carbon cycle Flashcards
What are the 3 types of stores?
Terrestrial, oceanic, atmospheric
What are the 6 important fluxes and stores in the geological carbon cycle?
1) terrestrial carbon held within the mantle is released into the atmosphere as CO2- outgassing
2)Co2 within the atmosphere combines with rainfall to produce a weak acid that dizzolves carbon-rich rocks, releasing bicarbonates, this is chemical weathering
3) rivers transport weathered carbon and CA sediments to the oceans where they are deposited.
4)Carbon in organic matter from plants and animal shells and skeletons sink to ocean bed building up strata of coal
5)Carbon rich rocks are subducted along plate boundries and emerge again as volcanoes erupt.
6)presence of intense heating along subduction plate boundries metamorphoses sedimentary rocks by creating metamorphic rock releasing CO2
How much CO2 did EFG emit in 2010?
Emitted between 150,000 and 300,000 tonnes of Co2 per day- same a portragal but contributed less than 0.3% of global emissions of GHG in 2010.
What is the bio-geochemical carbon cycle?
Involves 4 main processes; photosynthesis, respiration, combustion and decomposition- co2 released into soil or deposited on sea floor.
What are the 3 forms of carbon?
inorganic- rocks such as bicarbonate
organic- found in plant material
gaseous- found as co2 and CH4 and CO
How much pentagrams of carbon do oceans, earths crust atmosphere and soils store?
Atmosphere- 750pg
earths crust- 100,000,000pg
oceans- 38,000pg
soils-1500pg
How much of CO2 produced goes into different stores?
15-20% of co2 goes into biosphere, 55% of co2 goes into the atmosphere, 25% to 30% of Co2 goes into the ocean.
What is the biological carbon pump?
transfers 4 to 15 gt of carbon from the atmosphere to the deep ocean as showed. Oceans surface layer contain tiny phytoplankton containing cholorphyll and absrbong sunlight to live. Also have shells and sequester CO2 through photosynthesis creating calcuim carbonate as their shells develop. When die thse carbon rich orgnisms sink to ocean floor accumulating as sediment. Particular proccess known as carbonate pump and is part of the biological carbon pump . Pumps co2 out of atmosphere into the ocean store. Without contributions of phytoplankton, co2 conc in atmosphere would be far higher than it already is.
what threats are there to the biological carbon pump?
Naturally efficent system wbut also fragile. Phytoplankton require nutrients in vast quantities and existing ocean temps and currents maintain a constant supply, recycling of particles deep by upwelling i critical. Global movement of water through thermoshaline circulation maintains pump. However, slight changes in water temp can alter the flow. pollution and turbulance also reduce light penetration and slow pump. Each of these factors vulnerable to CC- making risk of pump breaking down real.
How does the thermohaline circulation work?
> water in the far north atlantic is cold and very saline making it denser and heavier causing it to sink.
> by sinking it draws warmer water in from the ocean surface above. This, in turn draws water from the tropics
> Eventually, this movement from the tropics draws cold water up from the ocean bottom, ready to be warmed again.
Is the gulf stream failing?
During 2004 gluf stream paused for 10 days. Data showed that current slowing with soeed if ocean circ between the gulf of mexico and europe had slowed by 30% since 2000. Hypothesis:
> Melting Arctic ice was increasing the amount of freshwater entering the North Atlantic
> Oceans salinity declining as a result, preventing cold water from sinking
> Meant there was nowhere for the warm waters of the gulf stream to go- north atlantic losing pulling effect.
Slowed by 6million tonnes of water per second over 12 years
What is the role of trees in the carbon cycle?
Growth of vegetation depends on water, nutrients and sunlight. 95% of a trees biomass made up of Co2 that it sequesters and converts into cellulose Carbon fixation turns co2 into living organic compounds. Amount of carbon stored within a tree, woodland or forest depends on the balance between photosynthesis and respiration.
what is the role of mangroves?
Biological carbon stored in soils in the form of dead organic matter or returned back to the atmosphere as a result of decomposition. Depending on the nature of the soil this proccess can be relatively quick or in tundra very slow. But deforestation and land use changes release these stores very rapidly as mangroves show;
Mangrove forests are found aling tropical and sub-tropical tidal coasts in africa, australia, asia and the americas. They are vital processors sequestering 1.5 metric tonnes of carbon per hectare each year mangrove soils consist of thick organic layers of litter,humus and peat containing high levels of carbon- over 10%.
Soils are anaeorbic as they can survive without oxygen. Bacteria and microbes dont survive without O2 so decomposition of plant matter is slow. As a result,little of the carbon can be respired back into the atmosphere, and the store remains intact. Any plant matter trapped by the tree roots tend to stay as it decomposes slowly stored for 1000s of years
however if they are cleared carbon released back into the atm. Throughout trop world mangroves cleared for tourism, shrimp farms and aquaculture. If just 2% of mangroves lost carbon released 50x natural sequestration rate.
What role to tundra soils play in the carbon cycle?
Much of soil in tundra regions are permanently frozen and contain ancient carbon. Microbe activity is only active in surface layer of soil when it thaws. The rest of the time the roots and dead and decayed organic matter frozen, locking in any carbon into an icy store. Tundra soils contain carbon that has been trapped for hundreds of thousands of years.
What is the role of tropical rainforests as carbon stores?
Huge carbon sinks, but fragile. Carbon mainly stored in trees,plant litter and dead wood. Soils are relatively thin and lacking in nutients as litter layer covers them, though very deep, decompose rapidly and nutrients released are rapidly consumed by vegetation.
As litter and dead wood decay, recycled so quickly that a soil store does not develop. Even carbon goven off by decomposers is rapidly recycled. Tropical forests absorb more atm co2 than any other biome, accounting for 30% of net primary production covering just 17% of earths surface. If they died off earth would lose a massive carbon sink.
What is the natural greenhouse effect?
sun is the natural driver of almost all the earths atmospheric energy. Energy is recieved as incoming solar radiation for sun. Dark surfaces absorb this radiation and radiate it back as heat. However, insufficent for life on earth and GHG such as CO2 and CH4 into the atmosphere. absorb and refelct beack radiated heat from earths surface retaining heat and keep earth 16C warmer allowing for life on earth.
What are the 4 main greenhouse gases?
CO2-89% of GHG increased by 30% since 1850
CH4-7% of GHG, 21x more powerful than CO2 increased by 250 % since 1850
N20- 3% of GHG producesd, 250X more powerful, 16% increase since 1850
Halocarbons- 1% of GHG produced, 300x more powerful and not natural.
What is the enhanced greenhouse gas effect?
Concentration of several GHG in the atmosphere have increased by 25% since 1750, when industrialisation began in the UK, and now are increasing faster than ever. Since 1980s 75% of CO2 emissions come from burning of fossil fuels. This had led to the enhanced GHG effect.
Human activities such as burning fossil fuels and deforestation release natural stores of carbon and nitrogen which combine with oxygen to form GHG;
Carbon combines with oxygen to form CO2, nitrogen combines with oxygen to form N20 Increased water vapour caused by more evapotranspiration has lead to increased cloud cover trapping heat in the atmosphere.
How does the enhanced GHG effect affect temperature and precipitation?
> the amount of solar energy reaching the earths surface varies at different locations which in turn influences temperature. Angle of the suns rays make solar radiation intense at the equator but dispersed over a wider area at the poles. Different characteristics of earths surface (albedo) affect refelction/absorption. Heat is redistibuted around the globe by air movement caused by pressure differences and ocean currents.
> precipitation heating of earths atmosphere and surface controls temperature,pressure, movement and moisture content of air. Warm air rises and cools, leading to water vapour & clouds
> Because solar radiation is most intense over the equator, convection and low pressure systems dominate there so rainfall is high all year.
> As air pressure rises around 30 degrees N & S of the equator precip decreases
> in mid latitudes air masses of dif characteristics meet and low pressure systems bring rain
> Nearer the poles, precipitation falls as the air cools further and is dense and dry creating polar deserts.
What is photosynthesis role in regulating the atmosphere?
Phytoplankton in oceans sequester CO2 through the process of photosynthesis- form atm to ocean- biological carbon pump and proccesses transfer 5-15 Gt of carbon from atm to ocean.
Terrestrail photosynthesis enables plants to sequester 100-120Gt of CO2 per year. Then released back into atm through respiration and decomposition.
Anything that affects lvl of phytoplankton in oceans or area of land covered by forest will have an impact of lvl of carbon sequestration. In turn affecting comp of atmosphere.
Tropical rainforests ideal for plant growth promoting photosynthesis.
Marin equivalents of rainforests in terms of plant growth are coral reefs and mangroves. Warm tropical shallow wwaters are ideal for both
Deserts meanwhile are areas of sparse vegetation hence relatively little CO2 absorbed there.
Increased melting of Arctic sea means hreater expenses of ocean exposed to direct sun as seasonal thaws last longer increasing photosynthesis by phytoplankton resulting in agal blooms as more CO2 is absorbed.
Soils role in the carbon cycle?
Carbon is vital is soils, organic material is meduim by which C passes through system, supports micro-organisms that maintain the carbon cycle, breaks down organic matter, provides pore spaces for infiltration and storage of water enhancing plant growth. Withou carbon, nutrient and water cycles cannot operate properly. Amount of carbon stored depends on system;
> amount of organic carbon stored within soil= inputs (plant litter/animal waste) minus outputs (erosion, decomposition and plant growth)
size of store depnds on biome
What are the characteristics of healthy soils?
> dark,crumbly and porous
contain many worm and other organisms
provide air, water and nutrients for microorganisms and plants to thrive
contain more carbon or organic matter
sequester carbon
improve resilience to wetter weather because they enable infiltration and percolation of water
retain moisture regulatinf soil temp reducin effect of drought
In winter more organic deacy increases co2 levels whilst in the spring plant growth reduces levels, if winters shorten possible less CO2 released.