Ozone is the 3 oxygen molecule in the stratosphere that absorbs UV radiation and protects the Earth’s surface from the mutating effects of the radiation
Causes of Ozone Depletion
Chlorine or Bromine containing compounds, UV radiation releases Cl or Br ions, Cl and Br ions destroy Ozone
As algae evolved in oceans, they released O2 into the atmosphere (Gia Hypothesis)
How Ozone Depletion Takes Place
Rowland and Molina (1974), Chlorine atoms are removed from CFCl3 by UV light, CFCl3 + UV -> CFCl2 + Cl, Cl + O3 -> ClO + O2, 2ClO + UV -> 2Cl + O2
Each chlorine atom can convert up to 100,000 O3 molecules to O2 before it finally combines with hydrogen to make HCl and it rains down
Ozone depletion in the 80’s should cause 12 million people to develop skin issues
Less Ozone results in more UV radiation (mutagen and carcinogen) reaching southern oceans
How Does Ozone Absorb UV Light?
Man-made chemicals known as Halons (Chlorine and Bromine) containing chemicals, Chlorofluorocarbons (CFC’s) containing Chlorine (Cl) used in aerosol cans, cooling agents in air conditioners and refrigerators (Freon)
How Ozone Depletion Takes Place
Cl and Br ions are not degraded by solar radiation, each ion destroys many O3 molecules
How Is Ozone Formed?
O2 + UV -> O + O, O + O2 -> O3
Chlorine acts as a catalyst in the reaction because it helps it, but is not used up in the reaction
The thinning 15-20% of the ozone layer over Antarctica is known as the Ozone Hole
Ecological Effects of Ozone Depletion
Increased high energy UV radiation reaching the earth’s surface, Adverse effects on Larval development
Effects of Acid Deposition
Acid Lakes
Physiological Tolerance/Abiotic factors
Acid Lake “Sweetening”
1987 - Montreal Protocol
Sources of Pollutants
SO2 + H2O ---> H2SO4 (Sulfuric acid)
NO2 + H2O ---> HNO3 (Nitric acid)
Controlling Acid Deposition
Coal Burning is the main cause
Cap and Trade economic approach as part of 1990 Clean Air law
Scrubbers and coal washing to remove sulfur (clean coal technologies)
Coal is being phased out by natural gas (no sulfur) and renewables
Ecological Effects of Ozone Depletion
Increased high energy UV radiation reaching the earth’s surface
Adverse effects on Larval development
Acidic soils cause minerals to be leached (washed out) from the soil
CFC production has fallen 77% between 1988 and 1995
Bioaccumulation
1978 - U.S. banned use of CFC’s
Chlorine levels have already begun to decrease and should be back to safe levels by 2045
Montreal Protocol
150 nations signed agreement
Agreed to cut emissions by 50% between 1989 and 2000
Larvae (baby ocean creatures) will decline
Measuring Acidity
pH scale (log scale)
Normal rainwater (pH of 5-6)
Acid rain has a pH between 3-4
Terrestrial Organisms
External damage to bark & leaves
Little resistance to pests
Lower rates of photosynthesis
Acid Rain is a Regional Issue
Effects of Ozone Depletion
Ozone depletion in the 80s should cause 12 million people to develop skin cancer in their lifetime
Glaucoma (blindness) increases
Results in a Ca2+ deficient food chain (thinning eggshells of local birds)
Acidic soils cause toxic Heavy metals ionize in soil and are taken up by plants (metal toxicity)
Gasoline used in personal automobiles does not release SOx
Acid deposition
The process by which acid compounds (H2SO4 or HNO3) condense out of the atmosphere in the form of rain, snow or fog
Impact of acidic snow melt in a shallow fresh water lake in the spring
Changes abiotic factor, physiological impact on base (aquatic insects), impact on Osprey populations in the adjacent forest, economic impact
Acid deposition impacts aquatic (fresh) water ecosystems
Alters the abiotic conditions of the system
The Clean Air Act of 1990 focused on controlling Sulfur and Nitrogen emissions by regulating stationary sources of these pollutants
Lake with granite bedrock is more prone to acidification than one with limestone bedrock
Reason
Clean air technology industry required to install when burning fossil fuels
Acid deposition weakens trees in the forest
Forests are a natural resource that we depend on economically