Consolidation Settlement e H e o VOIDS e f VOIDS H o H f 1 - - PDF document
Consolidation Settlement e H e o VOIDS e f VOIDS H o H f 1 - - PDF document
Consolidation Settlement e H e o VOIDS e f VOIDS H o H f 1 SOLIDS 1 SOLIDS 2.10 1.21 0.89 log 8 0.99 log 800 100 2.10 Compression Index 1.21 10 100
e
SOLIDS VOIDS
1 eo Ho
SOLIDS VOIDS
1 ef Hf H
2.10 1.21 10 100 1000
2.10 1.21 log 800 100 ⁄ 0.89 log 8 0.99
Compression Index
2.10 1.10 10 100 1000
2.10 1.10 log 1000 100 ⁄ 1.00 log 10 1.00 1 1.00
Compression Index
0.14 0.38
0.38 0.14 log 800 100 ⁄ 0.24 log 8 0.27
10 100 1000
Cc Compression Ratio
0.38 0.10 log 800 80 ⁄ 0.28 1 0.28
10 100 1000 0.38 0.10
Silty Sand = 100 pcf ´ = 50 pcf, Cc = 0.25 Surcharge = 125 pcf 20 ft 25 ft 20 ft
Silty Sand = 100 pcf Surcharge = 125 pcf 20 ft 25 ft 10 ft ´ = 50 pcf, Cc = 0.25 10 ft
´ = 50 pcf, Cc = 0.25 Surcharge = 125 pcf 20 ft 20 ft Silty Sand = 100 pcf 25 ft
Surcharge = 125 pcf 20 ft Silty Sand = 100 pcf 25 ft 10 ft 10 ft ´ = 50 pcf, Cc = 0.25
Normally-Consolidated Soils
log log log log
top top bot bot c vo vo vo vo top top bot bot c vf vf vf vf
C H C
´ = 50 pcf, Cc = 0.25 Surcharge = 125 pcf 20 ft 20 ft Silty Sand = 100 pcf 25 ft
Surcharge = 125 pcf 20 ft Silty Sand = 100 pcf 25 ft ´ = 50 pcf, Cc = 0.25 15.45 ft
FINAL GRADE 455.0 Clayey Sand, = 120 pcf, ´ = 60 pcf NC Sandy Clay, ´ = 60 pcf, Cc = 0.25 425.0 440.0 447.0 Compacted Fill, = 125 pcf 444.0 A 10 ft
(Holtz & Kovacs, An Introduction to Geotechnical Engineering, 1981)
OCM
(Holtz & Kovacs, An Introduction to Geotechnical Engineering, 1981)
(Holtz & Kovacs, An Introduction to Geotechnical Engineering, 1981)
Over-Consolidated Soils
log log log log log log
bot bot top top r c p p p p bot bot top top r vo vo vo vo bot bot top top c vf vf vf vf
C C H C C
For cases where the OCM is constant with depth
(Holtz & Kovacs, An Introduction to Geotechnical Engineering, 1981)
Over-Consolidated Soils
log log log log log log
bot bot bot top top top r c p p p p p p p bot bot bot top top top r vo vo vo vo vo vo
- bot
bot bot top top top c vf vf vf vf vf vf f
C C H s C s C s
For cases where the OCM is not constant with depth
p p
- vo
f vf
s d dz s d dz s d dz