Kirin meteorite - Temperature gradient produced during atmospheric passage

Details Kirin meteorite - Temperature gradient produced during atmospheric passage Kirin meteorite - Temperature gradient produced during atmospheric passage

Sep 1979

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1979metic..14..309m&link_type=abstract

Meteoritics, vol. 14, Sept. 30, 1979, p. 309-316.

Other

Aerodynamic Heating, Atmospheric Entry, Stony Meteorites, Temperature Gradients, Aerodynamic Heat Transfer, Crusts, Friction, Graphs (Charts), Taiwan, Thermoluminescence, Meteorites, Kirin Meteorite, Thermal Gradients, Heating, Atmosphere, Thermoluminescence, Stony Meteorites, Procedure, Conduction

Scientific paper

Thermoluminescence (TL) is used to determine the temperature gradient produced in the Kirin, China, meteorite by heating during atmospheric passage. The experimentally determined gradient of about 51 C/mm is more than twice as large as previously published values for other meteorites and agrees more closely with the theoretical predictions of a steady-state continuous ablation model. The normalized TL measured in the interior of the fragment is nearly constant over a distance of two centimeters.

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