knowt logo

APES Unit 9.1 & 9.2 (Stratospheric Ozone)

Stratospheric Ozone & Life on Earth

  • Ozone in the stratosphere absorbs UV-C and much of UV-B

    • Without ozone layer, life on land would not be possible since UV-B & C radiation causes significant tissue damage & mutates DNA

    • Human Health benefits of startosphereic ozone:

      • Prevention of skin cancer & cataracts

      • UV-B & C mutate DNA (skin cancer) & cause oxidative stress in eyes (cataracts)

  • Tropospheric ozone is bad (respi. Irritant, damaging to plant tissue & prescursor to photochemical smog)

How Ozone Absorbs UV-B & UV-C

  • UV-C breaks into O2 into two free oxygen atoms (2 O)

    • When a free oxygen atom from this rxn combines with an O2 molecule, ozone (O3) is formed

    • UV-C also reverses the rxn by breaking ozone (O3) into O2, and O, which can then bond with another free O to form O2

    • Continued formation and breakdown of O3 in stratosphere absorbs all UV-C & much UV-B radiation (protecting org. On earth)

Antrhopogenic Ozone Depletion

  • CFCs (chlorofluorcarbons) are a primary antrhopogeic (human) cause of O3 breakdown

    • Used as refrigerant chemicals and propellants in aerosol containers (hair spray, febreeze, etc.)

    • UV radiation causes free chlorine atom to separate from CFCs

    • Highly electroneg. Chlroine atom bonds to one of the oxygen atoms of ozoen (O3) converting it into oxygen (O2)

    • Free O atom then bonds to O from chlroine monoxide to form O2 and free CL atom to go break down more O3

    • One singel Cl atom persists in atm. for 50-100 years and can destroy up to 100000 ozone molecules

Natural Ozone Depletion

  • Antartica spring melt forms polar stratospheric clouds (PSC)

    • Clouds made of water & nitric acid (HNO3) that can only form in consistent -100oF temp. Range found above antartica 

    • In prescense of PSCs chlorine nitrate (ClONO2) and hydrochloric acid (HCl) react & give off Cl2

      • CL2 is photolyzed (broken by sun) into 2 free Cl atoms

  • Remember what Cl atoms due to ozone from CFCs (break O3 down into O2 over and over)

Reducing Ozone Depletion

  • Main way to reduce anthropogenic O3 depletion is phasing out & replacing CFCs

    • Montreal Protocol (87’) was a global agreement to phase CFCs out of production in refrigerators, aerosols and other uses

      • Replaced with HCFCs (CFCs with hydrogen added)

      • HCFCs still deplete O3 and act as GHGs but to a lesser degree than CFCs

      • Not a permanent solution, but a temporary transition option (phase out in dev. Nations after 2020, developing nations have until 2030)

    • Replacement for HCFCs is HFCs (still GHGs but not O3 depleting since they don’t contain Cl)

      • Replacements for HFCs are HFOs (just HFCs with C-C double bonds that shorten atm. Lifetime & GWP)

APES Unit 9.1 & 9.2 (Stratospheric Ozone)

Stratospheric Ozone & Life on Earth

  • Ozone in the stratosphere absorbs UV-C and much of UV-B

    • Without ozone layer, life on land would not be possible since UV-B & C radiation causes significant tissue damage & mutates DNA

    • Human Health benefits of startosphereic ozone:

      • Prevention of skin cancer & cataracts

      • UV-B & C mutate DNA (skin cancer) & cause oxidative stress in eyes (cataracts)

  • Tropospheric ozone is bad (respi. Irritant, damaging to plant tissue & prescursor to photochemical smog)

How Ozone Absorbs UV-B & UV-C

  • UV-C breaks into O2 into two free oxygen atoms (2 O)

    • When a free oxygen atom from this rxn combines with an O2 molecule, ozone (O3) is formed

    • UV-C also reverses the rxn by breaking ozone (O3) into O2, and O, which can then bond with another free O to form O2

    • Continued formation and breakdown of O3 in stratosphere absorbs all UV-C & much UV-B radiation (protecting org. On earth)

Antrhopogenic Ozone Depletion

  • CFCs (chlorofluorcarbons) are a primary antrhopogeic (human) cause of O3 breakdown

    • Used as refrigerant chemicals and propellants in aerosol containers (hair spray, febreeze, etc.)

    • UV radiation causes free chlorine atom to separate from CFCs

    • Highly electroneg. Chlroine atom bonds to one of the oxygen atoms of ozoen (O3) converting it into oxygen (O2)

    • Free O atom then bonds to O from chlroine monoxide to form O2 and free CL atom to go break down more O3

    • One singel Cl atom persists in atm. for 50-100 years and can destroy up to 100000 ozone molecules

Natural Ozone Depletion

  • Antartica spring melt forms polar stratospheric clouds (PSC)

    • Clouds made of water & nitric acid (HNO3) that can only form in consistent -100oF temp. Range found above antartica 

    • In prescense of PSCs chlorine nitrate (ClONO2) and hydrochloric acid (HCl) react & give off Cl2

      • CL2 is photolyzed (broken by sun) into 2 free Cl atoms

  • Remember what Cl atoms due to ozone from CFCs (break O3 down into O2 over and over)

Reducing Ozone Depletion

  • Main way to reduce anthropogenic O3 depletion is phasing out & replacing CFCs

    • Montreal Protocol (87’) was a global agreement to phase CFCs out of production in refrigerators, aerosols and other uses

      • Replaced with HCFCs (CFCs with hydrogen added)

      • HCFCs still deplete O3 and act as GHGs but to a lesser degree than CFCs

      • Not a permanent solution, but a temporary transition option (phase out in dev. Nations after 2020, developing nations have until 2030)

    • Replacement for HCFCs is HFCs (still GHGs but not O3 depleting since they don’t contain Cl)

      • Replacements for HFCs are HFOs (just HFCs with C-C double bonds that shorten atm. Lifetime & GWP)

robot