FREQUENCY OF OCCURRENCE 0 2 40 260 0 2 40 260 0 2 440 RATIO OF R/HR AT 1 HR TO ML SEA WATER/SO FT 26 80 Fig. 3016 Distribution of the Ratio of the Radiation Field to the Surface Density of the Sea Water Component varied from 0.045 x 10°7 to 0.070 x 10°7, For samples 251.03 and 251.04 on Shot 1, using only the island survey data (as corrected to 1 hr by Project 2,58)fave a ratio of 0,045 x 10"7 to 0,064 x 107 and 0.043 x 10°7 to 0.058 x 10°’ while other ipland station samples gave ratios varying from 0.01 x 1077 to 1.0 x 107’ when similarly compared. Excepting for those noted in Table 3.21, a factor 0.053 x 10°7 was used to estimate the field reading from the total gamma count. If the assumption of complete mixing of the three components with the radioactive device components is valid and if the sampling techniques are sound so that the sample is a representation of the over-all fallout in the particuler area, then the ratio of the field radiation to the surface density of the tracer fallout components should be a constant for each shot. The comparisons as given in Table 3.21 show lange variations instead of constancy, Actual field readings were available only for Shot 1 island stations where the sample recovery was actually the most questionable, The extent of error in the 79