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By Dr. Chris Meletis N. D. Minerals can generally be found in two different forms. The first form is that of a colloid, where minerals are suspended in a stable form. In this stable form, the minerals are evenly distributed throughout the medium in which they are suspended.Minerals in this colloid state are held in large, organized patterns, whereby they remain in suspension without settling out.Colloidal minerals are not readily absorbed by the body due to the absence of an electrical charge and their relatively large size, unlike other mineral forms.he first form is that of a colloid, where minerals are suspended in a stable form. In this stable form, the minerals are evenly distributed throughout the medium in which they are suspended. Minerals in this colloid state are held in large, organized patterns, whereby they remain in suspension without settling out.
The inorganic component includes both primary and secondary minerals. The secondary minerals normally are found in the clay fraction of the soil which is the fraction of the soil solids which is less the 2 micron or 0.002 mm. Clay minerals are minerals which mainly occur in the clay sized fraction of the soil.2.he clay minerals and soil organic matter are colloids. The most important property of colloids is their small size and large surface area. The total colloidal area of soil colloids may range from 10m2/g to more than 800 m2/g depending the external and internal surfaces of the colloid.