Topic 9 Flashcards

1
Q

Phase 1 of the Evolution of the Atmosphere

A
  • Volcanoes erupted and released hot gases
  • Mostly made up of carbon dioxide, with virtually no oxygen. Similar to Mars and Venus today
  • Volcanic activity also released nitrogen which built up of time, water vapour, and small amounts of methane and ammonia
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2
Q

Phase 2 of the Evolution of the Atmosphere

A
  • The water vapour condensed to form the oceans
  • Lots of carbon dioxide dissolved in the oceans, going through a series of reactions to form carbonate precipitates that formed sediments on the seabed
  • Marine animals evolved. Their shells and skeletons contained some carbonates
  • Green plants and algae evolved and absorbed carbon dioxide for photosynthesis
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3
Q

What happens to some of the carbon during the evolution of the atmosphere?

A
  • When plants, plankton, and marine animals die, they fall to the seabed and get buried by layers of sediment
  • Over millions of years they become compressed into sedimentary rocks, oil, and gas - trapping the carbon - fossil fuels.
  • Crude oil and natural gas are formed from deposits of plankton
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4
Q

What is coal

A
  • A sedimentary rock made from thick plant deposits
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5
Q

What is limestone

A
  • A sedimentary rock made mostly of calcium carbonate deposits from the shells and skeletons of marine organisms
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6
Q

Phase 3 of the Evolution of the Atmosphere

A
  • Algae evolved about 2.7 billion years ago
  • Over the next billion years green plants evolved
  • As oxygen levels built up in the atmosphere over time, more complex life (animals) could evolve
  • Around 200 million years ago the atmosphere reached a similar composition to the present day
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7
Q

Phase 3 of the Evolution of the Atmosphere

A
  • Algae evolved about 2.7 billion years ago
  • Over the next billion years green plants evolved
  • As oxygen levels built up in the atmosphere over time, more complex life (animals) could evolve
  • Around 200 million years ago the atmosphere reached a similar composition to the present day
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8
Q

Approximate composition of the atmosphere 200 million years ago

A
  • 80% nitrogen
  • 20% oxygen
  • small amounts of other gases making up 1%: mainly CO2, noble gases, and water vapour
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9
Q

The composition of the modern atmosphere

A
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10
Q

Greenhouse gases

A
  • Carbon dioxide, methane and water vapour
  • They act like an insulating layer, trapping heat, allowing the Earth to be warm enough to sustain life
  • Greenhouse gases absorb the long wave radiation that gets reflected back off the Earth, and re-radiate it in all directions
  • Because long-wave radiation is thermal radiation, the Earth’s surface warms up
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11
Q

Human activites that affect the amount of greenhouse gases

A
  • Deforestation: fewer trees means less CO2 being removed via photosynthesis
  • Burning fossil fuels: Carbon that was ‘locked up’ is released as CO2
  • Agriculture: More farm animals produce more methane through their digestive processes
  • Creating waste: More landfill sites and waste from agriculture mean more CO2 and methane released from the decomposition of waste
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12
Q

Carbon dioxide link to climate change

A
  • Despite the fact that the Earth’s temperature does vary naturally, the average temperature has been increasing by amounts greater than we would expect to see naturally
  • Most scientists agree that extra carbon dioxide from human activity is causing the global temperature to increase, leading to climate change
  • However it is hard to fully understand the Earth’s climate - it is very complex, and there are many variables. It is very hard to make a model that is not oversimplified
  • This had led to speculation about the CO2-climate change link, particularly in the media
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13
Q

Consequences of climate change

A
  • Polar ice caps melting: a rise in sea levels; increased flooding in coastal areas, and coastal erosion
  • Changes in rainfall patterns: causing some regions to get too much or too little water. Along with temperature, could affect ability to produce food
  • Frequency and severity of storms could increase
  • Changes in temperature and the amount of water: may affect wild species, and their distribution could be different
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14
Q

Carbon footprint

A
  • A measure of the amount of carbon dioxide and other greenhouse gases released over the full life cycle of something
  • Measuring the total
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