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1 maximum molecular moisture capacity
Agriculture: MMMCУниверсальный русско-английский словарь > maximum molecular moisture capacity
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2 влагоёмкость
moisture capacity, ( почвогрунта) moisture, humidity ratio* * *влагоё́мкость ж.
moisture capacity; specific retention (of moisture by soil, rock, etc.)абсолю́тная влагоё́мкость — absolute moisture capacityвесова́я влагоё́мкость — gravimetric moisture capacityкапилля́рная влагоё́мкость — capillary moisture capacityмолекуля́рная влагоё́мкость — molecular moisture capacityполева́я влагоё́мкость — field water capacityполе́зная влагоё́мкость — available moisture capacityпо́лная влагоё́мкость — total moisture capacity -
3 молекулярная влагоемкость горной породы
молекулярная влагоемкость горной породы
Параметр, равный максимально возможной массовой доле физически связанной воды, которую способна принять данная горная порода.
[ ГОСТ Р 50544-93]Тематики
Обобщающие термины
EN
DE
FR
Русско-английский словарь нормативно-технической терминологии > молекулярная влагоемкость горной породы
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4 молекулярный
Русско-английский новый политехнический словарь > молекулярный
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5 молекулярный
Авиация и космонавтика. Русско-английский словарь > молекулярный
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6 влагоёмкость
ж. moisture capacity; specific retention -
7 гигроскопичность
1) Medicine: absorbability2) Engineering: hygroscopic property3) Chemistry: hygroscopicity4) Construction: molecular moisture cantilevering, water absorbency5) Mining: water absorption6) Polygraphy: hydroscopic property7) Textile: porosity8) Ecology: hygroscopity, water-absorbing quality9) Oil&Gas technology water-absorbing capacity10) Polymers: hygroscopic properties, moisture retaining property11) Physical chemistry: hygroscopy12) Cement: molecular moisture capacity, water-absorption quality -
8 молекулярный
1. gram-molecular2. molal3. molecular -
9 молекулярная влагоёмкость
1) Geology: molecular moisture capacity2) Construction: molecular moisture cantileveringУниверсальный русско-английский словарь > молекулярная влагоёмкость
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10 максимальная молекулярная влагоёмкость
Makarov: maximum molecular moisture capacityУниверсальный русско-английский словарь > максимальная молекулярная влагоёмкость
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11 плёночная влажность
Cement: molecular moisture capacityУниверсальный русско-английский словарь > плёночная влажность
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12 молекулярная влагоемкость горной породы
молекулярная влагоемкость горной породы
Параметр, равный максимально возможной массовой доле физически связанной воды, которую способна принять данная горная порода.
[ ГОСТ Р 50544-93]Тематики
Обобщающие термины
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > молекулярная влагоемкость горной породы
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13 молекулярная влагоемкость горной породы
молекулярная влагоемкость горной породы
Параметр, равный максимально возможной массовой доле физически связанной воды, которую способна принять данная горная порода.
[ ГОСТ Р 50544-93]Тематики
Обобщающие термины
EN
DE
FR
Русско-французский словарь нормативно-технической терминологии > молекулярная влагоемкость горной породы
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14 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-английский словарь нормативно-технической терминологии > влажность почвы
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15 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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16 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-французский словарь нормативно-технической терминологии > влажность почвы
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