Chemistry Of The Atmosphere Flashcards
Phase 1 of evolution of atmosphere
- surface of earth was covered in volcanoes that erupted and released lots of gases
- the early atmosphere was probably mostly carbon dioxide, with virtually no oxygen. Quite like the atmospheres of mars and Venus today
- volcanic activity also released nitrogen, which built up in the atmosphere over time, as well as water vapour and small amounts of methane and ammonia
Phase 2 of evolution of atmosphere
- when the vapour in the atmosphere condensed, it formed oceans
- lots of carbon dioxide as removed from the early atmosphere as it dissolved in the oceans
- this dissolved carbon dioxide went through a series of reactions to form carbonate precipitates that formed sediments on the seabed
- green plants and algae evolved and absorbed some of the carbon dioxide so that they could carry out photosynthesis
- later marine animals evolved. Their shells and skeletons contained carbonates from the oceans
- some of the carbon these organisms to in from the atmosphere and oceans became locked up in rocks and fossil fuels after the organisms died
What happens when plankton, plants and marine animals die
- they fall to the sea bed and get buried by layers of sediment
- over millions of years, they become compressed and form sedimentary rocks, oil and gas - trapping carbon within them and helping to keep carbon dioxide levels in the atmosphere reduced
Where do coal, crude oil and natural gas come from
- deposits of plankton
- these fossil fuels form reservoirs under the seabed when they get trapped in rocks
Where does coal come from
- its a sedimentary rock made from thick plant deposits
Where does limestone come from
- its a sedimentary rock
- mostly made out of calcium carbonate deposits from the shells and skeletons in marine organisms
Phase 3 of evolution of atmosphere
- as well a absorbing carbon dioxide in the atmosphere, green plants and algae produced oxygen by photosynthesis
- algae evolved first (2.7 billion years ago) then over the next billion years or so, green pants also evolved
- as oxygen levels built up in the atmosphere over time, more complex life could evolve
Atmosphere today
- reached this level 20 million years ago
- 80% nitrogen
- 20% oxygen
- carbon dioxide, noble gases and water vapour make up less than 1% of the atmosphere
Examples of greenhouse gases
- carbon dioxide
- methane
- water vapour
What do greenhouse gases do
- act as an insulating layer in the earths atmosphere
- this, amongst other factors allows the earth to be warm enough to support life
What is the greenhouse effect
- greenhouse gases don’t absorb incoming short wavelength radiation from the sun
- they do absorb long wavelength radiation that gets reflected back off earth
- they then re-radiate it in all directions - including back towards the earth
- the longwave radiation is thermal radiation so it results in warming the surface of the earth
Human activity that affects the amount of greenhouse gases in the atmosphere
- deforestation
- burning fossil fuels
- agriculture
- creating waste
How does deforestation affect amount of greenhouse gases in the atmosphere
- fewer trees = less CO2 is removed from atmosphere via photosynthesis
How does burning fossil fuels affect amount of greenhouse gases in the atmosphere
Carbon that was ‘locked up’ in these fuels is released as CO2
How does agriculture affect amount of greenhouse gases in the atmosphere
More farm animals produce more methane through their digestive processes