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GEOCHEMICAL CYCLES

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Title: GEOCHEMICAL CYCLES


1
GEOCHEMICAL CYCLES LIMITING FACTORS
2
Cycles of Matter
  • While energy is crucial to an ecosystem, all
    organisms need more than energy to survive
  • Water
  • Minerals
  • Life-sustaining compounds
  • For most organisms, more than 95 of the body is
    made up of O, C, H, N
  • These common elements cannot be used by
    organisms unless the elements are in a chemical
    form that cells can take up

3
Recycling in the Biosphere
  • Unlike the one-way flow of energy through an
    ecosystem, matter is recycled within and between
    ecosystems
  • Elements, chemical compounds, and matter are
    passed from one organism to another and from one
    part of the biosphere to another through
    biogeochemical cycles
  • Biogeochemical cycles pass the same molecules
    around again and again within the biosphere

4
Root uptake
5
H2O CYCLE- BOOKLET
  • Evaporation
  • water changes from liquid ?gas
  • Transpiration
  • Water evaporates from leaves of plants
  • Precipitation
  • Ex rain, snow, sleet or hail
  • Runoff
  • The precip runs along the surface of the ground,
    enters a river or stream, carried to an ocean or
    lake

6
Nutrient Cycles
  • Nutrients are the bodys building blocks
  • - Every living organism needs nutrients to grow
    and carry out essential life functions
  • Nutrients, like water, are passed between
    organisms and the environment through
    biogeochemical cycles
  • Because nutrients are in short supply in many
    ecosystems, recycling of nutrients is essential
    for these ecosystems to keep functioning

7
CARBON CYCLE-BOOKLET
  • 4 processes involved with the C cycle
  • Biological
  • ex photosynthesis, respiration and decomposition
  • Geochemical
  • ex release of CO2 to the atmosphere by volcanoes
  • Biogeochemical processes
  • ex burial of C rich remains of organisms and
    their conversion into coal and petroleum
  • Human activity
  • ex mining, burning of fossil fuels and the
    cutting/burning of forests

8
The Carbon Cycle
9
N2 CYCLE-BOOKLET
  • N2 is most abundant, but only certain bacteria in
    the soil and lightning in the atmosphere can
    convert it to a useable form ammonia.
  • This conversion is called NITROGEN FIXATION.
  • When orgs die, decomposers break down the remains
    and return nitrogen to the soil as ammonia.

10
N2 CYCLE-BOOKLET
  • If not taken up by plants, other bacteria in the
    soil convert nitrates into nitrogen gas this
    conversion is denitrification. The nitrogen is
    now back in the atmosphere.
  • ammonia ?nitrate nitrite ions

11
The Nitrogen Cycle
12
Phosphorus Cycle
  • Phosphorus (P)-important (DNA structure), not
    very common in the biosphere.
  • P does NOT enter the atmosphere found mostly in
    rock, mineral form, and ocean sediments.
  • P taken up by plants, eaten by consumers.
  • In the ocean-used by microorganisms, eaten by
    ocean consumers

13
The Phosphorus Cycle
14
Nutrient Limitation
  • The primary productivity of an ecosystem is the
    rate at which organic matter is created by
    producers
  • Factor that control the primary productivity of
    an ecosystem are the amount of available
    nutrients
  • Nutrients in short supply will limit an
    organisms growth
  • When an ecosystem is limited by a single nutrient
    that is scarce or cycles very slowly, this
    substance is called a limiting nutrient

15
Ex. Algal Blooms- aquatic ecosystem
  • When an aquatic ecosystem receives a large input
    of a limiting nutrient, the result is often an
    immediate increase in the amount of algae other
    producers
  • Leads to algal blooms that cover the surface of
    the water if there are not enough consumers to
    eat the producers, the aquatic ecosystem is upset.
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