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Re-emission of HTO into the atmosphere after HT/HTO conversion in the soil

Journal Article · · Fusion Technol.; (United States)
OSTI ID:6385406
After HT is converted to HTO by the soil, the HTO is reemitted back into the atmosphere. Since HTO is more radiotoxic by a factor of 10/sup 4/, this reemission is an important part of the radioecological pathway of HT. Laboratory studies show that the reemission rate from natural soil cores depends on the turnover in the gas space above the soil surface. Up to a wind velocity of about 4 m s/sup -1/, the portion of HTO reemitted hourly increases to about 18% of the initial amount of the reaction product. However, after the first hour, the observed reemission rate decreases quickly to about 3% h/sup -1/. Varying the humidity of an air stream fed into the reaction chamber had no influence on the reemission rate. For the Canadian release study, small soil samples were exposed to the plume and afterwards to the air. Then, at certain intervals following the release, the soil containers were sealed with gastight lids. The remnant HTO activity was then determined by azeotropic distillation. The reemission rate was about 3% h/sup -1/ during the day. During the night, no HTO loss was observed, possibly due to dew formation.
Research Organization:
Nuclear Research Centre (KFA), Radioagronomy, Juelich (DE)
OSTI ID:
6385406
Journal Information:
Fusion Technol.; (United States), Journal Name: Fusion Technol.; (United States) Vol. 14:2; ISSN FUSTE
Country of Publication:
United States
Language:
English