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Wednesday, March 31, 2010

Societal Effects from of Air Pollution

People are mostly oblivious to the effects of air pollution.
They know it�s out there and it is a problem but excepting
skin cancer, there have been very few deaths with a direct
link to air pollution. It is probably because of this that people
aren�t as concerned with air pollution as they should be. Air
pollution has always been around, and has actually been on a
decline since the 1960�s (when coal was the major source of energy.)
It is relatively easy to decrease the amount of pollutants
we emit (each year new laws arise that crack down on
the amount of certain substances that can be released into the air)
but the harm has already been done, and next to impossible to
fix. The ozone layer is the part of the atmosphere that keeps
ultraviolet rays from penetrating humans and plants. But
because of all the air pollution, various chemicals are
slowly destroying the ozone layer. Each year the concentration
of the ozone decreases by approximately two percent and the
ozone layer over the South Pole is already fifty percent
of its
natural concentration. Ozone
depleters (the majority of which are
chlorofluorocarbons or CFC�s) react with
ultraviolet radiation and break down into their
component atoms, especially chlorine, bromine
and fluoride. These component atoms then go on
to steal an oxygen atom from the ozone layer
(opposite to the reaction which forms O3), thereby
destroying the ozone layer. This loss of protection from
UV rays can result in an increase of human skin cancer,
damage to various parts of the eyes as well as causing a
breakdown of the immune system. With health being such
a major issue in our society today, people have become
scared by this "outbreak" of cancer. People know that the
ozone layer is slowing depleting and that there is a health risk
involved with being in the sun for extended periods of time.
But very few people know that there is a connection between
this breakdown of the ozone layer and air pollution. Instead
of trying to control pollution emissions they just cut back on
their time outdoors, or wear more sunscreen. Ultraviolet
rays can also cause major environmental problems. These
rays enter the atmosphere and can kill small aquatic organisms,
such as plankton. When these small life forms decompose they
release carbon dioxide, CO2, another gas which can cause the
ozone layer to break down, thus resulting in a continuos cycle.

Another danger of air pollutants is before they get high

enough in the atmosphere to break down the ozone layer,

they are the leading cause of the greenhouse effect. These

chemicals reflect some of the earth�s heat back down to

earth, raising the surface temperature. The rise in

temperature is known as the greenhouse effect. If this

rise in temperature continues it could start to melt the

polar icebergs, which would result in the oceans rising

and in turn flooded coastal areas. This is one of the few

effects of pollution that our society is actively worried

about. The subject of the greenhouse effect is highly

publicized and therefore people know about the risks

concerning this topic. Even though people know about

the greenhouse effect, they fai,lonce again, to see the

why behind this event. People believe that the greenhouse

effect is due to the ozone layer breaking down and in

turn more ultraviolet rays enter our atmosphere

which is the reason the temperature is increasing.

Although this belief isn�t entirely accurate it is close

enough for our purposes. As in the case with the problems

of the ozone layer, society fails to see that this is all a

result of air pollution.


What can we do?

Although air pollution has relatively few immediate effects on humans at the present time it is important that we try to reduce the amount of pollutants we emit into the air. As discussed before the biggest cause of air pollution is use of transportation, followed by the combustion of fossil fuels. In the past thirty years many new standards have been passed in the United States which resulted in a dramatic reduction in the gases emitted by automobiles (such as the Clean Air Act of 1979). But even with these new laws air pollution is still on the increase. It is mostly due to the fact that there are more automobiles on the road today. Cars may be more efficient but there are too many of them, which in many ways dimishes their efficiency. One solution to this problem is encouraging people to carpool which would reduce the number of cars on the road and in turn reduce the amount of pollutants. Another solution is to make more laws enforcing more efficient cars. However this would cost car manufactures more money, resulting in more expensive cars which people wouldn�t want to buy. So the best solution to reducing the amount of pollutants emitted by automobiles is by encouraging people to carpool.

The combustion of fossil fuels is the other leading cause of

air pollution. Although the amount of pollutants these factories

emit has reduced since the 1950�s

(when coal was the primary source of energy) they

still release a large quantity of dangerous gases. More standards

can be enforced to reduce the emissions of these factories.

Nevertheless, as long as we rely on fossil fuels for energy these

factories will have to emit some sort of gas. At the moment, nuclear

energy appears to be the wave of the future and this type of energy

releases a lot less pollutants into the air than the combustion of oil

and coal. Although air pollution presents no immediate danger

it is important that we try to control the pollutants we emit.

Most of the harm has already been done and there are no

known ways to fix these problems. It is for this reason that

we try our best to help the situation as most as possible.

Pollution and Society

Pollution in our world effects two essential
aspects of our planet: air and water. Although
their pollutants are emitted in completely different
ways, they both harm living organisms. Air pollution is
predominately emitted though the exhaust of motor vehicles
and the combustion of fossil fuels, whereas water pollution is
the result of industrial waste and environmental accidents.
Our society knows that pollution is harmful and a serious
problem for Earth but generally people don�t care.
Nevertheless everybody needs to contribute to
prevention and pay attention to government control in the
amount of material large industries can emit into the air
and/or water. Industry gives off a good share of the waste
that is polluting our planet, but it�s every person is contributes
as well. Government involvement is key to regulating toxins,
building waste systems and protecting air and waters.

Air Pollutants

The earth�s atmosphere is composed primarily
of nitrogen, oxygen, argon and carbon dioxide (the major components)
as well as neon, krypton, helium and methane
(the most predominate of the minor components) it is
these gases which make up the 5.6*1015 ton "shell" that
surrounds our planet. However, humans, animals and vegetation
in the Unites States alone emit 264 million tons of substances
into the atmosphere each year. On a worldwide scale that turns
out to be approximately 6.6 billion tons. These substances, which
aren�t naturally part of the atmosphere, are called pollutants.
Over ninety percent of all air pollutants can be divided up into five
categories: carbon monoxide, nitrogen oxides, hydrocarbons, sulfur
oxides and suspended particulate matter. Mass is only one way
of categorizing pollutants. Substances can also be looked at from
an effect stand point. For example, carbon monoxide (CO)
comprises 56% of all air pollutants when looked at in terms
of total mass. However, when looked at in terms of effect, CO
makes up only 2.5% of the pollutants. In contrast, hydrocarbons
make up 13% of all pollutants when look at in terms of mass but that number jumps to 71.5% when looked at from an effect point of view.

Carbon Monoxide (CO) is a colorless,

odorless, tasteless gas and is the most abundant and widely

distributed air pollutant. Even though vast quantities of carbon

monoxide enter the atmosphere each year

(147 million tons in the US alone) the majority of the

emissions are due to natural causes instead of anthropogenic,

human causes. It is because of this that carbon monoxide is

viewed as the least danger to living beings. The largest natural

cause of CO is the oxidation of methane in the atmosphere.

Methane, CH4, is produced on the surface of earth by the

decay of organic matter. It then rises into the atmosphere

in a gaseous state, and oxidizes to form methyl radicals (CH3)

which react further to ultimately produce CO.


CH4+OH=H2O+CH3
CH4+O=OH+CH3











A smaller natural cause is the growth and decay of
chlorophyll which is the green pigment in the leaves of plants.
Eighty percent of the carbon monoxide that is emitted by
humans is by transportation (mostly by gasoline powered vehicles).
Because automobiles are the largest source of CO pollution,
the highest concentration of this gas is in highly
populated/urban areas. The next greatest anthropogenic
source is agricultural burning, which accounts for another
twelve percent. It has been shown that exposure to high
concentrations of carbon monoxide can harm living organisms,
but the current concentration in our atmosphere is still low
enough so that plants and humans are both at minimal risk.

The category of Nitrogen Oxides is made up primarily

of three different gases; nitrogen dioxide (NO2 ), nitrous

oxide ( N2O), and nitric oxide, NO. Nitrous oxide is

over four times more toxic than nitric oxide. Nitrogen

dioxide is generally not considered a pollutant because it

is not toxic and usually not produced by humans. On the

basis of mass, the nitrogen oxides make up the smallest

group of pollutants and have the second smallest effect on

life, behind CO. As with carbon monoxide, nature emits

greater amounts of these gases than humans do. The

leading natural causes include the decomposition of soil,

bacterial activity and lightning. Anthropogenic emissions

are mostly due to the combustion of fuel. Natural air is

composed of 78% nitrogen and 21% oxygen, which don�t

react at normal temperatures, but can react if the

temperature is hot enough (1300-2500° C). In these

cases, the quantity of nitrogen oxides released varies

depending on the temperature and the ratio of nitrogen

to oxygen. The increasing use of nitrogenous fertilizers is

among the reasons that emissions of N2O have been on the

rise. Damage to plants by N2O has only been observed near

nitric acid facilities and no evidence of NO damage has ever

been seen outside the laboratory. It was concluded that

the level of concentration of these gases is too low to cause

significant problems at this time.


The category of Sulfur Oxides mostly consists of

sulfur dioxide, SO2. Sulfur trioxide, SO3, does exist but

it doesn�t stay in our atmosphere. Sulfur trioxide is very

reactant with moisture (H2O) and forms sulfuric acid, H2SO4,

one of the substances in acid rain. Unlike the two prior groups,

the sulfur oxides are predominately emitted by humans.

However, a fair amount of SO2 is produced in the atmosphere.

Hydrogen Sulfide, H2S, is produced by the decay of organic

matter, and then rises to the atmosphere where it oxidizes

and forms sulfur dioxide. Around 80% of the sulfur oxides

emitted by humans are due to the combustion of coal. Coal,

which is formed from once-living organisms, contains some

sulfur. When this combusts (fire results when a substance

reacts with oxygen) sulfur oxides are formed. Although

sulfur is an element necessary for life, too much or too little

sulfur can harm organisms. The effect of sulfur oxides on

plants varies with time of exposure and concentration.

In general, too much exposure, either a short time with

a high concentration or a long time with a low

concentration, results in damage to the leaves.

Unlike the two prior categories, the present level

of sulfur oxides actually effects humans, generally

through the respiratory system. In most cases the

amount inhaled is not enough to give any serious

results besides coughing, but if vast quantities are

inhaled into the lungs it is possible to get a respiratory

infection. Hydrocarbons are the second largest

category of air pollutants by mass, but they are by far

the largest group of pollutants when considering their

effect. There are thousands of different hydrocarbon

compounds that are comprised solely of hydrogen and

carbon. They can be found in a gaseous, liquid or solid

states at room temperature. Most hydrocarbons are

emitted by the bacterial decomposition of organic material.

Methane, CH4, which was mentioned in the formation of carbon

monoxide, is the simplest of the hydrocarbons. Petroleum

is a complicated mixture of several simple hydrocarbons

showing again transportation by motor vehicles is the leading

cause of this category being emitted into the air.

Their evaporation during the refining of petroleum

is also important. Unlike the previous categories, the

hydrocarbons are relatively harmless in their released

state. It is in the atmosphere that they undergo chemical

reactions and become hazardous. With this change the

primary pollutants (substances within the five original categories)

become secondary pollutants (new resultant substances).


These secondary pollutants, ozone ( O3, ) and

peroxyacetyl nitrate ( PAN ), are known to cause

damage to plants, especially citrus trees, salad crops and

coniferous trees. However, even though hydrocarbons are

extremely dangerous to plants, studies have revealed no direct

effects on humans at the current level of concentration. As a matter

of fact, the concentration would have to be a hundred to a

thousand times larger in order to see any direct effects.


The final category of pollutants is the suspended particulate

matter, or particulates for short. Unlike the other four

categories particulates are not gases, they are small solid

or liquid particles such as smoke, mist, or dust that measure

between .0002m m to 5000m m (m m being a micrometer or

one millionth, 10-6 meters). Particulates are formed in

two ways, the clumping together of microscopic fragments

or the breaking up of larger particles. Nature emits particulates

in a variety of ways. Similar to hydrocarbons, various gases

react in the atmosphere and form particulates. Blowing dust

can be categorized as particulates, but the largest natural

cause of particles is the bursting of tiny air bubbles at the

surface of the ocean that results in the release of microscopic

salt particles into the air. Unlike the previous categories,

humans emit minimal quantities of particulates by

transportation; fires, incomplete combustion of fossil

fuels, and industrial breaking of stone, give off most

human released particulates. Few studies have been

conducted to see the effect of particulates on plants,

but it has been found that when dust settles on their

leaves sunlight is partially blocked, thus preventing

growth of the plant. The effect on humans is entirely

in the respiratory system. Small particles

(those less than 5m m) can get by the defenses

of the upper respiratory system and reach the lungs; the

smaller the particle, the deeper into the lungs it can get

and the more problems it can cause, because they become

increasingly difficult for the body to remove.



Tuesday, January 5, 2010

Hotel Sri Lanka 02

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photo gallery

  • Sri Lanka Trains View Photo Gallery ^

  • Sri Lankan Nation View Photo Gallery ^


  • Old Kandy and Nuwara Eliya View Photo Gallery ^

  • Old Colombo View Photo Gallery ^

  • Sri Lankan Elephant View Photo Gallery ^

  • Dutch Forts ( Galle ) View Photo Gallery ^
    Located at the extreme southwest of the country is the city of Galle . At this point the coastal line turns east towards Matara and Tangalle. The Fort, one of the main historical forts in Sri Lanka like many of the other forts is built upon a small peninsula. Jagged rocks in the water surround the fort and strong currents as well, making access difficult. A pilot was needed approach the fort. Entering from the seaside would have not been considered. The fort was built initially by the Portuguese in 1588 but at present the only part of the fort that is recognizable as Portuguese is a section of the thick wall that surrounds the town. The Galle fort was captured by the Dutch with a force of almost 2500 men under Koster from the Portuguese in 1640. The defenses of the fort were updated until the early 18 th century. It is the only inhabited fort in Sri Lanka with over a hundred houses inside that also date back to the Dutch period.

  • Waterfalls in Sri Lanka View Photo Gallery ^
    Click for LArger ImageSri Lanka is known for its many tourist destinations and also its beautiful beaches but there is also a side of Sri Lanka that offers those who appreciate the great outdoors a spectacular display of nature.

    Waterfalls are one of Sri Lanka’s most treasured parts of nature. Sri Lanka boasts of almost 400 waterfalls scattered all over the island. Breathtaking waterfalls cascading down mountain slopes enhance the beauty of the hill country. The geographical formation of the island, with the central highland sloping down to the coastal plains, has resulted in several rivers and streams starting from the central region flowing down the hilly slopes in a radial pattern, creating these wonders of nature in several places throughout the hill country. This section will take you through some of the most famous of them.

  • Adventure Sports in Sri Lanka View Photo Gallery ^

  • Sri Lanka Cultural Triangle View Photo Gallery ^

    Anuradhapura
    Anuradhapura is located 206 km from Colombo . Anuradhapura was founded in the 5th century B.C. and became the capital of Sri Lanka in 380 B.C. This ancient city was ruled by Sinhalese kings for over a 1,000 years. Currently, this ancient capital of Sri Lanka is considered as a Sacred City . It is a reflection of ancient Sinhalese power and the most extensive and important of Sri Lanka 's ancient cities. Sri Lanka is rich in historic sites, which are of great importance to culture of the island.
    Here, one finds the ruins of an ancient city that flourished once upon a time. This great past is reflected in the huge Dagobas, palaces and monuments. Its impressive remains were rediscovered to the wider world in the early 19th century and have been in the process of restoration ever since. They lie to the west and north of the modern town of Anuradhapura.
    Here you will find the Sacred Bo Tree - over 2,000 years old. The Sacred Bo-Tree is the city's holiest site, and was grown from the tree under which Buddha achieved enlightenment - originally a sapling from the tree in North India.

    Polonnaruwa (2 nd Century AD)
    Just 216 km from Colombo and 75 km South East of Anuradhapura is the ancient sacred city of Polonnaruwa . This city was once the medieval Capital of Sri Lanka from 11-12 century A.D. Polonnaruwa rose to fame after the decline of Anuradhapura . Historic ruins of the king's council chamber, Royal Citadel, Kumara Pokuna, Royal Pavilion, the Vatadage Relic Houses adorned with moonstones, guardstones and sculptured railings, temple houses, rock cut statues and a vast man made lake are some of the important sights. The largest of the man made reservoirs, the huge Parakrama Samudra, is occupies an area larger than the Colombo Harbour . The Kiri Vehera, a white stone dagoba of imposing height is one the many tributes to the Buddhist faith.

    Sigiriya (5 th Century AD)
    This magnificent rock citadel known as Sigiriya is a very secure fortress. It is also a monastic retreat, and a rock art gallery. The fortress was built by King Kasyapa (477-495 AD) in the 5th century A.D to fend a feared invasion and it is situated on top of a towering 200m (656ft) high rock. In a sheltered pocket of the rock are the famous frescoes. These 5th century paintings of damsels have withstood the elements for 15 centuries. Stone steps lead to the top where the ground is flat in an area of nearly one hectare. Here, the palace's outer wall was built on the very brink of the precipice. Courtyards and even a complex drainage system were constructed. For more than 18 centuries Sigiriya was the royal citadel. The summit of the rock offers beautiful views. The UNESCO Central Cultural Fund has restored Sigiriya's 5th century Water Gardens to their earlier glory.

    Dambulla
    Located 148 km from Colombo and South of Sigiriya is the vast isolated rock mass. On the summit of Dambulla is a cluster of five temples, which in ancient times have been the dwelling of monks. Here the King Valagam Bahu (104-76 BC) took refuge in the 1st century B.C. The king later turned caves into rock temples. Carved out of rock is a huge recumbent image of the Buddha 14m long. Dambulla is considered to be the gateway to the northwest and is the first of the greatest sites in the cultural triangle. Within the five large caves, where the largest is about 50m deep and 6m in height, are sitting, standing and reclining Buddha images by the dozen, as well as Hindu gods and each cave is full of mural paintings of scenes from the Buddha's life.

Sri Lanka Nature and Wild Life

Nature, a heritage in Sri Lanka
Sri Lanka Nature locations map
Sri Lanka National Parks and Santuaries
Sri Lanka Bio Diversity, Geography and Ecology
Sri Lanka Climate
Sinharaja Rain forest - Kitulgala Rain Forest
Hortain Plains - Ritigala Ecology
Sri Lanka Reptiles , Sri Lanka Butterflies
Endemic Amphibians in Sri Lanka
Sri Lanka Nature Distinct Locations
Plan Your Sri Lanka Nature Tour