landslide early warning system - wyatt bartlett and john nihi
TRANSCRIPT
Landslide Early Warning System
Wyatt Bartlett- UH ManoaJohn Nihi- UH Manoa
Melia Iwamoto - Graduate Student AdvisorPhillip Ooi - Faculty Advisor
UH Mānoa Geotechnical Engineering Lab
Overview1. Objectives
2. Project Locations
3. Field Instrumentation
4. Lab Methods
5. Results
6. Discussion of Findings
7. Summary & Conclusions
Objectives1. Soil Characterization
• Hydrometer (standard) vs. Laser Diffraction (new)
2. Suction Characterization• SWCC = w% vs. suction• Theoretical vs. Lab vs.
FieldCreate more accurate slope stability models for Hawaii DOT
Project Locations
Likelike Highway Pali Highway
Monitoring Instruments
• Inclinometer – Lateral Displacement• Tensiometer – Suction• Water content sensors – Water content• Rain gage - Precipitation
Datalogger
• Program collection frequency• Collects data remotely• Powered by solar energy
Lab Methods1. Grain Size Distribution
• Wet Sieve and Hydrometer (Conventional)
• Laser Diffraction (New and being studied)2. Soil Water Characteristic Curve
• Pressure Plate - Lab• VSA (Vapor Sorption Analyzer) - Lab• Tensiometers - Field• SoilVision - Theory
Grain Size DistributionHydrometer Laser DiffractionWet Sieve
4 days 15 minutes1 day
Suction in the LabPressure Plate Vapor Sorption Ana-
lyzer
Suction in the Field• Tensiometer to measure suction
Results - Grain Size Distribution
0.000010.00010.0010.010.11100
10
20
30
40
50
60
70
80
90
100
Wet Sieve and Hydrometer vs. Laser Diffraction
Horiba4 Hydrometer4
Diameter (mm)
%Pa
ssin
g
Discussion of FindingsHydrometer vs. Laser Diffraction
• Compared to Di Stefano, et al. (2010)
Di Stefano, C., et al. (2010) Comparison between grain-size analyses using laser diffraction and sedimentation methods. Biosystems Engineering 106 (2010) 205-215
Results - Suction
1 10 100 1000 10000 100000 10000000%
5%
10%
15%
20%
25%
30%
35%
40%
45%
50%
Soil Water Characteristic Curve
Soil Vision (B2-11)
Measured (Field MPS-6)
Measured (Lab - VSA)
Measured (Lab - PP)
Suction (kPa)
Gra
vim
etri
c W
ater
Con
tent
Summary and Conclusions
Grain Size Analysis• Laser diffraction provides a reasonable estimate of
the soil grain size distribution compared to wet sieve and hydrometer tests
Soil Water Characteristic Curve• Suction measurements in the lab matches well with
those in the field• They also match well with theoretical curves
These findings will be useful in development of the LEWS
Acknowledgements• Special thanks to:• NSF SEE 3 Program• Melia Iwamoto• Marica Ottorogram
• Phillip Ooi• Yogi Kwong Engineers• HDOT
Q & A
References• Di Stefano, C., et al. (2010) Comparison
between grain-size analyses using laser diffraction and sedimentation methods. Biosystems Engineering 106 (2010) 205-215
• Jotisankasa, A. and Vathananukij, H. (2008) Investigation of soil moisture characteristics of landslide-prone slopes in Thailand. International Conference on Management of Landslide Hazard in the Asia-Pacific Region