Chemistry of the Atmosphere Flashcards
what is the percentage composition of the atmosphere?
- 78% nitrogen
- 21% oxygen
- 1% all other gases incl. water vapour and CO2 (0.03%)
what was the atmosphere like 4.6 billion years ago?
- massive amounts of volcanic activity helped the earth cool down more quickly by releasing heat energy
- large amounts of CO2 released, as a consequence, along with water vapour - but the earth’s surface was still too hot for the water vapour to condense onto - at this time the atmosphere was ~90% CO2
what was the atmosphere like 3.4 billion years ago?
- the earth’s surface became cool enough for water to condense onto it, allowing lakes, rivers and oceans to develop
- CO2 dissolved into the developing oceans, enabling the amount of CO2 in the atmosphere to decrease
what was the atmosphere like 2.7 billion years ago?
- plants and algae photosynthesised, decreasing CO2 and increasing O2 levels
- O2 reacted in the atmosphere to produce ozone (O3) providing a protective layer of gas around the outer limits of the atmosphere, protecting life on earth from UV radiation
what was the atmosphere like 200 million years ago?
- oxygen rich, CO2 poor
- Nitrogen levels in the atmosphere begin to increase as denitrifying bacteria in soil break down compounds containing nitrogen
describe 5 ways in which today’s atmosphere is different from that of the Earth 4.6 billion years ago
- Higher oxygen levels
- higher nitrogen levels
- lower co2 levels
- less water vapour
- less hydrogen
describe the 4 key events that scientists theorise have changed the composition of the Earth’s atmosphere, from what is was 4.6 billion years ago to what it is today
- earth’s surface cooled enough for water vapour to condense on it
- CO2 dissolved in newly formed oceans and rivers
- plants and algae that photosynthesise began to evolve, increasing O2 and decreasing CO2 levels
- denitrifying bacteria began to break down nitrogen-containing compounds
what were the factors that reduced atmospheric carbon dioxide levels?
- formation of the oceans
- photosynthetic organisms evolved
- evolution of marine animals
how is human activity causing CO2 levels to rise?
- by unlocking carbon dioxide that has been locked up in fossil fuels and sedimentary rocks
- deforestation
- cattle farming
how is carbon dioxide unlocked from fossil fuels and sedimentary rocks?
- burning fossil fuels releases locked-up CO2 and energy - CH4 + O2 ⇒ CO2 +H2O
- thermal decomposition of limestone to produce cement and concrete released locked-up CO2 - CaCO3 ⇒ CaO + CO2
how do greenhouse gases cause global warming?
- UV radiation with a short wavelength comes from the sun and hits the earth’s surface
- it reflects as longer wavelength infra-red radiation but can’t get through the greenhouse gases, so the heat gets trapped
how do greenhouse gases help to support life on earth?
stop infra-red radiation passing out of the atmosphere and trapping heat which maintains a suitable temperature for life to thrive.
give two potential consequences of rising sea levels
Increased flooding and loss of coastal habitats/coastal erosion
give some potential consequences of climate change
Rising sea levels, extreme weather events, loss of biodiversity, crop failure and famine, drought
name 5 atmospheric pollutants from burning fossil fuels
- Carbon monoxide
- sulfur dioxide
- nitrogen oxides (NOx gases)
- carbon particulates
- carbon dioxide