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Unit 1: Electric Fields and Forces

Physics C E&M cheatsheet

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Charges exert forces on one another. Electric fields describe those forces throughout space, and symmetry often simplifies the field calculation. The subject is often called electrostatics when charges are at rest and magnetic effects from motion are absent or treated separately.



Charge is a fundamental property of matter. Protons carry a positive charge and electrons a negative charge of the same magnitude. The elementary charge has magnitude

e=1.602Ɨ10āˆ’19Ā C.e = 1.602 \times 10^{-19} \text{ C}.

By convention, the proton’s charge is +e+e and the electron’s is āˆ’e-e. The SI unit of charge is the coulomb (C).

In ordinary matter, charge is transferred by moving electrons; ion cores (with protons) do not hop between objects in classroom electrostatics. A positively charged object has lost electrons; a negatively charged one has gained them.

Experiments (notably Millikan’s oil-drop experiment) show that the charge on any isolated object occurs in discrete steps. Quantization of charge means the total charge qq on a body satisfies

q=ne,n∈Z.q = n e, \quad n \in \mathbb{Z}.

There is no known stable macroscopic object with charge that is a fraction of an electrons since nn is an integer. (Quarks carry fractional charge, but they are confined (meaning they have to be in pairs/trios); net observable charge remains integer multiples of ee.)


Conservation of charge states that the total charge in an isolated system stays constant over time. Charge is not created or destroyed; it is redistributed. Together with conservation of energy and momentum, this principle constrains what reactions and contact processes are possible and underlies much of circuit and field reasoning later in the course.


An electroscope uses thin metal leaves (or a similar mechanical indicator) that repel when they receive the same sign of charge, giving a rough measure of whether charge is present and sometimes how much.

  • Grounding connects a conductor to the Earth (or another large reservoir). The Earth supplies or accepts electrons until the conductor reaches a common potential with the ground; in practice, a grounded object is often treated as neutral after the process finishes.
  • Charging by conduction means direct contact. If a charged rod touches a neutral electroscope, charge shares between them; by conservation of charge, both end up with net charge of the same sign (not necessarily equal magnitude unless capacitances match, but the sign is shared in the simple picture).
  • Charging by induction needs no transfer of charge from the rod to the electroscope if the rod never touches the scope. A charged object is brought near, polarizing the conductor; while the influence is present, the electroscope is grounded so charge can leave or enter; the ground connection is broken first, then the inducing object is removed. The electroscope retains a net charge opposite in sign to the inducer, because electrons were driven by the external field and then trapped when the path to ground was removed.

Polarization is the separation of positive and negative charge within a neutral object when a charged object is brought nearby. A charged object can polarize a neutral insulator or conductor: internal charge shifts so that one side of the material presents a net excess closer to the inducer. For example, a negative balloon near a wall pushes electrons in the wall slightly away, so the nearer surface acts more positive. The balloon and wall can attract even though the wall’s net charge is still zero—attraction without net charge on the neutral object is the usual signature of polarization.

wallchargedĀ”+Ā”+Ā”+Ā”+attraction

The force between two point charges in vacuum (or air, approximately) is given by Coulomb’s law:

Fāƒ—=kq1q2r2r^,\vec{F} = k \frac{q_1 q_2}{r^2} \hat{r},

where r^\hat{r} points from the charge exerting the force to the charge experiencing it (or from source to test, depending on textbook convention—always check the direction rule your problems use). The Coulomb constant is

k=8.99Ɨ109Ā Nā‹…m2/C2.k = 8.99 \times 10^9 \text{ N}\cdot\text{m}^2/\text{C}^2.

Like charges give a repulsive force along r^\hat{r}; opposite charges attract (force opposite to r^\hat{r} if r^\hat{r} is defined as above). The magnitude falls as 1/r21/r^2, the same inverse-square geometry as Newton’s law of gravitation, but charge can be positive or negative so the force can be attractive or repulsive.

Example. Suppose q1=+2.0 μCq_1=+2.0\,\mu\text{C} is at x=0x=0 and q2=āˆ’3.0 μCq_2=-3.0\,\mu\text{C} is at x=0.50Ā mx=0.50\text{ m}. Find the force on q1q_1.

The magnitude is

F=k∣q1q2∣r2=(8.99Ɨ109)(2.0Ɨ10āˆ’6)(3.0Ɨ10āˆ’6)(0.50)2=0.216Ā N.F=k\frac{\lvert q_1q_2 \rvert}{r^2} =\left(8.99\times10^9\right)\frac{(2.0\times10^{-6})(3.0\times10^{-6})}{(0.50)^2} =0.216\text{ N}.

Because the charges are opposite, q1q_1 is attracted toward q2q_2, so the force on q1q_1 points in the +x+x direction.

Example. Two charges q1=+3.0 μCq_1 = +3.0\,\mu\text{C} and q2=+3.0 μCq_2 = +3.0\,\mu\text{C} sit at the base corners of an equilateral triangle of side d=0.20Ā md = 0.20\text{ m}. A third charge q3=+2.0 μCq_3 = +2.0\,\mu\text{C} sits at the apex. Find the net force on q3q_3.

Each base charge is the same distance dd from the apex, so the two forces have equal magnitude

F=kq1q3d2=(8.99Ɨ109)(3.0Ɨ10āˆ’6)(2.0Ɨ10āˆ’6)(0.20)2=1.35Ā N.F = k\frac{q_1 q_3}{d^2} = \left(8.99\times10^9\right)\frac{(3.0\times10^{-6})(2.0\times10^{-6})}{(0.20)^2} = 1.35\text{ N}.

Both forces are repulsive, pushing q3q_3 directly away from each base charge. By the symmetry of the equilateral triangle, each force makes an angle of 60∘60^\circ with the horizontal. Resolve into components, putting the apex above the midpoint of the base:

F1x=āˆ’Fcos⁔60∘,F2x=+Fcos⁔60∘,F_{1x} = -F\cos 60^\circ, \qquad F_{2x} = +F\cos 60^\circ,

so the horizontal components cancel, Fnet,x=0F_{\text{net},x} = 0. The vertical components both point up and add:

Fnet,y=2Fsin⁔60∘=2(1.35)(0.866)=2.34 N.F_{\text{net},y} = 2F\sin 60^\circ = 2(1.35)(0.866) = 2.34\text{ N}.

The net force on q3q_3 is 2.3Ā N2.3\text{ N} pointing straight up, away from the base. Whenever a problem has two or more sources, always resolve each force into xx and yy components, add the components separately, then recombine — never add magnitudes directly unless the forces are collinear.

Example. A charge q1=+4.0 μCq_1 = +4.0\,\mu\text{C} is at x=0x = 0 and q2=+1.0 μCq_2 = +1.0\,\mu\text{C} is at x=0.30Ā mx = 0.30\text{ m}. Where on the line can a third charge be placed so it feels zero net force?

A test charge feels zero net force where the two fields (or forces) are equal in magnitude and opposite in direction. Between two like charges there is always such a point between them, because the two fields point in opposite directions there. Let the point be a distance xx from q1q_1, so it is 0.30āˆ’x0.30 - x from q2q_2. Setting the magnitudes equal:

kq1x2=kq2(0.30āˆ’x)2.k\frac{q_1}{x^2} = k\frac{q_2}{(0.30 - x)^2}.

Cancel kk and cross-multiply:

q1q2=x2(0.30āˆ’x)2⇒q1q2=x0.30āˆ’x.\frac{q_1}{q_2} = \frac{x^2}{(0.30-x)^2} \quad\Rightarrow\quad \sqrt{\frac{q_1}{q_2}} = \frac{x}{0.30 - x}.

Since q1/q2=4=2\sqrt{q_1/q_2} = \sqrt{4} = 2,

x=2(0.30āˆ’x)⇒3x=0.60⇒x=0.20Ā m.x = 2(0.30 - x) \quad\Rightarrow\quad 3x = 0.60 \quad\Rightarrow\quad x = 0.20\text{ m}.

The null point is 0.20Ā m0.20\text{ m} from the larger charge — closer to the smaller charge, as expected, since you must move nearer the weaker source to balance it. (Taking the negative square root would place the point outside the segment, where the two fields point the same way and cannot cancel, so it is rejected.) For two charges of opposite sign, the null point lies outside the segment, on the side of the smaller-magnitude charge.


It is sometimes convenient to write

k=14πε0,k = \frac{1}{4\pi \varepsilon_0},

so Coulomb’s law becomes Fāƒ—=14πε0q1q2r2r^\vec{F} = \frac{1}{4\pi \varepsilon_0} \frac{q_1 q_2}{r^2} \hat{r}. The constant ε0\varepsilon_0 is the permittivity of free space,

ε0=8.85Ɨ10āˆ’12Ā C2/(Nā‹…m2)\varepsilon_0 = 8.85 \times 10^{-12} \text{ C}^2/(\text{N}\cdot\text{m}^2)

(equivalently farads per meter, F/m\text{F/m}). It sets how electric fields in vacuum relate to source charge.


The superposition principle for electrostatics says that the total force on a charge is the vector sum of the forces from every other charge, computed as if each pair were alone:

Fāƒ—net=āˆ‘iFāƒ—i.\vec{F}_{\text{net}} = \sum_i \vec{F}_i.

In practice: sketch each contribution, resolve into components if the geometry demands it, then add. The principle extends to fields once the field from each source is known.


The electric field Eāƒ—\vec{E} at a point is defined as the force per unit charge on a small positive test charge q0q_0:

Eāƒ—=Fāƒ—q0,units:Ā N/CĀ (orĀ V/m).\vec{E} = \frac{\vec{F}}{q_0}, \qquad \text{units: N/C (or V/m)}.

The field is attributed to source charges; conceptually it exists whether or not a test charge is present. By convention, Eāƒ—\vec{E} points in the direction of the force on a positive test charge, so a negative charge in the same field feels a force Fāƒ—=qEāƒ—\vec{F} = q\vec{E} opposite to Eāƒ—\vec{E}.

For a single point charge QQ,

Eāƒ—=14πε0Qr2r^.\vec{E} = \frac{1}{4\pi \varepsilon_0} \frac{Q}{r^2} \hat{r}.

Example. Two equal positive charges +Q+Q are placed at (0,a)(0,a) and (0,āˆ’a)(0,-a). Find the electric field at (x,0)(x,0).

Each charge is a distance r=x2+a2r=\sqrt{x^2+a^2} from the point. The vertical components cancel by symmetry. The horizontal component from one charge is

Ex=kQr2cos⁔θ=kQx2+a2ā‹…xx2+a2=kQx(x2+a2)3/2.E_x=\frac{kQ}{r^2}\cos\theta =\frac{kQ}{x^2+a^2}\cdot\frac{x}{\sqrt{x^2+a^2}} =\frac{kQx}{(x^2+a^2)^{3/2}}.

There are two equal horizontal components, so

Eāƒ—=2kQx(x2+a2)3/2ı^.\vec E=\frac{2kQx}{(x^2+a^2)^{3/2}}\hat{\imath}.

For x>0x>0 this points right; for x<0x<0 it points left.

Example. A charge q1=+5.0 nCq_1 = +5.0\,\text{nC} is at the origin and q2=āˆ’5.0 nCq_2 = -5.0\,\text{nC} is at (0.40Ā m,0)(0.40\text{ m}, 0). Find the net electric field at the point P=(0.40Ā m,0.30Ā m)P = (0.40\text{ m}, 0.30\text{ m}).

Treat each charge separately, then add the field vectors. The point PP is directly above q2q_2 at distance r2=0.30Ā mr_2 = 0.30\text{ m}, so the field from q2q_2 has magnitude

E2=k∣q2∣r22=(8.99Ɨ109)5.0Ɨ10āˆ’9(0.30)2=499Ā N/C.E_2 = k\frac{\lvert q_2 \rvert}{r_2^2} = (8.99\times10^9)\frac{5.0\times10^{-9}}{(0.30)^2} = 499\ \text{N/C}.

Since q2q_2 is negative, Eāƒ—2\vec E_2 points toward q2q_2, i.e. straight down: Eāƒ—2=(0,ā€‰āˆ’499)Ā N/C\vec E_2 = (0,\,-499)\ \text{N/C}.

The distance from q1q_1 to PP is r1=0.402+0.302=0.50Ā mr_1 = \sqrt{0.40^2 + 0.30^2} = 0.50\text{ m}, so

E1=kq1r12=(8.99Ɨ109)5.0Ɨ10āˆ’9(0.50)2=180Ā N/C.E_1 = k\frac{q_1}{r_1^2} = (8.99\times10^9)\frac{5.0\times10^{-9}}{(0.50)^2} = 180\ \text{N/C}.

Eāƒ—1\vec E_1 points away from the positive q1q_1, along the direction from the origin to PP. The unit vector is (0.40,0.30)/0.50=(0.80,0.60)(0.40, 0.30)/0.50 = (0.80, 0.60), so

Eāƒ—1=180 (0.80, 0.60)=(144, 108)Ā N/C.\vec E_1 = 180\,(0.80,\,0.60) = (144,\,108)\ \text{N/C}.

Add components:

Eāƒ—=Eāƒ—1+Eāƒ—2=(144,Ā 108āˆ’499)=(144,ā€‰āˆ’391)Ā N/C.\vec E = \vec E_1 + \vec E_2 = (144,\ 108 - 499) = (144,\,-391)\ \text{N/C}.

The magnitude is

E=1442+3912ā‰ˆ417Ā N/C,E = \sqrt{144^2 + 391^2} \approx 417\ \text{N/C},

directed at arctan⁔(391/144)ā‰ˆ70∘\arctan(391/144) \approx 70^\circ below the +x+x axis. The whole calculation is just superposition: compute each field’s magnitude from kq/r2kq/r^2, assign its direction (away from positive, toward negative), break into components, and sum.


When charge is spread through a line, surface, or volume, describe it with a density:

λ=dqdL(charge per unit length),\lambda = \frac{dq}{dL} \quad \text{(charge per unit length)}, σ=dqdA(charge per unit area),\sigma = \frac{dq}{dA} \quad \text{(charge per unit area)}, ρ=dqdV(charge per unit volume).\rho = \frac{dq}{dV} \quad \text{(charge per unit volume)}.

The field obeys superposition in integral form:

Eāƒ—=14πε0∫dqr2r^,\vec{E} = \frac{1}{4\pi \varepsilon_0} \int \frac{dq}{r^2} \hat{r},

or, for a scalar magnitude contribution along a chosen axis after symmetry,

dE=14πε0dqr2dE = \frac{1}{4\pi \varepsilon_0} \frac{dq}{r^2}

with dqdq replaced by λ dL\lambda\, dL, Ļƒā€‰dA\sigma\, dA, or ρ dV\rho\, dV according to the geometry. Set up coordinates, exploit symmetry, and integrate. Some common techniques are to convert into polar form, or only calculate non-cancelling portions of the field.

Proof (on-axis field of a uniformly charged ring). A ring of radius RR carries total charge QQ uniformly. Find the field a distance xx from the center along the ring’s axis.

xpointrtransversecomponentscancel

Every charge element dqdq is the same distance

r=x2+R2r=\sqrt{x^2+R^2}

from the field point by the Pythagorean theorem. Each dqdq produces a field dE=k dq/r2dE = k\,dq/r^2 pointing from the element to the axis point. As we go around the ring, the components perpendicular to the axis cancel in pairs (the element on the opposite side cancels them), so only the axial component survives. If Īø\theta is the angle the field makes with the axis, then cos⁔θ=x/r\cos\theta = x/r, and

dEx=dEcos⁔θ=kdqr2ā‹…xr=kx dq(x2+R2)3/2.dE_x=dE\cos\theta =k\frac{dq}{r^2}\cdot\frac{x}{r} =k\frac{x\,dq}{(x^2+R^2)^{3/2}}.

Because xx and RR are the same for every element, everything except dqdq pulls out of the integral:

Ex=kx(x2+R2)3/2∫dq=14πε0Qx(x2+R2)3/2.E_x=k\frac{x}{(x^2+R^2)^{3/2}}\int dq =\frac{1}{4\pi\varepsilon_0}\frac{Qx}{(x^2+R^2)^{3/2}}.

Two checks: at the center (x=0x=0) the field is zero, as symmetry demands; and far away (x≫Rx\gg R) it reduces to Eā‰ˆkQ/x2E\approx kQ/x^2, the field of a point charge. The field is also maximized at x=R/2x = R/\sqrt{2} (set dEx/dx=0dE_x/dx = 0).

Proof (on-axis field of a uniformly charged disk). A flat disk of radius RR carries uniform surface charge density σ\sigma. Find the field a distance xx along its axis.

diskasastackofchargedrings

Treat the disk as a stack of concentric thin rings. A ring of radius ss and thickness dsds has area dA=2Ļ€s dsdA = 2\pi s\,ds, so it carries charge

dq=Ļƒā€‰dA=Ļƒā€‰(2Ļ€s ds).dq = \sigma\,dA = \sigma\,(2\pi s\,ds).

Use the ring result above with R→sR\to s and Q→dqQ \to dq:

dEx=14πε0x dq(x2+s2)3/2=σx4πε02Ļ€s ds(x2+s2)3/2=σx2ε0s ds(x2+s2)3/2.dE_x = \frac{1}{4\pi\varepsilon_0}\frac{x\,dq}{(x^2+s^2)^{3/2}} = \frac{\sigma x}{4\pi\varepsilon_0}\frac{2\pi s\,ds}{(x^2+s^2)^{3/2}} = \frac{\sigma x}{2\varepsilon_0}\frac{s\,ds}{(x^2+s^2)^{3/2}}.

Integrate over all rings, from s=0s=0 to s=Rs=R. The substitution u=x2+s2u = x^2 + s^2, du=2s dsdu = 2s\,ds gives ∫s(x2+s2)āˆ’3/2 ds=āˆ’(x2+s2)āˆ’1/2\int s(x^2+s^2)^{-3/2}\,ds = -(x^2+s^2)^{-1/2}:

Ex=σx2ε0[āˆ’1x2+s2]0R=σx2ε0(1xāˆ’1x2+R2).E_x = \frac{\sigma x}{2\varepsilon_0}\left[-\frac{1}{\sqrt{x^2+s^2}}\right]_0^R = \frac{\sigma x}{2\varepsilon_0}\left(\frac{1}{x} - \frac{1}{\sqrt{x^2+R^2}}\right).

Therefore

E=σ2ε0(1āˆ’xx2+R2).E = \frac{\sigma}{2\varepsilon_0}\left(1 - \frac{x}{\sqrt{x^2+R^2}}\right).

This single result contains two famous limits. Infinite sheet (Rā†’āˆžR\to\infty, or equivalently x≪Rx\ll R): the fraction x/x2+R2→0x/\sqrt{x^2+R^2}\to 0, so

Eā†’Ļƒ2ε0,E \to \frac{\sigma}{2\varepsilon_0},

exactly the infinite-sheet field we will get from Gauss’s law below — independent of distance. Far away (x≫Rx\gg R): expanding x/x2+R2ā‰ˆ1āˆ’R2/2x2x/\sqrt{x^2+R^2} \approx 1 - R^2/2x^2 gives Eā‰ˆĻƒR2/(4ε0x2)=kQ/x2E\approx \sigma R^2/(4\varepsilon_0 x^2) = kQ/x^2 with Q=ĻƒĻ€R2Q = \sigma\pi R^2, the point-charge field again. One integral, both limiting behaviors.

Example. A rod of length 2L2L lies on the xx-axis from āˆ’L-L to LL with uniform charge density Ī»\lambda. Find the field at (0,a)(0,a).

For a small element dq=λ dxdq=\lambda\,dx at position xx, the distance to the point is r=x2+a2r=\sqrt{x^2+a^2}. Horizontal components cancel between +x+x and āˆ’x-x, so keep only the vertical component:

dEy=kdqr2ar=kĪ»a dx(x2+a2)3/2.dE_y=k\frac{dq}{r^2}\frac{a}{r} =k\lambda\frac{a\,dx}{(x^2+a^2)^{3/2}}.

Therefore

Ey=kĪ»aāˆ«āˆ’LLdx(x2+a2)3/2=2kĪ»LaL2+a2.E_y=k\lambda a\int_{-L}^{L}\frac{dx}{(x^2+a^2)^{3/2}} =\frac{2k\lambda L}{a\sqrt{L^2+a^2}}.

The field points away from the rod if Ī»>0\lambda>0 and toward the rod if Ī»<0\lambda<0.

pointchargedrod

Field lines are a pictorial tool: they leave positive charge, terminate on negative charge, and their spacing indicates field strength (closer lines mean larger ∣Eāƒ—āˆ£\lvert \vec{E} \rvert). Field lines never cross, because the field at a point has a single direction.

+”¯eldlinesstartonpositivechargeandendonnegativecharge

Electric flux measures how much electric field passes through a surface. For a flat area Aāƒ—\vec{A} (magnitude equal to area, direction along the normal) and uniform Eāƒ—\vec{E},

ΦE=Eāƒ—ā‹…Aāƒ—=EAcos⁔θ,\Phi_E = \vec{E} \cdot \vec{A} = EA\cos\theta,

where Īø\theta is the angle between Eāƒ—\vec{E} and the normal. When Eāƒ—\vec{E} is parallel to the surface, flux through that surface is zero; when perpendicular, ∣ΦE∣\lvert \Phi_E \rvert is maximal for fixed EE and AA.

For a general surface,

ΦE=∫Eāƒ—ā‹…dAāƒ—.\Phi_E = \int \vec{E} \cdot d\vec{A}.

Gauss’s law relates the flux through any closed surface to the charge enclosed:

∮Eāƒ—ā‹…dAāƒ—=Qencε0.\oint \vec{E} \cdot d\vec{A} = \frac{Q_{\text{enc}}}{\varepsilon_0}.

The closed surface used in the integral is called a Gaussian surface; it is a mathematical construct, not a physical shell. The law is always true; it is computationally powerful when symmetry lets you pull ∣Eāƒ—āˆ£\lvert \vec{E} \rvert outside the integral because it is constant on the chosen surface.

Gauss’s law is especially efficient for:

  • spherically symmetric charge (use a concentric sphere),
  • infinite cylindrical symmetry (use a coaxial cylinder),
  • infinite planar symmetry (use a pillbox, which is a very short cylinder).

Choose a surface on which EE is constant and parallel or perpendicular to dAāƒ—d\vec{A} on each piece, so the flux reduces to EE times an area.

Proof (Gauss’s law for a point charge). Put a point charge qq at the center of a sphere of radius rr. On the sphere,

E=14πε0qr2E=\frac{1}{4\pi\varepsilon_0}\frac{q}{r^2}

and Eāƒ—\vec E is parallel to dAāƒ—d\vec A everywhere. Thus

∮Eāƒ—ā‹…dAāƒ—=E(4Ļ€r2)=14πε0qr2(4Ļ€r2)=qε0.\oint \vec E\cdot d\vec A =E(4\pi r^2) =\frac{1}{4\pi\varepsilon_0}\frac{q}{r^2}(4\pi r^2) =\frac{q}{\varepsilon_0}.

The important cancellation is geometric: the field weakens like 1/r21/r^2 while the sphere’s area grows like r2r^2. A general proof of Gauss’s Law will not be described here but feel free to try on your own!

Example. A nonconducting sphere of radius RR has total charge QQ spread uniformly through its volume. Find E(r)E(r).

For r≄Rr\ge R, a spherical Gaussian surface encloses all the charge:

E(4Ļ€r2)=Qε0⇒E=14πε0Qr2.E(4\pi r^2)=\frac{Q}{\varepsilon_0} \quad\Rightarrow\quad E=\frac{1}{4\pi\varepsilon_0}\frac{Q}{r^2}.

For r<Rr<R, only the charge inside radius rr is enclosed. Since the volume fraction is r3/R3r^3/R^3,

Qenc=Qr3R3.Q_{\text{enc}}=Q\frac{r^3}{R^3}.

Then

E(4Ļ€r2)=Qr3ε0R3⇒E=14πε0QrR3.E(4\pi r^2)=\frac{Qr^3}{\varepsilon_0R^3} \quad\Rightarrow\quad E=\frac{1}{4\pi\varepsilon_0}\frac{Qr}{R^3}.

Inside the sphere, the field grows linearly with distance from the center.

Example. A thin conducting (or uniformly charged) spherical shell of radius RR carries total charge QQ. Find EE inside and outside.

Outside (r>Rr > R): a concentric Gaussian sphere encloses all of QQ, exactly like the solid case,

E(4Ļ€r2)=Qε0⇒E=14πε0Qr2.E(4\pi r^2) = \frac{Q}{\varepsilon_0} \quad\Rightarrow\quad E = \frac{1}{4\pi\varepsilon_0}\frac{Q}{r^2}.

From outside, any spherically symmetric charge looks like a point charge at the center.

Inside (r<Rr < R): a Gaussian sphere of radius r<Rr < R encloses no charge, since all the charge is on the surface at radius RR:

E(4Ļ€r2)=Qencε0=0⇒E=0.E(4\pi r^2) = \frac{Q_{\text{enc}}}{\varepsilon_0} = 0 \quad\Rightarrow\quad E = 0.

The field is exactly zero everywhere inside the shell. The field jumps discontinuously at the surface, from 00 to kQ/R2kQ/R^2.

Example. A nonconducting sphere of radius R=0.10Ā mR = 0.10\text{ m} carries Q=8.0 nCQ = 8.0\,\text{nC} spread uniformly through its volume. Find EE at r=0.050Ā mr = 0.050\text{ m} (inside) and at r=0.20Ā mr = 0.20\text{ m} (outside).

Inside, use E=14πε0QrR3E = \dfrac{1}{4\pi\varepsilon_0}\dfrac{Qr}{R^3} from the uniform-sphere result:

E=(8.99Ɨ109)(8.0Ɨ10āˆ’9)(0.050)(0.10)3=(8.99Ɨ109)4.0Ɨ10āˆ’101.0Ɨ10āˆ’3=3.6Ɨ103Ā N/C.E = (8.99\times10^9)\frac{(8.0\times10^{-9})(0.050)}{(0.10)^3} = (8.99\times10^9)\frac{4.0\times10^{-10}}{1.0\times10^{-3}} = 3.6\times10^3\ \text{N/C}.

Outside, the sphere acts like a point charge:

E=14πε0Qr2=(8.99Ɨ109)8.0Ɨ10āˆ’9(0.20)2=1.8Ɨ103Ā N/C.E = \frac{1}{4\pi\varepsilon_0}\frac{Q}{r^2} = (8.99\times10^9)\frac{8.0\times10^{-9}}{(0.20)^2} = 1.8\times10^3\ \text{N/C}.

At the surface (r=R=0.10Ā mr = R = 0.10\text{ m}) both formulas agree: E=kQ/R2=7.2Ɨ103Ā N/CE = kQ/R^2 = 7.2\times10^3\ \text{N/C}, the field’s maximum value. Inside, EE rises linearly from the center; outside, it falls off as 1/r21/r^2.

Example. An infinite line has uniform charge density Ī»\lambda. Find the electric field of the line a distance rr away from the line.

The field is radial and constant on the curved side. The end caps have zero flux because Eāƒ—\vec E is parallel to the caps, not perpendicular to them. Therefore

∮Eāƒ—ā‹…dAāƒ—=E(2Ļ€rL).\oint \vec E\cdot d\vec A=E(2\pi rL).

The enclosed charge is Qenc=λLQ_{\text{enc}}=\lambda L, so

E(2Ļ€rL)=Ī»Lε0⇒E=Ī»2πε0r.E(2\pi rL)=\frac{\lambda L}{\varepsilon_0} \quad\Rightarrow\quad E=\frac{\lambda}{2\pi\varepsilon_0 r}.
linechargeGaussiancylinder

Example. An infinite nonconducting sheet has surface charge density σ\sigma. Use a thin pillbox crossing the sheet.

The field points perpendicular to the sheet and has the same magnitude on both sides. The curved side of the pillbox contributes no flux, while the two flat faces contribute EAEA each:

∮Eāƒ—ā‹…dAāƒ—=2EA.\oint \vec E\cdot d\vec A=2EA.

The enclosed charge is σA\sigma A, so

2EA=σAε0⇒E=σ2ε0.2EA=\frac{\sigma A}{\varepsilon_0} \quad\Rightarrow\quad E=\frac{\sigma}{2\varepsilon_0}.
chargedsheetEexitsEexits

These examples are very common throughout AP Physics C E&M, and are worth memorizing how to do.


An electric dipole is a pair of equal and opposite charges +q+q and āˆ’q-q separated by a small displacement dāƒ—\vec d (pointing from the negative to the positive charge). It is described by its dipole moment

pāƒ—=qdāƒ—,\vec p = q\vec d,

a vector pointing from the negative charge to the positive charge, with magnitude p=qdp = qd (units Cā‹…m\text{C}\cdot\text{m}). Many neutral molecules (like water) behave as dipoles, and the dipole is the simplest charge distribution with zero net charge but a nonzero field.

”q+q~pd

Proof (far field on the dipole axis). Place +q+q at +d/2+d/2 and āˆ’q-q at āˆ’d/2-d/2 on the xx-axis. Find the field at a point on the axis a distance rr from the center, with r≫dr \gg d.

On the axis, both fields point along xx, so we just subtract magnitudes. The near (positive) charge is at distance rāˆ’d/2r - d/2 and the far (negative) charge at r+d/2r + d/2:

E=q4πε0[1(rāˆ’d/2)2āˆ’1(r+d/2)2].E = \frac{q}{4\pi\varepsilon_0}\left[\frac{1}{(r-d/2)^2} - \frac{1}{(r+d/2)^2}\right].

Combine over a common denominator. The numerator is (r+d/2)2āˆ’(rāˆ’d/2)2=2rd(r+d/2)^2 - (r-d/2)^2 = 2rd, and the denominator is (r2āˆ’d2/4)2ā‰ˆr4\big(r^2 - d^2/4\big)^2 \approx r^4 when r≫dr \gg d:

E=q4πε0ā‹…2rd(r2āˆ’d2/4)2ā‰ˆq4πε0ā‹…2rdr4=14πε02qdr3.E = \frac{q}{4\pi\varepsilon_0}\cdot\frac{2rd}{(r^2 - d^2/4)^2} \approx \frac{q}{4\pi\varepsilon_0}\cdot\frac{2rd}{r^4} = \frac{1}{4\pi\varepsilon_0}\frac{2qd}{r^3}.

With p=qdp = qd,

Eā‰ˆ14πε02pr3.E \approx \frac{1}{4\pi\varepsilon_0}\frac{2p}{r^3}.

The key feature is that a dipole’s field falls off as 1/r31/r^3, faster than a single charge’s 1/r21/r^2, because the two opposite charges nearly cancel at large distance. The field points along pāƒ—\vec p on the axis.

When a dipole sits in a uniform external field Eāƒ—\vec E, the forces on +q+q and āˆ’q-q are equal and opposite, so the net force is zero — but they form a couple that produces a torque:

Ļ„āƒ—=pāƒ—Ć—Eāƒ—,Ļ„=pEsin⁔ϕ,\vec\tau = \vec p \times \vec E, \qquad \tau = pE\sin\phi,

where Ļ•\phi is the angle between pāƒ—\vec p and Eāƒ—\vec E. The torque rotates the dipole toward alignment with the field (ϕ→0\phi \to 0), where the torque vanishes and the energy U=āˆ’pāƒ—ā‹…Eāƒ—U = -\vec p\cdot\vec E is minimized.

Example. A dipole with moment p=6.2Ɨ10āˆ’30Ā Cā‹…mp = 6.2\times10^{-30}\ \text{C}\cdot\text{m} (about that of a water molecule) sits in a uniform field E=3.0Ɨ105Ā N/CE = 3.0\times10^{5}\ \text{N/C}, oriented at Ļ•=30∘\phi = 30^\circ to the field. Find the torque on it.

Ļ„=pEsin⁔ϕ=(6.2Ɨ10āˆ’30)(3.0Ɨ105)sin⁔30∘=(6.2Ɨ10āˆ’30)(3.0Ɨ105)(0.5)ā‰ˆ9.3Ɨ10āˆ’25Ā Nā‹…m.\tau = pE\sin\phi = (6.2\times10^{-30})(3.0\times10^{5})\sin 30^\circ = (6.2\times10^{-30})(3.0\times10^{5})(0.5) \approx 9.3\times10^{-25}\ \text{N}\cdot\text{m}.

The torque is maximal when pāƒ—āŠ„Eāƒ—\vec p \perp \vec E (Ļ•=90∘\phi = 90^\circ) and zero when the dipole is aligned (Ļ•=0\phi = 0) or anti-aligned (Ļ•=180∘\phi = 180^\circ); only Ļ•=0\phi = 0 is stable equilibrium.


A charge in a field feels a force Fāƒ—=qEāƒ—\vec F = q\vec E. In a uniform field (such as the region between two large parallel charged plates), the force is constant, so the charge undergoes constant acceleration

aāƒ—=Fāƒ—m=qEāƒ—m,\vec a = \frac{\vec F}{m} = \frac{q\vec E}{m},

and the constant-acceleration kinematics from mechanics apply directly. This is the electrical analog of projectile motion under gravity.

Example. An electron (q=āˆ’eq = -e, m=9.11Ɨ10āˆ’31Ā kgm = 9.11\times10^{-31}\ \text{kg}) is released from rest next to the negative plate in a uniform field of magnitude E=2.0Ɨ104Ā N/CE = 2.0\times10^{4}\ \text{N/C}. The plates are separated by d=1.0Ā cmd = 1.0\text{ cm}. Find the electron’s acceleration and its speed when it reaches the other plate.

The force magnitude is F=∣q∣E=eEF = \lvert q \rvert E = eE, so

a=eEm=(1.602Ɨ10āˆ’19)(2.0Ɨ104)9.11Ɨ10āˆ’31ā‰ˆ3.5Ɨ1015Ā m/s2.a = \frac{eE}{m} = \frac{(1.602\times10^{-19})(2.0\times10^{4})}{9.11\times10^{-31}} \approx 3.5\times10^{15}\ \text{m/s}^2.

(The electron, being negative, accelerates toward the positive plate, opposite Eāƒ—\vec E.) Treating this as 1-D motion from rest through dd, use v2=v02+2adv^2 = v_0^2 + 2ad with v0=0v_0 = 0:

v=2ad=2(3.5Ɨ1015)(0.010)=7.0Ɨ1013ā‰ˆ8.4Ɨ106Ā m/s.v = \sqrt{2ad} = \sqrt{2(3.5\times10^{15})(0.010)} = \sqrt{7.0\times10^{13}} \approx 8.4\times10^{6}\ \text{m/s}.

Equivalently, work-energy gives the same answer: the field does work W=qEd=12mv2W = qEd = \tfrac{1}{2}mv^2. The huge acceleration comes from the electron’s tiny mass; the same field would push a proton the other way with an acceleration about 18001800 times smaller.


  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.