(contined) Comparing that to the data that were on the board yes showing the figures of maxisum and ainisue for fallout on the gumed paper, it seemsto ne like the range wes even with the muber of atations--40, 5D stations—it from thousands down to tens. You have the sans of balleon sampling which sight nover give you an great significance. KELLOGG: Aa I understood, the reason for these big peaks in tion at the cround was dus to the conjunction ef the « the proper kind of rain storm, which resulted in the va: concentration at the crousd. I would expect that there be changes in the atwaphers, es Jim pointed out there w be homogeneous mixing. oe . 4 not | mane bi nk Pena-tenot afndEnarny ‘hina tw 309