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Radioactivity atmospheric

The underlying physical and/or chemical mechanisms responsible for the differences observed between the radon progeny and the thoron progeny as related to different materials are not clearly understood. Finally, it should be pointed out that the main thrust in this paper was to determine differences in surface a-activity measured on different materials with the same geometrical characteristics exposed to identical radioactive atmospheres. The calculation of deposition velocities and attachment rates, although it follows from surface a-activity measurements, was not the intent of this paper. This topic is dealt with elsewhere (Bigu, 1985). [Pg.286]

Vilenskiy, V. D. (1970). The influence of natural radioactive atmospheric dust in determining the mean stay time of lead-210 in the troposphere. Izv. Acad. Sci. USSR, Atmos. Oceanic Phys. 6, 307-310. [Pg.711]

Plants can be contaminated by receiving radionuclides with nutrient solutions from water and soil. Also, soils can be contaminated by radioactive atmospheric precipitation and dust. In this way contamination is transferred to animals, since the contaminated plants are their forage. Animals can also be contaminated from the hydrosphere by drinking water. [Pg.4127]

In sodium hydroxide and hot sulfuric acid tests, K801 has shown better corrosion resistance than K701. K801 can also be used to advantage in radioactive atmospheres because the nickel binder has a much shorter half-life than the cobalt used as a binding element in most other carbides. [Pg.771]

Used (particularly He, Ar) to provide an inert atmosphere, e.g. for welding, and in electric light bulbs, valves and discharge tubes (particularly Ne). Liquid He is used in cryoscopy. The amounts of He and Ar formed in minerals by radioactive decay can be used to determine the age of the specimen. Xe and to a lesser extent Kr and Rn have a chemistry the other noble gases do not form chemical compounds. [Pg.281]

Classic examples are the spontaneous emission of light or spontaneous radioactive decay. In chemistry, an important class of monomolecular reactions is the predissociation of metastable (excited) species. An example is the fonnation of oxygen atoms in the upper atmosphere by predissociation of electronically excited O2 molecules [12, 13 and 14] ... [Pg.765]

The fusion of hydrogen into helium provides the energy of the hydrogen bomb. The helium content of the atmosphere is about 1 part in 200,000. While it is present in various radioactive minerals as a decay product, the bulk of the Free World s supply is obtained from wells in Texas, Oklahoma, and Kansas. The only known helium extraction plants, outside the United States, in 1984 were in Eastern Europe (Poland), the USSR, and a few in India. [Pg.6]

Del y for Dec y. Nuclear power plants generate radioactive xenon and krypton as products of the fission reactions. Although these products ate trapped inside the fuel elements, portions can leak out into the coolant (through fuel cladding defects) and can be released to the atmosphere with other gases through an air ejector at the main condenser. [Pg.285]

Several modes of waste management are available. The simplest is to dilute and disperse. This practice is adequate for the release of small amounts of radioactive material to the atmosphere or to a large body of water. Noble gases and slightly contaminated water from reactor operation are eligible for such treatment. A second technique is to hold the material for decay. This is appHcable to radionucHdes of short half-life such as the medical isotope technetium-9 9m = 6 h), the concentration of which becomes negligible in a week s holding period. The third and most common approach to waste... [Pg.228]

The fourth level of defense-in-depth is activated if all of the previous levels fail and radioactivity is released from the power-generating system. This level consists of containment systems and accident management processes that prevent the dissernination of radioactivity to the atmosphere even if it is released from the nuclear systems. The fifth level is the provision for emergency planning outside the plant boundary in the highly unlikely event that all of the first four levels of defense were to fad. [Pg.236]

Even higher organisms can be used for the production of labeled compounds. Plants, tobacco, or Canna indica for example, when grown in an exclusive atmosphere of radioactive carbon dioxide, [ 002], utilize the labeled precursor as the sole source of carbon for photosynthesis. After a suitable period of growth, almost every carbon atom in the plant is radioactive. Thus, plants can serve as an available source of C-labeled carbohydrates (9). [Pg.438]

Background Radiation. If the radiation from a radioactive source is measured, the spectmm also includes contributions from the radiations from the surrounding environment. This includes radiations from the radioactivity in the materials in and around the detector, including the stmcture of the building or nearby earth. There is also cosmic radiation that comes from space and interacts with the earth and atmosphere to produce radiations that may enter the detector, and thus is observed. [Pg.456]

Static eliminating devices that ionize the atmosphere around the device are available. Static eliminators are divided into two main groups silent (corona) discharge eliminators, such as inductive eliminators, or high voltage eliminators which initiate an impact ionization of the air by applying strong electrostatic fields, and radioactive eliminators that provide a multitude of ions from independent ion sources (9). [Pg.289]

Loss of radon in the ocean occurs typically through radioactive decay (producing four short-lived daughters before decaying to °Pb) or loss to the atmosphere at the air-sea interface. Loss of radon owing to turbulence or diffusion at the air-sea interface leads to a depletion of radon with respect to "Ra, allowing for studies on gas exchange at this interface. ... [Pg.49]

The chapter on Radioactive chemicals (Chapter 11) has been updated. Considerations of safety in design (Chapter 12) are presented separately from systems of work requirements, i.e. Operating procedures (Chapter 13). Tlie considerations for Marketing and transportation of hazardous chemicals are now addressed in two separate chapters (Chapters 14 and 15). Chemicals and the Environment are now also covered in two chapters (Chapters 16 and 17) to reflect the requirement that the impact of chemicals on the environment should be properly assessed, monitored and controlled. Although a substantial contribution to atmospheric pollution is made by emissions from road vehicles and other means of transport, and this is now strictly legislated for, this topic is outside the scope of this text. Chapter 18 provides useful conversion factors to help with the myriad of units used internationally. [Pg.617]

Containment Commercial reactors have a radioactivity which is the last barrier to an atmospheric release. [Pg.310]

Radioactivity reaches the public by ex-plant transport. If the completeness arguments presented in Section 3.2 are accepted, the only way the transport can happen is by fluid or gaseous transport. Published PSAs treat atmospheric transport as the only significant mechanism. [Pg.321]

Computer sensitivity studies show that hole size strongly affects the fraction of fission products released from the containment. The failure location determines mitigation due to release into another building in which condensation and particulate removal occur. The quantity released depends on the time of containment fails relative to reactor vessel failure. If containment integrity is maintained for several hours after core melt, then natural and engineered mechanisms (e.g., deposition, condensation, and filtration) can significantly reduce the quantity and radioactivity of the aerosols released to the atmosphere. [Pg.380]


See other pages where Radioactivity atmospheric is mentioned: [Pg.7]    [Pg.56]    [Pg.7]    [Pg.56]    [Pg.80]    [Pg.340]    [Pg.648]    [Pg.164]    [Pg.366]    [Pg.16]    [Pg.181]    [Pg.214]    [Pg.218]    [Pg.458]    [Pg.26]    [Pg.336]    [Pg.20]    [Pg.14]    [Pg.35]    [Pg.40]    [Pg.40]    [Pg.103]    [Pg.134]    [Pg.474]    [Pg.570]    [Pg.3]    [Pg.315]    [Pg.321]    [Pg.321]    [Pg.912]    [Pg.10]    [Pg.10]    [Pg.276]   
See also in sourсe #XX -- [ Pg.505 ]




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Atmosphere radioactivity

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