The range of validity of the two-body approximation in models of terrestrial planet accumulation: I. Gravitational perturbations
The range of validity of the two-body approximation in models of terrestrial planet accumulation: I. Gravitational perturbations
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类地行星堆积模型中二体近似的有效性范围:一、引力摄动
DOI:
10.1016/0019-1035(84)90137-4
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发表时间:
1984
期刊:
影响因子:
3.2
通讯作者:
L. Cox
中科院分区:
文献类型:
--
作者:
G. Wetherill;L. Cox
Gravitational perturbations in semimajor axis, eccentricity, and inclination resulting from close planetesimal encounters (near 1 AU) out to 10 Tisserand sphere of influence radii were calculated by two- and three-dimensional numerical integration. These are compared with the results of treating the encounter as a two-body problem, as is customary in Monte Carlo calculations of orbital evolution and in numerical and analytical studies of planetary accumulation. It is found that for values of ( V Ve) ⪅ 0.35 (V = relative velocity , Ve= escape velocity of largest body ) , the two-body body approximation fails to describe the outcome of individual encounters. In this low-velocity region, the two-body “gravitational focusing” cross section is no longer valid; “anomalous gravitational focusing” often leads to bodies on distant unperturbed trajectories becoming close encounters and vice versa. In spite of these differences, average perturbations given by the two-body approximation are valid within a factor of 2 when V Ve> 0.07 . In this same velocity range the “Arnold extrapolation,” whereby a few very close encounters are used to estimate the effect of many more distant encounters, is found to be a useful approximation.