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Gravity and Orbits Newton’s Law of Gravitation The attractive force of gravity between two particles G = 6.67 x 10 -11 Nm 2 /kg 2 Why is this important? 12/8/2015APHY1011 m1m1 m2m2 r
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Gravity and Orbits Earth’s composition and g The value of g = 9.8 m/s 2 is an average value for objects near the Earth’s surface Variations are due to altitude, the shape of the Earth and its local density 12/8/2015APHY1012
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Gravity and Orbits Tides Caused by differences in the force of gravity across an object 12/8/2015APHY1013
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Gravity and Orbits Tides The Sun’s tidal effect is smaller than the Moon’s even though it has a larger gravitational pull on the Earth. 12/8/2015APHY1014
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Gravity and Orbits Newton’s Cannon A thought experiment that related the motion of the Moon around the Earth and a falling object How fast would you need to travel to orbit the Earth? v ~ 8000 m/s ~ 17,600 mi/h Why does this only happen when in outer space? 12/8/2015APHY1015
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Gravity and Orbits Circular Orbits Satellites travel at a constant speed depending on their distance from the central body The mass of the satellite does not affect its orbital speed 12/8/2015APHY1016
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Gravity and Orbits Kepler’s First Law Planets orbit the Sun in elliptical paths Tycho Brahe – observations of Mars Johannus Kepler – mathematical explanation of orbits 12/8/2015APHY1017 Sun planet
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Gravity and Orbits More on ellipses and orbits Semimajor axis (a) and eccentricity (e) define the shape of an orbit 12/8/2015APHY1018 Sun a d
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Gravity and Orbits Kepler’s Second Law Planets sweep out equal areas in equal times 12/8/2015APHY1019 Sun
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Gravity and Orbits Kepler’s Third Law Relationship between the orbital period and the semimajor axis: T 2 ~ a 3 Assumes that m 1 >> m 2 12/8/2015APHY10110
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