View
7
Download
0
Category
Preview:
Citation preview
FOUNDATIONS ON SHRINKING AND SWELLING SOILS
(Prediction of Movement, Construction Issues)
Department of Civil Engineering, Texas A&M University, College Station,
Texas 77843-3136, USA
by
Jean-Louis Briaud, Sangho Moon, Xiong Zhang
J.L. Briaud, Texas A&M University
• ENVIRONMENTAL SOIL STABILIZATION LTD.
Russ Scharlin
Johny Sherwood
• SPENCER J. BUCHANAN PROFESSORSHIP
• GILES ENGINEERING ASSOCIATES INC.
Doug Dayton
ACKNOWLEDGEMENTSJ.L. Briaud, Texas A&M University
• FUNDAMENTAL BEHAVIOR
• SHRINK TEST – WATER CONTENT METHOD
• CASE STUDY
• SMART FOUNDATION
OUTLINEJ.L. Briaud, Texas A&M University
Saturated
uw ≠≠≠≠ 0ua = 0
σσσσ’ = σσσσ - uw
Occluded Air
uw = ua
σσσσ’ = σσσσ - uw
Continuous Air
uw ≠≠≠≠ 0ua = 0
σσσσ’ = σσσσ - ααααu
soil grain water
soil grain waterair
soil grainwaterair
J.L. Briaud, Texas A&M University
u0+-
hc
αααα ααααT T
Glass
ContractileSkin
Water
- 1,000 kPa
d
Water
ãd
á cos T 4 h
wc ====
mN/m 72 T where ====
h
Atmosphericpressure
hγγγγw
hcγγγγw0 kPa
J.L. Briaud, Texas A&M University
Pure Water Salt Water
initial state Initial stateafter time, t
after time, th = Osmotic Suction
J.L. Briaud, Texas A&M University
109 108Bottom of DeepestOcean
105 104Deepest OffshorePlatforms
Compression
103 102Large River
100 %0 0 0
25 to 50 %2 -102 -101Field Capacity
Swell Limit
8 to 15 %Near 100 %4 -104 -103Shrinkage LimitTension
6 -106 -105Air DrySuction NO
YES
YES
NO
007 -107 -106Oven Dry
ShrinkSwellWater
ContentDegree ofSaturation
Suction
pF cm kPaExamplesWater State
J.L. Briaud, Texas A&M University
Soil State Swell Shrink
Unsaturated Yes No
Saturated Yes Yes
Saturated No Yes
GWL
u0 +-
J.L. Briaud, Texas A&M University
PHASE DIAGRAMSJ.L. Briaud, Texas A&M University
w
wSW
∆∆∆∆V/V
wSH
wi
∆∆∆∆((((∆∆∆∆V/V)max
0
∆∆∆∆wmaxSaturated orOccluded Air
J.L. Briaud, Texas A&M University
SHRINK TEST PARAMETERS
Do
Ho H
D
WoW
t = 0 t
SHRINK
J.L. Briaud, Texas A&M University
SHRINK TEST
Shrink Test
25
20
15
10
5
Shrink Test Example (B/RF1/6)
0.3-0.9 m,Ew = 0.86, w = 17.15 %
1.2-1.8 m, Ew = 0.69, w = 21.66 %
2.1-2.7 m, Ew =0.83, w = 16.03 %
data chosen for calculation of Ew
-0.2 -0.15 -0.1 -0.05 0
Wat
er C
onte
nt, %
Volumetric Strain, ∆∆∆∆V/V
J.L. Briaud, Texas A&M University
SHRINK TEST RESULTS (1)
0 10 20 30 40 50 60 t, hr
0.0
-0.05
-0.10
-0.15
∆∆∆∆ H/H
o
-0.30 -0.25 -0.20 -0.15 -0.10 -0.05 0 ∆∆∆∆V/Vo
∆∆∆∆ H/H
o f1
f1
0.0
-0.05
-0.10
-0.15
0.4
∆∆∆∆V/Vo-0.30 -0.25 -0.20 -0.15 -0.10 -0.05 0
w
Ew1
1 Ew
wo
wsh wsh
0.3
0.2
0.1
0.0
wo
Porcelain Clay Bentonitic Clay
Porcelain Clay Bentonitic Clay
Porcelain Clay Bentonitic Clay
Porecelain Clay and Bentonite Clay
J.L. Briaud, Texas A&M University
SWELL TEST
Porous stone
Porous stoneSoil sample
Consolidometer
lOAD
L
∆∆∆∆2∆∆∆∆1
-0.015
-0.010
-0.005
0.000
0.005
0.010
0
Time, hrs
∆∆∆∆ H/H
0.00954
0.00458
-0.00996
Swell withno OverburdenPressure
Swell underOverburdenPressure
Recompressionunder Overburden Pressure
Max. SwellUnder Overburden,(∆H/H)PS
MaximumFree % Swell,(∆H/H)FS
% Recovery,(∆H/H)P
0 50 100 150 200 250 300
Swell Test Example (B/RF1/6 0.3–0.9 m)Swell Test
J.L. Briaud, Texas A&M University
EXAMPLE OF THE PREMISS METHODJ.L. Briaud, Texas A&M University
∆∆∆∆H/Ho-0.08 -0.06 -0.04 -0.02 0 0.02
∆∆∆∆V/Vo-0.2 -0.16 -0.12 -0.08 -0.04 0 0.04
0.25
0.20
0.15
0.10
0.05
0.00
w
∆∆∆∆D/Do-0.08 -0.06 -0.04 -0.02 0 0.02
0.25
0.20
0.15
0.10
0.05
0.00
0.25
0.20
0.15
0.10
0.05
0.00
ww
Sample(S) Overburden(O)
S (S1)S+O (S2)
Sample(S) Overburden(O)
S (S1)S+O (S2)
Sample(S) Overburden(O)
S (S1)S+O (S2)
SHRINK TEST RESULTS (3)
Influence of Vertical Pressure
J.L. Briaud, Texas A&M University
-0.4 -0.2 0.0 0.2 0.4 0.6 ∆∆∆∆V/Vo
∆∆∆∆ w
0.4
0.2
0.0
-0.2
-0.4
-0.6Bentonic Clay
ShrinkSwell
0.2
0.1
0.0
-0.1
-0.2
-0.3
∆∆∆∆ w
-0.20 -0.15 -0.10 -0.05 0.00 0.05 0.10 0.15 0.20 ∆∆∆∆V/Vo
ShrinkSwell
Porcelain Clay
SHRINK AND SWELL TEST RESULTS
Porecelain Clay and Bentonite Clay
J.L. Briaud, Texas A&M University
SUCTION VARIATION WITH DEPTH
Suction, u
Dep
th, z
ue0
zmaxSu
ctio
n E
nvel
ope
Suct
ion
Env
elop
e
u(z,t)
∆∆∆∆u(zmax) = 0.1×××× 2∆∆∆∆u0
∆∆∆∆u0∆∆∆∆u0
After Mitchell (1979)
J.L. Briaud, Texas A&M University
After Mitchell (1979)
z) ) á T /(-(∂ exp Äu 2Äu(z) 0.500====
) Äu(Äw f====0.5
0max ) á T (3.1z ====
characteristic curve
∆u = change in suction at depth z∆u0 = change in suction at ground surfaceT0 = period of weather cycleαααα = diffusion coefficientz = depth below ground surface∆w = change in water contentzmax = maximum depth of water content change
where
J.L. Briaud, Texas A&M University
After Styron et al. (2001)
30 (%) LL LI ±±±±====××××
)(PI/LL0.6Äw ====
J.L. Briaud, Texas A&M University
WATER CONTENT VARIATION AS A FUNCTION OF TIME
Ave
rage
Wat
er C
onte
nt
0.35
0.30
0.25
0.20
0.15
0.10
0.05
0.00 Fall Winter Spring Summer Fall Winter Spring 1992 1993 1993 1993 1993 1994 1994
CC = Corpus Christi (0-0.5m)SA = San Antonio (0-0.5m)CS = College Station (0-1.5m)OUTSIDE = Outside the Foundation ImprintUNDER = Under the Foundation Imprint
Time for SA and CC
Time for CS Fall Winter Spring Summer Fall Winter Spring 1993 1994 1994 1994 1994 1995 1995
CC OUTSIDESA OUTSIDE
CC UNDER
SA UNDER CS OUTSIDE
From Posey, Briaud, 1995, Woodfin, Briaud, 1997
J.L. Briaud, Texas A&M University
Hi
w
∆∆∆∆wiwi
z
w
wi+
∆∆∆∆ wi
wi
εεεεi+ ∆∆∆∆εεεεi εεεεi εεεεv
∑∑∑∑ ∑∑∑∑========i w
iiii E
ÄwfHÄåHS
MOISTURE INDUCED MOVEMENTJ.L. Briaud, Texas A&M University
∑∑∑∑∑∑∑∑ ========i
iiii E
ÄHÄåHS
σσσσ
εεεεi+∆∆∆∆εεεεi εεεεi εεεεvσσσσ ’
ov++++ ∆∆∆∆
σσσσ ’i
σσσσ ’ov
σσσσv
WEIGHT INDUCED SETTLEMENT
σσσσv
∆∆∆∆σσσσ’iσσσσ’ovHi
z
P
J.L. Briaud, Texas A&M University
PLAN VIEW OF THE SITE
Boring date
# 1 : 06/24/99# 2 : 07/13/99# 3 : 10/25/99# 4 : 02/11/00# 5 : 05/11/00# 6 : 08/11/00# 7 : 11/17/00# 8 : 03/13/01# 9 : 07/15/01
BM1
BM2
W2 RF2
W1
RF1
3m
2m 2m
0.6m
Boringlocation
Boringorder
..0.61m
0.67m
1 - deep.
0.67m
B/W1/7 redrill - deep
0.67m
.
...
. ..1
2 34
5 6
7
..
8
9
.
...
. ..1
2 34
5 6
7
..
8
9
.
...
. ..1
2 34
5 6
7
..
8
9
.
...
. ..1
2 34
5 6
7
..
8
9
NorthSite in Arlington,Texas
J.L. Briaud, Texas A&M University
SOIL STRATIGRAPHY
Dep
th,m
Legend
RF : Reference
W : Water injected
BM : Benchmark
1.5
2
2.5
3
0.5
1
0
Su = 179.8 kPawmean = 19.74 %h = 3.41 pFLL = 40.4, PL = 17.1
2m 2m
0.6m
Brown Silty Clay, trace fine Sand : Calcareous
γt = 20.4 kN/m3
Ew = 0.869, f = 0.39%SW = 4.31%<0.002= 45.5
NorthA’
W1
20m
10m
10m
RF2
W2RF1
A
BM2BM1
Su = 151.5 kPawmean = 20.73 %h = 3.42 pFLL = 51.3, PL = 22.3
Dark Gray Silty Clay : Trace Fine Sand
γt = 20.3 kN/m3
Ew = 0.752, f = 0.39%SW = 5.17%<0.002= 47.7
A A’
GWL : 4.27 m (Jun./25/99) 4.8 m (Feb./1/01) 4 m (Jul./15/01)
Site in Arlington,Texas
J.L. Briaud, Texas A&M University
WATER CONTENT AND SUCTION vs. DEPTH
0.0
0.5
1.0
1.5
2.0
2.5
3.0
3.5
4.0
0 1 2 3 4 5
B:Boring B1 B2 B3 B4 B5 B6 B7 B8 B9
Dep
th, m
Suction, pF
0.0
0.5
1.0
1.5
2.0
2.5
3.0
3.5
4.0
0.00 0.05 0.10 0.15 0.20 0.25 0.3
B:Boring B1 B2 B3 B4 B5 B6 B7 B8 B9
Dep
th, m
Water ContentFooting RF1 at a sitein Arlington, Texas
J.L. Briaud, Texas A&M University
GARNER’S STUDY (1999)
3 samples at 3 water contents sent to 5 laboratory.
Water Content, %
Sample 1
Sample 2
Sample 3
Suction, pF
Sample 1
Sample 2
Sample 3
Suction, kPa
Sample 1
Sample 2
Sample 3
0 5 10 15 20 25 30 %
0 1 2 3 4 5 pF
0 250 500 750 1000 kPa
0 500 1000 1500 2000 kPa
J.L. Briaud, Texas A&M University
∆∆∆∆V/Vo
0.30
0.25
0.20
0.15
0.10
0.05
0.00
w
-0.30 -0.25 -0.20 -0.15 -0.10 -0.05 0.00
B/RF1/4 0.3 – 0.9 m, Ew = 0.67 1.2 – 1.8 m, Ew = 0.60 2.1 – 2.7 m, Ew = 1.30
-0.30 -0.25 -0.20 -0.15 -0.10 -0.05 0.00 ∆∆∆∆V/Vo
B/RF2/4 0.3 – 0.9 m, Ew = 0.86 1.2 – 1.8 m, Ew = 0.76 2.1 – 2.7 m, Ew = 1.19
0.30
0.25
0.20
0.15
0.10
0.05
0.00
w
Three SamplesFrom Arlington,Texas
SHRINK TEST RESULTS (2)J.L. Briaud, Texas A&M University
SELECTED SOIL TEST RESULT FOR RF1
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Dep
th, m
0 0.5 1 1.5 2
Ew
0.1 0.3 0.5 0.7
f % SW
0 2.5 5 7.5 10
B3 B4 B5 B6 B7
J.L. Briaud, Texas A&M University
FOOTING MOVEMENT OVER TWO YEARS
08/1
/199
9
09/1
/199
9
10/1
/199
9
11/1
/199
9
12/1
/199
9
01/1
/200
0
02/1
/200
0
03/1
/200
0
04/1
/200
0
05/1
/200
0
06/1
/200
0
07/1
/200
0
08/1
/200
0
09/1
/200
0
10/1
/200
0
11/1
/200
0
12/1
/200
0
01/1
/200
1
02/1
/200
1
03/1
/200
1
04/1
/200
1
05/1
/200
1
06/1
/200
1
07/1
/200
1
08/1
/200
1
09/1
/200
1
40
30
20
10
0
-10
-20
-30
-40
-50
-60
Dis
plac
emen
t, m
m
Date
RF1
RF2
W1
W2
sum
mer
fall
win
ter
spri
ng
sum
mer
fall
win
ter
spri
ng
sum
mer
J.L. Briaud, Texas A&M University
RAINFALL AND TEMPERATURE
Date
08/1
/199
9
09/1
/199
9
10/1
/199
9
11/1
/199
9
12/1
/199
9
01/1
/200
0
02/1
/200
0
03/1
/200
0
04/1
/200
0
05/1
/200
0
06/1
/200
0
07/1
/200
0
08/1
/200
0
09/1
/200
0
10/1
/200
0
11/1
/200
0
12/1
/200
0
01/1
/200
1
02/1
/200
1
03/1
/200
1
04/1
/200
1
05/1
/200
1
06/1
/200
1
07/1
/200
1
08/1
/200
1
09/1
/200
1
Rai
nfal
l, m
m
7
6
5
4
3
2
1
0
Ave. Monthly TemperatureAve. Monthly Rainfall
Tem
perature, oC
35
30
25
20
15
10
5
0
J.L. Briaud, Texas A&M University
WATER CONTENT VARIATION AND MOVEMENT
24
22
20
18
16
Wat
er C
onte
nt, %
Date
30
20
10
0
-10
-20
-30
-40
-50
Dis
plac
emen
t, m
m
Average Measured movements
Average Water content
06/1
/199
9
08/1
/199
9
10/1
/199
9
12/1
/199
9
02/1
/200
0
04/1
/200
0
06/1
/200
0
08/1
/200
0
10/1
/200
0
12/1
/200
0
02/1
/200
1
04/1
/200
1
06/1
/200
1
08/1
/200
1
10/1
/200
1
Average of 4 Footings at a sitein Arlington, Texas
J.L. Briaud, Texas A&M University
60
40
20
0
−20
−40
−60
Dis
plac
emen
t, m
m
−100 0 100 200 300 400 500 600 700 800
Time, days
RF1+ RF2+ W1+ W24
Average Measured movements
Water Content Method
PREDICTED AND MEASURED MOVEMENTS
Average of 4 Footings at a sitein Arlington, Texas
J.L. Briaud, Texas A&M University
HOUSES ON EXPANSIVECLAYS
MOST EXPENSIVENATURAL HAZARDIN THE COUNTRY
J.L. Briaud, Texas A&M University
FOUNDATION SOLUTION
air gap
• Stiffened Slab on Grade
• Elevated Structural Slab on Piers
• Stiffened Slab on Grade & on Piers
• Thin Post Tensioned Slab
J.L. Briaud, Texas A&M University
HOUSES ONEXPANSIVE
CLAYS
VERY DIFFICULT TO PREDICTTHE SOIL MOVEMENT
(WEATHER, VEGETATION, DRAINAGE)
MUCH EASIER TO DESIGNAN ADJUSTABLE FOUNDATION
J.L. Briaud, Texas A&M University
SMART FOUNDATIONJ.L. Briaud, Texas A&M University
SMART FOUNDATION
52.5 ft(16 m)
13.1ft (4 m)
52.5 ft (16 m)
3.5 ft (1.1 m)
3.5 ft(1.1 m)
1ft(0.3 m)
1ft (0.3 m)
13.1ft (4 m)
J.L. Briaud, Texas A&M University
SMART FOUNDATION CONSTRUCTION
Make Cavity Cast Footing & Place Spacer
Excavate Trench Cast Beam
Back Fill
Finish
1ft
J.L. Briaud, Texas A&M University
COST COMPARISON
Conventional Waffle Slab 16 m ×××× 16 m ×××× 0.1 m Slab on Grade with 0.9 m deep ×××× 0.3 m thick Beams every 4 m $24,000
Smart Foundation 16 m ×××× 16 m ×××× 0.1 m Slab on Grade with 0.9 m deep ×××× 0.3 m thick Beams every 4 m and 1 m ××××1 m ××××0.3 m Footings $26,200
~ 10 % Increase in Cost
J.L. Briaud, Texas A&M University
Shrinking Excavation Jack up
SMART FOUNDATION ADJUSTMENT
Front View of Jack up Replace Spacer Finish
Back Fill
1ft
J.L. Briaud, Texas A&M University
FOUNDATION ANALYSIS BY SAFE
Edge drop case beam moment distribution
J.L. Briaud, Texas A&M University
jacking
Edge drop case+ jacking
beam moment distribution
FOUNDATION ANALYSIS BY SAFEJ.L. Briaud, Texas A&M University
• FUNDAMENTAL BEHAVIOR
• SHRINK TEST – WATER CONTENT METHOD PROPOSED
• SHRINK TEST – WATER CONTENT METHOD VERIFIED
• SMART FOUNDATIONS = ADJUSTABLE SOLUTION
CONCLUSIONSJ.L. Briaud, Texas A&M University
Recommended