Date Author Address
2006
EJ. Foeth, C.WH. van Doorne, T van Terwisga, B. Wieneke Deift University of Technology
Ship Hydromechanics Laboratory
Mekeiweg 2, 26282 CD Deift
Time resolved Ply and flow visualization Of 3D sheet cavitation
by
Ei. Foeth, C.W.H. van Doorne, T. van Terwisga and B. Wienke
Report Nò. 1538-P 2006
Magazine "Experiments in Fluids", Springer-verlag 2006, DOl 10.107./s00348-0O50082-9
TU D'e Ift
Deift University of Technology
Experiments in Fluids(2006)
DO! 10. 1007/s00348-005-0082-9
Rl!SIïARC'l-1 ARTICLE
E J. 'Foeth' C. W. H. van Doorne T. van Terwisga B. Wieneke
Time resolved PIV and flow visuälization of 3D sheet cavitation
Received: 20 ApriI 2005 / Revised: 22 July 2005 / Accepted: 24 October 2005 © Springer-Verlag 2006
Abstract Time-resolved PIV was applied to study ftilly
developed sheet cavitation on a hydrofoil with a spanwise
varying angle of attack. The hydrofoil was designed to
have a three-dimensional cavitation pattern closely
related to propeller cavitation, studied for its adversé effects as vibration, noise, and erosion production. For
the PIV measurements, fluorescent tracer particles were applied in combination with an optical filter, in order to
remove the reflections of the laser lightsheet by the
cavi-tation. An adaptive mask was developed to find the
interface'between.thevapor andiliquid phase. The velocity at the interface of the cavitywas found to be veryclose to
thevelocitypredicted by asimple streamlinemodeL Fora
visualizatión of the global flow dynamics, the laser beam was expanded and used to illuminate the entire hydrofoil
and cavitation structure. The time-resolved
record-ings reveal' the growth of the attached cavity and the
cloud shedding. Our investigation proves the viability of
accurate 'PIV measurements around developed' sheet cavitation. The presented' results will further be made
available as a benchmark for the validation of numerical simulations of this complicated flow.
i hthoductlon
Cavitation is' the evaporation of liquid' when thepressure falls below the vapor pressure. When such a low pressure región is formed near the leading edge of a hydrofoil, the
flow detaches and a pocket of vapor is formed, named' attached or sheet cavitation. Downstream of this sheet
.E J. Föeth () C. W. H. van Doorne T. van Terwisga
Laboratory of Ship Hydromechanics, Deift University of Technology, Mekelweg,2, 2628 ÇD Deift, The Netherlands
E,mail e.jFoeth@wbmt.tudeIft.nl
W Wieneke
LaVision GmbH, Anna-Vandenhoek-Ring 19, 37081 Goettingen, Germany
E-mail: bwieneke@lavisionde
cavity, the flow re-attaches to the hydrofoil and a
stag-nation point is formed. The positive pressure gradient in
this region forces a thin stream ofliquid upstream into thecavity, termed the re-entrantjet. When the re-entrant jet impinges farther upstream on the fluidvapor inter-face, part of the sheet cavity is pinched off and will be'
advected downstream. The advected cloud is often both
highly turbulent and bubbly in nature and may collapse
violently depending on the pressure condition. After the
shedding of a clóud, the attached cavity starts to grow again and the process is repeated. For an overview of cavitation, see Rood (1991, inception), Brennen (1995,
bubble cavitation), Arndt (2002, vortical cavitation) and Franc (2001, sheet cavitatiOn).
Sheet cavitation is a major cause of noise, vibration,
and erosion on ship propellers. As it is usually not': possible to avoid, it has to be controlled. Although the final evaluation of a propeller design is based on model experiments, numerical tools for cavitation simulation are becoming increasingly more important. Potential
flow solvers are currently the industrial standard(Young
and Kinnas 2001), and both Euler (Choi and Kinnas
1998; Sauer and Schnerr 2000) and RANS (Kunz et aL 1999; Senocak and Shyy 2001) codes are frequently
applied. More recently, LES is used to predict cavitatiOn
behavior (Wikstrom et al. 2003; Qin et al. 2003). How-ever, up to nOw simulations are not able to capture the
pressure radiated by cavitation or to predict erosion location and severity on propellers (ITTC 2002). In support of this rapidly expanding field of numerical
simulation, this experimental research was' started with a
threefold goal; firstly, analyzing the physical mecha
nisms of the instability of the flow; secondly, building a
data set of simple cavitating flows to be used as
bench-mark material and thirdly, extending the insights gained' to guidelines for propeller design. Validation material in the form of cavity volume, shedding frequency, velocity fields, and pressure measurement is essential.
Since cavitation forms one of the most important design criteria for ship propellers, there have been
interests have varied from the influence of the boundary
layer on the cavitation on axis-symmetric headforms (Arakeri and Acosta 1973), to the cavitation patterns observed on two-dimensional (2D) hydrofoils (Astolfi
et al. 2000). Callenaere et al. (2001) used a 2D backward
facing step to create a sheet cavity behind the step.
Despite the 2D geometry of the setup, the cavity was often found to shed vapor clouds intermittently and at
random locations, leading to a completely 3D and
complex flow field. Laberteaux and Ceccio (2001)
showed that the sweep (or skew) of the applied hydrofoil had a significant effect on the topology of the cavity and
on the direction of the re-entrant jet. For this 3D
geometry, the cavity was found to be far more stable.The importance of the re-entrant jet was further
demonstrated by Kawanami ( I 997), who blocked the re-entrant jet and subsequently altered the cavitationbehavior. From these and other experiments, it has
become clear that the form and stability of the cavitation
is very sensitive to the 3D geometry of the hydrofoil. Cavitation on ship propellers is distinctly 3D due to
the 3D geometry of the propeller, the radially increasing
velocity, the finite span of the blade and the periodic change of inflow conditions due to the wake behind a
ship. As studying cavitation on a rotating object is
inherently more difficult, it ¡s common practice to study
the flow on a steady (3D) hydrofoil with a cavitation topology and inflow condition closely related to pro-pellers. A 3D hydrofoil with its shedding mechanism
depending on its spanwise loading and reduced wall influence has a more structured and repeatable sheet
than a 2D hydrofoil at a constant angle of attack. This
allows for observations of the influence of controlled 3D
effects. Ultimately, we hope to be able to adjust the
propeller design in such a way that the cavitation pattern
is stabilized and the vapor shedding will be minimized. The main purpose of this paper is to show the via-bility of time resolved PIV measurements (Raffel et al.
1998) for the study of sheet cavitation. In Sect. 2, we first
present the experimental setup and the applied methods including a description of the cavitation, the applied 3D hydrofoil and the PIV setup. A common problem in the application of optical techniques to two-phase flows is
the risk of strong reflections in the direction of the
camera and the obstruction of the optical path (Tassin
1995). The first problem was avoided by the use of fluorescent tracer particles in combination with an
optical filter in front of the camera lens blocking all laser
light (Gopalan and Katz 2000; Bachert 2003). Particle
images of good quality were obtained in the liquid
phase, whereas the regions occupied by the vapor in the
cavity appeared as blurred region in the PlY images. To solve the latter problem, an adaptive mask was
devel-oped to find the interface between the vapor and the
liquid phase, as is discussed in Sect. 2.4. In Sect. 3 the
results are presented. When the vapor regions were
excluded from the PIV analysis, the velocity of the liquid
phase could be evaluated within about 1 mm from the cavity interface. Visualization is another indispensable
tool for the study of the global dynamics of the cavita-tion. When the laser beam was expanded to illuminate
the entire hydrofoil and cavitation structure, it was possible to obtain clear movies of the sheet cavity and vapor shedding. Finally, we summarize the work and
draw some conclusions in Sect. 4. 2 Experimental setup and methods
2.! Cavitation tunnel
The experiments were performed in the University of Delft Cavitation Tunnel shown in Fig. 1. The
measure-ment channel is 0.60 m long, the cross section is
0.297 mx0.297 m, with optical access from all sides.
Velocities up to 10 rn/s per second can be attained and the local pressure can be reduced to 5,000 Pa. The non-dimensional cavitation number, defined as
PoPv
a
Ipv0r,2 (1)and expresses the ratio of the pressure head to the
vaporization pressure (Pv) and the dynamic pressure (0.5 p V) at the entrance of the test section.The pressure was measured with ten Keller PAA-15 pressure transducers at each wall of both the inlet and
the outlet of the test section, and on two locations before
the contraction upstream of the test section (Fig. 2).
These sensors were calibrated in situ to within 1% error with a Keller PAA-33 pressure transmitter located in the
test section. The velocity at the entrance of the test
section (V0) was estimated from the pressure drop over
the contraction and the known contraction
ratio.Uncertainty analysis and error propagation indicated an
uncertainty in a of nearly 7.5% within a 95% confidence
interval for the presented measurements.
Fig. I Sketch of the cavitation tunnel. Theupperand leftleg are
rectangular, the lowerand right leg are cylindrical. The flow is counter clockwise and the air is evacuated at the dome on top of the tunnel
r,
L
Fig. 2 A close-up of the test section showing the hydrofoil, the location for the camera for Ply measurements (C) and the light sheet (L)
For the measurements, a stationary and spatially
uniform inflow was applied. The unsteady behavior of the cavity will, therefore, not be driven by an external
pressure field but by its intrinsic dynamics. In the future,
we also plan to apply periodic inflow conditions by
means of an upstream mounted flow oscillator.
2.2 Three-dimensional hydrofoil
The applied 3D hydrofoil was used before in a study by
Dang (2000), see Fig. 3. It spans the entire test section of 294 mm, and it has a chord length of 150 mm. The cross
section of the hydrofoil is defined by the NACA0009
thickness distribution (Abbott and von Doenhoff 1959).
In order to avoid damage during the manufacturing of
the hydrofoil, the profile's trailing edge was thickened to
a minimum of 0.4 mm. For this, the NACA polynomial
I(X)Nfor the dimensionless thickness was complemented
from x=0.35 until the trailing edge, where x=[0...1]
stands for the dimensionless chordwise coordinate, by
the following polynomial:
t(x) = t(X)N +
(maxm))C
t(l)N)
x
(x1)
H(x),
C is the chord length, t the non-dimensional thickness,
'min the non-dimensional minimum trailing edge
thick-ness, and Hthe heaviside function.
The hydrofoil is given a 3D shape by a variation in
the angle of attack (cc) along the spanwise direction (y):
C
Fig. 3 Top, side and front view of the hydrofoil. Theblack outlinein the top view indicates the viewing area of Fig. 6 (6.1-6.20)
cc(y) =
T(l6Y_
l2y
i2+i)
+ fi.The hydrofoil was manufactured with a span of 300 mm
trimmed to size to fit the test section. The center of
rotation of the hydrofoil is located halfway down the chord. The angle of attack increases smoothly toward the center of the hydrofoil by T= 8° (Fig. 4). The angle
fi is the rotation angle of the entire hydrofoil and is equal to the angle of attack at the wall, which was zero for our Ply experiment. This geometry results in a low-pressure
region in the center of the hydrofoil, and the cavitation
will develop here first. This immediately results in a 3D
shape of the sheet cavity without interference from the
walls.
In laminar flow, at low Reynolds number for smooth
objects, cavitation forms in the regions of laminar flow separation. Therefore, a natural transition to turbulence can temporarily suppress the leading edge detachment and the cavitation inception (Franc and Michel 1985).
Geometric angle of attack
8 7 6 4 2 o 0 50 lOO ISO 200 250 300 Span [mm]
This was avoided by the application of roughness ele-ments of 120 jim at the leading edge (4% of the chord length) as a turbulence tripping mechanism. Prior to the experiments, the tunnel was left to run for a few days
under minimum pressure conditions to ensure a minimal
gas content. The gas content was not measured, but the
roughness will supply the degassed flow with ample
nuclei for sheet cavitation to develop (Kuiper 1982). Incipient cavitation on roughness elements is typically observed when ti equals the minimum pressure coeffi-cient (Caron et al. 2000) and the nuclei content of the
flow is no longer critical.
2.3 PIV setup
The PIV experiment was performed with a New Wave
Pegasus dual-head, diode pumped Nd:YLF laser, with a 180 ns pulse duratiOn and an energy of 10 mJ/pulse at a repetition rate of 1,000 Hz. The light sheet wasP formed
with a compact system of cylindrical lenses, and the
lightsheet thickness was estimated at 2 mm. The energy density in the lightsheet was sufficiently low to avoid damage to the perspex windows of the test section.
An optical filter and fluorescent tracer particles were applied to block 'reflections of the lightsheet from the cavity interface This principle was successfully applied in cavitating flows by eg. Bachert (2003) The PMMA-Rhodamine B fluorescent particles' diameters are
typi-cally 20-50 jim and emit light in the orange band
(around 590 nm). Fourteen grams of tracer particles
were used on the tunnel volume estimated at 7.5 m3.
Although the particles are not neutrally buoyant
(p= 1.19x103 kg/rn3) and will settle between experiments (estimated settling velocity is less than 0.3 mm/s for the largest particles), they were quickly dispersed at start-up.
No appreciable decrease in the particle density was
noticed after i month of continuous running.
The camera used is a LaVision Flow-master High-SpeedStar 4 (Photron Ultima APX) with a FO bit dy-namic range, I Megapixel resolütiön at a repetition rate
of 2 kHz, and with 2.6 GB memory. A Nikon AF
Nikkor 50 mm lens was used, with an f-stop of 2.8. Thefield of view was 18x18 cm2, centered around the
hydrofoil in the lower part of the image. Small details such as the exact location of the flow detachment at the leading edge of the foil shown by Farhat and Avellan (2001) to occur within a region as small as 03% of the chord length for Re=:3x10,, corresponding to less than 2.5 pixels for the current magnification) are invariably
lost. However, the main focus of this research is to study
the large scale phenomena as the shedding sequence of the attached cavity and the flow around the cavitation
structures, and these were well resolved with the current setup.
Cavitation clouds that occur between the camera and the lightsheet can block the view of the camera on the lightsheet. In order to (partly) avoid this problem, the camera was tilted (8.2°) to view the cavitation structure
from above ('Fig. 2). This inclined viewing induces a small error in the vertical velocity component of about
1.4%. Viewing under large angles results in optical
aberrations and necessitates a larger depth of view but
for the applied angle neither effect was noticed.
2.4 PIV analysis
The evaluation of the vector fields from the PI V-images
is performed with the commercial PIV-software DaVis
7.0 from LaVision, and an overview of the parameters is
presented in Table 1. The effective measurement fre-quency (1 KHz) is half the camera frefre-quency, as single
exposure double frame PIV images were recOrded. With
a laser
pulse delay of 250 ms a
typical particledisplacement of 8 pixels at a flow rate of 7 rn/s was
obtained. The interrogation areas of 32x32 pixels large,
with 75% overlap were used, resulting in a
vector-to-vector spacing of 1.46 mm. Vectors with a deviation
larger than 1.5 times the R:MS of the neighboring
vectors were considered sptirious and were removed.
The final results are smoothed once with a 3x3 Gaussian kernel.
The refraction at the cavitation interface makes it impossible to have a clear view of the interior of the
attached cavity, and therefore no tracer particles can be
distinguished 'inside the sheet (Fig. 5.1), but particles can
be seen in the cloud. Although the optical filter in front
of the camera filters out the'strong reflections of the laser lightsheet, the cavity appears clearly in the PIV images,
as the entire test section is illuminated by the emitted light from the fluorescent tracer particles. For interro-gation areas that partly overlap the cloud, the blurred
and relatively high intensity level in this region can lead
to large errors in the estimated velOcities of the flúid motion at the cavity interface. To improve the accuracy
of the velocity near the cavitation interface, an adaptive
mask Was applied to the Ply images to exclude the
regions occupied by 'the cavitation, the hydrofoil and the entire región below the hydrofoil, from the vector
evaluation.
2.5 Adaptive mask
In order to exclude the regions occupied by vapor from the PIV analysis, an adaptive mask was developed to find 'the interface' between the liquid and gaseous flow
regions. The región within the mask was Set to zero
during PIV interrogation. The mask identified the vapor
region as the region where the minimal intensity (the background') level surpassed a certain threshold, due to the bright reflections on the cavity interface combined with the regions where the intensity of gradients was
small, indicating the absence of tracer particles. It is
stressed that the parameters of the mask, such as
threshold levels and filter lengths, were determined empirically in order to match the calculated cavitation
interface with the.iinterface observed by eye in the PIV
images The image was mirrored at its sides to avoid
errors when a filter window exceeded the borders of the
image.
In Fig. 5 (5.1-5.12) we show the intermediátesteps of the adaptive mask in more detail. Figure 5.1 shows an unprocessed PIV image The upper part of the image is
dárk as the frame of the test section blocked the view on this region of the flow. In the first step, a sliding median filter was applied to remove the particles from the image,
where the fifth minimal intensity level in a window of
5x5 pixels provided a convenient measure for the
background level, displayed in Fig. 5.2. A threshold was
applied to convert the background intensity into a
bin-ary image (Fig. 5.3), and pixels within a radial: distance
of 6 pixels of the active regions were added to the filter tO consolidate groups of neighboring pixels into con-tiguous regions (Fig. :5.4). As the intensity of the light-sheet was not constant, the threshold was varied across
the image.
Tracer particles1 typically a few pixels large, were detected in the original image by application of a
gra-dient filter using the following convolution kernels:
The gradient was calculated as + Kr. A
thresh-old was applied to the gradient level to obtain the binary image shown. in Fig. 5.5. Groups of isolated pixels were
identified and removed. The regions where no particles
occured within a radial
distance of 7 pixels were assigned to the masked region, as shown in Fig. 5.6.For the detection of the cavity interface, the region
occupied by the hydrofoil and the flow region below the hydrofoil were subtracted from the vapor region and the
vapor region was grown by another 6 pixels to smooth the surface (Fig 5 7) The interface was still very irreg-ulardue to either reflections ofbright tracer particles on the interface or the absence of tracer particles.
In Fig. 5.9 the regions detected by the large
'back-ground intensity and the absence of tracer particles were
combined to find the total región occupied by vapor.. Small and isolated regions corresponding to the wetted flow region were removed from the filter. 'For the final
smoothing of the cavitation interface, the' temporal
sequence of 2D masks was stagged into a 3D array and
smoothed three times by a 3D Gaussian kernel. The final
result is shown in Fig. 5.l'O, and the cavitationinterface
is shown together with the original PIV image in
Fig. 5.11..
The interface of the cavitation as determined 'by .the
adaptive mask corresponds reasonably well' toe the
interface observed by eye in the PIV images. However, the absence of particle images in several regions of the
flow, particularly near the' leading edge where the intensity of 'the lightsheet Was weak, resulted: in masking errors. For future measurements, the 'light sheet will be made more homogenous for an easier
identification of the sheet interface; The light 'sheet was
aimed' at the closure of the attached cavity, añd,
therefòre, this region was well illuminated. This is illustrated by 'the magnified view of the cavitation
interface in' the neighborhood of the closure region of 'the attached cavity in Fig. 5.1, and 'around the
sepa-'rated cavitation cloud in Fig. 5.2. From the latter image, it
can further be seen that
the cavitationi 0
±11 +.l+2 ±1
Kver = 2
0 +2
, Khor = O O O1 0 +1
1 2 1
Table I Overview of the
experimental parameters Tunnel Fluid Water
Max velocity 10 rn/s.
Min pressure 5,000 Pa
Min a '05
Test section Height 0.297 rn
Width 0.297 rn
Length 06 rn
Material Perspex
Wall .thickness 40 mm
Seeding Type Spherical
Diameter 20-50 pm
Light sheet Laser type. Nd:YLF
Maximum energy 10 mi/pulse
Wave length 527 nm
Pulse dùration 180 ns
Thickness 1.5 mm
Camera Type Photron Ultima APX Photron Ultima APX
Resolution 1,024x1,024 Pixels
Discretization '10 bit
Repetition rate 2,000 Hz
Imaging Lens focal length f-number
50 2.8
mm
Viewing area 180x180 mm2
Exposure delay time .1.0 IlS
Maximum particle displacement 8 Pixels
PIV analysis Interrogation, area 32x32 Pixels
Fig. 5 Steps in the adaptive mask to locating the cavity
interface.
5.1 Original Image
5.2 Sliding Median
interface around the vapor cloud is not well-defined, as
both particles and large reflections from the vapor cloud are observed in this region, but an exact
inter-face is unclear by any standard in this transitional
region. The cavity cloud was seen to strongly reflectthe light sheet thereby illuminating particles outside
5,5 Sobel edge filter. Isolated pixels removed
.Ss
5.6 Threshol and conglomeration 5.9 CombInation of the two filters
the measurement plane. Furthermore, liquid and
par-ticles are ingested into the cloud during its collapse. The mask is used to identify the entire region where
PlY interrogation will lead to unpredictable results but
makes no further attempt at differentiating between
sheet and encompassed cloud structures. 5.4 Grown threshôld 5.8 Gaussian icernel 5.11 PliaI result
5.7 Grown, known hydrofoil locatIons 5.10 3D Gaussian filtering substructed
Another problem is that vapor structures in front of the light sheet will block the view of the camera. It is, therefore, uncertain to what extent the cavitation
inter-face detected by the mask corresponds to the actual
interface in the cross section of the light sheet. However, since We performed our measurements in the symmetry plane of the 3D hydrofoil where the cavitation structures
are the largest, as follows from the results of the flow visualization, we assume that the mask provides a fairly
accurate estimation of the cavitation interface in the
plane of the light sheet.
3 Results
3.1 FlOw visualization
For the flow visualization shown in Fig. 6 (6.1_6.20): the
laser beam was expanded to illuminate the entire
cavi-tation structure. The images were recorded with the PIV
camera, repositioned to view the suction side of the
hydrofoil at a straight angle.
In Fig. 6.1 the. attached cavity has reached its maxi-mum length and is crescent shaped due to the spanwise
variation of the lôading of the hydrofoil. The strong
adverse pressure gradient in the stagnation region at the
downstream end of the cavity forces a re-entrant jet into the vapor structure. The velocity is known toreflect on the envelope of the cavitation interface (de Lange 199 8), and
for a cavity with a 3D shape the reentrant jet will thus
have different directions. The re-entrant floW Will c011ide
in the center of the foil and at this point the cavity Willi quickly change from a smooth pocket of attached vapor
into ahighly turbulent region and detach from.the leading
edge [Fig. 6 (6.2-68)] The vapor cloud becomes
turbu-lent and is advecteddownst ream bythe main flow, as seen in Fig. 6 (6.16, 6.17). In the final images of thecollapse of
the vapor cloud, a clear vortex structure is observed
[Fig. 6 (6..l7-6.20)] In Fig. 6 (6.1 3-6. 18; indicated by the
letter A in Fig. 6.17) also two smaller vortices are seen to form at the downstream end of the attached cavity,
considered a small secondary shedding.
The entire shedding cycle was very periodic and a full
period took approximately 47.5 ms, corresponding to a
Strouhal number of St=0.19, based on cavity chord
length and mean stream velocity V0. This is significantly
lower than the the Strouhal number observed for 2D flows (IL/v0 =0.251 + o- = 0.33) by Arndt (1995). From this, we conclude that the behavior of the 3D
cavity is significantly different from that in a 2D cavity,
and a more detailed study on the 3D effect of the cavity on the re-entrant jet and global dynamics will be pre-sented in later work.
3.2 Cavitation interface
The temporal development of the cavitation interface is shown in Fig. 7 fora period of 100 ms, corresponding
to a sequence of 100 PlY images. The shedding of the attached cavity is well visible The vapor cloud is fur-ther seen to increase quickly in height as it is advected downstream. This sudden expansion of the cavitation cloud above the hydrofoil has not been captured by 2D calculation with Euler codes (Sauer 2000). This
evOlu-tion of the cavitaevOlu-tion cloud is more likely to be the
captured by Large Eddy Simulations (Qin 2003) The variatiön in location
of the
flow separation atthe leading edge of the hydrofoil is not physicaL It
shows that the mask was less accurate near the leading.
edge, due to the poor illumination of this region. In
future, a more homogenous light sheet will applied to
improve the idéntification of the cavitation interface
close to the leading edge.
3.3 PIV results
Figures 8.1, 8.2 and 9 show different examples of the evaluated vector fields and the contours of the cavity
interface. The velocity appears to be parallel to the interface when the cavity is attached (Figs. 8. 1, 9).
Assuming the flow along the cavity to be (1.)
approxi-mately stationary, (2) two-dimensional and (3) at a
pressureequal to the vapor pressure, asimple streamline model can be used to estimate the velocity at the cavi-tation interface, refered to as the vapor pressure ( Vv).
From Bernoulli's equation (P0 ±O.5p V Pv + O5p Vv)
in conjunction with Eq. 1 we obtain:
Vv/(1+o-)Vo.
(2)Based on pressure measurements on both sides of the: contraction upstream of the measurement section, Po» and Vo were determined, and the vapor velocity was
estimated at Vv=9.24 m/s ±5%. For the veloòity
field shown in Fig. 9, we have plotted the vertical velocity profiles along the indicated lines in Fig. 10 Although some fluctuations due to the mean stream
turbulence can be observed, the (instantaneous) velocity
of the profiles AE are seen to converge toward the vapor velocity at
the cavitation interface. For the
profile F, a distinct velocity deficit is observed. This may be due to instationary effects near the end of thecavity,
as the cavitation closure
is moving down-stream. Profile F shows that just downstream fromthe sheet cavity, the streamwise velocity component is 20-30% smaller than the undisturbed inflow velocity
(V0). Behind the cavitation
cloud, a very strong
downwash is measured probably induced by the roll up of the cavitation cloud into a vortex. The stream-wise velocity is sometimes as low as 1 rn/s near the surface of the hydrofoil while the vertical velocity components can reach 4.5 rn/s.
The region directly upstream of the shed cavitation
cloud in Fig. 9 contains a large number of spurious véctors A ñumber of effects contribute to the poor
Fig. 6 Flow visualization at
14=7.04 rn/s ±1.16%, ß1°,
a=0.77±7.4%, recorded at f= 2.000 Hz showing every fifth
frame. Viewing area as outlined in Fig. 3. flow from top to bottom, white lines indicate leading and trailing edge location
6.1 1=0.Oms
cavitation interface around the vapor cloud is not well defined, as both particles and large reflections from the
vapor cloud are observed in this region. The large
background noise in the Ply images increases the PIV correlation noise significantly. Second, from the high-speed flow visualizations, it is seen that the cavitation cloud is highly turbulent. Gopalan and Katz measured a Reynolds shear stress 25-40% of normal stress in the closure region. The loss of particle pairs due to strong out-of-plane motions is therefore high, increasing the correlation noise further.
4 ConcIuson and discussion
Time-resolved PIV was applied to study sheet cavitation
on a hydrofoil with a spanwise varying angle of attack.
In order to block strong reflections of the laser lightsheet
by the cavitation, fluorescent tracer particles were
applied in combination with an optical filter. Neverthe-less, the cavitation structures were clearly visible in the Ply images, due to the reflection of light emitted by the fluorescent tracer particles. Refraction at the cavitation 6.5 1=10.0 ma 6.61=125 ma 6.71=15.0 ma 6.81=17.5 ma
6.91=20.0 nis 6.101=22.5 ms 6.111=25.0 ma 6.l2t=27,5ms
6.13t300ma 6.14t='32.5nis 6.l5t=35.Oms 6.161=37.5mg t.
6.17 1=40.0 ma 6.18 t=42.5 ais 6.19 t=450 ma 6101=47.5 ma
Fig. 7 Development of the cavity interface at the center plane of the foil as determined by the adaptive mask for a period of 100 ms
Fig. S Details of a PIV frame a at the closure region of the
attached cavity; b upstream of a collapsing vapor cloud. For the attached cavity, the velocity vectors are parallel to the interface.
The obstruction of the view on the light sheet close to the
stagnation point at the downstream end of the cavity (indicated by the letter A) makes it impossible to observe the re-entrant jet with the current setup
Hg. 9 A vector field near the end of growth cycle before post processing. Only 50% of the vectors are shown in the horizontal direction for clarity. The velocity profiles along the indicated lines are shown in
Fig. IO
s
interface makes it impossible to see into the cavity to perform PIV in the vapor region and the re-entrant jet could not be observed from the PlY images. In order to improve the velocity estimation close to the cavitation interface, an adaptive mask was developed to exclude the vapor region from the PIV analysis. The velocity at
the interface of the attached cavity was found to be parallel to the interface and very close to the vapor
velocity estimated with Bernoulli's equation. The inter-face of the shed cavitation cloud that appeared was not well defined as both particles and vapor could often be
observed simultaneously, leading to reduced
perfor-mance of the mask and PIV analysis close to the cloud. Due to strong turbulence levels around the collapsing cloud, there was a considerable loss of particle pairs in
the Ply images, leading to an increased noise level in this region.
For a visualization of the global flow dynamics, the
laser beam was expanded and used to illuminate
the entire hydrofoil and cavitation structure. The timeresolved visualizations reveal the growth of the attached
cavity and the cloud shedding that follows it in every
detail. The vapor cloud is seen to increase remarkably in height as it is advected downstream. The vapor shedding
cycle on the applied 3D hydrofoil was further found to be highly periodic with a Strouhal number 30% smaller
than observed for 2D sheet cavitation. This confirms the important influence of the 3D geometry of the hydrofoil
on the flow dynamics and stability of the cavitation
pattern.
In the near future, the current work will be extended to the study of the cavitation and flow dynamics under
instationary inflow conditions, and a more profound investigation of the effect of the 3D geometry of the
hydrofoil on the cavitation patterns will be performed.
Acknowledgements This research is funded by the Dutch Technol-ogy Foundation STW project TSF.61 70 and Royal Netherlands Navy. See http:/iwww.stw.nl for more details
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