Estimating transfer parameters in the absence of data.
The calculation of transfer of radionuclides from the abiotic to the biotic environment is a well-established practice in radiological assessments. Concentration ratios provide simple means to estimate radionuclide activity in biota, from measured (or estimated) radionuclide concentrations in either a food source or an abiotic component such as soil or water. They are typically reported by element, and data compilations may include information such as soil type (e.g., sand, loam, clay) and species. The data may be for multiple species at a single location, single species at multiple locations, or represent compilations from multiple sources. Recently published guidance suggests that estimates are best made using data from the same ecosystem. This paper examines this recent guidance, in the context of using measured data from within a single ecosystem and comparing results to more generic values. Results suggest that generic values may be an adequate substitute for site-specific information. It illustrates how ionic potential may be used as an alternative to group chemical properties in estimating transfer factors. Lastly, limited evidence is found to support the concept of allometric scaling functions for elemental concentrations in plants.
Higley
Kathryn A
KA
Department of Nuclear Engineering and Radiation Health Physics, Oregon State University, Corvallis, OR 97331-5902, USA. kathryn.higley@oregonstate.edu
D017753:Ecosystem; D004777:Environment; D004784:Environmental Monitoring / Q000379:methods*; D006801:Humans; D009922:Oregon; D018517:Plant Roots / Q000528:radiation effects; D018547:Plant Stems / Q000528:radiation effects; D010944:Plants / Q000528:radiation effects; D011834:Radiation Monitoring / Q000379:methods*; D011868:Radioisotopes / Q000032:analysis*; D012015:Reference Standards; D012621:Seasons; D012990:Soil Pollutants, Radioactive / Q000032:analysis*; D013696:Temperature
D011868:Radioisotopes; D012990:Soil Pollutants, Radioactive