colloidal fraction
Clay + humus particles
extremely small size-less than about 1 μm (0.000001 m)
colloid-like behavior.
properties of colloids
Extremely small (<1 μm, sub-microscopic),
remain in suspension
4 types of soil colloids
– Crystalline silicate clays (less weathering, temperate)
– Allophane & assoc. non-crystalline clays (volcanics)
– Fe- and Al-oxide clays (most prominent in tropics)
– Humus (product of organic matter)