Fr.: effet de microlentille
A type of → gravitational lens, where the foreground → lensing object is of low mass. Microlensing is used in the search for → dark matter inthe → Milky Way galaxy and its nearest neighbours, as well as for → extrasolar planets.
Fr.: dégénérescence des paramètres de l'effet de microlentille
Determining the three various parameters of a microlensing event (the lens-source relative parallax and proper motion, and the mass of the lens) from only one physical parameter (the event time scale). Currently the microlensing degeneracy affects the vast majority of events and makes any individual event impossible to interpret with certainty.
A small grain sized meteorite which can only be positively identified under the microscope.
1) A screw thread device used to make accurate physical linear measurements.
A unit of length in the metric system equal to one millionth of a meter (10-6 m); symbol μ. Also called micrometer.
Coined 1880 in Fr. from Gk. mikron, neutral of mikros "small."
Any organism too small to be seen by the naked eye, e.g. bacteria, viruses, and protozoa.
Controlling unit of a microcomputer; laid out on a tiny silicon chip and containing the logical elements for handling data, performing calculations, carrying out stored instructions, etc.
A → binary system where an ordinary star orbits around a → neutron star or a → stellar-mass black hole that accretes the outer layers of the star's atmosphere. The accreted material falling on the → compact object warms up drastically and emits huge amounts of energy as → X-rays. The → accretion disk that emits this radiation also produces → relativistic jets of → plasma along the rotation axis of the compact object. The jets of material exhibit superluminal motion and resemble those emitted from → quasars, but on scales millions of times smaller. The first microquasar, 1E1740.7-2942, was discovered by F. Mirabel et al. 1992, Nature, 358, 215.
rizbin (#), mikroskop (#)
A magnifying optical instrument for inspecting objects too small to be seen or too small to be seen distinctly and in detail by the unaided eye.
From Mod.L. microscopium "an instrument for viewing what is small," from Gk. → micro- + -skopion "means of viewing," from skopein "look at."
Rizbin, from riz→ micro- + bin "to see; seer" (present stem of didan; Mid.Pers. wyn-; O.Pers. vain- "to see;" Av. vaēn- "to see;" Skt. veda "I know;" Gk. oida "I know," idein "to see;" L. videre "to see;" PIE base *weid- "to know, to see").
Fr.: état microscopique
Same as → microstate.
The Microscope. A minor constellation in autumn southern sky lying just south of → Capricornus at 21h right ascension, 37° south declination. The constellation contains only 4th magnitude or fainter stars. Abbreviation: Mic; genitive: Microscopii.
Microscopium was named by Abbé Nicolas Louis de Lacaille (1713-1762); → microscope.
Statistical physics: For a system made up of a large number of components, a state of the system which is specified by describing the current dynamical variables of each constituting component. For example, for a gas system composed of a large number of molecules, the microstate is defined by the set of quantities which defines the state of each molecule in the system (position, velocity, vibration, etc.). In practice, it is impossible to know perfectly the microstate of a system. The aim of → statistical physics is to relate the macroscopic (average ) observables (→ pressure, → temperature, → internal energy) to the microstate of the system. Also called → microscopic state. See also → macrostate and → multiplicity.
The → turbulence phenomenon involving relatively smaller physical volumes compared to → macroturbulence. In stellar atmospheres, it is a bulk gas motion with a characteristic size less than the local photon → mean free path. Microturbulence is one of the most significant mechanisms that can cause → line broadening in the stellar spectrum. The presence of microturbulence de-saturates strong lines and increases their → equivalent widths. Microturbulence in → hot stars brings about gas motions with velocities 0-20 km s-1. A physical connection may exist between microturbulence in hot star atmospheres and a subsurface → iron convection zone. Microturbulence may also be at the origin of → wind clumping in hot stars.
Electromagnetic radiation having wavelengths in the 1 to 300 mm range.
microwave background radiation
tâbeš-e paszamine-ye rizmowj
Fr.: rayonnement micro-onde du fond cosmique
Thermal radiation with a temperature of 2.73 K that is apparently uniformly distributed in the Universe. It is believed to be a redshifted remnant of the hot radiation that was in thermal equilibrium with matter during the first hundred thousand years after the Big Bang. Same as → cosmic microwave background (CMB) radiation.
tâbeš-e rizmowj (#)
Fr.: rayonnement micro-onde
Electromagnetic radiation carried by → microwaves.
miyâni-; nim-, nimé (#)
Fr.: mi-; moyen
A prefix which means being at or near the middle point of; being or occupying a middle place or position.
M.E., from O.E. midd-, cognate with O.H.G. mitti, O.N. mithr, Gothic midjis, O.Ir. mide, L. medius, Gk. mesos, Skt. mádhya-, Av. maidiia- "middle, the middle," Pers. miyân, as below.
Miyâni, from miyân "within, between, center," from
Mid.Pers. mayân "middle; among, between," Av. maidiia- "middle, the middle,"
maiδiiāna- "middle, center,"
maδəma- [adj.] "middle, being in the middle;
middling, of a middling size or quality," maiδim "in the midst of,"
cf. Skt. mádhya-
"middle, located in the middle;" O.H.G. mitti "located in the middle."
ruk-e miyân Atlasi
Fr.: dorsale médio-atlantique
An immense chain of underwater mountains that runs down the middle of the Atlantic Ocean. The MAR, approximately 500-1000 km wide, extends 16,000 km from Iceland to the Antarctic Circle. The MAR is so high that it actually rises above sea level in many places, forming volcanic islands. The Azores, Ascension, St. Helena, and Iceland all arise from this great Atlantic range. The chain results from the movement of the continental plates. As these plates slowly separate, they leave gaps in the → Earth's crust. This allows molten rock from beneath the Earth's crust to reach the surface and forms a ridge. The MAR is a part of the global → mid-ocean ridge system.