i. Two wooden retort stands and clamps
ii. A cork and an optical pin
iii. A set of small bar magnet fixed with a pair of optical pins
iv. A plane mirror attached to a paper protractor
v. Thread of length about 40 cm
vi. A test-tube wound with copper wires
vii. A 1.5 V dry cell or any other stable power supply
viii. A (0-1A) d.c. ammeter
ix. A switch
x. A rheostat
xi. A pair of vernier calipers
xii. A micrometer screw gauge
xiii. Some connecting wires
a) The cork with a pin is clamped to the retort stand. The bar magnet is hung from the pin using the thread supplied, so that the magnet stays at a height of about 3 cm above the table. The magnet is allowed to stay stationary and horizontal. The mirror is placed with the protractor with the 0° - 180° axis directly below the pins.
b) The solenoid is held by using the other clamp in a horizontal position at the same level with the magnet. The orientation of the solenoid is adjusted so that its axis is perpendicular to the axis of the magnet and one end of the solenoid is at 3.0 cm from the axis of the magnet. A rheostat, ammeter, power supply and switch is connected to the solenoid in series. The ammeter should be kept at least 50 cm from the magnet. The experiment is set up as shown in Figure 14.
c) The rheostat is adjusted to maximum resistance and the switch is then closed. The current I reading of the ammeter is recorded and the average deflection of the magnet from the 0° - 180° axis is obtained.
d) The value of the resistance of the rheostat is decreased in stages so as to change the value of current I and then the corresponding value of θ is measured.
e) All the measurements for I, θ, and tan θ are recorded.
e) A graph of against I is plotted.
f) The gradient s of the graph of against I is calculated.
g) The solenoid is removed to measure
i)The internal diameter D of the solenoid,
ii) Average diameter d of the wire used in the solenoid,
iii) The length of the solenoid .
h) The values of d and are used to estimate the number of turns N in the solenoid.
i) The value of the horizontal componentBH of the Earth's magnetic field is calculated using the following estimation
Where and
.
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