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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



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 Failed to parse (MathML with SVG or PNG fallback (recommended for modern browsers and accessibility tools): Invalid response ("Math extension cannot connect to Restbase.") from server "":): {\displaystyle (1.5193+/-0.07)x 10^{-19} coulombs} , very close to the accepted value of Failed to parse (MathML with SVG or PNG fallback (recommended for modern browsers and accessibility tools): Invalid response ("Math extension cannot connect to Restbase.") from server "":): {\displaystyle 1.60217733x10^{-19}} Coulombs.


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



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)


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 Failed to parse (MathML with SVG or PNG fallback (recommended for modern browsers and accessibility tools): Invalid response ("Math extension cannot connect to Restbase.") from server "":): {\displaystyle V=\frac{d}{t}} . 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:

Failed to parse (MathML with SVG or PNG fallback (recommended for modern browsers and accessibility tools): Invalid response ("Math extension cannot connect to Restbase.") from server "":): {\displaystyle q=\frac{mg(v_f+v_r)}{Ev_f}}

q- the charge of the electron

p-barometric pressure-Failed to parse (MathML with SVG or PNG fallback (recommended for modern browsers and accessibility tools): Invalid response ("Math extension cannot connect to Restbase.") from server "":): {\displaystyle 8.33^4Pa} (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-

b- constant

a- radius in drop measured in meters

-density of the oil which is

- 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

- rise velocity (dividing .5mm by rise time)

- falling velocity (dividing .5mm by rise time)

E electric field (found by

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)


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.

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 (the "linest" command gives me the deviation and slope of the line).


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.

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.


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


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)
13.86 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)

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


voltage= 500V

Times Fall Time Rise Time
31.609 31.609
49.297 6.016
88.293 29.227
1:38.500 5.813
2:17.297 31.297
2:26.328 5.375
3:14.875 35.734
3:25.891 6.016
4:03.469 28.625
4:15.469 6.313
Avg Fall Avg Rise
31.2984 5.9066


resistance 2.023

temp 25c

viscosity 1.8480

voltage 503.7

Time Fall Time Rise Time
27.875 27.875
34.594 2.797
79.282 29.469
1:25.141 3.141
2:11.485 34.453
2:19.047 2.609
3:02.500 30.359
may have lost droplet
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
23.953 23.953
39.750 8.328
71.390 23.484
1:25.187 7.781
1:49.094 21.329
2:03.047 7.422
2:31.875 19.469
2:45.609 7.469
3:12.172 23.422
3:25.953 8.328
3:57.547 24.766
4:13.406 7.516
Avg Fall Avg Rise
22.737 7.807


resist 1.951

temp 26c

viscosity 1.8520

voltage 5.009

Time Fall Time Rise Time
25.344 25.344
39.750 8.375
77.484 21.859
1:29.625 8.234
1:58.094 22.625
2:12.250 7.609
2:42.563 25.485
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
15.593 15.593
39.031 14.781
64.64 17.734
1:27.000 13.594
1:50.140 15.765
2:13.375 14.172
2:37.312 17.125
2:57.953 13.766
3:19.359 15.109
3:39.828 14.297
Avg Fall Avg Rise
16.265 14.722


resistance 1.975

temp 25.5

viscosity 1.850

voltage 501.2

Time Fall time Rise time
17.375 17.375
28.828 1.86


resistance 1.974

temp 25.5

viscosity 1.850


Time Fall Time Rise Time
21.344 21.344
34.141 7.188
58.250 19.422
1:10.781 6.312
1:39.297 24.313
1:51.203 6.984
2:17.328 19.828
2:30.859 6
2:56.937 ugh, lost data pt
3:09.406 7.531
Avg Fall Avg Rise
21.226 6.803


resistance 1.956

temp 26c

viscosity 1.8520

voltage 500.9

Time Fall Time Rise Time
23.562 23.562
38.234 6.859
1:06.656 21.953
1:19.703 7.078
1:47.297 25.125
1:58.109 7.156
2:33.422 29.031
Avg Fall Avg Rise
22.417 7.031