Carbon Cycle Flashcards
when carbon moves directly from the atmosphere to surface ocean?
diffusion / direct gaseous exchange
what is the rate of carbon from the atmsohere to the surface ocean?
92 PgC/year
from the surface ocean back to the atmosphere flux rate is what?
90 PgC/year
when carbon is sequestered by phytoplankton, this is known as?
photosynthesis
carbon sequestration by phytoplankton accounts for what % of carbon sequestered from the atmopshere?
50%
when carbon is re-released into the atmosphere by marine biota the flux is known as?
respiration
how many more times larger are the oceans than the atmopshere as a carbon store?
50x
dissolved carbon dioxide is moved from the surface to the deep ocean via what process?
downwelling
carbon can be held in the surface ocean as what gas?
CO2
what are the 3 names of the ocean pumps?
1 - physical
2 - biological
3 - carbonate
the physical pump os also known as?
thermohaline ciruclation
how many PgC reach the ocean floor to become surface sediment?
0.2
the surface sediment over time undergoes the process of what?
sedimentation
the surface sediment is then transformed into what?
sedimentary / calcium rock
carbon can be removed from the terrestrial lithospere and makes its way to the oceans again via what flux?
weathering (chemical and mechanical)
what is the flux rate of weathering process in PgC/year
50
anthropogenic activity can release carbon from the lithosphere premeaturley via what process?
combustion
the flux of combustion happens at how many PgC/year
35
carbon can naturally return to the atmosphere from the lithosphere via what flux?
volcanic outgassing
what is the rate of volcanic outgassing?
0.15 PgC
why is volcanic outgassing needed to maintian what?
natural greenhouse effect
vegitation in the terrestrial biosphere sequesters carbon via the flux of what?
photosynthesis
what is the flux of photosynthesis per year?
123 PgC/year
at night, vegitation will release CO2 via what flux?
respiration
with reference to vegitation, what is the difference in the rate of the fluxes which sequester and release carbon?
1000
carbon moves from vegitation to the soil sotre by what process?
decomposition
what is the flux of decomposition?
50 PgC/year
decomposition is carried out byfunghi and detritivores. this means carbon can released by what process?
respiration
the lithosphere stores carbon as 2 things what are they?
1 - sedimantry rock
2 - calcium carbonate
how many PgC does the lithopshere hold?
100,000,000 (1 million)
how mang PgC are held as fossil feuls?
4,000
how many PgC are held as surface sedimentt at the bottom of the oceans?
1,750
the oceans hold how many PgC?
39,000 PgC
the terrestrial biosphere holds around how many PgC?
3,500
soild hold around how many PgC?
600
the atmosphere holds around how many PgC?
750
what % of the atmopshere is carbon dioxide?
0.04%
marine biota hold how many PgC?
3
phytoplankton hold what % of global biomass?
50%
what is the atmosphere to hydrosphere interaction?
fast biolgical cycle
what is the atmosphere to hydrosphere interaction?
fast biolgical cycle
what happens in the fast geological cycle (atmosphere to hydrosphere)? 3
- diffusion happens to the oceans
- carbon moves into phytoplankton by photosynthesis
- transferred to marine mammels to the atmosphere by respiration
what is the interaction between the hydrosphere and the lithosphere?
fast biological to slow geological
what happens in the hydrosphere into the lithosphere (fast biological to slow geological)?
- moves into the surface oceans as dissolved co2
- moves to deep ocean by downwelling
- moves to the ocean floor as surface sediment
- undergoes sedimentation and is turned into calcium carbonate or fossil fuels
- moves from lithosphere to hydrosphere by chemical weathering
what happens in the hydrosphere into the lithosphere (fast biological to slow geological)?
- moves into the surface oceans as dissolved co2
- moves to deep ocean by downwelling
- moves to the ocean floor as surface sediment
- undergoes sedimentation and is turned into calcium carbonate or fossil fuels
- moves from lithosphere to hydrosphere by chemical weathering
what is the interaction between the lithosphere and atmosphere?
slow geological to fast biological
what happens between the lithosphere and atmosphere (slow geological to fast biological)?
- moves through combustion
- can cause from volcanic outgassing and being released as carbon dioxide
what is the interaction between the atmosphere and the terrestrial biosphere?
fast biological
what happens between the atmosphere and the terrestrial biosphere (fast biological)?
- vegetation sequesters via photosynthesis and is released via respiration at night time
- move from soil store from the vegetation store by decomposition
- funghi and detritovores break it down and release back into the atmosphere by respiration
what is the formation of limestone?
- formed from shell fragments of marine organisms
- animals die and the fragments precipitate down
- lithified to form limestone
what is the formation of shale?
- organic material precipitates to the ocean floor
- material is embedded in mud layer
- exposed to heat and pressure and lithified
what is the formation of fossil feuls?
- organic matter precipitates onto ocean floor
- covered by mud
- material decays anaerobically
- if material is added faster than it decays it becomes a fossil fuel
what is oil and gas made from?
marine plants and animals
what is coal made from?
dead plants on land
how does carbon move through the water to the land and into the ocean and into the lithsophere?
- water mixes with co2 to form carbonic acid
- acid comes into contact with calcium cabronate by chemical weathering
- surface runoff caries carbonate into the ocean
- sinks to ocean floor becoming sedimentary rock
- convection currents force it into the volcanic outgassing
what is the negative feedback mechanism for the geological cycle?
- increase in volcanic activity -> increase volcanic outgassing -> increased levels of co2 in the air -> decreased diffusion and respiration -> increase in convectional rainfall
-> increase in chemical weathering
what do the ocean pumps do?
drive the flux of carbon from the surface ocean to the deep oceans and from the deep ocean to the surface ocean.
how many PgC are absorbed by the oceans?
92
how many PgC are released by the oceans?
90
what do the ocean pumps maintian?
diffusion gradient between the atmosphere and the surface ocean store
biological pump
- flux between polar and tropics
- phytoplankton in the photic zone use sunlight to convent co2 into carbohydrate by photosynthesis
- carbon enters marine biota as the phytoplankton are eaten by the zooplankton which store carbon in their bodies
- carbon goes from downwelling in deep ocean to surface ocean by upwelling
- marine biota precipitates to ocean floor
- compressed into rock where it lasts for 100 million years
carbonate pump
- carbon is held in coral generated from calcium ions of acid rain
- shellfish use these to make their shells
- die and precipitate to the ocean floor
- turns into sedimentary rock
- turns into limestone
physical pump - salty water sinking
- decreasing temp and increased salinity -> more dense so is cooler
- increasing temp and decreased salinity -> less dense so is warmer
- cooler water at polar region forms as sea ice which stores fresh water
- increases salinity at poles so ice sinks to deep ocean
- thermohaline circulation and combustion pulls warmer water from tropics towards poles
- deep currents flow to surface ocean where it is realised back into atmosphere
what are the 2 impacts of a carbon imbalance on the oceans?
- ocean acidification
- threats to ocean health and impacts on humans
what is ocean acidification?
decreasing ocean pH of the ocean over an extended period of time
what % of carbon do soils store?
20-30%
what are the 2 types of carbon in soils?
organic
inorganic
how is caron stored in soils?
dead biomass
what % of carbon is in humus?
60%
what is the longest store that carbon can be stored in soils?
pyrogenic carbonatious carbon
what are inputs into the soil store?
plants, animals and residues
what are outputs of the soil store?
decomposition and consumption
what does carbon give soil?
water retention capacity and structure and capacity
what does nutrient and carbon cycling varies on?
biome and climate
what is the soil and carbon balence?
if plant residue is added to the soil at a faster rate than soil organisms convert it to co2 - the carbon will be gradually removed from the atmosphere
what biome has the largest soil carbon store?
tundra
why is the carbon soil store so low at the equator?
high precipitation washes away nutrients
what are the 3 types of wetlands?
marshes
peat bogs
mangroves
what is the role of a marsh in the carbon cycle? 7
- waterlogged permanently
- soils are anerobic (low co2)
- oxygen diffuses through water
- decomposition is slow
- carbon in dead plants remains intact
- rather than being broken down by microbes and returned by respiration
- drought makes wetlands a carbon source
what is the role of peat bogs in the carbon cycle?
- 60% of wetlands are peat based
- dead organic matter is added to soils in waterlogged conditions
- occurs faster than the rate it decays as decomposition is anaerobic
what is anaerobic respiration?
lack co2 to repsire
what is the role of mangroves in the carbon cycle?
- blue carbon with carbon stored in coastal salt marshes
- grow in saline waters between 25 n and 25 s
- if 2% of the mangroves are lost, carbon will be released at 50x the sequestrion rate
- sequester into branches and roots and then soils
how many more x is carbon stored in mangroves compared to tropical rainforests?
5x
how many billion of tonnes does the Scottish peatland store and how many years worth of emissions?
1.7 billion ad 140 years of emissions
what is permaforst?
permantly frozen layer on the Earth’s surface. it is soil, gravel and sand that under 0 degrees
how many years worth does permaforst release of oil, coal and natural gas emissions?
4 to 6 years
what is the positive feedback mechanism of permafrost?
- increased thawing
- increased decomposition
- increased co2 released
- increased CH4 release in soil
- increased EHGHE
- increased global warming
what is the negative feedback mechanism for global warming?
- increased thawing
- increased decomposition by microbes
- increased nutrients as rain water avalibility decreases
- increased precipitation
- increased carbon sequestration
what are the 2 ways to manage soils?
draining of wetlands and burning of peatlands
how many % of the worlds wetlands have been lost over the past 300 years?
87%
how does the draining of wetlands increase co2 emission?
- led to expsoure of biomass to increase decomposition
- becomes a carbon store
- 30% of global methane emissions are from weltands
- will increase with climate change
how does the burning of peatlands increase carbon emissions?
- can take 1,000 years to form 1m of peat
- burning releases carbon rapidly
- Scotland peatland working to restore peatland areas
how many PgC does vegitation hold?
600
how many PgC does rainforests and wilfires occur at?
119
when does respiration happen?
at nightime
what does photosynthesis occur by?
location
when does photosynethesis occur the fast on?
day or night
summer or winter
high or low tree density
broad leaf species or thin leaf species
day - more sunlight
summer - more sunlight
high tree density - more photosythesis
broad leaf species as they have greater surface area
what is net primary productivity?
the rate at which energy is stored as biomass by plants or other primary producers