In the stratosphere, CFCs release chlorine free radical (
). CF2Cl2(g)
(g) +
F2Cl(g) Which react with O3 to give chlorine oxide (Cl
) radical not chlorine dioxide (Cl
2) radical.
(g) + O3(g) Cl
(g) + O2(g)
In the stratosphere, CFCs release chlorine free radical (
). CF2Cl2(g)
(g) +
F2Cl(g) Which react with O3 to give chlorine oxide (Cl
) radical not chlorine dioxide (Cl
2) radical.
(g) + O3(g) Cl
(g) + O2(g)
SO2 and NO2 are responsible for the discoloured and lustreless nature of marble.
Oxides of nitrogen and sulphur are acidic and settle down on ground as dry deposition.
Ammonium salts in rain drops result in wet deposition.
Ozone in the stratosphere is a product of UV radiations acting on dioxygen (O2) molecules.
Photochemical smog contains oxides of nitrogen.
Between 10-50 km above sea level is the lowest level which is called stratosphere.
Ozone is a strong oxidising agent like NO2.
In troposphere both O3 and NO2 react with the unburnt hydrocarbons to produce the chemical components of photochemical smog, like formaldehyde (HCHO), acrolein (CH2 = CH - CHO) and PAN or peroxyacetyl nitrate.
Hence, in troposphere, the presence of ozone generates photochemical smog.
Permissible limit for SO4 2- = 500 ppm Permissible limit for NO3 - = 50 ppm Permissible limit for F- = 1 ppm
Clean water would have BOD value of less than 5 ppm whereas highly polluted water could have a BOD value of 17 ppm or more.
Hence, the value of parameter ‘BOD’ is important for survival of aquatic life but optimum value of BOD is 17 ppm or more.
So, statement II is incorrect.
Among the given gases, the green house gases which are responsible for heating the atmosphere are CH4, water vapour and ozone.
Nitrogen is not a green house gas.