脉冲对脉冲相干多普勒声纳速度估计器的自动调谐

J. Dillon, L. Zedel, A. Hay
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引用次数: 3

摘要

脉冲对脉冲相干多普勒声纳能够同时测量湍流悬浮物中的速度和沉积物浓度。然而,当从速度的波动分量计算湍流统计时,测量噪声的存在会引入偏差。为了进一步发展相干多普勒声纳作为湍流测量工具,研制了一种基于最大a后验估计的速度估计器。该估计器最佳地结合了多个声学载波频率和多个换能器的测量结果。数据融合是使用概率方法实现的,通过数值方法将测量结果结合起来,得出速度似然函数。用户必须选择的唯一参数是平滑因子,它描述了在时间上从一个样本到另一个样本的速度扩散(在概率意义上)。提出了一种自动确定平滑参数的方法,该方法是通过对测量时间序列中具有代表性的一段光谱的检查来实现的。本文介绍了用多频相干多普勒声纳和粒子图像测速仪(PIV)同时测量湍流射流速度的实验结果。将PIV的时间序列和湍流谱与常规多普勒信号处理和MAP速度估计得到的时间序列和湍流谱进行了比较。结果表明,估计器的自动调谐可以得到一个速度时间序列,其中测量噪声被抑制,而高频湍流波动被保留。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Automatic tuning of a velocity estimator for pulse-to-pulse coherent Doppler sonar
Pulse-to-pulse coherent Doppler sonar is capable of measuring simultaneous profiles of veloctiy and sediment concentration in turbulent suspensions. However, the presence of measurement noise introduces biases when turbulence statistics are calculated from the fluctuating component of velocity. In order to further develop coherent Doppler sonar as a tool for turbulence measurement, a velocity estimator based on Maximum A Posteriori (MAP) estimation has been developed. The estimator optimally combines measurements from multiple acoustic carrier frequencies and multiple transducers. Data fusion is achieved using a probabilistic approach, whereby measurements are combined numerically to derive a velocity likelihood function. The only parameter which must be chosen by the user is a smoothing factor that describes the diffusion of velocity (in a probabilistic sense) from sample to sample in time. A method is presented for automatically determining the smoothing parameter from examination of the spectrum of a representative segment of the measurement time series. Results are presented from a laboratory turbulent jet in which velocity was measured simultaneously with multi-frequency coherent Doppler sonar and particle image velocimetry (PIV). Time series and turbulence spectra from PIV are compared to those obtained with conventional Doppler signal processing and MAP velocity estimation. It is shown that automatic tuning of the estimator results in a velocity time series where measurement noise is suppressed while high frequency turbulent fluctuations are retained.
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