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X-RAY HARDNESS VARIATIONS AS AN INTERNAL/EXTERNAL SHOCK DIAGNOSTIC

机译:X射线硬度变化作为内部/外部冲击的诊断

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The early, highly time-variable X-ray emission immediately following gamma-ray bursts (GRBs) exhibits strong spectral variations that are unlike the temporally smoother emission that dominates after t ~ 10~3 s. The ratio of hard-channel (1.3-10.0 keV) to soft-channel (0.3-1.3 keV) counts in the Swift X-ray telescope provides a new measure delineating the end time of this emission. We define T_H as the time at which this transition takes place and measure for 59 events a range of transition times that spans 10~2 to 10~4 s, on average 5 times longer than the prompt T_(90) duration observed in the gamma-ray band. It is very likely that the mysterious light-curve plateau phase and the later power-law temporal evolution, both of which typically occur at times greater than T_H and hence exhibit very little hardness ratio evolution, are both produced by external shocking of the surrounding medium and not by the internal shocks thought responsible for the earlier emission. We use the apparent lack of spectral evolution to discriminate among proposed models for the plateau phase emission. We favor energy injection scenarios with a roughly linearly increasing input energy versus time for six well-sampled events with nearly flat light curves at t ≈ 10~3 -10~4 s. Also, using the transition time T_H as the delineation between the GRB and afterglow emission, we calculate that the kinetic energy in the afterglow shock is typically a factor of 10 lower than that released in the GRB. Three very bright events suggest that this presents a missing X-ray flux problem rather than an efficiency problem for the conversion of kinetic energy into the GRB. Lack of hardness variations in these three events may be due to a very highly relativistic outflow or due to a very dense circumburst medium. There are a handful of rare cases of very late time t > 10~4 s hardness evolution, which may point to residual central engine activity at very late time.
机译:紧随伽马射线爆发(GRB)之后的早期,高度时变的X射线发射具有很强的光谱变化,这与t〜10〜3 s之后在时间上更平滑的发射不同。 Swift X射线望远镜中硬通道(1.3-10.0 keV)与软通道(0.3-1.3 keV)计数之比提供了一种新方法来描述这种发射的结束时间。我们将T_H定义为发生这种转变的时间,并针对59个事件测量过渡时间范围为10〜2到10〜4 s,平均比在伽马中观察到的瞬态T_(90)持续时间平均长5倍射线带。神秘的光曲线平稳期和后来的幂律时间演化很可能都是由周围介质的外部冲击产生的,它们通常都在大于T_H的时间发生,因此几乎没有硬度比的演化。而不是因为内部冲击被认为是造成早期排放的原因。我们使用频谱演化的明显不足来区分高原阶段发射的建议模型。我们赞成在六个时间采样的事件中,在t≈10〜3 -10〜4 s时光曲线几乎平坦的情况下,输入能量随时间大致线性增加的能量注入场景。同样,使用过渡时间T_H作为GRB和余辉发射之间的轮廓,我们计算出余辉冲击中的动能通常比GRB中释放的动能低10倍。三个非常明亮的事件表明,这提出了缺少的X射线通量问题,而不是将动能转换为GRB的效率问题。这三个事件中硬度变化的缺乏可能是由于相对论性非常高的流出或由于周向介质非常稠密。极少数情况下,非常晚的时间t> 10〜4 s会发生硬度变化,这可能表明在很晚的时间仍存在中央发动机剩余活动。

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