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47 . t 1 ’ ** If the curveof Fig. 3 is applied to the idealized mass contour ratioscalingfunctions, wherethe totalcratermass is mixed with EU the radlonuclides, the valueof the contourratio would decreaseas the scaledheightincreases and would increase as the scaleddepthIncreases maxiaarm). 'Itmaybe notedthatthe curveof Fig. 3 has no inflection at zeroctige depthsnd that it is very steep near zerochargedepth. Iherefore if Eq. 23 is validin:terms of the 9 givenin Fig. hei#rtor depthof burst. 6 (mg/sqf’t)/(r/hr at 1 k) and for the "U" Shot it was 85.
3 Variationin % 38 DEPTH)/(NUCLEAR YIELD IN us IN$ With NuclearScaledDepth . 47 . t 1 ’ ** If the curveof Fig. 3 is applied to the idealized mass contour ratioscalingfunctions, wherethe totalcratermass is mixed with EU the radlonuclides, the valueof the contourratio would decreaseas the scaledheightincreases and would increase as the scaleddepthIncreases maxiaarm). 'Itmaybe notedthatthe curveof Fig. 3 has no inflection at zeroctige depthsnd that it is very steep near zerochargedepth. Iherefore if Eq.
12 A generalincreasein the "R' valueswith distanceis shown-for sll the redionuclides in the Zuniand Tewaf&lwithrare gas precursors out. tion in the were fractionated. fallout(within ezqerimentalerror). of the "R" valuesof Table8 with distanceand Roughcorrelations 19 and 20 with particlesize (withaid of Eq. further, tbat . (30) Although the dataof Table8 are somewhatscattered withrespectto a withinabout continuous changein rj or 23, they all can be adjusted, the samedegreeof error,to E . 30 withthe semevalueof k, for a for x aud using l/d t inverseparticlediameter) givenshot.