= eis fers wa” > wee I, GEERaL se oa . . _ : - an manantattilley e . { —_~ ~ ’ oN » ey rahe, f - ( . : , “8 - re ake 8 bass Swe - . “Very little exnerinental data exists on the’ scavenging action of ralae on the atomic cloud. Hence it is possible to prepare a logical study undera a given set of assumptions to show that rain has the capability of scavenging. < out sufficient radioactivity from the atomiccloud to projuce a definite ~*.:) hazard to life. On tteother hand, if it’s assumed that the radioactivity‘2. scavenged out by rain is not confined toa relatively. smal] ‘surface area, “-* ©” then a stily could be prepared to show that the radioactive contamination’ Rie " produced by rain fs relatively unimportant. Since there is.‘very little. 3:7 quantitative data on the scavengingaction of rain, an attempt is wade in - . a this report to study the extent of the radivactive fall-out due. to soil debris. The particle size distribution of the soil debris uhich is sucked-“up: into the mushroom cloud is known; therefore, it is possible tocorrelate the . scaventing action vrotuced by sand with that of rain of a given intensity... 7 It may be possitle to determine the orderof ‘magnitude of the scavenging =~ an action of rain by such a method and it 1s just this order of magnitude of eette ne eee me the scavenzing action of rain that is réwuired in.order to evaluate some of. the presently available reports dealing with the efects,‘of rain on radiomactive fall—out from. theatonic cloud. wet wT & : Le: wa aco ee + + + ae It. SCAVENG DG ACTION OF PAIN AS REPORTED “DURING‘ATOMIC.‘TEST “OPERATIONS. "During both SANDSTONE (1) and TUMBLER/SNAPPER 2). Atonte Test‘Opsrations-” it was reported, that’ rainfall increased the_radioactive fall-out, ‘but this:La? increase in fall-out vas never greater, thin10 to158, of the. normal fall-outes=: Aire? TIT. - . ee t, SCAVENGING acrTow OF sor, DEBRIS piRIG TOMER‘ors‘or vs TEST OPERATIONS.* A, During TUMBIER/SYAPPER Test Operations: very Little fall-out of radio=~- activity occurred for air ¢rops, but the fall-out was significent during all 2 - four tower shots (290 ft. towers, 12 to 15 KT bombs). ,As a matter of fact, ..>5 anproxinstely 5 to 30% of the total Ag] hour activity. of the atomic bombs. ro 4 ye He+ detonated from towers vere deposited in an area of fron, 10 to 200 miles Prom= +: grount zero. In Figures 1, 2, 3 and 4 thisfall-out is“plotted_ in the form: of infinity dose lines. The data used in ‘plotting the infinity @ose lines.ae contained in the t/s Radiolopical Defense anual which is nowin the process* wk of being publisted. The inclosed tables ‘give more , detailed information with” reference to the last four tower shots ofT/S_ test‘operations and the radio-’ 4 ene tennenncain, mt ey _ active fall-out resulting from them. ‘There is_no doubt that the great increase = in radioactive fall-out for the tower shots eas convzred to theair. drops is < 8, due to the fact that a considerable amount of sand and” soil debris wes sucked'.+& up into the mushroom of the tower shots, but practically no mixing occurred” >" ‘for the air drops which were exploited from 1000 to 3000 ft. above terrain. Bt B. A stuiy of the inclosed figures and the tabulated ‘date, ‘shows that theres was a distinct area of maximum fall-out for each tover shot. The distance of 14% this maxima fall-out area vas pronortional 1to. the average> horizontalwind “speed:

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