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Davidson & Emerson 1990
Davidson, T.A. and Emerson, D.E. (1990). Direct determination of the helium 3 content of atmospheric air by mass spectrometry. Journal of Geophysical Research 95: doi: 10.1029/89JD03238. issn: 0148-0227.

The Bureau of Mines, Helium Field Operations, in Amarillo, Texas, has developed a method for direct measurement of the helium 3 content of air by mass spectroscopy. The helium is preconcentrated by passing samples of air through a charcoal trap at liquid nitrogen temperature. Sample measurements are compared with identically made measurements of gravimetrically prepared standards. The helium 3 content of near-surface atmospheric air is determined to be 7.27¿0.20 parts per trillion by volume (pptv). The accuracy of 0.20 pptv is at the 68% confidence level. The helium 4 content of near-surface atmospheric air has recently been determined at this facility to be 5.2204¿0.0041 parts per million by volume (ppmv). The helium 3/helium 4 ratio for atmospheric helium, RA, is established as 1.393¿10-6 by independent measurements of the separate components.

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Abstract

Keywords
Atmospheric Composition and Structure, Middle atmosphere—composition and chemistry, Atmospheric Composition and Structure, Instruments and techniques
Journal
Journal of Geophysical Research
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Publisher
American Geophysical Union
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