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Lecture 3 Plant nutrition
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Potassium deficiency Symptoms - mottled or marginal chlorosis, which
then develops into necrosis on tips, margins and between veins - symptoms initially on more mature (“older”) leaves - leaves may curl and crinkle - stems may be slender and weak, with abnormally short internodal regions - in K-deficient corn, nodes may have increased susceptibility to root-rotting fungus present in the soil - this together with stem weakness results in bending of stems to the ground (lodging) Soybean Corn
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Iron deficiency Symptoms
- strong chlorosis at the base of the leaves with some green netting - deficiency starts out with interveinal chlorosis of the youngest leaves, evolves into an overall chlorosis, and ends as a totally bleached leaf - bleached areas often develop necrotic spots - because iron has a low mobility, iron deficiency symptoms appear first on the youngest leaves - iron deficiency is strongly associated with calcareous soils and anaerobic conditions, and it is often induced by an excess of heavy metals
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Analysis of plant tissues reveals mineral deficiencies
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Influence of the pH on the availability of nutrient
elements in organic soils - main losses of nutrients from agricultural systems is due to leaching that carries dissolved ions, especially nitrate, away with drainage water - in acid soils, leaching may be decreased by the addition of lime – a mix of CaO, CaCO3 and Ca(OH)2 –to make the soil more alkaline, because many elements form lesssoluble compounds when the pH is higher than 6 - width of the shaded areas in the graph indicates the degree of nutrient availability to the plant root
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• Inorganic fertilizer… – Straight fertilizer..Super phosphate,
Treating nutritional deficiencies • Inorganic fertilizer… – Straight fertilizer..Super phosphate, ammonium nitrate – Compound fertilizer (i.e. contain two or more mineral nutrients) • Organic fertilizer – Residues of plant and animals – Mineralization (organic compounds broken down by microorganisms)
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• Deficiency can be prevented • Not tied up in soils (Fe, Mn and Cu)
Foliar application of fertilizers • Uptake is faster • Deficiency can be prevented • Not tied up in soils (Fe, Mn and Cu) • Expensive • Vineyards
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The principle of cation exchange on the surface of a soil particle
- cations are bound to the surface of soil particles, because the surface is negatively charged - addition of a cation such as K+ can displace another cation such as Ca2+ from its binding on the surface of the soil particle and make it available for uptake by the root - mineral anions (NO3 _, Cl_) tend to be repelled by the negative charge of the surface and remain dissolved in soil solution; capacity of exchange of anions is smaller than of cation
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