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Uranium is a chemical element with the symbol U and atomic number 92. It is a silvery-grey metal in the actinide series of the periodic table. A uranium atom has 92 protons and 92 electrons, of which 6 are valence electrons. Uranium is weakly radioactive because all isotopes of uranium are unstable; the half-lives of its naturally occurring isotopes range between 159,200 years and 4.5 billion years. The most common isotopes in natural uranium are uranium-238 (which has 146 neutrons and accounts for over 99% of uranium on Earth) and uranium-235 (which has 143 neutrons). Uranium has the highest atomic weight of the primordially occurring elements. Its density is about 70% higher than that of lead, and slightly lower than that of gold or tungsten. It occurs naturally in low concentrations of a few parts per million in soil, rock and water, and is commercially extracted from uranium-bearing minerals such as uraninite.[3] In nature, uranium is found as uranium-238 (99.2739–99.2752%), uranium-235 (0.7198–0.7202%), and a very small amount of uranium-234 (0.0050–0.0059%).[4] Uranium decays slowly by emitting an alpha particle. The half-life of uranium-238 is about 4.47 billion years and that of uranium-235 is 704 million years,[5] making them useful in dating the age of the Earth. Many contemporary uses of uranium exploit its unique nuclear properties. Uranium-235 is the only naturally occurring fissile isotope, which makes it widely used in nuclear power plants and nuclear weapons. However, because of the tiny amounts found in nature, uranium needs to undergo enrichment so that enough uranium-235 is present. Uranium-238 is fissionable by fast neutrons, and is fertile, meaning it can be transmuted to fissile plutonium-239 in a nuclear reactor. Another fissile isotope, uranium-233, can be produced from natural thorium and is studied for future industrial use in nuclear technology.[citation needed] Uranium-238 has a small probability for spontaneous fission or even induced fission with fast neutrons; uranium-235 and to a lesser degree uranium-233 have a much higher fission cross-section for slow neutrons. In sufficient concentration, these isotopes maintain a sustained nuclear chain reaction. This generates the heat in nuclear power reactors, and produces the fissile material for nuclear weapons. Depleted uranium (238U) is used in kinetic energy penetrators and armor plating.[6] Uranium is used as a colorant in uranium glass, producing lemon yellow to green colors. Uranium glass fluoresces green in ultraviolet light. It was also used for tinting and shading in early photography. The 1789 discovery of uranium in the mineral pitchblende is credited to Martin Heinrich Klaproth, who named the new element after the recently discovered planet Uranus. Eugène-Melchior Péligot was the first person to isolate the metal and its radioactive properties were discovered in 1896 by Henri Becquerel. Research by Otto Hahn, Lise Meitner, Enrico Fermi and others, such as J. Robert Oppenheimer starting in 1934 led to its use as a fuel in the nuclear power industry and in Little Boy, the first nuclear weapon used in war. An ensuing arms race during the Cold War between the United States and the Soviet Union produced tens of thousands of nuclear weapons that used uranium metal and uranium-derived plutonium-239. The security of those weapons is closely monitored. Since around 2000, plutonium obtained by dismantling cold war era bombs is used as fuel for nuclear reactors. The development and deployment of these nuclear reactors continue on a global base as they are powerful sources of CO2-free energy.
Elven gymyk yw uraniom, niver 92 y'n Vosen Beriodek. Y furvell gymyk yw U. An hanow a dheu dhyworth an planet Ouran, henwys yn y dro dhyworth duw an ebron yn mythologieth grek. Rann veur a dommder pervedhek an Norvys a dheu dhyworth breynans radyoweythresek atomow uraniom. Nyns eus rann vewoniethel dhe uraniom, drefen y vos radyoweythresek. Chif moon uraniom yw pygvoon (uraninit, UO2, po pitchblende yn Sowsnek, dhyworth an Almaynek pech du, ha blende toller). Yn 1789 Martin Heinrich Klaproth, kymygydh Almaynek yn Berlin, a hwithras pygvoon, ha kavos polter, aswonnys ganso avel elven nowydh, henwys uraniom ganso (diskudhys veu uraniom an keth bledhen). Enyshes veu alkan uraniom rag an kynsa prys yn 1841 gans Eugène-Melchior Péligot yn Paris. Ny aswonnys o uraniom avel alkan peryllus bys dhe 1896 pan dhiskudhas Henri Becquerel dell wrug sampel uraniom kawsya komol war blat skeusennek. Ev a dhamcanas bos uraniom ow tewynna dewynnow anweladow. Jynn ebron americanek a dhroppyas an danbellen atomek gynsa war Hiroshima yn Nihon yn 1945. An danbellen a gomprehendyas uraniom-235, kemmys hag hevelep dhe 12,500 tonnas a TNT, ha'n tardh iskevresek a ladhas a-dro dhe 75,000 a dus. Chif askorroryon uraniom yw Ostrali, an Statys Unys, Kanada, Gabon, Repoblek Werinel Kongo, Afrika Dheghow, Russi ha China. Askorrans ollvysel yw a-dro dhe 40,000 tonnas an vledhen, ha devnydh an brassa rann yw dinythi tredan. Usys yw uraniom re beu yn dasoberoryon nuklerek, h.y. uraniom diskargys (depleted uranium) rag laster gorholyon ha jynnow ebron, dhe liwa priweyth ha gweder, hag yn arvwisk tanbellenigow. Pan wrello atom uraniom folsa, askorrys yw elvennow erel, yn arbennek strontiom-90. Y'n 1950ow ha 1960ow, provow arvow nuklerek war enep an tir a worra strontiom-90 hag iodin-131 y'n ayrgylgh. Y feu droklamm yn Windscale, Pow Sows, yn 1957, hag yn Chernobyl, Ukrayn, yn 1986. Nans yw a-dro dhe 2 bilvil bledhen, y feu kreunyans a uraniom y'n kerrygi yn Oklo, Gabon, ow talleth dasoberor nuklerek naturel. Poos atomek yw 238.03, y boynt teudhi yw 1132°C ha'y boynt bryjyon yw 3754°C. Y dhosedh yw 19kg an liter. Alkan arghansek, es y vortholya ha'y dhyghtya yw. Uraniom a gomprehend tri chif isotop, uraniom-238, 99.3% anedha (hanter-bewnans 4.5 bilvil bledhen), uraniom-235, 0.7% anedha (hanter-bewnans 700 milvil bledhen) hag uraniom-234, 0.005% (hanter-bewnans 245000 a vledhynnyow). Usys yw komparrivow isotopow uraniom ha plomm rag dedhya kerrygi.langbot langbot
Uranium is a chemical element with the symbol U and atomic number 92. It is a silvery-grey metal in the actinide series of the periodic table. A uranium atom has 92 protons and 92 electrons, of which 6 are valence electrons. Uranium is weakly radioactive because all isotopes of uranium are unstable; the half-lives of its naturally occurring isotopes range between 159,200 years and 4.5 billion years. The most common isotopes in natural uranium are uranium-238 (which has 146 neutrons and accounts for over 99% of uranium on Earth) and uranium-235 (which has 143 neutrons). Uranium has the highest atomic weight of the primordially occurring elements. Its density is about 70% higher than that of lead, and slightly lower than that of gold or tungsten. It occurs naturally in low concentrations of a few parts per million in soil, rock and water, and is commercially extracted from uranium-bearing minerals such as uraninite.[3] In nature, uranium is found as uranium-238 (99.2739–99.2752%), uranium-235 (0.7198–0.7202%), and a very small amount of uranium-234 (0.0050–0.0059%).[4] Uranium decays slowly by emitting an alpha particle. The half-life of uranium-238 is about 4.47 billion years and that of uranium-235 is 704 million years,[5] making them useful in dating the age of the Earth. Many contemporary uses of uranium exploit its unique nuclear properties. Uranium-235 is the only naturally occurring fissile isotope, which makes it widely used in nuclear power plants and nuclear weapons. However, because of the tiny amounts found in nature, uranium needs to undergo enrichment so that enough uranium-235 is present. Uranium-238 is fissionable by fast neutrons, and is fertile, meaning it can be transmuted to fissile plutonium-239 in a nuclear reactor. Another fissile isotope, uranium-233, can be produced from natural thorium and is studied for future industrial use in nuclear technology.[citation needed] Uranium-238 has a small probability for spontaneous fission or even induced fission with fast neutrons; uranium-235 and to a lesser degree uranium-233 have a much higher fission cross-section for slow neutrons. In sufficient concentration, these isotopes maintain a sustained nuclear chain reaction. This generates the heat in nuclear power reactors, and produces the fissile material for nuclear weapons. Depleted uranium (238U) is used in kinetic energy penetrators and armor plating.[6] Uranium is used as a colorant in uranium glass, producing lemon yellow to green colors. Uranium glass fluoresces green in ultraviolet light. It was also used for tinting and shading in early photography. The 1789 discovery of uranium in the mineral pitchblende is credited to Martin Heinrich Klaproth, who named the new element after the recently discovered planet Uranus. Eugène-Melchior Péligot was the first person to isolate the metal and its radioactive properties were discovered in 1896 by Henri Becquerel. Research by Otto Hahn, Lise Meitner, Enrico Fermi and others, such as J. Robert Oppenheimer starting in 1934 led to its use as a fuel in the nuclear power industry and in Little Boy, the first nuclear weapon used in war. An ensuing arms race during the Cold War between the United States and the Soviet Union produced tens of thousands of nuclear weapons that used uranium metal and uranium-derived plutonium-239. The security of those weapons is closely monitored. Since around 2000, plutonium obtained by dismantling Cold War-era bombs is used as fuel for nuclear reactors. The development and deployment of these nuclear reactors continue on a global base as they are powerful sources of CO2-free energy.
Elven gymyk yw uraniom, niver 92 y'n Vosen Beriodek. Y furvell gymyk yw U. An hanow a dheu dhyworth an planet Ouran, henwys yn y dro dhyworth duw an ebron yn mythologieth grek. Rann veur a dommder pervedhek an Norvys a dheu dhyworth breynans radyoweythresek atomow uraniom. Nyns eus rann vewoniethel dhe uraniom, drefen y vos radyoweythresek. Chif moon uraniom yw pygvoon (uraninit, UO2, po pitchblende yn Sowsnek, dhyworth an Almaynek pech du, ha blende toller). Yn 1789 Martin Heinrich Klaproth, kymygydh Almaynek yn Berlin, a hwithras pygvoon, ha kavos polter, aswonnys ganso avel elven nowydh, henwys uraniom ganso (diskudhys veu uraniom an keth bledhen). Enyshes veu alkan uraniom rag an kynsa prys yn 1841 gans Eugène-Melchior Péligot yn Paris. Ny aswonnys o uraniom avel alkan peryllus bys dhe 1896 pan dhiskudhas Henri Becquerel dell wrug sampel uraniom kawsya komol war blat skeusennek. Ev a dhamcanas bos uraniom ow tewynna dewynnow anweladow. Jynn ebron americanek a dhroppyas an danbellen atomek gynsa war Hiroshima yn Nihon yn 1945. An danbellen a gomprehendyas uraniom-235, kemmys hag hevelep dhe 12,500 tonnas a TNT, ha'n tardh iskevresek a ladhas a-dro dhe 75,000 a dus. Chif askorroryon uraniom yw Ostrali, an Statys Unys, Kanada, Gabon, Repoblek Werinel Kongo, Afrika Dheghow, Russi ha China. Askorrans ollvysel yw a-dro dhe 40,000 tonnas an vledhen, ha devnydh an brassa rann yw dinythi tredan. Usys yw uraniom re beu yn dasoberoryon nuklerek, h.y. uraniom diskargys (depleted uranium) rag laster gorholyon ha jynnow ebron, dhe liwa priweyth ha gweder, hag yn arvwisk tanbellenigow. Pan wrello atom uraniom folsa, askorrys yw elvennow erel, yn arbennek strontiom-90. Y'n 1950ow ha 1960ow, provow arvow nuklerek war enep an tir a worra strontiom-90 hag iodin-131 y'n ayrgylgh. Y feu droklamm yn Windscale, Pow Sows, yn 1957, hag yn Chernobyl, Ukrayn, yn 1986. Nans yw a-dro dhe 2 bilvil bledhen, y feu kreunyans a uraniom y'n kerrygi yn Oklo, Gabon, ow talleth dasoberor nuklerek naturel. Poos atomek yw 238.03, y boynt teudhi yw 1132°C ha'y boynt bryjyon yw 3754°C. Y dhosedh yw 19kg an liter. Alkan arghansek, es y vortholya ha'y dhyghtya yw. Uraniom a gomprehend tri chif isotop, uraniom-238, 99.3% anedha (hanter-bewnans 4.5 bilvil bledhen), uraniom-235, 0.7% anedha (hanter-bewnans 700 milvil bledhen) hag uraniom-234, 0.005% (hanter-bewnans 245000 a vledhynnyow). Usys yw komparrivow isotopow uraniom ha plomm rag dedhya kerrygi.langbot langbot
4 sinne gevind in 4 ms. Hulle kom uit baie bronne en word nie nagegaan nie.