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Articles by Su-Chin Chen
Synchronized Multidisciplinary Observations in Large‐Scale Dam Breach Experiments to Enhance the Understanding of Dam Failure Evolution
1 Introduction Landslide dams, formed when landslides or debris flows block rivers, are typically triggered by earthquakes or extreme rainfall events. Their sudden formation and failure can cause catastrophic flooding, channel changes, and widespread damage, particularly in steep and unstable mountain regions (Soares-Frazão & Zech, 2008).
Numerical Simulations Using iRIC Nays2DH for Sediment Transport Behaviors in Dam Breach Tests
1. Introduction Large-scale landslides can be triggered by intense rainfall or earthquakes. The debris can fall into rivers and create a landslide dam, obstructing the flow and forming a landslide dam lake. When a dam erodes and fails, it can collapse suddenly, causing floods that lead to severe property damage and loss of life downstream According to Costa and Schuster [1], nearly 89% of landslide dams fail due to overtopping.
Characterization of Seismic Signal Patterns and Dynamic Pore Pressure Fluctuations Due to Wave-Induced Erosion on Non-Cohesive Slopes
1. Introduction Coastal slopes are often subject to wave erosion, leading to landslides into marine environments. Wave erosion not only exposes the slope and causes soil loss but also severely threatens the ecology, human activities, and the safety of public facilities. A “marine geohazard” is defined as geological features and processes in coastal and offshore environments that lead to loss of life and assets [1,2,3,4,5,6].
Natural Disasters Occurrence, Reduction, and Restoration in Mountain Regions
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