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10 - VORTEX CAVITATION 243
where V is the freestream axial velocity and n the nuclei density. This characteristic
time depends strongly on n. For example, with
amm= 09.
,
Vms= 8/
, t
a
can vary
between about 1 second for deaerated water with a nuclei density n of the order of
0.05 nuclei/cm
3
to about 5 milliseconds in the case of strong nuclei seeding at a
concentration of 10 nuclei/cm
3
.
Similar estimates can be obtained for radial capture, on the basis of the H
SIEH
equation (see § 4.4 and LIGNEUL & LATORRE 1989) and the RANKINE vortex model.
The nucleus radius R is generally small enough so that it can be assumed that the
pressure gradient balances the viscous S
TOKES drag. An estimate of the time t
r
required for a nucleus situated initially at a distance r
0
from the vortex axis to reach
the axis is:
t
n
w
r
R
r
a
=
Ê
Ë
Á
ˆ
¯
˜
3
4
22
0
4
(10.33)
In this equation, a and w are connected to the circulation G by the relation
G=2
2
pwa
and can be obtained from LDV measurements. Typical values are
amm= 09.
and
w=10 000,/rd s
. The initial position r
0
depends on the nuclei density n and on the
typical length of the portion of the vortex path along which the capture of a nucleus
can actually trigger cavitation. For a rough estimate, we suppose that inception can
occur over a length of the order of the maximum chord length c. Then, on average,
a cylinder of radius:
r
nc
* =
1
p
contains one nucleus whose mean distance from the vortex axis is
rr
0
2
3
ª *
. Taking
the same values as previously for the nuclei densities, i.e. 0.05 and 10 nuclei/cm
3
,
and considering nuclei of radius
Rm= 5 m
and a chord length of 60 mm, one obtains
t
r
s= 098.
and
tm
r
s= 26
respectively [BOULON et al. 1997].
Thus, for both modes, the capture times are around one second in the case of
deaerated water, and they are considerably reduced if the nuclei content is
increased (e.g. using nuclei seeding). The frequency of cavitation events for vortex
cavitation strongly depends on the nuclei density, which explains that the incipent
cavitation parameter s
vi
, often defined on the basis of a threshold rate of events,
also depends considerably on water quality.
The effect of nuclei content is particularly important in the case of unsteady tip
vortex cavitation, such as on an oscillating foil [B
OULON et al. 1997]. Tip vortex
cavitation is then expected to occur only if nuclei have enough time to reach the
vortex core during the period of oscillation. It requires that the previous capture
times be much smaller than the characteristic period of oscillation, i.e. that the
nuclei concentration is high. Otherwise, a significant delay in cavitation inception
is observed in comparison with the quasi-steady case and the effect of water quality
becomes important.