O3 Flashcards

1
Q

What is the function of the O3 layer?

A

The absorption of UV rays.

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2
Q

What have been the consequences of pollution?

A

A large hole over Antarctica, appearing over it every spring, largest in 2006.

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3
Q

What is the stratosphere?

A

Region lying between altitudes where temperature trends reverse, the bottom where it stops decreasing with height and begins to increase.

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4
Q

What are the two concentration measurements used to discuss gases within the atmosphere?

A

Absoloute and relative.

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5
Q

What is absolute concentration?

A

Number of molecules per cubic centimeter of air, or expressed as partial pressure.

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6
Q

What is the Ideal Gas Law?

A

This states that partial pressure id proportional to molar concentration, and thus molecular concentration per unit volume.

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7
Q

What is relative concentration?

A

This measures parts per x value, like amount of CO2 per 1 million molecules of air.

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8
Q

Why is relative concentration used?

A

Where concentrations are so small.

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9
Q

What is the absorption spectrum?

A

This graphically represents relative fraction of light absorbed by a molecule, as a function of wavelength.

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10
Q

What roles does O2 play in the atmosphere?

A

Filters UV light between 120-220nm above the stratosphere, and shorter than 120nm.

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11
Q

What filters UV from 220-290nm?

A

O3.

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12
Q

What UV does O3 not absorb?

A

290-320nm, thus 10-30%(depending on latitude), hits earth surface, this being UV-B.

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13
Q

What does E= hv describe?

A

Energy is related to frequency and the wavelength.

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14
Q

What does this imply?

A

That the lower the energy, the greater the wavelength.

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15
Q

How does photon energy relate to enthalpy change?

A

Proportional

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16
Q

What is an applied example?

A

O2 disassociation into 2 O requires 498.4 kJ/mol enthalpy change

17
Q

How much energy thus is required to dissassociate?

A

240nm, this being the enthalpy of a single O.

18
Q

What type of reaction is this?

A

Photochemical reaction.

19
Q

What happens to a compound in an excited state?

A

Immediate return to ground states by photon emission or heat transfer to free atoms/molecules through collisions.

20
Q

What does this mean for photolytic initiation?

A

Inability to accumulate energy from several photons, thus wavelengths higher than 240nm cannot disassociate.

21
Q

Why does most oxygen exist atomically above the stratosphere?

A

UV-C disassociation of O2, with reformation by collision into O2, however very thin.

22
Q

Why is atomic O more likely to react with O2 in the stratosphere?

A

Because O2 concentration is so large and O concentration is so small, thus forming ozone.

23
Q

Why is little ozone formed at the bottom of the stratosphere?

A

Less O due to less O2 dissociation and more O2 as air density increases approaching the surface.

24
Q

Where does O3 concentration maxmise?

A

Where UVC intensity and O2 is greatest

25
Q

Why is the temperature above/below the stratosphere lower?

A

Heat generated by O + O2 collision.

26
Q

How does UV-C and UV-B react with ozone?

A

Efficient absorption and dissociation into O2 and O, which subsequently reform O3, or O destroys O3 through reacting to two O2.

27
Q

What is the Chapman Cycle?

A

This is the process of continous regeneration of O3 in the stratosphere.

28
Q

Why is the term ‘ozone layer’ a misnomer?

A

The majority of it is NOT O3.

29
Q

How can pollutants then act as catalysts for O3 destruction?

A

Form a compound with O, and O2, then the pollutant-O xompound reacts with O, producing O2 and the standalone compound, further destroying O3.

30
Q

Where does this specific type of reaction occur?

A

Middle and upper stratosphere by free radicals.

31
Q

What is an example of a natural catalytic O3 pollutant?

A

Ntiric oxide, produced when N2O rise from troposphere to stratosphere.

32
Q
A