T. Dewit et al., Uranium and uranium decay series radionuclide dynamics in bone of rats following chronic uranium ore dust inhalation, HEALTH PHYS, 81(5), 2001, pp. 502-513
Citations number
19
Categorie Soggetti
Environment/Ecology,"Public Health & Health Care Science
The accumulation and release of uranium and some uranium decay chain radion
uclides were measured in the bones of rats that had been chronically expose
d to inhaled uranium ore dust during the first half (approximately) of thei
r natural adult lifespan. Endochondral bone (femur, tibia, humerus, radius,
and ulna), membrane bone (skull roofing bones) and muscle of Sprague-Dawle
y rats (n = 55) that died at various times up to 65 weeks after the end of
chronic inhalation of uranium ore dust aerosol (4.2 h d(-1) for 65 wk) and
from age matched controls (n = 10), were analyzed for uranium, Th-230, Ra-2
26, Pb-210, and Po-210. Overall, during the period of dust inhalation, the
nuclides accumulated in the above order of decreasing concentration in dry
bone. However, the results demonstrate that there was some differential acc
umulation of uranium and uranium decay series radionuclides in muscle and t
wo bone types of rats during the chronic inhalation period. The data also s
how that the bone levels of some, but not all, radionuclides decreased sign
ificantly with time after inhalation ceased. Lung uranium concentration at
the time of death was a highly significant covariant for temporal changes i
n the levels of some radionuclides in both endochondral bone and membrane b
one, indicating that lung remained a major source of these isotopes for acc
umulation in these bone types after ore dust inhalation had ceased. For som
e isotopes, the two bone types behaved differently during the dust inhalati
on period, and differently again after the dust inhalation ceased. The rela
tive behavior of one bone type compared to the other for a particular isoto
pe during the dust inhalation period did not predict the relative behavior
after dust inhalation ceased. However, a faster accumulation of one bone ty
pe compared to the other for a particular isotope during the dust inhalatio
n period predicted a faster decrease after dust inhalation ended.