This flight was part of a balloon expedition to study cosmic rays in the vicinity of the equator during the International Quiet Sun Year (IQSY) organized and managed by the National Center for Atmospheric Research as a joint United States - India activity. The program was conducted in Hyderabad, India during the late winter and early spring of 1965.
The main instrument on this flight was a fast neutron detector aimed to measure 1-10 Mev recoil-proton and heavily ionizing events produced by neutrons in an organic scintillator. The detector itself is a 5 cm x 5 cm cylindrical volume of organic liquid phosphor, which is surrounded by a 6 mm minimum thickness of plastic scintillator which acts as an anticoincidence shield for charged particles. The composite detector is viewed by a single 5 cm photomultiplier. The set is shown in the far left scheme.
Events produced in the composite scintilator by radiation other than neutrons (like protons and electrons produced by background radiation and gamma rays) are rejected by the detector electronics on the basis of pulse shape. The pulses produced by scintillations of recoil-protons between 1 and 10 MeV are amplified, gated as neutron events and sorted in a seven-channel pulse height analyzer. The seven channels of pulse height information are binary coded and recorded on three tracks of a four track magnetic tape recorder. The fourth track contains a time signal as well as a record of all events produced in the scintillator with a light output greater than that of 1 MeV proton. Ambient pressure, the temperature of the gondola, and time are registered by a photobarograph which also acts as a backup system for the tape recorder, registering the counts in neutron channels 1-5 and 4-7 and in total events.
The instrumented rack (shown in the far right scheme) was designed so that the mass distributed in the balloon gondola would subtend a minimal solid angle at the scintillator. This was to prevent background neutrons produced by high energy radiation in the local material, from reaching the detector. An exterior container housed the photobarograph and the batteries for the heaters in the gondola. Such heaters were required only during night flights, since the insulation, made of 10 cm of polyurethane foam, and the reflectivity of the yellow fiberglas gondola were sufficient to maintain the inside temperature.
Also was part of the flight a X-RAY Counter developed by the University of California aimed to measure atmospheric gamma ray as a continuation of an already performed measurement campaign carried out in Minneapolis and in New Mexico, thus completing a three-point latitude survey. Also using the low gamma ray background near the equator the scientists examined the quiet sun for X-ray emission in the 10 to 100 kev region.
Balloon launched on: 3/7/1965 at 6:33 ist
Launch site: Osmania University Campus, Hyderabad, India
Balloon launched by: Raven Industries Inc.
Balloon manufacturer/size/composition: Zero Pressure Balloon Winzen 2.940.000 cuft (0.7 Mil. Stratofilm)
Balloon serial number: SF-199.78-070-NS-01 S/N 154
Flight identification number: NYU 109
End of flight (L for landing time, W for last contact, otherwise termination time): 3/7/1965 at 12:23 ist
Balloon flight duration (F: time at float only, otherwise total flight time in d:days / h:hours or m:minutes - ): F 4 h
Landing site: Payload impact at coordinates: 16º 48' N - 78º 45' E
Campaign: No Data IQSY-EQEX
Payload weight: 327 lbs
Overall weight: 750 lbs
Wind velocity during launch was 2 to 3 mph. At release, the balloon moved downwind slowly, allowing the launch crew to position the instrument load directly under the balloon. The instruments were lifted with little or no shock. The anchor line was fired off after the instruments were 30 ft above the ground. A pressure switch was employed to extend the beacon antenna when the balloon reached 5,000 ft.
The system ascended at an average rate of 862 ft/min to 50,000 ft and a rate of 848 ft/min to 124,600 ft for an overall average ascent rate of 853 ft/min. Duration at altitude was 3.5 hr. Descent time was 31 min with impact at 160 48' N, 780 45' E. Recovery was successful and the crew returned to Hyderabad the same afternoon. The balloon barotransmitter indicated an irregular floating altitude, fluctuating from 110,000 to 103,000 ft and back to 107,000 ft. At the time this irregularity was not understood; however, on examining the Raven photobarograph, it was in agreement with beacon data. On the other hand, New York University's photobarograph indicated a pressure level of 3.95 mb, which was nearer the theoretical ceiling of the balloon.
The balloon control instruments were contained in a moisture proof container fitted with a small venting orifice and water trap. The orifice apparently was blocked by some small object, most likely a small chip of styrofoam. To perclude the re-occurrence of this situation, all orifices were enlarged.
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