Page 208 - Chemistry ICSE Class IX
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196                                                                                      ICSE Chemistry – 9

                                           How can global warming be reduced
                                           The global warming can be reduced by taking the following steps:
                                             ƒ  Minimise (or cut down) the use of fossil fuels. This can be achieved
                                                by using bicycle for short distances and public transport, metrorail or
                                                a car pool for going long distances.
                                             ƒ  Encourage the use of alternative renewable sources of energy, such
                                                as Wind, Hydel, Solar, and Biomass
                                             ƒ  Increase vegetation cover by planting more trees
                                             ƒ  Minimise the use of nitrogenous fertilisers
                                             ƒ  Do not burn dry agricultural waste, dry leaves, wood etc.
                                             ƒ  Use chlorine-free substitutes of chloro uorohydrocarbons in
                                                refrigeration and in chemical industry. Such substitutes which
                                                are available in market are hydro uorocarbons (HFCs) and
                                                methylcyclohexane (MCH).
                                             ƒ  Avoid smoking.
                                             ƒ  Spread awareness regarding the harmful effects of global warming.

                                                    ASSIGNMENT 5

                   Global warming, Sources of the greenhouse gases, The greenhouses effect, Adverse effects of global warming.

              ϭ͘  tŚĂƚ ŝƐ ŵĞĂŶƚ ďLJ ŐůŽďĂů ǁĂƌŵŝŶŐ͍
              Ϯ͘  tŚĂƚ ĂƌĞ ƚŚĞ ŐƌĞĞŶŚŽƵƐĞ ŐĂƐĞƐ͍ 'ŝǀĞ ƚǁŽ ĞdžĂŵƉůĞƐ ŽĨ ƚŚĞ ŐƌĞĞŶŚŽƵƐĞ ŐĂƐĞƐ͘
              ϯ͘  tŚŝĐŚ ŽĨ ƚŚĞ ŐƌĞĞŶŚŽƵƐĞ ŐĂƐĞƐ ĐŽŶƚƌŝďƵƚĞƐ ƚŚĞ ŵŽƐƚ ƚŽǁĂƌĚƐ ŐůŽďĂů ǁĂƌŵŝŶŐ͍
              ϰ͘  EĂŵĞ ƚŚĞ ƌĂĚŝĂƟŽŶ ǁŚŝĐŚ ĂƌĞ ƚƌĂƉƉĞĚ ďLJ ĐĂƌďŽŶ ĚŝŽdžŝĚĞ ŝŶ ƚŚĞ ůŽǁĞƌ ůĂLJĞƌ ŽĨ ƚŚĞ ĂƚŵŽƐƉŚĞƌĞ͘
              ϱ͘  EĂŵĞ ƚŚĞ ƉŽƐƐŝďůĞ ĂĚǀĞƌƐĞ ĞīĞĐƚƐ ŽĨ ŐůŽďĂů ǁĂƌŵŝŶŐ͘
              ϲ͘  ,Žǁ ĐĂŶ ǁĞ ƌĞĚƵĐĞ ƚŚĞ ŐůŽďĂů ǁĂƌŵŝŶŐ͍
                                           Ozone Depletion

                                           The most important gas present in the stratosphere is ozone (O ). Starting
                                                                                                        3
                                           at a height of about 16 km, the concentration of ozone becomes maximum
                                           at a height of about 23 km. Its concentration in the atmosphere at a height
                                           of about 23 km is nearly 10 parts per million (10 ppm).
                                           How is ozone formed in the atmosphere

                                           Ozone (O ) is formed in the atmosphere (in stratosphere) from oxygen (O )
                                                    3
                                                                                                                 2
                                           by the action of far ultraviolet rays present in the sunlight.
                                                O (g) + hv (O = 242 nm)   o O(g) + O(g)
                                                  2
                                                Oxygen         far ultraviolet rays
                                                           O (g) + O(g)   o       O (g)
                                                            2
                                                                                     3
                                                                                    ozone
                                                The blanket of ozone (16 – 23 km) around the earth is called ozone
                                           layer. Ozone layer is one of the most important life-support systems.

                                           What is the function (or role) of ozone layer
                                           The radiation coming from the sun consists of ultraviolet radiation. The
                                           ultraviolet radiation can penetrate deep into our body and cause diseases
                                           such as cataract, skin cancer, etc. Ozone layer absorbs the harmful
                                           ultraviolet radiation (in the region: O = 220–330 nm) coming from the sun.
                                           Thus, the ozone layer protects animal and plant life on the earth from the
                                           harmful effects of the ultraviolet radiation.
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