T9: chemistry of the atmosphere Flashcards
(54 cards)
Why is there not a long of evidence for the early atmosphere?
Evidence for the early atmosphere is limited because of the long time scale of 4.6 billion years.
What are the different ‘phases’ in the theories for how the earth’s atmosphere has evolved?
1) volcanoes gave out gases
2) oceans, algae and green plants absorbed carbon dioxide
3) algae and green plants produced oxygen
What were the first billion years of earth’s history like?
Pretty explosive: the surface was covered in volcanoes that erupted and released a lot of gases (this is how we think the early atmosphere was formed).
What was the early atmosphere like?
The early atmosphere was probably mostly carbon dioxide and virtually no oxygen. This is quite like the atmospheres of Mars and Venus today.
How did volcanic activity change the atmosphere?
Volcanic activity released nitrogen which built up in the atmosphere over time as well as water vapour and small amounts of methane and ammonia.
What happened to the water vapour in the atmosphere?
condensed to form oceans.
What was the 3 things that cause the concentration of carbon dioxide in the atmosphere to decrease?
-oceans
-green plants and algae
-rocks
How did the concentration of carbon dioxide decrease due to oceans?
Lot son carbon dioxide was removed from the early atmosphere as it dissolved in the oceans. This dissolved carbon dioxide then went through a series of reactions to form carbonate precipitates that formed sediments on the seabed.
How did the concentration of carbon dioxide decrease due to green plants and algae?
Green plants and algae evolved and absorbed some of the carbon dioxide so that they could carry out photosynthesis.
What happened to marine animals (during phase 2)?
Later marine animals evolved as they formed shells and skeletons containing carbonates from the atmosphere.
What happens when plants, plankton and marine animals die?
- they fall to the seabed and get buried by layers of sediment.
- Over millions of years they become compressed and form sedimentary rocks, oil and gas; trapping the carbon within them and helping to keep carbon dioxide levels in the atmosphere reduced.
How did the concentration of carbon dioxide decrease due to rocks?
Some of the carbon these organisms (the evolved marine animals) took in from the atmosphere and oceans became locked up in rocks and fossil fuels after these organisms died.
What are the fossil fuels?
Things like coal, crude oil and natural gas that are made by this process are called fossil fuels.
How is crude oil and natural gas formed?
Formed from the deposits of plankton. These fossil fuels form reservoirs under the seabed where they get trapped in rocks.
What is coal and how is coal formed?
Coal is a sedimentary rock made from thick plant deposits.
What is limestone and how is it formed?
Limestone is also a sedimentary rock. It’s mostly made of calcium carbonate deposits from the shells and skeletons of marine organisms.
How did the concentration of oxygen change and why?
Increased as green plants and algae produced oxygen by photosynthesis: where plants use light to convert carbon dioxide and water into sugars.
When was oxygen first produced?
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.
What happened as oxygen levels changed?
As the oxygen levels/percentage built up in the atmosphere over time, more complex life (animal life) could evolve.
For the past 200 millions years, what has the atmosphere been like?
the proportions of different gases in the atmosphere have been much the same as they are today:
- about four-fifths (approximately 80%) nitrogen
- about one-fifth (approximately 20%) oxygen
- small proportions of various other gases(each only makes up less than 1% of the atmosphere) , including carbon dioxide, water vapour and noble gases.
What are the greenhouse gases and what do they do?
Carbon dioxide, methane and water vapour act as an insulating layer in the earth’s atmosphere- this, among other factors, allows the earth to be warm enough to support life.
What do all particles do?
All particles absorb certain frequencies of radiation/
Describe the greenhouse effect in terms of the interaction of short and long wavelength radiation with matter.
-Greenhouse gases don’t absorb the incoming short wavelength radiation from the sun but they do absorb the long wavelength radiation that gets reflected back off the earth.
- Then they re-radiate it in all directions; including back towards the earth.
- The long wavelength radiation is thermal radiation, so it results in warming of the surface of Earth.
What forms of human activity affect the amount of greenhouse gases in the atmosphere?
deforestation, during fossil fuels, agriculture and creating waste.