Complex analysis is the most powerful tool in a physicist's mathematical arsenal. Contour integration evaluates impossible-looking real integrals; conformal maps solve 2D electrostatics; analytic continuation ties together special functions.
Verify analyticity using the Cauchy-Riemann equations and identify poles, branch cuts, and essential singularities.
Apply the residue theorem to evaluate real integrals by closing a contour in the complex plane.
Compute residues at simple and higher-order poles using the limit formula.
Derive the Kramers-Kronig relations from causality and explain why they connect absorption to dispersion.
Use Laurentseriestoclassifysingularitiesandextracttheresiduefromthecoefficientof(z−
CA.1 Analytic Functions and the Cauchy-Riemann Equations
A function f(z) = u(x,y) + iv(x,y) is analytic (holomorphic) at a point if it is complex-differentiable in a neighborhood. The necessary and sufficient condition is the Cauchy-Riemann equations:
Analytic functions are remarkable: they are infinitely differentiable, their real and imaginary parts are both harmonic (∇²u = ∇²v = 0), and they define conformal maps— angle-preserving transformations. Conformal maps reduce Laplace's equation in complicated domains to simple ones.
Key analytic functions and their singularities: e^z (entire), sin z (entire), 1/z (simple pole at z=0), ln z (branch cut), z^(1/2) (branch point), 1/(z²+1) (poles at ±i).
CA.2 The Residue Theorem
Theorem CA.1 — Cauchy's Residue Theorem
For a functionf(z)analyticinsideandonaclosedcontourCexceptatisolatedsingularitiesz1.., zn∮Cf(z)dz=2\pii∑kRes(f,zkwheretheresidueatasimplepolez0isRes(f,z0)=lim(z\toz0)(z−z0)f(z).Forapoleofordern:Res(f,z0)=(1/(n−1)!)lim(z\toz0)dn−1/dzn−1[(z−z0)nf(z
The residue theorem converts contour integrals (around closed paths in ℂ) into a sum of local quantities (residues) — a spectacular global-from-local result.
Example CA.1 — Evaluating a Real Integral by Contour Integration
EvaluateI=∫(−∞to∞)dx/(1+x4.
Poles of 1/(1+z⁴):z4=−1=eiπ→z=eiπ/4,ei3π/4,ei5π/4,ei7π/4.Upperhalf−planepoles: z1=eiπ/4=(1+i)/2,z2=ei3π/4=(−1+i)/2
Close contour:Takesemicircleinupperhalf−plane.AsR→∞,thearccontribution→0(Jordan′slemma:∣z−4∣→0fastenough.
Residue at z₁:Res(z1)=1/(4z13)=z1/(4z14)=z1/(4×(−1))=−z1/4=−(1+i)/(42.
Residue at z₂:Res(z2)=−z2/4=(1−i)/(42.
Sum of residues:∑Res=[−(1+i)+(1−i)]/(42)=−2i/(42)=−i/(22.
In physics, causality forces the real and imaginary parts of a response function χ(ω) (susceptibility, refractive index, dielectric function) to be related by the Kramers-Kronig relations:
Here P denotes the Cauchy principal value, and χ = χ' + iχ''. These follow from analyticity of χ(ω) in the upper half-plane (causality) and Jordan's lemma via the residue theorem. The relations connect absorption (Im part, χ'') to dispersion (Re part, χ') — you can measure one and compute the other.
CA.4 Laurent Series and Asymptotic Expansions
In an annular region around an isolated singularity z₀, any analytic function has aLaurent series:
f(z)=∑(n=−∞to∞)an(z−z0)na−1=Res(f,z0)(CA.3)
The residue is the coefficient of (z−z₀)^(−1). The principal part(negative powers) classifies singularities: finite number of negative powers → pole; infinitely many → essential singularity (e.g., e^(1/z) at z=0).
For large |z|, functions often have useful asymptotic expansions (not necessarily convergent, but useful term-by-term). Example: the Gamma function satisfiesStirling's approximation: