Lecture No. 5 Lecture Notes_โฆย ยท CE 60130 FINITE ELEMENT METHODS - LECTURE 5 - updated 2018- 01-...
Transcript of Lecture No. 5 Lecture Notes_โฆย ยท CE 60130 FINITE ELEMENT METHODS - LECTURE 5 - updated 2018- 01-...
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Lecture No. 5
๐ฟ๐ฟ(๐ข๐ข) โ ๐๐(๐ฅ๐ฅ) = 0 in ๐บ๐บ
๐๐๐ธ๐ธ(๐ข๐ข) = ๐๐๐ธ๐ธ on ๐ค๐ค๐ธ๐ธ
๐๐๐๐(๐ข๐ข) = ๐๐๐๐ on ๐ค๐ค๐๐
โข For all weighted residual methods
๐ข๐ข๐๐๐๐๐๐ = ๐ข๐ข๐ต๐ต + ๏ฟฝ๐ผ๐ผ๐๐๐๐๐๐
๐๐
๐๐=1
โข For all (Bubnov) Galerkin methods
๐ค๐ค๐๐ = ๐๐๐๐ (test = trial)
Summary of Conventional Galerkin Method
๐๐๐ธ๐ธ(๐ข๐ข๐ต๐ต) = ๐๐๐ธ๐ธ and ๐๐๐ธ๐ธ(๐๐๐๐) = 0, ๐๐ = 1,๐๐ on ๐ค๐ค๐ธ๐ธ
๐๐๐๐(๐ข๐ข๐ต๐ต) = ๐๐๐๐ and ๐๐๐๐(๐๐๐๐) = 0, ๐๐ = 1,๐๐ on ๐ค๐ค๐๐
ิ๐ผ๐ผ = ๐ฟ๐ฟ๏ฟฝ๐ข๐ข๐๐๐๐๐๐๏ฟฝ โ ๐๐(๐ฅ๐ฅ)
< ิ๐ผ๐ผ ,๐ค๐ค๐๐ > = 0, ๐๐ = 1,๐๐
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Fundamental Weak Weighted Residual Galerkin
โข Only satisfy the essential b.c.โs. This makes things a lot easier!
๐๐๐ธ๐ธ(๐ข๐ข๐ต๐ต) = ๐๐๐ธ๐ธ and ๐๐๐ธ๐ธ(๐๐๐๐) = 0 ๐๐ = 1,๐๐ on ๐ค๐ค๐ธ๐ธ
โข Only require a limited degree of functional continuity. Therefore we can piece together
functions to make up ๐๐๐๐. Again this makes the problem much easier.
โข Since weโre not satisfying the natural b.c.โs, we also consider the error associated with the
locations where the natural b.c.โs is violated:
ิ๐ผ๐ผ = ๐ฟ๐ฟ๏ฟฝ๐ข๐ข๐๐๐๐๐๐๏ฟฝ โ ๐๐(๐ฅ๐ฅ)
ิ๐ต๐ต,๐๐ = โ๐๐๐๐๏ฟฝ๐ข๐ข๐๐๐๐๐๐๏ฟฝ + ๐๐๐๐
< ิ๐ผ๐ผ ,๐ค๐ค๐๐ > +< ิ๐ต๐ต,๐๐ ,๐ค๐ค๐๐ > = 0 ๐๐ = 1,๐๐
This establishes the fundamental weak form. Thus we have relaxed the admissibility
conditions such that only โessentialโ b.c.โs must be satisfied.
โข The Interior and Boundary Error (for the natural boundary) must go to zero by requiring ๐ค๐ค๐๐
to the orthogonal to these combined errors. Hence we are no longer โclampingโ the natural
b.c. down at the time we set up our sequence but we are โdrivingโ the natural b.c. error to
zero as the number of trial functions increases.
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โข Expanding out the fundamental weak form by substituting ิ๐ผ๐ผ , ิ๐ต๐ต,๐๐ and ๐ข๐ข๐๐๐๐๐๐.
< ๐ฟ๐ฟ(๐ข๐ข๐ต๐ต) โ ๐๐,๐ค๐ค๐๐ > +๏ฟฝ๐ผ๐ผ๐๐ < ๐ฟ๐ฟ(๐๐๐๐),๐๐
๐๐=1
๐ค๐ค๐๐ >๐บ๐บ +< ๐๐๐๐ โ ๐๐๐๐(๐ข๐ข๐ต๐ต),๐ค๐ค๐๐ >๐ค๐ค๐๐
โ๏ฟฝ๐ผ๐ผ๐๐ <๐๐
๐๐=1
๐๐๐๐(๐๐๐๐),๐ค๐ค๐๐ >๐ค๐ค๐๐= 0 ๐๐ = 1,๐๐
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Symmetrical Weak Weighted Residual Form
โข Letโs continue to relax admissibility by integrating the fundamental weak form by parts.
The โhalfway pointโ of the integration represents the symmetrical weak formโ.
โข This integration by parts procedure:
โข Reduces the required functional continuity on the approximating functions. It reduces
functional continuity requirements on the trial functions while increasing them on the
test functions. At the symmetrical weak form these requirements are balanced. Thus
this is the optimal weak form.
โข Furthermore the unknown functions evaluated at the boundary disappear.
โข In general the natural b.c. is only satisfied in an average sense of ๐๐ โ โ.
โข When the operator is self-adjoint, the matrix generated will still be symmetrical for both the
symmetrical and fundamental weak forms.
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Definition and Use of Localized Functions
โข Split the domain up into segments over which trial/test functions are defined.
Motivation, itโs easier to satisfy b.c.โs for complex 2D/3D geometries since these can be
satisfied locally (for weak formulations we need only satisfy the essential b.c.โs). In addition
the matrix properties will in general be much better.
โข For the finite element method (FEM), we use functions defined over small subdomains, i.e.
localized functions.
โข However we must ensure that we satisfy the correct degree of functional continuity. For
example, consider:
๐ฟ๐ฟ(๐ข๐ข) =๐๐2๐ข๐ข๐๐๐ฅ๐ฅ2
๐๐(2) space is required for fundamental weak form (continuity of the function and the first
derivative and a finite second derivative).
๐๐(1) space is required for the symmetrical weak form (continuity of the function and a
finite first derivative).
โข Split the domain up into segments and define trial functions within each element.
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Option 1
No functional continuity but finite function โ ๐๐(0) space
(a) The simplest approximation is a histogram (i.e. constant value of the function over the
element). This defines only one unknown per โfinite elementโ.
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(b) We can define more complex functions over the element leading to more unknowns per
element (to represent an increased order of polynomial or function within the element).
However we still have no functional continuity between the elements and thus these
functions still are from the ๐๐(0) space.
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Option 2
The function is continuous which defines the ๐๐(1) = ๐ถ๐ถ๐๐ space. This space requires no
continuity of the derivative. We define the discrete variables equal to the functional values at
the nodes. Nodes must always join up at the inter element boundaries!
(a) The simplest approximation consists of a linear approximation over each element
which involves 2 unknowns per element and 1 unknown per node: Thus over each
element:
๐ข๐ข = ๐๐๐๐ + ๐๐1๐ฅ๐ฅ
Thus weโve gone from an element measure to a nodal measure.
An interpolating function defined with nodal functional values and ๐๐(1) = ๐ถ๐ถ๐๐ continuity is called a Lagrange interpolating function.
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(b) We can use higher degree functions within each element (i.e. more nodes per element)
however functional continuity will still only be ๐๐(1). For example:
๐ข๐ข = ๐๐๐๐ + ๐๐1๐ฅ๐ฅ + ๐๐2๐ฅ๐ฅ2 + ๐๐3๐ฅ๐ฅ3
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Option 3
The function and first derivative continuous defines the ๐๐(2) = ๐ถ๐ถ1 space. In this case we
must define the function and the first derivative as nodal variables.
(a) Simplest approximation involves 2 nodes with 2 unknowns per node. Thus over each
element:
๐ข๐ข = ๐๐๐๐ + ๐๐1๐ฅ๐ฅ + ๐๐2๐ฅ๐ฅ2 + ๐๐3๐ฅ๐ฅ3
Therefore u and ๐ข๐ข,๐ฅ๐ฅ are the unknowns. This involves 4 unknowns per element, 2 unknowns
per node.
Interpolating functions defined with nodal functional and first derivative values with
๐๐(2) = ๐ถ๐ถ1 continuity are called Hermite Interpolating functions.
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1st order Hermite: ๐ข๐ข and ๐ข๐ข,๐ฅ๐ฅ continuous
2nd order Hermite: ๐ข๐ข, ๐ข๐ข,๐ฅ๐ฅ and ๐ข๐ข,๐ฅ๐ฅ๐ฅ๐ฅ continuous โ 3 unknowns per node
Note 1
For the Galerkin method, ๐ค๐ค๐๐ = ๐๐๐๐
โข The fundamental weak form requires different order functional continuity for ๐๐๐๐ as
trial functions than the ๐ค๐ค๐๐ (or ๐๐๐๐ as test) functions.
โข The symmetrical weak form is obtained by integration by parts until the space
requirements for ๐๐๐๐ and ๐ค๐ค๐๐ are the same. This is the most attractive form to use. We
note that the number of unknowns has been minimized.
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Example
โข Fundamental weak form:
๏ฟฝ๏ฟฝ๐๐2๐ข๐ข๐๐๐๐๐๐๐๐๐ฅ๐ฅ2 + ๐ข๐ข๐๐๐๐๐๐ โ ๐ฅ๐ฅ๏ฟฝ๐ค๐ค๐๐๐๐๐ฅ๐ฅ + ๏ฟฝ๏ฟฝ๐๐ โ
๐๐๐ข๐ข๐๐๐๐๐๐๐๐๐ฅ๐ฅ ๏ฟฝ๐ค๐ค๐๐๏ฟฝ
๐ฅ๐ฅ=1= 0 ๐๐ = 1,๐๐
1
0
๐ค๐ค๐๐ โ ๐ฟ๐ฟ2 and ๐ข๐ข๐๐๐๐๐๐ (or ๐๐๐๐) โ ๐๐(2), ๐๐ = 1,๐๐
Therefore we must choose ๐ค๐ค๐๐ and ๐๐๐๐ โ ๐๐(2)
The functional and first derivative must be continuous) leading to a cubic approximation
over the element with 2 unknowns per node (function value and its 1st derivative). Thus we
require Hermite interpolation
โข Symmetrical Weak Form
๏ฟฝ๏ฟฝโ๐๐๐ข๐ข๐๐๐๐๐๐๐๐๐ฅ๐ฅ
๐๐๐ค๐ค๐๐๐๐๐ฅ๐ฅ + ๐ข๐ข๐ค๐ค๐๐ + ๐ฅ๐ฅ๐ค๐ค๐๐๏ฟฝ๐๐๐ฅ๐ฅ + ๏ฟฝ๐๐๐ค๐ค๐๐๏ฟฝ๐ฅ๐ฅ=1 = 0
1
0
๐๐ = 1,๐๐
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โข The opposite of the fundamental weak form is obtained by interchanging ๐ข๐ข๐๐๐๐๐๐ and ๐ค๐ค๐๐ and
leads to the B.E.M form
๏ฟฝ๐๐๐ค๐ค๐๐๐๐๐ฅ๐ฅ ๐ข๐ข๐๐๐๐๐๐๏ฟฝ
0
1
+ ๏ฟฝ๐๐๐ค๐ค๐๐๏ฟฝ๐ฅ๐ฅ=1 + ๏ฟฝ๏ฟฝ๐ข๐ข๐ค๐ค๐๐ + ๐ฅ๐ฅ๐ค๐ค๐๐ + ๐ข๐ข๐๐๐๐๐๐๐๐2๐ค๐ค๐๐๐๐๐ฅ๐ฅ2 ๏ฟฝ ๐๐๐ฅ๐ฅ = 0
1
0
๐๐ = 1,๐๐
Now ๐ค๐ค๐๐ โ ๐๐(2) and ๐ข๐ข๐๐๐๐๐๐ (or ๐๐๐๐) โ ๐ฟ๐ฟ2
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Note 2
Alternative strategy for deriving the symmetrical weak form:
โข Start with standard Galerkin formulation
โข Integrate by parts
โข Substitute in for the specified natural b.c.
Example
โข Standard Galerkin formulation
๏ฟฝ๏ฟฝ๐๐2๐ข๐ข๐๐๐๐๐๐๐๐๐ฅ๐ฅ2 + ๐ข๐ข๐๐๐๐๐๐ + ๐ฅ๐ฅ๏ฟฝ๐ค๐ค๐๐๐๐๐ฅ๐ฅ = 0
1
0
โข Integrate by parts:
๏ฟฝ๏ฟฝโ๐๐๐ข๐ข๐๐๐๐๐๐๐๐๐ฅ๐ฅ
๐๐๐ค๐ค๐๐๐๐๐ฅ๐ฅ + ๐ข๐ข๐ค๐ค๐๐ + ๐ฅ๐ฅ๐ค๐ค๐๐๏ฟฝ ๐๐๐ฅ๐ฅ + ๏ฟฝ
๐๐๐ข๐ข๐๐๐๐๐๐๐๐๐ฅ๐ฅ ๐ค๐ค๐๐๏ฟฝ
๐ฅ๐ฅ=0
๐ฅ๐ฅ=1
= 01
0
โ
๏ฟฝ๏ฟฝโ๐๐๐ข๐ข๐๐๐๐๐๐๐๐๐ฅ๐ฅ
๐๐๐ค๐ค๐๐๐๐๐ฅ๐ฅ + ๐ข๐ข๐ค๐ค๐๐ + ๐ฅ๐ฅ๐ค๐ค๐๐๏ฟฝ ๐๐๐ฅ๐ฅ + ๏ฟฝ
๐๐๐ข๐ข๐๐๐๐๐๐๐๐๐ฅ๐ฅ ๐ค๐ค๐๐๏ฟฝ
๐ฅ๐ฅ=1โ ๏ฟฝ
๐๐๐ข๐ข๐๐๐๐๐๐๐๐๐ฅ๐ฅ ๐ค๐ค๐๐๏ฟฝ
๐ฅ๐ฅ=0= 0
1
0
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โข However for our example case:
๐๐๐๐๐๐๐๐๐๐๐๐๐ฅ๐ฅ
๏ฟฝ๐ฅ๐ฅ=1
โ ๐๐ (specified natural b.c.)
โข Substituting the above equation as well as ๐ค๐ค๐๐๏ฟฝ๐ฅ๐ฅ=0 = 0 (since ๐๐๐๐ satisfies the
homogeneous form of the essential b.c.), leads to:
๏ฟฝ๏ฟฝ๐๐๐ข๐ข๐๐๐๐๐๐๐๐๐ฅ๐ฅ
๐๐๐ค๐ค๐๐๐๐๐ฅ๐ฅ + ๐ข๐ข๐ค๐ค๐๐ + ๐ฅ๐ฅ๐ค๐ค๐๐๏ฟฝ ๐๐๐ฅ๐ฅ + ๏ฟฝ๐๐๐ค๐ค๐๐๏ฟฝ๐ฅ๐ฅ=1 = 0
1
0
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Note 3
For collocation we cannot use an integration by parts procedure to lower the required degree
of functional continuity as we could for Galerkin methods. This is due to the form of the
weighting functions, ๐ค๐ค๐๐ = ๐ฟ๐ฟ๏ฟฝ๐ฅ๐ฅ โ ๐ฅ๐ฅ๐๐๏ฟฝ (the dirac delta function) which is not differentiable.
๐๐๐ฟ๐ฟ๏ฟฝ๐ฅ๐ฅ โ ๐ฅ๐ฅ๐๐๏ฟฝ๐๐๐ฅ๐ฅ
does not exist. Therefore it is not possible to find any weak forms!
Therefore for a 2nd order differential operator ๐ฟ๐ฟ we must use Hermite type interpolation
compared to the Galerkin Symmetrical weak form for which we only needed Lagrange type
interpolation.
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Note 4
โข Summary of Advantages of Weak Forms:
โข Fundamental weak form has relaxed b.c. requirements. Itโs much easier to find trial/test
functions which satisfy the homogeneous form of the essential b.c. than both the essential
and natural b.c.โs
โข In addition when we define local trial functions on finite elements, it will be much
simpler to satisfy the essential b.c.โs locally on the element level rather than on a global
level.
When using the FE method where we simply go into the matrix and set the essential b.c.
u and we need not worry about โstrictlyโ enforcing the natural boundary condition ๐๐๐ข๐ข/๐๐๐ฅ๐ฅ
โข Symmetrical weak form has relaxed functional continuity requirements. This is very
important when defining functions over split domains (FE method).
The symmetrical weak form lowers the inter-element functional continuity requirements
and thus lowers the number of unknowns.
โข In addition, part of the natural b.c. error falls out due to the way in which it was defined.
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Notes on a 4th derivative operator problem
Consider the equilibrium equation for a beam on an elastic foundation
๐ธ๐ธ๐ธ๐ธ๐๐4๐ฃ๐ฃ๐๐๐ฅ๐ฅ4 + ๐๐๐ฃ๐ฃ = ๐๐(๐ฅ๐ฅ)
where
v = beam displacement
E = modulus of elasticity
I = moment of inertia
k = foundation constant
p = distributed load on the beam
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Standard Galerkin
โจ๐ฟ๐ฟ(๐ฃ๐ฃ) โ ๐๐, ๐ฟ๐ฟ๐ฃ๐ฃโฉ = 0
โ
๏ฟฝ๏ฟฝ๐ธ๐ธ๐ธ๐ธ๐๐4๐ฃ๐ฃ๐๐๐ฅ๐ฅ4
+ ๐๐๐ฃ๐ฃ โ ๐๐๏ฟฝ๐ฟ๐ฟ๐ฃ๐ฃ๐๐๐ฅ๐ฅ = 0๐๐
0
โข We can establish what the essential and natural b.c.โs are by using the integration by parts
procedure to find:
โจ๐ฟ๐ฟ(๐ฃ๐ฃ), ๐ฟ๐ฟ๐ฃ๐ฃโฉ = โจ๐ฟ๐ฟโ(๐ฟ๐ฟ๐ฃ๐ฃ), ๐ฃ๐ฃโฉ +
๏ฟฝ [๐น๐น1(๐ฟ๐ฟ๐ฃ๐ฃ)๐บ๐บ1(๐ฃ๐ฃ) + ๐น๐น2(๐ฟ๐ฟ๐ฃ๐ฃ)๐บ๐บ2(๐ฃ๐ฃ) โ ๐น๐น1(๐ฃ๐ฃ)๐บ๐บโ1(๐ฟ๐ฟ๐ฃ๐ฃ) โ ๐น๐น2(๐ฃ๐ฃ)๐บ๐บโ2(๐ฟ๐ฟ๐ฃ๐ฃ)]๐๐๐ค๐ค
โข We perform 2 integration by parts to find the bcโs (assuming EI constant):
โจ๐ฟ๐ฟ(๐ฃ๐ฃ), ๐ฟ๐ฟ๐ฃ๐ฃโฉ = ๏ฟฝ๏ฟฝ๐ธ๐ธ๐ธ๐ธ๐๐2๐ฃ๐ฃ๐๐๐ฅ๐ฅ2
๐๐2๐ฟ๐ฟ๐ฃ๐ฃ๐๐๐ฅ๐ฅ2 + ๐๐๐ฃ๐ฃ๐ฟ๐ฟ๐ฃ๐ฃ๏ฟฝ๐๐๐ฅ๐ฅ
๐๐
0
+ ๏ฟฝโ๐ธ๐ธ๐ธ๐ธ๐๐2๐ฃ๐ฃ๐๐๐ฅ๐ฅ2
๐๐๐ฟ๐ฟ๐ฃ๐ฃ๐๐๐ฅ๐ฅ + ๐ธ๐ธ๐ธ๐ธ
๐๐3๐ฃ๐ฃ๐๐๐ฅ๐ฅ3 ๐ฟ๐ฟ๐ฃ๐ฃ๏ฟฝ๐ฅ๐ฅ=0
๐ฅ๐ฅ=1
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โข This is halfway point of the integration by parts procedure and represent the symmetrical
weak form:
โข Hence the essential b.c.โ are: ๐น๐น1(๐ฃ๐ฃ) = ๐ฃ๐ฃ โ displacement
๐น๐น2(๐ฃ๐ฃ) = ๐๐๐๐๐๐๐ฅ๐ฅโ slope
โข the natural b.c.โs are: ๐บ๐บ1(๐ฃ๐ฃ) = โ๐ธ๐ธ๐ธ๐ธ ๐๐3๐๐
๐๐๐ฅ๐ฅ3= ๐๐ โ applied shear
๐บ๐บ2(๐ฃ๐ฃ) = +๐ธ๐ธ๐ธ๐ธ ๐๐2๐๐
๐๐๐ฅ๐ฅ2= ๐๐ โ applied moment
โข Note that the weighting functions that are to be used in establishing the fundamental
weak form fall out of this integration by parts procedure used in establishing self-
adjointness of the operator (which also establishes b.c.โs). You want terms to drop later
on!
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โข Natural boundary errors
The error in the moment is:
ิ๐ต๐ตโฒ = ๏ฟฝ๐ธ๐ธ๐ธ๐ธ๐๐2๐ฃ๐ฃ๐๐๐ฅ๐ฅ2 โ ๐๐๏ฟฝ ๏ฟฝ
๐๐๐ฟ๐ฟ๐ฃ๐ฃ๐๐๐ฅ๐ฅ
๏ฟฝ
A error in the shear is:
ิ๐ต๐ต" = ๏ฟฝโ๐ธ๐ธ๐ธ๐ธ๐๐3๐ฃ๐ฃ๐๐๐ฅ๐ฅ3 โ ๐๐๏ฟฝ {๐ฟ๐ฟ๐ฃ๐ฃ}
โข Weighted natural boundary errors
A moment error is weighted by a rotation:
โจิ๐ต๐ตโฒ ,๐๐๐ฟ๐ฟ๐ฃ๐ฃ๐๐๐ฅ๐ฅ
โฉ = ๏ฟฝ ๏ฟฝ๐ธ๐ธ๐ธ๐ธ๐๐2๐ฃ๐ฃ๐๐๐ฅ๐ฅ2 โ ๐๐๏ฟฝ
ฮ๐๐
๏ฟฝ๐๐๐ฟ๐ฟ๐ฃ๐ฃ๐๐๐ฅ๐ฅ ๏ฟฝ ๐๐ฮ
A shear error is weighted by a displacement
โจิ๐ต๐ต" , ๐ฟ๐ฟ๐ฃ๐ฃโฉ = ๏ฟฝ ๏ฟฝโ๐ธ๐ธ๐ธ๐ธ๐๐3๐ฃ๐ฃ๐๐๐ฅ๐ฅ3 โ ๐๐๏ฟฝ
ฮ๐๐
{๐ฟ๐ฟ๐ฃ๐ฃ} ๐๐ฮ
C E 6 0 1 3 0 F I N I T E E L E M E N T M E T H O D S - L E C T U R E 5 - u p d a t e d 2 0 1 8 - 0 1 - 2 5 P a g e 22 | 22
โข Note that we must specify essential b.c.โs somewhere!
โข Boundary conditions must be specified in pairs for this problem
โข Displacement and rotation are paired
โข Shear and moment are paired
โข The error/weighting products fall out of the integration by parts process. They are also
dimensionally consistent with all terms in the total error equation.
โข The total error equation for this problem is the fundamental weak form
โจิ๐ผ๐ผ , ๐ฟ๐ฟ๐ฃ๐ฃโฉ + โจิ๐ต๐ตโฒ ,๐๐๐ฟ๐ฟ๐ฃ๐ฃ๐๐๐ฅ๐ฅ
โฉ + โจิ๐ต๐ต" , ๐ฟ๐ฟ๐ฃ๐ฃโฉ = 0
where
ิ๐ผ๐ผ = ๐ธ๐ธ๐ธ๐ธ๐๐4๐ฃ๐ฃ๐๐๐ฅ๐ฅ4 + ๐๐๐ฃ๐ฃ โ ๐๐
โข The symmetrical weak form is established by integrating the fundamental weak form by
parts.