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首页> 外文期刊>Defence Science Journal >Estimation of Compressional Wave Speed in Marine Sediments using Biot-Stoll Model and Buckingham's Grain-shearing Model
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Estimation of Compressional Wave Speed in Marine Sediments using Biot-Stoll Model and Buckingham's Grain-shearing Model

机译:使用Biot-Stoll模型和白金汉粉碎模型估算海洋沉积物中的压缩波速

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摘要

Acoustic properties of seafloor sediments can be estimated using theoretical models by giving geophysical properties of sediments as inputs to the respective models. Empirical relations connecting the geophysical and geoacoustic properties are available in literature. In this study an experimental assessment of two such theoretical models viz., Biot-Stoll model (BSM), a poro-elastic model and the Buckingham's grain shearing (GS) model, a visco-elastic model is done by estimating the compressional wave speed. Compressional wave speed is measured using in-house developed sediment velocimeter and is compared with the speed estimated using both the models and a regression analysis was done. It was observed that the Coefficient of determination R-2 for BSM and GS model are 0.769 and 0.729, respectively. It shows that once the constants used in GS model are evaluated for the Indian waters, then it can be used to estimate the acoustic properties of sediments.
机译:通过将沉积物的地球物理特性作为输入到各个模型的输入,可以估计海底沉积物的声学特性。连接地球物理和地理声学特性的实证关系在文献中提供。在这项研究中,通过估计压缩波速来完成对两个这样的理论模型的实验评估。,Biot-STOLS模型(BSM),Poro-Ellast型号(BSM),孔隙弹性模型和白金素剪切(GS)模型,通过估计压缩波速来完成粘弹性模型。使用内部开发的沉积物速度计测量压缩波速,并与使用模型和回归分析进行比较。观察到,BSM和GS模型的测定系数分别为0.769和0.729。它表明,一旦GS模型中使用的常数被评估印度水域,那么它可以用于估计沉积物的声学特性。

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