biogeochemical cycle
water cycle
evaporation of oceans lakes and streams+evapotranspiration through leaves of plants where it will now be a gas
carbon cycle
keywords
photosynthesis
respiration
captures light energy using pigments such as chlorphyll and converts low energy substances such as co2 and h20 into high energy carbohydartes such as proteins and lipids
respiration releases energy captured in photysnthesis and uses it to drive metabollic processes
food web
some of the carbs ,proteins and lipids produced by plants are eaten by herbivores
assimilation
plants take it ammonia through roots and we get it from eating it
condesntion in clouds then leads to precipiation
surface run off then occurs and it will return to ocean
released through cellular respiration goes back into atmosphere as carbon dioxide
resovoirs in the carbon cycle
atmosphere
hydrosphere
biosphere
lithosphere
main chemical forms
co2
methane
carbon monoxide
main chemical forms
carbohydrates e.g cellulose , starch
proteins
lipids
main chemical forms
hydrate carbonate ions
dissolved carbon dioxide
main chemical forms
limestone
fossil fuels mainly as carbons and hydrocarbons
how humans affect the carbon cyle
changes in photoysnthesis
deforestation reduces the movement of carbon from the atmosphere into the biomass
afforestation increases the movement of carbon from the atmosphere
marine pollution with toxic materials can reduce phytoplankton populations which reduces absorbtion of dissolved carbon dioxide
climate changeducing area of sea ice will cause less co2 to be removed from the sea . this is because there will be less algae habitats which mean less algae
changes in aerorbic respiration
carbon in DOM is slowly released as co2 by the aeoribic respeiration in soil organsims especially bacteria and fungi . ploughing increases the oxygen supply and speeds the aeroibic decomposition up causing there to be less carbon in the store and an increase in the atmosphere
in the absence of oxygen the respiration by aneoribc soil organisms releases methane gas . this methane is released into the atmosphere it gradually oxidides into co2
aneoribc environments produced by humans
rice padi fields
landfill sites
livestock intestines
carbonic acid concentration in the sea
dissolved co2 is in an equillibrium with carbonic acid which disasociates to form hydrogen carbonate and hydrogen ions . the concentration of the hydrogen ions affects the ph of the sea . an increase in dissoled co2 = increase in ph of sea .
methane may be released by fossilf fuel extractions
sustainable managament of the carbon cycle
conservation of biomass carbon stores
the use of alternatives
carbon sequestration
renewable energy sources and nuclear poweer produce lower co2 emmisions than fossil fuels
habitats such as peat bogs , and forests contain huge stores of carbon . protecting these from exploitation is important to prevent higher co2 releases
large scale tree planting could remove alot of co2 from the atmopshere .once the tree reaches its full sixe there will be no further net storage of carbon but the tree will be resovoir . if the trees are harvested and kept as wood then replanting would provide additional carbon storage as new trees grow
CArbon capture and storage
captures carbon and does not release it into the atmosphere
pre combustion technology
captures carbon before the fuel is used so that the fuel does not release CO2 when burnt .
gasification converts fuel such as coal into gaseous hydrogen and co2 . the co2 can then be removed for strage and the hydron can be distributed for use in vehicles homes or industry , when burnt the exhaust gases contain water vapour but not co2 .
podt combustion tchnology
co2 can be removed from echaust gases of fossil fuel combustion using several methods . dissolving it in solvent , high pressure membrane filtration , cyrogenic seperation
nitrogen cycle
basic summary of nitrogen cycle
animals die
DOM goes into soil
soil then releases into atmosphere
returns from the atmosphere and grows plants
the plants then get eaten. y animals and then the animals die (death and decay and cycle continues
resovoirs in nitrogen cycle
biosphere
lithosphere
hydrosphere
atmosphere
nitrogen gas
oxides of nitrogen
soil - ammonium compounds , nittrates ,nitrites
rocks , minerals contain nitrogen
living organisms -DNA , proteins (celll membranes , hormones and enxymes )
dissolved nitrates and ammonium ions
ionisation- processes such as lightning and meteor trails provide the energy for atmospheric nitrogen
pollution
haber proccess
this is an industrial process that produces ammonia from converting nitrogen and hydrogen . using an iron catalyst at a high temp and high pressure . the ammonia is then nitartes . this used for the manufacture of agricultrual fertilisers
agriculture
the use of nitarte fertilise may increase problems causied by leaching such as eutrophicationif applicatiojn is followed by heavy rainfall or applid close to rivers
drainage of fields wmake soil more aeoribic . this increases the number of aeorobic nitrifying bacteria and reduces the number of aneorobic dentrifying bacteria
NOX are released into the atmospher by combustion processes and may increase the quantity of nitrats washed into the soil by rain
sustainable management
control of combustion processes
control of NOX releases
a reduction in the use of fossil fuels would reduce the amkiunt of NOX reeleased into the atmosphere
managament of biological wastes
the use of Nox release can be controlled by the use of catayltic converters and urea sprays
the decomposotion of bioloigcal wast release ammonium ions as the amino acids in proteins de animate . enzymes produced by the bacteria remove amino groups which dissolve as ammonium ions . can be bad or good dependson where it occurs
surfcae run off can cause the biologic waste to be wsdhed into bodys of waters . the ammonium ions can be converted into nitrates and nitrites which can cause eutrophication .
organic fertilsiers
can be used to increase nutrient and hummus levelsn, these process reduced the bulk of material being used which makes application easier . also produces a fertiliser with a better c:n ratio.
managemtn of soil processes
cultivation of legume crops
crop roattion
minimal use of pesticides that harm soil biota
phosphrous cycle
main processes
absorbtion by roots
plants absorb the phosphates thye will use in metabollic processes , they arent effective of absorbing phosphates so most plnats have symbiotic relationshipss with mycorrixal fungi . they have a high network in the soil which increases the surface area for phosphate absorbtion
decompostion - the break down of the phosprelated proteins in dead organic matter releases phosphates and they are often made soluble by soil microbes which allow them to be absobrbed by plant s
sedimentatin
the phosoprpsu organisms that die and beocme incorporated into sediments may no longer be availble to other organsims such as planktonic organisms that sink to the bottom when they. diie .this reduces the productivity of surface waters of oceans because phodsphours avaialbikity is a limiting factor
proccesses that mobilise phosphorous and make it avauailble to living organisms are often slo
human impacts
mining of phosphate rocks
most phosphorous s mined as alscium phosphate then trested to produce ammonium phopshate which is more soluble
fertiliser use
use of fertilisers mobilises compounds unto the envrionment moresolubly . this increases crop production but can also contribute to eutrohphication
sustainable mamanagemtn
biological waste should be used as fertilisers to maintain phosphate nutrient avaiablity
crop breeding programmes increase the ffiency of phosphate absorbtion by cropds
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