C

T. Umebayashi, Norihito Katsuma, H. Nomura
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Abstract

We investigate the evolution of the ionization rates by the decay of radionuclides in protoplanetary disks at the early stage of planet formation where size growth and settling of dust particles proceed extensively. Because most of the nuclides to ionize gas, such as short-lived nuclide 26Al and long-lived one 40K, are refractory elements, they are contained in the solid material of dust particles. Thus, the ionization by these nuclides is affected by the following three processes: (1) the change of the relative abundance of dust particles due to the settling toward the midplane of the disk, (2) the energy loss of emitted energetic particles inside the solid material of dust particles, and (3) the absorption of energetic particles by the other dust particles located nearby. In this series of papers we comprehensively investigate the basic physical processes, calculate the settling and size growth of dust particles numerically, and clarify the evolution of the ionization rates relative to their initial values in various disk models at this stage. In this paper we investigate the energy-loss processes concerning dust particles, formulate the coalescence equation for settling particles, and apply them to quiescent disk models that are similar to the solar nebula. For simplicity, dust particles are assumed to be compact spheres that remain perfect sticking for mutual collisions. Because the settling of dust particles is not appreciable in the first 103 yr, the ionization rate varies little except in the outermost part near the disk surface. As the settling proceeds, the rate around the midplane increases considerably. The maximum ionization rates by 26Al in the minimum mass solar nebula are about 100, 51, and 14 times larger than their initial values for the orbits R = 0.5, 1, and 5 AU, respectively, which are close to or exceed the ionization rate by cosmic ray in the interstellar medium. The rates by 40K also increase by factors of about 36, 19, and 5 at the same orbits. In the inner orbital regions, these rates exceed the rates by the attenuated cosmic rays by an order of magnitude. The rates in the residual parts decrease extensively as time goes by, because amounts of the floating dust particles decrease continuously.
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在行星形成的早期阶段,我们通过放射性核素的衰变来研究电离率的演变,在这个阶段,尘埃颗粒的大小增长和沉降进行得很广泛。因为电离气体中的大多数核素,如短寿命核素26Al和长寿命核素40K,都是难熔元素,它们都包含在尘埃颗粒的固体物质中。因此,这些核素的电离受到以下三个过程的影响:(1)尘埃颗粒相对丰度的变化,因为尘埃颗粒沉降到圆盘的中间面;(2)发射的高能粒子在尘埃颗粒的固体物质内部的能量损失;(3)附近的其他尘埃颗粒对高能粒子的吸收。在这一系列的论文中,我们全面研究了基本的物理过程,数值计算了尘埃颗粒的沉降和尺寸增长,并阐明了在这一阶段在各种圆盘模型中电离率相对于初始值的演变。本文研究了尘埃粒子的能量损失过程,建立了沉降粒子的聚并方程,并将其应用于类似太阳星云的静止盘模型。为简单起见,我们假设尘埃粒子是致密的球体,它们在相互碰撞时保持完美的粘性。因为在最初的103年里尘埃颗粒的沉降是不明显的,所以电离率变化很小,除了在靠近圆盘表面的最外层。随着沉降的进行,背板周围的速率显著增加。在R = 0.5、1和5 AU的轨道上,26Al在最小质量太阳星云中的最大电离率分别是初始值的100倍、51倍和14倍,接近或超过了宇宙射线在星际介质中的电离率。在相同的轨道上,40K的速率也增加了大约36倍、19倍和5倍。在内轨道区域,这些速率超过衰减宇宙射线的速率一个数量级。随着时间的推移,残余部分的速率大幅度降低,这是由于浮尘颗粒的数量不断减少。
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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