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高空核爆炸下大气的X射线电离及演化过程数值模拟
Numerical simulation of X-ray ionization and atmospheric temporal evolutions with high-altitude nuclear explosions
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摘要: 用数值模拟程序模拟了不同高度核爆炸下大气的x射线电离及演化过程．结果表明：x射线电离产生的电子数密度在射线到达后约100ns时刻达到峰值，峰值数密度随着到裸核区距离的增加而减小；电子具有较长的寿命，电子寿命随着到裸核区距离的增加而增大；X射线电离空气产生正离子O＋，O2＋，N2＋，爆高为120km情况下O＋的峰值数密度与。手的相近，能维持约1S．X射线对空气的电离影响范围在数十千米以内，在距裸核区较近的区域，爆高为80km时产生的电子峰值数密度比爆高为120km时的电子峰值数密度高，在距裸核区较远的区域则相反．Abstract: The X-ray ionizations and the atmospheric temporal evolutions with different altitude nuclear explosions are numerically simulated in this paper. It is concluded that the density of electrons generated by X-ray ionization has a peak value at 100 ns after the X-rays have arrived, and the peak density reduced with the increase of distance from the stripped nucleus area. The life time of electrons is long, and increases with the distance from the stripped nucleus area. O＋, O＋2, N＋ are generated by X-ray ionization. The distance of X-ray ionization in atmosphere is within a few tens of kilometers. The peak density of explosion at 80 km high is larger than at 120 km high in the area close to stripped nucleus area. but the scenario is ormosite in the arwa far from stripped nucleus area.
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