๐”– Bobbio Scriptorium
โœฆ   LIBER   โœฆ

A Model of Orbital Diffusion

โœ Scribed by T.B. Smith


Publisher
Elsevier Science
Year
2001
Tongue
English
Weight
73 KB
Volume
151
Category
Article
ISSN
0019-1035

No coin nor oath required. For personal study only.

โœฆ Synopsis


It has been reported (Chapman et al. 1989, in Asteroids II, edited by R. P. Binzel, T. Gehrels, and M. S. Matthews, Univ. of Arizona Press, Tucson, p. 386) that the shapes of asteroid families tend to be asymmetric, with a relative flattening along the line toward the Sun. This article addresses that observation. We develop a simple model for this, with an initially localized cluster circularly orbiting the Sun in the ecliptic plane, and acted upon by a background of weak stochastic forces. The model's linearized equations of motion are such that a component of random force, perpendicular to the radius, acts back to affect the radial motion. The result is a flattening, over time, toward the Sun.


๐Ÿ“œ SIMILAR VOLUMES


A diffusion model for rinsing
โœ John A. Tallmadge; Bryan A. Buffham; Robert R. Barbolini ๐Ÿ“‚ Article ๐Ÿ“… 1962 ๐Ÿ› American Institute of Chemical Engineers ๐ŸŒ English โš– 624 KB
A Diffusion Model for Phyllotaxis
โœ Akira Yotsumoto ๐Ÿ“‚ Article ๐Ÿ“… 1993 ๐Ÿ› Elsevier Science ๐ŸŒ English โš– 567 KB

The mechanism of phyllotaxis is examined by computer simulation based on an inhibitor diffusion model in which the inhibitor is secreted from each new leaf formed at a shoot apex. It is assumed that leaf initiation can only take place in competent tissue which is in an initiation ring. Initiation oc

A simple model of solvation within the m
โœ J.Oakey Noell; Keiji Morokuma ๐Ÿ“‚ Article ๐Ÿ“… 1975 ๐Ÿ› Elsevier Science ๐ŸŒ English โš– 496 KB

A simple model of salvation within the molecular orbital method is proposed whereby the efiect of solvent molecuies is simulated by the inclusion of fractional point charges at the solvent atomic centers. The method is applied to three salvation problems: the hydr;ltion of Li+ and F-nnd the solvztio