VECTOR CALCULUS 17. 2 17.8 Stokes’ Theorem In this section, we will learn about: The Stokes’ Theorem and using it to evaluate integrals. VECTOR CALCULUS.

Slides:



Advertisements
Similar presentations
Section 18.4 Path-Dependent Vector Fields and Green’s Theorem.
Advertisements

Stoke's theorem. Topics of discussion History Definition of Stoke’s Theorem Mathematical expression Proof of theorem Physical significance Practical applications.
Teorema Stokes Pertemuan
Vector Analysis Copyright © Cengage Learning. All rights reserved.
Chapter 13-Vector Calculus Calculus, 2ed, by Blank & Krantz, Copyright 2011 by John Wiley & Sons, Inc, All Rights Reserved.
PARTIAL DERIVATIVES 14. PARTIAL DERIVATIVES 14.6 Directional Derivatives and the Gradient Vector In this section, we will learn how to find: The rate.
INFINITE SEQUENCES AND SERIES
MULTIPLE INTEGRALS MULTIPLE INTEGRALS 16.4 Double Integrals in Polar Coordinates In this section, we will learn: How to express double integrals.
MULTIPLE INTEGRALS MULTIPLE INTEGRALS Recall that it is usually difficult to evaluate single integrals directly from the definition of an integral.
17 VECTOR CALCULUS.
17 VECTOR CALCULUS.
VECTOR CALCULUS Fundamental Theorem for Line Integrals In this section, we will learn about: The Fundamental Theorem for line integrals and.
VECTOR CALCULUS VECTOR CALCULUS Here, we define two operations that:  Can be performed on vector fields.  Play a basic role in the applications.
16 MULTIPLE INTEGRALS.
MULTIPLE INTEGRALS MULTIPLE INTEGRALS 16.9 Change of Variables in Multiple Integrals In this section, we will learn about: The change of variables.
VECTOR CALCULUS The Divergence Theorem In this section, we will learn about: The Divergence Theorem for simple solid regions, and its applications.
MULTIPLE INTEGRALS Double Integrals over General Regions MULTIPLE INTEGRALS In this section, we will learn: How to use double integrals to.
17 VECTOR CALCULUS.
Stokes’ Theorem Divergence Theorem
Chapter 16 – Vector Calculus 16.5 Curl and Divergence 1 Objectives:  Understand the operations of curl and divergence  Use curl and divergence to obtain.
Chapter 16 – Vector Calculus
Multiple Integrals 12. Surface Area Surface Area In this section we apply double integrals to the problem of computing the area of a surface.
Copyright © Cengage Learning. All rights reserved. 16 Vector Calculus.
VECTOR FUNCTIONS 13. VECTOR FUNCTIONS Later in this chapter, we are going to use vector functions to describe the motion of planets and other objects.
DEPARTMENT OF MATHEMATI CS [ YEAR OF ESTABLISHMENT – 1997 ] DEPARTMENT OF MATHEMATICS, CVRCE.
Ch. 10 Vector Integral Calculus.
Multiple Integrals 12. Double Integrals over General Regions 12.3.
Copyright © Cengage Learning. All rights reserved Double Integrals over General Regions.
DOUBLE INTEGRALS OVER GENERAL REGIONS
Copyright © Cengage Learning. All rights reserved. 16 Vector Calculus.
Vector Analysis Copyright © Cengage Learning. All rights reserved.
Vector Analysis 15 Copyright © Cengage Learning. All rights reserved.
Vector Calculus CHAPTER 9.5 ~ 9.9. Ch9.5~9.9_2 Contents  9.5 Directional Derivatives 9.5 Directional Derivatives  9.6 Tangent Planes and Normal Lines.
DOUBLE INTEGRALS IN POLAR COORDINATES
Teorema Stokes. STOKES’ VS. GREEN’S THEOREM Stokes’ Theorem can be regarded as a higher-dimensional version of Green’s Theorem. – Green’s Theorem relates.
16 VECTOR CALCULUS.
Copyright © Cengage Learning. All rights reserved.
Vector Calculus 13. The Fundamental Theorem for Line Integrals 13.3.
SECTION 13.8 STOKES ’ THEOREM. P2P213.8 STOKES ’ VS. GREEN ’ S THEOREM  Stokes ’ Theorem can be regarded as a higher- dimensional version of Green ’
Vector Calculus CHAPTER 9.10~9.17. Ch9.10~9.17_2 Contents  9.10 Double Integrals 9.10 Double Integrals  9.11 Double Integrals in Polar Coordinates 9.11.
In section 11.9, we were able to find power series representations for a certain restricted class of functions. Here, we investigate more general problems.
Copyright © Cengage Learning. All rights reserved. Vector Analysis.
ME 2304: 3D Geometry & Vector Calculus
SECTION 12.8 CHANGE OF VARIABLES IN MULTIPLE INTEGRALS.
Copyright © Cengage Learning. All rights reserved. 16 Vector Calculus.
Chapter 16 – Vector Calculus
SECTION 12.5 TRIPLE INTEGRALS.
DOUBLE INTEGRALS OVER RECTANGLES
In Chapters 6 and 8, we will see how to use the integral to solve problems concerning:  Volumes  Lengths of curves  Population predictions  Cardiac.
Copyright © Cengage Learning. All rights reserved.
Copyright © Cengage Learning. All rights reserved. 16 Vector Calculus.
Copyright © Cengage Learning. All rights reserved.
Section 17.8 Stokes’ Theorem. DEFINITION The orientation of a surface S induces the positive orientation of the boundary curve C as shown in the diagram.
Operators in scalar and vector fields
CHAPTER 9.10~9.17 Vector Calculus.
1 Line Integrals In this section we are now going to introduce a new kind of integral. However, before we do that it is important to note that you will.
Electric Flux Density, Gauss’s Law, and Divergence
Curl and Divergence.
13 VECTOR CALCULUS.
17 VECTOR CALCULUS.
Copyright © Cengage Learning. All rights reserved.
Copyright © Cengage Learning. All rights reserved.
Copyright © Cengage Learning. All rights reserved.
13 VECTOR CALCULUS.
Copyright © Cengage Learning. All rights reserved.
16.2: Line Integrals 16.3: The Fundamental Theorem for Line Integrals
Presentation transcript:

VECTOR CALCULUS 17

Stokes’ Theorem In this section, we will learn about: The Stokes’ Theorem and using it to evaluate integrals. VECTOR CALCULUS

3 STOKES’ VS. GREEN’S THEOREM Stokes’ Theorem can be regarded as a higher-dimensional version of Green’s Theorem.  Green’s Theorem relates a double integral over a plane region D to a line integral around its plane boundary curve.  Stokes’ Theorem relates a surface integral over a surface S to a line integral around the boundary curve of S (a space curve).

4 INTRODUCTION The figure shows an oriented surface with unit normal vector n.  The orientation of S induces the positive orientation of the boundary curve C. Fig , p. 1129

5 INTRODUCTION This means that:  If you walk in the positive direction around C with your head pointing in the direction of n, the surface will always be on your left. Fig , p. 1129

6 STOKES’ THEOREM Let:  S be an oriented piecewise-smooth surface bounded by a simple, closed, piecewise-smooth boundary curve C with positive orientation.  F be a vector field whose components have continuous partial derivatives on an open region in that contains S. Then,

7 STOKES’ THEOREM The theorem is named after the Irish mathematical physicist Sir George Stokes (1819–1903).  What we call Stokes’ Theorem was actually discovered by the Scottish physicist Sir William Thomson (1824–1907, known as Lord Kelvin).  Stokes learned of it in a letter from Thomson in 1850.

8 STOKES’ THEOREM Thus, Stokes’ Theorem says:  The line integral around the boundary curve of S of the tangential component of F is equal to the surface integral of the normal component of the curl of F.

9 STOKES’ THEOREM The positively oriented boundary curve of the oriented surface S is often written as ∂S. So, the theorem can be expressed as: Equation 1

10 STOKES’ THEOREM, GREEN’S THEOREM, & FTC There is an analogy among Stokes’ Theorem, Green’s Theorem, and the Fundamental Theorem of Calculus (FTC).  As before, there is an integral involving derivatives on the left side of Equation 1 (recall that curl F is a sort of derivative of F).  The right side involves the values of F only on the boundary of S.

11 STOKES’ THEOREM, GREEN’S THEOREM, & FTC In fact, consider the special case where the surface S:  Is flat.  Lies in the xy-plane with upward orientation.

12 STOKES’ THEOREM, GREEN’S THEOREM, & FTC Then,  The unit normal is k.  The surface integral becomes a double integral.  Stokes’ Theorem becomes:

13 STOKES’ THEOREM, GREEN’S THEOREM, & FTC This is precisely the vector form of Green’s Theorem given in Equation 12 in Section 17.5  Thus, we see that Green’s Theorem is really a special case of Stokes’ Theorem.

14 STOKES’ THEOREM Stokes’ Theorem is too difficult for us to prove in its full generality. Still, we can give a proof when:  S is a graph.  F, S, and C are well behaved.

15 STOKES’ TH.—SPECIAL CASE We assume that the equation of S is: z = g(x, y), (x, y) D where:  g has continuous second-order partial derivatives.  D is a simple plane region whose boundary curve C 1 corresponds to C. Proof

16 If the orientation of S is upward, the positive orientation of C corresponds to the positive orientation of C 1. Proof STOKES’ TH.—SPECIAL CASE Fig , p. 1129

17 STOKES’ TH.—SPECIAL CASE We are also given that: F = P i + Q j + R k where the partial derivatives of P, Q, and R are continuous. Proof

18 STOKES’ TH.—SPECIAL CASE S is a graph of a function. Thus, we can apply Formula 10 in Section 17.7 with F replaced by curl F. Proof

19 STOKES’ TH.—SPECIAL CASE The result is: where the partial derivatives of P, Q, and R are evaluated at (x, y, g(x, y)). Proof—Equation 2

20 STOKES’ TH.—SPECIAL CASE Suppose x = x(t) y = y(t) a ≤ t ≤ b is a parametric representation of C 1.  Then, a parametric representation of C is: x = x(t) y = y(t) z = g(x(t), y(t)) a ≤ t ≤ b Proof

21 STOKES’ TH.—SPECIAL CASE This allows us, with the aid of the Chain Rule, to evaluate the line integral as follows: Proof

22 STOKES’ TH.—SPECIAL CASE  We have used Green’s Theorem in the last step. Proof

23 STOKES’ TH.—SPECIAL CASE Next, we use the Chain Rule again, remembering that:  P, Q, and R are functions of x, y, and z.  z is itself a function of x and y. Proof

24 STOKES’ TH.—SPECIAL CASE Thus, we get: Proof

25 STOKES’ TH.—SPECIAL CASE Four terms in that double integral cancel. The remaining six can be arranged to coincide with the right side of Equation 2.  Hence, Proof

26 STOKES’ THEOREM Evaluate where:  F(x, y, z) = –y 2 i + x j + z 2 k  C is the curve of intersection of the plane y + z = 2 and the cylinder x 2 + y 2 = 1. (Orient C to be counterclockwise when viewed from above.) Example 1

27 STOKES’ THEOREM The curve C (an ellipse) is shown here.  could be evaluated directly.  However, it’s easier to use Stokes’ Theorem. Example 1 Fig , p. 1131

28 STOKES’ THEOREM We first compute: Example 1

29 STOKES’ THEOREM There are many surfaces with boundary C.  The most convenient choice, though, is the elliptical region S in the plane y + z = 2 that is bounded by C.  If we orient S upward, C has the induced positive orientation. Example 1 Fig , p. 1131

30 STOKES’ THEOREM The projection D of S on the xy-plane is the disk x 2 + y 2 ≤ 1.  So, using Equation 10 in Section 17.7 with z = g(x, y) = 2 – y, we have the following result. Example 1 Fig , p. 1131

31 STOKES’ THEOREM Example 1

32 STOKES’ THEOREM Use Stokes’ Theorem to compute where:  F(x, y, z) = xz i + yz j + xy k  S is the part of the sphere x 2 + y 2 + z 2 = 4 that lies inside the cylinder x 2 + y 2 =1 and above the xy-plane. Example 2 Fig , p. 1131

33 STOKES’ THEOREM To find the boundary curve C, we solve: x 2 + y 2 + z 2 = 4 and x 2 + y 2 = 1  Subtracting, we get z 2 = 3.  So, (since z > 0). Example 2 Fig , p. 1131

34 STOKES’ THEOREM So, C is the circle given by: x 2 + y 2 = 1, Example 2 Fig , p. 1131

35 STOKES’ THEOREM A vector equation of C is: r(t) = cos t i + sin t j + k 0 ≤ t ≤ 2π  Therefore, r’(t) = –sin t i + cos t j Also, we have: Example 2

36 STOKES’ THEOREM Thus, by Stokes’ Theorem, Example 2

37 STOKES’ THEOREM Note that, in Example 2, we computed a surface integral simply by knowing the values of F on the boundary curve C. This means that:  If we have another oriented surface with the same boundary curve C, we get exactly the same value for the surface integral!

38 STOKES’ THEOREM In general, if S 1 and S 2 are oriented surfaces with the same oriented boundary curve C and both satisfy the hypotheses of Stokes’ Theorem, then  This fact is useful when it is difficult to integrate over one surface but easy to integrate over the other. Equation 3

39 CURL VECTOR We now use Stokes’ Theorem to throw some light on the meaning of the curl vector.  Suppose that C is an oriented closed curve and v represents the velocity field in fluid flow.

40 CURL VECTOR Consider the line integral and recall that v ∙ T is the component of v in the direction of the unit tangent vector T.  This means that the closer the direction of v is to the direction of T, the larger the value of v ∙ T.

41 CIRCULATION Thus, is a measure of the tendency of the fluid to move around C.  It is called the circulation of v around C. Fig , p. 1132

42 CURL VECTOR Now, let: P 0 (x 0, y 0, z 0 ) be a point in the fluid. S a be a small disk with radius a and center P 0.  Then, (curl F)(P) ≈ (curl F)(P 0 ) for all points P on S a because curl F is continuous.

43 CURL VECTOR Thus, by Stokes’ Theorem, we get the following approximation to the circulation around the boundary circle C a :

44 CURL VECTOR The approximation becomes better as a → 0. Thus, we have: Equation 4

45 CURL & CIRCULATION Equation 4 gives the relationship between the curl and the circulation.  It shows that curl v ∙ n is a measure of the rotating effect of the fluid about the axis n.  The curling effect is greatest about the axis parallel to curl v.

46 CURL & CIRCULATION Imagine a tiny paddle wheel placed in the fluid at a point P.  The paddle wheel rotates fastest when its axis is parallel to curl v. Fig , p. 1132

47 CLOSED CURVES Finally, we mention that Stokes’ Theorem can be used to prove Theorem 4 in Section 16.5:  If curl F = 0 on all of, then F is conservative.

48 CLOSED CURVES From Theorems 3 and 4 in Section 17.3, we know that F is conservative if for every closed path C.  Given C, suppose we can find an orientable surface S whose boundary is C.  This can be done, but the proof requires advanced techniques.

49 CLOSED CURVES Then, Stokes’ Theorem gives:  A curve that is not simple can be broken into a number of simple curves.  The integrals around these curves are all 0.

50 CLOSED CURVES Adding these integrals, we obtain: for any closed curve C.