Experiment 13 - Declan Rogers
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Report for Experiment #13
Simple Harmonic Motion
Declan Rogers
Lab Partner:
Aidan Kaneshiro
TA:
Zhuyao Wang
5-12-22
Abstract
This experiment examined harmonic motion. The experiment was done with a glider attached
to two springs on opposite ends while sitting on a track that produced an air buffer between it and the glider. The oscillation was examined with no motion to determine the equilibrium position and then it was observed with no added forces as it oscillated to determine a control motion for the glider. Then there were three trials with increasing weight added by two magnets to observe the effect that added weight had on the motion and in what manner it changed as the weight increased. Following all four trials it was determined that the period increased with the number of magnets attached. This result supports the theory that an increase in weight of an object in harmonic motion will directly decrease the period of motion of that onject.
Introduction
This experiment analyzed simple harmonic motion in the real world. In most instances of motion in the real world, friction is also involved and can be quantified. However, this experiment attempted to demonstrate simple harmonic motion uninhibited by outside factors like
friction. To this end, the glider, to which the springs of the experiment are attached, is set upon an air track to create a separation between the surfaces and ensuring that there is no dry friction present. This glider would oscillate along the track due to the two springs and data based on this oscillation was recorded. Then the weight of the glider was increased in increments of two magnets while repeating the oscillation and data collection. This was continued until trials had been completed for no magnets, two magnets, four magnets, and six magnets. Although the friction was limited, the data returned indicated that there was still a certain resistance to the motion of the glider, likely caused by the magnetic field of the magnets which create an electric field and attracts the track which is made of metal. The intention of the experiment was to quantify this resistance and correlate it to the magnetism of the magnets, ensuring that the simple
harmonic motion, at its base, performed as theoretically expected. The data collected was used to
create multiple graphs to observe the amplitude of oscillation and the compare it to the height of each peak recorded by the ultrasonic sensor. An exponential relationship between the ultrasound distance data and the amplitude of the oscillation.
Investigation 1
The first investigation focuses on simple harmonic motion without external factors, setting the control for the overall experiment. Data is recorded while the glider is in stasis and when it is pulled to the 40 cm location along the track.
To setup this investigation, first take the mass of the glider with the digital scale. Take down this value on a spreadsheet. Activate the air in the track so that the valve is three quarters open. Next ensure that the glider does not move along the track by balancing out the end with the screw lifting or lowering the track. Connect the PASPort USB to the computer and ensure that it is also connected to the ultrasonic motion sensor. Open the PASCO Capstone application on the computer and open the table and graph option. Create one column that records the position in meters and one column that records the time in seconds. Then, select the hardware setup and ensure that the sensor is set to Hz. Move the glider right in front of the sensor and turn the sensor
until it is facing the glider perfectly by turning the knob on the side.
Once the main setup has begun, attach the springs to the glider. One should be fastened to each side of the glider and then to their respective ends of the track. Ensure that all collected values are to the thousandths place. The first trial will document the state of equilibrium. Leave the glider as is and run the PASCO Capstone application for thirty seconds. Copy the table of
data into a separate spreadsheet. Then, pull the glider to the 40 cm location and begin the PASCO
Capstone application upon release. Once again, allow the program to run for 30 seconds and then
copy the data table into the separate spreadsheet. Ensure that error has been calculated for each trial
Table 1: Mass of the glider with error
mass of glider (kg)
δ
mass
δ
mass/mas
s
0.38360
0.0000
5
0.00013
The absolute error of the mass of the glider is 0.00005 kg because that is half of the minimum measurement gathered by the scale, 0.0001 kg. The equation below is then used to determine the propagated error in mass:
Equation 1:
δmass
mass
The average position was found by averaging the 614 data points collected in the equilibrium
test run with the equation below, each x a position value and n being the number of values, 614. The average was found to be 0.603 m.
Equation 2: x
1
+
x
2
+
...
+
x
n
n
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This average was utilized against the second trial points to graph the gliders position in relation to its equilibrium rather than in relation to the location of the sensor as the program collects. The graph below shows this relationship.
Object 7
Fig. 1: Position vs Time of the glider in relation to its equilibrium position
Through this graph the amplitude, phase angle, and period were determined and recorded in the table below:
Table 2: Estimated Amplitude, Period, and Phase Angle
A (m)
0.20
period (s)
2.60
phase ϕ
-0.99
Both the amplitude and the period can be found by analyzing the first peak of the graph and then put into the equation below to determine the phase angle:
Equation 3:
x
−
x
0
=
Acos
(
ϕ
)
Then, utilizing these estimated values, the frequency, angular frequency, spring constant, and actual phase angle can be determined.
Table 3: Frequency calculated using estimated data (with respective errors)
f (s)
δf
δf/f
0.3840
0.6232
1.6248
The frequency is found by calculating the reciprocal of the period:
Equation 4:
1
T
The propagated error can then be found using the absolute error in frequency of 0.6232 in the
following equation:
Equation 5:
δf
f
Table 4: Angular Frequency calculated with error
ω (s)
δω
δω/ω
2.4100
0.6232
0.2586
Angular frequency is determined using the frequency multiplied by 2
π
Equation 6:
f
=
ω
2
π
Then the propagated error in angular frequency can be found in the same way that it was found for frequency, using the equation below:
Equation 7:
δω
ω
Table 5: Phase Angle calculated with error
ϕ
(Degrees)
δ
ϕ
δ /
ϕ ϕ
-2.4100
-0.6232
0.2586
As the phase angle is inversely related to the angular frequency it can be found with Equation
8:
Equation 8:
ω
=−
ϕ
Likewise, the propogated error in phase can be found in the same manner as the frequency and angular frequency:
Equation 10:
δ
ϕ
ϕ
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Table 6: Spring Constant calculated with error
K (N/m)
δk
δk/k
2.2280
0.5761
0.2586
The spring constant is determined using the mass of the glider and the angular frequency in the manner shown below:
Equation 11:
ω
2
m
glider
Then the propagated error of the spring constant is then found with Equation 12:
Equation 12:
√
(
δω
ω
)
2
+
(
δ m
glider
m
glider
)
2
Then the absolute error of the spring constant is found with the expression below:
Equation 13:
δk
∗
k
Then the visualization of the linear decay in the motion as it approaches equilibrium is done via graphing. This included each peak plotted against the time at each peak which was recorded in Table 7.
Table 7: Each numbered peak and the time at that peak:
Peak
Time (s)
δ period
1
1.00
0.0005
2
3.65
0.0005
3
6.25
0.0005
4
8.85
0.0005
5
11.45
0.0005
6
14.05
0.0005
0
1
2
3
4
5
6
7
0.00
2.00
4.00
6.00
8.00
10.00
12.00
14.00
16.00
f(x) = 2.61 x − 1.58
R² = 1
Time (s) vs. Peak Number
Peak number
Time (s)
Fig. 2: Time (s) vs Peak Number Fig. 3: IPL Straight Line Fit Calculator
This graph displays the linear relationship between the peak number and each peak’s time. The slope of this graph is shown to be the period found in Table 2. The y-intercept of the graph is
then representative of the starting period. The IPL calculator also proves that there is very little error in the determined results. The period was calculated to be 2.6071 s and is thus within the bounds of 0.6232 s within 2.6041 s given by the IPL calculator. Similarly, the y-intercept is -1.5833, within the allowance of 2.4271 s of -1.5833 s.
Then with the period found by the graph, the frequency, angular frequency, and phase angle were calculated. Each of these were then used to calculate the spring constant which was finally determined to be 3.3380 N/m, incredibly close to the theoretical value of 2.2000 N/m.
Investigation 2
Much of the setup for the second investigation is identical to the first. Ensure that the track is still level with the screw at the end and that the sensor has not been moved. Open the PASCO Capstone again and select the graph and table function once more. Open the hardware setup and set it to 20 Hz. Following this, attach the two springs to the glider and make sure that it is stable.
Once the setup is complete, investigation two can begin. This investigation will focus on the manipulation of the mass of the glider and how it affects the nature of simple harmonic motion. To begin, find the mass of two magnets with a buffer to ensure the magnetic field doesn’t change
the reading. Then place a magnet on either side of the glider and pull the glider to the 40 cm location on the track. Release the glider and begin the PASCO Capstone program at the same time to record the position data for thirty seconds. Then copy the table of positions and times into
a separate spreadsheet. Repeat this testing process for four total magnets and then six total magnets. You should have three trials by the end of this investigation for each increment of magnets. Table 8: Mass of magnet with error
mass of magnet
(kg)
δ mass
δ mass/mass
0.0111
0.00005
0.00450450
5
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With the absolute error of the mass of 0.00005 kg, the propagated error is determined with the equation below:
Equation 14:
δ m
magnet
m
magnet
From the data of the program ran for each trial as well as the data gathered in the first investigation and the equilibrium point, the following graph was produced:
Fig. 4: Position vs. Time graph of all three trials and control trial centered about equilibrium
point
With this graph a table with each of the peaks and their times can be found alongside the error
Table 9: Peaks and their times for two magnets with error
Peak
Time (s)
δ period
δT/T
1
1.10000
0.00050
0.00046
2
3.75000
0.00050
0.00013
3
6.40000
0.00050
0.00008
4
9.10000
0.00050
0.00005
5
11.8000
0.00050
0.00004
6
14.5000
0.00050
0.00003
Table 10: Peaks and their times for four magnets with error
Peak
Time (s)
δ period
δT/T
1
2.50000
0.00050
0.00020
2
5.20000
0.00050
0.00010
3
8.00000
0.00050
0.00006
4
10.7500
0.00050
0.00005
5
13.4500
0.00050
0.00004
6
16.2000
0.00050
0.00003
Table 11: Peaks and their times for six magnets with error
Peak
Time (s)
δ period
δT/T
1
2.60000
0.00050
0.00019
2
5.45000
0.00050
0.00009
3
8.25000
0.00050
0.00006
4
11.0500
0.00050
0.00005
5
13.9000
0.00050
0.00004
6
16.6000
0.00050
0.00003
As the absolute error of time is 0.00050, the propagated error is found with Equation 15. Equation 15:
δT
T
As in the first investigation, each previous table can be graphed to find the relationship between the peak number and its time.
0
1
2
3
4
5
6
7
8
0.00
2.00
4.00
6.00
8.00
10.00
12.00
f(x) = 0
R² = 0
Time (s) vs. Peak Number
Peak Number
Time (s)
Fig. 5: Time vs. Peak Number graph for two magnets
Fig. 6: IPL straight line fit calculator for two magnets
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0
1
2
3
4
5
6
7
0.00
2.00
4.00
6.00
8.00
10.00
12.00
14.00
16.00
18.00
f(x) = 2.74 x − 0.25
R² = 1
Time vs. Peak Number
Peak Number
Time (s)
Fig. 7: Time vs. Peak Number graph for four magnets
Fig. 8: IPL straight line fit calculator for four magnets
0
1
2
3
4
5
6
7
0.00
2.00
4.00
6.00
8.00
10.00
12.00
14.00
16.00
18.00
f(x) = 2.8 x − 0.17
R² = 1
Time vs. Peak Number
Peak Number
Time (s)
Fig. 9: Time vs. Peak Number graph for six magnets
Fig. 10: IPL straight line fit calculator for six magnets
With each of the graphs and the IPL straight line fit calculation that follows, it is shown that most of the data is without error. The first trial has a slope of 2.6814 s with a y-intercept of -1.6100 s, as compared to the IPL values of 2.6814 ± 0.6410s and -1.6100 ± 2.4962s. The second
trial has a slope of 2.7429 s with a y-intercept of -0.2500 s, as compared to the IPL values of 2.7429 ± 0.6557s and -0.2500 ± 2.5534s. In the final trial the slope is 2.8043 s with a y-intercept of -0.1733 s, as compared to the IPL values of 2.8043 ± 0.6704s and -0.1733 ± 2.6107s. As is evident, each of the calculated values falls withing the range of each respective IPL error and is consistent with what is expected of the experiment. The data from the fourth figure was then used to produce a table with each peak and the amplitude at that point for each trial of investigation two.
Table 12: Peaks and amplitudes for two magnets with error
Peak
A (m)
δA
δA/A
1
0.2060
0.0005
0.0024
2
0.1780
0.0005
0.0028
3
0.1480
0.0005
0.0034
4
0.1250
0.0005
0.0040
5
0.1060
0.0005
0.0047
6
0.0840
0.0005
0.0060
Table 13: Peaks and amplitudes for four magnets with error
Peak
A (m)
δA
δA/A
1
0.1720
0.0005
0.0029
2
0.1350
0.0005
0.0037
3
0.1020
0.0005
0.0049
4
0.0760
0.0005
0.0066
5
0.0610
0.0005
0.0082
6
0.0460
0.0005
0.0109
Table 14: Peaks and amplitudes for six magnets with error
Peak
A (m)
δA
δA/A
1
0.1560
0.0005
0.0032
2
0.1140
0.0005
0.0044
3
0.0800
0.0005
0.0063
4
0.0570
0.0005
0.0088
5
0.0380
0.0005
0.0132
6
0.0240
0.0005
0.0208
As the absolute error of the amplitude is 0.0005m, the propagated error is determined with Equation 16.
Equation 16:
δA
A
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Each preceding table and its data was then used to produce a graph with a visual on the relationship between amplitude and peak.
0
1
2
3
4
5
6
7
0.000
0.050
0.100
0.150
0.200
0.250
f(x) = 0.25 exp( − 0.18 x )
R² = 1
Amplitude (m) vs. Peak Number
Peak Numbers
Amplitude (m)
Fig. 11: Amplitude vs. Peak Number graph for two magnets
0
1
2
3
4
5
6
7
0.000
0.020
0.040
0.060
0.080
0.100
0.120
0.140
0.160
0.180
0.200
f(x) = 0.23 exp( − 0.26 x )
R² = 1
Amplitude (m) vs. Peak
Peak Number
Amplitude (m)
Fig. 12: Amplitude vs. Peak Number graph for four magnets
0
1
2
3
4
5
6
7
0.000
0.020
0.040
0.060
0.080
0.100
0.120
0.140
0.160
0.180
f(x) = 0.24 exp( − 0.37 x )
R² = 1
Amplitude (m) vs. Peak
Peak Number
Amplitude (m)
Fig. 13: Amplitude vs. Peak Number graph for six magnets
These graphs show that there is an exponential relationship between the amplitude and peak number in simple harmonic motion. With this data the b value can be determined by observing the decay constant of each graph and plugging it into Equation 17: Equation 17:
α
=
b
2
m
magnet
With the b values of each trial and the magnet number of each trial, the following table was produced:
Table 15: Number of magnets and corresponding b value
number of
magnets
b
2
0.00392
9
4
0.02353
2
6
0.04941
7
Then a graph of this data can be made to display the relationship between magnets and b value:
1.5
2
2.5
3
3.5
4
4.5
5
5.5
6
6.5
0
0.01
0.02
0.03
0.04
0.05
0.06
f(x) = 0.01 x − 0.02
R² = 0.99
b vs. number of magnets
number of magnets
b
Fig. 14: b vs. Number of Magnets
This graph visualizes that the be value and the number of magnets have a linear relationship, therefore the b value is directly proportional to the weight of the glider.
This culminates in the calculation of the period of each trial using the data up until this point
Table 16: number of magnets and their T’ values
number of
magnets
T'
2
2.69851
9
4
2.77154
8
6
2.84318
5
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The T’ values were found using the b value, the spring constant, and the total mass of each trial. All of these variables were compiled into Equation 18 to find the T’ values for every trial with its respective data.
Equation 18:
2
π
√
(
k
m
)
−
(
b
2
4
m
2
)
The T’ values that were calculated can be compared to the T values directly from the data. The slope the graph with time versus the peak can be compared to the T’ in that trial as shown in Table 16. In the two-magnet trial the T was 2.6814 seconds and the T’ was 2.6985 seconds. In the
four-magnet trial the T was 2.7429 seconds and the T’ was 2.7715 seconds. In the six-magnet trial the T was 2.8043 seconds and the T’ was 2.8432 seconds. Each measured period is incredibly close to the following calculated value, both sets of data showing that increases in the mass of the glider results in increases in the period.
Conclusion
This experiment included finding the equilibrium of the glider connected to two springs and then the behavior of its oscillation with no added weight, followed by adding increments of two magnets to the weight for three added trials. The overall purpose was to determine the effect that added weight on the glider had on its motion. The first trial consisted of finding the position of equilibrium as well as the control trial with zero added magnets. Then the second trial had the three trials including added weight, with two, four, and six magnets respectively. The distance was measured with an ultrasonic sensor and then this data was used to calculate the period of each trial and determine the impact that the added magnets had on the simple harmonic motion.
The first investigation found the spring constant of 2.228 N/m which is incredibly close to the theoretical value of 2.200 N/m. This comparison was necessary to determine the basis of the following trials would be compared to a control that performed correctly. The second investigation found the different periods of the added weights through a time versus peaks graph.
The experimental period was found and then compared to the period found through the slope. For the two magnets the T was 2.6814s and the T’ was 2.6985s, for the four magnets the T was 2.7429s and the T’ was 2.7715s, and for the six magnets the T was 2.8043s and the T’ was 2.8432s. Each of these pairs of periods were very close to one another, signifying a limited error
in the overall experiment. As the weight of the glider increased, the period increased proportionally, supporting the idea that the magnets had a dampening effect on the glider’s motion.
Despite the extremely limited error, the experiment overall could be improved to close the small gaps. The major area where human error was allowed was during the release of the glider. The timing of the PASCO program was done by the human experimenter and allowed for some delay in the time between beginning the program and releasing the glider, adding a discrepancy to the data. With a synchronized release system the program could be activated the moment the glider was let go for near perfect data. Questions
1.
The period would increase by the square root of two as it is inversely proportional to the frequency which is in turn inversely proportional to the square root of the mass.
2.
The force is proportional to the velocity, therefore the point at which the kinetic energy is highest is where the greatest friction is located. The position with the highest kinetic energy is as the glider is speeding past the equilibrium point.
3.
In the first complete oscillation, there should be no friction force on the glider with no magnets as it is floating on an air track.
4.
The friction does not impact the magnitude of frequency as it is not part of the equations for k/m or the α
2
.
5.
The glider would not move as the decay constant would be greater than the angular frequency if α were greater than ω.
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