Electrostatics and Gauss's law
The divergence of D equals the volume charge density: ∇·D = ρv. For highly symmetric charge distributions, Gauss's law in integral form directly gives D. The electric field E = D/ε in linear isotropic media. Potential difference is the negative line integral of E.
Check yourself: Does the chosen Gaussian surface exploit the charge symmetry?
Magnetostatics and Ampère's law
The curl of H equals the volume current density: ∇×H = J (static case). For symmetric current distributions, Ampère's circuital law gives H directly. B = μH in linear isotropic media. The Biot-Savart law handles arbitrary current geometries but requires integration.
Check yourself: Is the Amperian path chosen so that H is constant and tangent along it?
Boundary conditions
At a boundary between two media: tangential E is continuous; normal D jumps by surface charge density. Tangential H jumps by surface current density; normal B is continuous. These conditions determine the refraction of fields at interfaces.
Check yourself: Have you identified whether surface charges or currents exist at the boundary?
Uniform plane waves
In a lossless medium, a uniform plane wave propagates at v = 1/√(με) with intrinsic impedance η = √(μ/ε). E and H are perpendicular to each other and to the propagation direction. The time-average Poynting vector gives power flow per unit area: S = |E|²/(2η).
Check yourself: Are E, H, and the propagation direction mutually orthogonal?
Transmission lines
A lossless transmission line has characteristic impedance Z₀ = √(L/C) per unit length. The reflection coefficient at a load is Γ = (ZL − Z₀)/(ZL + Z₀). The voltage standing wave ratio is VSWR = (1 + |Γ|)/(1 − |Γ|). A matched load (ZL = Z₀) eliminates reflections.
Check yourself: Is the impedance measured at the load or at a different point along the line?