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On the application of kinematic models to simulate the diffusive processes of debris flows

机译:运动学模型在泥石流扩散过程模拟中的应用

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摘要

Debris flows generally propagate along steep mountain torrents with dynamics primarily governed by gravitational and frictional forces. Thus, debris flows modelling can be successfully performed through the application of kinematic models, which consider only the effects of slope and friction and neglect the remaining terms of the momentum equation. However, the diffusion processes that can be observed in the field, such as the spreading of the debris flow wave as it flows downstream, can not be theoretically predicted by kinematic models, since diffusion is a second-order process neglected in the kinematic approximation. In this paper, this issue is discussed and an application for both a generalized diffusion wave model and a kinematic model is proposed of a debris flow which occurred in an Italian instrumented torrent to identify, in a real case scenario, the effective value of the neglected terms in the kinematic approximation.
机译:泥石流通常沿着陡峭的山洪扩散,其动力学主要受重力和摩擦力控制。因此,通过应用运动学模型可以成功地进行泥石流建模,该运动学模型仅考虑坡度和摩擦的影响,而忽略了动量方程的其余项。但是,运动模型无法从理论上预测在野外可以观察到的扩散过程,例如碎屑流向下游流动时的扩散,因为扩散是运动学近似中忽略的二阶过程。本文讨论了这个问题,并提出了一种泥石流的广义扩散波模型和运动学模型的应用,这些泥石流发生在意大利的仪表洪流中,以在实际情况下识别被忽略的有效值运动学近似中的项。

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