Spacecraft Dynamics and Control

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Transcription:

Spacecraft Dynamics and Control Matthew M. Peet Arizona State University Lecture 1: In the Beginning

Introduction to Spacecraft Dynamics Overview of Course Objectives Determining Orbital Elements Know Kepler s Laws of motion, Frames of Reference (ECI, ECEF, etc.) Given position and velocity, determine orbital elements. Given orbital elements and time, determine position + velocity. Plan Earth-Orbit Transfers Identify Required Orbit. Find Optimal Transfer. Determine Thrust and Timing. Plan Interplanetary Transfers Design Gravity-Assist Maneuvers. Use Patched-Conics. Linear Orbit Theory (Perturbations) Earth-Oblateness Drag Solar Wind Orbit Estimation M. Peet Lecture 1: Spacecraft Dynamics 2 / 23

Introduction to Spacecraft Dynamics Other Topics Things we may cover. Satellite Dynamics Pointing, Tracking Problems Vibration Damping 6 DOF motion Controllers Control Moment Gyros Spin Stabilization Gravity-Gradient Stabilization Attitude Thrusters Propulsion Chemical Rockets Nuclear Rockets Solar Sails Ion engines Gravity Assist 3-body orbits Ground Tracking M. Peet Lecture 1: Spacecraft Dynamics 3 / 23

The Two-Body Problem The class in a nutshell Modeling the system is 90% of the problem. M. Peet Lecture 1: Spacecraft Dynamics 4 / 23

Ptolemy (ca. 100-178 AD) Ptolemy observed that the moon and sun move in a circular motion about the spherical earth (daily and yearly). Wrote the Almagest Hypothesizes that all planets move in a similar manner. Beat out Sun-centered, rotating-earth model of Aristarchus. M. Peet Lecture 1: Spacecraft Dynamics 5 / 23

Concentric Circles: Daily Motion Yearly Motion Other Epicycles Allowed for accurate predictions Equinoxes Eclipses Latitude M. Peet Lecture 1: Spacecraft Dynamics 6 / 23

Copernican Fix (1473-1543) Increasing accuracy of observation made model of Ptolemy obsolete 1. Swap earth/sun. 2. Earth is spinning. 3. Moon still orbits earth Question: Would Ptolemy have won without the moon? M. Peet Lecture 1: Spacecraft Dynamics 7 / 23

Copernican Model Positives Aesthetically Appealing Epicycles are much smaller Less movement/rotation Intuitively appealing Negatives No physical Explanation Relies on Metaphysics, not physics No proof No empirical validation Still assumes circular orbits at constant speed Still requires Epicycles, albeit smaller ones M. Peet Lecture 1: Spacecraft Dynamics 8 / 23

Galileo Galilei (1564-1642) The Ptolemy Model was Disproven by the observations of Galileo Built the first decent telescope Observed the moons of Jupiter. Showed that planets could orbit other planets Observed the phases of venus. Death blow for Ptolemy s model An incorrect theory of tides. Imprisoned by church. M. Peet Lecture 1: Spacecraft Dynamics 9 / 23

Tycho Brahe (1546-1601) Tycho Brahe was a man with A fake nose (silver-gold alloy) A colorful personality A very bad model M. Peet Lecture 1: Spacecraft Dynamics 10 / 23

Tycho Brahe (1546-1601) However, he also had very good Equipment and Methodology. Most accurate pre-telescope equipment available Would catalogue the all relevant stars every night. Refused to share data. Data was stolen by Kepler post-mortem. M. Peet Lecture 1: Spacecraft Dynamics 11 / 23

Johannes Kepler (1571-1630) Contemporary with Sir Francis Bacon (1561-1626), father of empirical science. Became an assistant to Tycho in order to get access to data. Rudophine Tables. Primarily observed the motion of Mars Formulated experimentally the three laws of planetary motion No derivation. Postulated that earth exhibits a central force. A correct theory of tides. Ignored by Galileo, Descartes M. Peet Lecture 1: Spacecraft Dynamics 12 / 23

First Law of Planetary Motion Law 1: Planets move in elliptic orbits with one focus at the planet they orbit. The ellipse is a well-understood mathematical concept from geometry There are several well-studied parameters of the ellipse a - semi-major axis b - semi-minor axis e - eccentricity M. Peet Lecture 1: Spacecraft Dynamics 13 / 23

Second Law of Planetary Motion Law 2: Planets sweep out equal areas of the ellipse in equal time. First model to posit that planets slow down and speed up. Ṡ is constant for each planet Allows for quantitative predictions of locations and time. Allowed him to formulate Rudophine tables. M. Peet Lecture 1: Spacecraft Dynamics 14 / 23

Third Law of Planetary Motion Law 3: The square of the period of the orbit is proportional to the cube of the semi-major axis. A simple corollary of the second law? Second law applies to each orbit Area of ellipse: Area ellipse = a 2 1 e 2 Third law implies the rate of sweep changes from orbit to orbit M. Peet Lecture 1: Spacecraft Dynamics 15 / 23

More on Kepler s model Got almost everything right Postulated a central-force hypothesis First theory based on physics. Remember, to three laws of motion, so no inertia. Created a correct explanation for tidal motion Made the most accurate predictions Kepler s model was not initially accepted ignored by big names (Galileo, Descartes, etc.) Galileo had his own tides model Used but not believed Still no physical explanation. Must wait almost 60 years for an explanation. M. Peet Lecture 1: Spacecraft Dynamics 16 / 23

Isaac Newton (1643-1727) Most influential person in history? A quantitative model for motion Discovered differential equations Discovered modeling nature using equations Now we can use differential equations to model Everything. Newton used differential equations to model Force Velocity Acceleration Inertia Gravity M. Peet Lecture 1: Spacecraft Dynamics 17 / 23

PhilosophiæNaturalis Principia Mathematica Three Laws of Motion: Law 1 Every body remains at rest or in uniform motion unless acted upon by an unbalanced external force. Law 2 A body of mass m, subject to force F, undergoes an acceleration a where F = ma Law 3 The mutual forces of action and reaction between two bodies are equal, opposite and collinear. (In popular culture: Every action creates an equal and opposite reaction.) Law of Universal Gravitation: All bodies exert a force on all others Proportional to mass Inversely proportional to the square of the distance F = G m1m2 r 2 From this, Newton derived Kepler s laws of planetary motion. Or perhaps derived universal gravitation from Kepler s laws. M. Peet Lecture 1: Spacecraft Dynamics 18 / 23

Some other contributions Also discovered Refracting Telescope Integral calculus Infinite sequences and series Model for wave motion Theory of Color Speed of Sound Algorithms for solving nonlinear equations Newton s method is still the most common optimization algorithm. We will use it in this class. M. Peet Lecture 1: Spacecraft Dynamics 19 / 23

The model The Two-Body Problem Recall the force on mass 1 due to mass 2 is m 1 r1 = F 1 = G m 1m 2 r 12 3 r 12 where we denote r 12 = r 2 r 1. Clearly r 12 = r 21. The motion of mass 2 due to mass 1 is m 2 r2 = F 2 = G m 2m 1 r 21 3 r 21 The problem is a nonlinear coupled ODE with 6 degrees of freedom. Solution: Consider relative motion (only r 12 ) r 12 = G(m 1 + m 2 ) r 12 3 r 12 This is our model. M. Peet Lecture 1: Spacecraft Dynamics 20 / 23

Orbital Mechanics In this class, we study Definition 1. Orbital Mechanics is the study of motion about a center of mass. More generally, the field is Definition 2. Celestial Mechanics is the study of heavenly bodies Also includes Black holes Dark matter Big Bang Theory Relativistic mechanics We will stick to orbits. M. Peet Lecture 1: Spacecraft Dynamics 21 / 23

Conclusion In this Lecture, you learned: History Orbital mechanics is old Much of science was developed as part of the foundation of this discipline The Model Physical Modeling Models using differential equations Empirical Science Universal Gravitation Two-Body Problem 3DOF equations of relative motion M. Peet Lecture 1: Spacecraft Dynamics 22 / 23

Next Lecture: The two-body problem Universal Invariants Angular Momentum Linear Momentum N-body Problem Introduction Invariants Derivation of Kepler s Laws Kepler s First Law M. Peet Lecture 1: Spacecraft Dynamics 23 / 23