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21 уплотненная токопроводящая жила
- verdichteter Leiter, m
уплотненная токопроводящая жила
скрученная токопроводящая жила, в которой промежутки между составляющими элементами уменьшены путем механического обжатия, вытягивания или за счет соответствующего выбора формы и расположения проволок
Примечание. Французский термин «ame en paves» означает частично уплотненная токопроводящая жила большого сечения состоящая из нескольких проволок фасонного сечения
[IEV number 461-01-14]EN
compacted conductor
stranded conductor in which the interstices between the component wires have been reduced by mechanical compression or by drawing or by suitable choice of the shape and disposition of wires
NOTE – The French term «âme en pavés» means a particular compacted conductor of large cross-section comprising a small number of shaped wires.
[IEV number 461-01-14]FR
âme compacte
âme rétreinte
âme câblée dans laquelle les interstices entre les fils ont été réduits par compression mécanique ou tréfilage ou par un choix approprié de la forme et de la disposition des fils
NOTE – Une âme en pavés est une âme compacte de type particulier ayant une section importante et composée d'un nombre réduit de fils de forme.
[IEV number 461-01-14]
Тематики
- кабели, провода...
EN
DE
- verdichteter Leiter, m
FR
Русско-немецкий словарь нормативно-технической терминологии > уплотненная токопроводящая жила
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22 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)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > циркуляция морской воды
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