KQ1: How important are water and carbon to life on earth? Carbon Cycle Flashcards
Give reasons why carbon Is important to life on earth
- Carbon is of biological significance, biological molecules such as proteins and carbohydrates are made up of carbon
- Carbon Is used as an economic resource, fossil fuels such as gas and oil are used to power the global economy
▪︎Oil is used as a raw starting material in the manufacturing of many products such as plastics and paints
▪︎Agricultural crops and trees contain mass amounts of carbon and are used for food and textiles .etc
What is the largest carbon store on the planet?
Sedimentary(carbonate) rocks hold up to 99% of all carbon on the planet
How much carbon is stored in the oceans?
Up to 38,700 billion tonnes of carbon, mainly as dissolved CO2
How much carbon is stored in the atmosphere and plants/ soil?
Atmosphere (600 billion tonnes) and plants and soil ( 560 and 2300 billion tonnes), despite being a minute fraction of total carbon store they represent most of the carbon in circulation
what are the 6 principal carbon stores?
▪︎oceans
▪︎atmosphere
▪︎carbonate rocks
▪︎plants
▪︎soil
▪︎fossil fuels
How much carbon is circulated in the slow carbon cycle every year as an estimate?
10 to 100 million tonnes
How are the oceans involved in the slow carbon cycle?
Oceans absorb CO2 from the atmosphere where marine organisms suchas clams and corals make shells and skeletons by fixing dissolved CO2 with calcium to form CaCO3, on death, these sink to the sea floor and over millions of years are though to compress into sedimentary rock by digenesis
How can CO2 be released from rocks?
- Sedimentary rock subducted at the upper mantle near plate boundaries can be vented to the atmosphere by volcanic eruptions.
- Others exposed at or near the surface can be attacked by chemical weathering. E.g. carbonation, where precipitation a weak acid can attack carbonate minerals to release co2 into atmosphere or in dissolved form to the rivers and streams
Explain how carbonaceous rocks such as coal and natural gas form and how they are part of the slow carbon cycle
Partly decomposed organic material can become buried under younger sediments to form carbonaceous rocks, these can act as carbon sinks for millions of years
Between which stores does carbon circulate the fastest, and how much faster is this than the fast carbon cycle?
Atmosphere, oceans, biosphere and soils, the exchanges between these are up to 10 to 1000x faster than slow carbon cycle
Describe how land plants and microscopic phytoplankton are a key component of the fast carbon cycle.
They carry out photosynthesis to absorb Carbon dioxide, this produces carbohydrates, this process is fundamental in the food chain. These also respire (animals do the same), this releases carbon dioxide back into the atmosphere,. Decomposition of dead organic material by decomposers also releases carbon dioxide into the atmosphere as well as into the soil
How does carbon exchange occur between the atmosphere and oceans as part of the fast carbon cycle?
Atmospheric co2 can dissolve into the oceans whilst oceans ventilate them back, through this they can be stored by natural sequestration for a long period of time, the average residence time is around 350 years
what are the 6 main carbon exchanges?
- Precipitation (Polly)
- Photosynthesis (Pets)
- Weathering (white)
- Respiration (rabbits)
- Decomposition (delicately)
- Combustion (carefully)
Explain the role of precipitation as carbon flux and how it’s effects have exacerbated as well as the impacts of this exacerbation.
Precipitation contains dissolved carbon dioxide and this forms a weak carbonic acid, which is a natural process, however rising co2 concentrations by anthropogenic emissions can increase acidity of rainfall, this imbalance could have potentially negative consequences on marine life.
Explain the role of carbon flux in photosynthesis
Land and phytoplankton use co2 from the atmosphere and water to convert light energy to chemical energy, in the form of glucose, this energy is used to maintain growth reproduction and other processes