EI / SCOPUS / CSCD 收录

中文核心期刊

浅海中基于海底地震仪的声源三维定位

Three-dimensional source localization based on ocean bottom seismometers in shallow water

  • 摘要: 根据海底地震仪测量数据, 提出了浅海中一种声源方位、距离和深度估计方法。首先采用两个海底地震仪测量数据分别估计声源方位, 然后利用两个方位的交点确定声源水平位置, 得到声源相对于海底地震仪的方位和距离, 最后通过接收信号不同模态的能量比估计声源深度。根据浅海负跃层环境下模态函数特性, 对浅声源采用除第1阶模态以外的高阶模态能量比, 对深度较大的声源采用各高阶模态与第1阶模态的能量比, 能有效对不同深度的声源进行深度估计。对实验中的气枪声源定位结果表明, 估计的声源位置与其实际位置较接近, 声源距离远、近两个海底地震仪的距离误差分别约为1.5%和14.1%, 声源深度估计结果与实际布放的深度基本一致。

     

    Abstract: A method to estimate source direction, range, and depth is proposed based on the data measured by ocean bottom seismometers (OBSs). Firstly, source direction is estimated separately using the vector sound field data obtained by two OBSs. Then, the source location is determined by the intersection point of the two directions, and the direction and range of the source can be obtained. Finally, source depth is estimated by the energy ratios of different modes decomposed from the signals obtained by one OBS. Based on the properties of modal functions in a shallow water environment with a negative thermocline, the depth of a shallow source can be obtained by the energy ratios of the higher-order modes, excluding the first-order mode, and the depth of a deep source can be obtained by the energy ratios of the higher-order modes to the first-order mode. Therefore, the depth of sources located at different depths can be estimated efficiently. The analysis of the OBS-measured signals is shown that the estimated source position is close to its actual position. The distance errors of the source from the farther and nearer OBSs are 1.5% and 14.1%, respectively. The estimated source depth is in agreement with the air-gun depth deployed in the experiment.

     

/

返回文章
返回