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用垂直阵确定浅海波导特性 被引量:2

Waveguide characterization estimation in shallow water using a vertical array
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摘要 本文介绍利用声场复简正波近似确定浅海波导特性的方法。该方法的优点在于:(1)对环境参数的依赖程度大大降低。(2)在对海底介质结构(诸如层的数量、层的厚度、纵波和横波的速度和衰减等)知之不多或根本不了解的情况下,可同时获得波导特性参数(km,βm)。(3)确定波导海底界面平面波的反射系数V(k)。数值结果显示:对海底是单层或两层软固态的波导,用90M长、18阵元组成的垂直接收阵,接收频率分别为250Hz、150Hz的声信号,(1)获得的简正波水平波数km的精度均在10-5以上;简正波衰减系数βm的相对误差绝大部分在20%以内,其中前几号都在10%范围内,且简正波号数越低,误差越小。(2)基本反映海底在小掠角的反射相移和反射损失。本文在数值仿真的基础上,重点分析声场复简正波近似对93年冬季海上实验数据的处理结果。 Abstract: Waveguide characterization estimation in shallow water using the complex mode approxi metion of acoustic field is presented. The advantages of the method are that (l) the dependence on the environment parameters will obviously decrease. (2) the waveguide characterization parameters(km, βm )can be obtained the same time, when the fine structure in the bottom medium, such as the number and thickness of layers, the velocity of compressive and shear wave, and attenuation is less known or unknown. (3) it can extract the bottom reflection coefficient V(k). Numerical examples illustrate that (1) the accuracy of km is at least 10-5, the related error of βm is mostly less than 20%, and the smaller the mode number, the smaller the related error is; (2) the reflection coefficient in the the bottom at low grazing angle can be obtained using by a vertical array which the total number of samples is N = 18 and length L =90 m. The experimental data of 500 Hz is emphatically discussed here. The results for f =500 Hz wide impulse acoustic signal source which locates at Zs=11 m, rs=21 km show that the extracted accuracy of km is between 10-4 and 10-5, the related error of βm is between 9% and 26%.
作者 蒋德军
出处 《声学学报》 EI CSCD 北大核心 1997年第4期357-364,共8页 Acta Acustica
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参考文献4

  • 1Gao T F,Chin J Acoust,1996年,15卷,2期,157页
  • 2Shang E C,J Aoust Soc Am,1987年,83卷,103页
  • 3蒋德军,International conference on shallow water acoustics in 1997
  • 4蒋德军,声学学报

同被引文献23

  • 1金国亮,张仁和,候温良.负跃层浅海声传播的一个新现象──远程传播中的海底散射波[J].声学学报,1996,21(6):905-911. 被引量:5
  • 2卢博 黄韶健 张福生.东海大陆架某海区海底沉积物及其声学物理性质[J].声学技术,2002,(2002):42-42.
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  • 5Potty G R, Miller G M, Lynch G M and Smith K B. Tomographic inversion for sediment parameter in shallow water.J. Acoust. Soc. Am., 2000, 108(3): 973-986.
  • 6Munch W H and Wunsch C. Ocean acoustic tomagraphay:A scheme for scale monitoring. Deep Sea Res., 1979; 26:123-161.
  • 7Vaccaro R J. The past, present, and future of underwater acoustic signal processing. IEEE Signal Processing Mag.,1998; 7(1): 21-51.
  • 8Narasimhan S, Krolik J L. Fundamental limits on acoustic source range estimation performance in uncertain ocean channels. J. Acoust. Soc. Am., 1995; 97(1): 215-266.
  • 9Dosso S E, Brooke G H, Kilistoff S J et al. High-precision array element localization for vertical line arrays in the Arctic Ocean. IEEE Journal of Oceanic Engineering, 1998;23(4): 365-379.
  • 10Chapman N R, Yeremy M L. Matched field source localization with a horizontal line array. Journal of Computational Acoustic, 1994; 2(3): 315-325.

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