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Radiation from belt

When travelling into space, astronauts are subjected to primary cosmic ray particles, the radiation from solar flares, and also the intense radiation present in the two radiation belts. Savun et al. (1973) have reported measurements in the radiation belts in 1971. Measurements inside a 0.7 g cm" shield indicate that the maximum absorbed dose rate crossing the inner belt was 0.22 Gy h and crossing the outer belt 0.054 Gy h" . [Pg.52]

The second loss is by radiation from the belt. The belt, which is of heavy construction for rigidity and flatness is a very significant heat sink. Some of this heat transfers to the panel where it is needed and some where it is not needed. The remainder is lost to the atmosphere by radiation during its idle return to the input end. This loss can be reduced by insulation but the problem of removing and restoring this insulation for inspection and maintenance access makes it impractical. A measurement on a double belt revealed a 20°F (11°C) loss in belt temperature during the return run. [Pg.560]

Astronauts would be subject to radiation from gedactic (0,05 rads per day) emd soleU (a few hundred rads per soleU fleU e) cosmic rays as well as leU ge fluxes of low energy radiation when passing through the Van Allen belts (about 0,3 rads per traverse). [Pg.1966]

Observations of Jupiter at high angular resolution with radio interferometers have been used to map the synchrotron radiation from Jupiter s radiation belts and to separate the thermal from the nonthermal synchrotron components. The nonthermal component is easily identifiable with a radio interferometer because it is greatly extended relative to the optical disk of Jupiter and is strongly linearly polarized. [Pg.264]

The ionosphere is part of the larger magnetosphere, a cavity in the stream of particles from the sun. The cavity is produced by the earth s magnetic field (56,57). The ionosphere and the Van AHen radiation belt He within the plasmasphere, which extends to a maximum distance of about 15,000 km above the earth s surface. [Pg.113]

Figure 4 shows the coordinate systems associated with the example shown in Figure 3 The horizontal axis is x, and the vertical direction is y. The conveyor belt is perpendicular to the y axis and moves in a direction into the page. The disk rotation angle, 9, is measured counter-clockwise from the y-axis. This example has 501 detectors in a straight hne, which is defined as the 5 direction. The straight hnes running from the source to the detectors represent rays of radiation detected at each detector location. There are 501 such rays that the figure represents with 21 hnes. (The detector geometry is often modified to place individual detectors along an arc of a circle centered on the X-ray source.)... Figure 4 shows the coordinate systems associated with the example shown in Figure 3 The horizontal axis is x, and the vertical direction is y. The conveyor belt is perpendicular to the y axis and moves in a direction into the page. The disk rotation angle, 9, is measured counter-clockwise from the y-axis. This example has 501 detectors in a straight hne, which is defined as the 5 direction. The straight hnes running from the source to the detectors represent rays of radiation detected at each detector location. There are 501 such rays that the figure represents with 21 hnes. (The detector geometry is often modified to place individual detectors along an arc of a circle centered on the X-ray source.)...
Thermo Nuclean developed the segmented gate system (SGS) to segregate radioactive material from contaminated soil. The SGS is a combined system of conveyors, radiation detectors, software algorithms, and computer controls. The SGS diverts contaminated soil onto a conveyor belt that deposits the soil in a container for disposal or fnrther processing. The developer claims that the system removes minimal amounts of clean soil with the radioactive particles, reducing the amount of material requiring disposal. The SGS is commercially available. [Pg.1057]

The advent of the space age, the testing of intercontinental ballistic missiles, the use of space probes, the existence of radiation belts in outer space, and the increasing utilization of military and civilian satellites have triggered further studies on the effects of nuclear radiation on all types of materials, including expls, propints, pyrots and related materials. Nuclear radiation effects studies range from steady-state to transient environments, from ground zero to upper atmosphere levels and from underground nuclear tests to simulation techniques in the laboratory which in turn cover all phases of vulnerability and survivability... [Pg.29]

The discovery of the Van Allen radiation belt required a recalculation of this effect. Goldhaber and Nieto [49] used a recent survey and set the most accurate upper limit. A similar technique is to look at the magnetic field as a function of the distance from the earth using satellite data. An experimental term enters for a finite mass that would be distinguishable from the normal dependence of a magnetic dipole. Gintsburg set an upper limit using this method. [Pg.605]

All crop production, except protected cropping (for example, glasshouse, plastic covered), is vulnerable to the weather. Measures to combat frost and drought are common to most kinds of crop production wind protection (by shelter belts and so on) is practised for only a few crops (e.g. top fruit). In general, apart from choice of location, little can be done about solar radiation, rainfall or temperature. Problems with weeds, pests and diseases are also common to all crops but the remedies available to organic producers are much more limited than for conventional farmers. [Pg.181]

Disk temperatures would have decreased rapidly with distance from the Sun as accretional energy release, optical depth, and solar radiation all declined. For example, some meteorite samples from main-belt asteroids contain hydrated silicates, formed by reactions between anhydrous rock and water ice. This implies that temperatures at 2-3 AU became low enough for ice to condense while the asteroids were forming. [Pg.462]

A second possibility is that CAIs formed elsewhere in the nebula and were subsequently transported to the asteroid belt. In the X-wind model, solids in the disk drifted inwards, emerged from a partially shielded environment and were melted by solar radiation (Shu et al., 1996). Some of these objects were entrained in the wind of material flowing away from the Sun, and millimeter-sized particles would... [Pg.463]


See other pages where Radiation from belt is mentioned: [Pg.736]    [Pg.7]    [Pg.605]    [Pg.221]    [Pg.33]    [Pg.914]    [Pg.549]    [Pg.457]    [Pg.101]    [Pg.383]    [Pg.403]    [Pg.405]    [Pg.298]    [Pg.255]    [Pg.261]    [Pg.4]    [Pg.84]    [Pg.830]    [Pg.479]    [Pg.600]    [Pg.539]    [Pg.56]    [Pg.65]    [Pg.476]    [Pg.338]    [Pg.328]    [Pg.384]    [Pg.507]    [Pg.683]    [Pg.485]   
See also in sourсe #XX -- [ Pg.560 ]




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