A geologist observes that a rock sample repels a compass needle. Laboratory tests show the sample moves from stronger to weaker field regions between electromagnet poles, has no residual magnetism after field removal, and has susceptibility χ = −0.000085. A solenoid with 500 turns, length 25 cm, and current 2 A uses this material as its core.
A geologist is surveying a region and uses a magnetic compass to navigate. She notices that near a certain rocky outcrop, the compass needle is slightly repelled from the rock surface instead of being attracted to it. She collects a small sample of the rock and takes it to a laboratory. In the lab, the following observations are recorded:
(i) When placed between the poles of a strong electromagnet, the sample moves from the stronger field region to the weaker field region.
(ii) When the external magnetic field is removed, the sample shows no residual magnetism.
(iii) The susceptibility (χ) of the material is measured to be −0.000085.
(iv) A cylindrical bar of this material, wound with N = 500 turns over a length of 25 cm and carrying a current of 2 A, is used as a solenoid core.
Based on this scenario, answer the following:
(a) Identify the magnetic class of the rock sample. Name ONE common example of such a material.
(b) What is the relative permeability (μ<sub>r</sub>) of this material? Is it greater than, equal to, or less than 1?
(c) Calculate the magnetisation (M) of the material inside the solenoid. (Given: χ = −0.000085)
(d) The geologist's compass needle is deflected away from the rock. Justify this behaviour using the concept of magnetic susceptibility.
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The sample moves from stronger to weaker field regions, shows no residual magnetism, and has a small negative susceptibility (χ < 0). These are the characteristic properties of a DIAMAGNETIC material.
∴ The rock sample is DIAMAGNETIC.
Common example: Bismuth (Bi) [also acceptable: Copper (Cu), Gold (Au), Silver (Ag)].
(b) Relative permeability:
For any magnetic material, the relative permeability is given by:
μ<sub>r</sub> = 1 + χ
Substituting χ = −0.000085:
μ<sub>r</sub> = 1 + (−0.000085)
∴ μ<sub>r</sub> = 0.999915
Since χ < 0, μ<sub>r</sub> is slightly less than 1.
(c) Magnetisation (M) inside the solenoid:
The magnetising field H inside a solenoid is given by:
H = nI
where n = N/L = number of turns per unit length, and I = current.
n = 500 / 0.25 = 2000 turns m<sup>−1</sup>
→ H = 2000 × 2 = 4000 A m<sup>−1</sup>
Using the relation between magnetisation and susceptibility:
M = χ H
M = (−0.000085) × 4000
∴ M = −0.34 A m<sup>−1</sup>
(The negative sign confirms magnetisation is opposite to the applied field, consistent with diamagnetic behaviour.)
(d) Justification of compass deflection:
Magnetic susceptibility χ is defined as the ratio of magnetisation M to the magnetising field H, and it measures how a material responds to an external magnetic field.
For the diamagnetic rock sample, χ < 0 (χ = −0.000085). This means when an external magnetic field (from the Earth or nearby magnet) is applied, the sample acquires a small magnetisation in the DIRECTION OPPOSITE to the applied field.
As a result, the rock sample creates a weak field that opposes the external field near its surface. The compass needle, which aligns with the net local field, is therefore slightly pushed away (repelled) from the rock instead of being attracted.
Because diamagnets are repelled by both poles of a bar magnet and move toward regions of weaker field, the compass needle deflects away from the rock surface.