Paramount Property Group C/- Ghazi Al Ali Architect Unit 2, Level 2 14 Railway Parade Burwood NSW 2134 29 July 2016 RE: GEOTECHNICAL INVESTIGATION REPORT 401-405 LIVERPOOL ROAD, STRATHFIELD NSW Report ID: G16089STR-R01F Dear Darren, Please find below a report on the geotechnical investigation carried out at 401-405 Liverpool Road, Strathfield, New South Wales (herein referred to as the ‘site’). 1 PROJECT INFORMATION 1.1 INTRODUCTION AND OBJECTIVE Geo-Environmental Engineering Pty Ltd (GEE) was commissioned by Ghazi Al Ali Architect, on behalf of Paramount Property Group, to complete a geotechnical investigation at the site which relates to the proposed construction of a new multi- storey residential development. GEE understands that the investigation was required to support a Development Application with Council and to assist with the preliminary design and construction of the development, which comprises two detached, multi-storey residential developments, constructed over a single level basement. Currently, the site is occupied by a medium density development, operating as a motel. The report presents the factual results of the field investigations and provides interpretation and recommendations regarding the ground conditions at the site in accordance with client requirements and the agreed scope of work.
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Paramount Property Group
C/- Ghazi Al Ali Architect
Unit 2, Level 2
14 Railway Parade
Burwood NSW 2134
29 July 2016
RE: GEOTECHNICAL INVESTIGATION REPORT
401-405 LIVERPOOL ROAD, STRATHFIELD NSW
Report ID: G16089STR-R01F
Dear Darren,
Please find below a report on the geotechnical investigation carried out at 401-405 Liverpool
Road, Strathfield, New South Wales (herein referred to as the ‘site’).
1 PROJECT INFORMATION
1.1 INTRODUCTION AND OBJECTIVE
Geo-Environmental Engineering Pty Ltd (GEE) was commissioned by Ghazi Al Ali
Architect, on behalf of Paramount Property Group, to complete a geotechnical
investigation at the site which relates to the proposed construction of a new multi-
storey residential development.
GEE understands that the investigation was required to support a Development
Application with Council and to assist with the preliminary design and construction of
the development, which comprises two detached, multi-storey residential
developments, constructed over a single level basement. Currently, the site is occupied
by a medium density development, operating as a motel.
The report presents the factual results of the field investigations and provides
interpretation and recommendations regarding the ground conditions at the site in
accordance with client requirements and the agreed scope of work.
Geotechnical Investigation Report
401-405 Liverpool Road, Strathfield NSW
G16089STR-R01F Page 2 of 18
1.2 PROPOSED DEVELOPMENT
As previously mentioned, the proposed development will comprise the construction of
two detached, three storey developments over a lower ground floor level and a single
level basement. The finished floor level of the basement level is expected to be 33.10
above Australian Height Datum (AHD) at the eastern portion and 33.75m at the
western portion of the site. Taking into account the existing surface level across the
site and the necessary over excavation to accommodate the basement floor slab, a
maximum depth of excavation of between approximately 2.0m to 5.0m below ground
surface (bgs) is anticipated for the western portion of the basement while an
excavation depth of between 4.7m and 7.3m bgs is expected for the eastern portion.
The excavation for the basement is also expected to extend to the northern site
boundary and approximately 5.0m, 6.0m and 8.5m from the eastern, southern and
western site boundaries, respectively.
A copy of the architectural plans is provided for reference in Appendix A.
1.3 SCOPE OF WORK
The scope of work undertaken by GEE, to satisfy the above objectives, was as follows:
Dial Before You Dig (DBYD) desktop search for underground services,
Visual appraisal of the site conditions and locality,
Review of published geological and acid sulphate maps for the area,
The drilling of boreholes and the performance Standard Penetrometer Tests
(SPTs) to assess the subsurface conditions,
The installation of a monitoring well to assess presence and depth of stabilised
groundwater within the site, and
Engineering assessment and reporting.
Geotechnical Investigation Report
401-405 Liverpool Road, Strathfield NSW
G16089STR-R01F Page 3 of 18
2 SITE INFORMATION
2.1 SITE DESCRIPTION
The site is bounded by Liverpool Road to the east, and by low to medium residential
dwellings elsewhere. Further to the south lies the Australian International Academy.
The site covers an area of approximately 4,350m2 and comprises three allotments
which are legally referred to as:
Lot 1 in Deposited Plan 784561
Lot 2 in Deposited Plan 784561
Lot 3 in Deposited Plan 659289
At the time of the investigation, the site operated as a motel, with rooms running along
the northern and southern site boundaries. A structure operating as a reception was
located along the eastern boundary whilst an in-ground swimming pool occupied the
centre portion of the site. The remaining site surface was predominantly concrete, with
the exception of some garden beds and large trees.
Of particular significance to the proposed development is the presence of a Sydney
Water Sewer Line which crosses the north-western portion of the site (Appendix B).
Based on information from Sydney Water, the sewer comprises a 225mm vitrified clay
pipe with an invert depth of between approximately 1.2m and 1.3m. Considering the
extent and depth of the proposed basement, this section of sewer will require re-
alignment and discussions with Sydney Water are recommended.
2.2 TOPOGRAPHY
During the field investigation, it was noted that the site surface was highest in elevation
at the eastern site boundary, dipping down towards the west at approximately 10% in
gradient. A review of the regional topographical maps, available on the NSW Land and
Property Information’s SIXmaps (https://maps.six.nsw.gov.au), indicates that the
surface elevation is between 30m and 40m AHD.
2.3 REGIONAL GEOLOGY AND SOILS
A review of the regional geological map (reference 1) indicates that the site underlain
by the Triassic aged Bringelly Shale formation of the Wianamatta Group which typically
consists of “…shale, carbonaceous claystone, lamininte, fine to medium-grained lithic
sandstone, rare coal”.
Geotechnical Investigation Report
401-405 Liverpool Road, Strathfield NSW
G16089STR-R01F Page 4 of 18
A review of the regional soils map indicates that the site is located within the Blacktown
Soil Landscape Group (reference 2), recognised by gently undulating rises on the
underlying shale formation. Local reliefs are up to 30m and slopes are usually less than
5% in gradient. Soils of the Blacktown Group typically comprise heavy clays that have
been derived from the weathering process of shale bedrock, have low fertility and are
often strongly acidic.
2.4 REGIONAL HYDROGEOLOGY
The regional and permanent groundwater in the vicinity of the site is expected to be
confined or partly confined, discrete, water-bearing zones within the bedrock
formation. However, intermittent ‘perched’ water seepage is likely to occur at the soil /
bedrock interface following heavy and prolonged rainfall events.
Permanent groundwater associated with the Wianamatta group of Shale bedrock is
characterised by high salinity (reference 2 and 4) and high ammonia concentrations
(>10 mg/L, reference 5). In this regard, groundwater within the shale formation is not
extracted for potable use and rarely extracted for any commercial / industrial purposes.
The rate of groundwater movement is likely to be low as a result of low relief, low
altitude (approximately 35m AHD) and the low permeability of the Bringelly Shale
(between 10-13 and 10-9 m/sec – reference 6). Groundwater flow is dominated by water
movement through fractures (or joints), where stress has caused partial loss of
cohesion in the rock and evidence of potential water bearing fractures is usually the
presence of clay or iron-staining along the face of the joints.
2.5 ACID SULFATE SOIL RISK
Acid Sulfate Soil is naturally occurring sediments and soils containing iron sulfides
(principally iron sulfide, iron disulfide or their precursors). Oxidation of these soils
through exposure to the atmosphere or through lowering of groundwater levels results
in the generation of sulfuric acid.
Land that may contain potential acid sulfate soils was mapped by the NSW Department
of Land and Water Conservation (DLWC) and based on these maps local Councils
produced their own acid sulfate soil maps to be used for planning purposes.
The DLWC ‘Botany Bay’ Acid Sulfate Soil Risk Map (reference 7), indicates that the site
lies within an area with no known occurrences of acid sulphate soil and land activities
within this area are “...not likely to be affected by acid sulphate soil materials”.
Geotechnical Investigation Report
401-405 Liverpool Road, Strathfield NSW
G16089STR-R01F Page 5 of 18
The Acid Sulfate Soils Map produced by the NSW Department of Planning and
Environment, via interactive online mapping, indicates that the site lies within an area
defined as “Class 5”. In accordance with Clause 6.1 of Strathfield City Council’s LEP
(reference 8), a preliminary assessment of acid sulphate soil and potentially a
management plan, is required for “…works within 500m of adjacent Class 1, 2, 3 or 4
land that is below 5 metres Australian Height Datum and by which the watertable is
likely to be lowered below 1 metre Australian Height Datum on adjacent Class 1, 2, 3 or
4 land”.
Firstly, the surface elevation is greater than 5m AHD (at approximately 35-40m AHD).
Secondly, the maximum depth of proposed excavation is expected to be 7.3m below
the ground surface (bgs) which equates to a bulk excavation level which is significantly
greater than 1m AHD. In this regard, there is no need for an acid sulphate soil
assessment or management plan.
Additionally, as mentioned in Section 2.4, groundwater in this part of Sydney exists
within the discrete natural fractures and defects of the bedrock formation and therefore
any water seepage will be able to be controlled by pumping from a sump excavated
into the base of the excavation. Such pumping will not reduce the water table in
surrounding Class 1 to 4 acid sulphate areas below 1m AHD, which according to the
online interactive maps produced by the NSW Department of Planning and
Environment, is over 500m south of the site.
Geotechnical Investigation Report
401-405 Liverpool Road, Strathfield NSW
G16089STR-R01F Page 6 of 18
3 METHOD OF INVESTIGATION AND RESULTS
3.1 FIELDWORK METHODOLOGY
Fieldwork was undertaken on the 7th of July 2016 by Andy Chiem, a geotechnical
engineer, and comprised:
The drilling and logging of three boreholes (BH1 to BH3) in accessible areas of
the site to assess the soil conditions and depth to bedrock,
The performance of SPTs within each borehole to assess the consistency and/or
relative density of the soil profile and to assist with determining the depth to
bedrock, and
The installation of a groundwater monitoring well within a borehole to assess the
presence and depth of stabilised groundwater at the site, and to monitor the rate
of groundwater inflow.
The boreholes were drilled using a Nissan ute-mounted drill rig, owned and operated
by FICO Group, using solid flight augers (SFA) and equipped with a tungsten-carbide
drill bit (TC-bit). Boreholes BH1, BH2 and BH3 were advanced through any surface
filling and the natural (i.e. undisturbed) soil profile before terminating within the
underlying shale bedrock formation at depths of 2.60m, 0.85m and 1.15m bgs
respectively. Termination of each borehole was caused by practical TC-bit refusal.
The SPT tests were performed within the boreholes throughout the soil profile and in
accordance with Australian Standard 1289.6.3.1 (reference 9).
The monitoring well was installed within BH1, where the site elevation appeared to be
lower. The well was installed using a 50mm diameter uPVC pipe with a machine slotted
screen section, 2mm sand filter pack and a bentonite seal. Construction details of the
well are provided in the borehole logs (Appendix B).
The location of the boreholes was estimated using measurements from existing
features and is shown on Figure 1. A copy of the borehole is provided in Appendix
B.
Geotechnical Investigation Report
401-405 Liverpool Road, Strathfield NSW
G16089STR-R01F Page 7 of 18
3.2 SUBSURFACE CONDITIONS
The site stratigraphy, as observed in the boreholes, typically comprised fill material,
underlain by natural silty clay soil which graded into weathered siltstone bedrock.
Detailed descriptions of the subsurface conditions on site are provided in the borehole
logs provided in Appendix B, while the soil profile is also summarised in Table 1.
Table 1: Summary of Subsurface Conditions
Layer /
Unit Description
Depth to Base of Layer
(m)1 Consistency /
Relative
Density1
BH1 BH2 BH3
FILL /
TOPSOIL
Gravelly SAND / Clayey GRAVEL: brown /
orange / grey, fine to coarse sand, fine to
coarse gravel, brick, cobble
1.1 0.2 0.2 Loose
Silty CLAY: grey / brown, low to medium
plasticity, some fine to coarse gravel -- 0.6 0.4 Firm
NATURAL
SOIL
SILT: grey-brown 1.3 -- -- Soft
Silty CLAY: light grey mottled orange,
medium to high plasticity 2.4 0.75 1.0 Stiff
BEDROCK SILTSTONE: weathered >2.6 >0.85 >1.15 --
Note 1: Determined from the borehole and SPT observations
3.2.1 GROUNDWATER
Groundwater was not encountered during the drilling of the boreholes and the short
time in which they remained open (<10mins). However, water did eventually seep
into the monitoring well installed within borehole BH1 and a stabilised groundwater
level of 1.04m bgs was observed on the 15th of July, which was 8 days after installing
the well. The water in the well is considered to be perched water flowing along the
soil/bedrock interface which is recharged by rainfall and therefore its presence is
intermittent.
Geotechnical Investigation Report
401-405 Liverpool Road, Strathfield NSW
G16089STR-R01F Page 8 of 18
4 DISCUSSION
4.1 SITE PREPARATION
Following demolition of the existing structures and prior to bulk excavation works, all
topsoil with organic matter and any pavement materials, should be removed from the
proposed building and pavement areas. Stripped topsoil should be stockpiled for re-
use as landscape material, or disposed off-site.
Material removed from site will need to be managed in accordance with the provisions
of current legislation and may include segregation by material type classification in
accordance with NSW EPA (2014) Waste Classification Guidelines (reference 10) and
disposal at facilities appropriately licensed to receive the particular materials. GEE notes
that the natural soil and bedrock may be classified as Virgin Excavated Natural Material
(VENM) and re-used on other sites rather than disposed at a landfill, although it must
be proven to be free of contamination.
GEE notes that the natural silty clay soil profile is expected to be susceptible to loss of
strength when wet. In this regard, it may be necessary to construct a working platform
above the prepared sub-grade in areas of high construction vehicle traffic, comprising a
minimum of 150 mm of gravel or recycled concrete.
4.2 EARTHWORKS
As mentioned in Section 1.2, earthworks at the site are expected to comprise
excavation of between approximately 2.0m to 5.0m for the western portion of the and
between 4.7m and 7.3m bgs for the eastern portion. The excavation for the basement
is also expected to extend to the northern site boundary and approximately 5.0m, 6.0m
and 8.5m from the eastern, southern and western site boundaries, respectively.
4.2.1 EXCAVATION
Based on the fieldwork undertaken as part of this investigation, the excavation will
encounter fill material, underlain by natural silty clay soil before grading into weathered
siltstone bedrock at depths between 0.75m and 2.4m bgs. GEE notes that the strength
of the bedrock has not been assessed as part of this geotechnical investigation,
however, based on local knowledge, it is likely to be to low strength, becoming medium
to high strength within the depth of the proposed basement excavation. To confirm the
strength of the bedrock within the depth of proposed excavation, a more detailed
investigation would be required (preferably following demolition of the existing
dwellings) and would need to include the coring and strength testing of the bedrock
Geotechnical Investigation Report
401-405 Liverpool Road, Strathfield NSW
G16089STR-R01F Page 9 of 18
formation. Considering that the site is adjacent to a major road transport infrastructure
(Liverpool Road), coring and strength testing will likely be required by the Road and
Maritime Services (RMS) to satisfy their geotechnical technical direction (GTD
2012/001) entitled Excavation adjacent to RMS Infrastructure.
The excavation of the soil profile, and any extremely low to very low strength siltstone
is expected to be readily excavated using standard equipment such as excavators.
However, the use of an impact hammer is expected to be required upon encountering
low to medium strength (or better) bedrock, especially when combined with
unfavourable rock-defect geometry. When using an impact hammer the effects of
vibration should be considered and are discussed further in Section 4.2.3.
4.2.2 GROUNDWATER INFLOW
Permanent groundwater was not encountered during the drilling of the boreholes,
though a stabilised groundwater level of 1.04m bgs was observed within the monitoring
well on the 15th of July. Such water is considered to be perched groundwater,
recharged by rainfall events and therefore its presence is often intermittent. The
seepage is expected to be sufficiently managed during the earthworks phase by
pumping from a sump at the base of the excavation. Additionally, conventional
techniques such as strip drains behind basement walls and ag-lines will need to be
incorporated into the design of the basement, along with a sump and pump system
linked to the regional stormwater system.
4.2.3 CONSTRUCTION / EXCAVATION INDUCED VIBRATION
When using a hydraulic hammer, vibrations will be transmitted through the ground and
potentially impact on adjoining structures. Where possible, the use of other techniques
not involving impact (e.g. rock saws), should be adopted as they would reduce or
possibly eliminate risks of damage due to vibrations.
The structures on the adjacent properties (and nearby services) are sensitive to
vibrations above certain threshold levels (regarding potential for cracking). Given that
the proposed basement excavation will extend to within close proximity of the
boundaries and adjoining development, close controls by the excavation contractor
over the rock excavation are necessary, and are recommended, so that excessive
vibration effects are not generated.
Peak Particle Velocity (PPV) is usually the adopted measure of ground vibration and the
safe limits depend on the sensitivity of the adjoining structures and services. There is a
Geotechnical Investigation Report
401-405 Liverpool Road, Strathfield NSW
G16089STR-R01F Page 10 of 18
number of Australian and overseas publications which provide vibration velocity
guideline levels (or safe limits) including:
Australian Standard AS2187.2-2006 Explosives - Storage and use - Use of
explosives - Appendix J: Ground Vibrations and Airblast Overpressure (reference
11).
Australian Standard AS2670.2-1990 Evaluation of human exposure to whole-body
vibration - Part 2: Continuous and shock-induced vibration in buildings (1 to 80
Hz) (reference 12).
DIN 4150 – Part 3 – 1999. Effects if Vibration on Structures (reference 13).
Department of Environment and Conservation NSW, 2006. Assessing Vibration: a
technical guideline (reference 14).
British Standard BS 7385-1:1990. Evaluation and measurement for vibration in
buildings. Guide for measurement of vibrations and evaluation of their effects on
buildings (reference 15).
British Standard BS 7385-2:1993. Evaluation and measurement for vibration in
buildings. Guide to damage levels from groundborne vibration (reference 16).
The most appropriate guidelines levels for the proposed excavation work are provided
in AS2187.2-2006, which refers to guideline values from BS7385-2 for the prevention of
minor or cosmetic damage occurring in structures from ground vibration. Additionally,
the guideline levels provided in DIN 4150 Part 3 is considered an appropriate source for
guideline levels.
Ideally, safe limits should be determined by a specialist vibration consultant. However,
as a preliminary and conservative guide, and considering the above guidelines and the
type of adjoining structures present, GEE recommend that excavation methods should
be adopted which limit ground vibrations at the adjoining developments to not more
than 10mm/sec. Vibration monitoring will be required to verify that this is achieved.
However, if the contractor adopts methods and/or equipment which limit ground
vibration to 5mm/sec, vibration monitoring may not be required.
The PPV limits of 5mm/sec and 10mm/sec are expected to be achievable if rock
breaker equipment or other excavation methods are restricted as indicated in Table 2.
Geotechnical Investigation Report
401-405 Liverpool Road, Strathfield NSW
G16089STR-R01F Page 11 of 18
Table 2: Recommendations for Rock Hammer Equipment
Distance
from
adjoining
structure
(m)
Maximum Peak Particle Velocity
5mm/sec
Maximum Peak Particle Velocity
10mm/sec*
Equipment Operating Limit
(% of
Maximum
Capacity)
Equipment Operating
Limit (% of
Maximum
Capacity)
1.0 to 2.0 Hand operated
jackhammer only
100 300 kg rock hammer 50
2.0 to 5.0 300 kg rock hammer 50 300 kg rock hammer
or
600 kg rock hammer
100
50
5.0 to 10.0 300 kg rock hammer 100 600 kg rock hammer 100
or or
600 kg rock hammer 50 900 kg rock hammer 50
* Vibration monitoring is recommended for 10mm/sec vibration limit.
GEE notes human discomfort levels caused by vibration are typically less than the levels
that are likely to cause cosmetic or structural damage to structures. Therefore,
complaints may be lodged by neighbours before any cosmetic or structural damage
occurs. In this regard, consideration may be given to adopting more stringent vibration
limits recommended for human amenity or, as a minimum, ensuring that vibration
monitoring is undertaken as reassurance to confirm that vibrations are within safe
limits. Acceptable vibration limits for human comfort caused by construction and
excavation equipment are provided in DEC (2006) (reference 14). Specifically
maximum acceleration limits as specified in Table 2.2 of the guideline should be
adopted.
Finally, at all times, the excavation equipment should be operated by experienced
personnel, according to the manufactures instructions, and in a manner consistent with
minimising vibration effects. Measures which may be used to minimise vibration
include:
Progressive breakage from open excavated faces,
Selective breakage along open joints, where present,
Use of rock hammers in short bursts to prevent generation of resonant
frequencies,
Geotechnical Investigation Report
401-405 Liverpool Road, Strathfield NSW
G16089STR-R01F Page 12 of 18
Orientation of the rock hammer pick away from property boundaries and into the
existing open excavation,
Commencement of excavation as far away from other structures as possible, and
The use of a rock sawing or grinder adjacent to the site boundaries. GEE notes
that this equipment also reduces the possibility of overbreak and loosening of the
rock mass.
4.2.4 EXCAVATION SUPPORT
Based on the proposed development plans (Appendix A), the excavation for the lower
ground floor is expected to extend to the northern site boundary, while excavation for
the basement level will encroach on the zone of influence of a major transport
infrastructure. Therefore, either temporary shoring or the early construction of
permanent walls designed to shore up these boundaries, will be required. For
consistency, and taking into account the existing terrain, GEE recommends that the
southern and western excavation faces also be supported by either temporary shoring
or permanent walls.
At this preliminary stage, options for shoring include the use of evenly spaced mass
concrete piles (soldier piles), or contiguous piling combined with a pile cap. Open bored
piles or CFA piles are considered feasible and should be designed by a suitably
experienced structural engineer in accordance with AS 4678-2002 Earth Retaining
Structures (reference 17) and should consider the short and long term configurations.
In the short term, should the shoring walls be cantilevered or supported by a single
row of anchors and some wall movements can be tolerated (flexible wall), the pressure
acting on the wall can be estimated on the basis of a triangular earth pressure
distribution.
When internal props, such as the ground floor slab, restrain retaining wall movement,
or where significant movements cannot be tolerated (rigid wall), an ‘at-rest’ earth
pressure coefficient (Ko) should be adopted with either a uniform or trapezoidal
pressure distribution. This may also include the lengths of wall immediately adjacent to
adjoining structures that bound the site. It should be noted that shoring which is
designed for this ‘at rest’ coefficient will still undergo some lateral movements,
depending on the final configuration of the wall and construction sequence.
The design of any retaining structures should make allowance for all applicable
surcharge loadings including construction activities around the perimeter of the
Geotechnical Investigation Report
401-405 Liverpool Road, Strathfield NSW
G16089STR-R01F Page 13 of 18
excavation and adjacent buildings. Consideration should be given to the possibility of a
hydrostatic pressure due to build-up of water behind the wall (e.g. from broken
services), unless permanent subsurface drainage can be provided.
Finally, computer aided analysis may be carried out to assess potential ground
movements based on different wall designs and construction sequence, so as to control
deflections to within tolerable limits. It is also considered prudent to carry out surveys
before and after installation to measure the actual movement of the wall or soil.
Preliminary geotechnical parameters for the soil and bedrock profile encountered at the
site are provided in Table 3 and it is recommended that further investigation, including
the coring of the bedrock throughout the full depth of the basement level be
undertaken to confirm these parameters and provide more information on the various
strength characteristics of the bedrock formation.