The Method of Images
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You must be comfortable with Laplace's equation, the concept of boundary conditions (Dirichlet and Neumann), and the Uniqueness Theorem, which guarantees that a solution satisfying the correct boundary conditions is the only possible solution.
Why this matters
The method of images allows us to solve complex electrostatic boundary-value problems by replacing conducting surfaces with fictitious point charges.
In electrostatics, solving Laplace's equation for arbitrary geometries is often analytically intractable. The method of images provides a powerful shortcut for specific, highly symmetric configurations, such as a point charge near a grounded conducting plane or sphere. By introducing "image" charges in the region outside the physical domain, we construct a potential that satisfies the same boundary conditions as the original problem. Thanks to the Uniqueness Theorem, if our constructed potential matches the boundary conditions, it must be the correct physical potential within the region of interest.
The Core Idea
Imagine a point charge \( q \) placed a distance \( d \) above an infinite, grounded conducting plane. The electric field lines from \( q \) terminate perpendicularly on the plane. Instead of solving the differential equation for this setup, we can imagine removing the plane and placing a fictitious charge \( -q \) (the image charge) at a distance \( d \) below the plane, symmetric to the original charge. The potential at any point above the plane due to these two charges is identical to the potential of the original charge-plane system. The plane itself becomes an equipotential surface at zero potential. We do not place the image charge in the physical region; it exists only in the mathematical extension of the space to help us calculate the field in the real region.
Point Charge Near a Grounded Plane
Consider a charge \( q \) at \( (0,0,d) \) and a grounded plane at \( z=0 \). We propose an image charge \( q' = -q \) at \( (0,0,-d) \). The potential at a point \( P(x,y,z) \) with \( z > 0 \) is the superposition of the potentials from \( q \) and \( q' \):
On the plane \( z=0 \), the distances to \( q \) and \( q' \) are equal, so \( \phi(x,y,0) = 0 \). This satisfies the Dirichlet boundary condition. By the Uniqueness Theorem, this is the exact solution for \( z > 0 \). The electric field is obtained by \( \vec{E} = -\nabla\phi \). The induced surface charge density \( \sigma \) on the plane can be found from the discontinuity in the normal component of the electric field: \( \sigma = \varepsilon_0 E_z \) (just above the surface). Integrating \( \sigma \) over the plane yields a total induced charge of \( -q \), consistent with Gauss's law.
Point Charge Near a Grounded Sphere
For a grounded conducting sphere of radius \( a \) with a charge \( q \) located at a distance \( b > a \) from the center, the image charge \( q' \) is not simply \( -q \). To satisfy the boundary condition \( \phi = 0 \) on the sphere's surface, the image charge must have magnitude \( q' = -\frac{a}{b}q \) and be located at a distance \( b' = \frac{a^2}{b} \) from the center, along the line connecting the center to \( q \). This specific placement ensures that the potential vanishes everywhere on the spherical surface. The potential in the region outside the sphere is the sum of the potentials due to \( q \) and \( q' \). The force on the charge \( q \) is calculated by considering the field produced by the image charge \( q' \) at the location of \( q \), since the field of \( q \) itself does not exert a net force on \( q \).
Energy and Work
The electrostatic energy of the system can be calculated in two ways. First, by integrating the energy density \( u = \frac{1}{2}\varepsilon_0 E^2 \) over the region outside the conductor. Second, by considering the work done to bring the charge \( q \) from infinity to its position. The work done is equal to the potential energy \( U = \frac{1}{2} q \phi_{\text{image}}(q) \), where \( \phi_{\text{image}}(q) \) is the potential at the location of \( q \) due to the image charge alone. The factor of \( \frac{1}{2} \) arises because the image charge is a mathematical construct that moves as the real charge moves; the physical work is half the product of the charge and the potential due to the induced charges. This energy is always negative for a grounded conductor, indicating that the charge is attracted to the conductor.
The derivations
Uniqueness Theorem for Boundary-Value Problems
Let \( V \) be a bounded region with closed boundary surface \( S \), containing a fixed charge density \( \rho(\vec{r}) \). Any potential \( \phi \) satisfying Poisson's equation \( \nabla^2\phi = -\rho/\varepsilon_0 \) throughout \( V \) and matching prescribed Dirichlet data (\( \phi \) given on \( S \)) is unique. If instead Neumann data (\( \partial\phi/\partial n \) given on \( S \)) is prescribed, the solution is unique up to an additive constant, so the field \( \vec{E} = -\nabla\phi \) is unique.
Scalar Potential, Poisson and Laplace Equations
Because the electrostatic field is irrotational, \(\nabla\times\mathbf{E}=\mathbf{0}\), it can be written as the gradient of a scalar potential, \(\mathbf{E}=-\nabla\varphi\). Substituting this into the differential form of Gauss's law, \(\nabla\cdot\mathbf{E}=\rho/\varepsilon_0\), yields Poisson's equation \(\nabla^2\varphi=-\rho/\varepsilon_0\), whose source-free limit \(\rho=0\) is Laplace's equation \(\nabla^2\varphi=0\).
The image charge is a mathematical tool, not a physical entity. You cannot place a test charge in the region where the image charge resides to measure its field. The method only provides the correct field and potential in the physical region of interest (where the real charge is). Attempting to use the image charge to calculate fields in the region occupied by the conductor or outside the physical domain will yield incorrect results, as the boundary conditions are not satisfied in those regions. C
Worked example
Problem. A point charge \( q = 2.0 \times 10^{-9} \ \mathrm{C} \) is placed \( d = 0.05 \ \mathrm{m} \) above an infinite grounded conducting plane. Calculate the magnitude of the force exerted on the charge by the induced surface charges.
- Identify the image charge: \( q' = -q = -2.0 \times 10^{-9} \ \mathrm{C} \).
- Determine the distance between \( q \) and \( q' \): \( r = 2d = 0.10 \ \mathrm{m} \).
- Calculate the force using Coulomb's law: \( F = \frac{1}{4\pi\varepsilon_0} \frac{|q q'|}{r^2} \).
- Substitute values: \( \frac{1}{4\pi\varepsilon_0} = 9.0 \times 10^9 \ \mathrm{N \cdot m^2 / C^2} \).
Units check. \( \mathrm{N \cdot m^2 / C^2} \times \mathrm{C^2 / m^2} = \mathrm{N} \). The units are consistent.
Three quick tests
- Why is the image charge for a grounded plane always equal in magnitude and opposite in sign to the real charge?
Answer
To ensure the potential is zero everywhere on the plane, the contributions from the real and image charges must cancel exactly on the symmetry plane. - For a charge near a grounded sphere, where is the image charge located relative to the sphere's center?
Answer
It is located on the line connecting the center to the real charge, at a distance \( a^2/b \) from the center, inside the sphere. - Can you use the image charge to calculate the electric field inside the conducting sphere?
Answer
No, the method of images is only valid in the region outside the conductor where the real charge resides. Inside the conductor, the field is zero.
Problem set for PU-102 →
Each derivation in this unit ends with five graded problems with full solutions.
Lecture notes drafted with a local model and checked line by line by the editor; every number in the worked example was recomputed.
Derivations cited: D-044 · D-043 · Threads: force, energy, fields