chemistry of the atmosphere

    Cards (39)

    • percentage of gases in earths atmosphere - dry air (no water molecules)
      * nitrogen - 78%
      * oxygen - 21%
      * carbon dioxide - 0.04%
      * argon - 0.9%
      * other gases - 0.06%
    • how much water vapour can air contain (%)
      up to 5%
    • when was the earths early atmosphere
      4.6 billion yers ago
    • how did the early atmosphere evolve
      1 ) a lot of volcanic activity so atmosphere mainly made up of co2 and a bit of h2o, ch4, nh3, n2 - earth was very hot so no animal or plant life
      2 ) planet cooled so water vapour condensed to form oceans
      3 ) bacteria and algae evolved and then photosynthesised to produce oxygen
      4 ) co2 starts to decrease
      5 ) other gases decrease and some increase
    • how does co2 start to decrease in the early atmosphere
      1 ) photosynthesis
      2 ) sedimentary rocks take it in - dead sea matter builds up at bottom of ocean and forms rocks like limestone
      3 ) fossil fuels - some remains of these organisms become fossil fuels
    • why does methane decrease
      methane + oxygen = carbon dioxide + water
    • why does ammonia decrease
      ammonia + oxygen = nitrogen + water
    • why does nitrogen increase
      * inert / very unreactive
      * build up over time
    • how does the greenhouse effect work
      1 ) sun heats up earth with infrared radiation / heat
      2 ) some reflected back into space off atmosphere
      3 ) some infrared radiation absorbed by earths surface
      4 ) molecules of greenhouse gases absorb infrared radiation on its way out, “trapping” it in the earths atmosphere
    • adv v dis of greenhouse effect
      adv : if didn’t exist, earth would be too cold for life to form
      dis : increasing levels of greenhouse gases mean that scientists believe it is heating up earth too much
    • human activity - co2
      1 ) burning fossil fuels
      2 ) deforestation - reduces planets capacity to absorb co2
      3 ) oceans became less able to absorb co2 - rising
    • human activity - ch4
      1 ) swamp
      2 ) grazing cattle
      3 ) landfill
      4 ) rice fields / decomposing waste
    • why do people not believe humans are impacting climate change
      atmosphere temperature fluctuates
    • evidence of climate change (levels of co2 and temp increase)
      air pockets in ice cores
    • what type of radiation is absorbed by greenhouse gases
      long wavelength radiation (infrared / heat)
    • how does long wavelength cause global warming
      1 ) absorbed by greenhouse gases
      2 ) make bonds in molecules vibrate, bend and stretch more vigorously
      3 ) this raises the temperature as heat is trapped is trapped in the atmosphere
    • what are the main greenhouse gases
      h2o - water vapour
      co2 - carbon dioxide
      ch4 - methane
    • how much is the atmosphere temperature meant to rise in the next 100 years
      increase 5.8 degrees
    • 4 main effects of global change
      1 ) rising sea levels = flooding
      2 ) more frequent and extreme weather events
      3 ) changes to temp and rainfall - affects food production and how different countries grow food
      4 ) stress of ecosystems
    • what is the carbon footprint
      total amount of co2 and other greenhouse gases emitted over a full life cycle of a product, service or event
    • ways to reduce carbon footprint
      1 ) carbon capture - pump co2 into ground (expensive)
      2 ) plant based diet - reduce demand for beef and lowers transport
      3 ) insulate homes
      4 ) reforestation
      5 ) use alternative energy resources
    • what are atmospheric pollutants
      substances that contaminate the air making it harmful or damaging for human health or the environment
    • source of atmospheric pollutants
      factories
      lorries
      cars
    • examples of atmospheric pollutants
      water vapour - already in air
      carbon dioxide - already in air
      sulfur dioxide
      nitrogen oxides
      carbon monoxide
      carbon particulates
      unburnt hydrocarbons
    • what how does incomplete combustion occur - hydrocarbons
      burning hydrocarbons and fuels with longer chains
    • how is water vapour produced
      1 ) combustion of alkenes
      2 ) incomplete combustion
    • why is water vapour an atmospheric pollutant
      greenhouse gas - contributes to global warming
    • how is co2 produced
      combustion
    • why is co2 an atmospheric pollutant
      greenhouse gas - contributes to global warming
    • how is carbon monoxide produced
      incomplete combustion
    • why is carbon monoxide an atmospheric pollutant
      * colourless odourless gas
      * binds to haemoglobin in instead of oxygen, taking its place
      * starves body of oxygen
    • how are carbon particulates produced
      incomplete combustion
    • how are carbon particulates an atmospheric pollutant
      * small particles of solid carbon
      * global dimming - no photosynthesis
      * damage cells in our lungs
      * cause cancer
    • when are unburnt hydrocarbons released
      alongside carbon monoxide or carbon particulates
    • how is nitrogen oxide produced
      * nitrogen and oxygen in air react
      * very high temperatures in car engines - combustion
      1 ) no2
      2 ) no3
    • how is nitrogen oxide an atmospheric pollutant
      * cause breathing and respiratory problems (asthma)
      * acid rain
    • how is sulfur dioxide produced
      sulfur impurities in fuel react with oxygen
    • how is sulfur dioxide an atmospheric pollutant
      * acidic gas
      * acid rain - damage trees and buildings and harms wildlife
    • prevention of the formation of sulfur dioxide
      * remove sulfur from fuels before burning
      * acidic so2 can be neutralised at factories or power stations