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).

V=WPq0W=q0V

SI unit: Volt (V) = J/C  |  Scalar quantity  |  Reference: V = 0 at infinity

Potential due to a Point Charge

V=kQr=14πε0Qr

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:

Vtotal=V1+V2+V3+=kQiri

2. Potential due to a Dipole

V=kpcosθr2(ra)

Where θ is the angle from the dipole axis.

PositionθV
Axial (same side as +q)+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=kQ1Q2r

U > 0: like charges (repulsive, must do work to bring together). U < 0: unlike charges (attractive, system releases energy).

System of Three Charges

U=k(Q1Q2r12+Q2Q3r23+Q1Q3r13)

Sum over all distinct pairs — each pair counted once.

Work Done in Moving a Charge

W=q(VAVB)=qΔV

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

E=dVdrE=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).