Carbon, Nitrogen and Phosphorus cycles Nutrient Cycles Carbon, Nitrogen and Phosphorus cycles

Nutrients Nutrients are chemicals that are required for plant and animal growth and other life processes Nutrients are accumulated for short or long periods of time in Earth’s atmosphere, oceans and land masses Scientists refer to these accumulations as STORES Biotic and abiotic processes can cause nutrients to flow in and out of stores  this continuous flow of nutrients are called nutrient cycles

Nutrient Cycles There are 5 chemical elements (nutrients) that limit the amount of life possible in an ecosystem: Carbon Hydrogen Oxygen Nitrogen These four are cycled between living organisms and the atmosphere Phosphorus Enters the environment from sedimentary rock

Carbon Cycle All living things contain billions of carbon atoms in their cells Carbon is an essential component in the chemical reactions that sustain life, such as cellular respiration

Where Carbon is stored Short term carbon stores include: Vegetation on land Plants in oceans Land-based and marine animals Decaying organic matter in soil In the atmosphere as carbon dioxide (CO2) In the top layers of the ocean in its dissolved form

Where Carbon is Stored Long term carbon stores include: In the middle and deep layers of the ocean as dissolved CO2 Coal deposits Oil and gas deposits Coal, oil and gas are fossil fuels that are formed from dead plants and animals Marine sediments and sedimentary rock This is the largest long-term carbon store

Sedimentation Sedimentation = the process that contributes to the formation of sedimentary rock Soil particles and decaying and dead organic matter accumulate in layers on the ground/bottom of the ocean and are turned into rock by slow geological processes over a long period of time

How Carbon is cycled There are several ways in which carbon is cycled through ecosystems, including: Photosynthesis Cellular respiration Decomposition Ocean processes Natural events Volcanoes Large-scale forest fires

Photosynthesis Photosynthesis is a chemical reaction that converts solar energy into chemical energy During photosynthesis, carbon (in the form of CO2 in the atmosphere) enters through the plants and reacts with water in the presence of sunlight to produce carbohydrates and oxygen Energy + 6 CO2 + 6 H2O  C6H12O6 + 6 O2

Cellular Respiration Cellular respiration is the process in which both plants and animals release CO2 back into the atmosphere by converting carbohydrates and oxygen into CO2 and water During cellular respiration, energy is released within the cells of organisms and can be used for growth, repair and reproduction. CO2 gas is released as a waste product C6H12O6 + 6 O2  6 CO2 + 6 H2O + energy

Decomposition Decomposition is the breaking down of dead organic matter Decomposers, such as bacteria and fungi, convert organic molecules (such As cellulose) back into CO2, which is released into the atmosphere

Ocean Currents CO2 dissolves in cold ocean waters found at high latitudes The cold water sinks and moves slowly in deep water currents towards the tropics In the warm tropics, the water rises as it warms and mixes with the middle and top layers of the ocean At the surface, some CO2 is released to the tropical atmosphere while the ocean currents move the warmed water back towards the polar areas

Natural Events Some carbon dioxide is released from volcanoes Some carbon dioxide is slowly released from decomposing trees Some carbon dioxide is rapidly released during forest fires

Human Activities and Carbon Human activities that impact the carbon cycle include: Industry Motorized transportation Land clearing Agriculture Urban expansion Since the Industrial Revolution (1850s) the amount of CO2 in the atmosphere has increased by 30% It only increased ~ 3% during the previous 160,000 years!

Global Warming Human activities that involve burning fossil fuels have reintroduced carbon into the cycle that was removed from it long ago So much carbon is released so quickly that the natural carbon cycle can no longer move all of it into stores CO2 that is stored in the atmosphere (because it has no where else to go) is a greenhouse gas, which contributes to global warming 

Global Warming Clearing land for agriculture and the expansion of cities reduces the total amount of carbon taken from the atmosphere by plants during photosynthesis Farmed plants do remove some carbon from the atmosphere through photosynthesis, but not as much as natural vegetation does

Nitrogen Cycle Nitrogen is an important component of DNA and proteins, which are essential for the life processes that take place inside cells Nitrogen is essential for muscle function in animals and for growth in plants

Where Nitrogen is Stored The largest store of nitrogen is in the atmosphere as nitrogen gas (N2) Other major stores of nitrogen include oceans and organic matter in soil Smaller stores include living organisms, lakes and marshes

How Nitrogen is Cycled Most organisms cannot use nitrogen in the form of N2, so much of the nitrogen cycle involves processes that make nitrogen available to plants and animals Some of these processes include: Nitrogen fixation = when nitrogen gas (N2) is converted into compounds that contain either nitrate (NO3) or ammonium (NH4) Nitrogen fixation occurs in 3 ways: In the atmosphere In the soil In water bodies

Nitrogen Fixation - Atmosphere Nitrogen fixation in the atmosphere occurs when lightning converts N2 into NO3 compounds This NO3 then enters terrestrial and aquatic ecosystems through the rain

Nitrogen Fixation - Soil Nitrogen fixation in the soil occurs when nitrogen-fixing bacteria that lives in the root nodules of legumes and other plants converts N2 into NH4 during decomposition The plants supply the bacteria with food (sugars) and the bacteria supply the host with nitrogen needed for growth

Nitrogen Fixation - Water Nitrogen fixation in water bodies occurs when certain species of cyanobacteria fix N2 into NH4 Nitrogen-fixing cyanobacteria make the nitrogen compounds available to plants in the surface waters of oceans, wetlands and lakes

Nitrification and Uptake Nitrification is when NH4 is converted into NO3 This occurs in two steps: Certain species of nitrifying bacteria in the soil convert NH4 into NO2 (nitrite) Different species of nitrifying bacteria in the soil then convert the NO2 into NO3 (nitrate) Once nitrate is available in the soil it can enter plant roots and eventually be incorporated into plant proteins When these plants are consumed by herbivores and omnivores, they incorporate nitrogen into the proteins in their tissues

How Nitrogen is Returned Nitrogen is returned to the atmosphere in a process called DENITRIFICATION In a series of chemical reactions, denitrifying bacteria convert nitrate (NO3) back into nitrogen gas (N2) Nitrogen is also returned to the atmosphere as ammonia (NH3) in volcanic ash, nitrogen oxide and nitrogen dioxide

How N is removed from Ecosystems NO3 and NH4 that are not taken up by plants mix with rainwater and are washed from the soil into ground water and streams This unused nitrogen may settle to ocean, lake or river bottoms in sediments Eventually these sediments will form rock and the nitrogen will be trapped until centuries of weathering releases it back into the water

Human Activities and Nitrogen Human activities have doubled the available nitrogen in the biosphere in the past 50 years Millions of tonnes of nitrogen are added in the form of NO and NO2 as a result of fossil fuel combustion Clearing forests and grasslands by burning also releases trapped nitrogen into the atmosphere These compounds eventually return to terrestrial and aquatic ecosystems as acid rain (HNO3)  Chemical fertilizers that fix N2 into nitrogen compounds that crops can use are used in agriculture The excess nitrogen that is not used can escape back into the atmosphere or can be washed or leached (leak out of) from the soil and end up in water systems This can can lead to algae blooms, which deprive other aquatic plants of sunlight and oxygen, causing death

Algae Blooms

Phosphorus Cycle Phosphorus is essential for a variety of life processes in plants and animals In plants, phosphorus contributes to root development, stem strength and seed production In humans, a large amount of phosphorus is found in bones

Where Phosphorus is Stored Phosphorus is NOT stored in the atmosphere as a gas  it is trapped in phosphate (PO4, HPO4, and H2PO4) This phosphate is found in phosphate rocks and in the sediments of ocean floors

Where Phosphorus comes from Weathering (the process of breaking down rock into smaller fragments) releases phosphate into the soil Chemical weathering is when a chemical reaction causes phosphate rocks to break down and release phosphate into the soil This can be caused by ACID RAIN or from the chemicals released by lichens

Weathering and Erosion Physical weathering is when processes, such as wind, rain, and freezing, release particles of rock and phosphate into the soil

How Phosphorus is Cycled On land, plants take up phosphate through their roots and animals obtain phosphate by eating the plants Decomposers break down animal waste and dead organisms, returning the phosphorus to the soil to become available to the producers again In aquatic ecosystems, phosphate enters as a result of erosion, leaching, and run-off Water plants take up some dissolved phosphate and pass it through the aquatic food chain

How Phosphorus is Cycled Most phosphate in run-off settles on lake and ocean bottoms This sediment will eventually form sedimentary rock, and the phosphorus will remain trapped for millions of years Only when layers of rock become exposed will the phosphorus become available again when the cycle of weathering begins again

Human Activities and Phosphorus Phosphate rock is mined primarily to make commercial fertilizers and detergents Commercial fertilizers, phosphate-containing detergents, animal waste from large-scale livestock farming, some industrial waste, and untreated human sewage all enter the waterways through run-off and leaching Clearing of forests by the slash-and-burn method releases the phosphates contained in the trees in the form of ash, which accumulates in the soil and leaches into run off and settles on ocean bottoms and eventually becomes locked up as sedimentary rock

Human Activities & the P Cycle Slash-and-burn causes phosphate to leach from the ash and run off into the water supply to settle on the bottom of water bodies where it becomes unavailable to organisms Fertilizers, detergents, manure, waste and sewage contributes additional phosphate to the phosphorus cycle, unbalancing it Too much phosphorus can negatively affect species that are sensitive to an overload of this nutrient – this can lead to animal death (example: overload of phosphorus in the water can lead to toxic levels in fish that kills them)