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the carbon cycle includes the movement of molecules that contain
carbon (CO2, gluecose, CH4) between sources and sinks
fossil fuel combustion is
quick and rapid
sedementation and burial are very
slow
burial
over long periods of time pressure of water compress carbon and that contains sediments on ocean floor to sedimentary rock (limestone and sandstone)
is burial a carbon sink or reservoir
a carbon sink bc it takes much longer than extraction and combustion
sedimentation
Calcium carbonate precipitates out on sediment and sits on the ocean floor
direct exchange
co2 moves between atmosphere and the ocean by dissolving into and out of the ocean water at the surface
ocean acidification
happens because currently net into the ocean because of an increase in atmospheric co2
algae and phytoplankton
take co2 out of the ocean using photosynthesis
what organisms make calcium carbonate exoskeletons
coral mollusks, an some zooplankton and also take co2 in order to make calcium carbonate exoskeletons
carbon sink
take in more carbon than it actually releases
examples of carbon sinks
the ocean (algae and sediments) plants and soil
carbon source
release more carbon that it takes in
examples of carbon sources
fossil fuel combustion, animal agriculture, deforestation (releases co2 from releasing gas)
fossil fuels
formed in fossilized remains of organic matter into coal or oil, and their decomposition produces natural gas
photosynthesis
removes co2 from the atmosphere and converts it into glucose and is a co2 sink
cellular respiration
uses o2 to break gluecose down and release energy and releases co2 into the atmosphere
atmosphere in the nitrogen cycle
this is the main nitrogen reservoir
biotic fixation
bacteria that live in the soil and rhizobacteria in root nodules convert N2 into nh3 (ammonia) and is converted into ammoniam (nh4) in soil
rhizobacteria
live in root nodules of legumes (peas, beans) & fix N for them in return for amino acids from the plant
abiotic fixation
lightning converts n2 gas into nitrate (no3) synthetic fixation via fossil fuel combustion converts n2 gas into ammonia (nh3)
how to convert nh3 to nh4
nh3 is put into the soil in order to convert it from nh3 into nh4
assimiliation
plants roots take in nh4 or no3 and incorporate into a new biomass
ammonification
soil microbes decomposers convert organic n (waste biomass) into ammonium (nh4) soil
nitrification
aerobic bacteria convert nh4 into nitrite (no2) and then nitrate (no3)
denitrificaiton
bacteria in anaerobic conditions convert nitrate (no3) into n2 gas which returns to the atmosphere
leaching and eutrophication
synthetic fertelizer use leafs to nitrates (no3), leaching, or being carried out of soil by water
phosphorus sources
rocks and ocean sediments are the biggest reservoirs
major natural source of P
weathering of phosphorous containing rocks by wind and rain
assimilation and excretion/decomposition
p is absorbed by plant roots and assimilates into tissues and animals assimilate P by eating plants and other animals
decomposition of P
animal waste, pplant matter, and other biomass is broken down by bacteria/soil decomposers that return P to the soil
geological uplift of P
tectonic plate collision forcing up rock layers that form mountains
huamn sources of P
mining phosphate minerals and adding to products like synthetic fertelizers and detergent/cleaners
step one of eutrohpication (nitrogen and phosphorous)
algae bloom covers the surface of the water and blocks sunlight which ends up killing plants below the surface
step two of eutrohpication (nitrogen and phosphorous)
algae eventually will die off and bacteria that break down dead algae use up o2 in the water (because decomposition is an anaerobic process)
step three of eutrohpication (nitrogen and phosphorous)
levels of dissolved oxygen in water kills aquatic animals especially fish
step four of eutrohpication (nitrogen and phosphorous)
because use up even more o2 to decompose dead aquatic animals