The Electric Field
Coulomb's law has an embarrassment buried in it. It says charge pushes charge across empty space, instantly, with nothing in between doing any work. Newton himself found this "action at a distance" philosophically indigestible in gravity, and electricity inherited the itch. The fix — one of the deepest conceptual moves in all of physics — is to break the interaction into two local steps. First: charge modifies the space around it, dressing every point with a vector called the electric field . Second: charge , sitting at one such point, feels a force determined entirely by the field right where it is. never needs to know that exists. In electrostatics you could dismiss this as bookkeeping — a mere rearrangement of Coulomb's law, which is exactly how it enters this article. But the bookkeeping turns out to be the physics. Shake charge , and the news travels outward through the field at the speed of light; the field carries energy, carries momentum, and — once it has left its source — lives a life of its own as light itself. The static field you meet here is the gentle introduction to the most successful physical object of the modern era. This page builds the field concept with care: the test-charge definition and why it needs a limit, the point-charge field, what the units mean, and how charges move when a field grips them. Superposition, field lines, flux, and Gauss's law each get their own article next — all of them are this one vector field, interrogated in different ways.
- The electric field is the force per unit charge a stationary test charge would feel at : , in newtons per coulomb (equivalently volts per metre).
- It splits Coulomb's action-at-a-distance into two local steps: sources set up everywhere; any charge then feels at its own location.
- A point charge makes — radial, inverse-square, pointing away from positive and toward negative charge.
- The test-charge limit matters: a finite probe would shove the sources around and distort the very field it reports.
- is the field of the other charges — a charge feels no net force from its own field.
- A charge in a uniform field is projectile motion reborn: constant acceleration , parabolic paths, with gravity usually negligible by many orders of magnitude.
- Key idea: the field is force-readiness filling space — sources prepare a vector at every point before any probe arrives, and reads it out locally.
The electric field is force per unit charge: in the limit of a vanishingly small positive test charge. It encodes the influence of all source charges at every point of space, so that the force on any charge is simply evaluated at the charge's location.
Where this lives today
The two-step dance — solve for the field once, then bill every particle locally with — is the computational architecture of the modern world. Particle-in-cell plasma codes, which design fusion experiments and simulate solar storms, advance billions of macro-particles per step by exactly equation (4), with the field updated on a grid between kicks. Every accelerator, from a hospital X-ray tube to the 27-km LHC, is engineering built on : superconducting radio-frequency cavities hold oscillating fields of tens of megavolts per metre, timed so each passing bunch always feels the push. At the other end of the scale, atomic-force and Kelvin-probe microscopies map the stray electric field nanometres above a surface to image single-charge defects in semiconductors. And the "field is real" mental shift is now metrological fact: the fields that left a magnetar or a merging black-hole system carry energy across gigaparsecs to instruments on Earth — nobody's test charge required en route.
The physical picture
Think of the field as force-readiness saturating space. Before you place any probe anywhere, the source charges have already prepared, at every single point, a vector answering a hypothetical question: "if a unit positive charge sat here, which way would it be pushed, and how hard?" The test charge merely samples this pre-existing condition — it reads the answer; it does not create it. That is why we write as a function of position like a temperature map: it is defined everywhere, including all the empty places where nothing sits and nothing is measured.
Two features of the definition are engineered, and both repay attention. The probe is positive by convention — so points away from positive sources and toward negative ones, and a negative charge feels a force against the field. And the probe is vanishingly small — not because small charges are nicer, but because a finite test charge would exert forces back on the sources, dragging them into new positions (or polarizing them) and thereby rewriting the very field it was sent to measure. The limit is the instruction "measure without disturbing," made precise. The deepest sentence in this article is the mental shift it asks of you. In statics, you may treat as a computational convenience — Coulomb's law with the test charge factored out, which is literally how the derivation below produces it. But hold the concept loosely enough to upgrade it later: the moment charges accelerate, disturbances in detach and propagate at speed , carrying energy and momentum through genuinely empty space. Sunlight pressing on your skin is a field that left its source eight minutes ago. The field is not scaffolding around the "real" charges; by the end of this track it is the real thing, and the charges are where it starts and stops.
The definition, and the two-step dance
The operational definition comes first, because everything else is commentary on it. Put a small positive charge at rest at the point , measure the electric force on it, divide, and shrink the probe:
where: is the electrostatic force on the probe and the limit protects the sources from being disturbed by the measurement. The quotient strips the probe out of the story: what remains is a property of the place, manufactured by all the other charges. Units: newtons per coulomb, which you will soon prefer to write as volts per metre — the two are identical, , and the second form becomes natural once the potential arrives two articles from now. Read backwards, the definition becomes the force law, and this is how the field is actually used. If the field at a charge's location is — produced by everything else — then the force on the charge is
where: carries its sign: positive charges are pushed along the field, negative charges against it. Note what equation (2) does not contain: the positions of the sources, their number, their shapes. All of that has been pre-digested into one local vector. This is the two-step dance of field theory — sources make the field; the field moves the charge — and every force calculation in the rest of the track walks these two steps rather than reaching back to Coulomb pair sums. For the simplest source, one point charge at the origin, the field follows immediately from Coulomb's law (the first derivation below does it honestly):
where: points radially away from the charge, so a positive makes an outward-pointing hedgehog and a negative an inward one. The is the same sphere-dilution geometry as the force law — at 30 cm from a 5 μC charge the field is already N/C, and doubling the distance would cut it fourfold. When many charges are present their fields simply add as vectors, and when the sources smear into a continuum the sum becomes an integral — those two upgrades are the whole business of the next two articles, so here we keep a single source and get the concept right. For orientation, the local laws this field obeys — derived once the machinery of divergence and curl meets Gauss's law at the end of this chapter — are worth previewing as a destination sign: in statics, and . Every property of you will prove in tiers E1 and E2 is packed into that pair.
| question | answer | where it lives |
|---|---|---|
| what force on charge here? | , done | this article |
| what field does one point charge make? | eq. (3), radial hedgehog | this article |
| what field do several charges make? | vector-sum the individual fields | next article (superposition) |
| what about smeared-out charge? | sum becomes over density | continuous distributions |
| how do I see a field? | draw its lines | electric field lines |
| is there a shortcut for symmetric sources? | flux + Gauss's law | end of this chapter |
We want to extract the field of a point charge — equation (3) — from Coulomb's force law, and in doing so make precise what the test-charge limit is protecting. The strategy is almost embarrassingly short: write the Coulomb force on a probe charge, divide by the probe, and watch the probe cancel out. The honest content is in the two fine-print clauses: why a limit is required at all, and why the field a charge feels must exclude its own contribution. Both clauses are where beginners lose points, and both are physics rather than pedantry.
Step 1. Write the Coulomb force on a probe charge at position , exerted by a source charge fixed at the origin:
Why fix the source? Because Coulomb's law holds for charges at rest; we are constructing the static field, so the source must genuinely stay put during the measurement.
Step 2. Divide by the probe:
Why does everything about the probe vanish? Coulomb's law is linear in , so the quotient is probe-independent — the same vector for any probe. That probe-independence is precisely what entitles us to call the quotient a property of the point rather than of the measurement.
Step 3. Take the limit and define the result as . For an ideal rigid source the limit changes nothing — Step 2 was already probe-free. The limit earns its keep for real sources: a finite probe attracts or repels the source charges, moving them (or polarizing a nearby conductor), so the measured quotient would depend on through the disturbed source positions. Shrinking the probe shrinks the back-reaction to zero and recovers the undisturbed field. Why positive by convention? So the direction of means "which way a positive charge is pushed" — one convention fixed once, and every sign downstream (field lines out of , potential decreasing along ) inherits it.
Step 4. State the self-field exclusion. The force on a charge sitting in the field is , where is produced by all charges except itself. A point charge's own field is radially symmetric about the charge and yields no net push on it — a static charge does not bootstrap itself into motion. (The refined question, what happens when an accelerating charge interacts with its own field, is real physics — radiation reaction — and waits at the far end of the track.) Dimensions check: , as required. The -independence of Step 2 is exact linearity of Coulomb's law.
A charge in a uniform field: projectile motion reborn
The fastest way to feel that is usable is to let it accelerate something. Between closely spaced parallel plates (the workhorse geometry of the coming tiers) the field is nearly uniform — same magnitude, same direction everywhere. Drop a charge in, and equation (2) hands dynamics straight to Newton:
where: the acceleration is constant, so every kinematics result you own from mechanics — parabolic trajectories, , range formulas — transplants wholesale, with in the seat that used to occupy. Two new features have no gravitational analogue: the sign of can flip the acceleration against the field, and the charge-to-mass ratio makes different species respond wildly differently — an electron accelerates times harder than a proton in the same field. For an electron in even a modest N/C field, , some thirteen orders of magnitude beyond — which is why gravity is simply deleted from these problems without apology.
Go deeper · Derivation B · 2 minDeflection of a charge crossing a uniform field
We derive the workhorse formula for a charged particle shot across a uniform field — the geometry of the cathode-ray tube, the inkjet printhead, and the exam problem you will actually be handed. The goal: a particle of charge , mass , enters a region of uniform (perpendicular to its velocity ) that extends over a length ; find the sideways deflection and exit angle. The strategy is exactly projectile motion: the motion splits into an untouched coordinate along and a uniformly accelerated coordinate along , coupled only through the time spent inside. Watch that the deflection grows as — the quadratic footprint of constant acceleration — while the exit angle grows only as .
Step 1. Split the motion. Take along the initial velocity and along the force . No force acts along , so ; along , equation (4) gives constant acceleration starting from rest:
Why is the split legitimate? Newton's second law is a vector equation; with uniform, its components decouple exactly, just as gravity decouples from horizontal motion for a thrown ball.
Step 2. Eliminate time. The particle is inside the field for , so the deflection at exit is
Why and ? Doubling the plate length doubles the time inside and the deflection is quadratic in time; doubling the speed halves the time and the deflection falls fourfold. Fast particles are stiff — this single scaling explains why high-energy beams need long deflectors or strong fields.
Step 3. Exit angle. The transverse velocity at exit is , so
Why is exactly ? Compare the two boxed results: the exit angle equals that of a straight line drawn from the midpoint of the plates through the exit point — a parabola's exit tangent always back-projects to half the chord. Instrument designers use this: the beam behaves as if deflected sharply at the plate centre.
Step 4. Audit the neglect of gravity. The ratio of electric to gravitational force for an electron in N/C is . Dropping gravity is not an approximation so much as a rounding. Limits check: as or , as expected. The midpoint identity holds: . ✓ ✓
Limiting cases
| case | result | meaning |
|---|---|---|
| single point charge | the atomic unit of every field map | |
| far from any bounded distribution | from far enough away, everything looks like a point of its total charge | |
| uniform field region | constant | projectile motion with replaced; sign and new |
| inside a conductor in equilibrium | free charges rearrange until they cancel the field — the shielding principle | |
| infinite uniform sheet | , distance-independent | the plane never "recedes"; derived via Gauss's law soon |
| probe not small | measured depends on | sources disturbed — the limit in (1) is doing real work |
Worked examples
1 · Reading a field, then billing a force (confidence builder)
A point charge sits at the origin. (a) Find the field at , 30 cm away on the -axis. (b) A charge nC is now placed at ; find the force on it.
Step 1. Field magnitude from equation (3): the numerator is ; divide by to get .
Step 2. Direction: the source is positive, so points away from the origin — along at . Thus N/C, a property of the point itself, computed before any second charge appears.
Step 3. Now the two-step dance, step two. Force on : N.
Step 4. Read it physically: magnitude mN, directed along — toward the source, as it must be for unlike charges. Note what we never did: re-derive anything from Coulomb's law with two charges. The field at was fixed once; any charge dropped there afterwards is billed by alone.
Answer: N/C pointing away from the source; N on the −2 nC charge, directed toward the source.
2 · Electron through deflection plates (exam level)
An electron ( kg, ) enters midway between parallel plates with horizontal speed m/s. The plates are cm long and produce a uniform downward field N/C. Find the deflection and exit angle, and check gravity is negligible.
Step 1. Direction bookkeeping first. The field points down; the electron's charge is negative, so the force points up. The electron deflects upward with acceleration magnitude
Step 2. Time between the plates: s — about a nanosecond.
Step 3. Deflection at exit (Derivation B, Step 2): m mm.
Step 4. Exit angle: m/s, so , giving . Downstream, this sub-degree tilt is what paints the whole screen of an old oscilloscope: 30 cm after the plates the beam has climbed a further mm.
Step 5. Gravity audit: in ns, free fall drops the electron m — orders of magnitude smaller than an atomic nucleus. Deleted, with a clear conscience.
Answer: the electron exits deflected mm upward at to its initial direction; the electric acceleration () outguns gravity by thirteen orders of magnitude.
Origins · 1 minMichael Faraday and how this was discovered
The field concept was born in the mind of a bookbinder's apprentice with no formal mathematics. Faraday, hired by Humphry Davy as a laboratory assistant, became the greatest experimentalist of his century — and because he did not think in equations, he thought in pictures: space around charges and magnets filled with lines of force, real as rigging, transmitting push and pull hand-over-hand through the intervening space. His contemporaries mostly indulged this as a useful crutch while the serious people computed action-at-a-distance forces. It was Maxwell who insisted Faraday had it right — "Faraday, in his mind's eye, saw lines of force traversing all space where the mathematicians saw centres of force attracting at a distance" — and built the equations of the field on Faraday's pictures. Every you write is Faraday's intuition wearing Maxwell's notation.
Going further
References. Griffiths, Introduction to Electrodynamics, 4th ed., §2.1–2.2 · Purcell & Morin, Electricity and Magnetism, 3rd ed., Ch. 1 · Jackson, Classical Electrodynamics, 3rd ed., §1.1–1.5 · Zangwill, Modern Electrodynamics, §3.1–3.3 · Feynman Lectures on Physics, Vol. II, Ch. 1 The ring axial field and its and limits, and the infinite-line field via the standard integral giving , are both worked in the continuous-distributions article of this chapter. All numerical examples here use ; the worked numbers on this page ( N/C and mN; electron deflection mm, exit angle , , gravity ratio ) are illustrative arithmetic from equations (1)–(4).
Builds on: Coulomb's Law · Vectors and vector fields Leads to: Superposition Principle for Electric Fields · Continuous Charge Distributions · Electric Field Lines · Electric Flux · Gauss's Law in Integral Form · Electrostatic Potential
Is the electric field actually real, or just a bookkeeping device for Coulomb's law?
In statics you genuinely cannot tell — every static prediction of field theory matches action-at-a-distance exactly, which is why the question feels slippery. The tiebreaker is time dependence. Wiggle a charge: the news reaches a distant charge only after a light-travel delay, and during transit the energy and momentum must be somewhere — bookkeeping fails, because a ledger cannot carry momentum across a vacuum. The field can and does: radiation pressure, the momentum kick of light, is measured routinely. Physics' working verdict: the field is a real physical system with its own degrees of freedom; the static case is the corner where its reality happens to be invisible.
If the test charge has to be vanishingly small, how does anyone actually measure a field?
You don't literally shrink a charge to zero — you either (a) use a probe small enough that the back-reaction is below your error bars (a nanocoulomb near lab sources moves nothing measurable), (b) measure at several probe values and extrapolate to , or (c) sidestep force entirely: measure the potential difference between two points with a high-impedance voltmeter and divide by the separation, exploiting . Field mills — spinning shutters that chop the field and read the induced charge — measure atmospheric fields (about 100 V/m on a fair day) without any test charge at all. The limit in the definition is conceptual hygiene; the lab has workarounds.
Why doesn't a charge feel its own field? Its own field is strongest right where it sits.
By symmetry, for a point charge at rest: its own field points radially outward in every direction, so the self-push sums to zero — there is no direction it could pick. For extended or accelerating charges the question turns deep: an accelerating electron's field pattern is asymmetric in just the right way to push back on it (radiation reaction), and computing that self-force for a true point charge produces infinities that troubled Lorentz, Dirac, and ultimately quantum field theory, where renormalization tames them. At this tier the operational rule suffices and is exact: in , the field is that of all other charges.
N/C and V/m — which should I use, and why are they the same?
They are the same unit, two mnemonic costumes. advertises the definition, force per charge. advertises the geometry you will meet with the potential: field is how steeply the potential drops per metre. The identity is one line of dimensional algebra — , so . Practitioners overwhelmingly quote V/m (a capacitor gap "at 3 kV/mm," air breaking down "at 3 MV/m") because voltages are what instruments read. Use whichever your current equation makes natural; convert without ceremony.
Does the field at a point exist even if there's no charge there to feel it?
Yes — that is precisely what makes a field, a function defined over all of space, rather than a list of forces on existing particles. The sources have arranged a definite vector at every point, exactly as the atmosphere has a temperature at points where no thermometer sits. Operationally, "the field here is 500 N/C" is a conditional certified by physics: if a unit charge were placed here, it would feel 500 N. In statics you may treat that as shorthand; in electrodynamics the empty-space field carries measurable energy density , so the vacuum with a field in it is genuinely, physically different from the vacuum without.
Why does E point away from positive charges — is that a fact of nature or a choice?
A choice, made once, in the definition: the test charge is positive by convention. Had physics standardized on negative probes, every field arrow would flip and every law would hold with adjusted signs. What is a fact of nature is relational: unlike charges attract, and the electron's charge is opposite the proton's. The awkward heritage is Franklin's: his "positive" fluid turned out to be the one that mostly doesn't move in metals, so conventional field and current directions run opposite to actual electron drift. Engineers and physicists have lived comfortably with this inversion for a century and a half; you will too, provided you re-anchor on "which way would a positive charge go?" whenever signs wobble.
When exactly can I treat a field as "uniform," like in the deflection derivation?
When the field's fractional variation over the region your particle explores is small compared to the precision you need. Between parallel plates separated by and extending over , the interior field is uniform to corrections of order near the edges ("fringing fields"); the deflection formula is excellent for and instrument-grade beyond . The same judgment recurs everywhere: near any smooth charged surface, zoomed in closely enough, every field looks uniform — which is why the parallel-plate results are the local building blocks of much bigger electrostatics.
The overview says the static field is "Coulomb's law rearranged" — so what do I actually gain right now, before radiation?
Three immediate dividends. Modularity: solve for of a source once, then answer force questions for any charge dropped anywhere, without re-summing pairs — worked example 1 is deliberately structured this way. New solvable physics: the field concept lets you formulate conductors ( inside), dielectrics, and boundary conditions, none of which have clean pair-force formulations. The right language: Gauss's law, potential, capacitance — every tool in the next ten articles is a statement about , not about forces. You are not learning a rearrangement; you are learning the variables in which electromagnetism is actually written.