[meteorite-list] Asteroid orbital evolution
From: Matson, Robert D. <ROBERT.D.MATSON_at_meteoritecentral.com>
Date: Fri, 15 Oct 2010 09:43:47 -0700 Message-ID: <9180F6B27399C541B10663E21C8BDE9269FE11_at_0461-its-exmb09.us.saic.com> Hi Bob and List, > When I give presentations to groups about meteorites, I often get asked this > question, "After all this time, what would cause an asteroid to depart from > its orbital confines in the "asteroid belt" and to end up crossing the > Earth's orbit?" > Now I can give a graphical answer by pointing to the (new) images in this > most recent article: > <http://www.dailymail.co.uk/sciencetech/article-1320385/Asteroid-collisi on-90million-miles-Earth-caught-NASA-camera.html> (Massive collision between two asteroids 90 million miles from Earth caught on camera for first time) While collisions in the Main Belt provide a potential mechanism for producing asteroids in earth-crossing orbits, this is not the main source of near-earth asteroids. Usually, Main Belt inter-asteroid collision velocities are quite slow (a few hundred meters per second), which is far too low a delta-V to transform a Main Belt orbit into a planet-crossing one. The real delivery mechanism is orbital resonance, the most efficient of which is the nu-6 secular resonance. (When the Greek letter nu is transcribed to English, you'll usually see this resonance written as v6.) The v6 resonance zone is at a distance of roughly 2 a.u., and the most likely asteroid family to inject asteroids into the v6 resonance is the well-populated Flora family. Once in the v6 resonance zone, the eccentricity of an asteroid's orbit starts to get "pumped up": as the centuries go by, the orbit shape becomes less circular and instead more elongated. The asteroid's perihelion progressively decreases from 2 a.u., to 1.9, 1.8, 1.7 and so on, while its most distant point from the sun progressively increases (2.1, 2.2, etc.) Eventually, the perihelion has decreased so much that the asteroid crosses Mars' orbit (mean distance 1.52 a.u.), possibly even impacting Mars itself, or getting flung by Mars' gravity into an even more eccentric orbit that crosses that of earth. This series of events is the main way that meteorites are delivered to earth. To summarize: 1. Inter-asteroid collisions in the Main Belt produce asteroids with orbits that evolve into Flora-like orbits (inner Main Belt) 2. Further collisions or perturbations of inner Main Belt objects nudges them into the nearby v6 secular resonance. 3. v6 secular resonance operates quickly (roughly a million years), transforming the orbit into a Mars-crossing one. 4. One or more close encounters with Mars further perturb the orbit into an earth-crossing one. 5. Eventually the earth-crossing asteroid and the earth itself happen to be at the same place at the same time and voila: meteorites! The most common meteorites on earth (L chondrites, representing 38% of all meteorites) are believed to have come directly from the Flora family. --Rob Received on Fri 15 Oct 2010 12:43:47 PM PDT |
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