Masses of Asteroids and the Total Mass of the Asteroid Main Belt
Transactions of IAA RAS, issue 31, 3–10 (2014)
Keywords: Solar System, asteroid belt, planet ephemerides, asteroid masses.
About the paperAbstract
An updated database of planet and spacecraft observations, as well as asteroid data, has been used to improve the asteroid (included main belt asteroid) masses and perturbations caused by them on the motion of Solar System bodies. The direct estimation of the dynamical mass was obtained for a part of asteroids from their gravitation impacts on other celestial bodies. The masses of other large asteroids were calculated from their diameters and estimated densities. The mass of all the remaining small asteroids is estimated from the total gravitational influence caused by a two-dimensional ring with a constant mass distribution in the ecliptic plane. The work is based on the new version of the EPM2013 ephemerides and more than 792 000 positional observations (mainly radar ones) of planets and spacecraft made from 1913 to 2012. It is our first experience with a two-dimensional asteroid ring with dimensions obtained from its observable width instead of one-dimensional rings which we considered in our previous versions of EPM ephemerides for modeling perturbations of small asteroids. As a result, the accuracy of the two-dimensional asteroid ring's mass has grown considerably; orbits of all planets are obviously improved, and a particularly important gain is that the formal uncertainties o f the planets' semi-major axes has been halved. The total mass of the main asteroid belt is found: Mbelt = (12.25 ± 0.19) 10^-10 MSun or ≈ 2.5 MCeres.
Citation
E. V. Pitjeva, N. P. Pitjev. Masses of Asteroids and the Total Mass of the Asteroid Main Belt // Transactions of IAA RAS. — 2014. — Issue 31. — P. 3–10.
@article{pitjeva2014,
abstract = {An updated database of planet and spacecraft observations, as well as asteroid data, has been used to improve the asteroid (included main belt asteroid) masses and perturbations caused by them on the motion of Solar System bodies. The direct estimation of the dynamical mass was obtained for a part of asteroids from their gravitation impacts on other celestial bodies.
The masses of other large asteroids were calculated from their diameters and estimated densities.
The mass of all the remaining small asteroids is estimated from the total gravitational influence caused by a two-dimensional ring with a constant mass distribution in the ecliptic plane.
The work is based on the new version of the EPM2013 ephemerides and more than 792 000 positional observations (mainly radar ones) of planets and spacecraft made from 1913 to 2012. It is our first experience with a two-dimensional asteroid ring with dimensions obtained from its observable width instead of one-dimensional rings which we considered in our previous versions of EPM ephemerides for modeling perturbations of small asteroids. As a result, the accuracy of the two-dimensional asteroid ring's mass has grown considerably; orbits of all planets are obviously improved, and a particularly important gain is that the formal uncertainties o f the planets' semi-major axes has been halved. The total mass of the main asteroid belt is found: Mbelt = (12.25 ± 0.19) 10^-10 MSun or ≈ 2.5 MCeres.},
author = {E.~V. Pitjeva and N.~P. Pitjev},
issue = {31},
journal = {Transactions of IAA RAS},
keyword = {Solar System, asteroid belt, planet ephemerides, asteroid masses},
pages = {3--10},
title = {Masses of Asteroids and the Total Mass of the Asteroid Main Belt},
url = {http://iaaras.ru/en/library/paper/1026/},
year = {2014}
}
TY - JOUR
TI - Masses of Asteroids and the Total Mass of the Asteroid Main Belt
AU - Pitjeva, E. V.
AU - Pitjev, N. P.
PY - 2014
T2 - Transactions of IAA RAS
IS - 31
SP - 3
AB - An updated database of planet and spacecraft observations, as well
as asteroid data, has been used to improve the asteroid (included
main belt asteroid) masses and perturbations caused by them on the
motion of Solar System bodies. The direct estimation of the dynamical
mass was obtained for a part of asteroids from their gravitation
impacts on other celestial bodies. The masses of other large
asteroids were calculated from their diameters and estimated
densities. The mass of all the remaining small asteroids is
estimated from the total gravitational influence caused by a two-
dimensional ring with a constant mass distribution in the ecliptic
plane. The work is based on the new version of the EPM2013
ephemerides and more than 792 000 positional observations (mainly
radar ones) of planets and spacecraft made from 1913 to 2012. It is
our first experience with a two-dimensional asteroid ring with
dimensions obtained from its observable width instead of one-
dimensional rings which we considered in our previous versions of EPM
ephemerides for modeling perturbations of small asteroids. As a
result, the accuracy of the two-dimensional asteroid ring's mass has
grown considerably; orbits of all planets are obviously improved, and
a particularly important gain is that the formal uncertainties o f
the planets' semi-major axes has been halved. The total mass of the
main asteroid belt is found: Mbelt = (12.25 ± 0.19) 10^-10 MSun or ≈
2.5 MCeres.
UR - http://iaaras.ru/en/library/paper/1026/
ER -