carbon cycle 2.1.6a - pathways and processes Flashcards
what are the three timescales of the carbon cycle
- (seconds/minutes) Shortest timescale
- (10-500 years) Longer timescale
- (million years)Longest timescale
give an example of the shortest timescale of (seconds/minutes) in the carbon cycle
Plants take carbon out of the atmosphere through carbon sequestration via photosynthesis, then release it back out to the atmosphere through respiration
desribe where carbon is being stored that lasts along period of time in that one store of 10-500 years
Carbon being stored in dead plant material within the soil
Carbon is stored their for years until broken down by soil microbes
give an example of the longest timescale of millions of years in the carbon cycle
an example of when carbon is locked in for millions of years which is the longest timescale- occurs wehn organic matter is buried in deep sediments and over time transfers into deposits of coal, oil, natural gas and fossil fuels.
only when we burn these substances, is it released into the atmosphere
what is the name of the curve graph which shows the accumulation of carbon dioxide in the atmosphere
The Keeling Curve
why is their a variation of amounts of co2 in the atmosphere throughout the year
think about seasons
there are 3 points
due to:
- photosynthesis variation in seasons
- human activity (use more energy in winter)
- Forest fires more combustion in the summer
How many Gct of carbon is found in plant stores
560 Gct
What is an example of carbon fixation
carbon sequestration in trees can store large amounts of carbon due too the wood being big and dense,
this leads to carbon fixation because the carbon exists in the organic forms (in a tree)
Name the three types of sequestration
- Terrestrial sequestration (trees)
- Geological sequestration
- Ocean sequestration
Terrestrial sequestration
what is it
terrestrial sequestration is a large amount of carbon being stored in Soils and Vegetation
( 560 Gct of carbon is stored in plants, importance to woody stems of trees)
outline what geological sequestration is
What does the r….. serve as for the carbon
overtime what does this lead to
(r….)
geological sequestration is the natural pores in geologic (rock) formations, so the carbon is locked inside the rock for a long period of time
The rocks serve as a reservoir for carbon because it is stored their for a long period of time
Overtime, the rock gets layered by the compression of dead biological matter on the ocean floor, creating sedimentary layers
ocean sequestration
what is it
the carbon store though direct absorption or fertilisation
what are the contributing factors of terrestrial sequestration
- photosynthesis
- respiration
- leaf litter
-decomposition
-soil
within terrestrial sequestration
what is the role of ‘leaf litter’
leaf litter is dead plant material
All litter begins to decompose, which makes this a carbon flux ( a flow of carbon) in order to enrich the soil
within terrestrial sequestration
what is the role of ‘decomposition’
when living organisms die, decomposers e.g. worms and fungi, feed on the dead organic matter and break it down into
-co2
-nutrients
-water
This is soil respiration
- it releases carbon to surrounding soil and atmosphere
within terrestrial sequestration
what is the role of ‘soil’
carbon exists in soil, in the form of= soil organic carbon (SOC)
this is the main component of soil organic matter (SOM)
som is formed from the decay of organic materials (plants, animals, soil microbes, plant roots)
what is the total amount of carbon in the worlds ‘‘soil”
1500 Gtc- which is more than atmosphere store and vegetation store combined
outline was the ‘humus layer’ is and why it is important in relation to carbon
- its organic matter that if left undistrubed can store soil carbon for a long time period
Irs important because it’s a carbon sink, so absorbs more than it releases
How does co2 enter the ocean
Through the process of diffusion where molecules of co2 enter the ocean by diffusing into the sea surface water
name the four variables that contribute to the amount of co2 that diffuses and then dissolves into the ocean
- strong wind mixing with ocean circulation- enhances mixing of surface water and deep waters which helps dissolve the co2
- concentration of co2 in atmosphere- allows more to be diffused into oceans
- temperature of the water- colder waters absorb more co2
- ocean alkalinity and pH- more alkaline the more absorption of co2
what happens when the co2 is dissolved into the ocean?
the co2 enters the Ocean Carbon Cycle
through different mechanisms
name the 3 mechanisms of the ocean carbon cycle that co2 can enter
- physical carbon pump
- biological carbon pump
- carbonate pump
Summarise with key terms what the Physical Carbon Pump is, in terms of it being an ocean carbon pathway
-The Thermohaline System is the physical pump in oceans which allows co2 to be constantly exchanged between the ocean and atmosphere.
-The co2 is diffused into the cold surface waters in polar regions because co2 is absorbed more in cold temperatures
- The dissolved co2 is transported to the deep ocean via down-welling currents due the water being cold and dense so it sinks, and often remains in the deep ocean for centuries
-Then often near coastlines, up-welling occurs, when the water warms and rises to the surface, releasing some co2 back into the atmosphere, but most co2 is sequestered and stored in the deep ocean.
Summarise with key terms what the Biological Carbon Pump is, in terms of it being an ocean carbon pathway
what do the ……………. do to absorb co2
how does the food w influence this process
- The biological carbon pump is the organic sequestration of co2 from the atmosphere to the ocean by Phytoplankton.
They absorb co2 at the surface through photosynthesis
-Phytoplankton are the base of the marine food web, so when they are consumed or die, the carbon is passed on through marine life, or their rich-biomass sinks down to the deep ocean and is stored in sediments
Summarise with key terms what the Carbonate Pump is, in terms of it being an ocean carbon pathway
When CO2 dissolves in the ocean with the water molecules, it reacts and produces bicarbonate ions, which are key to marine organisms because they combine with calcium ions to form calcium carbonate.
Shell-building organisms such as coral, coccolithophores and foraminafera, use calcium carbonate to build their shells.
- They lived then died and sank to the ocean floor, where these shells accumulate and contribute to the sediment formation such as limestone e.g. white cliffs of dover
