+t ere sonra! pet y Lee come Nansen bottles, ‘ 4 rata j to 6 each cast. ] Speciakiy improvised plastic cottles, h in every cast. Bathythermograph at 12 positions. Plankton net cast, samples collected at two stations at 2 knots + onapRE and depths to about 500 feet, | | Vertical profile measurements of intensity to 2h0 feet at 3 stations. vee Eight hundred miles of continuous monitoring of surface layer intensity. A few intercomparisons were made at deck-level and bridge-level with Rad-Safe units. ° i ve PNDrE cpm Inter-station Measurements Extra surface water samples were taken at 15 points on the course without stopping. Preliminary Results Fig. 2.7-1 shows: Unprocessed field measurements of radiation intensity due to fall-out from Runt 2, Positions of hydrographic stations where deep water samples were Collected, and Positions where vertical profiles of intensity were measured directly. The broken line represents the intensity of filtered radiation, giving Telative intensityin terms of distance from the solid course line as a base. No correction has been applied for attenuation due to age, character of fall-out, nor for diffusion of surface water, and final instrumental calirations have not been utilized. —_ COPIED/DOE LANL RG 7 ey -TS7- . ~~ ‘ 4 * 3 #* —