Pt BEST AVAILABLE COPY Test results indicated that complete protection from an atomic explosion is afforded both personnel and equipment in a4 protected shelter installation of the type described. No functional damage to the shelter or to any of the installed quipment resulted from the blast. Increases of pressure and temperature within the shelter, due to the blast, were negligible. The antiblast closures functioned adequately in dampening the blast, in protecting the particulate filter-units from sandblast damage, and in preventing a hazardous pressure buildup within the structure. Protected-side pressures of not more than 12.6 lb/sq in.were measured in field instalZations located from 300 to 2,500 yd from ground zero. The indicated radiation level within the shelter closely approximated that which would be expected from direct radiation alone. WI-72 ted > - CLOUD PHENOMENA: STUDY OF GASEOUS AND PARTICULATE MATTER. Operation GREENHOUSE. Elmer H. Engquist and Thomas C. Goodale, October 1951. SECRET-RESTRICTED DATA Samrles gathered from atomic clouds indicated that the radiochemical composition of cloud particles yaries with their size. Specific radioactivity was found to vary considerably in the particle size range of 0.1 p to 27 pp. The ratio of inactive to active particles in a cloud - was found to vary between 100:1 and 1300:1, depending on the specific shot. The ratio also varied due to the method of collection by different aerosol sampling devices. The Secay rate of the cloud particulate matter varied with particle size; the decay exponent, n, ranging from 1.05 to 1.25 during the period 2 =o 40 days after detonation. The concentration of particulate beta activity in the cloud varied inversely with the size of the bomb. +a energy of the cloud contaminant ranged from 0.36 to 0.59 Mev; gamma energy ranged from 0.6 to 1.0 Mev. Electrostaticprecipitator samples indicated that 1.1 to 1.3 beta particles were emitted per gamma ray. Differing results were obtained when calculating the concentration of beta activity in samples collected by the electrostatic precipitator and by the cascade impactor, at H + 10 seconds after each of 3 shots. Electro-static-precipitator samples were calculated to range between 2.9 and 17.5 c/ee. Corresponding values for the impactor samples were between 0.75 end 4.0 uc/ec. gee! ee pul te

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