深水全波形反演及适配采集观测系统设计

    Full-waveform inversion for deep water and adaptive acquisition geometry design

    • 摘要: 全波形反演(FWI)是高精度速度建模的核心技术,常规最小二乘回折波FWI存在反演精度有限、有效反演深度不足等问题,难以满足深水复杂断裂区建模需求。为此,本文以相位驱动全波形反演为核心,针对深水复杂断裂地质条件开展高精度速度建模研究。算法层面,通过优化目标函数,强化纵波相位信息利用,弱化FWI对低频回折波振幅的强依赖,提升反演稳定性与有效反演深度;数据层面,优化拖缆长度、道间距等关键采集参数,改善排列覆盖次数与采集密度,实现观测系统与反演技术的协同适配。数值模拟与实际工区应用表明,相位驱动FWI可有效突破传统回折波FWI反演深度对排列长度的强依赖,显著提升速度反演精度;观测系统优化试验显示,适当减小道间距可有效提高FWI反演精度,合理增加排列长度有助于提升深层速度反演稳定性。本文提出的相位驱动FWI速度建模及配套观测系统优化方案,明确了深水复杂断裂区相位驱动FWI的技术优势与适配观测系统设计原则,可为类似区域高精度速度建模提供可靠技术支撑与理论参考。

       

      Abstract: The full waveform inversion (FWI) is a core technology for high-precision velocity modeling. However, conventional least-squares diving-wave FWI is limited by insufficient inversion accuracy and depth, failing to meet the velocity modeling needs from deep-water complex fault zones. Taking phase-driven FWI as the key issue,high-precision velocity modeling under deep-water complex fault conditions was conducted. At algorithm level, the FWI objective function was optimized to enhance the utilization of P-wave phase information and reduce FWI’s dependence on the amplitude of low-frequency diving waves, improving inversion stability and effective depth. At data level, key acquisition parameters (e.g., streamer length, trace interval) were optimized to improve fold coverage and acquisition density, by which the adaptation between acquisition geometry and FWI was realized. The results were then verified via numerical simulations and seismic data, showing that phase-driven FWI could effectively reduce the dependence of traditional diving-wave FWI on spread length and improve the velocity inversion accuracy. Moreover, optimization tests on the acquisition geometry indicated that, appropriately reducing the trace interval could enhance the FWI inversion accuracy, while reasonably increasing the spread length could improve the stability of deep velocity inversion. This study demonstrated the technical advantages of phase-driven FWI and the design principles of matched acquisition geometry for deep-water complex fault zones, and provided a reliable technical support and theoretical reference for high-precision velocity modeling in similar areas.

       

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