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首页> 外文期刊>Nonlinear Processes in Geophysics Discussions >Heliospheric pick-up ions influencing thermodynamics and dynamics of the distant solar wind
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Heliospheric pick-up ions influencing thermodynamics and dynamics of the distant solar wind

机译:影响热力学和遥远太阳风动力学的日球吸收离子

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Neutral interstellar H-atoms penetrate into the inner heliosphere and upon the event of ionization are converted into pick-up ions (PUIs). The magnetized solar wind flow incorporates these ions into the plasma bulk and enforces their co-motion. By nonlinear interactions with wind-entrained Alfvén waves, these ions are then processed in the comoving velocity space. The complete pick-up process is connected with forces acting back to the original solar wind ion flow, thereby decelerating and heating the solar wind plasma. As we show here, the resulting deceleration cannot be treated as a pure loading effect, but requires adequate consideration of the action of the pressure of PUI-scattered waves operating by the PUI pressure gradient. Hereby, it is important to take into proper account the stochastic acceleration which PUIs suffer from at their convection out of the inner heliosphere by quasi-linear interactions with MHD turbulences. Only then can the presently reported VOYAGER observations of solar wind decelerations and heatings in the outer heliosphere be understood in view of the most likely values of interstellar gas parameters, such as an H-atom density of 0.12 cm-3 . Solar wind protons (SWPs) appear to be globally heated in their motion to larger solar distances. Ascribing the needed heat transfer to the action of suprathermal PUIs, which drive MHD waves that are partly absorbed by SWPs, in order to establish the observed SWP polytropy, we can obtain a quantitative expression for the solar wind proton pressure as a function of solar distance. This expression clearly shows the change from an adiabatic to a quasi-polytropic SWP behaviour with a decreasing polytropic index at increasing distances. This also allows one to calculate the average percentage of initial pick-up energy fed into the thermal proton energy. In a first order evaluation of this expression, we can estimate that about 10% of the initial PUI injection energy is eventually transfered to SWPs independent of the PUI injection rate.
机译:中性星际H原子渗透到内部日球层,一旦发生电离,便会转换成吸收离子(PUI)。磁化的太阳风将这些离子结合到等离子体体中并强制它们共同运动。通过与风夹带的Alfvén波的非线性相互作用,这些离子然后在共同移动的速度空间中被处理。完整的拾取过程与作用回原始太阳风离子流的力有关,从而使太阳风等离子体减速并加热。正如我们在此处所示,所得的减速度不能视为纯粹的加载效果,而是需要充分考虑通过PUI压力梯度运行的PUI散射波的压力作用。因此,重要的是要适当考虑通过与MHD湍流的准线性相互作用,PUI在对流中从对流层内部受到的随机加速度。只有这样,鉴于星际气体参数的最可能值,例如H原子密度为0.12 cm-3,才可以理解目前报道的太阳系外层太阳风减速和加热的VOYAGER观测结果。太阳风质子(SWP)似乎在运动中被加热到更大的太阳距离。将必要的热传递归因于超热PUI的作用,该超热PUI驱使部分被SWP吸收的MHD波,以建立观测到的SWP多态性,我们可以获得太阳风质子压力随太阳距离的函数的定量表达式。 。该表达式清楚地显示了从绝热到准多向性SWP行为的变化,且随着距离的增加,多向性指数减小。这也使人们可以计算输入到热质子能量中的初始拾取能量的平均百分比。在此表达式的一阶评估中,我们可以估计大约有10%的初始PUI注入能量最终会独立于PUI注入速率转移到SWP。

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