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Soil Fertility Terms

Chapter 9
Soil Science and Management

AB
adsorptionbonding of an ion to a solid surface, usually temporarily
anion exchange capacitytotal sum of the number of exchangeable anions a soil can adsorb
cation exchangeexchange between a cation in solution and one adsorbed on a soil colloid
cation exchange capacitytotal number of exchangeable cations a soil can adsorb
Colloida very thin particle capable of being suspended in water without settling out rapidly
diffusionflow of matter through a liquid or gas by the random movement of molecules, caused by a concentration gradient, with the ions moving from more to less concentrated
essential elementsan element needed by plants for proper growth and reproduction
exchangeable basesa cation, excluding hydrogen and aluminum, held on cation exchange sites that can be easily replaced by another cation
expanding claysclays that expand greatly upon adsorption of interlayer water and shrink considerately upon drying
hydroponicsthe culture of plants in nutrients solutions rather than soil
isomorphous substitutionReplacement of one atom by another of similar size in a crystal lattice. May result in a charge if the atom has a different charge than the one replaced
luxury consumptionabsorption by plants of more nutrients, especially K, than they need at the time.
macronutrientsan essential element used in large amounts by plants, including N, P, K, Ca, Mg, S
mass actionlaw describing the principal of chemical equilibrium and the math description of this law called equilibrium constant expression
mass flowmovement of nutrients by movement of soil water
micellean individual particle of silicate clay
micronutrientessential element used in small quantities by plants
nonexchangeable ionsapplied to an ion so strongly adsorbed to a soil colloid that it is not normally available to be exchanged with ions in the soil solution
oxide clays (sesquioxide)finely divided particles of iron and aluminum oxides, most common in soils of warm, humid regions
percent base saturationpercentage of the cation exchange sites filled with exchangeable bases
primary macronutrientthree macronutrients (N,P,K) needed to be added to the soil in the greatest amounts for good crop growth
root interceptionroot surfaces find and adsorb nutrients directly from the surface of soil colloids
secondary macronutrientmacronutrients used less often as fertilizers than the primary elements (Ca, Mg, S)
silicate claysclays formed by association of structural units based on silica sheets and alumina sheets
soil fertilityability of a soil to supply the elements needed for plant growth
soil solutionthe liquid phase of soil, consisting of water and dissolved ions
trace element(micronutrient)essential elements used in small quantities by plants


Agriculture Teacher

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