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Colloidal complex of soils that consists of mainly clays and humus(organic matter)
soil colloids
Soil colloids play an important role in…
ion exchange and fertility
Clay’s small size translates to…
high surface area and adsorptive capacity
The four major types of Colloids
Crystalline silicate clays, non-crystalline silicate clays, Al and Fe Oxides, Humus-organic colloids
Crystalline vs non-crystalline silicate clays
crystalline clays are dominant and layered and non-crystalline is not layered
Al and Fe Oxides vs Humus-Organic Colloids
Al and Fe oxides are in highly weathered soils of warm regions
Humus-organic colloids are in mostly all soils(especially upper profiles) and is undefined structure
The building blocks of layered silicate clay structure
Si-tetrahedron, Al/Mg-octahedron, and sheets and layers
One cation by another of similar size but different charge
Isomorphous substitution
pH dependent charges are associated with…
hydroxyl(OH-) groups (as pH increases, deprotonation increases)
Organization of Select Layer Silicate Clays
Based on the number and arrangement of tetrahedral (Si) and octahedral (Al, Mg) sheets contained into crystal layers
Crystalline silicate clays are classified into what 3 groups
1:1 type, expanding 2:1, non expanding 2:1
Modified octahedral sheets found in highly weathered soils
Al and Fe Oxides
Organic Colloids are also known as
HUMUS (high negative charge)
In soil, the negative and positive charges are…
attracted to each other that result in many cations and anions present
In temperate-region soils, the …. is common and negatively charged
2:1 type silicate clays that absorb cations
In the tropics, soils are rich in…and positive charges are more abundant
1:1 clays, and Fe, Al oxides
Cation vs Anion Exchange Reactions
Cation- the colloidal site is negatively charged
Anion- colloidal site is positively charged
The total exchangeable cations a soil can absorb
Cation Exchange Capacity (CEC)
…. use cation exchange to assist in nutrient uptake from soil
plant roots