论文标题

极端碰撞系统APEP:红外中央二元和灰尘的已解决图像

The extreme colliding-wind system Apep: resolved imagery of the central binary and dust plume in the infrared

论文作者

Han, Y., Tuthill, P. G., Lau, R. M., Soulain, A., Callingham, J. R., Williams, P. M., Crowther, P. A., Pope, B. J. S., Marcote, B.

论文摘要

最近在系统中发现了壮观的灰尘羽流2xmm J160050.7-514245(称为“ APEP”)提出了通过“ Pinwheel”机制在碰撞的二进制中的物理起源。观察数据指向分层三星级系统,但是几种极端和意外的物理特性似乎无视此类对象的既定物理。最值得注意的是,与天空平面中灰尘的适当运动膨胀相比,在观察到的气体的流出速度中发现了明显的差异。这种神秘的行为出现在中央狼射线二进制的风库中:迄今为止在空间上仍未解决的系统。在这里,我们提出了一项更新的适当运动研究,该研究得出了APEP灰尘羽流的膨胀速度,这是两年的基线,该基线比光谱风速慢四倍,从而确认并增强了先前的发现。我们还提出了系统心脏中心的高角度分辨率近红外成像研究的结果,揭示了与狼射线碰撞系统相匹配的二进制的二进制。基于这些新的观察性约束,提出了一个改进的几何模型,与数据非常匹配,从而限制了狼射线二进制的轨道参数,并向各向异性风模型提供了进一步的支持。

The recent discovery of a spectacular dust plume in the system 2XMM J160050.7-514245 (referred to as "Apep") suggested a physical origin in a colliding-wind binary by way of the "Pinwheel" mechanism. Observational data pointed to a hierarchical triple-star system, however several extreme and unexpected physical properties seem to defy the established physics of such objects. Most notably, a stark discrepancy was found in the observed outflow speed of the gas as measured spectroscopically in the line-of-sight direction compared to the proper motion expansion of the dust in the sky plane. This enigmatic behaviour arises at the wind base within the central Wolf-Rayet binary: a system that has so far remained spatially unresolved. Here we present an updated proper motion study deriving the expansion speed of Apep's dust plume over a two-year baseline that is four times slower than the spectroscopic wind speed, confirming and strengthening the previous finding. We also present the results from high-angular-resolution near-infrared imaging studies of the heart of the system, revealing a close binary with properties matching a Wolf-Rayet colliding-wind system. Based on these new observational constraints, an improved geometric model is presented yielding a close match to the data, constraining the orbital parameters of the Wolf-Rayet binary and lending further support to the anisotropic wind model.

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