CCSD3ZF0000100000001NJPL3IF0PDSX00000001 PDS_VERSION_ID = PDS3 RECORD_TYPE = STREAM OBJECT = INSTRUMENT INSTRUMENT_HOST_ID = "ULY" INSTRUMENT_ID = "GRB" OBJECT = INSTRUMENT_INFORMATION INSTRUMENT_NAME = "SOLAR X-RAY/COSMIC GAMMA-RAY BURST INSTRUMENT" INSTRUMENT_TYPE = "GAMMA-RAY BURST DETECTOR" INSTRUMENT_DESC = " Instrument Overview =================== (excerpted from [HURLEYETAL1992]) The GRB experiment was proposed in 1977 with a twin experiment aboard the NASA spacecraft. This approach had numerous advantages: a carefully intercalibrated pair of experiments at opposite ecliptic latitudes would survey the solar equatorial regions extensively, and stereoscopic observations would be relatively easy to compare with matched detectors. Triangulation baselines for cosmic gamma-ray bursts would be long, and the fact that two detectors in the network would be out of the ecliptic plane would provide a particularly favorable geometry for localization (non-coplanar detectors are required for arrival time analysis). With the unique mission opportunities, however, came unique design constraints. A radiation-hardened microprocessor was required to survive the passage through the Jovian radiation belts; few were available during the design phase of the GRB experiment. The limited performance of the unit chosen dictated simplified operating modes for the experiment. Electrical power aboard Ulysses is provided by a radioisotope thermoelectric generator (RTG) containing 10 kg of 238Pu (about 10^5 Ci). The GRB instrument would be the first cosmic gamma-ray burst detector to have to operate in this unfavorable background environment. To minimize the interference from the RTG, the sensors had to be mounted on the magnetometer boom, and were required to be essentially amagnetic. (More precisely, the remnant field could not exceed 2 x 10^-5 G at 25 cm.) Finally, the mass and power allocations for the GRB experiment were small compared to inner planet missions-2 kg and 2.6 W, respectively. Scientific Objectives ---------------------- The Ulysses solar X-ray/cosmic gamma-ray burst instrument (acronym: GRB) has three main scientific objectives. The first is the study and monitoring of solar flare X-ray emission. The second is the detection and localization of cosmic gamma-ray bursts. The third is the in-situ detection of Jovian auroral X-radiation. . . . For a review of experimental data on solar flare X-rays, see [DENNIS1985], [DENNIS1988]. Reviews of cosmic gamma-ray burst observations have appeared in [HURLEY1988], [HURLEY1989]. Jovian X-radiation was first detected by [METZGERETAL1983] using the Einstein satellite. X-rays in the 0.2-3 keV band were imaged with 4'' resolution, and provided evidence that the sources of X-radiation were the Jovian north and south auroral zones. The origin of the X-rays could have been either electron bremsstrahlung in the Jovian upper atmosphere, or characteristic line emission from atmospheric atoms excited by heavy ions precipitating from the Io torus. These two models make very different predictions about the hard X-ray flux in the Ulysses GRB energy range." END_OBJECT = INSTRUMENT_INFORMATION OBJECT = INSTRUMENT_REFERENCE_INFO REFERENCE_KEY_ID = "DENNIS1985" END_OBJECT = INSTRUMENT_REFERENCE_INFO OBJECT = INSTRUMENT_REFERENCE_INFO REFERENCE_KEY_ID = "DENNIS1988" END_OBJECT = INSTRUMENT_REFERENCE_INFO OBJECT = INSTRUMENT_REFERENCE_INFO REFERENCE_KEY_ID = "HURLEY1988" END_OBJECT = INSTRUMENT_REFERENCE_INFO OBJECT = INSTRUMENT_REFERENCE_INFO REFERENCE_KEY_ID = "HURLEY1989" END_OBJECT = INSTRUMENT_REFERENCE_INFO OBJECT = INSTRUMENT_REFERENCE_INFO REFERENCE_KEY_ID = "HURLEY1992" END_OBJECT = INSTRUMENT_REFERENCE_INFO OBJECT = INSTRUMENT_REFERENCE_INFO REFERENCE_KEY_ID = "HURLEYETAL1992" END_OBJECT = INSTRUMENT_REFERENCE_INFO OBJECT = INSTRUMENT_REFERENCE_INFO REFERENCE_KEY_ID = "METZGERETAL1983" END_OBJECT = INSTRUMENT_REFERENCE_INFO END_OBJECT = INSTRUMENT END