Specific chemical processes in estuaries Flashcards

(13 cards)

1
Q

What does fluorine show in estuarine mixing diagrams?

A

Conservative, and higher concentration in sea water.

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2
Q

What does iron show in estuarine mixing diagrams?

A

Non-conservative

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3
Q

Why does iron concentration decrease with increasing salinity?

A

Ligands lost by flocculation and/or the effects of increased ionic strength.

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4
Q

What does silicon show in estuarine mixing diagrams?

A

Both conservative and non-conservative behaviour across the year.

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5
Q

What are the sources of dissolved silicon?

A

Salt marshes and desorption from resuspended sediments.

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6
Q

What do silicon isotope analyses provide evidence for?

A

Removal of light Si at salinities >20, especially in July.

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7
Q

Why does manganese experience intensive cycling in estuaries?

A

Chemistry linked to changes in redox conditions.

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8
Q

What happens to manganese in anoxic sediments?

A

Mn IV is reduced to Mn II which is soluble so it can diffuse out the sediments.

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9
Q

Where are maximum concentrations of dissolved manganese found?

A

Intermediate salinities ~10 due to input of dissolved Mn II from reducing sediments.

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10
Q

Why is silicon both conservative and non conservative

A

Conservative = Simple mixing of river and seawater - Low biological activity, clear water
Non-Conservative = Biological uptake, adsorption, desorption, sediment input - Productive estuaries, muddy waters, SGD zones

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11
Q

How do reducing sediments affect dissolved Mn?

A

Low salinity: High Mn²⁺ (released from sediments).
Mid-salinity: Mn oxidizes → particles (removal).
High salinity: Low Mn (scavenged).

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12
Q

Why is silicate non-conservative in summer?

A

Diatom uptake (blooms).

Measure: Diatom counts, nutrients (NO₃⁻, PO₄³⁻), light/temperature.

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13
Q

How does increasing temperature affect silicate weathering, and what is its impact on global climate?

A

Higher temperatures speed up silicate weathering, which removes CO₂ from the atmosphere.

This leads to long-term climate cooling, forming a negative feedback loop that helps stabilize Earth’s temperature over geological timescales.

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