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Organic chemistry
Fossil fuels
Catherine Mortimer-Hawkins, IEST
The fossil fuels
• Coal, oil, and gas are fossil fuels.
• Remains of plants and animals that lived
million of years ago.
• They are all from organic compounds – C.
• Give plenty of heat when burned – fuel!
• Ex. methane + oxygen carbondioxide + water + energy
(CH4 + 2O2 CO2 + H2O + energy)
Coal
• Dead vegetation collects on the bottom of a swamp.
• Decay stops – microbes need oxygen –oxygen
depleted.
• Vegetation buried under debris.
• Thousands of years.. Sediment piles up. Peat!
• Peat gets buried further down, more pressure, more
temp! COAL!
• The more pressure, the more temp the harder
coal!
Coal
Dead vegetation in swamp
DEBRIS
SEA
PEAT
COAL
Oil & gas
• Formed from the soft remains of sea plants
and animals that form on the sea floor.
• Similar stages as in the coal process.
• Oil – less dense, migrates up through rock into
oil trap.
Ocean
gasImpermeable rock
Oil
Problems!!!
• Contains SULPHIDES – when burning ACID RAIN
• When burning – upsets the natural balanse of
CO2 – GLOBAL WARMING
Fractional destillation
• Crude oil pumped in at
base.
• Compounds boil.
• Smallest compounds boil
first – rise to the top.
• Other compounds rise
part of the way.
• Heaviest stay at the
bottom.
• All depending on different
boiling points.
• The larger molecules –
less flammable, less
runny.
Further pocessing!
• Clean impurities – sulphur compounds.
• Some fractions devided into smaller groups –
methane, ethane, prophane…
• Cracking:
turns longer molecules into smaller
ex. have alot of naphtha but less gasoline, break
naphtha into smaller molecules!
it always procuces ethene and propene - plastics!

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Organic chemistry fossil fuels

  • 2. The fossil fuels • Coal, oil, and gas are fossil fuels. • Remains of plants and animals that lived million of years ago. • They are all from organic compounds – C. • Give plenty of heat when burned – fuel! • Ex. methane + oxygen carbondioxide + water + energy (CH4 + 2O2 CO2 + H2O + energy)
  • 3. Coal • Dead vegetation collects on the bottom of a swamp. • Decay stops – microbes need oxygen –oxygen depleted. • Vegetation buried under debris. • Thousands of years.. Sediment piles up. Peat! • Peat gets buried further down, more pressure, more temp! COAL! • The more pressure, the more temp the harder coal!
  • 4. Coal Dead vegetation in swamp DEBRIS SEA PEAT COAL
  • 5. Oil & gas • Formed from the soft remains of sea plants and animals that form on the sea floor. • Similar stages as in the coal process. • Oil – less dense, migrates up through rock into oil trap. Ocean gasImpermeable rock Oil
  • 6. Problems!!! • Contains SULPHIDES – when burning ACID RAIN • When burning – upsets the natural balanse of CO2 – GLOBAL WARMING
  • 7. Fractional destillation • Crude oil pumped in at base. • Compounds boil. • Smallest compounds boil first – rise to the top. • Other compounds rise part of the way. • Heaviest stay at the bottom. • All depending on different boiling points. • The larger molecules – less flammable, less runny.
  • 8. Further pocessing! • Clean impurities – sulphur compounds. • Some fractions devided into smaller groups – methane, ethane, prophane… • Cracking: turns longer molecules into smaller ex. have alot of naphtha but less gasoline, break naphtha into smaller molecules! it always procuces ethene and propene - plastics!