16.6 Parametric Surfaces and
Their Areas
Parametric Surfaces and Their Areas
Here we use vector functions to describe more general surfaces, called parametric surfaces, and compute their areas.
Then we take the general surface area formula and see how it applies to special surfaces.
Parametric Surfaces
Parametric Surfaces
In much the same way that we describe a space curve by a vector function r(t) of a single parameter t, we can describe a surface by a vector function r(u, v) of two parameters u and v.
We suppose that
r(u, v) = x(u, v)i + y(u, v)j + z(u, v)k
is a vector-valued function defined on a region D in the uv-plane.
Parametric Surfaces
So x, y, and z, the component functions of r, are functions of the two variables u and v with domain D.
The set of all points (x, y, z) in such that
x = x(u, v) y = y(u, v) z = z(u, v) and (u, v) varies throughout D, is called a parametric surface S and Equations 2 are called parametric
equations of S.
Parametric Surfaces
Each choice of u and v gives a point on S; by making all choices, we get all of S.
In other words, the surface S is traced out by the tip of the position vector r(u, v) as (u, v) moves throughout the
region D. (See Figure 1.)
Figure 1
A parametric surface
Example 1
Identify and sketch the surface with vector equation r(u, v) = 2 cos u i + v j + 2 sin u k
Solution:
The parametric equations for this surface are x = 2 cos u y = v z = 2 sin u
Example 1 – Solution
So for any point (x, y, z) on the surface, we have x2 + z2 = 4 cos2u + 4 sin2u
= 4
This means that vertical cross-sections parallel to the xz-plane (that is, with y constant) are all circles with radius 2.
cont’d
Example 1 – Solution
Since y = v and no restriction is placed on v, the surface is a circular cylinder with radius 2 whose axis is the y-axis (see Figure 2).
cont’d
Parametric Surfaces
If a parametric surface S is given by a vector function
r(u, v), then there are two useful families of curves that lie on S, one family with u constant and the other with v
constant.
These families correspond to vertical and horizontal lines in the uv-plane.
Parametric Surfaces
If we keep u constant by putting u = u0, then r(u0, v)
becomes a vector function of the single parameter v and defines a curve C1 lying on S. (See Figure 4.)
Parametric Surfaces
Similarly, if we keep v constant by putting v = v0, we get a curve C2 given by r(u, v0) that lies on S.
We call these curves grid curves. (In Example 1, for
instance, the grid curves obtained by letting u be constant are horizontal lines whereas the grid curves with v constant are circles.)
In fact, when a computer graphs a parametric surface, it
usually depicts the surface by plotting these grid curves, as we see in the next example.
Example 2
Use a computer algebra system to graph the surface
r(u, v) = 〈(2 + sin v) cos u, (2 + sin v) sin u, u + cos v〉
Which grid curves have u constant? Which have v constant?
Example 2 – Solution
We graph the portion of the surface with parameter domain 0 ≤ u ≤ 4π, 0 ≤ v ≤ 2π in Figure 5.
Figure 5
Example 2 – Solution
It has the appearance of a spiral tube.
To identify the grid curves, we write the corresponding parametric equations:
x = (2 + sin v) cos u y = (2 + sin v) sin u z = u + cos v If v is constant, then sin v and cos v are constant, so the parametric equations resemble those of the helix.
Thus the grid curves with v constant are the spiral curves in Figure 5.
cont’d
Example 2 – Solution
We deduce that the grid curves with u constant must be the curves that look like circles in the figure.
Further evidence for this assertion is that if u is kept
constant, u = u0 , then the equation z = u0 + cos v shows that the z-values vary from u0 – 1 to u0 + 1.
cont’d
Example 4
Find a parametric representation of the sphere x2 + y2 + z2 = a2
Solution:
The sphere has a simple representation ρ = a in spherical coordinates, so let’s choose the angles φ and θ in spherical coordinates as the parameters.
Example 4 – Solution
Then, putting ρ = a in the equations for conversion from spherical to rectangular coordinates, we obtain
x = a sin φ cos θ y = a sin φ sin θ z = a cos φ as the parametric equations of the sphere.
The corresponding vector equation is
r(φ, θ) = a sin φ cos θ i + a sin φ sin θ j + a cos φ k
cont’d
Example 4 – Solution
We have 0 ≤ φ ≤ π and 0 ≤ θ ≤ 2π, so the parameter domain is the rectangle D = [0, π] × [0, 2π].
The grid curves with φ constant are the circles of constant latitude (including the equator).
cont’d
Example 4 – Solution
The grid curves with θ constant are the meridians
(semi-circles), which connect the north and south poles (see Figure 7).
Figure 7
cont’d
Parametric Surfaces
Note
We saw in Example 4 that the grid curves for a sphere are curves of constant latitude or constant longitude.
For a general parametric surface we are really making a map and the grid curves are similar to lines of latitude and longitude.
Describing a point on a parametric surface (like the one in Figure 5) by giving specific values of u and v is like giving the latitude and longitude of a point.
Surfaces of Revolution
Surfaces of Revolution
Surfaces of revolution can be represented parametrically and thus graphed using a computer. For instance, let’s consider the surface S obtained by rotating the curve y = f(x), a ≤ x ≤ b, about the x-axis, where f(x) ≥ 0.
Let θ be the angle of rotation as shown in Figure 10.
Surfaces of Revolution
If (x, y, z) is a point on S, then
x = x y = f(x) cos θ z = f(x) sin θ
Therefore we take x and θ as parameters and regard Equations 3 as parametric equations of S.
The parameter domain is given by a ≤ x ≤ b, 0 ≤ θ ≤ 2π .
Example 8
Find parametric equations for the surface generated by rotating the curve y = sin x, 0 ≤ x ≤ 2π, about the x-axis.
Use these equations to graph the surface of revolution.
Solution:
From Equations 3, the parametric equations are
x = x y = sin x cos θ z = sin x sin θ and the parameter domain is 0 ≤ x ≤ 2π , 0 ≤ θ ≤ 2π.
Example 8 – Solution
Using a computer to plot these equations and then rotating the image, we obtain the graph in Figure 11.
Figure 11
cont’d
Tangent Planes
Tangent Planes
We now find the tangent plane to a parametric surface S traced out by a vector function
r(u, v) = x(u, v) i + y(u, v) j + z(u, v) k at a point P0 with position vector r(u0, v0).
Tangent Planes
If we keep u constant by putting u = u0, then r(u0, v)
becomes a vector function of the single parameter v and defines a grid curve C1 lying on S. (See Figure 12.) The tangent vector to C1 at P0 is obtained by taking the partial derivative of r with respect to v:
Tangent Planes
Similarly, if we keep v constant by putting v = v0, we get a grid curve C2 given by r(u, v0) that lies on S, and its tangent vector at P0 is
If ru × rv is not 0, then the surface S is called smooth (it has no “corners”).
For a smooth surface, the tangent plane is the plane that contains the tangent vectors ru and rv, and the vector
ru × rv is a normal vector to the tangent plane.
Example 9
Find the tangent plane to the surface with parametric equations x = u2, y = v2, z = u + 2v at the point (1, 1, 3).
Solution:
We first compute the tangent vectors:
Example 9 – Solution
Thus a normal vector to the tangent plane is
Notice that the point (1, 1, 3) corresponds to the parameter values u = 1 and v = 1, so the normal vector there is
–2 i – 4 j + 4 k
cont’d
Example 9 – Solution
Therefore an equation of the tangent plane at (1, 1, 3) is –2(x – 1) – 4(y – 1) + 4(z – 3) = 0
or
x + 2y – 2z + 3 = 0
cont’d
Surface Area
Surface Area
Now we define the surface area of a general parametric surface given by Equation 1.
For simplicity we start by considering a surface whose parameter domain D is a rectangle, and we divide it into subrectangles Rij.
Surface Area
Let’s choose to be the lower left corner of Rij. (See Figure 14.)
Figure 14
The image of the subrectangle Rij is the patch Sij.
Surface Area
The part Sij of the surface S that corresponds to Rij is called a patch and has the point Pij with position vector as one of its corners.
Let
and
be the tangent vectors at Pij as given by Equations 5 and 4.
Surface Area
Figure 15(a) shows how the two edges of the patch that
meet at Pij can be approximated by vectors. These vectors, in turn, can be approximated by the vectors and because partial derivatives can be approximated by
difference quotients.
Figure 15(a)
Approximating a patch by a parallelogram.
Surface Area
So we approximate Sij by the parallelogram determined by the vectors and .
This parallelogram is shown in Figure 15(b) and lies in the tangent plane to S at Pij.
Approximating a patch by a parallelogram.
Surface Area
The area of this parallelogram is
and so an approximation to the area of S is
Surface Area
Our intuition tells us that this approximation gets better as we increase the number of subrectangles, and we
recognize the double sum as a Riemann sum for the double integral
Surface Area
This motivates the following definition.
Example 10
Find the surface area of a sphere of radius a.
Solution:
In Example 4 we found the parametric representation x = a sin φ cosθ y = a sin φ sin θ z = a cos φ where the parameter domain is
D = {(φ, θ) | 0 ≤ φ ≤ π, 0 ≤ θ ≤ 2π}
Example 10 – Solution
We first compute the cross product of the tangent vectors:
cont’d
Example 10 – Solution
= a2 sin2φ cos θ i + a2 sin2 φ sin θ j + a2 sin φ cos φ k Thus
since sin φ ≥ 0 for 0 ≤ φ ≤ π.
cont’d
Example 10 – Solution
Therefore, by Definition 6, the area of the sphere is
cont’d
Surface Area of the Graph of a function
Surface Area of the Graph of a Function
For the special case of a surface S with equation z = f(x, y), where (x, y) lies in D and f has continuous partial
derivatives, we take x and y as parameters.
The parametric equations are
x = x y = y z = f(x, y) so
and
Surface Area of the Graph of a Function
Thus we have
and the surface area formula in Definition 6 becomes
Example 11
Find the area of the part of the paraboloid z = x2 + y2 that lies under the plane z = 9.
Solution:
The plane intersects the paraboloid in the circle
x2 + y2 = 9, z = 9. Therefore the given surface lies above the disk D with center the origin and radius 3.
(See Figure 16.)
Figure 16
Example 11 – Solution
Using Formula 9, we have
cont’d
Example 11 – Solution
Converting to polar coordinates, we obtain
cont’d