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arXiv 1002.4819astro-ph.EP
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撞击状态和形成后隔离过程:对类地行星中重惰性气体起源的影响

Impact regimes and post-formation sequestration processes: implications for the origin of heavy noble gases in terrestrial planets

Olivier Mousis, Jonathan I. Lunine, Jean-Marc Petit, Sylvain Picaud, Bernard Schmitt, Didier Marquer, Jonathan Horner, Caroline Thomas

摘要:

在金星、地球和火星上测得的氖、氩、氪和氙的大气丰度之间的差异是惊人的。由于这些丰度下降了至少两个数量级,从金星到火星,研究这种差异的起源是一个关键问题,必须解释,如果我们要充分了解不同的交付机制的挥发物吸积的类地行星。在这项工作中,我们的目标是调查是否有可能定量解释的变化,在金星,地球和火星上测量的重惰性气体丰度,假设彗星轰击是这些惰性气体的主要输送机制的类地行星。要做到这一点,我们使用最近的动力学模拟,使研究的影响通量的彗星在类地行星的形成和演化过程中。假设彗星释放的惰性气体的质量与它们与类地行星碰撞的速率成正比,我们证明了金星和地球中的氪和氙丰度可以用符合彗星轰击假说的方式来解释。为了解释地球和火星之间氪和氙丰度的差异,我们需要援引火星土壤中大量以CO2为主的包合物的存在,这些包合物可以有效地隔离这些惰性气体。

英文摘要:

The difference between the measured atmospheric abundances of neon, argon, krypton and xenon for Venus, the Earth and Mars is striking. Because these abundances drop by at least two orders of magnitude as one moves outward from Venus to Mars, the study of the origin of this discrepancy is a key issue that must be explained if we are to fully understand the different delivery mechanisms of the volatiles accreted by the terrestrial planets. In this work, we aim to investigate whether it is possible to quantitatively explain the variation of the heavy noble gas abundances measured on Venus, the Earth and Mars, assuming that cometary bombardment was the main delivery mechanism of these noble gases to the terrestrial planets. To do so, we use recent dynamical simulations that allow the study of the impact fluxes of comets upon the terrestrial planets during the course of their formation and evolution. Assuming that the mass of noble gases delivered by comets is proportional to rate at which they collide with the terrestrial planets, we show that the krypton and xenon abundances in Venus and the Earth can be explained in a manner consistent with the hypothesis of cometary bombardment. In order to explain the krypton and xenon abundance differences between the Earth and Mars, we need to invoke the presence of large amounts of CO2-dominated clathrates in the Martian soil that would have efficiently sequestered these noble gases.

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