SESSION IV DISCUSSION INDIVIDUAL-PAPER DISCUSSION Discussions that took place following the presentation of individual papers are given in this section. These discussions preceded the scheduled general discussions for the session. HERDE: Dr. Martin, in your slide showing theoretical buildup of 131] in milk and in human thyroids, you also showed an extrapolated value for the ‘I in the environs, i.e., in the atmosphere and on the foliage being eaten by animals. That line went straight to the zero-time ordinate. I wonder if you should have taken into consideration the buildup of "I that is not present immediately, which results from decay of Sn, 4Sb, and *!Te in this case. Iam not sure that it would change the model or the formula, but certainly the slide could show the buildup of '3'] in fallout as well as in the thyroid and in the milk. MARTIN: No data were obtained to show the theoretical buildup of 1311 on plants. Instead, an arbitrary value for the concentration on plants at time zero was obtained by extrapolation from determinations made on D+5 and D+ 10. In this case time zero is approximately H + 12 hr, which would correspond roughly to the real levels of '°J buildup from fission-product precursors. HERDE: In 1955 I made thyroid measurements of native rabbits killed during the first evening after detonations and found four or five times as much ‘J as 4], I wondered whether you thought it worth- while to assay for these shorter-lived nuclides. The challenge is en- hanced by evidence of the presence also of '*I. I have hoped that someone would start where my 1955 work for UCLAleft off and extend it to demonstrate the significance of those shorter-lived isotopes of 895

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