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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

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