首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >The influence of pool length on local turbulence production and energy slope: A flume experiment
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The influence of pool length on local turbulence production and energy slope: A flume experiment

机译:池长对局部湍流产生和能量斜率的影响:水槽实验

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The influence of pool length on the strength of turbulence generated by vortex shedding was investigated in a 6 m long recirculating flume. The experiment utilized a 38% constriction of flow and an average channel-bed slope of 0(.)007. The base geometry for the intermediate-length pool experiment originated from a highly simplified, 0(.)10 scale model of a forced pool from North Saint Vrain Creek, Colorado. Discharge in the flume was 31(.)61/s, which corresponds to a discharge in the prototype channel of 10 m(3)/s. Three shorter and four longer pool lengths also were created with a fixed bed to determine changes in turbulence intensities and energy slope with pool elongation. Three-dimensional velocities were measured with an acoustic Doppler velocimeter at 31-40 different 0(.)6-depth and near-bed locations downstream of the rectangular constriction. The average velocity and root mean square (RMS) of the absolute magnitude of velocity at both depths are significantly related to the distance from the constriction in most pool locations downstream of the constriction. In many locations, pool elongation results in a non-linear change in turbulence intensities and average velocity. Based on the overall flow pattern, the strongest turbulence occurs in the center of the pool along the shear zone between the jet and recirculating eddy. The lateral location of this shear zone is sensitive to changes in pool length. Energy slope also was sensitive to pool length due to a combination of greater length of the pool and greater head loss with shorter pools. The results indicate some form of hydraulic optimization is possible with pools adjusting their length to adjust the location and strength of turbulent intensities in the center of pools, and lower their rate of energy dissipation. Copyright (C) 2004 John Wiley Sons, Ltd.
机译:在6 m长的循环水槽中研究了池长对涡旋脱落产生的湍流强度的影响。该实验利用了38%的流量收缩率和0(。)007的平均河床坡度。中长度水池实验的基本几何形状源自科罗拉多州北圣弗兰溪的强迫水池的高度简化的0(。)10比例模型。水槽中的流量为31(。)61 / s,相当于原型通道中的流量为10 m(3)/ s。还使用固定床创建了三个较短的池长和四个较长的池长,以确定随池池伸长的湍流强度和能量斜率的变化。用声学多普勒测速仪在矩形颈缩下游的31-40个不同的0(。)6深度和近床位置上测量了三维速度。在两个深度处,速度的绝对大小的平均速度和均方根(RMS)与在收缩区下游大多数池位置中距收缩区的距离显着相关。在许多位置,池伸长会导致湍流强度和平均速度发生非线性变化。基于总体流动模式,最强的湍流发生在水池中心,沿着射流和再循环涡流之间的剪切带。该剪切带的侧向位置对池长的变化很敏感。能量斜率对池长也很敏感,这是由于池长更长,池更短时头部损失更大。结果表明,通过调整池的长度以调整池中心的湍流强度的位置和强度,并降低其能量耗散率,可以进行某种形式的水力优化。版权所有(C)2004 John Wiley Sons,Ltd.

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