carbon Flashcards
why is carbon important
Carbon is the main building block of life.
how is carbon held
Carbon is held in stores e.g. the atmosphere and can have many forms. For example in the atmosphere, carbon is present as gases (carbon dioxide and methane).
carbon stores
the atmosphere
the hydrosphere
the lithosphere
the biosphere
what carbon is stored in the atmosphere
carbon dioxide and methane
what carbon is stored in the hydrosphere
dissolved carbon
what carbon is stored in the lithosphere
carbonates in limestone and fossil fuels such as coal, oil and gas
what carbon is stored in the biosphere
in both living and dead organisms
what is the cycle of carbon
how carbon moves from one store to another
what processes are involved in the carbon cycle
respiration
photosynthesis
volcanic eruptions
store/reservoir
where carbon is held
fluxes
the flows of movement between the stores, which can operate at local and global scales
petagrams or gigatonnes
The units used to measure carbon; one petagram (Pg), also known as a gigatonne (Gt), is equal to one billion tonnes.
egs of carbon stores
crustal/terrestrial/geological
oceanic (deep)
terrestrial soil
oceanic (surface)
atmospheric
terrestrial ecosystems
crustal/terrestrial/geological
carbon store
Sedimentary rocks, very slow cycling over millennia
oceanic (deep)
carbon store
Most carbon is dissolved, inorganic carbon stored at great depths, very slowly cycled.
terrestrial soil
carbon store
From plant materials (biomass) microorganisms break most organic matter down into C02 in a process which can take days in a hot and humid climate to decades in colder climates
oceanic (surface)
carbon store
Exchanges are rapid with the atmosphere through physical processes such as C02 dissolving in the water and biological processes involving plankton. Some of this carbon sinks into the deeper ocean pool.
atmospheric
carbon store
C02 and CH4 store carbon as greenhouse gases with a lifetime up to 100 years
terrestrial ecosystems
carbon store
CO2 is taken from the atmosphere by photosynthesis, carbon is stored organically, especially in trees. Rapid exchange with the atmosphere- seconds/minutes.
crustal/terrestrial/geological pentagrams
100 000 000 fossil fuels store an extra 4 000
oceanic (deep) pentagrams
38 000
terrestrial soil pentagrams
1,500
oceanic (surface) pentagrams
1,000
atmospheric pentagrams
560
terrestrial ecosystems pentagrams
560
long term carbon stores
crustal/terrestrial/geological
oceanic (deep)
short term stores
terrestrial soil
oceanic (surface)
atmospheric
terrestrial ecosystems
where can carbon come from
geological carbon
biologicaly derived carbon
geological carbon
Carbon can be created through a number of chemical reactions in the rock cycle
biologically derived carbon
Carbon can also be present in organic matter as a result of processes such as respiration. This can later be stored in shale, coal and other sedimentary rocks
when is geological carbon formed
when rocks such as sedimentary rocks are created e.g. limestone and chalk.
why is there balance in the geologicaal carbon cycle
There tends to be a natural balance between the amount of carbon being released and the amount being absorbed.
However, there can be occasional disruptions and short periods before this balance is restored, such as during a volcanic eruption.
what happens in the geological carbon cycle
This is a natural cycle that moves between land, oceans and the atmosphere.
It involves a number of chemical reactions that create new stores which trap carbon for significant periods of time
case study example of a geological carbon cycle
One of earth’s largest stores of carbon is the Himalayas which started off as oceanic sediments rich in calcium- this is now being weathered and returned back to the oceans.
what is biologically derived carbon created from
is created from dead organisms such as coal and shale.
These organisms absorb carbon during respiration and photosynthesis.
Once they die they (if they are in oceans) sink to the sea bed.
They are then buried under sinking sediments and form layers called strata.
Eventually, the strata are squeezed together as a result of the weight on top, and can create fossil fuels such as coal and oil.
what is out gassing
Terrestrial carbon, held within the mantle, is released into the atmosphere as carbon dioxide (CO2) when volcanoes erupt
what is chemical weathering
CO2 within the atmosphere combines with rainfall to produce a weak acid (acid rain) that dissolves carbon-rich rocks, releasing bicarbonates
what happens to weathered carbon calcium sediments in the geoleogical carbon cycle
Rivers transport weathered carbon and calcium sediments to oceans, where they are deposited.
Carbon in organic matter from plants and from animal shells and skeletons sinks to the ocean bed when they die, building up strata of coal, chalk and limestone.
Carbon-rich rocks are subducted along plate boundaries and eventually emerge again when volcanoes erupt.
The presence of intense heating along subduction plate boundaries metamorphoses (alters) sedimentary rocks by baking, creating metamorphic rock. CO2 is released by the metamorphism of rocks rich in carbonates during this process.
what are the three ways carbon is released in the geological carbon cycle
volcanic outgassing
metamorphism
chemical weathering
eg of outgassing
in 2010, the Icelandic Eruption emitted between 150,000 and 300,000 tonnes of CO2 per day. It contributed less than 0.3% of global emissions that year.
in what form is carbon found in the atmosphere
a gas
Carbon is stored during the formation of which type of rock?
sedimentary
What is the term used for the movements of carbon between stores?
flux
How many tonnes is a petagram/gigatonne equal to?
One billion
What is the name of the sphere where all living things are found?
biosphere
what is the difference between a carbon source and carbon sink
A carbon source is shrinking in size and releasing emissions. Whereas a carbon sink is growing in size and storing more carbon.
what does the amount of carbon in the atmosphere depend on
the balance that exists between the sinks and sources.
when is the carbon cycle in equilibrium/balanced
If sources equal sinks
what happens if the carbon cycle is unbalanced
results in posotive or negative feedback
negative feedback loop
Earth systems normally operate by negative (stabilising) feedbacks, maintaining a stable state by preventing the system moving beyond certain thresholds. I.e. any change is cancelled out, maintaining equilibrium.
posotive feedback
Positive (amplifying) feedback loops occur when a small change in one component causes changes in other components. This shifts the system away from its previous state and towards a new one.
what is the biogeochemical carbon cycle
Biological and chemical processes determine just how much of the carbon available on the Earth’s surface is stored or released at any one time.
The role of living organisms are critical to the cycle and to controlling the balance between overall storage, release, transfer and absorption of carbon.
what 4 key processes are involved in the bio-geochemical carbon cycle
photosynthesis
respiration
decomposition
combustion
what is respiration
a chemical process that happens in all cells and is common to both plants and animals
glucose is converted into energy that can be used for growth and repair, movement and control of body temperature in mammals
carbon dioxide is then returned to the atmosphere mostly by exhaled air
what is decomposition
when organisms die they are consumed by decomposers such as bacteria, fungi and earthworms
during this carbon from their bodies is returned to the atmosphere as carbon dioxide
some organic material passes into the soil where it may be stored for hundreds of years
what is combustion
organic material contains carbon
when burned in the presence of oxygen it is converted into energy, carbon dioxide and water- combustion
carbon dioxide released into the atmosphere returning carbon that may have been stored in rock for millions of years
what is photosynthesis
the process where plants use the light energy from the sun to produce carbohydrates in the form of glucose
green plants absorb light energy using chloropyll in their leaves
absorbed light energy converts carbon dioxide in the air and water from the soil into glucose- during this oxygen is released into the air
some glucose is used in respiration the rest is converted into starch which is insolublebut can be converted back into glucose for respiration
how much larger is the ocean store for carbon than the atmosphere
The ocean’s are one of the Earth’s largest store, being 50 times greater than the atmosphere.
where is 93% of CO2 stored
in undersea algae, plants and coral, with the remainder dissolved in the water.
what are carbon cycle pumps
are processes operating within the oceans which circulate and store carbon.
what are the three carbon cycle pumps
the biological pump, the carbonate pump and the physical pump.
what are the three ocean pumps
biological pump
carbonate pump
physical pump
biological pump
this is the sequestration of C02 to oceans by phytoplankton. Phytoplankton float on the surface of the ocean to access sunlight and photosynthesise. They are autotrophs and are the base of the marine food web. Even though they are minute they make up over half the planets biomass.
Carbon is then passed up the food chain by consumers which in turn release C02 back to the atmosphere.
In this way most carbon is cycled in surface waters and only 0.1% reaches the sea floor through decompositions and sedimentation.
Phytoplankton sequester over 2 billion metric tonnes of C02 annually to the deep ocean.
carbonate pump
this relies on inorganic carbon sedimentation. Lots of marine organisms utilise calcium carbonate to make their outer shells/ skeletons. When these organisms die and sink to the sea floor many shells will dissolve on the way and the carbon will become part of the ocean and flow around the planet in currents. Shells that do not dissolve build up slowly on the sea floor forming limestone sediments such as those in the white cliffs of Dover.
physical pump
This is the oceanic circulation of water including upwelling, down welling and the thermohaline current. C02 in the oceans is mixed much slower than in the atmosphere so there are large spatial differences in concentration.
Colder water can absorb more C02 so C02 concentration is 10% higher in the deep ocean than the surface and polar regions store more than tropical regions. Warm waters release C02 into the atmosphere and cold waters absorb C02.
Large ocean currents like the North Atlantic Drift move water from the tropics to the poles, the water cools and absorbs more C02.
when did the iceland volcano erupt
2010
how much CO2 did the iceland volcano emmit
between 150,000 and 300,000 tonnes of CO2 per day placing it in the same emissions league as small-medium European countries such as Portugal or Ireland
what % of global emmisions of greenhouse gases did the Iceland volcano emit in 2010
However it contributed less than 0.3% of global emissions of greenhouse gases in 2010.
biological pump summed up
organic sequestration by phytoplankton
physical pump summed up
based on the rise (upwelling) and fall (downwelling) of the circulation of water
carbonate pump summed up
Based on CaCO3 used in the shells of marine organisms
where do phytoplankton live
Phytoplankton float on the ocean’s surface to access sunlight and photosynthesise.
how much of the worlds biomass do phytoplankton make up
half
what do phytoplankton absorb
The absorb carbon, when eaten that carbon is passed along the food chain.
Part of that carbon is released through respiration.
Some carbon reaches the sea floor through decomposition and sedimentation.
Threatened by warming oceans.
variations in phytoplankton
Thrive along coastlines and continental shelves.
Found along the equator in the Pacific and Atlantic Oceans.
Thrive in high latitude areas.
why do phytoplankton thrive in certain areas
Oceans rich in nutrients from deep water upwelling.
In high latitudes blooms peak in spring and summer when sunlight increases.
In subtropical oceans blooms decrease because surface waters warm up and become buoyant, with cold, dense water below the water not mixing easily, meaning nutrients are quickly used up.
what is the fastest part of the carbon cycle
terrestrial (land based) sequestration
globally what are the most productive biomes
tropical forests and savanah grasslands
what happens in terrestrial sequestration
Primary producers (plants) take in carbon through photosynthesis and then release CO2 back into the atmosphere through respiration.
Consumer animals then eat these plants and absorb the carbon which becomes part of its fats and proteins.
Initially after the animal has died, microorganisms and detritus feeders such as beetles feed on waste material which becomes part of these micro-organisms.
After death, tissues decay into the soils. This process is affected by climate and decomposition will happen fastest in tropical climates (warm and damp) or, in Arctic biomes, the process can be ‘locked down’ for substantial time periods.
what is 95% of a trees biomass made up of
95% of a tree’s biomass (leaves, branches, trunk and roots) is made up from thee CO2 that it sequesters and converts into cellulose.
what does carbon fixation do
turns gaseous carbon into living organic compounds that grow.
what % of global carbon do soils store
20-30%
sequestering about twice the quantity of carbon as the atmosphere and three times that of terrestrial vegetation. Whether the soil sequesters or emits C02 depends on local conditions.
what factors affect carbon sequestration in soils
climate
soil type
management and use of soils
how does climate affect carbon sequestration in soils
This dictates plant growth and microbe activity. Rapid decomposition occurs at higher temperatures or under water logged conditions. Places with high rainfall have an increased potential carbon storage than the same soil type in lower rainfall places. Arid soils store only 30 tonnes per hectare compared with 800 tonnes per hectare in cold regions.
how does soil type affect carbon sequestration in soils
Clay-rich soils have a higher carbon content than sandy soils as clay protects carbon from decomposition.
how does management and use of soils affect carbon sequestration in soils
Since 1850, soils globally have lost 40-90 billion gigatons of carbon through cultivation and disturbance. Current rates of carbon loss due to land-use change are 1.6 ± 0.8 billion gigatons of carbon per year.
what happens to 31% of short wave radiation
reflected by clouds, aerosols and gases in the atmosphere and by the land surface.
what happens to the other 69% of short wave radiation
absorbed, particularly by the oceans.
what happens when long wave radiation is reflected back
a large amount is re-radiated back to Earth by clouds and GHGs which traps the long wave radiation in our atmosphere.
what does the natural greenhouse effect do
gives us our life supporting average temperature of 15 degrees. Without this effect our average temperature would be -6.
holocene period
The present geological time we are living in is called the Holocene period but many people refer to it now as the Anthropocene because of the profound changes caused by humans.
how has the enhanced greenhouse effect affected c02 levels
The natural greenhouse effect has become enhanced; C02 in the atmosphere has increased in volume by 40% in the last 300 years.
causes of green house gases
industry
agriculture
electricity generation
transport
cement production
wetland/peatland loss
how does industry create greenhouse gases
combustion of fossil fuels
how does transport create greenhouse gases
c02 emmisions
how does agriculture create greenhouse gases
livestock-methane
deforestation- farm land
loss of soil carbon from ploughing
how does elecrticity generation create GHGs
increased demand due to rising population
how does cement production create GHGs
The most consumed product in the world after water.
Chemical processes involved in production release a substantial amount of carbon dioxide (6% of global carbon emissions).
how does wetland/peatland loss cause GHGs
The nature of wetlands is shaped by water and rainfall patterns – the unpredictable change due to climate change may result in wetlands drying out.
Peatlands store 550Gt of carbon – twice as much as all of the world’s forest biomass combined but only cover 3% of the earth’s surface.
how has human activity affected carbon distribution
Through burning fossil fuels we have transferred considerable amounts of carbon from fossil stores, where exchanges are very slow, into the fast category, significantly disturbing the carbon cycle.
CO2 levels in the atmosphere are higher than ever before.
This process has continued since the Industrial Revolution (1760-1840) and accelerated through the oil age (20th century), changing the chemistry of the atmosphere.
how have climate patterns- temperature and precipitation distribution affected carbon levels
Carbon dioxide and other GHGs naturally help to maintain the Earth’s temperature – and also determines the distribution of temperature and precipitation.
If the concentrations of these change, it is likely to alter these distribution patterns.
how is temperature distributed
The amount of solar energy (solar insolation) reaching the Earth’s surface varies at different locations which in turn influences temperature.
The angle of the sun’s rays makes solar insolation intense at the equator but dispersed over a wider area at the poles.
Different characteristics of the Earth’s surface (how light or dark it is) also affects how much heat is absorbed or reflected.
how is precipitation distributed
The heating of the atmosphere and surface controls the temperature, pressure, movement and moisture content of the air.
Because solar radiation is most intense at the equator, low pressure systems dominate there, meaning rainfall all year round.
Regional and seasonal variations also occur, because of the effects of relief, pressure patterns and wind systems.
what happens in the enhanced greenhouse effect
1) short wave radiation passes through the atmosphere
2) some long wave radiation is reflected back into space
3) some short wave radiation is absorbed and is converted to long wave (heat) radiation
evidence of climate change
The IPCC (Intergovernmental Panel for Climate Change) has been collecting evidence of natural changes of heat sources such as volcanism, solar changes and orbital changes such as the Milankovitch cycle and none of these can account for recent changes.
how do we know that c02 levels in the atmosphere are higher than ever before
compared with air bubbles found in ice cores up to 800,000 years ago
what is the primary energy source driving modern civilisation
fossil fuels
what does fossil fuel combustion create
fast carbon cycling
Without it, the carbon in the fossil fuels would transfer slowly through volcanic activity.
between 1750 and 2011 how much did the IPCC estimate concentratio of c02 in the atmosphere would increase by
40%
With approximately 50% of those emissions still in our atmosphere today.
how long does carbon remain in the atmosphere for
2000 years
so c;limate change will continue
what is the combustion of fossil fuels linked to
linked greenhouse gas concentrations, rising global temperatures and sea levels.
what are the three main areas fossil fuel combustion impacts on
climate
ecosystems
hydrological cycle
what was the hottest year on record
2015
average world temperature 1 degrees C above that of pre-industrial era; 2011 -2015 were the five hottest years on record.
how does climate change affect marine biodiversity
Marine biodiversity may be lost as fish move away from warming sea temperatures and about 80% of coral reefs could be bleached (e.g. Great Barrier Reef).
how does climate change affect permafrost
Permafrost areas will thaw and add more water to Arctic rivers.
how does climate change affect drought
The Sahel, Mediterranean, South Africa and South Asia will become drier, with drought more common in the tropics and subtropics – but some uncertainties remain due to other factors (El Nino).
how does fossil fuels impact oceanic circulation
Atlantic and Southern Ocean thermohaline circulation may weaken, altering the transfer of heat by oceans.
how does fossil fuels and climate change impact flash flooding
Uncertainty remains over increased river flooding, since multiple factors are involved, but more flash flooding is likely as a result of more intense precipitation.
by what year are shifting temperatures going to impact bird habitats
By 2080 shifting temperatures may reduce bird habitats in North America, affecting 314 species, with ocean and coastal habitats affected the most, also partly because of coastal flooding and salt encroachment).
habitat changes will mean that what % of land species with limited adaptability will face extinction
10%
as climate gets warmer and wetter or drier
Rates of extinction could rise to 15-40% of all species, especially in high polar regions.
what will a shift of subtropical high pressure areas northwards cause
cause a 20-30% decrease in water availability in Mediterranean climate zones.
how will fossil fuels and climate change affect ice shelves
Antarctic ice shelves will melt, adding more freshwater to the Southern Ocean, changing density and convection.
how has fossil fuels and climate change impacted average arctic temperatures
average Arctic temperature has already increased at twice the global average over the last 200 years. Snow and ice cover will contract with the ablation of glaciers.
how does climate change affect humidity levels
Humidity levels in the atmosphere will increase, consistent with what warmer air can hold.
how will fossil fuels and climate change impact precipitation
Precipitation will increase in higher latitudes and decrease in lower latitudes. Worldwide patterns will change, with wetter eastern parts of N/S America, northern Europe and northern/central Asia.
Extreme heavy precipitation events will become common, with precipitation increases over northern-hemisphere land areas.
how will climate change affect cold and warm days
The number of cold days and nights will decrease, and warm ones will increase. There have been fewer extreme cold events over the last 50 years, but more extreme heat events.
how will climate change affect biodiversity
Biodiversity will be affected as habitats shift poleward or into deeper ocean waters or higher altitudes. In north Brazil and central-southern Africa, lower rainfall and soil moisture, which causes changes to soil and oxygen will reduce biodiversity. Permafrost will thaw.
Acidification of sea water (carbonic acid) will threaten corals and the shells of marine creatures will get smaller and thinner.
Butterflies are a good example of the shift northwards of climate zones (6.1 km per decade).
climate negative outcomes to stores and pathways of carbon
Atlantic and Southern Ocean thermohaline circulation may weaken, altering the transfer of heat by oceans.
Antarctic ice shelves will melt, adding more freshwater to the Southern Ocean, changing density and convection.
Extratropical low-pressure system (depression) tracks will move northwards with climate pattern shift.
Temperate and tropical zones may experience stronger storm activity because of more heat and moisture in the atmosphere.
ecosystems negative outcomes to stores and pathways of carbon
Biodiversity will be affected as habitats shift poleward or into deeper ocean waters or higher altitudes. In north Brazil and central-southern Africa, lower rainfall and soil moisture, which causes changes to soil and oxygen will reduce biodiversity. Permafrost will thaw.
By 2080 shifting temperatures may reduce bird habitats in North America, affecting 314 species, with ocean and coastal habitats affected the most, also partly because of coastal flooding and salt encroachment).
hydrological cycle negative outcomes to stores and pathways of carbon
A shift of subtropical high-pressure areas northwards will cause a 20-30% decrease in water availability in Mediterranean climate zones.
Small glaciers will disappear (e.g. in the Andes and Himalayas), decreasing river discharges once they have gone.
what is an energy mix
The energy mix of a country is the proportion of each primary energy resource it uses per year. These resources may be domestic or imported.
non renewable (finite) energy mix
E.g. coal, oil and gas. Exploitation and use of these stocks will lead to their exhaustion.
renewable energy mix
E.g. solar, wind and wave power.
These are continuous flows of nature and can be constantly re-used.
recyclable energy mix
E.g. reprocessed uranium and plutonium from nuclear power plants and heat recovery systems
what factors affect energy mixes
Availability of primary energy resources within the country as well as their access to technology to extract the resources.
The accessibility of primary energy resources from outside the country.
The energy needs of the country, based on economic development, lifestyle and climate.
changing energy consumption patterns, linked to population and economic growth.
National and regional policies that affect energy production and consumption e.g. climate change.
Cultural and historical legacies and geopolitical links.
Financial costs of each energy option.
eg of how The energy needs of the country, based on economic development, lifestyle and climate affect the energy mix
US – consumerist lifestyle meaning higher demand. Plus hot/cold climate meaning air conditioning and heating required
eg of how The accessibility of primary energy resources from outside the country affects the energy mix
Europe – Russia exports 80% of it’s natural gas to Europe.
eg of how Availability of primary energy resources within the country as well as their access to technology to extract the resources affects the energy mix
Iceland – Domestic geothermal energy
eg of how National and regional policies that affect energy production and consumption e.g. climate change can affect the energy mix
UK – National policies to reduce emissions and invest in renewables
eg of how Financial costs of each energy option affect the energy mix
Countries with little capital e.g. India, consume the cheapest resources, which is currently fossil fuels
eg of how hanging energy consumption patterns, linked to population and economic growth can affect the energy mix
India – population of 1.2 billion meaning high demand
eg of how Cultural and historical legacies and geopolitical links can affect the energy mix
India – struck a deal with Canada for it to provide India with 3.2 million kilos of uranium.
what are the two types of energy
primary
secondary
primary energy
natural energy resources that have not been converted into another form of energy e.g. coal, oil, gas. (Consumed in their raw form)
secondary energy
refers to what the primary source has been converted into, usually electricity.
what % of the UKs energy mix does coal and oil make up
less than 1% combined
what % of the UKs energy mix does natural gas make up
38%
what % of the UKs energy mix does wind make up
20%
what % of the UKs energy mix does biomass make up
12%
what % of the UKs energy mix does solar make up
6%
what % of the UKs energy mix does nuclear make up
19%
why is the UK in an energy deficit and energy insecure
Despite economic and population growth in the UK, the adoption of energy-saving technologies (e.g. home heating and vehicle engines) resulted in the UK consuming less energy in 2015 than in 1998 with more of that energy coming from renewables.
However, the UK now imports more energy than it produces domestically (i.e. from it’s own reserves) due to a decline in the North Sea oil and gas reserves.
what is energy security
being able to access reliable and affordable energy sources – either domestic or from ‘friendly’, overseas countries
europe is dependent on russian gas for what % of its supply
40%
Countries such as Germany are particularly vulnerable (50% - shut down other resources)
what eastern european countries rely solely on russian gas
Moldova and North Macedonia for example. Finland and Latvia rely on it for over 90% of their energy.
what % of the Uks gas supply comes from domestic resources
50%
the other half mostly from Norway.
what % of gas supply did Russian imports make up for the UK in 2021
There are no gas pipelines directly linking the UK with Russia and imports from Russia made up less than 4% of total UK gas supply in 2021.
why does Europe want to wean istelf off russian gas
the aim of Europe to wean itself off Russian gas to make it less of a weapon during conflict.
what does russias economy heavily rely on
fossil fuel exports, so it needs to consider the consequences of this, if it decides to threaten the removal of the supply to Europe.
energy mix
The energy mix of a country is the proportion of each primary energy resource it uses per year.
recyclable energy
A resource that is reused or reprocessed
primary energy
natural energy resources that have not been converted into another form of energy/consumed in raw form
domestic energy
Energy extracted and used within the same country
what are the three types of resources that make up an energy mix
non renewable
renewable
recyclable
what does meeting the demand for energy involve
energy pathways from producer to consumer
energy pathway
describes the flow of energy between the producer and consumer, and how it reaches the consumer, e.g. pipeline, transmission lines, ship, rail etc.
what three objectives does the world energy council suggest energy players have
energy security-energy supply must meet demands
energy equity- there must be accessible and affordable energy for all countries
environmental sustainability
how has energy security been threatened during the recent ‘oil age’
geopolitical tension e.g. Arab uprising in North Africa, Arab-Israeli war.
what are the 5 major players in world energy
OPEC
energy companies
TNCs
consumers
governments
what does OPEC stand for
Organisation of the Petroleum Exporting Countries.