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首页> 外文期刊>The Astrophysical journal >THICK TO THIN: THE EVOLUTIONARY CONNECTION BETWEEN PG 1159 STARS AND THE THIN HELIUM-ENVELOPED PULSATING WHITE DWARF GD 358
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THICK TO THIN: THE EVOLUTIONARY CONNECTION BETWEEN PG 1159 STARS AND THE THIN HELIUM-ENVELOPED PULSATING WHITE DWARF GD 358

机译:细到薄:PG 1159星与薄薄的氦包络脉动白色矮星GD 358之间的进化联系

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Seismological observations with the Whole Earth Telescope (WET) allow the determination of the subsurface compositional structure of white dwarf stars. The hot DO PG 1159 — 035 has a helium surface layer with a mass of ~ 10~(-3) solar mass, while the cooler DB white dwarf GD 358 has a much thinner surface helium layer of 10~(-6) solar mass. Taken literally, these results imply that either there is no evolutionary relation between these two stars, or that there is an unknown mass-loss mechanism. In order to investigate a possible evolutionary link between these objects, we computed evolutionary sequences of white dwarf models that included time-dependent diffusive processes. We used an initial model based on the PG 1159 pulsational data, which has a surface layer 3 x 10~(-3) solar mass thick, and a composition of 30% helium, 35% carbon, and 35% oxygen. Below this surface layer is a thin transition zone where the helium fraction falls to zero. As expected, diffusion caused a separation of the elements; a thickening surface layer of nearly pure helium overlays a deepening transition zone where the composition changes to the surface composition of the original model. When the model reached the temperature range inhabited by GD 358 and the pulsating DB white dwarfs, this pure helium surface layer was ~ 10~(-5.5) M_* deep. The resulting evolved model is very similar to the model used by Bradley and Winget to match the pulsation observations of GD 358. The pulsation periods of this model also show a good fit to the WET observations. These results demonstrate the plausibility of a direct evolutionary path from PG 1159 stars to the much cooler DB white dwarfs by inclusion of time dependent diffusion. A problem still remains in that our models have no hydrogen, and thus must retain their DB nature while evolving through the T_(eff) 45,000 to 30,000 K. Since there are no known DB stars in this range, we plan to address this problem in future calculations.
机译:使用全地球望远镜(WET)进行的地震观测可以确定白矮星的地下成分结构。热的DO PG 1159 — 035的氦气表面层质量约为太阳质量的10〜(-3),而较冷的DB白矮星GD 358的氦气表面层质量更薄,为10〜(-6)太阳质量。 。从字面上看,这些结果暗示这两个恒星之间没有进化关系,或者存在未知的质量损失机制。为了研究这些对象之间可能存在的进化联系,我们计算了白矮星模型的进化序列,其中包括与时间有关的扩散过程。我们使用了基于PG 1159脉动数据的初始模型,该模型的表层厚​​度为3 x 10〜(-3)太阳质量,并且由30%的氦,35%的碳和35%的氧组成。在此表面层之下是一个薄的过渡带,氦气含量降至零。不出所料,扩散导致元素分离。几乎纯净的氦的增厚表面层覆盖了一个深化的过渡带,在该过渡带中,成分变为原始模型的表面成分。当模型达到GD 358和脉动DB白矮星所占据的温度范围时,该纯氦气表层的深度约为〜10〜(-5.5)M_ *。生成的演化模型与Bradley和Winget用于匹配GD 358的脉动观测结果的模型非常相似。该模型的脉动周期也非常适合WET观测结果。这些结果证明了通过包含时间依赖性扩散,从PG 1159星到更凉爽的DB白矮星的直接进化路径的合理性。仍然存在问题,因为我们的模型没有氢,因此必须在通过45,000至30,000 K的T_(eff)演化时保持其DB性质。由于在该范围内没有已知的DB星,我们计划在未来的计算。

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