-
声信号在海水中能够进行上千公里的传播，远距离声传播存在不同于近距离传播的特性。本文利用西太平洋声源与接收最远距离近2000km的远距离水声实验数据，对实验海区的海洋环境信息、实验使用的接收垂直阵信息进行处理，分析大洋完全声道环境下，远距离声传播能量衰减规律和多途到达结构特性。在远距离传播能量衰减规律方面，随着传播距离增加，海水吸收对声能衰减的作用凸显，海水吸收系数的选取对声场能量预报的准确性至关重要。较低频信号海水吸收较小，中心频率100Hz的声信号，传播距离从1000km到2000km，传播损失仅增加6dB左右。深海声道远距离声传播多途到达结构特性方面，实验海区温跃层声速较高，使得到达接收点的本征声线数目更多，多途到达结构更复杂，海面反射声线形成的到达结构处在整体到达结构的靠前位置，且能量相对较强；受西北太平洋副热带模态水的影响，声速剖面存在双跃层结构，导致部分声线到达接收点的时间较早，多途到达结构在时间轴上的长度延长。Acoustic signals can travel thousands of kilometers in seawater, and the characteristics of long-range sound propagation are different from short range propagation. This paper is based on a long-range underwater acoustic experiment data carried in the western Pacific Ocean, whose farthest propagation distance is nearly 2000km. The ocean environment information and vertical line array information are carefully processed. We analyze the attenuation in the seawater of long-distance acoustic propagation and multi-path arrival structure characteristics under the complete acoustic channel environment of the ocean. In terms of the attenuation law of long-distance propagation energy, with the increase of propagation distance, the effect of seawater absorption on the attenuation of sound energy becomes prominent, and the selection of absorption coefficient is very important for accurate prediction of sound field energy. Absorption in seawater of low frequency signals is small, and the transmission loss of acoustic signal with 100Hz center frequency only increases by about 6dB when the propagation distance is from 1000km to 2000km. In terms of multi-path arrival structure characteristics of deep-sea acoustic channel for long-distance sound propagation, the thermocline sound velocity profile in the experimental sea area has higher sound speed, which makes the number of eigenrays reaching the receiving point more and the multi-path arrival structure more complex. The arrival structure formed by sea surface reflected eigenrays is in the earlier position of the overall arrival structure and has relatively strong energy. Due to the influence of subtropical water over the northwest Pacific Ocean on the sound speed profile, the time of some eigenrays arriving at the receiving point is earlier, and the length of multi-way arrival structure on the time axis is prolonged.
-
Keywords:
- Long-rang sound propagation /
- transmission loss /
- arrival structure
-
[1] Worcester P F, Cornuelle B D, Hildebrand J A, Hodgkiss W, Spindel R C 1994 J. Acoust. Soc. Am. 95 3118
[2] Worcester P F, Cornuelle B D, Dzieciuch M A, Munk W H, Howe B M, Mercer J A, Spindel R C, Colosi J A, Metzger K, Birdsall T G 1999 J. Acoust. Soc. Am 105 3185
[3] Colosi J 2004 J. Acoust. Soc. Am 116 1538
[4] Vera M, Heaney K D 2005 J. Acoust. Soc. Am 117 1624
[5] Mercer J A, Colosi J A, Howe B M, Dzieciuch M A, Stephen R 2009 IEEE J. Oceanic.Eng. 34 1
[6] Worcester P F, Dzieciuch M A, Mercer J A, Andrew R K, Dushaw B D, Baggeroer A B, Heaney K D, D"Spain G L, Colosi J A, Stephen R A 2013 J. Acoust. Soc. Am 134 3359
[7] Li-Li WU, Zhao-Hui PENG 2015 Chin. Phys. Lett 32 9
[8] Guthrie A N 1974 J. Acoust. Soc. Am 56 58
[9] Beilis A 1983 J. Acoust. Soc. Am 68 171
[10] Boyles C A 1978 J. Acoust. Soc. Am 64 S74
[11] 张仁和, 何怡1994自然科学进展:国家重点实验室通讯 6 32
Zhang R H, He Y 1994 Progress in Natural Science. 6 32
[12] Colosi J A, Scheer E K, Flatté S, Cornuelle B D, Dzieciuch M A, Munk W H, Worcester P F, Howe B M, Mercer J A, Spindel R C 1999 J. Acoust. Soc. Am 105 3202
[13] Uffelen L V, Worcester P F, Dzieciuch M A, Rudnick D L 2009 J. Acoust. Soc. Am 125 3569
[14] Uffelen L V, Worcester P F, Dzieciuch M A, Rudnick D L, Colosi J A 2010 J. Acoust. Soc. Am 127 2169
[15] Kim H J 2009 Ph. D. Dissertation (Boston: Massachusetts Institute of Technolog
[16] Locarnini R A, Mishonov A V, Baranova O K, Boyer T P, Zweng M M, Garcia H E, Reagan J R, Seidov D, Weathers K, Paver C R, Smolyar I 2018 World Ocean Atlas 2018, Volume 1: Temperature. 81 p52
[17] Zweng M M, Reagan J R, Seidov D, Boyer T P, Locarnini R A, Garcia H E, Mishonov A V, Baranova O K, Weathers K, Paver C R, Smolyar I 2018 World Ocean Atlas 2018, Volume 2: Salinity. 82 p50
[18] Gandin L S 1963 Objective Analysis of Meteorological Fields (Translated from the Russian.) p184
[19] Amante C, Eakins B W. 2009 Psychologist 16 3
[20] Bershad, Susanne, Martin W. 1976 NOAA National Centers for Environmental Information.
[21] Straume E O, Gaina C, Medvedev S, Hochmuth K, Gohl K, Whittaker J M, Abdul Fattah R, Doornenbal J C, Hopper J R 2019 Geochem Geophy Geosy 20 4
[22] Collins M 1998 J.acoust.soc.Am 93 1736
[23] Jensen F, Kuperman W, Porter M, Schmidt H 2011
[24] Fisher, H. F 1977 J. Acoust. Soc. Am 62 13
[25] Lovett, Jack R 1980 J. Acoust. Soc. Am 67 338
[26] Munk W H 1974 J. Acoust. Soc. Am 55 220
计量
- 文章访问数: 1592
- PDF下载量: 0
- 被引次数: 0
下载:
