GEMET
General
Multilingual
Environmental
Thesaurus
režim vlhkosti půdní
Definition

The water regime of the soil is determined by the physical properties and arrangement of the soil particles. The pores in a soil determine its water-retention characteristics. When all the pores are full of water, the soil is said to be saturated.

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Scope note

Scope note is not available.

Concept URL: http://www.eionet.europa.eu/gemet/concept/7875