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ORIGINAL PAPER Strutted Excavation in Soft Soil Incorporating a Jet-Grout Base Slab: Analysis Considering the Consolidation Effect Jose ´ Leita ˜o Borges Ricardo Gomes Pinto Received: 1 February 2010 / Accepted: 8 January 2013 / Published online: 19 January 2013 Ó Springer Science+Business Media Dordrecht 2013 Abstract The influence of the consolidation on a strutted excavation in soft soil is analysed using a computer code based on the finite element method. A base jet-grout slab is considered in order to improve stability against bottom heave failure and minimize wall displacements. The numerical model incorporates the Biot consolidation theory (coupled formulation of the flow and equilibrium equations) with soil constitutive relations simulated by the pqh critical state model. Special emphasis is given to the analysis, during and after the construction period, of the pore pressures, shear stresses, stress levels and displacements in the ground, as well as strut compression loads, wall displacements and bending moments, earth pressures on the wall faces and compression loads and bending moments on the jet- grout slab. The safety factor against bottom heave is also evaluated from the finite element analysis considering formulations of the critical state soil mechanics, and also compared to values obtained with traditional methods that use limit equilibrium approach and bearing capacity fundamentals. Keywords Strutted excavation Soft soil Base slab Consolidation Critical state model Coupled analysis 1 Introduction Theoretically, when a strutted excavation is under- taken in a saturated soft clay and the wall is not extended below the excavation base, bottom heave failure occurs if the initial total vertical stress on the base level is higher than bearing capacity of the subjacent soil. The two most frequently quoted methods for analysing bottom heave stability has traditionally been the limit equilibrium approach based on Terzaghi (1943) and Bjerrum and Eide (1956). The latter was calibrated against observed bottom heave failures. In order to improve stability against bottom heave failure, several practical solutions can be considered. One solution is to extend the wall below the excava- tion base, usually down into a stronger stratum (hard stratum). In this case, in simple terms, earth pressure on the wall, below the excavation bottom, is trans- ferred to the hard stratum and to the lower strut levels. However, in practical terms, this solution may not be practicable if the hard stratum lies deeply. If this is the case, one possible solution consists of extending the wall a few meters below the excavation base and, before excavation, constructing a jet-grout slab to support the wall below the excavation level. Another solution consists of using diaphragm walls to act as cross-walls below the excavation base (Fig. 1). This concept was firstly developed by Eide et al. (1972) for constructing a 240 m long section of a double decked subway and railway tunnel in Oslo, J. L. Borges (&) R. G. Pinto Department of Civil Engineering, Faculty of Engineering, University of Porto, Rua Dr. Roberto Frias, 4200-465 Porto, Portugal e-mail: [email protected] 123 Geotech Geol Eng (2013) 31:593–615 DOI 10.1007/s10706-013-9611-0
Transcript

ORIGINAL PAPER

Strutted Excavation in Soft Soil Incorporating a Jet-GroutBase Slab: Analysis Considering the Consolidation Effect

Jose Leitao Borges • Ricardo Gomes Pinto

Received: 1 February 2010 / Accepted: 8 January 2013 / Published online: 19 January 2013

� Springer Science+Business Media Dordrecht 2013

Abstract The influence of the consolidation on a

strutted excavation in soft soil is analysed using

a computer code based on the finite element method.

A base jet-grout slab is considered in order to improve

stability against bottom heave failure and minimize wall

displacements. The numerical model incorporates the

Biot consolidation theory (coupled formulation of the

flow and equilibrium equations) with soil constitutive

relations simulated by the p–q–h critical state model.

Special emphasis is given to the analysis, during and

after the construction period, of the pore pressures, shear

stresses, stress levels and displacements in the ground,

as well as strut compression loads, wall displacements

and bending moments, earth pressures on the wall faces

and compression loads and bending moments on the jet-

grout slab. The safety factor against bottom heave is also

evaluated from the finite element analysis considering

formulations of the critical state soil mechanics, and also

compared to values obtained with traditional methods

that use limit equilibrium approach and bearing capacity

fundamentals.

Keywords Strutted excavation � Soft soil �Base slab � Consolidation � Critical state model �Coupled analysis

1 Introduction

Theoretically, when a strutted excavation is under-

taken in a saturated soft clay and the wall is not

extended below the excavation base, bottom heave

failure occurs if the initial total vertical stress on the

base level is higher than bearing capacity of the

subjacent soil. The two most frequently quoted

methods for analysing bottom heave stability has

traditionally been the limit equilibrium approach

based on Terzaghi (1943) and Bjerrum and Eide

(1956). The latter was calibrated against observed

bottom heave failures.

In order to improve stability against bottom heave

failure, several practical solutions can be considered.

One solution is to extend the wall below the excava-

tion base, usually down into a stronger stratum (hard

stratum). In this case, in simple terms, earth pressure

on the wall, below the excavation bottom, is trans-

ferred to the hard stratum and to the lower strut levels.

However, in practical terms, this solution may not be

practicable if the hard stratum lies deeply.

If this is the case, one possible solution consists of

extending the wall a few meters below the excavation

base and, before excavation, constructing a jet-grout

slab to support the wall below the excavation level.

Another solution consists of using diaphragm walls

to act as cross-walls below the excavation base

(Fig. 1). This concept was firstly developed by Eide

et al. (1972) for constructing a 240 m long section of a

double decked subway and railway tunnel in Oslo,

J. L. Borges (&) � R. G. Pinto

Department of Civil Engineering, Faculty of Engineering,

University of Porto, Rua Dr. Roberto Frias,

4200-465 Porto, Portugal

e-mail: [email protected]

123

Geotech Geol Eng (2013) 31:593–615

DOI 10.1007/s10706-013-9611-0

Norway. In both base-slab and cross-wall solutions,

the retaining wall can be founded on steel piles

extended to the hard stratum, as shown in Fig. 1.

Another pertinent question in excavations in soft

ground is the excess pore pressure generation during

construction and its dissipation after that period

(consolidation). Basically, during the excavation

period, the variation of the stress state in the ground

consists of a decrease of total mean stress and an

increase of deviatoric stress. In saturated normally

consolidated clays, the decrease of total mean stress

induces negative excess pore pressures whereas the

increase of shear stress gives rise to positive pore

pressures. Therefore, the sign of the excess pore

pressure at the end of excavation may be positive or

negative, depending on the magnitude of the above-

mentioned contrary effects. However, field measure-

ments of a number of excavations suggest that, in

general, excess pore pressure is usually negative at the

end of construction (Lambe and Turner 1970; DiBiagio

and Roti 1972; Clough and Reed 1984; Finno et al.

1989).

Thus, after construction there are pore pressure

gradients in the ground that determine a consolidation

process. This process is clearly dependent on both the

magnitude of excess pore pressure at the end of

construction and the long-term equilibrium conditions

regard to pore pressure. These conditions may corre-

spond to a hydrostatic pore pressure distribution or to a

steady flow state.

In the past, studies of excavations in saturated clays

have majority been based on undrained total stress

analyses. However, despite the importance of such

analyses in practice, a more realistic approach consists

of taking into account the consolidation effect during

and after excavation by performing coupled analyses

with adequate soil constitutive models (Potts et al.

1997).

In the present study, the consolidation effect on an

idealized strutted excavation in soft soil incorporating

a jet-grout base slab is analysed by using a computer

program based on the finite element method. This

program was developed by J. L. Borges and incorpo-

rates, among other features, coupled analysis and the

p–q–h critical state model for soil constitutive behav-

iour simulation. The initial version of the program was

presented in Borges (1995), but several improvements

were posteriorly developed, including a 3D coupled

analysis version (Borges 2004).

The study incorporates the analysis, during and

after the excavation period, of pore pressures, shear

stresses, stress levels and displacements in the ground,

as well as strut compression loads, wall displacements

and bending moments, earth pressures on the wall

faces and compression loads and bending moments on

the jet-grout slab. Comparing to the values obtained

with the methods of Terzaghi (1943) and Bjerrum and

Eide (1956), the safety factor against bottom heave is

also evaluated, at several stages of the excavation and

consolidation, with a computer program, described in

Sect. 3, which uses the results of the finite element

analysis and formulations of the critical state soil

mechanics.Fig. 1 Illustration of diaphragm cross-wall concept as used in

the tunnel of Oslo (1973–1975), Norway

594 Geotech Geol Eng (2013) 31:593–615

123

2 Finite Element Program

Basically, for the present applications, the finite

element program uses the following features:

(a) plane strain conditions; (b) coupled formulation

of the flow and equilibrium equations with soil

constitutive relations formulated in effective stresses

(Biot consolidation theory) (Borges 1995; Borges and

Cardoso 2000; Lewis and Schrefler 1987; Britto and

Gunn 1987), applied to all phases of the problem, both

during excavation and in the post-construction period;

(c) utilisation of the p–q–h critical state model (Borges

1995; Borges and Cardoso 1998; Lewis and Schrefler

1987), an associated plastic flow model, to simulate

constitutive behaviour of soil; (d) use of the 2D elastic

linear model to simulate constitutive behaviour of the

wall (reinforced concrete) and of the jet-grout slab;

(e) utilisation of the 1D elastic linear model to

simulate the constitutive behaviour of the struts;

(f) use of joint elements with elastic perfectly plastic

behaviour to simulate the soil–wall and soil–slab

interfaces.

In the p–q–h model—which is a extension

(improvement) of the Modified Cam-Clay model into

the three-dimensional stress space using the Mohr–

Coulomb failure criteria—the parameter that defines

the slope of the critical state line, M, is not constant

(which happens in the Modified Cam-Clay model), but

depends on the angular stress invariant h and effective

friction angle, /0:

M ¼ 3sin/0

ffiffiffi

3p

cos hþ sin/0sinh

ð1Þ

This defines the Mohr–Coulomb criteria when M is

introduced in the equation of the critical state line

q ¼ M � p ð2Þ

where p is the effective mean stress and q the

deviatoric stress.

This is an important feature of the p–q–h model

because, as shown in triaxial and plane strain tests

(Mita et al. 2004), the soil critical state depends on h.

This means, for instance, that, in the p–q–h model,

M takes different values whether compression or

extension stress paths take place, which does not occur

in the Modified Cam-Clay model. Numerical and

laboratorial results presented by several authors (Potts

and Zdravkovics 1999; Mita et al. 2004) showed that

strain–stress behaviour of the soil in plane strain

analyses is much better simulated if the slope of the

critical state line is defined according to the Mohr–

Coulomb criteria, which happens in the p–q–h model.

Figure 2a shows, in the principal effective stress

space, the yield and critical state surfaces of the p–q–hmodel. In the p–q plane, the yielding function is an

ellipse (Fig. 2b) and, depending on the over-consol-

idation ratio, the p–q–h model simulates hardening

behaviour or softening behaviour. Hardening occurs in

normally consolidated or lightly overconsolidated

clays while softening occurs in medially to strongly

overconsolidated clays.

The accuracy of the finite element program used in

the present study has been assessed against field

measurements (which is the adequate way for complex

problems without theoretical solutions) and used to

analyse a wide range of geotechnical structures

involving consolidation (Borges 1995, 2008; Costa

2005; Domingues 2006; Costa et al. 2007). With

regard to embankments on soft ground, Borges (1995)

compared numerical and field results of two geosyn-

thetic-reinforced embankments, one constructed up to

failure (Quaresma 1992) and the other observed until

the end of consolidation (Yeo 1986; Basset 1986a, b).

The accuracy was considered adequate in both cases.

Using the same computer code, very good agreements

with field measurements were also observed both in an

embankment on soft soils incorporating stone columns

(Domingues 2006) and in a braced excavation in a

very soft ground (Costa et al. 2007; Costa 2005). This

last case study was an excavation carried out in the

City of San Francisco, presented by Clough and Reed

(1984), to install a large sewer culvert. As an example

of the accuracy of the computer code in this kind of

works, comparisons of field and numerical results of

this case study are shown below.

Further details of its numerical simulation can be

seen in Costa et al. (2007). The width and maximum

depth of the excavation (Costa et al. 2007) were

approximately 7.6 and 9 m, respectively. The retain-

ing structure consisted of a steel sheet-pile wall braced

at three or four levels. The behaviours of two sections

were monitored—at Rankin Street and at Davidson

Avenue—and compared with numerical results, as

said above. The typical cross section of the excavation

is presented in Fig. 3. The ground was mainly

composed of rubble fill and soft clay (San Francisco

New Bay Mud); at Davidson Avenue the geotechnical

Geotech Geol Eng (2013) 31:593–615 595

123

parameters revealed a weaker soil than at Rankin

Street. At the Davidson Avenue section, two piezom-

eters were installed in the same hole behind the sheet-

pile at depths of 9.1 and 12.2 m. In Fig. 4 numerical

and field results are shown (in y-axis the pore pressure,

u, is divided by the initial pore pressure value, ui, and

in x-axis the evolution of excavation depth is repre-

sented). Although at 9.1 m the computation underes-

timated the decrease of pore pressure, the evolution of

the numerical results was quite similar to the mea-

surements in the field; for the lower piezometer the

agreement was excellent, independently of the exca-

vation depth.

The instrumentation of the excavation also included

some inclinometers, at both Rankin Street and David-

son Avenue sections. Computed and measured hori-

zontal displacements of the wall are shown in Fig. 5.

The behaviour at Rankin Street (Fig. 5a), with small

displacements at the top and tip and a pronounced

convexity of the external face of the wall, was in

agreement with typical patterns observed in similar

works when values of the safety factor against bottom

heave are not low. On the contrary, the pattern of

displacement at Davidson Avenue section (Fig. 5b),

where the soil was weaker, revealed low stability

conditions at the end of the excavation: the external

wall face became concave and the horizontal dis-

placement of its tip reached 23 cm (about 2.5 % of the

excavation depth). At the Rankin Street section, where

field results were available only at the end of the

excavation, a very good similarity of field and

computed results was observed, mainly on the upper

strutted zone of the wall (Fig. 5a). At the Davidson

Avenue section (Fig. 5b), where field measures were

available from stage 2 to stage 4, good agreements

with numerical values were observed, in general. At

stage 2, the computed results were higher than field

values, although a similarity of the curve shape was

(a)

(b)

Originalelasticregion

αp

Criticalstate line

p

ε ( ) qq

ε ( )v

4

3

2

1

Fig. 2 Yield and critical

state surfaces of the p–q–hcritical state model in

a principal effective stress

space and b p–q

596 Geotech Geol Eng (2013) 31:593–615

123

F. L.

Fill

Soft ClayV

aria

ble

3.0

4.5

1.8

4.3

Stage11

Stage

Stage 2

Stage 4

Stage 3

7.6

10.5

m -

R. R

anki

ne

15.0

m -

Dav

idso

n A

v.

Wall bending stiffness:

6.0 x 10 kN/m /m4 2

1st level: 1.3 x 10 kN/m

Axial strut stifness:

2nd/3rd level: 5.8 x 10 kN/m

5

5

Fig. 3 Typical cross

section of the excavation

(Costa et al. 2007)

0.0

0.2

0.4

0.6

0.8

1.0

1.2

0 2 4 6 8 10

Excavation depth (m)

u/ui

(kP

a)

0.0

0.2

0.4

0.6

0.8

1.0

1.2

0 2 4 6 8 10

Excavation depth (m)

u/ui

(kP

a)

Measured

Computed D1

(a) (b)

Fig. 4 Comparison between numerical and field results of pore pressures at Davidson Avenue: a depth of 9.1 m; b depth of 12.2 m

(Costa et al. 2007)

Geotech Geol Eng (2013) 31:593–615 597

123

observed; at stages 3 and 4, on the strutted length of the

wall, the similarity is very good, although some

discrepancies had arisen below the excavation bottom.

3 Program of Bottom Heave Stability Analysis

3.1 Preamble

As said above, the two most quoted methods for

analysing bottom heave stability has traditionally been

the limit equilibrium approach based on Terzaghi

(1943), and Bjerrum and Eide (1956). The latter,

which actually stems from Skempton (1951) and was

calibrated against observed bottom heave failures, is

based on the similarity between the bearing capacity of

a deeply embedded footing and a bottom heave failure

of an excavation.

Figure 6 shows the assumed failure surface of the

Terzaghi (1943) approach when the wall is embedded

below the excavation base. In this case, the value of

the safety factor is given by Eqs. 3 and 4, respectively

for Terzaghi (1943) the Bjerrum and Eide (1956)

methods:

0

5

10

15

20-0.08 -0.06 -0.04 -0.02 0.00

Horizontal displacement (m)

Dep

th (

m)

Stage 2 - Computed Stage 3 - Computed

Stage 4 - Computed 3 months - Computed

Stage 4 - Measured

0

5

10

15

20

25

-0.25 -0.20 -0.15 -0.10 -0.05 0.00

Horizontal displacement (m)

Dep

th (

m)

Stage 2 - Computed

Stage 3 - Computed

Stage 4 - Computed

Stage 4 - Measured

Stage 2 - Measured

Stage 3 - Measured

(a)

(b)

Fig. 6 Failure surface of the Terzaghi (1943) method for

bottom heave stability analysis

Fig. 5 Horizontal displacements of the wall. Comparison

between computed and measured results: a at Rankin Street;

b at Davidson Avenue (Costa et al. 2007)

b

598 Geotech Geol Eng (2013) 31:593–615

123

F ¼ð2þ pÞsu þ cd þ 2dsa

B

H c�ffiffi

2p

su

B

� � ð3Þ

F ¼Ncsu þ cd þ 2dsa

B

cHð4Þ

where su: average strength of the soil in the bottom

heave failure zone below the tip of the wall; sa:

average strength of the soil–wall interface over the

embedded depth d; c: unit weight of soil; H: length of

the wall; B: width of the excavation; d: embedded

depth of the wall below the excavation base; Nc:

bearing capacity factor, which depends on the values

of H, B and L (horizontal length of the excavation),

incorporating the effects of the strength of soil above

the excavation base and of the finite length of

excavation.

In the present study, the analysis of the bottom

heave stability is also evaluated by a computer

program that uses the results of the finite element

analysis with formulations of the critical state soil

mechanics, as described in Sect. 3.2. Considering

circular failure surfaces, similar procedures (in terms

of calculation of acting shear stress and shear strength

along a potential failure surface) were used in the

analysis of the overall stability in cut slopes in clayey

soils (Borges 2008) and in embankments on soft soils

(Borges and Cardoso 2002). However, in the present

study, a different type of failure surface is considered

(see below Fig. 7) since the failure mechanism of the

problem is different from those studied in Borges

(2008) and Borges and Cardoso (2002). The type of

surface proposed herein (Fig. 7) revealed to be the

most unfavourable potential failure surface in strutted

excavations, corresponding to the smallest value of

safety factor calculated from the finite element

analysis. As concluded below (Sect. 5.1), where its

results are compared with those of Terzaghi (1943)

and Bjerrum and Eide (1956) methods, this new

methodology for strutted excavations showed to be

very accurate in estimating the safety factor against

bottom heave, both during and after the excavation

period. The program used in the paper corresponds to

an improvement (generalization) of that used in

Borges (2008) and Borges and Cardoso (2002),

incorporating more complex types of potential failure

surfaces and also taking into account that some parts of

the failure surface can coincide with soil-wall inter-

face elements (like for the failure surface of Fig. 7).

3.2 Evaluation of Safety Factor

Using the results of the finite element analysis, the

program of bottom heave stability analysis computes

the safety factor along a defined failure surface, at any

stage of the excavation and consolidation. Figure 7

illustrates the type of failure surface used in the present

study, which is similar to that assumed in the Terzaghi

(1943) approach, except for the line segment above the

wall tip, which is not vertical but inclined 45�. As said

above, this type of surface revealed to be the most

unfavourable potential failure surface, corresponding

to the smallest value of safety factor calculated from

the results of the finite element analysis.

Firstly, the program determines the intersection

points of the failure line with the edges of the finite

Fig. 7 Failure surface of

the program of bottom heave

stability analysis

Geotech Geol Eng (2013) 31:593–615 599

123

elements of the mesh. This way, the failure line is

divided into small line segments, each of them located

inside of only one of the finite elements of the mesh

(Fig. 8).

Afterwards, the average values of the effective

stresses (r0x, r0y, r0z and sxy, normal and shear stresses in

the xyz-space, where xy is the plane of the 2D-finite

element analysis) at each of those segments are

computed extrapolating from stresses at the Gauss

points of the corresponding finite element. Mathemat-

ical procedures of this extrapolation are described in

detail in Borges (2008).

Thus, considering the failure line divided into line

segments, the safety factor is computed as follows:

F ¼

P

N

i¼1

sfili

P

N

i¼1

sili

ð5Þ

where si: acting shear stress at the i-segment (deter-

mined from effective stresses r0x, r0y, and sxy, known

the angle that defines i-segment direction); sfi: soil

shear strength at i-segment; li: i-segment length; N:

number of mesh elements intersected by the failure

line.

Since soil shear strength varies with consolidation

and a critical state model is used in the finite element

analysis, sfi at each stage is calculated by the following

equation of the critical state soil mechanics (Britto and

Gunn 1987):

sfi ¼1

2M � exp

C� vi

k

� �

ð6Þ

where M is given by Eq. 1, and vi, the specific volume

of soil at i-segment, is determined as follows:

mi ¼ C� k ln pi � ðk� kÞ ln api ð7Þ

At i-segment, pi ¼ ðr0xi þ r0yi þ r0ziÞ=3 is the effective

mean stress and api is the p value of the centre of the

yield surface in p–q plane (see Fig. 2b), extrapolated

from ap-values at Gauss points using the same

mathematical procedures as for stresses; k, k and Care parameters of the p–q–h model (soil properties)

whose meanings are indicated in the next section.

4 Description of the Problem

The idealized problem concerns a 10 m deep excava-

tion with width of 12 m (Fig. 9). The retaining

structure consists of a 0.7 m thick diaphragm wall of

reinforced concrete with length of 12.5 m (2.5 m

below the excavation base). Three steel strut levels are

considered at depths of 1, 4 and 7 m. The excavation is

carried out in a total time of 25 days at a uniform rate.

In order to increase stability against bottom heave

failure and minimize the wall displacements, a 1.3 m

thick jet-grout slab is included (constructed by secant

columns) to support the wall below the excavation

base (Fig. 9). Due to hydraulic reasons, ‘‘dissipation

holes’’ in the jet-grout slab (see Fig. 9b) are con-

structed after excavation in order to avoid long-term

over-pressures on the lower face of the slab. There-

fore, it is assumed that, after the end of excavation, the

water flows through the ‘‘dissipation holes’’, being

pumped within the excavated area. This corresponds

to define the boundary condition of pore pressure on

the lower face of the slab equal to 13 kPa (considering

the unit weight of water equal to 10 kN/m3 and that the

thickness of the slab is 1.3 m).

The ground consists of a 30 m thick soft clay

overlying a ‘‘hard stratum’’. The water table is at the

ground surface.

Circular steel tubes, spaced of 2.5 m in the

horizontal direction, are used for the struts. Their

cross sectional area is indicated in Fig. 9.

Figure 10 shows the finite element mesh of the

problem. Two types of the six-noded triangular

element are considered: (1) the coupled element, for

the clay elements where consolidation is considered;

(2) the non-coupled element, for the wall and jet-grout

slab elements, considered as ‘‘impermeable’’. All six

nodes of the coupled element have displacement

degrees of freedom while only the three vertices nodes

Node

Gauss point

Line segment of the slip surface

Fig. 8 Six-noded triangular finite element

600 Geotech Geol Eng (2013) 31:593–615

123

Fig. 9 a Cross section of the strutted excavation; b ‘‘dissipation holes’’ in the jet-grout slab

Geotech Geol Eng (2013) 31:593–615 601

123

have excess pore pressure degrees of freedom. The six

nodes of a non-coupled element have only displace-

ment degrees of freedom.

The struts are modeled with three-noded bar

elements with linear elastic behaviour. Six-noded

joint element (three nodes at each face) with elastic

perfectly plastic behaviour are used to simulate the

soil–wall and soil–slab interfaces. Since the jet-grout

slab is constructed after the wall and there is no liaison

(continuity) between them, joint elements are also

considered for slab–wall interfaces, supposing that a

thin portion of soil remains between these two

materials.

Regarding the boundary conditions, no horizontal

displacement is allowed on the vertical boundaries of

the mesh while the bottom boundary is completely

fixed in both the vertical and horizontal directions. The

left vertical boundary corresponds to the symmetry

line of the problem. The right vertical boundary is

located 60 m away from the wall, corresponding to 6

times the excavation depth of the problem. In

hydraulic terms, it is assumed that, in the supported

side, the water level remains on the ground surface

(which is a conservative and simplified assumption

and presupposes that there is a flow that provides water

to the ground) and, in the excavated side, the water

level coincides, at each stage of excavation, with the

excavation base (which means that the water, inside

the excavated area, is assumed to be pumped). A fully

coupled analysis is performed both during and after

the excavation period.

The constitutive behaviour of the clay is modeled

by the p–q–h critical state model (Borges 1995;

Borges and Cardoso 1998; Lewis and Schrefler 1987).

The values of its parameters are indicated in Table 1

(k, slope of normal consolidation line and critical state

line; k, slope of swelling and recompression line; C,

specific volume of soil on the critical state line at mean

normal stress equal to 1 kPa; N, specific volume of

normally consolidated soil at mean normal stress equal

to 1 kPa). Table 1 also shows other geotechnical

properties of the clay: c, unit weight; m0, Poisson’s ratio

for drained loading; /0, angle of friction defined in

effective terms; kh and kv, coefficients of permeability

in horizontal and vertical directions; K0, at rest earth

pressure coefficient; OCR, over-consolidation ratio;

su, undrained shear strength. The values adopted for

the clay are similar to those used by Finno et al. (1991)

regarding an excavation in soft soils constructed in

Chicago, USA.

The reinforced concrete wall is modeled as an

isotropic elastic material with a Young’s modulus

(E) of 18 GPa and a Poisson’s ratio (m) of 0.2.

The isotropic elastic model is also considered for the

Fig. 10 Finite element

mesh

Table 1 Geotechnical properties of the soil

c (kN/m3) K0 OCR k k N C m0 u0

(�)

kx = ky (m/s) su

Clay 16 0.5 1.0 0.18 0.025 3.158 3.05 0.25 26 10-9 0:28r0v0

r0v0, initial vertical effective stress

602 Geotech Geol Eng (2013) 31:593–615

123

jet-grout slab, adopting values of 150 MPa and 0.2 for

E and m, respectively. The value of E is the same as that

referred by Jaritngam (2003) for the jet-grout columns

carried out in a soft soil. The adopted value of E is

assumed as an average value (secant modulus) for the

stress level expected in the jet-grout slab.

The one-dimensional isotropic elastic model is used

in the strut simulation, with a Young’s modulus of

206 GPa for the steel. However, due to the difference

usually observed in practice between theoretical and

effective stiffnesses, the later was considered equal

to half the theoretical stiffness, as suggested by

O’Rourke (1992).

The soil–wall interfaces are modeled with joint

elements with elastic perfectly plastic behaviour

defined in total stresses. Taking into account the

results of laboratorial tests performed by Fernandes

(1983), the soil–wall interface strength was considered

equal to the shear strength of the soft soil. To define the

elastic tangential modulus of the interface, it was

supposed that a tangential displacement of 1 mm is

reached when shear strength is mobilised, also based

on what Fernandes (1983) proposed. Similar criteria

were considered to define the properties of the soil–

slab and wall–slab interfaces. As said above, since the

jet-grout slab is constructed after the wall and there is

no continuity between these two materials, a thin

portion of soil is supposed to remain between them,

which justifies the use of joint elements on the wall–

slab interfaces. A very high value of normal stiffness

in all joint elements was considered, so unrealistic

normal displacements could not be obtained in all

those interfaces.

5 Analysis of Results

5.1 Construction Period

Figure 11 shows results of excess pore pressure at

several stages during excavation. Excess pore pressure

is defined as the difference between pore pressure at a

particular instant and its initial hydrostatic value.

These results show that negative values are generated

during excavation, increasing as excavation pro-

gresses, as expected. Highest absolute value of excess

pore pressure occurs below the excavation base near

the left boundary (symmetry line). This is explained

by the highest decrease of total mean stress associated

to the excavation, which occurs in that zone. On the

supported side of the ground, a tendency of generating

negative excess pore pressure is also observed,

although with lower values than on the excavated

side. This is explained not only by the lower decrease

of total mean stress on that side (because there is no

excavation on the supported side) but also by the

presence of the wall and, mainly, of the base slab,

which decisively contributes to avoid a ground

decompression with similar magnitude to that on the

excavated side. Below the wall tip, this effect does not

take place and consequently higher absolute values of

excess pore pressure are observed on the supported

side.

Principal effective stresses at the end of excavation

are shown in Fig. 12. Rotations of the principal stress

directions on both sides of the wall, mainly below the

wall tip, can be observed in this figure, which means

that large shear stresses (deviatoric stresses) occur on

those zones. This fact is corroborated by the results of

shear stress on horizontal and vertical planes (sxy)

shown in Fig. 13: highest values of sxy are also

mobilised at the end of excavation below the wall tip.

It should be noted that high shear stresses are

observed in the vicinity of the bottom boundary due to

presence of the hard stratum (where displacements are

set as zero because of the very high stiffness of the

hard stratum when compared to the stiffness of soft

soil). These values of shear stress are mainly due to

differential horizontal displacements between the soft

soil and the hard stratum in that zone: as the hard

stratum is modeled without displacements, even small

values of horizontal displacement in the soft soil

determine high values of shear stress in that zone.

Figure 14 shows distributions of stress level in the

ground at several stages during excavation. Stress

level, SL, measures the proximity to the soil critical

state and is defined as follows:

SL ¼ q

pMð8Þ

where p, q and M have the meanings reported in Sect.

3. In normally consolidated soils, SL varies from zero

to 1, the latter being the critical state level. In

overconsolidated soils, because of the peak strength

behaviour, stress level may be higher than 1.

Figure 14 shows that SL significantly increases

during excavation, which is basically related with the

increase of deviatoric stress, q, as commented above.

Geotech Geol Eng (2013) 31:593–615 603

123

At the end of excavation, stress level takes values

close to 1, below the wall tip on both sides of the wall.

Lower values of SL are observed above the wall tip on

both sides of the wall, due to the jet-grout slab which

works as a support of the wall below the excavation

bottom. One can also note that, as the excavation depth

increases, higher values of stress level on the sup-

ported side spread in a direction of approximately 45�with the horizontal direction (which corresponds to the

failure direction for cohesive soils in active limit state,

considering the Mohr–Coulomb failure criterion).

This fact qualitatively indicates that the potential

failure surface takes that direction on that zone, which

was corroborated by the values of F obtained from the

finite element analysis, using the program of bottom

heave stability analysis described in Sect. 3.

Figure 15 shows, at several stages of excavation,

the values of the safety factor calculated by the

Terzaghi (1943) and Bjerrum and Eide (1956) meth-

ods and those obtained from the finite element analysis

along the failure surface defined in Fig. 7. These

results show that the values obtained from the finite

element analysis are very similar to those of the

Bjerrum and Eide (1956) method, at excavation depths

larger than 8 m when F takes smaller values; the

values of Terzaghi (1943) method are slightly higher

at those stages. For smaller depths of excavation

(smaller then 7 m), the values of F obtained from finite

Fig. 11 Excess pore

pressure during excavation:

a 2 m excavated; b 6 m

excavated; c 10 m

excavated (end of

excavation)

604 Geotech Geol Eng (2013) 31:593–615

123

element analysis tend to be higher than those of

Terzaghi (1943) and Bjerrum and Eide (1956) meth-

ods. This is explained by the fact that the application of

the program, calculating F along a potential failure

surface from soil shear strength and acting shear stress,

is less realistic at early stages of excavation when

failure condition is far away. However, the results

show that the program is very accurate [with values

very similar to those obtained by Bjerrum and Eide

(1956) method] when F takes values smaller than 1.5,

which actually corresponds to practical situations

where this stability analysis is more pertinent. At the

end of excavation, F takes the values of 1.145, 1.191

and 1.286 respectively for finite element analysis,

Bjerrum and Eide (1956) method and Terzaghi (1943)

formulation.

Wall horizontal displacements at several stages

during excavation are shown in Fig. 16. Unlike what

usually happens in strutted excavations without a base

slab, Fig. 16 shows that the displacements decrease

with depth at all stages of construction; i.e., the

maximum horizontal displacement takes place on

the top of the wall. This behaviour is obviously due to

the base slab support.

Settlements on the ground surface, on the supported

side, are shown in Fig. 17, for several depths of

excavation. These results show that the maximum

settlement takes place close to the wall, and another

local maximum occurs approximately 20 m away

from the wall. It should be noted that, as said in Sect. 4,

the wall–soil interface reaches its shear strength for

1 mm of tangential displacement, which explains that

high settlements may occur on that interface, as

observed in Fig. 17.

Figure 18 shows the excavation bottom vertical

displacements (on the upper face of the jet-grout slab)

for several depths of excavation. These results show

that upward displacements are higher on the left

boundary (middle of the slab), reaching a value of

11.28 cm at the end of excavation. Near the wall,

upward displacements are smaller, which is justified

by the tangential stress mobilized on the soil–wall

interface. However, this stress does not impede that

high values are also reached on that zone (approxi-

mately 9 cm), since the strength of the interface is

mobilized for a small value of 1 mm of tangential

displacement, as said above.

Strut compression loads for several stages of

excavation are illustrated in Fig. 19. Compression

load of 1st strut level increases with excavation until

2nd strut level is installed. After that, its compression

load decreases. Similar effect is observed on the 2nd

strut level, i.e. its compression load also increases with

excavation, decreasing after 3rd strut level is installed.

The decreasing effect is more expressive on the 1st

level than on the 2nd level.

Fig. 12 Principal effective

stresses at the end of

excavation

Geotech Geol Eng (2013) 31:593–615 605

123

Bending moment diagrams in the wall at several

stages of construction are illustrated in Fig. 20. These

results show that near the excavation base the sign of

the bending moment changes, which is explained by

the base slab support that works as a kind of a fixed

support. Below excavation base, bending moment

increases with excavation whereas above that level the

evolution is different, i.e. the maximum value is

reached at 6 m of excavation and reduces after that.

This reduction is determined by the installation of the

3rd strut level at 7 m of depth.

Compression loads in the jet-grout slab are illus-

trated in Fig. 21. This figure shows that compression

load increases as excavation progresses, as expected,

and does not significantly vary along the slab at each

stage.

Bending moment diagrams in the jet-grout slab are

shown in Fig. 22. These results illustrate that bending

moments also increase with excavation and are higher

at the slab extremities.

It should be noted that, at the end of excavation,

highest values of compression load and bending

moment are applied near the extremities of the slab,

which implies that the minimum and maximum values

of compression stress on the most unfavorable cross

section (extremity of the slab) are 56.06 kPa (lower

fiber) and 857.14 kPa (upper fiber) respectively; the

latter is significantly smaller than the jet-grout strength

Fig. 13 Shear stress on

horizontal and verticalplanes (sxy) during

excavation: a 2 m

excavated; b 6 m excavated;

c 10 m excavated (end of

excavation)

606 Geotech Geol Eng (2013) 31:593–615

123

Fig. 14 Stress level during

excavation: a 2 m

excavated; b 6 m excavated;

c 10 m excavated (end of

excavation)

Fig. 15 Safety factor against bottom heave at several stages of

excavation

-0.04 -0.03 -0.02 -0.01 0.00 0.01

Horizontal displacement (m)

D

epth

(m

)

-12.5

-10.5

-8.5

-6.5

-4.5

-2.5

-0.5

2 m

4 m

6 m

8 m

10 m

Fig. 16 Wall horizontal displacements at several depths of

excavation

Geotech Geol Eng (2013) 31:593–615 607

123

0 10 20 30 40 50 60

Distance from the wall (m)

Set

tlem

ent

(m)

-0.030

-0.020

-0.010

0.000

0.010

0.020

0.0302 m

4 m

6 m

8 m

10 m

Fig. 17 Settlements on ground surface at several depths of

excavation

0 1 2 3 4 5 6Distance from left boundary (m)

Ver

tica

l dis

pla

cem

ent

(m)

0.00

0.02

0.04

0.06

0.08

0.10

0.12

2 m

8 m

4 m

6 m10 m

Fig. 18 Excavation bottom heave for several depths of

excavation

0 1 2 3 4 5 6 7 8 9 10

Excavation depth (m)

Co

mp

ress

ion

load

(kN

/m)

0

50

100

150

200

250

300Strut level 1

Strut level 2

Strut level 3

Fig. 19 Strut compression loads during excavation

-12.5

-10.5

-8.5

-6.5

-4.5

-2.5

-0.5

-400-2000200400

Bending moment (kN.m/m)

Dep

th (

m)

2 m

4 m

6 m

8 m

10 m

Fig. 20 Bending moment in the wall at several stages of

excavation

0 1 2 3 4 5 6

Distance from left boundary (m)

Co

mp

ress

ion

load

(K

N/m

)

0

100

200

300

400

500

600

700

2 m

4 m

6 m

8 m10 m

Fig. 21 Compression loads in the jet-grout slab at several

stages of excavation

0 1 2 3 4 5 6

Distance from left boundary (m)

Ben

din

g m

om

ent

(kN

.m/m

)

-120

-100

-80

-60

-40

-20

0

20

2 m

4 m

6 m

8 m10 m

Fig. 22 Bending moment in the jet-grout slab at several depths

of excavation

608 Geotech Geol Eng (2013) 31:593–615

123

values usually reported in bibliography for this kind of

soils. If that was not the case, or traction stress was

detected on the jet-grout slab, the slab thickness

should be enlarged in design.

5.2 Post-construction Period

After construction, the behaviour of the problem is

globally determined by the consolidation process

associated to the dissipation of the excess pore

pressure gradients generated during construction.

Therefore a transient water flow takes place in time

until hydrodynamic equilibrium is reached. In this

case, the long term hydrodynamic equilibrium is

determined by the difference of the hydraulic load of

10 m caused by the water table lowering on the

excavated side.

In the analysis, the three steel strut levels were

maintained in the post-construction period. However,

it should be noted that in building construction, for

instance, it is usual to replace the steel struts by the

definitive concrete slabs of the building in the function

of supporting the wall. Costa (2005) showed that this

replacement, in numerical analysis of this kind of

problems, has insignificant effect on the long term

numerical results that are obtained. Thus, in this study,

Fig. 23 Excess pore

pressure at several stages

after construction: a end of

construction; b 2 years after

end of construction; c end of

consolidation

Geotech Geol Eng (2013) 31:593–615 609

123

by simplification, the steel struts are maintained during

all stages of the problem, during and after the

construction period, as said above.

Figure 23 shows results of excess pore pressure at

several stages after excavation. It should be noted that,

as said above, excess pore pressure is considered

herein (as defined in the computer code) the difference

between pore pressure at a particular instant and its

initial hydrostatic value (before excavation), and not

its final value at the end of consolidation. With the

consolidation, the most significant variations are

observed on the excavated side where water pressure

increases (reduction of the absolute value of excess

pore pressure). On the supported side, the evolution is

contrary, although with low magnitude: there is a

small increase of the absolute value of excess pore

pressure which correspond to reduction of the water

pressure (which is related with downward water flow),

especially below the excavation base level. At the end

of consolidation, very typical shapes of isovalue

curves of excess pore pressure are observed. These

curves are normal to the flow lines of the steady flow

reached at end of consolidation (determined, as said,

by the 10 m lowering of the water table on the

excavated side).

Principal effective stresses at the end of consolida-

tion are shown in Fig. 24. Compared with Fig. 12

(principal effective stresses at the end of excavation),

these results show that, with the consolidation, there is

no significant variation of shear stress (directions of

principal stresses remain approximately the same as

after construction) but some variation of mean effec-

tive stress is observed (variation of principal stress

magnitude), corresponding to an increase on the

supported side and a decrease on the excavated side,

below the excavation bottom. Obviously, these vari-

ations are contrary to the pore pressure changes

discussed above, since both phenomena are related.

After construction, stress level (Fig. 25) increases

on the excavated side below the excavation bottom

which is due to the reduction of mean effective stress

on that zone, whereas on the supported side the

contrary effect is observed: stress level decreases,

since mean effective stress increases.

Regarding the bottom stability, Fig. 26 shows the

effect of consolidation on the safety factor, calculated

with the program described in Sect. 3. These results

basically show that F slightly increases with the

consolidation (from 1.145 to 1.207). This small

increase is mainly related to the reduction of stress

level on the supported side, as explained above.

Diagrams of earth pressure (total horizontal stress,

i.e. sum of pore pressure and horizontal effective

stress) on both faces of the wall at ends of excavation

and consolidation are shown in Fig. 27 (pressure on

the excavated face is illustrated with negative sign).

Fig. 24 Principal effective

stresses at the end of

consolidation

610 Geotech Geol Eng (2013) 31:593–615

123

Fig. 25 Stress level at several stages after construction: a end of construction; b 6 months after end of construction; c 2 years after end

of construction; d end of consolidation

Geotech Geol Eng (2013) 31:593–615 611

123

A large increase of earth pressure is observed during

consolidation on the excavated face. This is due to the

swelling effect of the soil (associated to the decrease of

mean effective stress, as seen above) as consolidation

takes place in that zone. The soil swelling is partially

impeded by the wall in the horizontal direction, which

increases the earth pressure on the wall face.

On the supported side, above the excavation level, a

small decrease of earth pressure is observed. This fact

is justified by an effect contrary to what happens on the

excavated side; i.e., as seen above, an increase of

effective mean stress occurs with consolidation on the

supported side, which provokes reduction of the soil

volume and therefore decrease of earth pressure on the

wall.

In overall terms, wall horizontal displacements do

not change significantly with the consolidation, as

shown in Fig. 28. The most expressive variation is

observed below depth of 9 m, where displacements

reduce with consolidation. This effect is explained by

the increase of earth pressure on the excavated face, as

mentioned above.

Diagrams of vertical displacement on the supported

ground surface and on the excavation bottom are

illustrated in Figs. 29 and 30. These results show that,

with the consolidation, there are expressive downward

displacements on the supported ground and upward

displacements on the excavation bottom. These effects

are respectively justified by the reduction and increase

of volume on the supported and excavated soils, as

discussed above.

Diagrams of wall bending moments at ends of

construction and consolidation are illustrated in

Fig. 31. With the consolidation, there is an increase

of bending moment in the upper zone of the wall and a

decrease in the lower zone. This is due to the above-

mentioned increase of earth pressure on the wall on the

excavated side. This provokes the reduction of the

lower ‘‘fixed’’ bending moment (at the jet-grout slab

level) and therefore, due to the equilibrium (since earth

pressure does not change significantly above

Fig. 26 Safety factor against bottom heave at several stages

after the end of excavation

-150 -100 -50 0 50 100 150 200

Earth pressure (kPa)

Dep

th (

m)

-12.5

-10.5

-8.5

-6.5

-4.5

-2.5

-0.5

End of consolidation

End of excavation

Fig. 27 Earth pressure on

the wall faces at ends of

excavation and

consolidation

-12.5

-10.5

-8.5

-6.5

-4.5

-2.5

-0.5

-0.040 -0.035 -0.030 -0.025 -0.020 -0.015 -0.010

Horizontal displacement (m)

Dep

th (m

)

End of excavation End of consolidation

Fig. 28 Wall horizontaldisplacement at ends of

excavation and

consolidation

612 Geotech Geol Eng (2013) 31:593–615

123

excavation level), the increase of moments above the

excavation base.

As for compression loads on the steel struts, the

results of the study showed that there is no significant

variation of their values on the three levels of struts

during consolidation. These results are in consonance

with the small variation of earth pressure on the wall,

above the excavation bottom, as seen above.

Figure 32 shows that during the consolidation the

compression load on the jet-grout slab reduces. This is

due to the increase with consolidation of the earth

pressure (total horizontal stress) on the wall face of

excavated side, as discussed above, which decreases

the load that the wall transfers to the slab. On the other

hand, the reduction of the wall displacements with

consolidation (as seen in Fig. 28) corroborates this

reduction of compression load on the jet-grout slab.

Figure 33 shows that, during consolidation, the

absolute value of bending moment on the jet-

grout slab globally increases, the maximum value

-0.12

-0.10

-0.08

-0.06

-0.04

-0.02

0.00

0 10 20 30 40 50 60

Distance from the wall (m)

Ver

tica

l dis

pla

cem

ent

(m)

End of excavation End of consolidation

Fig. 29 Verticaldisplacement on supported

ground surface at ends of

excavation and

consolidation

0 1 2 3 4 5 6

Distance from left boundary (m)

Ver

tica

l dis

pla

cem

ent

(m)

0.00

0.03

0.06

0.09

0.12

0.15

0.18

0.21

End of excavation End of consolidation

Fig. 30 Verticaldisplacement on excavation

bottom at ends of excavation

and consolidation

-12.5

-10.5

-8.5

-6.5

-4.5

-2.5

-0.5

-400-2000200400Bending moment (kN.m/m)

Dep

th (

m)

End of consolidation End of excavation

Fig. 31 Wall bending moments at ends of construction and

consolidation

0 1 2 3 4 5 6

Distance from left boundary (m)

Co

mp

ress

ion

load

(kN

/m)

0

100

200

300

400

500

600

700

End of consolidation End of excavation

Fig. 32 Compression loads

on the jet-grout slab at ends

of construction and

consolidation

Geotech Geol Eng (2013) 31:593–615 613

123

(at extremities of the slab) increasing 33 % (from

112.819 to 150.137 kN m/m).

6 Conclusions

The influence of the consolidation on a strutted

excavation in soft soil incorporating a jet-grout base

slab was analysed using a computer program based on

the finite element method. The program incorporates

coupled analysis and soil constitutive relations simu-

lated by the p–q–h critical state model. The safety

factor against bottom heave was also evaluated from

the finite element analysis and compared to Terzaghi

(1943) and Bjerrum and Eide (1956) methods. Some

overall conclusions are pointed out below on the

results of the numerical analysis.

1. During excavation, negative excess pore pres-

sures are generated in all zones of the ground. The

highest absolute value of excess pore pressure

occurs below the excavation bottom where the

highest decrease of total mean stress takes place.

After construction, with the consolidation, water

pressure increases on the excavated side and

decreases on the supported side.

2. Stress level of soil significantly increases during

excavation, especially below the wall tip. Lower

values occur above the wall tip on both sides of

the wall due to the jet-grout slab which works as a

support of the wall below the excavation bottom.

After construction, stress level increases below

the excavation bottom, whereas decreases on the

supported side of the wall.

3. Unlike what usually happens in strutted excava-

tions without a base slab, the maximum wall

displacement takes place on the top of the wall at

all stages of excavation and post-excavation.

4. During consolidation, there are expressive down-

ward displacements on the supported ground

surface and upward displacements on the exca-

vation bottom.

5. During construction, below the excavation base,

the wall bending moments increase as excavation

progresses, whereas above that level the maxi-

mum bending moment is not reached at the end of

excavation.

6. During consolidation, there is no significant

variation of compression loads on the struts.

7. With consolidation, the compression load of the

jet-grout slab reduces whereas its bending

moments globally increase.

8. The values of the safety factor against bottom heave

obtained from the finite element analysis are very

similar to those of the Bjerrum and Eide (1956)

method, particularly when F takes values smaller

than 1.5. The values obtained from the Terzaghi

(1943) formulation revealed to be slightly higher.

After construction, the safety factor obtained from

the finite element analysis slightly increases with the

consolidation (from 1.145 to 1.207). This small

increase is mainly related to the reduction of stress

level on the supported side.

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