Sylvester's formula

Sylvester's formula

In matrix theory, Sylvester's formula, named after James Joseph Sylvester, expresses matrix functions in terms of the eigenvalues and eigenvectors of a matrix. It is only valid for diagonalizable matrices; an extension due to Buchheim covers the general case.

Statement

Let "A" be a diagonalizable matrix with "k" distinct eigenvalues, λ1, …, λ"k". The Frobenius covariants "A""i" are defined by: A_i = prod_{j=1 atop j e i}^k frac{1}{lambda_i-lambda_j} (A - lambda_j I). [Horn & Johnson, equation (6.1.36)] The Frobenius covariants "A""i" are projections on the eigenspace associated with λ"i". They can be found by diagonalizing the matrix "A". using the eigendecomposition "A" = "SDS"−1. First, suppose that "A" has no multiple eigenvalues. Let "A" = "SDS"−1 be the eigendecomposition of "A" where the diagonal matrix "D" has the eigenvalues λ1, …, λ"k" (in that order) on the diagonal. Denote the "i"th column of "S" by "c""i" and the "i"th row of "S"−1 by "r""i"; "c""i" and "r""i" are left and right eigenvectors of "A"). Then "A""i" = "c""i""r""i". If "A" has multiple eigenvalues then "A""i" = Σ"j" "c""j""r""j", where the sum is over all rows and columns associated with the eigenvalue λ"i". [Horn & Johnson, page 521]

Now, let "f": "D" → C with "D" ⊂ C be a function for which "f"("A") is well defined; this means that every eigenvalue λ"i" is in the domain "D" and that every λ"i" with multiplicity "m""i" is in the interior of the domain with "f" ("m""i" − 1) times differentiable at λ"i". [Horn & Johnson, Definition 6.4] Then, Sylvester's formula states that: f(A) = sum_{i=1}^k f(lambda_i) A_i. [Horn & Johnson, equation (6.2.39)]

Example

Consider the two-by-two matrix:: A = egin{bmatrix} 1 & 3 \ 4 & 2 end{bmatrix}.This matrix has two eigenvalues, 5 and −2. Its eigendecomposition is: A = egin{bmatrix} 3 & 1/7 \ 4 & -1/7 end{bmatrix} egin{bmatrix} 5 & 0 \ 0 & -2 end{bmatrix} egin{bmatrix} 3 & 1/7 \ 4 & -1/7 end{bmatrix}^{-1} = egin{bmatrix} 3 & 1/7 \ 4 & -1/7 end{bmatrix} egin{bmatrix} 5 & 0 \ 0 & -2 end{bmatrix} egin{bmatrix} 1/7 & 1/7 \ 4 & -3 end{bmatrix}. Hence the Frobenius covariants are: egin{align}A_1 &= c_1 r_1 = egin{bmatrix} 3 \ 4 end{bmatrix} egin{bmatrix} 1/7 & 1/7 end{bmatrix} = egin{bmatrix} 3/7 & 3/7 \ 4/7 & 4/7 end{bmatrix} \A_2 &= c_2 r_2 = egin{bmatrix} 1/7 \ -1/7 end{bmatrix} egin{bmatrix} 4 & -3 end{bmatrix} = egin{bmatrix} 4/7 & -3/7 \ -4/7 & 3/7 end{bmatrix}.end{align} Sylvester's formula states that: f(A) = f(5) A_1 + f(-2) A_2. , For instance, if "f" is defined by "f"("x") = "x"−1, then Sylvester's formula computes the matrix inverse "f"("A") = "A"−1 as: frac{1}{5} egin{bmatrix} 3/7 & 3/7 \ 4/7 & 4/7 end{bmatrix} - frac{1}{2} egin{bmatrix} 4/7 & -3/7 \ -4/7 & 3/7 end{bmatrix} = egin{bmatrix} -0.2 & 0.3 \ 0.4 & -0.1 end{bmatrix}.

Notes

References

* citation | first1=Roger A. | last1=Horn | first2=Charles R. | last2=Johnson | year=1991 | title=Topics in Matrix Analysis | publisher=Cambridge University Press | isbn=9780521467131 .

External links

* Jon F. Claerbout, [http://sepwww.stanford.edu/ftp/prof/fgdp/c5/paper_html/node3.html Sylvester's matrix theorem] , a section of "Fundamentals of Geophysical Data Processing", published in 1976.


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