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Alpha-particle emission

When bismuth-209 is bombarded with nickel-64, one neutron and a new isotope, X, is formed. The isotope then goes through a series of alpha particle emissions. [Pg.530]

No stable divalent salt is known. However, Am2+ has been detected in CaF2 matrix (0.1% Am) by paramagnetic resonance spectrum at low temperature. Its formation is attributed to the reduction of Am3+ by electrons in the lattice set free by the effects of alpha particle emission. [Pg.18]

Almost all radioactive nuclides that emit alpha particles are in the upper end of the periodic table, with atomic numbers greater than 82 (lead), but a few alpha-particle emitting nuclides are scattered through lower atomic numbers. The reason why alpha-particle emitters are limited to nuclides with larger mass numbers is that generally only in this region is alpha-particle emission energetically possible. Most radioactive nuclides with smaller mass numbers emit beta-particle radiation. [Pg.61]

The ion Es1 is stable. The isotopes of mass numbers 245. 252. 253 and 254 decay by alpha-particle emission that of mass number 250 by electron capture, those of mass numbers 24ft. 248. 249. and 251 by both of these processes, while those of mass numbers 255 and 256 emit electrons to form the corresponding fermium isotopes. [Pg.538]

Another isotope. Lr. hall-life about 45 seconds, was reported by the Soviet Union in 1965. It was produced by impact of oxygen atoms (l
    electron capture to form Fm See also Chemical Elements. [Pg.921]

    It can be seen that students can easily balance and complete nuclear equations if they are familiar with the symbols for nuclear particles and know the method of nuclear decay, such as alpha particle emission or electron capture. [Pg.342]

    Large isotopes often decay by alpha particle emission ... [Pg.99]

    There are three main types of radioactive decay alpha particle emission, beta particle emission, and the emission of gamma radiation. When an unstable isotope undergoes radioactive decay, it produces one or more different isotopes. We represent radioactive decay using a nuclear equation. Two rules for balancing nuclear equations are given below. [Pg.142]

    One example of alpha particle emission is the decay of radium. This decay is shown in the following equation ... [Pg.142]

    In another example of alpha particle emission, Berkelium-248 is formed by the decay of a certain radioisotope according to the balanced nuclear equation ... [Pg.143]

    Radon-222, 2g Rn, is known to decay by alpha particle emission. Write a balanced nuclear equation and name the element produced in this decay process. [Pg.143]

    Neodymium-144, a gNd, decays by alpha particle emission. Write the balanced nuclear equation for this nuclear decay. [Pg.143]

    The main source of the alpha particles is trace quantities of uranium and thorium in the silica filler. Because silica fillers that did not contain these radioactive elements were not available, other methods for preventing alpha particles from reaching the active DRAM cells were devised. These early methods consisted of cov-vering the active cells with either a silicone or polyimide chip coat or with Rapton tape. These methods added extra steps to the manufacturing process which were cumbersome and labor intensive and, if not done precisely, had a negative reliability impact. These processes were not widely used once "low alpha fillers" became commercially available in 1982/1983. Initially, these "low alpha fillers", which contain <1 ppb uranium, were only available from one or two natural sources. Now, however, there are additional natural and synthetic sources of silica, all of which contain <1 ppb of uranium and have an alpha particle emission rate of less than. 001 alpha particles/hr-cm. Figure 9 shows where the industry was in 1980 and where it stands today. An improvement by a factor of 30-50 has been achieved with "lower alpha" filler and compound manufacturing. [Pg.532]

    DRAHs HOLDING COMPOUND ALPHA PARTICLE EMISSION... [Pg.533]

    The deposition of polonium on metal wires gives rise to a useful a-source. Tips of metal wires having a length 10 mm and a diameter of 0.2 mm were utilized. They were made of Al, Ni, Pd, Pt or An. Each was immersed in 100 pi of a solution containing °Po (300 Bqml ) for 15 h at 27°. Alpha particle emission was measured using a liquid scintillation system. There was an observed diminution in the a-pulse spectra for all of the wires except Al. This was attributed to the mutual diffusion between the wire metal and °Po. The °Po deposited on the Al wire had a tendency to be eluted with the liquid scintillator. This was attributed to physical absorption on the porous metal oxide layer on the Al wire and °Po. The °Po deposited by the Al wire had a tendency to be eluted with the liquid scintillator. It was possible to prepare a °Po -Al wire as a useful a-source by heating at 120° for 30 minutes. [Pg.3936]

    In alpha particle emission, a nucleus simply emits two protons and two neutrons (bound together). An example is the element radon-222, which has an atomic number of 86 (86 protons) and an atomic mass of 222 (222 total protons and neutrons together). For this and other radioactive transitions, you can write an equation similar to a balanced chemical equation. Here it is ... [Pg.110]

    S. Alpha-particle emission (helium nucleus without the elections. If iti emission of the or particle leaves the nucleus in an excited enog) slate, the excc.ss energy is liberated in the form of a yrav. [Pg.456]

    Can ifiRn and °Rn decay by alpha particle emission Write balanced nuclear equations for these two decay processes, and calculate the changes in mass that would result. The masses of Rn and °Rn atoms are 222.01757 and 220.01140 u, respectively those of Po and Po are 218.0089 and 216.00192 u, respectively. [Pg.816]

    The long-lived isotope of radium, Ra, decays hy alpha particle emission to its daughter radon, Rn, with a half-life of 1622 years. The energy of the alpha particle is 4.79 MeV. Suppose 1.00 g of Ra, freed of all its radioactive progeny, were placed in a calorimeter that contained 10.0 g of water, initially at 25°C. Neglecting the heat capacity of the calorimeter and heat loss to the surroundings, calculate the temperature the water would reach after 1.00 hour. Take the specific heat of water to be 4.18 J g. ... [Pg.823]

    Radon derives its name from the element radium. The gas is radioactive and is formed by radioactive decay processes deep in the earth. Uranium-238 decays very slowly to radium-226, which further decays by alpha particle emission to radon-222 (see Chapter 17). The half-life of radon-222 is 3.825 days. Other shorter-lived isotopes are formed from the decay of thorium-232 and uranium-235. Every square mile of soil to a depth of 6 inches is estimated to contain about 1 g of radium, which releases radon in tiny amounts into the atmosphere. [Pg.200]

    The alkali metals are not found free in nature, because they are so easily oxidized. They are most economically produced by electrolysis of their molten salts. Sodium (2.6% abundance by mass) and potassium (2.4% abundance) are very common in the earth s crust. The other lA metals are quite rare. Francium consists only of short-lived radioactive isotopes formed by alpha-particle emission from actinium (Section 26-4). Both potassium and cesium also have natural radioisotopes. Potassium-40 is important in the potassium-argon radioactive decay method of dating ancient objects (Section 26-12). The properties of the alkali metals vary regularly as the group is descended (Table 23-1). [Pg.921]

    In the above equation, the first factor in square brackets on the RHS is the probability of finding the nucleus in the excited state Ex and spin Jr (with Jo being the ground state spin), while the second factor ra/% is the decay rate of the excited state with an alpha particle emission. Now since Ex = Er + Q, we have ... [Pg.246]

    Decay modes are a = alpha particle emission (B = negative beta emission p+ = positron emission EC = orbital electron capture IT = isomeric transition from upper to lower isomeric state n = neutron emission sf = spontaneous fission (B(B = double beta decay. Total disintegration energy in MeV units. [Pg.1796]


See other pages where Alpha-particle emission is mentioned: [Pg.333]    [Pg.530]    [Pg.19]    [Pg.348]    [Pg.602]    [Pg.144]    [Pg.95]    [Pg.610]    [Pg.287]    [Pg.84]    [Pg.46]    [Pg.104]    [Pg.672]    [Pg.13]    [Pg.354]    [Pg.813]    [Pg.816]    [Pg.114]    [Pg.938]   
See also in sourсe #XX -- [ Pg.364 ]




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