature of water in the column. At higher sub-cooling, i.e. 30oC it was found that the fluctuations existed at a distance within the vicinity of the nozzle exit. Also, the amplitudes associated with the fluctuations appeared in case of water temperature of 30oC were smaller than those obtained for temperatures higher than 45oC. The spontaneous appearance of fluctuations was mainly due to the high sub-cooling, in this case the penetration distance of the jet was small. Thus, the surface area accessible for the heat transfer as well as mass transfer from steam to water was small as well. The fluctuations across the interface occurred owing to the gradient of velocities within this region, subsequently these fluctuations propagated to the centerline of the jet. Due to the increase in water temperature, the distance, where the fluctuations occurred, increased in addition to the increase in fluctuations’ amplitude. Also, fluctuations shifted to the right, as seen in Figure. 6, exhibiting a dislocation of the interface away from the nozzle’s exit to the water region. These fluctuations may be ascribed as condensation oscillation (CO) as reported by Arinobu, 1980 [23]; Aya & Nariai, 1991 [24]; Chun et al., 1996 [22]; Yan et al., 2010 [20] which occurred at low mass flux with rise in water temperature in the vessel, thus giving rise to the instability at the interface of the steam jet and water [25]. Formation of these fluctuations along the axial axis of the jet at the temperature of the water in the vessel greater than 45oC may contribute to increase the shear across the interface, which caused KH instabilities. It is well known that at elevated values of inlet pressure, the flow rates and the Mach number of the steam leaving the nozzle may increase, which may induce additional momentum into the water layers in the neighbourhood of steam jet, which may provide added intensity to the KH Instabilities. These instabilities consequently grew into eddies that acted to entrain the water by the steam at its interface [18], which gave rise to fluctuations that propagated towards the mid, along the centre line (r= 0) of the jet. Moreover, in the case of higher condensation, however, the plots in Figure. 7 and Figure. 8 present the data obtained from all the six sensors.
The temperature profiles illustrated in Figure 8 became more uninterrupted at 30oC due to the increase in steam inlet pressure, this indicates an inclination of the jet transforming towards stability which was referred by Chun et al., (1996) [22] as stable condensation. At elevated water’s temperature in the column, the jet became fiercely unstable because, at elevated values for the temperature, the interface moved with larger velocity than the surrounding water, this resulted into the formation of KH instability at the interface. Moreover, the temperature profile in Figure 8, seems non-symmetric, the region within the centreline of the jet at a radial distance, r = 0, particularly when the temperature of the water in the column exceeds 45oC. It can also be seen in Figure 8, that the width of the jet has been raised with a rise in pressure, which supports work performed elsewhere [18][15][25][19]. The temperature profiles obtained at all pressures show peak temperature values at r=0, these values decrease to the ambient when the temperature sensors were moved away from the centre of the jet, which is found consistent with work reported by Song, Cho, & Kang, 2012 [26]; X.-Z. Wu, Yan, Li, et al., 2009 [15]; J. Yan et al., 2009 [17] for sonic and by X. Z. Wu et al., 2010 [16] by supersonic and on CFD basis by Davies, 1967[27]; Gulawani et al., 2006[18]; Xu et al., 2013[28] for steam jet. Since, the six sensors were not located at the same position on XYZ coordinates during recording temperatures, it is then worthwhile to disclose that the sensors may have recorded even the minor fluctuations in the temperature, which may have been generated transiently. However, these sensors were calibrated as being placed stationary and letting them in motion through water at temperatures varying from 30oC to 60oC, the sensors responded no departure from a linear response, thus, confirming the validity of measurements. It is useful to express here the earlier studies [24][17][16] [26][28], which were performed relating to the temperature measurement across the steam jet radially, the thermal sensors crossed one end of the jet on the horizontal axis to the other end of the jet. However, no study was performed supporting coordinated temperature measurement with six sensors located on a plane tending a fixed angle of 60o between each other to determine a temperature distribution at a high sample rate as performed here. The method adopted here, can acquire the factual temperature profile at the same time along six different angular locations at an elevated speed, accuracy and spatial resolution can apprehend the indication of KH instabilities and their propagation associated to the injection of the supersonic steam into the subcooled water.
3.2 Radial observation of Hydrodynamic instabilities:
Capturing temperature fluctuations across the steam jet’s interface with the surrounding water was mainly to find the sign of the presence of the Kelvin Helmholtz instabilities because of the change in velocities between the steam and the water. The instabilities were much short-lived. Thus the equipment specialised in highly spatially determined temperature measuring was utilised to capture them, as reflected in Figure. 9. The generation of these instabilities, along with their propagation across the interface, can be portrayed from the Figure. 9-10. The temperature profiles in Figure 10 were transformed with the help of scattered points in Figure. 8 & 9. However, when the scattered points were joined together, they did not convert to a solid line, rather small ridges and depressions indicating amplified fluctuations in the temperature profiles obtained for up to r > 0.02 m, as seen in area 1, 2, and 3 in Figure. 10. Such fluctuations were formed due to the velocity shear and buoyancy between steam and water. Whereas, the gravity normally acts to reduce the shear in the vertical flows. Thus, with lessened shear, the expectations of the formation of eddies are fewer. Because of the formation of a minimal number of eddies indicates the reduced ability of the steam’s jet to entrain the surrounding water through the interface. Thus, reduced entrainment of water across the interface provides comparatively lessened generation of KH instabilities, which is evident from the increased fluctuations in temperature as seen in Figure. 9.
Additional contribution into the generation of KH instabilities associated with the fluctuations in temperatures at low sub-cooling of 45oC – 60oC can be because of the variation in water stream's dynamic viscosity at the interface with an increase of temperature of the water in the column. This can be described as followed: the surface tension of the water surrounding the steam jet decreases from 71.20 x 10-3 down to 66.24 x 10-3 N/m (e.g. [29]) as a rise in temperature of surrounding water occurs from 30oC to 60oC respectively, whereas corresponding to the same range in temperature, the dynamic viscosity decreases from 0.798 x10-3 down to 0.467 x 10-3 N-s/m2. So, a drop of about 6% in surface tension and 60% in viscosity occur with increase in temperature from 30oC to 60oC. Thus, the role of viscosity to damp the discontinuous propagation of the instabilities is effective at higher sub-cooling values. However, when the water temperature in the vessel goes up from 30oC to 60oC, the viscosity may reduce nearly half of the value, thus supporting more to the propagation of instabilities being observed across the steam-water interface. Another contribution into the high amplitude associated to the fluctuations in the temperature is due to the thermal and momentum exchange across the interface. When the sensors were steered to the nozzle exit, drop in the local density and viscosity of the water surrounding the steam’s jet was occurred due to the higher temperature of the steam jet than the water. This in turn induced an increase in the upward axial flow velocity, which was smoothed by the thermal and momentum exchange acting perpendicular to the axial flow of the steam’s jet and this contributed towards a rise in abrupt temperature fluctuations [30].
A further significant from Figures. 9 and 10 is the asymmetric behaviour of the radial temperature distribution, which has become more apparent in their 3D profiles (Figures. 9 and 10). From these Figures, the asymmetric trend can be seen in two opposite directions, which was reported in many investigations [12,16, 28, 31-33] dealing with the flows of compressible fluids. The reason behind this trend could be associated to the high intensity of turbulence across the interface. Also, the asymmetric behaviour can not only be seen in the adjacent sensors (Figure. 10(a)) but is also true in case of opposite sensors (Figures. 8 and 1(b)).