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Tables of Orthogonal Polynomials

This is one of the variants of the finite element methods. The essence of orthogonal collocation (OC) is that a set of orthogonal polynomials is fitted to the unknown function, such that at every node point, there is an exact fit. The points are called collocation points, and the set of polynomials is chosen suitably, usually as Jacobi polynomials. The optimal choice of collocation points is to make them the roots of the polynomials. There are tables of such roots, and thus point placements, in Appendix A. The notable things here are the small number of points used (normally, about 10 or so will do), their... [Pg.173]

To use the Gauss formulae, it is necessary to know the zeroes of the polynomial Z and the weights Wi. They are tabled for many families of orthogonal polynomials and for many combinations of a and b and r x). [Pg.26]

When Pi x) is chosen to be the Legendre set of orthogonal polynomials [see Table 3.7], the weight w(a ) is unity. The standard interval of integration for Legendre poiynomials is [-1, 1]. The transformation equation (4.92) is used to transform the Legendre polynomials to the interval [ji , which applies to our problem at hand ... [Pg.326]

Based on the above assumptions, the model equations are shown in Table 4. The mass balance equations at the pellet and crystal level are based in the double linear driving model equations or bidisperse model[30]. The solution of the set of parabolic partial differential equations showed in Table 4 was performed using the method of lines. The spatial coordinate was discretized using the method of orthogonal collocation in finite elements. For each element 2 internal collocation points were used and the basis polynomial were calculated using the shifted Jacobi polynomials with weighting function W x) = (a = Q,p=G) hat has equidistant roots inside each element [31]. The set of discretized ordinary differential equations are then solved with DASPK solver [32] which is based on backward differentiation formulas. [Pg.380]

The 85th Edition includes updates and expansions of several tables, such as Aqueous Solubility of Organic Compounds, Thermal Conductivity of Liquids, and Table of the Isotopes. A new table on Azeotropic Data for Binary Mixtures has been added, as well as tables on Index of Refraction of Inorganic Crystals and Critical Solution Temperatures of Polymer Solutions. In response to user requests, several topics such as Coefficient of Friction and Miscibility of Organic Solvents have been restored to the Handbook. The latest recommended values of the Fundamental Physical Constants, released in December 2003, are included in this edition. Finally, the Appendix on Mathematical Tables has been revised by Dr. Daniel Zwillinger, editor of the CRC Standard Mathematical Tables and Formulae it includes new information on factorials, Clebsch-Gordan coefficients, orthogonal polynomials, statistical formulas, and other topics. [Pg.4]

These identities (7 and 11-13) form a very practical system of equations for the generation of the n a "anharmonic polynomials. In Table 4 we list first few and qj s. The present identities are sli tly more complicated than those of the classical orthogonal polynomials. For example the Hermite polynomials are defined by... [Pg.192]

Here, the permutations of j, k,l,... include all combinations which produce different terms. The multivariate Hermite polynomials are listed in Table 2.1 for orders < 6. Like the spherical harmonics, the Hermite polynomials form an orthogonal set of functions (Kendal and Stuart 1958, p. 156). [Pg.32]

The table below provides the roots of the Jacobi polynomials used as node points in orthogonal collocation, for some values of N. Values for X = 0 (i = 0) and X = 1 (i = N + 1) (the values are 0 and 1, resp.) are not included. The roots were computed using the subroutine JCOBI, modified from the original of Villadsen and Michelsen [562], discussed in Appendix C, using for a given N the call... [Pg.285]

Solution of the ag block of the Hiickel determinant for Cso leads to two linear combinations of ag irreducible symmetry. The first of these is the linear combination resulting from the projection of the lag polynomial of Table 3.20 on the 80 vertices, so that each coefficient is of equal value, while the second linear combination is identical to the one found by projecting the level 6 polynomial of the table onto the 80 vertices and rendering the result orthogonal to the first. [Pg.124]

Table 8.9 Matrices of First and Second Derivatives for Orthogonal Collocation Using Jacobi Polynomials (Source Finlayson, 1972)... Table 8.9 Matrices of First and Second Derivatives for Orthogonal Collocation Using Jacobi Polynomials (Source Finlayson, 1972)...
This polynomial, which is called the characteristic equation of matrix A, has n roots, which are the eigenvalues of A. These roots may be real distinct, real repeated, or complex, depending on matrix A (see Table 2.4). A nonsingular real symmetric matrix of order n has n real nonzero eigenvalues and n linearly independent eigenvectors. The eigenvectors of areal symmetric matrix are orthogonal to each other. The coefficients a, of the characteristic polynomial are functions of the matrix elements and must be delermined before the polynomial can be used. [Pg.122]

Table 1 Basis vectors of the D3Q19 model. Each row corresponds to a different basis vector, with the actual polynomial in Cia = Cia jc shown in the second column. The normalizing factor for each basis vector is in the third column. The polynomials form an orthogonal set when (f = (f (109)... Table 1 Basis vectors of the D3Q19 model. Each row corresponds to a different basis vector, with the actual polynomial in Cia = Cia jc shown in the second column. The normalizing factor for each basis vector is in the third column. The polynomials form an orthogonal set when (f = (f (109)...
There are several deficiencies in STO s. Because STO s replace the polynomial in r for a single term, STO s do not have the proper number of nodes and do not represent the inner part of an orbital well. Care must be taken when using STO s because orbitals with the different values of n but the same values of / and mi are not orthogonal to one another. Another deficiency is that ns orbitals where n > 1 have zero amplitude at the nucleus. Values have been obtained for the effective nuclear charge for a number of atoms by fitting STO s to numerically computed wavefunctions. These values are given Table 8-2 and supersede the values obtained empirically from Slater s rules. [Pg.203]


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