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Two topics in the physics of the solar wind : 1. A model of Fermi acceleration at shock fronts. 2. Effects of diffusion on the composition of the solar corona and solar wind

机译:太阳风物理学中的两个主题:1。冲击前沿的费米加速模型。 2.扩散对日冕和太阳风组成的影响

摘要

1. A Model of Fermi Acceleration at Shock FrontsududA model of first order Fermi acceleration at shock fronts is developed. A "fast" hydromagnetic shock is assumed to be propogating toward an isolated magnetic mirror in an otherwise uniform magnetic field which is not parallel to the shock front. The behavior of an ensemble of particles trapped between the mirror and the shock is studied and a differential equation describing the balance of particle injection into the trapping region, loss through the shock or mirror, and energy gain is obtained. A general expression for n(W, t), the number of trapped particles as a function of energy and time is obtained. Useful limiting forms are discussed. Possible sources of particles eligible for acceleration are discussed and an attractive source is shown to be the quasi-thermalized plasma behind the shock, a small fraction of which may leak out in front of the shock and be accelerated. The flux of particles through the shock is found to be small and due mainly to convection with magnetic irregularities behind the shock. The energy spectrum of accelerated particles behind the shock is therefore expected to be nearly the same as in the trapping region.ududThe general theory is then applied to the acceleration of electrons at the earth's bow shock. This leads to an attractive model for the energetic electron pulses which have been observed beyond the magnetopause. The observations and their interpretation are discussed. If a small fraction of the ~ 1 keV electrons in the quasi-thermalized plasma behind the shock escape to the region in front of the shock, many quantitative features of the observed pulses are explained by a model in which each pulse is due to the acceleration of these electrons by a mirror approaching the bow shock. In particular, the cutoff in >30 keV pulses at a few earth radii beyond the shock is readily explained. The theory predicts, further, that cutoffs for more energetic particles should be at smaller distances from the shock. The observed energy spectra are in excellent agreement with the model. Some critical observations are suggested.udud2. Effects of Diffusion on the Composition of the Solar Corona and Solar WindududA simple model is developed with which it is possible to estimate quantitatively the effects of radial diffusion on the composition of the solar corona and solar wind. As it flows out to form the solar wind, it is assumed that each constituent satisfies the time independent equation of continuity n[subscript t]v[subscript t]r[superscript 2] = constant, where n[subscript t] and v[subscript t] are the number density and velocity of element t at heliocentric radius r. For typical coronal temperatures of 1 - 2 x 10[superscript 6] [degrees] K and solar wind fluxes of 3 x 10[superscript 8] protons cm[- superscript 2]sec[- superscript 1] at r = 1 AU, the relative diffusion velocities of ions and protons are a substantial fraction of the local solar wind velocity. This diffusion is found to be mostly due to the coronal pressure gradient, with the effect of the temperature gradient relatively unimportant. The large relative velocities together with the above continuity equation lead to substantial changes in the relative composition of the solar wind. Effects of magnetic fields and turbulent mixing are briefly considered. It is concluded that, in conjunction with the diffusion, they may lead to appreciable fluctuations of the composition as a function of time and heliocentric radius. The conclusions are in agreement with the observed behavior of the He/H ratio observed on Mariner-2.
机译:1.冲击前费米加速度的模型 ud ud建立了冲击前费米加速度的一阶模型。假定“快速”水磁冲击在不平行于冲击前沿的均匀磁场中朝隔离磁镜传播。研究了在反射镜和冲击之间捕获的粒子整体的行为,并描述了一个微分方程,该方程描述了粒子注入到捕获区域中的平衡,通过冲击或反射镜的损失以及能量增益。获得n(W,t)的一般表达式,即被俘获的粒子数与能量和时间的函数关系。讨论了有用的限制形式。讨论了适合加速的可能的粒子源,并显示了一个有吸引力的源是冲击后的准热等离子体,其中一小部分可能在冲击前泄漏并被加速。发现通过冲击的颗粒通量很小,并且主要是由于在冲击后具有不规则磁性的对流。因此,预计在冲击后的加速粒子的能谱几乎与在俘获区域中的能谱相同。 ud ud然后将一般理论应用于地球弓形冲击处电子的加速。这就产生了一个吸引人的高能电子脉冲模型,该模型已经在绝经期之后被观察到。讨论了观察结果及其解释。如果在激波后面的准热等离子体中一小部分〜1 keV电子逃逸到激波前面的区域,则所观察到的脉冲的许多定量特征可以通过模型解释,其中每个脉冲都归因于加速度这些电子通过反射镜接近弓形冲击。尤其是,很容易解释了在超过冲击的几个地球半径处> 30 keV脉冲的截止。该理论还预测,更多高能粒子的截止点应与电击相距较小的距离。观察到的能谱与模型非常吻合。建议一些重要的观察结果。 ud ud2。扩散对太阳日冕和太阳风成分的影响 ud ud建立了一个简单的模型,利用该模型可以定量估计径向扩散对太阳日冕和太阳风成分的影响。当它流出形成太阳风时,假定每个组成部分都满足与时间无关的连续性方程n [下标t] v [下标t] r [上标2] =常数,其中n [下标t]和v [下标[t]是元素t在日心半径r处的数量密度和速度。对于典型的日冕温度为1-2 x 10 [上标6] [度] K,太阳风通量为3 x 10 [上标8]质子cm [-上标2] sec [-上标1],在r = 1 AU时,离子和质子的相对扩散速度是当地太阳风速的很大一部分。发现这种扩散主要归因于冠状压力梯度,而温度梯度的影响相对不重要。大的相对速度与上述连续性方程一起导致太阳风的相对组成发生实质性变化。简要考虑了磁场和湍流混合的影响。结论是,与扩散一起,它们可能导致组成随时间和日心半径变化的明显波动。结论与在Mariner-2上观察到的He / H比行为一致。

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    Jokipii J. Randolph;

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  • 年度 1965
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