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An Analysis of Teton Dam
Failure, USA
Teton Dam Facts
• constructed from February 1972 to June 1976.
• Bureau of Reclamation designed Teton Dam.
• Construction contract awarded to Morrison-Knudsen Company, Inc.
• located in southeastern Idaho, 12 miles northeast of Rexburg.
Dam Design and
Construction
Teton Dam Failure
• Failed on June 5th , 1976.
• 11 deaths resulted from the disaster.
• $400 million in property damage.
• The towns of Sugar City and Rexburg were struck the hardest.
Geology of Teton Dam’s Site
• Volcanic Plateau known as Rexburg Bench.
• Composed of Basalt and Rhyolite Tuff.
 High permeability
• Consisted of highly fissured and unstable rock.
• Seismically active area.
Basalt Rock
(https://flexiblelearning.a
uckland.ac.nz/rocks_min
erals/rocks/basalt.html)
Rhyolite Tuff
(http://markstein
metz.photoshelte
r.com/image/I000
0.T6UG4upcSw)
Analysis of Soil Material of Dam Core
• Required properties for large dam core
High Plasticity Index
Impermeability
Plasticity Properties
Relatively Deformable
Suitable Material – Clay Mineral
Soil Material used in Teton Dam
• Aeolian Silt, also called Idaho Loess Soil.
Classically Silty Soil
Lower plasticity index (PI) value
Slightly cohesive or even cohesionless
Sensitive to water content
Loess Soil
(https://commons.wikimedia.org/wiki/
File:LoessVicksburg.jpg)
Fig. The R/size diagram; the relation of bond/weight ratio to particle size for
ideal engineering soils (Smalley and Dijkstra, 1991).
Hydraulic Fracturing
• Finite element analyses
• Distribution of stress at the embankment
• Used to construct stress-strain parameter
• Water pressure is higher than soil’s tensile strength and total
transverse normal stress
• Pressure applied with wet condition, volume at key trench fill
decreases. Wetted fill reduce the stress of the soil.
Piping Failure
• Water leaking under the grout
cap due to erosion
• Piping failure along the key
trench fill
Field hydro-fracturing test
• Dye water is used to test the flows of fracture
• Vertical fracture is shown
• Soil at the key trenches and soil within the embankments
• Decrease in stress due to arching in the soil
Cubical soil sample test
• Borehole
• Water pressure increases, flow rate in the hole increases
• Fracturing pressure leads to rapid increase of flow rate, with or
without water pressure increase
• Fracturing happens along vertical planes
• Backfill compact
• Water penetrated to loess soil zone when water pressure is
applied.
• Soil wedge apart
Conclusion
• Stability of dams to protect Lives and property.
• Assessment of risks and liabilities with environmental considerations.
• Proper civil and geotechnical engineering design.
Thank you

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Teton-Dam-slides.pptx

  • 1. An Analysis of Teton Dam Failure, USA
  • 2. Teton Dam Facts • constructed from February 1972 to June 1976. • Bureau of Reclamation designed Teton Dam. • Construction contract awarded to Morrison-Knudsen Company, Inc. • located in southeastern Idaho, 12 miles northeast of Rexburg.
  • 3.
  • 5.
  • 6. Teton Dam Failure • Failed on June 5th , 1976. • 11 deaths resulted from the disaster. • $400 million in property damage. • The towns of Sugar City and Rexburg were struck the hardest.
  • 7.
  • 8.
  • 9. Geology of Teton Dam’s Site • Volcanic Plateau known as Rexburg Bench. • Composed of Basalt and Rhyolite Tuff.  High permeability • Consisted of highly fissured and unstable rock. • Seismically active area. Basalt Rock (https://flexiblelearning.a uckland.ac.nz/rocks_min erals/rocks/basalt.html) Rhyolite Tuff (http://markstein metz.photoshelte r.com/image/I000 0.T6UG4upcSw)
  • 10. Analysis of Soil Material of Dam Core • Required properties for large dam core High Plasticity Index Impermeability Plasticity Properties Relatively Deformable Suitable Material – Clay Mineral
  • 11. Soil Material used in Teton Dam • Aeolian Silt, also called Idaho Loess Soil. Classically Silty Soil Lower plasticity index (PI) value Slightly cohesive or even cohesionless Sensitive to water content Loess Soil (https://commons.wikimedia.org/wiki/ File:LoessVicksburg.jpg) Fig. The R/size diagram; the relation of bond/weight ratio to particle size for ideal engineering soils (Smalley and Dijkstra, 1991).
  • 12. Hydraulic Fracturing • Finite element analyses • Distribution of stress at the embankment • Used to construct stress-strain parameter • Water pressure is higher than soil’s tensile strength and total transverse normal stress • Pressure applied with wet condition, volume at key trench fill decreases. Wetted fill reduce the stress of the soil.
  • 13. Piping Failure • Water leaking under the grout cap due to erosion • Piping failure along the key trench fill
  • 14. Field hydro-fracturing test • Dye water is used to test the flows of fracture • Vertical fracture is shown • Soil at the key trenches and soil within the embankments • Decrease in stress due to arching in the soil
  • 15. Cubical soil sample test • Borehole • Water pressure increases, flow rate in the hole increases • Fracturing pressure leads to rapid increase of flow rate, with or without water pressure increase • Fracturing happens along vertical planes • Backfill compact • Water penetrated to loess soil zone when water pressure is applied. • Soil wedge apart
  • 16. Conclusion • Stability of dams to protect Lives and property. • Assessment of risks and liabilities with environmental considerations. • Proper civil and geotechnical engineering design.