Dashboard/Learning Hub/Physics HL/Chapter 18/18.3 Electric Potential, Potential Energy, and Equipotential Geometry

Physics HL · Chapter 18: Electric and Magnetic Fields

18.3 Electric Potential, Potential Energy, and Equipotential Geometry

Use scalar potential methods for work and energy, then connect potential gradients to electric-field direction and magnitude.

Estimated time: 48 minutes

Electric Potential and Potential Energy Definitions

Electric potential Ve at a point is work done per unit positive test charge to bring that charge from infinity to the point. Potential energy Ep belongs to a system of charges, and for a specific charge q at a location of potential Ve, Ep = qVe. Potential is scalar, so addition is algebraic rather than vectorial.

V_e= rac{W}{q},qquad V_e = k rac{Q}{r},qquad E_p=qV_e

For point or spherically symmetric source charge Q at distance r.

Sign handling matters. Positive source charge gives positive potential nearby; negative source gives negative potential. Potential energy sign then depends on both source potential and the sign of the inserted charge. This is why electron and proton scenarios at the same location can produce opposite Ep signs.

Potential Differences and Work

W=qDeltaVe=q(VBVA)W = qDelta V_e = q(V_B - V_A)

Use consistent sign convention for the agent doing work versus work done by the electric field.

Potential methods are usually faster than force-integration methods in exam settings because path details disappear for electrostatic fields. If the field is conservative, the work depends only on start and end potentials. This is the same strategic advantage you used in gravitation.

In uniform fields, potential changes linearly with distance along field direction. In point-charge fields, potential varies as 1/r. That difference in functional form changes graph shape and gradient behavior, so graph interpretation questions can often be solved with qualitative reasoning before any substitution.

Electric field magnitude equals the spatial rate of potential decrease. The field points toward lower potential for a positive test charge model. On a potential-versus-position graph, steeper slope means larger field magnitude.

E = - rac{dV_e}{dr}quad( ext{one-dimensional radial form})

Negative sign encodes direction toward decreasing potential.

Equipotential Surfaces and Field Lines

Equipotential surfaces connect locations with equal potential. Moving charge along one equipotential requires zero work because DeltaV = 0. Field lines are always normal to equipotentials; if they were not, the field would have a tangential component and would do work along the surface, contradicting the definition.

For isolated point charge, equipotentials are concentric spheres. For two-charge systems they become distorted surfaces whose spacing still encodes field strength. Regions where equipotentials are tightly packed correspond to stronger fields.

Simulation: Potential and Gradient Explorer

Move a probe through a two-charge map and connect local field vectors to potential values and test-charge force.

+-

|E| at probe

4.15e+6 N/C

Potential Ve

0.00 V

Force on test q

0.02 N

Field direction

0.0 deg

Test Yourself

A proton moves through a potential difference of 250 V from higher to lower potential. Enter its kinetic-energy gain.

Hint: Use Delta Ek = q Delta V with q = 1.6 x 10^-19 C.