Measuring Earth’s
magnetic field
using Tangent
Galvanometer
Made by: Ankita Tripathi
Roll no: 5648057
CERTIFICATE
_____________________________________________________________________________________________________________________________________ ____________________________________________________________________________________________________________________________________
This is to certify that Ankita Tripathi of class
XII-B has completed the physics project
entitled: ‘Measuring Earth’s magnetic field
using a tangent galvanometer’, herself and
under the guidance of Mr. Siby Sebastian.
All the work related to the thesis had been
done by the candidate herself. The
approach was sincere and scientific.
Mr. Siby Sebastian Examiner
(Subject teacher)
ACKNOWLEDGEMENT
I am grateful to the Almighty to give me
strength to successfully complete my
project.
This project wouldn’t have been feasible
without the proper and rigorous guidance
of my Physics teacher Mr. Siby
Sebastian, who guided me throughout
this project in every possible way.
I am deeply indebted to my school for
providing the best of facilities and
environment to bring out our innovation
and spirit of inquiry through this venture.
Index
Materials Required
Principle
Diagram
Theory
Procedure
Observations
Calculations
Result
Precautions
Sources of error
Bobliography
Materials Required
Tangent galvanometer (TG),
Rheostat (R),
Battery (E),
Ammeter (A),
Key (k)
Reversing key
Connecting wires
Metre scale
Principle
When a bar magnet is suspended in two
Magnetic fields B and B
h, it comes to rest
making an angle θ with the direction of
B
h.
Diagram
Theory
Tangent galvanometer is an early
measuring instrument for small electric
currents. It consists of a coil of insulated
copper wire wound on a circular
non-magnetic frame. Its working is based on
the principle of the tangent law of
magnetism. When a current is passed
through the circular coil, a magnetic field
(B) is produced at the center of the coil in
a direction perpendicular to the plane of
the coil. The TG is arranged in such a way
that the horizontal component of earth’s
magnetic field (B
h) is in the direction of
the plane of the coil. The magnetic needle
is then under the action of two mutually
perpendicular fields. If θ is the deflection
of the needle, then according to tangent
law,
Let I is the current passing through the
coil of radius a with n turns, then the field
generated by the current carrying circular
coil is,
Equating (1) and (2), we get,
The left hand side of equation (4) is a
constant and is called the reduction factor
(K) of the given tangent galvanometer.
Now from equation (3) & (5), the
horizontal intensity of earth’s magnetic
field Bh is,
Procedure
For performing in real life
Connections are made as shown in the figure,
where K is the key, E the battery, A the ammeter, R the rheostat, C the commutator, and T.G the tangent galvanometer.
The commutator can reverse the current through the T.G coil without changing the current in the rest of the circuit.
Taking the average of the resulting two readings for deflection averages out, any small error in positioning the TG coil relative to the earth’s magnetic field Bh .
The magnetic field can be calculated as
follows:
1. Make the circuit connections in accordance
with the circuit diagram.
2. Using a spirit level, level the base and
compass needle in compass box of tangent galvanometer by adjusting the leveling
screw.
3. Now rotate the coil of the galvanometer
about its vertical axis, till the magnetic
needle, its image in the plane of the mirror fixed at the base of the compass box and the coil ie all these three lie in the same vertical plane. In this setting, the ends of aluminum pointer should reads zero-zero. If this is not so, rotate the box without disturbing the position of the coil till at least one of the
4. By closing the key K, the current flows in the
galvanometer. Read the both ends of the pointer. Now reverse the direction of current by using the reserve key. when the mean values of deflections shown by the pointer in two cases (i.e. before and after reversing the
current) differ by more than 1o, then turn
slightly the vertical coil until the two values agree. This will set the plane of the coil
exactly in the magnetic meridian.
5. By adjusting the rheostat, bring the
deflection in galvanometer around 45
degree. The deflection should not be outside the range(30-60).
6. Record the reading of the ammeter and the
deflection of the compass needle in a box shown by two ends of pointer of the scale.
7. Reverse the current in the coil of the
galvanometer and again record the current and deflection of needle.
8. By changing the value of current, take four
more set of reading and plot the graph
between I and tan. The graph will be a
straight line.
9. Measure the inner and outer diameter of the
Observations
Range of ammeter r=_____________A Least count of ammeter = __________A Zero error in ammeter = __________A Number of turns used (N) = __________ Table for Variation of with I.
S. No. Value of deflection, Mean Tan Ammeter Reading (A) For direct current For reverse current 1 2 3 4 Observed Corrected 1. 2. 3. 4. 5.
Table for radius of tangent galvanometer S. no. Inner diameter d1 Outer diameter d2 Mean Diameter d Mean Radius 1. 2. 3.
Calculations
Result
The value of earth’s magnetic field by using tangent
galvanometer is
Precautions
1. The battery should be freshly charged.
2. The magnetic needle should swing freely in the
horizontal plane.
3. The plane of coil must be set in magnetic
meridian.
4. All the readings must be adjusted between 30
oand 60
0.
Sources of error
1. There may be a magnetic material around the
apparatus.
2.