Hwk Chapter2
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Transcript of Hwk Chapter2
Water Wave Mechanics, Spring 2012 Carlos Serrano Moreno
2.1 Consider the following transition section:
(a) The flow from left to right is constant at Q =12π m3/s. What is the total acceleration of a
water particle in the x direction at x=5 m? Assume that water is incompressible and that the
X component of velocity is uniform across each cross section.
Since the discharge and the area are known the velocity can be easily determined:
u ( x )=QA
=12 pp⋅(3−0 .15⋅x )2
Acceleration is defined as the derivative of velocity over time then:
dudt
=¶u¶t
+ ¶u¶ x
¶ x¶t
=¶u¶ t
+u ¶u¶ x
Since the flow is constant:
¶u¶t
=0 and the variation of velocity along the horizontal axis is due to the
truncated conical section:
dudt
( x )=12(3−0 .15⋅x )2
⋅24⋅0.15(3−0 .15⋅x )3
=12⋅24⋅0 .15(3−0.15⋅x )5
dudt
(5 )=12⋅24⋅0 .15(3−0.15⋅5 )5
=43 .257 .67
=0 .749»0 .75m / s2
(b) The flow of water from right to left in given by:
Q ( t )=p⋅t2
Calculate the total acceleration at x=5m for t=2s. Make the same assumptions as before.
Since the flow is going from right to left, the velocity can be now defined as:
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Water Wave Mechanics, Spring 2012 Carlos Serrano Moreno
u ( x , t )=QA
= −p⋅t2
p⋅(3−0.15⋅x )2
following the same procedure as before, but taking into account that this time it is not possible to
neglect the partial derivative of velocity over time, the acceleration will be:
dudt
( x , t )= −2⋅t(3−0 .15⋅x )2
− t2
(3−0 .15⋅x )2⋅2⋅t2⋅(−0 .15 )(3−0.15⋅x )2
= −2⋅t(3−0 .15⋅x )2
+ 2 t4⋅0 .15(3−0 .15⋅x )5
dudt
(5,2 )= −2⋅2(3−0 .15⋅5 )2
+ 2⋅24⋅0 .15(3−0 .15⋅5 )5
=−0 .707m/ s2
2.4 If the water (assumed inviscid) in the U-tive is displaced from its equilibrium position, it
will oscillate about this position with its natural period. Assume that the displacement of the
surface is: h (t )=A⋅cos( 2 pT ⋅t)
where the amplitude A = 10 cm and the natural period T is 8s. What will be the pressure at a
distance 20cm below the instantaneous water surface for = +10, 0, and -10cm?
Assume that g=980cm/s2 and =1g/cm3.
As the displacement of the water surface is know the expressions for velocity and acceleration can
be easily obtained:
w (t )=- A⋅2 pT
⋅sin(2 pT ⋅t)dwdt
( t )=- A⋅(2 pT )2
⋅cos (2 pT⋅t)
The fluid is known to be inviscid, then all the shear stress tensions can be neglected and Euler´s
Equation can be applied:
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Water Wave Mechanics, Spring 2012 Carlos Serrano Moreno
dwdt
(t )=¶w¶t
(t )+w¶w¶ z
(t )=-1ρ¶ p¶ z
−g
⇒¶ p¶ z
=- ρ⋅g+ ρ⋅A⋅(2 pT )2
⋅cos(2 pT ⋅t )=- ρ⋅g+ρ⋅(2 pT )2
⋅h (t )
∫z0
h ¶ p¶ z
dz=ρ⋅∫z0
h−g+(2 pT )
2
¿h (t )dz=ρ⋅(−g+(2 pT )2
¿h (t ))⋅(h−z0 )
p (h )−p ( z0 )=ρ⋅(−g+(2 pT )2
¿h (t ))⋅(h−z0 )
0−p ( z0 )=ρ⋅(−g+(2 pT )2
¿h (t ))⋅(h−z0 )
Since =1g/cm3, g=980cm/s2, A = 10cm, T is 8s and (h−z0) =20cm and assuming that there is no
pressure in the free surface, p (h )=0 .
Finally, the pressure at the desired points can be easily obtained:
h p (h−20 cm )
10 cm 19476 .62g
cm⋅s2⇒1947 .662 N
m2
0 cm 19600g
cm⋅s2⇒1960 N
m2
-10 cm 19723 .37g
cm⋅s2⇒1972 .337 N
m2
2.6 Derive the following equation for an inviscid fluid and a non divergent steady flow:
−1ρ¶ p¶ z
−g=(¶uw¶ x )+(¶ vw¶ y )+(¶w2¶ z )Again, if the fluid is inviscid, shear stress terms can be neglected. Taking a look to Euler´s
equation:
DwDt=-1ρ¶ p¶ z
−g⇒ DwDz
=¶w¶t
+u ¶w¶ x
+v ¶w¶ y
+w ¶w¶ z=-1ρ¶ p¶ z
−g
As the fluid is non divergent:
¶u¶ x
+ ¶ v¶ y
+¶w¶ z
=0. Playing with the equation above:
¶w¶t
+u ¶w¶ x
+v ¶w¶ y
+w ¶w¶ z
+w(¶ u¶ x + ¶ v¶ y
+ ¶w¶ z )=- 1ρ ¶ p
¶ z−g
Assuming that the fluid is steady and reorganizing the terms and applying the chain rule of
derivatives:
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Water Wave Mechanics, Spring 2012 Carlos Serrano Moreno
(u¶w¶ x +w¶u¶ x )+(v¶w¶ y
+w¶ v¶ x )+(w¶w
¶ z+w¶w
¶ z )=-1ρ ¶ p¶ z
−g
(¶ uw¶ x )+(¶ vw¶ y )+(¶w2¶ z )=-1ρ ¶ p¶ z
−g
2.9 For a particular fluid flow, the velocity components u,v and 2 in the x, y and z directivons
respectively are:
u=x+8⋅y+6⋅t⋅z+t4
v=8⋅x−7⋅y+6⋅z
w=12⋅x+6⋅y+12⋅z⋅cos (2⋅p⋅tT )+ t2a) Are there any times for which the flow is non divergent? If so, when?
If the flow is non divergent:
¶u¶ x
+ ¶ v¶ y
+¶w¶ z
=0
¶u¶ x
=1 ,¶ v¶ y
=- 7 ,¶ w¶ z
=12⋅cos (2⋅p⋅tT )⇒1−7+12⋅cos (2⋅p⋅tT )=0⇒ cos(2⋅p⋅tT )=12 ⇒2⋅p⋅t
T=p3
⇒ t=T6
However, since the solution comes from a cosinus: t = T/6 + k·T, (k = 1,2,...) is also valid.
b) Are there any times for which the flow is irrotational? If so, when?
If the flow is irrorational:
|
i j k¶¶ x
¶¶ y
¶¶ z
u v w
|=0=(¶w¶ y −¶ v¶ z
,¶u¶ z
−¶w¶ x
,¶ v¶ x
−¶ u¶ y )= (6−6,6⋅t−12 ,8−8 )
Then t=2s.
c) Develop the expression for the pressure gradient in the vertical (z) direction as a function
of space and time.
DwDz
=¶w¶ t
+u¶w¶ x
+v¶w¶ y
+w¶w¶ z
=-1ρ¶ p¶ z
−g
¶ p¶ z
=- ρ⋅g− ρ⋅(¶w¶ t +u¶w¶ x
+v ¶w¶ y
+w¶w¶ z )
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Water Wave Mechanics, Spring 2012 Carlos Serrano Moreno
since
¶w¶t=-24⋅pT
⋅z⋅sin ( 2⋅p⋅tT )+2⋅t , ¶ w¶ x =12 , ¶ w¶ y
=6 , ¶ w¶ z
=12⋅cos( 2⋅p⋅tT )¶ p¶ z=- ρ⋅g− ρ⋅(−24⋅pT ⋅z⋅sin( 2⋅p⋅tT )+2⋅t+12⋅u+6⋅v+12⋅cos( 2⋅p⋅tT )⋅w)
substituting the velocity values:
¶ p¶ z=- ρ⋅g− ρ⋅¿(−24⋅pT ⋅z⋅sin( 2⋅p⋅tT )+2⋅t+12⋅(x+8⋅y+6⋅t⋅z+t4 )+6⋅(8⋅x−7⋅y+6⋅z )+ ¿)¿
¿
¿¿
2.12 The pressures pA ( t ) and pB ( t ) act on the massless pistons containingg the inviscid,
incompressible fluid in the horizontal tube shown below. Develope an expression for the
velocity of the fluid as a function of time = 1 gm/cm3.
Note: pA (t )=C A sin (s⋅t )and pB (t )=CBsin ( s⋅t+α )
where: s=0 .5 rad / s ,α= p
2,CA=CB=10dyn /cm3
Once again, since the fluid is inviscid, shear stress terms can be neglected. Euler´s equation
along the x-axis:
DuDt=-1ρ¶ p¶ x
⇒ DuDz
=¶ u¶ t
+u ¶u¶ x
+v ¶ v¶ y
+w ¶ v¶ z=-1ρ¶ p¶ x
Pressure just depends on time. All convective acceleration terms can be neglected. Then:
¶u¶t=-1ρ¶ p¶ x
¶ p¶ x
=−pB−p A
100=
−10 sin (0 .5⋅t+ p2 )+10 sin (0 .5⋅t )
100
¶u¶t=-11
−10sin(0.5⋅t+ p2 )−10sin (0 .5⋅t )
100= 110 (sin (0 .5⋅t+ p
2 )+sin (0 .5⋅t ))
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Water Wave Mechanics, Spring 2012 Carlos Serrano Moreno
u (t )= 110⋅0 .5 (−cos(0.5⋅t+ p
2 )−cos (0 .5⋅t ))+C
If t = 0 u (0 )=1
5 (−cos ( p2 )−cos (0 .5⋅0 ))+C=0⇒C=15
u (t )=15 (−cos(0 .5⋅t+ p
2 )−cos (0 .5⋅t ))+ 15 cm/s
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