Inputs to Estuarine and Coastal Systems Flashcards

(20 cards)

1
Q

Rivers

A

Major source of most chemical elements to the ocean
- regulates ocean chemistry, PP
Chemical weathering regulates concentration of atmospheric carbon dioxide
- feedback between weathering and climate

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2
Q

Atmospheric inputs

A

Material supplied by dry or wet deposition
Inputs high in coastal zone as most particles from land
- dust generated by wind erosion
- sea salt
- anthropogenic inputs

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3
Q

Atmospheric N inputs

A

Mainly from:
- combustion sources to the atmosphere, forming nitrate
- agricultural emissions which release ammonia
Dispersed through coastal zone, not a point source
Fluxes highly variable in space and time

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4
Q

Atmospheric sampling, bermuda

A

Tower 23m
Different instruments at the top
only samples when wind blows over ocean
Power supplied from containers at the bottom

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5
Q

Inputs of toxic metals

A

Measurable increase in surface ocean water lead concs due to combustion of leaded petrol, now falling
Atmospheric deposition:
- volatile element, mainly deposited as Hg2+
- global atmospheric burden has increased by factor of 5 in last 200 years as a result of human activities

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6
Q

Trace gases

A

estuaries and coastal seas are an important source of some climatically active trace gases
Directly or indirectly biological in origin

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7
Q

Methane

A

Produced by anaerobic microbial processes
Contributes ~15% global radiative forcing
Mainly comes from sediments but may be produced at pycnocline
Oxygenated surface waters on coastal shelves supersaturated with methane, the methane paradox
Contribution from coastal waters ~3% of total emissions or ~10% if natural methane emissions doesn’t account for bubble fluxes

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8
Q

Penlee point

A

Plymouth marine lab
measures sulphur dioxide , carbon dioxide and methane in air
Trace metals

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9
Q

Ship Plumes

A

Large increase in pollution from ship fuel
Monthyl averaged sulphur dioxide mixing ratios which represent ships emissions
After policy for reduction is sulphate emissions, inputs to coastal regions was reduced

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10
Q

Nitrous oxide

A

Nitrous oxide contributes ~6% of global radiative forcing
By product of microbial nitrification and intermediate during microbial denitrification
Mean surface saturation in shelf ~109%, estuaries ~600%

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11
Q

Submarine ground water discharge

A

Water can move in and out of sediments by tides
creates mixing zones of varying salinities of water which increase with depth in the sediments
Significant impact on biogeochemical cycling
Slow diffuse flow but can be found as large point sources in certain terrains
Both freshwater and saltwater components
Composition may be modified by chemical reactions in the aquifer.

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12
Q

Components of SGD

A

Meteoric water (fresh)
Recirculated sea water (salt)
Connate waters (v salty)

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13
Q

Detecting and quantifying SGD

A

IR imaging:
- at high lats, SGD warm relative to ocean
- at low lats, tends to be cooler
Direct measurements:
- seepage meters
Tracer techniques:
- natural using radiotracers
- artificial dyes

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14
Q

Tracers

A

Radium
224Ra. 3.66d
223Ra. 11.6d
228Ra, 5.75y
226Ra, 1600y.
226 most often used as it is integrated over a larger time period and able to see how significant the flow is into the ocean

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15
Q

226Ra tracer

A

Less effective in fresh SGD as Ra is bound to particles in fresh water

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16
Q

Water and chemical fluxes

A

estimates of water flux from SGD is mostly 6-10%
Total dissolved salts contributed to SGD may be as much as 50% of that contributed by rivers
Conc of nutrients, trace metals, organic C, methane and carbon dioxide may be considerably higher

17
Q

Reactions in estuary

A

Oxidation of organic C adds carbon dioxide, results in calcite dissolution
high levels of nutrients due to water rock interactions and anthropogenic inputs
Removal of nitrate by denitrification in low O groundwaters
Removal of dissolved iron at fresh-salt water interface and scavenging of other components

18
Q

Glacial inputs

A

Input of Fe from melting sufficient to fuel a phyto bloom
Meltwaters supply Fe in solution as nanoparticles

19
Q

Benthic sources

A

Sediments are a sink for elements and particles introduced to marine waters.
But. active recycling of many elements at the benthic interface and longer timescale release of materials into water column

20
Q

DMS

A

Dimethylsulfide produced by phaeocystis, coccos and dinos, some diatoms are also important
Oxidised in troposhere, contribute to atmospheric acidity and cloud condensation nuclei formation.