Atmospheric Dispersion and Deposition of 131I Released from the Hanford Site

汉福德遗址 沉积(地质) 环境科学 羽流 大气扩散模型 色散(光学) 降水 气象学 大气科学 水文学(农业) 化学 空气污染 放射性废物 物理 核物理学 地质学 有机化学 古生物学 岩土工程 光学 沉积物
作者
J.V. Ramsdell,C.A. Simonen,K.W. Burk,Steven A. Stage
出处
期刊:Health Physics [Lippincott Williams & Wilkins]
卷期号:71 (4): 568-577 被引量:5
标识
DOI:10.1097/00004032-199610000-00014
摘要

Approximately 2.6 x 10(4) TBq (700,000 Ci) of 131I were released to the air from reactor fuel processing plants on the Hanford Site in southcentral Washington State from December 1944 through December 1949. The Hanford Environmental Dose Reconstruction Project developed a suite of codes to estimate the doses that might have resulted from these releases. The Regional Atmospheric Transport Code for Hanford Emission Tracking (RATCHET) computer code is part of this suite. The RATCHET code implements a Lagrangian-trajectory, Gaussian-puff dispersion model that uses hourly meteorological and release rate data to estimate daily time-integrated air concentrations and surface contamination for use in dose estimates. In this model, iodine is treated as a mixture of three species (inorganic gases, organic gases, and particles). Model deposition parameters are functions of the mixture and meteorological conditions. A resistance model is used to calculate dry deposition velocities. Equilibrium between concentrations in the precipitation and the air near the ground is assumed in calculating wet deposition of gases, and irreversible washout of the particles is assumed. RATCHET explicitly treats the uncertainties in model parameters and meteorological conditions. Uncertainties in 131I release rates and partitioning among the nominal species are treated by varying model input. The results of 100 model runs for December 1944 through December 1949 indicate that monthly average air concentrations and deposition have uncertainties ranging from a factor of two near the center of the time-integrated plume to more than an order of magnitude near the edge. These results indicate that approximately 10% of the 131I released to the atmosphere decayed during transit in the study area, approximately 56% was deposited within the study area, and the remaining 34% was transported out of the study area while still in the air.
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