The formulas for divergence and curl are easy to compute and easy to misread. Here is what they measure, in the language of a flowing fluid with velocity field $\mathbf{F} = \langle P, Q \rangle$. Divergence is net outflow per unit area. Curl is circulation per unit area: how strongly the flow turns a tiny paddle wheel.
Idea clave
Por qué funciona
Circulation around the same box, counterclockwise: bottom $P(x, y)\,\Delta x$, top $-P(x, y + \Delta y)\,\Delta x$, right $Q(x + \Delta x, y)\,\Delta y$, left $-Q(x, y)\,\Delta y$. These add to about $(Q_x - P_y)\,\Delta A$.
A rigid rotation $\mathbf{v} = \omega\langle -y, x \rangle$ has $Q_x - P_y = \omega + \omega = 2\omega$: curl is twice the angular velocity.
Worked examples
Ejemplo resuelto: Shear flow
- $P_x + Q_y = 0 + 0 = 0$: no spreading, no bunching.
- $Q_x - P_y = 0 - 1 = -1$: a paddle wheel turns clockwise, at every point.
- All arrows are horizontal, but they get longer as $y$ grows. The difference in speed across the wheel is what turns it.
Respuesta: divergence ${}0$, curl $-1$
Ejemplo resuelto: Radial flow
- $P_x + Q_y = 1 + 1 = 2$: every point is a source; any small region loses fluid at rate ${}2$ per unit area.
- $Q_x - P_y = 0 - 0 = 0$: no spin anywhere.
Respuesta: divergence ${}2$, curl ${}0$
Ejemplo resuelto: A whirlpool with no curl
- $Q_x = \frac{(x^2 + y^2) - x \cdot 2x}{(x^2 + y^2)^2} = \frac{y^2 - x^2}{(x^2 + y^2)^2}$.
- $P_y = -\frac{(x^2 + y^2) - y \cdot 2y}{(x^2 + y^2)^2} = \frac{y^2 - x^2}{(x^2 + y^2)^2}$.
- $Q_x - P_y = 0$. The arrows circle the origin, but their length ${}1/r$ drops off just fast enough that a paddle wheel away from the origin does not turn. (All the spin is concentrated at the origin; see Green's theorem for regions with holes.)
Respuesta: ${}0$ for $(x, y) \ne (0, 0)$
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