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Capstones in : 3.

3.1. Lorentz Law 3.2. Biot-Savart law and ’s law 3.3. Magnetic vector potential 3.4. Magnetic 3.5.

©2005 Oregon State University Philip J. (revised by Yun-Shik Lee) Magnetostatics page 3.2

3.1 LAW Lorentz force on a Q is F(r) = Q [E(r) + v ×B(r) ] Work done by the fields when particle moves by dr = v dt is dW = dr •F(r) = Q dt [E(r)•v +v •(v ×B(r) )] =Q dt E(r)•v (vanishes, since v ⊥v ×B ) † IDEALIZED CURRENTS THE IDEALIZATION OF THE WIRE = line λ J dA dL = I dL I = current dL ρ dA dL = λ dL ρ = charge density v = average velocity dA J = = ρ v

dFmagnetic = I dL × B(R) , Fmagnetic = I ∫ dL × B(R)

THE IDEALIZATION OF THE SHEET

K = surface current density J dA dd = K d A

σ = surface charge density ρ dA dd = σ d A

ρ = charge density d A v = average velocity d d J = current density = ρ v

dFmagnetic = dA K × B(R) , Fmagnetic = ∫ dA K × B(R)

©1999 Oregon State University Capstones in Physics Philip J. Siemens Magnetostatics page 3.3

3.2. BIOT-SAVART LAW AND AMPERE’S LAW

3.2.A. Biot-Savart law for B due to current distribution J steady state case: assume charge density ρ and current J independent of time; then E and B are also time independent May also be useful approximation when slowly varying! In this case the for E and B decouple: E depends only on ρ, B depends only on J

dvol = d3 R = dX dY dZ dQ = ρ dvol J = ρ V R J(R) ⇓ r–R V dQ = J dvol r

µo for time-independent sources, B(r) = d3R J(R)×(r−R)/|r−R|3 4π ∫ proof: check ∇ • B = 0, ∇ × B = µoJ important special case: thin wire, dA, total current I = J dA d3R J(R) = dL dA J = I dL where dL = path element

©1999 Oregon State University Capstones in Physics Philip J. Siemens Magnetostatics page 3.4

BIOT-SAVART EXAMPLE µoI B(r) = dL×(r−R)/|r−R|3, z 4π ∫ dL = dZ = zˆ dZ, I r R =Z = Z zˆ r–R = r –Z zˆ , R r - R z ˆ × (r –Z zˆ ) = zˆ × r, |r–R|2=r⊥2+Z2 ∞ 1 µ0I µ0I  2  µoI B(r) = ( zˆ ×r) dZ 3/ 2 = ( zˆ ×r)  = φˆ 4π ∫ 2 2 4π  2  2π|r | −∞ ()r⊥ + Z  r⊥  ⊥ check: ∫ dL •B = µo I on a circular path centered on the wire

3.2.B. AMPERE’S LAW

r r The for the curl of B : ∇ × B = µ0 J

r r r r ∇ × B ⋅ dar = B ⋅ dl = µ J ⋅ dar = µ I Stokes theorem : ∫ ( ) ∫ 0 ∫ 0

A much simpler way to find B

When the source distribution has lots of , we can often use Ampere's law directly to find the magnetic

Example: straight-line currents we can argue from symmetry that the field B(r)

• is independent of φ or z , so it depends only on r⊥ + ρ , B(r) = B(ρ) • is in the azimuthal direction, along φˆ B(ρ) = φˆ B(ρ) To find the remaining unknown function B(ρ) ,

©1999 Oregon State University Capstones in Physics Philip J. Siemens Magnetostatics page 3.5

we apply Ampere's law to a cleverly chosen path chosen so that it is • either along the field direction, but with constant field, or • perpendicular to the field

A circular path of radius ρ centered on the wire has dL = φˆ ρ dφ, µoI dL •B =⌠2πdφ ρ φˆ • φˆ B(ρ) = 2πρ B(ρ) = µ I ⇒ B(ρ) = ∫ ⌡0 o 2πρ

Example

Toroidal coil square cross section c N turns, current I a following Lorraine, Corson & Lorraine b Apply Ampere's cicuital law in form to paths: ∫ dL •B = µo ∫ dA •J = µoIenclosed paths a, b and c: dL is azimuthal, so ∫ dL •B = 2πρ Bφ where ρ is the radius of the path µo dL •B = µ dA •J = µ I , so B = I ∫ o ∫ o enclosed φ 2πρ enclosed path a: can find a surface bounded by this path with no current penetrating it, so Bφ =0. path c: likewise Bφ =0; note the surface can be chosen at will, only its boundary is fixed. For example, choose a plane surface, then equal currents flow up and down through the surface µo path b: current penetrating surface is NI , so B = ΝI φ 2πρ

©1999 Oregon State University Capstones in Physics Philip J. Siemens Magnetostatics page 3.6

3.3. MAGNETIC VECTOR POTENTIAL Because ∇ • B = 0, there exists a vector function A such that B = ∇ × A The ampere’s law r r r 2 r r ∇ × B = ∇ × (∇ × A)= ∇(∇ ⋅ A)− ∇ A = µ0 J You can add to the magnetic potential any function whose curl vanishes with no effect on B. ⇒ ∇ • A = 0 2 r r The Ampere’s law becomes ∇ A = −µ0 J : Poisson’s equation. r r r r µ0 J (R) 3 r A()r = r d R Therefore, 4π ∫ rr − R

For line and surface currents r r r r r r µ0 I µ0 I dl r r µ0 K()R A()r = r dl = r ; A()r = r da 4π ∫ rr − R 4π ∫ rr − R 4π ∫ rr − R

Mutipole expansion of the vector potential r r µ I dl µ I ∞ 1 r A()rr = 0 = 0 Rn P (cosα)dl ∫ r r ∑ n+1 ∫ n 4π r − R 4π n=0 r

µ0 I 1 r 1 r  = dl + 2 Rcosα dl +L 4π r ∫∫r  r µ I r µ I r r µ I A ()rr = 0 Rcosα dl = 0 rˆ⋅ Rdl = − 0 rˆ× dar dip 4πr 2 ∫ 4πr 2 ∫ 4πr 2 ∫ r µ mr ×rˆ A ()rr = 0 mr = I dar = I ar ⇒ dip 4π r 2 where ∫

©1999 Oregon State University Capstones in Physics Philip J. Siemens Magnetostatics page 3.7

3.4. MAGNETIC DIPOLE

3.4.A. MAGNETIC

SIMPLE DIPOLE: a loop of current I, area a of simple loop dipole moment is m =– I a

Far field has same pattern as electric dipole

1 3 more generally, m = 2 ∫ d R R × J(R) , which is independent of origin.

Dipole magnetic vector potential and field µ m×rˆ A ()rr = 0 dip 4π r 2 µ µ m B(r) = 0 []3(m ⋅ r))rˆ − m = 0 (2rˆcosθ + zˆsinθ ) 4π r3 4π r3 for r → ∞, m || zˆ

©1999 Oregon State University Capstones in Physics Philip J. Siemens Magnetostatics page 3.8

SIMPLE LOOP: a loop of current I, area dS = πa2 z µoI compute B(r)= dL×(r−R)/|r−R|3 4π ∫ coordinates: choose y = 0, r L in xy plane ⇒ Az = 0, θ dL = a dφ φˆ = a dφ(–xˆ sinφ+yˆ cosφ) symmetry ⇒ By = 0 ψ a y dipole moment is L m + I dS = I πa2 zˆ x φ dL numerator: dL × (r–L) = dL × r – dL × L ; substitute r = x xˆ + z zˆ → dL × (r–L) = a dφ {x (–zˆ cosφ) +z(–yˆ sinφ + xˆ cosφ)} + a2 dφ zˆ the yˆ component integrates to zero by symmetry, so we can use dL × (r–L) → a dφ { (z cosφ)xˆ + (a –x cosφ) zˆ } denominator: |r–L|2 = r2+a2 – 2a r cos ψ = r2+a2 – 2a x cos φ since r cos ψ = projection of r along L = x cos φ far away: look at r »a , let ε + a/r « 1, then 1 1 x 1 x = (1–2ε cosφ+ε2) –3/2≈ (1+3ε cosφ) |r–L|3 r3 r r3 r µoIa x ⇒ B(r) ≈ ⌠2πdφ {(z cosφ) xˆ + (a –x cosφ) zˆ } ( 1+ 3ε cosφ ) 4πr3 ⌡0 r x z now ⌠2πdφ = 2π, ⌠2πdφ cosφ = 0, ⌠2πdφ cos2φ = π, = sinθ, = cosθ ⌡0 ⌡0 ⌡0 r r µoIa xz x2 µoIa2 B(r)≈ 3ε xˆ +(2a –3ε )zˆ = 3sinθ cosθxˆ +(2–3sin2θ)zˆ 4r3 { r r } 4r3 { } µoIa2 but rˆ = sinθ xˆ + cosθ zˆ , so B(r) ≈ 3cosθ rˆ –zˆ , or 4r3 { } µo B(r) ≈ 3(m•rˆ ) rˆ –m 4πr3 { }

©1999 Oregon State University Capstones in Physics Philip J. Siemens Magnetostatics page 3.9

3.4.B. TORQUE ON A DIPOLE dipole moment m = I A

Force on dL(R) is dL dF(R) = I dL(R)×B

dA Torque on dL = R×dF(R) Total torque τ = I ∫ R×(dL(R)×B) vector identity 2: τ = I ∫ [ dL(r)(r • B) – B (dL(r) •r) ]

1 2 last term integrates out: r = 2 ∇(r ) consider part of τ proportional to Bx :

dL(r) = dr ⇒ I Bx ∫ dL(r) x = I ∫ dr x

= I Bx ∫(xˆdx + yˆdy + zˆdz)x

ˆ ˆ ˆ = I Bx (x∫ xdx + y∫ xdy +z∫ xdz)

= I Bx(xˆ ( 0 ) + yˆ Az – zˆ Ay) compare m × B = I A × B , part proportional to Bx is

I ( yˆ Az – zˆ Ay) Bx √

©1999 Oregon State University Capstones in Physics Philip J. Siemens Magnetostatics page 3.10

3.5. MAGNETIZATION

INTRINSIC MAGNETIC MOMENTS

Properties of elementary particles include:

1 • (quantized in units 3 e ) • Mass = in rest frame/c2 (no known natural unit)

• Angular (quantized in units − h /2 = h /π)

(no known natural unit)

– always parallel to the intrinsic – both are relativistic effects, arise in Dirac's theory

NUCLEI AND HAVE MAGNETIC MOMENTS

They arise partly from the intrinsic moments of the and , nucleus and partly from their in little current loops.

Result: every material has a magnetic moment per m

©1999 Oregon State University Capstones in Physics Philip J. Siemens Magnetostatics page 3.11

Magnetization M = m N , where m = magnetic moment per molecule N = number of per unit volume dipole m at R → dvol = d3 R magnetic field = dX dY dZ r r µ0 3(m • rˆR )rˆR − m B (r) = r m 4π | r − R |3 R M(R) r r − R Where rˆR = r r–R | r − R | r magnetization M(R) →

r r µo µ0 3(M • rˆR )rˆR − M field B (r) = d3R r M 4π ∫ 4π | r − R |3 Note M takes account of both • the intrinsic moments • motion of the bound charges. EFFECTIVE CURRENTS calculate (with some difficulty) ∇ × BM(r) = µo ∇ × M (r) + µoJpol(r) The field can be thought of as arising from an "effective current" Jpol(r) In addition to the fields and potentials due to M, there are other sources: • free currents Jfree • polarization current Jpol= ∂P/∂t due to the electric dipole density P see "Surface Polarization"(in Notes on Electrodynamics) Conclusion: the magnetic field arises from an effective current density Jeffective = ∇× M and the surface current density αeffective = M× nˆ in addition to the free current density Jfree and the polarization current Jpol= ∂P/∂t

©1999 Oregon State University Capstones in Physics Philip J. Siemens Magnetostatics page 3.12

3.5.A. MAGNETIC FIELD STRENGTH H

Inside magnetic materials ∇×B/µo = Jtotal = Jfreel+∇× M so

B Jfree = ∇× H where H = – M (units ) µo meter compare , ρfree = ∇•D , D + εoE + P integral form: use Stokes' theorem ⇒ ∫ H • dL = ∫ J•dA = Ifree the free current enclosed

at the surface of a magnetic material • integrate ∇•B = 0 over thin Gaussian volume B,H ∫dvol ∇•B = 0 B,H A (Stokes) ∫dSB • nˆ normal = 0 S(B –B ) = 0 outer⊥ inner⊥ α • loop surface L ∫ H •dL = Ifree positive B, H L(Houter||–Hinner||) = Ifree

⇒ B⊥, H|| are continuous see "Core Example"

DEFINITIONS AND NOTATION (linear response) • χm M = χm H • Permeability µ B = µ H • Relative permeability µrel = µ/µo = 1 + χm • Main equation B = µo(H + M) warning: ferromagnetic materials are not linear

©1999 Oregon State University Capstones in Physics Philip J. Siemens Magnetostatics page 3.13

CORE EXAMPLE

Wind a long on a magnetic core, N = N' L turns

L Ampere: ∫ H • dL = Ifree symmetries ⇒ choose path shown (Hin –Hout)|| L = N'IL independent of how far outside ⇒ Hout ≈ 0 ⇒ Hin ≈ N'I independent of where inside! I N' Bin = µHin ≈ µN'I > µoHin contrast capacitor, Ein = Din/ε < Din/εo

©1999 Oregon State University Capstones in Physics Philip J. Siemens Magnetostatics page 3.14

3.5.B.

A ferromagnet consists of microscopic domains, in each of which the atomic magnetic moments are lined up. a. If a ferromagnet is heated to a high enough temperature T ≥ TCurie and then cooled, the domains are randomly oriented. Thus the net magnetization is zero. b. An applied external field makes • the domains aligned with the field grow, • the domains with the wrong orientation shrink. This causes the magnetic (kinetic) energy to increase. see “Field Kinetic Energy”

H H = 0 H H c. When most of the domains are roughly aligned, a still stronger field causes the domains to align completely. d. Application of a larger external field produces no additional magnetization.

see “Hysteresis”

©1999 Oregon State University Capstones in Physics Philip J. Siemens Magnetostatics page 3.15

HYSTERESIS

Once a ferromagnet has been placed in a large field, it remains magnetized even when the external field is removed, because the alignment of the domains has increased the magnetic kinetic energy.

The residual field is the remanence. B full alignment domain To decrease the internal field to zero, existing boundaries domains move an external field must be applied. realign

H coercive The needed external field is the force coercive force. remanence

Energy stored in = ∫dB•H= area under B – H curve. In each cycle, energy is lost: Elost = area inside curve.

©1999 Oregon State University Capstones in Physics Philip J. Siemens Magnetostatics page 3.16

THE BAR MAGNET with uniform magnetization M || to its sides is equivalent to a solenoid with a current density N'I = M equal to the surface current.

Its external field flows from north pole to south.

N' B forms closed loops I through the interior; S N outside the magnet, H = B, but inside the magnet H is opposed to B !!!

• ∫ H•dL = 0, consider integral along line of B. • H|| must be continuous through the side of the magnet, where B reverses direction.

©1999 Oregon State University Capstones in Physics Philip J. Siemens