We have already discussed a version of Stokes' theorem in the plane in Theorem 11.7. We can view a plane domain as a (flat) surface in space. Here we want to extend the theorem given there to “curved” surfaces lying in space. In Theorem 11.7 we have used the “curl” for plane vector fields instead of the “real” curl. If we view a plane domain as a surface in \(\mathbb R^3\) then we can consider the vector field \(\vect f=(f_1,f_2,0)\text{.}\) We saw in Remark 8.17 that in this case
If we assume that \(\vect n=(0,0,1)\) then the boundary of a plane domain is oriented counterclockwise by convention. Then the integrand on the left hand side of (11.3) becomes \((\curl\vect f)\cdot\vect n\text{.}\) For curved surfaces this turns out to be the right expression.
Theorem13.2.Stokes' Theorem.
Suppose that \(S\subset\mathbb R^3\) is a smooth orientable surface with piecewise smooth boundary \(\partial S\text{.}\) Furthermore, let \(\vect f\) be a smooth vector field. Finally assume that \(\partial S\) is oriented as explained in the previous section, and denote the positive unit normal to \(S\) by \(\vect n\text{,}\) and the positive unit tangent vecctor to \(\partial S\) by \(\vect\tau\text{.}\) Then
For simplicity we only give a proof for surfaces that can be completely described by one parametrisation. We therefore assume that
\begin{equation*}
\vect g(\vect y)
=\bigl(g_1(y_1,y_2),g_2(y_1,y_2),g_3(y_1,y_2)\bigr),
\qquad (y_1,y_2)\in D
\end{equation*}
is a regular parametrisation of \(S\text{.}\) Suppose that \((y_1(t),y_2(t))\text{,}\)\(t\in[a,b]\text{,}\) is a parametrisation of \(\partial D\) which is regular on every smooth part of \(\partial D\text{.}\) Then set
Clearly the image of \(\vect\gamma\) contains \(\partial S\text{,}\) but it could be more. When deforming \(D\) into \(S\) we have to paste part of the edges together. Note however that \(\vect\gamma(t)\) runs twice along these `cuts' but in opposite directions. Hence
Examples are shown in Figure 13.3 and Figure 13.4. In the first example we cut a cylinder. The dotted parts of the boundary of \(D\) and \(S\) correspond to each other. Figure 13.4 shows a half sphere parametrised by spherical coordinates. We cut the half sphere along the dotted line and then deform it into a rectangle.
As with the proof of Green's theorem and the divergence theorem we start with very simple vector fields, and then add up the results to get the formula for a general vector field. Hence assume that \(\vect f=(f_1,0,0)\text{.}\) Then by the previous formula