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21 ultimate field water capacity
Англо-русский словарь по экологии > ultimate field water capacity
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22 effective field water capacity
Экология: полезная полевая влагоёмкостьУниверсальный англо-русский словарь > effective field water capacity
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23 ultimate field water capacity
Почвоведение: предельная полевая влагоёмкостьУниверсальный англо-русский словарь > ultimate field water capacity
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24 полевая влагоёмкость
1) Engineering: (нормальная) field capacity2) Forestry: field capacity (почвы)3) Ecology: field capacity, field moisture capacity, field water capacity4) Makarov: water field capacity( WFC)5) Soil science: normal (field) capacity, normal field capacity, normal moisture capacity, water field capacity6) General subject: effective water-holding capacity, field (capillary) moisture capacity, field carrying capacity, normal (field) moisture capacityУниверсальный русско-английский словарь > полевая влагоёмкость
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25 нормальная влагоёмкость
1) Makarov: water field capacity( WFC)2) Soil science: field capacity, field moisture capacity, field water capacity, normal (field) capacity, normal field capacity, normal moisture capacity, water capacity, water field capacityУниверсальный русско-английский словарь > нормальная влагоёмкость
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26 WFC
1) Спорт: Watford Football Club, Weaker Football Conference, Wimbledon Football Club, Womens Football Club2) Военный термин: Wallops Flight Center, War Force Clan, With Flying Colours3) Техника: wide field camera4) Электроника: Wide Field Channel5) Вычислительная техника: Windows Foundation Classes, Wait for Caller (BBS), Windows Foundation Classes (MS, Java, API)6) Экология: World Food Council7) Макаров: water field capacity8) NYSE. Wells Fargo & Company9) Хобби: Washington Flanders Club -
27 WFC
1. water field capacity - влажность полевой влагоёмкости; полевая влагоёмкость;2. wide field camera - камера с широким обзором -
28 зона почвенной влаги
1) Engineering: soil-water zone2) General subject: belt of soil water, field capacity zoneУниверсальный русско-английский словарь > зона почвенной влаги
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29 влажность полевой влагоёмкости
Engineering: water field capacityУниверсальный русско-английский словарь > влажность полевой влагоёмкости
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30 наименьшая влагоёмкость
1) Engineering: field moisture capacity2) Forestry: field capacity (почвы)3) Ecology: minimum moisture-holding capacity (почвы)4) Makarov: field moisture capacity (почвогрунта), minimum water capacity (почвы)Универсальный русско-английский словарь > наименьшая влагоёмкость
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31 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
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > влажность почвы
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32 humidité du sol
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
EN
DE
FR
Франко-русский словарь нормативно-технической терминологии > humidité du sol
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33 Bodenfeuchtigkeit
влажность почвогрунта
Содержание воды в почвогрунте.
Примечание
Различают: весовую влажность, которая выражается в процентах от веса абсолютно сухого почвогрунта или в процентах от веса сырого почвогрунта; объемную влажность - количество воды в почвогрунте, выраженное отношением объема воды к объему почвогрунта.
[ ГОСТ 19179-73]Тематики
Обобщающие термины
EN
DE
FR
влажность почвы
—
[ 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
EN
DE
FR
Немецко-русский словарь нормативно-технической терминологии > Bodenfeuchtigkeit
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34 влажность почвы
влажность почвы
—
[ 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
EN
DE
FR
Русско-английский словарь нормативно-технической терминологии > влажность почвы
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35 влажность почвы
влажность почвы
—
[ 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
EN
DE
FR
Русско-французский словарь нормативно-технической терминологии > влажность почвы
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36 soil moisture
влажность почвогрунта
Содержание воды в почвогрунте.
Примечание
Различают: весовую влажность, которая выражается в процентах от веса абсолютно сухого почвогрунта или в процентах от веса сырого почвогрунта; объемную влажность - количество воды в почвогрунте, выраженное отношением объема воды к объему почвогрунта.
[ ГОСТ 19179-73]Тематики
Обобщающие термины
EN
DE
FR
влажность почвы
—
[ 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
EN
DE
FR
Англо-русский словарь нормативно-технической терминологии > soil moisture
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37 полезная полевая влагоёмкость
1) Ecology: effective field water capacity2) Soil science: available field capacityУниверсальный русско-английский словарь > полезная полевая влагоёмкость
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38 Feldkapazität
f1. field capacity2. water holding capacity -
39 полевая влагоемкость
Русско-английский технический словарь > полевая влагоемкость
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40 полевая влагоемкость
Русско-английский политехнический словарь > полевая влагоемкость
См. также в других словарях:
Field capacity — is the amount of soil moisture or water content held in soil after excess water has drained away and the rate of downward movement has materially decreased, which usually takes place within 2–3 days after a rain or irrigation in pervious soils of … Wikipedia
field capacity — noun the maximum amount of water that a particular soil can hold • Hypernyms: ↑volume unit, ↑capacity unit, ↑capacity measure, ↑cubage unit, ↑cubic measure, ↑cubic content unit, ↑displacement unit, ↑cubature un … Useful english dictionary
field capacity — water in the soil once gravitational water has fully drained out i.e. capillary and hygroscopic water … Geography glossary
field capacity — /ˈfild kəˌpæsəti/ (say feeld kuh.pasuhtee) noun the amount of water held in a soil by capillary action after gravitational water has percolated downward and drained away; expressed as the ratio of the weight of water retained to the weight of dry …
Water retention curve — is the relationship between the water content, θ, and the soil water potential, ψ. This curve is characteristic for different types of soil, and is also called the soil moisture characteristic.It is used to predict the soil water storage, water… … Wikipedia
Water content — Soil composition by phase: s soil (dry), v void (pores filled with water or air), w water, a air. V is volume, M is mass. Water content or moisture content is the quantity of water contained in a material, such as soil (called soil moisture),… … Wikipedia
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Water supply and sanitation in Yemen — is characterized by poor service quality and low levels of access, the latter being almost as low as in Sub Saharan Africa for sanitation. Yemen is both the poorest country and the most water scarce country in the Arab world. In addition, the… … Wikipedia