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首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Novel high-frequency acoustic monitoring of streamflow-turbidity dynamics in a gravel-bed river during artificial dam flush
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Novel high-frequency acoustic monitoring of streamflow-turbidity dynamics in a gravel-bed river during artificial dam flush

机译:人工坝冲洗过程中砾石床河流流出浊度动力学的新型高频声学监测

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摘要

To assess the dynamics of rivers, a reliable characterization of river streamflow during unsteady flow regimes is of paramount importance. In this work, we aimed at investigating the characteristics of turbidity discharge (T-Q) dynamics corresponding to annual artificial dam flush release in a mountainous stream. Two methods for evaluating discharge were used in this study: the classical rating curve and the fluvial acoustic tomography (FAT) system that was developed by Hiroshima University. Interestingly, during dam flush, the discharge records obtained by FAT showed striking features of unsteady streamflow behavior, such as discharge shoulders and, in some events, secondary discharge peaks. According to the T-Q hysteresis loops, the common type of T-Q observed patterns were anticlockwise loops. During the studied DF events, sediment was supplied by river banks located at different sites along the river channel.
机译:为了评估河流的动态,在非定常的流动制度期间,河流流的可靠表征是至关重要的。 在这项工作中,我们旨在调查与山区流中的年人工坝冲洗释放相对应的浊度放电(T-Q)动态的特征。 本研究使用了两种评估的评估方法:广岛大学开发的经典额定曲线和河流声学断层扫描(脂肪)系统。 有趣的是,在坝冲洗期间,通过脂肪获得的放电记录显示出不稳定的流动行为的引人注目的特征,例如放电肩部,以及在一些事件中,二次放电峰值。 根据T-Q滞后环,常见的T-Q观察图案是逆时针环。 在研究期间,沉积物由位于沿河渠道的不同地点的河岸供应。

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