Özet:

The amarphic inorganic material of the soil is usually part of the fiber fraction, which is less than 2 microns with the upper limit of the equivalent diameter and is the active part of the soil. The minerals in the flame fraction of the soil can be classified as crystal flame minerals, crystal sound oxides, amorph sound oxides, and allofan. Important information has been obtained by using a wide variety of methods about the crystalline fiber minerals in the fiber fraction. But we have very little information about the nature of amorphic elements such as kidrate oxides and organominerals in the fence fraction. The amorphic inorganic material in the soil is opaline, silice, amorph hydrate ialuminium oxide, amorph dirate iron oxide, alloian, rutU and anatase. Combined oxyde,r and free oxyde in the soil are involved in Qnemli physical and chemical reactions. The significant effects on the formation of the soil structure, anion and cation changes, phosphorus julation, r ~ action with potassium and chloride are an example of this. This is why it has been focused on the research of these in recent times.