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Modelling Combined Subaerial-Subaqueous Flow-Like Landslides by Cellular Automata

机译:利用元胞自动机模拟地下-水下水流组合滑坡

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Macroscopic Cellular Automata characterize a methodological approach for modelling large scale (extended for kilometres) complex acentric phenomena, e.g. surface flows as lava flows, debris flows etc.. This paper concerns the extension of such a method in order to simulate combined subaerial-subaqueous flow-like landslides. The occurrence of heterogeneous interacting processes requires a more physical description of the energy balance and an explicit velocity management. The model SCIDDICA-SS2 proposes some empirical solutions, such as the computation at each step and inside each cell, of departing flows which are characterized by their mass centre position and velocity. An application to combined subaerial-subaqueous landslide is exhibited together with simulation results of the 1997 Albano lake (Rome, Italy) debris flow.
机译:宏观细胞自动机表征了一种方法方法,该方法用于对大规模(扩展至千米)复杂的无心现象进行建模(例如地表水流就像熔岩流,泥石流等。本文涉及这种方法的扩展,以便模拟地下-水流类似的组合滑坡。异质相互作用过程的发生需要能量平衡的更物理描述和明确的速度管理。模型SCIDDICA-SS2提出了一些经验解,例如以质量中心位置和速度为特征的离去流的每个步骤和每个单元内部的计算。与1997年阿尔巴诺湖(意大利罗马)泥石流的模拟结果一起,展示了一种组合式的航空-水下滑坡应用。

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