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Ejection of the inner accretion disk in GRS 1915+105: the magnetic rubber-band effect

机译:在GRs 1915 + 105中弹出内部吸积盘:磁性   橡皮筋效应

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摘要

We examine theoretically the behaviour of the inner accretion disk in GRS1915+105 when soft X-ray dips are present in the X-ray light curve. We assumethe presence of a radial shock in the accretion disk, as in some of the TwoComponent Advective Flow (TCAF) solutions. We discuss the behaviour of the fluxtubes inside a TCAF (which we name Magnetized TCAF or MTCAF model for brevity)and compare various competing forces on the flux tubes. In this MTCAF model, wefind that the magnetic tension is the strongest force in a hot plasma oftemperature $\gsim 10^{10}$K and as a result, magnetic flux tubes entering inthis region collapse catastrophically, thereby occasionally evacuating theinner disk. We postulate that this magnetic `rubber-band' effect inducedevacuated disk matter produces the blobby components of outflows and IR/radiojets. We derive the size of the post-shock region by equating the time scale ofthe Quasi-Periodic Oscillations to the infall time of accreting matter in thepost-shock region and found the shock location to be $\sim 45-66 r_g$. Wecalculate the transition radius $r_{tr}$, where the Keplerian disk deviatesinto a sub-Keplerian flow, to be $\sim 320r_g$. Based on the derived X-rayspectral parameters, we calculate the mass of this region to be $\sim10^{18}$g.We conclude that during the X-ray dips the matter in the post-shock region,which manifests itself as the thermal-Compton component in the X-ray spectrum,is ejected, along with some sub-Keplerian matter in the pre-shock region.
机译:我们从理论上检查了当X射线光曲线中出现软X射线倾角时,GRS1915 + 105内部吸积盘的行为。我们假定吸积盘中存在径向冲击,就像某些双组分顺向流动(TCAF)解决方案一样。我们讨论了TCAF(为简便起见,我们将其命名为磁化TCAF或MTCAF模型)内部的通量管行为,并比较了通量管上的各种竞争力。在此MTCAF模型中,我们确定在温度为\\ gsim 10 ^ {10} $ K的热等离子体中,磁力是最强的力,因此,进入该区域的磁通管会发生灾难性的坍塌,从而有时会抽空内盘。我们假设这种“橡胶带”效应引起的真空磁盘物质产生了流出和红外/射流的浮空成分。我们通过将准周期振荡的时间尺度与震后区域内增生物质的进入时间相等来推算震后区域的大小,发现震荡位置为$ \ sim 45-66 r_g $。我们计算过渡半径$ r_ {tr} $,其中Keplerian磁盘偏离为次Kelerian流,为$ \ sim 320r_g $。根据导出的X射线光谱参数,我们将该区域的质量计算为$ \ sim10 ^ {18} $ g。我们得出结论,在X射线浸没过程中,物质位于震后区域,表现为X射线谱中的热康普顿分量连同预震区中的一些次凯普勒物质一起被射出。

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