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Temporal variation of intermittent surges of debris flow

机译:泥石流间歇性涌浪的时间变化

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Debris flows (especially those of high-density or high viscosity) usually appear in the form of surge sequence. Each debris flow event consists of tens or hundreds of surges. A debris flow is thus equal to a surge series which is expected to feature the intrinsic properties. Statistics of observation data indicates that different events have the similar distributions in parameters such as velocity, flow depth, discharge, runoff, and time interval, which can be considered as the signs of an underlying dynamics. But there are currently difficulties in extracting the dynamics from the surge series. This paper is concerned with the temporal variations of surge series based on observation data in the last forty years in Jiangjia Gully (JJG) The temporal process of a surge series is characterized by the accumulative curve of the interval time. A surge series is found to be dominated by the peak discharge in that the peak discharge determines the exponent of the distribution. Moreover, the average discharge evolves with surge progress and finally decays in a power-law form. It follows that a surge series behaves as a whole which requires a unified dynamical framework to encompass all the appearances.
机译:泥石流(特别是高密度或高粘度的泥石流)通常以冲击序列的形式出现。每个泥石流事件都包含数十或数百个浪涌。因此,泥石流等于预期具有固有特性的波动序列。观测数据的统计数据表明,不同的事件在速度,流量深度,流量,径流和时间间隔等参数上具有相似的分布,这可以视为潜在动态的标志。但是目前在从喘振系列中提取动力学方面存在困难。本文基于江嘉沟壑区近40年的观测资料,对涌浪序列的时间变化进行了研究。涌浪序列的时间过程以间隔时间的累积曲线为特征。发现电涌序列受峰值放电的支配,因为峰值放电决定了分布的指数。而且,平均放电随着电涌的进展而发展,最终以幂律形式衰减。随之而来的是,喘振系列的行为表现为一个整体,需要一个统一的动力学框架来涵盖所有外观。

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