4.6 Article

Modeling and Risk Analysis of Dam-Break Flooding in a Semi-Arid Montane Watershed: A Case Study of the Yabous Dam, Northeastern Algeria

Journal

WATER
Volume 14, Issue 5, Pages -

Publisher

MDPI
DOI: 10.3390/w14050767

Keywords

dam breach parameters; dam failure scenario; flood hazard; flood hydrodynamics; flood simulation; simulated natural hazard

Funding

  1. European Regional Development Fund within the Activity 1.1.1.2 Post-doctoral Research Aid of the Specific Aid Objective 1.1.1 of the Operational Programme Growth and Employment [1.1.1.2/VIAA/4/20/606]

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This study simulated the dam breach failure scenario of Yabous dam in northeast Algeria and analyzed its influence on the downstream urban and natural environments. Sensitivity analysis showed that adjustments in breach width and slope resulted in positive changes in flood wave flow, height, and width, while adjustments in breach formation time had opposite effects. The HEC-RAS hydraulic model effectively simulated the flood wave propagation downstream and highlighted the impact of breach parameters and flood hydrographical pattern.
The risk related to embankment dam breaches needs to be evaluated in order to prepare emergency action plans. The physical and hydrodynamic parameters of the flood wave generated from the dam failure event correspond to various breach parameters, such as width, slope, and formation time. This study aimed to simulate the dam breach failure scenario of the Yabous dam (northeast Algeria) and analyze its influence on the related areas (urban and natural environments) downstream of the dam. The simulation was completed using the sensitivity analysis method to assess the impact of breach parameters and flooding on the dam break scenario. The flood wave propagation associated with the dam break was simulated using the one-dimensional HEC-RAS hydraulic model. This study applied a sensitivity analysis of three breach parameters (slope, width, and formation time) on five sites selected downstream of the embankment dam. The simulation showed that the maximum flow of the flood wave recorded at the level of the breach was 8768 m(3)/s, which gradually attenuated along the river course to reach 1972.7 m(3)/s at about 8.5 km downstream the dam. This study established the map of flood risk areas that illustrated zones threatened by the flooding wave triggered by the dam failure due to extreme rainfall events. The sensitivity analysis showed that flood wave flow, height, and width revealed positive and similar changes for the increases in adjustments (+/- 25% and +/- 50%) of breach width and slope in the five sites. However, flood wave parameters of breach formation time showed significant trends that changed in the opposite direction compared to breach slope and width. Meanwhile, the adjustments (+/- 25% and +/- 50%) of the flood hydrograph did not significantly influence the flood parameters downstream of the dam. In the present study, the HEC-RAS 1-D modeling demonstrated effectiveness in simulating the propagation of flood waves downstream of the dam in the event of dam failure and highlighted the impact of the breach parameters and the flood hydrographical pattern on flood wave parameters.

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