permitted comparison, the data are shown separately, and other data appear in columns headed with question marks for mesh, usually either No. 6 of 74/inch or No. 20 of 173/inch. Tatle 9 shows for the paired tows the ratio of the activ- {ty per unit weight in coarse mesh to that in fine (No.6/No.20 on both a wet and ash weight basis. Table 8 Ratio of radiazetivity is tewe with eearse apok te fine apenh (06 920) om wet and con veight Beece. aie i954 SAS Ribe Bede ter «Wet vos 1.481 33) oS 6 .27)— 49 1.23 1% -% 9A 1o/la2 nA 68 Yers_ =k Dante frep fables 7 cad 8. Deep Wie Pascegp ek tem tem -T7? 22 2.39 21. -49 67 1.39 1.18 CF 3.62 3.67 -59 .7O) 1.61 .76 5 .6€0 6.81 2.99 420.7200 2,00 0% (1.96 2.00 1.78 3.95 .% 32 vee 8 1.12 1.16 1.77 12.0 6.8 6.22 1.85 B.S 12/% 78 9 11/%6 -33 63 1l/er & 62 1.2% 2.20 1.82 8.22 -% 1.57 2.13 1.68 83 88 1.85 1.97 1.37 1.69 7.50 6.96 -21) (21.02 11/27 12/3 42.60 w/AT -18 .90 8B 1.9 -3% 2.11 Between the northern localities of Belle Island and the Mike crater and the southern localities of Wide Passage and Leroy Island, there was a difference using the t test, significant at the 2% level on the ash basis. The reason is not apparent for this association of high counts with fine mesh nets at northern, western localities. and with coarse at the southern and Whereas, in 1952 (WT-616) significantly higher radioac- tivity occurred in fine mesh net hauls than in coarse, the present data show wide variation. On the wet basis the coarse mesh was higher in 18 pairs and the fine mesh in 25 pairs, while on the ash basis the figures were reversed, the coarse mesh was higher in 25 pairs and the fine mesh in 18 pairs. Thus, neither wet nor ash vasis showed a significant difference due to mesh size. te a a metelh le ee

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