Mathematics · Upper Division

Complex Analysis

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.

PrerequisitesCalculus(Ch.22)Differentialequations(Ch.23)BasiccomplexnumbersCalculus (Ch. 22) \cdot Differential equations (Ch. 23) \cdot Basic complex numbers
Learning Goals
  • 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(zurent series to classify singularities and extract the residue from the coefficient of (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:

\partialu/\partialx=\partialv/\partialy\partialu/\partialy=\partialv/\partialx(CauchyRiemann)\partialu/\partialx = \partialv/\partialy \qquad \partialu/\partialy = -\partialv/\partialx \qquad (Cauchy-Riemann)(CA.1)

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.1Cauchy's Residue Theorem
For a functionf(z)analyticinsideandonaclosedcontourCexceptatisolatedsingularitiesz1unction f(z) analytic inside and on a closed contour C except at isolated singularities z_{1}.., znz_{n}Cf(z)dz=2\piikRes(f,zk\oint_C f(z) dz = 2\pii \sum_{k} Res(f, z_{k}wheretheresidueatasimplepolez0isRes(f,z0)=lim(z\toz0)(zz0)f(z).Forapoleofwhere the residue at a simple pole z_{0} is Res(f, z_{0}) = lim(z\toz_{0}) (z-z_{0})f(z). For a pole of ordern:Res(f,z0)=(1/(n1)!)lim(z\toz0)dn1/dzn1[(zz0)nf(zorder n: Res(f, z_{0}) = (1/(n-1)!) lim(z\toz_{0}) d^{n-1}/dz^{n-1} [(z-z_{0})^{n}f(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.1Evaluating a Real Integral by Contour Integration

EvaluateI=(to)dx/(1+x4Evaluate I = \int(-\infty to \infty) dx/(1+x^{4}.

Poles of 1/(1+z⁴):z4=1=eiπz=eiπ/4,ei3π/4,ei5π/4,ei7π/4.Upperhalfplanepolesz^{4} = -1 = e^{i\pi} \to z = e^{i\pi/4}, e^{i3\pi/4}, e^{i5\pi/4}, e^{i7\pi/4}. Upper half-plane poles: z1=eiπ/4=(1+i)/2,z2=ei3π/4=(1+i)/2z_{1} = e^{i\pi/4} = (1+i)/\sqrt2, z_{2} = e^{i3\pi/4} = (-1+i)/\sqrt2
Close contour:Takesemicircleinupperhalfplane.AsR,thearccontribution0(Jordanslemma:zTake semicircle in upper half-plane. As R\to\infty, the arc contribution \to 0 (Jordan's lemma: |z^{-}40fastenough^{4}| \to 0 fast enough.
Residue at z₁:Res(z1)=1/(4z13)=z1/(4z14)=z1/(4×(1))=z1/4=(1+i)/(42Res(z_{1}) = 1/(4z_{1}^{3}) = z_{1}/(4z_{1}^{4}) = z_{1}/(4\times(-1)) = -z_{1}/4 = -(1+i)/(4\sqrt2.
Residue at z₂:Res(z2)=z2/4=(1i)/(42Res(z_{2}) = -z_{2}/4 = (1-i)/(4\sqrt2.
Sum of residues:Res=[(1+i)+(1i)]/(42)=2i/(42)=i/(22\sum Res = [-(1+i) + (1-i)]/(4\sqrt2) = -2i/(4\sqrt2) = -i/(2\sqrt2.
Result:I=2\pii×(i/(22))=π/2.(Verify:dx/(1+x4)=π/(2sin(π/4))×1/2=π/2I = 2\pii \times (-i/(2\sqrt2)) = \pi/\sqrt2. ✓ (Verify: \int dx/(1+x^{4}) = \pi/(2sin(\pi/4)) \times 1/2 = \pi/\sqrt2

CA.3 Dispersion Relations and Kramers-Kronig

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:

χ(ω)=(1/π)P(to)χ(ω)/(ωω)dωχ(ω)=(1/π)Pχ(ω)/(ωω)dω\chi'(\omega) = (1/\pi) P \int(-\infty to \infty) \chi''(\omega')/(\omega'-\omega) d\omega' \qquad \chi''(\omega) = -(1/\pi) P \int \chi'(\omega')/(\omega'-\omega) d\omega'(CA.2)

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(zz0)na1=Res(f,z0)f(z) = \sum(n=-\infty to \infty) a_{n} (z-z_{0})^{n} \qquad a_{-1} = Res(f, z_{0})(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:

lnΓ(z)(z12)lnzz+12ln(2π)+1/(12z)(Stirling)ln Γ(z) \approx (z - \frac{1}{2}) ln z - z + \frac{1}{2} ln(2\pi) + 1/(12z) - \cdots \qquad (Stirling)(CA.4)
Example CA.2Green's Function via Contour Integration

FindtheretardedGreensfunctionfortheharmonicoscillator:(d2/dt2+ω02)G(t)=δ(tFind the retarded Green's function for the harmonic oscillator: (d^{2}/dt^{2} + \omega_{0}^{2})G(t) = \delta(t.

Fourier transform:G~(ω)=1/(ω2ω02).Polesatω=±ω0G̃(\omega) = -1/(\omega^{2} - \omega_{0}^{2}). Poles at \omega = \pm\omega_{0}.
Retarded condition:Shiftpolesbelowrealaxis:ωω±iε.Gret(ω)=1/((ω+iε)2ω02Shift poles below real axis: \omega \to \omega \pm i\varepsilon. G_{ret}(\omega) = -1/((\omega+i\varepsilon)^{2}-\omega_{0}^{2}.
Inverse transform:G(t)=(1/2π)G~(ω)ei\omegatdωG(t) = (1/2\pi) \int G̃(\omega) e^{-i\omegat} d\omega.
For t > 0:Closeinlowerhalfplane.Bothpolesnowinside.Sumresidues:G(t)=(1/ω0)sin(ω0t)forClose in lower half-plane. Both poles now inside. Sum residues: G(t) = (1/\omega_{0}) sin(\omega_{0}t) for t > 0.
For t < 0:Closeinupperhalfplane.Nopolesinside.G(t)=0fort<0(causalityClose in upper half-plane. No poles inside. G(t) = 0 for t < 0 (causality.
Result:Gret(t)=θ(t)sin(ω0t)/ω0.Thedrivenoscillatorresponsezerobeforetheimpulse,oscG_{ret}(t) = \theta(t) sin(\omega_{0}t)/\omega_{0}. The driven oscillator response — zero before the impulse, oscillates after.
Definition CA.1Common Traps
  • Analytic is stronger than differentiable on a line: complex differentiability constrains all directions.
  • Poles and branch points differ: only isolated poles have ordinary residues.
  • Contour orientation matters: reversing direction changes the sign of the integral.
  • Branch cuts are choices: physical results must be consistent across the chosen branch.
Exercises — CA.1–CA.4 Complex Analysis
1.
Usingtheresiduetheorem,evaluatetheintegraldx/(1+x4Using the residue theorem, evaluate the integral \int_{-}\infty^\infty dx/(1+x^{4}.
Straightforward
2.
StatethevalueoftheDirichletintegral0sin(x)/xdxandgiveitsnumericalvalueState the value of the Dirichlet integral \int_{0}^\infty sin(x)/x dx and give its numerical value.
Straightforward
3.Evaluate0sin(x)/xdx=π/2usingcontourintegration.WhichcontourdoyouuseandwhEvaluate \int_{0}^\infty sin(x)/x dx = \pi/2 using contour integration. Which contour do you use and why?
Straightforward
4.UsetheBromwichcontour(inverseLaplacetransform)tofindf(t)=L(1Use the Bromwich contour (inverse Laplace transform) to find f(t) = L^(-1{1/(s2+ω21/(s^{2}+\omega^{2}}. Compare to the Green's function result.
Intermediate
5.Use a conformalmaptosolvetheelectrostaticpotentialbetweentwoparallelconductingplatesatϕormal map to solve the electrostatic potential between two parallel conducting plates at \phi. How does this generalize to irregular geometries?
Intermediate
6.Derive Stirling's approximation for n! using the saddle-point method on the Gamma function integral. What is the reflection formula?
Challenging
Key Takeaways
  • CauchyRiemann:\partialu/\partialx=\partialv/\partialy,\partialu/\partialy=\partialv/\partialxanalyticreal/imaginarypartsharmonicCauchy-Riemann: \partialu/\partialx = \partialv/\partialy, \partialu/\partialy = -\partialv/\partialx — analytic ↔ real/imaginary parts harmonic.
  • Residuetheorem:\ointfdz=2\piiResconvertsintegralstosumsoflocalresiduesResidue theorem: \ointf dz = 2\pii \sum Res — converts integrals to sums of local residues.
  • Real integrals via contour: close in upper or lower half-plane; Jordan&apos;s lemma kills the arc.
  • KramersKronig:causalityforcesRe(χ)andIm(χ)tobeHilberttransformpairsKramers-Kronig: causality forces Re(\chi) and Im(\chi) to be Hilbert transform pairs.
  • Laurentseries:a1=residue.Poleorderfromprincipalpart;essentialsingularityhasLaurent series: a_{-1} = residue. Pole order from principal part; essential singularity has \infty terms.
  • Conformal maps preserve angles, reduce Laplace to simpler domains — key tool in 2D electrostatics.