active soil - translation to ρωσικά
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active soil - translation to ρωσικά

Pereletok; Intergelisol; Inactive layer; Active soil layer
  • The red dotted-to-solid line depicts the average temperature profile with depth of soil in a permafrost region. The trumpet-shaped lines at the top show seasonal maximum and minimum temperatures in the "active layer", which commences at the depth where the maximum annual temperature intersects 0 °C. The active layer is seasonally frozen. The middle zone is permanently frozen as "permafrost". And the bottom layer is where the geothermal temperature is above freezing. Note the importance of the vertical 0 °C line: It denotes the bottom of the active layer in the seasonally variable temperature zone and the bottom limit of permafrost as the temperature increases with depth.

active soil      

строительное дело

деятельный слой (грунта в зоне вечной мерзлоты)

active soil      
деятельный слой (грунта в зоне вечной мерзлоты)
active voice         
GRAMMATICAL VOICE
Active Voice; Active tense
действительный залог

Ορισμός

soil
(soils, soiling, soiled)
Frequency: The word is one of the 3000 most common words in English.
1.
Soil is the substance on the surface of the earth in which plants grow.
We have the most fertile soil in Europe.
...regions with sandy soils.
N-MASS
2.
You can use soil in expressions like British soil to refer to a country's territory.
The issue of foreign troops on Turkish soil is a sensitive one.
= territory
N-UNCOUNT: with supp
3.
If you soil something, you make it dirty. (FORMAL)
Young people don't want to do things that soil their hands...
He raised his eyes slightly as though her words might somehow soil him.
= dirty
VERB: V n, V n
soiled
...a soiled white apron.
= dirty
ADJ

Βικιπαίδεια

Active layer

In environments containing permafrost, the active layer is the top layer of soil that thaws during the summer and freezes again during the autumn. In all climates, whether they contain permafrost or not, the temperature in the lower levels of the soil will remain more stable than that at the surface, where the influence of the ambient temperature is greatest. This means that, over many years, the influence of cooling in winter and heating in summer (in temperate climates) will decrease as depth increases.

If the winter temperature is below the freezing point of water, a frost front will form in the soil. This "frost front" is the boundary between frozen and unfrozen soil, and with the coming of spring and summer, the soil is thawed, always from the top down. If the heating during summer exceeds the cooling during winter, the soil will be completely thawed during the summer and there will be no permafrost. This occurs when the mean annual temperature is above 0 °C (32 °F), but also occurs when the mean annual temperature is slightly below 0 °C on sites exposed to the sun with coarse-textured parent materials (vegetation).

When there is not sufficient heat to thaw the frozen soil completely, permafrost forms. The active layer in this environment consists of the top layers of soil which thaws during the summer, while the inactive layer refers to the soil below which is frozen year-round because the heat fails to penetrate. Liquid water cannot flow below the active layer, with the result that permafrost environments tend to be very poorly drained and boggy.

Μετάφραση του &#39active soil&#39 σε Ρωσικά