sulphur cycle Flashcards
common minerals
- pyrite - FeS2
- gypsum - CaSO4 2H2O
- anhydrite - CaSO4
overview of cycle
- has localised not global effects due to short residence times
- has massive anthropogenic effects as burning of coal and ore melting released SO2
- important for cloud formation - plankton release over 20 million tonnes of sulphur in the air (as DMS) acting of hygroscopic nuclei
sulphur reservoirs
- lithosphere
- ocean water
- ocean sediments
- soil and terrestrial biota
- lake and river water
- marine biota
fluxes of sulphur
- natural
- largest between ocean and atmosphere - sea salt sulphate - post industrialisation
- consumption from lithosphere highest
- anthropogenic emissions second
- aeolian emissions have doubled
OCS/COS
- carbonyl sulphide (II)
- produced directly by organisms or oxidised from carbon disulphide (CS2)
- stable in the troposphere
- long residence time
- unreactive
- slowly mixes into stratosphere
reaction of OCS in the stratosphere
OCS + hv = S + CO
S + O2 = SO + O
SO + O2 = SO2 + O
- forms a layer of aerosol particles that reflects incoming radiation
atmospheric sulphur cycle
release into the atmosphere
- volcanic eruptions
- sea spray
- biogenic emissions
- ff combustion
taken out of atmosphere
- precipitation / wet deposition
- dry deposition
sulphur emissions into the atmosphere
- biogenic emissions (reduced oxidation state)
- DMS dominates oceanic emissions
- more mixed over land - biomass burning, human activities, volcanoes
- SO2 released
- this gradually reacts to So42-
sulphur deposition from the atmosphere
- conversion of so2 to so42- is 1%/h
- therefore cycling takes place over several days
- is only direct absorption of gas - dry deposition
- dry Brownian flux
- gravitational setting - wet deposition
- SO42- in rain water
remote ocean S cycle
- assumed closed system (as sea salt ignored)
sea diagram in book - unknown processes occur as sea water passes over mid ocean ridges - precipitate pyrite and S compounds
what happens at mid ocean ridges
- as the plates move apart the exposed hot magma heats the water above
- this causes a circulation of water as water from the sides rush to replace it
- aqueous sulphate is chemically reduced to sulphide in this journey
- sulphur friendly elements are precipitated as sulphides where the water emerges = chimney effect
- the emerging water is rich in hydrogen sulphide (H2S) that bacteria use in chemosynthesis
- this bacteria is then consumed by organisms - small ecosystem forms around the vents
biological S
SRP - sulphate reducing prokaryotes
- gain energy from the electron transfer between organic matter/ hydrogen/ carbon monoxide and electron acceptors