Effect of Particle Size Variation in a Sample on Trace Element Concentration

摘要

Modern analytical chemistry of solid geomaterials has one specific feature: it does not account for the structure of an analyzed object. All efforts are directed to determination of its composition. The structure of the object comprises relations between its various parts, for example, with different characteristic sizes of composing particles, grains, and crystals. Actually the system structure is ignored on serious grounds; that is, the law of large numbers.