UY1: Electric Field Of An Electric Dipole
Derive exact and far-field electric-field formulas for a dipole on axial and equatorial lines, with direction and sign clarity.
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The core idea
On this page
Learning objectives
- Construct electric-field and potential models for discrete and continuous charge distributions.
This page gives the UY1 working model/result for Electric Field Of An Electric Dipole. You reuse it when you build fields/potentials by symmetry or superposition, and when you connect fields to forces, energy, and circuits.
- Module path: Electromagnetism (UY1)
- Practice: UY1 Electromagnetism Quiz
- Full routing: UY1 Assessment Map
- Math toolkit: Mathematics for Undergraduate Physics
1) At a glance
- Prerequisites: dipole moment and torque/energy ideas (Electric Dipole), superposition from point charges (Coulomb’s Law)
- Outcomes: compute vector E on axial/equatorial lines, choose exact vs far-field forms, and state direction correctly
- Key result (far field): dipole fields fall as 1/r³ (faster than a point charge’s 1/r²)
- Common trap: using the far-field forms when r is not much larger than a, or mixing axial vs equatorial directions
- A dipole has charges + q and -q separated by 2a.
- Dipole moment magnitude: p = 2aq (direction from -q to + q).
- On the axial line (far field):
- On the equatorial line (far field):
with direction opposite to vector p.
Motivation / intuition
Most real objects are electrically neutral overall (Qₙₑₜ = 0). Far away, their leading electric effect is often a dipole, so these 1/r³ results are the standard “first approximation” for many neutral systems.
2) Setup
- Place dipole on x-axis: -q at x = -a, + q at x = +a.
- Use superposition of fields from each charge.
- Keep vector directions explicit; many sign errors come from direction, not algebra.
3) Core derivation/explanation
Axial point
Let point P be at x > a on x-axis.
Simplify:
For x≫ a:
Direction is along + x hat (same direction as vector p on the + side).
Equatorial point
Let point P be on y-axis at distance r from center. By symmetry, y-components cancel and x-components add:
For r≫ a:
The minus sign shows direction opposite to vector p.
The approximations Eₐₓᵢₐₗ ≈ k(2p/r³) and E_eq ≈ k(p/r³) require r≫ a (distance from the dipole much larger than half-separation).
- Units: [k p/r³] = (N m² C⁻²)(C m)/m³ = N/C.
- Limits/signs: as r → ∞, E → 0 like 1/r³; on the +x axial side the field points with vector p, while on the equatorial line it points opposite vector p.
4) Worked example(s)
Given q = 2.0 μC, a = 0.020 m, find axial field at x = 0.30 m.
Exact:
Direction: + x hat.
Far-field estimate:
Close agreement confirms x≫ a approximation is reasonable.
5) Practice set (with hints + answers)
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A dipole has p = 3.0 × 10⁻⁸ C m. Find far axial field at r = 0.50 m. Hint: use Eₐₓᵢₐₗ ≈ k(2p/r³). Answer: E ≈ 4.31 × 10³ N C⁻¹.
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Same dipole, find far equatorial field magnitude at r = 0.50 m. Hint: E_eq ≈ k(p/r³). Answer: E ≈ 2.16 × 10³ N C⁻¹, opposite vector p.
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What is the far-field ratio Eₐₓᵢₐₗ/E_eq at equal r? Hint: compare coefficients. Answer: 2.
6) Summary + next steps
- Dipole fields come from superposition of two point-charge fields.
- Exact formulas are useful near the dipole; 1/r³ formulas are for far field.
- Direction differs by location: axial follows vector p, equatorial opposes vector p.
Next: Electric Field Of A Ring Of Charge Previous: Electric Field Lines Back To Electromagnetism (UY1) Back to Electromagnetism (UY1)