Transcript Biogeochemical Cycles - University of Washington

Lesson 3: Biogeochemical Cycles
Big Question:
Why Are Biogeochemical Cycles Essential
to Long-Term Life on Earth?
What is a Biogeochemical Cycle?
•
A biogeochemical cycle is the complete path a chemical takes
through the Earth’s four major reservoirs:
• atmosphere
• hydrosphere (oceans, rivers, lakes, groundwaters, and
glaciers)
• lithosphere (rocks and soils)
• biosphere (plants and animals).
Lesson 3/ ESRM 100 / University of Washington
Chemical Sinks
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Chemicals enter storage compartments - sinks
•
Amount that moves between compartments is the flux
•
net sink - when input exceeds output
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net source - if output exceeds input.
Lesson 3/ ESRM 100 / University of Washington
New Carbon versus Fossil Carbon
Lesson 3/ ESRM 100 / University of Washington
Essential Elements
24 elements are required for life
Macronutrients are required in large quantities
• carbon, hydrogen, nitrogen, oxygen, phosphorus, and
sulfur.
Micronutrients are required in small/medium quantities, or not
at all in some organisms
• copper, sodium, iodine
• See dhmo.org for a discussion of the deadly chemical
dihydrogen monoxide.
Lesson 3/ ESRM 100 / University of Washington
Essential Elements
Lesson 3/ ESRM 100 / University of Washington
Geological Cycle
The formation and change of Earth materials through physical,
chemical, and biological processes.
Here is a great move about the Geological Cycle:
http://www.britannica.com/EBchecked/topic/229677/geologiccycle
Lesson 3/ ESRM 100 / University of Washington
Tectonic Cycle
The lithosphere is comprised of several plates floating on denser
material.
Plates move slowly relative to each other – plate tectonics,
Divergent plate boundaries occur at spreading ocean ridges.
Convergent plate boundaries occur when plates collide.
Plate movements change the location of continents and alter
atmospheric and ocean circulation patterns.
Plate boundaries are geologically active, producing volcanoes
and earthquakes.
Lesson 3/ ESRM 100 / University of Washington
Major Tectonic Plates
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Hydrologic Cycle
Evaporation
Precipitation
Runoff
Groundwater
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Where Is the Earth's Water?
97% of water is stored in oceans, 2% in glaciers and ice caps, 1%
as freshwater on land or atmosphere.
Drainage basins or watersheds are the area contributing runoff
to a stream or river.
Vary in size from a hectare to millions of square miles (e.g.
Mississippi River drainage basin).
Human impacts include dam construction, irrigation,
stormwater runoff.
Lesson 3/ ESRM 100 / University of Washington
Rock Cycle
Lesson 3/ ESRM 100 / University of Washington
Rock Cycle
Lesson 3/ ESRM 100 / University of Washington
Biogeochemical Cycle of Ca in a Forest
Soluble in water and easily lost through runoff
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Sulfur Cycle In a Forest Ecosystem
Includes gaseous forms (sulfur dioxide and hydrogen sulfide)
and cycles much faster than calcium
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Nitrogen Cycle In a Forest Ecosystem
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Carbon Cycle
Carbon is vital for life but is not abundant
Enters biological cycles through photosynthesis to produce
organic forms of carbon
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Carbon Cycle in a Lake
Rob's daughter Joanna (on right) removes C in trout.
Lesson 3/ ESRM 100 / University of Washington
Fossil Fuels
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Fossil Fuels are created by the accumulation of carbon from dead
organisms in rock strata. Their decomposition is prevented by lack
of oxygen or low temperatures after their burial in sediments. After
thousands or millions of years of burial the stored organic carbon
is transferred into coal, oil or natural gas.
Lesson 3/ ESRM 100 / University of Washington
Global Carbon Cycle
Lesson 3/ ESRM 100 / University of Washington
Missing Carbon Sink
Several hundred million tons of carbon released from the
burning of fossil fuels cannot be accounted for.
Possible sinks include terrestrial forests, soils, and ocean
ecosystems.
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Nitrogen Cycle
Essential for manufacturing proteins and DNA
Although 80% of atmosphere is molecular nitrogen, it is
unreactive and cannot be used directly
Nitrogen fixation converts nitrogen to ammonia or nitrate
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Global Nitrogen Cycle
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Phosphorus Cycle
No gaseous phase
Slow rate of transfer
Released by erosion of exposed rock
Absorbed by plants, algae, and some bacteria
Exported from terrestrial ecosystems by runoff to oceans
May be returned through seabird guano
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Global Phosphorus Cycle
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Chapter 3: Biogeochemical Cycles
Questions? E-mail your TA.