(M2) Lecture 10 - Acidification Flashcards

1
Q

Definition of acid deposition: wet (eg acid rain) and dry (eg particulates)

A

Acid deposition: The settling, or depositions, of acidic or acidic forming pollutants from the atmosphere onto Earth’s surface.

Includes:
- Acidic precipitation: acidic rain, snow, sleet, hail
- Acidic fog
- Acidic gases
- Acidic dry particles

*pH <5.6

Wet Deposition: Acids removed from the atmosphere in the form of water (rain, snow, sleet, hail)

Dry Deposition: Acids removed from the atmosphere in the form of particulates or gases (=no water). Often in the form of fly ash, sulphates, nitrates, and SO2 and NOx gas.

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2
Q

Emissions that cause acidifications: SO2 and NOx (terrestrial and freshwater); CO2 (ocean/marine)

A

Sulfur dioxide (SO2)
- In Canada, largest source now is the oil and gas industry
- In the US, largest source is electricity generation

Nitrogen oxides (NOx)
- In Canada, largest source now is the oil and gas industry
- In Canada, NOx emissions have not decreased as much as SO2 has
- In the US it is still transportation
- Other sources: electricity generation, off-road vehicles

Carbon dioxide (CO2)
- CO2 from the atmosphere to the ocean
- 1/4 of CO2 released by burning coal, oil and gas dissolves into ocean; since the beginning of the industrial era
- In the pas 200 years, ocean water has become 30% more acidic
- Increase in emissions, mostly from oil and gas, and transport

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3
Q

How pollutants transform into acid depositions (know all the steps of the chemical rxns)

A

The pollutants are transformed into acid particles that can be transported long distances.

2SO2 + O2 —> 2SO3
SO3 + H2O —> H2SO4

3NO2 + H2O —> 2HNO3 + NO

CO2 + H2O <—> H2CO3
H2CO3 <—> HCO3- + H+
HCO3- <—> CO32- + H+

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4
Q

Acidification on landscapes: causes and impacts on soils, forests, streams lakes - including effects on organisms

A

Damages to soil
- depletes calcium and other base cations
- mobilizes aluminum, heavy metals from soil to water; toxic
- accumulate sulfur, nitrogen in soils; can lead to eutrophication

Damages to forests
- direct effect: leaches calcium out of needles; lose calcium in cell membranes, more susceptible to cold and freezing
- indirect effect: alters soil chemistry; even less calcium to uptake, more toxic aluminum

Damages to steams and lakes
- increased leaching of aluminum into surface waters as runoff from soils
- if pH too low, can be lethal for fish and aquatic organisms
- combined with low pH, can disrupt osmotic balance in fish, eventually leading to heart attacks
- zooplankton: dissolution of the calcium shells that prevent them from growing strong shells

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5
Q

Acidification of oceans: cause and impacts = including effects on organisms

A
  • Chemical changes in the ocean as a result of CO2 emissions in the atmosphere
  • 1/4 of CO2 released by burning coal, oil and gas doesn’t stay in the air, but dissolves into the ocean
  • pH of our oceans is dropping
  • many organisms with calcium carbonate shell; if pH of the water changes the marine water starts to take calcium carbonate from shell
  • coral bleaching = when the pH drops of if the temp changes, coral will expel its food source and lose colour
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6
Q

Important legislation dealing with acid deposition in Canada

A

1985 Eastern Canada Acid Rain Program:
- Cap SO2 emissions in 7 easternmost provinces
- Establish monitoring
- Updated in 2000 with additional national cap

1991 Canada-United States Air Quality Agreement:
- Cut SO2 and NOx emissions
- Increase monitoring

Canada-Wide Acid Rain Strategy Post-2000
- Signed in 1998
- Continued reductions in SO2 emissions
- More monitoring
- Regulate reports to the public
- Prevent clean/undamaged areas from being degraded

2004 Acid Rain Science Assessment
- Need to reduce emissions even further
- Need to address acidification in the West and North

*Effect of legislation overtime: things are slowly getting better. Regulating emissions are having a positive effect. Reduction in acidic deposition and how pH is being impacted for fresh water.

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7
Q

Definitions: Chemical and biological recovery of ecosystems

A

Chemical Recovery: decrease in damaging chemical (e.g., sulfate, nitrate, and aluminum) concentrations in soils and waters. If the decrease is sufficient, will lead to increase in pH.

Biological Recovery: multi-step return, and/or increase in health of organisms (animals and vegetation) in previously acidified ecosystems (aquatic or terrestrial).

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8
Q

Is Chemical Recovery Occurring?

A

Yes, rate dependent on the resistance and resilience of the ecosystem to acid precipitation; it’s mostly about the amount of calcium naturally found in soils and surface waters
- Lots of Calcium = more resistant and resilient
- Low Calcium = less resistant and resilient

The potential of soils and bedrock to reduce the acidity of atmospheric deposition depends on composition of bedrock. Calcium carbonate bedrock more resistant to acidification. Soils:
- further acidification is not occurring
- aluminum levels are decreasing
- pH is increased

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9
Q

Is Biological Recovery Occurring?

A

Probably, but slowly. Data is still limited.
- quicker for short lived species
- follows chemical recovery
- can take 10+ yrs for zooplankton to recover, 10-20+ for fish populations, and >20 for trees
- given the times, plus the stresses of climate change… it is hard to tell if organisms are rebounding and ecosystem fxn returning

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10
Q

Phytoplankton, Zooplankton, and Fish biomass in Lake 302S

A

Phytoplankton
- primary producers, base of food chain
- during lake recover, the biomass increased initially then a steep decrease back to normal levels
- big shift in species type of phytoplankton, still an overall decrease in biomass

Zooplankton
- feed directly on phytoplankton
- recovery follows similar trends to zooplankton

Fish
- only 1/7 species in the lake could tolerate the lower pH
- once lake recovered, bc of connection to other part of lake, all species previously present returned

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