118
()()()()
8350.09948.09959.09966.08457.0
p
p
p
p
p
p
p
p
p
p
1o
2o
2o
3o
3o
4o
4o
5o
1o
5o ===
Four oblique shocks:
°=δ
6
9972.0
p
4o
5o
=
Normal Shock
p
6o =
()()()()()
9097.09948.09959.09966.09972.09239.0
p
p
p
p
p
p
1o
2o
3o
4o
5o
1o
Problem 12. – Two oblique shocks intersect as shown in Figure P6.12. Determine the
flow conditions after the intersection, with γ = 1.4.
Figure P6.12
M = ?
p = ?
T = ?
V = ?
40º
40º
M = 2.2
p = 70 kPa
T = 270 K
From Gas Dynamics, Third Edition, by James E. John and Theo G. Keith. ISBN 0-13-120668-0. © 2006 Pearson Education, Inc.,
Upper Saddle River, NJ. All rights reserved. This material is protected under all copyright laws as they currently exist. No Portion of
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119
p
3
Problem 13. – Show that the entropy increase across an oblique shock is given by,
(Ref. 7)
+
γ
γ
θ
γ
=
γ
22
22
1
2
1
1
sinM
2
ln
s
From Eq.(6.13)
22
1
22
1
1o
1
1
sinM
1
2
sinM
2
1
1
p
+γ
γ
θ
+γ
γ
θ
γ
+
and since cv = R/(γ – 1), the above can be written as
1
22
1
1
1
sinM
2
1
+γ
+γ
θ
+γ
So
()
+γ
+γ
θ
+γ
γ
1
1
sinM
2
1
1
R
1
22
1
Or
From Gas Dynamics, Third Edition, by James E. John and Theo G. Keith. ISBN 0-13-120668-0. © 2006 Pearson Education, Inc.,
Upper Saddle River, NJ. All rights reserved. This material is protected under all copyright laws as they currently exist. No Portion of
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120
+
γ
γ
θ
γ
=
γ
22
22
1
2
1
1
sinM
2
ln
s
Problem 14. – Repeat the computations of Example 6.2. However, instead of using the
successive substitution method proposed by Collar, and described in Section 6.3, solve
the problem using the Newton-Raphson method.
γ M1 A B C B – AC 1rst guess
1.3 2.0 3.0000 2.9143 0.8870 0.2534 1.7321
Newton-Raphson Method
iteration xold f fprime xnew
Problem 15. – For the two-dimensional case shown in Figure P6.15, determine M3 and
p3. γ = 1.4.
Figure P6.15
°=δ
=
5
8.2M1
5677.2M
6427.24
2
=
°=θ
p3 = ?
p1 = 10 kPa
M1 = 2.8
M2 M3 = ?
From Gas Dynamics, Third Edition, by James E. John and Theo G. Keith. ISBN 0-13-120668-0. © 2006 Pearson Education, Inc.,
Upper Saddle River, NJ. All rights reserved. This material is protected under all copyright laws as they currently exist. No Portion of
this material may be reproduced, in any form or by any means, without permission in writing from the publisher.
=
5677.2M2
7305.26
°
=
θ
Problem 16. – Prove that: (a) at the minimum shock angle, M2 = M1 and (b) at the
maximum value of the shock angle, Eq.(6.17) becomes Eq.(4.9)
()
θsinM
2
1γ
1
θcosM
2
1γ
θsinMγ
M
2
1γ
1
M
22
1
22
1
22
1
2
1
2
2
+
+
+
= (6.17)
(a) at the minimum shock angle
The minimum shock angle is the angle of a Mach wave for which θ = sin1(1/M1).
Accordingly, (M1sinθ)2 = 1 and (M1cosθ)2 = M12 – 1. Therefore,
2
1
2
1
2
1
M
1
2
M
1
2
M
1
1
1
2
=
+γ
+γ
+
+γ
γ
+
+γ
=
(b) at the maximum value of the shock angle
From Gas Dynamics, Third Edition, by James E. John and Theo G. Keith. ISBN 0-13-120668-0. © 2006 Pearson Education, Inc.,
Upper Saddle River, NJ. All rights reserved. This material is protected under all copyright laws as they currently exist. No Portion of
this material may be reproduced, in any form or by any means, without permission in writing from the publisher.
122
0
M
2
1γ
1
θcosM
M
2
1γ
1
M
2
1
22
1
2
1
2
2
+
+
=
+
+
=
which is Eq.(4.9).
Problem 17. –Develop Prandtl’s relation for oblique shocks from conservation principles.
Begin by writing the energy equation, Eq.(6.5c), as
()
2
12
11
2
1
o
ρ
γ
ρ
γ
γ
Thus,
+
γ
22n
2
o
1
a
γ
γ
t
1n
11 VV
2
From the momentum equation, Eq.(6.5b),
Combining these yields
γ
γ
γ
γ
γ
γ
2
2
2
2
Rearrangement gives
From Gas Dynamics, Third Edition, by James E. John and Theo G. Keith. ISBN 0-13-120668-0. © 2006 Pearson Education, Inc.,
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123
t
o
12
22n2
2
1n1 V
1
a
1
+γ
+γ
=
ρρ
Using the continuity equation, Eq.(6.5a), the expression can be simplified to
obtain Prandtl’s relation for an oblique shock wave
t
o2n1n V
1
1
+γ
+γ
Problem 18. – The largest deflection angle for the limiting upstream Mach number,
M1 , can be found by differentiating Eq.(6.26), setting the result to zero and then
solving for θ. In other words, verify that Eq.(6.27) is correct.
From Example 6.4 it was shown that
θ
Therefore,
θ
θ
θ
θ
+
γ
()
2cos
d
θ+γ
θ
Cancel the 2 and rewrite the numerator as
Therefore,
γ
=θ=θθ=θ 1
sin21sincos2cos 222
So that
γ
+
γ
=θ 2
1
sin2
Problem 19. – In general, the angle of incidence, θi, and the angle of reflection, θr, of an
oblique shock reflected from a flat surface are not equal. However, see Refs. 8 and 9,
there is an angle θ* such that the two angles are equal. Also, if θi < θ*, then (θrδ) < θi,
and if θi > θ*, then (θrδ) > θi. Computationally verify that for M1 = 2, 3 and 4 at
γ = 1.4, the angle of incidence and the angle of reflection of an oblique shock reflected
from a flat surface will be equal if
From Gas Dynamics, Third Edition, by James E. John and Theo G. Keith. ISBN 0-13-120668-0. © 2006 Pearson Education, Inc.,
Upper Saddle River, NJ. All rights reserved. This material is protected under all copyright laws as they currently exist. No Portion of
this material may be reproduced, in any form or by any means, without permission in writing from the publisher.
At M1 = 2 and γ = 1.4, the computations yield the following values
-39.231520 39.231520
At M1 = 3 and γ = 1.4, the computations yield the following values
Note the flow in region 3 is just barely supersonic
At M1 = 4 and γ = 1.4, the computations yield the following values
And as seen the incident and reflected angles are not equal. Also M3 is subsonic, which
is possible for a weak shock. However, when we use the shock shock solution instead,
the following is obtained
From Gas Dynamics, Third Edition, by James E. John and Theo G. Keith. ISBN 0-13-120668-0. © 2006 Pearson Education, Inc.,
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125
Problem 20. – Complete the computations of Example 6.7, i.e., use the computed flow
angles to determine the deflection angles, and with M1 and M2, determine all parameters
in regions 3 and 4 of Figure 6.18.
Problem 21. – Derive the pressure-deflection equation, i.e., Eq.(6.30).
The expression for the pressure ratio across an oblique shock, is given in Eq.(6.10)
1
1
1
sinM2
p
p22
1
+γ
γ
+γ
θγ
This can be rearranged to obtain
The following identity is also used in this development
From Gas Dynamics, Third Edition, by James E. John and Theo G. Keith. ISBN 0-13-120668-0. © 2006 Pearson Education, Inc.,
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126
(
)
()
11sinM
11sinM
11sin1M
sin
sin1
sin
sin1
sin
cos
cot
1
22
1
22
1
2
22
+θ
+θ
+θ
±=
θ
θ
±=
θ
θ
±=
θ
θ
=θ
Now the deflection angle is connected to the shock wave angle and the upstream Mach
number by Eq.(6.18)
()
1sinMM
2
1
22
1
2
1
θ
+γ
Dividing the expression on the right into two pieces
2
2
1
2
2
1
2
22
2
22
1
p
1
p
p
p
1
1
1
p
p
2
1
1
1sinM
=
+γ
+γ
γ
+γ
=
+γ
θ
From Gas Dynamics, Third Edition, by James E. John and Theo G. Keith. ISBN 0-13-120668-0. © 2006 Pearson Education, Inc.,
Upper Saddle River, NJ. All rights reserved. This material is protected under all copyright laws as they currently exist. No Portion of
this material may be reproduced, in any form or by any means, without permission in writing from the publisher.
1
2
2
1
1
2
p
p
1
1
M
1
2
1
p
p
+γ
γ
+γ
γ
Problem 22. – Repeat the computations of Example 6.8 to find the angle the slip line
makes with the horizontal for γ = 1.4 and 1.667. How does the angle vary with γ?
Results of the computations for all three specific heat ratios (1.3, 1.4 and 5/3) is as
follows:
γ = 1.3
region 1 to region 2 to region 4
γ M1 δ1−2 θ1−2 p2/p1 ρ2/ρ1 T2/T1 po2/po1
region 1 to region 3 to region 5
γ M1 δ1−3 θ1−3 p3/p1 ρ3/ρ1 T3/T1 po3/po1
Downstream
flow angles
γ = 1.4
region 1 to region 2 to region 4
γ M1 δ1−2 θ1−2 p2/p1 ρ2/ρ1 T2/T1 po2/po1
region 1 to region 3 to region 5
γ M1 δ1−3 θ1−3 p3/p1 ρ3/ρ1 T3/T1 po3/po1
From Gas Dynamics, Third Edition, by James E. John and Theo G. Keith. ISBN 0-13-120668-0. © 2006 Pearson Education, Inc.,
Upper Saddle River, NJ. All rights reserved. This material is protected under all copyright laws as they currently exist. No Portion of
this material may be reproduced, in any form or by any means, without permission in writing from the publisher.
Downstream
flow angles
δ24 -14.8780 δ35 10.1220
γ = 5/3
region 1 to region 2 to region 4
γ M1 δ1−2 θ1−2 p2/p1 ρ2/ρ1 T2/T1 po2/po1
region 1 to region 3 to region 5
γ M1 δ1−3 θ1−3 p3/p1 ρ3/ρ1 T3/T1 po3/po1
Downstream
flow angles
From Gas Dynamics, Third Edition, by James E. John and Theo G. Keith. ISBN 0-13-120668-0. © 2006 Pearson Education, Inc.,
Upper Saddle River, NJ. All rights reserved. This material is protected under all copyright laws as they currently exist. No Portion of
this material may be reproduced, in any form or by any means, without permission in writing from the publisher.