surface were four to twenty times the lowest values (48 counts per minute per liter of gross beta) found northeast of Bikini, where test contamination was virtually absent. Thus it appeared that the westward fringe of the drift had reached, in September, the vicinity of Guam, but at levels so low that they were significant only for the purposes of identification. Furthermore, the maximum value for water, regardless of place or depth of the sample, was 19,000 disinte~- grations per minute of total beta, and this single sample was taken from the surface at Station 2, southwest of Eniwetok toward Ujelang Atoll, cruise began. as the Levels of radioactivity diminished sharply thereafter, trailing off to the lower values, while the samplings down to 150 meters were variable in content and seemed, as the report later stated, fall into regional patterns. surveys had discovered, to As all of the earlier the Marsh also found that plankton were the most sensitive indicators of the presence of radioactivity. beta activity in plankton, The highest value of total 21,000 disintegrations per minute per gram, was found in samples taken eighty miles north of Eniwetok, and the lowest, 27, near Guam. The average of ratios of plankton activity to sea water activity was 2,500 to 1, much lower than the ratio of 7,000 to 1 reported by the Walton three months earlier. The Marsh survey between September 1 and 20, 1956, completed the second phase of a two-stage study of a radiation-tagged water mass. It had found radioactivity

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