A curve is traced by one parameter; a surface needs two. Just as $\mathbf{r}(t)$ describes a curve in space, a function $\mathbf{r}(u, v)$ of two parameters sweeps out a surface. This lets us describe the quadric surfaces and many others in a form that is ready for integration.
Key idea
| Surface | Parametrization | Parameters |
|---|---|---|
| graph $z = f(x, y)$ | $\langle u, v, f(u, v) \rangle$ | $(u, v)$ in the domain |
| cylinder $x^2 + y^2 = a^2$ | $\langle a\cos u, a\sin u, v \rangle$ | ${}0 \le u \le 2\pi$ |
| sphere $x^2 + y^2 + z^2 = a^2$ | $\langle a\sin u\cos v, a\sin u\sin v, a\cos u \rangle$ | ${}0 \le u \le \pi$, ${}0 \le v \le 2\pi$ |
| cone $z = \sqrt{x^2 + y^2}$ | $\langle v\cos u, v\sin u, v \rangle$ | $v \ge 0$ |
| plane through $P_0$ spanned by $\mathbf{a}$, $\mathbf{b}$ | $P_0 + u\mathbf{a} + v\mathbf{b}$ | all $u$, $v$ |
Why it works
Worked examples
Worked example: A plane
- $\mathbf{r}(u, v) = \langle 1 + u, u + v, 2 - v \rangle$.
- $\mathbf{r}_u = \langle 1, 1, 0 \rangle$, $\mathbf{r}_v = \langle 0, 1, -1 \rangle$, and $\mathbf{r}_u \times \mathbf{r}_v = \langle -1, 1, 1 \rangle$.
- So the plane is $-(x - 1) + y + (z - 2) = 0$, that is, $-x + y + z = 1$.
Answer: $\langle 1 + u, u + v, 2 - v \rangle$, normal $\langle -1, 1, 1 \rangle$
Worked example: A cone
- $\mathbf{r}_u = \langle -v\sin u, v\cos u, 0 \rangle$, $\mathbf{r}_v = \langle \cos u, \sin u, 1 \rangle$.
- $\mathbf{r}_u \times \mathbf{r}_v = \langle v\cos u, v\sin u, -v \rangle$.
- This is $\mathbf{0}$ only when $v = 0$: the vertex, where the cone comes to a point.
Answer: $\langle v\cos u, v\sin u, -v \rangle$; not smooth at the vertex
Worked example: Recognizing a surface
- $x^2 + y^2 = 4\cos^2 u + 4\sin^2 u = 4$ for every $u$, while $z = v$ can be anything.
- It is the cylinder of radius ${}2$ around the $z$-axis.
Answer: the cylinder $x^2 + y^2 = 4$