Lecture 1 Vector algebra: A brief revie... · Lecture 1 Vector algebra: A brief review Outline 1....

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Transcript of Lecture 1 Vector algebra: A brief revie... · Lecture 1 Vector algebra: A brief review Outline 1....

Page 1: Lecture 1 Vector algebra: A brief revie... · Lecture 1 Vector algebra: A brief review Outline 1. Scalars and Vectors 2. Unit vectors ... The gradient of V is a vector eld that is

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

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• 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

.

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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

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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,

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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.

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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)].

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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).

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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

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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).

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Gradient

The vector separation of the points M and N :

dr = axdx + aydy + azdz. (1)

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

dV =∂V

∂xdx +

∂V

∂ydy +

∂V

∂zdz. (2)

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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.

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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!

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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.

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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.

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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

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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).

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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.

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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!

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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.

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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

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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.

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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.

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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.

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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.

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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.

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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)

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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.

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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.

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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

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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).

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F12 =Q1Q2

4πε0|R12|2aR12 =Q1Q2

4πε0|R12|2R12

|R12|︸ ︷︷ ︸aR12

=Q1Q2

4πε0|R12|3R12.

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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.

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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].

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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.

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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.

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Electric �elds of continuous distributions of charges

Elementary (in�nitesimal) charge

dQ =

ρvdv volume charge

ρSdS surface charge

ρLdl line charge

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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).

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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)

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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)

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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).

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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!!

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Example: a point charge

∮D · dS = D

∫ π

0

r2 sin θdθ

∫ 2π

0

︸ ︷︷ ︸4πR2

= Q;

E =D

ε0

=Q

4πε0r2ar.

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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.

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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.

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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.

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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.

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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).

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Hence to move Q from A to B:

W = −Q

∫ B

AE · dl.

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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.

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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.

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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).

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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.

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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)

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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).

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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.

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Thus,dV = −E · dr; dV = ∇V · dr. (17)

It follows from equation (17) that

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

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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

.

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

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

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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).

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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.

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• 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)

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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).

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Energy density of the electrostatic �eld

WE =1

2

v

ρvV dv =1

2

vsphere

∇ ·D︸ ︷︷ ︸=ρv

V dv (22)

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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)

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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.

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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.

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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.

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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.

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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.

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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

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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,

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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.

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• 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!

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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

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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.

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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).

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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

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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).

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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)

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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.

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Use Gaussian surface in �gure (b) to get

∆Qencl = ρS∆S = D1n∆S −D2n∆S.

ThusD1n −D2n = ρS . (27)

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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.

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

E1t = E2t =⇒ E1 sin θ1 = E2 sin θ2,

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D = εE =⇒ Dn = εEn

D1nno free charge

= D2n =⇒ ε1E1 cos θ1 = ε2E2 cos θ2.

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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.

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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.

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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)

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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

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Lecture 10 Poisson and Laplace equations

Outline

1. Poisson equation.

2. Laplace equation

3. Uniqueness of the solution to Laplace equation

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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)

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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)

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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.

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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.

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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.

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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.

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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).

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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.

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Parallel-plate capacitor

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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

.

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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)

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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

.

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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,

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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.

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Spherical capacitor

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

Q =

∮D · dS = ε

∮E · dS = εE4πr2.

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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.

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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.

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• 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.

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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.

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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.

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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.

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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.

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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.

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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.

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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.

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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]

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

dI = J · dS I =

S

J · dS .

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Convection versus conduction currents

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

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

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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 .

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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.

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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 .

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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.

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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)

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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 .

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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.

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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

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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

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Mathematical formulation of Bio-Savart law

dH =Idl sin α

4πR2=

Idl×R/R︷︸︸︷aR

4πR2=

Idl×R

4πR3

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Direction of H due to the current element:

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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

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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 .

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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.

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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).

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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.

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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.

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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.

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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?

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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).

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0 =

∮B · dS

divergence︷︸︸︷=

v

∇ ·Bdv.

It follows that

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

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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.

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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.

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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 .

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Superposition principle yields

A =

L

µ0Idl

4πR, (line current);

A =

S

µ0KdS

4πR, (surface current);

A =

v

µ0Jdv

4πR, (volume current).

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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.

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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.

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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.

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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.

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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).

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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.

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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.

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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.

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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.

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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.

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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).

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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).

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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.

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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.

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

|T| = |F|w sin α = IB lw︸︷︷︸S

sin α = IBS sin α.

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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.

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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.

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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

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B =µ0m

4πr3(2 cos θar + sin θaθ)

• small loop⇐⇒ magnetic dipole!

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Comparison with electric dipole

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Magnetization

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

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

M = lim∆v→0

∑Nk=1 mk

∆v

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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.

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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).

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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!

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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

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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.

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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.

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Consider a Gaussian surface indicated in the �gure,

B1n∆S −B2n∆S = 0

B1n = B2n

B=µH︷︸︸︷=⇒ µ1H1n = µ2H2n.

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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)

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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.

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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.

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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.

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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.

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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.

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• 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).

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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.

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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.

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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 .

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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.

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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!

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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.

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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.

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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

.

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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

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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!

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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!!

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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.

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∇′(

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

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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.

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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.

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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)

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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)

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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

Page 198: Lecture 1 Vector algebra: A brief revie... · Lecture 1 Vector algebra: A brief review Outline 1. Scalars and Vectors 2. Unit vectors ... The gradient of V is a vector eld that is

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).

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Page 199: Lecture 1 Vector algebra: A brief revie... · Lecture 1 Vector algebra: A brief review Outline 1. Scalars and Vectors 2. Unit vectors ... The gradient of V is a vector eld that is

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.

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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).

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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