airport central drained basement
TRANSCRIPT
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AIRPORT CENTRAL DRAINED BASEMENT
Terence J. Wiesner1
ABSTRACT
A case study is presented of the geotechnical design, construction and construction monitoring of the
drained basement of the Airport Central Sheraton Hotel building at Mascot, Sydney.
INTRODUCTION
This paper provides brief details of the geotechnical design and construction monitoring carried out for
the basement of the Airport Central Sheraton Hotel at Mascot, Sydney (Figure 1). The building is 12 stories
high with down to 4 levels (depth of excavation about 12.5m) of basement parking and contains commercial
premises as well as a five star hotel.
Figure 1 : Airport Central Sheraton Hotel at Mascot, Sydney.
The design and construct tender to build the hotel was won in 1990 by Concrete Constructions, now
Walter Constructions who, with Douglas Partners, geotechnical consultants, proposed a drained basement.
This nonconforming design eliminated the need for tanking and permanent anchors to resist hydrostatic
uplift. It facilitated an accelerated construction program using the 'top down' method, the first time this
technique was used in Australia. In 'top down' construction the external diaphragm wall, load bearing
barrettes and piles are installed and the basement floors and internal building structure used for lateral
support allowing excavation of the basement and construction of the superstructure to proceed together. This
can greatly reduce building construction time and cost.
1
Principal, Douglas Partners Pty Ltd, 96 Hermitage Road, West Ryde, Sydney, NSW 2114, Australia
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DESIGN CONSIDERATIONS
Analyses of seepage flows into the proposed basement area for hydraulic conductivity of the clays
ranging from 10 -6 to 5 x 10 -8 metres/second were carried out using MODFLOW, a 3 dimensional finitedifference numerical ground water modeling package. The diaphragm wall was assumed to be impermeable
and founded into the clays.Constant head boundaries were set
at the regional groundwater head
at a distance of 70m from the wall.
High inflows initially occurred
in the model due to water from the
subsoils inside the walls and
lowering of the water table to 12m
associated with construction of the
drained basement. Steady state
conditions were achieved in the
model within 50 days with most of
the flow coming from the shalelayer (k = 10 -6m/sec). Estimatedflows into the excavation after 200
days with the wall penetrating to
17m depth ranged from 35 m3/day
to 260 m3/day. Penetration into
the clays to 25m depth reduced
estimated inflow to around
100m3/day for 10 -6m/sec clay
hydraulic conductivity.
The estimated draw down in
the water table around the wall2000 days after construction of
the drained basement is shown in
Figure 2. Even immediately
adjacent to the wall draw down is
less than 300mm indicating a
permanently drained basement is
unlikely to significantly affect
neighbouring structures.
Removal of approximately
12m of predominantly sandy soil
and design of the basement floor
to allow seepage inflows to asump will result in upward
movement of the unloaded strata
due to elastic rebound and
swelling. Pore pressure gradients
causing flow through the clay
layer could lead to additional
upward movements. Accordingly
the effects of construction of a
drained basement on pore
pressures, flows and soil
movements were studied using
FLAC, a finite difference numerical computer program capable of modeling coupled groundwater changesand elastoplastic deformations of the soils during and after basement excavation.
Figure 2 : Predicted drawdown (mm) and instrumentation locations
Figure 3 : Pore pressures and flow vectors 3 days after excavation
Pore Pressures
B = 50 kPa
C = 100 kPa
D = 150 kPa
E = 200 kPa
Scale x 10 = metres
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The construction procedures and subsuface stratification represented in the model were relatively severe
compared with actual excavation and initially produced high pore pressure gradients as well as yield in a
limited section of the clays. Figure 3 shows pore pressure contours and flow vectors approximately 3 days
after rapid excavation to basement level. Pore pressure contour interval is 50 kPa and there are high values
of over 200kPa in the clayey shale and clay. With about 10 metres to basement level in the clayey shale a
simple calculation, neglecting the contribution of material strength, indicates a factor of safety against heave
of close to 1. In the model the strength and weight of overlying material confined this area. As pore
pressures dissipated and approached the long term steady state conditions, the clays returned to the elastic
state and stability increased. In a similar plot at 50 days pore pressures are approaching steady state
conditions and are approximately hydrostatic towards the centre of the excavation.
Long term swell movements resulting from the removal of approximately 12.5m of sands and water were
estimated using the model and other calculation methods to be of the order of 60 to 100mm. Approximately
one third to one half of this movement was expected to occur within a few days of removal of the overburden
materials.
Based on the FLAC, MODFLOW and other calculations it was therefore considered that conditions inside
the wall would eventually approach hydrostatic with very small upward flows. Significant heave was
considered unlikely provided the wall and underlying clays formed an effective seal. Monitoring during
construction was considered essential to ensure design requirements were met and pore pressures and groundresponses were as expected.
CONSTRUCTION MONITORING
After satisfactory completion of
design details and contract
negotiations, construction of a
diaphragm wall around the perimeter
of the site was commenced, followed
by barrettes to carry internal loads of
up to 13000kN, and driven steel H
piles to carry smaller loads of 1000to 3000kN. Line loadings on the
wall were estimated to range from 85
to 210kN/m although some sections
carried column loads of up to
3600kN. Full time geotechnical
monitoring was carried out during
slurry wall construction. Each wall
panel was logged during excavation
to ensure it was keyed at least 2
metres into low permeability clays
and the founding material was
adequate for the design loads.Piezometers, borehole
extensometers and inclinometers
were also installed to monitor ground
water and soil response during
excavation. The locations where
instrumentation was installed are
shown in Figure 2. Frequent
problems were experienced with the
excavation contractor damaging or
destroying the monitoring points.
Some success was eventually
achieved by encasing the upper section of the piezometers with heavy drill casing.
Figure 4 : Plot of measured and predicted excess pore pressures
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Piezometers were initially measured weekly then monthly then 3 monthly. Selected results are
summarised on Figure 4, which was a simple way of presenting the internal piezometer results and the
associated risk of heave. Measured pore pressures above the 'heave' line would have meant the excess
pressure head at the location of the piezometer screen was greater than the effective weight of overlying
material below final basement level. A factor of safety of 1.2 was applied for the 'marginal stability' line.
Excess pore pressures were at a relatively safe level by February 1991 when final excavation level was
achieved. Subsequently pore pressures slowly approached the theoretical long term predictions.
During construction, in order to facilitate excavation, a deep pumping bore was installed to lower
groundwater levels inside the excavation. Flows were initially higher than expected however they dropped
rapidly to well below 20 m3/day after a small leaky section of the western portion of the wall was located and
plugged. Water inflows measured after the project was completed were generally minimal and it was not
possible to distinguish between actual draw down and natural groundwater fluctuations in water level
measurements around the building.
The excavated sands were fine grained and silty in part. Problems were experienced with excessively wet
spoil, perched water tables, and traffickability due to the partially saturated sands and speed of excavation.
These were addressed by draining to and pumping from shallow sumps.
Excavation was initially carried out to the first basement level and the outer sections of the floor slab cast
to connect and brace the walls to the internal columns. This left a large central hole through which plant waslowered and further excavation carried out to the third basement floor level. This was also partly cast as it
was required to provide further bracing to the walls before the lowest basement level was excavated. A
subfloor drainage system and sumps were installed beneath the lowest basement floor slab. Construction
proceeded on the superstructure at the same time as the basement. Inclinometers just outside the basement
walls indicated lateral movements of less than 30mm in the perimeter walls confirming the adequacy of the
method of lateral support.
Unfortunately the borehole extensometers were destroyed early in the excavation and could not be located
or recovered despite the use of coloured grout around the holes. Observations after final excavation level
was reached indicated no discernible basement heave.
The building was successfully completed and the drained basement has operated for almost 10 years with
very low inflows and no known problems apart from normal routine maintenance to clean out iron oxide and
iron hydroxide precipitates in drains, sump and pumps.
ACKNOWLEDGEMENTS
All the work described in this paper was carried out by Douglas Partners personnel as geotechnical
consultants to Concrete Constructions Pty Ltd, now part of the Walter Construction Group. The permission
and assistance of Stephen Tamone, project director for Concrete Constructions, to publish details of the
project are gratefully acknowledged. Emged Rizkalla, site engineer for Douglas Partners at the time, made a
substantial contribution to the success of the project as he carried out much of the fieldwork and site
monitoring.