~~. c rt Soti UNITED STATES ATOMIC ENERGY COMMISSION Washington 25, D. C. Tel. ST 3-8000 Ext. 307 FOR RELEASE AT 9:30 A.M. (EST) FRIDAY, APRIL 26, 1957 Remarks Prepared by Dr. Willard F. Libby, Commissioner United States Atomic Energy Commission For Delivery before the Spring Meeting of The American Physical Society, Washington, D.C. April 26, 1957 RADICACTIVE FALLOUT I. INTRODUCTION The radioactivity preduced by the fission reaction changes its characteristics continuously and rapidly following the explosion of an atomic weapon and the conditions of . _. firing are of extreme importance in determining the rate of ~* which the radicactivity descends to earth. As a result there are in general three different kinds of radioactive fallout, the relative importance of which is determined by the nature of the weapon, principally its yield, and the conditions of firing. These three types are: First, the local fallout, which is insignificant unless the fireballtouches Or comes close to the zround, but which in case the fireball does touch the ground can amount to a major fraction, in scme instances as ™ th as &0 percent of the total debris. This pa be ra tyve of fallouz consists of radioactivity which is carried ERE &©§ wf fo. . a Ae aa“ i 6 - oe ow . &

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