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Physical geo
Water and carbon
3.1.1.3 the carbon cycle
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Jomera hoque
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Cards (16)
lithosphere -
99.9
% sedimentary rocks
hydrosphere -
2nd
largest carbon store
co2
dissolves
into ocean
0.04
%
phytoplankton
photosynthesise
biosphere -
0.004
%
cryosphere - permaforst
0.01
%
Photosynthesis
1. Living organisms convert
Carbon Dioxide
from the atmosphere and Water from the soil, into Oxygen and
Glucose
using Light Energy
2. Removes
CO2
from the atmosphere
Combustion
(Burning fossil fuels, wildfires etc.)
Releases
CO2
into the atmosphere
Decomposition
1. When living organisms die, they are broken down by
decomposers
which respire, returning
CO2
into the atmosphere
2. Some carbon is also returned to the
soil
Diffusion
The oceans can absorb CO2 from the atmosphere, but this harms aquatic life by causing coral bleaching
Weathering and Erosion
Rock particles broken down and transferred to the
ocean
, where the carbon> create
shells
Burial
and Compaction
Sea shell fragments become compacted > form
limestone
and organic matter may form
fossil fuels
Carbon Sequestration
Transfer of carbon from the atmosphere and can be both
natural
and
artificial
Main Carbon Stores (In order of magnitude):
Marine Sediments
and Sedimentary Rocks -
Lithosphere
- Long-term
Oceans
- Hydrosphere -
Dynamic
Fossil
Fuel Deposits - Lithosphere - Long-term but currently
dynamic
Soil Organic Matter
-
Lithosphere
- Mid-term
Atmosphere -
Dynamic
Terrestrial Plants
- Biosphere - Mid-term but very
dynamic
The
lithosphere
is the main store of carbon
with global stores
unevenly
distributed.
the oceans are
larger
in the southern hemisphere,
storage in the
biosphere
mostly occurs on
land.
Terrestrial plant storage is focussed in the
tropics
and the
northern
hemisphere.
The
Carbon Budget
is the balance between carbon inputs and
outputs
to a
store
at any scale
Carbon
Source
- A store that emits more carbon than it absorbs: E.g. a
damaged
rainforest
Carbon
Sink
- A store that absorbs more carbon than it emits: E.g. a
virgin
rainforest