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 />
(209) A model that describes the time-dependent distribution and excretion <strong>of</strong> a<br />
radionuclide in the body after it reaches the systemic circulation is referred to here as<br />
a systemic biokinetic model. In contrast to <strong>ICRP</strong>’s current and past biokinetic models<br />
describing the behaviour <strong>of</strong> radionuclides in the respiratory and alimentary tracts,<br />
<strong>ICRP</strong>’s systemic biokinetic models generally have been element-specific models with<br />
regard to model structure as well as parameter values. A generic model structure that<br />
depicts all potentially important systemic repositories and paths <strong>of</strong> transfer <strong>of</strong> all<br />
elements <strong>of</strong> interest in radiation protection would be too complex to be <strong>of</strong> much<br />
practical use. However, generic model structures have been used in previous <strong>ICRP</strong><br />
documents to describe the systemic biokinetics <strong>of</strong> small groups <strong>of</strong> elements, typically<br />
chemical families, known or expected to have qualitatively similar behaviour in the<br />
body. For example, Publication 20 (<strong>ICRP</strong>, 1973) introduced a generic model<br />
formulation for the alkaline earth elements calcium, strontium, barium, and radium,<br />
but provided element-specific values for most model parameters. In <strong>Part</strong>s 1-3 <strong>of</strong><br />
Publication 30 (<strong>ICRP</strong>, 1979, 1980, 1981) a model developed for plutonium, including<br />
parameter values as well as model structure, was applied to most actinide elements.<br />
The biokinetic models for several <strong>of</strong> these actinide elements were modified in <strong>Part</strong> 4<br />
<strong>of</strong> Publication 30 (<strong>ICRP</strong>, 1988), where the model structure for plutonium was used as<br />
a generic structure; a common set <strong>of</strong> parameter values was applied to plutonium,<br />
americium, and curium; and element-specific values were applied to selected<br />
parameters in the models for other elements. The use <strong>of</strong> generic systemic model<br />
structures was increased in <strong>ICRP</strong>’s reports on doses to members <strong>of</strong> the public from<br />
intake <strong>of</strong> radionuclides (<strong>ICRP</strong>, 1993, 1995a, 1995b) and is further expanded in the<br />
present document because it facilitates the development, description, and application<br />
<strong>of</strong> systemic biokinetic models.<br />
3.5.2 Formulation <strong>of</strong> systemic models in modern <strong>ICRP</strong> reports<br />
(210) Publication 30 (<strong>ICRP</strong>, 1979, 1980, 1981, 1988) provided a comprehensive set<br />
<strong>of</strong> systemic biokinetic models for radionuclides commonly encountered in<br />
occupational settings. The models were generally in the form <strong>of</strong> retention functions<br />
(e.g., sums <strong>of</strong> exponential terms) that may be interpreted as first-order compartmental<br />
models with one-directional flow. These models were designed mainly to estimate the<br />
cumulative activities <strong>of</strong> each radionuclide in its main repositories in the body. They<br />
do not depict realistic paths <strong>of</strong> movement <strong>of</strong> radionuclides in the body but describe<br />
only the initial distribution <strong>of</strong> elements after uptake to blood and the net biological<br />
half-times <strong>of</strong> elements in source organs. Activity absorbed from the gastrointestinal or<br />
respiratory tract or through wounds was assumed to enter a transfer compartment,<br />
from which it transfers to source organs with a specified half-time, typically 0.25 d or<br />
longer. Retention in a source organ was usually described in terms <strong>of</strong> 1 - 3 first-order<br />
retention components, with multiple biological half-times representing retention in<br />
multiple hypothetical compartments within a source organ. Feedback <strong>of</strong> activity from<br />
tissues to blood was not treated explicitly in Publication 30 with the exception <strong>of</strong> the<br />
model for iodine. It was generally assumed that activity leaving an organ moves<br />
directly to a collective excretion compartment, i.e., radioactive decay along actual<br />
routes <strong>of</strong> excretion is not assessed. Relatively short-lived radionuclides (half-lives up<br />
to 15 d) depositing in bone were generally assigned to bone surface and longer-lived<br />
88