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Active Absorption of Ions (Part Three) and Ionic Uptake by Roots

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Active Absorption of Ions (Part Three)

ATPase Mediated Transport

ATPase can also generate proton gradient across the membrane. ATPase helps in hydrolysis of ATP. ATP is broken down into ADP and inorganic phosphate (Pi) with the addition of water. Water is spilt up into H+ and OH-. Then cations are transported activity in exchange for H+ in a direction opposite to H+. Anions follow passively, if anions are transported activity in exchange for OH-, cations show passive movement.

Ionic Uptake by Roots

Ions are present in the soil either adsorbed to the clay micelles or free in the soil solution. The uptake of ions by roots can be explained by the following theories:

  • Contact Exchange Theory.
  • Carbonic Acid Exchange Theory.

Contact Exchange Theory

According to this theory, the ions adsorbed on the clay micelles get adsorbed to the root in exchange for H+ ions, previously, adsorbed on the root.

Ions adsorbed on solid particles oscillate within a small space.

Contact Exchange

Contact Exchange

When two particles are close enough, the oscillation space of an ion adsorbed to one particle overlaps the oscillation space of an ion adsorbed to another particle. Thus exchange of ions may take place.

Carbonic Acid Exchange Theory

The soil solution provides medium for exchange of ions between the root and clay micelles.

Carbonic Acid Exchange

Carbonic Acid Exchange

Carbon dioxide released in respiration of root forms carbonic acid by reacting with water of the soil solution.

CO2 + H2O H2CO3 H+ + HCO-3

Carbonic acid then dissociates in the soil solution to form H+ and HCO-3 ions shown above expression. H+ ions are adsorbed to the clay micelles in exchange for cations, such as K+, which are released into the soil solution. From here they may diffuse to the root, where they may be adsorbed in exchange for H+ ions.

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Written on

May 26th, 2009 at 8:51 pm