Atmosphere Flashcards

1
Q

How do scientists know the historic composition of the air

A
  • by analysing the tiny air bubbles trapped in ice cores taken at the poles
  • the air bubbles were trapped as the snow and ice was laid down tens of thousands of years ago
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2
Q

Evolution of the atmosphere

A
  • the surface of the early Earth was molten and there was no atmosphere surrounding the planet
  • cooling began to take effect and allow for molten materials to slowly solidify forming land masses
  • volcanoes formed on the land masses
  • the volcanoes released gases from the Earth’s interior through violent eruptions
  • the eruptions released large amounts of carbon dioxide and water vapour, as well as nitrogen, hydrogen, and other gases
  • Earth’s gravity prevented the gases from escaping into outer space and they formed the early atmosphere
  • the early atmosphere, therefore, is thought to have contained mainly CO2 and water vapour
    -> there was little or no oxygen present
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3
Q

How the oceans formed

A
  • when conditions cooled sufficiently, the water vapour later condensed and fell to the surface of the Earth, forming the oceans
  • when the water vapour condensed large amounts of CO2 dissolved in the oceans
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4
Q

How oxygen increased

A

Primitive plants and algae began photosynthesising which used up carbon dioxide from the atmosphere and released oxygen

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5
Q

How carbon dioxide decreased

A
  • the water vapour in Earth’s early atmosphere condensed large amounts of CO2 dissolved in the oceans
  • carbonates were precipitated during this process which later formed sediments on the seabed
  • green plants and algae began to evolve and absorbed considerable amounts of carbon dioxide during photosynthesis
  • animals fed on the plants which transferred carbon to their tissues including bones and shells
  • when these organisms died, their remains formed sedimentary rocks
    ->the formation of sedimentary rock and fossil fuels ‘locked up’ the carbon from carbon dioxide in the early atmosphere
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6
Q

Explain the greenhouse affect

A
  • short wavelength radiation from the sun is absorbed by the earths surface and re-emitted from the surface of the Earth as infrared radiation which has a longer wavelength
  • but a lot of the radiation is absorbed in the Earth’s atmosphere by greenhouse gases
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7
Q

Name the greenhouse gases

A
  • carbon dioxide
  • methane
  • water vapour
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8
Q

Effects of global climate change

A
  • rising sea levels
  • extinction of species
  • migration
  • decrease in crop yield
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9
Q

Carbon footprint

A

The total amount of CO2 and other greenhouse gases emitted over the full life cycle of a product

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10
Q

Human activities that increase greenhouse gases in the atmosphere

A
  • driving
  • consuming electricity
  • decay of waste in landfill sites
  • raising livestock
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11
Q

Life Cycle Assessment

A

A technique used to assess the environmental impact associated the life cycle of a product, a service or an event

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12
Q

What is the major source of atmospheric pollution

A

The combustion of fossil fuels

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13
Q

Combustion and incomplete combustion products

A
  • the burning of fossil fuels releases the gases carbon dioxide, carbon monoxide, nitrogen oxides and sulfur oxides
  • incomplete combustion of the fuels gives rise to unburned hydrocarbons and carbon particulates
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14
Q

What is formed when hydrocarbons are used as a fuel

A

Water and carbon dioxide

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15
Q

Incomplete combustion

A

Occurs when there is insufficient oxygen to burn

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16
Q

The source and effect of CO

A
  • incomplete combustion of fuels
  • toxic -> binds to haemoglobin
17
Q

Source and effect C (soot)

A
  • incomplete combustion
  • respiratory irritation + global dimming
18
Q

Source and effect of sulfure dioxide

A
  • sulfur impurities in fuels
  • causes acid rain + respiratory irritation
19
Q

Effect of NOx gases

A
  • causes acid rain
  • respiratory irritation
20
Q

Gas in the atmosphere today

A
  • nitrogen (main one)
  • oxygen
  • carbon dioxide, water vapour, and methane
21
Q

Early atmosphere of Earth

A
  • there was intense volcanic activity that released gases that formed the early atmosphere and water vapour that condensed to form the oceans
    -> at this time the atmosphere would’ve consisted of mainly carbon dioxide with little or no oxygen
  • volcanoes also produced hydrogen which gradually built up with small amounts of methane and ammonia
  • when the oceans formed carbon dioxide dissolved in the water and carbonates were precipitated producing sediments, reducing amount of CO2 in the atmosphere
22
Q

Why does nitrogen that is formed stay in the atmosphere

A

Because it’s unreactive

23
Q

How oxygen increased

A
  • algae and plants produced the oxygen that is no in the atmosphere by photosynthesis
  • oxygen increased to a level that allowed animals to evolve
24
Q

How carbon dioxide decreased

A

Algae and plants decreased it by photosynthesis

It was also decreased by the formation of sedimentary rocks (locked up) and fossil fuels that contain carbon

25
Q

2 human activities that increase amount of greenhouse gases

A
  • deforestation
  • transportation
26
Q

Carbon footprint

A

The total amount of carbon dioxide and other greenhouse gases emitted over the full life cycle of a product