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UDC 629.78
Technical mechanics, 2019, 3, 54 - 65
ESTIMATION OF THE POSSIBLE ATMOSPHERIC DENSITY FOR DIFFERENT ORBITAL FLIGHT CONDITIONS
DOI:
https://doi.org/10.15407/itm2019.03.054
Maslova A. I.
Maslova A. I.
Institute of Technical Mechanics of the National Academy of Sciences of Ukraine and the State Space Agency of Ukraine
Improving the quality of Earth remote sensing systems is largely due to the development of spacecraft motion
control algorithms. A new control problem is to maintain given orbit parameters over a long period of time.
To do this, it is proposed to constantly (continuously or discretely) counteract disturbing actions on the
spacecraft. The capabilities of modern electrojet engines make it possible to counteract significant
aerodynamic actions. This, in its turn, opens up possibilities of reducing the range of working orbits
for remote sensing spacecraft to unconventionally low (very low or superlow) orbits of altitude about 300 km.
Such superlow orbits for remote sensing spacecraft` have a number of advantages.
In low Earth orbits, one of the main disturbing actions is aerodynamic drag. Its estimation is necessary
at the preliminary design stage of spacecraft power supply systems when developing requirements
for disturbance-counteracting engines. The purpose of this paper is to estimate the possible atmospheric
density, which would allow one to quickly conduct pre-design calculations of the aerodynamic drag on the
spacecraft for given orbital flight conditions. The density was estimated using the Standard GOST
R 25645.166 – 2004, “The Earth’s Upper Atmosphere. Density Model for Ballistic Support of Satellite
Flights,” depending on the altitude and a fixed level of solar activity. In doing so, the effect
of the following factors on the atmospheric density was considered: the daily effect, the semi-annual
effect, and the effect of solar and geomagnetic activity. The coefficients that describe the effect
of these factors were estimated at altitudes of 300 to 700 km, and the conditions under which these
coefficients and the atmospheric density take extreme (maximum/minimum) were determined. As an example,
it was shown that at an altitude of 300 km, the density can theoretically vary by more than two orders
of magnitude (from 1.07e-12 kg/m3 to 1.22e-10 kg/m3). The results presented in this paper allow one
to quickly estimate the possible range of the aerodynamic drag on the spacecraft.
atmospheric density, estimated values, maximum and minimum value
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7. Standard GOST R 25645.166 - 2004. The Earth's Upper Atmosphere. Density Model for Ballistic Support of Satellite Flights. Introduced on March 9, 2004. Moscow: Standard Publishing House, 2004. 24 pp. (in Russian).
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9. Maslova A. I., Pirozhenko A. V. Atmosphere density changes caused by the motion of spacecrafts in low Earth orbits. Kosm. Nauka Tehnol. 2009. V. 15. No. 1. Pp. 13-18. (in Russian).
https://doi.org/10.15407/knit2009.01.013
10. Space Weather Website. URL: http://www.spaceweather.com
DOI:
https://doi.org/10.15407/itm2019.03.054
Copyright (©) 2019 Maslova A. I.
Copyright © 2014-2019 Technical mechanics
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