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Occupational Intakes of Radionuclides Part 1 - ICRP

Occupational Intakes of Radionuclides Part 1 - ICRP

Occupational Intakes of Radionuclides Part 1 - ICRP

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DRAFT REPORT FOR CONSULTATION<br />

database to different subgroups <strong>of</strong> the population and to times outside the period <strong>of</strong><br />

observation (for example, a parameter value found to depend on the rate <strong>of</strong> bone<br />

remodelling can be varied with age on the basis <strong>of</strong> age-specific data on bone<br />

remodelling rates); facilitates the extrapolation <strong>of</strong> biokinetic data from laboratory<br />

animals to man, in that it helps to focus interspecies comparisons on specific<br />

physiological processes and specific subsystems <strong>of</strong> the body for which extrapolation<br />

may be valid, even if whole-body extrapolations are not; facilitates the extrapolation<br />

<strong>of</strong> biokinetic data from an element to its chemical analogues, in that the degree <strong>of</strong><br />

physiological similarity <strong>of</strong> chemical analogues may vary from one physiological<br />

process to another (for example, the alkaline earth elements show similar rates <strong>of</strong><br />

transfer from blood to bone but much different rates <strong>of</strong> transfer to non-exchangeable<br />

sites in bone); links excretion with exchanges <strong>of</strong> activity among body tissues and<br />

fluids, so that the same model can be used for dose calculation and bioassay<br />

interpretation; allows modelling <strong>of</strong> the differential biokinetics <strong>of</strong> parent radionuclides<br />

and their radioactive progeny produced in the body; and allows the addition <strong>of</strong><br />

compartments and pathways to the model for purposes <strong>of</strong> extending the model to new<br />

applications, as was demonstrated in the <strong>ICRP</strong> documents on doses to the embryo and<br />

fetus (<strong>ICRP</strong>, 2001) and to the nursing infant (<strong>ICRP</strong>, 2004) from intakes <strong>of</strong><br />

radionuclides by the mother.<br />

(219) On the other hand, the level <strong>of</strong> physiological realism in the systemic biokinetic<br />

models currently used in radiation protection, including those recommended in the<br />

present report, should not be overstated. Even the most sophisticated models represent<br />

a compromise between biological realism and practical considerations regarding the<br />

quantity and quality <strong>of</strong> information available to determine parameter values. For<br />

example, the recycling models applied to bone-seeking radionuclides in the<br />

Publication 72 series all include s<strong>of</strong>t-tissue compartments representing fast,<br />

intermediate, and slow exchange with blood for all s<strong>of</strong>t tissues not explicitly<br />

identified in the models. These s<strong>of</strong>t tissue compartments typically are defined on a<br />

kinetic basis rather than a physiological basis, i.e., the compartment sizes and<br />

turnover rates are set for reasonable consistency with data on accumulation and loss<br />

<strong>of</strong> elements by s<strong>of</strong>t tissues. For some elements, these s<strong>of</strong>t tissue compartments appear<br />

to be associated with specific sites or processes, but the associations generally are not<br />

confirmed by available information. For example, biokinetic studies <strong>of</strong> calcium<br />

suggest, but do not establish, that the rapid-turnover pool in s<strong>of</strong>t tissues may<br />

correspond roughly to interstitial fluids plus some rapidly exchangeable cellular<br />

calcium (Heaney, 1964 Harrison et al, 1967;Hart and Spencer 1976); the intermediate<br />

turnover rate may stem from a composite <strong>of</strong> several pools with slower exchange rates,<br />

including mitochondrial calcium, cartilage calcium, and exchangeable dystrophic<br />

calcium (e.g., arterial plaque and calcified nodes) (Heaney, 1964; Borle, 1981); and<br />

long-term retention in s<strong>of</strong>t tissues may be associated with relatively nonexchangeable<br />

dystrophic calcium that gradually accumulates in the human body (Heaney, 1964).<br />

(220) For many elements it is not feasible to develop genuine physiological system<br />

models due to inadequate information on the processes that determine the systemic<br />

behaviour <strong>of</strong> these elements. Even for relatively well understood elements the model<br />

components are <strong>of</strong>ten intended only to represent the net result <strong>of</strong> multiple processes.<br />

For example, in the model for bone-surface-seeking radionuclides shown in Figure 18<br />

93

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