Definition:
Restoring acceleration proportional to displacement.
Differential Equation: d2x/dt2 = -ω2x:
Simple harmonic oscillator equation.
Restoring acceleration proportional to displacement.
Differential Equation: d2x/dt2 = -ω2x:
Simple harmonic oscillator equation.
Simple harmonic oscillator equation.
Position as function of time.
Where:
Velocity as function of time.
Acceleration as function of time.
Spring provides restoring force: (Hooke's Law)
Equation of motion:
Compare to SHM equation:
Where k = spring constant (N/m).
Period: T = 2π√(m/k):
Frequency:
Angular frequency:
Valid for small angles (θ < 15 degrees ), where .
Properties:
At any position:
Energy exchange:
For small angles, gravity provides restoring torque.
Equation of motion:
Compare to SHM:
Frequency:
Angular frequency:
Damping small enough for oscillations.
Differential equation:
Solution: Oscillation with exponentially decaying amplitude.
Minimum damping without oscillation.
Condition:
Returns to equilibrium fastest without overshooting.
Large damping, no oscillations.
Condition:
Returns to equilibrium slowly, no overshoot.
F = G m1 m2 / r2:
Newton's law of universal gravitation.
Where:
Reference: U = 0 at r -> ∞
Escape velocity:
First Law: Planetary (and satellite) orbits are ellips with central mass at one focus.
Second Law (Equal Area): Radius vector sweeps equal areas in equal times (consequence of angular momentum conservation).
Third Law: (period squared ∝ semi-major axis cubed)
Special case of elliptical orbit with e = 0.
Circular orbit condition:
Orbital speed:
Orbital period:
Total mechanical energy: (negative for bound orbits)
Restoring acceleration proportional to displacement.
Differential Equation: d2x/dt2 = -ω2x:
Simple harmonic oscillator equation.
Simple harmonic oscillator equation.
Position as function of time.
Where:
Velocity as function of time.
Acceleration as function of time.
Spring provides restoring force: (Hooke's Law)
Equation of motion:
Compare to SHM equation:
Where k = spring constant (N/m).
Period: T = 2π√(m/k):
Frequency:
Angular frequency:
Valid for small angles (θ < 15 degrees ), where .
Properties:
At any position:
Energy exchange:
For small angles, gravity provides restoring torque.
Equation of motion:
Compare to SHM:
Frequency:
Angular frequency:
Damping small enough for oscillations.
Differential equation:
Solution: Oscillation with exponentially decaying amplitude.
Minimum damping without oscillation.
Condition:
Returns to equilibrium fastest without overshooting.
Large damping, no oscillations.
Condition:
Returns to equilibrium slowly, no overshoot.
F = G m1 m2 / r2:
Newton's law of universal gravitation.
Where:
Reference: U = 0 at r -> ∞
Escape velocity:
First Law: Planetary (and satellite) orbits are ellips with central mass at one focus.
Second Law (Equal Area): Radius vector sweeps equal areas in equal times (consequence of angular momentum conservation).
Third Law: (period squared ∝ semi-major axis cubed)
Special case of elliptical orbit with e = 0.
Circular orbit condition:
Orbital speed:
Orbital period:
Total mechanical energy: (negative for bound orbits)