Abstract

Sudden avulsions, unexpected channel migrations and backfilling phenomena are autogenic phenomena that can considerably change the propagation patterns of sediment-laden flows on alluvial fans. Once the initial and boundary conditions of the hazard scenario with a given return period are determined, the assessment of the associated exposed areas is based on one numerical, essentially deterministic, process simulation which may not adequately capture the underlying process variability. We generated sediment-laden flows on an experimental alluvial fan by following a “similarity-of-process concept”. Specifically, we considered a convexly shaped alluvial fan model layout featuring a curved guiding channel. As loading conditions, we defined a reference, an increased and a reduced level for the released water volume and the predisposed solid fraction, respectively. Further, we imposed two different stream power regimes and accomplished, for each factor combination, eight experimental runs. The associated exposure areas were recorded by video and mapped in a GIS. We then analysed exposure data and determined exposure probability maps superposing the footprints of the eight repetitions associated with each experimental loading condition. The patterns of exposure referred to the specific loading conditions showed a noticeable variability related to the main effects of the total event volume, the solid fraction, the interactions between them, and the imposed stream power in the feeding channel. Our research suggests that adopting a probabilistic notion of exposure in risk assessment and mitigation is advisable. Further, a major challenge consists in adapting numerical codes to better reflect the stochastics of process propagation for more reliable flood hazard assessments.

Highlights

  • Since time immemorial alluvial fans have been privileged settlement areas, despite being prone to fluvial hazards (Okunishi et al 2001; Mazzorana et al 2020)

  • According to the stated objectives of the accomplished research, we first show the obtained total exposure probability maps as a suitable form to visualize the spatial variability and uncertainty of the alluvial fan areas affected by the sediment-laden flow

  • Third and fifth columns the total exposure probability maps resulting from the full stream power experiments, (Φf), are arranged, whereas in the second, fourth and sixth column the probability maps generated by imposing half stream power (Φh) are displayed

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Summary

Introduction

Since time immemorial alluvial fans have been privileged settlement areas, despite being prone to fluvial hazards (Okunishi et al 2001; Mazzorana et al 2020) They are depositional landforms widespread in almost all climatic environments of the world (Antronico et al 2015) interfering with the sediment transfer in mountainous watersheds as temporary storage areas. Starting from a topographic apex, they normally spread in a radiating pattern (Bowman, 2019), forming conical bodies with concave longitudinal and convex cross profiles (Drew 1873; Galloway et al 1996; Clevis et al 2003) On these landforms, flood hazards may hit in an often rapid and almost unforeseeable manner (Blair & McPherson 1994; National Research Council 1996) and flood control is a challenging social and engineering endeavour (Mazzorana and Fuchs 2010a). Vicious risk cycles frequently unfolded whenever the construction of additional protective elements induced a strong perception of protection and unleashed further land occupation (MacDonald et al 2000; Mazzorana et al 2018)

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