pail 4 pou) 19! 1 QUALITY OF FIT db ual (not olf data shown) a ’ (1) BEST, EXPONENTIAL (2) GOO, POWER (3) POOR, LOGARITHMIC (4) POOR, LINEAR yl I-129 ACTIVITY PER GRAM OF SURFACE SOIL, pCi g"! 102 fp pad oO” —— ioe 3 Oe * ===3 = io-* Z 0.5 e OCTOBER | Lt 200 1995) i - JULY 1956) i JULY #1 400 600 800 1000 TIME POST CETONATION, days ! 1957) : s«1200 Figure 3. Curve fit of archival soil results. 1.5 days was taken from Table 3 of Crocker's report (Cr65). Individual nuclide activities were calculated by Crocker's methods and the original input data used by him (Cr63). The values for the hypothetical ratio of nuclide activity rela- tive to total fission product activity are tabulated in Table 7, column E. 6. The Ratio of Nuclide Activityto Total Activity for Bikini Ash. Bikini ash was the name given by the Japanese for actual fallout from BRAVO (1355). Estimates of Bikini ash activity per unit mass of soil were calculated from results for activity per unit area given in Table 13 of this report. Table 13 was devised by normalizing Bikini ash measurements to external exposure-rate measurements. Using the nuclide composition of Bikini ash, a fallout decay expo- nent specific for BRAVO fallout was developed (see Section IID.1l.e) and was ~1.4. Values for individual nuclide and total activity were developed for the surfaces of Rongelap, Utirik and Sifo Islands for different points in time. Bikini ash activity per unit mass of soil estimates were tabulated in Table 7, colum C. The times are 1.5 days post detonation at Utirik and 0.5 days post detonation at Rongelap. To estimate specific activity from areal activity, approximately 65,000 g/mof soil were assumed to be present in the top 5 cm (2 in.) of soil. This value comes from a conversion factor of 6000 g/ ft? proposed by the survey team which visited Rongelap on March 8, 1954 (0C68). A bulk soil-humis density of 1.3 g/em3 in the top 5 cm (2 in.) of soil could be assumed to estimate a similar conversion factor. -15mo eu Ui u U "3 eee