(b) If and , find the rate of change of
intensity with respect to depth at a depth of 20 m.
(c) Using the values from part (b), find the average light
intensity between the surface and a depth of 20 m.
;
61. The flash unit on a camera operates by storing charge on a
capacitor and releasing it suddenly when the flash is set off.
The following data describe the charge remaining on the
capacitor (measured in microcoulombs, )C) at time (mea-
sured in seconds).
(a) Use a graphing calculator or computer to find an expo-
nential model for the charge.
(b) The derivative represents the electric current (mea-
sured in microamperes, )A) flowing from the capacitor to
the flash bulb. Use part (a) to estimate the current when
s. Compare with the result of Example 2 in
Section 2.1.
;
62. The table gives the US population from 1790 to 1860.
(a) Use a graphing calculator or computer to fit an exponen-
tial function to the data. Graph the data points and the
exponential model. How good is the fit?
(b) Estimate the rates of population growth in 1800 and 1850
by averaging slopes of secant lines.
(c) Use the exponential model in part (a) to estimate the rates
of growth in 1800 and 1850. Compare these estimates
with the ones in part (b).
(d) Use the exponential model to predict the population in
1870. Compare with the actual population of 38,558,000.
Can you explain the discrepancy?
63. Prove the second law of exponents [see (3)].
64. Prove the fourth law of exponents [see (3)].
65. Deduce the following laws of logarithms from (3):
(a)
(b)
(c)
66. Show that for any .
x ' 0lim
n l !
!
1 "
x
n
"
n
! e
x
log
a
$x
y
% ! y log
a
x
log
a
$x#y% ! log
a
x $ log
a
y
log
a
$xy% ! log
a
x " log
a
y
t ! 0.04
Q#$t%
t
Q
a ! 0.38I
0
! 8
;
44. If , find . Check that your answer is reason-
able by comparing the graphs of and .
45–50 Evaluate the integral.
46.
47. 48.
50.
51. Find the area of the region bounded by the curves ,
, , and .
52. The region under the curve from to is
rotated about the -axis. Find the volume of the resulting
solid.
;
53. Use a graph to find the root of the equation cor-
rect to one decimal place. Then use this estimate as the initial
approximation in Newton’s method to find the root correct to
six decimal places.
Find if .
55. Find the inverse function of .
56. Calculate .
57. The geologist C. F. Richter defined the magnitude of an
earthquake to be , where is the intensity of the
quake (measured by the amplitude of a seismograph 100 km
from the epicenter) and is the intensity of a “standard”
earthquake (where the amplitude is only 1 micron cm).
The 1989 Loma Prieta earthquake that shook San Francisco
had a magnitude of 7.1 on the Richter scale. The 1906 San
Francisco earthquake was 16 times as intense. What was its
magnitude on the Richter scale?
58. A sound so faint that it can just be heard has intensity
watt#m at a frequency of 1000 hertz (Hz). The
loudness, in decibels (dB), of a sound with intensity is then
defined to be . Amplified rock music is
measured at 120 dB, whereas the noise from a motor-driven
lawn mower is measured at 106 dB. Find the ratio of the
intensity of the rock music to that of the mower.
59. Referring to Exercise 58, find the rate of change of the loud-
ness with respect to the intensity when the sound is measured
at 50 dB (the level of ordinary conversation).
60. According to the Beer-Lambert Law, the light intensity at a
depth of meters below the surface of the ocean is
, where is the light intensity at the surface and
is a constant such that .
(a) Express the rate of change of with respect to in
terms of .
I$x%
xI$x%
0
(
a
(
1
aI
0
I$x% ! I
0
a
x
x
L ! 10 log
10
$I#I
0
%
I
2
I
0
! 10
$12
! 10
$4
S
Ilog
10
$I#S %
lim
x l !
x
$ln x
f $x% ! log
10
!
1 "
1
x
"
x
y
! y
x
y#
54.
2
x
! 1 " 3
$x
x
x ! 1x ! 0y ! 10
$x
x ! 1x ! $1y ! 5
x
y ! 2
x
y
2
x
2
x
" 1
dx
y
3
sin
&
cos
&
d
&
49.
y
x2
x
2
dx
y
log
10
x
x
dx
y
$x
5
" 5
x
% dx
y
2
1
10
t
dt
45.
f #f
f #$x%f $x% ! x
cos x
446
|| ||
CHAPTER 7 INVERSE FUNCTIONS
t 0.00 0.02 0.04 0.06 0.08 0.10
Q 100.00 81.87 67.03 54.88 44.93 36.76
Year Population Year Population
1790 3,929,000 1830 12,861,000
1800 5,308,000 1840 17,063,000
1810 7,240,000 1850 23,192,000
1820 9,639,000 1860 31,443,000