Tải bản đầy đủ (.pdf) (508 trang)

Solution a first course in differential equations with modeling applications 9th ziill

Bạn đang xem bản rút gọn của tài liệu. Xem và tải ngay bản đầy đủ của tài liệu tại đây (17.97 MB, 508 trang )

Complete Solutions Manual

A First Course in Differential Equations
with Modeling Applications
Ninth Edition

Dennis G. Zill

Loyola Marymount University

Differential Equations with
Boundary-Vary Problems
Seventh Edition

Dennis G. Zill

Loyola Marymount University

Michael R. Cullen

Late of Loyola Marymount University

By

Warren S. Wright

Loyola Marymount University

Carol D. Wright

*



; BROOKS/COLE
C E N G A G E Learning-

Australia • Brazil - Japan - Korea • Mexico • Singapore • Spain • United Kingdom • United States


Table of Contents
1 Introduction to Differential Equations

2 First-Order Differential Equations

27

3 Modeling with First-Order Differential Equations

86

4 Higher-Order Differential Equations

137

5 Modeling with Higher-Order Differential Equations

231

6 Series Solutions of Linear Equations

274


7 The Laplace Transform

352

8 Systems of Linear First-Order Differential Equations

419

9 Numerical Solutions of Ordinary Differential Equations

478

10 Plane Autonomous Systems
11 Fourier Series

538

12 Boundary-Value Problems in Rectangular Coordinates

586

13 Boundary-Value Problems in Other Coordinate Systems

675

14 Integral Transforms

717

15 Numerical Solutions of Partial Differential Equations


761

Appendix I
A ppendix

1

Gamma function

II Matrices

506

783
785


3.ROOKS/COLE
C 'N G A G E L e a rn in g ”

ISBN-13. 978-0-495-38609-4
ISBN-10: 0-495-38609-X

i 2009 Brooks/Cole, Cengage Learning
ALL RIGHTS RESERVED. No part of this work covered by the
copyright herein may be reproduced, transmitted, stored, or
used in any form or by any means graphic, electronic, or
mechanical, including but not limited to photocopying,
recording, scanning, digitizing, taping, Web distribution,

Information networks, or information storage and retrieval
systems, except as permitted under Section 107 or 108 of the
1976 United States Copyright Act, without the prior written
permission of the publisher except as may be permitted by the
license terms below.

For product information and technology assistance, contact us at
Cengage Learning Customer & Sales Support,
1-800-354-9706
For permission to use material from this text or product, submit
all requests online at www.cengage.com/permissions
Further permissions questions can be emailed to
permissionreq uest@cenga ge. com

Brooks/Cole
10 Davis Drive
Belmont, CA 94002-3098
USA
Cengage Learning is a leading provider of customized
[earning solutions with office locations around the globe,
including Singapore, the United Kingdom, Australia,
Mexico, Brazil, and Japan. Locate your local office at:
international.cengage.com/region
Cengage Learning products are represented in
Canada by Nelson Education, Ltd.
For your course and learning solutions: visit
academic.cengage.com
Purchase any of our products at your local college
store or at our preferred online store
www.ichapters.com


NOTE’. UNDER NO C\RCUMST ANCES MAY TH\S MATERIAL OR AMY PORTION THEREOF BE SOLD, UCENSED, AUCTIONED,
OR OTHERWISE REDISTRIBUTED EXCEPT AS MAY BE PERMITTED BY THE LICENSE TERMS HEREIN.

READ IMPORTANT LICENSE INFORMATION
Dear Professor or Other Supplement Recipient:
Cengage Learning has provided you with this product (the
“Supplement' ) for your review and, to the extent that you adopt
the associated textbook for use in connection with your course
(the ‘Course’ ), you and your students who purchase the
textbook may use the Supplement as described below. Cengage
Learning has established these use limitations in response to
concerns raised by authors, professors, and other users
regarding the pedagogical problems stemming from unlimited
distribution of Supplements.
Cengage Learning hereby grants you a nontransferable license
to use the Supplement in connection with the Course, subject to
the following conditions. The Supplement is for your personal,
noncommercial use only and may not be reproduced, posted
electronically or distributed, except that portions of the
Supplement may be provided to your students IN PRINT FORM
ONLY in connection with your instruction of the Course, so long
as such students are advised that they

:"tcd in Canada
1 3 4 5 6 7 11 10 09 08

may not copy or distribute any portion of the Supplement to any
third party. You may not sell, license, auction, or otherwise
redistribute the Supplement in any form. We ask that you take

reasonable steps to protect the Supplement from unauthorized
use. reproduction, or distribution. Your use of the Supplement
indicates your acceptance of the conditions set forth in this
Agreement. If you do not accept these conditions, you must
return the Supplement unused within 30 days of receipt.
All rights (including without limitation, copyrights, patents, and
trade secrets) in the Supplement are and will remain the sole and
exclusive property of Cengage Learning and/or its licensors. The
Supplement is furnished by Cengage Learning on an "as is” basis
without any warranties, express or implied. This Agreement will
be governed by and construed pursuant to the laws of the State
of New York, without regard to such State’s conflict of law rules.
Thank you for your assistance in helping to safeguard the integrity
of the content contained in this Supplement. We trust you find the
Supplement a useful teaching tool


1 Introduction to Differential Equations

1 . Second order; linear
2 . Third order; nonlinear because of (dy/dx)4

3. Fourth order; linear
4. Second order; nonlinear bccausc of cos(r + u)
5. Second order; nonlinear because of (dy/dx)2 or

1 + (dy/dx)2

6 . Second order: nonlinear bccausc of R~


7. Third order: linear
8 . Second order; nonlinear because of x2

9. Writing the differential equation in the form x(dy/dx) -f y2 = 1. we sec that it is nonlinear in y
because of y2. However, writing it in the form (y2 —1)(dx/dy) + x = 0, we see that it is linear in x.
10. Writing the differential equation in the form u(dv/du) + (1 + u)v = ueu wc see that it is linear in
v. However, writing it in the form (v + uv —ueu)(du/dv) + u — 0, we see that it, is nonlinear in ■
Ji­

ll.

From y = e-*/2 we obtain y' = —\e~x'2. Then 2y' + y = —e~X//2 + e-x/2 = 0.

12 . From y = | — |e-20* we obtain dy/dt = 24e-20t, so that

% + 20y = 24e~m + 20
- |e_20t) = 24.
clt
\'o 5
/
13. R'om y = eix cos 2x we obtain y1= 3e^x cos 2x — 2e3* sin 2a? and y” = 5e3,xcos 2x — 12e3,xsin 2x, so
that y" — (k/ + l?>y = 0.
14. From y = —cos:r ln(sec;r + tanrc) we obtain y’ — —1 + sin.Tln(secx + tana:) and
y" = tan x + cos x ln(sec x + tan a?). Then y" -f y = tan x.
15. The domain of the function, found by solving x + 2 > 0, is [—2, oo). From y’ = 1 + 2(x + 2)_1/2 we

1


Exercises 1.1 Definitions and Terminology

have

= (y - ®)[i + (20 + 2)_1/2]

{y - x)y'

= y — x + 2(y - x)(x + 2)-1/2
= y - x + 2[x + 4(z + 2)1/2 - a;](a: + 2)_1/2
= y — x + 8(ac + 2)1;/i(rr + 2)~1/2 = y —x + 8.
An interval of definition for the solution of the differential equation is (—2, oo) because y
defined at x = —2.
16. Since tan:r is not defined for x = 7r/2 + mr, n an integer, the domain of y = 5t£v.
{a; |5x ^ tt/2 + 7i-7r} or {;r |x ^ tt/IO + mr/5}. From y' — 25sec2 §x we have
y' = 25(1 + tan2 5x) = 25 + 25 tan2 5a: = 25 + y2.
An interval of definition for the solution of the differential equation is (—7r/ 10, 7T/10 . A:,
interval is (7r/10, 37t/10). and so on.
17. The domain of the function is {x \4 —x2 ^ 0} or {x\x ^ —2 or x ^ 2}. Prom y' — 2.::

-=-

we have

An interval of definition for the solution of the differential equation is (—2, 2). Other
(—oc,—2) and (2, oo).
18. The function is y — l/y /l — s in s . whose domain is obtained from 1 —sinx ^ 0 or
the domain is {z |x ^ tt/2 + 2?i7r}. From y' = —1(1 —sin x)

. = 1 T

2(—cos.x) we have


2y' = (1 —sin;r)_ ‘?/’2 cos# = [(1 — sin:r)~1//2]3 cos:r - f/3 cosx.

An interval of definition for the solution of the differential equation is (tt/2. 5tt/2
is (57r/2, 97r/2) and so on.
19. Writing ln(2X — 1) —ln(X — 1) = t and differentiating implicitly we obtain
dX
2 X - 1 dt
2

dX
X - l dt
1

2X - 2 - 2X + 1 d X _
(2X - 1)(X - 1) dt
IX
— = -C2X - 1)(X - 1) = (X - 1)(1 - 2X .

2

A :..

.


Exercises 1.1 Definitions and Terminology
x

Exponentiating both sides of the implicit solution we obtain

2X-1
----- = el
X - l
2 X - 1 = X el - ef
-4

(e* - 1) = (e‘ - 2)X
X =

-2

-2

ef' — 1
e* - 2 '

-4

Solving e* — 2 = 0 we get t = In 2. Thus, the solution is defined on (—oc.ln2) or on (In 2, oo).
The graph of the solution defined on (—oo,ln2) is dashed, and the graph of the solution defined on
(In 2. oc) is solid.
20. Implicitly differentiating the solution, we obtain

y

—x 2 dy — 2xy dx + y dy — 0
2xy dx + (a;2 —y)dy = 0.

Using the quadratic formula to solve y2—2x2y —1 = 0 for y, we get
y = (2x2 ± V4;c4 + 4)/2 = a’2 ± v V 1+ 1 . Thus, two explicit

solutions are y\ = x2 + \A'4 + 1 and y-2 = x2 — V.x4 + 1. Both
solutions are defined on (—oo. oc). The graph of yj (x) is solid and
the graph of y-2 is daalied.
21 . Differentiating P = c\?}} ( l + cie^ we obtain

dP _ ( l + cie*) cie* - cie* • cie* _
(1 + cie*)"

eft

Cie«

[(l + cie‘) - cie4]

1 + cief

1 + cie(

CiC
= P( 1 - P).
1 + ci ef

Ci

1 + CI&-

2 PX ,2
,2
22 . Differentiating y = e~x / e: dt + c\e~x we obtain
Jo

2* f X
*22
-r.2
y/ = e-*2er 2 2xe
/ e dt — 2c\xe
=1
Jo
Substituting into the differential equation, we have
___

r x

J

2

2xe x

rx +2
e dt — 2cixe —X
Jo

y' + 2xy = l — 2xe x I e* dt — 2cixe x +2xe x [ e* dt 4- 2cio;e x = 1.
Jo
Jo

3


Exercises 1.1 Definitions and Terminology


23. From y — ci e2x+c.2 xe2x we obtain ^

- (2c\+C2 )e2x-r2c2xe2x and —| = (4cj + 4c;2)e2x + 4c2xe2j'.

so that
n
.T.
dx2

—4 ^ + Ay = (4ci + 4co - 8ci - 4c2 + 4ci)e2x + (4c2 — Sc2 + 4e2)xe2x — 0.
d:r
dx

24. From y — Cix-1 + c^x + c%x ]n x + 4a;2 we obtain
^ = —c\x 2 + C2 + c$ + C3 In x + 8rc,
dx
d2y
= 2cix,_3 + C3;r_1 -f 8.
dx2

and

= —6cix -4 - c3a r 2,
so that
dx'3 +
_r “J/
J' dx + V ~ ^_6ci + 4ci + Cl + Cl^x 3 + ^_ °3 + 2cs ~~02 ~ C3 + C2^X
2a'2 dx2 ~ X
t (—C3 + cz)x In a; + (16 - 8 + 4)x2

= 12x2.
( —x2, x < 0
,
f —2x,
25. From y = <
'
we obtain y' = < ^
tx .
x> 0
{ 2x,

x< 0
^ „ so that
x> 0

- 2/y = 0.

26. The function y(x) is not continuous at x = 0 sincc lim y(x) = 5 and lim y(x) = —5. Thus. y’(x)
x —>0“

x —>0+

does not exist at x = 0.
27. From y = emx we obtain y' = mernx. Then yf + 2y — 0 implies
rnemx + 2emx = (m + 2)emx = 0.
Since emx > 0 for all x} m = —2. Thus y = e~2x is a solution.
28. From y = emx we obtain y1= mernx. Then by' — 2y implies
brriemx = 2e"lx or

m =


5

Thus y = e2:c/5 > 0 is a solution.
29. From y = emx we obtain y' = memx and y" = rn2emx. Then y" —5y' + Qy = 0 implies
m 2emx - 5rnemx + 6emx = (rn - 2)(m - 3)emx = 0.
Since ema! > 0 for all x, rn = 2 and m = 3. Thus y = e2x and y = e3:r are solutions.

30.

From y = emx we obtain y1= rnemx an2m2emx + 7rnemx - 4ema: = (2m - l)(m + 4)ema' = 0.

0 implies


Exercises 1.1 Definitions and Terminology
Since emx > 0 for all x, rn ~ | and m = —4. Thus y — ex/2 and y = e ^ are solutions.
31. From y = xm we obtain y' = mxm~1 and y" = m(m — l)xm~2. Then xy" + 2y' = 0 implies
xm(m, — l)xm~2 + 2mxm~l = [m(rn -1)4-

= (m 2 + m)xm_1

- rn(m + l).xm_1 = 0.
Since a:"'-1 > 0 for ;r > 0. m = 0 and m = —1. Thus y = 1 and y — x~l are solutions.
32. From y = xm we obtain y' = mxm~1 and y" = m(m — l)xm~2. Then x2y" —7xy' + 15y — 0 implies
x2rn{rn — l)xrn~2 — lxm xm~A+ 15:em =

[m(m — 1) — 7m + 15]xm


= (ro2 - 8m + 15)a,m = (m - 3) (to - 5)xm = 0.
Since xm > 0 for x > 0. m = 3 and m = 5. Thus y — x^ and y = xa are solutions.
In Problems 33-86 we substitute y = c into the differential equations and use y' — 0 and y" — 0
33. Solving 5c = 10 we see that y ~ 2 is a constant solution.
34. Solving c2 + 2c —3 = (c + 3)(c — 1) = 0 we see that, y = —3 and y = 1 are constant solutions.
35. Since l/(c — 1) = 0 has no solutions, the differential equation has no constant solutions.
36. Solving 6c = 10 we see that y = 5/3 is a constant solution.
37. From x — e~2t + 3ec< and y — —e~2t + 5ew we obtain
^ = —2e~2t + 18e6* and
dt

dt

= 2e~2t + 30e6*.

Then

and

x-+ 3y = (e~2t + 3e6t) + 3 (- e '2* + oe6t) = -2e"2* + 18e6t = ^
\
Jub
5:r + 3y = 5(e~2* + 3eet) + 3(-e~2* + 5e6') = 2e~2t + 30e6* = ^ .
at

38. From x = cos 21 + sin 21 +

and

and y — —cos 21 —sin 21 —


— = —2 sin 2t -f 2 cos 22 +
d.t
5

and

d2:r
,

. . ^
1 ^
,
= —4 cos 2t — 4 sm 22 + re
and
dt2
Id

we obtain

^ = 2 sin 22 — 2 cos 2t — -e*
dt
5
^2V
,
1 /
-r-^- = 4 cos 2t + 4 sin 22-- e .
d22
5


Then

cPx

and

1
1
4y + et = 4(—cos 21 — sin 21 — pef) + el — —4 cos 21 — 4 sin 22 + -el = -7-^
0
o
dt

5


Exercises 1.1 Definitions and Terminology

4x — ef = 4(cos 21 + sin 21 -I- ^e*) — e* = 4 cos 2£ + 4 sin 2t — \ef —
39. (t/ ) 2 + 1 = 0 has no real solutions becausc {y')2 + 1 is positive for all functions y = 4>(x).
40. The only solution of (?/)2 + y2 = 0 is y = 0, since if y ^ 0, y2 > 0 and (i/ ) 2 + y2 > y2 > 0.
41. The first derivative of f(x ) = ex is eT. The first derivative of f{x) = ekx is kekx. The differential
equations are y' — y and y' = k.y, respectively.
42. Any function of the form y = cex or y = ce~x is its own sccond derivative. The corresponding
differential equation is y" — y = 0. Functions of the form y = c sin x or y — c cos x have sccond
derivatives that are the negatives of themselves. The differential equation is y" -+
-y = 0.
43. We first note that yjl —y2 = \/l — sin2 x = Vcos2 x = |cos.-r|. This prompts us to consider values
of x for which cos x < 0, such as x = tt. In this case
%


dx

i {sklx)

= c o s x l ^ , . = COS7T =

— 1.

X=7T

but
\/l - y2\x=7r = V 1 - sin2 7r = vT = 1.
Thus, y = sin re will only be a solution of y' - y l —y2 when cos x > 0. An interval of definition is
then (—tt/ 2, tt/ 2). Other intervals are (3tt/ 2, 5tt/ 2), (77t/ 2, 9tt/ 2). and so on.
44. Since the first and second derivatives of sint and cos t involve sint and cos t, it is plausible that a
linear combination of these functions, Asint+ B cos t. could be a solution of the differential equation.
Using y' — A cos t —B sin t and y" = —A sin t —B cos t and substituting into the differential equation
we get
y" + 2y' + 4y = —A sin t — B cos t + 2A cos t — 2B sin t + 4A sin t + 4B cos t
= (3A — 2B) sin t + (2A + 3B) cos t = 5 sin t.
-- --+
TT7«
Thus 3A — 2B = 5 and 2A + 3B = 0. Solving these simultaneous equations
we ^ITirl
find AA =
j#
and
13


B = —

. A particular solution is y =

sint — ^ cost.

45. One solution is given by the upper portion of the graph with domain approximately (0,2.6). The
other solution is given by the lower portion of the graph, also with domain approximately (0. 2.6).
46. One solution, with domain approximately (—oo, 1.6) is the portion of the graph in the second
quadrant together with the lower part of the graph in the first quadrant. A second solution, with
domain approximately (0,1.6) is the upper part of the graph in the first quadrant. The third
solution, with domain (0, oo), is the part of the graph in the fourth quadrant.

6


Exercises 1.1 Definitions and Terminology
47. Differentiating (V1+ y^)/xy = 3c we obtain
xy(3x2 + 3y2y') - (a?3 + y*)(xi/ + y)
= 0
x?y2
3x3y + 3xy^y' —x'^y' — x% —xy^y’ — yA — 0
(3:ry3 - xA - xyz}i/ = -3x3y + xi y + y4
, = y4 - 2x3y _ y(y[i - 2x3)
^

2.ry3 —x4

rt:(2y3 —a:3)


48. A tangent line will be vertical where y' is undefined, or in this case, where :r(2y3 — x3) = 0. This
gives x = 0 and 2y3 = a:3. Substituting y?J — a;3/2 into ;r3 + y3 = 3xy we get

x 3 + h 3 = 3x { w x)
-x3 = — r 2
2
2V3a
a:3 = 22/ V
z 2(.x - 22/3) = 0.
Thus, there are vertical tangent lines at x = 0 and x = 22/3, or at (0, 0) and (22/ 3, 21'/3). Since
22/3 ~ 1.59. the estimates of the domains in Problem 46 were close.

49. The derivatives of the functions are ^(.x) — —xf a/25 —x2 and ^ { x ) = x/\/25 —x2, neither of
which is defined at x = ±5.
50. To determine if a solution curve passes through (0,3) we let 2 = 0 and P = 3 in the equation
P = c-ie1/ (1 + eye*). This gives 3 = c j/(l + ci) or c\= —| . Thus, the solution curve
(—3/2)e* = —3e*
1 - (3/2)eL 2 - 3e{
passes through the point, (0,3). Similarly, letting 2 = 0 and P = 1 in the equation for the oneparameter family of solutions gives 1 = c t/(l + ci) or ci = 1 + c-|. Since this equation has no
solution, no solution curve passes through (0. 1).
51. For the first-order differential equation integrate f(x). For the second-order differential equation
integrate twice. In the latter case we get y = f ( f f(x)dx)dx + cja: + C2 52. Solving for y’ using the quadratic formula we obtain the two differential equations
y>= — ^2 + 2\J1 + 3ar®^

and

y1= — ^2 — 2 y 1 4-3a?^^ ,

so the differential equation cannot be put in the form dy/dx = f(x,y).


7


Exercises 1.1 Definitions and Terminology
53. The differential equation yy'—xy = 0 has normal form dy/dx = x. These are not equivalent because
y = 0 is a solution of the first differential equation but not a solution of the second.
54. Differentiating we get y' = c\+ 3c2%2 and y" = 602x. Then C2 - y"/(>x and

~ 1/ —xy"f 2, so

v=iy'-^-)x+{t)x3=xy'-rv
and the differential equation is x2y" —3xy' + Sy = 0.
2

55. (a) Since e~x is positive for all values of x. dy/dx > 0 for all x, and a sohition. y(x), of the
differential equation must be increasing on any interval.
(b) lim ^ = lim e~x‘ = 0 and lim ^ = lim e~x = 0. Since dy/dx approaches 0 as x
v ' x^-cc dx
x-+-x
dx
approaches —oc and oc, the solution curve has horizontal asymptotes to the left and to the
right.
(c) To test concavity we consider the second derivative
d2y

d (dy\
d {
*\ _
\ dr.)-dx\ e'


2

Since the sccond derivative is positive for x < 0 and negative for x > 0, the solution curve is
concave up on (—00. 0) and concave down 011 (0. 00). x

56. (a) The derivative of a constant solution y — c is 0, so solving 5 — c = 0 we see that, c — 5 and so
y = 5 is a constant sohition.
(b) A solution is increasing where dyjdx = 5 — y > 0 or y < 5. A solution is decreasing where
dy/dx = 5 —y < 0 or y > 5.
57. (a) The derivative of a constant solution is 0, so solving y(a — by) = 0 we see that y = 0 and
y = a/b are constant solutions.
(b) A solution is increasing where dy/dx = y(a —by) = by(a/b —y) > 0 or 0 < y < a/b. A solution
is decreasing where dy/dx = by(a/b — y) < 0 or y < 0 or y > a/b.
(c) Using implicit differentiation we compute
= y(-by') + y'{a - by) = y'(a - 2by).
Solving d2y/dx2 = 0 we obtain y = a/2b. Since dl y/dx2 > 0 for 0 < y < a/2b and d2y/dx2 < 0
for a/26 < y < a/b, the graph of y =
8


Exercises 1.1 Definitions and Terminology

(d)

58. (a) If y = c is a constant solution I lien y' = 0. but c2 + 4 is never 0 for any real value of c.
(b) Since y* = y2 + 4 > 0 for all x where a solution y = o(x) is defined, any solution must be
increasing on any interval on which it is defined. Thus it cannot have any relative extrema.

x


59. In Mathematica use
Clear [y]
y[x_]:= x Exp[5x] Cos[2x]

y[xl
y""[x] — 20 y ’ "[x] + 158y"[x] — 580y'[x] +84 ly [x]//S im plify
The output will show y{x) = e0Xx cos 2x. which verifies that the corrcct function was entered, and
0, which verifies that this function is a solution of the differential equation.

60. In Mathematica use
C lear [y]
y[x_]:= 20 Cos[5 Log[x]]/x — 3Sin[5Log[x]]/x

y (x 3
x~3 y'"[x] + 2x~2 y"[x] + 20x y'[x] — 78y[x]//Sim plify
The output will show y(x) = 20 cos(o In x)/x—Z sin(5 In x)/x. which verifies that the correct function
was entered, and 0, which verifies that this function is a solution of the differential equation.

9


Exercises 1.2 Initial-Value Problems

.problem s

1 . Solving —1/3 = 1/(1 + ci) we get c\— —4. The solution is y = 1/(1 — 4e~x).
2 . Solving 2 = 1/(1 + c\e) we get c\= - ( l/ 2)e_1. The solution is y — 2/(2 - e " ^ -1)) .
3 . Letting x = 2 and solving 1/3 = 1/(4 + c) we get c = —1. The solution is y — 1/ (x2 — 1). This


solution is defined on the interval (l,oc).
4. Letting x = -2 and solving 1/2 = 1/(4 + c) we get c = —2. The solution is y = 1/(.:;;2 — 2). This
solution is defined on the interval (—oo, —y/2).
5 . Letting x = 0 and solving 1 = 1/e we get c — 1. The solution is y = l/(a ;2 + 1). This solution is

defined on the interval (—oo, oo).
6 . Lotting x = 1/2 and solving —4 = l/ ( l/ 4 + c) we get c = —1/2. The solution is y = lj( x 2 —1/2) =

2/(2x2 — 1). This solution is defined on the interval (—l/y/2 , l/\/2 )In Problems 7-10 we use x — c\cos t + 0 2 sin t and x' — —c\sin t + C2 cos t to obtain a system, of two
equations in the two unknowns ei and C2 ■
7. From the initial conditions we obtain the system

C2 = 8 .

The solution of the initial-value problem is x = —cost + 8 sint.
8 . From the initial conditions we obtain the system
02

= 0

-ci - 1.
The solution of the initial-value problem is x = —cos t.
9. From the initial conditions we obtain
\/3
VS

1

I


- 7 T C] + - C2 = -

Solving, we find c\ = V3/4 and C2 =

1/4.

x = (a/3/4) cost + (1/4) s in t

10

The solution of the initial-value problem is


Exercises 1.2 Initial-Value Problems
10. From the initial conditions we obtain
\/2

\/2

T Q

T

r-

2=

\/2
2~


~2~

=

Solving, we find ci = —1 and c>2 = 3. The solution of the initial-value problem is x = —cost+3 sin t.
Problems 11-14 we use y = c\ax + C2 e~x and if — c\e£ — C2 e~x to obtain a system of two equations
the two unknowns c\ and

09-

11. From the initial conditions we obtain

Ci + C2 = 1
ci - c2 = 2.
Solving, wo find c\= ^ and C2 = —5 . The solution of the initial-value problem is y = |ex — ^e~x.
12. From the initial conditions we obtain

ec\+ e-1C2 = 0
ec\— e~lC2 = e.
Solving, we find ci = \and C2 = —^e2. The solution of the initial-value problem is
:j = \ex - \e2e~x = \ex - \e2~x.
13. From the initial conditions we obtain
e-1ci 4- ec2 = 5
— ec2 = —5.
Solving, we find ci = 0 and C2 = 5e 1. The solution of the initial-value problem is y = 5e 1e x =
-

Of

— 1 — t*


-

14. From the initial conditions we obtain
ci + C2 = 0
Cl - c2 = 0.
Solving, we find ci = C2 = 0. The solution of the initial-value problem is y = 0.
15. Two solutions are y = 0 and y = x%i.
I ' . Two solutions are y — 0 and y = x2. (Also, any constant multiple of x2 is a solution.)
1

For fix, y) = y2/3 we have

df

~

2

/

Thus, the differential equation will have a unique solution
ay
3'
any rectangular region of the plane where y ^ 0.

11


Exercises 1.2 Initial-Value Problems

18. For f'(x,y) = yjxy we have d f /dy - \\jx/y ■ Thus, the differential equation will have a unique
solution in any region where x > 0 and y > 0 or where x < 0 and y < 0.

?

df

l

19. For fix . y) = — we have
= —. Thus, the differential equation will have a unique solution in
x
ay
x
any region where x ^ 0 .
20. For f(x,y) = x + y we have

= 1. Thus, the differential equation will have a unique solution in

the entire plane.
21. For f(x, y) - x2/{& —y2) we have d f /dy — 2x‘1y/(A. —y2)2. Thus the differential equation will have
a unique solution in any region where y < —2, —2 < y < 2, or y > 2.
df
_3x2y2
22. For f(x. y) ~ —-—* we have -1- *- ----- h-. Thus, the differential equation will have a unique
V J>
1 + y3
dy
(l + y3)2
solution in any region where y ^ —1.

y2
df
2x^y
23. For f(x, y) = —tt-- rr we have — = ---- :— k . Thus, the differential equation will have a unique
M
x2 + y2
dy
(x2 + y2)2
solution in any region not containing (0, 0).
24. For / ( x, y) = (y + x)/(y — x) we have d f/dy = —2x/(y — x)2. Thus the differential equation will
have a unique solution in any region where y < x or where y > x.
In Problems 25-28 we identify f{x,y) = \jy2 —9 and d f/d y = y/\jy2 —9.

We see that f and

d f/d y are both continuous in the regions of the plane determined by y < —3 and y > 3 with no
restrictions on x.
25. Since 4 > 3, (1,4) is in the region defined by y > 3 and the differential equation has a unique
solution through (1,4).
26. Since (5,3) is not in cither of the regions defined by y < —3 or y

there is no guarantee of a

unique solution through (5,3).
27. Since (2, —3) is not in either of the regions defined by y < —3 or y > 3, there is no guarantee of a
unique solution through (2, —3).
28. Since (—1,1) is not in either of the regions defined by y < —3 or y > 3, there is no guarantee of a
unique solution through (—1, 1).
29. (a) A one-parameter family of solutions is y = ex. Since y' = c, xy' = xc = y and y(0) = c ■0 = 0.
(b) Writing the equation in the form y' — y/x, we see that R cannot contain any point on the y-axis.

Thus, any rectangular region disjoint from the y-axis and containing (xq, ijq) will determine an

12


Exercises 1.2 Initial-Value Problems
interval around xg and a unique solution through (so- yo). Since ;i’o = 0 in part (a), we are not
guaranteed a unique solution through (0. 0).
(c) The piecewise-defined function which satisfies y(0) = 0 is not a solution sincc it is not differ­
entiable at x - 0.
(I

9

9

30. (a) Since — tan (a; + c) = sec-(a: + c) = 1 + tan"(x -i-c), we see that y = tan(x + c) satisfies the
L lX

differential equation.
(b) Solving y(0) = tan <: — 0 we obtain c = 0 and y = tan x. Since tan:r is discontinuous at
x — ±7t/2; the solution is not defined on (—2,2) because it contains ±tt/2.
(c) The largest interval on which the solution can exist is (—tt/2, 7t/ 2).
d

1

1

1


31. (a) Since — (----- ) = 7---- = i f . we see that y = ------- is a solution of the differential
v '
rJ
((x
r . A+
- c)"‘
X-h C
dx ^ rx. A+- equation.
(b) Solving y(0) = —1jc = 1 we obtain c = —1 and y — 1/(1 — x). Solving y(0) = —1/c = —1
wc obtain c — 1 and y = —1/(1 + x-). Being sure to includc x = 0, we see that the interval
of existence of y — 1/(1 — x) is (—oc, 1), while the interval of existence of y = —1/(1 + x) is
( 1, oc).
(c) By inspection we see that y = 0 is a solution 011 ( — 00, 00).
32. (a) Applying y(l) = 1 to y = —l/(x -f c) gives
1
1 =

or

1+c

1 + c = —1.

Thus c = —2 and
1

y


x —2

2 —x

(b) Applying y(3) = —1 to y = —1/ (;r + c) gives
1
-1 =

or

3 + c = 1.

Thus c = —2 and
y

x —2

2 —x
,

1

(c) No, they are not the same solution. The interval I
of definition for the solution in part (a) is (—00, 2);
whereas the interval I of definition for the solution
in part (b) is (2. 00). See the figure.

/

}


;
\

(1,1)
(3, -1)

13

--- 4 ‘


Exercises 1.2 Initial-Value Problems
33. (a) Differentiating 3x2 — y2 = c we get 6x — 2yyf = 0 or yy' = 3a;.
(b) Solving 3a:2 —y2 = 3 for y we get
y = ©1 (a:) = \/3{x2 - 1).

1 < a; < oo,

y = ‘3(x- - 1)

1 < x < oo.

y = M x)

—oc < x < —1.

=


y =
—oo < x < —1.

(c) Only y = 34. (a) Setting x = 2 and y = —4 in 3;r2 —y2 = c we get 12 — 16 = —4 = c,

y

4:
i

so the explicit solution is
y = —y 3a:2 + 4, —oo < x < oo.
(b) Setting c. = 0 we have y = \/3a: and y = —\/3^, both defined on
(—oo;oc).

Jn Problems 35-38 we consider the points on the graphs with x-coordinates xq = —1. xq = 0 , a
;Z*0 = 1. 77?,e slopes of the tangent lines at these points are compared with the slopes given by y'(xo)
(a) through (f).

35.
36.
37.
38.
39.

The graph satisfies the conditions in (b) and (f).
The graph satisfies the conditions in (e).
The graph satisfies the conditions in (c) and (d).

The graph satisfies the conditions in (a).
Integrating y' = 8e2x + 6x we obtain

y=j

(8e2x’ + Qx)dx = 4e2x

+ 3x2 + c.

Setting x = 0 and y — 9 we have 9 = 4 + c so c = 5 and y — 4e2x -f 3a:2 + 5.
40. Integrating y" — 12x —2 we obtain
y' = j ( 12a; - 2)dx = dx2 - 2x + ci.
Then, integrating y! we obtain
y = / (6x2 —2x + ci)dx = 2x?J —x2 + Cix + oi-

14


Exercises 1.2 Initial-Value Problems
- 1 the y-coordinate of the point of tangency is y = —1+5 = 4. This gives the initial condition
= 4. The slope of the tangent line at x = 1 is y'(l) = —1. From the initial conditions we
n

2 — 1 + ci + C2 = 4

or

ci + c-2 — 3

6 — 2 + ci = —1


or

Ci ~ —5.

. ci = —5 and oi = 8, so y = 2a'3 —x2 —5ir + 8.
l x = 0 and y = ^ , y' = —1, so the only plausible solution curve is the one with negative slope
5 ), or the black curve.

solution is tangent to the .i’-axis at (rro, 0), then y' = 0 when x -xq and y = 0 . Substituting
values into y' + 2y = 3x — G we get 0 + 0 = 3-I'q — 6 or :co = 2.
heorcm guarantees a unique (meaning single) solution through any point. Thus, there cannot
o distinct solutions through any point.

2) = ^ (16) = 1. The two different solutions are the same on the interval (0, oo), which is all

h required by Theorem 1.2.1.
= 0. dP/dt = 0.15P(0) + 20 = 0.15(100) + 20 = 35. Thus, the population is increasing at a
.■
f 3.500 individuals per year.
population is 500 at time t = T then

= 0.15P(r) +*20 = 0.15(500) + 20 = 95.
dt t=T
. at this time, the population is increasing at a rate of 9,500 individuals per year.


Exercises 1.3 Differential Equations as Mathematical Models

r


. ..... ..................................... :

.

7

T ' " „ >.

r;;

; ;*:* :

;

-D ifferential Eqti^feioiis

dP
dP
1. —— — kP + r;
— kP —r
dt
dt
2. Let b be the rate of births and d the rate of deaths. Then b -k]_P and d = k^P- Since dPjdt — b—d,
the differential equation is dP/dt = k\P —k^P-

3.

Let b be the rate of births and d the rate of deaths. Then b — k\P and d = k^P'2. Since dP/dt = b—d.


the differential equation is dP/dt — kiP — I^ P 2.
d.P
4. —— — h P - k2P 2 - h , h > 0
dt
5 . From the graph in the text we estimate To = 180° and Tm = 75°. We observe that when T = 85,
dT/ dt « —1. From the differential equation we then have
k

=

t m

'

_

=

T - Tm

^

i _

=

_ 01

85-75


6 . By inspecting the graph in the text we take Tm to be Tm(t) = 80 — 30 cos nt/12.

Then the

temperature of the body at time t is determined by the differential equation
dT
dt



7.

— k

T-

80 - 30 cos

5*)]

t > 0.

The number of students with the flu is x and the number not infected is 1.000 — x, so dx/dt —
fcc(1000 - a:).

8 . By analogy, with the differential equation modeling the spread of a disease, we assiune that the rate

at which the technological innovation is adopted is proportional to the number of people who have
adopted the innovation and also to the number of people, y(t), who have not yet adopted it. Then
x + y — n. and assuming that initially one person has adopted the innovation, we have

dr

— kx(n —a?),

x(0) = 1.

(a*L

9. The rate at which salt is leaving the .tank is
Rout (3 gal/min) •

(A

\
4
lb/gal j = — lb/min.

Tims dA/dt = —A/100 (where the minus sign is used since the amount of salt is decreasing. The
initial amount is A(0) = 50.
10. The rate at which salt is entering the tank is
Riu = (3 gal/min) • (2 lb/gal) = 0 lb/min.

16


Exercises 1.3 Differential Equations as Mathematical Models
Since the solution is pumped out at a slower rate, it is accumulating at the rate of (3 —2)gal/min
1 gal/min. After t minutes there are 300 + 1 gallons of brine in the tank. The rate at which salt is

R„t = (2 gal/min) •


leaving is

lb/gal) =

^ - lb/miu.

The differential equation is
dA
dt



2A

= 6

300 + 1

11. The rate at which salt is entering the tank is
R in

= (3 gal/min) • (2 lb/gal) = 6 lb/min.

Since the tank loses liquid at the net rate of
3 gal/min — 3.5 gal/min = —0.5 gal/min.
after t minutes the number of gallons of brine in the tank is 300 — \t gallons. Thus the rate at
which salt is leaving is

^=


/

lb/gal)

A

\

3 54

7/4

' (3'5 gal/min) = so S ^tT S lb/m in = 6 0 0 ^ 7 lb/mi,L

The differential equation is
dA

~dt=

7A
600^-i

°r

dA
7
M + 600^1 A = 6'

12. The rate at which salt is entering the tank is

R in

= {('in lb/gal) • (rin gal/min) = cinrin lb/min.

Xow let A(t) denote the number of pounds of salt and N(t) the number of gallons of brine in the tank
at time t. The concentration of salt in the tank as well as in the outflow is c(t) = x(t)/N(t). But
'he number of gallons of brine in the tank remains steady, is increased, or is decreased depending
:m whether r*n = rQUt, n n > rout. or r.,;n < rou*. In any case, the number of gallons of brine in the
:ank at time t is N(t) = N q + (r?:n —rout)i. The output rate of salt is then
Rout = ( v

A---- - lb/min.
, , A---- rr lb/gal J • (rout gal/min) = rmt
+ (nn - rout)t
J
M + (rin - rout)t

The differential equation for the amount of salt,-dA/dt = Rin — R 0Uf, is
dA
i,
dt

A
— (% nr i n

r out

. ,
A q H- yTin
.r


dA
_
T o v t /t

or

,

Tout

,, +
dt

AT

Aq

,

i [Tin

Touf ) t

A

— ^H nX in

The volume of water in the tank at time t is V = Awh. The differential equation is then
d,h _


1 dV _

1 /

\

17

cAft f

V2g h .


Exercises 1.3 Differential Equations as Mathematical Models
{ 2 \~ 7r
Using Aft = 7T( ——) — — , Aw = 102 = 100, and g = 32. this becomes
12J
36
dt

100

450

14. The volume of water in the tank at time t is V = ^wr2h where r is the radius of the tank at hcig;.'
h. Prom the figure in the text we see that r/'h - 8/20 so that r = ‘l h and V = |tt (j J i) h =
Differentiating with respect to t, we have dVjdt = ^ n h 2 dh/dt or
dh
dt


25 dV
A-nh2 dt

From Problem 13 wc have dV/dt = —cA}ly/2gh where c = 0.6, .4/,. = tt

, and g = 32. Thu-

dV/dt = —2tt\//i/15 and
dh _ _25_ (
dt

2tr\/h.\_____ 5 _

4tt/j2 y

15 )

6/i3/2

15.
16.

By KirchhofFs second law we obtain R ^ + ~q

17.
18.

do
From Newton’s second law we obtain m — - —kv2 + mg.

dt
Sincc the barrel in Figure 1.3.16(b) in the text is submerged an additional y feet below its equilibrium

Since i = dq/dt and L d 2q/d,t2 + Rdq/dt = E(t), we obtain Ldi/dt + Ri = E(t).

= E(t).
*

position the number of cubic feet in the additional submerged portion is the volume of the circular
cylinder: 7rx (radius)2x height or ix{s/2)2y. Then we have from Archimedes’ principle
upward force of water on barrel = weight of water displaced
= (62.4) x (volume of water displaced)
= (62.4)-7r(6'/2)2jt/ = 15.67rs2y.
It then follows from Newton’s second law that
w d2u
,„ „ o
- - f = —15.67TS y
g dt1

or

d2y
15.67r,s2o
- £ + ----- £ y = 0,
dtr
w

where g = 32 and w is the weight of the barrel in pounds.

19.


The net force acting on the mass is
_
(f2x
,.
F = ma = m
= —k{s + x) + mg = —kx + mg — ks.
Since the condition of equilibrium is mg - ks, the differential equation is
c£2x
m d P = ~kX'

18


Exercises 1.3 Differential Equations as Mathematical Models
20. From Problem 19. without a damping force, the differential equation is rnd2x/dt 2 = —kx. W ith a
damping force proportional to velocity, the differential equation becomes
d2x
,
,.dx
rn —7T = —kx — p —
dt2
’ dt

d2x
dt/

or

Ax

dt

m ~37> + f t —

+ k'x = 0 .

21. From g — k /R 2 we find k = g li2. Using a = d2r/d,t2 and the fact that the positive direction is

upward wc get
___
k

cfr= _

or *5+1^ =a
d2r

gR2

i 1f

dt2

a

r2

-----------

gR?


— I—

----

r2

22. The gravitational force on m is F = —kMrm /r2. Since Mr = 4irSr^/3 and M = 47r5i ?3/3 wc have
M r = i:iM j R3 and
F = -k

Mrm
=

= -k

-k

m.M
r.
R*

Now from F = rria = d?7'/dt2 we have
d-r
, rnM
m —w = —k ——r- r
dt2
R*

or


d~r
—=•
dt2

kM
r.

dA
23. The differential equation is —- = k(M —A).
dt
dA
24. The differential equation is
= k i(M — A) — k^A.
dt
25. The differential equation is x'(t) = r — kx(t) whore k > 0.
26. By the Pvthagorcan Theorem the slope of the tangent line is y — ,—
27. We see from the figure that 29 + a = tt. Thus
V
2 tan 9
—- = tan a = tan(7r — 29) = —tan 2$ = ------ .
-x
v
;
1 — tan2 9
Sincc the slope of the tangent line is ?/ -tan 0 we have y/x = 2y'/[l —{yr)2]
or y —y(y')‘2 = 2xy', which is the quadratic equation y(y')'2 + 2xy' —y — i)
in y'. Using the quadratic formula, we get
f


—2 x ± ^4 x 2 + 4y2

—x ± ijx 2 + y2

2y

y

V

Since dy/dx > 0, the differential equation is
dy _ -x + ^ x 2 + y2
dx

or

y

dy
dx

.lie differential equation is dP/dt = kP, so from Problem 41 in Exercises 1.1, P ~ eki, and a
e-paramcter family of solutions is P = cekt.

19


Exercises 1.3 Differential Equations as Mathematical Models
29. The differential equation in (3) is dT/ dt = k(T — Tm). When the body is cooling, T > Tm, so
F


Tm > 0. Since T is decreasing, dT/dt < 0 and k < 0. When the body is warming. T < T m. so

T —Tm < 0. Since T is increasing. dT/dt > 0 and k < 0.
30. The differential equation in (8) is dA/dt — 6 —.4/100. If A(t) attains a maximum, then dA/dt = 0
at this time and A — 600. If A(t) continues to increase without reaching a maximum, then A'{t) > 0
for t > 0 and A cannot exceed 600. In this case, if A'(i) approaches 0 as t increases to infinity, we
see that A(t) approaches 600 as t increases to infinity.
31. This differential equation could describe a population that undergoes periodic fluctuations.
32. (a) As shown in Figure 1.3.22(b) in the text, the resultant of the reaction force of magnitude F
and the weight of magnitude mg of the particle is the ccntripctal force of magnitude muJ2x.
The centripetal force points to the center of the circle of radius x on which the particle rotates
about the y-axis. Comparing parts of similar triangles gives
F cos 9 — mg

and

F sin 6 = moj2x.

(b) Using the equations in part (a) we find
muj2x
mg

u>2x
g

33. Frorn Problem 21, d~r/dt2 — —gR?/r2. Since R is a constant, if r = R + s, then d?r/dt? = d2s/dt?
and, using a Taylor series, we get

Thus, for R much larger than s, the differential equation is approximated by cPs/dt2 = —g.

34. (a) If p is the mass density of the raindrop, then m — pV and

If dr/dt, is a constant, then dm/dt = kS where pdr/dt = k or dr/dt = k/p. Since the radius is
decreasing, k < 0. Solving dr/dt — k/p we get r = (k/p)t + co- Since r(0) = ro, co —
r = kt/p + ro.
(b) From Newton’s sccond law. -r[rmi\ = mg, where v is the velocity of the raindrop. Then
LL'L
dv
dm
rn — + v —— ~ mg
or
dt
dt
Dividing by 4p7rr3/3 we get
dv

3k

dv |

3k/p

and


Exercises 1.3 Differential Equations as Mathematical Models
35. We assume that the plow clears snow at a constant rate of k cubic miles per hour. Let t be the
time in hours after noon, x(t) the depth in miles of the snow at time t, and y(t) the distance the
plow has moved in t hours. Then dy/dt is the velocity of the plow and the assumption gives


dy

.

w x - = k,
where w is the width of the plow. Each side of this equation simply represents the volume of anow
plowed in one hour. Now let to be the number of hours before noon when it started snowing and
let s be the constant rate in miles per hour at which x increases. Then for t > —to, x = s(t + to).
The differential equation then becomes
dy _ k
1
dt
ws t + to
Integrating, we obtain
y = — [ln(t + io) + c]
ws
where c is a constant. Now when i = 0,y = 0 s o c = —Into and

y = i- ln ( l +f ) .
WS

\

to J

Finally, from the fact that when t — 1, y = 2 and when t = 2, y = 3, we obtain
2 \

2


IV
V1 + t0J

1 + t0)

Expanding and simplifying gives tg + to — 1 = 0. Since to > 0. we find to ~ 0.618 hours
37 minutes. Thus it started snowing at about 11:23 in the morning.
36. (1):

= kP is linear

dt
dT
(3): — = k(T - Tm) is linear

dA
(2): — = kA is linear
dt
dx
(•5): — = kx(n + 1 — a;) is nonlinear
dt

j y

(6):
(10):
(12):

dt


= k(a — X)(,3 — X ) is nonlinear
A-h

y/2gh is nonlinear

= —g is linear

dA

(8):
I 11):

l i



A

.

,

= 6 “ Too 18 Unear
+ R 'j-t + ^,'1 = E (t) is linear

dv
(14): m,—~ = mg — kv is linear
dt

d?s

. ds
. ..
(15): m-rrr + k— = mq is linear
'
dt2
dt
(16): linearity or nonlinearity is determined by the manner in which W and T\ involve x.

21


Chapter 1 in Review

Chapter 1 in Review
1 . 4- ci el0x = 10cie10x:
dx

!:“v•“‘
' c .........•':r~
“•

vf,7
r \
r”‘
5'::.........*
r‘j :v..*». ;f/

^ = 10y
ax


2. -y-(5 + cie~2x) = —2cie~2x = —2(5 + cie_2;C — 5);
dx
3. — (c\cos
dx

„t tr. -litJ? Si ..

. *

^ = -2{y - 5)
ax

or

^ = -2y + 10
ax

4-C2 sin A:.X') = —A;ci sin fcr + fcc? cos kx:

d2
9
(ci cos fcrc + C2 sin kx) = —k2c\cos kx — fc2C2 sin fcx = —k?{c\cos kx + 0 2 sin kx);
dx2

d2y

d%lJ , ,2

,2


n

*3 = - ^
or 5 ? + A:!' = 0
d
4. — (ci cosh A~;r + co sinh kx) ~ kci sinh kx + kca cosh kx:
dx
d2
(ci cosh fcc + C2 sinh kx) = k2c\cosh kx + k2c:-2 sinh kx = k2{c\cosh kx + C2 sinh kx);
dx2

5.

^ =k2y 01 ^ ~ k2y=0
y = c\ex + C2 xex;

y' — c\ex + C2 xex + C2 ex;

y" = c\ex + C2 xex + 2c2(?;

y" + y = 2(ciex + C2 xex) + 2c2ex = 2(ciex + C2 xex + C2 ex) = 2y';

y" —2yr + y = 0

6 . y' — —c\ex sin x + c\ex cos x + C2 &x cos x 4- C2 CXsin x;

y" = —c\ex cos x —c\ex sinx —c\ex sin x + c\ex cos x —&2 (tx sin x 4-C2 &x cos x 4-C2 ex cos x + C2 ex sin
= —2ciex sin x + 2 c2 ex cos x:

7.

13.
14.
15.
16.

y" — 2y' — —2ciex oosx — 2 c2 ex sinx = —2y;

y” —2y' + 2y = 0

a,d

10.

8. c

9. b

a,c

11.

b

12.

a,b;d

A few solutions are y = 0, y = c, and y = e1'.
Easy solutions to see are y = 0 and y = 3.
The slope of the tangent line at (x. y) is y'. so the differential equation is tj — x2 + y2.

The rate at which the slope changes is dy'fdx — y", so the differential equation is y" = —y' c
y” 4- y' = 0.

17.

(a) The domain is all real numbers.
(b) Since y' = 2j'ix1^ . the solution y = x2^ is undefined at x — 0. This function is a solution ■
the differential equation on (—oo,0) and also on (0, oo).

22


×