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Proportions of gases in the modern atmosphere
For 200 million years, the proportions of different gases in the atmosphere have been much the same as they are today:
approx 80% nitrogen
approx 20% oxygen
small proportions of various other gases, including carbon dioxide, water vapour and noble gases
Theories about the formation of the Earth’s atmosphere
Theories about what was in the Earth’s early atmosphere and how the atmosphere was formed have changed and developed over time
Evidence for the early atmosphere is limited because of the time scale of 4.6 billion years
What was Earth’s early atmosphere like (first billion years)?
Hot when it was formed
Intense volcanic activity released gases that formed the early atmosphere and water vapour that condensed to form the oceans
Atmosphere may have been like the atmospheres of Mars and Venus today, consisting of mainly carbon dioxide with little or no oxygen gas
Volcanoes also produced nitrogen which gradually built up in the atmosphere
There may have been small proportions of methane and ammonia
First decrease of CO2 in the atmosphere
When oceans formed, carbon dioxide dissolved in the water
This CO2 went through a series of reactions to form carbonate precipitates that formed sediments on the seabed
This reduced the amount of carbon dioxide in the atmosphere
Increase of oxygen in the atmosphere
Algae and plants produced the atmospheric O2 by photosynthesis, represented by the equation:
6 CO2 + 6 H2O → C6H12O6 + 6 O2
Carbon dioxide + water > (+light) > glucose + oxygen
Algae first produced oxygen about 2.7 billion years ago and soon after this oxygen appeared in the atmosphere
Over the next billion years plants evolved and the percentage of oxygen gradually increased to a level that enabled animals to evolve
Second decrease of carbon dioxide in the atmosphere
Algae and plants decreased the percentage of carbon dioxide in the atmosphere by photosynthesis
Was also decreased by the formation of sedimentary rocks and fossil fuels that contain carbon when
Formation of fossil fuels
some of the carbon organisms took in from the atmosphere and oceans became locked up in rocks and fossil fuels after the organism died
when plants, plankton and marine animals die, they fall to the seabed and get buried by layers of sediment
they get compressed over millions of years to form sedimentary rocks, oil and gas
they trapped carbon within them, keeping the levels of carbon in the atmosphere reduced
things like coal, crude oil and natural gas are fossil fuels
How are limestone, crude oil, coal and natural gas formed?
crude oil and natural gas - deposits of plankton
these fossil fuels form reservoirs under the seabed when they are trapped in rocks
coal - sedimentary rock made from thick plant deposits
limestone - sedimentary rock mostly made of calcium carbonate deposits from the shells and skeletons of marine organisms
Examples of greenhouse gases
Water vapour - H2O
Carbon dioxide - CO2
Methane - CH4
Necessity of the greenhouse effect for life
Greenhouse gases in the atmosphere maintain temperatures on Earth high enough to support life by allowing short wavelength radiation from the sun to pass through but absorbing outgoing long wavelength radiation
It is a natural phenomenon
Greenhouse gas effect
EM radiation at most wavelengths (both long and short) from the sun passes through the Earth’s atmosphere
The Earth absorbs some radiation and thus warms up (essential for life on Earth)
But some heat is radiated from the Earth as infrared radiation
Some of this IR radiation is absorbed by an increasing amount of greenhouse gases in the atmosphere
Atmosphere warms up leading to the greenhouse effect and global warming
Human activities increasing greenhouse gases
Carbon dioxide - driving, consuming electricity, combustion and deforestation
Methane - increased farming and decomposition in landfills
Global climate change
Based on peer-reviewed evidence, many scientists believe that human activities will cause the temperature of the Earth’s atmosphere to increase at the surface and that this will result in global climate change
However, it is difficult to model such complex systems as global climate change
This leads to simplified models, speculation and opinions presented in the media that may be based on only parts of the evidence and which may be biased.
What is a major cause of climate change?
An increase in average global temperature
Potential effects of global climate change
extinction of species
raising sea levels due to the melting of polar ice caps
migration- people will move from areas suffering drought/flooding
decrease in crop yield for all major world crops
Carbon footprint
The total amount of carbon dioxide and other greenhouse gases emitted over the full life cycle of a product, service or event
What action can be taken to reduce a carbon footprint?
By reducing emissions of carbon dioxide and methane:
increased use of alternative energy supplies
energy conservation
carbon capture and storage
carbon taxes and licences
carbon off-setting including tree planting
carbon neutrality
Challenges in reducing a carbon footprint
Scientific disagreement over climate change causes
Lack of public information
Lifestyle changes
Economic considerations
e.g. planting trees takes away land that could be used to grow crops
Incomplete international cooperation
Can be more expensive
Pollution caused by combustion
Combustion of fuels is a major source of atmospheric pollutants
Most fuels, including coal, contain carbon and/or hydrogen and may also contain some sulfur
The gases released into the atmosphere when a fuel is burned may include carbon dioxide, water vapour, carbon monoxide, sulfur dioxide and oxides of nitrogen
Solid particles and unburned hydrocarbons may also be released that form particulates in the atmosphere
What are the advantages of complete combustion?
Less soot is made
More heat per gram of fuel is released
Poisonous carbon monoxide is not produced
What does incomplete combustion release?
Solid particles of soot (carbon)
Carbon monoxide
Unburnt fuel
What are the properties and effects of atmospheric pollutants?
Carbon monoxide - toxic gas which is colourless and odourless so not easy to detect
Sulfur dioxide and oxides of nitrogen - cause acid rain and respiratory problems in humans
Particulates - cause global dimming and human health problems