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Foundations of Electromagnetics
The four Maxwell equations
\[\nabla\cdot\mathbf D=\rho_v\] \[\nabla\cdot\mathbf B=0\] \[\nabla\times\mathbf E=-\frac{\partial\mathbf B}{\partial t}\] \[\nabla\times\mathbf H=\mathbf J+\frac{\partial\mathbf D}{\partial t}.\]Together with
\[\mathbf D=\epsilon\mathbf E,\qquad \mathbf B=\mu\mathbf H,\qquad \mathbf J=\sigma\mathbf E,\]these generate much of classical EM engineering.
How to navigate the foundations
From Maxwell to applications
\[\boxed{ \text{Maxwell} \rightarrow \text{wave equation} \rightarrow \text{propagation / boundaries} \rightarrow \text{guided waves / radiation} \rightarrow \text{devices and systems} }\]and for matter interaction,
\[\boxed{ \mathbf E,\mathbf B \rightarrow \text{Lorentz force / polarization / magnetization} \rightarrow \text{motion, energy shift or induced current} }\]Essential scales
Before solving a problem, compare geometry and timescales with:
- $L/\lambda$: is the structure electrically small or distributed?
- $R/R_{FF}$: near field or far field?
- $\delta/t$: does skin effect dominate conductor thickness?
- $\omega\epsilon/\sigma$: displacement current or conduction current?
- material dispersion/loss across the bandwidth of interest.
See Scaling Laws and Orders of Magnitude.
Measurement bridge
Maxwell’s equations predict fields, but experiments often measure voltages, currents, wave ratios, optical power or detector outputs. The Measurements & Instruments page shows how those observables are connected back to field quantities.
Recommended sequence
Maxwell → waves → boundaries → Poynting → transmission lines → antennas → RF systems → interaction with matter → quantum/atomic sensing.
For compact formulas use Fundamental Equations; for history see History Timeline.
Advanced roadmap — graduate electromagnetic field theory
The next level beyond Maxwell-equation recall is solving boundary-value and inverse problems using dyadic Green functions, surface equivalence, spectral methods, radiation conditions and scattering operators. In a homogeneous isotropic region, an electric field driven by current may be expressed using a dyadic Green tensor:
\[\mathbf E(\mathbf r)=i\omega\mu\int\overline{\overline{\mathbf G}}(\mathbf r,\mathbf r')\mathbf J(\mathbf r')\,d^3r',\]under the (e^{-i\omega t}) convention and a compatible definition of (\overline{\overline{\mathbf G}}). Boundary and radiation conditions determine the correct Green function.
Advanced sequence: derive Lorentz reciprocity; calculate an angular spectrum with evanescent components; solve a layered-medium reflection problem; formulate an electric-field integral equation; compare FEM/FDTD/MoM convergence on the same finite scatterer. Distinguish mathematical field singularities from poor meshing and erroneous physical models.
Further reading: MIT 6.635 Advanced Electromagnetism; W. C. Chew, Waves and Fields in Inhomogeneous Media.