Eden Wharf Extension - Preliminary Dredge Plume Modelling
Transcript of Eden Wharf Extension - Preliminary Dredge Plume Modelling
Eden Wharf Extension -
Preliminary Dredge Plume
Modelling
Report
October 2016
Level 17, 141 Walker St
North Sydney NSW 2060
Australia
301020-07698-001
www.advisian.com
Department of Primary Industries
Eden Wharf Extension - Preliminary
Dredge Plume Modelling
Report
Advisian ii
Synopsis
This report provides an update on the preliminary dredge plume modelling carried out in August
2015 for inclusion in the EIS to include updated dredge quantities and assess the impact of two
different dredging methodologies as considered in the Final Dredge Plan (September 2016).
Disclaimer
This report has been prepared on behalf of and for the exclusive use of Department of Primary
Industries, and is subject to and issued in accordance with the agreement between Department of
Primary Industries and Advisian.
Advisian accepts no liability or responsibility whatsoever for it in respect of any use of or reliance
upon this report by any third party.
Copying this report without the permission of Department of Primary Industries and Advisian is not
permitted.
Project No: 301020-07698-001 – Eden Wharf Extension - Preliminary
Dredge Plume Modelling: Report
Rev Description Author Review
Advisian
Approval Date
A Draft for Internal
Review
C Adamantidis
B Williams
C Adamantidis
B Draft
C Adamantidis
B Williams
C Adamantidis
C Final
C Adamantidis
B Williams
C Adamantidis
24/10/16
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Table of Contents
Executive Summary ............................................................................................................................ v
1 Introduction ........................................................................................................................... 1
1.1 Background .............................................................................................................. 1
1.2 Consultant Engagement ...................................................................................... 1
1.3 Scope .......................................................................................................................... 1
1.3.1 Exclusions ................................................................................................................. 2
2 Physiography ......................................................................................................................... 3
2.1 Bathymetry ............................................................................................................... 3
2.2 Tides and Currents ................................................................................................. 3
2.3 Waves ......................................................................................................................... 4
2.4 Wind ............................................................................................................................ 4
2.5 Sediment Properties ............................................................................................ 10
3 Model Setup ........................................................................................................................ 12
3.1 Model Description ............................................................................................... 12
3.2 Model Domain ...................................................................................................... 12
3.3 Simulation Period ................................................................................................. 14
3.4 Dredge Plan ............................................................................................................ 15
3.4.1 Location and Extent of the Dredge Pocket ...............................................15
3.4.2 Preferred Dredge Method ...............................................................................15
3.4.3 Option 1 BHD (Base Case) ...............................................................................17
3.4.4 Option 2 BHD + TSHD (Single handling method) ..................................17
3.4.5 Option 3 BHD + TSHD (Partial Double-handling method) .................18
3.5 Assumptions in dredge plume dispersal ..................................................... 19
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3.5.1 Sediment Classes and Settling Velocity ......................................................19
3.5.2 Deposition..............................................................................................................20
3.5.3 Erosion .....................................................................................................................20
3.5.4 Flocculation ...........................................................................................................21
3.5.5 Parameters Summary.........................................................................................21
3.6 Model Scenarios ................................................................................................... 21
3.6.1 Scenario 1 – Backhoe Dredging ....................................................................21
3.6.2 Scenario 3 - Trailer Suction Hopper Dredging.........................................22
3.7 Plume Dispersion Methodology ..................................................................... 25
3.7.1 Scenario 1 (BHD) .................................................................................................26
3.7.2 Scenario 3 (Combination BHD and TSHD) .................................................26
4 Model Results ...................................................................................................................... 28
4.1 Presentation of Model Results ........................................................................ 28
4.1.1 Visual Impact of TSS...........................................................................................28
4.2 Model Results – Percentile Exceedance Maps ........................................... 30
4.3 Impact of Sediment Disposal at Offshore Spoil Ground ....................... 40
5 Discussion and Recommendations.............................................................................. 42
Appendix List
Model results for E and SE wind directions Appendix A:
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Executive Summary
This report provides an update on the preliminary dredge plume assessment carried out in August
2015 for the Eden Port Expansion project (WorleyParsons 2015a, Report no. 301020-07698-MA-
REP-0002). It considers an increase in the volume to be dredged and explores the relative impact
of an additional dredging scenario, where Trailer Suction Hooper Dredging (TSHD) is considered in
conjunction with Backhoe Dredging (BHD), as described in the Final Dredging Plan (Report no.
301020-07698-MA-PLN-0002).
The generation, transport and fate of dredge plume material has been simulated at Port of Eden
using a state-of-the-art 3D hydrodynamic and sediment transport model. Two cases have been
considered in the dredge plume modelling:
Use of a medium-sized backhoe dredger (BHD) to dredge the entire dredge footprint in
conjunction with two barges;
Used of a Trailer Suction Hopper Dredge (TSHD) to deliver dredged materials to the
offshore disposal site. Most of the material would be bulked out direct by the TSHD, with
material in areas inaccessible or containing material too hard for a TSHD dredged by the
BHD and loaded into hopper barge(s). The hopper barge(s) would bottom dump the
material in deep water within the dredging footprint in an area accessible by the TSHD (i.e.
there would be double-handling of material within the dredge footprint).
Multiple sediment sources have been included at various locations in the model, to provide a more
realistic simulation of the likely sources of sediment from the dredging and the sediment disposal
when compared with the earlier preliminary dredge plume modelling. However, the analysis
presented herein remains preliminary, as no field data are yet available for model calibration or
validation.
The preliminary far-field dredge plume simulations suggest that, for the dredge methodology
considered, the footprint of areas that exceed 10mg/l above background will not occur beyond the
boundaries of the dredge pocket, for both the BHD only and combined BHD/TSHD scenarios with
double-handling. As wind-driven and tidal currents within Snug Cove are rather low, the dredge
plume is only slowly dispersed in to the wider marine environment.
Assessment of the potential for sediment dispersal from the OSG to Snug Cove has also been
carried out. Maximum near-surface simulated TSS concentrations did not exceed 1mg/L beyond
approximately 2 km from the offshore spoil disposal site. This implies that, once added to TSS
concentrations generated by the local dispersal of fine sediments from the dredge plant, TSS
concentrations will not exceed ANZECC environmental trigger levels at (10mg/L) at the mussel
farm.
A field data collection program has been commenced as of September 2016, which will provide
data for calibration and validation of a detailed dredge plume assessment.
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1 Introduction
1.1 Background
The Port of Eden is the southernmost “declared port” in NSW. The Port services the south coast of
NSW including the towns of Bega, Merimbula, Bombala and Cooma. The Port of Eden is also home
to a large fishing fleet and services the needs of a variety of importers and exporters, including
woodchip, pine logs, explosives and general cargo.
The Port of Eden has a deep water harbour with three existing wharves, including a multi-purpose
(Navy) wharf, a private berth operated by a woodchip exports company, and a breakwater berth
located in Snug Cove.
Substantial funds have been committed by various Government authorities operating at the
Federal, State and Shire level to expand the capacity of the breakwater wharf to accept cruise ships
up to 300m in length, thus facilitating access to the cruise ship industry at Eden and thereby
increasing Tourism at Eden.
1.2 Consultant Engagement
Advisian have been engaged by NSW Department of Primary Industries – Lands to provide design
services for the development of the new wharf and breakwater extension.
This report addresses, in a preliminary fashion, concerns about the impact dredge operations may
have on a nearby shellfish farm, which is sensitive to the level of fine suspended sediments within
the water column. The impact is assessed through the numerical simulation of the expected
advection and dispersal of the dredge plume during excavation of the new berth pocket, which is
deepened to accommodate the larger class of cruise vessel.
The position and plan alignment of the mussel farm is given in Australian Hydrographic Service
Chart A00192 (Figure 1-1).
1.3 Scope
The purpose of this preliminary dredge plume dispersion study is to assess the dispersal and fate
of dredge spoil material within Eden, and the potential for dredge spoil material to settle on the
shell fish farm adjacent to Snug Cove.
The study is a simplified assessment, assuming a few meteorological conditions that are of
relevance to the dispersal of any dredge plume material towards the shellfish farm. The preliminary
studies are designed to provide a first-estimate on the expected concentration of suspended
material within Snug Cove from dredge plant operations.
It is expected that, following this preliminary investigation, a more thorough numerical modeling
analysis would be conducted to calibrate the model against observed wave and current activity at
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the site, to more properly assess the range of environmental forcing at Eden and the associated
occurrence probabilities, and to undertake an appropriate level of statistical analysis on the
simulation results to define the range of expected TSS concentrations and exceedance probabilities
during the dredge season.
This report updates previous modelling undertaken in August 2015 (WorleyParsons 2015a) to
account for a larger volume of dredging than previously envisaged (so as to accommodate cruise
ships up to 325 m length), as well as updated dredge methodology as documented in the Eden
Breakwater Wharf Extension – Final Dredging Plan (Report no. 301020-07698-MA-PLN-0002).
Figure 1-1 - Location of mussel farm (“Marine Farm”) relative to Snug Cove and Eden Breakwater.
Source: Chart A00192.
1.3.1 Exclusions
The following are excluded from the preliminary modelling:
Detailed statistical analysis of the numerical model results
Collection of field data
Calibration of the model to field data
Consideration of the full range of environmental conditions.
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2 Physiography
2.1 Bathymetry
Bathymetry of Twofold Bay is described by AUS Charts 192 and 806. Detailed hydrographic survey
data have also been made available by Crown Lands, dated May 2015. This information has been
combined within the sediment plume model to provide the most accurate possible description of
the surrounding seafloor topography and adjacent coastline.
Incorporated into the model bathymetry is the proposed dredge footprint as provided in the Final
Dredging Plan (Report no. 301020-07698-MA-PLN-0002).
2.2 Tides and Currents
Tide conditions for the Eden area are derived from a Global Inverse Tide reanalysis model derived
from satellite altimeter data. The TPXO 8.0 global model of ocean tides best-fits, in a least-squares
sense, the Laplace Tidal Equations and along-track averaged data from TOPEX/Poseidon and Jason
satellite constellations (Egber, Bennet & Foreman, 1994; Egbert and Erofeeva, 2002). The tides are
provided as complex amplitudes of earth-relative sea-surface elevation for eight primary (M2, S2,
N2, K2, K1, O1, P1, Q1), two long period (Mf, Mm) and three non-linear (M4, MS4, MN4) harmonic
constituents. These constituents are used to provide boundary conditions for the tidal
hydrodynamic model.
Previous analysis of tidal elevations and tidal currents are given in Cardno (2011) and GHD (2013).
Tidal planes at Port of Eden are given in Table 2-1. Peak spring tidal currents are in the region of
0.03m/s at the south-west tip of the breakwater. This compares with a 5-year ARI wind-driven
current magnitude of 0.4m/s in the vicinity of Snug Cove and the breakwater (GHD, 2013).
Table 2-1 Tidal Planes at Eden, relative to Chart Datum. Reproduced from Australian National Tide
Tables (2009).
Highest Astronomical Tide (HAT) 2.1m
Mean Higher High Water (MHHW) 1.8m
Mean Lower High Water (MLHW) 1.2m
Mean Sea Level (MSL) 1.0m
Mean Higher Low Water (MHLW) 0.8m
Mean Lower Low Water (MLLW) 0.2m
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2.3 Waves
Wave conditions within Twofold Bay consist of (a) swell waves generated within the Pacific Ocean
basin, and (b) wind-sea wave conditions generated by local squall activity generated by weather
fronts passing over Eden. In general, wave energy is low within Twofold Bay. GHD (2013) report 1-
year ARI wave heights at the south-west tip of the breakwater to be in the region of <1.1m (wind-
sea) and ~2.0m (swell). Associated peak wave periods for wind-sea are in the region of 4 seconds,
whilst those for swell are in the region of 9 - 12s (MHL, 2007; GHD, 2013).
Although wind-sea Hm0 during squalls are typically of the same magnitude as longer-crested swell
waves refracting and diffracting in from the Pacific, the potential for sediment resuspension during
dredge operations will be governed by swell wave activity due to much greater orbital velocities at
the sea floor (~10m below Chart Datum at the dredge pocket) . Locally generated wind-sea waves
are therefore excluded from this analysis.
Seasonal mean swell wave parameters obtained from analysis of a global wave hindcast model are
given in Table 2-2 for position 37.0°S, 150.5°E. The Hm0 given is the seasonal mean value. The
imposed wave direction is taken as the energy-weighted peak wave direction averaged across the
season. The peak wave period is derived from a fitting relationship between Hm0 and Tp observed in
the data for waves occurring within ±45° of the seasonal wave direction.
Table 2-2: Seasonally representative integral wav parameters derived from analysis of NOAA
WaveWatch3 global hindcast model at location 37.0°S, 150.5°E.
Season Hm0 (m) Tp (s) MWD (°TN)
Summer 1.73 8.4 62.6
Winter 1.72 9.3 77.0
The swell wave parameters are imposed as uniform boundary wave conditions in the wave model
and propagated to shore.
2.4 Wind
Wind data for the region is taken from Bureau of Meteorology station Merimbula Airport AWS
(36.91°S, 149.90°E) for a period of 10 years encompassing 1998 to 2008. Prior to analysis wind
speeds were adjusted to 10m above mean sea level using a 1/7th
power law relationship.
Merimbula Airport AWS was selected over other weather stations due to the proximity of the
weather station to Eden (18km), the completeness of data records (close to 100%) and the relative
modernity of the observations.
It is noted that Cardno (2011) and GHD (2013) produced a wind climate by blending a combination
of CFS wind fields used in the NOAA WaveWatch3 wave hindcast model and wind observations
made at Green Cape, which is a similar distance to the south of Eden. It is considered unnecessarily
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complex to reproduce this wind climate for the purpose of dredge plume simulations at this initial
stage, noting that the blended Green Cape wind field did not successfully reproduce measured
wind-sea wave heights at the EWS observation point (Cardno, 2011).
Figure 2-1 to Figure 2-4 show seasonal wind roses for spring, summer, autumn and winter. In
general, the most common directions are south-west and north-east. However the most sensitive
sectors in terms of dredge plume impacts will be for winds approaching from the north-east to
south-east, as these will induce currents in the water column that will move dredge plume material
towards the mussel farm.
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Figure 2-1: Wind rose at Merimbula Airport AWS for Autumn, 1998 – 2008.
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Figure 2-2: Wind rose at Merimbula Airport AWS for Summer, 1998 – 2008.
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Figure 2-3: Wind rose at Merimbula Airport AWS for Autumn, 1998 – 2008.
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Figure 2-4: Wind rose at Merimbula Airport AWS for Winter, 1998 – 2008.
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2.5 Sediment Properties
A summary of the sediment characteristics are provided in Table 2-3 based on the results and
findings as outlined in the Eden Breakwater Wharf Extension, Sediment Sampling and Analysis Plan.
(Australasian Marine Associates, 15/8/2016, Rev 3). The sediments are dominated by the sand
fraction with a mean of 83% sand, and minor components of clay and silt (maximum of 12% fines).
A variable percentage of gravels was recorded, up to 32%.
Table 2-3: Summary of Sediment Particle Size Analysis
Cla
y
(<2µ
m)
(%)
Sil
t (2
–
60
µm
)
(%)
San
d
(60
µm
–
2m
m)
(%)
Gra
vel
(>2m
m)
(%)
Co
bb
les
(>6 c
m)
(%)
Number of
samples 44 44 44 44 44
Mean 5 2 83 10 <1
Standard
Deviation 2 1 10 9 -
Maximum 8 4 96 32 <1
Minimum 1 <1 61 1 <1
The sediment properties at the site of the proposed dredging were estimated by examining the
individual vibrocores within the dredge footprint. That analysis found that the Clay and Silt
components are approximately 5% each of the sediment composition throughout the dredge
footprint, as illustrated in Figure 2-5. The updated modelling has therefore assumed a sediment
composition of 5% silt, 5% clay and 90% sand throughout the dredge area.
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Figure 2-5 – Percentage of sand, silt and clay at each location within the dredge footprint as indicated
in the map above.
000000000 250250250250250250250250250 500500500500500500500500500
metresmetresmetresmetresmetresmetresmetresmetresmetres
D1D2
D3D4
D5
D7
D6
05
101520253035404550556065707580859095
100
D1 D2 D3 D4 D5 D6 D7
% o
f se
dim
en
t co
mp
osi
tio
n
Sediment source location
Clay
Silt
Sand
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3 Model Setup
3.1 Model Description
The dredge plume dispersion simulations are undertaken Delft3D, which is a fully integrated
computer software suite for a multi-disciplinary approach and 3D computations for coastal, river
and estuarine areas. It can carry out simulations of flows, sediment transports, waves, water quality,
morphological developments and ecology.
The FLOW module, which is used to simulate tidal and wind-driven currents, is a multi-dimensional
(2D or 3D) hydrodynamic (and transport) simulation program which calculates non-steady flow and
transport phenomena that result from tidal and meteorological forcing on a curvilinear, boundary
fitted grid. For the 3D simulations considered in this study, the vertical grid is defined following the
σ co-ordinate approach. That is, the model is split in to a number of layers that are defined as a
constant percentage of water depth. Four layers have been used in the hydrodynamic model, with
a fifth “bed layer” describing sedimentation.
As a refinement on the previous dredge plume modelling, the water quality model used to
describe the dredge plume behaviour was D-WAQ PART, a 3D random walk particle tracking
model which is part of the Delft 3D suite and is coupled to the hydrodynamic model. Re-
suspension of material is included within the model predictions, with all fines released from the
dredging and suspended during the dredge disposal settling through the water column and being
available for later re-suspension as based on a critical shear-stress formulation.
3.2 Model Domain
A domain-decomposition approach is used to downscale wave and hydrodynamic processes
occurring on the continental shelf (grid resolution order of 1km) to Eden Breakwater (grid
resolution 20m). Four domains are used, with simulated variables dynamically passed between
each domain:
A ‘coarse’ domain, horizontal grid resolution 540m by 540m, driven by tidal elevation
boundaries derived from TPXO 8.0 global tide inversion model;
An ‘outer’ medium resolution domain of grid cell size 180m by 180m;
An ‘inner’ medium resolution domain of grid cell size 60m by 60m, encompassing Twofold
Bay;
A ‘fine’ model of grid cell size 20m by 20m, encompassing Snug Cove, the breakwater
extension, the dredge pocket, and the adjacent mussel farm.
Each model domain was implemented in 3D with four σ-layers in the vertical, each layer
comprising 25% of the local water column thickness.
Figure 3-1 and Figure 3-2 show the model domains and bathymetry used in the dredge plume
model.
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Figure 3-1: Extent of Delft3D model domains comprising Eden hydrodynamic model. Location of OSG
dredge spoil disposal site in model (see Section 4.3) shown by white asterisk.
OSG
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Figure 3-2: Expanded view of model domain and bathymetry around Snug Cove.
3.3 Simulation Period
All simulations are run for a total of
2 days to achieve numerical stability within the model from cold start, and allow wind-
driven currents to achieve quasi-equilibrium;
1 day to allow local quasi-equilibrium of the dredge plume in the immediate vicinity of the
dredger;
29 day lunar cycle during which simulation results are output and analysed for statistics.
A 29 day lunar cycle is considered long enough to allow a reasonable estimate of the dredge
plume dispersal to the wider environment. The ultimate selection of simulation time is a
compromise between accuracy (longer is better) and computational efficiency (shorter is better).
The key criterion is that some form of quasi-equilibrium is achieved with the dispersal of fine
suspended sediment at the site. As a number of simplifying assumptions are made about the
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dredge plant operations (see Section 3.6) to maximise environmental impact to the mussel farm,
there is no need to simulate the entire dredge season at this level of assessment.
3.4 Dredge Plan
3.4.1 Location and Extent of the Dredge Pocket
Figure 3-3 shows the location and footprint of the dredge pocket at -10.5m CD.
Since the Concept Dredging Plan some refinements have been made to the design of the dredge
basin including:
The berth pocket has been defined (refer to Drawing 301020-07698-MA-DWG-3002 Rev A
- Figure 3-3)
Some 231,500 m3 (net) of dredged materials is expected to require dredging. This includes
an average over-dredge allowance of 0.5m over an area of 116,500 m2 but excludes
contingency from sedimentation since the time of the most recent hydrographic survey
(2015).
Approximately 6,000 m3 of rock or rock like materials is included in the above figure.
3.4.2 Preferred Dredge Method
The Concept Dredging Plan compared the use of a Backhoe Dredge (BHD), Cutter Suction Dredge
(CSD) or Trailer Suction Hopper Dredger (TSHD) working independently over the entire dredge
footprint.
The report recommended a medium sized BHD for the following main reasons:
Availability of three vessels of this type operating in south east Australia and New Zealand
The three BHD’s are expected to be able to dredge most, if not all, of the fractured rock
that may be encountered without secondary pre- treatment.; and
The material can be dredged at or near its natural moisture content to minimise the
generation of plumes.
Subsequently to the Concept Dredging Plan, a final design workshop was undertaken to compare
the relative advantages and disadvantages for a dual dredge spread (using a BHD in combination
with a TSHD) compared to a single medium sized BHD operating independently. The principal
objective of the workshop was to establish if the environmental assessment process, related
studies and tender documents are to allow for potential use of a TSHD to undertake part of the
dredge works.
For all options, work would be carried out on a 24 hours, 7 days a week basis. A shorter duration
time is beneficial in reducing any risk of harm to the environment, regardless of the dredging
method.
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Figure 3-3 – Revised dredge pocket extent
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A description of three dredging options considered in the Final Dredge Plan is provided below.
Option 1 and Option 3 have been modelled, with Option 3 likely to represent the worst case
environmental scenario with the highest potential for adverse impacts from sediment dispersal.
3.4.3 Option 1 BHD (Base Case)
The backhoe dredger excavates material and places into the accompanying hopper barge(s). The
material is then transported and disposed by bottom dumping in the marine disposal area. This
method generally requires two barges to facilitate continuous dredging. For a disposal ground
within 6.0 nautical miles, each barge would require a hopper capacity of 900 to 1200 m3. The BHD
removes material at or near its natural moisture content to minimise the generation of plumes.
The BHD is an essential component of the dredge project as it will be the only effective means of
removing rock.
Typical plant likely to be used to fulfil the above dredge method includes:
Medium BHD currently in use in the region (equivalent to approx. 200 tonne excavator and
up to 10m3 bucket capacity);
Two appropriately sized barges (i.e. 900 m3 to 1,200 m
3) in size either towed by tugs or
self-propelled; and
Appropriately sized tugs or work boats to assist with dredger positioning, move barges
and take barges offshore as necessary.
In addition to the base case option of using a BHD for dredging and hopper barge to transport the
material to the offshore spoil ground, there are two additional methods which are considered
viable/feasible for dredging work at Eden. These are described below:
3.4.4 Option 2 BHD + TSHD (Single handling method)
This involves bulk dredging of OTR materials using the TSHD and use of the BHD and hopper
barges to remove rock and sediments near existing structures and in areas where the TSHD cannot
manoeuvre. It is envisaged the TSHD would undertake most of the dredging of Zone 2 and the
BHD would dredge Zone 1 and a portion of Zone 2, including areas alongside the existing
Multipurpose Jetty and Breakwater Wharf. In this scenario both dredges would transport dredged
materials directly to the Offshore Disposal Site (ODS). The BHD would require two barges in the
order of 900 to 1200m3 for efficient operation and one tow vessel. A towed barge would achieve
up to 6 knots in open waters. Accordingly, return transit times of 2 to 3 hours would be expected
for each barge movement.
The single handling method:
Reduces barge movements to ODS, increases the safety of dredge operations and reduces
the risk to other users.
Has the potential to reduce the execution time by up to 30% to approximately 10 weeks;
and
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Reduces the overall cost of the works by up to 20% compared to the base case method.
Typical plant likely to be used to fulfil the above dredge methods include:
Medium BHD currently in use in the region (equivalent to approx. 200 tonne excavator and
up to 10m3 bucket capacity);
Two appropriately sized barges (i.e. 900 m3 to 1,200 m
3) in size either towed by tugs or
self-propelled;
Appropriately sized tugs or work boats to assist with dredger positioning, move barges
and take barges offshore as necessary; and
TSHD such as the MV Brisbane (2,900m3 hopper capacity).
3.4.5 Option 3 BHD + TSHD (Partial Double-handling method)
In order to maximise overall safety during the works, this method uses the TSHD to deliver most (if
not all dredged materials to the ODS. Most of the material would be bulked out direct by the
TSHD. Material in areas inaccessible or containing material too hard for a TSHD would be dredged
by the BHD and loaded into hopper barge(s). The hopper barge(s) would bottom dump the
material in deep water within the dredging footprint in an area accessible by the TSHD. Any large
rock that cannot be handled by the TSHD would either be disposed of elsewhere within the site
(e.g. along the lee side of the breakwater) or at the ODS.
The partial double-handling method:
Minimises barge movements to ODS, maximises the safety of dredge operations and
minimises the risk to other users.
Has the potential to reduce the execution time by up to 50% to approximately 6 weeks;
Reduces the overall cost of the works by up to 30% compared to the BHD option; and
Requires a temporary stockpile site within the dredge footprint. A suitable site which
could be considered in the environmental impact assessment would be the lee-side of the
existing breakwater in between the fender line of the proposed wharf and the toe line of
the breakwater. This site is in approximately 8m of water, and is sufficiently clear from
moorings and other marine structures to allow continued access to these assets.
Typical plant likely to be used to fulfil the above dredge methods include:
Medium BHD currently in use in the region (equivalent to approx. 200 tonne excavator and
up to 10m3 bucket capacity);
Two appropriately sized barges (i.e. 900 m3 to 1,200 m
3) in size either towed by tugs or
self-propelled;
Appropriately sized tugs or work boats to assist with dredger positioning, move barges
and take barges offshore as necessary; and
TSHD such as the MV Brisbane (2,900m3 hopper capacity).
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3.5 Assumptions in dredge plume dispersal
The TSHD dredges by pulling a drag head across the seafloor, mobilising the seabed material into
the water column, while sucking the subsequent water and suspended material up through the
drag head. This mixture of water and dredged material is then pumped through external pipes
into a hopper. Heavier particles settle to the bottom of the hopper and lighter particles remain in
suspension within the hopper. Once the hopper is full of water, the hopper is typically allowed to
overflow with the low-density mixture overflowing back into the sea, while continuing to capture
the denser material within the hopper. This reduces the number of trips required from the dredge
area to the offshore disposal area and therefore reduces the overall duration of the dredging
campaign. Sediment is introduced into the water column from the TSHD near the seabed at the
drag head and from propeller wash, and near the surface from the overflow.
In comparison, sediment from the BHD is introduced near the bed only at the dredge area. For this
reason, Option 3 is considered to present the greatest potential for the generation of sediment
plumes in Snug Cove, as sediment is introduced both at the bed and near the surface, and this
option involves double-handling of material.
The dredge plume simulations consider the dredge pocket excavated to a depth of 10.5m below
CD, as this represents the most conservative scenario in terms of environmental impact.
3.5.1 Sediment Classes and Settling Velocity
Sediment plume dispersion studies typically require three to five particle size classes to be defined,
based on their distinct settling patterns and potential for re-suspension as a result of current
and/or wave action. As the plume dispersion model is used to simulate the dispersion of material
suspended into the water column, typically only the fine particles, including silts and clays, are
included in the model as coarser materials, including sands and gravels, settle out almost
immediately.
For this preliminary plume model study, four particle settling velocity classes were used for the
assessment, which was considered sufficient to characterise the material fractions at the various
locations where dredging is to take place. These settling velocity classes are presented in Table 3-1
together with the corresponding particle fraction.
Table 3-1 Particle size classes and settling velocities used for the modelling assessment
Particle Faction [micron] Settling Velocity [cm/sec]
<2 (Clay) 0.00035
2 – 65 (Silt) 0.035
65 – 125 (Fine Sand) 1.2
> 125 (Coarse Sand) 3.0
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The sediment velocity classifications listed above are based on an unflocculated sediment sample,
that is, all the particles were separated in the analysis. In reality at high suspended sediment
concentrations (>300 mg/l) the finer clay and silt particles are likely to floc together in the plume
upon entering salt water, resulting in larger particles (or flocs) that have much higher settling
velocities. Below this level of concentration flocculation appears to be of minor importance (van
Rijn, 1989). The modelling presented in this report has assumed that the particles will not flocculate
and have a constant settling velocity. This assumption is expected to give slightly conservative
estimates of the plume dimensions and concentrations as particles with lower settling velocities
will remain in suspension for longer periods, allowing the plume to travel further.
3.5.2 Deposition
In the model, the deposition rate is formulated as a function of the settling velocity, the near-bed
concentration and a threshold bed shear stress below which sediment is deposited (‘critical shear
stress for deposition’). For the current study, a critical bed shear stress for deposition of 0.05 N/m2
was employed for the finer size classes (clays and fine silts), consistent with recommendations for
dredge dispersion studies in areas of similar seabed characteristics (Doorn-Groen & Foster 2007;
Van Rijn, L.C. 1989).
3.5.3 Erosion
The erosion rate depends on the seabed properties, whether the seabed is dense and consolidated
or soft and only partly consolidated. In the present model, the bed is described as one layer with
the material deposited and resuspended solely that which results from the dredging works at the
project site. This enabled the impact of the proposed dredging works to be isolated in the analysis.
The layer contains the material which is re-suspended and subsequently settled during each tidal
cycle. A threshold shear stress determines whether the deposition material is re-suspended or not.
The criterion for erosion is exceeded corresponding to the driving forces exceeding the sediment
stabilising forces.
Partheniades (1965) and Parchure & Mehta (1985) investigated the critical shear stress for erosion
of cohesive sediments as listed in Table 3-2. For the present modelling study the critical shear
stress parameter in the model was set to the value of 0.2 N/m2 as the particle tracking analysis is
primarily concerned with the transport and fate of unconsolidated silt and soft mud suspended by
the dredging processes, rather than the rapidly settling sand component which does not remain in
the water column and therefore does not contribute to turbidity.
Table 3-2 - Criteria Shear Stress for Sedimentation and Erosion. (Partheniades (1965) and Parchure &
Mehta (1985))
Mud Type Density (kg/m3)
Typical critical shear
stress (N/m2)
Mobile fluid mud 180 0.05 – 0.1
Partly consolidated
mud 450 0.2 – 0.4
Hard mud 600+ 0.6 – 2.0
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3.5.4 Flocculation
In marine environments the settling velocity of fine sediments is largely governed by the extent of
flocculation of the individual particles. The settling velocity of the floccs is strongly related to the
salinity, sediment concentration, water depth, flow velocity and the type of type of instrument used
to make the observation (Van Rijn, 1993).
Experimental laboratory research shows a clear effect of salinity on settling velocity for salinities up
to 10PSU when the sediment concentration is smaller than 1000 mg/l (Krone, 1962), which is within
the expected range of concentrations at Eden for back-hoe dredger operations. Beyond 10PSU,
which is the case for Eden, the settling velocity for sediment suspensions below 1000 mg/l is
essentially that of the unflocculated particles. Therefore only the unflocculated settling velocities
are considered within the model.
The settling velocity of each fraction is considered constant during the simulations.
3.5.5 Parameters Summary
The dispersion coefficient is a critical parameter with respect to the spatial excursion of the
sediment plume. This and other sediment parameters used in the model set-up, based upon
Advisian’s experience in other sediment dispersion studies, have been summarised in Table 3-3.
Table 3-3 - Key parameters and formulations used in the dredge plume models
Model Parameter
Critical shear stress for deposition 0.05 N/m2
Critical shear stress for erosion 0.2 N/m2
Horizontal dispersion coefficient 1.0 m2/s
Vertical dispersion coefficient 0.01 m2/s
Number of vertical sigma layers 4 (equal layers each spanning 25% of the depth)
3.6 Model Scenarios
3.6.1 Scenario 1 – Backhoe Dredging
Under this scenario, a backhoe dredger is proposed to be used for dredging of the entire dredge
pocket.
The backhoe dredger comprises a long-reach excavator mounted on a floating pontoon. The
dredger excavates the seabed and fills two non-propelled split-hopper barges with a hopper
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capacity of 900 m3 to 1,200 m
3. Once filled, the barges are propelled to the spoil disposal ground
by a tug and would typically sail at around 5 knots, for a sailing time from the dredge site to the
spoil ground of around 80 minutes. The two non-propelled barges are assumed to work in series,
with the dredger filling one barge while the other is being towed by the tug to the spoil disposal
area.
Advisian’s experience with similar dredge studies has shown that the following production rates for
backhoe dredging can be expected:
14,000 m3 per week in “hard” material (i.e. “rock”);
24,000 m3 to 28,000 m
3 per week in “soft” material (sand and silt, which comprises the
majority of sediment to be removed from the dredge pocket).
Table 3-4 summarises the production rate characteristics that have been assumed for the purposes
of the modelling.
Dredging cycle times have been estimated from Table 3-4 and assuming both split hopper barges
being used, for an overall dredge cycle time of 280 minutes.
Based on the volume of dredging required and the assumed production rate of the dredger, using
the backhoe dredger would result in an estimated dredging campaign duration of at least 10
weeks, assuming that dredging will occur for 24 hours a day, 7 days per week.
Table 3-4 - Summary of dredging characteristics (adapted from WorleyParsons 2005)
Backhoe TSD 2900 (Brisbane)
Sand Silt Sand Silt
Time to fill (min) 179 195 120 120
Time of overflow (min) - - 10 10
In-situ sediment volume to fill barge incl. bulking (m3) 625 600 2,074 1,160
Mean filling sediment discharge (kg/s) 1.2 9
5.8 5.22
Mean overflow discharge (kg/s) 19.1 19.1
Amount suspended per barge load 12,900 105,300 24,200 11,600
3.6.2 Scenario 3 - Trailer Suction Hopper Dredging
Under Option 3, most of the material would be bulked out direct by the TSHD. Material in areas
inaccessible or containing material too hard for a TSHD would be dredged by the BHD and loaded
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into hopper barge(s). The hopper barge(s) would bottom dump the material in deep water within
the dredging footprint in an area accessible by the TSHD. Any large rock that cannot be handled
by the TSHD would either be disposed of elsewhere within the site (e.g. along the lee side of the
breakwater) or at the ODS.
The assumed TSHD dredge for this project is the BRISBANE or similar (Figure 3-4). The
characteristics of the Brisbane vessel and proposed modes of operation relevant to the modelling
are summarised below:
Average sailing speed = 10 knots (loaded and empty)
Production rate between 750 and 1000 m3/hr (based on filling times between 1.5 and 2
hours and an average load of 1,500 m3)
Draft of 6.2 m when loaded . Propeller wash will apply for dredging at Eden, due to the
relatively shallow dredging depth.
Overflow released through “green valve” at the vessel’s draft level of 6 m
During dredging, fine sediment will be generated from bottom disturbance and from overflow
from the hopper barges as well as potentially from propeller wash. The majority of the visual
turbidity at the dredging sites is likely to be attributed to the overflow water from the barges rather
than effects from bottom disturbance.
The sediment characteristics and rate of overflow is dependent on the type of dredge and varies
with make and model. WorleyParsons (2005) undertook a detailed analysis of various options of
dredge to assess filling times and the length of time the barge will overflow.
Economic loading times and length of overflow discharge were assed in WorleyParsons (2005),
considering the following factors:
Type of dredge
Hopper capacity
Type of material dredged
Behaviour of sediment during dredging
Fully laden sailing speed
Length of the dredging area
Distance to disposal site
Time to turn dredger
Time to dispose (dump) sediment
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Figure 3-4 – Brisbane TSHD (http://www.marinetraffic.com/en/ais/details/ships/503380000)
Concentrations of suspended sediment released during the dredging operation (excluding
overflow) were estimated by the S factor method that provides estimates of sediment that passes
out of the immediate dredging area, typically 50 m from the dredger. The S factor is defined as the
following:
𝑆 =𝐴𝑚𝑜𝑢𝑛𝑡 𝑟𝑒𝑠𝑢𝑠𝑝𝑒𝑛𝑑𝑒𝑑
𝐴𝑚𝑜𝑢𝑛𝑡 𝑜𝑓 𝑆𝑜𝑖𝑙 𝐷𝑟𝑒𝑑𝑔𝑒𝑑 (𝑘𝑔/𝑚3)
Typical expected “S factors” assuming that overflow and degassing discharge is prohibited for TSD
are in the order of 5 kg/m3. Calculated S Factor for silt based on the material behaviour during
extraction has previously been estimated at approximately 180 kg/m3, and has been assumed for
this analysis.
Suspended sediment concentration of the overflow discharge was based on the WorleyParsons in-
house database of recorded overflow concentrations for dredging in Western Australia, as reported
in WorleyParsons (2005). Typical mean overflow concentrations are generally in the order of 6,000
to 8,000 mg/l. For this dredge plume study 8,000 mg/l is considered.
The sediment during dredging is likely to behave as non-cohesive sediment. It is expected that
during dredging via TSHD the material will breakdown from the cohesive state and behave similar
to a non-cohesive material.
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Table 3-4 summarises the production rate characteristics that have been assumed for the purposes
of the modelling.
Scenario 3 uses a combination of BHD and TSHD, with the BHD dumping material within the
dredge pocket and the TSHD removing this material and disposing it at the Offshore Spoil Disposal
site. While the quantity of material that would be removed by BHD is not known precisely, for the
purposes of the preliminary modelling it is assumed that 50,000 m3 of material would need to be
removed using the BHD and that this would be likely located near the breakwater. Based on the
volume of sediment and an assumed production rate of 750 m3/h for the TSHD, the dredge
campaign is assumed to take approximately 3 weeks.
3.7 Plume Dispersion Methodology
The release and settlement of sediments during dredging has been simulated using the particle
tracking model. The particle tracking extension to Delft3D incorporates variable settling rates and
allows the particles to be grounded and resuspended.
For the TSHD, sediment releases would occur from the drag head (i.e. distributed in Layer 4 of the
model, i.e. near the bed at 80% of the water depth), and overflow releases nearer to the surface
based on the overflow release valve at the vessel’s draft level of 6 m (Layer 2 of the model at 40%
of the water depth). While there would be little contribution from propeller wash expected, as the
draft of the vessel is 6 m over an overall water depth of 11 m, this was included in the near-bed
sediment contribution.
At the spoil disposal ground and for disposal of the BHD spoil within the dredge footprint,
sediment suspended during disposal was added to model at 20%, 40% and 60% of the model
depth (Layer 1, Layer 2 and Layer 3) over 20 minutes. The discharge depths are based on physical
measurements presented in US Army Engineer Waterways Experiment Station (1992).
For the backhoe dredging, it is assumed that at the dredge site, sediment is released near the bed
– i.e. in the bottom layer of the model domain (Layer 4).
The following assumptions were used in modelling the production rate of sediment at the spoil
ground and at the dredging site:
For the TSHD, the overall cycle time used in the model is 220 minutes, which includes 120
minutes dredge time (to fill the hopper), 10 minutes overflow time at the dredge site, 40
minutes sailing time, 20 minutes dumping at the spoil ground (and within the dredge
footprint) and 40 minutes return sailing time.
For the backhoe dredging for Option 1, the cycle times used in the model includes 195 min
filling, 80 minutes sailing (@ 5 knots), 20 minutes dumping at the spoil ground, 20 minutes
return sailing time and two hopper barges working in series, 24 hours per day, 7 days per
week.
For the backhoe dredging for Option 3, the material is dumped within the dredge pocket
and so there would be no sailing time required.
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Based on previous experience with capital dredging works it is assumed that 80% of the
reworked dredged material will settle immediately to the seabed with the dumped mass.
The remainder will slowly settle and disperse into the environment.
The location of each sediment source in the dredge area has been assumed to be
sequential.
Multiple sediment sources were introduced into the model to indicate the likely sequence of
dredging in the different areas, as well as the main sediment disposal location at the spoil ground,
as indicated in Figure 3-5.
3.7.1 Scenario 1 (BHD)
For the BHD scenario, a full 29 day lunar cycle of BHD was simulated, with sediment being released
near the bed at the 7 locations (D1 – D7) indicated in Figure 3-5. Sediment was released at the
spoil ground over 20 minutes for each dredging cycle.
3.7.2 Scenario 3 (Combination BHD and TSHD)
For Scenario 3, dredging was assumed to occur over the first three weeks of the month, to simulate
the expected duration of dredging under this method, and also the persistence of the plume
following cessation of dredging. Sediment was released near the bed at 3 locations (D1 to D3)
indicated in Figure 3-5, which were assumed to require BHD. It was then assumed that the
sediment from the BHD would be released at location D7 over the top three layers of the model.
The TSHD would then remove sediment from Locations D4 to D7, from which sediment is released
near the bed (from the drag head) and at around 40% of the depth (from the dredge overflow).
Sediment was then released at the spoil ground over 20 minutes for each dredging cycle.
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000000000 250250250250250250250250250 500500500500500500500500500
metresmetresmetresmetresmetresmetresmetresmetresmetres
D1D2
D3D4
D5
D7
D6
Location (D7) where material placed
from BHD for removal by TSHD
0 1 2
kilometres
Mussel Farm
Offshore Spoil
Disposal Ground
Figure 3-5 – Sediment sources in the model
Area where BHD assumed under
Scenario 3
Area where TSHD assumed under
Scenario 3