Differential forms, integration and the generalized Stokes theorem (part II)

Today let's see how to integrate differential forms. We begin with \mathbb{R}^n and then move on to manifolds. The n-form dx^1 \wedge \cdots \wedge dx^n is a basis for the space of linear n-forms on \mathbb{R}^n; therefore any differential n-form on \mathbb{R}^n is given by \omega = f(x^1, \ldots, x^n) dx^1 \wedge \cdots \wedge dx^n To recover the function f from \omega we can just evaluate it on the standard basis: f(p) = \omega_p(e_1, \ldots, e_n) Therefore n-forms in \mathbb{R}^n are in direct correspondence to scalar functions. Integrating \omega is easy: we set \int_{\mathbb{R}^n} \omega = \int_{\mathbb{R}^n} f(x^1, \ldots, x^n) dx^1 \cdots dx^n where the integral on the right hand side is the ordinary Riemann integral of the function f[1]. The same definition holds for integrating \omega over any domain D \subseteq \mathbb{R}^n (some reasonably well-behaved subset, possibly with boundary).

Now let M be an oriented n-dimensional manifold[2]. For simplicity we'll assume given a (properly oriented) parametrization[3] \phi : D \to M of M. If \omega is an n-form on M, we define \int_M \omega = \int_D \phi^* \omega where \phi^* \omega is the pullback form defined by, given tangent vectors v_1, \ldots, v_n at the point p \in D[4], (\phi^* \omega)_p(v_1, \ldots, v_n) = \omega_{\phi(p)}(D_p \phi \cdot v_1, \ldots, D_p \phi \cdot v_n) This integral can be proven to be independent of the parametrization, provided it induces the given orientation on M.

Example: Consider a vector field X on \mathbb{R}^n. We can re-interpret it as a differential 1-form X^\flat defined by X^\flat_p(v) = X(p) \cdot v Exercise: Show that, if X = (X^1(x^1, \ldots, x^n), \ldots, X^n(x^1, \ldots, x^n)), then X^\flat = X^1 dx^1 + \cdots + X^n dx^n Now suppose \gamma : [0, 1] \to \mathbb{R}^n parametrizes a curve. We have \int_{\gamma} X^\flat = \int_{[0,1]} \gamma^* X^\flat By definition, (\gamma^* X^\flat)_t(v) = X^\flat(\gamma'(t)v) = X(\gamma(t)) \cdot \gamma'(t)v where v is a tangent vector at t \in [0, 1]. Since this is just a number, dt(v) = v. The expression in coordinates is then \gamma^* X^\flat = X(\gamma(t)) \cdot \gamma'(t)\ dt Therefore \int_\gamma X^\flat = \int_{0}^{1} X(\gamma(t)) \cdot \gamma'(t)\ dt is the line integral of the vector field X along the curve \gamma. Observe that, indeed, such line integrals get a flipped sign if you switch the direction of the parametrization of \gamma.

Example: Consider a vector field X on \mathbb{R}^3. We can re-interpret it as a 2-form \omega[5] given by \omega_p(v, w) = \det(X(p), v, w) Exercise: Show that, for X = (X^1(x,y,z),X^2(x,y,z),X^3(x,y,z)), \omega = X^1 dy \wedge dz - X^2 dx \wedge dz + X^3 dx \wedge dy Suppose \phi : D \to \mathbb{R}^3, where \phi = \phi(u,v) and D \subseteq \mathbb{R}^2, parametrizes a surface \Sigma oriented by the normal \hat{n}, so that \frac{\partial \phi}{\partial u} \times \frac{\partial \phi}{\partial v} = \left| \frac{\partial \phi}{\partial u} \times \frac{\partial \phi}{\partial v} \right| \hat{n} Taking e_1 = (1, 0) and e_2 = (0, 1) we find \begin{equation*} \begin{split} (\phi^* \omega)_p(e_1, e_2) & = \omega_{\phi(p)} \left( D_p \phi \cdot e_1, D_p \phi \cdot e_2 \right) \\ & = \omega_{\phi(p)} \left( \frac{\partial \phi}{\partial u}, \frac{\partial \phi}{\partial v} \right) \\ & = \det \left( X(\phi(p)), \frac{\partial \phi}{\partial u}, \frac{\partial \phi}{\partial v} \right) \\ & = X(\phi(p)) \cdot \left( \frac{\partial \phi}{\partial u} \times \frac{\partial \phi}{\partial v} \right) \\ & = X(\phi(p)) \cdot \hat{n} \left| \frac{\partial \phi}{\partial u} \times \frac{\partial \phi}{\partial v} \right| \end{split} \end{equation*} Therefore \phi^* \omega = \left( X(\phi(p)) \cdot \hat{n} \right) \left| \frac{\partial \phi}{\partial u} \times \frac{\partial \phi}{\partial v} \right| du \wedge dv and thus \int_\Sigma \omega = \int_D \left( X(\phi(p)) \cdot \hat{n} \right) \left| \frac{\partial \phi}{\partial u} \times \frac{\partial \phi}{\partial v} \right| du dv is the flux of X through \Sigma. Again, we would've gotten a flipped sign by choosing the opposite orientation -\hat{n}.

This previous example can be generalized to arbitrary dimensions: a vector field X on \mathbb{R}^n can be re-interpreted as the (n-1)-form \omega given by \omega_p(v_1, \ldots, v_{n-1}) = \det(X(p), v_1, \ldots, v_{n-1}) In coordinates, \omega = X^1 dx^2 \wedge \cdots \wedge dx^n - X^2 dx^1 \wedge dx^3 \wedge \cdots \wedge dx^n + \cdots + (-1)^{n-1} X^n dx^1 \wedge dx^2 \wedge \cdots \wedge dx^{n-1} Then the integral of \omega over an oriented hypersurface \Sigma \subset \mathbb{R}^n is equal to the flux of X through \Sigma.

Next time we'll be ready to see how it all fits together into the generalized Stokes theorem.

Notes

[1] Of course this may or may not converge -- we typically integrate compactly supported forms only, i.e. those where f is zero outside a compact set

[2] If you don't know the precise definitions, don't worry -- it'll be clear in the examples.

[3] More specifically, \phi is a surjective map D \to M that is injective and C^1 with invertible derivative within the interior of the domain D \subseteq \mathbb{R}^n, such that the boundary of D maps to a set of n-dimensional volume equal to zero. (As an example, think of D = [0, 2\pi] \times [0, \pi] and \phi : D \to S^2 the spherical coordinates parametrization).

[4] Here D_p \phi \cdot v_1 is the directional derivative of \phi at p acting on the vector v_1 and so forth.

[5] This is also known as *X^b, where * is the Hodge star.

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