Lecture 5: Biogeochemical Cycles
January 19, 2010
9:00 |
1. Kolbert chap 4 |
Reading for today was second half of Chapter 3 and Kolbert Chapter 4
scanned images from text - not available online
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2. cycles |
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3. reasons to study cycles |
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4. water |
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5. carbon |
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6. phosphorus |
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7. nitrogen |
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8. inter-related cycles |
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1. Discuss chapter 4 in Kolbert
multiple lines of evidence from species distribution shifts
- comma butterfly
- Wyeomyia smithii
- golden toad
- pine and other tree species
- Mountain ringlet butterfly
compared to climate changes (rainfall and temp)
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2. Cycles
molecule and element cycles
- water
- carbon
- nitrogen
- phosphorus
- sulfur
- iron
need to track and understand
- the different forms or compartments of the molecule or element
and the amount in each category
- such as:
- water in the ground, water in the lake
- carbon in CO2, carbohydrate in trees, fossil fuels
- N in plants, soil inorganic compounds, atmospheric NO2
- the processes that connect these compartments
- such as:
- evapotranspiration of water from soil to atmosphere
- carbon fixation of trees (ATM C as CO2 --> Plant C as biochemical)
- rate control relationships for these processes
- such as:
- evapotranspiration controlled by sun light, wind, temp, humidity, plant characteristics, etc.
- net growth rate of tree biomass from photosynthesis and usual factors light, temp, CO2, nutrients, etc.)
- interactions between cycles
- water cycle - major control over flows
- plant nutrition (C:N:P:S:Si:Fe)
- others
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3. Reasons why these cycles are important
understanding the "baseline" that used to be a fairly stable set of interacting cycles
how they have changed with human activities
- acceleration of specific transformations
- fossil fuels - C input
- erosion - trace elements accelerated 100x
- mining of specific elements, co-traveling such as release of Cd when mining other elements
- limitation of some transformations
- substitution of some land use actions
how these might change on their own
- threshold
- catastrophe
- self accelerating
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4. Water cycle - Hydrologic cycle
key concepts:
- evaportation, precipitation, transpiration
- groundwater, aquifers
ways in which humans effect the cycle
- withdrawal of freshwater
- clearing natural cover for agriculture or forestry
- increase flooding
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5. Carbon cycle
key concepts:
- CO2 is 0.038% of the atmosphere (380 ppm)
- CO2 is a greenhouse gas, traps heat
- photosynthesis, aerobic respiration
- fossil fuels (coal, oil, natural gas, oil-shale)
ways we change the cycle
- burning fossil fuels
- deforestation
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6. Phosphorus cycle
key concepts:
- phosphate ion is the main compound
- even in biological use
- no gas phase
- travels with water and sediments
ways we change the cycle:
- mining for fertilizer
- sewage into water
phosphorus is being buried in lakes and sediments around the world, as it is becoming a scarce resource
excess P in lakes can lead to toxic cyanobacteria blooms and degrade water
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7. Nitrogen cycle
key concepts:
- enormous reservoir in the atmosphere as N2
- nitrification - ammonia to nitrate
- denitrification - ammonia to N2 or N2O
- nitrogen fixation N2 to ammonia by bacteria and symbiotic associations
ways in which we interfere:
- NO from fuel combustion
- N2O from livestock and fertilizers
- N release from soils
- upset nitrogen cycle in lakes
- deplete soil through agriculture
- doubled the release of nitrogen from the land
water resource degradation from increased N load and aquatic organisms
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8. Inter-relatedness of these cycles
Redfield ratio - the average composition of biological material
- 106 C - 256 H - 106 O - 16 N - 1 P - 0.7 S
- elements are taken up in this ratio in the surface oceans
- degraded by respiration
- long time scale sediment burial and geological processes complete the cycle
energy is stored in organic carbon compounds and released in aerobic respiration
liquid water is a major player in these processes
- dissolving rocks
- carrying compounds
- supporting plant growth
- storage (in the oceans)
- Goldilocks hypothesis (planetary temperature with/without water)
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