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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

 

  2. cycles
 

3. reasons to study cycles

  4. water
  5. carbon
  6. phosphorus
  7. nitrogen
  8. inter-related cycles

 

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)

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

 

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

 

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

 

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

 

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

 

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

 

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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Last modified on January 17, 2010 by John Rueter