geos3009 - mod 1 - estuaries
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ESTUARY TYPES ANDPROCESSES
Module 1
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What is an estuary?
Definition is difficult. Classified by physio graphical parameters ie:
geomorphology and hydrology only early definition(Cameron and Pritchard, 1963) an estuary is a semienclosed coastal body of water having a free connectionwith the open sea and within which sea water is
measurably diluted with fresh water derived from landdrainage
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Four major elementsi) its a coastal feature,ii) it has provision for salt water,iii) the salt water must be measurable,iv) fresh water is derived by rivers.
Excludes tides
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Dalrymple et al. (1982) a new geologically-orientateddefinition the seaward portion of a drowned river
system that receives sediment from both fluvial andmarine sources and contains facies influenced by tide,wave and fluvial processes. The estuary is consideredto extend from the inner limit of the tidal facies at its
head to the outer limit of coastal facies at its mouth.
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Classification by tidal range (Hayes, 1975) Micro-tidal estuaries Meso-tidal estuaries
Macro-tidal estuaries
Evolutionary classification (Dalrymple et al., 1992) Wave dominated estuaries
Tide dominated estuaries
Morphological classification (Fairbridge, 1980) Seven types
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ESTUARIES
Comprise 5% of Earths surface, but only 2% of ocean
volume; However ~60% of world population Estuaries amongst most populated areas in world For transport, industry, residence, and recreation.
Estuaries have high biological productivity
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High level of food production Coastal waters supply ~90% of global fish catch. Human activities - sedimentation from cleared land,
over fishing/trawling, destruction Wetlands,eutrophication, pollution, dams, canals and dykes forflood protection
Dynamic systems associated with river mouths
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Estuaries are tidal, lower part of rivers and associated
valleys Distinction difficult consider it a continuum ofdelta estuarine landforms
Processes function of catchment and receiving basin
Balance of wave, tide and river exerts controlover morphology and evolution.
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Deltas Shore-line protuberances River supplied sediment accumulates faster thanredistributed
By waves, currents and tides Affected by tidal dynamics, mixing of fresh & salinewaters
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Estuaries Seaward part of drowned river system receivingfluvial & marine sediment
Influenced by tide, wave, fluvial processes. Comprises fluvial-dominated upper section
- marine-influenced lower zone
- central mixed region.
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Tide-dominated estuaries Macro tidal Dominated by tidal currents
On pro-graded coastal plains Funnel shaped, wide entrances Well mixed due to strong bi directional tidal currents Rapid flows re-suspend & transport sediment
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Three zones- upstream river dominated,
- central mixed energy zone- seaward marine dominated Central zone area of sediment convergents river
and marine processes
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Wave-influenced estuaries Enclosed or partly enclosed behind wave built sandbarrier
On wave dominated coast
Separated from open ocean by sand barrier Inlet intermittently closed Gradation to coastal lagoon may be permanently orintermittently open
Decrease in water area and depth with time due to:- input of sand from shelf- extension of fluvial deltas from rivers- vertical accretion of mud in central estuary
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Sedimentation rates in central mud basins ~1mm/yr Along NSW coast - different stages of infill
Tidal range attenuated by narrow entrance
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Coastal lagoonsFeatures:
i) shallow where salt and fresh water interact,
ii) water impounded by some type of sedimentarybarrier and,iii) connection with sea restricted Aligned parallel to coast, separated by barrier
Impounded by sand barrierLow salinity
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Morphological definition of estuaries (Roy 1982, 1984
Three types of estuary on basin morphology & condition
of seaward entrance- Type 1: Drowned river valley estuary - Deep, openocean entrance, full tidal range
- Type 2: Bay Mouth Barrier Estuary - Narrow entrance,
attenuated tides- Type 3: Saline Coastal Lake/Lagoon Closedentrances
All have central basin
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Type 1 drowned barrier estuaries
sub aqueous flood tide delta
extensive fluvial delta & channel fill sequence
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Type 2 barrier estuaries Due to shallow valleys Marine-sourced sediments have considerable subaerial expression ie barriers, spits, & wash over flats
Landward portion terrestrially derived forming networkof delta distributory mouth bars, medial channel bars
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Type 3 coastal lakes Relatively small barriers, beaches & wash-over fans Flood tide deltas poorly developed or absent
Fluvial deposits consist thin wedge of sandy delta &flood plain deposits mantling peaty muds of centrallake - dominant facies
Estuaries evolved from one type into another
Sometimes a continuum.
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AUSTRALIAN ESTUARINE AUDIT(Oz estuaries)
Of 979 estuaries, >40% small catchments (
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Value of estuaries (NLWRA, 2002). Middens of Indigenous Australians shellfish and fishbones
Sydney Harbour middens >40m high For transportation, agricultural manufactured goods Ports, shipping, industry, agriculture, tourism,residential development
Human-made capital and natural capital
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Natural capital - habitat, sporning, nursery environmentsfor fish Habitats & breeding regions for birds, and marine
animals Nutrient cycling Provide natural buffer between land & ocean Salt marshes and mangroves
Sediment and nutrient filtration by trees, salt marsh &other wetland flora
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Human capital - natural assets Sheltered deep water for shipping, industry & urbandevelopment
Detrimental influences on natural assets
Fisheries critically dependent on environmental statusof ecosystem
Survival of commercial activities dependent on
disturbance Commercial fishing in Australian estuaries ~$0.4 b/y Prawn fisheries, oyster farming, barramundi & mudcrab fisheries
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Estuary-dependent fisheries are fish and crustaceansspend part of life cycle in Estuarine environment i.e.estuary a nursery area.
Estuaries worth ~$40 m/yr NSW oyster industry worth ~$29m 1999/2000 Productivity 1997 to 2000 declined by 350 t due to
poor estuarine condition Prawn production north NSW worth $107m 1999/2000
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Production declined 8912 t in 1997/1998 to 5605 t1999/2000
Catch declined 1800 t from Qld and NT to ~600 t
recreational catch $3.6 m.Commercial crab productionin 1999/2000 - $42.3 m Qld, NSW, SA, WA and NT.
Recreational fisheries in Aust $2.9 b/y with >60% in
estuaries (i.e. $1.7 b)
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Port infrastructure (NLWRA, 2002). Port Melbourne, largest port in Aust, handles $50 b/y Trade Qldss ports >$14 b/y
Marine-based tourist industry from Aust ports >$5 b/y
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Australian Estuaries Audit (NLWRA, 2002)
Classified by process, type and condition.
Six sub classes relative to wave, tide and river energyto control geomorphology
Includes drowned river valleys, embayments, smallcoastal lakes, lagoons and creeks.
About 40% total estuaries strand plains & tidal creeksdue to low river discharge low relief.
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Stage 1: Assessment Australian near-pristine estuaries.
Provided cost effective basis to focus management These estuaries require improved understanding ofprocesses to provide conservation & managementstrategies.
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Summary of condition
50% near-pristine,
22% largely unmodified, 19% modified and 9% extensively modified.
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Key pressures identified by Audit
1. Excess nutrientsFrom decaying plant & animal material, eroded soil,sewage, industrial discharge, storm water run off,fertilizers, garden waste, agricultural run off.
2. Sedimentation Fine grain sediments from catchment & near shoremarine sands important
Excess sediment associated with nutrients, toxicants,and pathogens
Catchment erosion caused by vegetation clearing &land use practices
Sediments may bypass estuary.
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3. Habitat lossShallow sandy flats, sea grass beds, salt marshes,mangroves and wetlands influenced by drainage, landclearing & dredging activities.
4. Changes to flow and tidal flushingConstruction of dams, removal of fresh water increasedsedimentation, shell fish survival and impact fishreproduction.
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5. Pathogens and contaminantsSources human and animal waste, sewage andstormwater, contaminants associated with industrialdischarge, agricultural run off, shipping and stormwater.
6. Introduced pestsIntroduction of exotic biota result in ecological &economic impacts. May destroy native populations;
degrade habitats, effect fishing, boating, swimming.
7. Modifications to ocean entrancesArtificial entrances impact estuarine ecology e.g. larval
recruitment & export to & from estuary.
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SEDIMENT TRANSPORT PROCESSES
Estuaries are conduit by which sediment transported
from rivers to sea.
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Modes of sediment transport Three transport modes - wash load, suspension &bedload within a continuum
Wash load - finest fraction, clay particles kept in
motion by turbulence Suspension by erosion of sediment of estuary bed Grain size
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Grains >150mm move as bedload
Initially grains move by saltatingReversal of current velocities give periods of slackwater, suspended material settles
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Mud, silt and sand (Wolanski, 2007) Cohesive sediment mean particle size 62.5m Silt is 4-62.5m Mud & sand transported in water column by differentprocesses
Sand carried mainly on bottom, mud in suspensionSuspended particulate matter (SPM) comprisessediment & biological matter
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PHYSICAL, CHEMICAL, BIOLOGICAL ANDANTHROPOGENIC PROCESSES CONTROLLING
CONTAMINANT BEHAVOUR IN ESTUARIES
Physical partitioning is grain size, surface area, specificgravity, magnetic properties
Chemical partitioning refers to separation, identification& quantification chemical components Physical & chemical factors strongly interrelated.
A 1, 2
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B 1, 2 G 1, 2
C
D
E
F
A.Atmospheric deposition 1. wet, 2. dryB.Fluvial inflow 1. particulate 2. dissolved phases
C.Permanent burialD.Benthic diffusionE. ResuspensionF. ResettlementG.Export 1. particulate 2. dissolved phasesH.Absorption/desorption
H
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ESTUARINE PROCESSES
Inputs of metals to estuary
Stormwater: Fluvial discharges to estuary for dissolved & particulateheavy metal phases
High- and low-precipitation conditions Stormwater most important point source of heavymetal contaminants to estuaries
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Atmospheric deposition:
Atmospheric metal contributions to estuary by directdeposition & indirectly via the catchment.
Leachates from reclaimed lands: Original area of estuaries reduced by reclamation ofintertidal areas using domestic/industrial waste &contaminated estuary sediments
High dissolved metal-release rates measured inlaboratory leachate column experiments usingsimulated rainwater and seawater percolating throughfield infill material
Metal measured in leachate from reclaimed lands
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Benthic diffusion: Calculated from core data & from analyses of porewater
Metals tightly bound in bottom sediment by sulfides,
metal influx insignificant.
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Export of metals from the estuary
Permanent burial: Sediment surface layer (hydrous layer)(top 20cm)
interacts with water column through resuspension Underlying sediment physically isolated fromoverlying water
Underlying sediment is a chemical sink
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Contaminant export under low- and high-precipitationconditions for stratified estuaries:
During dry weather, small supply of stormwater mixes
with saline water close to entry points Particulates flocculate out of water column &dissolved forms adsorb to particles
Main water body well mixed at, or close to normal sea
water salinity throughout waterway Particulate-dissolved metal phases stable over periodsof weeks in main water body
Under these conditions marine export negligible
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During high-precipitation, stormwater rapidly entersestuary as discrete, buoyant layer of high-turbiditywater ~1m thick & moves quickly down harbour exits
estuary Density differences between salt & overlyingfreshwater during rainfall events retard mixing &promote seaward transport
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Plumes provide mechanism for contaminants("first flush") to bypass estuary -dispersed at sea
Settling rates under these conditions minor Settled matter metal concentrations low with minimalmixing along boundary layer in upper estuary
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