论文标题

在两个中子星形壳冷却来源中观察到意外的后期温度升高-XTE〜J1701-462和EXO〜0748-676

Unexpected late-time temperature increase observed in two neutron star crust cooling sources -- XTE~J1701-462 and EXO~0748-676

论文作者

Parikh, A. S., Wijnands, R., Homan, J., Degenaar, N., Wolvers, B., Ootes, L. S., Page, D.

论文摘要

托管中子星(NSS)的瞬时LMXB为探测NS外壳中存在的密集物理物质提供了出色的实验室。在LMXBS的积聚爆发期间,放热反应可能会加热NS外壳,从而破坏地壳核平衡。当爆发停止时,地壳会冷却以恢复与核心的热平衡。监测这种演变使我们能够探测地壳中的密集物理物理。爆发结束后的稍后时间,可以探测更深的地壳层的性能。我们报告了LMXBS,XTE J1701-462和EXO 0748-676的两个NSS的意外延迟温度演化(爆发结束后的2000天> 2000天)。尽管这两个来源表现出非常不同的爆发(就持续时间和平均积聚率而言),但它们在观察到的有效温度(在〜700天内发生)在爆发结束后约2000天内表现出异常陡峭的衰减〜7 eV。此外,在这种陡峭的衰变之后,它们在温度(在〜500-2000天的时间内)显示出〜3 eV的升高。对于XTE J1701-462和EXO 0748-676的2.4σ和8.5σ水平的这一上升是显着的。这种行为的物理解释尚不清楚,在冷却假设中不能直接解释。此外,在不调用许多假设的情况下,低级积聚也不能很好地解释这种观察到的进化。我们研究了可以再现这种异常行为的理论加热和冷却模型中的潜在途径,到目前为止,这在两个地壳冷却来源中都可以观察到。在类似的晚期,在其他NS地壳冷却来源中尚未观察到这种温度升高,尽管不能排除这可能是由于在这样的后期获得的采样不足的结果。

Transient LMXBs that host neutron stars (NSs) provide excellent laboratories for probing the dense matter physics present in NS crusts. During accretion outbursts in LMXBs, exothermic reactions may heat the NS crust, disrupting the crust-core equilibrium. When the outburst ceases, the crust cools to restore thermal equilibrium with the core. Monitoring this evolution allows us to probe the dense matter physics in the crust. Properties of the deeper crustal layers can be probed at later times after the end of the outburst. We report on the unexpected late-time temperature evolution (>2000 days after the end of their outbursts) of two NSs in LMXBs, XTE J1701-462 and EXO 0748-676. Although both these sources exhibited very different outbursts (in terms of duration and the average accretion rate), they exhibit an unusually steep decay of ~7 eV in the observed effective temperature (occurring in a time span of ~700 days) around ~2000 days after the end of their outbursts. Furthermore, they both showed an even more unexpected rise of ~3 eV in temperature (over a time period of ~500-2000 days) after this steep decay. This rise was significant at the 2.4σ and 8.5σ level for XTE J1701-462 and EXO 0748-676, respectively. The physical explanation for such behaviour is unknown and cannot be straightforwardly be explained within the cooling hypothesis. In addition, this observed evolution cannot be well explained by low-level accretion either without invoking many assumptions. We investigate the potential pathways in the theoretical heating and cooling models that could reproduce this unusual behaviour, which so far has been observed in two crust-cooling sources. Such a temperature increase has not been observed in the other NS crust-cooling sources at similarly late times, although it cannot be excluded that this might be a result of the inadequate sampling obtained at such late times.

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