kolmikerroksisuus
Kolmikerroksisuus, word for “three-layeredness” in Finnish, refers to a structural feature in which a system is organized into three distinct layers that are separable and have different properties. The core idea is a tripartite stratification with interfaces between layers that typically correspond to changes in composition, density, porosity, conductivity, mechanical behavior, or other relevant characteristics. The term is used across disciplines, and its exact definition depends on the field and context.
In geology and soil science, kolmikerroksisuus describes a stratified medium with three main layers, often representing
Identification of kolmikerroksisuus relies on detecting distinct boundaries between layers through field observations, boreholes, geophysical surveys,