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  • Virtually every phenomenon in the nature, whether biological, geological or mechanical

    can be described with the aid of laws of physics in terms of algebraic, differential or

    integral equations relating various quantities of interest.

    Studying a physical phenomenon involved two major tasks

    ( i). Mathematical formulation of the physical process

    (ii) Numerical analysis of the mathematical model

    The mathematical formulation of a physical process needs background in

    the related subjects. The formulation results in mathematical statement, often differential

    equations. The derivation of the governing equation for most of the problem is not a

    difficult task. But their solution by exact methods of analysis is not at all a easy task. In

    such cases approximate method of analysis are used to find the solution. Among these

    methods, functional approximation method, finite difference method, and finite element

    method are most frequently used.

    Functional approximation:-

    In this method, a set of independent functions satisfying the boundary

    condition are chosen. A linear combination of finite number of them is taken to specify

    the field variable at any point. The unknown parameters that combine the functions are

    found out.

    Examples for this method of solution are

    ( i). Collocation methods

    (ii). Least square methods

    (iii).Sub domain methods

    (iv).Galerkin methods

  • Finite element method :-

    In this method a given domain (area) is divided into a number of sub domains

    (sub area), called element or finite elements and an approximate solution to the problem

    is developed over each of these finite elements.

    The sub division of a whole geometry in to part involves two advantages

    (i). It allows accurate representation of complex geometries.

    (ii). It enables accurate representation of the solution within each element to bring out

    local effects (e.g. Stress concentration).

    Practical applications :-

    (i). Determining the system distribution in a pressure vessel with oddly shaped holes

    and number of stiffness which are subjected to mechanical , thermal and

    Aerodynamic loads.

    (ii).Finding the concentration of pollutant in sea water or in the atmosphere

    (iii). Simulating the weather in an attempt to understand and to predict the formation

    of thunderstorms

    Steps involved in FEM:-

    (1). Divide the whole geometry in to parts.

    (2). Over each part, find an approximate solution.

    (3). Assemble them to obtain the solution to the whole geometry

    The process of dividing a complex geometry into a number of sub domains is called

    discretization or meshing.

  • Example to understand the basic idea of FEM

    To determine the circumference of a circle

    Ancient mathematician estimated that the value of circumference of the circle by

    approximating the circle by line segment whose lengths can be measured.

    The approximate value of P can be obtained by summing the lengths of the line elements.

    This ancient method lays the building for the development of FEM techniques

    FEM Procedure

    (1). Finite element discretization:-

    The domain, the circumference of the circle represented as a collection of finite

    number n sub domain. This process is called discretization of domain.

    Each sub domain is called an element. The collection of element is called as finite

    element mesh.

    R

    Uniform

    Mesh

    Non-

    Uniform

    Mesh

  • An element is connected with another one element at selected points called nodes.

    The line segment can be of same length or of different length. When the lengths of

    the line segment are same for all elements, then the resulting mesh is called as uniform

    mesh.

    If the lengths of line segments are not uniform then the resulting mesh is called as

    non-uniform mesh.

    (2).Element equation

    An element is isolated form mesh and its required property (length) is

    computed by same approximate means

    he/2

    From the geometry,

    Sin (2

    e) =

    R

    he

    he = 2Rsin (2

    e) (1)

    R is the radius of the circle and e is the subtended angle by the element.

    Equation (1) is called as element equation.

    he e e/2

  • (3). Assembly of element equation and solution

    The approximate value of the circumference of the circle is obtained by putting

    together the element properties in a meaningful manner. This process is called as the

    assembly of element equation. In our case, the perimeter or circumference of the circle is

    equal to the sum of the lengths of the individual elements.

    Pn =

    n

    e 1

    he

    Here, Pn represents an approximation to the actual perimeter P. If the mesh size is

    uniform, then

    e = n2

    Here n is the number of elements.

    Pn = n2R sin ( n22

    )

    Pn = n2R sin ( n

    )

    (4). Convergence and Error estimate

    In our case, the exact solution is known to us i.e. P =2R

    So, we can estimate the error in the approximation. Also, we can show that the

    approximate solution Pn converges to the exact solution P in the limits n

    For our case, the error in the approximation is equal to

    En = P- Pn

    =2R- n2R sin ( n

    )

    =2R (- n sin ( n

    ))

  • Proof for convergence

    En 0 when n

    En = P- Pn, 0= P- Pn, P= Pn

    Pn = n2R sin ( n

    ) put x = n

    1

    Pn = x

    R2 sin ( x )

    As n x 0

    Lim Pn = Lim x

    R2 sin ( x )

    n x

    = Lim (2Rcos x ) (Apply L Hospital Rule )

    x

    =2R =P

    From the above proof, it is clear that as the number of elements increases, the

    approximation improves i.e. the error in the approximation decreases.

    APPROXIMATE DETERMINE OF CENTROID / CENTRE OF MASS

    Here, the body is conveniently divided in to several elements of simple shape for

    which the centre of mass can be computed readily.

    In our case, the complex geometry is divided into a finite number of rectangular strips.

    Each elements are having he as the width and be as the height. The area of an elemental

    strip is Ae= he be. here the area Ae is an approximation of the true area of the element.

    Because, be is the estimated average height of the elements. The co-ordinates of the

    centroid of the region is given by

  • X =

    Ae

    exAe & Y =

    Ae

    eyAe where

    ex and ey are the co-ordinate of the centroid of the e th element with respect to the co-

    ordinate system used for the whole body

    The accuracy of approximation will be improved by increasing the number of strips ie

    by decreasing the width; we can increase the number of elements

    Instead of rectangular shaped elements, we use any geometry as elements that can be

    approximate the given domain to a satisfactory level of accuracy.

    For example, a trapezoidal element will require two height

    to compute its area.

    Ae = he (be + be+1)

    . .

    ex

    ey Y

    X

    be+1 be

    he

  • FINITE DIFFERENCE METHOD

    In the functional approximation technique, the assumed trial function must be

    continuous and should satisfy all the prescribed boundary condition. No simple

    guidelines are available to select such functions. Hence except in simple situation, this

    approach could not be used to solve practical problems

    In this finite difference method, the given geometry is bounded with in a solid region

    and the region is discretized by nodal points as shown

    Here, the field variable is represented by the discrete values of the variable at the nodal

    points. The governing differential equation and the boundary condition are converted into

    finite difference form. The finite difference form of the governing D.E and B.C are then

    applied over each of the nodes in turn, this will yield a set of algebraic equations. The

    resulting equations are then solved for the nodal values of the field variables.

  • In this method, the finite difference form of the D.E can be obtained easily for meshing

    regular shapes but it becomes tedious to derive it for irregular shapes. Move over the

    governing D.E itself will become move complex in the case materials other than

    isotropic.

    Determine the approximate solution of the D.E

    x

    dd

    u2

    2

    - u + x2 = 0; u (0) = 0; u

    l (1) = 1

    Let the trial function be

    u(x) = a0 + a1x + a2x2 + a3x

    3

    u(0) = 0 = a0 ( by applying B.C 1 )

    dx

    du = a1 + 2a2x

    2+ 3a3x

    2

    ul(1) = 1 a1 + 2a2+ 3a3= 1

    a1 = 1- 2a2- 3a3 ( A )

    u(x) = (1- 2a2- 3a3) x + a2x2 + a3x

    3

    = x + a2(x2-2x) + a3(x

    3+3x) ( 1 )

    dx

    du = 1 + a2(2x-2) + a3(3x

    2+3)

    2

    2

    dx

    ud = 2a2 + 6a3x ( 2 )

    Sub (1) and (2) in given D.E

    -2a2 - 6a3x - x a2(x2-2x) - a3(x

    3+3x) + x

    2 = 0

    x2 - x + a2(2x -x

    2-2) + a3(3x -x

    3-6x) = 0

    x2 - x + a2(2x -x2-2) + a3(-x

    3-3x) = 0 is the residue equation

  • Collocation method

    Collocation points are to be selected with in the limits. Here 1/3, 2/3 are to be

    taken as collocation points.

    R (3

    1) = (

    3

    1)

    2 -

    3

    1 + a2(2*

    3

    1 -(

    3

    1)

    2-2) + a3(-(

    3

    1)

    3-3*

    3

    1) = 0

    = 1.4444a2 + 1.037a3 = -0.222 ( 3 )

    R (3

    2) = (

    3

    2)

    2 -

    3

    2 + a2(2*

    3

    2 -(

    3

    2)

    2-2) + a3(-(

    3

    2)

    3-3*

    3

    2) = 0

    = 1.1111a2 + 2.2963a3 = -0.222 (4)

    (3) *- 0.7694 = -1.1111a2 0.7978a3 = .01708

    1.4985a3 = -0.0512

    a3 = -0.03416

    Sub a3 = -0.03416 in (3) a2 = -0.1292

    Sub a2, a3 in (A)

    a1 = 1+ 2*0.1292+ 3*0.03416

    a1 = 1.3609

    u (3

    1) = 1.3609*

    3

    1 - 0.1292x (

    3

    1)

    2 - 0.03416 (

    3

    1)

    3

    u (3

    1) = 0.4405

    u (3

    2) = 0.8397

    Least square method

    1

    0

    R * Coeff of a2 =0

    1

    0

    {( x2 - x )+ a2(2x -x

    2-2) + a3(-x

    3-3x) }(2x -x

    2-2)dx =0

  • 1

    0

    2x2- x

    4-2x

    2-2x

    2+ x

    3+2x+ a2(4x

    2-2x

    3-4x-2x

    3+ x

    4+2x

    2-4x+2x

    2+4) +

    a3(-2x4+ x

    5+2x

    3-6x

    2+3x

    3+6x)dx=0

    1

    0

    - x4-2x

    2+ x

    3+2x+ a2(8x

    2-4x

    3-8x+ x

    4+4) + a3(-2x

    4+ x

    5+5x

    3-6x

    2+6x)dx=0

    2

    2 2x-

    3

    2 3x+

    4

    4x-

    5

    5x+ a2(8

    3

    3x-

    2

    8 2x+4x-

    4

    4 4x+

    5

    5x)+ a3(

    2

    6 2x-

    3

    6 3x+

    4

    5 4x-

    5

    2 5x+

    6

    6x)

    1

    0] = 0

    1-3

    2+

    4

    1-

    5

    1+ a2(

    3

    8-4+4-1+

    5

    1) + a3(3-2+

    4

    5 -

    5

    2+

    6

    1)=0

    0.3833+1.867a2+2.0167 a3=0

    1

    0

    R * Coeff of a3 =0

    1

    0

    {(x2 - x) + a2 (2x -x2-2) + a3 (-x

    3-3x)}(-x

    3-3x) dx = 0

    1

    0

    -x5- 3x

    3 + x

    4 + 3x

    2 +

    a2(-2x

    4-6x

    2+x

    5+3x

    3+2x

    3+6x)+a3(x

    6+3x

    4+3x

    4+9x

    2) dx = 0

    6

    6x-

    4

    3 4x+

    5

    5x+

    3

    3 3x+ a2(

    2

    6 2x-

    3

    6 3x+

    4

    5 4x-

    5

    2 5x+

    6

    6x)+ a3(

    3

    9 3x+

    5

    3 5x-

    5

    3 5x+

    7

    7x)

    1

    0] = 0