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Iron line spectroscopy with Einstein–dilaton–Gauss–Bonnet black holes

机译:用爱因斯坦-狄拉顿-高斯-帽子黑洞进行铁谱分析

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Einstein–dilaton–Gauss–Bonnet gravity is a well-motivated alternative theory of gravity that emerges naturally from string theory. While black hole solutions have been known in this theory in numerical form for a while, an approximate analytical metric was obtained recently by some of us, which allows for faster and more detailed analysis. Here we test the accuracy of the analytical metric in the context of X-ray reflection spectroscopy. We analyze innermost stable circular orbits (ISCO) and relativistically broadened iron lines and find that both the ISCO and iron lines are determined sufficiently accurately up to the limit of the approximation. We also find that, though the ISCO increases by about 7% as dilaton coupling increases from zero to extremal values, the redshift at ISCO changes by less than 1%. Consequently, the shape of the iron line is much less sensitive to the dilaton charge than expected.
机译:爱因斯坦-狄拉顿-高斯-邦尼特引力是一种动力十足的替代性引力理论,它自然而然地从弦理论中产生。虽然黑洞解决方案已经在理论中以数字形式出现了一段时间,但我们中的一些人最近获得了近似的分析指标,从而可以进行更快,更详细的分析。在这里,我们在X射线反射光谱学的背景下测试分析指标的准确性。我们分析了最内层的稳定圆形轨道(ISCO)和相对论拓宽的铁线,发现ISCO和铁线都被足够精确地确定到近似值的极限。我们还发现,尽管随着dilaton耦合从零增加到极值,ISCO大约增加了7%,但ISCO的红移变化不到1%。因此,铁线的形状对狄拉顿电荷的敏感性远低于预期。

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