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OH
Fr.: OH
See also: From → hydro- + ox(y)- a combining form meaning “sharp, acute, pointed, acid,” used in the formation of compound words, from Gk, oxys “sharp, keen, acid” + -yl a suffix used in the names of chemical radicals, from Fr. -yle, from Gk. hyle “matter, substance.” |
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OH 231.8+4.2
Fr.: OH 231.8+4.2
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xatt-e OH
Fr.: raie de OH
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meyzer-e OH
Fr.: maser OH
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xan-e OH (hidroksil)
Fr.: source OH
An astronomical source emitting microwave radiation characteristic of the hydroxyl OH molecule, especially one showing a maser effect. OH sources are found in molecular clouds in interstellar medium and in the cool envelopes of evolved stars. See also: OH, chemical compound hydroxyl; → source. |
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setâre-ye OH/forusorx
Fr.: étoile OH/IR
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ohm (#)
Fr.: ohm
A unit of electrical resistance equal to that of a conductor in which a current of one ampere is produced by a potential of one volt across its terminals. See also: Named after Georg Simon Ohm (1789-1854), the German physicist who discovered the law which bears his name. |
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qânun-e Ohm (#)
Fr.: loi d'Ohm
J = σ(E + v x B),
where v is the velocity and
B |
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Ohmi (#)
Fr.: ohmique
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zamân-e tabâhi-ye Ohmi
Fr.: temps de dissipation ohmique
An upper bound on the time scale on which the magnetic field of a system would decay in the absence of any other agent. It is expressed as: τμ = R2 / μ, where R is the scale size of the system, η the magnetic diffusivity (η = 1 / μσ, where μ is the magnetic permeability and σ the electrical conductivity). For a star like the Sun, τμ ≅ 1010 years, so a fossil magnetic field could survive for the star’s lifetime on the main sequence. For the Earth, τμ ≅ 104 years, so a → dynamo is required to explain the persistence of the geomagnetic field. |
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eftâl-e ohmi
Fr.: dissipation ohmique
See also: → Ohmic; → dissipation. |
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dastraft-e Ohmi
Fr.: perte ohmique
Same as → Ohmic dissipation. |