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Laboratory validation of acoustic Doppler current profiler (ADCP) techniques for suspended sediment investigations

机译:声学多普勒电流剖面仪(ADCP)技术的实验室验证,用于悬浮泥沙调查

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The aim of this paper is to validate a method of investigating the grain size distribution of suspended sediments using acoustic Doppler current profilers (ADCPs) and to compare different calibration strategies of the ADCP backscattering power, which can be correlated with the concentration of corresponding sediments. Over the last two decades, the methods for suspended sediment investigation using the backscattering power of ADCPs have been gaining increasing acceptance within the river engineering community. This acceptance is due to acoustic backscattering providing the opportunity to indirectly quantify suspended sediment by non-intrusive measurements with high temporal and spatial resolution. We have already presented the method using two ADCPs working at different frequencies (600 and 1200 kHz) on the same water column to profile the concentration and grain size in the Parana River (Argentina). The present work, as a complement to the Parana application, demonstrates the reliability of the method by a laboratory validation of monitored concentrations and known grain size distributions. The context of our research is introduced in a discussion of the topic of river sediment transport measurement using ADCPs. Then, the underwater acoustic physics is briefly presented with a focus on acoustic backscattering (ABS) methods for the estimation of suspended sediment grain size. The laboratory tests, which were conducted at the sediment tower-mixing facility using four different known distributions of sand in the range 50-700 μm, are described in detail to demonstrate the reliability of the ABS methods and to justify the adopted experimental strategies to overcome undesired air bubble interference with the ABS due to injected sand.
机译:本文的目的是验证一种使用声学多普勒电流剖面仪(ADCP)研究悬浮沉积物粒度分布的方法,并比较ADCP反向散射功率的不同校准策略,该方法可以与相应沉积物的浓度相关。在过去的二十年中,利用ADCP的反向散射能力进行悬浮泥沙调查的方法已在河流工程界得到越来越多的认可。这种接受是由于声学反向散射,通过非侵入性测量以高时间和空间分辨率提供了间接量化悬浮沉积物的机会。我们已经介绍了使用在同一水柱上以不同频率(600和1200 kHz)工作的两个ADCP来描述巴拉那河(阿根廷)中的浓度和粒度的方法。作为对Parana应用程序的补充,本工作通过实验室对监测浓度和已知粒度分布的验证来证明该方法的可靠性。在讨论使用ADCP进行河流泥沙输送测量的主题时,介绍了我们的研究背景。然后,简要介绍了水下声学物理学,重点介绍了用于估计悬浮沉积物粒径的声学反向散射(ABS)方法。详细描述了在沉积物塔混合设施中使用四种已知的沙分布范围为50-700μm进行的实验室测试,以证明ABS方法的可靠性并证明所采用的克服实验方法的合理性由于注入的沙子,气泡会干扰ABS。

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