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Conditions that are oxygen poor (lacking oxygen). Not all the fixed carbon in dead plant tissue returns to the atmosphere as CO2: some may be retained as carbon-enriched residue and yet more converted into hydrocarbons.
Wood and other plant materials that can be used as fuels.
Organic compounds of carbon, hydrogen and oxygen, with the general formula CnH2nOn. Glucose, one of the simplest carbohydrates, has the formula C6H12O6.
The movement of carbon between the major natural stores of carbon (called ‘reservoirs’) on the Earth. The two major divisions of the cycle are the terrestrial and marine carbon cycles.
The capacity to do work, measured in joules (J).
The amount of energy stored by a resource relative to the volume that it occupies.
The total energy content of a physical system.
The means by which the direction or speed of movement of an object is changed; equal to mass x acceleration.
Combustible resources derived from ancient organisms, especially coal, oil and natural gas.
Organic compounds, such as methane, that contain only hydrogen and carbon.
Marine carbon cycle
That part of the carbon cycle that involves the circulation of carbon in seawater through biological activity and inorganic processes.
CH4; a gaseous hydrocarbon that is the main component of natural gas.
The force that gives a mass of one kilogram (kg) an acceleration of one metre per second per second (m s−2), and is therefore equivalent to 1 kg m s−2.
Energy resources that are replenished naturally over extended timescales of thousands or millions of years. As they are exploited faster than they are replenished they are considered as non-renewable.
Photovoltaic (PV) effect
The average time that carbon stays in a reservoir before moving to another reservoir, estimated by the amount in the reservoir divided by the transfer rate.
Terrestrial carbon cycle
That part of the carbon cycle involving biological and inorganic processes on land.
Tonne oil equivalent (toe)