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1 слой грунта
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2 верхний слой грунта
Русско-английский научно-технический словарь Масловского > верхний слой грунта
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3 верхний слой грунта
Русско-английский словарь нормативно-технической терминологии > верхний слой грунта
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4 верхний горизонт
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5 пахотный слой почвы
1) Ecology: surface soil, tilth-top soil2) Makarov: topsoil3) General subject: tilth top soil, top soilУниверсальный русско-английский словарь > пахотный слой почвы
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6 верхний слой почвы
Универсальный русско-английский словарь > верхний слой почвы
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7 верхний (пахотный) ёлок почвы
Agriculture: surface soil, top soilУниверсальный русско-английский словарь > верхний (пахотный) ёлок почвы
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8 верхний пахотный слой почвы
Makarov: surface soil, top soilУниверсальный русско-английский словарь > верхний пахотный слой почвы
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9 глубина пахотного слоя
1) Engineering: plowing horizon2) Agriculture: surface soil thickness3) Ecology: depth of top soil, plowing depthУниверсальный русско-английский словарь > глубина пахотного слоя
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10 подпахотный слой почвы
1) Agriculture: subsurface soil2) Makarov: surface soilУниверсальный русско-английский словарь > подпахотный слой почвы
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11 верхний ёлок почвы
Универсальный русско-английский словарь > верхний ёлок почвы
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12 верхний горизонт
1) Geology: higher level, rise level, shallow horizon, upper level2) Engineering: headwater3) Construction: head water, head-water4) Ecology: surface soil layer, upper layer -
13 верхний слой грунта
Oil: surface soilУниверсальный русско-английский словарь > верхний слой грунта
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14 поверхностная засолённость почвы
Ecology: surface-soil salinityУниверсальный русско-английский словарь > поверхностная засолённость почвы
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15 поверхностный слой земли
Geology: surface soilУниверсальный русско-английский словарь > поверхностный слой земли
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16 поверхностный слой почвы
1) Geology: surface soil2) Automobile industry: topsoilУниверсальный русско-английский словарь > поверхностный слой почвы
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17 приповерхностный слой почвы
Ecology: near-surface soilУниверсальный русско-английский словарь > приповерхностный слой почвы
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18 герметичный слой на поверхности почвы
герметичный слой на поверхности почвы
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
soil surface sealing
Any activity or process in which ground surface areas are packed or plugged to prevent percolation or the passage of fluids. (Source: SIS / ERG)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
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Русско-английский словарь нормативно-технической терминологии > герметичный слой на поверхности почвы
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19 почвенный процесс
почвенный процесс
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
soil process
The major processes in soils are gains, losses, transfers, and transformations of organic matter, soluble salts, carbonates, silicate clay minerals, sesquioxides, and silica. Gains consist normally of additions of organic matter, and of oxygen and water through oxidation and hydration, but in some sites slow continuous additions of new mineral materials take place at the surface or soluble materials are deposited from groundwater. Losses are chiefly of materials dissolved or suspended in water percolating through the profile or running off the surface. (Source: PARCOR)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
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Русско-английский словарь нормативно-технической терминологии > почвенный процесс
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20 влажность почвы
влажность почвы
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
soil moisture
1) Water stored in soils.
2) One of the most important elements involved in pedological processes and plant growth. There are three basic forms:
a) water adhering in thin films by molecular attraction to the surface of soil particles and not available for plants is termed hygroscopic water.
b) Water forming thicker films and occupying the smaller pore spaces is termed capillary water. Since it is held against the force of gravity it is permanently available for plant growth and it is this type of soil water which contains plant nutrients in solution.
c) Water in excess of hygroscopic and capillary water is termed gravitational water, which is of a transitory nature because it flows away under the influence of gravity. When the excess has drained away the amount of water retained in the soil is termed its field capacity, when some of its pore spaces are still free of water.
(Source: LANDY / DUNSTE)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
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Русско-английский словарь нормативно-технической терминологии > влажность почвы
См. также в других словарях:
surface soil — noun the layer of soil on the surface • Syn: ↑topsoil • Hypernyms: ↑soil, ↑dirt * * * noun : the upper 5 to 8 inches of the soil layer : the portion of the soil usually tilled … Useful english dictionary
Soil horizon — Soil samples illustrating horizons (subsoil on right) A soil horizon is a specific layer in the land area that is parallel to the soil surface and possesses physical characteristics which differ from the layers above and beneath … Wikipedia
Soil morphology — is the field observable attributes of the soil within the various soil horizons and the description of the kind and arrangement of the horizons. [cite book | last = Buol | first = Stanley W. | authorlink = | coauthors = Southard, Randal J.,… … Wikipedia
Soil Moisture and Ocean Salinity satellite — Global soil moisture and ocean salinity measurements are needed to better understand Earth’s water cycle and climate. Currently, there is no thorough dataset on soil moisture or ocean salinity. Current satellites operated by NASA have provided… … Wikipedia
soil creep — noun : slow down slope movement of earth materials under the influence of gravitation * * * Geol. creep of soil on even slopes; often accelerated by spring freeze and thaw or general periglacial conditions. Cf. creep (def. 17a). [1895 1900] * * * … Useful english dictionary
Soil conservation — is set of management strategies for prevention of soil being eroded from the earth’s surface or becoming chemically altered by overuse, salinization, acidification, or other chemical soil contamination. The principal approaches these strategies… … Wikipedia
Soil pH — is the pH of soil water. It is based on the measurement of pH, which depends on the activity of hydrogen ions (H+) in a solution.There are many different methods to collect soil water, all which influence the measured soil pH in one way or… … Wikipedia
Soil structure — is determined by how individual soil granules clump or bind together and aggregate, and therefore, the arrangement of soil pores between them. Soil structure has a major influence on water and air movement, biological activity, root growth and… … Wikipedia
Soil science — is the study of soil as a natural resource on the surface of the earth including soil formation, classification and mapping; physical, chemical, biological, and fertility properties of soils; and these properties in relation to the use and… … Wikipedia
Soil salinity — is the salt content in the soil. [ [http://europeandcis.undp.org/WaterWiki/index.php/Soil salinity from Soil salinity in WaterWiki, the on line Knowledge and Collaboration Tool of the Community of Practice (CoP) on Water and UNDP related… … Wikipedia
Surface mining — is a type of mining in which soil and rock overlying the mineral deposit are removed. It is the opposite of underground mining, in which the overlying rock is left in place, and the mineral removed through shafts or tunnels. Surface mining is… … Wikipedia
