Electric Charge in a Magnetic Field
1. Compensating for Earth's Magnetic Field
- Note that there are two independent circuits in this experiment:
- Supply current to the coils that create the magnetic field ( Figure 2). The current is set by a rotary dial, and the circuit includes a digital ammeter that allows the current to be measured. A double-pole double-throw switch is used to reverse the direction of the current supplied to the coils, which reverses the magnetic field.
- The second circuit ( Figure 3) runs the electron tube. There is a high-voltage supply, which sets the accelerating voltage and an alternating signal of 6.3 V connected to a filament. Electrons are, in some sense, boiled off the filament and then accelerated by the accelerating voltage.
- In the second circuit, turn on the high-voltage power supply to turn on the filament. The light that switches on inside the tube is the glowing filament.
- Gradually turn up the high voltage to about 2,000 V. The part of the screen inside the tube, which is being hit by the electron beam, should glow blue, making the electron beam visible.
- Note that this does not mean electrons are blue - the coating on the screen is phosphorescent and gives off a blue glow when the atoms of this coating are energized by the electrons.
- Adjust the current through the coils, which create the uniform magnetic field. As the current is adjusted up or down, the path of the beam changes. Adjust the current to pass the beam through a particular (X, Y) point on the grid. Make note of the magnitude of the current required to have the beam pass through that point.
- Reverse the current to curve the beam in the opposite direction, and adjust the current until the beam passes through the point (X, −Y) (the mirror image of the original point). Again, make note of the magnitude of the current required to have the beam pass through that particular point.
- Check to see if the magnitudes of the two currents are different. Unless the tube happens to be aligned so the electron beam is parallel to Earth's magnetic field, the Earth's field adds to the field of the coils when the current is in one direction and subtracts from it when the current is in the other direction.
- Throughout the experiment, average the magnitudes of the two currents, the current required to have the beam pass through a particular (X, Y) point on the grid, and the current required to pass through the mirror-image point (X, −Y), to remove the effect of Earth's magnetic field.
Figure 2: Circuit diagram for the Helmholtz coils. The strength of the magnetic field created by the Helmholtz coils is proportional to the current passing through them. The current supplied to the coils by the adjustable power supply is measured by the digital ammeter. The purpose of the double switch is to easily reverse the direction of the current passing through the coils, which reverses the direction of the magnetic field. Note that the two connections to each coil are marked A and Z, and the two Z's should be connected together to ensure that the coils are producing magnetic fields in the same direction, and not in opposite directions.
Figure 3: Circuit diagram for running the electron tube. The glowing filament that is the source of the electrons is run by a 6.3 V alternating current source. Note that the negative side of the high voltage signal is also connected to one side of the filament, while the positive high voltage signal (on the order of 2,000-3,000 V DC) is connected to an electrode on the right side of the acceleration zone. This produces a large electric field directed left in the acceleration zone, accelerating the electrons from left to right.
2. Data Collection for a Particular (X, Y) and (X, − Y) Combination
- Note that the tubes are expensive and somewhat fragile. Do not exceed 3,500 V for the accelerating voltage, and turn the accelerating voltage down to zero when measurements are not being taken.
- In this part of the experiment, record five sets of data, each with a different accelerating voltage with the same (X, Y) and (X, −Y) combination.
- Note that as the accelerating voltage increases and the electrons travel faster, they do not bend as much, and thus, the magnetic field from the coils needs to be increased to have the beam pass through the same point on the screen. Choose a particular (X, Y) and (X, −Y) point to use for this part of the experiment. Use Equation 10 to calculate the corresponding radius of the beam's path.
- For a particular accelerating voltage, record the magnitude of the current needed to have the beam pass through the chosen (X, Y) point. Reverse the current, and record the magnitude of the current needed to have the beam pass through the mirror-image point (X, −Y).
- Average the two currents to remove the influence of Earth's magnetic field.
- Use the average current in Equation 8 to calculate the strength of the magnetic field.
- Use the values of the accelerating voltage, radius, and magnetic field to calculate the magnitude of the charge-to-mass ratio of the electron.
- Choose a new accelerating voltage, and repeat steps 2.3-2.7. Continue to do this until five sets of data have been collected.
- Compute the magnitude of the average charge-to-mass ratio for the electron.
3. Data Collection for a Particular Accelerating Voltage
- Collect five more data sets. This time, keep the accelerating voltage constant and change the (X, Y) and (X, −Y) points that the beam passes through. Record the data.
- Compute the magnitude of the average charge-to-mass ratio for the electron.
- Average the two average charge-to-mass ratios determined from Section 2 and 3, and state possible sources of error in the experiment.
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
- Note that there are two independent circuits in this experiment:
- Supply current to the coils that create the magnetic field ( Figure 2). The current is set by a rotary dial, and the circuit includes a digital ammeter that allows the current to be measured. A double-pole double-throw switch is used to reverse the direction of the current supplied to the coils, which reverses the magnetic field.
- The second circuit ( Figure 3) runs the electron tube. There is a high-voltage supply, which sets the accelerating voltage and an alternating signal of 6.3 V connected to a filament. Electrons are, in some sense, boiled off the filament and then accelerated by the accelerating voltage.
- In the second circuit, turn on the high-voltage power supply to turn on the filament. The light that switches on inside the tube is the glowing filament.
- Gradually turn up the high voltage to about 2,000 V. The part of the screen inside the tube, which is being hit by the electron beam, should glow blue, making the electron beam visible.
- Note that this does not mean electrons are blue - the coating on the screen is phosphorescent and gives off a blue glow when the atoms of this coating are energized by the electrons.
- Adjust the current through the coils, which create the uniform magnetic field. As the current is adjusted up or down, the path of the beam changes. Adjust the current to pass the beam through a particular (X, Y) point on the grid. Make note of the magnitude of the current required to have the beam pass through that point.
- Reverse the current to curve the beam in the opposite direction, and adjust the current until the beam passes through the point (X, −Y) (the mirror image of the original point). Again, make note of the magnitude of the current required to have the beam pass through that particular point.
- Check to see if the magnitudes of the two currents are different. Unless the tube happens to be aligned so the electron beam is parallel to Earth's magnetic field, the Earth's field adds to the field of the coils when the current is in one direction and subtracts from it when the current is in the other direction.
- Throughout the experiment, average the magnitudes of the two currents, the current required to have the beam pass through a particular (X, Y) point on the grid, and the current required to pass through the mirror-image point (X, −Y), to remove the effect of Earth's magnetic field.
Figure 2: Circuit diagram for the Helmholtz coils. The strength of the magnetic field created by the Helmholtz coils is proportional to the current passing through them. The current supplied to the coils by the adjustable power supply is measured by the digital ammeter. The purpose of the double switch is to easily reverse the direction of the current passing through the coils, which reverses the direction of the magnetic field. Note that the two connections to each coil are marked A and Z, and the two Z's should be connected together to ensure that the coils are producing magnetic fields in the same direction, and not in opposite directions.
Figure 3: Circuit diagram for running the electron tube. The glowing filament that is the source of the electrons is run by a 6.3 V alternating current source. Note that the negative side of the high voltage signal is also connected to one side of the filament, while the positive high voltage signal (on the order of 2,000-3,000 V DC) is connected to an electrode on the right side of the acceleration zone. This produces a large electric field directed left in the acceleration zone, accelerating the electrons from left to right.
2. Data Collection for a Particular (X, Y) and (X, − Y) Combination
- Note that the tubes are expensive and somewhat fragile. Do not exceed 3,500 V for the accelerating voltage, and turn the accelerating voltage down to zero when measurements are not being taken.
- In this part of the experiment, record five sets of data, each with a different accelerating voltage with the same (X, Y) and (X, −Y) combination.
- Note that as the accelerating voltage increases and the electrons travel faster, they do not bend as much, and thus, the magnetic field from the coils needs to be increased to have the beam pass through the same point on the screen. Choose a particular (X, Y) and (X, −Y) point to use for this part of the experiment. Use Equation 10 to calculate the corresponding radius of the beam's path.
- For a particular accelerating voltage, record the magnitude of the current needed to have the beam pass through the chosen (X, Y) point. Reverse the current, and record the magnitude of the current needed to have the beam pass through the mirror-image point (X, −Y).
- Average the two currents to remove the influence of Earth's magnetic field.
- Use the average current in Equation 8 to calculate the strength of the magnetic field.
- Use the values of the accelerating voltage, radius, and magnetic field to calculate the magnitude of the charge-to-mass ratio of the electron.
- Choose a new accelerating voltage, and repeat steps 2.3-2.7. Continue to do this until five sets of data have been collected.
- Compute the magnitude of the average charge-to-mass ratio for the electron.
3. Data Collection for a Particular Accelerating Voltage
- Collect five more data sets. This time, keep the accelerating voltage constant and change the (X, Y) and (X, −Y) points that the beam passes through. Record the data.
- Compute the magnitude of the average charge-to-mass ratio for the electron.
- Average the two average charge-to-mass ratios determined from Section 2 and 3, and state possible sources of error in the experiment.
Electrons play the leading role many areas of science and technology, as they possess electric charge, enabling them to carry current.
Electric charge, or q, is a physical property describing whether a unit of matter has more protons, making it positively charged, more electrons, making it negatively charged or an equal number of protons and electrons, making it uncharged. This fundamental property describes electromagnetic interactions, where like charges are repelled, and opposite charges are attracted.
J.J. Thomson is credited with the discovery of the electron, where he showed that a cathode ray could be deflected by a magnetic field in an evacuated tube. This led to the conclusion that electrons carry a permanent negative charge, and enabled his calculation of the electrons charge-to-mass ratio.
This video will introduce the concept of the force applied to a charge in a magnetic field, and the calculation of the charge-to-mass ratio of an electrode using a cathode ray tube experiment similar to the one used by J.J. Thomson.
Before learning about the cathode ray tube experiment, let's talk about the effects of magnetic field on an electric charge which form the basis of this experiment. When a moving charge is introduced in a magnetic field, the field exerts a force F on the charge.
This is called the Lorentz force. The magnitude of this force is given by the formula qVB sine theta, where q is the magnitude of the charge, V is the velocity, B is the magnitude of the magnetic field, and theta is the angle between the velocity and the magnetic field.
Thus the Lorentz force is maximum when the angle between the V and B is 90 degrees, and is such cases, the direction of the force exerted on a positive charge is given by the right hand thumb rule, making all the vectors perpendicular to each other. If the charge is negative, then the force acts in the opposite direction. Now let's imagine all the magnetic field lines are going into the plane.
These are conventionally denoted by the crosses inside circles. If a positive charge with a velocity perpendicular to the magnetic field is introduced into the field, then the force exerted on this charge will have a direction perpendicular to the velocity. This force has no effect on the magnitude of the velocity, but it affects the direction, and the resultant velocity vector is between the two perpendicular vectors, which forces the charge to move.
Therefore, the charged particles follow a circular path at a constant speed, with all three vectors, velocity, force, and magnetic field perpendicular to each other at all times. Looking at this diagram, it is apparent the force vector represents the centripetal force.
As per Newton's second law, this force is mass of the charge times centripetal acceleration, which is v squared divided by r, the radius of curvature. Recall this force is also given by the Lorentz force formula. Combining these two equations with the law of conservation of energy applicable to the cathode ray tube experiment, we can derive the equation for the charge-to-mass ratio of an electron.
Note that three pieces of information, the potential difference through which electrons are being accelerated, the strength of the magnetic field, and the radius of the circular path followed by the charged particles are needed for the calculation.
Now let's set up and demonstrate how to set up and conduct this cathode ray tube experiment in a physics lab.
First, become familiar with the experimental apparatus. Locate the coils that generate the magnetic field and the digital ammeter, which enables the measurement of current. Locate the double-pole-double-throw switch, which is used to reverse direction of the current, and therefore reverses the magnetic field.
Supply current to the coils that create the magnetic field using the rotary dial. Next, locate the high-voltage supply, which sets the accelerating voltage and an alternating signal of 6.3 V connected to a filament. Electrons are generated by the filament and accelerated by the accelerating voltage.
Now, turn on the high-voltage power supply to turn on the filament. Note that the light that comes on inside the tube is the glowing filament.
Gradually turn up the high voltage to about 2000 V. The part of the screen inside the tube, which is being hit by the electron beam, should glow blue making the electron beam visible.
Next, adjust the current through the coils, creating a uniform magnetic field. Observe that as the current is adjusted up or down, the path of the beam changes. Adjust the current to pass the beam through a particular (x, y) point on the grid. Record the magnitude of the current required to hit this point.
Reverse the current in order to curve the beam in the opposite direction, and adjust the current until the beam passes through the point (x, negative y): or the mirror image of the original point. Record the magnitude of the current. Repeat for four more accelerating voltages, using the same (x, y) and (x, negative y) points.
Observe that as the accelerating voltage is increased and the electrons travel faster, the beam bends less. Thus the coil current must be higher to reach the same (x, y) point.
Next, repeat the full experiment, while this time keeping accelerating voltage constant, and varying the (x,y) and (x, negative y) locations. Collect five data sets, recording the point coordinates and current magnitude for each point and its mirror image.
The radius, r, of the beam path for each accelerating voltage can be calculated using the Pythagorean theorem.
Average the two currents needed to hit both (x,y) and (x, negative y) points for each accelerating voltage to remove the effect of the Earths magnetic field. Do the same for the varied (x, y) and (x, negative y) couples at the same accelerating voltage. Then use the average current to calculate the strength of the magnetic field, B. In the case of this setup, the magnetic field is equal to 0.00423 times the current.
When varying the accelerating voltage, use the value of the magnetic field, the constant radius, and the corresponding voltage to calculate the magnitude of the charge to mass ratio of an electron. Similarly, when varying the (x, y) locations, use the value of the magnetic field, the constant voltage, and the corresponding radius to calculate the electron's charge-to-mass ratio.
Then calculate the average for both varying accelerating voltage and varying (x and y) locations conditions. These experimentally calculated ratio values compare well to the known charge-to-mass ratio of an electron.
Charged particles, which move in a circular path due to an applied magnetic field, have a wide range of applications in technology.
Mass spectrometers identify unknown components of a sample based on their charge-to-mass ratio. Particles travel in a different radius depending on their charge-to-mass ratio, the accelerating voltage and the applied magnetic field. These parameters enable the separation of various components.
Prior to LCD, LED and plasma screen technology, cathode ray tubes, like the experimental set up used in this video, were the basis for all TV screens and computer monitors.
Common lab equipment still uses cathode ray tube displays, such as basic oscilloscopes. The difference being that the deflection of electrons is done via electrostatic deflection, rather than magnetic deflection.
You've just watched JoVE's introduction to electric charges in a magnetic field. You should now understand how electrons are influenced by magnetic fields, and how to use a magnetic field to determine the charge-to-mass ratio of an electron. Thanks for watching!
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...
Chapters in this video
0:06
Overview
1:20
Principles of Charges in a Magnetic Field
4:05
Experimental Setup
6:28
Data Analysis and Results
7:50
Applications
8:47
Summary
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