Lecture No. 5. For all weighted residual methods. For all (Bubnov) Galerkin methods. Summary of Conventional Galerkin Method

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Lecture No. 5 LL(uu) pp(xx) = 0 in ΩΩ SS EE (uu) = gg EE on ΓΓ EE SS NN (uu) = gg NN on ΓΓ NN For all weighted residual methods NN uu aaaaaa = uu BB + αα ii φφ ii For all (Bubnov) Galerkin methods ii=1 ww ii = φφ ii (test = trial) Summary of Conventional Galerkin Method SS EE (uu BB ) = gg EE and SS EE (φφ ii ) = 0, SS NN (uu BB ) = gg NN and SS NN (φφ ii ) = 0, ii = 1, NN on ΓΓ EE ii = 1, NN on ΓΓ NN Ԑ II = LL uu aaaaaa pp(xx) < Ԑ II, ww jj > = 0, jj = 1, NN CE 60130 FINITE ELEMENT METHODS- LECTURE 5 - updated 2018-01- 25 Page 1 22

Fundamental Weak Weighted Residual Galerkin Only satisfy the essential b.c. s. This makes things a lot easier! SS EE (uu BB ) = gg EE and SS EE (φφ ii ) = 0 ii = 1, NN on ΓΓ EE Only require a limited degree of functional continuity. Therefore we can piece together functions to make up φφ ii. Again this makes the problem much easier. Since we re not satisfying the natural b.c. s, we also consider the error associated with the locations where the natural b.c. s is violated: Ԑ II = LL uu aaaaaa pp(xx) Ԑ BB,NN = SS NN uu aaaaaa + gg NN < Ԑ II, ww jj > +< Ԑ BB,NN, ww jj > = 0 jj = 1, NN This establishes the fundamental weak form. Thus we have relaxed the admissibility conditions such that only essential b.c. s must be satisfied. The Interior and Boundary Error (for the natural boundary) must go to zero by requiring ww jj to the orthogonal to these combined errors. Hence we are no longer clamping the natural b.c. down at the time we set up our sequence but we are driving the natural b.c. error to zero as the number of trial functions increases. CE 60130 FINITE ELEMENT METHODS- LECTURE 5 - updated 2018-01- 25 Page 2 22

Expanding out the fundamental weak form by substituting Ԑ II, Ԑ BB,NN and uu aaaaaa. NN < LL(uu BB ) pp, ww jj > + αα ii < LL(φφ ii ), ww jj > ΩΩ +< gg NN SS NN (uu BB ), ww jj > ΓΓNN ii=1 NN αα ii < SS NN (φφ ii ), ww jj > ΓΓNN = 0 jj = 1, NN ii=1 CE 60130 FINITE ELEMENT METHODS- LECTURE 5 - updated 2018-01- 25 Page 3 22

Symmetrical Weak Weighted Residual Form Let s continue to relax admissibility by integrating the fundamental weak form by parts. The halfway point of the integration represents the symmetrical weak form. This integration by parts procedure: 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. Furthermore the unknown functions evaluated at the boundary disappear. In general the natural b.c. is only satisfied in an average sense of NN. When the operator is self-adjoint, the matrix generated will still be symmetrical for both the symmetrical and fundamental weak forms. CE 60130 FINITE ELEMENT METHODS- LECTURE 5 - updated 2018-01- 25 Page 4 22

Definition and Use of Localized Functions Split the domain up into segments over which trial/test functions are defined. Motivation, it s easier to satisfy b.c. s for complex 2D/3D geometries since these can be satisfied locally (for weak formulations we need only satisfy the essential b.c. s). In addition the matrix properties will in general be much better. For the finite element method (FEM), we use functions defined over small subdomains, i.e. localized functions. However we must ensure that we satisfy the correct degree of functional continuity. For example, consider: LL(uu) = dd2 uu ddxx 2 WW (2) space is required for fundamental weak form (continuity of the function and the first derivative and a finite second derivative). WW (1) space is required for the symmetrical weak form (continuity of the function and a finite first derivative). Split the domain up into segments and define trial functions within each element. CE 60130 FINITE ELEMENT METHODS- LECTURE 5 - updated 2018-01- 25 Page 5 22

Option 1 No functional continuity but finite function WW (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 finite element. CE 60130 FINITE ELEMENT METHODS- LECTURE 5 - updated 2018-01- 25 Page 6 22

(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 WW (0) space. CE 60130 FINITE ELEMENT METHODS- LECTURE 5 - updated 2018-01- 25 Page 7 22

Option 2 The function is continuous which defines the WW (1) = CC oo 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: uu = cc oo + cc 1 xx Thus we ve gone from an element measure to a nodal measure. An interpolating function defined with nodal functional values and WW (1) = CC oo continuity is called a Lagrange interpolating function. CE 60130 FINITE ELEMENT METHODS- LECTURE 5 - updated 2018-01- 25 Page 8 22

(b) We can use higher degree functions within each element (i.e. more nodes per element) however functional continuity will still only be WW (1). For example: uu = cc oo + cc 1 xx + cc 2 xx 2 + cc 3 xx 3 CE 60130 FINITE ELEMENT METHODS- LECTURE 5 - updated 2018-01- 25 Page 9 22

Option 3 The function and first derivative continuous defines the WW (2) = CC 1 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: uu = cc oo + cc 1 xx + cc 2 xx 2 + cc 3 xx 3 Therefore u and uu,xx are the unknowns. This involves 4 unknowns per element, 2 unknowns per node. Interpolating functions defined with nodal functional and first derivative values with WW (2) = CC 1 continuity are called Hermite Interpolating functions. CE 60130 FINITE ELEMENT METHODS- LECTURE 5 - updated 2018-01- 25 Page 10 22

1 st order Hermite: uu and uu,xx continuous 2 nd order Hermite: uu, uu,xx and uu,xxxx continuous 3 unknowns per node Note 1 For the Galerkin method, ww jj = φφ jj The fundamental weak form requires different order functional continuity for φφ jj as trial functions than the ww jj (or φφ jj as test) functions. The symmetrical weak form is obtained by integration by parts until the space requirements for φφ jj and ww jj are the same. This is the most attractive form to use. We note that the number of unknowns has been minimized. CE 60130 FINITE ELEMENT METHODS- LECTURE 5 - updated 2018-01- 25 Page 11 22

Example Fundamental weak form: dd2 uu aaaaaa ddxx 2 0 1 + uu aaaaaa xx ww jj dddd + gg dduu aaaaaa dddd ww jj xx=1 ww jj LL 2 and uu aaaaaa (or φφ ii ) WW (2), jj = 1, NN = 0 jj = 1, NN Therefore we must choose ww jj and φφ jj WW (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 1 st derivative). Thus we require Hermite interpolation Symmetrical Weak Form dddd aaaaaa dddd 0 1 dddd jj dddd + uuuu jj + xxxx jj dddd + gggg jj xx=1 = 0 jj = 1, NN CE 60130 FINITE ELEMENT METHODS- LECTURE 5 - updated 2018-01- 25 Page 12 22

The opposite of the fundamental weak form is obtained by interchanging uu aaaaaa and ww jj and leads to the B.E.M form dddd 1 jj dddd uu aaaaaa 0 dd 2 ww jj + gggg jj xx=1 + uuuu jj + xxxx jj + uu aaaaaa dddd = 0 dddd2 0 1 jj = 1, NN Now ww jj WW (2) and uu aaaaaa (or φφ jj ) LL 2 CE 60130 FINITE ELEMENT METHODS- LECTURE 5 - updated 2018-01- 25 Page 13 22

Note 2 Alternative strategy for deriving the symmetrical weak form: Start with standard Galerkin formulation Integrate by parts Substitute in for the specified natural b.c. Example Standard Galerkin formulation Integrate by parts: 1 dd2 uu aaaaaa dddd 2 + uu aaaaaa + xx ww jj dddd = 0 0 dddd aaaaaa dddd 0 1 dddd aaaaaa dddd 0 1 dddd jj dddd + uuuu jj + xxxx jj dddd + dddd xx=1 aaaaaa dddd ww jj xx=0 dddd jj dddd + uuuu jj + xxxx jj dddd + dddd aaaaaa dddd ww jj xx=1 = 0 dduu aaaaaa dddd ww jj xx=0 = 0 CE 60130 FINITE ELEMENT METHODS- LECTURE 5 - updated 2018-01- 25 Page 14 22

However for our example case: dddd aaaaaa dddd xx=1 gg (specified natural b.c.) Substituting the above equation as well as ww jj xx=0 = 0 (since φφ jj satisfies the homogeneous form of the essential b.c.), leads to: dddd aaaaaa dddd 0 1 dddd jj dddd + uuuu jj + xxxx jj dddd + gggg jj xx=1 = 0 CE 60130 FINITE ELEMENT METHODS- LECTURE 5 - updated 2018-01- 25 Page 15 22

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, ww jj = δδ xx xx jj (the dirac delta function) which is not differentiable. dddd xx xx jj dddd does not exist. Therefore it is not possible to find any weak forms! Therefore for a 2 nd order differential operator LL we must use Hermite type interpolation compared to the Galerkin Symmetrical weak form for which we only needed Lagrange type interpolation. CE 60130 FINITE ELEMENT METHODS- LECTURE 5 - updated 2018-01- 25 Page 16 22

Note 4 Summary of Advantages of Weak Forms: Fundamental weak form has relaxed b.c. requirements. It s 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. s In addition when we define local trial functions on finite elements, it will be much simpler to satisfy the essential b.c. s 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 strictly enforcing the natural boundary condition dddd/dddd 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. In addition, part of the natural b.c. error falls out due to the way in which it was defined. CE 60130 FINITE ELEMENT METHODS- LECTURE 5 - updated 2018-01- 25 Page 17 22

Notes on a 4 th derivative operator problem Consider the equilibrium equation for a beam on an elastic foundation where v = beam displacement E = modulus of elasticity I = moment of inertia k = foundation constant p = distributed load on the beam EEEE dd4 vv + kkkk = pp(xx) ddxx4 CE 60130 FINITE ELEMENT METHODS- LECTURE 5 - updated 2018-01- 25 Page 18 22

Standard Galerkin ll LL(vv) pp, δδδδ = 0 EEEE dd4 vv + kkkk pp δδδδδδδδ = 0 dddd4 0 We can establish what the essential and natural b.c. s are by using the integration by parts procedure to find: LL(vv), δδδδ = LL (δδδδ), vv + [FF 1 (δδδδ)gg 1 (vv) + FF 2 (δδδδ)gg 2 (vv) FF 1 (vv)gg 1(δδδδ) FF 2 (vv)gg 2(δδδδ)]dddd We perform 2 integration by parts to find the bc s (assuming EI constant): LL(vv), δδδδ = EEEE dd2 vv dd 2 δδδδ ddxx 2 + kkkkkkkk dddd dddd2 0 ll + EEEE dd2 vv dddddd ddxx 2 dddd + EEEE dd3 xx=1 vv ddxx 3 δδδδ xx=0 CE 60130 FINITE ELEMENT METHODS- LECTURE 5 - updated 2018-01- 25 Page 19 22

This is halfway point of the integration by parts procedure and represent the symmetrical weak form: Hence the essential b.c. are: FF 1 (vv) = vv displacement FF 2 (vv) = dddd dddd slope the natural b.c. s are: GG 1 (vv) = EEEE dd3 vv ddxx3 = QQ applied shear GG 2 (vv) = +EEEE dd2 vv ddxx2 = MM applied moment 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 selfadjointness of the operator (which also establishes b.c. s). You want terms to drop later on! CE 60130 FINITE ELEMENT METHODS- LECTURE 5 - updated 2018-01- 25 Page 20 22

Natural boundary errors The error in the moment is: Ԑ BB = EEEE dd2 vv MM dddddd ddxx2 dddd A error in the shear is: Ԑ BB " = EEEE dd3 vv QQ {δδδδ} ddxx3 Weighted natural boundary errors A moment error is weighted by a rotation: Ԑ BB, dddddd dddd = EEEE dd2 vv ddxx 2 MM dddddd ddγ ddxx Γ NN A shear error is weighted by a displacement Ԑ " BB, δδδδ = EEEE dd3 vv ddxx 3 QQ {δδδδ} ddγ Γ NN CE 60130 FINITE ELEMENT METHODS- LECTURE 5 - updated 2018-01- 25 Page 21 22

Note that we must specify essential b.c. s somewhere! Boundary conditions must be specified in pairs for this problem Displacement and rotation are paired Shear and moment are paired 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. The total error equation for this problem is the fundamental weak form where Ԑ II, δδδδ + Ԑ BB, dddddd dddd + Ԑ BB ", δδδδ = 0 Ԑ II = EEEE dd4 vv + kkkk pp dddd4 The symmetrical weak form is established by integrating the fundamental weak form by parts. CE 60130 FINITE ELEMENT METHODS- LECTURE 5 - updated 2018-01- 25 Page 22 22