aneurin, eRe fachinatest cadKas want. xchat waa sae Mek ces rn : Chapter 3 RESULTS moomwak gerresintematemin sen -roe we] fa cd Selenite etaeen ahh >athwf cc nearteeny \, "leeeopaetmtn wd aki 3-1 SHOT 1 3.1.1 Recovery PO: ; 3 \ Py Of the 32 gages used to instrument Shot 1, all but four were \gecovered. Station 123.01, the reef station nearest ground zero, was blownfgut of the coral. after; the shot. 3.1.2 Neither the gages nor the mounts.were found a o�� Bog Records fo& AlL yocbrds on Station 122.05, the station nearest ground zero, were discounted because excessive overpressure caused the pressure cap- sules to syst| All pressure capsules used at Station 122.06 were stressed appro reLy 75 percent above their rated range. This caused & permanent sct in the diaphragm, and the stylus did not return to the zero baseline. Fregsure capsules of the same range were calibrated to 100 percent abov whgir rated range in an attempt to evaluate records from this station. Fu.tit: obtained by this method may be in error as much as - 15 percent. . Ti)» records of pressure versus time from the remaining staticy: <r * +>-- for obtaining positive-phase durations, because of the: ' . .. . of hash present on the records. Excessive hash and high-f: | ‘ ‘ ¥eptions present on the records are thought to be due to turntable wobblé caused by poor bearings and lack of precision workmanship in the gagd@ assembly. 3.1.3 Presentation of Data ha “4 The station numbers, distanbés arrival times, duration of positive phase, and peak overpresshifes where obtained are listed in Table 43.1. All pressure readings ‘are ligted, although some readings are questionable. Brief explanations regarding the reliability of the reading, type of reading, and Punct ont of the gage have been includ- ed under the remarks column. presented in Figure 3.1. A curve off pressure versus distance is The points plotted ere.averages of values from records considered to be reliable. valuédfor arrival time versus distance are listed in Table 3.1, but pee not been plotted. These values may be less than those obtained py-glectronic measure- ments because of the delay in the fusible link"THitd iion system. plot has been attempted for the positive phase duratis No because of the scatter and need of a better method of determining the values. The values of the peak overpressure have been jr guced to 1 KT at sea level and plotted in Figure 4.1, along with reduced values of succeeding shots and a standard 1.6-KT free-air curve. 24

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