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AP® Physics 2: Algebra-Based · Unit 12 · Topic 12.1

Magnetic Fields: Revision Notes (Physics 2 12.1)

One-page recap of magnetic fields: dipoles and closed field loops, no monopoles, compasses, ferro-, para- and diamagnetism, Earth's dipole field and permeability.

Short on time? This page is the recap. For explanations, Figure 1 and the worked examples, use the full study guide.

Recap

  • A magnetic field B is a vector field (unit: tesla, T). It is used to find forces on moving charges, currents and magnetic materials.
  • Fields come from dipoles, never from a lone pole. Cutting a magnet gives two smaller dipoles.
  • Like poles repel; unlike poles attract.
  • B points the way the north end of a compass points. A compass (a dipole) tends to line up with the field.
  • A dipole’s field gets weaker with distance.
  • Dipoles come from moving charge: electrons orbiting and spinning in atoms.
  • Permanent and induced magnetism are both alignment of dipoles in a system. Induced alignment disappears when the external field goes.
  • Earth is modelled as a dipole. The magnetic pole near the geographic North Pole is a magnetic south pole.

Key relationships

Idea What to remember
Field-line rules direction = tangent and arrow; closer lines = stronger B; lines never cross; every line is a closed loop
Bar magnet outside: away from N, into S; inside: S to N
Adding fields B_total is the vector sum; for perpendicular parts, B = √(B₁² + B₂²), angle from B₂ = tan⁻¹(B₁/B₂)
Vacuum permeability μ₀ = 4π × 10⁻⁷ T·m/A ≈ 1.26 × 10⁻⁶ T·m/A (a constant)
Materials ferromagnetic μ ≫ μ₀; paramagnetic μ slightly > μ₀; diamagnetic μ slightly < μ₀
Material type Examples In a field Afterwards
Ferromagnetic Fe, Ni, Co domains align, strong attraction can stay magnetised
Paramagnetic Al, Ti, Mg weak alignment with B, weak attraction alignment lost
Diamagnetic all materials (main effect in Cu, water) weak alignment against B, weak repulsion nothing left

Assumptions behind the answers

  • “Direction of B” means the direction the north end of a small compass would point.
  • Earth’s field is treated as a dipole field; real Earth’s field is only approximately a dipole.
  • A material’s permeability μ is not a constant: it varies with temperature, orientation and field strength.

Mistakes to avoid

  1. Stopping field lines at the poles. Continue them inside, S to N.
  2. Saying a cut magnet gives a separate N piece and S piece.
  3. Calling Earth’s Arctic magnetic pole a north pole.
  4. Saying magnets attract all metals.
  5. Treating field lines as the paths of moving charges.
  6. Giving a magnetic force to a charge at rest.

Quick self-check

  1. Earth’s field somewhere is 5.0 × 10⁻⁵ T. What is that in μT? (50 μT)
  2. Which way does B point inside a bar magnet? (From the S end to the N end.)
  3. A sample is weakly pushed away from both poles of a strong magnet. What kind of material is it? (Diamagnetic.)

Next: practice questions.

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