Solucionario Ecuaciones Diferenciales
Chapter One
Section 1.1
1.
For C "Þ& , the slopes are negative, and hence the solutions decrease. For C "Þ& , the
slopes are positive, and hence the solutions increase. The equilibrium solution appears to
be Ca>b œ "Þ& , to which all other solutions converge.
3.
For C "Þ& , the slopes are :9=3tive, and hence the solutions increase.For C "Þ&
, the slopes are negative, and hence the solutions decrease. All solutions appear to
diverge away from the equilibrium solution Ca>b œ "Þ& .
5.
For C "Î# , the slopes are :9=3tive, and hence the solutions increase. For
C "Î# , the slopes are negative, and hence the solutions decrease. All solutions
diverge away from________________________________________________________________________
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the equilibrium solution Ca>b œ "Î# .
6.
For C # , the slopes are :9=3tive, and hence the solutions increase. For C # ,
the slopes are negative, and hence the solutions decrease. All solutions diverge away
from
the equilibrium solution Ca>b œ # .
8. For all solutions to approach the equilibrium solutionCa>b œ #Î$ , we must have
C w ! for C #Î$ , and C w ! for C #Î$ . The required rates are satisfied by the
differential equation C w œ # $C .
9. For solutions other than Ca>b œ # to diverge from C œ # , C a>b must be an increasing
function for C # , and a decreasing function for C # . The simplest differential
equation
whose solutions satisfy these criteria is C w œ C # .10. For solutions other than Ca>b œ "Î$ to diverge from C œ "Î$ , we must have C w !
for C "Î$ , and C w ! for C "Î$ . The required rates are satisfied by the differential
equation C w œ $C " .
12.
Note that C w œ ! for C œ ! and C œ & . The two equilibrium solutions are C a>b œ ! and
Ca>b œ & . Based on the direction field, C w ! for C & ; thus solutions with initial
valuesgreater than & diverge from the solution Ca>b œ & . For ! C &, the slopes are
negative, and hence solutions with initial values between ! and & all decrease toward the
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solution Ca>b œ ! . For C ! , the slopes are all positive; thus solutions with initial
valuesless than ! approach the solution Ca>b œ ! .
14.
Observe that C w œ ! for C œ ! and C œ # . The two equilibrium solutions are C a>b œ !
and Ca>b œ # . Based on the direction field, C w ! for C # ; thus solutions with initial
values greater than # diverge from Ca>b œ # . For ! C #, the slopes are also
positive, and hence solutions with initial values between ! and # all increasetoward the
solution
Ca>b œ # . For C ! , the slopes are all negative; thus solutions with initial
values less than ! diverge from the solution Ca>b œ ! .
16. a+b Let Q a>b be the total amount of the drug ain milligramsb in the patient's body at
any
given time > a2
a71Î2b œ > $ is a solution.
20.
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All solutions approach the equilibrium solution Ca>b œ ! Þ
23.
All solutions appear to diverge from the sinusoid Ca>b œ
$
È#
=38Ð> 1 Ñ " ,
%
which is also a solution corresponding to the initial value Ca!b œ &Î# .
25.
All solutions appear to converge to Ca>b œ ! . First, the rate of change is small. The
slopes
eventually increasevery rapidly in magnitude.
26.
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The direction field is rather complicated. Nevertheless, the collection of points at which
the slope field is zero, is given by the implicit equation C$ 'C œ #># Þ The graph of
these points is shown below:
The y-intercepts...
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