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Liquefaction of soil By Dr. J.N.Jha Professor Department of Civil Engineering Guru Nanak Dev Engineering College Ludhiana Email: jagadanand@gmail.com
Chile earthquake 1960 :  An island near Valdivia- Mag. 9.5   Large settlements and differential settlements of the ground surface - Compaction of loose granular soil by  EQ
Japan earthquake 1964:  Niigata- Mag. 7.5 Settlement and tilting of structures - liquefaction of soil
Alaska earthquake 1964:Mag. 9.2   Major landslide - combination of dynamic stresses and induced pore water pressure
Caracas earthquake 1967: Mag. 6.6 Response of building  during EQ found to depend on the thickness of soil under the building.
Observed Damage from Earthquakes  ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Seismic waves Arrival of Seismic waves at site ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Influence of local soil conditions on Acceleration(Cause for damage during EQ)  ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
 
Site approximately same distance from the zone of energy release
Development of Peak/Max. Acceleration ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Sites  (Increasing order of softness) Period (sec) (Maximum spectral acceleration)  A 0.3 B 0.5 C 0.6 D 0.8 E 1.3 F 2.5
velop
[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],Building  Response variation during Earthquake
[object Object],[object Object],[object Object],[object Object]
Damage potential coefficient varies with building characteristics and soil depth
Relationship between building characteristics, soil depth and damage potential coefficient (S v /k) Structure Fundamental period Damage intensity (D r ) 2 to 3 storey 0.2 sec Remains same regardless of soil depth 4 to 5 storey 0.4 sec Max. damage intensity expected at soil depth of about 20 to 30 m 10 to 12 storey 1.0 sec Damage intensity expected to increase with soil depth up to 150 m or so 15 to 20 storey Damage intensity even greater for soil depth of 150 to 250 m & relatively low for soil depth up to 80 m or so
Liquefaction of Soil ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Total stress, Pore water pressure and Effective stress Figure-1 Figure-2 Case Total Pressure Pore Pressure Effective Pressure Figure- 1 475 150 325 Figure- 2 475 250 225
 
Liquefaction of Soil ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
 
Influence of soil conditions on liquefaction potential
Liquefaction Damage:  1964  Niigata,  Japan
Tokachi-oki Earthquake: 2003 The Damage of Sewerage Structures kushiro (Town) Lifted up manhole and gushed soil  during liquefaction Lifted up manhole
The Damage of Sewerage Structures Failure Mode   (notice : this is only concept) Replaced Soil (Liquefied) Lift-up Force Crack or Residual Strain Sand Boiling Sand Boiling Manhole Flexible Pipe Rigid Pipe Residual Strain Original Soil (Liquefied)
The Damage of Embankment Structures Toyokoro Collapsed Embankment
Place where Embankment was collapsed Abashiri River  (1) Shibetsu River  (6) Kushiro River  (5) Kiyomappu River  (2) Tokachi River  (66) Under investigation Lateral Spread was observed ( ) : the number of collapsed points Tokachi River The Damage of Embankment Structures
Toyokoro Liquefied Soil Collapsed Embankment The Damage of Embankment Structures Liquefied Soil
Failure Mode   (notice : this is only concept) Liquefied Stratum Embankment Settlement Land Slide Lateral Spread The Damage of Embankment Structures
The Damage of Port Structures  (at Kushiro Port) Kushiro Settlement behind Quay Wall Trace of Sand Boiling
Alaska Earthquake ( 1964 )
 
Caracas ( 1967 )
Alaska  2002 Boca del Tocuyo, Venezuela,  1989
Lateral spread at Budharmora ( Bhuj, 2001 )
Arial view of kandla port, Marked line sows ground crack and sand ejection (Gujrat Earthquake 2001)
Adverse effects of liquefaction Most catastrophic ground failure Lateral displacement of large masses of soil Mass comprised of completely liquefied soil or blocks of intact material riding on a layer of liquefied soil Flow develop in loose saturated sand or silts or relatively steep slope (>3 degree) Flow failure
Lateral Spread ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Ground oscillation ,[object Object],[object Object],[object Object]
Loss of bearing strength ,[object Object],[object Object]
 
Soil conditions  in Areas where  Liquefaction  has  occurred : Case Study:  Niigata Earthquake
Survey of damaged structure(Liquefaction Zone) Zone Damage Soil Characteristics Water table Remark A No damage (Coastal dune area) Dense Sand soil up to depth of 100 ft At great depth from ground level ,[object Object],[object Object],[object Object],[object Object],[object Object],B Relatively light damage (Low land area)  Medium to light  Sand soil up to depth of 100 ft Depth of water table less than ‘A’ C Damage and Liquefaction (Low land area) Medium to light  Sand soil up to depth of 100 ft Depth of water table less than ‘A’ But similar to ‘B’
Standard Penetration Resistance Test (Zone-B & C)   ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Soil Foundation condition and Building Performance (Zone-C) ,[object Object],[object Object],[object Object],[object Object]
Classification of extent of damage for each building (Zone-C)  ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
 
Relationship between depth of pile, ‘N’  of sand at pile tip and Extent of Damage (Zone-C)
Case Study :  Gujrat Earthquake, 2001 ,[object Object],S.No. Region Type of Soil 1 Ahmedabad and Surrounding region Alluvial belt 2 Bhuj and Surrounding region Silty sand 3 Coastal area (Kandla) Soft clay 4 South Gujrat Expansive Clay
Condition of soil before and after earthquake Relative density (D) of sand with depth before and after earthquake D vs depth of layer of three section charaterized by predominant period T p  of microseismic vibrations
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Case Study: Others sites Site Soil Property Standard Penetration Mino-Owari,Tonankai and Fukui Earthquakes D 10 ~ 0.05 to 0.25 mm Uniformity coefficient < 5 <10 (upper 30 ft) Jaltipan Earthquake D 10 ~ 0.01 to 0.1 mm Uniformity coefficient ~2 to 10 Alaska Earthquake D 10 ~ 0.01 to 0.1 mm Uniformity coefficient ~2 to 4 < 20 to 25
What are the options for liquefaction mitigations? ,[object Object],[object Object],[object Object]
Counter measures against Liquefaction ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Uttarkashi Earthquake, 1991 ,[object Object],[object Object],[object Object]
Cross-section(Retaining Geogrid Reinforced cohesionless backfill)
Field Performance of wall 4 O.P. Fixed in the Wall: To monitor the lateral movement of wall top away from backfill using Electronic Distance Meter for a period of 36 months
Average Lateral Deflection of wall with time ,[object Object],[object Object],[object Object],[object Object],[object Object]
Hyogoken Nambu Earthquake  1995 Height of wall – 4 to 8 m Conventional Retaining Wall – suffered maximum damage  Geo-synthetic reinforced soil  retaining wall –Performed very well  (due to relatively high ductility  of the wall)
[object Object],[object Object],[object Object]
Preloading for oil tanks ,[object Object],[object Object],[object Object],B- Before Preloading, A – After Preloading   Depth Range (Metre)  SPT Resistance (Bloe/0.3m) B  A 0  -  5.5 6  22 5.5 -  8.0 22  34 8.0 -  26.0 10  39
Rokko & Port (Kobe) ,[object Object],[object Object],[object Object],[object Object],[object Object]
SAFETY AGAINST LIQUEFACTION Zone Depth below ground level ‘ N’ value III, II, I Up to 5 m 15 III, II, I Up to 10 m 25 I and II (For important structure) Up to 5 m 10 I and II (For important structure) Up to 10 m 20
Liquefaction Analysis ,[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Time history of shear stress during earthquake for liquefaction analysis
Cyclic resistance ratio   ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Foundation (Guidelines) ,[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Foundation of modern building that survived earthquake ,[object Object],[object Object],[object Object],[object Object],[object Object]
 
Can Liquefaction be predicted? ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Criteria for liquefaction potential map ,[object Object],[object Object],[object Object],[object Object]
Is it possible to prepare for liquefaction ? ,[object Object],[object Object],[object Object],[object Object]
Acknowledgements ,[object Object],[object Object],[object Object],[object Object]

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Liquefaction of Soil

  • 1. Liquefaction of soil By Dr. J.N.Jha Professor Department of Civil Engineering Guru Nanak Dev Engineering College Ludhiana Email: jagadanand@gmail.com
  • 2. Chile earthquake 1960 : An island near Valdivia- Mag. 9.5 Large settlements and differential settlements of the ground surface - Compaction of loose granular soil by EQ
  • 3. Japan earthquake 1964: Niigata- Mag. 7.5 Settlement and tilting of structures - liquefaction of soil
  • 4. Alaska earthquake 1964:Mag. 9.2 Major landslide - combination of dynamic stresses and induced pore water pressure
  • 5. Caracas earthquake 1967: Mag. 6.6 Response of building during EQ found to depend on the thickness of soil under the building.
  • 6.
  • 7.
  • 8.
  • 9.  
  • 10. Site approximately same distance from the zone of energy release
  • 11.
  • 12. velop
  • 13.
  • 14.
  • 15.
  • 16. Damage potential coefficient varies with building characteristics and soil depth
  • 17. Relationship between building characteristics, soil depth and damage potential coefficient (S v /k) Structure Fundamental period Damage intensity (D r ) 2 to 3 storey 0.2 sec Remains same regardless of soil depth 4 to 5 storey 0.4 sec Max. damage intensity expected at soil depth of about 20 to 30 m 10 to 12 storey 1.0 sec Damage intensity expected to increase with soil depth up to 150 m or so 15 to 20 storey Damage intensity even greater for soil depth of 150 to 250 m & relatively low for soil depth up to 80 m or so
  • 18.
  • 19. Total stress, Pore water pressure and Effective stress Figure-1 Figure-2 Case Total Pressure Pore Pressure Effective Pressure Figure- 1 475 150 325 Figure- 2 475 250 225
  • 20.  
  • 21.
  • 22.  
  • 23. Influence of soil conditions on liquefaction potential
  • 24. Liquefaction Damage: 1964 Niigata, Japan
  • 25. Tokachi-oki Earthquake: 2003 The Damage of Sewerage Structures kushiro (Town) Lifted up manhole and gushed soil during liquefaction Lifted up manhole
  • 26. The Damage of Sewerage Structures Failure Mode   (notice : this is only concept) Replaced Soil (Liquefied) Lift-up Force Crack or Residual Strain Sand Boiling Sand Boiling Manhole Flexible Pipe Rigid Pipe Residual Strain Original Soil (Liquefied)
  • 27. The Damage of Embankment Structures Toyokoro Collapsed Embankment
  • 28. Place where Embankment was collapsed Abashiri River (1) Shibetsu River (6) Kushiro River (5) Kiyomappu River (2) Tokachi River (66) Under investigation Lateral Spread was observed ( ) : the number of collapsed points Tokachi River The Damage of Embankment Structures
  • 29. Toyokoro Liquefied Soil Collapsed Embankment The Damage of Embankment Structures Liquefied Soil
  • 30. Failure Mode   (notice : this is only concept) Liquefied Stratum Embankment Settlement Land Slide Lateral Spread The Damage of Embankment Structures
  • 31. The Damage of Port Structures (at Kushiro Port) Kushiro Settlement behind Quay Wall Trace of Sand Boiling
  • 33.  
  • 35. Alaska 2002 Boca del Tocuyo, Venezuela, 1989
  • 36. Lateral spread at Budharmora ( Bhuj, 2001 )
  • 37. Arial view of kandla port, Marked line sows ground crack and sand ejection (Gujrat Earthquake 2001)
  • 38. Adverse effects of liquefaction Most catastrophic ground failure Lateral displacement of large masses of soil Mass comprised of completely liquefied soil or blocks of intact material riding on a layer of liquefied soil Flow develop in loose saturated sand or silts or relatively steep slope (>3 degree) Flow failure
  • 39.
  • 40.
  • 41.
  • 42.  
  • 43. Soil conditions in Areas where Liquefaction has occurred : Case Study: Niigata Earthquake
  • 44.
  • 45.
  • 46.
  • 47.
  • 48.  
  • 49. Relationship between depth of pile, ‘N’ of sand at pile tip and Extent of Damage (Zone-C)
  • 50.
  • 51. Condition of soil before and after earthquake Relative density (D) of sand with depth before and after earthquake D vs depth of layer of three section charaterized by predominant period T p of microseismic vibrations
  • 52.
  • 53. Case Study: Others sites Site Soil Property Standard Penetration Mino-Owari,Tonankai and Fukui Earthquakes D 10 ~ 0.05 to 0.25 mm Uniformity coefficient < 5 <10 (upper 30 ft) Jaltipan Earthquake D 10 ~ 0.01 to 0.1 mm Uniformity coefficient ~2 to 10 Alaska Earthquake D 10 ~ 0.01 to 0.1 mm Uniformity coefficient ~2 to 4 < 20 to 25
  • 54.
  • 55.
  • 56.
  • 58. Field Performance of wall 4 O.P. Fixed in the Wall: To monitor the lateral movement of wall top away from backfill using Electronic Distance Meter for a period of 36 months
  • 59.
  • 60. Hyogoken Nambu Earthquake 1995 Height of wall – 4 to 8 m Conventional Retaining Wall – suffered maximum damage Geo-synthetic reinforced soil retaining wall –Performed very well (due to relatively high ductility of the wall)
  • 61.
  • 62.
  • 63.
  • 64. SAFETY AGAINST LIQUEFACTION Zone Depth below ground level ‘ N’ value III, II, I Up to 5 m 15 III, II, I Up to 10 m 25 I and II (For important structure) Up to 5 m 10 I and II (For important structure) Up to 10 m 20
  • 65.
  • 66.
  • 67.
  • 68.
  • 69.
  • 70.
  • 71.
  • 72.  
  • 73.
  • 74.
  • 75.
  • 76.