Guo Yijun, Zhang Yu*, zhao Zhongxi

" /> 河道流量的高频声层析监测研究

南京大学学报(自然科学版) ›› 2015, Vol. 51 ›› Issue (7): 60–.

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河道流量的高频声层析监测研究

郭宜君1,张宇1*,赵宗曦1   

  • 出版日期:2015-12-26 发布日期:2015-12-26
  • 作者简介:(1. 厦门大学水声通信与海洋信息技术教育部重点实验室,厦门 361005)
  • 基金资助:

    基金项目:国家自然科学基金(1117424041276040),福建省自然科学基金(2060203

    收稿日期:2015-06-30

    *通讯联系人:Email: yuzhang@xmu.edu.cn

Study of the river discharge observation based on high frequency

Guo Yijun, Zhang Yu*, zhao Zhongxi

  

  • Online:2015-12-26 Published:2015-12-26
  • About author:Key Laboratory of Underwater Acoustic Communication and Marine Information Technology Ministry of Education, Xiamen, 361005, China

摘要: 海洋声层析作为一种有效的温流监测手段不仅可以用于大洋、近海等大中尺度海域的观测,同样可以应用于对河道、湖泊、航道等小尺度(几百米至上千米)的观测。声层析反演结果的分辨率主要取决于声波的频率以及声波传输时间的测量精度。本文为了研究高频声层析在河道的应用,在福建省漳州市九龙江北溪的江东水库设置了两个可以发射高频声波的声层析观测站点。北溪的平均水深为8 m,深度由中间向两岸递减,站点之间距离415 m,观测中所采用的声波频率带宽为40-80 kHz,中心频率为60 kHz,采用声层析互易原理监测水库的温流参数变化。实验证明本文所使用的方法能够较稳定地测量出声波参数随传输环境的变化,所测得的互易声传输时间可以有效地反演出该区域的温流参数,说明海洋声层析技术在提高频率的情况下也适用于对河道这种小尺度水域的流量、温度监测。

Abstract: Ocean Acoustic Tomography (OAT) is an effective technology for the measurement of ocean temperature, sound speed distribution and current field observations in estuaries and bays with complicated hydrological conditions. The frequency of sound plays an important role in the inversion of current and temperature. Both precise positioning and clock accuracy are required for velocity tomography. In this study, a high frequency experiment with two Acoustic Tomography Systems was carried out in the Jiangdong Reservoir of Beixi River in Zhangzhou city. The systems were set up at E and W stations with a distance of 415 m across Jiangdong Reservoir, the mean water depth was 8 m in both location, and transducers were suspended down to 1.5 m depth from surface of river. In order to improve the resolution of travel-time and the inversion accuracy of velocity, 60 kHz sound with a bandwidth of 40 kHz, phase-modulated by the 8th order M sequence, was transmitted every 10 second. The travel-time obtained by systems was well corrected with the river discharge. This experiment suggests that the ocean acoustic tomography, with high frequency sound, can also be regarded as an effective observational method for small-scale coastal estuary areas.

[1] Munk W, Wunsch C. Ocean acoustic tomography: a scheme for large scale monitoring. Deep Sea Research Part A. Oceanographic Research Papers, 1979, 26(2): 123-161.

[2] 廖光洪, 朱小华, 杨成浩, 等. 基于声传播时间的二维流场反演数值仿真研究. 海洋学报, 2009, 31(8-16): 65-68.

[3] Grosso V A D. New equation for the speed of sound in natural waters (with comparisons to other equations). Journal of the Acoustical Society of America, 1974, 56(4): 1084-1091.

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