global biogeochemical cycles - lakehead university · 2016. 2. 4. · global biogeochemical cycles...
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GLOBAL BIOGEOCHEMICAL CYCLES
GEOG/ENST 3331 – Lecture 10 Turco: Chapter 10; Dearden and Mitchell: Chapter 4
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Assignment 4
1. Suppose that a layer of air 1000 m thick has conditional stability. A rising parcel of dry air within the layer will be pushed back down.
1. What does ‘conditional stability’ tell us about the temperature profile of the layer? What can you say quantitatively about the environmental lapse rate?
2. How would the stability be affected if the layer passed over a very warm surface?
3. How would the stability be affected if the layer passed over open water?
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Last Lecture
¨ Weather forecasting ¤ Prediction methods ¤ Numerical weather prediction
¨ Long-range forecasting ¤ Memory ¤ ENSO and NAO
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Global biogeochemical cycles
¨ Objectives ¤ Recognize biologically important and abundant
chemicals and their associated reservoirs ¤ Understand the flows between reservoirs and be able
to characterize them as large or small, fast or slow ¤ Consider anthropogenic perturbations to these cycles
and gain an idea of their implications
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Global biogeochemical cycles
¨ Reservoirs ¤ Box models and fluxes ¤ Sources and sinks ¤ Residence time
¨ Hydrological cycle ¨ Carbon cycle
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Box models
¨ Q ~ total mass ¨ S ~ source ¨ L ~ sink ¨ Mass balance
¤ ΔQ = S – L
¨ Steady state ¤ L = S, ΔQ = 0
Turco: Figure 10.2
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Residence time
¨ Residence time of the substance in a reservoir:
LQ
=τ
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Multiple reservoirs
¨ Closed system ¤ Extend mass balance ¤ Every flux is a source
and a sink
Example
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Reservoirs
¨ Atmosphere ¨ Hydrosphere
¤ Mixed layer ¤ Deep ocean
¨ Lithosphere ¤ Crust and upper
mantle ¤ Sediments
¨ Biosphere ¨ Cryosphere
Turco: Figure 10.1
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Hydrological cycle
‘Groundwater’ includes water in lakes, soil and ice sheets
Turco: Figure 10.15
17,000 Gt⋅H2O
4.9×107 Gt⋅H2O
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Importance
¨ Redistribution to the land ¤ Liquid sinks in and flows downhill ¤ Important to biosphere
¨ Desalinization ¨ Mobilizing Contaminants
¤ Universal solvent ¤ Precipitation washes out atmosphere ¤ Runoff leaches compounds from rocks/soil
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Human impacts
¨ Consumption ¤ Freshwater for drinking ¤ Cooking ¤ Transportation ¤ Hydroelectricity
¨ Water quality ¤ Toxins ¤ Nutrients
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Carbon cycle
¨ Multiple processes ¨ Multiple timescales
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Terrestrial biosphere cycle ¨ Photosynthesis
¤ Water, CO2 and sunlight turned into carbohydrates and oxygen (O2)
¨ Respiration ¤ Includes decomposition
by bacteria
¨ Combustion
Turco: Figure 10.11
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Oceans
¨ Surface (100 m or less) ¤ Well-mixed (winds) ¤ Photosynthesis only in top few metres
n Some life exists further down
¨ Deep ocean (average nearly 4 km deep) ¤ Stratified ¤ Mostly barren ¤ Thermohaline: very slow circulation
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Air-sea cycle
Small biomass reservoir in ocean; small fluxes
Large exchange with atmosphere
Thermohaline: slow circulation to deep ocean
Turco: Figure 10.12
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Recap: Fast Processes
¨ Air-biomass exchange: 80 GtC/year ¨ Air-ocean exchange: 50 GtC/year ¨ Surface-deep ocean exchange: 25 GtC/year ¨ Ocean-biosphere exchange: 5 GtC/year
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Geologic carbon cycle
¨ Geologic time scale ¤ Note the very small
size of fluxes
¨ Dissolution ¨ Sedimentation
¤ Mostly CaCO3
¤ Uplift/weathering ¤ Subduction
¨ Outgassing
Turco: Figure 10.10
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Turc
o: F
igur
e 10
.13
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Importance
¨ Plant food ¨ Greenhouse effect from CO2
¤ Also Methane (CH4) n Anaerobic decomposition n Transformed into CO2 in atmosphere
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Human impact
¨ Gradual burial of organic material over hundreds of millions of years
n Converted by temperature and pressure into fossil fuels n Extracted and consumed for energy n Unbalanced flux to the atmosphere of 7-8 GtC/year
¨ Deforestation: increased flux from biosphere to atmosphere of 2 GtC/year
¨ Also increases in methane (CH4), and carbon monoxide (CO)
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Effects of additional CO2
¨ Global warming ¨ Fertilization of plant growth ¨ Increased carbonic acid in ocean
¤ Decreased calcium carbonate formation ¤ Uncertain other direct effects
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Global geochemical cycles, continued
¨ Oxygen cycle ¨ Nitrogen cycle ¨ Sulfur cycle
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Oxygen
¨ 1 million GtO in the atmosphere (mostly O2) ¤ Much, much more oxygen is contained in the crust in the
form of mineral oxides
¨ Very reactive ¨ Source: photosynthetic consumption of CO2
¤ 6CO2 + 6H2O + sunlight → C6H12O6 + 6O2
¤ O2 is a by-product of this reaction ¤ Removes carbon from the atmosphere; if the carbon is
not returned to the atmosphere, there is a net oxygen source
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Oxygen cycle
¨ Link: 0.18 GtCO2
¤ 0.05 GtC ¤ 0.13 GtO
¨ Burial is largely sediments in the ocean
¨ Long-term: sink is balanced by recycling buried carbon
Turco: Figure 10.9
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Importance
¨ Critical to aerobic respiration ¤ Historically, led to the evolution of complex organisms
¨ Required for combustion ¤ Forest fires
¨ Absorbs UV radiation ¤ Leads to presence of ozone (O3) in atmosphere ¤ Some O2 is split apart by UV radiation and reacts with
other O2 to form O3
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Human impact
¨ Insignificant ¨ Atmosphere: τ = 5000 years
¤ If photosynthesis stopped respiration would deplete the atmosphere in 5000 years
¨ Fossil fuel combustion ¤ Sinks O2 at rate of 18 GtO/year ¤ Turco estimate: all accessible fossil fuels would sink
23000 GtO from atmosphere
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Nitrogen
¨ N2 is 78% of the atmosphere by volume ¤ Inert gas ¤ Some bacteria specialize in nitrogen fixation
¨ N2O is a trace gas ¤ Also inert
¨ NOx (NO and NO2) ¤ Reactive gases ¤ Soluble
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N2 cycle
Atmosphere N2
4 × 106 GtN
Land/Biosphere
CN 300 GtN
Ocean N2
2 × 104 GtN
Denitrification
Fixation
Outgassing
Dissolution 0.26 GtN/year 50 GtN/year
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N2O cycle
Atmosphere
N2O 1500 MtN
Atmosphere N2
Biosphere
CN
Fuel combustion
Photolysis
Denitrification 4 MtN/year
8 GtN/year
10 MtN/year
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NOx cycle
Atmosphere
NOx 5 MtN
Atmosphere N2
Land/biosphere
CN
Fuel combustion Lightning
Emissions
Precipitation
22 MtN/year
24 MtN/year
5 MtN/year
51 MtN/year
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Importance
¨ N2
¤ Nitrogen fixation is vital for the biosphere
¨ N2O ¤ Potent greenhouse gas ¤ ‘Regulates’ stratospheric ozone
¨ NOx
¤ Smog ¤ Acid rain ¤ Fertilizer
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Human influence
¨ Fertilizer ¤ Eutrophication ¤ Increased N2O
¨ Fossil fuels ¤ Increased N2O and NOx
¨ Fires ¤ Increased NOx
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Sulfur
¨ Mainly found in mineral form ¨ Important trace nutrient
¤ Present in fossil fuels
¨ Sulfuric acid ¤ Common industrial uses ¤ Car batteries
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Atmospheric Sulfur
¨ Natural sources: ¤ Oceans ¤ Volcanoes ¤ Biological activity
¨ Sink: ¤ Precipitation (deposition)
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Sulfur cycle
Turco: Figure 10.5
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Importance
¨ Essential nutrient ¨ Major source of cloud condensation nuclei (CCN)
¤ Gaia hypothesis: n Ocean phytoplankton release sulfur gases n Modify albedo n Biospheric thermostat?
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Human impact
¨ Gaseous emissions ¤ Fossil fuels ¤ 90 MtS/year ¤ Acidic rain and fog
¨ Fertilizer ¤ 30 MtS/year
¨ Wastewater ¤ 30 MtS/year
Turco: Figure 10.6
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Reservoir review
Chemical Atmosphere Ocean Biosphere Crust
S Minor Large Small Large
N Large Minor Small Minor
O Small Small Minor Large
C Minor Small Minor Large
Turco: Table 10.1
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Next lecture
¨ Air pollution and air quality ¨ Smog