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Agrometeorological normal for: rice, wheat, maize, potato, sugarcane, cotton, soybean, citrus and vegetable crops
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Learn Introductory Agrometerology with Rahul

Composition of the atmosphere

  • consists of a uniform mixture permanent gases called dry air and varying amount of other material including water vapour and both organic and inorganic impurities like dust, smoke, pollen, etc.
  • Pure dry air is very stable all over the earth upto an altitude of about 50 km.
  • The lower layer, where the chemical composition of air is uniform, is called homosphere and the higher layer is called heterosphere
  • Nitrogen and Oxygen constitute about 99% of clean dry air
  • Remaining 1% are mostly inert gases.

Constituents

% by volume

Nitrogen (N2)

78.08

Oxygen (O2)

20.95

Argon (Ar)

0.93

Carbondioxide (CO2)

0.03

Neon (Ne)

0.0018

Helium (He)

0.0005

Ozone (O3)

0.00004

Hydrogen (H2)

0.00006

 

a) Oxygen:

  • It alone contributes about 1/5th of dry air,
  • No life without oxygen; plays important role in oxidation (respiration, soil mineralization, soil formation etc.)
  • Essential for combustion so called combustible gas.

 

b) Nitrogen:

  • Contribute major component of the atmosphere and attribute more than 78%,
  • It is relatively inactive chemically, though many of its compounds are very active.
  • Its main function in the atmosphere is to regulate combustion by diluting oxygen.

 

c) Carbon dioxide:

  • It contributes only about 0.03% of the dry air,
  • Green plants, in the process of photosynthesis, consume CO2 and in the process of respiration, CO2 is evolved into the atmosphere,
  • It is the product of combustion,
  • It is one of the greatest contributing gases on atmospheric phenomenon i.e. on climate change,
  • % CO2 is increasing in atmosphere, which contribute a vital role in global warming.

 

d) Ozone:

  • Contribute a small percentage of about 0.00006%, found in upper atmosphere and it is not uniformly distributed.
  • Mostly concentrates on 30-60 km from earth surface called ozonosphere.
  • O3 is an efficient absorber of ultraviolet radiation and help to protect the biosphere.

 

e) Chemical compounds:

  • Ar, Ne, He, Kr, Xe are so inert chemically that they are never found in any chemical compounds.
  • Ar is used extensively in electric lamp bulbs because of its inertness. It is also used inflorescent tubes. It flows with blue light.
  • Ne is used to fill florescent tubes. It flows with distinctive orange red colour.
  • He is the second highest element with a density of 0.177 gm per liter (Hydrogen 0,08988gms /liter). It is used to inflate balloons because it will not burn.
  • Kr glows with brilliant green and yellow colour.
  • Xe is chemically inert and glows with a blue green colour.

 

f) Water vapor:

  • Absorb long wave length terrestrial radiation and solar radiation
  • Source of all clouds & precipitation
  • 90% of water vapor lies below 6 km of atmosphere and only1% is above 10 km.

 

g) Solid particles:

  • The air also contains a variable amount of both organic and inorganic impurities such as dust, soot, salts, fungal spores, bacteria and pollen.
  • The main source of dust is the arid regions such as deserts and steppes (grassland).
  • The industrial regions, forest fires and volcanoes constitute the main source of soot.
  • During evaporation from the ocean, the salt remains in the air in the form of minute particles.
  • The salt particles from the oceans are most active as condensation nuclei on which the water vapour condenses to form fog or rain.
  • Absorb short wave solar radiation
  • Determine blue color of sky by absorbing short wave blue color and red & orange color in sun rise and sun set.
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