Carbon Flashcards
Fast carbon cycle
Circulates between 10 to 1000 times times faster than the slow carbon cycle
Plants absorb co2 by photosynthesis
Co2 is released back into the atmosphere by plant and animal respiration
Co2 and methane are released back into the atmosphere by decomposition of dead organic matter by microbial activity
Gas exchange occurs between the the atmosphere and the oceans ( atmospheric c02 dissolves in ocean surfaces waters while the oceans ventilate co2 back into the atmosphere through respiration.
Through this, individual carbon atoms are stored in oceans by natural sequestration for 350 years
Fast movement between the soil, vegetation and atmosphere.
Slow carbon cycle
Movement of carbon between rock stores, atmosphere and oceans by weathering over millions of years
Carbon is stored in rocks, sea -floor sediments and fossil fuels.
Betweeen 10-100 million tonnes of carbon is circulated by the slow carbon cycle a year.
Weathering of rocks on continents creates a net carbon sink in the oceans
Chemical weathering of rocks by carbonic acid produces carbonate run-off which gets transferred to oceans
Used to make shells on marine organisms such as clams and corals ( fixes carbon with with calcium calcium carbonate)
Organisms die - remains sink to ocean floor
Carbonate sediment produced forms limestone through heat and pressure - held in rocks for 150 million years
Long term carbon store is released to the atmosphere by volcanic eruptions through subduction into the upper mantle by at tectonic plate boundaries.
Carbon availability by the natural world and humans
Stores : carbonate rocks ( limestone) ,atmosphere, oceans,see floor sediments and the biosphere
Large molecules are built from carbon molecules eg, proteins,carbohydrates and nucleic acids
Contained in fossil fuels = economic resource powering the global economy and oil used for the manufacture of certain products
Agricultural crops and forest trees, human use of food,timber, textiles
Is the carbon cycle open or closed
Global scale = closed with only energy passing the boundary not matter
Local scale = open with materials and energy moving between system boundaries eg, forest ecosystem
Atmospheric carbon cycle
Co2 and methane
Methane is a powerful greenhouse gas but is short lived in the atmosphere
Co2 is removed from the atmosphere through terrestrial and oceanic interactions such as photosynthesis and water absorption.
Co2 levels in the atmosphere are the highest they have ever been in 800,000 years
Oceanic carbon cycle
Dissolved carbon is held in the ocean water and in the tissues of oceanic organisms
Gas exchange move the inputs and outputs with inputs of organic carbon and and carbonate ions from continental run-off
Large store so any changes in the carbon cycling have large global impacts
Long term carbon store - 38,700 Gt store
Use of carbon - flora
Respiration - releases co2 into the atmosphere due to glucose being converted to energy
Photosynthesis - needs co2 to produce glucose
Cycling between atmosphere and biomass
Use of carbon - human and animals
Carbon is present in carbs, protein and lipids
Stable molecule to form bonds for living organisms
Carbon based fossil fuels and wood and trees.