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1 граница между воздухом и поверхностью океана
граница между воздухом и поверхностью океана
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
ocean-air interface
The sea and the atmosphere are fluids in contact with one another, but in different energy states - the liquid and the gaseous. The free surface boundary between them inhibits, but by no means totally prevents, exchange of mass and energy between the two. Almost all interchanges across this boundary occur most effectively when turbulent conditions prevail. A roughened sea surface, large differences in properties between the water and the air, or an unstable air column that facilitates the transport of air volumes from sea surface to high in the atmosphere. Both heat and water (vapor) tend to migrate across the boundary in the direction from sea to air. Heat is exchanged by three processes: radiation, conduction, and evaporation. The largest net exchange is through evaporation, the process of transferring water from sea to air by vaporization of the water. (Source: PARCOR)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
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Русско-французский словарь нормативно-технической терминологии > граница между воздухом и поверхностью океана
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2 двустабильное электрическое реле
двустабильное электрическое реле
Электрическое реле, которое, изменив свое состояние под воздействием входной воздействующей или характеристической величины, после устранения воздействия не изменяет своего состояния до приложения другого необходимого воздействия
[ ГОСТ 16022-83]EN
bistable relay
electrical relay which, having responded to an energizing quantity and having changed its condition, remains in that condition after the quantity has been removed; a further appropriate energization is required to make it change its condition
[IEV number 444-01-08]FR
relais bistable, m
relais électrique qui, ayant changé d'état sous l'action d'une grandeur d'alimentation d'entrée, reste dans le même état lorsqu'on supprime cette grandeur ; une autre action appropriée est nécessaire pour le faire changer d'état
[IEV number 444-01-08]Параллельные тексты EN-RU
In a bistable relay with one winding, the opposite energizing is created by a voltage with opposite polarity being applied to the same winding.
In a bistable relay with two windings, the opposing energizing is created by a voltage being applied to the second winding with opposite winding sense.
[Tyco Electronics]В двустабильном реле с одной обмоткой изменение коммутационного положения осуществляется подачей напряжения противоположной полярности на эту же самую обмотку.
В двустабильном реле с двумя обмотками изменение коммутационного положения осуществляется подачей напряжения на другую обмотку (т. е. на обмотку, действие которой противоположно действию предыдущей обмотки).
[Перевод Интент]A remanent, bistable relay which adopts a particular switching position following an energizing direct current in any direction and is then held in this position by the remanence in the magnetic circuit, i.e. through the magnetization of parts of the magnetic circuit. The contacts return to their original position following a small energizing current of limited amplitude of the opposite polarity. This demagnetises the magnetic circuit.
[Tyco Electronics]Двустабильное реле с остаточной намагниченностью переходит в определенное коммутационное положение при подаче постоянного тока любой полярности и затем удерживается в этом положении за счет остаточной намагниченности частей магнитопровода. Контакты реле возвращаются в исходное положение после воздействия небольшого тока обратной полярности. При этом происходит размагничивание магнитопровода.
[Перевод Интент]Недопустимые, нерекомендуемые
- бистабильное реле
- реле с механической блокировкой
- реле с самоудерживанием
- реле самозамыкающее
- реле самоудерживающее
Тематики
Классификация
>>>EN
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14. Двустабильное электрическое реле
D. Bistabiles Relais
Е. Bistable relay
F. Relais bistable
Электрическое реле, которое, изменив свое состояние под воздействием входной воздействующей или характеристической величины, после устранения воздействия не изменяет своего состояния до приложения другого необходимого воздействия
Источник: ГОСТ 16022-83: Реле электрические. Термины и определения оригинал документа
Русско-французский словарь нормативно-технической терминологии > двустабильное электрическое реле
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3 циркуляция морской воды
циркуляция морской воды
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
sea circulation
Large-scale horizontal water motion within an ocean. The way energy from the sun, stored in the sea, is transported around the world. The currents explain, for example, why the UK has ice-free ports in winter, while St. Petersburg, at the same latitude as the Shetland Islands, needs ice breakers. Evidence is growing that the world's ocean circulation was very different during the last ice age and has changed several times in the distant past, with dramatic effects on climate. The oceans are vital as storehouses, as they absorb more than half the sun's heat reaching the earth. This heat, which is primarily absorbed near the equator is carried around the world and released elsewhere, creating currents which last up to 1.000 years. As the Earth rotates and the wind acts upon the surface, currents carry warm tropical water to the cooler parts of the world. The strength and direction of the currents are affected by landmasses, bottlenecks through narrow straits, and even the shape of the sea-bed. When the warm water reaches polar regions its heat evaporates into the atmosphere, reducing its temperature and increasing its density. When sea-water freezes it leaves salt behind in the unfrozen water and this cold water sinks into the ocean and begins to flow back to the tropics. Eventually it is heated and begins the cycle all over again. (Source: MGH / WRIGHT)
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Русско-французский словарь нормативно-технической терминологии > циркуляция морской воды
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