4.1 how important are water and carbon to life on earth Flashcards
(13 cards)
how is water essential for development and evolution of life on earth
- 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 - comparison with mars
- mars has very little water in liquid form - most frozen in vapour
- water increases potential for life
what is waters environmental and climate role
- 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
what are the 5 key uses of water - plants, humans
- BIOLOGICALLY: makes 65-95% of living organisms, vital for photosynthesis, respiration and transpiration plants, circulation, temp reg + nutrient tranpsort humans/ animals
- PHOTOSYNTHESIS: in leaves producing biomass
water + co2 + sun –> glucose + oxygen - RESPIRATION
glucose + oxygen –> co2 + energy + water - TRANSPIRATION: water evaporates from leaf surfaces –> cools plants
- OTHER: irrigation, hydroelectric power, drinking, sewage, industiral
what is the importance of carbon to life on earth
- carbon - chemical element
1. BIOLOGICAL –> found in large complex molecules eg carbs, proteins, lipids, DNA, RNA. essential in photosynthesis and respiration
- STORAGE –> found in: carbonate rocks (eg limestone), ocean (dissolved), atmosphere (gas), biosphere (living organisms)
- ECONOMIC –> carbon based fuels (coal, oli, gas) power global economy. manufacturing plastics, textiles, paints etc
how are the water and carbon cycles open and closed systems
- 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 - OPEN
- local scale
- energy and matter cross system boundaries between atmosphere, oceans and land
main water stores and their % of global water
- oceans 97%
- glaciers 2%
- groundwater (aquifers) 0.7%
- lakes 0.01%
- soils 0.005%
- atmosphere 0.001%
- rivers 0.0001%
- biosphere 0.00004%
inputs and outputs of water
- INPUTS INTO THE ATMOSPHERE:
- evaporation from oceans, lakes, soils
- transpiration from plannts
- = evapotranspiration - OUTPUTS
- precipitation: rain, snow, hail etc
- condensation: forms clouds
- ablation and sublimation from glaciers and ice sheets - OUTPUTS - RUN-OFF
- precipitation that doesn’t infiltrate contributes to run-off - flows to rivers/oceans
- dry areas –> water flows into inland basins - OUTPUT INFILTRATION
- water entering soil
- may percolate to groundwater and return via springs
whats the average residence time of a water molecule in the atmosphere
9 days
main stores in the carbon cycle and how much carbon is in these stores per billion tonnes
- sedimentary rock 100,000,000
- oceans 40,000
- sea floor sediment 6000
- fossil fuels 4000
- soils/peat 2500
- atmosphere 600
- land plants 550
the slow carbon cycle - inputs and outputs
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
the fast carbon cycle - inputs and outputs
- 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
the main processes in the carbon cycle
- 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)