4.1 how important are water and carbon to life on earth Flashcards

(13 cards)

1
Q

how is water essential for development and evolution of life on earth

A
  1. essential for development + evolution on earth:
    - organic molecules mix + form complex structures
    - the large amount of water on earth due to its distance from sun - allowing it to exist in liquid form
  2. comparison with mars
    - mars has very little water in liquid form - most frozen in vapour
    - water increases potential for life
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2
Q

what is waters environmental and climate role

A
  • waters cover 71% of earths surface
  • water regulates earths temps by absorbing, storing and releasing heat
  • clouds reflecting incoming sunlight which lowers surface temps
  • water vapour absorbs outgoing long-wave radiation, keeping global temps approaching 15 degrees warmer than without it
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3
Q

what are the 5 key uses of water - plants, humans

A
  1. BIOLOGICALLY: makes 65-95% of living organisms, vital for photosynthesis, respiration and transpiration plants, circulation, temp reg + nutrient tranpsort humans/ animals
  2. PHOTOSYNTHESIS: in leaves producing biomass
    water + co2 + sun –> glucose + oxygen
  3. RESPIRATION
    glucose + oxygen –> co2 + energy + water
  4. TRANSPIRATION: water evaporates from leaf surfaces –> cools plants
  5. OTHER: irrigation, hydroelectric power, drinking, sewage, industiral
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4
Q

what is the importance of carbon to life on earth

A
  • carbon - chemical element
    1. BIOLOGICAL –> found in large complex molecules eg carbs, proteins, lipids, DNA, RNA. essential in photosynthesis and respiration
  1. STORAGE –> found in: carbonate rocks (eg limestone), ocean (dissolved), atmosphere (gas), biosphere (living organisms)
  2. ECONOMIC –> carbon based fuels (coal, oli, gas) power global economy. manufacturing plastics, textiles, paints etc
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5
Q

how are the water and carbon cycles open and closed systems

A
  1. CLOSED
    - global scale
    - energy enters and leaves (from sun) but matter does not
    - but the speed of this cycle gets affected by the energy of the sun eg the high intensity of sunlight - the higher rate of photosynthesis
  2. OPEN
    - local scale
    - energy and matter cross system boundaries between atmosphere, oceans and land
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6
Q

main water stores and their % of global water

A
  • oceans 97%
  • glaciers 2%
  • groundwater (aquifers) 0.7%
  • lakes 0.01%
  • soils 0.005%
  • atmosphere 0.001%
  • rivers 0.0001%
  • biosphere 0.00004%
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7
Q

inputs and outputs of water

A
  1. INPUTS INTO THE ATMOSPHERE:
    - evaporation from oceans, lakes, soils
    - transpiration from plannts
    - = evapotranspiration
  2. OUTPUTS
    - precipitation: rain, snow, hail etc
    - condensation: forms clouds
    - ablation and sublimation from glaciers and ice sheets
  3. OUTPUTS - RUN-OFF
    - precipitation that doesn’t infiltrate contributes to run-off - flows to rivers/oceans
    - dry areas –> water flows into inland basins
  4. OUTPUT INFILTRATION
    - water entering soil
    - may percolate to groundwater and return via springs
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8
Q

whats the average residence time of a water molecule in the atmosphere

A

9 days

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9
Q

main stores in the carbon cycle and how much carbon is in these stores per billion tonnes

A
  • sedimentary rock 100,000,000
  • oceans 40,000
  • sea floor sediment 6000
  • fossil fuels 4000
  • soils/peat 2500
  • atmosphere 600
  • land plants 550
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10
Q

the slow carbon cycle - inputs and outputs

A

INPUTS
- operates over millions of years
- co2 diffuses from atmosphere to oceans, marine organisms (clams, corals) combine dissolved carbon and calcium to form calcium carbonate shells
- these shells sink to sea floor and accumulate over millions of years –> sedimentary rock (99.9%)
OUTPUTS
- these sedimentary rocks r subducted and re-emitted via volcanic eruptions, or exposed to chemical weathering
- co2 in rainwater forms carbonic acids, which dissolves carbonate rocks, releasing co2 into rivers, oceans and atmosphere
- on land, dead organic matter gets buried and converted into fossil fuels like coal, oil and natural gas

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11
Q

the fast carbon cycle - inputs and outputs

A
  • rapid transfer of carbon between atmosphere, biosphere, oceans and soils
  • 10 to 1000 times fast than the slow cycle
  • key components:
    BIOSPHERE –> ATMOPSHERE
    1. phytoplankton (ocean algae) and land plants uses photosynthesis converting co2 –> glucose. respiration opposite reaction and releases co2 to atmosphere
    2. decomposition of organic matter releases co2

ATMOSPHERE –> HYDROSPHERE
1. c02 dissolves from atmosphere into ocean surfaces
2. upwelling and downwelling circulates this water and releases co2 back into atmosphere

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12
Q

the main processes in the carbon cycle

A
  • photosynthesis: atmosphere –> biosphere
  • respiration: biosphere –> atmosphere
  • oxidation: reaction of rocks with the air which then releases carbon
  • decomposition: biosphere –> atmosphere
  • weathering: biosphere –> atmosphere/ hydrosphere (leaching of carbonated top soil into air/ lakes, rivers)
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13
Q
A
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