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Lecture 1 Vector algebra: A brief review

Outline

1. Scalars and Vectors

2. Unit vectors

3. Position and distance vectors

4. Algebraic operations with vectors: addition, pair and triple products.

5. Vector projections

1

• Scalar quantities have only magnitudes (mass, pressure, temperature, speed,distance, charge, potential)

• Vector quantities have both magnitudes and directions (velocity, force, electric�eld).

Any vector in terms of coordinates, A = (Ax, Ay, Az)

a =A

|A| ,⇐⇒, unit vector;

the magnitude by Pythagorus' theorem

|A| =√

A2x + A2

y + A2z.

Alternative representation,

A = (Ax, Ay, Az) ⇐⇒ A = Axax + Ayay + Azaz.

a =Axax + Ayay + Azaz√

A2x + A2

y + A2z

.

2

Vector addition

C = A±B ⇐⇒ C = (Ax ±Bx)ax + (Ay ±By)ay + Az ±Bz)az.

Position vector

rP = xax + yay + zaz

Distance vector

rPQ = rQ − rP = (xQ − xP )ax + (yQ − yP )ay + (zQ − zP )az

3

Dot Product

A ·B = |A||B| cos θAB = AxBx + AyBy + AzBz.

Properties:

• A ·B = B ·A, commutativity,

• A · (B + C) = A ·B + A ·C, distributivity

• A ·A = |A|2

Corollaries:|A| =

√A ·A.

ai · aj =

0, i 6= j = x, y, z

1, i = j = x, y, z,

4

Cross Product

A×B = |A||B| sin θABan.

A×B =

∣∣∣∣∣∣∣∣

ax ay az

Ax Ay Az

Bx By Bz

∣∣∣∣∣∣∣∣Properties:

• A ·B = −B ·A, anti-commutativity,

• A× (B + C) = A×B + A×C, distributivity

• A×A = 0

Corollaries:ai · aj = ak, i, j, k = x, y, z, cyclic permutations

For example, ax × ay = az , az × ax = ay.

5

Example 1. Let A = αax + 3ay − 2az and B = 4ax + βay + 8az . Find α and β

such that (i)A ‖ B, (ii)A⊥B.Example 2 Show that (A ·B)2 + (A×B)2 = (AB)2.

Triple Products

Scalar:A · (B×C) = B · (A×C) = C · (A×B).

A · (B×C) =

∣∣∣∣∣∣∣∣

Ax Ay Az

Bx By Bz

Cx Cy Cz

∣∣∣∣∣∣∣∣.

Vector:A× (B×C) = B(A ·C)−C(A ·B).

Example 3 Show that

ax =ay × az

ax · ay × az

.

Example 4 Simplify the expressions (a)A× (A×B), (b)A× [A× (A×B)].

6

Scalar component of A in direction of a:

A‖ = |A| cos θ = |A||a| cos θ = A · a.

Vector components of A, parallel and perpendicular to a:

A‖ = (A · a)a,

A⊥ = A− (A · a)a

Example 5 Show that A⊥⊥a.Example 6 Given H = 2xyax − (x + z)ay + z2az , �nd a unit vector parallel to H atP (1, 3,−2).

7

Lecture 2 Vector calculus: Part I

Outline

1. Del Operator.

2. Gradient of a scalar �eld.

3. Flux of a vector �eld.

4. Divergence of a vector �eld and divergence theorem

8

The del operator, denoted∇ is given by the expressions

∇ = ax∂

∂x+ ay

∂y+ az

∂z, (Cartesian);

∇ = aρ∂

∂ρ+ aφ

1

ρ

∂φ+ az

∂z, (cylindrical);

∇ = ar∂

∂r+ aθ

1

r

∂θ+ aφ

1

r sin θ

∂φ, (spherical).

1. The gradient of a scalar, grad V ≡ ∇V .

2. The divergence of a vector, div E ≡ ∇ · E, (Cartesian coordinates only).

3. The curl of a vector, curl A ≡ ∇×A, (Cartesian coordinates only).

9

Gradient

The vector separation of the points M and N :

dr = axdx + aydy + azdz. (1)

10

The scalar �eld V change in going from M to N :

dV =∂V

∂xdx +

∂V

∂ydy +

∂V

∂zdz. (2)

11

Introduce the gradient of the scalar �eld V to be a vector �eld such that

grad V ≡ ∂V

∂xax +

∂V

∂yay +

∂V

∂zaz. (3)

dV =

(∂V

∂xax +

∂V

∂yay +

∂V

∂zaz

·(axdx + aydy + azdz) = grad V · dr. (4)

gradV lies in the direction of maximum increase of V !

It follows from the de�nition of the Del operator that

grad V = ∇V.

12

Alternative interpretation of the gradient:

• dV = 0 =⇒ ∇V⊥dr.

• dr is a tangent to the surface V (x, y, z) = const =⇒ ∇V ‖an, (an · dr = 0).

The gradient of V is a vector �eld that is everywhere normal to the surfaceV (x, y, z) = const!

13

Gradient in curvilinear coordinate systems:

∇V =∂V

∂xax +

∂V

∂yay +

∂V

∂zaz; (Cartesian),

∇V =∂V

∂ρaρ +

1

ρ

∂V

∂φaφ +

∂V

∂zaz; (cylindrical),

∇V =∂V

∂rar +

1

r

∂V

∂θaθ +

1

r sin θ

∂V

∂φaφ. (spherical).

Example 1 Find the gradient of the �eld V = E0r cos θ.

14

Outward �ux of a vector �eld

The outward �ux Ψ of a vector �eld D through a closed surface is de�ned as

Ψ ≡∮

S

D · dS =

S

D · andS.

15

Divergence of vector �elds

The divergence of A at a point P is the outward �ux per unit volume in the limit∆v → 0:

divA ≡ lim∆v→0

∮SA · dS∆v

= lim∆v→0

∮SA · andS

∆v

16

Physical interpretation of divergence:

• measure of the �eld divergence at a point,

• measure of the �eld source/sink strength per unit volume (source/sink density).

17

In curvilinear coordinate systems:

∇ ·A =∂Ax

∂x+

∂Ay

∂y+

∂Az

∂z; (Cartesian),

divA =1

ρ

∂(ρAρ)

∂ρ+

1

ρ

∂Aφ

∂φ+

∂Az

∂z; (cylindrical),

divA =1

r2

∂(r2Ar)

∂r+

1

r sin θ

∂(Aθ sin θ)

∂θ+

1

r sin θ

∂Aφ

∂φ; (spherical).

Example 2 Find the divergence of the position vector (a) in Cartesian coordinates and(b) in spherical coordinates.Example 3 Determine the divergence of the �eld B = (k/ρ)aφ.

∇ · F = 0 ⇐⇒ F is solenoidal.

18

Note: divA 6= ∇ ·A in cylindrical and spherical coordinates!!

For, example, in cylindrical coordinates

divA =1

ρ

∂(ρAρ)

∂ρ+

1

ρ

∂Aφ

∂φ+

∂Az

∂z;

by the same token,

∇ ·A =

(aρ

∂ρ+ aφ

1

ρ

∂φ+ az

∂z

)· (Aρaρ + Aφaφ + Azaz)

=∂Aρ

∂ρ+

1

ρ

∂Aφ

∂φ+

∂Az

∂z6= divA! (5)

Note: even though divA 6= ∇ ·A in curvilinear coordinates, we use∇ ·A instead ofdivA for notational simplicity!

19

Divergence theorem (Gauss-Ostrogradsky theorem)

Divergence theorem: The total outward �ux of a vector �eld A through a closedsurface = the volume integral of divergence of A.

Example 4 Verify Gauss's theorem for the �eld F = krar and the spherical shellsurface, R1 ≤ r ≤ R2.

20

Lecture 3 Vector calculus: Part II

Outline

1. Laplacian of scalar and vector �elds

2. Circulation of a vector �eld

3. Curl of a vector �eld

4. Stokes's theorem

21

Laplacian of scalar and vector �elds

Laplacian of a scalar �eld:

∇2V ≡ div (gradV ) .

In Cartesian coordinates,

∇2V = ∇ · ∇V =

(ax

∂x+ ay

∂y+ az

∂z

·(

∂V

∂xax +

∂V

∂yay +

∂V

∂zaz

). (6)

Hence,

∇2V =∂2V

∂x2+

∂2V

∂y2+

∂2V

∂z2.

22

In cylindrical coordinates:

∇2V =1

ρ

∂ρ

(ρ∂V

∂ρ

)+

1

ρ2

∂2V

∂φ2+

∂2V

∂z2;

In spherical coordinates:

∇2V =1

r2

∂r

(r2∂V

∂r

)+

1

r2 sin θ

∂θ

(sin θ

∂V

∂θ

)+

1

r2 sin2 θ

∂2V

∂φ2.

Laplacian of a vector �eld (rational: div(gradA) doesn't make sense!):

∇2A ≡ grad (div A)− curl curlA.

23

Circulation of a vector �eld

The circulation of a vector �eld A along a closed path:

circulation of A along closed path L ≡∮

L

A · dl.

Note: if the path is not closed,∫

LA · dl is the circulation.

24

Curl of a vector �eldCurl of A: a vector �eld whose

• magnitude = maximum circulation of A per unit area as the area tends to zero;

• direction coincides with the unit normal to the area oriented so as to maximize thecirculation of A.

25

Mathematically,

curlA ≡(

lim∆S→0

∮LA · dl∆S

)

maxan.

Physically, curl

• (a) provides the maximum value of the circulation of a vector �eld per unit area and

• (b) indicates the direction along which the maximum is attained.

26

Curl in Cartesian coordinates

curlA = ∇×A =

∣∣∣∣∣∣∣∣

ax ay az

∂∂x

∂∂y

∂∂z

Ax Ay Az

∣∣∣∣∣∣∣∣or,

∇×A =

[∂Az

∂y− ∂Ay

∂z

]ax +

[∂Ax

∂z− ∂Az

∂x

]ay

+

[∂Ay

∂x− ∂Ax

∂y

]az. (7)

27

Curl in curvilinear coordinates

curlA =1

ρ

∣∣∣∣∣∣∣∣

aρ ρaφ az

∂∂ρ

∂∂φ

∂∂z

Aρ ρAφ Az

∣∣∣∣∣∣∣∣; (cylindrical).

curlA =1

r2 sin θ

∣∣∣∣∣∣∣∣

ar raθ r sin θaφ

∂∂r

∂∂θ

∂∂φ

Ar rAθ r sin θAφ

∣∣∣∣∣∣∣∣; (spherical).

Note: even though curlA 6= ∇×A in curvilinear coordinates, we use∇×A insteadof curlA for notational simplicity!Example 1 Calculate curl of (a) A = (k/ρ)aφ; (b) A = f(r)ar.

∇×A = 0 ⇐⇒A is irrotational/conservative.

28

Stokes's theorem

Stokes's theorem: The circulation of a vector �eld A around a path L = the surfaceintegral of curl of A over the surface bounded by L.

Example 2 Verify Stokes's theorem for A = sin(φ/2)aφ over the hemisphere surfaceand its circular contour lying in the plane z = 0.Example 3 Given F = (3y − c1z)ax + (c2x− 2z)ay + (c3y + z)az . Find c1, c2

and c3 such that F is irrotational.

29

Lecture 4 Coulomb's Law and Field Intensity

Outline

1. Electric charge, Coulomb's Law and superposition principle.

2. Electrostatic �eld intensity.

3. Electric �elds of continuous charge distributions

30

Coulomb's law and superposition principle

The force F between two point charges Q1 and Q2 is:

1. along the line joining the charges;

2. directly porportional to Q1Q2;

3. inversely proportional to the distance R12 = r1 − r2 between the charges.

Hence, force on charge Q1 due to Q2:

F12 = k︸︷︷︸constant

×Q1Q2

|R12|2 × aR12︸︷︷︸unit vector

=Q1Q2

4πε0|R12|2aR12 .

where the permittivity of free space

ε0 = 8.854× 10−12 [F/m ] (farads per meter).

31

F12 =Q1Q2

4πε0|R12|2aR12 =Q1Q2

4πε0|R12|2R12

|R12|︸ ︷︷ ︸aR12

=Q1Q2

4πε0|R12|3R12.

32

F12 =Q1Q2

4πε0|R12|2aR12 .

Note

1. aR21 = −aR12 =⇒ F21 = −F12

2.

sign(Q1) =

−sign(Q2) attraction,

sign(Q2) repulsion.

3. Q1 and Q2 are at rest.

33

Consider charges Q1, Q2 . . . QN at positions r1, r2, . . . rN .

Superposition principle. The force on a probe charge Q at r is

F =Q

4πε0

N∑

k=1

QkRk

|Rk|3 , Rk = r− rk.

Units:

• Charge=Coulombs, [C], 1C = 6× 1018 electronic charges (large unit!).

• Force=Newtons, [N].

34

Electric �eld intensity

The electric �eld intensity(or simply electric �eld)=force per unit charge:

E ≡ F

Q. (8)

Example. Force acting on a probe charge q at r due to Q at r′:

F =qQ

4πε0|R|2aR, R = r− r′. (9)

It follows from equations (8) and (9) that the electric �eld intensity at the position of q is

E = F/q =Q

4πε0|R|2aR.

Field at r due to Q1, Q2 . . . QN at r1, r2, . . . rN :

E =1

4πε0

N∑

k=1

QkRk

|Rk|3 , Rk = r− rk.

Units: Newton/Coulomb=Volt/meter.

35

Example 1 Calculate the electrostatic �eld of a dipole, consisting of two equal andopposite charges +Q and−Q, separated by a distance d, at a large distance from thedipole, r À d.

36

Electric �elds of continuous distributions of charges

Elementary (in�nitesimal) charge

dQ =

ρvdv volume charge

ρSdS surface charge

ρLdl line charge

37

Summing (integrating) contributions of elementary charges using the superpositionprinciple:

E =

∫ρvdv

4πε0|R|2aR, (volume charge).

E =

∫ρSdS

4πε0|R|2aR, (surface charge).

E =

∫ρLdl

4πε0|R|2aR, (line charge).

38

Lecture 5 Electric Flux Density and Gauss's Law

Introduce the electric �ux density �eld as

D ≡ ε0E,

and de�ne the electric �ux Ψ by the expression

Ψ =

∫D · dS.

Gauss's law. The total �ux Ψ through a closed surface S = total enclosed charge Qin:

Ψ =

S

D · dS = Qenc =

v

ρvdv (10)

39

Thus∮

S

D · dS =

v

ρvdv, (integral form of the �rst Maxwell's equation). (11)

Divergence theorem ∮

S

D · dS =

v

∇ ·Ddv. (12)

It follows by comparing Eqs. (11) and (12):

∇ ·D = ρv, (differential form of the �rst Maxwell's equation). (13)

40

Applications of Gauss's law to calculating electric �elds

Use∮

SD · dS = Qenc for charge distributions with

• spherical symmetry (example: sphere),

• axial symmetry (example: in�nite cylinder),

• re�ectional symmetry (examples: in�nite straight line, in�nite plane).

41

Choose a special Gaussian surface such that

1. The surface is closed.

2. At each point of the surface D is either normal or tangential to the surface.

3. D is constant over the parts of the surface where D‖an.

=⇒ ∮SD · dS = D × total area where D‖an!!

42

Example: a point charge

∮D · dS = D

∫ π

0

r2 sin θdθ

∫ 2π

0

︸ ︷︷ ︸4πR2

= Q;

E =D

ε0

=Q

4πε0r2ar.

43

Example Use Gauss's law to determine the electric �eld due to the following chargecon�gurations

• spherical shell of radius R carrying a charge Q;

• uniformly charged, with the density ρv, sphere of radius R;

• uniformly charged in�nitely long cylinder of radius a with the charge density ρv;

• in�nite straight line, carrying a charge ρl per unit length;

• in�nite plane charged with ρs per unit surface.

44

Lecture 6 Electrostatic potential

Outline

1. Work done to move a charge in an electric �eld. Electric potential.

2. Electric potentials of continuous charge distributions.

3. Relation between electric �eld and potential.

4. Example: potential of a dipole.

45

Motivation: why need potential?

Argument:

• It is easier to deal with a scalar potential then with a vector electric �eld.

• We will show that the latter can be obtained from the former.

46

Work done to move a charge in an electric �eld. Electric potential.

To keep a charge in equilibrium in the �eld E, a force Fa must be applied such that

Fa = −F = −QE.

47

The work done in displacing Q by dl is (work=force× displacement)

dW = Fa · dl = −QE · dl.

dl = dxax + dyay + dzaz, (Cartesian),

dl = dρaρ + ρdφaφ + dzaz, (cylindrical),

dl = drar + rdθaθ + r sin θdφaφ, (spherical).

48

Hence to move Q from A to B:

W = −Q

∫ B

AE · dl.

49

De�ne a potential difference as

VAB =W

Q= −

∫ B

AE · dl.

• VA and VB are referred to as the initial and �nal points.

• Units of VAB : [Joules/Coulomb=Volts].

• the work done by an external agent = change in potential energy of the charge in the�eld.

• VAB < 0 =⇒ work is done by the �eld; VAB > 0 =⇒ work is done by the externalagent.

50

Example: potential of a point charge

From Coulomb's law for the �eld due to a point charge at the origin:

E(r) =Q

4πε0r2ar

Hence, by de�nition

VAB = VB − VA = −∫ rB

rA

Q

4πε0r2ar

︸ ︷︷ ︸E

· drar︸︷︷︸dl‖

=Q

4πε0

(1

rB

− 1

rA

)(14)

Pick a reference point rA → const, and choose rB → |r| ≡ r:

V (r) =Q

4πε0r+ const.

51

Choose the convenient reference point at in�nity, rA →∞, const ∝ 1/rA → 0:

V (r) =Q

4πε0r, (charge at the origin).

Generalization. Potential at r due to a charge at r′: shifting the origin to the point r′;r → r− r′, so that

V (r) =Q

4πε0|r− r′| , (charge at r′).

Superposition of point charges. Potential at r due to charges Q1, . . . Qn at pointswith r1, . . . rn:

V (r) =1

4πε0

n∑

k=1

Qk

|r− rk| , (by superposition principle).

52

Potential due to continuous distributions of charge

V (r) =1

4πε0

L

ρL(r′)dl′

|r− r′| , (line charge);

V (r) =1

4πε0

S

ρS(r′)dS ′

|r− r′| , (surface charge);

V (r) =1

4πε0

v

ρv(r′)dv′

|r− r′| , (volume charge).

Example 1 Obtain an expression for the electric �eld potential and intensity on the axisof a uniformly charged disk of radius b with the charge density ρl.

53

Relation between electric �eld and potential.

The work done in moving a charge in time-independent (electrostatic) �eld isindependent of the path:

1

E · dl = −∫

2

E · dl, or∮

1−2

E · dl = 0. (15)

54

Stokes's theorem: ∮

1−2

E · dl =

S

∇× E · dS = 0 (16)

S

∇× E · dS = 0 =⇒ ∇× E = 0, (potentiality of electrostatic �elds)!

Two forms to represent the electrostatic potential:

V = −∫

E · dl, (integral form) ⇐⇒ dV = −E · dl (differential form).

55

For an in�nitesimally small length element dl = dr (straight line approximation).

dV = −E · dr.

Recall the de�nition of the gradient:

dV = ∇V · dr.

56

Thus,dV = −E · dr; dV = ∇V · dr. (17)

It follows from equation (17) that

E = −∇V, (connection between potential and �eld).

57

Example: potential due to a dipole

Dipole: two equal, opposite charges, separated by a small distance d.

Potential due to a dipole by superposition:

V =Q

4πε0

(1

r1

− 1

r2

)=

Q

4πε0

(r2 − r1)

r1r2

.

58

Consider the potential at a remote point, r À d:

r2 − r1 ' d cos θ; r1r2 ' r2, (in denomenator).

59

It follows that

V =Q

4πε0

d cos θ

r2,

d = daz =⇒ d · ar = d cos θ.

De�ne the dipole moment: p = Qd.

V =p · ar

4πε0r2.

The corresponding electric �eld:

E = −∇V =p

4πε0r3(2ar cos θ + aθ sin θ).

60

Lecture 7 Energy and Energy Density of Electrostatic Fields

Energy of assembly of charges = work done to assemble them.

• Move Q1 ⇒ P1, Q2 ⇒ P2, Q3 ⇒ P3 in this order.

61

• Vij : potential at Pi due to charge at Pj .

WE = W1 + W2 + W3 = 0︸︷︷︸no �eld

+Q2V21 + Q3(V31 + V32). (18)

Reverse the order of charge movement

WE = W1 + W2 + W3 = 0 + Q2V23 + Q1(V12 + V13). (19)

Adding (1) and (2) and grouping terms

2WE = Q1(V12 + V13) + Q2(V21 + V23)

+ Q3(V13 + V32) = Q1V1 + Q2V2 + Q3V3. (20)

WE =1

2(Q1V1 + Q2V2 + Q3V3). (21)

62

Generalizations

• N point chrages

WE =1

2

N∑

k=1

QkVk .

• Continuous distributions of charge

WE =1

2

L

ρLV dl, (line charge);

WE =1

2

S

ρSV dS, (surface charge);

WE =1

2

v

ρvV dv, (volume charge).

63

Energy density of the electrostatic �eld

WE =1

2

v

ρvV dv =1

2

vsphere

∇ ·D︸ ︷︷ ︸=ρv

V dv (22)

64

Use the vector identity

∇ · (V A) = A · ∇V + V∇ ·A ⇐⇒ (fg)′ = f ′g + fg′.

scalar �eld lhs=scalar �eld rhs.

WE =1

2

vsphere

∇ ·DV dv

=1

2

vsphere

∇ · (V D)dv − 1

2

vsphere

D · ∇V dv. (23)

Using divergence theorem,

1

2

vsphere

∇ · (V D)dv =1

2

Ssphere

V D · dS. (24)

65

As R →∞, (�nite charged volume = point charge) =⇒|D| ∝ 1/R2 V ∝ 1/R V D ∝ 1/R3 and surface area∝ R2.

Hence,

limR→∞

1

2

Ssphere

V D · dS = 0.

So that in the limit R →∞

WE = −1

2

∫D · ∇V︸︷︷︸

=−E

dv =1

2

∫(D · E)dv.

66

Since D = ε0E,

WE =1

2

∫(D · E)dv =

1

2

∫ε0E

2dv

The density of the �eld can be inferred from the de�nition

WE =

∫wE︸︷︷︸

density

dv

It follows that

wE =1

2(D · E) =

1

2ε0E

2 .

Example Determine the electrostatic energy needed to assemble a uniformly chargedsphere of radius R with the charge density ρv.

67

Lecture 8 Conductors and Dielectrics

• abundance of free charge carriers in conductors;

• no volume charge or electric �eld inside a conductor, ρv = 0, Ein = 0 ;

• E = −∇V = 0 =⇒ V = const , conductor=equipotential body.

Example 1 Two spherical conductors of radii R1 and R2, respectively carry a totalcharge of Q. The conductors are connected by a very long conducting wire. Find thecharges on the two spheres.

68

Polarization in Dielectrics

Dielectrics: positive nuclear charge (+Q) +negative electron charge, (−Q)=neutralatom.

Response of a dielectric to an applied electric �eld, E; p=dipole moment.

69

Classi�cation of dielectric materials

• nonpolar; p = 0 at E = 0 =⇒, dipole alignment at E 6= 0.

• polar; p 6= 0, even at E = 0, random orientation of permanent dipoles=⇒ dipoles rotate to align along E 6= 0.

70

Dipole moment of an individual atom (molecule):

p = Qd.

N dipoles in a small volume ∆v,

p =N∑

k=1

Qkdk.

De�ne the polarization as a dipole moment per unit volume,

P = lim∆v→0

∑Nk=1 Qkdk

∆v

71

Field due to a polarized dielectric

Starting with the potential dV due to an in�nitesimal polarized volume dv:

dV =

dp︷ ︸︸ ︷(Pdv′) ·aR

4πε0R2

where R =√

(x− x′)2 + (y − y′)2 + (z − z′)2,

72

we can demonstrate � see Appendix A � that the expression for the potential due topolarized charge,

V =

∫dv′(P · aR)

4πε0R2,

can be transformed into a volume and surface contributions as

V =

S′

ρps︷ ︸︸ ︷P · a′n4πε0R

dS ′ +∫

v′

ρpv︷ ︸︸ ︷−∇′ ·P4πε0R

dv′

ρps = P · an, polarization surface charge,

ρpv = −∇ ·P, polarization volume charge.

73

• surface polarization charge:

Q =

∫ρpsdS =

∮P · dS,

• volume polarization charge:∫

v

ρpvdv = −∫

v

∇ ·Pdvdivergence

= −∮

P · dS.

It follows ∫ρpsdS +

v

ρpvdv = 0, neutrality of dielectric!

74

Dielectric susceptibility and permittivity

Consider a dielectric region containing free charge of density ρv.

The total charge density ρt:

ρt = ρv + ρpvGauss= ∇ · (ε0E).

Hence,ρv = ∇ · (ε0E)− ρpv = ∇ · (ε0E + P)︸ ︷︷ ︸

D

.

De�ne the �ux density �eld in dielectric D:

D ≡ ε0E + P

∇ ·D = ρv , Gauss's law in dielectrics

75

De�ne the electric susceptibility χ by the expression

P = χε0E, if χ = scalar, D‖E.

De�ne the dielectric permittivity ε such that

D = ε0E + P = ε0(1 + χ)E = εE .

De�ne the relative permittivity as

εr = 1 + χ =ε

ε0

.

• εr and χ are dimensionless, while ε and ε0 are measured in [farads/meter].

Example 2 A positive charge Q is at the center of a spherical dielectric shell (ε = εrε0)of the inner and outer radii R1 and R2, R1 < R2. Determine E, D, P, ρps and ρpv.

76

ε is independent of the applied �eld E, of the position and direction withindielectric =⇒ linear, homogeneous, isotropic dielectric.

Energy density of the �eld in dielectric

w =1

2(D · E) =

1

2ε0εrE

2

Example 3 Let V (x, y, z) = x2y2z in a region de�ned by−1 < x, y, z < 1. Theregion is �lled with the dielectric ε = 2ε0. Determine the volume charge density ρv

within the region.Example 4 A solid sphere of radius a and dielectric constant εr has a uniform volumecharge density ρ0. Show that the potential at the center of the sphere is given by

V =ρ0a

2

6εrε0

(2εr + 1).

77

Lecture 9 Boundary conditions in electrostatics

Outline

1. Dielectric-dielectric interface boundary conditions. Law of refraction.

2. Conductors: a brief overview

3. Dielectric-conductor interface boundary conditions

78

Introductory comments

Boundary conditions take place at the interface separating two different media.

• Decompose the �eld E into normal (to the interface) and tangential (to theinterface) components on both sides of the interface

Ej = Ejn + Ejt, j = 1, 2.

• Use Maxwell's equations:∮

E · dl = 0; (potentiality of electrostatic �eld),

∮D · dS = Qencl; (Gauss's law).

79

Dielectric-dielectric boundary conditions

Apply∮

E · dl = 0 to the closed path abcda:

E1t∆w − E1n∆h

2− E2n

∆h

2

−E2t∆w + E2n∆h

2+ E1n

∆h

2= 0. (25)

80

It follows from Eq. (40) that as ∆h → 0,

E1t = E2t . (26)

D = εE =⇒ Dt = εEt.

Thus,D1t

ε1

=D2t

ε2

.

• Tangential component of the �eld is continuous across the interface.

• Tangential component of the �ux density is discontinuous across the interface.

81

Use Gaussian surface in �gure (b) to get

∆Qencl = ρS∆S = D1n∆S −D2n∆S.

ThusD1n −D2n = ρS . (27)

82

In the absence of the free charge on the surface, ρS = 0,

D1n = D2n . (28)

Since D = εE,ε1E1n = ε2E2n.

• Normal component of the �eld is discontinuous across the interface.

• Normal component of the �ux density is continuous across the interface in theabsence of free surface charge.

Example 1 A dielectric sheet with εr is introduced into a uniform �eld E = E0ax in freespace. Find E, D and P inside the dielectric sheet.

83

Refraction of the electric �eld at the interface of two dielectic media

E1t = E2t =⇒ E1 sin θ1 = E2 sin θ2,

84

D = εE =⇒ Dn = εEn

D1nno free charge

= D2n =⇒ ε1E1 cos θ1 = ε2E2 cos θ2.

85

E1 sin θ1 = E2 sin θ2, (29)

ε1E1 cos θ1 = ε2E2 cos θ2. (30)

Dividing Eq. (38) by eq. (37) term by term,

tan θ1

ε1

=tan θ2

ε2

⇐⇒ tan θ1

tan θ2

=ε1

ε2

. (31)

• law of refraction of the �eld at a boundary free of surface charge.

Example 2 Work out the magnitude of E2 in terms of E1 as well.

86

Brief overview of conductors

• abundance of free charge carriers;

• no volume charge or electric �eld inside a conductor, ρv = 0, Ein = 0 ;

• E = −∇V = 0 =⇒ V = const , conductor=equipotential body.

87

Dielectric-conductor boundary conditions

Consider a circulation of E along the contour abcda (E = 0 inside conductor)

Ein=0︷︸︸︷0 ×∆w − 0× ∆h

2+ En

∆h

2

−Et∆w − En∆h

2+ 0× ∆h

2= 0. (32)

88

As ∆h → 0,Et = 0 . (33)

Applying Gauss's law to the �ux across the interface,

∆Qencl = ρS∆S = Dn∆S − 0×∆S,

Dn = ρS . (34)

• The electric �eld outside of a conductor is normal to its surface,

Et = 0, En = ρS/ε

89

Lecture 10 Poisson and Laplace equations

Outline

1. Poisson equation.

2. Laplace equation

3. Uniqueness of the solution to Laplace equation

90

Poisson and Laplace equations

Recall Gauss's law in differential form,

∇ ·D = ∇ · ( εE︸︷︷︸D

) = ρv. (35)

The potential V is de�ned asE = −∇V. (36)

On substituting from Eq. (44) into Eq. (43), we obtain a general form of the Poissonequation

∇ · (−ε∇V ) = ρv . (37)

Only If ε = const (homogeneous, isotropic, linear dielectric media),

∇2V = −ρv

ε. (38)

91

In the absence of charge, ρv = 0, Poisson's equation reduces to Laplace's equation:

∇ · (ε∇V ) = 0 . (39)

Only If ε = const (homogeneous, isotropic, linear dielectric media),

∇2V = 0 . (40)

92

Laplace's equation in curvilinear coordinates

∇2V = 0 :

∂2V

∂x2+

∂2V

∂y2+

∂2V

∂z2= 0

1

ρ

∂ρ

(ρ∂V

∂ρ

)+

1

ρ2

∂2V

∂φ2+

∂2V

∂z2= 0 ,

1

r2

∂r

(r2∂V

∂r

)+

1

r2 sin θ

∂θ

(sin θ

∂V

∂θ

)+

1

r2 sin2 θ

∂2V

∂φ2= 0 .

Uniqueness theorem: A solution to Poisson's equation satisfying given boundarycondition(s) is unique.

93

Example 1 Find the electrostatic potential inside an in�nite strip, 0 ≤ z ≤ a of aninhomogeneous dielectric medium with the dielectric constant εr(z) = εr0/(1 + z/a).The potential satis�es the boundary conditions V (z = 0) = 0 and V (z = a) = V0.Example 2 Determine the electrostatic potential in the space between two very longconcentric cylinders of radii a and b, b > a. The internal cylinder is grounded, whereasthe external one is held at the �xed potential V0.Example 3 What is a potential distribution in between the two planes, φ = 0 andφ = α, if the �rst plane is grounded, and the second has the potential V0?Example 4 Determine the potential distribution in the region of space between twocones, θ = θ1 and θ = θ2, θ1 < θ2. The surfaces of the cones are held at the potentialsV = 0 and V = Vex, respectively. The common vertex of the cones is insulated.Example 5 Calculate E inside and outside a spherical cloud of a uniform volumecharge, ρv. The radius of the cloud is R.

94

Lecture 11 Capacitance and capacitors

Outline

1. De�nition and calculation of the capacitance.

2. Capacitance of parallel-plate, cylindrical and spherical capacitors.

3. Muliti-dielectric capacitors.

95

Consider two conductors, referred to as plates, carrying equal but opposite charges,±Q=capacitor.

Potential difference between the conductors:

V = V1 − V2 = −∫ 2

1

E · dl.The charge on each capacitor is related to the �eld by Gauss's law

Q =

∮D · dS = ε

∮E · dS; assuming ε = const.

96

Capacitance of such a capacitor is de�ned as

C =Q

V=

ε∮

E · dS∫ 2

1E · dl

Methods of calculating capacitance

• Assume Q is given and determine V in terms of Q using Coulomb or Gauss's law.(Method I)

• Assume V0 ≡ V is given and determine the corresponding Q by solving theappropriate Laplace's equation (Method II).

97

Method I

• Choose a suitable coordinate system.

• Let the two conductors carry charges +Q and−Q, respectively.

• Determine E using Coulomb's or Gauss's law and �nd the potential fromV = − ∫

E · dS.

• Obtain the capacitance from C = Q/V .

Illustrating Method I by examples.

98

Parallel-plate capacitor

99

Neglecting fringing, the uniform surface charge density is

ρS = Q/A.

Use Gauss's law to calculate the �eld between the plates:

Qenc =

top

D · dS︸ ︷︷ ︸

=0

+

bottom

D · dS +

side

D · dS︸ ︷︷ ︸

=0

.

100

Consequently,

Qenc = ρSA = D

∫dS = DA =⇒ D = ρSan.

Hence

E =ρS

εan =

Q

εAan

Calculate the potential difference between the plates, an = −az

V = −∫ 2

1

E · dl = −∫ d

0

Q

εAaz · (−az)dz

=Q

εA

∫ d

0

dz (az · az)︸ ︷︷ ︸=1

=Q

εAd. (41)

101

Thus, the capacitance of a parallel-plate capacitor:

C =Q

V=

εA

d.

Application: Measuring C with the dielectric and with the air, we infer the relativedielectric constant εr viz.,

εr =C

C0

.

102

Cylindrical (coaxial) capacitor

Choose Gaussian surface to be another coaxial cylinder such that a < ρ < b.

Q =

∮D · dS = ε

∮E · dS = εE(2πρ)L,

103

It follows that

E =Q

2περLaρ

Neglecting fringing, the potential difference between the plates is

V = −∫ 2

1

E · dl = −∫ a

b

(Q

2περLaρ

)· aρdρ

=Q

2πεL

∫ a

b

ρ(aρ · aρ)︸ ︷︷ ︸

=1

=Q

2πεLln

b

a. (42)

Thus,

C =Q

V=

2πεL

ln b/a.

104

Spherical capacitor

Choose Gaussian surface to be another coaxial sphere such that a < r < b.

Q =

∮D · dS = ε

∮E · dS = εE4πr2.

105

Hence,

E =Q

4πεr2ar

And, the potential difference is calculated as follows

V = −∫ 2

1

E · dl = −∫ a

b

(Q

4πεr2ar

)· ardr

=Q

4πε

∫ a

b

dr

r2(ar · ar)︸ ︷︷ ︸

=1

=Q

4πε

(1

a− 1

b

). (43)

Thus, the capacitance of such a capacitor is

C =Q

V=

4πε1a− 1

b

.

• b →∞, C = 4πεa, useful to estimate capacitance of a single conductor (theother plate in in�nity) of a typical size a.

106

Multiple-dielectric capacitors

• Compound capacitor with the interface parallel E and D⇐⇒ arrangement ofcapacitors in parallel.

Example. parallel-plate capacitors:

Ceq = C1 + C2 =

ε0εr1︷︸︸︷ε1 A1

d+

ε0εr2︷︸︸︷ε2 A2

d.

107

• Compound capacitor with the interface normal to E and D⇐⇒ arrangement ofcapacitors in a series.

Example. parallel-plate capacitors:

1

Ceq

=1

C1

+1

C2

=ε1d1 + ε2d2

ε1ε2A.

108

Energy stored in a capacitor

Recall the expression for the energy to assemble a system of surface charges

WE =1

2

∫ρSV dS.

Applying to a capacitor with∫

ρ1SdS = − ∫ρ2SdS = Q:

WE =1

2

∑j=1,2

∫ρjSVjdS =

1

2(V1

∫ρ1SdS + V2

∫ρ2SdS)

= Q(V1 − V2)/2 = QV/2 (44)

WE =1

2QV =︸︷︷︸

Q=CV

1

2CV 2 =︸︷︷︸

V =Q/C

Q2

2C(45)

Example 1 In the arrangement displayed in �gure (a), determine the voltage dropacross each dielectric.

109

Lecture 12 Method of images

Motivation

1. hard to solve Poisson's equation for complicated systems of point charges andconductors

2. uniqueness theorem: any solution to Poisson's equation is unique =⇒ a cleverguess will work!

Areas of application: useful to �nd potential and electric �eld strength for systems ofpoint/line charges in the vicinity of conducting bodies.

110

A point charge +Q, located a distance d above a grounded conducting plane

The solution must satisfy the conditions:

1. V (ρ, 0) = 0, the plane z = 0 is grounded;

2. V (ρ, z) → 0 as ρ, z →∞;

3. by symmetry, V (ρ, z) = V (−ρ, z).

Solution satisfying 1-3:

V (ρ, z) =

Q4πε0

(1

R+− 1

R−

)z > 0,

0 z < 0.

HereR+ = [ρ2 + (z − d)2]1/2,

R− = [ρ2 + (z + d)2]1/2.

111

Interpretation: the effect of the plane⇐⇒ an image charge−Q, located at z = −d.

The electric �eld:

E = −∇V =

Q4πε0

[ρaρ+(z−d)az

R3+

− ρaρ+(z+d)az

R3−

]z > 0,

0 z < 0.

The force on the charge +Q due to the image charge−Q

F = − Q2

4πε0(2d)2az.

112

Surface density of induced charge

Boundary condition at the plane surface, (ε1 = ε2 = ε0):

(E− − E+) · an = ρs/ε0.

an = az ; E− = 0 ( the �eld in the half-space z < 0) and E+ = −∇V .

ρs = − ε0∂V

∂z

∣∣∣∣z=0

.

Thus

ρs = − Qd

2π(ρ2 + d2)3/2.

113

Further Examples to be discussed in class

Example 1. A point charge Q is placed a distance d above a grounded conductingplane. Find the work done to remove the charge far away from the plane.Example 2. Determine the electrostatic potential distribution and the induced surfacecharge due to an in�nitely long, charged � with the charge κ per unit length � �lament,located a distance h above a grounded conducting plane.

114

Lecture 13 Electric current and current density. Continuity equation

Outline

1. De�nition of the current and current density.

2. Convection and conduction currents. Point form of Ohm's law.

3. Continuity equation.

4. Volume charge relaxation in materials.

115

Electric current and current density

Electric current, I : rate of charge transport past a point or across a speci�ed surface.

I =dQ

dt, [Coulomb/second]

116

Current density, J : current per unit cross-section [Amp�eres/meter2]:

dI = J · dS I =

S

J · dS .

117

Convection versus conduction currents

• Convection current⇐⇒ simply �ow of charged particles.

• Conduction current⇐⇒ �ow of particles in a conductor.

118

Derive an expression for the density of any type of current.

∆I =∆Q

∆t= ρv∆S

∆l

∆t︸︷︷︸U

= ρvU ·∆S

Since J = ∆I/∆S, we obtainJ = ρvU .

119

Point form of Ohm's law

Drift velocity of electrons in a conductor (liquid, crystalline, gas) = average velocity ofsuch electrons due to applied �eld, subject to collisions.

120

Drift velocity is related to mobility µ [meter2/(Volt·second)] as follows

U = µE.

Using the derived expression for the current density in terms of the drift velocity,

J = ρvU,

we obtain the point form of Ohm's law:

J = ρvµE = σE .

• σ = conductivity (Siemens/meter).

• σ decreases with the temperature =⇒ increase of resistivity of the material tocurrent �ow.

Recall the integral form of Ohm's law:

V = IR R = resistance .

121

Resistance calculations

Ohm's law:

R =V

I=− ∫

LE · dl∮

SJ · dS =︸︷︷︸

σ=const

− ∫LE · dl

σ∮

SE · dS .

Recall the expression for the capacitance

C =Q

V=

∮SD · dS

− ∫LE · dl =︸︷︷︸

ε=const

ε∮

SE · dS

− ∫LE · dl .

It follows

RC =ε

σ

Example 1 Calculate the resistance per unit length of a coaxial cable of inner and outerradii a and b, a < b.Example 2 A conducting material of uniform thickness h and conductivity σ has theshape of the quarter of an annulus in the xy-plane: 0 ≤ φ ≤ π/2, a ≤ ρ ≤ b.Determine the resistance between the end faces.

122

Continuity equation

Law of charge conservation: time rate of decrease of charge inside a closed volume =outward current �ux through the surface of the volume.

−dQin

dt=

∮J · dS. (46)

Using the divergence theorem,∮

J · dS =

v

∇ · Jdv (47)

The time rate of decrease of the charge in terms of volume charge density:

−dQin

dt= − d

dt

v

ρvdv = −∫

v

∂ρv

∂tdv. (48)

123

It follows from equations (54), (55) and (56) that∫

v

∇ · Jdv = −∫

v

∂ρv

∂tdv. (49)

In other words, ∫

v

dv

(∂ρv

∂t+∇ · J

)= 0. (50)

Implying that∂ρv

∂t+∇ · J = 0 .

• current continuity equation

• stationary case, ∂ρv/∂t = 0 =⇒ ∇ · J = 0 .

124

Relaxation of introduced charge inside volume

Introduce volume charge ρv at the interior of a given conducting material.

Ohm's + Gauss's laws, assuming ε = const and σ = const:

J = σE Ohm,

∇ · E = ρv/ε.

It follows∇ · J = ∇ · (σE) = σ∇ · E = σρv/ε.

125

On substituting to the continuity equation,

∂ρv

∂t+∇ · J = 0,

one obtains∂ρv

∂t+

σ

ε︸︷︷︸const

ρv = 0. (51)

The solution to this homogeneous, linear differential equation is

ρv = ρv0︸︷︷︸ρv(t=0)

exp

(−σt

ε

)= ρv0e

−t/τ .

• τ = ε/σ ⇐⇒ relaxation time

126

Lecture 14 Biot-Savart's and Amp�ere's Laws

Biot-Savart's law: The magnetic �eld intensity dH due to a current element Idl at apoint P is proportional to Idl, to sine of the angle α between the element and the linejoining the element and P and inversely proportional to the square of the distance fromthe element to P

127

Mathematical formulation of Bio-Savart law

dH =Idl sin α

4πR2=

Idl×R/R︷︸︸︷aR

4πR2=

Idl×R

4πR3

128

Direction of H due to the current element:

129

Volume, surface and line current con�gurations

De�ne J (volume current in Amp�eres/meter square); K (surface current inAmp�eres/meter) such that

Idl = KdS = Jdv

130

Applying the principle of superposition yields:

H =

L

Idl×R

4πR3, (line current);

H =

S

KdS ×R

4πR3, (surface current);

H =

v

Jdv ×R

4πR3, (volume current).

Example 1 A current �lament of length 2L, carrying the current I , is placed along thez-axis. Calculate the magnetic �eld H generated by the current at the point P (ρ, 0, 0)

Example 2 Calculate the magnetic �eld on the axis of a ring of radius R carrying thecurrent I .

131

Amp�ere's Law

Circulation of H around a closed path = net current enclosed by the path∮

H · dl = Ienc , (integral form of Amp�ere's law).

Applying Stokes's theorem,

Ienc =

L

H · dlStokes︷︸︸︷

=

S

(∇×H) · dS.

132

By de�nition of the current density,

Ienc =

S

J · dS.

Hence, ∫

S

J · dS =

S

(∇×H) · dS,

Implying that

∇×H = J (differential form of Amp�ere's law= 3rd Maxwell's equation).

133

Application of Amp�ere's law

1. Current distribution possesses axial, spherical or re�ectional symmetry.

2. At each point of the closed path H is either tangential or normal to the path.

3. H has the same magnitude at all points of the path where H is tangential.

Illustrative examples of the Amp�ere's law application to be considered:

• in�nite �lamentary current

• in�nitely long solenoid

• in�nitely long coaxial transmission line.

134

Lecture 15 Magnetic �ux density and magnetic �ux

Introduce the magnetic �ux density in free space by analogy with the correspondingelectric �ux density (D = ε0E):

B = µ0H.

where

µ0 = 4π × 10−7, (Henries/meter)=magnetic permiability of free space.

135

The magnetic �ux through a �nite surface is de�ned as

Φ =

S

B · dS.

Example 1 A coaxial cylindrical conductor with an inner conductor of radius a and anouter one of radius b carries current I inside the inner conductor. Find the magnetic �uxper unit length crossing the surface φ = const between the conductors.

136

Comparison between electric and magnetic �uxes

• Electrostatic �eld: electric �ux lines are not necessarily closed.

• Magnetostatic �eld: magnetic �ux lines must be either closed or go to in�nity⇐⇒ no isolated magnetic charges in nature!!

Can one isolate a pole of a permanent magnet then?

137

No isolated magnetic charge of any form in nature ⇐⇒∮

B · dS = 0.

Note

• This is a law of conservation of magnetic �ux (Gauss's law for magnetic �elds).

138

0 =

∮B · dS

divergence︷︸︸︷=

v

∇ ·Bdv.

It follows that

∇ ·B = 0, (differential form of magnetic �ux conservation).

139

Scalar magnetic potential

Recall two identities from the vector analysis that hold for any scalar �eld f and vector�eld F:

∇× (∇f) = 0; (curl of a gradient =0)

∇ · (∇× F) = 0; (divergence of a curl=0).

In the absence of a volume current, J = 0, introduce a scalar magnetic potential Vm

(in Amp�eres) such thatH = −∇Vm if J = 0.

140

Justi�cation

0 = JMaxwell′s eq︷︸︸︷

= ∇×H = ∇× (−∇Vm)

curl(grad(...))=0︷︸︸︷= 0.

In free space, J = 0,

∇ ·H = 0, H = −∇Vm =⇒ ∇2Vm = 0.

• Vm satis�es Laplace's equation in free space.

141

Vector magnetic potential

Introduce a vector magnetic potential A (in Weber/meter) such that

B = ∇×A.

Justi�cation:

0no magnetic charge︷︸︸︷

= ∇ ·B = ∇ · (∇×A)

div(curl(...))=0︷︸︸︷= 0.

• Scalar �eld Vm can be used only if J = 0.

• Vector �eld A can always be employed.

Example 2 Given A = −µ0Iρ2/(4πa2)az , what is B?Example 3 Determine A of the magnetic �eld produced by an in�nitely long, straight�lamentary current I .

142

Superposition principle yields

A =

L

µ0Idl

4πR, (line current);

A =

S

µ0KdS

4πR, (surface current);

A =

v

µ0Jdv

4πR, (volume current).

143

The �ux of a magnetic �eld in terms of the vector potential

Φ =

S

B · dS =

S

(∇×A) · dS =︸︷︷︸Stokes

∮A · dl.

Thus

Φ =

∮A · dl.

144

Summary of Maxwell's equations for static �elds

Gauss's law for electrostatic (left) and magnetostatic (right) �elds

Differential (point) form:

∇ ·D = ρv, ∇ ·B = 0.

Integral form:∮

S

D · dS = Qenc,

S

B · dS = 0.

145

Amp�ere's law for electrostatic (left) and magnetostatic (right) �elds

Differential (point) form:

∇× E = 0, ∇×B = J.

Integral form:∮

L

E · dl = 0,

L

H · dl = Ienc.

146

Lecture 16 Forces and torques due to magnetic �elds

Outline

1. Lorentz force on a charged particle

2. Force on a current element

3. Force between two current elements

4. Torque on a current loop.

147

Force on a charged particle

Force on a stationary or moving charge due to an electric �eld (Coulomb's law):

Fe = QE.

Force on a moving charge due to a magnetic �eld (Lorentz force):

Fm = QU×B.

In presence of both electric and magnetic �eld =⇒ Lorentz force equation:

F = Fe + Fm = Q(E + U×B).

148

Newton's equation of motion for a charged particle:

MdU

dt= Q(E + U×B).

Properties of the electric and magnetic forces

• Fe performs work.

• Fm does not perform work, (Fm · dl = 0!) =⇒ Fm changes direction of motionof a charged particle.

149

Force on a current element

Recall the connection between the current density J and the drift velocity U:

J = ρvU;

as well as the relation between the different current elements

Idl = KdS = Jdv.

Hence,Idl = Jdv = ρvdv︸︷︷︸

dQ

U = dQU.

150

Thus,Idl = dQU.

• charge element dQ moving with velocity U⇐⇒ a conduction current element Idl.

Consequently, the force (Amp�ere force) on a current element:

dF = Idl×B.

151

For a closed circuit,

F =

L

Idl×B.

Similarly, for surface and volume current elements,

dF = KdS ×B, dF = Jdv ×B;

or, in the integral form,

F =

S

KdS ×B, F =

v

Jdv ×B.

152

Force between two current elements

The force between elements I1dl1 and I2dl2 ⇐⇒ force on I1dl1 due to the magnetic�eld dB2 generated by I2dl2:

dF12 = I1dl1 × dB2.

Example 1 Determine the force per unit length between two in�nitely long parallelstraight wires with the currents I1 and I2, respectively, placed a distance d apart.

153

Biot-Savart law implies

dB2 =µ0I2dl2 ×R12

4πR312

Consequently,

dF12 =µ0I1dl1 × (I2dl2 ×R12)

4πR312

The force between �nite current elements is found by the superposition principle:

F12 =µ0I1I2

L1

L2

dl1 × (dl2 ×R12)

R312

.

• Analog of Coulomb's law for interaction between two charges.

• F21 = −F12 due to the third law of Newton (action=reaction).

154

Magnetic torque and moment

Torque on a magnetic loop is a vector product of the force and the moment arm:

T = r× F, (Newtons · meter).

155

Calculate a total force on a rectangular loop placed in a uniform magnetic �eld:

• Along the sides 12 and 34: dl‖B;

• dF ∝ dl×B =⇒ dF12 = dF34 = 0.

156

The elementary forces on the other sides,

dF23 = Idz(az × ax)B; dF14 = Idz(−az × ax)B.

The total force,

F =

∫ 3

2

dF23 +

∫ 4

1

dF14 =︸︷︷︸uniform B

IBlay − IBlay = 0.

157

However, the forces form a couple, whose torque has the magnitude

|T| = |F|w sin α = IB lw︸︷︷︸S

sin α = IBS sin α.

158

De�ne a magnetic dipole moment m as

m = ISan ; (Amp�ere·meter2). (52)

The torque on a small loopT = m×B . (53)

• The de�nition of magnetic moment, Eq. (60), holds for a loop of any geometricalshape.

• The expression for the torque, Eq. (61), holds only for a small loop such that B isuniform across the loop.

159

Lecture 17 Magnetization in materials

Outline

1. A small current loop as a magnetic dipole: Comparison with electric dipoles.

2. Magnetization of a material. Magnetization volume and surface currents.

3. Brief classi�cation of magnetic materials.

160

Small current loop as magnetic dipole

The magnetic vector potential A and magnetic �ux density B far away from a small loop,r À a:

A =µ0(m× ar)

4πr2

and

161

B =µ0m

4πr3(2 cos θar + sin θaθ)

• small loop⇐⇒ magnetic dipole!

162

Comparison with electric dipole

163

Magnetization

Orbital motion of electrons around atoms or internal degree of freedom (spin)⇐⇒magnetic moment m = ISan.

164

Magnetization M, (Amp�eres/meter) is a magnetic dipole moment per unit volume:

M = lim∆v→0

∑Nk=1 mk

∆v

165

By de�nition, the dipole moment of elementary volume, dv′ is dm = Mdv′, and

dA(r) =µ0

dm︷ ︸︸ ︷Mdv′×

R/R︷︸︸︷aR

4πR2=

µ0M×R

4πR3dv′. (54)

R = |r− r′| =√

(x− x′)2 + (y − y′)2 + (z − z′)2.

166

Hence,

A =

∫µ0M×R

4πR3dv′.

It can be shown � see Appendix A � in strict analogy with the similar derivation fordielectrics that the last expression can be transformed into

A =µ0

v′

Jmdv′

R+

µ0

S′

KmsdS ′

R, (55)

where we have introduced

Jm = ∇×M , (magnetization volume current);

Kms = M× an , (magnetization surface current).

167

Recall Amp�ere's law in free space, M = 0, Jf being a free current,

∇×H = Jf , ⇐⇒ ∇×(

B

µ0

)= Jf .

In a medium, M 6= 0, and Amp�ere's law is modi�ed as follows

∇×(

B

µ0

)= Jf + Jm = ∇×H +∇×M = ∇× (H + M).

Thus in the medium,B = µ0(H + M).

• This relation holds for any medium!

168

In linear media, one can introduce magnetic susceptibility such that

M = χmH

It follows that

B = µ0(H + M) = µ0(H + χmH) = µ0(1 + χm)︸ ︷︷ ︸µ

H;

so thatB = µH, µ ⇐⇒ magnetic permeabilty, Henries/meter.

Relative permeability:

µr = 1 + χm =µ

µ0

169

Classi�cation of magnetic materials

1. Diamagnetic materials: B = 0, zero magnetic moments of atoms; µr ≤ 1.

2. Paramagnetic materials: B = 0, zero magnetic moments of atoms; µr ≥ 1.

3. Ferromagnetic materials: permanent magnetic moments of atoms; µr À 1.

• Paramagnetics and diamagnetics µr ' 1 =⇒ weak magnetic materials.

• Ferromagnetics, µr À 1 =⇒ strong magnetic materials (permanent magnets).

Example A ferromagnetic sphere of radius R is magnetized uniformly such thatM = M0az . Determine the equivalent magnetization current densities, Jm and Jms.

170

Lecture 18 Magnetic boundary conditions

To derive the boundary conditions at the interface of two magnetic media, we use

• Gauss's law for magnetic �elds∮

B · dS = 0.

• Amp�ere's circuit law∮

H · dl = Ienc.

Express B and H in terms of normal (to the surface) and tangential (to the surface)components:

B = Bn + Bt, H = Hn + Ht.

171

Consider a Gaussian surface indicated in the �gure,

B1n∆S −B2n∆S = 0

B1n = B2n

B=µH︷︸︸︷=⇒ µ1H1n = µ2H2n.

172

Consider a closed abcda path indicated in the �gure, K⊥ path

K∆w = H1t∆w + H1n∆h

2+ H2n

∆h

2

−H2t∆w −H2n∆h

2−H1n

∆h

2(56)

173

K∆w = H1t∆w + H1n∆h

2+ H2n

∆h

2

−H2t∆w −H2n∆h

2−H1n

∆h

2(57)

As ∆h → 0,H1t −H2t = K.

Generalizing,

(H1 −H2)× an12 = K ; an12 ⇐⇒ unit normal from medium 1 to medium 2.

174

In the absence of the free surface current K = 0,

H1t = H2t =⇒︸︷︷︸B=µH

B1t/µ1 = B2t/µ2.

• The normal component of B is continuous and the tangential one isdiscontinuous across the interface.

• The tangential component of H is continuous and the normal one isdiscontinuous across the interface.

175

Refraction of magnetic �ux lines at the interface

B1n = B2n =⇒ B1 cos θ1 = B2 cos θ2;

H1t = H2t =⇒ B1

µ1

sin θ1 =B2

µ2

sin θ2.

176

B1 cos θ1 = B2 cos θ2;

B1

µ1

sin θ1 =B2

µ2

sin θ2.

Dividing these equations term by term, we obtain the law of refraction of the magnetic�ux density, similar to the one for the electric �ux density:

tan θ1

µ1

=tan θ2

µ2

=⇒ tan θ1

tan θ2

=µ1

µ2

Example 1 Work out the magnitude of H2 in terms of H1 as well.Example 2 A long circular rod of magnetic material with permeability µ is insertedcoaxially into a long solenoid. The radius a of the rod is less than the radius b of thesolenoid. The solenoid winding has n turns per unit length and it carries the current I .Find B, H and M everywhere. Determine also Jm and Jms.

177

Lecture 19 Inductance and inductors

Flux linkage λ is a �ux Φ =∫

B · dS through a circuit with N identical turns:

λ = NΦ = LI ; L ⇐⇒ inductance.

178

• Inductor⇐⇒ circuit with inductance.

Inductance as a property of the geometry of the inductor (independent of the current)

L =λ

I=

I, (Henry=Weber/Amp�ere).

179

Mutual inductance and self-inductance

Generalization to two circuits

Φij is a magnetic �ux through ith circuit due to the magnetic �eld of the current in thejth circuit, (i, j = 1, 2).

Φij =

Si

dSi ·Bj i, j = 1, 2.

180

De�ne mutual inductance L12 as

L12 =λ12

I2

=N1Φ12

I2

.

By the same token,

L21 =λ21

I1

=N2Φ21

I1

.

Reciprocity theorem: L12 = L21.

Self-inductances of circuits 1 and 2 are de�ned as

L1 =λ11

I1

=N1Φ1

I1

;

L2 =λ22

I2

=N2Φ2

I2

;

Here, the total �ux through ith circuit is

Φi =∑j=1,2

Φij, i = 1, 2.

181

Calculation of self-inductance and mutual inductance

Method I

1. Choose a suitable coordinate system.

2. Let the conductor carry a current I .

3. Determine B from either Biot-Savart law or from Amp�ere's law ( if there is symmetryof current distribution).

4. Calculate the �ux viz., Φ =∫

B · dS.

5. Find the self-inductance, L = NΦ/I .

182

Example 1 Calculate the self-inductance of a toroid consisting of N turns of wire, tightlywound on a frame of a rectangular cross-section with the inner and outer radii a and b,respectively, and the height h.Example 2 Find the inductance per unit length of a very long solenoid with the air corehaving n turns per unit length.Example 3 Find the mutual inductance between a very long straight wire and a coplanarcircular loop of radius R. The distance between the center of the loop and the wire is d.

183

Lecture 20 Electromagnetic Induction

Faraday's observations: The current is induced in a circuit whenever

• a steady current in an adjacent circuit is turned on/off;

• there is a relative motion of the primary and secondary circuits

• a permanent magnet is thrust into/out of the circuit

Qualitatively: the induced current is caused by an induced electromotive force (emf)brought about by the changing magnetic �ux!

184

Quantitative Description

The magnetic �ux though a closed circuit C with the cross-section S

Φ =

S

dS ·B,

The electromotive force by de�nition,

E =

C

dl · E.

Faraday's law:

E = −dΦ

dt.

Either a magnetic �eld changes or a circuit moves, or else the circuit moves in atime-dependent and/or inhomogeneous magnetic �eld.

185

Consider a static circuit C linked to a time-varying magnetic �eld B

E =

C

dl · E = − d

dt

S

dS ·B = −∫

S

dS · ∂B

∂t∮

dl · E =

S

dS · (∇× E) = −∫

S

dS · ∂B

∂t.

The Maxwell equation for time-varying EM �elds:

∇× E = −∂B

∂t

Example 1 A metal bar slides over a pair of conducting rails in a uniform magnetic �eldB = Boaz , with a constant velocity u = uax. Determine the voltage generated acrossthe bar.

186

Example 2 An h× w rectangular conducting loop is placed in a magnetic �eldB(t) = ayB0 sin(ωt). The normal to the loop makes the angle α with y-axis. Find aninduced emf in the loop when: (a) the loop is at rest and (b) the loop rotates with theangular velocity ω around the x−axis.Example 3 Determine the emf induced in a triangular loop to be drawn in class. Thevertical bar moves with a constant velocity u = uax in the inhomogeneous magnetic�eld, B = Axaz , where A is a constant. Assume the bar starts at the origin at t = 0.

Application: Transformers

The voltage in a primary coil by Faraday's law: V1 = −N1dΦ/dt.The voltage in a secondary coil by Faraday's law: V2 = −N2dΦ/dt.

V1

V2

=N1

N2

.

Energy conservation yields for the powers:

P1 = P2 =⇒ I1V1 = I2V2 =⇒ I1

I2

=N2

N1

.

187

Magnetic Energy

In complete analogy with the electrostatic case, the magnetic energy stored in the �eld isgiven by

Wm =1

2

∫(B ·H)dv =

1

2

∫µH2dv

The derivation is less straightforward, though, as even static magnetic �elds aregenerated by steady currents which would have to be turned on at some instant. Thus, atransient regime must be considered � which is done in Appendix B � to determine thework done to switch on the currents generating the magnetic �eld. The self-inductancecan then be determined as follows

Wm =1

2

∫(B ·H)dv =

1

2LI2, =⇒ L =

∫(B ·H)

I2dv

188

Displacement current

Motivation: Incompatibility of Ampere's law and the charge conservation law

∇×H = J,

It follows that∇ · J = ∇ · (∇×H) = 0.

Charge conservation law implies contradiction

∇ · J = −∂ρv

∂t6= 0!

189

Resolution: introducing Maxwell's displacement current Jd as

∇×H = J + Jd.

∇ · (∇×H) = 0 = ∇ · J +∇ · Jd.

∇ · Jd = −∇ · J =∂ρv

∂t=

∂t(∇ ·D) = ∇ · ∂D

∂tThus,

Jd =∂D

∂t.

The Maxwell equation for time-varying EM �elds:

∇×H = J +∂D

∂t.

Displacement current manifestations: electromagnetic waves!!

190

Appendix A: Derivation of Surface and Volume Polarized Charges

Starting with the potential dV due to an in�nitesimal polarized volume dv:

dV =

dp︷ ︸︸ ︷(Pdv′) ·aR

4πε0R2(58)

Noting, R =√

(x− x′)2 + (y − y′)2 + (z − z′)2, we can show that

∇′(

1

R

)=

aR

R2.

Exercise: Check the above expression explicitly calculating the gradient of 1/R.

191

∇′(

1

R

)=

aR

R2.

It follows thatP · aR

R2= P · ∇′

(1

R

). (59)

Using the vector identity,

∇′ · (fA) = f∇′ ·A + A · ∇′f (60)

It follows from Eq. (37) and (38) with the identi�cation, f → 1/R′ and A → P that

192

P · aR

R2= ∇′ ·

(P

R

)− ∇′ ·P

R(61)

Substituting back into equation (25) and integrating, we obtain

V =1

4πε0

v′

[∇′ ·

(P

R

)− ∇′ ·P

R

]dv′. (62)

Applying the divergence theorem to the �rst term on the rhs of Eq. (29), we obtain

V =

S′

ρps︷ ︸︸ ︷P · a′n4πε0R

dS ′ +∫

v′

ρpv︷ ︸︸ ︷−∇′ ·P4πε0R

dv′ (63)

ρps = P · an, polarization surface charge,

ρpv = −∇ ·P, polarization volume charge.

193

Appendix B: Derivation of Magnetization Currents

By de�nition, the dipole moment of elementary volume, dv′ is dm = Mdv′, and

dA(r) =µ0

dm︷ ︸︸ ︷Mdv′×

R/R︷︸︸︷aR

4πR2=

µ0M×R

4πR3dv′. (64)

R = |r− r′| =√

(x− x′)2 + (y − y′)2 + (z − z′)2.

194

Hence,

∇′(

1

R

)=

(x− x′)ax + (y − y′)ay + (z − z′)az

[(x− x′)2 + (y − y′)2 + (z − z′)2]3/2=

R

R3

Using the last expression, one can express R/R3 in equation (66) in terms of∇1/R

and integrating over the volume, obtain the expression for the vector potential:

A =µ0

∫M×∇′

(1

R

)dv′. (65)

195

A =µ0

∫M×∇′

(1

R

)dv′. (66)

Use the vector identity,

∇× (fF) = f∇× F− F× (∇f),

with f = 1/R and F = M, that is,

M×∇′(

1

R

)=

1

R∇′ ×M−∇′ ×

(M

R

).

Substituting the lhs back into equation (68), we obtain

A =µ0

v′

∇′ ×M

Rdv′ − µ0

v′∇′ ×

(M

R

)dv′. (67)

196

A =µ0

v′

∇′ ×M

Rdv′ − µ0

v′∇′ ×

(M

R

)dv′. (68)

Using yet another vector identity,∫

v′∇′ × Fdv′ = −

S′F× dS,

we cast Eq. (70) into the form

A =µ0

v′

∇′ ×M

Rdv′ +

µ0

S′

M× an

RdS ′

=µ0

v′

Jmdv′

R+

µ0

S′

KmsdS ′

R. (69)

197

A =µ0

v′

∇′ ×M

Rdv′ +

µ0

S′

M× an

RdS ′

=µ0

v′

Jmdv′

R+

µ0

S′

KmsdS ′

R. (70)

Introduce,Jm = ∇×M , (magnetization volume current);

Kms = M× an , (magnetization surface current).

198

Appendix C: Magnetic energy derivation

Power associated with the Faraday emf inducing a current I :

P =dWm

dt= IE = −I

dt.

Incremental change in the energy = incremental work against emf:

δWm = IδΦ

∆(δWm) = Jδσ︸︷︷︸I

S

dS · δB︸ ︷︷ ︸

δΦ

= Jδσ

S

dS · (∇× δA) = Jδσ

C

dl · δA.

The total incremental work:

δWm =∑

l

Jδσ

C

dl · δA.

using Jδσdl = Jδv, we arrive at

δWm =

∫dvδA · J.

199

Using the Maxwell equation:∇×H = J,

δWm =

∫dvδA · (∇×H).

Using the vector identity,

∇ · (P×Q) = Q · (∇×P)−P · (∇×Q),

we obtain

δWm =

∫dv[H · (∇× δA) +∇ · (H× δA)]

The second term on the r.h.s. is zero for any localized �eld distribution (why?). Hence,

δWm =

∫dv(H · δB).

200

For para- or diamagnetic media, H ∝ B so that � using the same rules as forderivatives � we have

H · δB =1

2δ(H ·B),

and adding all incremental contributions, we obtain for the total energy stored inmagnetic �eld,

Wm =1

2

∫dv(B ·H) =

1

2

∫dvµH2

201

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