ap! CGuapter 2 X-RAY AMD THERMAL RAD LATION 2.1 THEGRY AND AxZALYSIS 2.1.1 Ineroducciaon X-ray measurements vere made on the Teak event and chenm! seasuresects were usde on both the Yeak and Orange events. The rocket-borne stations, TK-252 and TK-209, were plamed to be 30,000 feet from Teak air zero with Station TK-252 in a direction perpendicular to the Eedstone axis and Station IX-209 in a direction parallel to the Redstoue axis as shown in Fig. 1.1. As it turned out, at rero time Station TK-292 was at an altitude of 252,000 feet and at a radial distance of 63,600 feet frum air zero, Station TK-209 was at an altitnde of 205,700 feet and at a radial distance of 58,600 feet from air zero. The instrumere rocket of Station IK252 wes exposed side-on to the detonation as planned; however, the rocket statiou, TK-209, was oct exposed exactly nnse-ca as planed but tilted aboct 55 degrees from planned orientation with an uncertainty of about 5 degrees. Air zero of the Orange event was at an altitude of 140,965 feet. The *rocket-borne station, OR-125S, located at an altimde of 124,700 feet and at a@ radial distance of 42,100 feet, carried thermal detectors. The station vas in a direction perpendicular to the Redstone axis and the instrument rocket was exposed to the detonation with a side-on attitmde. The instruments are described in Section 2.2; however, designations will be given here to the X-ray detectors to clarify references to them. Each I-ray instrument consists of a pair of calorimeters each shielited by a different X-ray filter. A calorimeter and the thin filter are designated detector 4, and calorin- eter and thick filter are designated detector B. aze designated filters A and B, respectively. The filters of these detectors Subscripts going from 1 to 6 are used to indicate the angular position of the decectsr on the rocaet. In a sea level atoosphere, l0-cew X-rays are attemiated to one-balf istensity in about 1 meter, whereas in a 250,000-foot ataosphere a half-chickoess is , aie. od iow

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