The Heating of the Solar Wind by Alfvenic Fluctuations
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摘要: 本文采用了空间飞船Helios 1和2在0.3AU到0.9AU之间对太阳风高速流的观测数据,检验了Alfvén脉动对太阳风加热的理论以及Alfvén脉动的衰减机制。计算表明,在Helios观测的空间范围内,(1)若脉动耗散的能量转化为质子的热能,由能量守恒方程计算出的质子温度的径向变化与观测一致;(2)经典粘性衰减机制预计的能量耗散率与实测结果相差很大,因而不能解释脉动能量转化为质子能量的过程;(3)波能串级模式预计的能量耗散率与实测一致,说明太阳风质子的加热很可能是由于串级到质子迴旋频率范围的脉动能量转化为质子的热能所致。Abstract: The theory of the heating of the solar wind by the Alfvenic fluctuation and two models for the attenuation of the Alfvenic fluctuation (Viscous model and Wave energy cascading model) have been tested against the observed data by Helios 1 and 2. The calculation showed that, in the space range where Helios observed, (1) from the energy equation under the assumption that the Alfvenic fluctuations changes into the heat energy of the solar wind protons, the calculated radial variation of the temperature of the solar wind protons agrees with the observed results; (2) the rate of the energy dissipation of the fluctuations predicted by the viscous model is different from the observed results. The difference is about 8 orders, so it can not discribe the process of the energy dissipation; (3) the rate of energy dissipation of the fluctuations predicted by the wave energy cascading model agrees with the observed results. The possible mechanism of the heating of the solar wind protons is the dissipation of the energy cascading to the frequency range of the proton gyro-frequency.
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