Gravitation Part III. Orbits
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1 VLA/LWA Tour Saturday Sept 29 (avoid fall break) Depart 9am from PandA parking lot 10am: pickup burritos in Socorro 11am: Arrive at VLA gift shop 1pm: Lunch at VLA 3:30pm: Return to PandA parking lot
2 Gravitation Part III Orbits
3 Supermassive (3 million solar mass) Black Hole at the Galactic Center 3
4 Orbit of S2 P =15.6 yrs a = 955 AU e = i = From Keplar s 3 rd law M = a 3 /P 2 = 3.6 x 10 6 M sun
5 Satellites Remote Sensing: Weather forecasting Tracking hurricanes Soil moisture and other climate data Astronomy (Chandra, Swift, Fermi, Hubble,...) Communications Spy satellites 5
6 Space Debris Launching satellites and probes At last count US strategic command says there are more than 22,000 man-made objects 10 cm and larger, and NASA estimates could be few x 10 5 or even 10 6 smaller, nontrackable pieces of debris. Right: Region of space within 2000 km of Earth surface to show most concentrated area for orbital debris. Tragedy of the commons 6
7 Space Debris Telkom-1 in August 2017 explodes Need to have plan to de-orbit (or move to graveyard orbit ) all vehicles at end of life Need to clean up LEO and GEO 7
8 The Importance of Orbits More examples: Can use to measure masses (most fundamental way of measuring masses of stars, their most fundamental property) Clues to origin and history of whatever is orbiting (e.g. comet orbits imply huge reservoirs of unseen comets, orbits of stars and gas in galaxies imply existence of Dark Matter). 8
9 Gravity's predictive power Halley's comet: Edmund Halley found orbit of 1682 comet appeared similar to other comets spotted 1607 and 1537 => predicted it would return in 1758/59. It did! The discovery of Neptune: 1781 Herschel discovered Uranus, but by 1840 the predicted positions were much offset from measured => gravitational influence from other body. The 8th planet found 1845!
10 Generalized form of Kepler's 3rd law P 2 = 4 G( m π m 2 ) a 3 a is mean separation of the two objects over the orbit. The solar system is a special case: if m 1 is the mass of the Sun, it is much larger than the mass of any planet (even Jupiter is 1000x less massive), so m 1 +m 2 ~ M sun. 10
11 Universal - valid everywhere Example: At what height above the surface of the Earth are geosynchronous satellites located? Geosynchronous orbits are defined to keep the satellite above the same place on Earth, which means they have a period P=23.93 hrs (why not 24 hrs?). a is mean separation of the objects. For circular orbits where one is much more massive, a is approximately the orbit radius of the less massive one. 11
12 P = hr/day 3600 s/hr = s m 1 + m 2 m Earth = kg 2 3 GP m a = 2 4π a = Earth = 11 m = 42,100 km 3 m /kg/s 2 ( π 4 s) 2 ( kg) = m 3 Now subtract off Earth s radius to get the altitude: 35,750 km. Can you have a geosynchronous satellite anywhere else than above the equator? 12
13 Weight versus mass reminder Mass is a measure of how much matter an object has Weight is a measure of how strong gravity pulls on the object Weight is felt by the support given to us by the floor, seat, etc. The mass stays the same no matter what force acts upon an object Is your mass greater or smaller on Mars than on the Earth? 13
14 Weightlessness Astronauts on the space shuttle feel weightless because: a) there is no gravity in space and they do not weigh anything. but then what would make them orbit in the first place? b) space is a vacuum and there is no gravity in a vacuum. c) they are in free-fall where the net force on them is zero. right! not true d) the astronauts are far from Earth's surface at a location where gravitation has a minimal affect. Hm, at 400 km orbit, g is reduced from 9.8 to 8.7 m/s 2 - not enough 14
15 Weightlessness is a sensation Weightlessness In orbit no force counteracts gravity - you are constantly accelerating. In "free-fall". So is the shuttle and everything in it. So it does not push up on you like the Earth does => simulates gravity-free environment 15
16 Paths A-F correspond to harder and harder throws. If throws are hard enough, rock misses the Earth completely! Cases D-F are orbits of the rock around the Earth. The type of orbit depends on the injection velocity. DEMO Projectile Motion
17 The Coriolis Effect First described by the French physicist Gustave Coriolis 1835 An effect of viewing straight-line motion from a rotating frame of reference. On Earth, it results in an apparent deflection of a projectile Example: fire a cannonball due north from the equator. 17
18 The cannon is also moving east with the rotation of the Earth at 1670 km/h. The cannonball retains this initial eastward speed as it travels north (Newton's first law). But the further north it gets, the slower is the eastward motion of the Earth's surface beneath. Result is an eastward deflection of the cannonball with respect to its initial trajectory northward. 18
19 The same happens if you fire your cannonball to the south. What about projectile fired south from north pole? 19
20 Earth's rotation speed vs. latitude Equator rotation speed: 1670 km/h Rotation speed greatest at the equator, and decreases with increasing latitude, as the distance covered in 1 day is less (2πx) Figure shows rotation speed decreases as cos(latitude) In Albuquerque (35º N), the rotation speed is (1670 km/h) x (cos(35º)) 20 =1370 km/h.
21 Consequences of the Coriolis effect Affects storms and low/high pressure systems: Flow around a low pressure system in N hemisphere Hurricanes in the northern hemisphere rotate counter-clockwise In the southern hemisphere they rotate clockwise 21
22 Hurricane Florence
23 Hurricane Florence
24 Example: How fast does a satellite have to move in order for it to be in a circular orbit around the Earth? Worksheet #3
25 Example: How fast does a satellite have to move in order for it to be in a circular orbit around the Earth? For circular motion, the acceleration is the centripetal acceleration: So a = V 2 circular centripetal r F gravity = ma centripetal GM Earth m rock r 2 = m rock V circular 2 r
26 Canceling m rock and one factor of 1/r, or GM Earth r V circular = = V circular 2 GM Earth r This circular speed is the magnitude of the injection velocity, perpendicular to direction to center of Earth, needed for a circular orbit at distance r from the Earth.
27 This is general! Example: what is the circular speed of an object located at 1 AU from the Sun? M = M Sun = 2 x kg; r is 1.5 x m, and the constant G is 6.7 x in SI units, so V circular = ( )( ) V circular = m/s V circular = 30 km/s
28 Accurate average speed of the Earth around the Sun: km/s How about if the Earth had twice the mass? Question: How would the speed of the planets around the Sun vary with distance from the Sun? Eg., what is functional relation between v and r? This is what Kepler saw!
29 Keplerian rotation curves When the system is dominated by the central mass: v r -1/2
30 Milky Way also rotates. But rotation curve not Keplerian, but nearly flat. Milky Way mass is not dominated by a central mass 30
31 What if injection velocity isn t the circular velocity? In general, orbits are conic sections (Newton). Ellipses and circles are closed orbits, hyperbolic and parabolic orbits are open. Objects on these orbits do not return some comets do this!
32 Escape speed How large must the injection speed be to make the object escape gravity of the body it was launched from altogether? Quantitatively, this means object gets infinitely far away from the body it is escaping when its speed has dropped to zero (if speed = 0 km/s at finite distance, gravity would bring it back) Examine in terms of energies. Its kinetic energy is: At escape, then, KE = 0. (Why?) KE = 1 2 mv 2 32
33 When it escapes, what is its potential energy? (Recall potential energy is energy due to its position, in the presence of a force.) PE = GMm r At escape, its PE is 0. (Why?) Its total energy is then TE = KE + PE, which is zero when it escapes. If TE=0 when it escapes, it must have been 0 at launch, too (and everywhere else). WHY?
34 Since total energy is conserved, it is also zero at launch: GMm r V escape = mv escape 2 = 0 2GM r Escape speed (see box 7.2 in text) This relation is very useful! Example: V escape from the surface of the Earth is 11.2 km/s (you can show this).
35 Escape from the moon How fast would you have to throw a baseball to get it to escape from the moon? Start with the fact that you weigh 1/6 as much on the moon and the escape velocity on Earth is 11.2 km/s. v 2 = 2GM/r = 2rg g m /g e = 1/6 v m 2 2r m g m r m = 1737 km v e 2 = 2r r e = 6378 km e g e v m = 11.2*sqrt(1737/(6378*6)) = 2.4 km/s
36 Another example A neutron star is a stellar remnant with about twice the mass of the Sun, but a radius of only 10 kilometers. How fast would you have to be going to escape the surface of a neutron star? V escape = 2GM r = m s kg 4 10 m kg = m/s Q: How does this compare to c?
37 General rules of orbits Orbit shape Parabolic Elliptical/circular Hyperbolic System energy Zero Negative Positive Negative energy orbits are bound, positive energy orbits are unbound. What orbit is the most bound (minimum energy)?
38
39 NGC4258 fits
40 Lagrange Points
41 Rotation Curves
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