Ozone Depletion Topic 5 Atmosphere A S S

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Ozone Depletion Topic 5 Atmosphere A. S: S – W Depletion of Stratospheric Ozone

Ozone Depletion Topic 5 Atmosphere A. S: S – W Depletion of Stratospheric Ozone

The Role of Ozone • Stratospheric ozone shields earth against biologically harmful Ultraviolet radiation

The Role of Ozone • Stratospheric ozone shields earth against biologically harmful Ultraviolet radiation (up to 99%). • UV rays are absorbed during the formation and destruction of ozone (O 3) from oxygen (O 2).

How is ozone formed? • Ozone, under natural conditions, is constantly being consumed and

How is ozone formed? • Ozone, under natural conditions, is constantly being consumed and created by a cyclic photolytic reaction. What does this mean? • Oxygen (O 2) is continuously being converted to ozone (O 3) and back again to O 2. • Reaction is driven by UV rays • Net Reaction: 2 O 3 + UV 3 O 2 • It is in steady state equilibrium

Depletion of Ozone • The natural process of ozone formation is slowing down due

Depletion of Ozone • The natural process of ozone formation is slowing down due to gases that we are putting into the atmosphere! • Halogenated organic gases like Chlorofluorocarbons (CFCs) and molecules with chlorine, flourine and bromine, and nitrous oxide (N 2 O). • CFCs are used as aerosol propellants, gas blown plastics like Styrofoam and plastic bottle shapes, pesticides, flame retardants, and as refrigerants. • These gases cause ozone in the stratosphere to be destroyed faster than it is formed.

http: //www. epa. gov/ozone/science

http: //www. epa. gov/ozone/science

How Does Depletion Occur? • CFCs are stable in the troposphere and were thought

How Does Depletion Occur? • CFCs are stable in the troposphere and were thought to be heavy enough to stay in there, however, they move from troposphere into stratosphere • UV breaks off chlorine molecule (Cl) from CFC • Cl acts as a catalyst to break down ozone (O 3) – catalyst – promotes a chemical reaction without itself being used up in the reaction. – shifts equilibrium of oxygen / ozone reaction. – more O 3 destroyed than made.

Effects of UV radiation • Damage DNA, causes many problems, including cancer. • Increase

Effects of UV radiation • Damage DNA, causes many problems, including cancer. • Increase in skin cancer & cataracts. • Lower crop yield • Decline in forest productivity • Reduction of surface dwelling phytoplankton, which would therefore affect who? – This would impact ocean productivity and oxygen production. • Damage & degrade materials paints & plastics

Methods of reducing the manufacture and release of ozone depleting substances 1. Use of

Methods of reducing the manufacture and release of ozone depleting substances 1. Use of CFC Alternatives: • Replace CFCs with: • HFCs (hydrofluorocarbons) - alternative to CFCs don’t contain chlorine. – Contain fluorine (1000 times less efficient in UV Reactions) • HCFC - replace a Cl atom with H atom which enables it to be broken down in troposphere. – Problem: if it gets to stratosphere it will deplete ozone • **The problem with most of these replacements is that they are greenhouse gases!** 2. Recycle old refrigerators to allow for the proper capture and disposal of the CFCs inside.

Role of national & world organizations in reducing the emissions of ozone depleting substances

Role of national & world organizations in reducing the emissions of ozone depleting substances National: • EPA made amendments to 1967 clean air act and is responsible for monitoring air quality standards for hazardous substances. International: • UNEP has had a key role in providing information, and creating and evaluating international agreements, for the protection of stratospheric ozone. • An illegal market for ozone-depleting substances persists and requires consistent monitoring.

Montreal Protocol “Perhaps the single most successful international agreement to date has been the

Montreal Protocol “Perhaps the single most successful international agreement to date has been the Montreal Protocol. ” -Kofi Annan, Former Secretary General of the United Nations • UNEP agreement originally signed in 1987; amended in 1990 & 1992. • The treaty provided a timetable on which the production of ozone depleting substances must be phased out and eventually eliminated. • Provided aid for developing nations to do so as well. • If international agreement is adhered to, ozone layer expected to recover by 2050. IMPACTS: Atmospheric concentration of CFCs has leveled off and/or decreased. Concentration of HFCs (an alternative) has increased substantially. Currently there are plans for a complete worldwide phase out by 2030.