history of ozone
DESCRIPTION
History of Ozone. Discovered in 1840 by Christian Friedrich Schönbein . In the 1920’s Gordon Dobson made the first O 3 column measurements. 1 DU = 1x10 -3 m thick layer of pure ozone at standard temperature and pressure. - PowerPoint PPT PresentationTRANSCRIPT
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History of Ozone• Discovered in 1840 by Christian Friedrich
Schönbein .
• In the 1920’s Gordon Dobson made the first O3 column measurements.
1 DU = 1x10-3m thick layer of pure ozone at standard temperature and pressure.
• In 1930 Sydney Chapman proposed a mechanism for ozone in the stratosphere.
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The Stratosphere
from: http://okfirst.ocs.ou.edu/train/meteorology/graphics/VertTP.gif
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Ozone in the Stratosphere
• Shields the surface of the Earth from harmful UV radiation.
From: http://www.atmosphere.mpg.de/enid/208.html
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Ozone in the Stratosphere
From: Jacob
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The Chapman Mechanism
2k
3
2
320nmhJ
3
3k
2
240nmhJ
2
O2OO 4.
OOhO 3.
MOOO 2.
OO hO 1.
4
3O
2
2O
M
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The Chapman Mechanism
From: Jacob
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The Chapman Mechanism
O2 O O3(1)
slow
(4)slow
(2)fast(3)
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The Ox Family
• Reaction 1: Production of Ox
• Reaction 4: Loss of Ox
OO hO 240nmh2
23 O2OO
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The Chapman Mechanism
]O][O[k]O[J-M]][O][O[k]O[
]O][O[k-M]][O][O[k]O[J]O[J2O][
343O223
34223O2O
3
32
dt
ddt
d
M]][[Ok
J
][O
[O]
M]][O][O[k]O[J
22
O
3
223O
3
3
Assuming steady-state for either O or O3:
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The Chapman Mechanism
1M]][[Ok
J
][O
[O]
22
O
3
3
Everywhere in the stratosphere
]O[][O][OO][ x33
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O3 in the Stratosphere
O][2k
]O[J2][O
0]O][O[2k-]O[J2]O[
4
2O3
342Ox
2
2
dt
d
Derive an expression for the steady-stateof O3 in the stratosphere:
Find steady-state for O
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O3 in the Stratosphere
]O[kJ
M][kJ]O[
]O[kJ
M]][O[k]O[J]O[
M]][[Ok
][OJO][
M]][O][O[k]O[J
2
2
1
4O
2O3
34O
222O3
22
3O
223O
3
2
3
2
3
3
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O3 in the Stratosphere
From: Jacob
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Catalytic Ozone Destruction
223
2
23
OOOO :net
OXOXO
OXOO X
X is a catalyst and may be:X = H, OH, NO, Cl, or Br
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The HOx Family in the Stratosphere
• Source: Water vapor
• Source: methane, H2
z
T
cold trap, T≈190KPH2O≈2.5x10-4 torr at 75mbar (3.5ppmv)
tropopause
stratosphere
troposphere
ppmv5.0 OHO2
1H
1.7ppmv OH2COO2 CH
222
2224
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The HOx Family in the Stratosphere
OH2OHD)O(
D)O(P)O(hO
OD)O(hO
21
13180nm2
21320nm
3
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Catalytic Ozone Destruction (HOx)
223
2
23
OOOO :net
OHOOH
OOHO H
223
22
223
OOOO :net
OOHOHO
OHOO OH
2
22
22
2
OOO :net
OOHOHO
MHOMOH
OHO OH
233
2232
223
3OOO :net
OOOHOHO
OHOO OH
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Catalytic Ozone Destruction (HOx)
223
2
23
OOOO :net
OXOXO
OXOO X
233
223
23
3OOO :net
OOXOXO
OXOO X
Cycle I Cycle II
•Cycle I: important at higher z and only during the day
•Cycle II: important at lower z and also at night
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Catalytic Ozone Destruction (HOx)
• Termination occurs when:
• H2O and HNO3 may mix back to the troposphere and be removed.
• However:
32
222
HNONO OH
OOHHO OH
23
12
NOOHhHNO
OH2 D)O(OH
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The NOx Family in the Stratosphere
• Source: N2O
• Source: Direct emissions of NO to the stratosphere
2NOD)O( ON
OND)O( ON
ND)O(h ON
12
221
2
21
2
only about 5%
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Catalytic Ozone Destruction (NOx)
223
22
223
OOOO :net
ONOONO
ONOO NO
23
23
2332
223
3O2O :net
ONOhNO
ONOONO
ONOO NO
Active in the daytime-reaction scheme should look familiar?!
Active in the day or night-a little different than cycle II
To complete the catalyticcycle in the daytime
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Null Cycles
OOhO :net
ONOhNO
ONOO NO
23
2
223
Ox Ox
‘Null cycles’ do not lead to the formation or destruction of O3.
-ties up reactive species (in this case, NOx) reducing their ability to destroy ozone.
OOhO :net
ONOhNO
OHNONOHO
OHOO OH
23
2
22
223
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Catalytic Ozone Destruction
• Cycles may be ‘short-circuited’ through competing reactions:
ONOhNO
ONOONO
2
22
Leads to O3 destruction
Leads to null cycle
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Catalytic Ozone Destruction (NOx)
• Termination of catalytic cycles occur when:
• However:
MONMNO NO
MHNOMNO OH
5223
32
3(s)(s)252
3252
23
2HNOOHON
NONOhON
NOOHhHNO
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Reservoirs• For NOx:
– HNO3, and N2O5 are reservoirs of NOx
– NOy = NOx + reservoirs
– NOx/NOy gives us an idea of how effective NOx is at destroying ozone.
• For HOx:
– H2O and HNO3 are reservoirs of HOx
– HOy = HOx + reservoirs
– HOx/HOy gives us an idea of how effective HOx is at destroying ozone.
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Mixed Cycles• The HOx and NOx cycles are coupled:
323
23
32
22
NOOHOHHNO
NOOHhHNO
MHNOMNOOH
OHNONOHO
An increase of stratospheric HOx causes a decreasein the effectiveness of NOx towards destroying O3.
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Transport in the Stratosphere
From: http://www-as.harvard.edu/people/faculty/djj/book/powerpoints/
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Global Ozone Distribution
From: http:woudc.ec.gc.ca/e/ozone/Curr_allmap_g.htm
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Global Ozone Distribution
From: http:woudc.ec.gc.ca/e/ozone/Curr_allmap_g.htm
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Tropospheric NOx and HOx
versusStratospheric NOx and HOx
• In the troposphere (ozone production):
• In the stratosphere (ozone destruction):
ONOhNO
NOOONO
OHNONOHO
HCOCOOH
2
223
22
2
HOx
NOx
22
223
232
223
ONOONO
NOOONO
O2OHOHO
OHOOOH
HOx
NOx
The troposphere has extremely low atomic oxygen concentrations.
The stratosphere has high ozone and atomic oxygen concentrations relative to the troposphere.