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沉积层海底界面Scholte波水池实验

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海底界面Scholte波具有衰减小、传播距离远等特点,可应用于水下目标探测与海底参数反演.在实际海洋环境中,海水与弹性海底之间的沉积层会对Scholte波的激发和传播产生显著影响.该文利用缩比原理设计并开展水池实验研究,将实际海洋环境按1:5000的比例缩比至实验室水池尺度,利用声压场Scholte波识别方法在包含沉积层的实验环境下对Scholte波的激发与传播规律进行探究.实验结果表明,该实验条件下,1mm厚度的沉积层时海底界面依然有Scholte 波激发,但沉积层的存在会增大其衰减;而厚度超过1mm的沉积层会导致Scholte波无法激发.根据缩比原理,实验环境对应为声源频率10 Hz、水深3000 m、沉积层厚度5m的实际海洋环境,即在上述实际海洋环境中,海底界面Scholte波仍可以正常激发,而厚度大于5m的粉沙质沉积层会导致Scholte波无法激发.
Sediment's influence on Scholte wave by tank experiment
With less attenuation and longer transmission distance,Scholte waves at the seafloor interface can be applied in underwater target detection and seafloor parameter inversion.In the real ocean,the sediment between the seawater and the elastic seafloor could significantly affect the excitation and propagation of Scholte waves.In this paper,by scaling down the real ocean environment to laboratory scale according to the scale principle,a tank experiment is designed and carried out to investigate the excitation and propagation of Scholte waves in an experimental environment containing sediment using Scholte wave identification method based on acoustic pressure field measurement.It is shown in results that under the experimental conditions,Scholte waves could still be excited at the seafloor interface with the sediment of 1 mm thickness,but the sediment increases its attenuation;and the thicker sediment would prevent Scholte waves'excitation.According to the scaling principle,the experimental environment can be converted to the real ocean environment with a source frequency of 10 Hz,a water depth of 3000 m and a sediment thickness of 5 m,i.e.,in the above-mentioned real ocean environment,Scholte waves at the seafloor could be excited normally,and slit sediment thicker than 5 m would cause the failure of Scholte waves'excitation.

Scholte waveTank experimentModal decompositionSediment

王志超、梁民帅、李东林、郁高坤、彭临慧

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中国海洋大学海洋技术系 青岛 266100

Scholte波 水池实验 模态分离 沉积层

声场声信息国家重点实验室开放课题国家自然科学基金项目

SKLA20220611474258

2024

应用声学
中国科学院声学研究所

应用声学

CSTPCD北大核心
影响因子:1.128
ISSN:1000-310X
年,卷(期):2024.43(5)