Chlorofluoromethanes (CFMs) are carbon compounds of chlorine and fluorine and are also known as Freons. Examples are Freon-11 (CFCl 3 ) and Freon-12 ( CF 2 Cl 2 ) , which were used as aerosol propellants. Freons have also been used in refrigeration and air-conditioning systems. In 1995 Mario Molina, F. Sherwood Rowland, and Paul Crutzen were awarded the Nobel Prize mainly for demonstrating how these and other CFMs contribute to the “ozone hole” that develops at the end of the Antarctic winter. In other pares of the world, reactions such as those shown below occur in the upper atmosphere where ozone protects the earths inhabitants from harmful ultraviolet radiation. In the stratosphere CFMs absorb high-energy radiation from the sun and split off chlorine atoms that hasten the decomposition of ozone, O 3 . Possible reactions are O 3 ( g ) + Cl ( g ) → O 2 ( g ) + ClO ( g ) Δ H ° = − 126 kJ ClO ( g ) + O ( g ) → Cl ( g ) + O 2 ( g ) Δ H ° = − 268 kJ O 3 ( g ) + O ( g ) → 2 O 2 ( g ) Δ H ° = ? The O atoms in the second equation come from the breaking apart of O 2 molecules caused by ultraviolet radiation from the sun. Use the first two equations to calculate the value of Δ H ° (in kilojoules) for the last equation, the net reaction for the removal of O 3 from the atmosphere.
Chlorofluoromethanes (CFMs) are carbon compounds of chlorine and fluorine and are also known as Freons. Examples are Freon-11 (CFCl 3 ) and Freon-12 ( CF 2 Cl 2 ) , which were used as aerosol propellants. Freons have also been used in refrigeration and air-conditioning systems. In 1995 Mario Molina, F. Sherwood Rowland, and Paul Crutzen were awarded the Nobel Prize mainly for demonstrating how these and other CFMs contribute to the “ozone hole” that develops at the end of the Antarctic winter. In other pares of the world, reactions such as those shown below occur in the upper atmosphere where ozone protects the earths inhabitants from harmful ultraviolet radiation. In the stratosphere CFMs absorb high-energy radiation from the sun and split off chlorine atoms that hasten the decomposition of ozone, O 3 . Possible reactions are O 3 ( g ) + Cl ( g ) → O 2 ( g ) + ClO ( g ) Δ H ° = − 126 kJ ClO ( g ) + O ( g ) → Cl ( g ) + O 2 ( g ) Δ H ° = − 268 kJ O 3 ( g ) + O ( g ) → 2 O 2 ( g ) Δ H ° = ? The O atoms in the second equation come from the breaking apart of O 2 molecules caused by ultraviolet radiation from the sun. Use the first two equations to calculate the value of Δ H ° (in kilojoules) for the last equation, the net reaction for the removal of O 3 from the atmosphere.
Chlorofluoromethanes (CFMs) are carbon compounds of chlorine and fluorine and are also known as Freons. Examples are Freon-11
(CFCl
3
)
and Freon-12
(
CF
2
Cl
2
)
, which were used as aerosol propellants. Freons have also been used in refrigeration and air-conditioning systems. In 1995 Mario Molina, F. Sherwood Rowland, and Paul Crutzen were awarded the Nobel Prize mainly for demonstrating how these and other CFMs contribute to the “ozone hole” that develops at the end of the Antarctic winter. In other pares of the world, reactions such as those shown below occur in the upper atmosphere where ozone protects the earths inhabitants from harmful ultraviolet radiation. In the stratosphere CFMs absorb high-energy radiation from the sun and split off chlorine atoms that hasten the decomposition of ozone,
O
3
. Possible reactions are
O
3
(
g
)
+
Cl
(
g
)
→
O
2
(
g
)
+
ClO
(
g
)
Δ
H
°
=
−
126
kJ
ClO
(
g
)
+
O
(
g
)
→
Cl
(
g
)
+
O
2
(
g
)
Δ
H
°
=
−
268
kJ
O
3
(
g
)
+
O
(
g
)
→
2
O
2
(
g
)
Δ
H
°
=
?
The O atoms in the second equation come from the breaking apart of
O
2
molecules caused by ultraviolet radiation from the sun. Use the first two equations to calculate the value of
Δ
H
°
(in kilojoules) for the last equation, the net reaction for the removal of
O
3
from the atmosphere.
One of the components of smog is ozone,O3, a colorless, toxic gas. It is a very strong oxidizing agent and causes respiratory illnesses. Ozone is produced in the lower atmosphere due to the catalytic effect of nitric oxide, NO, a byproduct of the combustion process in car engines.
However, in the upper atmosphere ozone is a very useful gas, because it absorbs ultraviolet radiation and protects the earth from this high energy, damaging radiation. It is referred to as the ozone layer. This ozone layer is depleted by the catalytic action of gases like Freon, which are commonly used in refrigerators and air conditioners. Chemically these gases are unreactive and rise into the upper atmosphere. The high energy radiation in the upper atmosphere produces very reactive chlorine atoms according to the reaction below:
CCl2F2(g) → CClF2(g) + Cl(g) (catalyzed by uv radiation)The following questions refer to the depletion of ozone in the upper atmosphere according to the mechanism shown below:…
Use the bond enthaplies in this table to determine triangleH for the formafion of hydrazine, N2H4, according to this equation.
Write the law for this reaction and explain how it is determined
SO2CL2 ->SO2 + CL2
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