Prerequisites
Before studying this topic, make sure you understand:
- Electric Field — Field creates potential
- Work-Energy Theorem — Work and energy concepts
- Line integrals (basic calculus)
The Hook: Why Don’t Birds Get Shocked on Power Lines?
You’ve seen birds sitting comfortably on high-voltage power lines carrying thousands of volts. Why don’t they get electrocuted?
Or in Thor movies, why can Thor withstand lightning (millions of volts) while humans can’t? Or in Iron Man, how does the arc reactor store massive energy in a tiny space?
The answer isn’t about voltage (potential) alone — it’s about potential difference. The bird’s two feet are at the same potential, so no current flows through it!
Understanding electric potential is the key to understanding how circuits work, how batteries store energy, and why some shocks are deadly while others are harmless.
What is Electric Potential?
where:
- $V$ = electric potential (unit: Volt, V = J/C)
- $W$ = work done
- $q_0$ = test charge (positive)
In simple terms: Potential is the “electric energy per unit charge” at a location.
Electric potential is like gravitational potential energy per unit mass (height).
| Gravity | Electricity |
|---|---|
| Height ($h$) | Potential ($V$) |
| Mass falls down | Positive charge moves to lower potential |
| PE = $mgh$ | PE = $qV$ |
| Force: $\vec{F} = m\vec{g}$ | Force: $\vec{F} = q\vec{E}$ |
Just as water flows downhill, positive charges “flow” from high to low potential!
Electric Potential vs Electric Field
| Electric Field $\vec{E}$ | Electric Potential $V$ |
|---|---|
| Vector quantity | Scalar quantity |
| Force per unit charge | Energy per unit charge |
| Unit: N/C or V/m | Unit: Volt (V) or J/C |
| Tells direction of force | Tells “height” in energy landscape |
| Difficult to add (vectors) | Easy to add (scalars) |
Key Advantage of Potential: It’s a scalar! Much easier to calculate and add than vector fields.
Potential Due to a Point Charge
For a point charge $Q$ at distance $r$:
$$\boxed{V = k\frac{Q}{r} = \frac{1}{4\pi\varepsilon_0}\frac{Q}{r}}$$where $k = 9 \times 10^9$ N·m²/C²
Sign convention:
- Positive charge ($Q > 0$): $V > 0$ (positive potential)
- Negative charge ($Q < 0$): $V < 0$ (negative potential)
At infinity: $V = 0$ (reference point)
“Voltage equals K-Q-over-R”
Compare with field: $E = k\frac{Q}{r^2}$ (has $r^2$ in denominator)
Pattern:
- Field: $E \propto \frac{1}{r^2}$
- Potential: $V \propto \frac{1}{r}$
Potential falls off slower than field!
Potential Difference
Also called: Voltage (when referring to potential difference)
Example: A 12V battery means the potential difference between its terminals is 12 volts — it can do 12 joules of work per coulomb of charge.
A bird on a power line has both feet at (nearly) the same potential!
$$V_A - V_B \approx 0 \implies W = 0$$No potential difference → no current → no shock!
But if the bird touches two wires or touches the wire and ground — huge potential difference → electrocution!
Same reason you can touch one terminal of a battery safely, but touching both simultaneously with wet hands is dangerous.
Relation Between Electric Field and Potential
Electric field is the negative gradient of potential:
$$\boxed{\vec{E} = -\nabla V}$$In 1D (say, along x-axis):
$$\boxed{E = -\frac{dV}{dx}}$$Or equivalently:
$$\boxed{V_B - V_A = -\int_A^B \vec{E} \cdot d\vec{l}}$$Interactive Demo: Visualize Electric Field and Potential
Explore how electric field lines relate to equipotential surfaces.
Physical meaning:
- Field points from high potential to low potential
- Steeper potential change → stronger electric field
- Constant potential (plateau) → zero field
Potential = Height of mountain
Field = Steepness of slope
- Steep cliff (large $E$) → rapid potential drop
- Flat plateau ($E = 0$) → constant potential
- Water flows downhill (high to low potential)
In Pushpa 2, when characters stand on a cliff — height difference is like potential difference, steepness is like electric field!
Potential Due to Multiple Charges (Superposition)
Since potential is a scalar, we can simply add potentials due to individual charges:
$$\boxed{V = V_1 + V_2 + V_3 + ... = \sum_{i=1}^n k\frac{q_i}{r_i}}$$Much easier than adding vector fields!
Example: For two charges $q_1$ and $q_2$ at distances $r_1$ and $r_2$ from point P:
$$V_P = k\frac{q_1}{r_1} + k\frac{q_2}{r_2}$$(No vector addition, no components — just arithmetic!)
Potential Due to Special Charge Distributions
1. Electric Dipole
For a dipole with moment $\vec{p}$, at distance $r$ making angle $\theta$ with dipole axis:
$$\boxed{V = \frac{kp\cos\theta}{r^2}}$$Special cases:
- On axis ($\theta = 0°$): $V = \frac{kp}{r^2}$
- On equatorial line ($\theta = 90°$): $V = 0$
2. Uniformly Charged Ring
Ring of radius $R$ with total charge $Q$, at distance $x$ on axis:
$$\boxed{V = \frac{kQ}{\sqrt{R^2 + x^2}}}$$Special cases:
- At center ($x = 0$): $V = \frac{kQ}{R}$
- Far away ($x >> R$): $V \approx \frac{kQ}{x}$ (point charge)
3. Uniformly Charged Disk
Disk of radius $R$ with surface charge density $\sigma$, at distance $x$ on axis:
$$V = \frac{\sigma}{2\varepsilon_0}\left(\sqrt{R^2 + x^2} - x\right)$$4. Uniformly Charged Spherical Shell (radius $R$, charge $Q$)
Outside ($r \geq R$):
$$V = k\frac{Q}{r}$$On surface ($r = R$):
$$V = k\frac{Q}{R}$$Inside ($r < R$):
$$\boxed{V = k\frac{Q}{R} = \text{constant}}$$Key point: Potential is constant inside (but not zero!)
Since $E = -\frac{dV}{dr}$ and $V$ is constant inside, $E = 0$ inside (consistent with Gauss’s Law).
5. Uniformly Charged Solid Sphere (radius $R$, charge $Q$)
Outside ($r \geq R$):
$$V = k\frac{Q}{r}$$Inside ($r < R$):
$$\boxed{V = \frac{kQ}{2R^3}(3R^2 - r^2)}$$At center ($r = 0$):
$$V_{center} = \frac{3kQ}{2R}$$Equipotential Surfaces
Properties:
No work to move a charge along an equipotential surface
$$W = q(V_B - V_A) = 0 \quad (\text{if } V_B = V_A)$$Electric field is perpendicular to equipotential surfaces
- Field is along direction of steepest potential decrease
- Along equipotential, potential doesn’t change → field must be perpendicular
Field lines and equipotential surfaces are always orthogonal (at 90°)
Closer surfaces → stronger field (rapid potential change)
Conductors in electrostatic equilibrium are equipotential volumes
- Entire conductor at same potential
- Surface is an equipotential
Think of topographic maps used in hiking:
- Contour lines = equipotential surfaces
- Closer contours = steeper terrain = stronger field
- Water flows perpendicular to contours (like field lines perpendicular to equipotentials)
In Interstellar, when they show topographic maps of planets — same concept!
Equipotential Surfaces for Common Configurations
| Charge Distribution | Equipotential Surfaces |
|---|---|
| Point charge | Concentric spheres centered at charge |
| Infinite line charge | Concentric cylinders around line |
| Infinite plane sheet | Parallel planes to the sheet |
| Electric dipole | Complex 3D surfaces (figure-8 shape near dipole) |
| Uniform field | Equally spaced parallel planes perpendicular to field |
| Conductor | Surface of conductor (entire conductor at same potential) |
Electric Potential Energy
For a system of two point charges $q_1$ and $q_2$ at distance $r$:
$$\boxed{U = k\frac{q_1 q_2}{r}}$$Sign convention:
- Same signs ($q_1 q_2 > 0$): $U > 0$ (repulsion, positive energy)
- Opposite signs ($q_1 q_2 < 0$): $U < 0$ (attraction, negative energy)
Reference: $U = 0$ when charges are at infinite separation
Potential Energy of a System of Charges
For a system of $n$ charges, the total potential energy is:
$$\boxed{U = k\sum_{iExample: Three charges
For charges $q_1$, $q_2$, $q_3$:
$$U = k\left[\frac{q_1 q_2}{r_{12}} + \frac{q_1 q_3}{r_{13}} + \frac{q_2 q_3}{r_{23}}\right]$$(3 pairs: 1-2, 1-3, 2-3)
Wrong: Add $U = q_1 V_1 + q_2 V_2 + q_3 V_3$
This double counts each pair!
Correct: Use pairwise formula: $U = \sum_{i Or: $U = \frac{1}{2}\sum_{i=1}^n q_i V_i$ (where $V_i$ is potential at $q_i$ due to other charges)
Work-Energy Theorem in Electrostatics
Work done by electric field on charge $q$ moving from A to B:
$$W_{field} = q(V_A - V_B)$$Work done by external agent (against field):
$$W_{external} = q(V_B - V_A) = -W_{field}$$Change in kinetic energy:
$$\Delta KE = W_{field} = q(V_A - V_B)$$Conservation of energy:
$$KE_A + U_A = KE_B + U_B$$ $$\frac{1}{2}mv_A^2 + qV_A = \frac{1}{2}mv_B^2 + qV_B$$Electron Volt (eV)
Useful for atomic and nuclear physics where energies are tiny!
Examples:
- Ionization energy of hydrogen: 13.6 eV
- Rest mass energy of electron: $m_e c^2 = 0.511$ MeV
- Energy per photon (visible light): ~2 eV
Conversion:
If electron accelerates through potential $V$:
$$KE = eV = 1.6 \times 10^{-19} \times V \text{ joules}$$Or simply: $KE = V$ eV
Memory Tricks & Patterns
Mnemonic for Potential Formulas
“Voltage is K-Q-over-R” → $V = k\frac{Q}{r}$
“U equals Q-V” → $U = qV$
“Energy is K-Q-Q-over-R” → $U = k\frac{q_1 q_2}{r}$
Pattern Recognition
| Quantity | Point Charge | Dipole |
|---|---|---|
| Field $E$ | $\frac{1}{r^2}$ | $\frac{1}{r^3}$ |
| Potential $V$ | $\frac{1}{r}$ | $\frac{1}{r^2}$ |
Rule: Potential always has one less power of r than field!
This is because $E = -\frac{dV}{dr}$ (derivative reduces power by 1)
When to Use Potential vs Field
Use Electric Potential when:
- Asked about energy, work, or voltage
- Multiple charges (scalar addition is easier!)
- Need to find field later using $E = -\frac{dV}{dr}$
- Given equipotential surfaces
Use Electric Field when:
- Asked about force or acceleration
- Need direction of force
- Using Gauss’s Law (symmetric problems)
- Field line visualization
Common Mistakes to Avoid
Wrong: “Potential and potential energy are the same”
Correct:
- Potential $V$ = energy per unit charge (property of space)
- Potential energy $U = qV$ = energy of a specific charge at that point
Wrong: “Positive charge moves to higher potential, gaining energy”
Correct:
- Positive charge naturally moves to lower potential (loses PE, gains KE)
- To move to higher potential requires external work
Same as ball rolling downhill vs lifting it uphill!
Wrong: “Field inside shell is zero, so potential is zero”
Correct:
- Field inside = 0 (true!)
- Potential inside = $k\frac{Q}{R}$ = constant (not zero!)
$E = 0$ means $\frac{dV}{dr} = 0$ (constant), not $V = 0$
Wrong: “No field on equipotential surface”
Correct:
- No work along equipotential ($\vec{E}$ perpendicular to motion)
- Field exists but is perpendicular to surface
Zero work ≠ zero field!
Practice Problems
Level 1: Foundation (NCERT)
Find the potential at a distance of 9 cm from a charge of $+5$ μC.
Solution:
$$V = k\frac{Q}{r} = 9 \times 10^9 \times \frac{5 \times 10^{-6}}{0.09}$$ $$V = 9 \times 10^9 \times \frac{5 \times 10^{-6}}{9 \times 10^{-2}} = 5 \times 10^5 \text{ V}$$ $$\boxed{V = 5 \times 10^5 \text{ V} = 500 \text{ kV}}$$An electron is accelerated from rest through a potential difference of 100 V. Find its final kinetic energy in eV and joules.
Solution:
In eV:
$$KE = eV = 100 \text{ eV}$$In joules:
$$KE = 100 \times 1.6 \times 10^{-19} = 1.6 \times 10^{-17} \text{ J}$$ $$\boxed{KE = 100 \text{ eV} = 1.6 \times 10^{-17} \text{ J}}$$Two charges $+3$ μC and $+5$ μC are placed at $(0, 0)$ and $(4, 0)$ m. Find potential at $(4, 3)$ m.
Solution:
Distance from $q_1 = 3$ μC at origin to point $(4, 3)$:
$$r_1 = \sqrt{4^2 + 3^2} = 5 \text{ m}$$Distance from $q_2 = 5$ μC at $(4, 0)$ to point $(4, 3)$:
$$r_2 = 3 \text{ m}$$ $$V = k\frac{q_1}{r_1} + k\frac{q_2}{r_2} = 9 \times 10^9 \left[\frac{3 \times 10^{-6}}{5} + \frac{5 \times 10^{-6}}{3}\right]$$ $$V = 9 \times 10^3 \left[\frac{3}{5} + \frac{5}{3}\right] = 9 \times 10^3 \left[\frac{9 + 25}{15}\right]$$ $$V = 9 \times 10^3 \times \frac{34}{15} = 20.4 \times 10^3 \text{ V}$$ $$\boxed{V = 20.4 \text{ kV}}$$Level 2: JEE Main
A hollow metal sphere of radius 10 cm is charged to 100 V. Find the potential at (a) the center, (b) the surface, (c) 20 cm from center.
Solution:
(a) At center ($r = 0$):
Inside a spherical shell, potential is constant:
$$\boxed{V_{center} = 100 \text{ V}}$$(b) At surface ($r = R = 10$ cm):
$$\boxed{V_{surface} = 100 \text{ V}}$$(Given)
(c) At $r = 20$ cm (outside):
Outside: $V = k\frac{Q}{r}$
At surface: $V_R = k\frac{Q}{R} = 100$ V
So, $kQ = 100R = 100 \times 0.1 = 10$ V·m
At $r = 0.2$ m:
$$V = \frac{10}{0.2} = 50 \text{ V}$$ $$\boxed{V = 50 \text{ V}}$$Find the work done to bring three charges $q$, $q$, and $-q$ from infinity to the vertices of an equilateral triangle of side $a$.
Solution:
Step-by-step assembly:
Bring first $q$: $W_1 = 0$ (no other charges present)
Bring second $q$ to distance $a$ from first:
$$W_2 = k\frac{q \cdot q}{a} = \frac{kq^2}{a}$$Bring third $-q$:
- Potential due to first two charges at third vertex: $$V = k\frac{q}{a} + k\frac{q}{a} = \frac{2kq}{a}$$
- Work: $W_3 = (-q) \times V = -q \times \frac{2kq}{a} = -\frac{2kq^2}{a}$
Total work:
$$W = W_1 + W_2 + W_3 = 0 + \frac{kq^2}{a} - \frac{2kq^2}{a}$$ $$\boxed{W = -\frac{kq^2}{a}}$$(Negative work means system releases energy — it’s bound!)
A uniform electric field $E = 1000$ V/m points in the +x direction. Find the potential difference between points $(0, 0, 0)$ and $(1, 0, 0)$ m.
Solution:
For uniform field:
$$V_B - V_A = -\int_A^B \vec{E} \cdot d\vec{l}$$ $$V(1,0,0) - V(0,0,0) = -\int_0^1 E \, dx = -E \times 1$$ $$V_B - V_A = -1000 \text{ V}$$ $$\boxed{\Delta V = -1000 \text{ V}}$$(Moving in direction of field → potential decreases)
Level 3: JEE Advanced
Four charges $q$, $-q$, $q$, $-q$ are placed at the corners of a square of side $a$ in order. Find the work to bring a fifth charge $Q$ from infinity to the center.
Solution:
Potential at center due to four charges:
Distance from each corner to center: $r = \frac{a}{\sqrt{2}}$
$$V_{center} = \sum k\frac{q_i}{r} = k\frac{1}{a/\sqrt{2}}\left[q + (-q) + q + (-q)\right]$$ $$V_{center} = \frac{k\sqrt{2}}{a} \times 0 = 0$$Work to bring $Q$:
$$W = Q \times V_{center} = Q \times 0$$ $$\boxed{W = 0}$$Key insight: Alternating charges create zero net potential at center!
A non-uniform electric field $\vec{E} = (200x)\hat{i}$ V/m exists in a region. Find the potential difference between origin and point $(2, 0, 0)$ m.
Solution:
$$V(2,0,0) - V(0,0,0) = -\int_0^2 \vec{E} \cdot d\vec{l}$$ $$= -\int_0^2 200x \, dx = -200 \left[\frac{x^2}{2}\right]_0^2$$ $$= -200 \times 2 = -400 \text{ V}$$ $$\boxed{\Delta V = -400 \text{ V}}$$An electric dipole with charges $\pm 10$ μC separated by 2 mm is placed at the origin along the y-axis (positive charge at +y). Find the potential at point $(3, 4)$ cm.
Solution:
Dipole moment: $p = q \times 2a = 10 \times 10^{-6} \times 2 \times 10^{-3} = 2 \times 10^{-8}$ C·m
Point $(3, 4)$ cm = $(0.03, 0.04)$ m
Distance: $r = \sqrt{0.03^2 + 0.04^2} = 0.05$ m = 5 cm
Angle with dipole axis (y-axis):
$$\cos\theta = \frac{y}{r} = \frac{0.04}{0.05} = 0.8$$ $$V = \frac{kp\cos\theta}{r^2} = \frac{9 \times 10^9 \times 2 \times 10^{-8} \times 0.8}{(0.05)^2}$$ $$V = \frac{144 \times 10}{2.5 \times 10^{-3}} = 57.6 \times 10^3 \text{ V}$$ $$\boxed{V = 57.6 \text{ kV}}$$Quick Revision Box
| Concept | Formula/Key Point |
|---|---|
| Electric potential | $V = \frac{W}{q_0}$ (work per unit charge from ∞) |
| Point charge potential | $V = k\frac{Q}{r}$ |
| Potential difference | $V_A - V_B = -\int_B^A \vec{E} \cdot d\vec{l}$ |
| Field from potential | $\vec{E} = -\nabla V$ or $E = -\frac{dV}{dr}$ |
| Superposition | $V = \sum k\frac{q_i}{r_i}$ (scalar sum) |
| Potential energy | $U = qV$ or $U = k\frac{q_1 q_2}{r}$ |
| System energy | $U = \sum_{i |
| Work by field | $W = q(V_A - V_B)$ |
| Equipotential | $V =$ constant, $\vec{E} \perp$ surface |
| Conductor | Entire volume at same potential |
| Inside shell | $V = k\frac{Q}{R}$ (constant) |
| Electron volt | 1 eV = $1.6 \times 10^{-19}$ J |
JEE Weightage: 2-3 questions in JEE Main, 1-2 in JEE Advanced (often with capacitors or energy)
Time-Saver: Use potential (scalar) instead of field (vector) when possible — much easier to add!
Teacher’s Summary
- Potential is scalar — much easier to work with than vector field
- Potential difference drives current — voltage, not absolute potential, matters
- Field points from high to low potential — like water flowing downhill
- Equipotentials are perpendicular to field lines — fundamental relationship
- Conductor is equipotential — field inside = 0, potential = constant
“Potential is the landscape of energy. Charges naturally ‘roll downhill’ from high to low potential, just like water flows from mountains to valleys.”
Related Topics
Within Electrostatics
- Electric Field — Field creates potential
- Electric Charges — Point charge potential
- Gauss’s Law — Field calculations for potential
- Capacitors — Storing charge and energy using potential difference
Connected Chapters
- Current Electricity — Potential difference drives current
- Work-Energy-Power — Energy conservation
- Magnetism — Magnetic potential (analogous concept)
Math Connections
- Calculus — Gradient, line integrals
- Vectors — Gradient operator
- Differential Equations — Laplace’s equation