1964
DOI: 10.1029/jz069i015p03199
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Mass spectrometric investigations of the atmosphere between 100 and 227 kilometers above Wallops Island, Virginia

Abstract: The diffusive separation of argon and nitrogen was measured by means of a Bennett radio frequency mass spectrometer carried on an Aerobee 150A rocket (NASA 4.14) launched at 1141 EST, November 15, 1960. The primary purpose of the spectrometer measurements was to obtain temperate latitude diffusive separation data to compare with those measurements obtained in the arctic (Fort Churchill, Canada) during the International Geophysical Year. The results indicate that diffusive separation occurred above about 110 km… Show more

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Cited by 16 publications
(3 citation statements)
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“…There is a tendency for this ratio to approach I at heights just below 100 km on both up and downleg, but downleg data indicate that 30 + becomes dominant again below this region. This result differs from some earlier midday results (Holmes et al, 1965, Johnson, 1916, Narcisi, 1968 which show regions where i30+]/[32+] becomes less than one but agrees with others not exhibiting this behavior (Taylor and Brinton, 1961, Meadows-Reed and Smith, 1964, Arnold et al, 1969.…”
Section: B E and F Region Resultscontrasting
confidence: 57%
“…There is a tendency for this ratio to approach I at heights just below 100 km on both up and downleg, but downleg data indicate that 30 + becomes dominant again below this region. This result differs from some earlier midday results (Holmes et al, 1965, Johnson, 1916, Narcisi, 1968 which show regions where i30+]/[32+] becomes less than one but agrees with others not exhibiting this behavior (Taylor and Brinton, 1961, Meadows-Reed and Smith, 1964, Arnold et al, 1969.…”
Section: B E and F Region Resultscontrasting
confidence: 57%
“…We have recorded the ionograms corresponding to the trace vapors of different 4B. We have estimated that the limit of detection for TNT is ~1*10 -13 g/cm 3 .…”
Section: Resultsmentioning
confidence: 99%
“…The first installation of the mass spectrometer on the aircraft dates back to the 50-th, when Bennett radio frequency mass spectrometers where installed on the sounding rockets and artificial satellites and were used for the investigation of the ionic composition of the upper atmosphere [1][2][3] . Further development of the field resulted in the introduction of more complicated aircraft-borne mass spectrometers designed for specific purposes: aerosol mass spectrometers 4 , dust impact mass analyzer 5 etc.…”
mentioning
confidence: 99%