Computer Science
Scientific paper
Dec 1977
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1977metic..12..401g&link_type=abstract
Meteoritics, vol. 12, Dec. 31, 1977, p. 401-408. Research supported by the Research Corp. and University of Hawaii;
Computer Science
4
Chemical Fractionation, Chondrites, Meteoritic Composition, Vapor Phases, Iron, Mass Spectroscopy, Nickel, Potassium, Sodium, Vapor Pressure, Vaporizing
Scientific paper
The vapor phase composition obtained by heating samples of the Holbrook L6 chondrite to 1300 C was determined quantitatively by Knudsen cell-quadrupole mass spectrometry. Maximum observed vapor pressures, produced at 1200 C, are reported for Na, K, Fe, and Ni, and the implications of the Na/K ratio are considered. The Fe and Ni data are discussed with attention to their migration in individual equilibrated chondrites. S2 (with minor SO2), H2O, and CO2 were also present in the high-temperature gas phase. Vesicles formed by the release of intrinsically derived volatiles are compared with vesicles in the Ibitira eucrite. Chondrite evolution is briefly discussed.
Gooding James L.
Muenow David W.
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