Nonstationary predictive filtering for seismic random noise suppression-A tutorial

被引:0
|
作者
Wang, Hang [1 ]
Chen, Wei [2 ]
Huang, Weilin [3 ]
Zu, Shaohuan [4 ]
Liu, Xingye [5 ]
Yang, Liuqing [3 ]
Chen, Yangkang [1 ]
机构
[1] Zhejiang Univ, Sch Earth Sci, Hangzhou 310027, Peoples R China
[2] Yangtze Univ, Key Lab Explorat Technol Oil & Gas Resources, Minist Educ, Daxue Rd 111, Wuhan 430100, Peoples R China
[3] China Univ Petr, State Key Lab Petr Resources & Prospecting, Fuxue Rd 18th, Beijing 102200, Peoples R China
[4] Chengdu Univ Technol, Coll Geophys, Chengdu 610059, Peoples R China
[5] Xian Univ Sci & Technol, Coll Geol & Environm, Xian 710054, Peoples R China
关键词
ATTENUATION; RECONSTRUCTION; REDUCTION;
D O I
10.1190/GEO2020-0368.1
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Predictive filtering (PF) in the frequency domain is one of the most widely used denoising algorithms in seismic data processing. PF is based on the assumption of linear or planar events in the time-space domain. In traditional PF methods, a predictive filter is fixed across the spatial dimension, which cannot deal with spatial variations in seismic data well. To handle the curved events, the predictive filter is either applied in local windows or extended into a nonstationary version. The regularized nonstationary autoregression (RNAR) method can be treated as a nonstationary extension of traditional PF, in which the predictive filter coefficients are variable in different spatial locations. This highly underdetermined inverse problem is solved by shaping regularization with a smoothness constraint in space. We further extend the RNAR method to the more general case, in which we can apply more constraints to the filter coefficients according to the features of seismic data. First, apart from the smoothness in space, we also apply a smoothing constraint in frequency, considering the coherency of the coefficients in the frequency dimension. Second, we apply a frequency-dependent smoothing radius in the spatial dimension to better take advantage of the nonstationarity of seismic data in the frequency axis and to better deal with noise. The effectiveness of our method is validated using several synthetic and field data examples.
引用
收藏
页码:W21 / W30
页数:10
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