Question Acta Geotechnica (2013) 8:3-15
DOI 10.1007/s11440-012-0193-4
RESEARCH PAPER
Re-assessment of foundation settlements for the Burj Khalifa,
Dubai
Gianpiero Russo Vincenzo Abagnara.
Harry G. Poulos John C. Small
Received: 14 April 2012/Accepted: 12 October 2012/Published online: 30 October 2012
© Springer-Verlag Berlin Heidelberg 2012
Abstract This paper deals with the re-assessment of
foundation settlements for the Burj Khalifa Tower in
Dubai. The foundation system for the tower is a piled raft,
founded on deep deposits of calcareous rocks. Two com-
puter programs, Geotechnical Analysis of Raft with Piles
(GARP) and Non-linear Analysis of Piled Rafts (NAPRA)
have been used for the settlement analyses, and the paper
outlines the procedure adopted to re-assess the foundation
settlements based on a careful interpretation of load tests
on trial piles in which the interaction effects of the pile test
set-up are allowed for. The paper then examines the
influence of a series of factors on the computed settle-
ments. In order to obtain reasonable estimates of differ-
ential settlements within the system, it is found desirable to
incorporate the effects of the superstructure stiffness which
act to increase the stiffness of the overall foundation sys-
tem. Values of average and differential settlements for the
piled raft calculated with GARP and NAPRA were found
to be in reasonable agreement with measured data on set-
tlements taken near the end of construction of the tower.
Keywords Case history Footings and foundations.
Full-scale tests Piles Rafts · Settlement
.
G. Russo (). V. Abagnara
University of Naples, Naples, Italy
e-mail: pierusso@unina.it
H. G. Poulos J. C. Small
Coffey Geotechnics, Sydney, Australia
J. C. Small
University of Sydney, Sydney, Australia
1 Introduction
The Burj Khalifa in Dubai was officially opened in January
2010 and, at a height of 828 m, is currently the world's
tallest building. The foundation system is a piled raft, a
form of foundation that is being used increasingly to sup-
port tall structures where the loads are expected to be
excessively large for a raft alone and where the raft and the
piles are able to transfer load to the soil. The foundation
design process for this building has been described by
Poulos and Bunce [12].
An important component of the design of a piled raft
foundation is the detailed assessment of the settlement and
differential settlement of the foundation system, and their
control by optimising the size, location and arrangement of
the piles, and the raft thickness. Many different methods of
analysis have been devised in order to predict the behav-
iour of raft and piled raft foundations [2, 4, 5, 6, 10, 13, 15,
17, 19, 20], and these range from simple hand-based
methods to complex three-dimensional numerical analyses.
In this paper, attention is focussed on two methods that
model the raft as an elastic plate and the piles as interacting
non-linear springs. The computer codes implementing
these methods are described very briefly and are then
applied to the Burj Khalifa, which is founded on a piled
raft. The evaluation of the ground modulus values is
described using a combination of field test and laboratory
data and the results of pile load tests. The method of
interpreting the pile load test data is discussed, and the
importance of allowing for interaction between the test pile
and the surrounding reaction piles in emphasised. The two
programs are then used to compare the computed settle-
ments with available measurements of foundation settle-
ments, and with the "Class A" predictions made by the
foundation designers and the peer reviewers.
Springer 4
An important objective of the paper is to explore how
pile load test data should be used when predicting the
settlement performance of piled and piled raft foundation
systems, and to examine some factors that may have an
important influence on predicted foundation settlements.
2 Computer analyses
The settlement analyses used in this paper for the Burj
Khalifa have employed two computer programs, Geo-
technical Analysis of Raft with Piles (GARP) and Non-
linear Analysis of Piled Rafts (NAPRA), which idealise the
piled raft foundation as a plate supported by non-linear
interacting springs. A very brief description of these pro-
grams is given below.
2.1 Program GARP
The computer program GARP [18] uses a simplified
boundary element analysis to compute the behaviour of a
piled raft when subjected to applied vertical loading,
moment loading, and free-field vertical soil movements.
The raft is represented by a thin elastic plate and is
discretized via the finite element method using eight-noded
elements. The soil is modelled as a layered elastic con-
tinuum, and the piles are represented by elastic-plastic or
hyperbolic springs, which can interact with each other and
with the raft. Pile-pile interactions are incorporated via
interaction factors [9]. Simplifying approximations are
utilised for the raft-pile and pile-raft interactions. Beneath
the raft, limiting values of contact pressure in compression
and tension can be specified so that some allowance can be
made for non-linear raft behaviour. The output of GARP
includes: the settlement at all nodes of the raft; the trans-
verse, longitudinal, and torsional bending moments within
each element of the raft; the contact pressures below the
raft; and the vertical loads on each pile. In its present form,
GARP can consider vertical and moment loadings, but not
lateral loadings or torsion.
2.2 Program NAPRA
The computer program NAPRA [13, 15] computes the
behaviour of a raft subjected to any combination of vertical
distributed or concentrated loading and moment loading.
The raft is modelled as a two-dimensional elastic body
using the thin plate theory, and utilising the finite element
method, adopting a four- or nine-noded rectangular
element.
The piles and the soil are modelled by means of inter-
acting linear or non-linear springs. It is assumed that the
interaction between the raft and the soil (the piles) is purely
Springer
Acta Geotechnica (2013) 8:3-15
vertical; accordingly, only the axial stiffness of the springs
is required.
The soil is assumed to be a layered elastic continuum.
The Boussinesq solution for a point load and the closed
form solution for a rectangular uniformly loaded area at the
surface of an elastic half space are used to calculate the soil
displacements produced by the contact pressure developed
at the interface between the raft and the soil. The layered
continuum is solved by means of the Steinbrenner
approximation [3, 13], and as such, invokes the simple
assumption that the stress distribution within an elastic
layer is identical with the Boussinesq distribution for a
homogeneous half space [13].
The interaction factor method is used to model pile to
pile interaction and a preliminary boundary element (BEM)
analysis allows calculation of the interaction factors
between two piles at various spacings. Interaction between
axially loaded piles beneath the raft and the raft elements is
accounted for via pile-soil interaction factors computed
with a preliminary BEM procedure. The reciprocal theorem
is used to maintain that the soil-pile interaction factor is
equal to the pile-soil interaction factor.
A stepwise incremental procedure is used to simulate the
non-linear load-settlement relationship of a single pile, the
total load to be applied is subdivided into a number of
increments, and the diagonal terms of the pile-soil flexi-
bility matrix are updated at each step. A computation of the
nodal reactions vector is made at each step to check for
tensile forces between raft and soil and an iterative pro-
cedure is used to make them equal to zero. Basically, this
procedure releases the compatibility of displacements
between the raft and the pile-soil system in the node where
tensile forces were detected, although the overall equilib-
rium is maintained by a re-distribution of forces. An iter-
ative procedure is needed since after the first run some
additional tensile forces may arise in different nodes. The
output of the code is represented by the distribution of the
nodal displacements of the raft and the pile-soil system,
the load sharing among the piles and the raft, the bending
moments and the shear in the raft, for each load increment.
Abagnara et al. [1] have compared GARP and NAPRA
analyses for a simple case, and have concluded that both
programs give comparable results, but that some of the
simplifying assumptions employed in each program give
rise to differences in detail. For example, the difference in
raft settlements may be due to the differences in the details
of calculation of the soil layer stiffness using the Bous-
sinesq/Steinbrenner approach. The difference in plate ele-
ment types may also contribute to the differences. For the
piled raft, the differences may arise because of differences
in the methods used to compute the single pile stiffness
values, the interaction factors and the pile-raft and raft-
pile interactions. Acta Geotechnica (2013) 8:3-15
In this paper, attention will be focussed on analyses
carried out with NAPRA, although a comparison will also
be presented between the GARP and NAPRA analyses.
3 Settlement assessment for the Burj Khalifa Tower,
Dubai
3.1 Foundation layout
The Burj Khalifa project in Dubai, United Arab Emirates
(UAE), comprises a 160 storey high rise tower, with a
podium development around the base of the tower,
including a 4-6 storey garage. The Burj Khalifa is located
on a 42,000 m² site. The tower is founded on a 3.7 m thick
raft supported on 194 bored piles, 1.5 m in diameter,
extending 47.45 m below the base of the raft; podium
structures are founded on a 0.65 m thick raft (increased to
1 m at column locations) supported on 750 bored piles,
0.9 m in diameter, extending 30-35 m below the base of
the raft. A plan view of the foundation is shown in Fig. 1.
3.2 Ground investigation and site characterisation
The investigations involved the drilling of 32 boreholes to
a maximum depth of about 90 m below ground level and 1
borehole to a depth of 140 m under the tower footprint.
Standpipe piezometers were installed to measure the
ground water level which was found to be relatively close
to the ground surface, typically at a level of 2.5 m DMD.
The ranges of measured SPT N values are summarised in
Table 1. There was a tendency for N values to increase
with depth, beyond an elevation of about -8 m DMD.
y axis [m]
E
150
100
50
O
-50
-100-
-150
L
-150 -100
wing C
1
-50
podium
wing A
wing B
1
100
0
x axis [m]
Fig. 1 Plan view of the Khalifa Tower foundation system
50
150
200
The ground conditions at the site comprise a horizon-
tally stratified subsurface profile which is complex and
highly variable in terms of the strata thickness due to the
nature of deposition and the prevalent hot arid climatic
conditions. The main strata identified were as follows:
1. Very loose to medium dense silty sand (Marine
deposits).
2.
Weak to moderately weak calcarenite, generally
unweathered with fractures close to medium spaced
interbedded with cemented sand. This material is
generally underlain by very weak to weak sandstone
which is generally unweathered with fractures close to
medium spaced interbedded with cemented sand.
3. Very weak to weak calcarenite, calcareous sandstone,
and sandstone; this formation is slightly to highly
weathered with fractures extremely close to closely
spaced and interbedded with cemented sand. Bands of
1-5 m thickness are also present of medium dense to
very dense, cemented sand with sandstone bands and
locally with bands of silt.
4.
Very weak to weak gypsiferous sandstone, gypsiferous
calcareous sandstone occasionally gypsiferous silt-
stone. This material is generally unweathered to
slightly weathered with fractures extremely close to
closely spaced and interbedded with cemented sand.
The formation is interbedded with dense to very dense,
cemented silty sand and occasionally silt with sand-
stone bands.
5
5.
Very weak to weak calcisiltite, conglomeritic calcisil-
tite, and calcareous calcisiltite. This material is gen-
erally moderately to highly weathered, occasionally
slightly and completely weathered with fractures
extremely close to medium spaced. Calcareous silt-
stone was encountered in the majority of the deeper
boreholes comprising very weak to weak occasionally
moderately weak calcareous siltstone in bands with a
thickness of 0.5-14.4 m generally slightly to moder-
ately weathered occasionally highly to extremely
weathered.
6. Very weak to weak and occasionally moderately weak
calcareous siltstone, calcareous conglomerate, con-
glomeritic sandstone, and limestone. This material is
Table 1 Summary of measured SPT values
Elevation (m)
2.5 to
-1 to
-8 to
14
-14 to -30
-30 to -40
-40 to 80
1
8
Range of SPT values
0-40
50-400
0-100
40-200
100-200
100-400
Springer 6
generally slightly weathered and occasionally
unweathered and moderately weathered to highly
weathered. Occasionally encountered as calcisiltite
interbedded with bands of siltstone and conglomerate.
7. Very weak to moderately weak claystone interbedded
with siltstone. This material is generally slightly
weathered with close to medium-spaced fractures.
Between 112.2 and -128.2 m occasional bands of
up to 500 mm thick gypsum were encountered. Below
- 128.2 m the stratum was encountered as weak to
moderately weak siltstone with medium to widely
spaced fractures.
Table 2 summarises the stratigraphy adopted for the
foundation settlement analyses.
3.3 In situ and laboratory test results
A comprehensive series of in situ tests was carried out,
including pressuremeter tests, down-hole seismic, cross-
hole seismic, and cross-hole tomography to determine
compression (P) and shear (S) wave velocities through the
ground profile. The vertical profile of P-wave velocity with
depth gave a useful indication of variations in the nature of
the strata between the borelogs.
Conventional laboratory classification tests (moisture
content of soil and rock, Atterberg limits, particle size
distribution, and hydrometer) and laboratory tests for
determining physical (porosity tests, intact dry density,
specific gravity, particle density) and chemical properties
were carried out. In addition, unconfined compression tests,
point load index tests, and drained direct shear tests were
carried out. A considerable amount of more advanced
laboratory testing was undertaken, including stress path
triaxial tests, resonant column testing for small-strain shear
modulus, undrained cyclic triaxial tests, cyclic simple
Table 2 Stratigraphic model adopted for settlement assessment
Stratum Description
1
2
3a
3b
4
5a
5b
6
7
Marine deposits
Calcarenite/calcareous sandstone
Calcareous sandstone/sandstone
Gypsiferous sandstone
Calcisiltite/conglomeritic calcisiltite
Calcareous siltstone
Calcareous/conglomeritic strata
Claystone/siltstone interbedded
with gypsum layers
Springer
1.15 to 2.96
-0.27 to 1.95
-4.13 to 12.06
-21.54 to -26.69
-27.64 to -31.15
-67.19 to -76.04
-98.19
shear, and constant normal stiffness (CNS) direct shear
tests.
Some of the relevant findings from the in situ and lab-
oratory testing are as follows:
Level at the top of
the stratum (m DMD)
1. The cemented materials were generally very weak to
weak; unconfined compressive strength (UCS) values
ranged mostly between about 0.1 and 6 MPa, the
average values for each layer being the ones reported
in Table 2.
2.
3.
4.
Values of the Young's modulus from pressuremeter
tests (first and second reload cycle) were found to be in
good agreement with values from correlation with
shear waves velocities. From calcarenite (0 to -7.5 m)
to sandstone (-7.5 to −24 m), Young's modulus is
approximately constant with depth; at greater depths,
the average values decrease in the gypsiferous sand-
stone (-24 to 28.5 m) then they slightly increase in
the calcisiltite (from -28.5 to -68.5 m) and finally
decrease in the siltstone (from -68.5 to -91 m).
Triaxial stress path testing (at strain levels of 0.01 and
0.1%) was found to give results for Young's modulus
that were in good agreement with pressuremeter and
geophysics testing results.
Resonant column testing was found to give lower
values for the Young's modulus when compared with
values from pressuremeter tests, geophysics tests, and
triaxial stress tests.
5.
Constant normal stiffness (CNS) tests were carried out
on three samples taken from stratum 5a to assess the
ultimate skin friction values and the potential for
cyclic degradation at the pile-soil interface. These
tests indicated values of peak monotonic shear stress
ranging from 360 to 558 kPa, with only a little
difference between the peak monotonic and the
residual cyclic shear stress values.
Acta Geotechnica (2013) 8:3–15
Thickness (m)
1.85 to 4.3
2.87 to 10.75
10.5 to 21.43
1.7 to 7.75
39.2 to 46.75
31 (from 140 m deep
BH only)
Proved to 39.6 m
thickness
Adopted level at top
of layer (m DMD)
2.5
-1.2
-7.3
-13.5
-24
-28.5
-50
-68.5
-90
UCS qu (MPa)
2
1.3
1.7
2.5
T Acta Geotechnica (2013) 8:3-15
3.4 Geotechnical model
The key parameters for the assessment of the settlement
behaviour of the Khalifa Tower piled raft foundation sys-
tem are the values of the Young's modulus of the strata for
both raft and pile behaviour under static loading. In a non-
linear analysis, the values of ultimate skin friction of piles,
the ultimate end-bearing resistance of the piles, and the
ultimate bearing capacity of the raft would also be
required, but in this paper, only linear elastic analyses have
been undertaken using NAPRA and GARP analyses, hav-
ing explored the little influence of non-linearity up to the
maximum observed load level. Attention has thus been
focussed on evaluating relevant values of Young's modulus
for each stratum.
As a first step in obtaining these values, the relative
stiffness of the various soil layers was assessed considering
values of the Young's modulus from the following data:
1. pressuremeter tests (initial loading, first reload, second
reload cycles);
2.
geophysics tests (correlation with shear wave
velocities);
3. resonant column tests (Initial, 0.0001, 0.001, 0.01 %
strain levels);
4. triaxial stress path tests (0.01 and 0.1 % strain levels);
Values of the various Young's modulus values are
plotted in Fig. 2, and although inevitable scatter exists
among the different values, there is a reasonably consistent
general pattern of variation with depth.
Layer 3b (see Table 2) has arbitrarily been chosen as the
reference layer, and for each type of test, values of the
Young's modulus for a layer i, Ei, have been related to the
value for layer 3b, E36. The values of E/E36 have then been
averaged using the following data: reload cycles from
pressuremeter testing; seismic data; resonant column data
at a strain level of 0.01 %, and the triaxial stress path tests.
Figure 3 shows the different assessed relative stiffness
profiles so obtained, and Table 3 summarises the average
values of relative Young's modulus that were adopted for
the analyses and the interpretation of the pile load test data.
The absolute values of Young's modulus for each of the
different layers have been then obtained by fitting the load-
settlement curves of the single piles obtained from the load
tests, and the process of fitting the load-settlement curves
to obtain the Young's modulus values is described below.
3.5 Pile load tests
A program of pile load testing was undertaken which
involved the installation of seven test piles in the podium
area near the location of the Khalifa Tower. All the test
piles and reaction piles were bored cast in situ and
7
constructed under polymer fluid. A permanent casing, 6 m
long, was installed from the top of each pile to just above
the highest strain gauge level for all the trial piles tested in
compression and tension. Five piles, designated as P1, P2,
P3, P4, and P5, were tested in compression; two, P3 and
P5, were shaft grouted. Test pile P6 was tested in tension
and test pile P7 was laterally loaded.
Only the compression load tests on trial piles P1, P2, and
P4 have been considered for the present paper. Table 4
summarises the main features of these piles. Figure 4a shows
the load test arrangements for piles P1 and P2, which con-
sisted of the test pile and six reaction piles, while Fig. 4b
shows the set-up for pile P4, which consisted of the test pile
and four reaction piles. All the reaction piles were 1.5 m in
diameter. Steel load distribution plates were grouted to the
top of the test piles and hydraulic jacks were placed between
the steel plates and the reaction beams. Steel reaction beams
were used to transfer the load from the hydraulic jacks to the
installed reaction piles. Macalloy bars were used as reaction
anchors to transfer the load from the beams to the reaction
piles. Six cycles of loading were applied to trial piles P1 and
P2 while nine cycles of loading were applied to trial pile P4,
which was the pile designated to be tested cyclically.
Four main types of instrumentation were used in the
compression test piles:
1. concrete embedment vibrating wire strain gauges, to
allow measurement of axial strains at six levels along
the pile shafts and hence estimation of the axial load
distribution;
2. extensometers, to measure change in length of the
piles, and installed at the same levels as the vibrating
wire strain gauges to provide back-up information on
axial load distribution with depth;
3.
displacement transducers at the top of piles, to measure
the vertical movement at the pile heads;
4. load cells, to monitor the load applied to the pile via
the jacks.
3.6 Back-analysis interpretation of load tests to obtain
Young's modulus values
The computer program NAPRA was used to carry out the
back analyses of compression tests on the three test piles
considered. Since a detailed soil profile at each trial pile
location was not available, the same geotechnical model
was adopted for all three piles.
For comparison purposes, the three load tests were back-
analysed both taking and not taking into account interac-
tion between test piles and reaction piles. It is now well
recognised that ignoring interaction between the test pile
and the reaction piles can lead to an over-estimation of the
pile head stiffness [8, 9, 11, 14].
Springer/n 6th International Conference on
Case Histories in Geotechnical Engineering, Arlington, VA, August 11-16, 2008
FOUNDATION DESIGN FOR THE BURJ DUBAI - THE WORLD'S TALLEST
BUILDING
Harry G. Poulos
Coffey Geotechnics
Sydney, Australia.
ABSTRACT
This paper describes the foundation design process adopted for the Burj Dubai, the world's tallest building. The foundation system is a
piled raft, founded on deep deposits of carbonate soils and rocks. The paper will outline the geotechnical investigations undertaken,
the field and laboratory testing programs, and the design process, and will discuss how various design issues, including cyclic
degradation of skin friction due to wind loading, were addressed. The numerical computer analysis that was adopted for the original
design together with the check/calibration analyses will be outlined, and then the alternative analysis employed for the peer review
process will be described. The paper sets out how the various design issues were addressed, including ultimate capacity, overall
stability under wind and seismic loadings, and the settlement and differential settlements.
Grahame Bunce
Hyder Consulting (UK),
Guildford, UK
The comprehensive program of pile load testing that was undertaken, which included grouted and non-grouted piles to a maximum
load of 64MN, will be presented and “Class A” predictions of the axial load-settlement behaviour will be compared with the measured
behavior. The settlements of the towers observed during construction will be compared with those predicted.
INTRODUCTION
The Burj Dubai project in Dubai comprises the construction of
an approximately 160 storey high rise tower, with a podium
development around the base of the tower, including a 4-6
storey garage. The client for the project is Emaar, a leading
developer based in Dubai. Once completed, the Burj Dubai
Tower will be the world's tallest building. It is founded on a
3.7m thick raft supported on bored piles, 1.5 m in diameter,
extending approximately 50m below the base of the raft.
Figure 1 shows an artist's impression of the completed tower.
The site is generally level and site levels are related to Dubai
Municipality Datum (DMD).
The Architects and Structural Engineers for the project were
Skidmore Owings and Merrill LLP (SOM) in Chicago. Hyder
Consulting (UK) Ltd (HCL) were appointed geotechnical
consultant for the works by Emaar and carried out the design
of the foundation system and an independent peer review has
been undertaken by Coffey Geosciences (Coffey). This paper
describes the foundation design and verification processes,
and the results of the pile load testing programs. It also
compares the predicted settlements with those measured
during construction.
Paper No. 1.47
GEOLOGY
The geology of the Arabian Gulf area has been substantially
influenced by the deposition of marine sediments resulting
from a number of changes in sea level during relatively recent
geological time. The country is generally relatively low-lying
(with the exception of the mountainous regions in the north-
east of the country), with near-surface geology dominated by
deposits of Quaternary to late Pleistocene age, including
mobile Aeolian dune sands, evaporite deposits and marine
sands.
Dubai is situated towards the eastern edge of the geologically
stable Arabian Plate and separated from the unstable Iranian
Fold Belt to the north by the Arabian Gulf. The site is
therefore considered to be located within a seismically active
area.
GEOTECHNICAL INVESTIGATION & TESTING
PROGRAM
The geotechnical investigation was carried out in four phases
as follows:
Phase 1 (main investigation): 23 boreholes, in situ SPT's, 40
pressuremeter tests in 3 boreholes, installation of 4 standpipe
piezometers, laboratory testing, specialist laboratory testing
1 6th International Conference on
Case Histories in Geotechnical Engineering, Arlington, VA, August 11-16, 2008
and contamination testing – 1st June to 23rd July 2003;
Phase 2 (main investigation): geophysical boreholes with
cross-hole and tomography geophysical surveys carried out
between 3 new boreholes and 1 existing borehole - 7th to 25th
August, 2003;
Phase 3: 6 boreholes, in situ SPT's, 20 pressuremeter tests in
2 boreholes, installation of 2 standpipe piezometers and
laboratory testing - 16th September to 10th October 2003;
Phase 4: 1 borehole, in situ SPT's, cross-hole geophysical
testing in 3 boreholes and down-hole geophysical testing in 1
borehole and laboratory testing.
The drilling was carried out using cable percussion techniques
with follow-on rotary drilling methods to depths between 30m
and 140m below ground level. The quality of core recovered
in some of the earlier boreholes was somewhat poorer than
that recovered in later boreholes, and therefore the defects
noted in the earlier rock cores may not have been
representative of the actual defects present in the rock mass.
Phase 4 of the investigation was targeted to assess the
difference in core quality and this indicated that the
differences were probably related to the drilling fluid used and
the overall quality of drilling.
Disturbed and undisturbed samples and split spoon samples
were obtained from the boreholes. Undisturbed samples were
obtained using double tube core barrels (with Coreliner) and
wire line core barrels producing core varying in diameter
between 57mm and 108.6mm.
Standard Penetration Tests (SPTs) were carried out at various
depths in the boreholes and were generally carried out in the
overburden soils, in weak rock or soil bands encountered in
the rock strata.
Pressuremeter testing, using an OYO Elastmeter,
was carried out in 5 boreholes between depths of about 4m to
60m below ground level typically below the Tower footprint.
The geophysical survey comprised cross-hole seismic survey,
cross-hole tomography and down-hole geophysical survey.
The main purpose of the geophysical survey was to
complement the borehole data and provide a check on the
results obtained from borehole drilling, in situ testing and
laboratory testing.
The cross-hole seismic survey was used to assess compression
(P) and shear (S) wave velocities through the ground profile.
Cross-hole tomography was used to develop a detailed
distribution of P-wave velocity in the form of a vertical
seismic profile of P-wave with depth, and highlight any
Paper No. 1.47
variations in the nature of the strata between boreholes.
Down-hole seismic testing was used to determine shear (S)
wave velocities through the ground profile.
Fig 1: Impression of Burj Dubai when Complete
Laboratory Testing
The geotechnical laboratory testing program consisted of two
broad classes of test:
1. Conventional tests, including moisture content,
Atterberg limits, particle size distribution, specific
gravity, unconfined compressive strength, point load
index, direct shear tests, and carbonate content tests.
2. Sophisticated tests, including stress path triaxial,
resonant column, cyclic undrained triaxial, cyclic
simple shear and constant normal stiffness (CNS)
direct shear tests. These tests were undertaken by a
variety of commercial, research and university
laboratories in the UK, Denmark and Australia.
2 6th International Conference on
Case Histories in Geotechnical Engineering, Arlington, VA, August 11-16, 2008
GEOTECHNICAL CONDITIONS
The ground conditions comprise a horizontally stratified
subsurface profile which is complex and highly variable, due
to the nature of deposition and the prevalent hot arid climatic
conditions. Medium dense to very loose granular silty sands
(Marine Deposits) are underlain by successions of very weak
to weak sandstone interbedded with very weakly cemented
sand, gypsiferous fine grained sandstone/siltstone and weak to
moderately weak conglomerate/calcisiltite.
Table 1. Summary of Geotechnical Profile and Parameters
Strata
1
2
3
4
Paper No. 1.47
Sub-
Strata
la
1b
2
3a
3b
3c
4
Subsurface Material
Medium dense silty
Sand
Loose to very loose
silty Sand
Medium dense to
very dense Sand/ Silt
frequent
with
sandstone bands
Very weak to weak
Calcareous
Sandstone
Very weak to
moderately weak -1.20
Calcarenite
Very weak to weak
Calcareous
Sandstone
Level at top
of stratum
(m DMD)
Very weak to weak
gypsiferous
Sandstone/
calcareous Sandstone
+2.50
+1.00
-7.30
-13.50
-21.00
-24.00
S
(m)
Thicknes
1.50
2.20
6.10
6.20
7.50
3.00
Groundwater levels are generally high across the site and
excavations were likely to encounter groundwater at
approximately +0.0m DMD (approximately 2.5m below
ground level).
The ground conditions encountered in the investigation were
consistent with the available geological information.
4.50
The ground profile and derived geotechnical design
parameters assessed from the investigation data are
summarized in Table 1.
UCS
(MPa)
2.0
1.0
1.0
2.0
Undrained Drained
Modulus* Modulus*
Eu (MPa) E' (MPa)
34.5
11.5
500
50
250
140
140
30
10
400
40
200
110
110
Ult.
Comp.
Shaft
Frictio
n
(kPa)
350
250
250
250
250
3 6th International Conference on
Case Histories in Geotechnical Engineering, Arlington, VA, August 11-16, 2008
5
6
7
5a
5b
6
Paper No. 1.47
Very weak to
moderately
weak
Calcisiltite/
7
Conglomeritic
Calcisiltite
Very weak to
moderately
weak
Calcisiltite/
Conglomeritic
Calcisiltite
Very weak to weak
Calcareous/
Conglomerate strata
-28.50
-50.00
-68.50
-91.00
Stiffness values from the pressuremeter reload cycle, the
specialist tests and the geophysics are presented in Figure 2.
There is a fair correlation between the estimated stiffness
profiles from the pressuremeter and the specialist testing
results at small strain levels.
Non-linear stress-strain responses were derived for each strata
type using the results from the SPT's, the pressuremeter, the
geophysics and the standard and specialist laboratory testing.
Best estimate and maximum design curves were generated and
the best estimate curves are presented in Figure 3.
Weak to moderately
weak Claystone/
Siltstone interbedded
with gypsum layers
* Note that the Eu and E' values relate to the relatively large strain levels in the strata.
An assessment of the potential for degradation of the stiffness
of the strata under cyclic loading was carried out through a
review of the CNS and cyclic triaxial specialist test results,
and also using the computer program SHAKE91 (Idriss and
Sun, 1992) for potential degradation under earthquake loading.
The results indicated that there was a potential for degradation
of the mass stiffness of the materials but limited potential for
degradation of the pile-soil interface. An allowance for
degradation of the mass stiffness of the materials has been
incorporated in the derivation of the non-linear curves in
Figure 3.
21.50
18.50
22.50
1.3
>46.79
1.7
2.5
1.7
0.00
-10.00
-20.00
-30.00
-40.00
-50.00
-60.00
-70.00
-80 00
-90.00
ON.
1.xx
XX
0
310
405
560
405
5000.0
**
10000.0
O
250
325
450
325
E Value (MPa)
15000.0
20000.0
Strata 3a (Sand)
285
Strata 4 (Gypsiferous Sandstone)
Strata 2 (Calcarenite)
Strata 5a (Calcisiltite/ conglomeritic Calcisiltite)
325
400
Strata 3b (Sandstone)
Strata 3c (Sand)
Strata 5b (Calcisiltite/ conglomeritic Calcisiltite)
325
25000.0
-Strata 1 (Sand)]
Fig 2: Modulus Values vs Elevatio
◆ Borehole 2 -
Pressuremeter
Reload 1
Borehole 2-
Pressuremeter
Reload 2
◆ Borehole 3-
Pressuremeter
Reload 1
Borehole 3-
Pressuremeter
Reload 2
Borehole 4-
Pressuremeter
Reload 1
Borehole 4-
Pressuremeter
Reload 2
Borehole 25-
Pressuremeter
Reload 1
Borehole 25-
Pressuremeter
Reload 2
◆ Borehole 28 -
Pressuremeter
Reload 1
Borehole 28-
Pressuremeter
Reload 2
* Stress Path Txl at
0.01% strain
* Stress Path Txl at
0.1% strain
Resonant Column
at 0.0001% strain
A Resonant Column
at 0.001% strain
O Resonant Column
at 0.01% strain
Geophysics E
Values (lowest)
Adopted Small
Strain Design
Values
4 3.5
3
2.5
2
1.5
1
0.5
0
0
6th International Conference on
Case Histories in Geotechnical Engineering, Arlington, VA, August 11-16, 2008
0.02
Strata 2
Proposed Nonlinear Ground Strata Characteristics
0.04
Strata 3a
0.06
Strata 3b
0.08
Paper No. 1.47
Strain
Strata 3c & 4
0.1
0.12
Strata 5a, 5b, 6,
Fig 3: Non-linear Stress-strain Curves
0.14
GEOTECHNICAL MODELS AND ANALYSES
A number of analyses were used to assess the response of the
foundation for the Burj Dubai Tower and Podium. The main
design model was developed using a Finite Element (FE)
program ABAQUS run by a specialist company KW Ltd,
based in the UK. Other models were developed to validate
and correlate the results from the ABAQUS model using
software programs comprising REPUTE (Geocentrix, 2002),
PIGLET (Randolph, 1996) and VDISP (OASYS Geo, 2001).
The ABAQUS model comprised a detailed foundation mesh
of 500m by 500m by 90m deep. The complete model
incorporated a 'far field' coarse mesh of 1500m by 1500m by
300m deep. A summary of the model set up is as follows:
Soil Strata: Modeled as Von Mises material (pressure
independent), based on non-linear stress-strain curves Tower
Piles: Modeled as beam elements connected to the soil strata
by pile-soil interaction elements. Class A load-settlement
predictions were used to calibrate the elements;
Podium Piles: Beam elements fully bonded to the soil strata;
Tower and Podium Loadings: Applied as concentrated
loadings at the column locations;
Tower raft submerged weight: Applied as a uniformly
distributed load;
Tower Shearing Action: Applied as a body load to the tower
raft elements, in a direction to coincide with the appropriate
wind action assumed;
Building Stiffness Effect: Superstructure shear walls (not
interrupted at door openings) were modeled as a series of
beam elements overlaid on the tower raft elements. The
moment of inertia was modified to simulate the stiffening
effect of the tower, as specified by SOM.
FOUNDATION DESIGN
An assessment of the foundations for the structure was carried
out and it was clear that piled foundations would be
appropriate for both the Tower and Podium construction. An
initial assessment of the pile capacity was carried out using the
following design recommendations given by Horvath and
Kenney (1979), as presented by Burland and Mitchell (1989):
0.5
Ultimate unit shaft resistance f = 0.25 (qu)
where f, is in kPa, and qu= uniaxial compressive strength in
MN/m²
The adopted ultimate compressive unit shaft friction values for
the various site rock strata are tabulated in Table 1. The
ultimate unit pile skin friction of a pile loaded in tension was
taken as half the ultimate unit shaft resistance of a pile loaded
in compression.
The assessed pile capacities were provided to SOM and they
then supplied details on the layout, number and diameter of
the piles. Tower piles were 1.5m diameter and 47.45m long
with the tower raft founded at -7.55mDMD. The podium piles
were 0.9m diameter and 30m long with the podium raft being
founded at -4.85mDMD. The thickness of the raft was 3.7m.
Loading was provided by SOM and comprised 8 load cases
including four load cases for wind and three for seismic
conditions.
The initial ABAQUS runs indicated that the strains in the
strata were within the initial small strain region of the non-
linear stress strain curves developed for the materials. The
secant elastic modulus values at small strain levels were
therefore adopted for the validation and sensitivity analyses
carried out using PIGLET and REPUTE. A non-linear
analysis was carried out in VDISP using the non-linear stress
strain curves developed for the materials.
Linear and non-linear analyses were carried out to obtain
predictions for the load distribution in the piles and for the
settlement of the raft and podium.
The settlements from the FE analysis model and from VDISP
have been converted from those for a flexible pile cap to those
for a rigid pile cap for comparison with the REPUTE and
PIGLET models using the following general equation and are
shown in Table 2:
Srigid
=
1/2 (8
centre
+ 8 edge) flexible
5/n