首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >A model for high-frequency acoustic Doppler current profiler backscatter from suspended sediment in strong currents
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A model for high-frequency acoustic Doppler current profiler backscatter from suspended sediment in strong currents

机译:强流中悬浮沉积物的高频声多普勒电流剖面仪反向散射模型

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摘要

Acoustic current Doppler profilers (ADCP's) have been used to measure currents for over 20 years. Although ADCP's are not designed to measure acoustic backscatter intensity accurately, several researchers have (successfully) related the backscatter intensity to suspended sediment concentration (SSC) using a random phase acoustic backscatter model. However, this paper shows experimental evidence that in a tidal inlet during high tidal current velocities, a random phase acoustic backscatter model overestimates the SSC by factors up to 60, which could not be explained by a time-varying particle size distribution. An acoustic backscatter model is developed that includes the effect of acoustic backscatter enhanced by coherence in the particles' spatial distribution as a result of turbulence-induced sediment fluctuations. The model results are compared with field measurements, showing a good correspondence between measured and modelled SSC, including the strong high current conditions for which the random phase acoustic backscatter model was shown to fail. (c) 2006 Elsevier Ltd. All rights reserved.
机译:声电流多普勒轮廓仪(ADCP's)已用于测量电流超过20年。尽管ADCP并非旨在准确地测量声后向散射强度,但仍有一些研究人员使用随机相位声后向散射模型(成功地)将后向散射强度与悬浮泥沙浓度(SSC)相关联。但是,本文显示了实验证据,即在高潮汐流速度期间的潮汐入口处,随机相位声学反向散射模型高估了SSC达60倍,这不能用随时间变化的粒度分布来解释。建立了一个声学反向散射模型,该模型包括由于湍流引起的泥沙波动而使粒子空间分布的相干性增强了声学反向散射的效果。将模型结果与现场测量结果进行了比较,显示了测量的SSC与建模的SSC之间具有良好的对应关系,其中包括强大电流条件,随机相位声反向散射模型显示出此条件失败。 (c)2006 Elsevier Ltd.保留所有权利。

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