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Occupational Intakes of Radionuclides Part 1 - ICRP

Occupational Intakes of Radionuclides Part 1 - ICRP

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DRAFT REPORT FOR CONSULTATION<br />

2376 Table 6 Central values <strong>of</strong> dissolution parameters for Type F, M, and S material from a review<br />

<strong>of</strong> experimental data a<br />

2377<br />

Type F(fast) M (moderate) S (slow)<br />

Fraction dissolved rapidly<br />

Dissolution rates:<br />

fr 0.95 (0.84) [1.4] 0.20 (0.18) [4] 0.007 (0.003) [9]<br />

Rapid (d-1) sr 12 (9) [8] 1.7 (1.5) [9] 2.0 (3.8) [14]<br />

Slow (d-1) ss 0.02 (0.02) [8] 0.003 (0.003) [4] 0.00018 (0.00008) [9]<br />

2378<br />

2379<br />

a<br />

Median value, with geometric mean in parentheses, and geometric standard deviation in<br />

2380<br />

2381<br />

brackets.<br />

2382 (149) Updated default values, given in Table 7, were based mainly on the following<br />

2383 considerations, but also take account <strong>of</strong> the large uncertainties in the central values<br />

2384<br />

2385<br />

and the need for simple rounded numbers.<br />

2386 Rapid fraction fr:<br />

2387 (150) For Type F, the median value (0.95) is close to the current default value <strong>of</strong><br />

2388 1.0. For simplicity in implementation it is preferable not to change to two-phase<br />

2389 dissolution. The default value remains 1.0.<br />

2390 For Type M, the median value is higher (0.20) than the current default (0.1). The<br />

2391 updated default value is taken to be 0.2.<br />

2392 For Type S, the median value is higher (0.007) than the current default (0.001).<br />

2393<br />

2394<br />

The updated default value is rounded to 0.01.<br />

2395 Rapid dissolution rate, sr:<br />

2396 (151) Type F: the median <strong>of</strong> values <strong>of</strong> sr estimated from experimental data for<br />

materials that would be assigned to Type F, is 12 d –1 2397<br />

(Table 5), (much lower than the<br />

original HRTM default value <strong>of</strong> 100 d –1 2398<br />

). However, this outcome is heavily<br />

2399 influenced by results for a few elements: about half <strong>of</strong> the results are from only four<br />

2400 elements. To include information from a wider range <strong>of</strong> elements in choosing the<br />

2401 default value, consideration was also given to the element-specific values <strong>of</strong> sr for<br />

2402 soluble (Type F) forms <strong>of</strong> the element, which were assessed where suitable<br />

2403 experimental information was available (see above). There are element-specific<br />

2404 values for several elements for which no material-specific values were assessed.<br />

2405 Hence the distribution <strong>of</strong> element-specific values covers a wider range <strong>of</strong> elements,<br />

2406 and in it each element makes the same contribution (one entry): its median value is 50<br />

d –1 2407 . Taking both medians into account, the updated default value <strong>of</strong> sr for Type F is<br />

taken to be 30 d –1 2408<br />

.<br />

2409 (152) Types M and Type S: The medians <strong>of</strong> estimated values <strong>of</strong> sr for materials that<br />

would be assigned to Types M and S, are 1.7 d –1 , and 2 d –1 2410<br />

, respectively (Table 5),<br />

(very much lower than the original HRTM default <strong>of</strong> 100 d –1 2411<br />

). As for Type F, the<br />

2412 distributions are heavily influenced by results for a few elements. For Type F,<br />

2413 consideration <strong>of</strong> element-specific values <strong>of</strong> sr involved a wider range <strong>of</strong> elements, and<br />

2414 led to the choice <strong>of</strong> a somewhat higher value than the material-specific values.<br />

2415 However, whereas for Type F materials the rapid dissolution rate, sr, represents<br />

2416 overall absorption, and is assumed to be element-specific, for Type M and S materials<br />

2417<br />

sr is more likely to be determined by dissolution <strong>of</strong> the particle matrix, and so less<br />

68

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