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3.6: Surface Area

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Learning Objectives
  • Find the parametric representations of a cylinder, a cone, and a sphere.
  • Describe the surface area of a parametric surface.

We have seen that a line integral is an integral over a path in a plane or in space. However, if we wish to integrate over a surface (a two-dimensional object) rather than a path (a one-dimensional object) in space, then we need a new kind of integral that can handle integration over objects in higher dimensions. We can extend the concept of a line integral to a surface integral to allow us to perform this integration.

Surface integrals are important for the same reasons that line integrals are important. They have many applications to physics and engineering, and they allow us to develop higher dimensional versions of the Fundamental Theorem of Calculus. In particular, surface integrals allow us to generalize Green’s theorem to higher dimensions, and they appear in some important theorems we discuss in later sections.

Parametric Surfaces

A surface integral is similar to a line integral, except the integration is done over a surface rather than a path. In this sense, surface integrals expand on our study of line integrals. Just as with line integrals, there are two kinds of surface integrals: a surface integral of a scalar-valued function and a surface integral of a vector field.

However, before we can integrate over a surface, we need to consider the surface itself. Recall that to calculate a scalar or vector line integral over curve C, we first need to parameterize C. In a similar way, to calculate a surface integral over surface S, we need to parameterize S. That is, we need a working concept of a parameterized surface (or a parametric surface), in the same way that we already have a concept of a parameterized curve.

A parameterized surface is given by a description of the form

r(u,v)=x(u,v),y(u,v),z(u,v).

Notice that this parameterization involves two parameters, u and v, because a surface is two-dimensional, and therefore two variables are needed to trace out the surface. The parameters u and v vary over a region called the parameter domain, or parameter space—the set of points in the uv-plane that can be substituted into r. Each choice of u and v in the parameter domain gives a point on the surface, just as each choice of a parameter t gives a point on a parameterized curve. The entire surface is created by making all possible choices of u and v over the parameter domain.

Definition: Parameter Domain

Given a parameterization of surface

r(u,v)=x(u,v),y(u,v),z(u,v).

the parameter domain of the parameterization is the set of points in the uv-plane that can be substituted into r.

Example 3.6.1: Parameterizing a Cylinder

Describe surface S parameterized by

r(u,v)=cosu,sinu,v,<u<,<v<.

Solution

To get an idea of the shape of the surface, we first plot some points. Since the parameter domain is all of R2, we can choose any value for u and v and plot the corresponding point. If u=v=0, then r(0,0)=1,0,0, so point (1, 0, 0) is on S. Similarly, points r(π,2)=(1,0,2) and r(π2,4)=(0,1,4) are on S.

Although plotting points may give us an idea of the shape of the surface, we usually need quite a few points to see the shape. Since it is time-consuming to plot dozens or hundreds of points, we use another strategy. To visualize S, we visualize two families of curves that lie on S. In the first family of curves we hold u constant; in the second family of curves we hold v constant. This allows us to build a “skeleton” of the surface, thereby getting an idea of its shape.

  • Suppose that u is a constant K. Then the curve traced out by the parameterization is cosK,sinK,v, which gives a vertical line that goes through point (cosK,sinK,v in the xy-plane.
  • Suppose that v is a constant K. Then the curve traced out by the parameterization is cosu,sinu,K, which gives a circle in plane z=K with radius 1 and center (0,0,K).

If u is held constant, then we get vertical lines; if v is held constant, then we get circles of radius 1 centered around the vertical line that goes through the origin. Therefore the surface traced out by the parameterization is cylinder x2+y2=1 (Figure 3.6.1).

Three diagrams in three dimensions.
Figure 3.6.1: (a) Lines cosK,sinK,v for K=0,π2,π, and 3π2. (b) Circles cosu,sinu,K for K=2,1,1, and 2 (c) The lines and circles together. As u and v vary, they describe a cylinder.

Notice that if x=cosu and y=sinu, then x2+y2=1, so points from S do indeed lie on the cylinder. Conversely, each point on the cylinder is contained in some circle cosu,sinu,k for some k, and therefore each point on the cylinder is contained in the parameterized surface (Figure 3.6.2).

An image of a vertical cylinder in three dimension.
Figure 3.6.2: Cylinder x2+y2=r2 has parameterization r(u,v)=rcosu,rsinu,v,0u2π,<v<.
Analysis

Notice that if we change the parameter domain, we could get a different surface. For example, if we restricted the domain to 0uπ,<v<6, then the surface would be a half-cylinder of height 6.

Exercise 3.6.1

Describe the surface with parameterization

r(u,v)=2cosu,2sinu,v,0u2π,<v<

Hint

Hold u and v constant, and see what kind of curves result.

Answer

Cylinder x2+y2=4

It follows from Example 3.6.1 that we can parameterize all cylinders of the form x2+y2=R2. If S is a cylinder given by equation x2+y2=R2, then a parameterization of S is r(u,v)=Rcosu,Rsinu,v,0u2π,<v<.

We can also find different types of surfaces given their parameterization, or we can find a parameterization when we are given a surface.

Example 3.6.2: Describing a Surface

Describe surface S parameterized by r(u,v)=ucosv,usinv,u2,0u<,0v<2π.

Solution

Notice that if u is held constant, then the resulting curve is a circle of radius u in plane z=u. Therefore, as u increases, the radius of the resulting circle increases. If v is held constant, then the resulting curve is a vertical parabola. Therefore, we expect the surface to be an elliptic paraboloid. To confirm this, notice that

x2+y2=(ucosv)2+(usinv)2=u2cos2v+u2sin2v=u2=z

Therefore, the surface is the elliptic paraboloid x2+y2=z (Figure 3.6.3).

Two images in three dimensions.
Figure 3.6.3: (a) Circles arise from holding u constant; the vertical parabolas arise from holding v constant. (b) An elliptic paraboloid results from all choices of u and v in the parameter domain.
Exercise 3.6.2

Describe the surface parameterized by r(u,v)=ucosv,usinv,u,<u<,0v<2π.

Hint

Hold u constant and see what kind of curves result. Imagine what happens as u increases or decreases.

Answer

Cone x2+y2=z2

Example 3.6.3: Finding a Parameterization

Give a parameterization of the cone x2+y2=z2 lying on or above the plane z=2.

Solution

The horizontal cross-section of the cone at height z=u is circle x2+y2=u2. Therefore, a point on the cone at height u has coordinates (ucosv,usinv,u) for angle v. Hence, a parameterization of the cone is r(u,v)=ucosv,usinv,u. Since we are not interested in the entire cone, only the portion on or above plane z=2, the parameter domain is given by 2<u<,0v<2π (Figure 3.6.4).

A three-dimensional diagram of the cone x^2 + y^2 = z^2, which opens up along the z axis.
Figure 3.6.4: Cone x2+y2=z2 has parametrization r(u,v)=ucosv,usinv,u,u,<u<,0v2π.
Exercise 3.6.3

Give a parameterization for the portion of cone x2+y2=z2 lying in the first octant.

Hint

Consider the parameter domain for this surface.

Answer

r(u,v)=ucosv,usinv,u,0<u<,0v<π2

We have discussed parameterizations of various surfaces, but two important types of surfaces need a separate discussion: spheres and graphs of two-variable functions. To parameterize a sphere, it is easiest to use spherical coordinates. The sphere of radius ρ centered at the origin is given by the parameterization

r(ϕ,θ)=ρcosθsinϕ,ρsinθsinϕ,ρcosϕ,0θ2π,0ϕπ.

The idea of this parameterization is that as ϕ sweeps downward from the positive z-axis, a circle of radius ρsinϕ is traced out by letting θ run from 0 to 2π. To see this, let ϕ be fixed. Then

x2+y2=(ρcosθsinϕ)2+(ρsinθsinϕ)2=ρ2sin2ϕ(cos2θ+sin2θ)=ρ2sin2ϕ=(ρsinϕ)2.

This results in the desired circle (Figure 3.6.5).

A three-dimensional diagram of the sphere of radius rho.
Figure 3.6.5: The sphere of radius ρ has parameterization r(ϕ,θ)=ρcosθsinϕ,ρsinθsinϕ,ρcosϕ,0θ2π,0ϕπ.

Finally, to parameterize the graph of a two-variable function, we first let z=f(x,y) be a function of two variables. The simplest parameterization of the graph of f is r(x,y)=x,y,f(x,y), where x and y vary over the domain of f (Figure 3.6.6). For example, the graph of f(x,y)=x2y can be parameterized by r(x,y)=x,y,x2y, where the parameters x and y vary over the domain of f. If we only care about a piece of the graph of f - say, the piece of the graph over rectangle [1,3]×[2,5] - then we can restrict the parameter domain to give this piece of the surface:

r(x,y)=x,y,x2y,1x3,2y5.

Similarly, if S is a surface given by equation x=g(y,z) or equation y=h(x,z), then a parameterization of S is r(y,z)=g(y,z),y,z or r(x,z)=x,h(x,z),z, respectively. For example, the graph of paraboloid 2y=x2+z2 can be parameterized by r(x,y)=x,x2+z22,z,0x<,0z<. Notice that we do not need to vary over the entire domain of y because x and z are squared.

A three-dimensional diagram of a surface z = f(x,y) above its mapping.
Figure 3.6.6: The graph of a surface z=f(x,y), with height determined by f(x,y) over the x-y plane.

Let’s now generalize the notions of smoothness and regularity to a parametric surface. Recall that curve parameterization r(t),atb is regular (or smooth) if r(t)0 for all t in [a,b]. For a curve, this condition ensures that the image of r really is a curve, and not just a point. For example, consider curve parameterization r(t)=1,2,0t5. The image of this parameterization is simply point (1,2), which is not a curve. Notice also that r(t)=0. The fact that the derivative is the zero vector indicates we are not actually looking at a curve.

Analogously, we would like a notion of regularity (or smoothness) for surfaces so that a surface parameterization really does trace out a surface. To motivate the definition of regularity of a surface parameterization, consider the parameterization

r(u,v)=0,cosv,1,0u1,0vπ.

Although this parameterization appears to be the parameterization of a surface, notice that the image is actually a line (Figure 3.6.7). How could we avoid parameterizations such as this? Parameterizations that do not give an actual surface? Notice that ru=0,0,0 and rv=0,sinv,0, and the corresponding cross product is zero. The analog of the condition r(t)=0 is that ru×rv is not zero for point (u,v) in the parameter domain, which is a regular parameterization.

A three-dimensional diagram of a line on the x,z plane where the z component is 1.
Figure 3.6.7: TThe parameterization r(u,v)=0,cosv,1, where 0u1 and 0vπ. The result is straight line segment parallel to the z-axis.
Definition: Regular Parameterization

Parameterization r(u,v)=x(u,v),y(u,v),z(u,v) is a regular parameterization if ru×rv is not zero for point (u,v) in the parameter domain.

If parameterization r is regular, then the image of r is a two-dimensional object, as a surface should be. Throughout this chapter, parameterizations r(u,v)=x(u,v),y(u,v),z(u,v)are assumed to be regular.

Recall that curve parameterization r(t),atb is smooth if r(t) is continuous and r(t)0 for all t in [a,b]. Informally, a curve parameterization is smooth if the resulting curve has no sharp corners. The definition of a smooth surface parameterization is similar. Informally, a surface parameterization is smooth if the resulting surface has no sharp corners.

Definition: Smooth Surfaces

A surface parameterization r(u,v)=x(u,v),y(u,v),z(u,v) is smooth if vector ru×rv is not zero for any choice of u and v in the parameter domain.

Exercise 3.6.4

Is the surface parameterization r(u,v)=u2v,v+1,sinu,0u2,0v3 smooth?

Hint

Investigate the cross product ru×rv.

Answer

Yes

Surface Area of a Parametric Surface

Our goal is to define a surface integral, and as a first step we have examined how to parameterize a surface. The second step is to define the surface area of a parametric surface. The notation needed to develop this definition is used throughout the rest of this chapter.

Let S be a surface with parameterization r(u,v)=x(u,v),y(u,v),z(u,v) over some parameter domain D. We assume here and throughout that the surface parameterization r(u,v)=x(u,v),y(u,v),z(u,v) is continuously differentiable—meaning, each component function has continuous partial derivatives. Assume for the sake of simplicity that D is a rectangle (although the following material can be extended to handle nonrectangular parameter domains). Divide rectangle D into subrectangles Dij with horizontal width Δu and vertical length Δv. Suppose that i ranges from 1 to m and j ranges from 1 to n so that D is subdivided into mn rectangles. This division of D into subrectangles gives a corresponding division of surface S into pieces Sij. Choose point Pij in each piece Sij. Point Pij corresponds to point (ui,vj) in the parameter domain.

Note that we can form a grid with lines that are parallel to the u-axis and the v-axis in the uv-plane. These grid lines correspond to a set of grid curves on surface S that is parameterized by r(u,v). Without loss of generality, we assume that Pij is located at the corner of two grid curves, as in Figure 3.6.9. If we think of r as a mapping from the uv-plane to R3, the grid curves are the image of the grid lines under r. To be precise, consider the grid lines that go through point (ui,vj). One line is given by x=ui,y=v; the other is given by x=u,y=vj. In the first grid line, the horizontal component is held constant, yielding a vertical line through (ui,vj). In the second grid line, the vertical component is held constant, yielding a horizontal line through (ui,vj). The corresponding grid curves are r(ui,v) and (u,vj) and these curves intersect at point Pij.

Two diagrams, showing that grid lines on a parameter domain correspond to grid curves on a surface.
Figure 3.6.9: Grid lines on a parameter domain correspond to grid curves on a surface.

Now consider the vectors that are tangent to these grid curves. For grid curve r(ui,v), the tangent vector at Pij is

tv(Pij)=rv(ui,vj)=xv(ui,vj),yv(ui,vj),zv(ui,vj).

For grid curve r(u,vj), the tangent vector at Pij is

tu(Pij)=ru(ui,vj)=xu(ui,vj),yu(ui,vj),zu(ui,vj).

If vector N=tu(Pij)×tv(Pij) exists and is not zero, then the tangent plane at Pij exists (Figure 3.6.10). If piece Sij is small enough, then the tangent plane at point Pij is a good approximation of piece Sij.

Visualization of tangent plane.
Figure 3.6.10: If the cross product of vectors tu and tv exists, then there is a tangent plane. On the left is a rectangular region divided into many subrectangles with the point (u0,v0). On the right is the same point transformed on a surface using the vector function r.

The tangent plane at Pij contains vectors tu(Pij) and tv(Pij) and therefore the parallelogram spanned by tu(Pij) and tv(Pij) is in the tangent plane. Since the original rectangle in the uv-plane corresponding to Sij has width Δu and length Δv, the parallelogram that we use to approximate Sij is the parallelogram spanned by Δutu(Pij) and Δvtv(Pij). In other words, we scale the tangent vectors by the constants Δu and Δv to match the scale of the original division of rectangles in the parameter domain. Therefore, the area of the parallelogram used to approximate the area of Sij is

ΔSij||(Δutu(Pij))×(Δvtv(Pij))||=||tu(Pij)×tv(Pij)||ΔuΔv.

Varying point Pij over all pieces Sij and the previous approximation leads to the following definition of surface area of a parametric surface (Figure 3.6.11).

A surface S_ij that looks like a curved parallelogram.
Figure 3.6.11: The parallelogram spanned by tu and tv approximates the piece of surface Sij.
Definition: Smooth Parameterization of a Surface

Let r(u,v)=x(u,v),y(u,v),z(u,v) with parameter domain D be a smooth parameterization of surface S. Furthermore, assume that S is traced out only once as (u,v) varies over D. The surface area of S is

D||tu×tv||dA,

where tu=xu,yu,zu

and

tv=xu,yu,zu.

Example 3.6.4: Calculating Surface Area

Calculate the lateral surface area (the area of the “side,” not including the base) of the right circular cone with height h and radius r.

Solution

Before calculating the surface area of this cone using Equation ???, we need a parameterization. We assume this cone is in R3 with its vertex at the origin (Figure 3.6.12). To obtain a parameterization, let α be the angle that is swept out by starting at the positive z-axis and ending at the cone, and let k=tanα. For a height value v with 0vh, the radius of the circle formed by intersecting the cone with plane z=v is kv. Therefore, a parameterization of this cone is

s(u,v)=kvcosu,kvsinu,v,0u<2π,0vh.

The idea behind this parameterization is that for a fixed v-value, the circle swept out by letting u vary is the circle at height v and radius kv. As v increases, the parameterization sweeps out a “stack” of circles, resulting in the desired cone.

A right circular cone in three dimensions, opening upwards on the z axis.
Figure 3.6.12: The right circular cone with radius r=kh and height h has parameterization s(u,v)=kvcosu,kvsinu,v,0u<2π,0vh.

With a parameterization in hand, we can calculate the surface area of the cone using Equation ???. The tangent vectors are tu=kvsinu,kvcosu,0 and tv=kcosu,ksinu,1. Therefore,

tu×tv=|ˆiˆjˆkkvsinukvcosu0kcosuksinu1|=kvcosu,kvsinu,k2vsin2uk2vcos2u=kvcosu,kvsinu,k2v.

The magnitude of this vector is

||kvcosu,kvsinu,k2v||=k2v2cos2u+k2v2sin2u+k4v2=k2v2+k4v2=kv1+k2.

By Equation ???, the surface area of the cone is

D||tu×tv||dA=h02π0kv1+k2dudv=2πk1+k2h0vdv=2πk1+k2[v22]h0=πkh21+k2.

Since k=tanα=r/h,

πkh21+k2=πrhh21+r2h2=πrh1+r2h2=πrh2+h2(r2h2)=πrh2+r2.

Therefore, the lateral surface area of the cone is πrh2+r2.

Analysis

The surface area of a right circular cone with radius r and height h is usually given as πr2+πrh2+r2. The reason for this is that the circular base is included as part of the cone, and therefore the area of the base πr2 is added to the lateral surface area πrh2+r2 that we found.

Exercise 3.6.5

Find the surface area of the surface with parameterization r(u,v)=u+v,u2,2v,0u3,0v2.

Hint

Use Equation ???.

Answer

\≈43.02

Example 3.6.5: Calculating Surface Area

Show that the surface area of the sphere x2+y2+z2=r2 is 4πr2.

Solution

The sphere has parameterization

rcosθsinϕ,rsinθsinϕ,rcosϕ,0θ<2π,0ϕπ.

The tangent vectors are

tθ=rsinθsinϕ,rcosθsinϕ,0

and

tϕ=rcosθcosϕ,rsinθcosϕ,rsinϕ.

Therefore,

tϕ×tθ=r2cosθsin2ϕ,r2sinθsin2ϕ,r2sin2θsinϕcosϕ+r2cos2θsinϕcosϕ=r2cosθsin2ϕ,r2sinθsin2ϕ,r2sinϕcosϕ.

Now,

||tϕ×tθ||=r4sin4ϕcos2θ+r4sin4ϕsin2θ+r4sin2ϕcos2ϕ=r4sin4ϕ+r4sin2ϕcos2ϕ=r2sin2ϕ=rsinϕ.

Notice that sinϕ0 on the parameter domain because 0ϕ<π, and this justifies equation sin2ϕ=sinϕ. The surface area of the sphere is

2π0π0r2sinϕdϕdθ=r22π02dθ=4πr2.

We have derived the familiar formula for the surface area of a sphere using surface integrals.

Exercise 3.6.6

Show that the surface area of cylinder x2+y2=r2,0zh is 2πrh. Notice that this cylinder does not include the top and bottom circles.

Hint

Use the standard parameterization of a cylinder and follow the previous example.

Answer

With the standard parameterization of a cylinder, Equation ??? shows that the surface area is 2πrh.

In addition to parameterizing surfaces given by equations or standard geometric shapes such as cones and spheres, we can also parameterize surfaces of revolution. Therefore, we can calculate the surface area of a surface of revolution by using the same techniques. Let y=f(x)0 be a positive single-variable function on the domain axb and let S be the surface obtained by rotating f about the x-axis (Figure 3.6.13). Let θ be the angle of rotation. Then, S can be parameterized with parameters x and θ by

r(x,θ)=x,f(x)cosθ,f(x)sinθ,axb,0x2π.

Two diagrams, a and b, showing the surface of revolution.
Figure 3.6.13: Parametrization of a surface of revolution by r(x,θ)=x,f(x)cosθ,f(x)sinθ,axb,0x<2π.
Example 3.6.6: Calculating Surface Area

Find the area of the surface of revolution obtained by rotating y=x2,0xb about the x-axis (Figure 3.6.14).

A solid of revolution drawn in two dimensions.
Figure 3.6.14: The surface of revolution obtained by rotating y=x2,0xb about the x-axis.
Solution

This surface has parameterization r(x,θ)=x,x2cosθ,x2sinθ,0xb,0x<2π.

The tangent vectors are tx=1,2xcosθ,2xsinθ and tθ=0,x2sinθ,x2cosθ.

Therefore,

tx×tθ=2x3cos2θ+2x3sin2θ,x2cosθ,x2sinθ=2x3,x2cosθ,x2sinθ

and

tx×tθ=4x6+x4cos2θ+x4sin2θ=4x6+x4=x24x2+1

The area of the surface of revolution is

b02π0x24x2+1dθdx=2πb0x24x2+1dx=2π[164(24x2+1(8x3+x)sinh1(2x))]b0=2π[164(24b2+1(8b3+b)sinh1(2b))].

Exercise 3.6.7

Use Equation ??? to find the area of the surface of revolution obtained by rotating curve y=sinx,0xπ about the x-axis.

Hint

Use the parameterization of surfaces of revolution given before Example 3.6.7.

Answer

2π(2+sinh1(1))

Key Concepts

  • Surfaces can be parameterized, just as curves can be parameterized. In general, surfaces must be parameterized with two parameters.
  • Surfaces can sometimes be oriented, just as curves can be oriented.
  • If S is a surface, then the area of S is SdS.

Glossary

Grid curves
curves on a surface that are parallel to grid lines in a coordinate plane
Parameter domain (parameter space)
the region of the uv-plane over which the parameters u and v vary for parameterization r(u,v)=x(u,v),y(u,v),z(u,v)
Parameterized surface (parametric surface)
a surface given by a description of the form r(u,v)=x(u,v),y(u,v),z(u,v), where the parameters u and v vary over a parameter domain in the uv-plane
Regular parameterization
parameterization r(u,v)=x(u,v),y(u,v),z(u,v) such that ru×rv is not zero for point (u,v) in the parameter domain
Surface area
the area of surface S given by the surface integral SdS

Contributors and Attributions

  • Gilbert Strang (MIT) and Edwin “Jed” Herman (Harvey Mudd) with many contributing authors. This content by OpenStax is licensed with a CC-BY-SA-NC 4.0 license. Download for free at http://cnx.org.


This page titled 3.6: Surface Area is shared under a CC BY-NC-SA 4.0 license and was authored, remixed, and/or curated by Fatemeh Yarahmedi (OpenStax) via source content that was edited to the style and standards of the LibreTexts platform.

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