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режим влажности почвы
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[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en] |
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soil moisture regime
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. (Source: DUNSTE)
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