Temperatures of shock-induced shear instabilities and their relationship to fusion curves

Details Temperatures of shock-induced shear instabilities and their relationship to fusion curves Temperatures of shock-induced shear instabilities and their relationship to fusion curves

Nov 1983

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1983georl..10.1077s&link_type=abstract

Geophysical Research Letters (ISSN 0094-8276), vol. 10, Nov. 1983, p. 1077-1080.

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18

Emission Spectra, Glass, Metamorphism (Geology), Shock Heating, Black Body Radiation, Emissivity, Magnesium Oxides, Phase Diagrams, Pressure Effects, Radiance, Temperature Measurement, Transparence

Scientific paper

New emission spectra for MgO and CaAl2Si2O8 (glass) are observed from 430 to 820 nm. Taken with previous data, it is suggested that transparent solids display three regimes of light emission upon shock compression to successively higher pressures: (1) characteristic radiation such as observed in MgO and previously in other minerals, (2) heterogeneous hot spot (greybody) radiation observed in CaAl2Si2O8 and previously in all transparent solids undergoing shock-induced phase transformations, and (3) blackbody emission observed in the high pressure phase regime in NaCl, SiO2, CaO, CaAl2Si2O8, and Mg2SiO4. The onset of the second regime may delineate the onset of shock-induced polymorphism whereas the onset of the third regime delineates the Hugoniot pressure required to achieve local thermal equilibrium in the shocked solid. It is also proposed that the hot spot temperatures and corresponding shock pressures determined in the second regime delineate points on the fusion curves of the high pressure phase.

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