C9 Flashcards
How long ago did the Earth form?
4.6 billions years
How was the early atmosphere formed and what was its composition?
- the early atmosphere was formed from lots of intense volcanic eruption (which released a lot of gases)
- the early atmosphere composition was mainly CO2, there was also a lot of water vapour (which later formed oceans), some nitrogen which has built up over time, a little bit of methane and ammonia, and hardly any oxygen
How do we know this was the composition? Why can’t we be sure? What do we base our assumptions on?
We don’t, scientists think the Earth’s early atmosphere was similar to the atmospheres found on Mars and Venus today. That is, lots of carbon dioxide and very little oxygen
Describe the composition of the atmosphere today
for the last 200 million years:
- about 4/5 (80%) of nitrogen
- 1/5 (20%) of oxygen
- and small proportions of various other gases (eg: CO2, water vapour & noble gases)
How did the oceans form?
- due to the heat from the volcanoes, the water vapour in the atmosphere cooled below 100oC
- and condensed into liquid water this formed oceans
How did the oceans forming change CO2 levels? Where did the carbon in the carbon dioxide go to next?
- ocean forming made CO2 levels decreased as most of the CO2 would overtime dissolve into the ocean(as carbon dioxide can dissolve in water)
Where did the carbon in the carbon dioxide go to next?
- the dissolved CO2 ended up being used by sea creatures to build their shells
- when they died their shells ended up as sediments, which now forms carbonate rocks, such as limestone
- we say the carbon has been “locked up”
How did the level of oxygen increase?
- first algae then plants (over the next billion years) evolved and started to carry out photosynthesis
- oxygen is of product
- this % of oxygen gradually increased due to it being released into the atmosphere allowing the animals to evolve
Write the word and symbol equations for this process(photosynthesis)
6CO2 + 6H20 → C6 H12 O6 +6O2
→ = photosynthesis
carbon dioxide + water → glucose + oxygen
How did the level of carbon dioxide fall?
- algae & plants decreased the % of CO2 in the atmosphere by carrying out photosynthesis. CO2 is a reactant in the photosynthesis chemical reaction
- CO2 was also decreased by it dissolving into the ocean and the formation of sedimentary rocks & fossil fuels that contains carbon
Why are GHG essential for our survival?
they keep temperatures on Earth high enough to support life
Give 3 examples of greenhouse gases
Carbon dioxide, methane and water vapour
Describe the Greenhouse Effect
1) radiation reaches us from the sun (shorter wavelengths such as visible light and UV light) and enters the atmosphere
2) a lot of this radiation is absorbed by the Earth’s surface, then re-emitted as longer wavelength infrared
3) some of the heat radiates back into space
4) while some of it is absorbed by a layer of greenhouse gases (water vapour, CO2 and methane), then re-emitted, warming up the Earth – this is called The Greenhouse Effect
Describe the greenhouse effect in terms of the interaction of short and long wavelength radiation with matter
- the radiation from the sun enters our atmosphere at a short wavelength
- it is absorbed by the Earth’s surface & re-emitted at a longer wavelength
- the infrared radiation is absorbed by GHG then re-emitted in all direction causing an increase in global temperature
Name 2 human activities which increase the amount of carbon dioxide in the atmosphere
- burning fossil fuels (when fueling up our cars)
- deforestation (as when trees are cut down the removal of CO2 decrease)