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Foundations of Electromagnetics

Illustration of Maxwell's equations and electromagnetic field quantities.
Maxwell's equations provide the field-law foundation for the topics collected here. Image source: Wikimedia Commons, Euisudyi, CC BY-SA 4.0.
30-second intuitionElectromagnetics is a theory of fields, sources, propagation and energy transfer. Maxwell's equations tell fields how to diverge and curl; material relations tell the fields how matter responds; boundary conditions connect regions; the Lorentz force tells charged matter how fields push it.

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:

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.

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.