Radiated temperature of light flash produced by hypervelocity impact on natural dolomite plate
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摘要: 为研究超高速碰撞天然白云石板产生闪光温度衰减阶段的演化特征,利用二级轻气炮和瞬态光纤高温计,进行入射角度(与靶板平面的夹角)为45、碰撞速度分别为1.9,4.2 km/s两种条件下的超高速碰撞实验。根据冲击波理论,推导出超高速碰撞天然白云石板产生闪光温度衰减阶段的半理论半经验公式。分析结果表明,弹丸撞击靶板的速度越高,闪光辐射温度衰减的持续时间越长。闪光辐射温度衰减阶段的理论推导与实验数据一致性较好,闪光辐射温度衰减阶段的理论推导可对类似碰撞问题闪光辐射温度衰减阶段进行预估。Abstract: To investigate the evolutionary characteristics of decay phase of the flash temperature produced by hypervelocity impact on dolomite plate, an experimental measurement system platform was established with two-stage light-gas gun loading system and optical pyrometer measurement system, and the hypervelocity impact experiments were executed in two different velocities (as 1.9, 4.2 km/s)at the same impact angle 45. Theoretical and empirical formula was deduced by shock wave theory. The analysis of the results show that the larger the impact velocity is, the longer the decay time will be and that the theoretical derivation formula is better consistent with the experimental data, and it can be used for estimating such collisions radiation decay phase of the flash temperature.
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Key words:
- hypervelocity impact /
- dolomite plate /
- impact light flash /
- flash temperature /
- theoretical derivation
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