(Q-1) |
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(Q-2)
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(Q-3)
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Computation of k from the graph: The uncertainties in x’ and the
hanging masses M should be very small . Thus, the precision of your value of k will be limited
by the graphing process. Thus, you can proceed without using error bars . Since the uncertainties in ΔFs
and Δx’ are so small, the precision is limited by the drawing
process. In this case, you can compute the uncertainty in the slope k like
this:
Δk = lcy/ Δx’, where lcy is the least count of the grid for the y (Fs)
axis and Δx’ is the base of the slope of the triangle used to find kbest .
From what we have discussed in class, your drawing in the y-direction
should have every 20 small divisions be equal to 1.0 (N) . Thus,
each small division in the y direction equals 0.05 (N). This number, in
combination with the base of the triangle Δx’, will give you
Δk= lcy/ Δx’. See the previous
paragraph.
The horizontal scale has 20 small division equaling 0.1000 m. Thus, one
small horizontal unit equals 0.005 (N).
Follow the steps in the hand out while graphing; I am skipping the
beginning steps on errors bars given the expected good precision. See page 59,
Step 4. Try to make a small circle around each point, two or three mm in
diameter, centered at the dot. Since there are no expected error bars you
could skip to 60, Graphical Slopes . (See fig. 5.4--Getting the best slope.)
Step 6 emphasizes not trying to make the line pass through any particular point,
though if the points line up well, it may be difficult avoiding going through
many or all the points. Remember to extend the line beyond the data points
to the left and right. (Step 6. c. ). In Step 7, you read about determining a
right triangle, called the slope triangle. Here is how you draw: Choose two
points on the graph, indicating them with arrows approximately spanning
the domain of the data. The slope equals the rise/run.
a. Here are guidelines for the run . The run should begin and end on
major vertical grid lines. for example 0.5000 m and 1.0000 m marks. The run
should be rather wide, about as wide as the domain, as in the above
mentioned choice of vertical major gridlines for the run.
d. Show the beginning and ending values of x and y,
in this case x' and Fs , that you read at the two arrows.
Substitute these values into your expression for the slope = rise/
run. Note that a point has an inherent ( "simple") uncertainty
(1/4)*(0.005) = 0.00125 = 0.001 to one sig. fig in the x direction and
(1/4)*(0.05) = 0.0125= 0.01 to one sig . fig. in the y direction. What
this basically means is that you are rounding to the nearest small
division. Include units. Do not round off since you will be using
the slope k in intermediate computations. Here is what I
report for the above sample data.
kBEST = (4.80 - 0.80)/(0.900 - 0.500) = 4.00 (N)/
0.400 (m) = 10.0 N/m.
We might as well compute the uncertainty in k =
Δk= lcy/ Δx’ = 0.0125/0.400 = 0.03125. We
will use that under (Q-5) for the uncertainty in theoretical T.
(Q-4)
masses related to total mass m | |
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Note that the uncertainty in each measurement is considered
to be 1 g. Thus Δms = 1 g and Δmo =
1 g. Since m = msEFF + mo, Δm
= 1g + 1 g/3 = 1.33333 g = 1 g if rounded to one sig. fig.
CORRECTIVE NOTE: This last conclusion may be an overestimation and lead to
conceptual inconsistencies since you used a mass scale which has a smaller
uncertainty than 1 g. In the centripetal force lab, we said the
uncertainty in mass scale measurements is (1/4)*(0.1 g) = 0.025 g = 0.03
if rounded. So a better approximation would be Δm = 0.025 +
0.025/3 = 0.03333 = 0.03 g if rounded down. This dovetails with the
1/100th place precision of the mass.
(Q-5)
We are now in the position
to find the theoretical period given by formula (1):
T =
2π· (1)
or T2 = 4*pi2*(0.357 kg/10.0
N/m).
This leads to TTH_BEST = 1.18717 seconds, where the underlined
8 indicates there are only three sig. figs. Now we have a
"benchmark"
for the experimental value of T which I am about to compute; see below.
Before we address the direct measurement of T , let's find the uncertainty in
the theoretical value ΔTTH given by formula
under (Q-2):
(1.18717)*( 1.3333/714.700
+ 0.03125/20.0) = (1.18717)*( 0.000186554
+ 0.0015625) = (1.18717)*( 0.00342804)
= 0.0040697 = 0.004 if rounded down to one sig.
fig.
If you use the more accurate condition of 0.025 g for the uncertainty, we
get:
(1.18717)*( 0.0333/714.700
+ 0.03125/20.0) = (1.18717)*( 0.00004663865546
+ 0.0015625) = (1.18717)*( 0.001609138655)
= 0.001910321138 = 0.002 if rounded down to one sig. fig.
These errors seem inconsistent with the precision of the reported average
TTH_BEST = 1.18717 seconds, which is precise only to the 1/100
th place. It is impossible for the third decimal place (1/1000th place) in
the uncertainty to be meaningful (as in 0.004 or 0.002) when the
average period TTH_BEST is precise to only the 1/100th
place. Thus, one might conclude that the error is "zero."
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Note that in this case, since the uncertainty is 0.01
s rounded to the 1/100th place and the average period is precise to the
1/100,000th place, then
you would report the answer by rounding down the average to the same place: TEX
= 1.18 (s) +/-0.01 (s). Note that this is very different from the previous
example where the precision of the average ("best") was less than
that of the uncertainty, in which case the uncertainty is taken as
"zero."
(Q-6)
Now check the discrepancy.
|TEX – TTH| < 2(ΔTEX + ΔTTH),
| 1.181958 - 1.18717 | < 2*| 0.011404 + 0| = 0.022808
Now, the left hand side is zero since 1.181958 - 1.18717 = -
0.005213 = 0. Thus we can conclude that the theoretical period
equals the measured experimental period.