In a seismic profile, the amplitude of time and space can be expressed as:
|
(1) |
where
is a set of orthogonal polynomials and is the number of basis functions and
is a set of coefficients. The is a unit basis function that satisfies the condition:
|
(2) |
where
denotes the Kronecker delta. The spectrum defined by denotes the energy distribution of the domain data in the orthogonal polynomials transform domain. Besides, the low-order coefficients represent the effective energy and the high-order coefficients represent the random noise energy. We provide a detailed introduction about how we construct the orthogonal polynomial basis function in Appendix A.
In a matrix-multiplication form, equation 1 can be expressed as the following equation
|
(3) |
where
is constructed from ,
is constructed from ,
is constructed from .
is known and
can be constructed using the way introduced in Appendix A. The unknown is
.
can be obtained by inverting the equation 3
|
(4) |
where denotes matrix tranpose.
In this paper, we choose , which indicates that we select 20 orthogonal polynomial basis function to represent the seismic data. Hence, inverting equation
is simply inverting a
matrix and is computationally efficient.
In the OPT method, we need to define the order of coefficients we want to preserve, the process of which corresponds to applying a mask operator to the orthogonal polynomial coefficients. Mask operator can be chosen to preserve low-order coefficients and reject high-order coefficients. It takes the following form:
|
(5) |
where
denotes the mask operator, denotes the orthogonal polynomial coefficients at time and order .
The coefficients after applying the mask operator 5 become
|
(6) |
The useful signals can be reconstructed by
|
(7) |
where
denotes the denoised data.
2020-03-27