chemistry of the atmosphere Flashcards
atmospheric gas proportions today
approximately 78% nitrogen approximately 21% oxygen small proportions of various other gases: - carbon dioxide - water vapour - noble gases.
why is evidence of he early atmosphere limited?
because of the time scale of 4.6 billion years, therefore theories about what was in the Earth’s early atmosphere and how the atmosphere was formed have changed and developed over time
gas proportions in early atmosphere
mostly carbon dioxide with little or no oxygen gas
reasons for the early atmosphere
intenseVOLCANIC activity that released gases - volcanoes also produced NITROGEN (which gradually built up in the atmosphere), - small proportions of methane and ammonia - water vapour formed oceans
how carbon dioxide decreased
- carbon dioxide dissolved in the ocean and
- carbonates were precipitated producing sediments
- photosynthesis (by algae and plants)
- formation of sedimentary rocks and fossil fuels that contain carbon
- marine aminals formed removing carbonates from the oceans to produce shells
how oxygen increased
- photosynthesis (by algae and plants)
word equation for photosynthesis
carbon dioxide + water –light energy–> glucose + oxygen
symbol equation for photosynthesis
6CO2 + 6H2O —> C6H12O6 + 6O2
how many years ago did the earth form?
4.6 billion years ago
when did the first photosynthetic organisms form?
2.7 billion years ago
name greenhouse gases
Water vapour
carbon dioxide
methane
explain the greenhouse effect
_sun emits SHORT wavelengt_h infrared radiation that enters the atmosphere and travels towards the Earth’s surface.
Earth ABSORBS some of this radiation
LONG wavelength radiation is REFLECTED back into the atmosphere.
Greenhouse gases can’t absorb the frequency of radiation emitted by the SUN (SHORT), but they can ABSORB the LONGER wavelength reflected radiation.
gases then RE-RADIATE this energy in all directions, including back towards Earth.
This increases the temperature at the Earth’s surface.
good use of the greenhouse effect
maintains temperatures on Earth high enough to support life
Human activities which contribute to an increase in greenhouse gases in the atmosphere
land fills (more decomposition which releases methane)
deforestation (less photosynthesis = less uptake of CO2)
agriculture (animals release methane during digestion)
burining fossil fuels (releases carbon in the form of CO2)
scientific concensus on greenhouse effect
human activities will cause the temperature of the Earth’s atmosphere to increase at the surface
and that this will result in global climate change
(all based on PEER-REVIEWED evidence)