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Unit 2: Electric Potential

Physics C E&M cheatsheet

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Michael’s a bum

For two point charges QQ and qq separated by distance rr, with the usual choice that potential energy is zero when the charges are infinitely far apart, the electric potential energy of the pair is

U=14πε0Qqr=kQqr.U = \frac{1}{4\pi \varepsilon_0} \frac{Qq}{r} = k \frac{Qq}{r}.

If the separation changes from rir_i to rfr_f, the change in potential energy is

ΔU=kQq(1rf−1ri).\Delta U = kQq \left( \frac{1}{r_f} - \frac{1}{r_i} \right).

This mirrors gravitation: the interaction energy depends on 1/r1/r, and you must fix a reference (here, U→0U \to 0 as r→∞r \to \infty) before speaking of “the” energy at a finite separation. Unlike gravitation, however, the sign of UU can be positive (like charges, which repel) or negative (unlike charges, which attract).


For more than two charges, the total potential energy is the sum over distinct pairs:

U=k∑i<jqiqjrij.U = k \sum_{i<j} \frac{q_i q_j}{r_{ij}}.

The condition i<ji<j counts each pair exactly once. A clean way to see this is to assemble the configuration one charge at a time: bringing in the first charge takes no work (empty space), the second is brought in against the first charge’s field, the third against the field of the first two, and so on. The total work needed equals UU, and because the electrostatic force is conservative, the answer does not depend on the order of assembly.

q1q2q3sumpairwisepotentialenergies

Example. Three point charges are fixed at the corners of an equilateral triangle of side a=0.20 ma = 0.20\ \text{m}: q1=+2.0 μCq_1 = +2.0\ \mu\text{C}, q2=−3.0 μCq_2 = -3.0\ \mu\text{C}, and q3=+4.0 μCq_3 = +4.0\ \mu\text{C}. How much total electric potential energy is stored in this configuration? Use k=8.99×109 N m2/C2k = 8.99\times10^{9}\ \text{N}\,\text{m}^2/\text{C}^2.

Every pair is separated by the same distance rij=ar_{ij} = a, so

U=k∑i<jqiqjrij=ka(q1q2+q1q3+q2q3).U = k\sum_{i<j}\frac{q_iq_j}{r_{ij}} = \frac{k}{a}\big(q_1q_2 + q_1q_3 + q_2q_3\big).

Compute the products (in C2\text{C}^2), keeping the microcoulomb factor 10−6×10−6=10−1210^{-6}\times10^{-6} = 10^{-12}:

q1q2=(2.0)(−3.0)×10−12=−6.0×10−12,q_1q_2 = (2.0)(-3.0)\times10^{-12} = -6.0\times10^{-12}, q1q3=(2.0)(4.0)×10−12=+8.0×10−12,q_1q_3 = (2.0)(4.0)\times10^{-12} = +8.0\times10^{-12}, q2q3=(−3.0)(4.0)×10−12=−12.0×10−12.q_2q_3 = (-3.0)(4.0)\times10^{-12} = -12.0\times10^{-12}.

The sum of products is (−6.0+8.0−12.0)×10−12=−10.0×10−12 C2(-6.0 + 8.0 - 12.0)\times10^{-12} = -10.0\times10^{-12}\ \text{C}^2. Therefore

U=8.99×1090.20 (−10.0×10−12)=(4.50×1010)(−1.00×10−11)≈−0.45 J.U = \frac{8.99\times10^{9}}{0.20}\,(-10.0\times10^{-12}) = (4.50\times10^{10})(-1.00\times10^{-11}) \approx -0.45\ \text{J}.

The negative total means the attractive pairs dominate: net work is released in assembling this configuration, and an external agent would have to do +0.45 J+0.45\ \text{J} of work to pull all three charges back out to infinity.


The electric potential VV at a point is potential energy per unit charge for a small positive test charge q0q_0 placed at that point:

V=Uq0.V = \frac{U}{q_0}.

Units are volts (V), where 1 V=1 J/C1 \text{ V} = 1 \text{ J/C}. Colloquially, VV is often called voltage, especially when discussing potential difference ΔV\Delta V between two points.

For a single source point charge QQ, with V=0V = 0 at infinity,

V=14πε0Qr=kQr.V = \frac{1}{4\pi \varepsilon_0} \frac{Q}{r} = \frac{kQ}{r}.

Potential is a scalar: many-source problems add VV by ordinary addition (no vector triangles), unlike electric field.

Proof (potential of a point charge). Define potential as the work per unit charge to bring a test charge from infinity to the point, equivalently the negative line integral of the field from infinity to rr:

V(r)=−∫∞rE⃗⋅dr⃗.V(r) = -\int_\infty^r \vec{E}\cdot d\vec{r}.

The field of a point charge QQ points radially, E⃗=kQr′2r^\vec{E} = \dfrac{kQ}{r'^2}\hat{r}. Integrating in along a radial path, dr⃗=dr′ r^d\vec{r} = dr'\,\hat{r}, so E⃗⋅dr⃗=kQr′2 dr′\vec{E}\cdot d\vec{r} = \dfrac{kQ}{r'^2}\,dr':

V(r)=−∫∞rkQr′2 dr′=−kQ[−1r′]∞r=kQ(1r−1∞)=kQr.V(r) = -\int_\infty^r \frac{kQ}{r'^2}\,dr' = -kQ\left[-\frac{1}{r'}\right]_\infty^r = kQ\left(\frac{1}{r} - \frac{1}{\infty}\right) = \frac{kQ}{r}.

The reference V(∞)=0V(\infty) = 0 is exactly what makes the lower-limit term vanish. The radial path is allowed because the field is conservative (proved below), so any path from infinity gives the same answer.

Proof (the electrostatic field is conservative). The field of a single point charge QQ is radial, E⃗=kQr2r^\vec{E} = \dfrac{kQ}{r^2}\hat{r}. For any path between two points aa and bb, write the displacement in spherical-like terms: only the radial component of dr⃗d\vec{r} survives the dot product with r^\hat{r}, and that radial component is just drdr. Hence

∫abE⃗⋅dr⃗=∫rarbkQr2 dr=kQ(1ra−1rb),\int_a^b \vec{E}\cdot d\vec{r} = \int_{r_a}^{r_b}\frac{kQ}{r^2}\,dr = kQ\left(\frac{1}{r_a} - \frac{1}{r_b}\right),

which depends only on the endpoints ra,rbr_a,r_b, not on the route. Around a closed loop the start and end radii are equal, so

∮E⃗⋅dr⃗=0.\oint \vec{E}\cdot d\vec{r} = 0.

By superposition, any electrostatic field is a sum of point-charge fields, and a sum of terms each integrating to zero around a loop also integrates to zero. Because the work around every closed loop vanishes, the work between two points is path-independent, and a single-valued potential VV can be defined. This is the electrostatic analog of gravity being conservative.


Potential from many charges and distributions

Section titled “Potential from many charges and distributions”

Since potential is a scalar, the potential of several source charges is just the signed algebraic sum

V=k∑iqiri,V = k \sum_i \frac{q_i}{r_i},

where rir_i is the distance from source ii to the field point. For a continuous distribution, integrate over charge elements:

V=k∫dqr,dq=λ dℓ, σ dA, or ρ dV.V = k \int \frac{dq}{r}, \qquad dq = \lambda\, d\ell,\ \sigma\, dA,\ \text{or}\ \rho\, dV.

There are no components to track, only distances, so potential integrals are usually easier than field integrals. When the field is already known from symmetry (Gauss’s law), it is often faster to integrate the field instead:

Vb−Va=−∫abE⃗⋅dr⃗.V_b - V_a = -\int_a^b \vec{E} \cdot d\vec{r}.

Example. Two point charges sit on the xx-axis: q1=+5.0 nCq_1 = +5.0\ \text{nC} at x=0x = 0 and q2=−3.0 nCq_2 = -3.0\ \text{nC} at x=0.40 mx = 0.40\ \text{m}. Find the electric potential at the point P=(0.40 m, 0.30 m)P = (0.40\ \text{m},\ 0.30\ \text{m}), which lies directly above q2q_2.

Potential is a scalar, so just add the contributions with their signs—no vector components. The distances from each source to PP are

r1=(0.40)2+(0.30)2=0.16+0.09=0.25=0.50 m,r_1 = \sqrt{(0.40)^2 + (0.30)^2} = \sqrt{0.16 + 0.09} = \sqrt{0.25} = 0.50\ \text{m}, r2=0.30 m(straight down to q2).r_2 = 0.30\ \text{m} \quad (\text{straight down to } q_2).

Then

VP=k(q1r1+q2r2)=8.99×109(5.0×10−90.50+−3.0×10−90.30).V_P = k\left(\frac{q_1}{r_1} + \frac{q_2}{r_2}\right) = 8.99\times10^{9}\left(\frac{5.0\times10^{-9}}{0.50} + \frac{-3.0\times10^{-9}}{0.30}\right).

Evaluate each term: 5.0×10−90.50=1.0×10−8\dfrac{5.0\times10^{-9}}{0.50} = 1.0\times10^{-8} and −3.0×10−90.30=−1.0×10−8\dfrac{-3.0\times10^{-9}}{0.30} = -1.0\times10^{-8}, which cancel:

VP=8.99×109 (1.0×10−8−1.0×10−8)=0 V.V_P = 8.99\times10^{9}\,(1.0\times10^{-8} - 1.0\times10^{-8}) = 0\ \text{V}.

The potential at PP is exactly zero. Crucially, this does not mean the field is zero there: E⃗\vec{E} is a vector sum of two nonzero, non-collinear contributions and is generally nonzero on the V=0V=0 surface. Adding scalars (with sign) is far easier than adding the vector fields, which is the whole reason potential is convenient.

For a thin spherical shell of radius RR and total charge QQ (with V→0V \to 0 at infinity),

V(r)={kQ/R,r≤R,kQ/r,r≥R.V(r) = \begin{cases} kQ/R, & r \le R,\\ kQ/r, & r \ge R. \end{cases}

Inside the shell the field is zero, so VV is constant, not zero—no field does not mean no potential. For a uniformly charged solid sphere of radius RR,

V(r)={kQ2R(3−r2R2),r≤R,kQ/r,r≥R.V(r) = \begin{cases} \dfrac{kQ}{2R}\left(3 - \dfrac{r^2}{R^2}\right), & r \le R,\\[2mm] kQ/r, & r \ge R. \end{cases}

In both cases VV is continuous everywhere, even at a boundary where the field changes abruptly.

Proof (on-axis potential of a uniformly charged ring). A ring of radius RR carries total charge QQ spread uniformly. Find VV at a point on the axis a distance xx from the center.

Every charge element dqdq on the ring lies at the same distance from the axial point,

r=x2+R2,r = \sqrt{x^2 + R^2},

by the Pythagorean theorem. Since potential is a scalar, dV=k dq/rdV = k\,dq/r and the constant rr comes straight out of the integral:

V=∫k dqr=kx2+R2∫dq=kQx2+R2.V = \int \frac{k\,dq}{r} = \frac{k}{\sqrt{x^2+R^2}}\int dq = \frac{kQ}{\sqrt{x^2+R^2}}.

Notice how painless this is: the field calculation for the same ring requires resolving each dE⃗d\vec{E} into components and arguing that the radial parts cancel, leaving only the axial part with an extra cos⁡θ=x/r\cos\theta = x/r factor. The potential integral has no direction to worry about—just one distance—so the scalar nature of VV saves all that bookkeeping. At the center (x=0x=0) this gives V=kQ/RV = kQ/R; far away (x≫Rx\gg R) it reduces to kQ/xkQ/x, the point-charge result, as it must.

Proof (on-axis potential of a uniformly charged disk). A flat disk of radius RR carries uniform surface charge density σ\sigma, so total charge Q=σπR2Q = \sigma\pi R^2. Find VV on the axis at distance xx from the center.

Slice the disk into thin concentric rings of radius aa and width dada. Each ring has area dA=2πa dadA = 2\pi a\,da and charge dq=σ 2πa dadq = \sigma\,2\pi a\,da. Every point of that ring is a distance x2+a2\sqrt{x^2 + a^2} from the axial point, so by the ring result its contribution to the potential is

dV=k dqx2+a2=k σ 2πa dax2+a2.dV = \frac{k\,dq}{\sqrt{x^2 + a^2}} = \frac{k\,\sigma\,2\pi a\,da}{\sqrt{x^2 + a^2}}.

Integrate over all rings from a=0a = 0 to a=Ra = R:

V=2πkσ∫0Ra dax2+a2.V = 2\pi k\sigma \int_0^R \frac{a\,da}{\sqrt{x^2 + a^2}}.

The substitution u=x2+a2u = x^2 + a^2, du=2a dadu = 2a\,da turns the integral into 12∫u−1/2 du=u\tfrac{1}{2}\int u^{-1/2}\,du = \sqrt{u}, giving

V=2πkσ[x2+a2 ]0R=2πkσ(x2+R2−x).V = 2\pi k\sigma \left[\sqrt{x^2 + a^2}\,\right]_0^R = 2\pi k\sigma\left(\sqrt{x^2 + R^2} - x\right).

Finally use k=14πε0k = \dfrac{1}{4\pi\varepsilon_0}, so 2πk=12ε02\pi k = \dfrac{1}{2\varepsilon_0}:

V=σ2ε0(x2+R2−x).V = \frac{\sigma}{2\varepsilon_0}\left(\sqrt{x^2 + R^2} - x\right).

We took x>0x > 0; for a point on the other side replace xx with ∣x∣\lvert x\rvert. The disk’s potential is built entirely from scalar ring potentials—no components ever appear.


The electrostatic force is conservative. For a charge qq moving from an initial point aa to a final point bb, the work done by the electric field relates to the change in potential energy:

Wfield=−ΔU.W_{\text{field}} = -\Delta U.

Since U=qVU = qV for a charge in a fixed external potential (treating qq as the object being moved),

ΔU=qΔV,\Delta U = q \Delta V,

so

Wfield=−q(Vb−Va)=−qΔV.W_{\text{field}} = -q \left( V_b - V_a \right) = -q \Delta V.

If an external agent moves the charge slowly against the field with no change in kinetic energy, the work that agent does is the negative of the field’s work:

Wext=−Wfield=qΔV.W_{\text{ext}} = -W_{\text{field}} = q \Delta V.

Example. An electron (charge −e-e, mass me=9.11×10−31 kgm_e = 9.11\times10^{-31}\ \text{kg}) starts from rest and is accelerated through a potential difference of ΔV=500 V\Delta V = 500\ \text{V}, gaining energy. Find its final kinetic energy in both eV and joules, then its final speed.

Since the electron is negatively charged, it speeds up when moving toward higher potential. The magnitude of the energy gained equals the charge magnitude times the potential difference. By the work–energy theorem (only the electric force acts), all of that energy becomes kinetic:

12mev2=e ΔV.\tfrac{1}{2}m_e v^2 = e\,\Delta V.

Working in electron volts is immediate: a charge of magnitude ee moving through 500 V500\ \text{V} gains exactly

K=500 eV.K = 500\ \text{eV}.

Converting to joules,

K=(1.602×10−19 C)(500 V)=8.01×10−17 J.K = (1.602\times10^{-19}\ \text{C})(500\ \text{V}) = 8.01\times10^{-17}\ \text{J}.

Solve for the speed:

v=2Kme=2(8.01×10−17)9.11×10−31=1.76×1014≈1.33×107 m/s.v = \sqrt{\frac{2K}{m_e}} = \sqrt{\frac{2(8.01\times10^{-17})}{9.11\times10^{-31}}} = \sqrt{1.76\times10^{14}} \approx 1.33\times10^{7}\ \text{m/s}.

That is about 4%4\% of the speed of light, so the nonrelativistic formula is still a fair approximation here. The electron volt is handy precisely because q ΔVq\,\Delta V with q=eq = e comes out as the voltage in volts, numerically equal to the energy in eV.


Potential and field are linked by

E⃗=−∇V\vec{E} = -\nabla V

in differential form (∇\nabla is just a 3D differential operator, for most purposes, just remember that it is the derivative along an axis). Along a path, the line integral gives the potential difference:

Vb−Va=−∫abE⃗⋅dr⃗.V_b - V_a = -\int_a^b \vec{E} \cdot d\vec{r}.

For a uniform electric field of magnitude EE and a displacement d⃗\vec{d},

ΔV=−E⃗⋅d⃗.\Delta V = -\vec{E} \cdot \vec{d}.

If d⃗\vec{d} points in the direction of E⃗\vec{E}, potential decreases along that direction—consistent with electric field lines pointing from higher to lower potential (for the conventional positive-test-charge picture).

In one dimension the gradient is just an ordinary derivative, so the axial component of the field is recovered by differentiating the potential:

Ex=−dVdx.E_x = -\frac{dV}{dx}.
Ex=¡dV=dxxV

Example. Take the on-axis disk potential derived above,

V(x)=σ2ε0(x2+R2−x),V(x) = \frac{\sigma}{2\varepsilon_0}\left(\sqrt{x^2 + R^2} - x\right),

and recover the on-axis electric field by differentiation, confirming it agrees with the standard field-integral result.

Apply Ex=−dV/dxE_x = -dV/dx. Differentiate term by term, using ddxx2+R2=xx2+R2\dfrac{d}{dx}\sqrt{x^2+R^2} = \dfrac{x}{\sqrt{x^2+R^2}}:

dVdx=σ2ε0(xx2+R2−1).\frac{dV}{dx} = \frac{\sigma}{2\varepsilon_0}\left(\frac{x}{\sqrt{x^2+R^2}} - 1\right).

Therefore

Ex=−dVdx=σ2ε0(1−xx2+R2).E_x = -\frac{dV}{dx} = \frac{\sigma}{2\varepsilon_0}\left(1 - \frac{x}{\sqrt{x^2+R^2}}\right).

This is exactly the on-axis field of a uniformly charged disk obtained the hard way—by integrating the axial components dExdE_x of every ring. Differentiating the scalar potential reproduces it in two lines. As a sanity check, for x≫Rx \gg R a binomial expansion gives 1−xx2+R2≈R22x21 - \dfrac{x}{\sqrt{x^2+R^2}} \approx \dfrac{R^2}{2x^2}, so Ex→σR24ε0x2=kQx2E_x \to \dfrac{\sigma R^2}{4\varepsilon_0 x^2} = \dfrac{kQ}{x^2} with Q=σπR2Q = \sigma\pi R^2—the point-charge field, as expected far away.


An equipotential is a surface (or curve in 2D diagrams) on which VV is constant. No work is required to move a charge along an equipotential, because ΔV=0\Delta V = 0. For that reason, E⃗\vec{E} is everywhere perpendicular to equipotentials (except where E⃗=0\vec{E} = 0): a component of E⃗\vec{E} tangent to the surface would do nonzero work over a small step along the surface, contradicting constant VV.

+q¯eldlinesareperpendiculartoequipotentials

A clean special case is the uniform field between two large parallel plates. The plates themselves are equipotentials, and intermediate equipotentials are evenly spaced planes parallel to them. With the field magnitude EE and plate separation dd, integrating ΔV=−∫E⃗⋅dr⃗\Delta V = -\int \vec{E}\cdot d\vec{r} along the field direction gives the simple magnitude relation ∣ΔV∣=Ed\lvert\Delta V\rvert = Ed.

Example. Two large parallel plates are separated by d=2.0 cm=0.020 md = 2.0\ \text{cm} = 0.020\ \text{m} and connected to a battery so the potential difference between them is ΔV=120 V\Delta V = 120\ \text{V}. Find the magnitude of the uniform field between the plates, and the work the field does on a proton (q=+eq = +e) that travels from the high-potential plate to the low-potential plate.

Between large plates the field is uniform, so ∣ΔV∣=Ed\lvert\Delta V\rvert = Ed gives

E=∣ΔV∣d=120 V0.020 m=6.0×103 V/m.E = \frac{\lvert \Delta V \rvert}{d} = \frac{120\ \text{V}}{0.020\ \text{m}} = 6.0\times10^{3}\ \text{V/m}.

For the proton moving from high to low potential, ΔV=Vb−Va=−120 V\Delta V = V_b - V_a = -120\ \text{V} (potential drops). The work done by the field is

Wfield=−q ΔV=−(1.602×10−19)(−120)=+1.92×10−17 J.W_{\text{field}} = -q\,\Delta V = -(1.602\times10^{-19})(-120) = +1.92\times10^{-17}\ \text{J}.

The work is positive: a positive charge is pushed from high toward low potential by the field, gaining kinetic energy—consistent with 1.92×10−17 J=120 eV1.92\times10^{-17}\ \text{J} = 120\ \text{eV}, again the tidy electron-volt bookkeeping. An electron, with the opposite sign of charge, would instead be pushed from the low-potential plate toward the high-potential plate.


The electron volt (eV) is a unit of energy, not potential. One electron volt is the energy change of a particle with charge magnitude ee when it moves through a potential difference of magnitude 1 V1 \text{ V}:

1 eV=e⋅(1 V)≈1.602×10−19 J.1 \text{ eV} = e \cdot (1 \text{ V}) \approx 1.602 \times 10^{-19} \text{ J}.

Atomic and nuclear scales use multiples such as keV, MeV, and GeV (10310^3, 10610^6, and 10910^9 eV). The joule remains the SI energy unit; the eV is a convenience because ee is the natural charge quantum at microscopic scales.


The standard result above quotes the interior potential of a uniformly charged solid sphere without derivation. Here is where it comes from.

Proof (interior potential of a uniformly charged solid sphere). A solid sphere of radius RR carries total charge QQ at uniform volume density. By Gauss’s law, the field is radial with magnitude

E(r)={kQ rR3,r≤R(only the enclosed charge contributes),kQr2,r≥R.E(r) = \begin{cases} \dfrac{kQ\,r}{R^3}, & r \le R \quad (\text{only the enclosed charge contributes}),\\[2mm] \dfrac{kQ}{r^2}, & r \ge R. \end{cases}

Start at infinity where V=0V = 0 and integrate the field inward. From infinity to the surface r=Rr = R, the exterior field is the point-charge field, giving the surface potential

V(R)=kQR.V(R) = \frac{kQ}{R}.

To reach an interior radius r<Rr < R, continue integrating with the interior field:

V(r)=V(R)−∫RrE dr′=kQR−∫RrkQ r′R3 dr′.V(r) = V(R) - \int_R^r E\,dr' = \frac{kQ}{R} - \int_R^r \frac{kQ\,r'}{R^3}\,dr'.

Evaluate the interior integral:

∫RrkQ r′R3 dr′=kQR3[r′22]Rr=kQ2R3(r2−R2).\int_R^r \frac{kQ\,r'}{R^3}\,dr' = \frac{kQ}{R^3}\left[\frac{r'^2}{2}\right]_R^r = \frac{kQ}{2R^3}\left(r^2 - R^2\right).

Substituting (note the double minus sign turns it into a plus),

V(r)=kQR−kQ2R3(r2−R2)=kQR+kQ2R−kQ r22R3.V(r) = \frac{kQ}{R} - \frac{kQ}{2R^3}\left(r^2 - R^2\right) = \frac{kQ}{R} + \frac{kQ}{2R} - \frac{kQ\,r^2}{2R^3}.

Combining the constant terms kQR+kQ2R=3kQ2R\dfrac{kQ}{R} + \dfrac{kQ}{2R} = \dfrac{3kQ}{2R}:

V(r)=kQ2R(3−r2R2),r≤R.V(r) = \frac{kQ}{2R}\left(3 - \frac{r^2}{R^2}\right), \qquad r \le R.

At the surface (r=Rr = R) this gives kQ2R(3−1)=kQR\dfrac{kQ}{2R}(3 - 1) = \dfrac{kQ}{R}, matching the exterior value—VV is continuous even though EE has a kink there. At the center (r=0r = 0) the potential reaches its maximum 3kQ2R\dfrac{3kQ}{2R}, 1.51.5 times the surface value.


  1. Temporary placeholder FRQ for wiring/testing — replace with a real free-response question for this unit.

    (A)(A) State one key idea from this unit and explain it in your own words.

    (B)(B) Give a worked example or application of that idea.