Physics307L F07:People/Le/FormalFin

Discovering the Fundamental Charge and Investigating Quantized Amounts of Charge Using the Milikan Oil Drop Experiment

Linh Le, Cary Dougherty

Physics and Astronomy Department, Junior Lab 307, University of New Mexico, Albuquerque, New Mexico

Email: linhle@unm.edu

Abstract

To explain the connection between electricity and matter, scientists in the late 19th century argued there had to be a fundamental unit of electricity. To find this fundamental unit, we repeated Robert Millikan's famous Oil-Drop Experiment. The Millikan Oil drop experiment is the product of other attempts. The Millikan experiment was best at determining the charge of an electron, and showing the quantized nature of these charges.

To repeat Millikan we sprayed oil droplets into a capacitor and then ionized the droplets to give them excess electrons. We then exposed these droplets to a constant electric field. Measuring the fall time of the droplets without the field, then measuring the rise time with the field on, we were able to compare the force of gravity pulling down on the droplets to the force of the electric field causing them to rise. In doing so, we were able to get a fundamental charge of [math]\displaystyle{ (1.5193+/-0.07)x 10^{-19} coulombs }[/math], very close to the accepted value of [math]\displaystyle{ 1.60217733x10^{-19} }[/math] Coulombs.

Introduction

There have been many attempts by many different people to measure the charge of an electron. The first notable was Townsend. Townsend was the first to show that some of the gases created by electrolyzing sulphuric acid came out charged. He then bubbled these gases through water, then through sulphuric acid to dry them. He assumed that the charged ions collected water molecules around them. He measured the rate of fall of the water droplets to find their mass and used Stoke's Law to find the volume. Bubbling the gas through the acid dried up the water. The drying of the water causes the excess charge to collect in the air molecules, which were then passed into drying tubes, then weighed. He divided the weight of the gas cloud by the average weight of the water to find the amount of excess charge, then divided that by the volume of the droplets to find the amount of charge per ion.(3)

The next notable experiment was done by J.J Thompson, which closely resembled Townsend's work. Instead of measuring a gas, Thompson ionized particles using an X-ray tube. He then took this ionized gas and ran it through a small voltage to find the charge per cubic centimeter of the gas. Thompson then allowed the gas to enter a pistoned chamber, which he then expanded the gas to allow it to cool and collect water droplets. Mimicking Townsend, Thompson calculated fall times to get the mass and size of the droplets. (3)

Both Townsend and Thompson had some fundamental flaws in their experiments, namely, not accounting for evaporation in the droplets as they fell, and assuming the number of droplets was equal to the amount of charged ions. H.A Wilson had a solution for this problem. Wilson took Thompson's experiment, but placed 2 charged plates in the "falling chamber". By comparing the velocities with the field on and with the field off, in a short distance, he eliminated a great deal of uncertainty in the amount of charge and the evaporation.(3)

With these experiments under our belt, we now follow in Millikan's footsteps in recreating his famous Oil Drop experiment. Since evaporation was such a topic of uncertainty, we, as Millikan proposed, use an electric field strong enough to not just slow the fall of these particles, but to suspend them or cause them to rise. The ionized droplets, in this case oil since it does not evaporate as easily as water, are observed through a microscope. This method is a huge improvement since we can observe individual droplets, rather than a statistical overview of many.

Methods and Materials

Fig 1)A picture of the equipment used for the experiment(Photo taken in the lab by Antonio Rivera)

Fig 2) A basic drawing of the apparatus taken from the PASCO manual. The round cylinder in the middle is the capacitor, to the left of it is the thermistor, behind it is the light source, in front of it is the microscope and off to the right is the switch to change polarities.

Fig 3) Close up diagram of the apparatus(taken from the PASCO manual)

Fig 4) Rough schematic of our (taken from the PASCO manual)right

Fig 5) View of inside the capacitor and its housing(taken from the PASCO manual)

Fig 6) Detailed picture of the ionizer lever(taken from the PASCO manual)

• "Millikan Oil Drop Apparatus" by PASCO Scientific Model AP-8210.Manual
• Tel-Atomic 50V & 500V supply
• Fluke 111 True RMS Multimeter
• Squibb's Mineral Oil
• Smiec 0-25mm 0.01mm Micrometer

Procedure

Setup

The apparatus did not require any extra assembly to operate. We connected a power supply to the capacitor leads, a digital multimeter to the thermistor, plugged the light source into a wall socket, and filled the oil spray bottle with the mineral oil. After raising the apparatus to a comfortable eye level (books were used) we adjust it to be level using the built in leveling gauge and the adjustable feet. (See Fig 4)

To calibrate the apparatus, we opened up the cylindrical housing for the capacitor and took out the droplet hole cover, the upper capacitor plate and the spacer. After measuring the spacer with a micrometer, we replaced it and the upper plate. Unscrewing the focusing wire (located to the right of the capacitor) we placed the wire through the hole in the top of the upper plate and replaced everything else but the droplet hole cover. With the room dark and the lamp plugged in, we looked through the microscope and put the needle in focus, adjusting the amount of light entering the capacitor as appropriate. With the needle and grid inside the eyepiece all focused, we opened the housing, removed the needle, and replaced the droplet hole cover. (See Fig 5)

Experiment

After the apparatus has been setup, we begin by introducing the oil to the capacitor. We placed the special nozzle of the oil sprayer into a small hole in the top of the lid. To the right of the housing is a lever,(see fig 6) the lever must be set to the middle position "Spray Droplet" to allow the oil to enter the capacitor. While someone is watching the microscope, a quick spray followed by smaller, slower sprays are applied (it is helpful to remove the nozzle from the hole before releasing the sprayer to prevent the air from being sucked back out of the capacitor). The oil droplets will appear to be a "shower of sparkles" as the fall into view. Continue spraying until you see a fair amount of particles in view.

After the oil is inside the chamber, we remove the nozzle and set the lever down to the "off" position. We then switch the lever to the "on" position for 2 or 3 seconds to allow the ionizer to ionize the oil particles, then switch it back to the "off" position. To check that the oil droplets are properly ionized, we looked through the microscope and switched the polarity of the plates (see fig 3) to see if the oil droplets react differently. Ideally, they should rise when the upper plate is polarized positive (+) and fall faster when the it is polarized negative (-).

After the droplets have been properly ionized, we sought out to isolate a single droplet of which to study. The droplets can be separated by moving them by switching the polarities in the plates. Using the grid within the eyepiece of the microscope, we looked for a droplet that fell .5mm (one large unit in the grid, or 5 smaller units) in 15 seconds and rose the same amount in 3 seconds. Once a particle of that nature was found, we recorded its fall time and rise times 10 times each(when possible). After taking sufficient data, we turned the ionizer back to the "on" position for 1 or 2 seconds and repeated the experiment with the same droplet (when possible).

Data Analysis

Using the fall and rise times, we were able to determine a few things about the droplets and the charge.

To find the fall and rise times, we said that [math]\displaystyle{ V=\frac{d}{t} }[/math]. We use this simple formula since the droplets reach terminal velocity very quickly and travel at a constant rate after that.

The chart from the manual used to find the temperature of the air in the capacitor from the resistance in the thermistor fig 7

The chart from the manual used to find the viscosity of the air in the capacitor from the temperature of the air fig 8

To find the charge stored in the electron:

[math]\displaystyle{ q=\frac{mg(v_f+v_r)}{Ev_f} }[/math]

[math]\displaystyle{ m=\frac{4}{3}\pi a^3 \rho }[/math]

[math]\displaystyle{ a=\sqrt{(\frac{b}{2p})^2 +\frac{9 \eta v_f}{2g\rho}}-\frac{b}{2p} }[/math]

[math]\displaystyle{ q = {\frac{4}{3}}\pi \rho g[\sqrt{(\frac{b}{2p})^2 +\frac{9 \eta v_f}{2g\rho}}-\frac{b}{2p}]^3\frac{v_f + v_r}{Ev_f} }[/math]

q- the charge of the electron

p-barometric pressure-[math]\displaystyle{ 8.33^4Pa }[/math] (Note: This value was taken from the internet. The pressure is measured with respect to my current elevation above sea level. Any small variations due to specific locations or weather are assumed negligible)

d-distance between capacitor plates 7.60mm

g- acceleration due to gravity- [math]\displaystyle{ 9.8 \frac{m}{s^2} }[/math]

b- constant [math]\displaystyle{ 8.20E(-3)Pa * m }[/math]

a- radius in drop measured in meters

[math]\displaystyle{ \rho }[/math]-density of the oil which is [math]\displaystyle{ 886 \frac{kg}{m^3} }[/math]

[math]\displaystyle{ \eta }[/math]- viscosity of air (found by the comparing temp inside the capacitor see figs 7,8. This was an "eyeball" read, but the variations between 1 degree are very nominal)

V- potential difference across the plates in Volts

[math]\displaystyle{ v_r }[/math]- rise velocity (dividing .5mm by rise time)

[math]\displaystyle{ v_f }[/math]- falling velocity (dividing .5mm by rise time)

E electric field (found by [math]\displaystyle{ \frac{V}{d}) }[/math]

After calculating the charge of a particle, we plot it against the rise time. Taking the charges that appear close together, we then plot those averages and take a linear regression to find the value of e.

(All data calculated with MATLAB and plots created with Excel)

Results

Raw Data

Due to the length of the raw data, it will be included at the end of the paper in an appendix

Calculated Data

Trial	E field (V/m)	Viscoscity of Air e-5(Ns/m^2)	Vfall Avg e-5(m/s)	Vrise Avg e-4(m/s)	Q e-19 (couloumbs)
1A	65921.05	1.848	3.408	1.205	3.60
1B	66039.47	1.848	3.608	2.118	5.98
2	65789.47	1.852	3.225	1.683	4.54
3	65921.05	1.844	2.855	1.106	2.89
4	65973.68	1.852	3.243	2.304	5.95
5	65789.47	1.852	1.598	.8465	1.44
5A	66276.31	1.848	1.637	1.755	2.84
6	65815.79	1.848	2.199	.6404	1.52
6B	65907.89	1.852	2.098	.6225	1.42
7	65776.21	1.852	3.074	.3396	1.42
7B	65947.36	1.850	2.877	2.688	6.24
8	65815.78	1.850	2.355	.7349	1.79
8B	65907.89	1.852	2.230	.7111	1.66

There is a noticeable trend in rise times vs the number we got for Q. Plotting them below, we can see that some values tend to group together. This leads me to believe the quantized nature of the charges.

http://openwetware.org/images/0/02/Qvsrise2.JPG

Taking notice of this, I averaged the values that were close, and set the lowest value as 1Q, 2nd highest as 2Q, etc. Using a least squares fit, I found the value for the fundamental charge to be [math]\displaystyle{ (1.5193+/-0.07)x 10^{-19} coulombs }[/math] (the "linest" command gives me the deviation and slope of the line).

http://openwetware.org/images/b/be/Qvalue1.JPG

Conclusion

The experiment went very well, with no huge sources of conflict. Since the actual value of the fundamental charge is known, our value can be compared to it for a qualitative accuracy of the experiment.

[math]\displaystyle{ %error= \frac{|Actual-Experimental|}{|Actual|}x100 }[/math]

[math]\displaystyle{ %error= \frac{|1.60217646 x 10^{-19}-1.5193 x 10^{-19}|}{|1.60217646 x 10^{-19}|}x100 }[/math]

[math]\displaystyle{ %error=5.17 }[/math]

The largest contributer to errors was the small size of the droplets. The droplets experienced a high amount of Brownian motion. The droplets would move about the viewing area, leaving view completely before enough measurements could be made. Also, the droplets were no bigger than the partition lines in the grid, so it is easy to lose them behind a line and miss stopping the clock.

The best fix would be to hook up a camera to the microscope. It would allow us to record the movement of the droplets, allowing us a very detailed an accurate way to measure rise and fall times and measure more than one droplet at a time.

Acknowledgments

I would like to thank the following people:

• My lab partner Cary Dougherty, for helping take measurements
• The lab professor, Dr. Koch, for getting this all working
• Kyle Martin and Jesse Smith, from whom I borrowed my charge calculation method from
• Millikan, for discovering this in the first place

References

Julian Tribun 1

Determination of the Charge on an Electron 2

The Electron: Its Isolation and Measurements and the Determination of Some of its Properties by Robert Andrews Millikan (Pgs 43-63) 3

Appendix 1

Spacing of plates: 8.10mm

Density of Squibb's Mineral Oil: 886kg/m^3

Atmospheric Pressure in Abq (as looked up on the internet): 8.33X10^4 Pa

Set 1

Voltage: 501V Resistance: 1.9982 M(ohms) Distance: .5mm

Fall Time (s)	Rise Time (s)
18.38	3.31
14.38	3.15
14.11	5.14
13.7	5.7
13.8	5.19
14.72	5.52
14.5	5.23
13.13	5.27
15.37	5.37
Avg Fall Time	Avg Rise Time
14.67s	4.877s

In this set, we were able to change the charge on the droplet and remeasure

Voltage=501.9V Resistance=1.976M(ohms)

Fall Time (s)	Rise Time (s)
13.28
13.86	2.19
14.58	2.21
13.09	2.70
14.38	2.46
13.94	2.24
Avg Fall Time(s)	Avg Rise Time(s)
13.855	2.36

Set 2

Voltage: 500V Resistance: 1.923M(ohms)

Fall Time(s)	Rise Time(s)
15.97	2.99
14.50	3.13
13.80	2.95
15.50	2.69
15.17	2.75
15.36	3.36
Avg Fall Time(s)	Avg Rise Time(s)
15.05	2.97

We changed the charge of the oil droplet in this set as well, but the droplet moved so fast, that it was very hard to sync Cary's observations and oral commands with my data collecting. As that is the case, we only took 2 data points.

Fall Time (s)	Rise Time(s)
9.70	.72
10.32	.73

Set 3

Starting Voltage: 501.0 V Resistance: 2.07 M(ohms) Ending Voltage:501.8 V 2.041M(Ohms)

FALL TIME (s)	RISE TIME (s)
14.87	4.81
17.53	4.87
17.17	4.85
18.67	4.57
17.89	4.53
17.77	4.37
15.93	4.56
16.49	4.90
18.97	4.61
18.41	5.11
19.24	2.50
Avg Fall Time(s)	Avg Rise Time(s)
17.54	4.52

Set 4

Starting Voltage:501.4 V Resistance:1.945 M(Ohms)

Fall Time (s)	Rise Time (s)
16.13	2.23
14.29	2.14
14.85	2.47
15.96	1.93
16.49	1.99
14.79	2.25
Avg Fall Time(s)	Avg Rise Time(s)
15.42	2.17

trial 1a

resist= 2.086 ohms

temp 26 c

viscosity=1.8520

voltage= 500V

Times	Fall Time	Rise Time
0
31.609	31.609
43.281
49.297		6.016
59.016
88.293	29.227
1:32.687
1:38.500		5.813
1:46.000
2:17.297	31.297
2:20.953
2:26.328		5.375
2:39.141
3:14.875	35.734
3:19.875
3:25.891		6.016
3:34.844
4:03.469	28.625
4:09.156
4:15.469		6.313
	Avg Fall	Avg Rise
	31.2984	5.9066

a2

resistance 2.023

temp 25c

viscosity 1.8480

voltage 503.7

Time	Fall Time	Rise Time
0
27.875	27.875
31.797
34.594		2.797
49.813
79.282	29.469
1:22.000
1:25.141		3.141
1:37.032
2:11.485	34.453
2:16.438
2:19.047		2.609
2:32.141
3:02.500	30.359
may have	lost droplet
3:08.469
3:10.219		1.75
	Avg Fall	Avg Rise
	30.539	2.849

trial 2

resist 1.990

temp 25c

viscosity 1.8480

voltage 500.2v

Time	Fall Time	Rise Time
0
23.953	23.953
31.422
39.750		8.328
47.906
71.390	23.484
1:17.406
1:25.187		7.781
1:27.765
1:49.094	21.329
1:55.625
2:03.047		7.422
2:11.406
2:31.875	19.469
2:38.140
2:45.609		7.469
2:48.750
3:12.172	23.422
3:17.625
3:25.953		8.328
3:32.781
3:57.547	24.766
4:05.890
4:13.406		7.516
	Avg Fall	Avg Rise
	22.737	7.807

2b

resist 1.951

temp 26c

viscosity 1.8520

voltage 5.009

Time	Fall Time	Rise Time
0
25.344	25.344
31.375
39.750		8.375
55.625
77.484	21.859
1:21.391
1:29.625		8.234
1:35.469
1:58.094	22.625
2:04.641
2:12.250		7.609
2:17.078
2:42.563	25.485
2:46.859
2:54.766		7.907
	Avg Fall	Avg Rise
	23.828	8.031

trial 3

resistance 1.978

temp 26c

viscosity 1.8520

voltage 499.9

Time	Fall Time	Rise Time
0
15.593	15.593
24.250
39.031		14.781
46.906
64.64	17.734
1:13.406
1:27.000		13.594
1:34.375
1:50.140	15.765
1:59.203
2:13.375		14.172
2:20.187
2:37.312	17.125
2:44.187
2:57.953		13.766
3:04.250
3:19.359	15.109
3:25.531
3:39.828		14.297
	Avg Fall	Avg Rise
	16.265	14.722

3b

resistance 1.975

temp 25.5

viscosity 1.850

voltage 501.2

Time	Fall time	Rise time
0
17.375	17.375
26.968
28.828		1.86

4

resistance 1.974

temp 25.5

viscosity 1.850

voltage500.2

Time	Fall Time	Rise Time
0
21.344	21.344
26.953
34.141		7.188
38.828
58.250	19.422
1:04.469
1:10.781		6.312
1:14.984
1:39.297	24.313
1:44.219
1:51.203		6.984
1:57.500
2:17.328	19.828
2:24.859
2:30.859		6
2:56.937	ugh, lost data pt
3:01.875
3:09.406		7.531
	Avg Fall	Avg Rise
	21.226	6.803

4b

resistance 1.956

temp 26c

viscosity 1.8520

voltage 500.9

Time	Fall Time	Rise Time
0
23.562	23.562
31.375
38.234		6.859
44.703
1:06.656	21.953
1:12.625
1:19.703		7.078
1:22.172
1:47.297	25.125
1:50.953
1:58.109		7.156
2:04.391
2:33.422	29.031
	Avg Fall	Avg Rise
	22.417	7.031