The Turnover of Nitrogen
Just as carbon is the key elements for the synthesis of carbohydrates, so is nitrogen for he synthesis of protein. The atmosphere is a vast reservoir of nitrogen but the N2 of the atmosphere must necessarily combine with H2 or O2 before it can be assimilated by higher plants. The inert atmospheric nitrogen occupies approximately 75% by weight, and 78% by volume of the atmosphere and totals 3.8 x 1015 tonnes.
However, the amount of nitrogen in the biosphere is dependent on the rates of transfer within the nitrogen cycle and can be estimated only within broad limits. Some authors have estimated that 400 x 106 t N/yr by are transferred between the various nitrogen pools, with losses of 215 x 106 t N/yr by denitrification and 185 x 106 t N/yr by volatilization and combustion.





