Chemistry Of The Atmosphere Flashcards
Roughly how old is the Earth?
4.6 billion years old
Percentage of Nitrogen in today’s atmosphere
Around 80%
Percentage of Oxygen in today’s atmosphere
Around 20%
Other gases in the the atmosphere and their percentage
- Carbon Dioxide
- Water Vapour
- Argon
- Noble Gases
- Less than 1%
Early Atmosphere Formation
(The First 1 Billion Years)
- Early atmosphere was mostly CO2 (similar to Mars and Venus’ atmosphere today)
- Volcano eruptions released water vapour, nitrogen and small amounts of methane and ammonia into the atmosphere
- Water vapour condensed, forming oceans and CO2 dissolved in it to form carbonate precipitate
How did Oxygen in the atmosphere increase?
(2.7 Billion Years Ago)
- Algae and plants evolved and
photosynthesised - They took in CO2, releasing O2
- CO2 levels decreased, O2 levels increased allowing complex life forms (animals) to
evolve - Plants and algae died and got trapped in sediment layers
- Sediment eventually compressed (due to pressure) and became sedimentary rock, oil and gas
- This trapped carbon in the layers
How did crude oil and natural gas form?
From dead plankton
How did coal (sedimentary rock) form?
From dead plant matter
How did limestone (sedimentary rock) form?
From the calcium carbonate precipitate formed when the CO2 dissolved in the oceans
Greenhouse Gases
Maintain temperatures on Earth high enough to support life on Earth
What are the Greenhouse Gases?
- Water Vapour
- Methane
- CO2
The Greenhouse Effect
- Sun’s energy is radiated in short wavelengths
- Passes through the atmosphere hitting the Earth’s surface
- Some is absorbed, some is reemitted in long wavelengths
- Most of the remission hits gas particles that reemit and absorb the energy again and again
- This keeps the Earth warm as the energy doesn’t leave the atmosphere
The Problem of the Greenhouse Effect
- Human activities increase the concentration of CO2 and methane in the atmosphere
- Greenhouse effect increases, causing global warming
2 Main Reasons for Global Warming
- Increase in burning fossil fuels that release carbon
- Deforestation so less trees for photosynthesis to take in CO2
Climate Change
- Effects of global warming
- Leads to the alteration of long term weather patterns on the planet