Tropospheric ozone is produced when UV light interacts with gas particles near the earth's surface. But most UV light is blocked by the stratospheric ozone layer. How is it possible to get significant levels of low-altitude ozone? Select one: O a. Tropospheric ozone is produced by reacting O2 with photons with wavelength < 240 nm. Most of the photons are already blocked by the ozone layer, but what little light gets through is able to start a catalytic chain where Og molecules attack 02 and make more O3. O b. Tropospheric ozone is produced by reacting NO, with UV light with wavelength < 424 nm to produce O* radicals, which can then attack oxygen to make ozone. This wavelength is not within ozone's absorption profile and penetrates significantly to the surface. O . The sun's peak output is at 635 nm. Enough of this color of light reaches the surface to do multiphoton reactions with tropospheric O2 to create Og. o d. The sun's peak output is at 635 nm. Enough of this color of light reaches the surface to do multiphoton reactions with tropospheric NO2 to create O3.
Tropospheric ozone is produced when UV light interacts with gas particles near the earth's surface. But most UV light is blocked by the stratospheric ozone layer. How is it possible to get significant levels of low-altitude ozone? Select one: O a. Tropospheric ozone is produced by reacting O2 with photons with wavelength < 240 nm. Most of the photons are already blocked by the ozone layer, but what little light gets through is able to start a catalytic chain where Og molecules attack 02 and make more O3. O b. Tropospheric ozone is produced by reacting NO, with UV light with wavelength < 424 nm to produce O* radicals, which can then attack oxygen to make ozone. This wavelength is not within ozone's absorption profile and penetrates significantly to the surface. O . The sun's peak output is at 635 nm. Enough of this color of light reaches the surface to do multiphoton reactions with tropospheric O2 to create Og. o d. The sun's peak output is at 635 nm. Enough of this color of light reaches the surface to do multiphoton reactions with tropospheric NO2 to create O3.
Chemistry
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ISBN:9781305957404
Author:Steven S. Zumdahl, Susan A. Zumdahl, Donald J. DeCoste
Publisher:Steven S. Zumdahl, Susan A. Zumdahl, Donald J. DeCoste
Chapter1: Chemical Foundations
Section: Chapter Questions
Problem 1RQ: Define and explain the differences between the following terms. a. law and theory b. theory and...
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Transcribed Image Text:Tropospheric ozone is produced when UV light interacts with gas particles near the earth's surface. But most UV light is blocked by the stratospheric ozone layer. How is it possible to get significant levels of low-altitude
ozone?
Select one:
O a. Tropospheric ozone is produced by reacting 02 with photons with wavelength < 240 nm. Most of the photons are already blocked by the ozone layer, but what little light gets through is able to start a catalytic chain
where Og molecules attack 02 and make more O3.
O b. Tropospheric ozone is produced by reacting NO2 with UV light with wavelength < 424 nm to produce 0* radicals, which can then attack oxygen to make ozone. This wavelength is not within ozone's absorption profile
and penetrates significantly to the surface.
O c. The sun's peak output is at 635 nm. Enough of this color of light reaches the surface to do multiphoton reactions with tropospheric O2 to create 03.
O d. The sun's peak output is at 635 nm. Enough of this color of light reaches the surface to do multiphoton reactions with tropospheric NO2 to create 03.
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