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Sandbox Physics

Fields · potential and force

Electric Field

Shape a dipole or a quadrupole. Move a probe across the potential landscape, scan the field, and test how its direction follows the downhill slope.

Interactive modelElectric Field
Probe potential—\text{—}
Probe field strength—\text{—}
Horizontal field—\text{—}
Vertical field—\text{—}
Net source charge—\text{—}
Closed-loop circulation—\text{—}

FOLLOW THE EVIDENCE

A scan through the field

The scan follows the probe’s vertical position. The field and potential use one softened kernel. Dots estimate the negative slope of the sampled potential; they provide a separate numerical check.

E=−∇V,∮E⋅dℓ=0\mathbf E=-\nabla V,\qquad \oint\mathbf E\cdot\mathrm d\boldsymbol\ell=0

Height and colour visualize potential; they are not a physical surface. The moving beads only show field-line direction. The amber rectangle defines the circulation readout. Coordinates, charge, potential and field use normalized units; the source core has radius 0.1.

Physics tutorial

Electric fields: from potential terrain to force

BackgroundElectric potential is potential energy per unit charge at each position. Point-charge potentials add directly, and their spatial variation gives the field.

Why it mattersSolving for a scalar potential is often easier than summing vector fields and immediately explains voltage, equipotentials, and shielding.

Start with the essentials

Focus question
Why are field lines perpendicular to equipotentials, and why is the field stronger where color changes faster?
One-sentence intuition
Treat potential as terrain: the electric field is its steepest downhill direction, the negative gradient.

Core mathematical model

Normalized softened model in this Lab

V(r)=∑iqi∣r−ri∣2+a2,a=0.1V(\mathbf r)=\sum_i\frac{q_i}{\sqrt{|\mathbf r-\mathbf r_i|^2+a^2}},\quad a=0.1

The plane is a section of a three-dimensional field. Softening makes the source core finite; the field is the negative gradient of this same potential.

Superposed point-charge potential

V(r)=14πε0∑iqi∣r−ri∣V(\mathbf r)=\frac{1}{4\pi\varepsilon_0}\sum_i\frac{q_i}{|\mathbf r-\mathbf r_i|}

Positive charges raise potential, negative charges lower it, and scalar contributions add.

Field from potential

E=−∇V\mathbf E=-\nabla V

The gradient points uphill; the minus sign makes the field point toward decreasing potential.

Common difficulties

Zero potential does not mean zero field

Typical misconceptionA test charge feels no force wherever V=0V=0.

Better mental modelPotential depends on the chosen reference; force depends on nearby change, the gradient.

Field lines are not particle paths

Typical misconceptionA released charge must trace one field line.

Better mental modelField lines give instantaneous force direction; inertia means velocity need not stay parallel to the field.

Run the experiment

  1. 01

    Read a dipole

    Choose Dipole and show field lines with equipotentials.

    What to observe: The line families are nearly orthogonal and field lines run positive to negative.
  2. 02

    Compare the midpoint

    Switch to Like charges and inspect the center.

    What to observe: Potential adds while symmetric field vectors can cancel.
  3. 03

    Change the geometry

    Drag a source, or edit it with the source sliders.

    What to observe: Potential surface, contours, and field lines rebuild together.
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