Knowledge (XXG)

Explorer 20

Source ๐Ÿ“

584:(with two low-voltage, 0.5- and 3.2-kHz sinewave forms impressed upon it) provided a profile of voltage versus ion current. The change in slope of the voltage versus ion current profile, gives the energy distribution profile, which, for thermal ions, is a function of ion mass and satellite velocity. Thermal ion velocities broaden the mass peaks somewhat and thereby degrade mass resolution slightly, but this broadening effect was used to determine the ion temperature. Analysis of current variations resulting from the two sinewave forms on the sweep voltage, provided the required slope change data for analysis of the profiles. The probe was mounted at the positive end of the spin (Z) axis on a short tubular support. With the nominal spin axis, perpendicular to the orbit plane, this arrangement eliminated spin modulation of the observations. Although this experiment functioned properly, the occurrence of a large plasma sheath about the spacecraft, prevented acquisition of scientifically useful data. 1719: 559:
transmitter-receiver that recorded the time delay between a transmitted and a returned radio pulse. Six specific frequencies from 1.5 to 7.22-MHz were sampled in sequence once every 0.105-second. Several delay times were often observed for each frequency due to plasma resonances, birefringence of the ionosphere, nonvertical propagation, etc. Delay time was primarily a function of distance traversed by the signal, electron density along the signal path, and the mode of propagation. A total of 1450 hours of data was acquired. Most of these data were of adequate quality to prepare ionograms. Since only time is noted on each ionogram, satellite position and other related information must be obtained from world maps.
92: 633: 617:. Data were recorded for periods of 1/2 hour to over 4 hours per day depending upon available power. The experiments operated satisfactorily for about 16 months, despite problems with telemetry and interference. The ion probe was rendered useless due to large spacecraft plasma sheath that developed around the spacecraft, and efforts to compensate proved fruitless. 906: 874: 842: 787: 464:
Explorer 20 was a short cylinder capped at both ends by truncated cones. The satellite's primary experiment was a six-frequency ionospheric sounder: six sounding antennas (three dipoles) extended from the satellite equator, one pair of 18.28 m (60.0 ft) antennas forming the dipole used for
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The satellite's responses to command signals became undependable after 20 December 1965, and the satellite transmitter often spuriously turned on. Though equipped with a one-year automatic satellite turnoff, this device was disconnected just prior to launch. Explorer 20 did not respond to a turnoff
469:. An ion mass-spectrometer, mounted on a short boom, extended from the upper cone and measured ion concentrations and temperatures in the satellite's immediate vicinity. Explorer 20 also measured cosmic emissions using the noise signal from the sounder receivers. This experiment was provided by the 500:
of 864 km (537 mi), an inclination to the equator of 79.90ยฐ, and a period of 104.00 minutes. Upon reaching orbit, the antennas extended from the spacecraft, and tests of the primary and secondary experiments were completed within the first orbit. The satellite was spin stabilized at 1.53
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in the altitude range 300 km (190 mi) to 1,000 km (620 mi). The experiment was most useful for the study of irregularities in the electron density distribution and for the investigation of fine structure in the plasma resonances. The fixed-frequency ionosonde was a radio
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on Explorer 20 was a spherical retarding potential instrument from which ion mass spectra and ion temperatures could be determined. It consisted of a spherical inner electrode, 9 cm (3.5 in) in diameter, surrounded by a spherical, gridded (0.5-mm holes),
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concentration is at its highest. This data could then be compared and correlated with ionospheric data collected from the ground. In addition, Explorer 20 would measure electron distribution, ion density, and temperature, and to estimate cosmic noise.
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Explorer 20 was not equipped with a tape recorder, so data were only received when the satellite was in sight of ground telemetry stations, located to provide primary data coverage near 80ยฐ West plus areas near
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frequency range. The measurements were in rough agreement with previous observations of cosmic noise. The receiver calibration, however, was not sufficiently accurate to yield new scientific results.
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effects. The more massive ions passed through the grid to form an ion current dependent upon the voltage condition of the inner electrode. A slow-sweeping sawtooth potential from about -2 to +10
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low frequencies, the other two dipoles consisting of four 9.14 m (30.0 ft) antennas. The principal investigator for this experiment was the Central Radio Propagation Lab of the
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It was expected that information gathered from Explorer 20 would help in the study of long-range radio transmissions, particularly the cause of periodic radio black-outs.
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just after antenna extension, with the spin axis initially very close to the orbit plane. After a year in orbit, the spin had slowed to 0.45 rpm.
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covering, 10 cm (3.9 in) in diameter and 0.1-mm thick. A negative charge was maintained in the grid to remove
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booster's harness and subsequent pad requirements resulted in five months of delay. On 25 August 1964, at 13:43
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experiment utilized the noise signal from the sounder receiver to investigate cosmic noise in the 1.5- to 7.2
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Payloads are separated by bullets ( ยท ), launches by pipes ( | ). Crewed flights are indicated in
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Symbol indicates failure en route or before intended mission data returned
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Originally planned for launch in March 1964, electrical issues with the
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Explorer 20 was a 44.5 kg (98 lb) satellite designed by
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This article incorporates text from this source, which is in the
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1966: 1463: 581: 449: 421: 72: 1813: 922: 492:, Explorer 20 was launched into a near-perfect orbit, with an 428:. Its purpose was two-fold: long-term investigation of the 448:'s Airborne Instrument Laboratory under the management of 436:
investigation of ion concentrations and temperatures.
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Uncatalogued launch failures are listed in 1825: 934: 892:"Experiment: Spherical Ion-Mass Spectrometer" 8: 728: 726: 724: 722: 720: 718: 716: 21: 1832: 1818: 1810: 1730: 969: 941: 927: 919: 90: 20: 767: 765: 763: 761: 759: 757: 755: 860:"Experiment: Fixed-Frequency Ionosonde" 773:"Display: Explorer 20 (IE-A) 1964-051A" 657: 16:NASA satellite of the Explorer program 496:of 1,025 km (637 mi) and a 7: 804:McDowell, Jonathan (21 July 2021). 550:The purpose of the fixed-frequency 959:List of Explorers Program missions 738:Aviation Week and Space Technology 14: 1785:indicates active current missions 1717: 904: 872: 840: 785: 631: 27: 1797:indicate missions yet to launch 563:Spherical Ion-Mass Spectrometer 520:Spherical Ion-Mass Spectrometer 368:Spherical Ion-Mass Spectrometer 424:satellite launched as part of 102: 1: 734:"Explorer 20 Launch Succeeds" 1791:indicates cancelled missions 556:ionospheric electron density 471:University College of London 467:National Bureau of Standards 2534:Spacecraft launched in 1964 672:. Mark Wade. Archived from 454:Goddard Space Flight Center 330:1,025 km (637 mi) 2560: 828:"Experiment: Cosmic Noise" 2506: 1864: 1778: 1715: 956: 808:. Jonathan's Space Report 670:Encyclopedia Astronautica 546:Fixed-Frequency Ionosonde 517:Fixed-Frequency Ionosonde 372: 366:Fixed-Frequency Ionosonde 363: 354: 320:864 km (537 mi) 285: 281: 264: 260: 197: 193: 175:44.5 kg (98 lb) 126: 122: 54: 26: 894:. NASA. 28 October 2021 862:. NASA. 28 October 2021 830:. NASA. 28 October 2021 775:. NASA. 28 October 2021 210:25 August 1964, 13:43 44:Ionospheric Explorer-A 402:Ionosphere Explorer-A 295:Reference system 131:Spacecraft properties 33:Explorer 20 satellite 1848:Orbital launches in 147:Ionospheric Explorer 118:16 months (achieved) 63:Ionospheric research 2544:1964 in spaceflight 2468:Surveyor Mass Model 554:was to investigate 116:12 months (planned) 23: 1135:25 (Injun 4, IE-B) 639:Spaceflight portal 290:Orbital parameters 2539:Explorers Program 2521: 2520: 1807: 1806: 1774: 1773: 1713: 1712: 1220:42 (Uhuru, SAS-A) 950:Explorers Program 395: 394: 2551: 1909:Jupiter Nosecone 1853: 1852: 1851: 1834: 1827: 1820: 1811: 1790: 1784: 1731: 1721: 1672: 1665: 1658: 1646: 1624: 1595: 1591: 1587: 1555: 1548: 1541: 1534: 1527: 1520: 1437: 1430: 1423: 1416: 1409: 1402: 1380: 1366: 970: 943: 936: 929: 920: 914: 908: 907: 903: 901: 899: 888: 882: 876: 875: 871: 869: 867: 856: 850: 844: 843: 839: 837: 835: 824: 818: 817: 815: 813: 801: 795: 789: 788: 784: 782: 780: 769: 750: 749: 747: 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Index


Ionospheric research
NASA
COSPAR ID
1964-051A
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SATCAT no.
Bus
Cutler-Hammer
Solar cells
batteries
GMT
Scout X-4
Vandenberg
SLC-5
Vought
Geocentric orbit
Low Earth orbit
Perigee altitude
Apogee altitude
Inclination
Period
Explorer S-66
Explorer 21
NASA
Explorer program
ionosphere
Cutler-Hammer
NASA
Goddard Space Flight Center

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