Algorithm for Surface Wave Suppression on 2D Seismic Data Using the Slant Karhunen–Loeve Transform in a Time-Frequency Domain

A. Yablokov, M.V. Moiseev, A. Serdyukov, D.A. Litvichenko
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Abstract

—Surface waves are the main source of coherent noise in land seismic survey, and their suppression is one of the main stages of common depth point data processing designed to improve the quality of tracking primary reflections on time sections. In practice, noise reduction is carried out using procedures from modern software based on numerical modeling of waveforms. However, they are too resource-intensive and have a large number of subjectively customizable parameters. The known algorithms have a common drawback: either the energy of reflected waves is distorted in an interference zone with a noise wave or the noise suppression quality is unsatisfactory. The current research is aimed at improving the filtering algorithm in a time-frequency domain using the slant Karhunen–Loeve transform in order to overcome these limitations, to increase the accuracy and rate of its software implementation, and also to test it when processing profile field data from land-based 2D seismic surveys. The algorithm is modified by developing a new method for determining static corrections for surface wave hodograph rectification in a time-frequency domain and by the application of preprocessing in which the reflected wave signal is removed preliminarily. These and other modifications ensure faster calculations and improve the quality of surface wave interference suppression. In addition, the slant Karhunen–Loeve transform is accelerated by parallelizing calculations across logical processor cores. In this paper, the algorithm is described in detail, its significant advantage over the standard methods of bandpass filtering and F–K filtering is shown, and the results of processing the field data obtained by the SWANA procedure (Geovation 2.0) and by the slant Karhunen–Loeve transform. The result obtained by the slant Karhunen–Loeve transform is superior to the SWANA procedure in terms of the surface wave filtering quality and has only four adjustable parameters (SWANA has 20 parameters)
在时频域使用斜卡尔胡宁-洛夫变换对二维地震数据进行面波抑制的算法
-地表波是陆地地震勘探中相干噪声的主要来源,抑制地表波是普通深度点数据处理的主要阶段之一,旨在提高时间剖面上一次反射的跟踪质量。实际上,降噪是利用基于波形数值建模的现代软件程序进行的。然而,这些程序过于耗费资源,而且有大量可主观定制的参数。已知的算法都有一个共同的缺点:要么反射波的能量在与噪声波的干扰区域被扭曲,要么噪声抑制质量不尽人意。目前的研究旨在利用斜卡尔胡宁-洛夫变换改进时频域滤波算法,以克服这些局限性,提高其软件实施的精度和速度,并在处理陆基二维地震勘探的剖面现场数据时对其进行测试。通过开发一种新的方法来确定时频域中表面波霍多图校正的静态校正,并通过应用预处理(初步去除反射波信号)对算法进行了修改。这些及其他修改确保了更快的计算速度,并提高了面波干扰抑制的质量。此外,通过在逻辑处理器内核之间并行计算,斜卡尔胡宁-洛夫变换也得到了加速。本文详细描述了该算法,展示了它相对于带通滤波和 F-K 滤波标准方法的显著优势,以及通过 SWANA 程序(Geovation 2.0)和斜卡休宁-洛夫变换获得的野外数据处理结果。就表面波滤波质量而言,斜卡尔胡宁-洛夫变换得到的结果优于 SWANA 程序,而且只有四个可调参数(SWANA 有 20 个参数)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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