Plutonium Biokinetics in Human Body A. Luciani - Kit-Bibliothek - FZK
Plutonium Biokinetics in Human Body A. Luciani - Kit-Bibliothek - FZK
Plutonium Biokinetics in Human Body A. Luciani - Kit-Bibliothek - FZK
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elements the spectral distribution of background radiations shows a preponderance at low<br />
energies which is due to the degradation of γ photons by multiple Compton scatter<strong>in</strong>g <strong>in</strong> the<br />
shield. The <strong>in</strong>teraction of natural radiation with Lead shield reduces background below 250<br />
keV but adds lead fluorescence x rays of about 80 keV. To reduce this component further<br />
layers are used <strong>in</strong> decreas<strong>in</strong>g order of Z (e.g. Lead, Cadmium and Copper) to absorb the<br />
characteristic x rays emitted by the preced<strong>in</strong>g shield layer. Therefore a cover<strong>in</strong>g with<br />
Cadmium (Z=48) absorbs Lead x rays but add its own fluorescence x rays of about 22 keV.<br />
Thus, a f<strong>in</strong>al cover<strong>in</strong>g with Copper is used to absorb Cadmium fluorescence x rays. Copper<br />
fluorescence x rays of about 8 keV can be neglected because they fall below the energy<br />
region, even for low energy photon measurements [61].<br />
Contributions to the natural background from gas and dust are due to 222 Rn and 220 Rn,<br />
daughters of Ra 226 and Th 232 , together with their progenies that can diffuse <strong>in</strong> the air from the<br />
build<strong>in</strong>g materials and the ground. This source of radioactivity is normally limited with<br />
ventilation system filter<strong>in</strong>g the air <strong>in</strong>troduced <strong>in</strong> the shielded rooms where the detection<br />
system is located.<br />
Table 2.3.1 Activity concentration <strong>in</strong> build<strong>in</strong>g materials for few common natural<br />
radionuclides.<br />
Material Country Average activity concentration [Bqkg -1 ]<br />
48<br />
226 Ra<br />
232 Th<br />
Natural Orig<strong>in</strong><br />
granite Germany 100 80 1200<br />
granite Russia 110 170 1500<br />
tuff Italy 130 120 1500<br />
pumice stone Germany 130 130 1100<br />
concrete with alum Sweden 1500 70 850<br />
Industrial Orig<strong>in</strong><br />
phosphorite chalk Germany 600 < 5 110<br />
phosphate chalk Great Brita<strong>in</strong> 800 20 70<br />
calcium silicate Canada 2150 - -<br />
calcium silicate USA 1400 - -<br />
red mud brick Germany 280 230 330<br />
ash Germany 210 130 700<br />
aggregate of coal,<br />
ash and concrete<br />
2.3.1.2 Detectors<br />
40 K<br />
F<strong>in</strong>land 100 70 190<br />
Different k<strong>in</strong>ds of detectors are available for direct measurements of activity <strong>in</strong> human<br />
organs. For the particular case of detect<strong>in</strong>g low energy photon emitters two k<strong>in</strong>ds of detect<strong>in</strong>g