The Carbon Cycle Flashcards
(176 cards)
Flux
The rate of movement of carbon between stores
Organic
Carbon found in living organisms
Store
A location where carbon is held (sometimes called a carbon sink)
Anthropogenic
Impacts of human activity on the carbon cycle
Systems
How the carbon cycle operates with inputs, outputs, stores, and flows
Equilibrium
A balance between different fluxes
Petagrams/Gigatonnes
Units used to measure carbon (1 billion tonnes)
Reservoir Turnover
Time taken for a store to refresh its carbon (output old, and input new)
What is the carbon cycle?
A biogeochemical cycle whereby carbon is stored and moved between the atmosphere, land and the oceans through flows or fluxes
Is the carbon cycle an open or closed system?
Closed
What are the two main components of the carbon cycle?
- biological
- geological
Which of the two components of the carbon cycle is shorter and which is longer?
- biological= shorter
- geological= longer
How is oil formed?
- remains of dead aquatic plants and animals die and sink to the sea bed
- lack of oxygen causes anaerobic decomposition
- compression and heating occurs
- oil and gas occurs in pockets under caprocks
How is coal formed?
- remains of trees, ferns and other plants are covered in layers of silt/mud
- lack of oxygen causes anaerobic decomposition
- compression and heating occurs
- the higher the compression and heating, the harder the coal
Mechanical weathering
The breakup of rocks by frost shattering and exfoliation produces small easy-to-transport particles
Chemical weathering
breakdown of rocks by carbonic acid in rain, which dissolves carbonate-based rocks
Biological weathering
burrowing animals and the roots of plants can break rocks up
Transportation
rivers carry particles (ions) to the ocean, where they are deposited
Sedimentation
over millennia these sediments accumulate, burying older sediments below, such as shale and limestone
Metamorphosis
the layering and burial of sediment causes pressure to build, which eventually becomes so great that deeper sediments are changed into rock
positive feedback mechanism example
more volcanoes = more CO2 in atmosphere (increases temp) = more C acid = more chemical weathering = more transportation of bicarbonate ions to oceans = more sedimentation and burial of CaCo3 = more metamorphism (so more metaphorphises of rocks) = more rocks melting
the movement of c between stores in the geological c cycle (EXPLAINED)
processes:
chemical weathering - CO2 in atmosphere reacts with some minerals to form calcium carbonate (limestone)
(or)
biological weathering - plant and animal particles break down after death
Then….
Transportation - this calcium is then dissolved by rainwater/ or small rock pieces (ions) are carried to the oceans. These form with bicarbonate ions to become calcite
Sedimentation - once there, it can precipitate out of the ocean water, forming layers of sediment on the sea floor. These will accumulate for millennia, burying the older sediments below (eg. shale and limestone)
Metamorphises - the layering and buryal of these sediments causes pressure to build and the limestone becomes marble and the shale becomes slate OR form oil deposits
Then….
through tectonic uplift, these sediments are either subducted underneath the continents, or the uplift will expose previously buried limestone
Finally….
The CO2 is then re-emitted into the atmosphere through volcanic erruptions (volcanic outgassing - eg Iceland 2010 volcano)
the movement of c between stores in the geological c cycle (SUMMARY)
chemical or biological weathering
transportation
sedimentation
metamorphises
tectonic uplifting
CO2 re-emitted through outgassing
biological c cycle (fast cycle)…. what is it?
fast movement of c between the atmosphere, ocean and ecosystems
large exchange fluxes between stores and rapid turnover (between a few years to a milennia)
c is sequestrated in and flows between land, atmosphere and oceans