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ÀRCHIEF

J. Fluid Mech. (1968), voi. 31, part 3, pp. 455-458 Printed in Great Britain

A note on shock diffraction

by a

By H. E. HUPPERTt AND L W. MILESt

Institute of Geophysics and Planetary Physics,

University of California, La Jolla

(Received 17 July 1967)

An earlier treatment of the diffractiOn of a shock wave advanòing into a regionof uniform flow, based on Clusnell's (1965) extension of Whitham's (1957) rule for shock diffraction, is corrected for analgebraic error and then compared with an analogous treatment based on the more recent extension derived by Whitham (1968). The basis for comparison is the pressure just behind a shock wave that is diffracted by a thin wedge travelling at supersomc speed The approximation provided by Whitham's extension is both simpler than, and typically superior to, that provided by Chisnell's extension (although the numerical differences are small in the Mach-number régime considered).

Lab.

y.

Schov;kinh

455.

Technscbe Ekgschc'oI

supersonic wedgEIf L

1. Introduction

We consider the diffraction of an approximately uniform, plane shock wave that moves into a regiòn of uniform, plane flow, inodifring an earlier analysis by Miles (1965). This analysis was based on Chisnell's (1965) extension of Whit-ham's (1957) treatment of a shock wave moving into a uniform, quiescent region and was applied to the calculation of the pressurejust bhind a diffracted shock wave on a wedge which penetrates that shock wave at supersonic speed. Theresult was compared with thatinferred from Smyrl's (1963) solution of the linearized boundary-value problem. Since then, Whitham (1968) has proposed that his original treatment be extended through a Gafflean trañsformation, with rsults that differ fröm those based on Chisnell's modification. Moreover, we have found that Miles's (1965) calculation of the initial angle of diffraction of the shock contained an error.

We present here a comparison of the alternative approximations to the

wedge pressure just behind the diffracted shock wave, based on the respective

methods of Chisnell (1965) and Whitham (1968).

.2. Shock-diffraction approximations

Assuming that all veloôities are approximatelyparallel (so that we may neglect -the squares of thê anglés of inclination), we consider an approximately uniform, plane shock wave that moves to the right with relative Mach number into .a uniform, plane flow of Mach number M. We require the change in ,ìz, say &z, associated with a small change, say 80, in the angle of inclination of the shock

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456 H. E. HuppertandJ. W. Miles

(80> 0 implies that the shock is locally concave with respect to the uniform flow on the right; see figure 1 of Miles 1965).

Employing ()hisnell's (1965) extension of Whitham's method to determine the variation of n with angle of diffraction of the shock, we obtain (Miles 1965)

(ôm\

-f

n+M

(òm\

\88jM

+L()MJ

8OJ

-where: (&m/80)0 is given by Whitham's [1957, equation (22)] 'shock-shock' relation for a shock moving into a quiescent region (M 0); the function L(») is given by Miles (1965) and decreases from 1

at m

=

1 through a very flat

minimum of approximately OE7774 near»z =3 to 07848 at -; = co (for y= 1.4). Employing WÏ:uitham's method in a reference frame for which the fluid velocity ahead of the shock is zero (Whitham 1968),we obtain, with no further assumptions,

f 6.m\ f 8m\

We remark that (1) reduces to (2) for

t-

1,

-co, and M-0, and that the

maximum discrepancy between the two results is roughly 30%.

3. Numerical comparisons.

Recalculating the ratio of the initial angle of diffraction of the shock wave to the wedge angle, we obtain (wheree is the shock-diffraction angle and a is the wedge deflexion angle; see Miles 1965, figure 2)

e/a=

M{m(M+)+[(1 K)i(M+)2(2+ 1)_m2(n2_ 1) (M2- 1)]}-1

x {M + m - (y +1) M( 1- Kn2) +

2r

X [(y± 1)m(2m+M-M2)

- (y- 1) (M+e)2(1 _K)-1J},

(3)

where

-2( +yKm2)t(1 _K)i{(n+M)2_(1

K)(cm2

1) (M2 1)}-i. (4)

This differs from the erroneous result reported by Miles[1965, equation (3.2)],

but can be shown to be in agreement with the

corresponding result implied by Smyrl's (1963) formulation. Typical numerical results are plotted in figures 1 and 2.

for all M. (2)

FIGuRE 1. The ratio of the shock diffraction angle e to the wedge deflexion angle for M=2 and F4 12

8

04 o 0 2 -4 o lo

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Shock diffraction by a .supersonic wedge 457 Repeating the approximate calculation of the pressure just behind the diffrac-ted shock wave on the wedge (Miles 1965, § 4), we find that the result based on (&m/&O)0 is significantly closer to the exact result than that

based on (8/O)

' -2

M

FIGURE 2. The ratio of the shock diffraction angle ç to the wedge deflexion ag1e a

for n = 2 and = 14. 300 275 250 225 200

.0

20 40 80 100

FIGURE 3. The relative pressure on the wedge, just behind thediffracted shock wave, for

M = 2 and y = F4. Curves O and i are based on (6n/t1O)0 and (8ø/&O)1, respectively;

curve 2 is based on the linearized boundary-value problem. p is the undisturbed pressure behind the incident shock wave.

for most 2 and M.t Typical results areplotted in figures 3 and 4, from which it can be seen that the use of eithervalue for (&m/8O) leads to an error of approxi-mately 5% (note that in both these figures the zero of the vertical axis has been suppressed and the vertical scale exaggerated in or4er to emphasize the difference between the different formulations).

t There do exist values of m; M for which the result based on is closer to the exact result than that based on (v/8O)0, but for these cases either formulation typically leads to an error of less than i %.

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458

4.5

40

3.5

3-0

H. E. Jiuppert and J. W. Milà

(1,

-I I I

o 1-0 2-O 3-O 4-0 5-0

se

Fiotmu 4. The pressure on the wedge, just behind the diffracted shock wave, for M = 4 and y = 14. Curves C) and i are based on (rn/8O)0 and 8(se/&8)1,respectively; curve 2 is

based on the linearized boundary-value problem.

4. Conchisiön

We infer from this comparison that Whitharn's original (1957) formulation typically provides a more accurate approximation for the diffraction of a shock wave moving into an area of uniform flow than does Chisnell's (1965) generaliza-tion thereof.

This work was supported in part by the National ScienceFoundation, in part

by the Office of Naval Research, and in part by

a Sydney University Post-Graduate Travelling Fellowship (H.E.H).

REFERENCES

Cmsizx, R. F. 1965 A note on Whitham's rule. J. Fluid Meché 22, 103-4. W 1965 A note on shock-shock diffraction. J. Fluid Mech. 22, 95-102.

Suyai, J. L. 1963 The impact of a shock wave on a thin two.dimensionai aerofoilmoving at supersonic speed. J. Fluid Mech. 15, 223-40.

Wnzm&j, G. B. 1957 A new approach to problems of shock dynamics.Part I. J. Fluid

Mèch. 2, 145-71.

Wrn&ai, G. B. 1968 A note on shock dynamics reintive to a moving frame. J. Fluid

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