1 / 10

The Two-body Equation of Motion

The Two-body Equation of Motion. Newton’s Laws gives us:. The solution is an orbit described by a conic section (circle, ellipse, parabola, or hyperbola) that is fixed in space The satellite will trade kinetic energy for potential energy (speed for altitude) as it moves around in orbit

london
Download Presentation

The Two-body Equation of Motion

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. The Two-body Equation of Motion Newton’s Laws gives us: • The solution is an orbit described by a conic section (circle, ellipse, parabola, or hyperbola) that is fixed in space • The satellite will trade kinetic energy for potential energy (speed for altitude) as it moves around in orbit • We need six initial conditions to solve this equation • The six Classical Orbital Elements (a, e, i, W, w, n) are often used to visualize the location and motion of the satellite

  2. Classical Orbital Elements Orbit Size: Semi-major Axis a Orbit Shape: Eccentricity e Orbit Tilt: Inclination i Orbit Twist: Right Ascension of Ω the Ascending Node Orbit Rotation: Argument of Perigee ω Satellite Location: True Anomaly 

  3. Size: Semi-Major Axis (a) US: Fig. 5-2 • How big is an orbit? We measure the length of the longest side of the ellipse and, by convention, divide it in half • Orbit size depends on how fast we “throw” our satellite into orbit • The faster we throw it, the more energy its orbit has and the bigger its orbit is

  4. Shape: Eccentricity (e) e = .8 e = .5 e = .7 US, Fig. 5.3 e = 0 (circular) Circle e = 0.0 Ellipse e = 0.0 to 1.0 Parabola e = 1.0 Hyperbola e > 1.0

  5. Tilt: Inclination (i) Inclination K h i Angular momentum vector Equatorial Plane

  6. Tilt: Inclination (i) US: Table 5-2

  7. Twist: Right Ascension of the Ascending Node () Vernal Equinox Direction (Originally pointed to the constellation Aries, the Ram) Equatorial Plane Ascending Node  Right Ascension of the Ascending Node (Also called the Longitude of the Ascending Node) We measure how an orbit is twisted by locating its ascending node relative to the vernal equinox direction (in the equatorial plane)

  8. Rotation: Argument of Perigee () Argument of Perigee  Equatorial Plane Ascending Node Perigee (Point Closest to the Earth) We locate perigee relative to the ascending node (in the orbit plane)

  9. Satellite Location: True Anomaly () Equatorial Plane  True Anomaly Perigee (Point Closest to the Earth) Finally, we locate the satellite relative to perigee, (in the orbit plane)

  10. Classical Orbital Elements w 2a K i e = .8 h   Vernal Equinox Direction Ascending Node Perigee

More Related