Radial Distribution of Electron Quasi-thermal Noise in the Inner Heliosphere

Yi-Lun Li, 逸伦 李, Ling Chen, 玲 陈, De-Jin Wu and 德金 吴
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Abstract

The electron population in the solar wind plasma can be described with three different components: a core, a halo, and a magnetic field aligned strahl. The electron quasi-thermal noise (QTN) is investigated by using an electron population model consisting of a core with a Maxwellian distribution and a halo with a kappa distribution, based on the empirical equations for electron density and temperature and the index for the kappa halo. The power spectra of the electron QTN are calculated at different heliocentric radial distances from 10 to 200 Rs. The dependence of the QTN spectrum and effective Debye length on model parameters, including the ratio of the halo to the core for the density and temperature, the kappa index, and the antenna length, is further discussed. The results show that the electron QTN spectrum consists of a plateau in the low-frequency band f < fpt, a peak at the total plasma frequency fpt, and a rapidly decreasing part in the high-frequency band f > fpt. The QTN peak and plateau level continuously decrease as the radial distance increases, with the peak’s shape changing due to the variation of the kappa index. Although the model parameters are variable, the QTN plateau level presents less than an order of change with these parameters changing greatly, and only a monotonic change of the plateau is shown when the parameters are close to the practical situation. The results can provide a reference for future deep-space exploration in the inner heliosphere, and also for the design of detectors.
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内太阳圈电子准热噪声的径向分布
太阳风等离子体中的电子群可以用三个不同的部分来描述:内核、光环和磁场对齐的 strahl。根据电子密度和温度的经验公式以及卡帕光环的指数,使用由麦克斯韦分布的内核和卡帕分布的光环组成的电子群模型对电子准热噪声(QTN)进行了研究。计算了在 10 到 200 Rs 的不同日心径向距离上的电子 QTN 功率谱。进一步讨论了 QTN 谱和有效德拜长度对模型参数的依赖性,包括密度和温度的晕核比、卡帕指数和天线长度。结果表明,电子 QTN 光谱由低频段 f < fpt 的高原、等离子体总频率 fpt 的峰值和高频段 f > fpt 的快速下降部分组成。随着径向距离的增加,QTN 峰值和高原水平不断降低,峰值的形状因卡帕指数的变化而改变。虽然模型参数是可变的,但这些参数变化较大时,QTN 高原水平的变化还不到一个数量级,只有当参数接近实际情况时,高原才会出现单调变化。这些结果可以为未来在内日球层的深空探测以及探测器的设计提供参考。
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