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Air
The Ocean of Air
• We live in a vast ocean of air, (called
atmosphere) which extends upwards for over
1000 km. It has a mass of about 5 x 1015
tonnes
and is spread over an area of 5x108
km2
.
• There is no definite boundary between the
atmosphere and outer space. It slowly becomes
thinner and fades into space.
• An altitude of 120 km marks the boundary
where atmospheric effects become noticeable
during atmospheric reentry
The Ocean of Air
• Three quarters of the atmosphere's mass is
within 11 km of the surface. This lowest part of
this ocean of air is known as the troposphere. It
contains about 75% of the total mass of the
atmosphere and 90% of water vapour.
• 99% of the atmosphere is spread approximately
about 30 km from the sea level
• As we move away from the earth, the density of
air decreases
The Ocean of Air
• Apart from providing us air to breathe, this
blanket of air traps the sun's heat that is
essential for life on the earth, and also acts as a
barrier against harmful and excessive radiation.  
• This ocean of air provides us O2, which is
essential for life; CO2, which is used by the
plants to manufacture food for the living
organisms; N2 which plants use to make proteins
and water vapour that condenses to form life
and thus gives us rain and determines the
climatic conditions of the globe.
Composition of Air
• Filtered air includes trace amounts of many of
the chemical elements.
• Substantial amounts of argon, nitrogen, and
oxygen are present as elementary gases.
• Note the major greenhouse gases: water vapor,
carbon dioxide, methane, nitrous oxide, and
ozone.
Composition of Air
• Many additional elements from natural sources
may be present in tiny amounts in an unfiltered
air sample.
• Various industrial pollutants are also now
present in the air, such as chlorine (elementary
or in compounds), fluorine (in compounds),
elementary mercury, and sulfur (in compounds
such as sulfur dioxide [SO2]).
Composition of Dry Air
• Gas Volume
• N2
780,840 ppmv (78.084%)
• O2
209,460 ppmv (20.946%)
• Ar 9,340 ppmv (0.9340%)
• CO2
383 ppmv (0.0383%)
• Ne 18.18 ppmv (0.001818%)
• He 5.24 ppmv (0.000524%)
• CH4
1.745 ppmv (0.0001745%)
• Kr 1.14 ppmv (0.000114%)
• Gas Volume
• H2
0.55 ppmv (0.000055%)
• N2
O 0.3 ppmv (0.00003%)
• Xe 0.09 ppmv (9x10-6
%)
• O3
0.0 to 0.07 ppmv (0%-7x10-6
%)
• NO2
0.02 ppmv (2x10-6
%)
• I 0.01 ppmv (1x10-6
%)
• CO 0.1 ppmv
• NH3
trace
ppmv: parts per million by volume
Not included in above dry atmosphere:
Water vapor (H2O): ~0.40% over full atmosphere, typically 1%-4% at surface
Air | Class 8 | Science
Parts of the Atmosphere
• The troposphere is the lowest layer of the
atmosphere; it begins at the surface and
extends to between 7 km (23,000 ft) at the poles
and 17 km (56,000 ft) at the equator, with some
variation due to weather factors
• All the activities of living beings are possible in
this region, so this area is suitable for living
beings
Troposphere
Parts of the Atmosphere
• Though part of the Stratosphere, the ozone layer
is considered as a layer of the Earth's atmosphere
in itself because its physical and chemical
composition is far different from the Stratosphere.
• Ozone (O3) in the Earth's stratosphere is created
by UV light splitting O2 atoms into individual
oxygen atoms which then combine with unbroken
O2 to create O3.
• Hence, ozone provides protection against UV
rays
Ozone Layer
Parts of the Atmosphere
• The stratosphere extends from the troposphere's
7–17 km (4.3–11 miles; 23,000–56,000 ft) range to
about 51 km (32 miles; 170,000 ft).
• The stratosphere contains the ozone layer, the
part of the Earth's atmosphere which contains
relatively high concentrations of ozone.
• Temperature increases with height
Stratosphere
Parts of the Atmosphere
• The mesosphere extends from about 50 km
(31 mi; 160,000 ft) to the range of 80–85 km (50–
53 mi; 260,000–280,000 ft).
• Temperature decreases with height, reaching
−100 °C (−148.0 °F; 173.1 K) in the upper
mesosphere.
• This is also where most meteors burn up when
entering the atmosphere.
Mesosphere
Parts of the Atmosphere
• The thermosphere extends from 80–85 km (50–
53 miles; 260,000–280,000 ft) to over 640 km
(400 miles; 2,100,000 ft)
• The temperature increases with height. The
temperature of this layer can rise to 1,500 °C
(2,730 °F).
• The International Space Station orbits in this
layer, between 320 and 380 km (200 and
240 mi).
Thermosphere
Parts of the Atmosphere
• The part of the atmosphere that is ionized by
solar radiation stretches from 50 to 1,000 km (31
to 620 miles; 160,000 to 3,300,000 ft) and
typically overlaps both the exosphere and the
thermosphere.
• It plays an important part in atmospheric
electricity.
• Because of its charged particles, it has
practical importance because it influences, for
example, radio propagation on the Earth.
Ionosphere
Parts of the Atmosphere
• The exosphere extends from 500–1,000 km
(310–620 miles; 1,600,000–3,300,000 ft) up to
10,000 km (6,200 miles; 33,000,000 ft)
• This region contains free-moving particles
Exosphere
Atmospheric Pressure
• Atmospheric pressure is a direct result of the
total weight of the air above the point at which
the pressure is measured
• The average atmospheric pressure, at sea level,
is about 1 atmosphere (atm) = 101.3 kPa
(kilopascals)
• The density of air decreases with height,
thereby causing a corresponding decrease in
pressure. This explains the difficulty in
breathing at high altitudes
Oxygen (O2)
Oxygen – An Introduction
• Oxygen is the third most abundant element in
the universe by mass after hydrogen and helium
and the most abundant element by mass in the
Earth's crust.
• Diatomic oxygen gas constitutes 20.9% of the
volume of air.
• Oxygen is present in compound state in almost
all the minerals and rocks
• Oxygen is present in water as compound to
88.8% by weight
Obtaining Oxygen ……
• Electrolysis of water (containing strong acid or
strong base to make it conduct electricity)
2H2O electrolysis
2H2 + O2
• Oxygen is evolved at the positive electrode and
hydrogen at the negative electrode
• This method gives 100% pure oxygen
Obtaining Oxygen ……
• Oxygen can also be obtained from its
important compounds like oxides, nitrates and
chlorates
4CrO3 2Cr2O3 + 3O2
2NaNO3 2NaNO2 + O2
2KClO3 2KCl + 3O2 (Lab method)
• In the lab method, manganese dioxide is used
as a catalyst – something that does not take
part in a reaction, only affects the rate
Obtaining Oxygen ……
• Another method involves the addition of water
to sodium peroxide and the collection, over
water, of the liberated oxygen
• 2Na2O2 + 2H2O 4NaOH + O2
Oxygen – Properties
• It is colourless, odourless and tasteless
• Oxygen is not inflammable, but it is a
supporter of combustion
• It occurs in a diatomic form in nature – O2
• It easily forms compounds with other elements
Oxygen – Uses
• Required for breathing in all living organisms
(animals) and by plants for respiration
• Oxygen inhalers for patients suffering from
asthma, pneumonia etc
• Oxygen cylinders are used by scuba divers and
mountaineers
• Oxy-hydrogen and oxy-acetylene flame used for
cutting and welding metals
• For producing chlorine, nitric and sulphuric
acid
Nitrogen (N2)
Nitrogen – An Introduction
• Nitrogen constitutes 78% (by volume) of the
atmosphere
• Nitrogen is an inert gas and is not directly used
by plants and animals, but it occurs in all living
organisms.
• It is a constituent element of amino acids and
thus of proteins, and of nucleic acids (DNA
and RNA).
Obtaining Nitrogen ……
• Air is passed over heated copper or coke to
remove oxygen
• Carbon dioxide formed due to coke is removed
by dissolving in water
• The remaining air is liquefied and nitrogen is
separated
Nitrogen Cycle
Nitrogen Cycle
• The nitrogen cycle is the biogeochemical cycle
that describes the transformations of nitrogen
and nitrogen-containing compounds in nature.
• The conversion of nitrogen (N2) from the
atmosphere into a form readily available to
plants and hence to animals and humans is an
important step in the nitrogen cycle, which
distributes the supply of this essential nutrient.
• There are four ways to convert atmospheric N2
gas into more chemically reactive forms:
Nitrogen Cycle
• Biological fixation: some symbiotic bacteria
(most often associated with leguminous plants)
and some free-living bacteria are able to fix
nitrogen as organic nitrogen.
• Industrial N-fixation: Under great pressure, at
a temperature of 600o
C, and with the use of a
catalyst, atmospheric nitrogen and hydrogen
can be combined to form ammonia (NH3).
Nitrogen Cycle
• Combustion of fossil fuels: automobile engines
and thermal power plants, which release
various nitrogen oxides (NOx).
• Other processes: Additionally, the formation of
NO from N2 and O2 due to photons and
especially lightning, are important for
atmospheric chemistry, but not for terrestrial or
aquatic nitrogen turnover
Properties of Nitrogen
• It is a colourless, odourless and tasteless gas
• It is not inflammable and neither does it
support combustion
• It is non-poisonous, although it inhibits
breathing
• It is present in nature as a diatomic molecule
• It has the capacity to form compounds with
various elements
Uses of Nitrogen
• It is useful in the preparation of chemicals like
ammonia, nitric acid etc.
• It is used to create inert atmosphere – for e.g.,
many volatile / inflammable liquids are stored
in containers that contain nitrogen. It helps
reduce the possibility of fire
Pollution
Pollution
• Due to industrialization, many unwanted
chemical compounds in the form of gas, liquid
and solid are thrown into the soil and
atmosphere
• When these chemical compounds start showing
adverse effect, it is called pollution
• The compounds spreading pollution are called
pollutants
Types of Pollution
• Pollution is of different types:
• Air pollution
• Water pollution
• Soil pollution
• Noise (sound) pollution
Pollution
• Pollutants bring about physical, chemical and
biological changes in the air, water and soil
• These changes may prove fatal to man as well
as other living organisms
• They also destroy the delicate balance of the
eco-system
• Pollutants are produced in our daily life – when
we use detergents, drive a petrol / diesel car,
generate rubbish, dump effluents in rivers etc.
Air Pollution
Air | Class 8 | Science
Air Pollution
• Pollutants in the air, mainly in the form of gas or
minute particles, consist of:
– Gaseous state of some solid/liquid compounds
– Dust and Fog
– Minute particles of unnecessary chemicals and
carbon
– Smoke produced as gaseous residue due to
incomplete combustion of C, Fe, Si, Al, Pb, Zn,
hydrocarbons, acid, base etc
– Radiation
Air Pollution - Effects
• Diseases of the oesophagus and lungs,
intestinal cancer, damages to the kidney, blood
pressure
• Can affect the reproduction power of people
working in chemical industries
• Life expectancy of animals and men is reduced
• Physical and sometimes genetic defects result
• Vegetation affected – reduced crop output,
slowing down of photosynthesis etc.
Air Pollution - Remedies
• Reduction of dust particles, polluting gases at
source
• Changing the raw materials and improving
process systems
• Diffusing the pollutants over a larger area
• Separation of industrial and residential areas
• Regular checking and maintenance of vehicles
• Use of ‘clean’ and ‘alternative’ fuel (CNG, bio-
fuels)
Air Pollution - Remedies
• Developing hybrid vehicles that run on
electricity, hydrogen cells etc
• Increasing the green cover by planting more
trees
• Developing forests and bio-reserves, parks etc.,
which act as ‘lungs’
• Recycling trash, rather than burning it
Greenhouse Effect
• The greenhouse effect is the heating of the
surface of the earth due to the presence of
an atmosphere containing gases that absorb
and emit infrared radiation.
• Greenhouse gases, which include water
vapor, carbon dioxide and methane, trap
heat within the surface-troposphere system
Greenhouse Gases
• In order, Earth's most abundant greenhouse
gases are:
– water vapor
– carbon dioxide
– methane
– nitrous oxide
– ozone
– CFCs
Greenhouse Gases
• When these gases are ranked by their
contribution to the greenhouse effect, the most
important are:
– water vapor, which contributes 36–70%
– carbon dioxide, which contributes 9–26%
– methane, which contributes 4–9%
– ozone, which contributes 3–7%
Greenhouse Effect - Mechanism
• The carbon dioxide proportion in the air is
maintained at around 0.3% by the actions
and activities of:
– animals (who release it during respiration)
– plants (which use it during
photosynthesis)
– sea water that absorbs CO2
Greenhouse Effect - Mechanism
• The earth receives energy from the sun
mainly in the form of light and this is
absorbed by the surface of the earth
• The earth radiates this absorbed energy in
the form of heat
• Carbon dioxide absorbs heat and along with
the other greenhouse gases helps to
maintain the average surface temperature of
the earth (14o
C).
Exchange of Energy
Solar radiation
absorbed by the
Earth
Thermal Energy
into space
Directly radiated
from the surface
Heat and energy in
the atmosphere
Greenhouse gas
absorption
Earth’s land and ocean surface
warmed to a temp. of 14o
C
Greenhouse Effect - Impact
• When the proportion of CO2 increases, the
temperature of the earth also increases as more
heat is now absorbed by the atmosphere
• Polar ice-caps start melting leading to a rise in
water levels, submerging of coastal areas,
flooding etc.
• An overall increase in the temperature of the
earth leading to ‘hotter’ summers and ‘warm’
winters
Acid Rain
• "Acid rain" is a popular term referring to the
deposition of wet (rain, snow, sleet, fog and
cloud-water, dew) and dry (acidifying particles
and gases) acidic components.
• A more accurate term is “acid deposition”.
• Acid rain is mostly caused by human emissions
of sulfur and nitrogen compounds which react
in the atmosphere to produce acids.
Acid Rain
• Dry form: This can be responsible for as much
as 20 to 60% of total acid deposition.
• This occurs when acidic gases like Sulfur
dioxide spread in the atmosphere and stick to
the ground, plants or other surfaces.
• Wet form: when humidity increases,
atmospheric gases like SO2 and NOx turn into
sulphuric acid and nitric acid.
• When this acid falls along with the
precipitation (rain, snow) it is called ‘acid rain’
Acid Rain - Causes
• The principal cause of acid rain is sulfur and
nitrogen compounds from human sources,
such as electricity generation, factories, and
motor vehicles.
• Coal power plants are one of the most
polluting.
• Sulphur dioxide is produced in the atmosphere
due to the sulphur present in coal
• Vehicles are responsible for nitrogen oxides,
hydrocarbons and carbon monoxide
Origin of Acid Rain
Acid Rain - Effects
• The higher aluminum concentrations in surface
water that occur as a result of acid rain can
cause damage to fish and other aquatic animals
• As lakes and rivers become more acidic
biodiversity is reduced
• Soil biology and chemistry can be seriously
damaged by acid rain
• Microbes producing essential fertilizers are
killed and essential minerals are leached
Acid Rain - Effects
• High altitude forests are especially vulnerable
as they are often surrounded by clouds and fog
which are more acidic than rain.
• Fine particles, a large fraction of which are
formed from the same gases as acid rain (sulfur
dioxide and nitrogen dioxide), have been
shown to cause illness and premature deaths
such as cancer and other diseases
• Acid rain can also cause damage to certain
building materials and historical monuments
Effect of Acid Rain on Trees
Effect of Acid Rain on Statues
Acid Rain - Prevention
• Use fuel containing less sulphur
• Removal of sulphur containing gases before
release to atmosphere
• Production of crude oil with less sulphur
content
• Usage of calcium carbonate to absorb sulphur
dioxide
• Stricter automobile emission controls to reduce
the emission of nitrogen oxides

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Air | Class 8 | Science

  • 1. Air
  • 2. The Ocean of Air • We live in a vast ocean of air, (called atmosphere) which extends upwards for over 1000 km. It has a mass of about 5 x 1015 tonnes and is spread over an area of 5x108 km2 . • There is no definite boundary between the atmosphere and outer space. It slowly becomes thinner and fades into space. • An altitude of 120 km marks the boundary where atmospheric effects become noticeable during atmospheric reentry
  • 3. The Ocean of Air • Three quarters of the atmosphere's mass is within 11 km of the surface. This lowest part of this ocean of air is known as the troposphere. It contains about 75% of the total mass of the atmosphere and 90% of water vapour. • 99% of the atmosphere is spread approximately about 30 km from the sea level • As we move away from the earth, the density of air decreases
  • 4. The Ocean of Air • Apart from providing us air to breathe, this blanket of air traps the sun's heat that is essential for life on the earth, and also acts as a barrier against harmful and excessive radiation.   • This ocean of air provides us O2, which is essential for life; CO2, which is used by the plants to manufacture food for the living organisms; N2 which plants use to make proteins and water vapour that condenses to form life and thus gives us rain and determines the climatic conditions of the globe.
  • 5. Composition of Air • Filtered air includes trace amounts of many of the chemical elements. • Substantial amounts of argon, nitrogen, and oxygen are present as elementary gases. • Note the major greenhouse gases: water vapor, carbon dioxide, methane, nitrous oxide, and ozone.
  • 6. Composition of Air • Many additional elements from natural sources may be present in tiny amounts in an unfiltered air sample. • Various industrial pollutants are also now present in the air, such as chlorine (elementary or in compounds), fluorine (in compounds), elementary mercury, and sulfur (in compounds such as sulfur dioxide [SO2]).
  • 7. Composition of Dry Air • Gas Volume • N2 780,840 ppmv (78.084%) • O2 209,460 ppmv (20.946%) • Ar 9,340 ppmv (0.9340%) • CO2 383 ppmv (0.0383%) • Ne 18.18 ppmv (0.001818%) • He 5.24 ppmv (0.000524%) • CH4 1.745 ppmv (0.0001745%) • Kr 1.14 ppmv (0.000114%) • Gas Volume • H2 0.55 ppmv (0.000055%) • N2 O 0.3 ppmv (0.00003%) • Xe 0.09 ppmv (9x10-6 %) • O3 0.0 to 0.07 ppmv (0%-7x10-6 %) • NO2 0.02 ppmv (2x10-6 %) • I 0.01 ppmv (1x10-6 %) • CO 0.1 ppmv • NH3 trace ppmv: parts per million by volume Not included in above dry atmosphere: Water vapor (H2O): ~0.40% over full atmosphere, typically 1%-4% at surface
  • 9. Parts of the Atmosphere • The troposphere is the lowest layer of the atmosphere; it begins at the surface and extends to between 7 km (23,000 ft) at the poles and 17 km (56,000 ft) at the equator, with some variation due to weather factors • All the activities of living beings are possible in this region, so this area is suitable for living beings Troposphere
  • 10. Parts of the Atmosphere • Though part of the Stratosphere, the ozone layer is considered as a layer of the Earth's atmosphere in itself because its physical and chemical composition is far different from the Stratosphere. • Ozone (O3) in the Earth's stratosphere is created by UV light splitting O2 atoms into individual oxygen atoms which then combine with unbroken O2 to create O3. • Hence, ozone provides protection against UV rays Ozone Layer
  • 11. Parts of the Atmosphere • The stratosphere extends from the troposphere's 7–17 km (4.3–11 miles; 23,000–56,000 ft) range to about 51 km (32 miles; 170,000 ft). • The stratosphere contains the ozone layer, the part of the Earth's atmosphere which contains relatively high concentrations of ozone. • Temperature increases with height Stratosphere
  • 12. Parts of the Atmosphere • The mesosphere extends from about 50 km (31 mi; 160,000 ft) to the range of 80–85 km (50– 53 mi; 260,000–280,000 ft). • Temperature decreases with height, reaching −100 °C (−148.0 °F; 173.1 K) in the upper mesosphere. • This is also where most meteors burn up when entering the atmosphere. Mesosphere
  • 13. Parts of the Atmosphere • The thermosphere extends from 80–85 km (50– 53 miles; 260,000–280,000 ft) to over 640 km (400 miles; 2,100,000 ft) • The temperature increases with height. The temperature of this layer can rise to 1,500 °C (2,730 °F). • The International Space Station orbits in this layer, between 320 and 380 km (200 and 240 mi). Thermosphere
  • 14. Parts of the Atmosphere • The part of the atmosphere that is ionized by solar radiation stretches from 50 to 1,000 km (31 to 620 miles; 160,000 to 3,300,000 ft) and typically overlaps both the exosphere and the thermosphere. • It plays an important part in atmospheric electricity. • Because of its charged particles, it has practical importance because it influences, for example, radio propagation on the Earth. Ionosphere
  • 15. Parts of the Atmosphere • The exosphere extends from 500–1,000 km (310–620 miles; 1,600,000–3,300,000 ft) up to 10,000 km (6,200 miles; 33,000,000 ft) • This region contains free-moving particles Exosphere
  • 16. Atmospheric Pressure • Atmospheric pressure is a direct result of the total weight of the air above the point at which the pressure is measured • The average atmospheric pressure, at sea level, is about 1 atmosphere (atm) = 101.3 kPa (kilopascals) • The density of air decreases with height, thereby causing a corresponding decrease in pressure. This explains the difficulty in breathing at high altitudes
  • 18. Oxygen – An Introduction • Oxygen is the third most abundant element in the universe by mass after hydrogen and helium and the most abundant element by mass in the Earth's crust. • Diatomic oxygen gas constitutes 20.9% of the volume of air. • Oxygen is present in compound state in almost all the minerals and rocks • Oxygen is present in water as compound to 88.8% by weight
  • 19. Obtaining Oxygen …… • Electrolysis of water (containing strong acid or strong base to make it conduct electricity) 2H2O electrolysis 2H2 + O2 • Oxygen is evolved at the positive electrode and hydrogen at the negative electrode • This method gives 100% pure oxygen
  • 20. Obtaining Oxygen …… • Oxygen can also be obtained from its important compounds like oxides, nitrates and chlorates 4CrO3 2Cr2O3 + 3O2 2NaNO3 2NaNO2 + O2 2KClO3 2KCl + 3O2 (Lab method) • In the lab method, manganese dioxide is used as a catalyst – something that does not take part in a reaction, only affects the rate
  • 21. Obtaining Oxygen …… • Another method involves the addition of water to sodium peroxide and the collection, over water, of the liberated oxygen • 2Na2O2 + 2H2O 4NaOH + O2
  • 22. Oxygen – Properties • It is colourless, odourless and tasteless • Oxygen is not inflammable, but it is a supporter of combustion • It occurs in a diatomic form in nature – O2 • It easily forms compounds with other elements
  • 23. Oxygen – Uses • Required for breathing in all living organisms (animals) and by plants for respiration • Oxygen inhalers for patients suffering from asthma, pneumonia etc • Oxygen cylinders are used by scuba divers and mountaineers • Oxy-hydrogen and oxy-acetylene flame used for cutting and welding metals • For producing chlorine, nitric and sulphuric acid
  • 25. Nitrogen – An Introduction • Nitrogen constitutes 78% (by volume) of the atmosphere • Nitrogen is an inert gas and is not directly used by plants and animals, but it occurs in all living organisms. • It is a constituent element of amino acids and thus of proteins, and of nucleic acids (DNA and RNA).
  • 26. Obtaining Nitrogen …… • Air is passed over heated copper or coke to remove oxygen • Carbon dioxide formed due to coke is removed by dissolving in water • The remaining air is liquefied and nitrogen is separated
  • 28. Nitrogen Cycle • The nitrogen cycle is the biogeochemical cycle that describes the transformations of nitrogen and nitrogen-containing compounds in nature. • The conversion of nitrogen (N2) from the atmosphere into a form readily available to plants and hence to animals and humans is an important step in the nitrogen cycle, which distributes the supply of this essential nutrient. • There are four ways to convert atmospheric N2 gas into more chemically reactive forms:
  • 29. Nitrogen Cycle • Biological fixation: some symbiotic bacteria (most often associated with leguminous plants) and some free-living bacteria are able to fix nitrogen as organic nitrogen. • Industrial N-fixation: Under great pressure, at a temperature of 600o C, and with the use of a catalyst, atmospheric nitrogen and hydrogen can be combined to form ammonia (NH3).
  • 30. Nitrogen Cycle • Combustion of fossil fuels: automobile engines and thermal power plants, which release various nitrogen oxides (NOx). • Other processes: Additionally, the formation of NO from N2 and O2 due to photons and especially lightning, are important for atmospheric chemistry, but not for terrestrial or aquatic nitrogen turnover
  • 31. Properties of Nitrogen • It is a colourless, odourless and tasteless gas • It is not inflammable and neither does it support combustion • It is non-poisonous, although it inhibits breathing • It is present in nature as a diatomic molecule • It has the capacity to form compounds with various elements
  • 32. Uses of Nitrogen • It is useful in the preparation of chemicals like ammonia, nitric acid etc. • It is used to create inert atmosphere – for e.g., many volatile / inflammable liquids are stored in containers that contain nitrogen. It helps reduce the possibility of fire
  • 34. Pollution • Due to industrialization, many unwanted chemical compounds in the form of gas, liquid and solid are thrown into the soil and atmosphere • When these chemical compounds start showing adverse effect, it is called pollution • The compounds spreading pollution are called pollutants
  • 35. Types of Pollution • Pollution is of different types: • Air pollution • Water pollution • Soil pollution • Noise (sound) pollution
  • 36. Pollution • Pollutants bring about physical, chemical and biological changes in the air, water and soil • These changes may prove fatal to man as well as other living organisms • They also destroy the delicate balance of the eco-system • Pollutants are produced in our daily life – when we use detergents, drive a petrol / diesel car, generate rubbish, dump effluents in rivers etc.
  • 39. Air Pollution • Pollutants in the air, mainly in the form of gas or minute particles, consist of: – Gaseous state of some solid/liquid compounds – Dust and Fog – Minute particles of unnecessary chemicals and carbon – Smoke produced as gaseous residue due to incomplete combustion of C, Fe, Si, Al, Pb, Zn, hydrocarbons, acid, base etc – Radiation
  • 40. Air Pollution - Effects • Diseases of the oesophagus and lungs, intestinal cancer, damages to the kidney, blood pressure • Can affect the reproduction power of people working in chemical industries • Life expectancy of animals and men is reduced • Physical and sometimes genetic defects result • Vegetation affected – reduced crop output, slowing down of photosynthesis etc.
  • 41. Air Pollution - Remedies • Reduction of dust particles, polluting gases at source • Changing the raw materials and improving process systems • Diffusing the pollutants over a larger area • Separation of industrial and residential areas • Regular checking and maintenance of vehicles • Use of ‘clean’ and ‘alternative’ fuel (CNG, bio- fuels)
  • 42. Air Pollution - Remedies • Developing hybrid vehicles that run on electricity, hydrogen cells etc • Increasing the green cover by planting more trees • Developing forests and bio-reserves, parks etc., which act as ‘lungs’ • Recycling trash, rather than burning it
  • 43. Greenhouse Effect • The greenhouse effect is the heating of the surface of the earth due to the presence of an atmosphere containing gases that absorb and emit infrared radiation. • Greenhouse gases, which include water vapor, carbon dioxide and methane, trap heat within the surface-troposphere system
  • 44. Greenhouse Gases • In order, Earth's most abundant greenhouse gases are: – water vapor – carbon dioxide – methane – nitrous oxide – ozone – CFCs
  • 45. Greenhouse Gases • When these gases are ranked by their contribution to the greenhouse effect, the most important are: – water vapor, which contributes 36–70% – carbon dioxide, which contributes 9–26% – methane, which contributes 4–9% – ozone, which contributes 3–7%
  • 46. Greenhouse Effect - Mechanism • The carbon dioxide proportion in the air is maintained at around 0.3% by the actions and activities of: – animals (who release it during respiration) – plants (which use it during photosynthesis) – sea water that absorbs CO2
  • 47. Greenhouse Effect - Mechanism • The earth receives energy from the sun mainly in the form of light and this is absorbed by the surface of the earth • The earth radiates this absorbed energy in the form of heat • Carbon dioxide absorbs heat and along with the other greenhouse gases helps to maintain the average surface temperature of the earth (14o C).
  • 48. Exchange of Energy Solar radiation absorbed by the Earth Thermal Energy into space Directly radiated from the surface Heat and energy in the atmosphere Greenhouse gas absorption Earth’s land and ocean surface warmed to a temp. of 14o C
  • 49. Greenhouse Effect - Impact • When the proportion of CO2 increases, the temperature of the earth also increases as more heat is now absorbed by the atmosphere • Polar ice-caps start melting leading to a rise in water levels, submerging of coastal areas, flooding etc. • An overall increase in the temperature of the earth leading to ‘hotter’ summers and ‘warm’ winters
  • 50. Acid Rain • "Acid rain" is a popular term referring to the deposition of wet (rain, snow, sleet, fog and cloud-water, dew) and dry (acidifying particles and gases) acidic components. • A more accurate term is “acid deposition”. • Acid rain is mostly caused by human emissions of sulfur and nitrogen compounds which react in the atmosphere to produce acids.
  • 51. Acid Rain • Dry form: This can be responsible for as much as 20 to 60% of total acid deposition. • This occurs when acidic gases like Sulfur dioxide spread in the atmosphere and stick to the ground, plants or other surfaces. • Wet form: when humidity increases, atmospheric gases like SO2 and NOx turn into sulphuric acid and nitric acid. • When this acid falls along with the precipitation (rain, snow) it is called ‘acid rain’
  • 52. Acid Rain - Causes • The principal cause of acid rain is sulfur and nitrogen compounds from human sources, such as electricity generation, factories, and motor vehicles. • Coal power plants are one of the most polluting. • Sulphur dioxide is produced in the atmosphere due to the sulphur present in coal • Vehicles are responsible for nitrogen oxides, hydrocarbons and carbon monoxide
  • 54. Acid Rain - Effects • The higher aluminum concentrations in surface water that occur as a result of acid rain can cause damage to fish and other aquatic animals • As lakes and rivers become more acidic biodiversity is reduced • Soil biology and chemistry can be seriously damaged by acid rain • Microbes producing essential fertilizers are killed and essential minerals are leached
  • 55. Acid Rain - Effects • High altitude forests are especially vulnerable as they are often surrounded by clouds and fog which are more acidic than rain. • Fine particles, a large fraction of which are formed from the same gases as acid rain (sulfur dioxide and nitrogen dioxide), have been shown to cause illness and premature deaths such as cancer and other diseases • Acid rain can also cause damage to certain building materials and historical monuments
  • 56. Effect of Acid Rain on Trees
  • 57. Effect of Acid Rain on Statues
  • 58. Acid Rain - Prevention • Use fuel containing less sulphur • Removal of sulphur containing gases before release to atmosphere • Production of crude oil with less sulphur content • Usage of calcium carbonate to absorb sulphur dioxide • Stricter automobile emission controls to reduce the emission of nitrogen oxides