Planetary Orbits: Kepler s Laws 1/18/07
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1 Planetary Orbits: Kepler s Laws
2 Announcements The correct link for the course webpage The first homework due Jan 25 (available for download on website). Starry Night Backyard software program blue CD that comes with textbook Preceptors Please fill out a preceptor application. Please also give me your schedule on the back of the form Mission update volunteers? LPL Public Lecture Series next Tuesday
3 Today s Topics Finish discussion on Copernican revolution A long-standing Earth-centered view of the solar system is turned on its head with the invention of the telescope Phases of Venus The modern view of the solar system and the epiphany that gravity is important! Kepler s revision to the system devised by Copernicus Kepler s Laws Galileo s experiments on gravity Newton s law of universal gravitation
4 The Ptolemaic System
5 , Polish Nicholas Copernicus Re-proposed heliocentric theory Put the Sun at the center, but still believed the orbits of the planets were circles + epicycles He felt that this was a more natural explanation of the solar system
6 Tycho Brahe , Danish Nose cut off in duel by a fellow student Observed a supernova, and periodic comets Proof that the stars and planets are not constant, as the ancient astronomers believed Best pre-telescope observer Given island of Hven to build an observatory Best, most observations Still no parallax
7 , Italian Galileo Galilei Used telescope Jupiter s moons Lunar mountains, sunspots Phases of Venus Experiments on motion Including attempts to measure the speed of light Famous gravity experiment using the leaning tower of Pisa
8 Galileo also discovered four moons, now called the Galilean satellites, orbiting Jupiter The positions of these moons change rapidly and can be seen during the course of one evening Especially Io and Europa, the two closest to Jupiter
9 Jupiter and 3 of the Galilean satelites (only Callisto is missing from this amateur photograph) This is what Jupiter looks like through a standard amateur telescope. Galileo probably saw it similarly
10 Phases of Venus Galileo s observations of Venus s gibbous ( full-ish ) phase definitively ruled out Ptolemy s geocentric model!
11 The phases of Venus in the Ptolemaic Model only a crescent Venus is possible
12 The Phases of Venus in Heliocentric Model including the gibbous phase of Venus, as observed
13 Conclusion The 1000-year-old paradigm of a Earth-centered solar system, was proved incorrect as the result of simple observations made by a new technology -- the telescope. New technologies often lead to rewriting of textbooks. Current new technologies include Space age Super computers
14 Johannes Kepler proposed elliptical paths for the planets about the Sun Using data collected by Tycho Brahe, Kepler deduced three laws of planetary motion: 1. the orbits are ellipses 2. a planet s speed varies as it moves around its elliptical orbit 3. the orbital period of a planet is related to the size of its orbit
15 Kepler s First Law The planets move about the sun in elliptical orbits with the Sun at one foci of the ellipse Perihelion Aphelion
16 Semi-major axis The Semi-major axis is ½ the long width of the ellipse Planetary fact sheets usually quote the semi-major axis of the orbit
17 Ellipses Eccentricity a measure of how oblong an ellipse is.
18 Here are two elliptical orbits with the Sun at one focus. The orbits of most of the planets are nearly circles. But other objects, especially comets, have orbits with high eccentricities.
19 Kepler s Second Law The Planet sweeps out equal areas of the elliptical orbit, in equal time intervals The planet moves fastest when it is closest to the Sun and slowest when it is farthest away
20 Kepler s Third Law The square of a planet s period (P) is proportional to the cube of its semi-major axis (a). or The farther a planet is from the sun, the longer it takes to go around the sun P = the period (in years) a = semi-major axis (in AU)
21
22 A warning about this formula! It only applies to planetary motion about the Sun! Also, the units must be P in years, and a in AU. Otherwise you will NOT get the correct result P = the period (in years) a = semi-major axis (in AU)
23 Galileo discovered that the higher an object is dropped, the greater its speed when it reaches the ground All falling objects near the surface of the Earth have the same acceleration (9.8 m/s 2 ) Acceleration Due to Gravity The acceleration of gravity on the surface of other solar-system bodies depends on their mass and radius Mars and the Moon have a smaller acceleration of gravity Saturn is about the same as Earth Jupiter is more than Earth
24 Objects fall at the same rate independent of mass! Galileo s famous experiment Showed that objects of different masses dropped from the same height arrive to Earth at the SAME time Disproved Aristotle s theory Did he really do it? The experiment was also performed by an astronaut on the moon?
25 Astronaut Alan Bean Did Galileo s experiment on the Moon
26 Isaac Newton ( ) Developed the Laws of Motion Discovered the law of gravity Used physics to derive Kepler s 3 rd Law (see page 81 and box 4-4 of the textbook)
27 Newton s Law of Universal Gravitation Gravitation force between two bodies G = Gravitational Constant = 6.67x10-11 N m 2 / kg 2 m 1 and m 2 = the masses of the two objects r = the distance between the two (more precisely, the distance between the two centers)
28 Galilean Satellites and Kepler s Laws Newton derived Kepler s third law using physics and his universal law of gravitation. His form of Kepler s 3 rd law for the orbits of the planets about the Sun is:
29 Today s in-class activity You may work together in small (2-3 people) groups You must hand in your own work Please remain in your seats until we collect all of the finished activities After the activity is turned in, we will toss a coin to decide if it will be graded Heads it is graded Tails it will not be graded If time permits, we will go over the activity afterwards
30 Reading for next class Chapter 4 Box 4-2 (p. 67) Section 4-6, 4-7, 4-8 (pp ) Chapter 2 Section 2-3, 2-4, 2-5 (pp )
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