mikrofinaatsiooni
mikrofinaatsioon refers to a scientific methodology for analyzing and characterising materials at the micro‑fine scale. The term merges the Greek root mikro meaning “small” with the Estonian suffix –finaatsioon, signifying the act of fine analysis. It is commonly applied in geology, agronomy, soil science, and materials engineering to assess the physical and chemical properties of sub‑millimetre particles, such as soil clays, sedimentary grains, and manufactured powders. The primary objective of mikrofinaatsioon is to quantify particle size distributions, surface area, mineral composition, and textural features that influence reactive behaviour, transport phenomena, and ecological functions.
The methodology typically combines optical microscopy, scanning electron microscopy (SEM), X‑ray diffraction (XRD), and spectroscopic techniques
Applications of mikrofinaatsioon span from detailed soil fertility assessment, where clay mineralogy determines nutrient retention, to
The field continues to evolve with advances in nano‑characterisation techniques and machine‑learning‑driven image recognition, allowing faster,