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Quantitative Magnetohydrodynamic Modeling of the Solar Transition Region

机译:太阳过渡区的定量磁流体动力学模拟

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The transition region (TR) is assumed to be a collision-dominated plasma. The dissipation and transport of energy in such a plasma is accurately described by the classical transport coefficients, which include the electrical and thermal conductivity, viscosity, and thermoelectric tensors. These tensors are anisotropic and are functions of local values of temperature, density, and magnetic field strength. The transport coefficients are valid for all magnetic field strengths and so may be used to study the physics of weakly as well as strongly magnetized regions of the TR. They may be used in an MHD model to obtain a self-consistent, realistic description of the TR. The physics of kinetic processes is included in the MHD model through the transport coefficients. As a first step in studying heating and cooling processes in the TR in a realistic, quantitative manner, a 1.5 dimensional, steady state MHD model with a specified temperature profile is developed. The momentum equation includes the inertial, pressure, magnetic, and gravitational forces. Ohm's law includes the exact expressions for the electrical conductivity and thermoelectric tensors. It is found that the contribution of the dissipation of large-scale electric currents to in situ heating of the TR is negligible, but that thermal energy flowing into the TR from the corona can provide the energy required to heat the TR. The possibility that significant in situ heating of the TR takes place through viscous dissipation or small-scale electric current dissipation such as may occur in current sheets or filaments is discussed, although these processes are not described by the model. The importance of thermoelectric and electron pressure gradient effects in Ohm's law, and in determining the electron heat flux, is demonstrated. Results of the model suggest that the force-free approximation is not valid over most of the TR. Justification for assuming that the TR is collision dominated is presented. In particular, a self-consistent calculation of the ratio of the electric field parallel to the magnetic field to the Dreicer electric field yields a value 10-3, which suggests that anomalous transport processes are not important. The necessity of using a realistic description of transport processes in modeling heating mechanisms in the solar atmosphere is stressed.
机译:过渡区域(TR)假定为碰撞为主的等离子体。通过经典的传输系数可以精确地描述这种等离子体中能量的耗散和传输,其中包括电导率和导热率,粘度和热电张量。这些张量是各向异性的,并且是温度,密度和磁场强度的局部值的函数。传输系数对所有磁场强度均有效,因此可用于研究TR的弱磁区和强磁区的物理性质。它们可以用于MHD模型中,以获得TR的自洽,逼真的描述。通过传输系数将动力学过程的物理学包括在MHD模型中。作为以现实,定量的方式研究TR中加热和冷却过程的第一步,开发了具有指定温度曲线的1.5维稳态MHD模型。动量方程式包括惯性力,压力,磁力和重力。欧姆定律包括电导率和热电张量的精确表达式。已经发现,大电流耗散对TR的原位加热的贡献可以忽略不计,但是从电晕流入TR的热能可以提供加热TR所需的能量。讨论了通过粘性耗散或小规模电流耗散(例如可能在电流板或灯丝中发生)发生TR大量原位加热的可能性,尽管模型并未描述这些过程。证明了热电和电子压力梯度效应在欧姆定律以及确定电子热通量中的重要性。模型的结果表明,在大多数TR上,无力逼近都是无效的。提出了假设TR是碰撞主导的理由。特别地,对平行于磁场的电场与Dreicer电场之比的自洽计算得出值10-3,这表明异常传输过程并不重要。强调了在对太阳大气中的加热机制进行建模时使用运输过程的真实描述的必要性。

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