Sea salt: Composition, source and fate Flashcards

1
Q

99% of all the salt ions in the sea are:

A
  • Sodium (Na+)
  • Chloride (Cl-)
  • Sulfate (SO4-2)
  • Magnesium (Mg+2)
  • Calcium (Ca+2)
  • Potassium (K+)
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2
Q

Conservative properties of sea water

A
  • Nitrogen and the noble gases (inert because they are chemically non-reactive)
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2
Q

86% of the salt in the sea

A

Sodium and chloride

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3
Q

Major nutrients in the sea are compounds of :

A
  • Phosphorus - 0.07ppm
  • Nitrogen - 0.5 ppm
  • Silicon- 3ppm
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4
Q

Non- conservative property of the sea

A

= Concentration of nutrients - vary greatly over time
= Oxygen and CO2 due to biological recycling

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5
Q

In order of decreasing abundance the major gases in the sea are:

A
  1. Nitrogen (N2)
  2. Oxygen (O2)
  3. Carbon Dioxide (CO2)
  4. The noble gases (Ar,Ne,He)
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6
Q

Trace elements

A

Occurs in minute quantities (ppm or ppb).
n small quantities can be important for either promoting or killing life

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7
Q

Nitrogenase

A

Enzyme that is used to fix nitrogen- the reduction of nitrogen to ammonia uses iron in its active site

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8
Q

Marine organic compounds

A

Occur in low concentrations and consist of large complex molecules such as :
- fat
- Proteins
- Carbohydrates
- Hormones
- Vitamins

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9
Q

Organic compounds

A

Molecules are produced by organisms (faeces) or through decay

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10
Q

Why is the sea salty?

A
  • On land, PRECIPITATION exceeds evaporation- run off carries dissolved salts from land
  • In the Ocean, EVAPORATION exceeds precipitation- evaporating water leaves salts behind
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11
Q

Salt in seawater

A

35 g/kg (35%)

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12
Q

Not all products of chemical weathering is carried into the sea

A

Most Si, Al and Fe is left behind on land

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13
Q

Dissolution of CO2 in water

A

CO2+H2O<–> H2CO3
H2CO3<–> HCO3-+ H+
HCO3-<–> CO32-+ H+

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14
Q

Dissolved substances in river water

A

Not the same proportions as those in oceans

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15
Q

Why does sodium have a higher concentration in seawater than minerals such as Ca, Mg and K?

A

Na is more soluble than other elements.

16
Q

Processes regulating seawater salts

A
  • Primordial source from Earth’s interior
  • Volcanic gases that fall as rain
  • Fluids introduced at ridge crests/vents
  • River outflow into the ocean
  • Dusts from land (aeolian transport)
17
Q

Salt sinks examples

A
  • Wind blows sea spray
  • Absorption of clays into organic matter
  • Shells and organic matter formation by organisms
  • Volcanic reactions under the sea
  • Burial in sediments
18
Q

Balance of inputs and outputs

A
  • Seawater composition uniforms through time over the last 1.5 Ga
19
Q

Residence Time

A
  • Ions with long residence time tend to accumulate in the sea
  • Ions with short residence time are removed
  • Rapid mixing and long residence times explain the constant composition of sea water
20
Q

Mixing time

A

The time it takes for any variation to be homogenised. it is the property of the forces acting on the fluid and the size of the reservoir.

21
Q

Steady state (no change in reservoir content)

A

Flux in = flux out

22
Q

The principle of constant proportion

A

The absolute amount of salt in seawater varies, but the relative proportions of the ions is constant