Mathematical methods in the physical sciences 3rd edition Mary L. Boas Chapter 5 Multiple integrals; applications of integration (다중적분 ; 적분의 응용) Lecture 16 Double & Triple integrals 1. Introduction - Use for integration : finding areas, volume, mass, moment of inertia, and so on. - Computers and integral tables are very useful in evaluating integrals. 1) To use these tools efficiently, we need to understand the notation and meaning of integrals. 2) A computer gives you an answer for a definite integral. 2. Double and triple integrals (이중, 삼중 적분) b b a a ydx f ( x)dx AREA under the curve A f ( x, y )dA f ( x, y )dxdy A VOLUME under the surface “double integral” - Iterated integrals Example 1. V z dA ( z)dxdy (1 y)dxdy A A A 2x y 1 V ( z)dxdy (1 y)dxdy (1 y)dydx A A A ‘Integration sequence does not matter.’ 22 x (a) 2 2 x 2 2 x y2 y0zdy y0(1 y)dy ( y 2 ) 0 4 6x 2x2 1 2 2 x 5 2 zdydx zdy dx ( 4 6 x 2 x ) dx A y0 x0 3 x 0 1 (b) 2 1 y / 2 1 y / 2 zdxdy ( 1 y ) dx dy x ( 1 y ) dy A y 0 x0 0 y 0 2 2 y 0 (1 y )(1 y / 2)dy 5 3 Integrate with respect to y first, A y2 ( x ) f ( x, y )dxdy f ( x, y )dy dx xa y y1 ( x ) b Integrate with respect to x first, A x2 ( y ) f ( x, y )dxdy f ( x, y )dxdy y c x x1 ( y ) d Integrate in either order, A d x2 ( y ) y2 ( x ) f ( x, y)dxdy f ( x, y)dy dx f ( x, y)dxdy xa y c y y1 ( x ) x x1 ( y ) b In case of A f ( x, y) g ( x)h( y), b d f ( x, y )dxdy g ( x)h( y )dydx g ( x)dx h( y )dy x a y c a c b d Example 2. mass=? (2,1) density f(x,y)=xy dM f ( x, y)dxdy xydxdy 2 1 M dM xydxdy xdx ydy 1 A x 0 y 0 x 0 y 0 2 (0,0) 1 Triple integral f(x,y,z) over a volume V, f ( x, y, z )dV f ( x, y, z )dxdydz V Example 3. Find V in ex. 1 by using a triple integral, 1 2 2 x y 0 z0dz dydx x0 y0(1 y)dydx 1 2 2 x 1 y dxdydz V x 0 V Example 4. Find mass in ex. 1 if density =x+z, dM ( x z)dxdydz M dM ( x z )dz dydx V x 0 y 0 z 0 1 2 2 x 2 1 y z ( xz ) dydx 2 z 0 x 0 y 0 1 2 2 x 1 y 1 22 x x(1 y) (1 y) / 2dydx 2 x 0 y 0 x 2 3 {( 3 2 x ) 1 } 1 / 6 {( 3 2 x ) 1 } x0 2 dx 2 1 3. Application of integration; single and multiple integrals (적분의 응용 ; 단일적분, 다중적분) Example 1. y=x^2 from x=0 to x=1 (a) area under the curve (b) mass, if density is xy (c) arc length (d) centroid of the area (e) centroid of the arc (f) moments of the inertia y x2 0 1 1 1 1 x3 1 2 A ydx x dx 3 0 3 x 0 x 0 (a) area under the curve (b) mass, if density of xy 1 x5 x 1 M dM xydxdy xdx ydy dx 12 A x 0 y 0 x 0 y 0 x 0 2 1 x2 1 2 (c) arc length of the curve y x2 ds2 dx2 dy2 ds dx dy 1 (dy / dx) dx 1 (dx / dy) dy 2 2 2 2 ds dy dx dy 2 x, dx ds 1 4 x 2 dx 1 s ds 1 4 x 2 dx 0 2 5 ln(2 5 ) 4 (d) centroid of the area (or arc) xdA xdA, xdA x dA xdA xdA , ydA ydA , cf. centroid : constant zdA zdA In our example, 1 x2 1 1 x2 xdA xdydx xdydx, or x 0 y 0 1 x2 x 0 y 0 1 x4 1 3 xA x 4 0 4 4 1 x2 x5 1 3 yA y 10 0 10 10 ydA ydydx ydydx, or x 0 y 0 (e) x 0 y 0 x dM xdM : centroid of mass x ds xds : centroid of arc If is constant, 1 1 2 x ds x 1 4 x dx x 1 4 x dx 2 0 0 1 1 1 2 2 y ds y 1 4 x dx y 1 4 x dx x 1 4 x dx 2 0 2 0 0 (f) moments of the inertia I l 2 dM , for dM (r )dxdydz I x ( y 2 z 2 )dM ( y 2 z 2 ) dxdydz I y ( z 2 x 2 )dM ( z 2 x 2 ) dxdydz I z ( x 2 y 2 )dM ( x 2 y 2 ) dxdydz In our example, (=xy) 1 x2 1 x2 1 x2 1 x2 1 9 x 1 I x ( y 2 z 2 ) xydydx y 2 xydydx dx , 4 40 x 0 y 0 x 0 y 0 0 1 x7 1 I y ( z x ) xydydx x xydydx dx , 2 16 x 0 y 0 x 0 y 0 0 2 1 Iz x2 2 2 2 2 ( x y ) xydydx I x I y x 0 y 0 7 80 cf . I z I x I y EX. 2 Rotate the area of Ex. 1 (y=x^2) about x-axis (a) volume (b) moment of inertia about x axis (c) area of curved surface (d) centroid of the curved volume (a) volume 1 (i) 1 V y dx x 4 dx 2 0 (ii) 0 5 V dxdydz y x 4 z 2 to y x 4 z 2 x2 z x2 1 V x2 y x 4 z 2 x 0 z x 2 y x 4 z 2 dydzdx (b) I_x (=const.) I x ( y z ) dV 2 4 2 1 z x 2 y x z 2 x 0 z x 2 y (c) area of curved surface dA 2yds 1 A 2yds x 0 1 2 2 2 x 1 4 x dx x 0 (d) centroid of surface 1 x A xdA x 2yds x 0 5 4 2 ( y z )dydzdx 18 18 M x z 2 2 Mathematical methods in the physical sciences 3rd edition Mary L. Boas Chapter 5 Multiple integrals: applications of integration Lecture 17 Change of variables in integrals 4. Change of variables in integrals: Jacobians (적분의 변수변환 ; Jacobian) In many applied problems, it is more convenient to use other coordinate systems instead of the rectangular coordinates we have been using. - polar coordinate: 1) Area x r cos y r sin dA dxdy dr rd rdrd 2) Curve ds2 dx2 dy2 dr2 (rd )2 ds ( dr 2 2 d ) r d 1 r 2 ( ) 2 dr d dr Example 1 r=a, density (a) centroid of the semicircular area cf . y 0 xd A x dA dA dxdy a /2 a rdrd rdr r 0 / 2 a r 0 /2 2 a2 a /2 a 2a 3 xdA r0 (/ r2 cos )(rdrd ) r0 r/ 2 cos drd r02r dr 3 2 x dA xdA a2 2a 3 4a x x 2 2 3 2 (b) moment of inertia about the y-axis I y ( x 2 z 2 )dM x 2 dM x 2 dxdydz x 2 dxdy x 2 rdrd a /2 r cos rdrd 2 2 r 0 / 2 M rdrd a /2 rdrd r 0 / 2 2M a 4 Ma 2 Iy 2 a 8 4 a 2 2 , a 4 8 - Cylindrical coordinate x r cos y r sin zz dV rdrddz ds2 dr2 r 2 d 2 dz2 - Spherical coordinate x r sin cos y r sin sin z r cos dV r 2 sin drdd ds2 dr 2 r 2 d 2 r 2 sin 2 d 2 Jacobians (Using the partial differentiation) x x, y ( x, y ) s J J s, t ( s, t ) y s x t y t dxdy dA J dsdt x ( x, y) r (r , ) y r x y u r (u , v, w) v J ( r , s, t ) r w r ** Prove that cos r sin u s v s w s r sin r cos u t v t w t dxdy rdrd f (u, v, w)dudvdw f (r , s, t ) J drdsdt dV r 2 sin drdd Example 2. z ? and I z ? z r=h Mass: 2 z2 h3 M dV rdrddz 2 dz 2 3 z 0 r 0 0 0 Centroid: h z h z dV zdV h z y 2 h zrdrddz x z 0 r 0 0 z2 h 4 2 z dz , 2 4 0 h z h3 3 h 4 4 z 2 z4 h5 3 I z r rdrddz 2 dz Mh2 4 10 10 z 0 r 0 0 0 h Moment of inertia: 3h 4 z h 2 Example 3. Moment of inertia of ‘solid sphere’ of radius a M dV 2 a r 2 sin drdd 0 0 r 0 a3 4 a 3 4 3 3 I ( x y )dM 2 2 2 a (r 2 sin 2 )r 2 sin drdd 0 0 r 0 a5 4 8a 5 2 5 3 15 cf . x r sin cos 2 I z Ma 2 5 y r sin sin z r cos dV r 2 sin drdd ds2 dr 2 r 2 d 2 r 2 sin 2 d 2 Example 4. I_z of the solid ellipsoid x2 y 2 z 2 2 2 1 2 a b c x ax' , y by' , z cz' , thenx'2 y'2 z'2 1 dx adx' , dy bdy' , dz cdz' M abc dx ' dy ' dz ' abc ( volume of sphere of radius 1) 4 4 M abc 13 abc 3 3 In a similar way, I ( x 2 y 2 ) dV abc (a 2 x'2 b 2 y '2 )dV ' 2 2 2 x ' dV ' y ' dV ' z ' dV ' r ' dV ' 2 1 2 1 r '2 (r '2 sin ' dr' d ' d ' ) 0 0 r 0 4 r '4 dr' 0 1 2 2 2 2 2 r ' dV ' , where r ' x ' y ' z ' 3 4 5 1 4 I abc a 2 x'2 dV ' b 2 y '2 dV ' abc (a 2 b 2 ) 3 5 I 1 M (a 2 b 2 ) 5 5. Surface integrals (?) (표면적분) dxdy dA cos , dA sec dxdy ‘projection of the surface to xy plane’ cos n k dA sec dxdy ( x, y, z ) const. normal to surface grad ( x, y, z ) i j k x y z n ( grad ) / grad nk k grad / z cos grad grad grad 1 1 sec cos n k / z ( 2 2 2 ) ( ) ( ) x y z / z For z f ( x, y ), ( x, y, z ) z f ( x, y ), so 1 z sec 1 f f ( )2 ( )2 1 cos x y Example 1. Upper surface of the sphere by the cylinder x 2 y 2 z 2 1, x 2 y 2 y 0 ( x, y, z ) const. ( x, y, z) x 2 y 2 z 2 sec grad / z 1 1 1 (2 x) 2 (2 y ) 2 (2 z ) 2 2z z 1 x2 y 2 1 y y2 y 0 x 0 2 x from 0 to y y 2 dxdy 1 x2 y 2 y from 0 to1 / 2 sin 2 r from 0 to sin from 0 /2 0 x 0 rdrd 1 r 2 /2 2 1 r 2 d 0 0 /2 /2 /2 2 ( 1 sin 1)d 2 (1 cos )d 2 2 0 0 H. W. (due 5/28) Chapter 5 2-43 3-17, 18, 19, 20 4-4