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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >An acoustic Doppler velocimeter (ADV) for the characterisation of turbulence in concentrated fluid mud
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An acoustic Doppler velocimeter (ADV) for the characterisation of turbulence in concentrated fluid mud

机译:声学多普勒测速仪(ADV)用于表征浓缩液泥浆中的湍流

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The paper describes a velocimeter, based on the back-scattering of ultrasonic waves by particles, designed for measuring instantaneous turbulent velocities in a concentrated fluid mud mixture. The acoustic Doppler velocimeter (ADV) needs no calibration and is therefore a potentially useful tool for measuring velocities in the laboratory or in the field. We investigate its reliability for measurements in concentrated cohesive sediment suspensions, where the particle size is usually unknown due to the occurrence of flocculation, and where there is considerable acoustic wave absorption. Measurements in a resonant standing wave demonstrate the ability of the apparatus to measure unsteady velocities. The data validation rate ranges between 20 and 80 Hz for a cohesive sediment concentration in the range 20-140 gl(-1) Experiments were performed with two different natural mud mixtures. It is observed that using an ADV does not require prior determination of particle and flee properties. It is furthermore demonstrated that the amplitude of the back-scattered signal received by the transceiver results mainly from a single reflection on particles, whereas echoes experiencing multiple reflections an strongly damped. The use of an ADV for measuring turbulence properties is finally assessed for low Reynolds turbulence, which occurs in Concentrated Benthic Suspension layers. (C) 2000 Elsevier Science Ltd. All rights reserved. [References: 18]
机译:本文介绍了一种基于粒子对超声波的反向散射的测速仪,该测速仪旨在测量浓缩液泥浆混合物中的瞬时湍流速度。声学多普勒测速仪(ADV)无需校准,因此是在实验室或现场测量速度的潜在有用工具。我们研究了其在浓缩内聚性沉积物悬浮液中测量的可靠性,该浓度通常由于发生絮凝而未知,并且存在相当大的声波吸收,因此粒径通常是未知的。在共振驻波中的测量表明了该装置测量不稳定速度的能力。粘性泥沙浓度范围为20-140 gl(-1)的数据验证率范围为20到80 Hz,使用两种不同的天然泥浆混合物进行了实验。可以看出,使用ADV不需要事先确定颗粒和起毛特性。此外还表明,收发器接收到的反向散射信号的幅度主要是由对粒子的单次反射引起的,而经历多次反射的回波则被强烈衰减。最后评估了在低浓度的底栖悬浮液层中发生的雷诺湍流较低的情况下,使用ADV测量湍流特性的情况。 (C)2000 Elsevier ScienceLtd。保留所有权利。 [参考:18]

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