chem of atmosphere Flashcards
phase 1
- 1st billion years surface covered with volcanoes that erupted and released lots of gases
- this is how we think early atmosphere was formed
what was early atmosphere probably mostly made up of
carbon dioxide
virtually no oxygen
(similar to atmopsheres of mars and venus today)
volcanic activity also released nitrogen which built up in atmosphere over time as well as water vapour and small amounts of methane and ammonia
Phase 2
- water vapour in atmosphere condensed and formed oceans
- lots of carbon dioxide removed from early atmosphere as it dissolved in oceans
- marine animals evolved their shells and skeletons contained some carbonates from the oceans
- green plants and algae evolved and absorbed some carbon dioxide in order to carry out photosynthesis
what happened to dissolved carbon dioxide in oceans
went through series of reactions to form carbonate precipitates that formed sediments on the seabed
what happened to some carbon that organisms took up from atmosphere when they died
it became locked up in rocks and fossil fuels
how do fossil fuels and rocks containing carbon form
- marine animals die and fall to seabed and get buried by layers of sediment
- over 1 mill years they become compressed and form sedimentary rocks, oil and gas, trapping carbon within them
examples of fossil fuels
coal, crude oil, natural gas
crude oil and natural gas
formed from deposits of plankton and form reservoirs under seabed when thet get trapped in rocks
coal
it is sedimentary rock made from thick plant deposits
limestone
sedimentary rock made mostly of calcium carbonate deposits from shells and skeletons of marine organisms
phase 3
- green plants and algae produce oxygen by photosynthesis
- algae evolved first (2.7 bill years)
- then over next bill years green plants evolved
- as oxygen levels built up in atmosphere over time more complex life like animals could evolve
composition of atmopshere today and when did the atmosphere reach this point
approx. 200 million years ago
* 80% nitrogen
* 20% oxygen
* small amount of other gases each making up less than 1% ( carbon dioxide, noble gases, water vapour)
what do greenhouse gases do + examples
(carbon dioxide, methane, water vapour)
* act like an insulating layer in the earths atmosphere which contributes to allowing the earth to be warm enough to support life
greenhouse effect
- don’t absorb incoming short wavelength radiation from sun
- do absorb long wavelength radiation that gets relfected back off earth
- they then re-radiate in all directions including back towards earth
- longwave radiation is thermal radiation so results in warming the surface of the earth
examples of human activity that affect amount of greenhouses gases in atmosphere
- deforestation (fewer trees= less Co2 removed via photosyntheis)
- burning fossil fuels (carbon ‘locked up’ in these fuels is released in form of CO2)
- agriculture (more farm animals produce more methane through their digestive processes)
- creating waste (more landfill sites, more agricultural waste means more CO2 and methane released by decomposition of waste