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. 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. For simplicity we'll assume given a (properly oriented) parametrization
\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,
(\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 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
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