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    基于变水速模型驱动的深水水层多次波压制技术研究与应用

    Research and application on deepwater water-layer multiple elimination technology based on variable water velocity model

    • 摘要: 深水地震资料处理中, 水层多次波因深水水层为变速体的特性, 无法应用浅水水层多次波压制技术(Shallow Water Multiple Attenuation, SWMA)进行压制, 而传统的自由界面多次波压制技术(Surface-Related Multiple Elimination, SRME)压制水层多次波则不具有针对性。为此, 开展了基于变水速模型驱动的深水水层多次波压制技术(Deepwater Water-layer Multiple Elimination, DWME)研究。该技术通过构建海底和变水速模型计算出水层多次波准确旅行时, 在τ-p域根据水层多次波旅行时将地震数据进行延拓, 得到水层多次波模型, 然后应用自适应匹配相减方法完成水层多次波压制。理论模型验证及海外某工区实际地震资料应用结果表明, DWME对深水水层多次波压制效果较好, 且针对性强。

       

      Abstract: It is difficult to attenuate deepwater water-layer multiple using the shallow water multiple attenuation (SWMA) method or the conventional surface-related multiple elimination (SRME) method, because the deepwater water-layer velocity is not constant.This paper proposes a deepwater water-layer multiple elimination (DWME) method driven by a variable water velocity model.The method first estimates the water-layer multiple travel-time by building the sea bottom model and variable water velocity model.Then, seismic data wave field extrapolation is performed according to the estimated travel-time in the τ-p domain to predict water-layer multiple.Finally, the adaptive matching subtraction is applied to eliminate the multiples.Testing results on both synthetic data and field data show that the DWME can effectively suppress deepwater water-layer multiples.

       

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