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Generalized inverse of a matrix

The generation of the inverse square root of a matrix is a special case of the calculation of a general function of a matrix... [Pg.481]

Both the inversion of a matrix and the multiplication of a vector by a matrix irrvolve a great plenty of elementary calculations, for which reason they are corrverriently achieved by a computer. Already general-use spreadsheet apphcatiorrs like Excel provide high-level commands MINV for matrix inversion and MMULT for matrix multiphcation. [Pg.190]

The time derivative 9W/9t can be obtained from discretized forms of the partial derivatives of the atmospheric model as described later. However, because we do not know the value of t, we approximate (9 W ldt)t=r att = to. In this case, the time extrapolation is explicit. If we approximate (9W/9t)f=T at t = to -I- At, the procedure of Eq. (15) is called implicit because the evaluation of (9W/9t), i at t = to -I- At requires the value of W at to -I- At, which is still unknown at to. Hence, an implicit scheme requires some kind of iteration or inversion of a matrix for the calculation of 9W/9t and generally is time consuming to solve. In any case, repetition of Eq. (15) will yield a prediction of W for any later time. [Pg.369]

The matrix (C) is called the generalized inverse of C. Having estimated the matrix K, one can then estimate the amounts of analytes in an unknown sample. If the number of sensors is equal to the number of analytes, iCis a square matrix. If K exists then... [Pg.427]

It should be noted that in the case of a singular matrix A, the dimensions of V and A are pxr and rxr, respectively, where r is smaller than p. The expression in eq. (29.53) allows us to compute the generalized inverse, specifically the Moore-Penrose inverse, of a symmetric matrix A from the expression ... [Pg.38]

Let us examine these symbolic transformations with a view toward seeing how they translate into the required arithmetic operations that will provide the answers to the original simultaneous equations. There are two key operations involved. The first is the inversion of the matrix, to provide the inverse matrix. This is an extremely intensive computational task, so much so that it is in general done only on computers, except in the simplest cases for pedagogical purposes, such as we did in our previous chapter. [Pg.26]

A matrix of independent variables, defined for a linear model in Eq. (29) and for nonlinear models in Eq. (43) Transpose of matrix X Inverse of the matrix X Conversion in reactor A generalized independent variable... [Pg.180]

For the valence bond orbitals themselves, it is generally natural to specify a starting guess in the AO basis. Such a guess might, of course, not lie entirely inside the space spanned by the active space, and it must therefore be projected onto the space of the active MOs. This is achieved trivially in CASVB, by multiplication by the inverse of the matrix of MO coefficients. [Pg.315]

However, one has to keep in mind that [C] is not really known, only a model exists. Now [A] can be estimated with the generalized inverse of the model matrix ... [Pg.81]

Afh (q) is the current element of a matrix A (q) called the constraint-matrix. A (q) is a real symmetric matrix whose diagonal elements are positive it depends on the generalized coordinates as variables and parametrically on the constraints. This matrix possesses an inverse since det A(q) = 0 is not possible it would correspond to a supplementary relationship between the coordinates only, i.e a supplementary holonomic constraint. [Pg.25]

For the numerical study of the whole spectrum (for g R fixed), [79] uses a spectral tau-Chebychev discretization in y and the Arnold method (see [88]) to solve the generalized eigenvalue problem (see [89]). This numerical method is based on the orthonormalization of the Krylov space of the iterates of the inverse of the matrix A B. This method has been used more recently in [90]. It has been proven efficient in the stiff problems arising in the study of spectral stability of viscoelastic fluids. [Pg.224]

The inverse mapping from the c space to the c space is equally important as the forward mapping, not only because it provides a link between the lumped species and the original species, but because its existence is a necessary and sufficient condition for exact lumping. For a reduced system hstandard definition of an inverse will not apply. Therefore, we use the concept of a generalized inverse. The generalized inverse of an m X n matrix A satisfies the following criteria ... [Pg.344]

Although this solution appears to be straightforward, it is well documented in the lilerature [6,8-10] that small errors in p, (i.e., quadrature and experimental errors) result in large errors in p. The amplification of errors occurs independently of the fact that the inverse of (A A) can be calculated exactly, and it is a direct consequence of the near singularity of the matrix A (if m=n), or more generally (if m>n) of its near incomplete rank. [Pg.272]

In algebra, a number multiplied by its inverse results in a value of 1. In matrix algebra, the inverse of a square matrix (denoted by a superscript T) multiplied by itself results in the identity matrix. In other words, the inverse of X is the matrix X-1 such that XX-1 = X-1X = I. Two matrices are said to be orthogonal or independent if XYT = I. The inverse of an orthogonal matrix is its transpose. Not all matrices can be inverted. However, one condition for inversion is that the matrix must be square. Sometimes an inverse to a matrix cannot be found, particularly if the matrix has a number of linearly dependent column. In such a case, a generalized estimate of inverted matrix can be estimated using a Moore Penrose inverse (denoted as superscript e.g., X-). [Pg.342]

Since the quantum chemical calculation of energy and derivatives is easiest in the Cartesian space, it is necessary to convert these values to, and from, internals. Although the transformation from Cartesian coordinates to internals (minimal or redundant) is straightforward for the positions, the transformation of Cartesian gradients and Hessians requires a generalized inverse of the transformation matrix [49] viz. [Pg.201]

The matrix of phenomenological coefficients and Kki are related by K = where is the inverse of the matrix L. In a general matrix form in terms of the conductance Lq and resistance Kq coefficients becomes... [Pg.154]


See other pages where Generalized inverse of a matrix is mentioned: [Pg.9]    [Pg.129]    [Pg.11]    [Pg.195]    [Pg.9]    [Pg.129]    [Pg.11]    [Pg.195]    [Pg.131]    [Pg.71]    [Pg.164]    [Pg.1502]    [Pg.251]    [Pg.63]    [Pg.114]    [Pg.159]    [Pg.35]    [Pg.65]    [Pg.251]    [Pg.202]    [Pg.198]    [Pg.326]    [Pg.64]    [Pg.133]    [Pg.268]    [Pg.310]    [Pg.289]    [Pg.158]    [Pg.54]    [Pg.158]    [Pg.48]    [Pg.408]    [Pg.223]   
See also in sourсe #XX -- [ Pg.9 ]

See also in sourсe #XX -- [ Pg.9 ]




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