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sound 1) sedâ (#); 2) dorvâ Fr.: 1) son; 2) sain 1) A physiological sensation received by the ear. It is caused by a vibrating
source and transmitted as a longitudinal pressure wave motion through a material
medium such as air. 1) M.E. soun; O.Fr. son, from L. sonus "sound," sonare "to sound;"
PIE base *suen- "to sound;" cf.
Av. xvan- "to sound;"
Pers. xvân-, xvândan "to sing, read;"
Skt. svana- "sound," svan-
"to sound," svanati "it sounds;" O.E. swinn "music, song"
(Cheung 2007). 1) Sedâ "sound," most probably a Pers. term, since it exists also in Indo-Aryan
languages: Skt. (late Vedic): sabda "articulate sound, noise,"
Pali and Prakriti: sadda "sound, noise," Sindhi: sadu, sado "shout, call,"
Gujrâti sad "call, voice, echo,"
Marathi: sad "shouting to," Konkani sad "sound,"
Sinhali: sada "sound." Therefore,
sadâ in Ar. "reverberating noise, echo" maybe a loan
from Pers., or a coincidence. Note that for the author of the classical Pers.
dictionary Borhân-e Qâte' (India, 1652 A.D.), the Ar. term is
a loanword from Pers. |
sound barrier divâr-e sedâ, varqe-ye ~ Fr.: mur du son A sharp increase in aerodynamic drag that occurs as the speed of an aircraft approaches the speed of sound. Also called sonic barrier. |
sound energy kâruž-e sedâ Fr.: énergie acoustique The energy which → sound waves impart to a medium. Same as acoustic energy. |
sound field meydân-e sedâ Fr.: champ acoustique The distribution of → sound energy in a defined space. |
sound horizon ofoq-e sedâ Fr.: horizon sonore The maximum distance a → sound wave could have traveled through the ionized plasma from the → Big Bang until the → recombination era. It is 150 → Mpc, or bout 500 million → light-years. Sound horizon is the equivalent of the concept of → cosmic horizon, where one replaces → electromagnetic wave by → sound wave. The sound horizon is a fixed physical scale at the → last scattering surface. Cosmological models relate the value of sound horizon to the angle it subtends on the sky today. Same as acoustic horizon and sonic horizon. See also → CMB angular power spectrum. |
sound intensity dartanuyi-ye sedâ Fr.: intensité de son The average → sound power passing through a unit area perpendicular to the direction that the sound is traveling. It is usually expressed in watts per square meter. |
sound intensity level tarâz-e dartanuyi-ye sedâ Fr.: niveau de l'intensité de son The expression of sound intensity in decibel units. The sound intensity level (LI), in decibels, is computed as: LI = 10 log (I/I0), where I is the measured sound intensity and I0 is the reference intensity (1 x 10 -12 watt per square meter). |
sound power tavân-e sedâ Fr.: puissance de son The → sound energy emitted by a source per unit time, usually expressed in → watts. Sound power causes → sound pressure. |
sound power level tarâz-e tavân-e sedâ Fr.: niveau de la puissance de son The sound energy emitted by a sound source per unit time and expressed in → decibels. Sound power, in → watts, is converted to sound power level in decibels (L), by L = 10 log (W/W0), where W0 is the reference power (1 x 10 -12 watt). |
sound pressure fešâr-e sedâ Fr.: pression de son The periodic fluctuation above and below atmospheric pressure created by an oscillating body which provides the → sound power. Instantaneous sound pressure is the peak value of air pressure. |
sound quality cunâ-ye sedâ Fr.: qualité de son The number of → overtones present in a sound and their respective intensity. Like → loudness, it is a subjective quantity and cannot be measured with instruments. |
sound speed tondi-ye sedâ Fr.: vitesse du son The velocity of propagation of a → longitudinal wave in a medium under specified conditions. Also known as sonic speed, sonic velocity, acoustic velocity, sound velocity, velocity of sound, speed of sound. The speed of sound is a thermodynamic property that relates to the change in pressure and density of the medium and can be expressed as C = (dP/dρ)1/2, where C is the sound velocity, dP is the change in pressure, and dρ the change in density. It can also be expressed as C = (E/ρ)1/2, where E is the bulk modulus elasticity. This equation is valid for liquids, solids and gases. The sound travels faster through media with higher → elasticity and/or lower density. If a medium is → incompressible the speed of sound is infinite. For → ideal gases, a simple relationship exists between the sound speed and temperature: C = (γR T)1/2, where γ is the → specific heat ratio (CP/CV), and R is the → gas constant. We see that for ideal gases it the speed is independent of pressure. In air at 0°C it is 332 m/sec. The speed of sound in a gas of hydrogen is 1315 m/s. → Mach number. |
sound wave mowj-e sedâ (#) Fr.: onde sonore A → longitudinal wave which when striking the ear gives rise to the sensation of sound. Such waves can be propagated in solids, liquids, and gases. The material particles transmitting sound waves oscillate in the direction of propagation of the wave itself. There is a large range of frequencies within which longitudinal waves can stimulate the human ear and brain to the sensation of hearing. This range is from about 20 → Hz to about 20,000 Hz and is called the audible range. → ultrasound; → infrasound. |
sounding gomâné-zani Fr.: sondage, radiosondage 1) In geophysics, any penetration of the natural environment for
scientific observation. From Fr. sonder, → sonde. From gomâné, → sonde, + zani verbal noun of zadan "to do; to strike, beat; to play an instrument" (Mid.Pers. zatan, žatan; O.Pers./Av. jan-, gan- "to strike, hit, smite, kill" (jantar- "smiter"); cf. Skt. han- "to strike, beat" (hantar- "smiter, killer"); Gk. theinein "to strike;" L. fendere "to strike, push;" Gmc. *gundjo "war, battle;" PIE *gwhen- "to strike, kill"). |
sounding balloon bâlon-e gamâne-zani Fr.: ballon-sonde A small, free balloon sent into the upper atmosphere to measure, record, and transmit meteorological reports to a ground station. |
soundness dorvâyi Fr.: santé 1) The quality of being → sound. |
source xan Fr.: source General: Any thing or place from which something comes, arises, or is obtained. M.E., from O.Fr. sourse "a rising, beginning, fountainhead of a river or stream," from p.p. of sourdre "to rise, spring up," from L. surgere "to rise," → surge. Xan "source," variant xân (Gilaki xoni, Tabari xoni,Laki kyani, Tâleši xâni, xoni,); Mid.Pers. xân, xânig "source, spring," Av. xâ-, xan- "source, fountain, spring," xayana- "belonging to a spring;" cf. Khotanese khâhâ- "spring, fountain;" Skt. khâ'- "spring, source." |
source function karyâ-ye xan Fr.: fonction source For a radiating material, the ratio of emissivity to opacity. |
south daštar Fr.: Sud The cardinal point which is opposite to north. It is also the direction of the Sun at local noon (in the northern hemisphere). M.E. suth(e), south(e), from O.E. suth "southward, in the south;" cf. O.S., O.Fris. suth "southward, in the south," M.Du. suut), O.H.G. sund, perhaps related to base of *sunnon "sun," with sense of "the region of the sun." Note:
South is related to right since it is to the right when one faces the rising Sun.
This occurs in, for example, in Av., Skt., and O.Ir., as below. |
South Atlantic Anomaly (SAA) nâsâni-ye Atlas-e daštar Fr.: Anomalie Atlantique Sud A region of the Earth where the inner → Van Allen belt comes closest to the Earth's surface. It is due to the fact that the → geomagnetic field is offset from the center of the Earth. The region is centered near 25 degrees South 50 degrees West, close to the Atlantic coast of Brazil. The excess of trapped energetic particles in that region presents a problem for satellites in orbit around the Earth. |
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