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7 - Scientific requirements for understanding the near-Earth asteroid population

Published online by Cambridge University Press:  12 October 2009

Alan W. Harris
Affiliation:
DLR Institute of Planetary Research, Berlin
Michael J. S. Belton
Affiliation:
Belton Space Exploration Initiatives
Thomas H. Morgan
Affiliation:
National Aeronautics and Space Administration, Washington DC
Nalin H. Samarasinha
Affiliation:
National Optical Astronomy Observatory
Donald K. Yeomans
Affiliation:
Jet Propulsion Laboratory, California Institute of Technology
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Summary

Introduction

The known NEA population contains a confusing variety of objects: there are many different “animals in the zoo” of near-Earth asteroids. Some NEAs are thought to be largely metallic, indicative of material of high density and strength, while some others are carbonaceous and probably of lower density and less robust. A number of NEAs may be evolved cometary nuclei that are presumably porous and of low density but otherwise with essentially unknown physical characteristics. In terms of large-scale structure NEAs range from monolithic slabs to “rubble piles” and binary systems (asteroids with natural satellites or moons). An asteroid that has been shattered by collisions with other objects may survive under the collective weak gravitational attraction of the resulting fragments as a cohesionless, consolidated, so-called rubble pile. A rubble pile may become a binary system if it makes a close approach to a planet and becomes partially disrupted by the gravitational perturbation. More than 20 NEAs in the currently known population are thought to be binary systems and many more are probably awaiting discovery.

The rate of discovery of NEAs has increased dramatically in recent years and is now seriously outstripping the rate at which the population can be physically characterized. The NEA population is still largely unexplored.

Which physical parameters are most relevant for mitigation considerations? Preventing a collision with an NEA on course for the Earth would require total destruction of the object, to the extent that the resulting debris poses no hazard to the Earth or, perhaps more realistically, deflecting it slightly from its catastrophic course.

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Publisher: Cambridge University Press
Print publication year: 2004

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