Prediction of a Hypothetical Debris Flow using LS-DYNA Second JTC1 - - PowerPoint PPT Presentation

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Prediction of a Hypothetical Debris Flow using LS-DYNA Second JTC1 - - PowerPoint PPT Presentation

Prediction of a Hypothetical Debris Flow using LS-DYNA Second JTC1 Workshop Arthur Cheung Geologist Hong Kong 4 December 2018 Brief Self-introduction Work as a geologist in Arup Have been working in natural terrain hazard study since


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Prediction of a Hypothetical Debris Flow using LS-DYNA

Arthur Cheung Geologist Hong Kong 4 December 2018 Second JTC1 Workshop

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Brief Self-introduction

➢Work as a geologist in Arup ➢Have been working in natural terrain hazard study since 2011 ➢Interested in the development of LS-DYNA in debris mobility modelling and debris-barrier interaction

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Acknowledgement

Richard Sturt Yuli Huang Jack Yiu AT&R UK and San Francisco HK Geotechnics

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Outline

➢Brief Introduction of LS-DYNA ➢Benchmarking Exercise – Case D1 ➢Model Setup ➢Model Parameters ➢Results ➢Summary

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The Numerical Model – LS-DYNA

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What is LS-DYNA?

➢LS-DYNA is a multi- purpose finite element program for linear and non-linear mechanics

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What is LS-DYNA?

➢LS-DYNA is a multi- purpose finite element program for linear and non-linear mechanics

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What is LS-DYNA?

➢Track records on impact analyses ➢Able to model large deformation and movement of debris mass with the use of advanced finite element meshing method ➢Able to simulate soil-structure interaction

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Development since 2012

The Interactions between Landslide Debris and Flexible Barriers

2012 - 2014

Energy Balance

  • f Flexible

Barrier System

2014 - 2016

Engineering Application Perspective

2016 - current

Research Validation Adopt in Real Work

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Debris Mobility Modelling

LS-DYNA Capabilities

PRIVATE AND CONFIDENTIAL

4 5 1 2

Rock Fall

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Optimisation in Design of Flexible and Rigid Barriers Energy Balance Interaction between the flexible barrier and the landslide debris

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LS-DYNA Results Validated by Well-documented Cases

Volkwein rock fall tests in Switzerland

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LS-DYNA Results Validated by Well-documented Cases

Yu Tung Road Landslide Sham Tseng San Tsuen landslide Fei Tsui Road landslide Kwun Yam Shan landslide 1 1 2 2 3 3 4 4

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LS-DYNA Results Validated by Well-documented Cases

Illgraben flexible barrier field test Full-scale field test flexible barrier in Veltheim

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LS-DYNA Debris Mobility Modelling in Different Regions

Area: Mount. Umyeon, Seoul Area: Conghua Training Centre, China Area: Fo Tan, Hong Kong Area: Victoria Public Mortuary and Cavern Area: Ocean Park, Hong Kong

SIERRA LEONE

Area: Freetown, Sierra Leone

SEOUL MAINLAND CHINA HONG KONG HONG KONG HONG KONG

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Hypothetical Landslide – Case D1

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Case D1 – A historical landslide catchment in Hong Kong

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Model Setup – The Topography

➢Modelled by rigid shell elements ➢Resolution = 5m x 5m ➢No. of elements = 11,550

Topography Boulders Dam Landslide Source

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Model Setup – Debris Modelling

➢Volume = 10,000 m³ ➢Debris modelled as ALE solid ➢Unit Weight = 1900 kg/m³

Topography ALE Container Landslide Source

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Model Setup – Debris Mass and Basal Friction

Rheology Material Property Adopted input parameters Remarks Voellmy Internal friction angle, ϕi 15° Arup (2014) Basal friction angle, ϕb 8° GEO TGN 29 (Adverse Site Setting Parameters) Turbulence coefficient 500 m/s²

➢Debris mass movement captured at regular 0.5s interval

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Model Setup – Gravity Initialisation

➢Debris mass initialised at source location by applying gravity load within first 2 seconds ➢An artificial rigid tube and lid, acting as the gate, to confine and restrict the debris mass movement during initialization ➢The gate has very low contact friction with the debris mass to minimize disturbance

Topography Lid Gate Debris

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Model Setup – Gravity Initialisation

➢Debris mass initialised at source location by applying gravity load within first 2 seconds ➢An artificial rigid tube and lid, acting as the gate, to confine and restrict the debris mass movement during initialization ➢The gate has very low contact friction with the debris mass to minimize disturbance

Topography Lid Gate Debris

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Model Animation

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Model Results

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Model Results – Velocity Hydrograph

Point A Point B Point C Maximum Velocity (m/s) 9.7 8.2 7.3 Time Recorded (s)* 40.5 47.5 50.0

*Debris are allowed to slide downslope at t=2s A B C

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Model Results – Debris Thickness Hydrograph

Point A Point B Point C Maximum Thickness (m) 3.0 3.0 3.0 Time Recorded (s)* 40.0 72.5 52.0

*Debris are allowed to slide downslope at t=2s

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Model Animation – Debris Thickness at Point A

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Model Results – Time History of Debris Frontal Velocity

2 4 6 8 10 12 14 16 18 100 200 300 400 500 600 700 800 900 1000 Velocity (m/s) Approximate Chainage (m)

Average Velocity vs. Chainage

Boulders Dam

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Possible Mitigation Measures

➢Rigid Barrier ➢Baffles ➢Flexible Barriers

Example of multiple barriers

  • ption design using LS-DYNA

Debris-flexible barrier interaction using LS-DYNA

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Possible Mitigation Measures

Rigid Barrier

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Summary

➢LS-DYNA are found to produce generally reasonable results for the benchmarking case ➢LS-DYNA using ALE formulation to provide a continuum-based numerical solution can provide realistic motions of landslide debris using Voellmy rheology with conventional parameters ➢LS-DYNA has the capability to carry out soil-structure interaction to visualise and

  • ptimise design mitigation measures
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Thank you

A.K.C. Cheung, J. Yiu, H.W.K. Lam & E.H.Y. Sze (2018) “Advanced Numerical Analysis of Landslide Debris Mobility and Barrier Interaction” HKIE Transaction Theme Issue on Landslides and Debris Flow – Theory and Design, Mitigation, Stabilisation and Monitoring, 2018, Hong Kong Institution of Engineers.