Sättigungswasser
Sättigungswasser refers to water that is present in a porous material when all available pore spaces are completely filled with water. In essence, it is the maximum amount of water that a substance can hold under given conditions. This concept is particularly relevant in soil science, hydrogeology, and material science.
When a material is saturated, any additional water introduced will not be absorbed by the material itself
In soils, saturated conditions are important for understanding groundwater recharge, water table levels, and the transport