R-process nucleosynthesis from magnetar giant flares in neutron star--white dwarf mergers: A unified picture for peculiar long gamma-ray bursts
磁星巨耀发驱动的中子星-白矮星合并r-过程核合成:奇特长伽马暴的统一图像
Peculiar long gamma-ray bursts (GRBs), exemplified by GRBs 211211A and 230307A, exhibit a long-duration multi-component prompt emission, an X-ray plateau in their afterglow, and a kilonova signature. Their origin remains highly debated. In this work, we present a unified picture for these events based on neutron star--white dwarf (NS--WD) mergers involving a pre-merger magnetar and a massive WD. In this picture, tidal disruption of the WD forms a constant-entropy accretion disk. Hyperaccretion from this disk onto the NS during the early accretion phase amplifies its toroidal magnetic field to strengths sufficient to trigger repeated magnetar giant flares (GFs). The main burst (MB) of the prompt emission consists of a ``forest'' of initial spikes from these GFs, while the subsequent magnetic propeller phase generates the extended emission (EE) and naturally explains the observed MB--EE trough. Crucially, the $e^{\pm}$-$γ$ fireball associated with each GF initial spike shocks the NS crust, leading to crustal ejection that synthesizes r-process heavy elements via the $α$-rich freeze-out mechanism, thereby resolving the r-process deficit in conventional NS--WD hydrodynamic simulations. The ensemble of such fireballs over the MB duration collectively yields $M_{\rm ej}\gtrsim 10^{-5}-10^{-3}\,M_\odot$ of ejecta, sufficient to power the observed kilonova signature when further boosted by the spin-down of the post-merger magnetar. Meanwhile, the spin-down radiation also powers the X-ray plateau. This tidally disrupted NS--WD merger picture provides a self-consistent framework that unifies the prompt emission, afterglow, kilonova, and r-process nucleosynthesis observed in peculiar long GRBs.
展开 ▾创新性地利用磁星巨耀发的初始脉冲激波剥离中子星壳层,在α-富丰冻结机制下实现高效r-过程,克服了传统NS-WD合并模拟中r-过程产额严重不足的瓶颈;同时为奇特长暴提供了一体化图像,将多成分瞬时辐射、X射线平台和千新星统一在同一个物理框架中。
奇特长伽马暴如GRB 211211A和GRB 230307A兼具长时标多分量辐射、X射线平台和千新星特征,传统上长暴与短暴的起源分类难以容纳此类事件。先前的中子星-白矮星合并模拟虽可解释部分观测,却普遍面临r-过程核合成产额过低的问题,难以匹配千新星亮度。本文通过引入磁星巨耀发与中子星壳层抛射的协同作用,在α-丰富冻结机制下有效产生r-过程重元素,并利用磁星星风为X射线平台供能,为奇特长暴提供了自洽的统一模型。随着宽视场巡天能力提升和千新星光谱模板的完善,该模型的多信使预言——如巨耀发驱动的抛射物丰度模式、磁星自转减速对光变的影响——将有望通过统计样本和精细谱线分析得到检验,从而进一步照亮致密天体合并中的元素合成与磁星物理。
预印本 2026-07-27 · 收录 2026-07-28