INTEGRAL CALCULUS DIFFERENTIATION UNDER THE INTEGRAL SIGN: Consider an integral involving one parameter and denote it as

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INTEGRAL CALCULUS DIFFERENTIATION UNDER THE INTEGRAL SIGN: Consider an integral involving one parameter and denote it as, where a and b may be constants or functions of. To find the derivative of when it exists it is not possible to first evaluate this integral and then to find the derivative, such problems are solved by using the following rules. (A) Leibnitz s Rule for Constant limits of Integration: (B) Let,, be continuous functions of x and then,,, where a, b are constants and independent of parameter Leibnitz s Rule for Variable Limits of Integration: If in the integral,, satisfies the same conditions, and are functions of the parameter, then,,,, *********************************************************** ** Example 1: Evaluate by using differentiation under integral sign. Solution: Let and hence show that Differentiate w.r.t by Leibnitz s Rule under integral sign. sin sin then.. 1,

2 2 0 ***************************************************** Example 2: using differentiation under the integral sign, evaluate, 0 Solution: Let.. 1 Integrating both sides w.r.t log1.. 2 From 1 when 0 0 0 From 2 when I0log 1C 0 The solution is ***************************************************** Example 3: Evaluate under integral sign. Solution: Let I using the method of differentiation Differentiate w.r.t a by Leibnitz s rule under integral sign Let Solving, 0, 1 1 1 1. 1 1 1 by partial fractions, 0, Integrating w.r.t Then C 0 by putting 0 1 1 1 log 1 C 2 1

***************************************************** Example 4: Evaluate 1 using the method of differentiation under integral sign **************************************************************** Reduction formulae f ormulae: I II III Sin θ d θ cos θ d sin θcos θ And to evaluate I II sin θ d / cos θ d III sin θcos θ d ( a) sin n x dx n 1 sin x.sin x dx sin n 1 x.( cos x) With x ( n 1)sin n 2 x.cos x( cos x) dx sin n 1 sin n 1 x.cos x + ( n 1) x.cos x + ( n 1) sin n 2 sin n 2 x.(1 sin 2 x) dx xdx ( n 1) sin n x dx n sin n x dx sin n 1 x.cos x + ( n 1) sin n 2 x dx Or sin n sin x dx n 1 x.cos x n 1 + n n sin n 2 x dx... (1) n 1 Similarly, (b) n sin x.cos x n 1 cos x dx + cos n n Thus (1) and (2) are the required reduction formulae n 2 x dx... (2)

TO Evaluate Then etc i) ii) ( put x a sinθ, so that dx a cosθ dθ θ Also when x 0, θ 0, when x a, θ π/2)

iii) Evaluate π/2) ( put x a tan θ, so that dx a sec 2 θ dθ Also when x 0, θ 0, when x, θ / cos θ dθ..... iv) Evaluate sin x cos x dx sin x sinx cosx dx dx sin 2x sin 2x cos2x dx dx sin 2x cos2x. 2dx dx cos 4x dx dx / v) Evaluate cos θ sin 6θ d / cos θ 2sin3θcos3θ d / sin θ cos 3θ d / sin x cos x d...... x (Put 3 x ; so that 3d dx. Also when 0, x 0 When /6, x /2 vi) Evaluate 1 / / / /

..... (put x sint so that dx cost dt, when x 0, t 0 when x 1, t /2 ) ************************************************************************ Tracing of Curves: For the evaluation of Mathematical quantities such as Area, Length, Volume and Surface area we need the rough graph of the equation in either Cartesian or parametric or polar form depending on the statement of the problem. We use the following theoretical steps to draw the rough graph. A) Cartesian Curves: y f (x) a) Symmetry: i) If the power of y in the equation is even, the curve is symmetric about x- axis ii) If the power of x in the equation is even, the curve is symmetric about y- axis iii) If both the powers x and y are even then the curve is symmetric about both the axis. iv) If the interchange of x and y leaves the equation unaltered then the curve is symmetric about the line y x v) Replacing x by x and y by y leaves the equation unchanged the curve has a symmetry in opposite quadrants. b) Curve through the origin: The curve passes through the origin, if the equation does not contain constant term. c) Find the origin, is on the curve. If it is, find the tangents at 0, by equating the lowest degree terms to zero. i) Find the points of intersections with the coordinate axes and the tangents at these points. For, put x 0 find y; and put y 0, find x. At these points, find., then the tangent is parallel to y axis. If 0, then the tangent is parallel to x axis. d) Asymptotes: express the equation of the curve in the form y f (x). Equate the denominator to zero. If the denominator contains x, then there is an asymptote.

e) Find the region in which the curve lies. f) Find the interval in which the curve is increasing or decreasing. B) Parametric Form: xf(t), yg(t) In this case we try to convert the parametric form into Cartesian form by eliminating the parameter (if possible). Otherwise we observe the following I) Find dy/dt and dx/dt and hence dy/dx. II) Assign a few values for t and find the corresponding value for x, y,y. III) Mark the corresponding points, observing the slope at these points. C) Polar curves: r f() a) Symmetry: 1. If the substitution of - for in the equation, leaves the equation unaltered, the curve symmetrical about the initial line. 2. If the power of r are even, the curve is symmetrical about the pole. b) Form the table, the value of r, for both positive and negative values of and hence note how r varies with. Find in particular the value of which gives r 0 and r. c) Find tan. This will indicate the direction of the tangent. d) Sometimes by the nature of the equation it is possible to ascertain the value of r and that are contained between certain limits. e) Transform into Cartesian, if necessary and adopt the method given before. f) Sketch the figure. PROBLEMS FOR TRACING THE CURVES 1. Astroid :, ) It is symmetrical about the x-axis Limits and The curve lies entirely within the square bounded by the lines,

Points: we have when t 0 or, when t As t increases x From 0 to From to π +ve decreases a to 0 and from -ve and increases numerically from 0 to -a Y +ve and increases from 0 to a + ve and decreases from a to 0 From 0 to From to 0 Portion traced A to B B to C As t increases from π to 2π, we get the reflection of the curve ABC in the x - axis. The values of t > 2π give no new points. Hence the shape of the curve is as shown in the fig. Y -X O X -Y Here ox oy a

It is symmetrical about the y axis. As such we may consider the curve only for positive values of x or. Limits: The greatest value of y is 2a and the least value is zero. Therefore the curve lies entirely between the lines y 0 and y 2a. Points: We have As increases x From 0 to π From π to 2π Y increases from increases from 0 to aπ 0 to 2π increases from decreases a π to 2aππ from 2a to 0 Portion traced From to 0 0 to A From 0 to A to B As decreases from 0 to - 2π, we get the reflection of the arch OAB in the y- axis. Hence the shape of the curve is as in the fig. Y 2. Cardioid: r Fig., X Initial Line A cardioids is symmetrical about the initial line and lies entirely within the circle r 2a. Its name has been derived from the Latin word Kardia - meaning heart. Because it is a heart shaped curve. ********************************************************************* ***

APPLICATIONS OF CURVE TRACING I) Length II) Area III) Volume IV) Surface area Table to find the values: Area, Length,VolumeThe surface area Quantity Coordinate system Cartesian form y f (x) Parametric form x x(t) y y(t) Area (A) Length (S) By revolving about the axis of rotation to form solid Volume (V) Surface area (SA) 1 2 Where 1 2 Where Polar form r f () 1 2 2 Where 3. Find the entire length of the cardioid 1, Also show that the upper half is bisected by The cardioid is symmetrical about the initial line and for its upper half, increases from 0 to π Also, -a sin θ. Length of the curve 2 d 2 1 2 21

4a /2 4a / / 8a (sin π/2 - sin 0) 8a Length of upper half of the curve of the cruve is 4a. Also length of the arch AP from 0 to π/3 2 21 2 cos. / 4 sin /2 Fig. 4 0 2a ( half the length of upper half of the cardioids ) 1. Find the entire length of the curve Solution: The equation to the curve is ), the curve is symmetrical about the axis and it meets the x axis at x a Fig. If S 1 the length of the curve AB Then required length is 4S 1 S 4S 1 1 Now, / S 4 1 / 4 / / /

4 / / 4 / / 4 / / / s 6a units Fig. 2. Find the perimeter of cardioid r a (1+cosθ). Solution: The equation to the curve is symmetrical about the initial line. Fig. The required length of the curve is twice the length of the curve OPA At O, θ π and at A θ 0 Now, r a(1+cosθ) s s s s a 1 cosθ 2 2acos dθ 8a units 3. Find the area of the Solution: The parametric equation to the curve is given by : x, Area 4 Put x, dx -3a cos 2 θ sinθ dθ when x 0, θ π/2 ; when x a, θ 0 / A 4-3a cos 2 θ sinθ dθ / 12 cos 2 θ dθ 12. Sq. units

4. Find the area of the cardioid r a (1+cosθ). Solution: The curve is symmetrical about the initial line. Total area 2 area above the line θ 0 A A A 2 is the formula for area in polar curves 2 a 1 cosθ 2 A 4 Put θ/2 t 2 / 4 2 Sq. units 5. Find the area bounded by an arch of the cycloid x, 1, 0 2 and its base. Solution: x, 1 for this arch t varies from 0 to 2π. 1 1 1 4 8 / 16... 3. since dx 1 6. Find the volume generated by revolving the cardiod r a (1+cosθ) about the initial line. Solution: For the curve, varies from 0 to Find the volume of the solid obtained by revolving the Astroid x 2/3 + y 2/3 a 2/3

Solution: the equation of the asteroid is x 2/3 + y 2/3 a 2/3 Volume is obtained by revolving the curve from x 0 to x a about x-axis and taking two times the result. 2 2 3 2 Problems for practice: 1. Find the surface area of r a (1 - cosθ) 2. Find the volume of the solid obtained by revolving the cissoid 2 about its asymptote. 3. Find the length between [0, 2 ] of the curve sin, 1 cos. Find the surface area of solid generated by revolving the astroid about the axis. Solution: The required surface area is equal to twice the surface area generated by revolving the part of the astroid in the first quadrant about the axis. Taking x, we have, / / Surface area 2 2 4 / 4 / 4π asin t 3acos t sint 3acos t sint 1/2dt / 12a sin t cos t dt. Put z sint 7. Find the surface area of the solid generated when the cardioid r a (1+cosθ) revolves about the initial line.

Solution: The equation to the curve is r a (1+cosθ). For the upper part of the curve, θ varies from 0 to π Put x r cosθ, y rsinθ Surface area 2 2 2 2 1. 1 cos 16a 2 UNIT IV: IV: VECTOR CALCULUS Scalar and Vector point functions: (I) If to each point p(r) of a region E in space there corresponds a definite scalar denoted by f(r), then f (R) is called a scalar point function in E. The region E so defined is called a scalar field. Ex: a) The temperature at any instant b)the density of a body and potential due to gravitational matter. (II) If to each point p(r) of a region E in space there corresponds a definite vector denoted by F(R), then it is called the vector point function in E. the region E so defined is called a vector field. Ex: a) The velocity of a moving fluid at any instant b) The gravitational intensity of force. Note: Differentiation of vector point functions follows the same rules as those of ordinary calculus. If F (x,y,z) be a vector point function then

( 1) Vector operator del ( ) The operator is of the form GRADIENT, DIVERGENCE, CURL (G D C) Gradient of the scalar point function: It is the vector point function f defined as the gradient of the scalar point function f and is written as grad f, then grad f f DIVERGENCE OF A VECTOR POINT FUNCTION The divergence of a continuously differentiable vector point function F(div F)is defined by the equation.

. CURL OF A VECTOR POINT FUNCTION The curl of a continuously differentiable vector point function F is defined by the equation curl F curl F curl F DEL APPLIED TWICE TO POINT FUNCTIONS Le being vector point functions, we can form their divergence and curl, whereas being a scalar point function, we can have its gradient only. Then we have Five formulas: div grad f 0 3. 0 0 F

F F F PROOF: (I) To prove that curl grad f f f f 0 (II) To prove that curl grad f f

i j k f 0 (III) To prove that 0 (IV) To prove that F F curl curl F F F (V) To prove that We have by (IV) which implies F F F F

1,, 5 3 2. : r nn 1r : r r n r R r n r R nr. R r R n n 2r R r R r 3 nn 2r r 3r nn 1r Otherwise: r Now nr nr nr x ^2 r^n / x^2 nr^n 2 n 2 r^n 3 r/ x x nr^n 2 n 2 r^n 3 x/r x nr n 2r x. 1 SImilarly, nr n 2r y.. 2 nr n 2r z 3 Adding equations 1, 2and 3, gives r n3r n 2r x y z n3r n 2r r nn 1r In particular 0

Ex: A particle moves along the curve 1,, 5 find the components of velocity and acceleration at t2 in the direction of 3 2 Solution:,

1 5 3 2 6 2 2, 12 4 12 2 3 2 12 4 3 2 12 2 : 4 1, 1,2 : 1, 1,2 3 2 4 12 4 4 12 4

:,, 2, 1,1 2 2 :,, 2, 1,1 i. e. 2 3 3 3 2 2,, r nn 1r r r 3 3 :,, 2 2 : 2 2 0 2 2 1 1 1.., 1 1 1 0, 1 0, 1 0, 1 0 1, 1, 1 Orthogonal curvilinear co-ordinates

Let the rectangular co-ordinates (x,y,z) of Any point be expressed as function of (u,v,w), So that x x(u,v,w),y y(u,v,w),z z(u,v,w)..(1) Suppose that (1) can be solved for u,v,w in terms of x,y,z i,e u (x,y,z), v v(x,y,z),w w(x,y,z).(2) We assume that the functions in (1) and (2) are single valued functions and have continuous partial derivatives so that the correspondence between (x,y,z) and (u,v,w) is unique. Then (u,v,w) are called curvilinear co-ordinates of (x,y,z). Each of u,v,w has a level of surface through an arbitrary point. The surface surface through are called co-ordinate Each pair of these co-ordinate surface intersects In curves called the cow-curve, for ordinate curves. The curve of intersection of will be called the only w changes along this curve. Similarly we define u and v-curves. In vector notation, (1) can be written as R x(u,v,w)i + y(u,v,w)j + z(u,v,w)k

The co-ordinate curves for ρ are rays perpendicular to the Z-axis; axis; for ф horizontal circles with centers on the Z-axis; Z axis; for z lines parallels to the Z-axis. Z x ρ cos ф,

y ρ sin ф, zz So that scale factors are h11, 1 h 2 ρ, h 3 1. Also the volume element dvρ dρ dф dz. 2) Spherical polar co-ordinates: Let p(x,y,z) be any point whose projection on the xy-plane is Q(x,y). Then the Spherical polar co-ordinates of p are such that r op,. The level surfaces are respectively spheres about O, cones about the Z-axis with vertex at O and planes through the Z-axis. The co-ordinate curves for r are rays from the origin; for θ, vertical circles with centre at O (called meridians); for ф, horizontal circles with centres on the Z- axis. x OQ cosф OP cos(90-θ) )cosф r sinθ cosф, y OQ sinф r sinθ sinф z r cosθ So that the scale factors are Also the volume element