Fallout Radioactivity due to the Underground Nuclear Test of U.S.S.R. (Jan. 15, 1965)
スポンサーリンク
概要
- 論文の詳細を見る
Fallout radioactivity due to a leakage of the underground nuclear explosion test of U. S. S. R. (Jan. 15, 1965) was investigated. Abnormal increase of radioactive fallout was observed at first on the early morning of Jan. 20 at Nagaoka, Niigata Pref. In the fallout after Feb. 10, the influence by short lived nuclides could not be found. Gamma-ray spectrum of rain-snow sample of Jan. 20 coincided well with that of ^<140>Ba + ^<140>La, and the counting rate of gamma-rays decayed to a half in every 13 days through the beginning of March. Most part of gamma-activity was considered to be attributed to ^<140>Ba + ^<140>La in the transient equilibrium state. Radioactive product, ^<140>Ba, was used as a checking source and ^<140>Ba + ^<140>La content in each fallout sample collected after Jan. 20 was estimated. After subtraction ^<140>Ba + ^<140>La activity from the total activity in each sample, the residual decayed almost exponentially, with a half-life of 51-53 days, extending for a fairly long period of time. Maximum beta-ray energy was estimated to be L5-L6 MeV at the end of March when ^<140>Ba + ^<140>La was considered practically to have been extinct. Thus a chief component of the residual was thought to be ^<89>Sr. Cumulative deposition of ^<140>Ba + ^<140>La and other nuclides during the period from Jan. 19 to Feb. 9 was estimated to be about 110 mCi/km^2 and 270 mCi/km^2 respectively as values of Feb. 15.
- 日本放射線影響学会の論文
著者
-
小林 宇五郎
Faculty Of Engineering Niigata University
-
佐々木 秀穂
Faculty of Engineering, Niigata University
-
佐々木 秀穂
Faculty Of Engineering Niigata University