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Suppose that D is a simple region (a region which is both x-simple and y-simple) and that F = P(x,y)i + Q(x,y)j where P(x,y) and Q(x,y) are each functions with continuous first partial derivatives. y x ab a x b 1 (x) y 2 (x) y x c d c y d 1 (y) x 2 (y) We shall let C + represent the boundary of the region D traversed in the counterclockwise (positive) direction, that is, so that the region is on the left as the path is traversed. Observe that Q — dA = x D Q — dx dy = x c d 1(y)1(y) 2(y)2(y)
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y x ab a x b 1 (x) y 2 (x) y x c d c y d 1 (y) x 2 (y) Observe that Q — dA = x D Q — dx dy = x c d 1(y)1(y) 2(y)2(y) c d Q(x,y) dy = x = 1 (y) 2(y)2(y) c d Q( 2 (y), y) – Q( 1 (y), y) dy = F = P(x,y)i + Q(x,y)j
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y x ab a x b 1 (x) y 2 (x) y x c d c y d 1 (y) x 2 (y) c d Q( 2 (y), y) – Q( 1 (y), y) dy = F = P(x,y)i + Q(x,y)j c d Q( 2 (t), t) dt –Q( 1 (t), t) dt = c d
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y x ab a x b 1 (x) y 2 (x) y x c d c y d 1 (y) x 2 (y) F = P(x,y)i + Q(x,y)j c d Q( 2 (t), t) dt –Q( 1 (t), t) dt = c d c d (Q( 2 (t), t)j) ( 2 (t), 1) dt –(Q( 1 (t), t)j) ( 1 (t), 1) dt = c d Note that this line integral is over the right half of C in the counterclockwise direction. Note that this line integral is over the left half of C in the clockwise direction.
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y x ab a x b 1 (x) y 2 (x) y x c d c y d 1 (y) x 2 (y) F = P(x,y)i + Q(x,y)j c Q( 2 (t), t) dt –Q( 1 (t), t) dt = c c d (Q( 2 (t), t)j) ( 2 (t), 1) dt –(Q( 1 (t), t)j) ( 1 (t), 1) dt = c d C+C+ Q(x,y)j ds dd
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y x ab a x b 1 (x) y 2 (x) y x c d c y d 1 (y) x 2 (y) F = P(x,y)i + Q(x,y)j We see then that Q — dA = x DC+C+ Q(x,y)j ds. Similarly, we find P — dA = y DC+C+ – P(x,y)i ds.
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y x ab a x b 1 (x) y 2 (x) y x c d c y d 1 (y) x 2 (y) F = P(x,y)i + Q(x,y)j Q P — – — dA = x y DC+C+ (P(x,y)i + Q(x,y)j) ds = Q — dA – x D P — dA = y DC+C+ Q(x,y)j ds + C+C+ P(x,y)i ds. C+C+ F ds.
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y x ab a x b 1 (x) y 2 (x) y x c d c y d 1 (y) x 2 (y) F = P(x,y)i + Q(x,y)j This proves Green’s Theorem (Theorem 1 on page 522) which can be stated as follows: Q P — – — dA = x y DC+C+ F ds = Note: Green’s Theorem can be extended to a region which is not a simple region but can be partitioned into several simple regions. C+C+ P dx + Q dy. Note that this is what we have called the scalar curl of F
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ExampleLet F(x,y) = yi – xj and let C represent the circle of radius a centered at the origin and traversed counterclockwise. C F ds(a) Findusing the definition of a line integral. First, we parametrize C with (a cos t, a sin t) for 0 t 2 . C F ds = 2 0 F(c(t)) c (t) dt = 22 0 (a sin t, – a cos t) (– a sin t, a cos t ) dt = – 2 a 2
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C F ds (b) Find by using Green’s Theorem to write the line integral as a double integral, and evaluating this double integral. Since F(x,y) = yi – xj, then we let P(x,y) = and Q(x,y) = From Green’s Theorem, we have y– x– x C F ds = Q P — – — dx dy = x y D where D is the disk of radius a centered at the origin (– 1 – 1) dx dy = D – 2 dx dy = D D – 2(area of D) = – 2 a 2
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By applying Green’s Theorem with the vector field F = P(x,y)i + Q(x,y)j with P(x,y) = – y /2 and Q(x,y) = x / 2, we can find the area of a region D in R 2 (as stated in Theorem 2 on page 524), because Q P — – — dA = x y D dx dy = D 1 1 — + — dA = 2 2 D (area of D). In other words, we have that (area of D) = C F ds where C is the boundary of D traversed in the counterclockwise direction, and F = (– y /2)i + (x / 2)j
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ExampleConsider the area in the xy plane inside the graph of x 2/3 + y 2/3 = a 2/3 (where a > 0 is a known constant). (a) Sketch a graph of this area. x y (0, a) (0, – a) (– a, 0) (a, 0)
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(b) Write a double integral using rectangular coordinates to obtain the area, and write a double integral using polar coordinates to obtain the area. Observe how difficult evaluating each of these integrals will be. – a a (a 2/3 – x 2/3 ) 3/2 dy dx – (a 2/3 – x 2/3 ) 3/2 0 22 a / (cos 2/3 + sin 2/3 ) 3/2 r dr d 0
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(c) Use Green’s Theorem to obtain the area. First, we parametrize the curve which is the boundary of D by Then, by letting F = (– y /2)i + (x / 2)j, the area bounded by the curve is C( ) = ( a cos 3 , a sin 3 ) for 0 2 C F ds = 22 0 (– a sin 3 , a cos 3 ) 1 — 2 (– 3a cos 2 sin , 3a sin 2 cos ) d = 22 0 – (a sin 3 )(– 3a cos 2 sin ) + (a cos 3 )(3a sin 2 cos ) d = 1 — 2
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22 0 sin 4 cos 2 + sin 2 cos 4 d = 3 —a 2 2 22 0 sin 2 cos 2 d = 3 —a 2 2 22 0 sin 2 2 ——— d = 4 3 —a 2 2 22 0 1 – cos4 ———— d = 8 3 —a 2 2 22 0 – (1/4)sin4 —————— = 8 3 —a 2 2 3 —a 2 2 2 —= 8 3 — a 2 8 Recall the half-angle and double-angle formulas which give us the following trig identities: 1 sin cos =— sin(2 ) 2 1 sin 2 = — (1 – cos(2 )) 2
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y x Suppose that D is a simple region (a region which is both x-simple and y-simple) and that the closed path along the border of D in the counterclockwise direction, sometimes denoted as D, is parametrized by c(t) = (x(t), y(t)). Note: If (a, b) is a non-zero vector in R 2, then any vector which is orthogonal to, and to the right of, (a, b) must be a positive multiple of y x (a, b) (, )– ab (b, – a). At any point along the path, an “outward” normal vector must be one which is orthogonal to the velocity vector c / (t) = (x / (t), y / (t)). That is, an “outward” normal vector must be one which is a positive multiple of (x / (t), y / (t)) (y / (t), – x / (t)) (y / (t), – x / (t)). D
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Suppose F = P(x,y)i + Q(x,y)j is a vector field defined on D. Recall Green’s Theorem (Theorem 1 on page 522): Q P — – — dA = x y D DD F ds Define the vector field V = – Q(x,y)i + P(x,y)j on D, and observe that V c / (t) = V (x / (t), y / (t)) = Applying Green’s Theorem with the vector field V, we have – Q(x,y) x / (t) + P(x,y) y / (t) = F (y / (t), – x / (t)) P Q — + — dA = x y D DD V ds div(F) DD = F n ds where n is understood to be the outward normal to D This proves the Divergence Theorem in the Plane (Theorem 4, page 527)
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