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Published byBartholomew Caldwell Modified over 9 years ago
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Chapter 10 - Soil Fertility
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Essential Plant Nutrients - 14 are Mineral Based Macros - N, P, K, Ca, Mg, S Micros - B, Cu, Cl, Fe, Mn, Mo, Zn, Ni
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Nutrients Exist in the Soil as Ions Ions are charged particles and can be… positively charged (cations): Ca +2, K +, NH 4 + or negatively charged (anions): Cl -, H 2 PO 4 -, SO 4 -2
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Ions are either adsorbed or absorbed adsorbed - “like a magnet” absorbed - “like a sponge”
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Stored (held in reserve) minerals (quartz, feldspar, etc.) organic material soil colloids (clay and humus particles) Readily Available soil solution (ions + water) Nutrient Sources
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Soil Colloids very small particles (< 1 millionth of a meter) large surface area negative charges along surfaces types of soil colloids: clays, oxides and humus clay humus
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Soil Colloids Silicate Clays - flat, plate-like crystals arranged in layers - negative surface charge Oxide Clays (sesquioxides) - iron and aluminum based - red in color - common in older soils with hot, humid climates Humus - decomposed organic matter - dark brown to black in color - mostly negative surface charge - high water holding capacity
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Tetrahedron: Basic building block is 1 silicon atom, connected to 4 oxygen atoms Octahedron: Basic building block is aluminum or magnesium, connected to six hydroxyl groups or oxygen atoms There are many layers in each micelle Typical Clay Structure silica alumina silica
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Illite
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- - - - Mg +2 Na + Mg +2 K+K+ Ca +2 - - - - - - - - - - - - - - - Al +3 - - - K+K+ Clay Particle Clay and Organic Particles have Negative Charges Cations are “attracted” and held to these particles with varying degrees of attraction…the order of relative strength of attraction is: Al +3 > H + > Ca +2 > Mg +2 > K + = NH 4 + > Na + NH 4 +
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CEC - the ability of a soil to hold and release nutrients (cations)
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Roots Access Nutrients in Solution by… root interception mass flow diffusion
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