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Tidal Forces Section 19.2 By Greg Potember
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Basic Point-Mass Gravitational Forces
Assuming Spherical Symmetry A
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Basic Point-Mass Gravitational Forces
Assuming Spherical Symmetry A B
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Basic Point-Mass Gravitational Forces
Assuming Spherical Symmetry A B Force of B on A Force of A on B
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A B Force of B on A Force of A on B Radius r M m
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Gravitation Forces on Large Objects
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What is
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Differential Force is Tidal Force
Creates a “bulge” in water and land masses In land, creates small deformations Earth- 10 cm Bulges Moon- 20 m Bulges In water, creates tides Two high tides every 24 hours 53 minutes
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Where are the bulges? Earth’s bulges do not line up with Earth- Moon axis Moon’s bulge occurs on one side
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Analyzing ΔF r R
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Analyzing ΔF r R
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Pulling r^2 out of the denominator...
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Using a combination of approximations and algebra...
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R θ r
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Tidal bulges create Torque
Creates Torque on Earth and Alters Orbital Path
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Torque Effects Creates Drag
Earth’s Rotational Kinetic Energy is slowly decreasing Moon has complete 1:1 Synchronous Rotation
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The Sun’s Effects
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Roche Limit
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Roche Limit
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Roche Limit
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Roche Limit
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Gravitational Acceleration < Differential Acceleration
Roche Limit We assume the differential force is greater than the Force of gravity holding the moon together Fd Fg Gravitational Acceleration < Differential Acceleration
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Gravitational Acceleration < Differential Acceleration
Roche Limit We assume the differential force is greater than the Force of gravity holding the moon together Fd Fg Gravitational Acceleration < Differential Acceleration In terms of Densities:
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Example 19.2.1 p. 724 Saturn’s Density = 687 kg/m^3
Saturn’s Radius = 6.03x10^7 m Moon Density = 1200 kg/m^3 Remember: What is the Roche Limit radius?
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Example 19.2.1 p. 724 Saturn’s Density = 687 kg/m^3
Saturn’s Radius = 6.03x10^7 m Moon Density = 1200 kg/m^3 r = 1.23 x 10^8 m
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