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Biology Project on Ozone

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Akansha Agarwal
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    OZONE DEPLETION

    Submitted by :- Yash Singh

    Class- XII-A

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    CERTIFICATE

    TO WHOMSOEVER IT MAY CONCERN:-

    This is to certify that Yash Singh, student of class XII-A, Delhi Public

    School, Kalyanpur, have successfully completed his project on OZONE

    DEPLETION, under my guidance. While doing the report they got

    exposure of the latest environmental problems that are surfacing, majorly

    ozone depletion and the aftermath. He acquired good knowledge of

    concepts, sense of responsibility, professional judgment and decision

    making ability.

    Mrs. Rupali Tyagi

    ( Mentor)

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    CONTENTS

    Introduction

    1) ULTRAVIOLET RAYS

    1.1) Sources of UV rays

    1.2) UV-A, UV-B & UV-C

    2) EFFECTS OF UV RADIATION ON NATURE

    2.1) Damage to marine life

    2.2) Degradation of polymers, pigments and dyes

    3) HARMFUL EFFECTS ON HUMANS

    3.1) Effects on Eye

    3.2) Effects on Skin

    3.3) Genetic effects

    3.4) Effects on immune system

    4) OZONE DEPLETION AND UV RADIATIONS

    5) VULNERABILITIES DUE TO UV RADIAT1ONS

    ULTRAVIOLET RAYS

    Bibliography

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    INTRODUCTION

    In the present 21st century world, one does not need to say about ultra

    violet rays, it is the most ignited topic in this era. From the common man

    to the Academicians, UV rays hold an important place in their debate.

    UV rays have been discussed for a long time all around the world

    especially after the discovery of the hole in the ozone layer in 1990s.The

    hole meant the approaching slow death of our mother earth. A host of

    studies on this topic has been undertaken by many people and

    organizations such as the United Nations, Green Peace, etc.

    At the United Nations Conference on Environment

    and Development (UNCED) in 1992, it was declared under Agenda 21

    that there should be activities on the effects of UV radiation. In response

    to Agenda 21, WHO in collaboration with the United Nations

    Environment Programme, the World Meteorological Organization, The

    International Agency on Cancer Research and the International

    Commission on Non-Ionizing Radiation Protection set up Intersun, The

    Global UV Project.

    Even when the whole world only speaks about this great calamity that has

    befallen on our mother earth, it would surely be a great injustice on part

    of the young generation as this slow killer is growing old with the young

    generation and they are the one who should live on this earth with thisgrowing menace. Thus taking into consideration of these points, this

    project has been taken up not only to know about UV rays but also how it

    affects the bio diversity of our planet and how its effect can be

    minimized.

    Here, this project deals with the above mentioned points. Also the project

    aims to give a comprehensive picture on the impending disaster that

    would take place if we be ignorant on this issue.

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    In 1801, the German Physicist Johann Wilhelm Ritter, found that there is

    existence of some invisible rays beyond the violet end of the visible

    spectrum of the light. Those invisible rays darken silver chloride even

    more efficiently than visible light. This spectra region between visible

    light and X-rays was found to be more chemically active than visible

    light, and was named as the ultraviolet region.

    Ultraviolet (UV) light is electromagnetic radiation with a wavelength

    shorter than that of visible light, but longer than x-rays, in the range of 10

    nm to 400 nm, and energies from 3 eV to 124 eV.

    The name Ultra Violet means beyond violet (from Latin ultra, =

    beyond). Violet, being the colour of the shortest wavelengths of visible

    light, UV light has even shorter wavelength than that of the violet light.

    The electromagnetic spectrum of ultraviolet light can be subdivided in a

    number of ways. The draft ISO standard on determining solar radiances

    (ISO-DIS-21348) describes the following ranges:

    Name AbbreviationWavelength range in

    nanometers

    Energy per

    photon

    Ultraviolet A, long

    wave, or black lightUVA 400 nm320 nm 3.103.94 eV

    Near NUV 400 nm300 nm 3.104.13 eV

    Ultraviolet B or medium

    waveUVB 320 nm280 nm 3.944.43 eV

    Middle MUV 300 nm200 nm 4.136.20 eV

    Ultraviolet C, short

    wave, or germicidalUVC 280 nm100 nm 4.4312.4 eV

    Far FUV 200 nm122 nm 6.2010.2 eV

    Vacuum VUV 200 nm10 nm 6.20124 eV

    Extreme EUV 121 nm10 nm 10.2124 eV

    SOURCES OF UV RAYS

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    The Sun emits ultraviolet radiation in UV-A, UV-B, and UV-C bands.

    The Earths ozone layer blocks 98.7% of this UV radiation from

    penetrating through the Earths atmosphere. 98.7% of the ultraviolet

    radiation that reaches the Earths surface is UVA.

    Other sources: There are also several artificial methods to produce UV

    rays such as from black light (Woods light), Ultraviolet fluorescent

    lamps, Ultraviolet LEDs, Ultraviolet lasers, synchrotron radiation

    sources, Argon and deuterium discharge lamps etc.

    UV-A, UV-B & UV-C

    Among the different types of UV rays, we consider the main subdivisions

    as UV-A, UV-B & UV-C.

    UV-A (320-400

    nm):-

    Ultraviolet light, type A. These are rays of light from the sun which are

    not visible but can cause damage to the skin.UV-B (280-320 nm) :-

    Ultraviolet light, type B.

    These are rays of light from the sun which are not visible but can cause

    damage to the skin.

    The amount of UV-B light received by a location is strongly dependent

    on:- Latitude and elevation of the location: - At high-latitude Polar

    Regions, the sun is always low in the sky. So the sunlight passes

    through atmosphere and most of the UV-B rays are absorbed. For

    this reason, average UV-B exposure at the poles is over a thousand

    times lower than at the equator.

    Cloud Cover: - The reduction in UV-B exposure depends on the

    thickness of cloud cover.

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    Proximity to an industrial area: - Due to the protection offered

    by photochemical smog, industrial processes produce ozone, one of

    the most irritating components of smog. So it absorbs UV-B. This

    is thought to be one of the main reasons of ozone losses in the

    southern hemisphere. The loss has not been mirrored in the

    northern hemisphere.

    UV-C (100-280 nm) : - UV-C rays are highest energetic and most

    dangerous type of ultraviolet light. Exposure to it can even lead to death.

    Little attention has been given to UV-C rays in the past since they are

    filtered out by the atmosphere. However, their use in equipment such as

    pond sterilization units may pose an exposure risk, if the lamp is switched

    on outside of its enclosed pond sterilization unit.

    EFFECTS OF UV RADIATION ON NATURE

    The effects of UV radiation on earths ecosystems are not completely

    understood. Even isolating the effects of UV-A versus UV-B is somewhat

    arbitrary. Studies have shown that increased UV radiation can cause

    significant damage, particularly to small animals and plants.

    Phytoplankton, fish eggs, and young plants with developing leaves are

    particularly susceptible to damage from over exposure to UV. Solar UV

    radiation levels are highest during the middle of the day. In total, almost

    half the daytime the total UV radiation is received during the few hours

    around noontime. The sunlight reaching us consists of approximately

    0.5% of UV-B radiation in terms of radiant energy. Clouds, as well as

    ozone have a tremendous affect on UV radiation levels. However, cloudy

    skies generally do not offer significant protection from UV. Thin or

    scattered clouds can have minor impacts on UV and even, for a short time

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    increase in UV, it would be on a blue sky day by further scattering the

    radiation and increasing the levels that reach the surface.

    DAMAGE TO MARINE LIFE

    The penetration of increased amounts of UV-B light has caused great

    concern over the health of marine plankton that densely populates the top

    2 meters of ocean water. The natural protective response of most

    chlorophyll containing cells to increased light-radiation is to produce

    more light-absorbing pigments but this protective response is not

    triggered by UV-B light. Another possible response of plankton is to sink

    deeper into the water but this reduces the amount of visible light that they

    need for photosynthesis, and thereby reduces their growth and

    reproduction rate. In other words, the amount of food and oxygen

    produced by plankton could be reduced by UV exposure without killing

    individual organisms.

    DEGRADATION OF PIGMENTS, POLYMERS AND DYES

    Many polymers used in consumer products are degraded by UV light.

    The problem appears as discoloration or fading, cracking and sometimes

    disintegration of total product, if cracking has proceeded sufficiently. Therate of attack increases with exposure time and sunlight intensity. It is

    known as UV degradation, and is one form of polymer degradation.

    Sensitive polymers include thermoplastics, such as polypropylene and

    polyethylene as well as special fibres like Aramids. There are several

    other considerations:

    Ultraviolet levels are over 1,000 times higher at the equator than at

    the Polar Regions so it is presumed that marine life at the equator is

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    much better adapted to the higher environmental UV light radiation

    than organisms in the Polar Regions. The current concern of

    marine biologists is mostly over the more sensitive Antarctic

    phytoplankton which normally would receive very low doses of

    UV. Only one large-scale field survey of Antarctic phytoplankton

    has been carried out so far [Smith et.al _Science_1992]; they found

    a 6-12% drop in phytoplankton productivity in Antarctica. Since

    the hole only lasts from 10-12weeks, this translates into a 2-4%

    loss overall, a measurable but not yet a catastrophic loss.

    Both plants and phytoplankton vary widely in their sensitivity to

    UV-B. When over 200 agricultural plants were tested, more than

    half of them showed sensitivity to UV-B light. Other plants showed

    a small increase in vigor or even negligible effects. Even within a

    species there were marked of differences. For example, one variety

    of soybeans showed a 16% decrease in growth while another

    variety of the same soybean showed no effect [R. Parson]. An

    increase in UV-B could cause a shift in population rather than a

    large die-off of plants.

    An increase in UV-B will cause in production of Ozone at lower

    levels in the atmosphere. While some have hailed the protectionoffered by this pollution-shield. Many plants have shown

    themselves to be very sensitive to photochemical smog.

    HARMFUL EFFECTS ON HUMANS

    Being the one which commonly affects our health, we usually discuss the

    harmful effects of UV-B. The consequences of increased exposure of the

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    human body to UV-B radiation will in the first instance be characterized

    by the physical properties of this type of radiation. UV-B radiation does

    not penetrate far into the body as most of it is absorbed in the superficial

    tissue layers of 0.1 mm depth. This limits the primary effects to the skin

    and the eyes. However, there are also systemic effects. These start with a

    primary reaction in the superficial layers, but have consequences

    throughout the body. It is the main cause of sunburn and tanning and it

    has some influences on the immune system too. UV-B radiation is also

    the main cause of snow blindness and an important factor in the induction

    of cataracts. UV-B radiation contributes significantly to the ageing of the

    skin and eyes and it is the UV-B range that is most effective in causing

    skin cancer.

    GENETIC

    Ultraviolet photons harm the DNA molecules of living organisms in

    different ways. DNA absorbs UV-B light and the absorbed energy can

    break bonds in the DNA. Most of the DNA breakages are repaired by

    proteins present in the cells nucleus. These may mend the damage or part

    of the damage. The repair systems may, however, themselves be damaged

    by increased UV-B exposure. But unrepaired genetic damage of the DNA

    can lead to skin cancers. In one common damage event, adjacent thymine

    bases bond with each other, instead of across the ladder. This makes abulge, and the distorted DNA molecule does not function properly.

    EFFECTS ON SKIN

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    1. Sunburn:

    One of the most common effects of UV exposure is erythema also

    known as sunburn. Sunburn occurs when skin cells are damaged by the

    absorption of energy from UV rays. To compensate for this injury, the

    skin sends extra blood to the damaged skin in an attempt to repair it.

    Thus, accounting for the redness that is associated with sunburn, the

    amount of time it takes for sunburn to occur is dependent mostly on the

    relative amounts of UV rays that are hitting the skin and on a personsskin type. People with naturally dark skin already have inherently high

    levels of melanin, and so are able to spend a longer amount of time in the

    sun before burning. Fair-skinned people dont have it quite so easy as

    burning can occur within a relatively short amount of time.

    2. Sun tan: As a defence against UV radiation, the amount of the brownpigment melanin in the skin increases when exposed to moderate

    (depending on skin type) levels of radiation. This is commonly known as

    sun tan. The purpose of melanin is to absorb UV radiation and dissipate

    the energy as harmless heat, blocking the UV from damaging skin tissue.

    UV-A gives a quick tan that lasts for days by oxidizing melanin that was

    already present and triggers the release of the melanin from melanocytes.

    UV-B yields a tan that takes roughly 2 days to develop because it

    Ultraviolet (UV) radiation present in sunlight is an

    environmental human carcinogen. The toxic effects of UV from

    natural sunlight and therapeutic artificial lamps are a major

    concern for human health. The major acute effects of UV

    irradiation on normal human skin comprise sunburn,

    inflammation, erythema, tanning and local or systemic

    immune-suppression.

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    stimulates the body to produce more melanin. The photochemical

    properties of melanin make it an excellent photoprotectant.

    Photodermatoses: Photodermatoses are skin diseases where the skin

    lesions are caused by light. Such lesions may be itching papules, whaling

    of the skin, fierce reddening and peeling etc. The more sensitive patients

    cannot even stand one minute of outdoor daylight. In these diseases the

    UV-B radiation in sunlight is the predominant causative agent. Loss of

    adaptation of the skin to light appears to be a predominant factor for these

    diseases.

    Premature Ageing of Skin: Another effect of ultraviolet rays on the

    skin is premature ageing of the skin. Recent studies have shown that

    many of the symptoms commonly associated with mere ageing (i.e.

    wrinkles, loosening of the skin) may instead be related to UV exposure.

    Even careful tanning kills skin cells, damages DNA and causes

    permanent changes in skin connective tissues which lead to wrinkle

    formation in later life. UV-A, UV-B and UV-C, all these can damage

    collagen fibers and thereby accelerate aging of the skin. Both UV-A and

    UV-B destroy vitamin A in skin which may cause further damage.

    5. Skin Cancer: 9 0% of the skin carcinomas are attributed to UV-Bexposure [Wayne] and the chemical mechanism by which it causes

    skin cancer has been identified [Tevini]. The above named

    carcinomas are relatively easy to treat, if detected in time, and are

    rarely fatal.

    There are various types of skin cancer. One main class is formed by the

    coetaneous melanomas, the cancers of the pigment cells. This appears to

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    be a correlation between brief and high intensity exposures to UV and

    eventual appearance (as long as 10-20yrs) of melanoma.

    The other main types are basal cell carcinomas and squamous cell

    carcinomas, cancers of the epithelial cells. These carcinomas of the skin

    are sometimes, collectively, called non-melanoma skin cancers. For the

    present example we will deal with these non-melanoma skin cancers. In

    white Caucasians, the incidence of these cancers ranks high among the

    various types of cancer. In some populations it is in fact the highest of all.

    The incidence is lower in more pigmented populations, typically by a

    factor of 10 or even 100. The mortality rate is low in comparison with

    that for other types of cancer approximately 1% in areas with good

    medical care.

    The non-melanoma skin cancers are clearly correlated to sunlight. They

    occur mostly in light-skinned people and then predominantly on skin

    areas which are most exposed to sunlight, such as the face. In people of

    comparable genetic background, the incidences are higher in the sunnier

    geographical areas.

    Early experiments showed that white rats exposed to sunlight developed

    skin cancers, but similar rats exposed to sunlight filtered through window

    glass did not. As the window glass absorbed mainly UV-B radiation, this

    result indicated that the carcinogenic effect to a large extent due to the

    UV-B radiation in sunlight.In technical terms, carcinogenic effectiveness was defined as the

    reciprocal value of the daily dose of radiation at a certain wavelength

    required for the induction of tumors of 1 mm diameter in 50% of a group

    of mice in 300 days. The tumors in these mice were predominantly

    squamous cell carcinomas.

    DNA

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    UV-B light can cause direct DNA damage. The radiation excites DNA

    molecules in skin cells, causing aberrant covalent bonds to form between

    adjacent cytosine bases, producing a dimer. When DNA polymerase

    comes along to replicate this strand of DNA, it reads the dimer as AA

    and not the original CC. This causes the DNA replication mechanism

    to add a TT on the growing strand. This is a mutation, which can result

    in cancerous growths and is known as a classical C-T mutation. The

    mutations that are caused by the direct DNA damage carry a UV

    signature mutation that is commonly seen in skin cancers.

    EFFECTS ON EYES

    High intensities of UV-B light are hazardous to the eyes and exposure can

    cause welders flash (photokeratitis or arc eye) and may lead to cataracts,

    pterygium, and pinguecula formation. Another possible eye damage that

    can result from high doses of UV light is particularly to the cornea which

    is a good absorber of UV light. High doses of UV light can cause a

    temporary clouding of the cornea called snow-blindness and chronic

    doses has been tentatively linked to the formation of cataracts. High

    incidences of cataracts are found at high elevations, Tibet and Bolivia and

    higher incidences are seen at lower latitudes (approaching the equator).

    UV light is absorbed by molecules known as chromophores, which arepresent in the eye cells and tissues. Chromophores absorb light energy

    from the various wavelengths at different rates a pattern known as

    absorption spectrum. If too much UV light is absorbed, eye structures

    such as the cornea, the lens and the retina can be damaged.

    EFFECTS ON IMMUNE SYSTEM

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    Prolonged exposure can damage the human immune system. Cells or

    tissue components which are altered by the radiation may be recognized

    as foreign material by the immune system and are removed. Certain

    functions of the immune system are however, suppressed by exposure to

    UV-B radiation. When skin is exposed to more UV-B radiation then it is

    accustomed to its ability to adapt.

    OZONE DEPLETION AND UV RADIATIONS

    Ozone depletion results in an increase of UV-B radiation, but the shorter

    the wavelength, the stronger the increase within the UV-B range. 1%

    decrease in the ozone layer will cause an estimated 2% increase in UV-B

    irradiation; it is estimated that this will lead to a 4% increase in basal

    carcinomas and 6% increase in squamous-cell carcinomas [Graedel &

    Crutzen]. Many scientists today believe that this life-protecting

    stratospheric ozone layer is being reduced by the chlorofluorocarbon

    (CFCs) gases released into the atmosphere by different sources on the

    earth. Many environment groups are vehemently protesting against the

    use of these gases and their use in many places in the world has been

    banned. Pollution on the earth has already caused a hole in the ozone

    layer above the Antarctic.

    VULNERABILITIES DUE TO UV RADIATIONSA diagram produced by WHO based on global burden of diseases from

    solar ultraviolet radiation in the year 2006.

    CONCLUSION

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    Thus we can conclude that UV rays have a disastrous impact on our

    planet. It will lead to many dangers which would affect not only us but

    also the entire living community on this earth. UV rays can lead to many

    unforeseen disasters which can signal the end of life on this beautiful

    planet.

    All the dangers attributed to UV rays reaching our earth reside only on

    man. Man by his reckless actions has dug graves not only for himself but

    also for the earth too. Its his only responsibility to restore the earth back

    to its healthy mode.

    Thus, a concerted effort is needed on the side of mankind to quickly

    address this danger. Steps have to be taken from individual to the

    international level to protect our earth. From abandoning plastics to

    decrease the dependence on automobiles, man has to be careful to ensure

    that he does not push earth to its death. We also need to ensure that we do

    not create UV rays by machines and their usage must be strongly

    restricted only to the academic field. Also we need to create awareness

    among ourselves on the need of the hour to protect life. Its a pity that we

    try to blame domestic animals for increasing the levels of methane in the

    atmosphere. What we need to understand is that their methane levels are

    nothing as compared to our creation of a hole on the ozone layer. Their

    actions are too small to be compared to our sins.

    Being a part of future generation, the student community also needs to beaware about the topic which is a prime reason for me selecting this

    project. We too should take care not to harm our earth in any way.

    Always we should remember that we have not inherited the earth

    from our fathers but have leased it from our future

    generations. This alone will make us responsible and be steadfast in

    our Endeavour to combat the penetration of UV rays.

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    Bibliography

    http://www.google.com

    http://www.wikipedia.org

    www.epa.gov/ozone

    environment.nationalgeographic.com/.../ozone-depletion-

    overview

    ozonewatch.gsfc.nasa.gov

    http://www.google.com/http://www.wikipedia.org/http://www.epa.gov/ozonehttp://www.google.com/http://www.wikipedia.org/http://www.epa.gov/ozone