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Chemistry in the Atmosphere
Chapter 17
Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display.
17.1
The Nitrogen Cycle
Atmospheric Nitrogen Fixation
2NO (g) + O2 (g) 2NO2 (g)
2NO2 (g) + H2O (g) HNO2 (aq) + HNO3 (aq)
Industrial Nitrogen Fixation
N2 (g) + 3H2 (g) 2NH3 (g)
catalyst
N2 (g) + O2 (g) 2NO (g)
electrical
energy
17.1
NH3 + 2O2 HNO3 + H2O
NH3 + HNO3 NH4NO3
CH4 + 2H2O 4H2 + CO2
17.1
The Oxygen Cycle
17.1
hn + N2 2N
hn + N N + e-
hn + O2 O2
+ + e-
e-
p+
+ O O* + e-
O* O + hn
+ N2 N2
* + p+ + e-
+
+
N2
* N2 + hn
+
green and red
blue and violet
O + NO NO2
*
NO2
* NO2 + hn
Glowing tail section of space shuttle
orange
17.2
Chemical Rxs in the Thermosphere
Depletion of Ozone in the Stratosphere
17.3
UV
O2 O + O
< 240 nm
O + O2 + M O3 + M
O3 production
O3 destruction
O3 O + O2
UV
O + O3 2O2
dynamic equilibrium
constant concentration
of O3 in stratosphere
UV
Ozone Layer
Depletion of Ozone in the Stratosphere
Anthropogenic O3 destruction
CFCl3 CFCl2 + Cl
UV
CF2Cl2 CF2Cl + Cl
UV
Cl + O3 ClO + O2
ClO + O Cl + O2
+
O3 + O 2O2
Cl catalyzes the reaction
17.3
17.3
Concentrations of Chlorine Monoxide and
Ozone Versus Latitude
Polar stratospheric clouds
provide a surface for the rx:
Cl2 + hn 2Cl
Spring sunlight
HCl + ClONO2 Cl2 + HNO3
17.3
Cl + O3 ClO + O2
ClO + O Cl + O2
+
O3 + O 2O2
Ozone Depletion (in purple) Over the South Pole
17.3
2H2S (g) + 3O2 (g) 2SO2 (g) + 2H2O (g)
SO2 (g) + OH (g) HOSO2 (g)
SO3 (g) + H2O (g) H2SO4 (g)
H2SO4 aerosols have a local cooling effect on the atmosphere.
17.4
HOSO2 (g) + O2 (g) HO2 (g) + SO3 (g)
The trapping of heat near Earth’s surface by gases in the
atmosphere is the greenhouse effect.
17.5
H2O + hn H2O*
CO2 + hn CO2
*
Why don’t N2 and O2 contribute to
the greenhouse effect ?
N2 and O2 cannot
absorb IR radiation.
3 vibration
modes of
H2O
2 of the vibration modes of CO2
17.5
17.5
The Carbon Cycle
17.5
The Yearly Variation in the CO2 Concentration
At Mauna Loa, Hawaii
17.5
The Temperature Rise on Earth’s
Surface from 1880 to 1996
Mean
precipitation
pH in 1994
SO2 (g) + OH (g) HOSO2 (g)
SO3 (g) + H2O (g) H2SO4 (g)
HOSO2 (g) + O2 (g) HO2 (g) + SO3 (g)
Acid Rain
17.6
CaCO3 (s) + H2SO4 (aq) CaSO4 (s) + H2O (l) + CO2 (g)
2CaCO3 (s) + 2SO2 (g) + O2 (g) 2CaSO4 (s) + CO2 (g)
17.6
The Effect of Acid Rain on the Marble Statue of George
Washington (New York, City). Photos Taken in 1944 and 1994
17.6
17.7
Photochemical smog is formed by the reactions of
automobile exhaust in the presence of sunlight.
Primary pollutants: NO, CO and unburned hydrocarbons
Secondary pollutants: NO2 and O3
N2 (g) + O2 (g) 2NO (g)
2NO (g) + O2 (g) 2NO2 (g)
NO2 (g) + hn NO (g) + O (g)
O (g) + O2 (g) + M O3 (g) + M
17.7
Typical Variations with Time in the Concentration of
Air Pollutants on a Smoggy Day
17.8
U
238
92
4.51 x 109 yr
Th
234
90
24.1 days
Pa
234
91
1.17 min
U
234
92
2.47 x 105 yr
Th
230
90
7.5 x 104 yr
Ra
226
88
1.6 x 103 yr
Rn
222
86
3.82 d
Atmospheric Chemistry Cycles & Pollution

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Atmospheric Chemistry Cycles & Pollution

  • 1. Chemistry in the Atmosphere Chapter 17 Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display.
  • 3. Atmospheric Nitrogen Fixation 2NO (g) + O2 (g) 2NO2 (g) 2NO2 (g) + H2O (g) HNO2 (aq) + HNO3 (aq) Industrial Nitrogen Fixation N2 (g) + 3H2 (g) 2NH3 (g) catalyst N2 (g) + O2 (g) 2NO (g) electrical energy 17.1 NH3 + 2O2 HNO3 + H2O NH3 + HNO3 NH4NO3 CH4 + 2H2O 4H2 + CO2
  • 5. 17.1 hn + N2 2N hn + N N + e- hn + O2 O2 + + e-
  • 6. e- p+ + O O* + e- O* O + hn + N2 N2 * + p+ + e- + + N2 * N2 + hn + green and red blue and violet O + NO NO2 * NO2 * NO2 + hn Glowing tail section of space shuttle orange 17.2 Chemical Rxs in the Thermosphere
  • 7. Depletion of Ozone in the Stratosphere 17.3 UV O2 O + O < 240 nm O + O2 + M O3 + M O3 production O3 destruction O3 O + O2 UV O + O3 2O2 dynamic equilibrium constant concentration of O3 in stratosphere UV Ozone Layer
  • 8. Depletion of Ozone in the Stratosphere Anthropogenic O3 destruction CFCl3 CFCl2 + Cl UV CF2Cl2 CF2Cl + Cl UV Cl + O3 ClO + O2 ClO + O Cl + O2 + O3 + O 2O2 Cl catalyzes the reaction 17.3
  • 9. 17.3 Concentrations of Chlorine Monoxide and Ozone Versus Latitude
  • 10. Polar stratospheric clouds provide a surface for the rx: Cl2 + hn 2Cl Spring sunlight HCl + ClONO2 Cl2 + HNO3 17.3 Cl + O3 ClO + O2 ClO + O Cl + O2 + O3 + O 2O2
  • 11. Ozone Depletion (in purple) Over the South Pole 17.3
  • 12. 2H2S (g) + 3O2 (g) 2SO2 (g) + 2H2O (g) SO2 (g) + OH (g) HOSO2 (g) SO3 (g) + H2O (g) H2SO4 (g) H2SO4 aerosols have a local cooling effect on the atmosphere. 17.4 HOSO2 (g) + O2 (g) HO2 (g) + SO3 (g)
  • 13. The trapping of heat near Earth’s surface by gases in the atmosphere is the greenhouse effect. 17.5 H2O + hn H2O* CO2 + hn CO2 *
  • 14. Why don’t N2 and O2 contribute to the greenhouse effect ? N2 and O2 cannot absorb IR radiation. 3 vibration modes of H2O 2 of the vibration modes of CO2 17.5
  • 16. 17.5 The Yearly Variation in the CO2 Concentration At Mauna Loa, Hawaii
  • 17. 17.5 The Temperature Rise on Earth’s Surface from 1880 to 1996
  • 18. Mean precipitation pH in 1994 SO2 (g) + OH (g) HOSO2 (g) SO3 (g) + H2O (g) H2SO4 (g) HOSO2 (g) + O2 (g) HO2 (g) + SO3 (g) Acid Rain 17.6
  • 19. CaCO3 (s) + H2SO4 (aq) CaSO4 (s) + H2O (l) + CO2 (g) 2CaCO3 (s) + 2SO2 (g) + O2 (g) 2CaSO4 (s) + CO2 (g) 17.6 The Effect of Acid Rain on the Marble Statue of George Washington (New York, City). Photos Taken in 1944 and 1994
  • 20. 17.6
  • 21. 17.7 Photochemical smog is formed by the reactions of automobile exhaust in the presence of sunlight. Primary pollutants: NO, CO and unburned hydrocarbons Secondary pollutants: NO2 and O3 N2 (g) + O2 (g) 2NO (g) 2NO (g) + O2 (g) 2NO2 (g) NO2 (g) + hn NO (g) + O (g) O (g) + O2 (g) + M O3 (g) + M
  • 22. 17.7 Typical Variations with Time in the Concentration of Air Pollutants on a Smoggy Day
  • 23. 17.8 U 238 92 4.51 x 109 yr Th 234 90 24.1 days Pa 234 91 1.17 min U 234 92 2.47 x 105 yr Th 230 90 7.5 x 104 yr Ra 226 88 1.6 x 103 yr Rn 222 86 3.82 d