Radioactivity of Marine Organisms = 3 A ¥ _ if / ¥ / 100 F / oO # ; ‘ iN 4 ! i Fe] 3 © Page 153 x r i eo, } ‘. if / «| S \ \ \ i \ \, \ / ‘ = i 5 ao | aed @ fswor s. 4 \ \ i | \ x é H > ’ \ / ‘ ; *. ' “AL “4 7 ™s. “A er “ey ~ ~ } a ss ; , 2 ‘ o —_——— GULF OF SIAM) ____. \ ? : e ------ PALAU \ / | GUAM , s 1 an j -f a os ge i. bt shed. hewlett gh i a Te. RESTS R TAS ZAM THROM SK ORI Sr Tage HL OLY SORH SSeS oe sar LAReOUNgr sen oegosri ge — ts @ @ k ise 8 F & . € € . GF £ § F to 35 per cent fhe percentage error was estimat- Guam x& * Sample type Date collected (surgeonfish) muscle : B . unknown dates of origin. The best source of information about decay rates that are most like the Guam and Palau samples is Bonham (1959), who has determined the gross beta decay rates for 106 types of samples from the Eniwetok area for periods up to seven years. However, because of within-sample and between-sample variation, Number of Potassium Manganese specimens ~40 ~54 liver April 4, 1959 October 6, 1959 6 liver January 8, 1959 4 3 4+1 . ~ July 29, 1959 October 7, 1959 6 7 78+ 11 54% 13 liver November 3, 1959 6 91+ 2 1959 10 muscle September 29, 1959 10 3+ 1 adney kidney kidney September 29, 1958 April 14, 1959 September 28, 1959 7 1 3 (Tridacna clam) ney October 21, (goat fish) (Tridacna clam) ~ a Cobalt -57 Cobalt -60 Zinc -65 Zirconium Silver -95 -110m 1 28 + 17 liver liver (spiny lobster) Palau E - Nuclide+ identified by gamma spectrometry in single samples from Guam, Palaw and Gulf of Siam, 19581959. (Vaiues in terme of micremicrocuries per gram of wet weight and corrected to date of collection,) (spider snail) % ¢ & . Palau, and the Gulf with different, -1.5 for samples «.:ie:ted prior to the arrival of the Hardtack feliout and -1.4 for later samples. Area £€ A reliable correction factor for decay was difficult to derive either empirically fromother data or theoretically from consideration of the composition of fallout because the nuclides present in the samples were a mixture of unknown nuclides ed from decay curves that were arbitrarily selected after inspect.or of 19 decay curves for these data and also deca. .urves of Bonham (1959). Ona log-log plot the s:upes of the selected curves were Table 1. » 9 Figure 3. Gross beta activity of plankton from Guam, of aiam, 1958-1959, based on single observations. ing the sample. This interval averaged 247 days for the first collection, 161 days for collection II, and 38 to 78 days for the other four collect_ ions. Therefore, «wii reported values are low and by an amount that is estimated to range from 12 F 180 + 357% 207% ~ 8 5 3 ? 20+ &% 2+ 59+ 3 4+ ~ 231% 109% 25 ~ 3 2 2b ~ 3 19% 104 1 1 ~ ? 16+ 1 114 1 294+ 20 57+ 20% 50+ 63+ 40 1 1 7 : C ~ 2 1003 + 31 2340 + 30 275 + 19 ~ ~ ~ 12+ 2 5+ 1 85 + 20 137 + 12 ~ 5 30 2 22 + 1 ~ 30+ ~ 6 Gulf of Siam © gamma emitting nuclides other than Potassium-40 identified in the six samples examined which included: @uscle (Epinephelus), fish Ss. (Dictyota), and p ankton. 11 ver (Katsuwonus) , clam kidney (Tridacna), clam soft parts *° (Arca), alga ° * 1 95 per cert error in net count; E 95 7 1.96 (Ns/t + Nb/t, 17? ; from U. S. Public Health Service Radiological Beaith Handbook, 1960. 2 Approximate standard for ai teen sed upon decay scheme for silver-110m and efficiency factor for cesium-137. Without a in sample 50 fish r-110m Compton correction factors not calculated and therefore estimates of other radionuclides #150 are approximate. DOE ARCHIVES

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