Ozone Flashcards

1
Q

Where does Ozone get it’s name?

A

From Greek derivative “to smell” - has distinct smell

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2
Q

ozone discovery timeline

A
  • introduced to science in 1840 by Dr. C. Shoenbein
  • 1845: ozone linked to oxygen
  • 1863: ozone identified as O3
  • 1872: existence in atmosphere confirmed
  • 1870s to today: systematic observations
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3
Q

How is ozone formed?

A

O2 + sunlight —> O + O
O + O2 —> O3

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4
Q

What are the natural destructions of ozone?

A
  • via UV radiation: O3 + UV –> O2 + O
  • via interaction with chlorine (CL):
    CL + O3 —> CLO + O2
    CLO + O —> CL + O2
    CLO = chlorine monoxide
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5
Q

Where is ozone primarily found?

A

stratosphere at 1 part per thousand

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6
Q

How and when is ozone created in the troposphere?

A

-can be created in the troposphere when hydrocarbons react with nitrogen oxides
- not good, leads to bas air quality
- O3 can aggravate asthma, etc.

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7
Q

Stratospheric Ozone

A
  • good thing
  • absorbs UV radiation
  • ozone layer
  • being depleted
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8
Q

What is the ozone layer?

A
  • high concentration of ozone in the stratosphere
  • is 0.00005% total atmospheric volume
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9
Q

Chlorofluorocarbon (CFCs) - composition, created for what and when, what was used prior

A
  • single carbon, two chlorines, two fluorines
  • created in 1928 as non-toxic, non-flammable refridgerant, trademarked as Freon
  • prior we used ammonia, sulfur dioxide, and methyl chloride
  • worldwide consumption in 1988 was at over 1 billion kgs
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10
Q

Why are CFCs a problem?

A
  1. CFCs dissolve in the sunlight
  2. A single Cl molecule floats around until it attacks an O3 molecule, pulling an O off it
  3. Chlorine atom and oxygen atom join to form chlorine monoxide
  4. A free oxygen pulls the O off the chlorine monoxide
  5. Once free, the chlorine atom is off to attack another ozone molecule
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11
Q

For each 1% decrease in ozone, UV radiation increases ___%

A

2%

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12
Q

Where is the greatest reduction in stratospheric ozone and why?

A

Antarctica due to combo of cold temperatures, formation of polar stratospheric clouds, and the Antarctic vortex

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13
Q

Montreal Protocol (1986)

A

international treaty to reduce CFC emissions and other ozone-depleting chemicals

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14
Q

What is the timeline of the Montreal Protocol

A

-1974: chemists Rowland and Molina presented evidence suggesting that breakdown of CFCs could destroy ozone
- initially criticized, but were invited to testify before Congress
- led to substantial funding to study problem
- 1976: National Academy of Sciences released report confirming hypothesis - US govt declared CFCs only be used in important things
- 1985: studies by British Antarctic Survey found “ozone hole”
- treaty has been revised about 7 times
- 1992: ozone hole began in northern hemisphere - pushed president Bush to accelerate US implementation of treaty
- replaced CFCs with HCFCs, which also deplete O3, so plan is for them to be phased globally by 2040

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15
Q

What is the Ozone Hole?

A
  • the reduction in the amount of ozone of stratospheric ozone every year over Antarctica in its springtime (and now Greenland)
  • any area under 220 Dobson units
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16
Q

Why is O3 reduction largely in Arctic/Antarctic regions?

A
  • Antarctica winters have very strong circumpolar winds that isolate the atmosphere over Antarctica
  • stratospheric clouds form, chlorine atoms attach themselves
  • when sun returns to Antarctica in Spring (Sept), chlorine atoms are released, setting up ozone-destroying chain reaction that lasts 5-6 weeks, until ozone from lower latitudes can mix back into Antarctic atmosphere