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Return to the Intermediate Level Page. Issac Newton devised a universal law of gravitation that stated all objects exert a gravitational force of attraction on each other even when separated by large distances. The force of gravity between two masses (m1 and m2) separated by a distance (r) is: ![]() (Equation 1-16) G is a constant that equals roughly 6.67 x 10-11 N m2/kg2. We can actually use this to derive the value of g (acceleration at the surface of the earth due to gravity). We will let m1 equal the mass of the earth, which is roughly 6.0 x 1024 kg. Also, m2 can be any arbitary mass; it will be cancelled out later as you will see. And finally r will be the radius of the earth (roughly 6.4 x 106) since we want the acceleration at the surface. Now let's begin: ![]() (Equation 1-17) ...and we get our good old 9.8 m/s2. Kepler's LawsJohannes Kepler was a 16th century astronomer who studied the motion of the planets. Through years of analyzing data, he came up with three laws that govern the motion of the planets around the sun. He arrived at them trial-and-error, but Newton's laws of motion and gravitation would later explain why they were true.![]() An ellipse looks like a flattened circle. The greater the distance between the two foci, the greater the eccentricity of the ellipse. If the foci are located at the same point, the ellipse becomes a perfect circle. Planets orbiting the sun are traveling in slightly elliptical orbits but they seem circular because the distance between the foci is small. In an orbit, the sun is located at one of the foci. ![]() Kepler's third law is a relationship between the mean radius of a planet's orbit (R) and it's period of revolution (T): ![]() (Equation 1-18) K is a constant that is the same value for anything orbiting the sun. This constant has a value of roughly 2.5 m3/day2. We can use this relationship to find the mean orbit radius of every planet if we know the periods. ![]() ![]() |
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