sdsolns07

73
Solutions Manual c to accompany System Dynamics, First Edition by William J. Palm III University of Rhode Island Solutions to Problems in Chapter Seven PROPRIETARY AND CONFIDENTIAL This Manual is the proprietary property of The McGraw-Hill Companies, Inc. (“McGraw- Hill”) and protected by copyright and other state and federal laws. By opening and using this Manual the user agrees to the following restrictions, and if the recipient does not agree to these restrictions, the Manual should be promptly returned unopened to McGraw-Hill. This Manual is being provided only to authorized professors and instructors for use in preparing for the classes using the af f iliated textbook. No other use or distribution of this Manual is permitted. This Manual may not be sold and may not be distributed to or used by any student or other third party. No part of this Manual may be reproduced, displayed or distributed in any form or by any means, electronic or otherwise, without the prior written permission of McGraw-Hill. c Solutions Manual Copyright 2005 by The McGraw-Hill Companies, Inc. 7-1 PROPRIETARY MATERIAL Manual may be displayed, reproduced or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. If you are a student using this Manual, you are using it without permission. . © 2005 The McGraw-Hill Companies, Inc. All rights reserved. No part of this

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Page 1: SDsolns07

Solutions Manual c!

to accompany

System Dynamics, First Edition

by

William J. Palm III

University of Rhode Island

Solutions to Problems in Chapter Seven

PROPRIETARY AND CONFIDENTIAL

This Manual is the proprietary property of The McGraw-Hill Companies, Inc. (“McGraw-Hill”) and protected by copyright and other state and federal laws. By opening and usingthis Manual the user agrees to the following restrictions, and if the recipient does not agreeto these restrictions, the Manual should be promptly returned unopened to McGraw-Hill.This Manual is being provided only to authorized professors and instructors for use inpreparing for the classes using the af f iliated textbook. No other use or distribution ofthis Manual is permitted. This Manual may not be sold and may not be distributed toor used by any student or other third party. No part of this Manual may be reproduced,displayed or distributed in any form or by any means, electronic or otherwise, without theprior written permission of McGraw-Hill.

c!Solutions Manual Copyright 2005 by The McGraw-Hill Companies, Inc.

7-1

PROPRIETARY MATERIALManual may be displayed, reproduced or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. If you are a student using this Manual, you are using it without permission.

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Page 2: SDsolns07

7.1 Note that f1 = pA1 and f2 = pA2. Thus f1 = (A1/A2)f2 = (10/30)60 = 20 lb.Also, A1x1 = A2x2 from conservation of fluid mass. Thus x1 = (A2/A1)x2 = (30/10)6 =

18 in.The work done is f2x2 = 60(6) = 360 lb-in.

7-2

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Page 3: SDsolns07

7.2 The cross-sectional area is A = !(11/2)2 = 95.033 ft2. The net inflow rate is

(1000 " 800)(0.13368) = 26.736 ft3/min

The initial volume is 5A = 475.166 ft3, and the volume after 5 hrs (300 minutes) is

475.166 + 26.736(300) = 8495.97 ft3

Thus the height after 5 hrs is

h =8495.97

A=

8495.9795.033

= 89.4 ft

7-3

PROPRIETARY MATERIALManual may be displayed, reproduced or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. If you are a student using this Manual, you are using it without permission.

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Page 4: SDsolns07

7.3 Summing forces in the horizontal direction and assuming zero acceleration, we obtain

µmg = A(p1 " p2)

orA =

µmg

p1 " p2=

0.6(1000)(3 " 1) # 105

= 0.003 m2

This corresponds to a radius of 30 mm.

7-4

PROPRIETARY MATERIALManual may be displayed, reproduced or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. If you are a student using this Manual, you are using it without permission.

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Page 5: SDsolns07

7.4 Let ft be the tangential force of the surface acting on the cylinder (positive to the left).Summing moments in the clockwise direction about the mass center of the cylinder gives

I" = Rft (1)

From kinematics, if there is no slipping, x = R" and thus x = R".Summing horizontal forces on the cylinder gives

mx = f " ft

Thus ft = f " mx. Substituting this into (1) gives

I" = Rf " mRx = Rf " mR(R")

or(I + mR2)" = Rf = R(p1 " p2)A

With the given values, this becomes!7 + 100(0.4)2

"" = 0.4(3 # 105)0.005 = 600

or" = 26.087

Thus"(t) = 26.087t

7-5

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Page 6: SDsolns07

7.5 Assuming no friction and summing horizontal forces, we obtain

mx = A(p1 " p2)

or60032.2

x =3

144(10)144 = 10

orx = 0.537 ft/sec2

Thusx = 0.537t

andx =

0.5372

t2 = 0.268t2

The volume isV = Ax =

3144

0.067 = 0.001396 ft3

or 2.412 in3.

7-6

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Page 7: SDsolns07

7.6 From conservation of water mass, qo = 10 + 2 = 12 m3/s.From conservation of salt mass,

d

dt(300so) = 2si " qoso

or300

dso

dt= 2si " 12so

7-7

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Page 8: SDsolns07

7.7 From conservation of water mass, qo = 10 + 2 = 12 m3/s.From conservation of salt mass,

d

dt(V so) = 2si " qoso

orV

dso

dt= 2si " 12so

The time constant is # = V/12. Taking the lag time to be four time constants, we have

4# = 4V

12= 20 s

which gives

V =20(12)

4= 60 m3

7-8

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Page 9: SDsolns07

7.8 The capacitance can be computed from (7.2.3).

C =A(h)

g

The liquid surface area isA(h) = 2L

#Dh " h2

ThusC =

2Lg

#Dh " h2

7-9

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Page 10: SDsolns07

7.9 The capacitance can be computed from (7.2.3).

C =A(h)

g

The liquid surface area is A = D1L if h < D2 and

A =2L(h " D2)

tan $+ D1L h $ D2

Thus

C =$ D1L

g h < D22L(h!D2)

g tan ! + D1Lg h $ D2

7-10

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Page 11: SDsolns07

7.10 From (7.2.5),

%A(h)dh

dt= qmi " qmo

where qmo = 0 and qm = qmi here. From Problem 7.8,

A(h) = 2L#

Dh " h2

Thus%2L

#Dh " h2

dh

dt= qm

7-11

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Page 12: SDsolns07

7.11 From (7.2.5),

%A(h)dh

dt= qmi " qmo

where qmo = 0 here. From Problem 7.9,

A(h) =$

D1L h < D22L(h!D2)

tan ! + D1L h $ D2

Thus the model is%D1L

dh

dt= qmi h < D2

%%2L(h " D2)

tan $+ D1L

&dh

dt= qmi h $ D2

7-12

PROPRIETARY MATERIALManual may be displayed, reproduced or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. If you are a student using this Manual, you are using it without permission.

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Page 13: SDsolns07

7.12 For the laminar resistanceR =

128µL

!%D4

where L = 1 m, D = 10!3 m. Thus

R =128(1.58 # 10!5)1!(0.12885)(10!3)4

= 4.996 # 108 m!1s!1

The mass flow rate is

qm =p

R=

1.0133 # 104

4.996 # 108= 2.028 # 10!5 kg/s

The average velocity is found from

v =qm

A%=

2.028 # 10!5

!(10!3/2)2(1.2885)= 20 m/s

The Reynolds number is

Ne =%vD

µ=

1.2885(20)10!3

1.58 # 10!5= 1634

which is less than 2300, so the flow is laminar.The maximum entrance length Le is found from

Ne = 0.06DNe = 0.06(10!3)1634 = 0.098 m

Since this length is much less than the pipe length of 1 m, most of the pipe has laminarflow.

7-13

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Page 14: SDsolns07

7.13 From (7.3.1)

R ='

dp

dqm

(

r(1)

The flow rate isqm =

)p

Ro

whereRo =

12%C2

dA2o

Thusp = Roq

2m

and from (1),

R = 2Roqmr = 2Ro

)pr

Ro

But pr = %ghr, so

R = 2Ro

*%ghr

Ro=

1CdAo

#2ghr

7-14

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Page 15: SDsolns07

7.14 a) From (7.3.12),

Cdp

dt= qmi " qmo

whereC =

A

g

andqmo =

)p

R1

ThusA

g

dp

dt= qmi "

)p

R1

b) From conservation of mass,

%Adh

dt= qmi " qmo = qmi "

)p

R1

But p = %gh, so

%Adh

dt= qmi ""

*%gh

R1

7-15

PROPRIETARY MATERIALManual may be displayed, reproduced or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. If you are a student using this Manual, you are using it without permission.

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Page 16: SDsolns07

7.15 a) The model is

Adh

dt= " g

Rh

where A = 20. The time constant is # = RA/g. Taking the time to empty to be 4# , weobtain # = 200/4 = 50 s. Thus

R =#g

A= 24.525 m!1s!1

b) The model is

Adh

dt= 3 " g

Rh

Thushss =

3Rg

=3(24.525)

9.81= 7.5 m

7-16

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Page 17: SDsolns07

7.16 a) The model is

Adh

dt= " g

Rh

The time constant is# =

RA

g=

150(2)32.2

= 93.168 sec

The time to empty is approximately 4# , regardless of the initial height, and is 4# = 372.671sec.

b) The model is

Adh

dt= 0.1 " g

Rh

The time constant is # = 93.168 and the steady-state height is hss = 0.1R/g = 0.466 ft.The response is

h(t) = 0.466+1 " e!t/93.168

,(1)

Setting h(t) = hss/3 = 0.466/3 in (1) gives

13

= 1 " e!t/93.168

ort = "93.168 ln

23

= 37.776 sec

7-17

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Page 18: SDsolns07

7.17 The model isA

dh

dt= qvi " CdAo

#2gh

At steady state,qvi = CdAo

#2gh

so thatCdAo =

qvi%2gh

(1)

Note that 1 cm is 10!2 m and that

1 liter/min =10!3

60= 1.667 # 10!5 m3/s

So (1) in consistent units becomes

CdAo =qvi(1.667 # 10!5)#

2(9.81)h(10!2)= 3.763 # 10!5 qvi%

h(2)

where qvi is in liters/min and h is in cm. We will compute CdAo from (2) for each data pairin the table, and then average the results. The answers are

CdAo =(6.7329 6.7350 6.9899 7.0619 7.1843 7.2870 7.3867 7.9023 8.6029 10.6456) # 104

The mean of the CdAo values is 7.6528 # 104, and the standard deviation is 1.1936 # 104,which is 16% of the mean.

7-18

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Page 19: SDsolns07

7.18 Let p1 " p3 denote the pressure drop from the bottom of the tank to the outlet ofpipe 3. Denote the pressure drop over the length of pipe 1 by !p1, that across pipe 3 by!p3, and that across the component by !p2. The turbulent resistance relation (7.3.3) isRq2

m = p1 " p3. Thus, because the mass flow rate qm is the same through each element,R1q2

m = !p1, R2q2m = !p2, and R3q2

m = !p3. The total pressure drop across all threeelements is the sum of the drops across each element. Thus

p1 " p3 = !p1 + !p2 + !p3 = R1q2m + R2q

2m + R3q

2m

orp1 " p3 = (R1 + R2 + R3) q2

m

and thus the total resistance is R = R1 + R2 + R3, which shows that turbulent resistanceobeys the series law.

b) From conservation of mass,

%Adh

dt= qmi " qmo = qmi "

)p1 " p3

R

Because p1 " p3 = %gh, the model becomes

%Adh

dt= qmi "

*%gh

R

7-19

PROPRIETARY MATERIALManual may be displayed, reproduced or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. If you are a student using this Manual, you are using it without permission.

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Page 20: SDsolns07

7.19 From (7.3.3),

%Adh

dt= qmi "

*%gh

R1

where p = %gh.

7-20

PROPRIETARY MATERIALManual may be displayed, reproduced or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. If you are a student using this Manual, you are using it without permission.

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Page 21: SDsolns07

7.20 If h < D,

%Adh

dt=

1R1

ps + qmi

If h $ D,

%Adh

dt=

1R1

ps + qmi "1

R2%g(h " D)

7-21

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Page 22: SDsolns07

7.21 a) The model is

%Adh

dt= qmi "

%g

Rh

If there is no inflow,

Adh

dt= " g

Rh

The time constant is # = RA/g and the response is

h(t) = h(0)e!t/"

Take the log of both sides:

ln h(t) = ln h(0) " 1#t (1)

Equation (1) has the form of the equation of a straight line:

ln h(t) = mt + b

where m = "1/# and b = ln h(0). Use the least-squares method to find m and b. TheMATLAB code is

t = [0:300:2400];h = [20.2, 17.26, 14.6, 12.4, 10.4, 9, 7.6, 6.4, 5.4];lnh = log(h);coeff = polyfit(t,lnh,1)

where m is given by coeff(1) and b is given by coeff(2). The results are m = "5.48868#10!4 and b = 3.01. Thus, # = 1.822 # 103 and

R =g#

A= 9.778 # 103 ft!1sec!1

b) If h(0) is known to be exactly 20.2 ft, then (1) becomes

ln h(t) " 3.006 = "1#t = mt (2)

Using (1.6.3) from Chapter 1, we have

m9-

i=1

t2i =9-

i=1

ti ln h(ti)

Continue the code above as follows

m = sum(t.*(lnh-log(20.2)))/sum(t.^2)

This gives m = "5.463 # 10!4. Thus, R = 9.824 # 103.

7-22

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Page 23: SDsolns07

7.22 Applying conservation of mass to each tank gives

%A1dh1

dt= qmi "

%g

R1h1

%A2dh2

dt=

%g

R1h1 "

%g

R2h2

Note that % cancels out in the second equation.

7-23

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Page 24: SDsolns07

7.23 a) Applying conservation of mass to each tank gives

%A1dh1

dt= qmi "

%g

R1(h1 " h2)

%A2dh2

dt=

%g

R1(h1 " h2) "

%g

R2h2

Note that % cancels out in the second equation.b) Substituting the given values we obtain

%Adh1

dt= qmi "

%g

R(h1 " h2)

4Adh2

dt=

g

R(h1 " h2) "

g

3Rh2

Applying the Laplace transform with zero initial conditions, we obtain'

As +g

R

(H1(s) "

g

RH2(s) =

Qmi(s)%

" g

RH1(s) +

'4As +

4g3R

(H2(s) = 0

Let b = g/RA. After dividing both equations by A, they can be expressed as

(s + b)H1(s) " bH2(s) =Qmi(s)

%

"bH1(s) +'

4s +43b(

H2(s) = 0

Using Cramer’s method to solve these equations, we obtain

H2(s) =

.....s + b Qmi(s)/%"b 0

..... /D =bQmi(s)

%D

where

D =

.....s + b "b"b 4s + 4b/3

..... = (s + b)(4s +43b) " b2 = 4s2 +

163

bs +13b2

ThusH2(s)Qmi(s)

=b/%

4s2 + (16/3)bs + (1/3)b2

7-24

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Page 25: SDsolns07

7.24 Applying conservation of mass to each tank gives

%Adh1

dt= "%g

R(h1 " h2)

2%Adh2

dt= qmi +

%g

R(h1 " h2) "

%g

3Rh2

If we divide both equations by %A and let b = g/RA, these equations can be expressed as

dh1

dt= "b(h1 " h2)

2dh2

dt=

qmi

%+ b(h1 " h2) "

b

3Rh2

Applying the Laplace transform with zero initial conditions, we obtain

(s + b) H1(s) " bH2(s) = 0

"bH1(s) +'

2s +43b(

H2(s) =Qmi(s)

%

Using Cramer’s method to solve these equations, we obtain

H1(s) =

.....0 "b

Qmi(s)/% 2s + 4b/3

..... /D =bQmi(s)

%D

where

D =

.....s + b "b"b 2s + 4b/3

..... = (s + b)'

2s +43b(" b2 = 2s2 +

103

bs +13b2

ThusH2(s)Qmi(s)

=b/%

2s2 + (10/3)bs + (1/3)b2

The characteristic roots are

s ="10b/3 ±

#100b2/9 " 8b2/34

='"5

6± 1

6%

19(

b = "1.56b, "0.1069b

7-25

PROPRIETARY MATERIALManual may be displayed, reproduced or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. If you are a student using this Manual, you are using it without permission.

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Page 26: SDsolns07

7.25 From Example 7.4.4 the damping constant is given by

c =128µLA2

!D4

Substituting the given and desired values, we obtain

2000 =128(0.9)LA2

!D4

which givesLA2

D4=

2000!0.9(128)

= 54.5415 (1)

So we have three parameters to select: L, A, and D.Let n be the ratio of the piston area A to the area Ao of the hole through the piston.

n =A

Ao(2)

But

Ao = !'

D

2

(2

and thus

A =n!D2

4From (1),

LA2

D4= L

n2!2

16= 54.5416

soL =

16(54.5415)n2!2

=88.419

n2

Now we try various values for n to see if we obtain a reasonable value for the pistonlength L. Using n = 50 gives L = 0.035 m, which is 1.38 in., which is a reasonable length.

Now we pick the piston area A. A cylinder diameter of 0.05 m (1.96 in.) gives

A = !'0.05

2

(2

= 1.963 # 10!3 m2

So from (2),

Ao =A

n=

1.963 # 10!3

50= 3.9 # 10!5 = !

'D

2

(2

Thus the hole diameter isD = 7.1 # 10!3 m

which is about 0.3 in.So one of many possible designs is

piston diameter = 0.05 m

piston length, L = 0.035 mpiston hole diameter, D = 7.1 # 10!3 m

7-26

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Page 27: SDsolns07

7.26 (a) If m1 = 0, a force balance on the spool valve gives

f(t) = k1x + c1x (1)

Considering the masses m2 and m3 to constitute a single rigid body, Newton’s law gives

(m2 + m3)y + c2y + k2y = A(p1 " p2) (2)

where A is the piston area and (p1 " p2) is the pressure di"erence across the piston (referto Figure 7.4.8).

From equation (5) in Example 7.4.9,

p1 " p2 = ps " 2!p (3)

In this problem, unlike Example 7.4.9, we cannot make the assumption that (m2 +m3)(y) = 0 because the load inertia and the forces k2y and c2y are not negligible. Thusp1 &= p2 here.

Assuming that x, y, and !p are small deviations from equilibrium, then the deviationps will be 0 if the supply pressure is constant, and (3) becomes

p1 " p2 = "2!p (4)

and (2) becomes(m2 + m3)y + c2y + k2y = "2A!p (5)

In addition, we can linearize the relation qv = f(x,!p) for the volume flow rate throughthe spool valve, as follows:

qv = B1x + B2!p

From conservation of mass,Ay = qv = B1x + B2!p

This gives

!p =Ay " B1x

B2

Substitute this into (5) to obtain

(m2 + m3)y + c2y + k2y = "2AAy " B1x

B2

Collect terms:

(m2 + m3)y +/

c2 +2A2

B2

0

y + k2y =2AB1

B2x (6)

The system model is given by equations (1) and (6).(b) The total mass of the spool valve (considered to be rigid) is 2m1. Newton’s law

applied to the spool valve gives

2m1x = f(t) " k1x " c1x

7-27

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Page 28: SDsolns07

or2m1x + c1x + k1x = f(t) (7)

The rest of the problem proceeeds as in part (a). The system model is given by equations(6) and (7).

7-28

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Page 29: SDsolns07

7.27 The equivalent mass of the cylinder is

me = m +I

R2

Use this instead of m in equation (9) of Example 7.4.6 to obtain'

m +I

R2

(x = (R1 + R2)%A2x = A(p1 " p2)

7-29

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Page 30: SDsolns07

7.28 Let qv1 and qv2 be the volume flow flow rates into and out of the center section wherethe pressure is p. If the pressure drop %gh in going up a height h from this point to theplate is small compared to the pressure p, then the pressure at the plate is approximatelythe same as p. From Newton’s law applied to the plate,

mx = pA " kx (1)

where the force pA is that due to the liquid pressure p acting on the plate. Assuming thatmx of the plate is small, then the above equation shows that the pressure force equals thespring force.

pA = kx (2)

Thus x = pA/k. Di"erentiate this with respect to time to obtain.

dx

dt=

A

k

dp

dt(3)

From conservation of volume,

d

dt(Ax) = A

dx

dt= qv1 " qv2 (4)

The model for the dynamic behavior of the pressure as a function of the flow rates isobtained by substituting this expression for dx/dt into (3). The result is

A2

k

dp

dt= qv1 " qv2 (5)

Using the resistances upstream and downstream, the flow rates qv1 and qv2 can beexpressed as functions of the upstream and downstream pressures. The mass flow rates inthe sections are

%qv1 =1R

(p1 " p)

%qv2 =1R

(p " p2)

and (5) becomes

%A2

k

dp

dt=

1R

(p1 " p) " 1R

(p " p2)

orR

2%A2

k

dp

dt+ p =

p1 + p2

2This equation can be solved for p as a functions of time if we are given p1 and p2 as timefunctions.

7-30

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Page 31: SDsolns07

7.29 A force balance on the plate gives kx = Ap. The volume swept out by the plate isV = Ax. With V = 30 in3 and p = 1.5 psi, we have that

x =30A

and k =Ap

x=

1.5A2

30

We were given no indication of any size limits or available spring constants, so we are free tochoose a reasonable value for A. For example, using a plate 6 inches in diameter, A = 9!,and this gives k = 40 lb/in. This gives a plate displacement of x = 3.75 in.

7-31

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Page 32: SDsolns07

7.30 a) For the two resistances in series:

qm2 =1

R1 + R2!p

From the straight line on the graph,

30 =1

R1 + R23 # 104

Since R2 = 400, we obtainR1 = 600 N · s/kg · m2

From equation (4) of Example 7.4.10,

%gh =R2

R1 + R2!p

Thush =

'400100

3 # 104(

/9.81% = 1223/%

where %, in kg/m3, is the mass density of the liquid (which was not specified).b)

&qm1 = "1r&(!p)

where "1/r is the slope of the straight line. Thus r = 700.We have

d

dt&h = "b&h

whereb =

'1r

R1 + R2

R2+

1R2

(g

A=

' 1700

1000400

+1

400

( 9.812

= 0.02978

Thusd

dt&h = "0.02978&h

The time constant is 1/0.02978 = 33.58 s.

7-32

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Page 33: SDsolns07

7.31 From (7.2.5),

%A(h)dh

dt= qmi " qmo

whereA(h) = (2L tan ')h

andqmo =

1R

%gh

Thus% (2L tan ')h

dh

dt= qmi "

1R

%gh

7-33

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Page 34: SDsolns07

7.32 From (7.2.5),

%A(h)dh

dt= qmi " qmo

whereA(h) = (2L tan ')h

and

qmo =

*%gh

Ro

Ro =1

2%C2dA2

o

Thusqmo = %CdAo

#2gh

and% (2L tan ')h

dh

dt= qmi " %CdAo

#2gh

7-34

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Page 35: SDsolns07

7.33 From (7.2.5),

%A(h)dh

dt= qmi " qmo

where, from Problem 7.8,A(h) = 2L

#Dh " h2

and

qmo =)

p

R=

*%gh

R

Thus

2%L#

Dh " h2 dh

dt= qmi "

*%gh

R

7-35

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Page 36: SDsolns07

7.34 (a) From conservation of mass and (7.3.9):

%Ah = %qv " CdAo

#2p% = %qv " %CdAo

#2gh

Thus % cancels out of the equation, and we obtain

100h = qv " 0.5%

64.4h = qv "%

16.1h (1)

(b) At steady state, h = 0 and qv =%

16.1h. With qv = 5, this gives

h =q2v

16.1= 1.55 ft

(c) At h = 1.55,

%16.1h '

116.1(1.55) +

12

(16.1h)!1/2...h=1.55

(h " 1.55) = 5 +110

(h " 1.55)

Then (1) becomes

100h = qv " 5 +110

(h " 1.55)

Let x = h " 1.55 and u = qv " 5 to obtain the linearized model:

100x = u " 0.1x

whose time constant is 100(0.1) = 10 sec.

7-36

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Page 37: SDsolns07

7.35 a) The capacitance can be obtained from

C =A(h)

g

where

A(h) = !'

h

tan '

(2

Thus

C =!

g

'h

tan '

(2

b) From (7.2.5),

%A(h)dh

dt= qmi " qmo

where, from part (a),

A(h) = !'

h

tan '

(2

andqmo =

%gh

R

Thus

!%'

h

tan '

(2 dh

dt= qmi "

%gh

R

7-37

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Page 38: SDsolns07

7.36 For an isothermal process, n = 1, and from (7.5.6),

C =V

nRgT=

201(1715)(70 + 460)

= 2.2 # 10!5 slug " ft2/lb

7-38

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Page 39: SDsolns07

7.37 If pi " p < 0, the flow will be out of the tank (and will be negative). Thus,

Cdp

dt= "f(|pi " p|)

7-39

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Page 40: SDsolns07

7.38 For the left-hand tank,

C1d(&p1)

dt=

1R1

(&pi " &p1) "1

R2(&p1 " &p2)

For the right-hand tank,

C2d(&p2)

dt=

1R2

(&p1 " &p2)

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Page 41: SDsolns07

7.39 a)C = %V cp = 1000(250 # 10!6)4.18 # 103 = 1045 J/"C

b)E = C(T " To) = 1045(99 " 20) = 8.256 # 104 J

7-41

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Page 42: SDsolns07

7.40 a)V = 15(10)(8) = 1200 ft3

C = %V cp = 0.0023(6.012 # 103)1200 = 1.659 # 104 ft " lb/"F

b)E = C(T " To) = 1.659 # 104(72 " 68) = 6.636 # 104 ft " lb

7-42

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Page 43: SDsolns07

7.41 See Example 7.6.1, which with T (0) = 20, qv = 0.5, and V = 12 gives

T (t) = 20e!t/24 ++1 " e!t/24

,80

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Page 44: SDsolns07

7.42 a) For conduction, the thermal resistance is given by

R =L

kA

Thus

R1 =10 # 10!3

400!(10!3)2= 7.958 "C/W

R2 =5 # 10!3

400!((1.5/2) # 10!3)2= 7.074 "C/W

The total resistance isR = R1 + R2 = 15.032 "C/W

b) The heat flow rate is

q =30R

=30

15.032= 1.995 W

7-44

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Page 45: SDsolns07

7.43 The total resistance isR =

1h1A

+L

kA+

1h2A

R =' 1

85+

3/[16(12)]47

+115

( 1A

=0.0788

A

7-45

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Page 46: SDsolns07

7.44 The resistances are in series and thus they add. Using R = L/kA for conduction andR = 1/hA for convection, and letting x be the required thickness of the middle layer, wehave

R =130

/130

+10 # 10!3

0.2+

x

0.04+

20 # 10!3

0.1

0

=130

'0.047634 +

x

0.04

(

whereq =

1R!T

With q = 400 and !T = 40, we have

R =40400

=130

'0.047634 +

x

0.04

(

This gives x = 3.54 m, which is rather large.

7-46

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Page 47: SDsolns07

7.45 a) The resistance formula is

R =L

kA

For the brick,

Rbrick =4/12

0.086(12)2/144= 3.876

For the concrete,

Rconcrete =4/12

0.02(36)2/144= 1.852

The segments are in parallel because they have the same temperature di"erence, so thetotal resistance is given by

1R

=1

Rbrick+

1Rconcrete

which givesR = 1.253 "F " sec/lb " ft

b) The heat flow rate is given by q = !T/R. For the brick,

qbrick =40

Rbrick= 10.32

For the concrete,

qconcrete =40

Rconcrete= 21.6

The total heat flow rate is

q = qbrick + qconcrete = 31.92 ft " lb/sec

7-47

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Page 48: SDsolns07

7.46 The solution procedure follows that of Example 7.7.4.a) Assuming that the temperature inside the pipe wall does not change with time, then

the same heat flow rate occurs in the inner and outer convection layers and in the pipe wall.Thus the three resistances are in series and we can add them to obtain the total resistance.The inner and outer surface areas are

Ai = 2!riL = 2!'1

2

( ' 112

(10 = 2.618 ft2

Ao = 2!roL = 2!'3

4

( ' 112

(10 = 3.927 ft2

The inner convective resistance is

Ri =1

hiAi=

116(2.618)

= 0.0239sec "Fft lb

Ro =1

hoAo=

11.1(3.927)

= 0.2315sec "Fft lb

The conductive resistance of the pipe wall is

Rc =ln

+rori

,

2!Lk=

ln+

3/41/2

,

2!(10)(10.1)= 6.389 # 10!4 sec "F

ft lb

Thus the total resistance is

R = Ri + Rc + Ro = 0.0239 + 6.389 # 10!4 + 0.2315 = 0.256sec "Fft lb

The heat loss from the pipe, assuming that the water temperature is a constant 120" alongthe length of the pipe, is

qh =1R!T =

10.256

(120 " 70) = 195ft lbsec

To investigate the assumption that the water temperature is constant, compute thethermal energy E of the water in the pipe, using the mass density % = 1.94 slug/ft3 andcp = 25, 000 ft-lb/slug-"F:

E = mcpTi = (!r2i L%)cpTi = 3.1743 # 105 ft lb

Assuming that the water flows at 1 ft/sec, a slug of water will be in the pipe for 20 sec. Dur-ing that time it will lose 195(20) = 3900 ft-lb of heat. Because this amount is approximatelyonly 1% of E, our assumption that the water temperature is constant is confirmed.

7-48

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Page 49: SDsolns07

7.47 The thermal energy E of the water in the pipe is

E = mcpTi = (!r2i L%)cpTi = !

' 148

(2

6(1.94)(2.5 # 104)Ti = 396.8Ti

From conservation of heat energy,

dE

dt= " 1

R(Ti " 70)

ormcp

dTi

dt= " 1

R(Ti " 70)

The resistance of the inside surface is

Ri =1

6(0.785)= 0.2123

and the total resistance is

R = Ri + Rv + Ro = 0.2123 + 2.15 # 10!4 + 0.77 = 0.925

Thus396.8

dTi

dt= "1.081 (Ti " 70)

or367

dTi

dt+ Ti = 70

For Ti(0) = 120, the solution is

Ti(t) = 50e!t/367 + 70

7-49

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Page 50: SDsolns07

7.48 a)C1 = mcp = %V cp = 1.94(1000)2.5 # 104 = 4.85 # 107 ft " lb/"F

b) From conservation of heat energy,

d

dt(C1T1) = " 1

R1(T1 " To)

or4.85 # 107R1

dT1

dt+ T1 = To

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Page 51: SDsolns07

7.49 The steady-state temperature di"erence is 90 " 70 = 20", and the temperature dif-ference has decayed by 98% (to 70.4") in 4000 sec. So we take 4000 sec to be four timeconstants. Thus # = 4000/4 = 1000 sec. This value is confirmed by noting from the datathat it took 1000 sec for the temperature di"erence to decay by 63% (to 77"). From Problem7.48, the model is

4.85 # 107R1dT1

dt+ T1 = To

so# = 4.85 # 107R1 = 1000

ThusR1 = 2.06 # 10!5 "F " sec/ft " lb

7-51

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Page 52: SDsolns07

7.50 From conservation of heat energy,

d

dt(C1T1) = qi " q1

d

dt(C2T2) = q1 " qo

whereq1 =

1R1

(T1 " T2) qo =1

R2(T2 " To)

ThusC1

dT1

dt= qi "

1R1

(T1 " T2)

C2dT2

dt=

1R1

(T1 " T2) "1

R2(T2 " To)

7-52

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Page 53: SDsolns07

7.51 a) From conservation of heat energy,

C1dT1

dt= " 1

R1(T1 " To) +

1R2

(T2 " T1) (1)

C2dT2

dt= " 1

R2(T2 " T1) (2)

b) If C2 ' 0, (2) shows that T1 = T2, and (1) becomes

C1dT1

dt= " 1

R1(T1 " To)

7-53

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Page 54: SDsolns07

7.52 a) The sphere model is

cp%VdT

dt= " 1

R(T " To)

where R = 1/hA. The time constant is # = cp%V/hA, and the response is

T (t) = 22 + [T (0) " 22]e!t/"

which has the form!T (t) = !T (0)e!t/"

where !T = T " 22. The following MATLAB session computes the answer.

t = [0:15:135,180:60:960];DeltaT = [95,93,92,90,89,88,87,86,85,84,82,79,...

76,73,71,69,67,65,62,61,59,57,56,54]-22;p = polyfit(t,log(DeltaT),1)tau = -1/p(1);cp = 500; rho = 7920;d = 0.025;r = d/2;V = (4/3)*pi*r^3;A = 4*pi*r^2;h = cp*rho*V/(A*tau)

The regression coe#cients are p = [-0.0008 4.2533]. The answer is h = 13.69 J/(m2 sK).

b) The Biot number is

NB =hL

k=

hr/3k

=13.69(0.025/2)/3

400= 1.426 # 10!4

Because NB is much less than 0.1, the lumped parameter model can be considered accurate.c) Radiation heat transfer, which is dependent on T 4, is thus more significant at higher

temperatures, and does not give an exponential response. A plot of the data and theregression curve shows that the curve is a good fit. The greatest error occurs when T > 90"

and is less than 3". This indicates that radiation heat transfer is a"ecting the process, butonly for the first 30 seconds or so.

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Page 55: SDsolns07

7.53 From conservation of heat energy,

CdT

dt=

1R

(To " T )

whereR =

1hA

C = %V cp

The surface area isA = 4!r2 = 4!(30 # 10!3)2 = 1.131 # 10!2

and the volume isV =

43!r3 =

43!(30 # 10!3)3 = 1.13 # 10!4

The resistance isR =

1hA

= 0.2947

The capacitance isC = %V cp = 8900(1.13 # 10!4)385 = 387.5

Thus the model is387.5

dT

dt=

10.2947

(50 " T )

or114.2

dT

dt= 50 " T

The time constant is # = 114.2. The response is

T (t) = T (0)e!t/" + To(1 " e!t/" ) = 400e!t/" + 50(1 " e!t/" ) = 50 + 350e!t/"

The time to reach 130" is found from

50 + 350e!t/" = 130

which givest = "# ln(0.2286) = 168.5 s

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Page 56: SDsolns07

7.54 Let T1 be the sphere tempewrature and T2 be the bath temperature. From conservationof heat energy

C1dT1

dt=

1R

(T2 " T1)

C2dT2

dt=

1R

(T1 " T2)

where R is the surface convective resistance.The sphere’s surface area is

A = 4!r2 = 4!(30 # 10!3)2 = 1.131 # 10!2

and the volume isV1 =

43!r3 =

43!(30 # 10!3)3 = 1.13 # 10!4

R =1

hA=

1300(1.131 # 10!2)

= 0.2947

C1 = %V1cp = 8900(1.13 # 10!4)385 = 387.5

C2 = %V2cp = 7900(0.1)400 = 3.16 # 105

SoRC1 = 114.2 RC2 = 9.3125 # 104

Thus114.2

dT1

dt= T2 " T1

9.3125 # 104 dT2

dt= T1 " T2

Let #1 = 114.2 and #2 = 9.3125# 104. Applying the Laplace transform to each equationgives

#1sT1(s) " #1T1(0) = T2(s) " T1(s)

#2sT2(s) " #2T2(0) = T1(s) " T2(s)

These have the solutionT1(s) =

bs + c

s(s + a)

wherea =

#1 + #2

#2#20.008767

b = T1(0) = 400

c =T1(0)#2

+T2(0)#1

= 0.4421

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Page 57: SDsolns07

The response is

T1(t) =c

a+

ab " c

ae!at = 50.43 + 349.6e!0.008767t

The temperature T1 will reach 130" at

t =1

0.008767ln 0.2276 = 168.8 s

Contrast this result with the result of Problem 7.53, which is t = 168.5 s. Thus theassumption of a constant bath temperature in Problem 7.53 is very justified.

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Page 58: SDsolns07

7.55 The last three equations in Example 7.7-1 are:

(R1 + R2)T1 " R1T2 = R2Ti

R3T1 " (R2 + R3)T2 + R2T3 = 0

"R4T2 + (R3 + R4)T3 = R3To

In matrix form these are2

34(R1 + R2) "R1 0

R3 "(R2 + R3) R2

0 "R4 (R3 + R4)

5

67

2

34T1

T2

T3

5

67 =

2

34R2Ti

0R3To)

5

67

Once T1 is computed, qh can be computed from q = (T1 " Ti)/R1.The script file is:

R = [0.036,4.01,0.408,0.038];Ti = 20;To = -10;A = [R(1)+R(2),-R(1),0;R(3),-(R(2)+R(3)),R(2);0,-R(4),R(3)+R(4)];b = [R(2)*Ti;0;R(3)*To];T = A\bq = (1/R(1))*(Ti - T(1))

The results are T = [19.7596,"7.0214,"9.7462] "C and q = 6.6785 watts/m2. Thus thetotal heat loss is 10(6.6785) = 66.785 W.

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Page 59: SDsolns07

7.56 (a)

q2 =1

R2(p1 " pb)

q3 =1

R3(p1 " pc)

b) Rearrange the equations by bringing all the unknowns to the left side.

R1q1 + p1 = pa

R2q2 " p1 = "pb

R3q3 " p1 = "pc

q1 " q2 " q3 = 0

These equations have the form Ax = b where

A =

2

3334

R1 0 0 10 R2 0 "10 0 R3 "11 "1 "1 0

5

6667 b =

2

3334

pa

"pb

"pc

0

5

6667 x =

2

3334

q1

q2

q3

p1

5

6667

(c) The script file is

pa = 30*144;pb = 25*144; pc = 20*144;R = [10000,14000,14000];A = [R(1),0,0,1;0,R(2),0,-1;0,0,R(3),-1;1,-1,-1,0];b = [pa;-pb;-pc;0];format longx = A\b

When this file is run it gives the following output.

x =1.0e+003 *0.000063529411760.000006050420170.000057478991603.68470588235294

Thus q1 = 6.35 # 10!2, q2 = 6.05 # 10!3, q3 = 5.75 # 10!2 ft3/sec, and p1 = 3685 lb/ft2.

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Page 60: SDsolns07

7.57 For the given values

CdA = 0.5!(2 # 10!2)2 = 2! # 10!4

and the di"erential equation is

!(6h " h2)dh

dt= "2! # 10!4

%19.62h

ordh

dt= "2 # 10!4

%19.62h

6h " h2

(a) The greatest outflow rate occurs when the water level is the highest (h = 5). Thus usingh = 5 in the di"erential equation, we can obtain an lower bound on the time required todrain the tank. When h = 5,

dh

dt= "2 # 10!4

%19.62h

6h " h2= "3.9618 # 10!4

This implies that h(t) = "3.9618# 10!4t+5, and h = 0 at t = 5/(3.9618 # 10!4) = 12, 620s, or 210 minutes. Thus the tank will empty in no less than 210.34 minutes.

Instead of a lower bound on the estimate, we can obtain a higher estimate by using themid-point value for h; namely, h = 5/2 = 2.5. This gives

dh

dt= "2 # 10!4

%19.62h

6h " h2= "1.6008 # 10!4

This implies that h(t) = "1.6008# 10!4t+5, and h = 0 at t = 5/(1.6008 # 10!4) = 31, 234s, or 521 minutes.

(b) To use the ode45 solver, solve for the derivative:

dh

dt= "2 # 10!4

%19.62h

6h " h2

and create the following function file:

function hdot = tank(t,h)hdot = -(0.0002*sqrt(19.62*h))/(6*h-h^2);

Then use the ode45 solver in the following script file.

[t, h] = ode45(’tank’, [0, 25200], 5);plot(t,h),xlabel(’t (seconds)’),ylabel(’ h (feet)’)

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Page 61: SDsolns07

Start with a final time of something more than 12,620 s, and run the file until the plotshows the height approaching zero. The time to empty, which is 25,200 s or 420 minutes,was found this way. The estimate of 521 minutes obtained with the mid-point height is notmuch di"erent, and establishes confidence in the numerical result.

Note that if you choose a final time somewhat larger than 25,200 s, the denominator inthe expression for dh/dt becomes zero because h = 0, and the expression for dh/dt becomesundefined. This causes di#culties for the numerical algorithm. Thus it is best to start witha small value for the final time, and increase it. The plot is shown in the figure.

0 0.5 1 1.5 2 2.5 3x 104

0

0.5

1

1.5

2

2.5

3

3.5

4

4.5

5

t (seconds)

h (f

eet)

Figure : for Problem 7.57.

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Page 62: SDsolns07

7.58 (a) Write the equation asdy

dt= 4 " 2y

10 + 2tThen create the following function file.

function ydot = salt(t,y)ydot = 4-2*y/(10+2*t);

The following file solves the problem using the ode45 solver.

[t, h] = ode45(’salt’, [0, 10], 0);plot(t,h),xlabel(’Time t’),ylabel(’Salt Mass y’)

The plot is shown in the figure.

0 1 2 3 4 5 6 7 8 9 100

5

10

15

20

25

30

Time t

Salt

Mas

s y

Figure : for Problem 7.58.

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Page 63: SDsolns07

(b) The variable coe#cient 2/(10 + 2t) varies from 2/10 to 2/30 as t varies from 0 to10. Its mid-point value is 4/30. Using this value the model becomes

dy

dt+

430

y = 4

The step response is

y(t) =4

4/30

+1 " e!30t/4

,= 30

+1 " e!30t/4

,

This equation predicts that y(10) = 30. The plot shows that the numerical solution givesy(10) = 27 approximately. Thus we can have confidence that the numerical solution iscorrect.

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Page 64: SDsolns07

7.59 The relation between height h and the volume inflow rate r is

100dh

dt= r

Thush(t) =

1100

8 t

0r dt

The MATLAB m-file is

t = [0:10];r = [0,80,130,150,150,160,165,170,160,140,120];for k=2:11

h(k) = (1/100)*trapz(t(1:k),r(1:k));endplot(t,h)

The answer for the final height is given by h(11) and is 13.65 ft. The plot is shown below.

0 1 2 3 4 5 6 7 8 9 100

2

4

6

8

10

12

14

t (sec)

h (ft

)

Figure : for Problem 7.59

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Page 65: SDsolns07

7.60 This problem requires both analytical and numerical methods.(a) Let

b =13!

'R

H

(2

=13!

'1.54

(2

=3!64

Then V = bh3. When the cup is full, h = 4 in, and the water volume is V = b(4)3 = 64b =3!.

Let q be the flow rate (q = 2 cubic in/sec). From mass conservation,

dV

dt= q

andV (t) =

8 t

0q(t) dt =

8 t

02 dt = 2t

Equating the two expressions for the water volume gives 2t = 64b, or t = 32b = 3!/2 = 4.7s. So we do not need MATLAB for this part of the problem.

(b) If q(t) = 2(1 " e!2t), then

V (t) =8 t

0q(t) dt =

8 t

02(1 " e!2t) dt =

9

2t " 2e!2t

"2

:.....

t

0

= 2t + e!2t " 1

The time to fill is found by equating the two expressions for the volume:

2t + e!2t " 1 = 64b = 3!

We can solve this for t by using the fzero function. First define the function cup:

function f = cup(t)f = 2*t+exp(-2*t)-1 - 3*pi;

Use the fzero function with the answer from part (a) as the starting guess:

(fzero(’cup’,4.7)ans =5.2124

Thus it will take about 5.2 sec to fill the cup.

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Page 66: SDsolns07

7.61 a) The model is just like that shown in Figure 7.10.2 except that the two SSR blocksare not present. Create a subsystem block and save it.

b) Create a Simulink model like that shown in Figure 7.10.3, using the subsystem blockcreated in part (a).

c) In the MATLAB Command window, type the following parameter values.

(A_1 = 2;A_2 = 5;R_1 = 400;R_2 = 600;(rho = 1000; g = 9.81; q_1 = 50;(h10 = 1.5;h20 = 0.5;

Then run the simulation. A Stop time of 2000 s shows the complete response.

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Page 67: SDsolns07

7.62 Using the values given, the equation can be reduced to

dh

dt= " CdA

%2gh

!(2rh " h2)= "8.8589 # 10!4

%h

(6h " h2)

The model is shown in the following figure. Set the Initial condition of Integrator to 5. Inthe Fcn block type -8.8589*10^(-4)*sqrt(u(1))/(6*u(1)-u(1)^2) for the expression.You can plot the results by typing

(plot(tout,simout),xlabel(#t#),ylabel(#x#)

By experimenting with the Stop time, we find that the height is essentially 0 after 25,230 s.

Figure : for Problem 7.62

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Page 68: SDsolns07

7.63 From conservation of fluid mass, 100h = q, where q is the flow rate. Thus

h(t) =1

100

8 t

0q(t) dt

The model is shown in the following figure. We assume that the flow rate remains constantat the previous value for 1 min. Thus in the Lookup Table block, we select the Look-upmethod to be Use Input Below. In this block, the Vector of input values is [0:10] and theVector of output values is [0,80,130,150,50,160,165,170,160,140,120]. The height isapproximately 13 ft after 10 min.

Figure : for Problem 7.63

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Page 69: SDsolns07

7.64 From conservation of mass, the rate of change of water mass in the cup is

d(%V )dt

= %q

or%dV )dt

= %q

where % is the mass density of the water. We see that % cancels out of the equation, whichcan then be expressed as

dV

dt= !

'R

H

(2

h2 dh

dt= q

Using the values given for R and H and solving for dh/dt we obtain

dh

dt=

q

!+

RH

,2h2

=q

!+

964

,h2

a) With q = 2 the equation becomes

dh

dt=

2

!+

964

,h2

The model is shown in the following figure. Set the Initial condition of the Integratorto a small positive number, say 0.01, to avoid a singularity (because h appears in thedenominator of dh/dt. In the Fcn block type 2/pi*(9/64)*u(1)^2) for the expression.You can plot the results by typing

(plot(tout,simout),xlabel(#t#),ylabel(#x#)

By experimenting with the Stop time, we find that the height is essentially equal to 4 in.after 4.7 sec.

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Page 70: SDsolns07

Figure : for Problem 7.64a

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Page 71: SDsolns07

b) With q a function of time, we must modify the model in part (a). The equationbecomes

dh

dt=

q(t)

!+

964

,h2

The model is shown in the following figure. Set the Initial condition of the Integratorto a small positive number, say 0.01, to avoid a singularity (because h appears in thedenominator of dh/dt. In the Fcn block type pi*(9/64)*u(1)^2 for the expression. In theFcn1 block type 2*(1-exp(-2*u(1))) for the expression. The Clock block provides theinput time t to compute the expression 2(1 " e!2t). We use the Divide block to divide q(t)by !

+964

,h2. In the Divide block enter the number of inputs as */ (to multiply by q(t) and

to divide by !+

964

,h2). You can plot the results by typing

(plot(tout,simout),xlabel(#t#),ylabel(#x#)

By experimenting with the Stop time, we find that the height is essentially equal to H = 4after 5.21 sec.

Figure : for Problem 7.64b

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7.65 Use the model developed in Example 7.10.1 and change the Relay settings.

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7.66 The model is shown in the following figure. In the Relay block, set the Switch onpoint to 5.5 and the Switch o" point to 4.5. Set the Output when on to 0 and the Outputwhen o" to 50. Set the Initial condition of the Integrator to 1. Set the gain of the Gainblock to 1/%A = 1/2000. Set the gain of the other block to %g/R. Set the Stop time to1000. Using a value of R = 400, the height does not reach the desired band of 4.5 to 5.5ft because the inflow cannot compensate for the loss due to the small resistance. However,for a larger value, say R = 4000, the height oscillates between the desired values. You canplot the results by typing

(plot(tout,simout),xlabel(#t#),ylabel(#x#)

Figure : for Problem 7.66

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