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CYCLING OF
  MATTER
• ENERGY FLOWS THROUGH ECOSYSTEM
• WATER—NITROGEN—CARBON—PHOSPHORUS ARE
  RECYCLED!!!
• THEY MOVE THRU A BIOGEOCHEMICAL CYCLE:
• ABIOTIC (non-living) PORTION OF ENVIRONMENT
  (ATMOSPHERE) Biotic THEN BACK AGAIN
The Water Cycle
Water Cycle
  CELLS CONTAIN 70-90% H20
  • VERY LITTLE OF EARTHS AVAILABLE H20 IS
    IN LIVING THINGS
  • RIVERS / LAKES /
    STREAMS / OCEANS CONTAIN A BIG %
  • ATMOSPHERE CONTAIN WATER = WATER
    VAPOR
  • GROUND WATER = IN SOIL OR
    UNDERGROUND IN POROUS ROCK
  • WATER CYCLE = MOVEMENT OF H20 B/T
    RESERVOIRS
     – EVAPORATION
     – TRANSPIRATION
     – PRECIPITATION
Evaporation
• Liquid  gas (water vapor)
• HEAT (sun) CAUSES
  WATER TO EVAPORATE
• 90% OF EVAPORATED
  WATER FROM
  TERRESTRIAL
  ECOSYSTEM PASSES
  THROUGH PLANTS IN A
  PROCESS CALLED…
Transpiration
• PLANTS TAKE IN H20 THRU ROOTS
• RELEASE WATER & TAKE IN CO2 (CARBON
  DIOXIDE)
Condensation
• Water vapor cools in the atmosphere
  and condenses (gasliquid) around
  dust particles to form clouds.
• The water droplets stick to each
  other and become too heavy, so they
  must fall out of the sky and back to
  earth…
Precipitation
• WATER LEAVES
  ATMOSPHERE
• TEMP & AIR
  PRESSURE
  DETERMINE HOW
  MUCH WATER CAN
  BE HELD
• Then it will:
 – SNOW, RAIN, SLEET,
   HAIL OR FOG
Carbon Cycle
• PHOTOSYNTHESIS + CELLULAR RESPIRATION
• PHOTOSYNTHESIS = PLANTS & OTHER
  AUTOTROPHS USE:
  CO2 + H20 & SUNLIGHT = CARBOHYDRATES
HUMAN INFLUENCE ON THE CARBON
           CYCLE
              • IN THE PAST 150 YEARS
                CO2 IN THE ATMOSPHERE
                HAS RISEN 30%
                ALMOST ½ IN THE LAST
                40 YEARS
              • HUMAN ACTIVITY IS THE
                CAUSE
              • BURNING FOSSIL FUEL:
                 – REMAINS OF
                   ORGANISMS THAT
                   HAVE BEEN
                   TRANSFORMED BY
                   DECAY, HEAT, &
                   PRESSURE 
                   ENERGY RICH ORGANIC
                   MOLECULES
• BURNING
  RELEASES ENERGY
  & CO2
• BURNING
  VEGETATION
  RELEASES CO2
• TROPICAL
  RAINFOREST
  DESTRUCTION
• WITH NO PLANTS
  CO2 IS NOT
  ABSORBED
Nitrogen Cycle
• NITROGEN IS NEEDED TO MAKE PROTEINS &
  NUCLEIC ACIDS (DNA OR RNA)
• N2 (NITROGEN GAS) MAKES UP 78% OF THE
  ATMOSPHERE (unusable in this form)
• N2 must be changed
  to AMMONIA
   to be used by
   living things.
NITROGEN FIXATION
• CONVERSION OF N2 TO AMMONIA
• CERTAIN BACTERIA CAN CONVERT N2 NH3
  NITROGEN-
  FIXING
  BACTERIA




• LIVE IN SOIL &
  IN SOME ROOTS
Recycling Nitrogen
• BODIES OF DEAD ORGANISMS CONTAIN “N”
   – URINE & DUNG ALSO
• DECOMPOSERS BREAK DOWN CORPSES &
  WASTE OF ORGANISMS GIVE OFF NITROGEN
  AS AMMONIA =
  AMMONIFICATION
• NITRIFICATION =
  BACTERIA IN SOIL
  TAKE IN AMMONIA
  & OXIDIZE IT INTO
  NITRITES, NO2 &
  NITRATES, NO3
• PLANTS CAN ABSORB NITRATES & AMMONIA
  FROM SOIL
  – ANIMALS CANNOT!
• ANIMALS OBTAIN IT
  BY EATING OTHER
  ORGANISMS &
  DIGESTING THE
  PROTEINS &
  NUCLEIC ACIDS
• DENITRIFICATION
• RETURNING NITROGEN TO ATMOSPHERE
PHOSPHORUS CYCLE
Short Term
 Phosphorus is cycled from the soil to
  producers and then from the
  producers to consumers.
Long Term
 Weathering or erosion of rocks that
  contain phosphorus slowly adds
  phosphorus to the cycle.

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Nutrient cycles for blog

  • 1. CYCLING OF MATTER
  • 2. • ENERGY FLOWS THROUGH ECOSYSTEM • WATER—NITROGEN—CARBON—PHOSPHORUS ARE RECYCLED!!! • THEY MOVE THRU A BIOGEOCHEMICAL CYCLE: • ABIOTIC (non-living) PORTION OF ENVIRONMENT (ATMOSPHERE) Biotic THEN BACK AGAIN
  • 4. Water Cycle CELLS CONTAIN 70-90% H20 • VERY LITTLE OF EARTHS AVAILABLE H20 IS IN LIVING THINGS • RIVERS / LAKES / STREAMS / OCEANS CONTAIN A BIG % • ATMOSPHERE CONTAIN WATER = WATER VAPOR • GROUND WATER = IN SOIL OR UNDERGROUND IN POROUS ROCK • WATER CYCLE = MOVEMENT OF H20 B/T RESERVOIRS – EVAPORATION – TRANSPIRATION – PRECIPITATION
  • 5. Evaporation • Liquid  gas (water vapor) • HEAT (sun) CAUSES WATER TO EVAPORATE • 90% OF EVAPORATED WATER FROM TERRESTRIAL ECOSYSTEM PASSES THROUGH PLANTS IN A PROCESS CALLED…
  • 6. Transpiration • PLANTS TAKE IN H20 THRU ROOTS • RELEASE WATER & TAKE IN CO2 (CARBON DIOXIDE)
  • 7. Condensation • Water vapor cools in the atmosphere and condenses (gasliquid) around dust particles to form clouds. • The water droplets stick to each other and become too heavy, so they must fall out of the sky and back to earth…
  • 8. Precipitation • WATER LEAVES ATMOSPHERE • TEMP & AIR PRESSURE DETERMINE HOW MUCH WATER CAN BE HELD • Then it will: – SNOW, RAIN, SLEET, HAIL OR FOG
  • 9. Carbon Cycle • PHOTOSYNTHESIS + CELLULAR RESPIRATION • PHOTOSYNTHESIS = PLANTS & OTHER AUTOTROPHS USE: CO2 + H20 & SUNLIGHT = CARBOHYDRATES
  • 10. HUMAN INFLUENCE ON THE CARBON CYCLE • IN THE PAST 150 YEARS CO2 IN THE ATMOSPHERE HAS RISEN 30% ALMOST ½ IN THE LAST 40 YEARS • HUMAN ACTIVITY IS THE CAUSE • BURNING FOSSIL FUEL: – REMAINS OF ORGANISMS THAT HAVE BEEN TRANSFORMED BY DECAY, HEAT, & PRESSURE  ENERGY RICH ORGANIC MOLECULES
  • 11. • BURNING RELEASES ENERGY & CO2 • BURNING VEGETATION RELEASES CO2 • TROPICAL RAINFOREST DESTRUCTION • WITH NO PLANTS CO2 IS NOT ABSORBED
  • 12. Nitrogen Cycle • NITROGEN IS NEEDED TO MAKE PROTEINS & NUCLEIC ACIDS (DNA OR RNA) • N2 (NITROGEN GAS) MAKES UP 78% OF THE ATMOSPHERE (unusable in this form) • N2 must be changed to AMMONIA to be used by living things.
  • 13. NITROGEN FIXATION • CONVERSION OF N2 TO AMMONIA • CERTAIN BACTERIA CAN CONVERT N2 NH3 NITROGEN- FIXING BACTERIA • LIVE IN SOIL & IN SOME ROOTS
  • 14. Recycling Nitrogen • BODIES OF DEAD ORGANISMS CONTAIN “N” – URINE & DUNG ALSO • DECOMPOSERS BREAK DOWN CORPSES & WASTE OF ORGANISMS GIVE OFF NITROGEN AS AMMONIA = AMMONIFICATION • NITRIFICATION = BACTERIA IN SOIL TAKE IN AMMONIA & OXIDIZE IT INTO NITRITES, NO2 & NITRATES, NO3
  • 15. • PLANTS CAN ABSORB NITRATES & AMMONIA FROM SOIL – ANIMALS CANNOT! • ANIMALS OBTAIN IT BY EATING OTHER ORGANISMS & DIGESTING THE PROTEINS & NUCLEIC ACIDS • DENITRIFICATION • RETURNING NITROGEN TO ATMOSPHERE
  • 17. Short Term  Phosphorus is cycled from the soil to producers and then from the producers to consumers. Long Term  Weathering or erosion of rocks that contain phosphorus slowly adds phosphorus to the cycle.