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水平层状海底Scholte波频散特性

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海底Scholte波沿着海底流—固界面传播,具有典型的频散特性.Scholte波的频散特性可以反演海底浅层的横波速度,是海底横波速度建模的有效手段.建立准确的Scholte波频散理论模型至关重要.根据真实海水—海底环境建立水平层状海水—海底弹性模型,并利用边界应力和位移连续性条件推导了该模型的Scholte波频散方程及位移方程.分析了海水深度和海底物性参数对Scholte波频散特性的影响,6层海水—海底模型实验结果表明:①无论是硬海底还是软海底,Scholte波都具有明显的频散特性,硬海底Scholte波能量主要集中在海水中,基阶能量最弱,2阶能量最强,随着海水深度增加,Scholte波频散特性减弱;软海底模型固体海底的Scholte波能量明显增强,此时海水深度对Scholte波频散特性影响很小.②相比于深海环境,浅海Scholte波能量更强,频散特征更明显,因此在浅海环境利用Scholte波反演海底浅层横波速度的精度和可信度更高.最后,基于东海某工区的实际海底弹性地质模型模拟海底多分量地震数据并从中提取频散曲线,与理论计算的频散曲线进行对比分析,二者的频散曲线吻合很好,验证了所提理论方法的正确性.
Dispersion characteristics of Scholte waves on horizontal layered seabed
Scholte waves propagate along the seafloor fluid-solid interface and exhibit typical dispersion charac-teristics.The dispersion properties of Scholte waves can be utilized for the inversion of the shear wave velocity of the shallow seabed,making it an effective tool for seabed shear wave velocity modeling.It is of critical im-portance to establish the theoretical model of Scholte wave dispersion.In this study,a horizontal layered model of seawater-seabed elasticity is developed based on a real seawater-seabed environment.The dispersion equa-tion and displacement equation for Scholte waves in this model are derived using the continuity conditions of boundary stress and displacement.The influence of seawater depth and seabed property parameters on the dis-persion characteristics of Scholte waves is analyzed.Experimental results using a 6-layer seawater-seabed model show that:①Regardless of the seabed is hard or soft,Scholte waves exhibit distinct dispersion charac-teristics.In the case of a hard seabed,the energy of Scholte waves is mainly concentrated in the seawater,with the fundamental mode having the weakest energy and the second mode having the strongest energy.As the sea-water depth increases,the dispersion characteristics of Scholte waves weaken.For the soft seabed model,the energy of Scholte waves on the solid seabed significantly increases,and the seawater depth has little effect on Scholte wave dispersion characteristics.②Compared with deep-water environments,Scholte waves have stron-ger energy and more pronounced dispersion characteristics in shallow water.Therefore,utilizing Scholte waves for inverting the shallow seabed shear wave velocity in shallow water environments yields higher accuracy and reliability.Finally,based on an actual seabed elastic geological model of a working area in the East China Sea,multi-component seismic data are simulated,and dispersion curves are extracted.A comparison analysis be-tween the theoretically calculated dispersion curves and the extracted dispersion curves shows a good agree-ment,confirming the accuracy of our theoretical approach.

Scholte wavehorizontal and layered seabeddispersion characteristicsamplitude-depth distributionshear wave velocity

于鹏飞、陈隽琳、江佳萌、杨小慧

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河海大学海洋学院,江苏南京 210024

中国石化石油物探技术研究院,江苏南京 211103

Scholte波 水平层状海底 频散特性 振幅深度分布 横波速度

国家自然科学基金江苏省自然科学基金

42074149BK20201318

2024

石油地球物理勘探
东方地球物理勘探有限责任公司

石油地球物理勘探

CSTPCD北大核心
影响因子:1.766
ISSN:1000-7210
年,卷(期):2024.59(2)
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