C9: Chemistry of the atmosphere Flashcards
What are the approximate proportions of gases in Earth’s atmosphere today?
- 80%nitrogen
- 20% oxygen
- small proportions of other gases, including carbon dioxide, water vapour and noble gases.
Theories about the Earth’s early atmosphere and how the atmosphere was formed have developed over time.
Why is evidence for the composition of the early atmosphere limited?
Because of the time scale of 4.6 billion years.
Explain the theory which suggests the composition of Earth’s early atmosphere during the first billion years of its existence.
- intense volcanic activity released gases which formed the early atmosphere (CO2 and nitrogen; possibly small proportions of methane and ammonia)
- volcanoes also produced water vapour that condensed to form the oceans
- the Earth’s atmosphere was like the atmospheres of Mars and Venus today, consisting of mainly carbon dioxide with little or no oxygen
One theory suggests Earth’s early atmosphere may have consisted of mainly CO2.
Now, there is much less CO2 in the atmosphere; where does the theory suggest it went?
- When the oceans formed, carbon dioxide dissolved in the water.
- When algae and plants evolved, they decreased the percentage of CO2 in the atmosphere by photosynthesis.
- Dissolved CO2 went through a series of reactions to form carbonate precipitates. When marine organisms evolved, their shells and skeletons contained calcium carbonate.
- When they died, they fell to the seabed and were buried with sediment, becoming compressed over millions of years to form sedimentary rocks (limestone + coal), crude oil and natural gas.
One theory suggests Earth’s early atmosphere may have consisted of mainly CO2 and little or no oxygen gas.
Now, the atmosphere is approximately 20% oxygen; how does the theory suggest it appeared?
• Algae first produced oxygen, about 2.7 billion years ago, by photosynthesis:
carbon dioxide + water → glucose + oxygen
- Soon after this, oxygen appeared in the atmosphere.
- Over the next billion years, plants evolved.
- The percentage of oxygen gradually increased to a level that enabled animals to evolve.
Explain how deposits of limestone, coal, crude oil and natural gas formed.
- When the oceans formed, carbon dioxide dissolved in the water.
- Dissolved CO2 went through a series of reactions to form carbonate precipitates. When marine organisms evolved, their shells and skeletons contained calcium carbonate.
- When they died, they fell to the seabed and were buried with sediment, becoming compressed over millions of years to form sedimentary rocks (limestone + coal), crude oil and natural gas.
What are greenhouse gases?
Gases which act as an insulating layer in Earth’s atmosphere, allowing Earth to be warm enough to support life.
Name 3 greenhouse gases.
- water vapour
- carbon dioxide
- methane
Explain the greenhouse effect.
- short-wavelength radiation from the Sun hits the Earth’s surface and is reradiated back out as long-wavelength radiation
- greenhouse gases in the atmosphere (including CO2 and methane) absorb much of this and reradiate it in all directions, including back towards Earth
- this long-wavelength radiation is thermal radiation, so results in the heating of the Earth’s surface
Explain how the greenhouse effect is related to global heating.
- greenhouse gases in the atmosphere absorb long-wavelength radiation that has been reradiated from the Earth’s surface, and reradiate it in all directions, including towards the earth - this is the greenhouse effect.
- the heat retained by the Earth should be in equilibrium with the heat it emits (so that the planet is at a constant temperature)
- but increasing levels of greenhouse gases have disrupted the balance, meaning earth is heating up - this is global heating.
Name 2 human activities which increase the amount of methane in the atmosphere.
- agriculture: farm animals produce methane through digestive processes
- decomposition of waste (including agricultural) produces methane (as well as CO2)
Name 3 human activities which increase the amount of carbon dioxide in the atmosphere.
- deforestation
- burning fossil fuels
- creation of waste - its decomposition releases CO2 (as well as methane)
In what ways does deforestation increase the amount of carbon dioxide in the atmosphere?
- Removing vegetation means less CO2 is removed from the atmosphere
- The combustion and decay of vegetation also releases CO2
- Deforestation is done either to create space for crops (agricultural waste releases CO2 and methane) or for farm animals (which release methane)
Based on peer-reviewed evidence, many scientists believe that human activities cause the heating of the Earth’s surface, and that this results in global climate change.
Why is there misrepresentation and “skepticism”?
It is difficult to model global climate change, as it’s such a complex system.
This leads to simplified models, speculation, and potentially biased opinions presented in the media that may be based on only parts of the evidence.
An increase in average global temperature is a major cause of climate change. Describe 5 potential effects of global climate change.
- sea level rise (caused by expansion of water and polar ice caps melting), leading to coastal erosion, increased flooding and loss of habitats.
- changes in rainfall patterns. Along with increased temperatures, this may affect the ability of some regions to produce food.
- increased frequency and severity of storms
- reduction in biodiversity (heating leads to changes in habitats)
- changes in animal migration patterns and distribution of species (due to rainfall and temperature changes)