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positron pozitron Fr.: positron The → antiparticle of the → electron, which has the same → mass, → spin, and → electric charge as the electron, but the charge is → positive. Positrons may be generated by → radioactive decay or by → pair production from energetic → gamma ray photons. |
positronium pozitroniom Fr.: positronium A short-lived bound state of a positron and an electron. From → positron + -ium (as in barium, titanium), from N.L., from L. neuter suffix. |
possession dârešt Fr.: possession 1) The act or fact of possessing; the state of being possessed. Dârešt, verbal noun of dâštan "to have, possess" (on the model of konešt, from kardan; xoršt, from xordan; bâlešt, from bâlidan; râmešt, from râmidan; (Lori) zenešt, from zadan; (Nowdân, Fârs) perešt, from paridan); Mid.Pers. dâr-, dâštan "to have, hold, preserve;" O.Pers./Av. dar- "to hold, keep back, maintain, keep in mind;" Skt. dhr- "to hold, keep, preserve," dharma- "what is established or firm; law;" Gk. thronos "elevated seat, throne," L. firmus "firm, stable," Lith. daryti "to make," PIE *dher- "to hold, support." |
post-Newtonian expansion sopâneš-e pasâ-Newtoni Fr.: développement post-newtinien |
post-Newtonian formalism disegerâyi-ye pasâ-Newtoni Fr.: formalisme post-newtonien An approximate version of → general relativity that applies when the → gravitational field is → weak, and the matter → velocity is → small. Post-Newtonian formalism successfully describes the gravitational field of the solar system. It can also be applied to situations involving compact bodies with strong internal gravity, provided that the mutual gravity between bodies is weak. It also provides a foundation to calculate the → gravitational waves emitted by → compact binary star systems, as well as their orbital evolution under radiative losses. The formalism proceeds from the Newtonian description and then, step by step, adds correction terms that take into account the effects of general relativity. The correction terms are ordered in a systematic way (from the largest effects to the smallest ones), and the progression of ever smaller corrections is called the → post-Newtonian expansion. |
postpone pas afkandan (#) Fr.: renvoyer, remettre, ajouner To put off to a later time; defer. From L. postponere "put after; neglect; postpone," from → post- "after" + ponere "to put, place," → position. Pas afkandan, literally "to throw after," "to postpone" (Dehxodâ), from pas- "after," → post-, + afkandan "to throw," → stopword. |
power function karyâ-ye tavâni Fr.: fonction de puissance A function of the form f(x) = xn, where n is a → real number. |
power-law distribution vâbâžeš bâ qânun-e tavâni Fr.: distribution en loi de puissance For a → random variable X, any → distribution which has the form: P(X ≥ x) = (k/x)α, where x is a value in the range defined for X, k > 0 is a parameter termed location parameter, and α > 0 is the → slope parameter. → power; → law; → distribution. |
Poynting-Robertson drag kerre-ye Poynting-Robertson Fr.: traînée de Poynting-Robertson A loss of → orbital angular momentum by tiny ring particles associated with their absorption and re-emission of → solar radiation. Also known as the → Poynting-Robertson effect (Ellis et al., 2007, Planetary Ring Systems, Springer). → Poynting-Robertson; → drag. |
Poynting-Robertson effect oskar-e Poynting-Robertson Fr.: effet Poynting-Robertson The effect of → solar radiation on a small (centimeter-sized) particle in → orbit around the Sun that causes it to lose velocity and fall gradually into the Sun. The particle → absorbs solar radiation and → radiates the energy → isotropically in its own frame. The particle thereby preferentially radiates (and loses → angular momentum) in the forward direction in the → inertial frame of the Sun (aberration effect). This leads to a decrease in the particle's angular momentum and causes it to spiral sunward. In contrast, the → Yarkovsky effect is anisotropic; the object may be accelerated or decelerated. → Poynting's theorem; Howard Percy Robertson (1903-1961), American physicist and mathematician; → effect. |
practitioner varzmand Fr.: praticien A professional man, especially in medicine and the law. |
pre-dispersion piš-pâšeš Fr.: pré-dispersion A technique in spectroscopy which uses a combination of several dispersive elements (prisms in series or a grism) before focusing the light on the primary disperser, usually a grating, in order to achieve high spectral resolutions. → pre-; → dispersion. |
precession pišâyân Fr.: précession The periodic motion of the → rotation axis of a
body such as a → spinning top
in which the axis of rotation gradually sweeps out a conical shape.
In the case of the spinning Earth, it is due to the combined
→ gravitational attractions of
the → Sun, the → Moon,
and → planets on Earth's
→ equatorial bulge. Since
the Earth's axis is tilted to its → orbital plane or
→ ecliptic, the gravitational force of the Sun and the Moon
on the Earth's equatorial bulge tend to pull it back
toward the plane of ecliptic. As a result, the axis → precesses.
Earth's axis of rotation precesses with a period of about 25,770 years, describing
one complete circle on the → celestial sphere
(→ precession constant). This circle has a radius
of approximately 23°.5, equal to the → inclination
of the Earth's orbit. Since the → vernal equinox
is the reference direction for the
→ equatorial coordinate system, the coordinates of "fixed" objects
change with time and must therefore be referred to an
→ epoch at which they are correct.
→ sign of zodiac. L.L. præcissionem "a coming before," from L. præcessus, p.p. of præcedere "to happen before," from the fact that the equinoxes occur earlier each year with respect to the preceding year, from præ- "before," → pre-, + cedere "to walk, to go, to happen." Pišâyân, literally "coming before," from piš- "before" → pre- + ây- (present stem of âmadan "to come, arrive, become"), from Av. ay- "to go, to come," aēiti "goes;" O.Pers. aitiy "goes;" Skt. e- "to come near," eti "arrival;" L. ire "to go;" Goth. iddja "went," Lith. eiti "to go;" Rus. idti "to go;" + -ân suffix of space and time. |
precession constant pâyâ-ye pišâyân Fr.: constante de précession The amount by which the equinoctial points drift westward annually due to precession. Its value for epoch J2000.0 is 50''.26, resulting from the westward → precession of the equator (50".38), and the eastward → precession of the ecliptic (0".12). → precession; → constant. |
precession of the ecliptic pišâyân-e hurpeh Fr.: précession de l'écliptique The component of general precession caused by the gravitational attraction of the planets on the Earth's center of mass. It causes the equinox to move eastward by about 0''.12 per year in the opposite direction to the → precession of the equator. This terminology replaces → planetary precession, according to an IAU resolution adopted in August 2006. → precession; → ecliptic. |
precession of the equator pišâyân-e hamugâr Fr.: précession de l'équateur That component of general precession caused by the combined effect of the Moon, the Sun and the planets on the equatorial protuberance of the Earth, producing a westward motion of the equinoxes along the ecliptic about 50'' per year. According to an IAU resolution adopted in August 2006, the present terminology replaces lunisolar precession. → precession; → equator. |
precession of the equinoxes pišâyân-e hamugânhâ Fr.: précession des équinoxes The slow motion of the equinoxes along the ecliptic, resulting from
the combined motion of the equator (→ precession of the equator)
and the ecliptic (→ precession of the ecliptic), or in other words the
precession of the Earth's axis of rotation.
Also know as → general precession.
The First Point of Aries moves westward along the ecliptic at 50.38 arcseconds
per year (1 degree every 71.6 years), causing the equinoxes to occur
about twenty minutes earlier each sidereal year.
See also → nutation.
→ precession; → equinox. |
precession of the nodes pišâyân-e gereh-hâ Fr.: précession des nœuds The gradual change in he orbital planes of a binary system. → precession; → node. |
precession period dowre-ye pišâyân Fr.: période de précession The interval with which a rotating body precesses. The precession period of the Earth is 25,770 years. For a → spinning top it is given by: Tp = (4π2I)/(mgrTs), where I is the → moment of inertia, m the mass of the top, g gravity, r the distance between the center of mass and the contact point, and Ts is the spinning period of the top. → precession; → period. |
precession time zamân-e pišÃ¢yân Fr.: temps de précession A time interval over which an orbit precesses by 2π radians in its plane. → precession; → time. |
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