A classical result from vector calculus says that if a vector field $F: \mathbb{R}^3 \to \mathbb{R}^3$ satisfies curl$(F) = 0$, then $F$ is conservative, i.e. $F = \nabla f$ for some $f: \mathbb{R}^3 \to \mathbb{R}$. I am curious about the following rough sketch of a proof of this fact, using Stokes's theorem:
"Proof:" Recall that $F$ is conservative if and only if $\int_C F \cdot dr = 0$ for every closed curve $C$. To show the latter condition, let $C$ be any curve, and choose an oriented surface $S$ with $\partial S = C$(!). By Stokes's theorem,
$\int_C F \cdot dr = \int_S \text{curl}(F) \cdot dS = \int_S 0 \cdot dS = 0.$
Thus $F$ is conservative.
I am wondering how the formal details of (!) would go: namely, how does one show that any closed curve $C$ is the boundary of some oriented surface $S$? This seems intuitively obvious. I would be happy with a proof of this fact even under very nice assumptions on $C$, say if $C$ is a simple, closed, smooth curve.
I haven't been able to find a reference for this, other than a parenthetical mention in Stewart's calculus, which says 'This can be done, but the proof requires advanced techniques.'
Look for "Seifert surface" in any knot-theory reference.
A quick-and-easy version is this (assuming C is smooth enough):
Project $C$ to the plane so that the image has no cusps or triple points or other weirdness (yeah, that needs Sard's theorem or something to guarantee such a projection exists -- - that's the tough part).
Mark all "crossings" as "overcrossings" or "undercrossings" -- look at any knot-diagram to see what this means.
At each crossing that looks like this:
(You can rotate others to look that way) "smooth out" the crossing to look like this:
The end result is a collection of simple closed curves in the plane. Fill in the innermost one with a disk, then remove it from your drawing; repeat until they're all filled in.
Now stack up those disks, one atop the other, each a little higher off the plane than the one below it, and glue in little "half-twisted ribbons" to put back in the crossings.
The end result is a surface whose boundary is like the curve $C$.
There's a problem: that surface may be nonorientable. And that's where a proper proof of the existence of Seifert surfaces comes in. :)