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MONITORING FLOW RATE AND SALINITY INTRUSION IN A TIDAL FLOODWAY USING FLUVIAL ACOUSTIC TOMOGRAPHY

机译:使用河流声学断层扫描监测潮汐泄洪中的流速和盐度入侵

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Six-year record of tidal current and sound speed has been collected in a tidal diversion channel using Fluvial Acoustic Tomography System (FATS) with a couple of 30 kHz broad-band transducers. The FATS was located around 9 km upstream far from the mouth of Ota River diversion channel, Japan. The reciprocal sound transmission that was performed between the two acoustic stations, located on both sides of the channel, enabled us to measure range-averaged sound speed and water velocity along an oblique transmission line. The channel is a shallow tidal-forced river with a maximum tidal range of 4 m at the mouth. The freshwater runoff into the channel is regulated by the array of sluice gates, located 270 m upstream of the observation site. The saline water was flushed out by the gate operation for flood events. Thus, the flow and the salinity intrusion presented strong unsteady nature. The salinity intrusion was investigated from the mean sound speed measured by FATS. The recovering time of the salinity ranged from 9.5 days to 27 days after the gates got back. The tidal velocity amplitude and the outflow velocity associated the river discharge basically controlled the recovery of salinity intrusion.
机译:使用具有几个30 k​​Hz宽带传感器的河流声学断层扫描系统(FAT),在潮流通道中收集六年的潮流和声速。脂肪位于日本Ota河流转移渠道的口交左右9公里。在位于通道两侧的两个声学站之间执行的互易声音传输使我们能够沿着倾斜传输线测量范围平均声速和水速度。通道是浅潮汐河流,口腔最大潮汐范围为4米。淡水径流到通道中由位于观察部位的上游270米的闸门阵列调节。通过用于洪水事件的栅极操作冲出盐水。因此,流动和盐度入侵呈现强烈的不稳定性。从脂肪测量的平均声速研究了盐度侵入。盐度回收时间范围从盖茨回来后的9.5天至27天。潮流幅度和流出速度相关的河流放电基本上控制了盐度侵入的回收。

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