Quantitative analysis of soil elay minerals after X-ray, differential thermal, infrared, cation exchange and chemica! analysis is treated. Partiele size, crystallite size, the grade of structural ordening in the minerals, and the surface being covered by an amorphous (Beilby) layer, have large influence on the results. Examples are given.
|Journal||Acta Universitatis Carolinae. Geologica|
|Issue number||supplementum 1|
|Publication status||Published - 1961|
- clay minerals
- clay soils
- chemical analysis