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nutrient cycles
In a functioning ecosystem the elements that living organisms need are constantly recycled
These elements are incorporated into biological molecules within the tissues of living organisms, and then released back into the environment when decomposers break down dead or waste matter
Examples of nutrient cycles are:
the nitrogen cycle
the phosphorous cycle
the nitrogen cycle
Nitrogen is present as N2 gas in the atmosphere and within biological molecules, e.g. proteins, in the tissues of living organisms
nitrogen fixation
ammonification
nitrification
denitrification
the nitrogen cycle - nitrogen fixation
N2 gas is converted into ammonium compounds by nitrogen-fixing bacteria; these bacteria can be free-living in the soil, or may live within root nodules of legume plants
Ammonium compounds are converted into nitrates, which are then absorbed by plants and used to build plant proteins
the nitrogen cycle - ammonification
Nitrogen from living organisms is returned to the soil in the form of ammonia by the action of saprobionts such as bacteria and fungi
This ammonia forms ammonium ions in the soil
the nitrogen cycle - nitrification
The ammonium ions in the soil are converted into nitrates by nitrifying bacteria
Nitrosomonas bacteria convert ammonium ions into nitrites
Nitrobacter bacteria then convert nitrites into nitrates
the nitrogen cycle - denitrification
Denitrifying bacteria use nitrates in the soil for respiration
This occurs in anaerobic conditions, such as in waterlogged soil
This process produces nitrogen gas, which returns to the atmosphere
the phosphorus cycle
Plants and animals require phosphorus for production of, e.g.:
phospholipids
nucleic acids (DNA and RNA)
ATP
The phosphorus cycle includes the following processes:
phosphorus in rocks is released into the soil and into water sources in the form of phosphate ions (PO₄³⁻) due to weathering
Phosphate ions are taken up from the soil by plants, or absorbed from water by algae
Phosphate ions are transferred to consumers during feeding
Phosphate ions in waste products and dead organisms are released into the soil or water during decomposition by saprobionts
The phosphate ions can be taken up and used again by producers, or may be trapped in sediments that may turn into phosphorus-containing rock once again
what are saprobionts
organisms that decompose dead and waste organic matter
what do saprobionts do
Examples include fungi and bacteria
Decomposition by saprobionts releases chemical elements, such as phosphorus and nitrogen, from within dead and waste material
The process of decomposition by saprobionts is as follows:
enzymes are secreted onto a food source
extracellular digestion occurs
nutrients are absorbed
Importantly, not all of the products of extracellular digestion are absorbed by saprobionts; some mineral ions remain in the soil where they can be absorbed by plants
what are mycorrhizae
symbiotic relationships between fungi and the roots of plants
what do mycorrhizae do
Fungi form long, thin filaments known as hyphae, which connect with plant roots
The hyphae effectively increase the surface area of the root systems of the plants, increasing absorption of water and inorganic ions
In return the fungi receive carbon compounds, e.g. glucose, from the plant
role in mineral cycling - saprobionts
Decompose dead and waste matter via extracellular digestion, making inorganic ions available to other organisms
Carry out ammonification by converting nitrogen compounds in waste and dead matter into ammonia
role in mineral cycling - nitrogen fixing bacteria
Convert atmospheric nitrogen gas into nitrogen-containing compounds, such as ammonia
role in mineral cycling - nitrifying bacteria
Convert ammonium ions in soil into nitrates then nitrites
role in mineral cycling - denitrifying bacteria
Convert nitrates into nitrogen gas
role in mineral cycling - mycorrhizal fungi
Increase surface area of root systems, helping plants to absorb water and mineral ions from soil
fertilisers
In natural ecosystems, decomposition by saprobionts recycles nutrients from waste and dead organisms back into the soil
In agricultural ecosystems, crops and livestock are harvested and removed, so the nutrients contained in their biomass are not returned to the soil
This disrupts nutrient cycles and can lead to reduced soil fertility
To maintain productivity, fertilisers are used to replace lost mineral ions
natural fertilisers
Natural fertilisers are made from organic matter, such as:
manure
compost
crop residues
sewage
advantages of natural fertilisers
Release nutrients slowly over time, so nutrients are less likely to be washed away into rivers and lakes after rain
Contain organic matter, so can improve soil structure and water retention
disadvantages of natural fertilisers
Contain organic matter, so can improve soil structure and water retention
Nutrient content is variable and harder to control
artificial fertilisers
Artificial fertilisers are made up of inorganic matter in the form of powders or pellets that contain chemical compounds, e.g. ammonium nitrate
advantages of artificial fertilisers
Nutrients are concentrated and easy to apply
Precise nutrient content allows controlled dosing
disadvantages of artificial fertilisers
Are highly soluble in water so can be leached out of soil into rivers and lakes when it rains
Do not improve soil structure
environmental issues caused by fertilisers
Fertilisers are often applied in larger quantities than crops require; as a result, excess mineral ions may remain dissolved in the soil water
These mineral ions can be carried by rainwater into nearby rivers, lakes or streams; this is known as leaching
Leaching is more likely to occur:
after heavy rainfall
when using artificial fertilisers, as the inorganic ions are highly soluble
Leaching is less likely to occur with natural fertilisers as organic matter must be decomposed by microorganisms before minerals become water-soluble
environmental issues caused by fertilisers - eutrophication
Leaching can lead to a process called eutrophication, which occurs as follows:
mineral ions enter water bodies, causing rapid growth of algae at the surface
This is known as an algal bloom
algae block sunlight, which prevents aquatic plants below the surface from photosynthesising
these plants, and eventually the algae, begin to die and dead organic matter accumulates
bacteria decompose the dead matter, respiring aerobically and using up the oxygen dissolved in the water
oxygen levels fall and aquatic animals such as fish and insects can no longer survive