0018933 Ad TE DeBiAyF BRA. CG.hi i 4. The amount of Cm242 loaded on KOA was 2,418 x 1014 disintegra- tions per minute as of the zero time of KOA. 5, The amount of Cm*** loaded on OAK was 5,674 x 10)4 disintegrations per minute as of the zero time of OAK. 6. All Sr89 and Sr?9 R values have been normalized to the LASL values by means of the KOA samples analyzed at both LASL and NRDL. 7. All x?! R values have been normalized to the NRDL values by means of the KOA samples analyzed at both LASL and NRDL. 8. The term "probe velocity" refers to the pumping speed in the gas- particle coincident sampler, Samples collected at 2 low probe velocity are very likely non-representative of the cloud. 9. On KOA the Massive samples were collected on the 60,000 foot height line; the Wilson Special sample wes from the general fallout, 10. The fine 4nd coarse fractions for the KQA and OAK size-separated samples were separated at a nominal fall rate of 1 cm/sec. 1 7 te Nominal fall rates for the WALNUT fractions were: fine fraction, less than 0,1 cm./sec.; medium fraction, 0.1 - 1,0 cm,/sec.; coarse fraction, greater than 1 cm. /sec. 11, The sampling altitudes given for Aircraft 978 on WALNUT end 981 on OAK are thought to be too high, but mere reliable figures are not available.