Entropy proxy inversions as tracers of the evolution of physical conditions at the base of the solar convective envelope

IF 5.8 2区 物理与天体物理 Q1 ASTRONOMY & ASTROPHYSICS
G. Buldgen, A. Noels, V. A. Baturin, J. Christensen-Dalsgaard, S. V. Ayukov, A. V. Oreshina, R. Scuflaire
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Abstract

Context. The Sun is an important calibrator in the theory of stellar structure and evolution. However, the accuracy of our solar evolution models is tightly linked to the physical elements that enter their computations. This includes, among others, the equation of state, the opacities, the transport of chemicals, and the modelling of turbulent convection. Deriving model-independent probes of these elements is therefore crucial to further testing the quality of these ingredients and potentially revealing their shortcomings using observational data.Aims. We aim to provide additional constraints to the thermodynamic properties of the solar plasma at the base of the solar convective zone using a revised helioseismic indicator mimicking the properties of the specific entropy in the envelope.Methods. We derived a revised entropy proxy for the solar convective envelope, which is directly accessible when using helioseismic structure inversions. We then used solar evolutionary models with various modifications of input physics to study the properties of the proxy of the entropy in the convective envelope.Results. We find that the entropy proxy for the solar convective envelope allows us to invalidate adiabatic overshooting as a solution to the solar modelling problem and strongly points towards the need for revised opacities. Our results show that this new indicator is a strong diagnostic of the overall evolution of the thermodynamical conditions at the base of the convective zone.Conclusions. The new entropy proxy indicator allows for a more accurate characterisation of the conditions at the base of the solar convective zone. While it already allows us to rule out overshooting as a solution to the solar modelling problem, its sensitivity to the shape of the opacity modification and the evolution of the properties at the base of the convective zone makes it a powerful helioseismic diagnostic for solar models.
熵代理逆温作为太阳对流包层底部物理条件演变的示踪剂
上下文。太阳是恒星结构和演化理论的重要校准器。然而,我们的太阳演化模型的准确性与计算中的物理元素密切相关。这其中包括状态方程、不透明度、化学物质的传输和湍流对流的建模。因此,对这些元素进行独立于模型的探测对于进一步测试这些成分的质量和利用观测数据潜在地揭示它们的缺点至关重要。我们的目标是使用一种改进的日震指标来模拟包络层中特定熵的性质,为太阳对流带底部的太阳等离子体的热力学性质提供额外的约束。我们推导了一个修正的太阳对流包络的熵代理,当使用日震结构反演时可以直接获得。然后,我们使用带有各种输入物理修改的太阳演化模型来研究对流包络中熵代理的性质。我们发现,太阳对流包络的熵代理使我们能够使绝热超调作为太阳模拟问题的解决方案无效,并强烈指出需要修改不透明度。我们的研究结果表明,这一新指标对对流区底部热力条件的整体演变有很强的诊断作用。新的熵代理指标允许更准确地描述太阳对流区底部的条件。虽然它已经允许我们排除超调作为太阳建模问题的解决方案,但它对不透明度变化的形状和对流区底部属性的演变的敏感性使其成为太阳模型的强大日震诊断。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Astronomy & Astrophysics
Astronomy & Astrophysics 地学天文-天文与天体物理
CiteScore
10.20
自引率
27.70%
发文量
2105
审稿时长
1-2 weeks
期刊介绍: Astronomy & Astrophysics is an international Journal that publishes papers on all aspects of astronomy and astrophysics (theoretical, observational, and instrumental) independently of the techniques used to obtain the results.
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