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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