In regions with ρ=0This reduces to Laplace’s equation:
∇2V=0
Theorem 2.2 (Uniqueness --- statement). The solution to Laplace’s (or Poisson’s) equation in a Region is unique given either Dirichlet boundary conditions (V specified on the boundary) or Neumann boundary conditions (∂V/∂n specified on the boundary).
Theorem 2.3 (Uniqueness for Dirichlet conditions). The solution to Poisson’s equation ∇2V=−ρ/ε0 in a volume V is unique if V is specified on the Boundary S.
Proof. Suppose V1 and V2 both satisfy Poisson’s equation with the same boundary Conditions. Define U=V1−V2. Then ∇2U=0 in V and U=0 on S.
Apply Green’s first identity with ϕ=ψ=U:
∫V(U∇2U+∣∇U∣2)dV=∮SU∂n∂UdA
Since ∇2U=0 and U=0 on S:
∫V∣∇U∣2dV=0
Since the integrand is non-negative, ∇U=0 everywhere in VSo U is Constant. With U=0 on the boundary, U=0 throughout V. Hence V1=V2. ■
Theorem 2.4 (Uniqueness for Neumann conditions). The solution is unique up to an additive Constant when ∂V/∂n is specified on S.
Proof. The same argument applies, but now ∂U/∂n=0 on S and the Right-hand side of Green’s identity vanishes for a different reason. We again conclude ∇U=0So U is constant. ■
The method of images replaces a problem with conductors by an equivalent problem with charges only, Exploiting the uniqueness theorem.
Point charge above a grounded plane. A charge q is placed at distance d above an Infinite grounded conducting plane (V=0 at z=0).
Replace the plane by an image charge q′=−q at z=−d. The potential for z>0 is:
V(x,y,z)=4πε01[x2+y2+(z−d)2q−x2+y2+(z+d)2q]
This satisfies ∇2V=0 for z>0 (away from the charge), V=0 at z=0And V→0 as r→∞. By the uniqueness theorem, this is the correct solution.
The force on q is the force due to the image charge:
F=−4πε0(2d)2q2z^
The induced surface charge density on the plane:
σ(x,y)=−ε0∂z∂Vz=0=−2π(x2+y2+d2)3/2qd
Example: Point charge inside a grounded sphere. A charge q is at distance a from the centre Of a grounded conducting sphere of radius R (a<R).
The image charge is q′=−qR/a located at distance b=R2/a from the centre, along the same Radial line.
Solution: Verifying the image charge
We must verify that V=0 on the sphere. Place q at distance a from the origin along the z-axis and q′ at distance b along the z-axis. At any point on the sphere at distance R From the origin, the distances to q and q′ are d1 and d2 where:
d12=R2+a2−2Racosθ,d22=R2+b2−2Rbcosθ
For V=0 on the sphere, we need q/d1=−q′/d2 for all θ. This requires the ratio d2/d1 to be constant. Setting b=R2/a:
d12d22=R2+a2−2RacosθR2+R4/a2−2R3cosθ/a=a2R2
The ratio is indeed constant. Choosing q′=−qR/a gives q/d1+q′/d2=0 on the sphere. ■
For a localized charge distribution ρ(r′)The potential at large distance r=∣r∣≫r′=∣r′∣ is expanded using ∣r−r′∣1=∑n=0∞rn+1r′nPn(cosα) Where α is the angle between r and r′:
V(r)=4πε01∑n=0∞rn+11∫r′nPn(cosα)ρ(r′)d3r′
Monopole term (n=0):
V0=4πε01rQ,Q=∫ρ(r′)d3r′
This is the potential of a point charge at the origin.
Dipole term (n=1):
V1=4πε01r2p⋅r^,p=∫r′ρ(r′)d3r′
Where p is the electric dipole moment.
Quadrupole term (n=2): Depends on the quadrupole moment tensor:
Qij=∫(3ri′rj′−r′2δij)ρ(r′)d3r′
V2=4πε012r31∑i,jQijr^ir^j
For a neutral charge distribution (Q=0), the dipole term dominates. If additionally p=0The quadrupole term dominates.
Example: Dipole potential of two charges
A charge +q at z=+d/2 and −q at z=−d/2.
The dipole moment: p=q(d/2)z^+(−q)(−d/2)z^=qdz^.
On the z-axis (θ=0): V1=4πε0r2qd.
In the equatorial plane (θ=π/2): V1=0.
The exact potential on the z-axis is:
V=4πε0q(r−d/21−r+d/21)=4πε0qr2−d2/4d
For r≫d: this reduces to V1=4πε0r2qdConfirming the Dipole approximation. ■
Polarization. When an external field E is applied to a dielectric, the material Develops a polarizationPThe dipole moment per unit volume. This produces bound charges:
ρb=−∇⋅P,σb=P⋅n^
The displacement fieldD is defined as:
D=ε0E+P
Gauss’s law in terms of D:
∇⋅D=ρf
Where ρf is the free charge density. This form is useful because D depends Only on free charges, not bound charges.
Linear dielectrics. For an isotropic linear dielectric:
P=ε0χeE,D=εE
Where χe is the electric susceptibility and ε=ε0(1+χe) is the Permittivity. The relative permittivity (dielectric constant) is εr=ε/ε0=1+χe.
Boundary conditions at dielectric interfaces (no free charges):
D1n=D2n⟹ε1E1n=ε2E2n
E1t=E2t
The tangential component of E is continuous, but the normal component changes. The angles of the field with respect to the normal satisfy ε1tanθ2=ε2tanθ1.
Example: Dielectric slab in a uniform field
A dielectric slab of permittivity ε and thickness d is placed in a uniform External field E0 perpendicular to its faces.