Romney E M, Lindberg R G, Kinnear J E, Wood R A
Health Phys. 1983 Sep;45(3):643-50. doi: 10.1097/00004032-198309000-00007.
Measurements of 90Sr and 137Cs in soil, vegetation and small mammals were made periodically at sites in southern Nevada and Utah that were contaminated by radioactive fallout from nuclear detonations at the Nevada Test Site (NTS) as well as from global sources. Results from a survey in 1980 indicate that both of these fallout-derived radionuclides have remained primarily within the top 5-cm layer of undisturbed soil in these arid land areas. Trace amounts of 90Sr and 137Cs were measured in soil and biota samples. The 90Sr concentrations in jackrabbit and rodent bone samples in 1980 varied within the range of 2-8 pCi/g ash (equivalent to 0.4-1.6 pCi/g wet bone or 5-20 pCi/g Ca). The 137Cs concentrations in muscle-tissue samples were generally less than 1.5 pCi/g ash (less than 0.045 pCi/g wet muscle). Comparisons of data obtained periodically since the early 1950s show that measured concentrations of 90Sr in bone tissues have been highly variable in trace amounts, and that the concentration attenuation appears to be following radioactive decay of this radionuclide.
在内华达州南部和犹他州的一些地点,定期对土壤、植被和小型哺乳动物中的锶 - 90(90Sr)和铯 - 137(137Cs)进行测量。这些地点受到内华达试验场(NTS)核爆炸产生的放射性沉降物以及全球来源的污染。1980年的一项调查结果表明,在这些干旱地区,这两种源自沉降物的放射性核素主要仍保留在未受干扰的土壤顶部5厘米土层内。在土壤和生物群样本中检测到痕量的90Sr和137Cs。1980年长耳大野兔和啮齿动物骨骼样本中的90Sr浓度在2 - 8皮居里/克灰分范围内变化(相当于0.4 - 1.6皮居里/克湿骨或5 - 20皮居里/克钙)。肌肉组织样本中的137Cs浓度一般低于1.5皮居里/克灰分(低于0.045皮居里/克湿肌肉)。自20世纪50年代初以来定期获得的数据比较表明,骨骼组织中测得的90Sr浓度在痕量水平上变化很大,而且浓度衰减似乎遵循这种放射性核素的放射性衰变规律。