1. Electric Potential — Definition
The Electric Potential V at a point is defined as the work done per unit positive test charge in bringing it from infinity to that point, without acceleration (quasi-statically).
SI unit: Volt (V) = J/C | Scalar quantity | Reference: V = 0 at infinity
Potential due to a Point Charge
V > 0 for positive charge; V < 0 for negative charge. V falls as 1/r (slower than E which falls as 1/r²).
Superposition Principle for Potential
Total potential = algebraic sum (scalar sum, not vector sum) of potentials due to individual charges:
2. Potential due to a Dipole
Where θ is the angle from the dipole axis.
| Position | θ | V |
|---|---|---|
| Axial (same side as +q) | 0° | +kp/r² |
| Axial (same side as −q) | 180° | −kp/r² |
| Equatorial (perp. bisector) | 90° | 0 (always, at all distances) |
Example: p = 4 nC·m, r = 20 cm, θ = 60°: V = kp cosθ/r² = 9×10⁹ × 4×10⁻⁹ × 0.5 / (0.2)² = 450 V
3. Potential Energy of a System of Charges
Two Charges
U > 0: like charges (repulsive, must do work to bring together). U < 0: unlike charges (attractive, system releases energy).
System of Three Charges
Sum over all distinct pairs — each pair counted once.
Work Done in Moving a Charge
Moving from B to A. Work done by external agent (against electric force). If Va > Vb and q > 0: positive work must be done.
4. Relationship Between E and V
Electric field points in the direction of decreasing potential (from high V to low V). E is the negative gradient of V.
For uniform field: E = V/d (V = potential difference, d = distance between plates).
5. Equipotential Surfaces
An equipotential surface is a surface on which all points are at the same electric potential. Key properties:
- E is always perpendicular to an equipotential surface — no work is done moving a charge along the surface.
- Equipotential surfaces never cross each other.
- For a point charge: equipotential surfaces are concentric spheres.
- For a uniform field: equipotential surfaces are parallel planes ⊥ to E.
- For a dipole: equipotential surfaces are more complex; V = 0 on the equatorial plane.
- Closer equipotential surfaces → stronger E field (larger potential gradient).

