Sea salt: Composition, source and fate Flashcards
99% of all the salt ions in the sea are:
- Sodium (Na+)
- Chloride (Cl-)
- Sulfate (SO4-2)
- Magnesium (Mg+2)
- Calcium (Ca+2)
- Potassium (K+)
Conservative properties of sea water
- Nitrogen and the noble gases (inert because they are chemically non-reactive)
86% of the salt in the sea
Sodium and chloride
Major nutrients in the sea are compounds of :
- Phosphorus - 0.07ppm
- Nitrogen - 0.5 ppm
- Silicon- 3ppm
Non- conservative property of the sea
= Concentration of nutrients - vary greatly over time
= Oxygen and CO2 due to biological recycling
In order of decreasing abundance the major gases in the sea are:
- Nitrogen (N2)
- Oxygen (O2)
- Carbon Dioxide (CO2)
- The noble gases (Ar,Ne,He)
Trace elements
Occurs in minute quantities (ppm or ppb).
n small quantities can be important for either promoting or killing life
Nitrogenase
Enzyme that is used to fix nitrogen- the reduction of nitrogen to ammonia uses iron in its active site
Marine organic compounds
Occur in low concentrations and consist of large complex molecules such as :
- fat
- Proteins
- Carbohydrates
- Hormones
- Vitamins
Organic compounds
Molecules are produced by organisms (faeces) or through decay
Why is the sea salty?
- On land, PRECIPITATION exceeds evaporation- run off carries dissolved salts from land
- In the Ocean, EVAPORATION exceeds precipitation- evaporating water leaves salts behind
Salt in seawater
35 g/kg (35%)
Not all products of chemical weathering is carried into the sea
Most Si, Al and Fe is left behind on land
Dissolution of CO2 in water
CO2+H2O<–> H2CO3
H2CO3<–> HCO3-+ H+
HCO3-<–> CO32-+ H+
Dissolved substances in river water
Not the same proportions as those in oceans
Why does sodium have a higher concentration in seawater than minerals such as Ca, Mg and K?
Na is more soluble than other elements.
Processes regulating seawater salts
- 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)
Salt sinks examples
- 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
Balance of inputs and outputs
- Seawater composition uniforms through time over the last 1.5 Ga
Residence Time
- 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
Mixing time
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.
Steady state (no change in reservoir content)
Flux in = flux out
The principle of constant proportion
The absolute amount of salt in seawater varies, but the relative proportions of the ions is constant