Topic 6: The Carbon Cycle and Energy Security Flashcards
(20 cards)
carbon sequestration
the removal and storage of carbon from the atmosphere, usually in oceans, forests and soils through photosynthesis
photosynthesis
the use of energy from sunlight to produce nutrients from carbon dioxide and water
natural greenhouse effect
the warming of the atmosphere as gases such as CO₂, CH₄ and water vapour absorb heat energy radiated from the Earth
enhanced greenhouse effect
the increase in the natural greenhouse effect, said to be caused by human activities that increase the quanitity of greenhouse gases in the Earth’s atmosphere
tonnes of oil equivalent
a unit designed to include all forms of energy by comparing them with oil in terms of heat output - it measures each type of energy by calculating the amount of heat obtained by burning one tonne, and then converting it to however much oil would be required to produce an equivalent amount of energy
energy security
being able to access reliable and affordable sources of energy which may be domestic, but could also include energy sources from ‘friendly’ countries
energy pathway
the flow of energy between a producer and a consumer, and how it reaches the consumer, e.g. pipeline, transmission lines, ship, rail
transit state
a country or state through which energy flows on its way from producer to consumer
bio-geochemical carbon cycle
the continuous transfer of carbon from one store to another, through the processes of photosynthesis, respiration, decomposition and combustion
biological carbon pump
where phytoplankton in the oceans sequester carbon dioxide through the process of photosynthesis, pumping it out of the atmosphere and into the ocean store
biological decomposers
organisms such as insects, worms and bacteria which feed on dead plants, animals and waste
biologically derived carbon
carbon which is stored in shale, coal and other sedimentary rocks
carbon capture and storage (CCS)
the technological ‘capturing’ of carbon emitted from power stations
carbon fixation
turns gaseous carbon (CO₂) into living organic compounds that grow
energy mix
the range and combination of sources required to supply a country with energy
geological carbon
carbon which results from the formation of sedimentary carbonate rocks (limestone and chalk) in the oceans
ocean acidification
the process of the ocean’s pH decreasing as the level of CO₂ in the ocean increases
long-term slow geological cycle
- volcanic out-gassing, releases terrestrial carbon into atmosphere as carbon dioxide
- carbon dioxide combines with rainfall to produce weak carbonic acid/acid rain, dissolves carbon-rich silicate rocks, releases bicarbonates (chemical weathering)
- rivers transport weathered carbon/calcium sediments to oceans (deposition)
- carbon in plants and animal shells/skeletons sinks to ocean bed when they die, strata of coal/chalk/limestone build up
- carbon-rich rocks subducted along plate boundaries, intense heating creates metamorphic rocks and this process releases carbon dioxide
short-term fast biological cycle
- phytoplankton sequester atmospheric carbon during photosynthesis in surface ocean waters
- carbonate shells/tests move into the deep ocean water through the carbonate pump and action of the thermohaline circulation
- terrestrial primary producers sequester carbon during photosynthesis
- some of this carbon is returned to the atmosphere during respiration by consumer organisms
- biological carbon can be stored as dead organic matter in soils, or returned to the atmosphere via biological decomposition over several years