Evolution of Oxygen in the Atmosphere - PowerPoint PPT Presentation

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Evolution of Oxygen in the Atmosphere

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Title: What about the Oceans and the Atmosphere? Author: Whitney King Last modified by: Whitney King Created Date: 2/5/1998 2:55:23 PM Document presentation format – PowerPoint PPT presentation

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Title: Evolution of Oxygen in the Atmosphere


1
Evolution of Oxygen in the Atmosphere
  • Early reactions driven by high energy sunlight
  • H2O --- hn lt 240 nm ---gt H OH
  • CO2 --- hn lt 240 nm ---gt CO O
  • Recombination reactions
  • 2OH -----gt H2O O
  • 2O -- M ---gt O2
  • 2H -- M --gt H2 (H2 can be lost to
    space)
  • 2H2 O2 -----gt 2H2O
  • This was a minor process!

2
To produce large amounts of O2 we need LIFE
Sunlight
132 O2
BUG
  • What regulates the global Oxygen concentration?

3
Global scale oxygen feedback loop
Atmosphere
Continental Crust
O2
Ocean
4
Global scale oxygen feedback loop
Atmosphere
Continental Crust
O2
Ocean
Deep, Cold, O2-rich Water
5
Global scale oxygen feedback loop
Atmosphere
Continental Crust
O2
Ocean
Deep, Cold, O2-rich Water
Respiration
6
Feedback on Atmospheric O2
  • Correct Atmospheric Oxygen
  • Photosynthesis Respiration
  • Too Little Atmospheric Oxygen
  • Photosynthesis gtgt Respiration
  • Too Much Atmospheric Oxygen
  • Photosynthesis ltlt Respiration

7
How fast is O2 cycling in the environment?
  • The rate of photosynthesis respiration
    5 x 1015 mol/yr.
  • The atmosphere is 20 oxygen, or 3.8 x 1019
    mol.

8
How fast is O2 cycling in the environment?
  • The rate of photosynthesis respiration
    5 x 1015 mol/yr.
  • The atmosphere is 20 oxygen, or 3.8 x 1019 mol.
  • Residence time for oxygen 7600 years
  • What does this mean?? Oxygen is well mixed in
    the atmosphere!

9
Nitrogen in the atmosphere
  • Nitrogen was outgassed early in Earth formation
    and constitutes 80 of the atmosphere. (1.4 x
    1020 moles)
  • Two major sinks
  • N2(g) O2(g) ----- gtT ----gt 2 NO(g)
  • N2(g) 3H2(g) ---- gtT, catalyst ---gt 2 NH3(g)
  • Total flux 4.6 x 1012 moles/year
  • Residence time 3 x 107 years

10
Source http//www.esrl.noaa.gov/gmd/ccgg/trends/
11
CO2
  • Mass in the atmosphere 700 Gt
  • Annual flux to the atmosphere is about 150 Gt
  • Residence time 5 years
  • Does this make sense with observed CO2?

12
  • Major Constituents of the Atmosphere (atm.)
  • N2 0.781
  • O2 0.209
  • Ar 0.0093
  • CO2 0.00035
  • What about WATER?
  • Variable concentration 0 - 0.05 atm

13
Temperature --gt (oC)
  • p(H2O) p(saturation)(RH)/100
  • Average amount of water 7 x 1014 mol.
  • average flux 2.5 x 1016 mol/yr
  • residence time 10 days
  • Water is poorly mixed!

14
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