Copyright © 2009 Pearson Education, Inc. Lecture 7 Gravitation 1.

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Copyright © 2009 Pearson Education, Inc. Lecture 7 Gravitation 1

Copyright © 2009 Pearson Education, Inc. Chapter 6 Gravitation 2

Copyright © 2009 Pearson Education, Inc. Units of Chapter 6 Newton’s Law of Universal Gravitation Vector Form of Newton’s Law of Universal Gravitation Gravitational Field Strength or Gravity Near the Earth’s Surface Gravitational field Satellites Escape velocity (Lecture 3b) 3

Copyright © 2009 Pearson Education, Inc. 6-1 Newton’s Law of Universal Gravitation If the force of gravity is being exerted on objects on Earth, what is the origin of that force? Newton’s realization was that the force must come from the Earth. He further realized that this force must be what keeps the Moon in its orbit. 4

Copyright © 2009 Pearson Education, Inc. 6-1 Newton’s Law of Universal Gravitation The gravitational force on you is one-half of a third law pair: the Earth exerts a downward force on you, and you exert an upward force on the Earth. When there is such a disparity in masses, the reaction force is undetectable, but for bodies more equal in mass it can be significant. 5

Copyright © 2009 Pearson Education, Inc. 6-1 Newton’s Law of Universal Gravitation Therefore, the gravitational force must be proportional to both masses. By observing planetary orbits, Newton also concluded that the gravitational force must decrease as the inverse of the square of the distance between the masses. In its final form, the law of universal gravitation reads: where 6

Copyright © 2009 Pearson Education, Inc. 6-1 Newton’s Law of Universal Gravitation The magnitude of the gravitational constant G can be measured in the laboratory. This is the Cavendish experiment. 7

Copyright © 2009 Pearson Education, Inc. 6-1 Newton’s Law of Universal Gravitation Example 6-1: Can you attract another person gravitationally? A 50-kg person and a 70-kg person are sitting on a bench close to each other. Estimate the magnitude of the gravitational force each exerts on the other. 8

Copyright © 2009 Pearson Education, Inc. 6-1 Newton’s Law of Universal Gravitation Example 6-2: Spacecraft at 2 r E. What is the force of gravity acting on a 2000-kg spacecraft when it orbits two Earth radii from the Earth’s center (that is, a distance r E = 6380 km above the Earth’s surface)? The mass of the Earth is m E = 5.98 x kg. 9

Copyright © 2009 Pearson Education, Inc. 6-1 Newton’s Law of Universal Gravitation Example 6-3: Force on the Moon. Find the net force on the Moon ( m M = 7.35 x kg) due to the gravitational attraction of both the Earth ( m E = 5.98 x kg) and the Sun ( m S = 1.99 x kg), assuming they are at right angles to each other. 10

Copyright © 2009 Pearson Education, Inc. 6-1 Newton’s Law of Universal Gravitation Using calculus, you can show: Particle outside a thin spherical shell: gravitational force is the same as if all mass were at center of shell Particle inside a thin spherical shell: gravitational force is zero Can model a sphere as a series of thin shells; outside any spherically symmetric mass, gravitational force acts as though all mass is at center of sphere 11

Copyright © 2009 Pearson Education, Inc. 6-2 Vector Form of Newton’s Universal Gravitation If there are many particles, the total force is the vector sum of the individual forces: 12

Copyright © 2009 Pearson Education, Inc. 6-3 Gravity Near the Earth’s Surface; Geophysical Applications Now we can relate the gravitational constant to the local acceleration of gravity. We know that, on the surface of the Earth: Solving for g gives: g is also called the gravitational field strength. Now, knowing g and the radius of the Earth, the mass of the Earth can be calculated: 13

Copyright © 2009 Pearson Education, Inc. 6-3 Gravity Near the Earth’s Surface; Geophysical Applications Example 6-4: Gravity on Everest. Estimate the effective value of g on the top of Mt. Everest, 8850 m (29,035 ft) above sea level. That is, what is the acceleration due to gravity of objects allowed to fall freely at this altitude? 14

Copyright © 2009 Pearson Education, Inc. 6-3 Gravity Near the Earth’s Surface; Geophysical Applications The acceleration due to gravity varies over the Earth’s surface due to altitude, local geology, and the shape of the Earth, which is not quite spherical. 15

Copyright © 2009 Pearson Education, Inc. 6-4 Satellites and “Weightlessness” Satellites are routinely put into orbit around the Earth. The tangential speed must be high enough so that the satellite does not return to Earth, but not so high that it escapes Earth’s gravity altogether. 16

Copyright © 2009 Pearson Education, Inc. 6-4 Satellites and “Weightlessness” The satellite is kept in orbit by its speed—it is continually falling, but the Earth curves from underneath it. 17

Copyright © 2009 Pearson Education, Inc. 6-4 Satellites and “Weightlessness” Example 6-6: Geosynchronous satellite. A geosynchronous satellite is one that stays above the same point on the Earth, which is possible only if it is above a point on the equator. Such satellites are used for TV and radio transmission, for weather forecasting, and as communication relays. Determine (a) the height above the Earth’s surface such a satellite must orbit, and (b) such a satellite’s speed. (c) Compare to the speed of a satellite orbiting 200 km above Earth’s surface. 18

Copyright © 2009 Pearson Education, Inc. 6-4 Satellites and “Weightlessness” Conceptual Example 6-7: Catching a satellite. You are an astronaut in the space shuttle pursuing a satellite in need of repair. You find yourself in a circular orbit of the same radius as the satellite, but 30 km behind it. How will you catch up with it? 19

Copyright © 2009 Pearson Education, Inc. 6-4 Satellites and “Weightlessness” Objects in orbit are said to experience weightlessness. They do have a gravitational force acting on them, though! The satellite and all its contents are in free fall, so there is no normal force. This is what leads to the experience of weightlessness. 20

Copyright © 2009 Pearson Education, Inc. 6-4 Satellites and “Weightlessness” More properly, this effect is called apparent weightlessness, because the gravitational force still exists. It can be experienced on Earth as well, but only briefly: 21

Copyright © 2009 Pearson Education, Inc. 6-6 Gravitational Field The gravitational field is the gravitational force per unit mass: The gravitational field due to a single mass M is given by: 22

Copyright © 2009 Pearson Education, Inc. Newton’s law of universal gravitation: Total force is the vector sum of individual forces. Satellites are able to stay in Earth orbit because of their large tangential speed. Summary of Chapter 6 23

Copyright © 2009 Pearson Education, Inc. Summary of Chapter 6 Gravitational field is force per unit mass. 24