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Lesson 15 of 30

Surfaces of revolution and special examples

Reduce surface calculations to a profile curve.

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Rotate the profile r(s)=sin s, z(s)=cos s, 0<s<π, around the z-axis. It produces the unit sphere away from its poles. The profile has unit speed, so its revolution metric is ds²+sin²s dθ².

A surface of revolution reduces many calculations to a planar profile, but a convenient parameter must still be identified. If the profile is not parametrized by arc length, the coefficient of ds² is not automatically one.

Predict

Predict which coordinate degenerates when r=0. The angular derivative vanishes, so this revolution chart loses rank. The resulting surface could be smooth, as at a sphere pole, or singular, as at a cone vertex.

Predict whether every parallel circle is a geodesic. The metric and connection will later show that only parallels at stationary profile radius have that property, except in special cases.

Experiment

For a unit-speed profile (r(s),z(s)) with r>0, compare exact coefficients.

QuantityFormula
Metricds²+r²dθ²
Chosen unit normal(−z′cos θ,−z′sin θ,r′)
Meridian curvaturer′z″−z′r″
Parallel curvaturez′/r

Insert the sphere profile: both principal values are −1 with this outward normal. Insert a vertical line profile r=R, z=s: the chosen normal points inward and the values are zero and 1/R. The sign difference is an orientation choice, not a contradiction.

Understand

Differentiate X(s,θ)=(r cos θ,r sin θ,z). The coordinate vectors have norms one and r and are orthogonal. Their ordered cross product divided by r gives the displayed N.

The second derivatives give b_ss=r′z″−z′r″, b_sθ=0 and b_θθ=rz′. Dividing by the diagonal metric coefficients yields the two principal values. Their product simplifies to K=−r″/r. Indeed differentiating r′²+z′²=1 gives r′r″+z′z″=0, and substitution into (r′z″−z′r″)z′ eliminates z″. The identity remains valid at points where z′=0 by using the undivided relation.

For a nonplanar minimal example use the catenoid X(u,v)=(cosh v cos u,cosh v sin u,v). Here E=G=cosh²v and F=0. With N from X_u×X_v, the second coefficients are e=−1, f=0, g=1. Thus the principal values are −1/cosh²v and 1/cosh²v, proving H=0 and K=−1/cosh⁴v.

Apply

Repair “The catenoid is minimal because its profile looks like a hanging chain.” A physical analogy does not verify the surface equation. The two fundamental forms and their trace supply an exact proof. Moreover, global area-minimizing behavior depends on the selected boundary and allowable competitors; stationarity alone is insufficient.

For optional depth, the torus of revolution has both positive and negative K regions because its profile radius has changing second derivative. Its total curvature will later be constrained by topology. A single revolution chart also has periodic seams, so integration requires correct coverage accounting.

At a profile pole, return to the chart definition rather than canceling r in formulas that assumed r>0.

Continue

Use the profile’s parameter, orientation and regular region explicitly in every revolution calculation. Continue to ruled and developable surfaces to compare another geometric construction that simplifies one second derivative.

Apply · explain · revise

Practice and reasoning

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For a unit sphere, using profile radius r(s)=sin s, compute −r″/r away from the poles.

Integers, fractions and finite decimals are accepted. Expressions such as sqrt(2) are not parsed by this checker.

For an arc-length profile (r(s),z(s)), r>0, the revolution metric is

Your response

Derive E=1,F=0,G=r² for X(s,θ)=(r cos θ,r sin θ,z), assuming r′²+z′²=1.

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Using N=(−z′cos θ,−z′sin θ,r′), derive k_s=r′z″−z′r″ and k_θ=z′/r.

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Verify X(u,v)=(cosh v cos u,cosh v sin u,v) has H=0.

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Why cannot the revolution chart r>0 be used to decide regularity at a profile point where r=0?

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Reflect and continue

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