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Nutrient Cycles

Nutrient Cycles. Nitrogen and Phosphorus. WHY DO WE NEED NITROGEN??. Nitrogen is needed to make up DNA and protein! In animals, proteins are vital for muscle function. In plants, nitrogen is important for growth. NITROGEN. Nitrogen “stores” Largest store = atmosphere (N 2 )

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Nutrient Cycles

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  1. Nutrient Cycles Nitrogen and Phosphorus

  2. WHY DO WE NEED NITROGEN?? • Nitrogen is needed to make up DNA and protein! • In animals, proteins are vital for muscle function. • In plants, nitrogen is important for growth.

  3. NITROGEN Nitrogen “stores” Largest store = atmosphere (N2) Also stored in.... • Oceans • Organic matter (in soil)

  4. NITROGEN PROBLEM! 78% of the planet’s Nitrogen is N2 (atmosphere) there are 3 main ways that nitrogen is made available to plants/ animals.... Most organisms CANNOT use N2! SOLUTION:

  5. #1 – Nitrogen Fixation • This is a process that changes N2 into forms that plants can use! N2 NO3- NH4+ (nitrate) (ammonium) Happens in atmosphere... LIGHTNING! Happens in soil, and in water bodies

  6. N2 NO3- Lightning provides the energy for nitrogen to react with oxygen in the atmosphere!

  7. N2 NH4+ Nitrogen-fixing cyanobacteria in water can also do this! Nitrogen-fixing bacteria in the soil can convert (“fix”) N2 to ammonium. Usually live on roots of legumes and other plants. In the water In the soil Rhizobium Video

  8. Nitrogen fixing bacteria In the soil – are an example of SYMBIOSIS!! • These bacteria grow on the root nodules of legumes like peas. • The plants provide sugars, while bacteria provide nitrogen ions.

  9. #2 – Nitrification and #3- Uptake In the soil, nitrifying bacteria convert: NH4+ NO2-  NO3- Nitrate can be taken up by plant roots! (Uptake) So, plants that don’t live with nitrogen fixing bacteria, can also get nitrogen from the soil.

  10. The Nitrogen Cycle How does N2 get back to the atmosphere? Denitrification = changes NO3- back to N2 This occurs in aquatic and land ecosystems by denitrifying bacteria

  11. Excess nitrogen dissolves in water, enters the waterways, and washes into lakes and oceans. The nitrogencompoundseventually becometrapped insedimentary rocksand will not bereleased againuntil the rocksundergo hundredsof years ofweathering.

  12. The Nitrogen Cycle

  13. Human activities can also affect the nitrogen cycle. • Due to human activities, the amount of nitrogen in the ecosystem has doubled in the last 50 years. • Burning fossil fuels and treating sewage releases nitrogen oxide (NO) and nitrogen dioxide (NO2). • Burning also releases nitrogen compounds that increase acid precipitation in the form of nitric acid (HNO3). Acid rain damaged these trees

  14. Agricultural practices often use large amounts of nitrogen-containing fertilizers. • Excess nitrogen is washed away, or leaches, into the waterways. • This promotes huge growth in aquatic algae called algae blooms. • Algae blooms use up all CO2 and O2 and block sunlight, killing many aquatic organisms. • Algae blooms can also produce neurotoxins that poison animals.

  15. A nice summary...

  16. The Phosphorus Cycle • Phosphorus is essential for life processes in plants and animals. • Phosphorus is a part of the molecule that carries energy in living cells = ATP (cellular respiration)!!

  17. The Phosphorus Cycle • How do plants and animals use phosphorus? PlantsAnimals (humans) Developing healthy seeds, root growth, and stem strength! Developing healthy bones (works with Ca to build bone tissue) Corn with a Phosphorus deficiency

  18. Where do we find P? • It is not stored as a gas in the atmosphere like C and N.... • P is stored in phosphate rock and sediments on the ocean floors (Phosphates: PO43-, HPO42-, and H2PO4-)

  19. How it gets from rock  soil Phosphorus is released from rock into the soil by a process called “weathering” CHEMICAL PHYSICAL • Acid rain • Chemical in • lichens • Wind, rain, • freezing Weathering = rock breaks down into smaller pieces. These pieces make their way into the soil.

  20. The Land Cycle • Plants take up phosphate through their roots • Animals eat the plants (get phosphate) • Decomposers return it to the soil

  21. The Aquatic Cycle • Phosphate gets into the water by erosion, leaching, run-off • Most settles at the bottom (turns into sediment) • Some phosphate is taken up by aquatic plants

  22. Geological Uplift • Mountains and hills are created when rock gets “uplifted” • The earth’s crust folds (very slowly) and deeply buried rock layers rise up Mt. Everest is made of limestone that must have originally formed on ancient sea floor. It contains fossils of marine creatures.

  23. This is a rock in Scotland. Below the yellow line was once horizontal rock. It has been uplifted over time. It has now started to erode due to weathering.

  24. Human Activity & the P Cycle • We affect the P cycle by: • Mining phosphate rock (for fertilizers and detergents) • Making fertilizers and detergents (industrial waste) • Applying fertilizer to land • Fishing (remove aquatic organisms – small effect)

  25. A Nice Summary

  26. How Changes in Nutrient Cycles Affect Biodiversity • Any significant changes to any of these nutrients (C, H, O, N, or P) can greatly affect biodiversity. • Carbon cycle changes contribute to climate change and global warming. • Slight temperature fluctuations and changes in water levels can drastically change ecosystems. • Changes influence other organism in the food webs.

  27. How Changes in Nutrient Cycles Affect Biodiversity • Increased levels of nitrogen can allow certain plant species to outcompete other species, decreasing resources for every species in the food webs. • Decreased levels of phosphorus can inhibit the growth of algae that are very important producers in many food chains.

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