Q.A long solenoid has 1000 turns per metre and carries a current of 1 A. It has a soft iron core of μr=1000. The core is heated beyond the Curie temperature, Tc.
(a) The H field in the solenoid is (nearly) unchanged but the B field decreases drastically.
(b) The H and B fields in the solenoid are nearly unchanged.
(c) The magnetisation in the core reverses direction.
(d) The magnetisation in the core diminishes by a factor of about 108.
Concept understanding — Magnetic Materials Magnetization
From a Paperclip to a Magnet: The Intuition
You already know that a magnet can pick up iron nails. But what is actually happening inside that nail when it gets near the magnet? And why does a plastic comb, rubbed on hair, pick up tiny bits of paper — but never iron filings?
The answer lies in magnetization — the process by which a material becomes magnetic.
Think of a piece of iron as a chaotic crowd of tiny compass needles. Each needle is an atomic magnetic moment (a tiny magnet, arising from the spin of electrons). In unmagnetized iron, these needles point in random directions. Their magnetic effects cancel out, so the iron as a whole shows no net magnetism.
Now bring a strong magnet close. Its magnetic field acts like a command: "Line up!" The tiny compass needles inside the iron start rotating, aligning themselves with the external field. The more they align, the stronger the iron's own magnetic field becomes. This alignment is magnetization.
Note
Magnetization is not the same as inducing a current. It is a purely magnetic reorientation of atomic dipoles inside a material.
The Precise Definition
Magnetization (M) is the net magnetic dipole moment per unit volume of a material. It tells you how strongly a material is magnetized — how many tiny atomic magnets are aligned, and in which direction.
If a material has N atoms per unit volume, each with an average magnetic moment μavg, then:
M=Nμavg
The SI unit of M is amperes per metre (A/m). Why? Because a magnetic dipole moment has units of A·m², and dividing by volume (m³) gives A/m.
M=volumetotal magnetic dipole moment
How Magnetization Connects to the Magnetic Field
When a material gets magnetized, it produces its own magnetic field. The total magnetic field B inside the material is the sum of:
The external applied fieldH (caused by free currents, like the current in a solenoid)
The material's response — the magnetization M
The fundamental relation is:
B=μ0(H+M)
where μ0=4π×10−7T⋅m/A is the permeability of free space.
Watch out
Do not confuse H (magnetic field intensity, or "magnetizing field") with B (magnetic flux density). H is what you apply; M is what the material does; B is the total field you measure.
The Three Kinds of Magnetic Materials
Not all materials respond the same way to an external field. The magnetization M is proportional to H for most materials (at least for small fields):
M=χmH
where χm is the magnetic susceptibility — a dimensionless number that tells you how easily a material magnetizes.
Material Type
χm
Behaviour
Example
Diamagnetic
Small and negative (≈−10−5)
Weakly repelled by a magnet; M opposes H
Water, copper, bismuth
Paramagnetic
Small and positive (≈10−5 to 10−3)
Weakly attracted; M aligns with H
Aluminium, oxygen gas
Ferromagnetic
Large and positive (≫1)
Strongly attracted; M can be huge and persists even after H is removed
Iron, nickel, cobalt
Why this formula?
Magnetic Materials & Magnetization: Why the Key Formulas Hold
Let's build this from the ground up — starting with what magnetization physically means, then deriving the formulas step by step.
1. What is Magnetization (M)?
Magnetization is the net magnetic dipole moment per unit volume of a material.
Inside a material, atoms act like tiny magnetic dipoles (due to electron spin and orbital motion).
Without an external field, these dipoles point randomly → net M=0.
When an external field H is applied, dipoles align partially → net M=0.
Definition:
M=volumenet magnetic dipole moment
Units: A/m (same as H).
2. The Fundamental Relation: B=μ0(H+M)
This is the master equation linking the three magnetic fields:
B = magnetic flux density (the total field inside the material)
H = applied magnetic field (due to free currents)
M = magnetization (response of the material)
μ0 = permeability of free space (4π×10−7 H/m)
Why this form?
Step 1: In vacuum, there is no material, so M=0. Then:
B=μ0H
Step 2: Inside a material, the dipoles themselves produce an additional field. The total B is the sum of:
The field due to free currents (μ0H)
The field due to bound currents (from aligned dipoles), which is μ0M
Hence:
B=μ0H+μ0M=μ0(H+M)
Key insight:M is not an independent field — it's the material's response to H.
3. Magnetic Susceptibility (χm) and Permeability (μ)
For linear, isotropic, homogeneous materials (most common in exams), magnetization is proportional to the applied field:
M=χmH
χm = magnetic susceptibility (dimensionless)
χm>0 for paramagnetic materials
χm<0 for diamagnetic materials
χm≫1 for ferromagnetic materials (but not linear!)
Derivation of relative permeability μr:
Substitute M=χmH into the master equation:
B=μ0(H+χmH)=μ0(1+χm)H
Define:
μr=1+χm(relative permeability)
μ=μ0μr(absolute permeability)
Thus:
B=μH
Why this matters: It shows that the material simply scales the applied field by a factor μr.
4. Why χm Has Different Signs (Physical Reasoning)
Material Type
χm
Why?
Diamagnetic
χm<0 (small, ~10−5)
Applied field induces opposing dipole moments (Lenz's law at atomic level). M opposes H.
Paramagnetic
χm>0 (small, ~10−3)
Permanent atomic dipoles align partially with H. Thermal agitation fights alignment.
Inside the solenoid, H=nI is fixed entirely by the free (coil) current and does not care about the core, so H stays essentially unchanged as the core is heated through Tc. But B=μ0μrH collapses drastically because μr falls from 1000 to nearly 1 once the core stops being ferromagnetic - matching options (a) and (d).
Setting up the numbers
Given: n=1000turns/m, I=1A, and (below Tc) μr=1000.
The magnetising field H
Ampere's law for a long solenoid gives the magnetising field purely from the free current in the coil:
H=nI=(1000)(1)=1000A/m.
This expression never involves the core at all - H is set only by the current and the winding density, so it is (nearly) unchanged whether the core is ferromagnetic or not. This confirms the first half of option (a).
The magnetic field B
Below Tc (ferromagnetic core, μr=1000):
Bbelow=μ0μrH=(4π×10−7)(1000)(1000)≈1.26T.
Above Tc (core no longer ferromagnetic, μr→ nearly 1 - the material becomes ordinary paramagnetic material):
Babove=μ0(1)H=(4π×10−7)(1000)≈1.26×10−3T.
So B drops by roughly a factor of 1000 - a drastic decrease, while H is unchanged. This is exactly option (a): "the H field is (nearly) unchanged but the B field decreases drastically." Option (b), that both H and B stay nearly unchanged, is therefore false (B changes hugely).
Method: Tracking H, B, and M Through a Core-Material Change
Use this method whenever a solenoid or toroid's core undergoes a change — heated past its Curie temperature, swapped for a different material, etc. — and you must determine what happens to H, B, and M.
Steps
Step 1: Identify what is fixed by the external circuit
The magnetising field for a long solenoid, H=nI, depends only on the free (coil) current and the winding density — it is set entirely by the external circuit and does not depend on what the core is made of. If n and I are unchanged, H stays unchanged, whatever happens to the core.
Step 2: Identify what depends on the core's relative permeability
B=μ0μrH
μr is a property of the core material. When the material's magnetic character changes (e.g. ferromagnetic → paramagnetic above Tc), μr can change by orders of magnitude, so B changes by that same factor even though H does not.
Step 3: Compute magnetisation from B=μ0(H+M), i.e. M=(μr−1)H …