Basic Calculus of Planetary Orbits and Interplanetary Flight

2020 ◽  
Author(s):  
Alexander J. Hahn
2017 ◽  
Vol 2017 ◽  
pp. 1-6
Author(s):  
Wenxia Chen ◽  
Danping Ding ◽  
Xiaoyan Deng ◽  
Gang Xu

The evolution process of four class soliton solutions is investigated by basic calculus theory. For any given x, we describe the special curvature evolution following time t for the curve of soliton solution and also study the fluctuation of solution curve.


1989 ◽  
Vol 10 (4) ◽  
pp. 347-365
Author(s):  
M. Michalodimitrakis ◽  
F. Grigorelis

1976 ◽  
Vol 56 (1) ◽  
pp. 324-326 ◽  
Author(s):  
C. Hoenselaers
Keyword(s):  

1998 ◽  
Vol 13 (17) ◽  
pp. 1393-1400 ◽  
Author(s):  
D. V. AHLUWALIA

The local galactic cluster, the Great attractor, embeds us in a dimensionless gravitational potential of about -3×10-5. In the solar system, this potential is constant to about 1 part in 1011. Consequently, planetary orbits, which are determined by the gradient in the gravitational potential, remain unaffected. However, this is not so for the recently introduced flavor-oscillation clocks where the new redshift-inducing phases depend on the gravitational potential itself. On these grounds, and by studying the invariance properties of the gravitational phenomenon in the weak fields, we argue that there exists an element of incompleteness in the general relativistic description of gravitation. An incompleteness-establishing inequality is derived and an experiment is outlined to test the thesis presented.


2019 ◽  
Vol 621 ◽  
pp. A44
Author(s):  
D. Hidalgo ◽  
R. Alonso ◽  
E. Pallé

Phase curves, or the change in observed illumination of the planet as it orbits around its host star, help us to characterize their atmospheres. However, the variability of the host star can make their detection challenging. The presence of starspots, faculae, flares, and rotational effects introduce brightness variations that can hide other flux variations related to the presence of an exoplanet: ellipsoidal variation, Doppler boosting, and a combination of reflected light and thermal emission from the planet. Here we present a study to quantify the effect of stellar variability on the detectability of phase curves in the optical. In the first stage we simulated ideal data, with different white noise levels, and with cadences and total duration matching a quarter of the Kepler mission. We performed injection and recovery tests to evaluate the minimum number of planetary orbits that need to be observed in order to determine the amplitude of the phase curve with an accuracy of 15%. We also evaluate the effect of a simplistic stellar variability signal with low amplitude in order to provide strong constraints on the minimum number of orbits needed under these ideal conditions. In the second stage we applied these methods to data from Q9 of the Kepler mission, known for its low instrumental noise. The injection and recovery tests are performed on a selected sample of the less noisy stars in different effective temperature ranges. Even for the shortest explored planet period of 1 day, we find that observing a single orbit of the planet fails to detect accurately more than 90% of the inserted amplitude. The best recovery rates, close to 48%, are obtained after 10 orbits of a 1 day period planet with the largest explored amplitude of 150 ppm. The temperature range of the host stars providing better recovery ratios is 5500 K < Teff < 6000 K. Our results provide guidelines to selecting the best targets in which phase curves can be measured to the greatest accuracy, given the variability and effective temperature of its host star, which is of interest for the upcoming TESS, CHEOPS, and PLATO space missions.


The Geologist ◽  
1863 ◽  
Vol 6 (12) ◽  
pp. 441-444

Every day's experience confirms more and more the opinion that the central heat doctrine has less foundation than formerly it was supposed to possess. Its great supporters have gradually increased the necessary thickness of the solid crust in proportion to the internal supposed fluid core from forty to eight hundred miles at least: rather a wide difference in itself, but not perhaps so very great in respect to the absolute diameter of the earth, to which such a relationship would be about in proportion to the thickness of a sheet of cartridge-paper round a 12-inch globe. We know nothing, however, so perfectly a non-conductor that so thin would resist the heat of the internal molten mass. Moreover, upon the alleged increase of temperature with depth in coal and other mines, much doubt has been thrown by the subsequently ascertained facts that in many instances the higher temperatures have disappeared after the mines had ceased to be worked. The necessity, if the interior were fluid, for internal tides below the supposed solid crust, also militates against the existence of a fluid core, because we can detect no such tides at the surface of our earth; and if they existed, it is difficult to conceive the rigidity and strength of so thin a crust to be equal to restraining them entirely; and if the crust were in the least degree yielding or elastic, we must have evidence of such tides in the heavings of the surface.


Sign in / Sign up

Export Citation Format

Share Document