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Effects of suspended sediment concentration and turbulence on settling velocity of cohesive sediment

机译:悬浮泥沙浓度和湍流对粘性泥沙沉降速度的影响

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Using a 5-MHz acoustic Doppler velocimeter (ADV),laboratory experiments were carried out to investigate the effects of suspended sediment concentration (SSC) and turbulence on the settling velocity (w s) of cohesive sediment. The measurement of w_swith the Clay Bank sediment showed that w_sincreased non-linearly with SSC in the range of 300–700 mg L~(-1), and that turbulence can increase w_sup to one order higher than w_s for nonturbulent conditions. This turbulence effect can explain why w_s derived by ADV is 1 to 3 orders higher than w_s estimated by Owen tube where the ambient turbulence is totally blocked.When the turbulent shear stress was higher than about 0.14 Pa,however, it contributed to tear apart flocs and reduce w_s. This study suggests that ADV is a useful tool to concurrently measure the instantaneous current velocities, SSC and w_s in turbulence-dominant environments without breaking up flocs and disturbing ambient flow.
机译:使用5 MHz声学多普勒测速仪(ADV),进行了实验室实验,以研究悬浮泥沙浓度(SSC)和湍流对粘性泥沙沉降速度(w s)的影响。用粘土库沉积物测得的w_s表明,SSC在300-700 mg L〜(-1)范围内w_s非线性增加,在非湍流条件下,湍流可使w_sup比w_s高一阶。这种湍流效应可以解释为什么ADV得出的w_s比欧文管估计的w_s高出1到3个数量级,其中欧文管完全阻塞了周围的湍流。当湍流剪应力高于约0.14 Pa时,它有助于将絮状物撕裂并减少w_s。这项研究表明,ADV是一种有用的工具,可在湍流占主导地位的环境中同时测量瞬时流速,SSC和w_s,而不会破坏絮凝物和扰乱环境流量。

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