The Carbon Cycle Flashcards
Slow Carbon Cycle/Geological Carbon Cycle
Terrestrial carbon, held within the mantle, is released into the atmosphere as carbon dioxide this is known as volcanic outgassing
Carbon dioxide combines with rainfall to produce a weak acid (carbonic acid) that dissolves carbon-rich rocks releasing biocarbonates through chemical weathering of SILICATE ROCKS
Rivers transport weathered carbon and calcium sediments to the oceans where they are deposited
Carbon in organic matter 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 the subduction plate boundaries metamorphoses sedimentary rocks by baking, creating metamorphic rocks. Carbon dioxide is released by the metamorphosis of rocks rich in carbonates.
What are the types of carbon?
Inorganic - found in rocks as bicarbonates and carbonate
Organic - found in plant material
Gaseous - found as carbon dioxide, methane or carbon monoxide
Fluxes
Combustion
Decomposition
Diffusion
Sedimentation: e.g when organisms die and there shells sink to the ocean floor and become compacted over time to form limestone
Weathering and erosion
Metamorphosis - extreme heat and pressure forms metamorphic rock, during which some carbon is released
Volcanic outgassing
Is there more carbon dioxide released in the northern or southern hemisphere?
Carbon dioxide fluxes vary with latitude. Levels are always higher in the Northern Hemisphere, because it contains a greater landmass and greater temperature variations that in the Southern Hemisphere.
Himalayas
One of the largest carbon stores is the Himalayas which started off as oceanic sediments rich in calcium carbonate. Folded up by mountain building, this carbon is being actively weathered, eroded and transported back to the ocean.
How is oil and natural gas formed?
Formed from the remains of tiny aquatic animals and plants
Gas and oil occur in ‘pockets’ in rocks migrating up through the crust until meeting caprocks (impermeable rock layers that seal the top of reservoirs)
Natural gas, such as methane is made up of fractions of oil molecules so small they are in gas form not liquid and usually found with crude oil.
Other hydrocarbon deposits include oil shales, tar sands and gas hydrates.
How is coal formed?
Formed from the remains of trees, ferns and other plants
Soft coals such as lignite and brown coal are lower in carbon (25-35%) and energy potential; these are the major global source of energy supplies but emit more carbon dioxide than hard coals
Peat is the stage before coal and it is an important carbon source
How are fossil fuels made?
Made up to 300 million years ago from the remains of organic material, organisms, once dead, sank to the bottom of the rivers and seas, were covered in silt and mud and decayed anaerobically. The deeper the deposit, the more heat and pressure exerted on the deposits.
Carbon sequestered in limestone and sedimentary rock
Shell building (calcifying) organisms (coral) and plankton
These are precipitated onto the ocean floor, form layers are cemented together and turned into limestone
Other rocks contain organic organisms carbon from organic organims that have been embedded in layers of mud over millions of years heat and pressure compress the mud and carbon into sedimentary rock such as shale
Phytoplankton
Phytoplankton (tiny microscopic marine plants) live in the surface ocean although minute their enormous make up half of the planets primary productivity. Phytoplankton absorb carbon by photosynthesis and have rapid growth rates. Fish and other animals eat the phytoplankton and release the CO2.
Carbon in oceans
CO2 reacts with water to make carbonic acid and carbonate ions. Many organisms then use the carbonate ions to make their hard outer shells. When organisms die they either sink to the ocean bed and build up to create limestone or their shells dissolve releasing carbon back into the ocean.
Thermohaline circulation
The main current begins in the polar oceans where the water gets very cold and sea ice forms surrounding sea water gets saltier increases in density and sinks
The current is recharged as it passes Antarctica by extra cold salty, dense water
Division of the main current northward into the Indian ocean and Western Pacific
The two branches warm and rise as they travel northward then loop back southward and westward
The now warmed surface water continue circulating around the globe on their eventual return to the North Atlantic they cool once again
Why are mangroves being cleared?
Mangroves are being cleared for tourism, shrimp farms and aquaculture.
Precipitation at different latitudes
Because solar energy is insolation is most intense over the equator, convection and low pressure systems dominate their rainfall is high all year round
As the pressure rises around 30 degrees north and south of the equator precipitation decreases
In the mid latitudes air masses of different characteristics meet and low pressure systems bring rainfall
Nearer the Poles, precipitation falls as the air cools further and is dense and dry creating polar deserts
Carbon in soils
Carbon stored in soils is vital it supports the micro-organisms and maintains the nutrient cycle break down organic matter, provide pore spaces for infiltration and storage of water, and enhances plant growth.
Urban energy usage
Cities consume 75% of the world’s energy
Manhattan Island in New York is home to 1.7 million people who consume more energy a year than the average Madagscan will in a lifetime
City of London generates 1.8 tonnes of carbon per capita
Rural energy usage
Peru carried out a national programme of solar-panel installation and electricity was made available to 500,000 homes in remote villages across the country.In 2013 only 66% had acess to electricty.
UK case study
Until 1970s relied heavily on coal
Discovery of large gas and oil reserves in North Sea
One of the global leaders of nuclear power 1950s-70s
North sea oil reserves are a viable alternative when Middle Eastern oil price increase however, it is expensive to extract so the UK rely heavily on oil exports
There are currently 150 years left of coal supplies in the UK
However, the UK’s last deep coal mine closed in 2015
Average annual household energy costs for a three bedroom house around £1700 (British gas)
Norway case study
Norway is mountainous with steep valleys and plentiful rainfall and hydro electric power is a good choice
Coal from Svalbard is exported
Norsk Hydro has over 600 HEP sites which supply 97.5% of Norway’s renewable energy
GDP per capita $61,500
Average annual household energy costs £2400 (2015)
OPEC
The organisation of petroleum exporting countries
Between OPEC producers they control 81% of the world’s proven oil reserves
Coal India Ltd
World’s largest coal producer
Nationalised in 1972
80 mining areas and responsible for 5.9% of the world’s coal
Gazprom
Put under state control in 2000
Russian gas exports to Europe have declined from 40% to 9%
Two Nord Stream pipelines built at a cost of over €20 billion lie holed on the bottom of the Baltic. Meanwhile, its share price is down 88 percent since the February invasion and the company in August was spotted flaring large quantities of unsold gas.