1.
|
This problem is easy with a calculator: ò05 |v(t)| dt = ò05 |t2
– .2t3| dt » 10.417 ft. Remember that the absolute value
function (abs) is found under 2nd CATALOG ENTER on your calculator, since abs
is the first function listed alphabetically.
However, make sure you can also do this problem without a calculator. First,
you must rewrite v(t) as t2(1 – .2t)
so that you can see that v(t) is a product of nonnegative factors
on [0, 5]. Why is this so important? You need to make sure that there are no
pesky sign changes to worry about.
Now apply FTC1 to find the answer. This is somewhat tedious, but it is like
eating your vegetables: you feel better afterward.
Since v(t) ³ 0 on [0, 5], ò05 |v(t)| dt = ò05 v(t) dt.
We evaluate as follows:
ò05 (t2 – .2t3) dt = (t3/3 – .2t4/4) |05
= 53/3 – .2(54)/4 – (0 – 0)
= 53/3 – (53)/4 = 53(⅓ – ¼) = 53(1/12)
= 125/12 ft.
|
|
|
4.
|
This is a standard “variable-factor”
problem that you can anticipate seeing on your test. The real world is
crawling with such problems, which is one of the main reasons for studying the
calculus in the first place. If density were uniform (as in Form II math and
science), we could simply multiply density times length to find the total
mass of the rod.
But, of course, density is varying here. The density function is not p but rather r (the Greek letter rho). We must assemble a Riemann
sum and then use our standard limiting trick to convert the Riemann sum to a
definite integral.
In most problems, density equals mass divided by volume. However, in this
problem, the rod has a certain mass per unit length (not per unit volume), and it is this quantity that we use
for density.
Since density = M/x if both M and x are fixed, we
know that density » DM/Dx even when both are changing, provided Dx is small. Therefore r(x) » DM/Dx.
At this point, some of you are saying, “It looks as if the density function, r(x), is
actually nothing more than M ¢, namely the derivative of M.” Well, you’re right!
By algebra, we can manipulate the equation r(x) » DM/Dx to get
DM » rDx
This is a very useful equation, and it has a real-world explanation: A little
chunk of mass (DM) approximately equals density times a little bit of length. We say
“approximately,” since if density is always changing as a function of x, there is no way we can make Dx small enough to avoid some fluctuation of density.
This is unavoidable, and we accept the small error that occurs. We need to
add up all the rDx values (Riemann-sum style) in order to approximate
the total value of M. We do this as
follows:
M » S (DM) = S (rDx)
Now, we apply the limiting process, the magical thing known as the definite
integral, and the “approximately equal” sign becomes a true equal sign:
M = ò□□ (dM) = ò02 (rdx).
Why did I use boxes as placeholders in the first definite integral? Answer:
because the limits for M are not
the same as the limits for x. I
don’t really care what the limits for M
are, but I have to show something
there to remind myself that I have a definite integral, not an indefinite
integral. This is a fine point; don’t worry too much about it.
Also, note that the density function r satisfies r(x) ³ 0 on [0, 2]. (It had better! After all, how could
we have negative density?)
For people who understand the previous discussion, it is OK to omit all of
the earlier stuff and start showing work only at this point:
M = ò02 (rdx) = ò02 (11 – 4x) dx = (11x – 2x2) |02
= 11(2) – 2(22) – (0 – 0) = 22 – 8 = 14 g.
|
|
|
5.
|
This problem also involves a variable-factor
product, and again, you should be able to work the entire problem without a
calculator. I will shorten the explanation below. If you have any uncertainty
at all, please reread #4 above and make sure that you understand every single
word, symbol, and punctuation mark in #4.
By inspection, E(t) ³ 300 on [0, 24]. Reason: Since the cosine of
anything cannot exceed 1, the quantity (2 – cos(blah blah blah)) must be
greater than or equal to 1. Therefore,
E(t) = 300(2 – cos(blah blah blah)) = (300 times something greater
than or equal to 1).
Therefore, E(t) ³ 0 on [0, 24], meaning that there are no sign changes to worry about.
Total power consumption = ò024 E(t) dt
= ò024 300(2
– cos(pt/12)) dt
= 300 ò024 (2 –
cos(pt/12)) dt
= 300 (2t – (12/p) sin(pt/12)) |024
= 300 (2·24 – (12/p) sin 2p – (0 – (12/p) sin 0))
= 300 (48 – 0 – (0 – 0))
= 300·48
= 14,400 kwh
|
|
|
10.
|
We did this one in class. Let there be two
functions of y, namely
x1(y) = (y2 –
4)/4
x2(y) = (y + 16)/4
You must plot these to see what is going on. Note that x1 is a parabola opening to the right, with vertex at
(–1, 0). If you have forgotten how to get that, please review your
Precalculus class notes or contact me. There is insufficient time to reteach
basic material like that in our class.
Note that x2 is a
straight line with slope 4, x-intercept
at (4, 0), and y-intercept at (0,
–16).
The two curves intersect where they both have the same values for x and y. The easiest way to find the points of intersection is to set 4x = 4x and therefore y2
– 4 = y + 16. By Algebra I (steps
omitted), y = –4 or y = 5.
Since x2 is always to
the right of x1 when y Î [–4, 5], our Riemann sum to find area must have as
its variable factor the difference x2
– x1. (Think of a number
line. Since x2 always
lies to the right of x1
for the interval of interest, x2
– x1 is a positive
quantity that tells us the width of the Riemann sum rectangles. The height is
always Dy, which
becomes dy in the integral.)
Area = ò–45 (x2 – x1) dy = 30.375
by calc. You should also be able to compute the answer by FTC1, as we did in
class on Thursday, 2/17/2005. (Please refer to your class notes.)
|
|
|
16.
|
Although this problem does not require a calculator,
it is certainly much easier if you use one. Let
y1 = 1 + cos x
y2 = 2 – cos x
and observe that for one of the larger “beads,” y2 is always the upper function. Consider the first
bead in Quadrant I, and use root finder or intersection finder to determine
the x-values of the left and right
bounds of the bead, namely a =
1.047... and b = 5.235…
You should also be able to find the exact values by algebra: a = p/3, b = 5p/3.
Note: I strongly recommend that you
use the calculator feature X®A ENTER after finding the first root and X®B ENTER after finding the second one. That way, you
need not write down all the digits, and you will be guaranteed to minimize
the roundoff errors. Click here for a 2-point
bonus.
Finally, area = òab (y2
– y1) dx » 7.653 by calc. You should also practice
solving the problem by FTC1, and you should prove that the exact answer
equals 4p/3 + 2Ö3.
For additional practice, do #15 and make sure you can get the answer given on
p. 702.
|
|
|
18.
|
Since we did this one in class, you should
already have it in your notes. A calculator is required for this problem. Let
the functions be y1 and y2, respectively, where y1 is the upper function.
By root finder or intersection finder, the x values of intersection are a
= –1.893... and b = 1.893...
(symmetric about y-axis since both
functions are even).
Area = òab (y1
– y2) dx » 5.731 by calc.
|