PREDICTION OF RADIONUCLIDE DEPOSITION 735 = Wc v C q bh 4 ~ SF 9 ~ i L z < a U 7 0 O a < _ a = Te 4 _ S = C Lbputypeptttpett pty q a 4 ad — 10 F T Ise r 7 _ 4 | +) 3° 7 = - - = 10 Le g zZ ps Foe poe *} Z 1° r ; = j= Jee Tt tT it Tt tT 7 - { ao _— z Label Uv 4 «=O O z iT TCUS eee i pot ft 1/24 3/21 5/16 7/11 9/5 10/3112/26 2/20 4/16 6/11 [1963 i 1964 Fig. 8—Average airy and rain concentrations of gross beta radioactivity for four-week sampling periods between Dec. 27, 1962, and June 15, 1964, in the western Lake Erie area. ‘but the correlation coefficient was less than 0.2 and not significant at any reasonable level of confidence. The samples were divided into periods of fresh and older fallout, but still no significant correlation could be found between air concentration and rainfall. It was concluded from these observations that in the climate studied at least the air concentrations of radioactivity at a given location are less dependent on the amount of local rainfall than they are on some more widespread phenomena. However, this may not be true in other climates.!” CONCLUSIONS There appears to be a correlation between the radioactivity in surface air and the radioactivity in rain. The measurements reported here and those of others indicate that this relation can be described by an exponential model. However, the use of such a modelto predict depo- Sition will be limited until the behavior of certain terms in the model

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