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Titan's hydrodynamically escaping atmosphere: Escape rates and the structure of the exobase region

机译:土卫六的流体动力逃逸大气:逃逸率和外碱区域的结构

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In Strobel [Strobel, D.F., 2008. Icarus, 193, 588-594] a mass loss rate from Titan's upper atmosphere, ~ 4.5 × 10~(28) ? amu s~(- 1), was calculated for a single constituent, N_2 atmosphere by hydrodynamic escape as a high density, slow outward expansion driven principally by solar UV heating due to CH_4 absorption. It was estimated, but not proven, that the hydrodynamic mass loss is essentially CH_4 and H_2 escape. Here the individual conservation of momentum equations for the three major components of the upper atmosphere (N_2, CH_4, H_2) are solved in the low Mach number limit and compared with Cassini Ion Neutral Mass Spectrometer (INMS) measurements to demonstrate that light gases (CH_4, H_2) preferentially escape over the heavy gas (N_2). The lightest gas (H_2) escapes with a flux 99% of its limiting flux, whereas CH_4 is restricted to ≥75% of its limiting flux because there is insufficient solar power to support escape at the limiting rate. The respective calculated H_2 and CH_4 escape rates are 9.2 × 10~(27) and 1.7 × 10~(27) ? s~(- 1), for a total of ~ 4.6 × 10~(28) ? amu s~(- 1). From the calculated densities, mean free paths of N_2, CH_4, H_2, and macroscopic length scales, an extended region above the classic exobase is inferred where frequent collisions are still occurring and thermal heat conduction can deliver power to lift the escaping gas out of the gravitational potential well. In this region rapid acceleration of CH_4 outflow occurs. With the thermal structure of Titan's thermosphere inferred from INMS data by Müller-Wodarg et al. [Müller-Wodarg, I.C.F., Yelle, R.V., Cui, J., Waite Jr., J.H., 2008. J. Geophys. Res. 113, doi:10.1029/2007JE003033. E10005], in combination with calculated temperature profiles that include sputter induced plasma heating at the exobase, it is concluded that on average that the integrated, globally average, orbit-averaged, plasma heating rate during the Cassini epoch does not exceed ~ 5 × 10~8 ? eV cm~(- 2) s~(- 1) (~ 0.0008 ? erg cm~(- 2) s~(- 1)).
机译:在Strobel [Strobel,D.F.,2008. Icarus,193,588-594]中,土卫六高层大气的质量损失率为〜4.5×10〜(28)? amu s〜(-1)是通过水动力逸出以高密度,缓慢向外扩展(主要是由于吸收了CH_4的太阳紫外线加热)而计算出的单一成分N_2大气的amu s〜(-1)。据估计但没有证明,流体动力质量损失基本上是CH_4和H_2逸出。在这里,在低马赫数限制下求解了高层大气的三个主要成分(N_2,CH_4,H_2)的动量方程的守恒,并与卡西尼离子中性质谱仪(INMS)的测量结果进行了比较,证明了轻质气体(CH_4 ,H_2)优先逸出重气(N_2)。最轻的气体(H_2)以其极限通量的99%的通量逃逸,而CH_4被限制为其极限通量的≥75%,因为没有足够的太阳能来支持极限率的逃逸。分别计算出的H_2和CH_4逃逸率分别为9.2×10〜(27)和1.7×10〜(27)≤1.7。 s〜(-1),总计约为4.6×10〜(28)? amu s〜(-1)。根据计算出的密度,N_2,CH_4,H_2的平均自由程和宏观长度尺度,可以推断出经典外底之上的扩展区域,该区域仍在发生频繁的碰撞,并且热传导可以提供动力,将逸出的气体从管道中排出。引力势良好。在该区域中,CH_4流出迅速加速。根据Müller-Wodarg等人从INMS数据推论得出的泰坦热圈的热结构。 [Müller-Wodarg,I.C.F.,Yelle,R.V.,Cui,J.,Waite Jr.,J.H.,2008. J. Geophys。 Res。 113,doi:10.1029 / 2007JE003033。 [E10005],结合计算出的温度曲线,包括在外底处的溅射诱导的等离子体加热,得出的结论是,平均而言,卡西尼时期的整体,全球平均,轨道平均的等离子体加热速率不超过〜5×10 〜8? eV cm〜(-2)s〜(-1)(〜0.0008?erg cm〜(-2)s〜(-1))。

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