To see how currents running through wires can create magnetic fields, and how the strength of those magnetic fields depends on distance from the wire.
Even if you don't have a magnet, you can still create a magnetic field. The current passing through a wire will create a magnetic field near the wire. Ampere's Law can help you to figure out the strength of such a field in some circumstances.
Turn on the power supply. Because the patch cords provide only a very small resistance, a large current will run through them. The power supply's built-in current limiter should activate -- you'll see the red bulb above "C.C." light up -- preventing the current from rising too high. Use the ammeter to read the current running through the wire. It should be somewhere between 1 and 3 amps. If the current is above 3 amps, adjust the power supply so that it goes down to 3 amps.
Place the probe so that it lies parallel to the straight section of the wire. Twist the probe so that the white dot is pointing straight up, as shown.
When the current is flowing, it will create a magnetic field around the wire. Which way will the magnetic field point? Indicate the direction of the magnetic field near the position of the probe in the figure above.
Measure the magnetic field when the power supply is turned off; you are detecting a "background" consisting of the Earth's magnetic field as well as components generated by electrical appliances in the room. Then turn the power supply on and measure the field again; your probe now detects the "background" plus the field generated by the current running through the wire. The difference between the two readings is the magnetic field created by the current in the wire alone.
In order to determine only the magnetic field produced by the wire, and not the changes in the ambient magnetic field, you need to make a differential measurement like so:
Start with the probe on the side of the wire away from the power supply. Place it a distance of r = 20 cm and measure the field strength B. Write down your results. Then acquire more measurements at distances r of 18, 16, 12, 10, 8, 6, 5, 4, 3, 2, 1 cm.
Now, actually move the probe to the other side of the wire. Make sure that the white dot still faces straight up, and make the measurement. Was your prediction correct? If not, can you explain what changed as you moved the probe from one side of the wire to the other? Perhaps it would help to draw the direction of the magnetic field on both sides of the wire in the diagram above....
Make measurements on this other side of the wire at the same set of distances: 1, 2, 3, 4, 5, 6, 8, 10, 12, 16, 18, 20 cm.
B = k1 / r^2or is it
B = k2 / ror perhaps
- r B = k3 * e
One way to decide is to look at your data in a numerical fashion. Consider your measurement of B at the distance r = 3 cm. If the first model is correct, what should happen to the magnetic field strength if you double the distance? Should it be cut in half, or by some other factor? Then look at the measurement at double the distance, r = 6 cm. Does it agree with the model's prediction? What about the other models?
predicted B2, for models r1 B1 r2 -r actual B2 (cm) (mT) (cm) 1/r^2 1/r e (mT) ------------------------------------------------------------------------
Plot all your measurements on this graph. You should have two values at each distance, one from each side of the wire.
Now, how can we compare the models to the data on this graph? We will normalize all three mathematical functions,
B = k1 / r^2 B = k2 / r - r B = k3 * eso that they match the graph exactly at one point, somewhere in the middle of the range. We'll use r = 4 cm as the point in common. Calculate the average value of your magnetic field strength at this distance. For each of the three functions,
If one of the mathematical models is a good match to reality, then it ought to follow the actual measured values pretty closely. All of the lines will run through the data at r = 4 cm, but which of them does the best job of matching the data at other distances?
The equation in your textbook includes a number of factors which your empirical function lumped together as a single constant (k1 or k2 or k3). In a perfect universe, those factors would exactly equal your empirical constant; in other words, if you plugged into the textbook equation the values for the current through the wire, etc., you'd end up with exactly the magnetic field strength you actually measured.
Last modified 10/18/2003 by MWR