Physics · Magnetism And Matter · NEET
Time period is the time for ONE oscillation. So T = total time / number of oscillations = t / N. Example: 20 oscillations in 5 s gives T = 5/20 = 0.25 s. Never plug the raw 5 s into the formula — always convert to one-oscillation time first. This single step is where most marks are lost.
They are two different things that both appear in the formula. Magnetic moment m (unit A m²) measures how strong the magnet is — it decides the restoring torque mB that pulls the needle back. Moment of inertia I (unit kg m²) measures how the mass is spread out — it decides how sluggishly the needle turns. In T = 2π√(I/mB), I is on top (more I → slower → bigger T) and mB is on the bottom (stronger magnet or field → faster → smaller T).
Square both sides: T² = 4π² (I/mB). Then multiply both sides by mB and divide by 4π²: I = mBT² / 4π². To instead solve for the magnetic moment, rearrange the same equation to m = 4π²I / (BT²). Pick whichever unknown the question asks for.
Yes. The restoring torque is τ = mB sinθ, and for small angles sinθ ≈ θ, giving SHM only when B is uniform over the needle. In the Earth's field experiment, B is the horizontal component B_H of Earth's field, and the same formula holds with B replaced by B_H.
In a uniform magnetic field of 0.049 T, a magnetic needle performs 20 complete oscillations in 5 seconds. The moment of inertia of the needle is 9.8 × 10⁻⁶ kg m². If the magnetic moment of the needle is x × 10⁻⁵ A m², the value of x is:
Try the real previous-year questions from this chapter — each with the answer and a full solution.
T = 2π√(I / mB), where I is the moment of inertia (kg m²), m is the magnetic moment (A m²), and B is the uniform magnetic field (T). It is the magnetic version of the pendulum formula.
Rearrange the period formula: I = mBT² / 4π². Measure the time for one oscillation T, and use the known m and B to compute I in kg m².
The restoring torque τ = mB sinθ ≈ mBθ for small angles. A torque proportional to the negative of the angular displacement is exactly the condition for SHM, giving the standard T = 2π√(I/mB).
B is replaced by the horizontal component of the Earth's field, B_H. A vibration magnetometer uses T = 2π√(I / mB_H) to compare or measure m and B_H.