Title: Ozone Layer and Extinction of Species
1Ozone Layer and Extinction of Species
2Contents
- Ozone layer depletion
- Extinction of species and loss of biodiversity
3Ozone Layer Depletion
4Source of ozone
- Consisted of 3 oxygen atoms, unlike ordinary
oxygen molecule (which has 2 atoms). - It has a bluish colour.
5Dual role of Ozone
- At near ground level, ozone is an air pollutant.
Even at a low concentration (ppm), it is
irritating to respiratory system. - It is strongly oxidizing, and is now commonly
used in sterilization of water. - Its presence in the stratosphere is vital to life
on Earth as it can absorb harmful ultra-violet
radiation (known as UVB, wavelength 270-315nm)
from sunlight.
6Structure of Atmosphere
7Source NASA
8Formation of Ozone in stratosphere
- O2 (radiation lt 240nm) ? 2 O
- O2 O M ? O3 M
- Molecule M carries the energy of the reaction but
remain unchanged.
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10Destruction of Ozone (I)
- Ozone can be destroyed by a number of free
radical catalysts, the most important of which
are the hydroxyl radical (OH), the nitric oxide
radical (NO) and atomic chlorine (Cl) and
bromine (Br). - Human activity has dramatically increased the
chlorine and bromine. These elements are found in
certain stable organic compounds, especially
chlorofluorocarbons (CFCs), which may find their
way to the stratosphere without being destroyed
in the troposphere due to low reactivity. Once in
the stratosphere, the Cl and Br atoms are
liberated from the parent compounds by the action
of ultraviolet light, and can destroy ozone
molecules through a variety of catalytic cycles.
11Destruction of Ozone (II)
- Cl O3 ? ClO O2
- ClO O ? Cl O2
- In sum O3 O ? O2 O2
- gtIncrease rate of recombination of oxygen,
leading to an overall decrease in the amount of
ozone.
12Ozone hole in September 2006
Largest hole in the record. Size of North
America
Source NASA
13Concentration Ozone in Antarctic region
14Consequences of Ozone depletion
- Since the ozone layer absorbs UVB ultraviolet
light from the Sun, ozone layer depletion is
expected to increase surface UVB levels. - Possible linked to higher incidence of skin
cancer. - Lead to decrease of crop yield.
15Montreal Protocol
- The Montreal Protocol on Substances That Deplete
the Ozone Layer is an international treaty
designed to protect the ozone layer by phasing
out the production of a number of substances
believed to be responsible for ozone depletion.
The treaty entered into force on January 1, 1989.
- Due to its widespread adoption and implementation
it has been hailed as an example of exceptional
international cooperation - "Perhaps the single most successful international
agreement to date...".
16Ozone Depleting Substances
- Chlorofluorocarbons (CFCs) were used in air
conditioning/cooling units, as aerosol spray
propellants prior to the 1980s, and in the
cleaning processes of delicate electronic
equipment. - It is calculated that a CFC molecule takes an
average of 15 years to go from the ground level
up to the upper atmosphere, and it can stay there
for about a century, destroying up to 100,000
ozone molecules during that time.
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18Current situation
- CFCs have been replaced to some extent by the
less damaging hydro-chloro-fluoro-carbons
(HCFCs), although concerns remain regarding HCFCs
also. In some applications, hydro-fluoro-carbons
(HFCs) have been used to replace CFCs. - HFCs, which contain no chlorine or bromine, do
not contribute at all to ozone depletion although
they are potent greenhouse gases.
19Recovery of Ozone Layer
- Since the adoption and strengthening of the
Montreal Protocol has led to reductions in the
emissions of CFCs, atmospheric concentrations of
the most significant compounds have been
declining. These substances are being gradually
removed from the atmosphere. - By 2015, the Antarctic ozone hole would have
reduced by only 1 million km² out of 25 - Complete recovery of the Antarctic ozone layer
will not occur until the year 2050 or later. - A detectable recovery will not occur until around
2024, with ozone levels recovering to 1980 levels
by around 2068.
20Extinction and Loss of Biodiversity
21Earths Sixth Mass Extinction
- Since 1500 AD, 784 extinctions have been
documented by the International Union for
Conservation of Nature and Natural Resources. - However, since most extinctions are likely to go
undocumented, scientists estimate that during the
last century, between 20,000 and two million
species have become extinct, but the precise
total cannot be determined more accurately within
the limits of present knowledge.
22- The World Conservation Unions IUCN Red List
contains 15,589 species threatened with
extinction in 2004. - According to a 1998 survey of 400 biologists
conducted by New York's American Museum of
Natural History, nearly 70 percent of biologists
believe that we are currently in the early stages
of a human-caused mass extinction - The same proportion of respondents agreed with
the prediction that up to 20 percent of all
living species could become extinct within 30
years (by 2028).
23Cause of extinction of species
- Deforestation
- Habitat destruction, degradation or fragmentation
- Over-exploitation / hunting
- Human population growth
- Pollution
- Introduction of exotic species
- Climate change
24Some examples of extinct species
Dodo on a flightless bird living on A small
island in Indian Ocean. They Are hunted to
extinction in late 17th Century by sailors and
dogs brought By them as food.
25Baiji, Chinese River Dolphin Declared functionaly
extinct in 2006
Bali Tiger gone extinct in 1937
26Link
27Extinction of Species and Biodiversity
- Extinction of species cause a irreversible loss
of biodiversity.
28Importance of biodiversity
- Possible new sources of food and drink in unknown
species - Possible new medicine
- Possible new industrial materials
- Ecosystem provides important vital resources such
as oxygen, fresh water and food. - Leisure, cultural and aesthetic value
29Discussion Question
- What can we do in response of the mass extinction
of species?
30The End