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AASHTO LRFD: Structural Foundations and Earth Retaining Structures ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
? New Legal Load
AASHTO Specification Background: Geotechnical Engineering Presence ,[object Object],[object Object],[object Object],[object Object],[object Object]
History of AASHTO: Design & Construction Specifications for Bridges and Structures ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
“ Geotechnical Scope”:   AASHTO Design & Construction Specifications for Bridges and Structures ,[object Object],[object Object]
Standard and LRFD AASHTO Specifications ,[object Object],[object Object],[object Object]
LRFD IMPLEMENTATION STATUS ,[object Object],[object Object],[object Object]
What are UNIQUE Geotechnical issues related to LRFD? ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
What Should I Know and Do? ,[object Object],[object Object],[object Object],[object Object],[object Object]
What Happening Now? ,[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
A Limit State is a  defined condition  beyond which a structural component, ceases to satisfy the provisions for which it is designed. Resistance is a  quantifiable value that defines  the point beyond which the particular limit state under investigation for a particular component will be exceeded.
Resistance can be defined in terms of: ,[object Object],[object Object],[object Object],[object Object],[object Object]
Limit States ,[object Object],[object Object],[object Object],[object Object],L I S T
Strength Limit State
Extreme Event Limit State
Service Limit State
Service Limit State
Rn / FS      Q  i  i Q i   ≤ R r  =   R n ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Load modifier (eta) Load factor (gamma) Force effect Factored resistance Resistance factor (phi) Nominal resistance
 i  i Q i   ≤ R r  =   R n f(  ,  ) Q n R n Q R    Q n    R n Q or R Probability of Occurrence 
Subsurface Materials ,[object Object],[object Object],[object Object],[object Object]
10.4	SOIL AND ROCK PROPERTIES 10.4.1	Informational Needs 10.4.2	Subsurface Exploration 10.4.3	Laboratory Tests 10.4.3.1	Soil Tests 10.4.3.2	Rock Tests 10.4.4	In-situ Tests 10.4.5	Geophysical Tests 10.4.6	Selection of Design Properties 10.4.6.1	Soil Strength 10.4.6.1.1	Undrained strength of Cohesive Soils 10.4.6.1.2	Drained Strength of Cohesive Soils 10.4.6.1.3	Drained strength of Granular Soils 10.4.6.2	Soil Deformation 10.4.6.3	Rock Mass Strength 10.4.6.4	Rock Mass Deformation 10.4.6.5	erodibility of rock
Overview of Soil and Rock Materials ,[object Object],[object Object],[object Object],[object Object],[object Object]
Soil Characteristics ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Rock Characteristics ,[object Object],[object Object],[object Object],[object Object]
% Finer by Weight Uniform Well Graded Gravel Sand Silt Clay Grain Diameter (mm) 100 100 10 1 0.1 0.01 0.001 US Standard Sieves 3” 2” 1” 3/4 ” 3/8” 4 6 10 20 40 60 100 200 80 60 40 20 0
Atterberg Limits ,[object Object],[object Object],Solid Semi-Solid Plastic Liquid SL PL LL PI Increasing water content
Effective Stress –  Spring Analogy ,[object Object],[object Object],[object Object],[object Object], ’  u P
Soil Shear Strength  ’  = c’ +   n ’ tan   f ’  ’ a  ’ a  ’ r  ’ r  ’  ’ n  ’  ’ n  ’ f  ’  ’ c’ Strength envelope
Undrained Strength of Cohesive Soils, s u Unconfined Compression s u  = q u /2 Vane Shear Test s u  q u  =0 Typical Values s u  = 250 - 4000 psf
Drained Strength of Cohesive Soils, c’ and   ’ f Triaxial Compression  CU Test Typical Values c’ = 100 - 500 psf  ’ f  = 20 o  - 35 o
Drained Strength of Cohesionless Soils,   ’ f Standard Penetration Test (SPT) Typical Values  ’ f  = 25 o  - 45 o Friction angle is correlated to SPT results.  ’ f  ’ q’ c=0
 
Guided Walk Through For N 1 60  = 10, select   ’ f  = 30 o (modified after Bowles, 1977) N 1 60  f <4 25-30 4 27-32 10 30-35 30 35-40 50 38-43
Soil Deformation 0 -2 -4 -6 -8 -10 -12 1 10 100 1000 10000 Time (days) Settlement (in) Initial elastic settlement (all soils) Primary consolidation Secondary consolidation Fine-grained (cohesive) soils
Consolidation Properties Log 10    v ’ Void Ratio (e)  p ’ =  Preconsolidation  Stress C s C r C c 0.1 1 10 100 0.5 1 e o
One log cycle  e=C  =0.06 0.1 1 10 100 1000 10000 Elapsed Time (min) Void ratio (e) 2.65 2.6 2.55 2.5 2.45 2.4 2.35 2.3 2.25 Stress Range, 40 – 80 kPa t p
Typical Consolidation Properties Property Typical Value C c 0.1 to 1.0 C r 10 % of C c C s Approximately C r C  4% to 6% of C c C v 0.01 to 1.0 ft 2 /day
Elastic Properties of Soil ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Rock Properties ,[object Object],[object Object],[object Object],[object Object]
Intact Rock Strength Point Load Test Unconfined Compression, q u Typical Values q u  = 1500 - 50000 psi
Rock Quality Length, L 0.8 ft 0.7 ft 0.8 ft 0.6 ft 0.2 ft 0.7 ft Sound Not sound, highly weathered Not sound, centerline pieces < 4 inches, highly weathered Sound Not sound Sound Core Run Total = 4 ft CR  = 95% RQD  = 53%
CSIR Rock Mass Rating System ,[object Object]
Rock Mass Strength C 1 ’ Shear stress,   Effective Normal Stress,   ’  tm  3  1    ’ i    = (cot   ’ i  – cos   ’ i )mq u /8  ’ i  = tan -1 (4 h cos 2 [30+0.33sin -1 (h -3/2 )]-1) -1/2 h = 1 + 16(m  ’ n +sq u )/(3m 2 q u )
Rock-Mass Quality and Material Constants ,[object Object]
Intact Rock Deformation, E i ,[object Object],[object Object],[object Object]
Rock Mass Deformation E   = 2 RMR - 100 90 70 50 30 10 In situ  modulus of deformation, E M  (GPa) 10 30 50 70 90 12 10 8 6 4 2 (psi x 10 6 ) Rock mass rating  RMR
Read More About It GEC 5 FHWA-IF-02-034
Jerry A. DiMaggio P. E. Principal Bridge Engineer  TEL: (202) 366-1569 FAX: (202) 366-3077 The best Geotechnical web site in town!  www.fhwa.dot.gov/bridge WOW!  FREE STUFF FROM THE FEDERAL GOVERNMENT!

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Bridge structural foundations-and_earth_retaining_structures

  • 1.
  • 2. ? New Legal Load
  • 3.
  • 4.
  • 5.
  • 6.
  • 7.
  • 8.
  • 9.
  • 10.
  • 11.
  • 12. A Limit State is a defined condition beyond which a structural component, ceases to satisfy the provisions for which it is designed. Resistance is a quantifiable value that defines the point beyond which the particular limit state under investigation for a particular component will be exceeded.
  • 13.
  • 14.
  • 19.
  • 20.  i  i Q i ≤ R r =  R n f(  ,  ) Q n R n Q R  Q n  R n Q or R Probability of Occurrence 
  • 21.
  • 22. 10.4 SOIL AND ROCK PROPERTIES 10.4.1 Informational Needs 10.4.2 Subsurface Exploration 10.4.3 Laboratory Tests 10.4.3.1 Soil Tests 10.4.3.2 Rock Tests 10.4.4 In-situ Tests 10.4.5 Geophysical Tests 10.4.6 Selection of Design Properties 10.4.6.1 Soil Strength 10.4.6.1.1 Undrained strength of Cohesive Soils 10.4.6.1.2 Drained Strength of Cohesive Soils 10.4.6.1.3 Drained strength of Granular Soils 10.4.6.2 Soil Deformation 10.4.6.3 Rock Mass Strength 10.4.6.4 Rock Mass Deformation 10.4.6.5 erodibility of rock
  • 23.
  • 24.
  • 25.
  • 26. % Finer by Weight Uniform Well Graded Gravel Sand Silt Clay Grain Diameter (mm) 100 100 10 1 0.1 0.01 0.001 US Standard Sieves 3” 2” 1” 3/4 ” 3/8” 4 6 10 20 40 60 100 200 80 60 40 20 0
  • 27.
  • 28.
  • 29. Soil Shear Strength  ’ = c’ +  n ’ tan  f ’  ’ a  ’ a  ’ r  ’ r  ’  ’ n  ’  ’ n  ’ f  ’  ’ c’ Strength envelope
  • 30. Undrained Strength of Cohesive Soils, s u Unconfined Compression s u = q u /2 Vane Shear Test s u  q u  =0 Typical Values s u = 250 - 4000 psf
  • 31. Drained Strength of Cohesive Soils, c’ and  ’ f Triaxial Compression CU Test Typical Values c’ = 100 - 500 psf  ’ f = 20 o - 35 o
  • 32. Drained Strength of Cohesionless Soils,  ’ f Standard Penetration Test (SPT) Typical Values  ’ f = 25 o - 45 o Friction angle is correlated to SPT results.  ’ f  ’ q’ c=0
  • 33.  
  • 34. Guided Walk Through For N 1 60 = 10, select  ’ f = 30 o (modified after Bowles, 1977) N 1 60  f <4 25-30 4 27-32 10 30-35 30 35-40 50 38-43
  • 35. Soil Deformation 0 -2 -4 -6 -8 -10 -12 1 10 100 1000 10000 Time (days) Settlement (in) Initial elastic settlement (all soils) Primary consolidation Secondary consolidation Fine-grained (cohesive) soils
  • 36. Consolidation Properties Log 10  v ’ Void Ratio (e)  p ’ = Preconsolidation Stress C s C r C c 0.1 1 10 100 0.5 1 e o
  • 37. One log cycle  e=C  =0.06 0.1 1 10 100 1000 10000 Elapsed Time (min) Void ratio (e) 2.65 2.6 2.55 2.5 2.45 2.4 2.35 2.3 2.25 Stress Range, 40 – 80 kPa t p
  • 38. Typical Consolidation Properties Property Typical Value C c 0.1 to 1.0 C r 10 % of C c C s Approximately C r C  4% to 6% of C c C v 0.01 to 1.0 ft 2 /day
  • 39.
  • 40.
  • 41. Intact Rock Strength Point Load Test Unconfined Compression, q u Typical Values q u = 1500 - 50000 psi
  • 42. Rock Quality Length, L 0.8 ft 0.7 ft 0.8 ft 0.6 ft 0.2 ft 0.7 ft Sound Not sound, highly weathered Not sound, centerline pieces < 4 inches, highly weathered Sound Not sound Sound Core Run Total = 4 ft CR = 95% RQD = 53%
  • 43.
  • 44. Rock Mass Strength C 1 ’ Shear stress,  Effective Normal Stress,  ’  tm  3  1    ’ i  = (cot  ’ i – cos  ’ i )mq u /8  ’ i = tan -1 (4 h cos 2 [30+0.33sin -1 (h -3/2 )]-1) -1/2 h = 1 + 16(m  ’ n +sq u )/(3m 2 q u )
  • 45.
  • 46.
  • 47. Rock Mass Deformation E  = 2 RMR - 100 90 70 50 30 10 In situ modulus of deformation, E M (GPa) 10 30 50 70 90 12 10 8 6 4 2 (psi x 10 6 ) Rock mass rating RMR
  • 48. Read More About It GEC 5 FHWA-IF-02-034
  • 49. Jerry A. DiMaggio P. E. Principal Bridge Engineer TEL: (202) 366-1569 FAX: (202) 366-3077 The best Geotechnical web site in town! www.fhwa.dot.gov/bridge WOW! FREE STUFF FROM THE FEDERAL GOVERNMENT!