Everything about Sparse Matrix totally explained
In the
mathematical subfield of
numerical analysis a
sparse matrix is a
matrix populated primarily with zeros.
Conceptually, sparsity corresponds to systems which are loosely coupled. Consider a line of balls connected by springs from one to the next; this is a sparse system. By contrast, if the same line of balls had springs connecting every ball to every other ball, the system would be represented by a
dense matrix. The concept of sparsity is useful in
combinatorics and application areas such as
network theory, of a low density of significant data or connections.
Huge sparse matrices often appear in
science or
engineering when solving
partial differential equations.
When storing and manipulating sparse matrices on a
computer, it's beneficial and often necessary to use specialized
algorithms and
data structures that take advantage of the sparse structure of the matrix. Operations using standard matrix structures and algorithms are slow and consume large amounts of memory when applied to large sparse matrices. Sparse data is by nature easily
compressed, and this compression almost always results in significantly less
memory usage. Indeed, some very large sparse matrices are impossible to manipulate with the standard algorithms.
Storing a sparse matrix
The naive
data structure for a matrix is a two-dimensional array. Each entry in the array represents an element
ai,j of the matrix and can be accessed by the two indices
i and
j. For a
m×
n matrix we need at least enough memory to store (
m×
n) entries to represent the matrix.
Many if not most entries of a sparse matrix are zeros. The basic idea when storing sparse matrices is to store only the non-zero entries as opposed to storing all entries. Depending on the number and distribution of the non-zero entries, different
data structures can be used and yield huge savings in
memory when compared to a naïve approach.
One example of such a sparse matrix format is the (old) Yale Sparse Matrix Format[1]. It stores an initial sparse
m×
n matrix,
M, in row form using three one-dimensional arrays. Let
NNZ denote the number of nonzero entries of
M. The first array is
A, which is of length
NNZ, and holds all nonzero entries of
M in left-to-right top-to-bottom order. The second array is
IA, which is of length
(for example, one entry per row, plus one).
IA(i) contains the index in
A of the first nonzero element of row
i. Row
i of the original matrix extends from
A(IA(i)) to
A(IA(i+1)-1). The third array,
JA, contains the column index of each element of A, so it also is of length
NNZ.
For example, the matrix
[ 1 2 0 0 ]
[ 0 3 9 0 ]
[ 0 1 4 0 ]
is a three-by-four matrix with six nonzero elements, so
A = [ 1 2 3 9 1 4 ]
IA = [ 1 3 5 7 ]
JA = [ 1 2 2 3 2 3 ]
Another possibility is to use
quadtrees.
Example
A
bitmap image having only 2 colors, with one of them dominant (say a file that stores a handwritten
signature) can be encoded as a sparse matrix that contains only row and column numbers for
pixels with the non-dominant color.
Diagonal matrices
A very efficient structure for a
diagonal matrix is to store just the entries in the main diagonal as a one-dimensional array, so a diagonal
n×
n matrix requires only
n entries.
Bandwidth
The
lower bandwidth of a matrix
A is the smallest number
p such that the entry
aij vanishes whenever
i >
j + p. Similarly, the
upper bandwidth is the smallest
p such that
aij = 0 whenever
i <
j −
p . For example, a
tridiagonal matrix has lower bandwidth 1 and upper bandwidth 1.
Matrices with small upper and lower bandwidth are known as
band matrices and often lend themselves to simpler algorithms than general sparse matrices; one can sometimes apply dense matrix algorithms and simply loop over a reduced number of indices.
Reducing bandwidth
The
Cuthill-McKee algorithm can be used to reduce the bandwidth of a sparse
symmetric matrix. There are, however, matrices for which the
Reverse Cuthill-McKee algorithm performs better.
The
U.S. National Geodetic Survey (NGS) uses Dr. Richard Snay's "Banker's" algorithm because on realistic sparse matrices used in Geodesy work it has better performance.
There are many other methods in use.
Reducing fill-in
» "Fill-in" redirects here. For the puzzle, see Fill-In (puzzle).
The
fill-in of a matrix are those entries which change from an initial zero to a non-zero value during the execution of an algorithm. To reduce the memory requirements and the number of arithmetic operations used during an algorithm it's useful to minimize the fill-in by switching rows and columns in the matrix. The
symbolic Cholesky decomposition can be used to calculate the worst possible fill-in before doing the actual
Cholesky decomposition.
There are other methods than the
Cholesky decomposition in use. Orthogonalization methods (such as QR factorization) are common, for example, when solving problems by least squares methods. While the theoretical fill-in is still the same, in practical terms the "false non-zeros" can be different for different methods. And symbolic versions of those algorithms can be used in the same manner as the symbolic Cholesky to compute worst case fill-in.
Solving sparse matrix equations
Both
iterative and direct methods exist for sparse matrix solving. One popular iterative method is the
conjugate gradient method.
Further Information
Get more info on 'Sparse Matrix'.
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