potassium fixation in different clay minerals

clay minerals

1. Potassium (k) fixation in different clay minerals Rohith d.s palb8356

2. CONTENTS Potassium Forms of potassium Fixation of potassium Relation to clay minerals Factor affecting potassium fixation Practical implications of fixed potassium References

3. Potassium (k) K Constitutes About 2.5% Of Earth Crusts, The Seventh Abundant Element And Fourth Abundant Mineral. It Is Found In Large Concentration 1-5% In Plants. Roles Of K + In Plants Osmotic Regulation, Translocation Of Assimilates, Metabolic Processes, Improving Quality Of Fruits, Flowers And Vegetables, Imparting Resistance To Disease, Pests And Environmental Stress.

4. Forms of potassium

5. FIXATION OF POTASSIUM Fixation Of Potassium Was First Reported By Kellner In 1887 And Dyer In 1894 The K Which Penetrates The Intermicellar And Gets Fit Snugly Into The Holes And such are held tightly as they come in contact. Becomes Relatively Nonexchangeable Called Fixed (Rich 1968, Bolt Et Al 1976, Van Der Marel 1959)

6. LATTICE HOLE THEORY According to PAGE AND BAVER,1940 , the exposed surface and surfaces between sheets of 2:1 layer mineral consist of oxygen ions, arranged hexagonally. The opening within the hexagon is equal to the diameter of an oxygen ion (2.8Å). Any cation(K) with similar size can get fitted

7. EXPANDIBLE LAYER SILICATE

8. Order of K fixation in clay minerals Vermiculite > I llite > Montmorillonite > Kaolinite

9. VERMICULITE: High Charge Density More exchange sites ILLITE: Interlayer Space Is Same As K+ Ion Non Expanding MONTMORILLONITE: It Has Large Interlayer Space FILLED WITH Ca & Mg Kaolinite: Low Charge Density Non Expanding No Interlayer Space

10. FACTORS AFFECTING POTASSIUM FIXATION CHARGE DENSITY OF CLAY: Vermiculites fix more potassium compared to smectites due to internal charge density. EXTENT OF WEDGE ZONE: Deeper the wedge zone higher the amount of potassium fixed.

11. SOLUTION CONCENTRATION The solution K+ concentration affects the equilibrium between exchangeable and fixed K+ in soil. NATURE AND CONCENTRATION OF OTHER CATIONS The presence of cations like NH 4 + (2.86Å) and Rb +(2.96Å) compete with the K+ ion for interlayer space.

12. PRACTICAL IMPLICATION OF FIXED K + Tisdal and nelson (1975) Said That Potassium Fixation Is A Process Of Conserving Potassium In Nature. Non Exchangeable K+ Contributes Substantially To K+ Availability In Soils. Haylocks (1956) Introduced Terms Of “STEP-K” And “CONSTANT RATE K” As A Measure Of Potassium Reserve In Soils.

13. REFERENCES FUNDAMENTALS OF SOIL SCIENCE – ISSS (A.SUBBA RAO, M.S.BRAR) INTRODUCTORY SOIL SCIENCE – D.K DAS