Bio 20-1 chapter 3, cycling matter in the biosphere

  1. Abiotic factors that regulate decomposition
    • -Time
    • -Temp
    • -Water
    • -Oxygen
    • -Fire
  2. 2 phosphorus cycles
    1.Rain causes tiny rocks to peel off mountains and roll into rivers, which lead into runoff lakes. This creates a phosphate solution, with new rocks from sedimentation going to the top

    2.Plants absorb phosphorus from soil, then are decomposed or eaten, decomposers then put the phosphorus back into the soil.
  3. The phosphorus cycle
    Phosphorus is an essential nutrient found in DNA. Does not go through the atmosphere
  4. The problem with fertiliser
    causes algal blooms which block out sunlight for plants, resulting in less o2
  5. 4 types of bacteria in the nitrogen cycle
    • 1.Nitrogen Fixing bacteria: turns nitrogen gas and ammonia into Nitrates
    • 2.Legume bacteria: bacteria on the roots of legume plants, turns nitrogen gas into nitrates
    • 3.nitrifying bacteria: turns ammonia and ammonium into nitrites then nitrates
    • 4. Denittrifying bacteria: turn no3 in the soil back into nitrogen gas
  6. Aerate
    Allowing oxygen into your lawn to stop denitrifying bacteria. (it hates oxygen). This keeps the lawn green.
  7. Denitrification
    NO3 in the soil is converted back into nitrogen gas by denitrifying bacteria
  8. Nitrification
    Ammonium and Ammonia in the soil is converted to nitrites (NO2) and then into nitrates (NO3) by nitrifying bacteria
  9. Ammonification
    Dead Plants and Animals are decomposed and return to the soil as NH3(ammonia) and turned into NH4(ammonium) by bacteria.
  10. Assimilation
    Nitrogen gas absorbed into soil is converted into ammonium (NH4) which is then taken by plants and turned into NO3
  11. 3 ways to fix nitrogen(make it useful)
    • 1.Lighting fuses nitrogen gas with h2o, making nitrates
    • 2.Nitrogen gas is absorbed into soil, and then is turned into nh4, ammonium which is taken by plants and turned into no3 (assimilation)
    • 3.Nitrogen gas is absorbed by soil and the bacteria on legume plants and is turned into no3 for the plant to use.
  12. Nitrogen Gas
    Found mostly in the atmosphere, but is a useless substance. It can be absorbed by soil and changed by bacteria to create no3, useful
  13. Earth's carbon balance in the past
    Usually, carbon dioxide levels change little year to year, originally however, earth's atmosphere was high in co2. Along with this, the earth's temp would be very high, this was because the first living organisms consumed co2 and made methane. The greenhouse gases got so high, they began to block the sunlight, resulting in a decreases of methane, balancing things out. This created room for photosynthetic bacteria, which gave us o2 to breathe
  14. Albedo Effect
    How much a surface reflects light back into the sky, dark things absorb more, light things reflect. Snow and ice have high albedo, without them, the earth will heat up more (forests also have a high albedo)
  15. Sink V. Sources
    A sink is where we store carbon dioxide that's out of the atmosphere. A source releases it back into the atmosphere
  16. Bogs
    A sink for organic carbon, has little decomposition due to acid.
  17. Organic carbon reservoirs
    Stored in the bodies of organic things, when we die and decompose, the carbon is returned to the cycle as inorganic
  18. Inorganic carbon reservoirs
    Stored in the earth's atmosphere and oceans
  19. Inorganic carbon
    (carbon dioxide) released from cellular respiration, turned into organic carbon through plants and animals
  20. Organic Carbon
    Found in plants and animals, turned into co2(inorganic carbon during cellular respiration)
  21. Acid Rain
    Rain made from carbon monoxide released into the atmosphere, it kills fish, plants and soil bacteria
  22. The burning of fossil fuels
    Releases carbon monoxide along with sulfur dioxide and nitrous oxide into the atmosphere. This causes acid rain
  23. Most of our water is
    groundwater
  24. Leaching
    As water flows through soil, it absorbs its nutrients
  25. Groundwater
    Underground water
  26. Bedrock
    Where water can flow underground no more
  27. Transpiration
    Water being evaporated through tiny pores on leaves.
  28. Percolation
    The force that pulls water molecules down in the earth, and the speed in which it travels through a substance. A substance with bigger chunks is easier to move through.
  29. Water Adhesion
    allows water molecules to stick to other surfaces without bonding (water droplets)
  30. Water Cohesion
    force that pulls water molecules together
  31. Water has high melting and boiling points because
    it takes alot of energy to break the hydrogen bonds
  32. Frozen water floats
    Most substances solid version is heavier than the liquid version.
  33. Water is a ____ molecule
    A polar molecule, one side is positive, and the other negative
  34. Water Properties
    • 1.Water exists in all three states
    • 2.Frozen water floats
    • 3.Water has high melting and boiling points
    • 4.Water has high surface tension
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Bio 20-1 chapter 3, cycling matter in the biosphere
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