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Soil Cation & Anion Exchange Capacity: Terms, Factors, & Measurement, Lab Reports of Agricultural engineering

An overview of cation exchange capacity (cec) and anion exchange capacity (aec) in soil. It covers terms related to these concepts, sources of charge, strength of hold and likeliness of adsorption, and factors affecting cec and ph. Additionally, it discusses the role of anion exchange capacity and the methods to measure cec and aec.

Typology: Lab Reports

Pre 2010

Uploaded on 08/31/2009

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Download Soil Cation & Anion Exchange Capacity: Terms, Factors, & Measurement and more Lab Reports Agricultural engineering in PDF only on Docsity! Cation Exchange Capacity (CEC) Terms to Know • Cation • Isomorphous Substitution • Anion • Hydroxyl • Colloid • pH – power of hydrogen – neutral pH = 7 – acidic < 7 – basic > 7 • adsorption – electrostatic attraction to the outside of the colloid (think adhere) – NOT the same as absorption! Strength of Hold & Likeliness of Adsorption • How tight an ion is held is determined by 1) Size of ion’s hydrated radius • Smaller radius = tighter hold 2) Magnitude of ion’s charge • Higher charge = tighter hold Al3+ > Ca2+ > Mg2+ > K+, NH4+ > Na+ > Li+ • How likely an ion species is to be adsorbed is determined by its concentration in the soil solution • Higher concentration = more adsorption • High concentration of one ion species relative to another ion species can supersede the effect of radius and charge Balanced by Charge colloid K+ K+ colloid Ca2+ + 2K+ + Ca2+ Charge for Charge….. NOT ion for ion Also note: This is a reversible reaction Cation Exchange Capacity (CEC) • Total amount of exchangeable cations that can be held by a given soil mass • Total CEC impacted by 1) Soil texture (amount of clay) 2) Clay type 3) Soil organic matter 4) pH Anion Exchange Capacity (AEC) • When the pH drops below 6 and clays become positively charged – Positive charge on colloids attracts anions • Colloids with AEC: oxide clays, amorphous clays, 1:1 clays – Humus generally retains a negative charge regardless of pH, but will increase its negativity at higher pH values • Allows soils to adsorb anionic nutrients – e.g. NO3- , PO43- • Allows soils to adsorb anionic toxins and keep them out of groundwater – e.g. 2,4-D Cation/anion exchange capacity (emol,,/kg) CEC/AEC and pH 4 Cation exchange sat capacity 2 } Anion exchange s capacity ! i = oO | l 4 5 6 7 Sail pH Measuring CEC/AEC • Measure charge • Units are cmolc/kg (charge/soil mass) • 2 ways to estimate CEC: – Add up charge given by each ion species – Add up charge held by each soil colloid type
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