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首页> 外文期刊>Meteoritics & planetary science >Impact flash evolution of CO2 ice, water ice, and frozen Martian and lunar regolith simulant targets
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Impact flash evolution of CO2 ice, water ice, and frozen Martian and lunar regolith simulant targets

机译：CO2冰，水冰和冷冻火星和月球升降机模拟目标的影响闪光演化

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摘要

The wavelength dependence and temporal evolution of the hypervelocity impact self-luminous plume (or "flash") from CO2 ice, water ice, and frozen Martian and lunar regolith simulant targets have been investigated using the Kent two-stage light-gas gun. An array of 10 band-pass filtered photodiodes and a digital camera monitored changes in the impact flash intensity during the different phases of the emitting ejecta. Early-time emission spectra were also recorded to examine short-lived chemical species within the ejecta. Analyses of the impact flash from the varied frozen targets show considerable differences in temporal behavior, with a strong wavelength dependence observed within monitored near-UV to near-IR spectral regions. Emission spectra showed molecular bands across the full spectral range observed, primarily due to AlO from the projectile, and with little or no contribution from vaporized metal oxides originating from frozen regolith simulant targets. Additional features within the impact flash decay profiles and emission spectra indicate an inhomogeneity in the impact ejecta composition. A strong correlation between the density of water ice-containing targets and the impact flash rate of decay was shown for profiles uninfluenced by significant atomic/molecular emission, although the applicability to other target materials is currently unknown. Changes in impact speed resulted in considerable differences in the temporal evolution of the impact flash, with additional variations observed between recorded spectral regions. A strong correlation between the impact speed and the emission decay rate was also shown for CO2 ice targets. These results may have important implications for future analyses of impact flashes both on the lunar/Martian surface and on other frozen bodies within the solar system.
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  • 来源
    《Meteoritics & planetary science》 |2020年第10期|共19页
  • 作者

    Tandy Jon D.; Price Mark C.; Wozniakiewicz Penny J.; Cole Mike J.; Alesbrook Luke S.; Avdellidou Chrysa;

  • 作者单位

    London Metropolitan Univ Sch Human Sci London N7 8DB England;

    Univ Kent Ctr Astrophys &

    Planetary Sci Sch Phys Sci Ingram Bldg Canterbury CT2 7NH Kent England;

    Univ Kent Ctr Astrophys &

    Planetary Sci Sch Phys Sci Ingram Bldg Canterbury CT2 7NH Kent England;

    Univ Kent Ctr Astrophys &

    Planetary Sci Sch Phys Sci Ingram Bldg Canterbury CT2 7NH Kent England;

    Univ Kent Ctr Astrophys &

    Planetary Sci Sch Phys Sci Ingram Bldg Canterbury CT2 7NH Kent England;

    Lab Lagrange Blvd Observ CS 34229 F-06304 Nice France;

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  • 正文语种 eng
  • 中图分类 天文学;
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