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— 学术系列讲座(五)
报告题目:The Mechanics of Debris Flow
报
告 人:CHAN, Dave
Hung Kwan
报告时间:2018年4月24日,下午3:00
报告地点:地学楼416
报告摘要:
Debris flow is a natural phenomenon that
occurs in mountainous terrains. The flow process is usually initiated by slope
failure at high ground followed by rapid mass movement along steep channels.
Debris can grow in size due to erosion of the channel, called entrainment, and
it can become smaller due to deposition along the channel as levies and
depositional fans. Debris is mainly composed of soil and rock of a wide range of
sizes and it can include trees, vegetation and other materials collected in its
path. Water is a common element in debris and the presence of water changes its
flow characteristic dramatically.
The presentation will discuss the mechanics
of debris flow and various numerical techniques to calculate the velocity and
extend of the flowing mass. Discussion will include entrainment and
constitutive modelling for debris flow analysis. Laboratory test and case histories are used
to study the effectiveness of the models in debris flow analysis
报告人简介:
Dr. Dave现为加拿大阿尔伯塔大学土木与环境学院教授,博士生导师,研究生院副经理。担任岩土工程领域顶级刊物《Canadian Geotechnical Journal》副主编;研究方向涉及地下结构、边坡稳定性、大坝稳定、泥石流及土体液化等研究领域,特别是在土体本构模型和数值计算等方面具有很高的学术造诣。发表SCI论文120余篇,发表超过50余次大会报告。