-6The Bectar teet (May 14, 1953) vas used as the date of origin except where othervise iadicated, but earlier shots alse contributed redicactivity to the samples studied. Especially the Bikini (March 1, 1958) shot con‘ributed greatly to seme of the seaples. Resid) long-lived products from eariier ietanetienes peior to 195% rendered the curves leas steep than they would have been as @ result of the 1954 series sisme. The treads of activity as releted to time are of two kinds, the physicel decay of individual samples, and the rate of chaage im activity of ea certain type of sample et a certain locality. fe distinguish it from ohysical decey. the latter tread will be Preferred to tn this report as decline. Results are shown es grephs of the relationship of 1 ithm of rediocactivity to logarithm of time of collection detonation. The date of origin used may deviate somewhat from detonation day or the true origin without markedly effecting linearity of the plot over the period of study. Phe slope is changed according to the date of origin selected, but if the same origin is used for both decay and decline, the two may be compared. Hunter and Ballou (1951) show on logarithmic plot the theoretical decay of mixed slow-neutroninitiated fission products of J-235 over a period from 1 to 1000 days as a slightly curving line vith a predoat- nantly below) downward curvature (concave and ®@® generel slope varying from -1.0 to -1.7, averaging -1.2 (Pig. 2). A similar presentation of the trends of radioactivity observed in the present study facilitates comparison with this curve and within the study itself. In log-log graphs it will be conwentent to speak of slopes or rates of decline and decay as becoming more or less steep vith the pessage of time, and | ap ie aren tome a a when the terms steepening or leveling are applied to the trends, the log-log relationship is implied. A single Pig. 2. Mixed fission product decay, gross rithmically gives a straight line, and Ballou). half life when plotted semiloga- while on the same plot a aixture of half lives results in a line of increasing steepness. beta. (After Hunter In the declines shown as streight lines on log-log plots possible fluctuations of a cyclic nature attributable to season or other variables are ignored.

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