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Math 240

Scalar integrals Surface area Vector integrals

Changing Surface Integrals orientation

Math 240 — III

Summer 2013, Session II

Wednesday, July 3, 2013 Surface Integrals Agenda

Math 240

Scalar integrals Surface area Vector integrals

Changing 1. Scalar surface integrals orientation Surface area

2. Vector surface integrals

3. Changing orientation P1: OSO coll50424˙ch07 PEAR591-Colley July 29, 2011 13:58

464 Chapter 7 Surface Integrals and Vector Analysis

3 the cube’s faces by Xi :[0, 1] × [0, 1] → R , i = 1,...,6, where

X1(s, t) = (0, s, t); X2(s, t) = (1, s, t); X3(s, t) = (s, 0, t);

X4(s, t) = (s, 1, t); X5(s, t) = (s, t, 0); X6(s, t) = (s, t, 1). 1 Each map Xi is clearly of class C and one-one. In addition, the faces have well-defined nonzero vectors. For example, for both X1 and X2,

N1 = N2 = Ts × Tt = j × k = i. Similarly,

N3 = N4 = i × k =−j and N5 = N6 = i × j = k. None of these vectors vanishes. There is no consistent way to define normal vectors along the edges of the cube (where two faces meet). That is why the cube is only piecewise smooth. ◆

Area of a Smooth Parametrized Surface Now, we use the notion of a parametrized surface to calculate the surface area of a = Surface smooth surface. In the discussion that follows, we take S X(D) to be a smooth Integrals parametrized surface, where D is the union ofScalar finitely many surface elementary regions integrals in R2 and X: D → R3 is of class C1 and one-one except possibly along ∂ D. Math 240 t z Scalar integrals S = X(D) Surface area Δt X Vector Δs X s t integrals ( 0, 0) (s , t ) T Changing 0 0 t T orientation s s y

x DefinitionFigure 7.13 The image of the s × t rectangle in D is approximately a parallelogram spanned by Ts (s0, t0)s and Tt (s0, t0)t. 2 3 Let X : DThe keyR geometricR observationbe a smooth is as follows: parameterized Consider a small rectangular surface. Let ⊆ → , ∈ f be asubset continuous of D whose lower scalar left corner is at the whose point (s0 domaint0) D and includes whose width and height are s and t, respectively. The image of this rectangle under X is a S = Xpiece(D of). the The underlyingscalar surface surfaceS that is approximately of thef parallelogramalong X withis a corner at X(s0, t0) and spanned by the vectors Ts(s0, t0)s and Tt (s0, t0)t. (See ZZ  ZZ Figure 7.13.) Thef dS area= A of thisf piece(X( iss, t)) T T ds dt  ≈ ,  × ,  = , s × t,   . A X Ts(s0 t0) s TDt (s0 t0) t Ts(ks0 t0) ×Tt (s0 kt0) s t Now, suppose D = [aZZ, b] × [c, d]; that is, suppose D itself is a rectangle. Partition D into n2 subrectangles= f via(X(s, t)) N(s, t) ds dt. D k k a = s0 < s1 < ···< sn = b and c = t0 < t1 < ···< tn = d.

Let si = si − si−1 and t j = t j − t j−1 for i, j = 1,...,n. Then S is in turn partitioned into pieces, each of which is approximately a parallelogram, assuming si and t j are small for i, j = 1,...,n.IfAij denotes the area of the piece P1: OSO coll50424˙ch07 PEAR591-Colley July 29, 2011 13:58 Surface Integrals Scalar surface integrals

Math 240 472 Chapter 7 Surface Integrals and Vector Analysis

Scalar z To define and evaluate scalar surface integrals over piecewise smooth para- Example S : z = 15 integrals 3 metrized surfaces, simply calculate the surface integral over each smooth piece Surface area Let S be the closed cylinder of radius 3 with and add the results. Vector EXAMPLE 2 Let S be the closed cylinder of radius 3 with axis along the z-axis, integrals axis along the z-axis, top face at z = 15, and top face at z = 15, and bottom face at z = 0, as shown in Figure 7.15. Then S S x2 + y2 = 1: 9 is a piecewise smooth surface; it is the union of the three smooth parametrized Changing bottom face at z = 0. Let’s calculate RR z dS.  orientation S surfaces S1, S2, and S3 described next. We calculate S zdS. The three smooth pieces may be parametrized as follows: Denote the lateral cylindrical face of S by S1 ⎧ y ⎨x = 3 cos s S : z = 0 = ≤ ≤ π ≤ ≤ and the bottom and top faces by S2 and S3, x 2 S1 (lateral cylindrical surface): ⎩y 3 sin s 0 s 2 ,0 t 15, z = t respectively. Figure 7.15 The closed ⎧ cylinder of radius 3 and ⎨x = s cos t height 15 of Example 2. = ≤ ≤ ≤ ≤ π We compute S2 (bottom disk): ⎩y s sin t 0 s 3, 0 t 2 , z = 0

ZZ ZZ ZZ and z dS = 675π, z dS = 0, and z dS = 135π. ⎧ S S S ⎨x = s cos t 1 2 3 = ≤ ≤ ≤ ≤ π S3 (top disk): ⎩y s sin t 0 s 3, 0 t 2 . Therefore, z = 15 Using Definition 2.1, we have    ZZ ZZ ZZ ZZ 15 2π z dS = z dS + z dS + z dS = 810π. zdS= t (−3 sin s i + 3 cos s j) × k ds dt S1 0 0   S S1 S2 S3 15 2π = t 3 sin s j + 3 cos s i ds dt 0 0    15 2π 15  = = π = π 215 = π. 3tdsdt 6 tdt 3 t 0 675  0 0 0 Now, zdS= 0, since z vanishes along the bottom of S.ForS3,wehave S2    zdS= 15 dS = 15 · 1 dS S3 S3 S3 = 15 · area of disk = 15 · (9π) = 135π. Therefore,     zdS= zdS+ zdS+ zdS S S1 S2 S3 ◆ = 675π + 0 + 135π = 810π.

If a surface S is given by the graph of z = g(x, y), where g is of class C1 on some region D in R2, then S is parametrized by X(x, y) = (x, y, g(x, y)) with (x, y) ∈ D. (See Example 4 of 7.1.) Then, from Example 13 in 7.1, § § N(x, y) =−gx i − gy j + k, so that    = , , , 2 + 2 + . fdS f (x y g(x y)) gx gy 1 dx dy (4) X D P1: OSO coll50424˙ch07 PEAR591-Colley July 29, 2011 13:58

464 Chapter 7 Surface Integrals and Vector Analysis

3 the cube’s faces by Xi :[0, 1] × [0, 1] → R , i = 1,...,6, where

X1(s, t) = (0, s, t); X2(s, t) = (1, s, t); X3(s, t) = (s, 0, t);

X4(s, t) = (s, 1, t); X5(s, t) = (s, t, 0); X6(s, t) = (s, t, 1). 1 Each map Xi is clearly of class C and one-one. In addition, the faces have well-defined nonzero normal vectors. For example, for both X1 and X2,

N1 = N2 = Ts × Tt = j × k = i. Similarly,

N3 = N4 = i × k =−j and N5 = N6 = i × j = k. None of these vectors vanishes. There is no consistent way to define normal vectors along the edges of the cube (where two faces meet). That is why the cube is only piecewise smooth. ◆ Surface Integrals Area of a Smooth Parametrized Surface Surface area Math 240 Now, we use the notion of a parametrized surface to calculate the surface area of a smooth surface. In the discussion that follows, we take S = X(D) to be a smooth parametrized surface, where D is the union of finitely many elementary regions Scalar in R2 and X: D → R3 is of class C1 and one-one except possibly along ∂ D. integrals t z Surface area Vector S = X(D) integrals Δt X Figure: The quantity Δs Changing X s t ( 0, 0) Ts Tt is the orientation s t T ( 0, 0) t k × k T area of the gray s s y square on the right.

x

Figure 7.13 The image of the s × t rectangle in D is approximately a parallelogram spanned by Ts (s0, t0)s and Tt (s0, t0)t. FactThe key geometric observation is as follows: Consider a small rectangular subset of D whose lower left corner is at the point (s0, t0) ∈ D and whose width 2 3 andIf heightS is are as smoothand t, respectively. surface The image parameterized of this rectangle under byX isX a : D R R piecethen of the the underlying surface surface S areathat is approximately of S is given the parallelogram by with a ⊆ → corner at X(s0, t0) and spanned by the vectors Ts(s0, t0)s and Tt (s0, t0)t. (See Figure 7.13.)ZZ The area A of this piece is ZZ ZZ A ≈ Ts(s0, t0)s × Tt (s0, t0)t = Ts(s0, t0) × Tt (s0, t0) st. N ds dt = Ts Tt ds dt = 1 dS. Now, suppose Dk= [ak, b] × [c, d]; that is, supposek D itself× is a rectangle.k Partition D into nD2 subrectangles via D X

a = s0 < s1 < ···< sn = b and c = t0 < t1 < ···< tn = d.

Let si = si − si−1 and t j = t j − t j−1 for i, j = 1,...,n. Then S is in turn partitioned into pieces, each of which is approximately a parallelogram, assuming si and t j are small for i, j = 1,...,n.IfAij denotes the area of the piece Surface Integrals Surface area

Math 240

Scalar integrals Example Surface area Recall our parameterization of a : Vector integrals X(s, t) = r(cos s)(sin t) i + r(sin s)(sin t) j + r(cos t) k. Changing orientation We calculate

Ts = r sin s sin t i + r cos s sin t j, − Tt = r cos s cos t i + r sin s cos t j r sin t k, − N = r2 cos s sin2 t i r2 sin s sin2 t j r2 sin t cos t k, − − − and N = r2 sin t. k k Therefore, the surface area of the sphere is Z π Z 2π Z π r2 sin t ds dt = 2πr2 sin t dt = 4πr2. 0 0 0 Surface Integrals Vector surface integrals

Math 240

Scalar integrals Surface area Vector Definition integrals 2 3 Let X : D R R be a smooth parameterized surface. Let Changing ⊆ → orientation F be a continuous vector field whose domain includes S = X(D). The vector surface integral of F along X is ZZ ZZ F dS = F(X(s, t)) N(s, t) ds dt. X · D ·

In physical terms, we can interpret F as the flow of some kind of fluid. Then the vector surface integral measures the volume of fluid that flows through S per unit time. This is called the flux of F across S. P1: OSO coll50424˙ch07 PEAR591-Colley July 29, 2011 13:58

478 Chapter 7 Surface Integrals and Vector Analysis

The parametrized surface Y is the same as X, except that the standard nor- mal vector arising from Y points in the opposite direction to the one arising from X. ◆

The calculation in Example 7 generalizes thus: Suppose X is a smooth parametrized surface and Y is a smooth reparametrization of X via H, mean- ing that Y(s, t) = X(u,v) = X(H(s, t)). Since H is assumed to be of class C1, we can show from the that the standard normal vectors are related by the equation ∂(u,v) N (s, t) = N (u,v). (11) Y ∂(s, t) X (See the addendum at the end of this section for a derivation of formula (11).) Formula (11) shows that NY is a scalar multiple of NX. In addition, since H is invertible and both H and H−1 are of class C1, it follows that the Jacobian of H is either always positive or always negative. (To see this, note that both H ◦ H−1 and H−1 ◦ H are the identity function. Hence, the chain rule may be applied to show that the matrix DH(s, t) is invertible for each (s, t); therefore, its , which is the Jacobian of H, must be nonzero. Since the determinant is a of the entries of H, it thus cannot change sign.) Hence, the standard normal N either always points in the same direction as N or else Surface Y X Integrals always points in the opposite direction (Figure 7.20). Under these assumptions,Changing we orientation say that both H and Y are orientation-preserving if the Jacobian ∂(u,v)/∂(s, t) Math 240 is positive, orientation-reversing if ∂(u,v)/∂(s, t)isnegative. v D Scalar 1 integrals Surface area NX Vector u X Figure: X and Y integrals parameterize the Changing t same surface with orientation D 2 opposite normal N S = X(D ) = Y(D ) Y 1 2 directions. Y s

Figure 7.20 If Y is an orientation-reversing reparametrization of X, then NY points opposite to NX. ZZ ZZ The following result, a close analogue of Theoremf dS 1.4,= Chapter 6,f shows dS that Y X smooth reparametrization has no effectZZ on the value of a scalarZZ . 3 THEOREM 2.4 Let X: D1 → R be a smoothF parametrizeddS = surface andF fdanyS → 3 continuous function whose domain includesY X(·D1). If Y: D−2 R Xis any smooth· reparametrization of X, then This can be achieved by exchanging s and t: fdS= fdS. Y X Tt Ts = (Ts Tt) . × − ×