Source: Andrew Duffy, PhD, Department of Physics, Boston University, Boston, MA
This experiment duplicates J.J. Thomson's famous experiment at the end of the 19th century, in which he measured the charge-to-mass ratio of the electron. In combination with Robert A. Millikan's oil-drop experiment a few years later that produced a value for the charge of the electron, the experiments enabled scientists to find, for the first time, both the mass and the charge of the electron, which are key parameters for the electron.
Thomson was not able to measure the electron charge or the electron mass separately, but he was able to find their ratio. The same is true for this demonstration; although here there is the advantage of being able to look up the values for the magnitude of the charge on the electron(e) and the mass of the electron (me), which are now both known precisely.
1. Compensating for Earth's Magnetic Field
Representative results for Section 2 can be seen in Table 1. Those values give an average charge-to-mass ratio of 1.717 x 10-11 C/kg. Note that that is the magnitude of the ratio, because the charge of the electron is a negative value.
Representative results for Section 3 can be seen in Table 1. Those values give an average charge-to-mass ratio of 1.677 x 10-11 C/kg. Again,
This experiment, first performed by J.J. Thomson in the late 19th century, demonstrated the existence of the electron, making it a tremendously important experiment from a historical perspective. Electrons have since been exploited in countless electronic devices.
The following is a list of some applications of charged particles that are traveling in circular or spiral paths, and thus they are traveling in a magnetic field:
1)The formation of the Northern
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