Forces (2) Flashcards

1
Q

Angular Velocity

A
  • Angular displacement: The change in angle, (radians), as a body rotates around a circle.
  • Angular Velocity (⍵): The rate of change of angular displacement over time, where the velocity changes direction but speed remains constant in uniform circular motion.
  • Key relationships:
    • Greater rotation angle (θ) in a given time results in higher angular velocity (⍵).
    • Objects farther from the center (larger r) have smaller angular velocity due to less frequent directional changes
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2
Q

Frequency and period in a circle

A
  • Frequency (f): The number of complete revolutions per second, measured in hertz (Hz) or s⁻¹.
  • Period (T): The time taken for one complete revolution, measured in seconds (s).
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3
Q

Centripetal Acceleration

A
  • The acceleration of an object directed towards the centre of a circle when it moves in circular motion at a constant speed.
  • Perpendicular to the object’s velocity.
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4
Q

Centripetal Force

A
  • The resultant force directed towards the centre of a circle, necessary to maintain uniform circular motion.
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5
Q

Linear Velocity in Circular Motion

A

Uniform Circular Motion:

  • Linear velocity (v): Depends on linear displacement, not angular displacement.
  • As the radius (r) increases, linear velocity (v) increases.

….

Angular vs. Linear Speed:

  • Angular speed and angular velocity are independent of the radius.
  • Linear speed depends directly on the radius of the circle.
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6
Q

Centripetal Force examples

A

-Friction between car tyres and road
-tension in rope
-gravity

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7
Q

Simple Harmonic Motion

A
  • Definition: SHM is a type of oscillation where acceleration is proportional to displacement but acts in the opposite direction

  • Defining Equation: a ∝ −x, where a is acceleration and x is displacement.

  • Conditions for SHM:
    • Acceleration is proportional to displacement.
    • Acceleration acts in the opposite direction to displacement.
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8
Q

SHM graphs

A

Undamped SHM Graphs:

  • Periodic and described using sine and cosine curves.

===

Displacement-Time Graph:

  • Amplitude (A): Maximum displacement (x).
  • Time period (T): Time for one full cycle.
  • May not start at 0; maximum displacement indicates amplitude.

===

Velocity-Time Graph:

  • 90° out of phase with the displacement-time graph.
  • Velocity is the gradient of the displacement-time graph.
  • Maximum velocity occurs at equilibrium (displacement = 0).

===

Acceleration-Time Graph:

  • Reflection of the displacement graph along the x-axis.
  • 90° out of phase with the velocity-time graph.
  • Acceleration is the gradient of the velocity-time graph.
  • Maximum acceleration occurs at maximum displacement.
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9
Q

Isochronous oscillation

A

The period of oscillation is independent of the amplitude

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10
Q

Conditions for SHM

A
  1. Isochronous oscillations: The time period is independent of amplitude.
  2. Central equilibrium point: The object oscillates around this point.
  3. Continuous variation: Displacement, velocity, and acceleration change sinusoidally over time.
  4. Restoring force: Always directed towards the equilibrium point.
  5. Hooke’s Law: The magnitude of the restoring force is proportional to the displacement from equilibrium.
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11
Q

Potential and Kinetic energy in SHM

A

Energy in Simple Harmonic Motion (SHM):

  • An object exchanges kinetic energy (KE) and potential energy (PE) as it oscillates.
  • Potential energy depends on the restoring force (e.g., gravitational or elastic).

===

Energy at Key Points:

  • Equilibrium:
    • PE = 0, KE = maximum (velocity is maximum).
  • Maximum displacement (amplitude):
    • PE = maximum, KE = 0 (velocity is zero).

===

Total Mechanical Energy:

  • Constant throughout the motion (assuming no damping).
    E = 1/2 m ω2 x02
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12
Q

Time period in a spring/pendulum

A
  • T = 2π √(m÷k)
  • T = 2π √(l÷g)
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13
Q

Free oscillations

A
  • Occur when a system is displaced and oscillates without energy transfer to or from the surroundings.
  • Oscillate at the natural (resonant) frequency.
  • Only internal forces act; no external forces or energy input.
  • Amplitude remains constant in ideal conditions (e.g., in a vacuum).
  • Energy alternates between kinetic (Ek) and potential energy (Ep) without loss.
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14
Q

Forced Oscillations

A
  • Forced oscillations occur when a periodic external force is applied to sustain motion.
  • The external force does work against damping forces (like friction), replacing lost energy.
  • The system oscillates at the frequency of the external driving force, not its natural frequency.
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15
Q

Natural frequency

A

Frequency of an oscillation when it is oscillating freely

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16
Q

Resonance

A

Resonance:

  • Occurs when the driving frequency matches the natural frequency of an oscillating system.
  • Results in a significant increase in amplitude.

===

Key Points:

  • Energy transfer from the driving force to the system is most efficient at resonance.
  • The system achieves maximum kinetic energy and vibrates with maximum amplitude.
17
Q

Damping

A

Damping:

  • The reduction of energy and amplitude caused by resistive forces (e.g., friction, air resistance).
  • Energy is proportional to amplitude².

===

Damped Oscillations:

  • Amplitude decreases over time, and the system eventually comes to rest at the equilibrium position.
  • The frequency of oscillations remains constant as the amplitude decreases.
18
Q

Types of damping

A

Light Damping:

  • Amplitude decreases exponentially over time.
  • Oscillations continue with gradually decreasing amplitude.
  • Frequency and time period remain constant.

===

Critical Damping:

  • The oscillator returns to equilibrium without oscillating in the shortest time possible.
  • Displacement-time graph: No oscillations, fast decrease to zero.
  • Example: Car suspension systems.

===

Heavy Damping:

  • The oscillator returns to equilibrium slowly without oscillating.
  • Displacement-time graph: Slow decrease in amplitude.
  • Example: Door dampers preventing doors from slamming.
19
Q

Amplitude-Frequency Graphs

A

Resonance Curve:

  • A graph of driving frequency (f) vs. amplitude (A) of oscillations.

===

Key Points:

  1. f < f₀: Amplitude increases as driving frequency approaches the natural frequency (f₀).
  2. f = f₀ (resonance): Amplitude reaches its maximum.
  3. f > f₀: Amplitude decreases as driving frequency exceeds the natural frequency.
20
Q

The Effects of Damping on Resonance

A

Effect of Damping on Resonance:

  • Damping reduces the amplitude of resonance vibrations.
  • The natural frequency (f₀) remains unchanged.

===

Changes with Increased Damping:

  • Amplitude of resonance decreases, lowering the peak of the resonance curve.
  • The resonance peak broadens.
  • The peak shifts slightly to the left of the natural frequency when heavily damped.

===

Conclusion:

  • Damping reduces the sharpness of resonance and lowers the amplitude at the resonant frequency.
21
Q

Examples of Forced Oscillations & Resonance

A

Microwaves and Resonance:

  • Microwaves use electromagnetic radiation at a frequency that resonates with the natural frequency of water molecules in food.
  • Resonance causes water molecules to oscillate, generating heat energy through molecular friction.

===

Heating Mechanism:

  • Unlike conduction or convection, microwaves transfer heat directly via radiation to water molecules.
  • Resonance ensures efficient energy transfer, as the microwave frequency matches the natural frequency of water molecules for optimal energy absorption.

===

Efficiency:

  • The principle of forced oscillations and resonance allows microwaves to heat food more efficiently than traditional methods.
22
Q

force field

A

Region of space where an object will experience a force

23
Q

Gravitational Fields

A
  • A gravitational field is a force field generated by any object with mass, causing other masses to experience an attractive force.
  • Gravitational fields are created around any object with mass and influence other nearby masses.
  • They represent the action of gravitational forces acting between masses in their vicinity.
24
Q

Gravitational field lines

A
  • Show the direction of the gravitational force on a mass, always pointing toward the center of mass due to gravity’s attractive nature.
  • Around a point mass, the field is radial, with lines converging toward the center.
  • Represent the direction of acceleration for a mass placed in the field.
25
Q

Radial Vs Uniform field lines

A

Radial Fields:

  • Non-uniform, with field strength (g) varying with distance from the center.
  • Represented by radially inward lines.

===

Uniform Fields:

  • Have equally spaced parallel lines, with field strength (g) remaining constant.
  • On the Earth’s surface, gravitational field lines are parallel, approximating a uniform field.
26
Q

Newton’s Law of Gravitation

A

Newton’s Law of Gravitation:

  • The gravitational force (F) is:
    • Directly proportional to the product of two masses (m₁ and m₂).
    • Inversely proportional to the square of their separation (r).
  • The negative sign indicates the force is attractive.

===

Distance (r):

  • Measured between the centers of the two masses.
  • For objects above a planet’s surface, add the planet’s radius to the height above the surface.
27
Q

Gravitational field strength in radial

A

Gravitational Field Strength (g) in a Radial Field:

  • Equation: g = -GM/r²,
    where:
    • G = gravitational constant.
    • M = mass of the object.
    • r = distance from the center of the mass.
  • The negative sign indicates the field is attractive, with field lines pointing toward the mass.

===

Key Points:

  • g decreases with increasing r, following an inverse square law.
  • On Earth’s surface, g ≈ 9.81 N kg⁻¹, but outside Earth, g is not constant.
28
Q

GPE in a radial field

A

Gravitational Potential:

  • Defined as the work done per unit mass to bring a mass from infinity to a defined point.
  • Always negative because work is required to move mass away from the gravitational source (attractive).
  • Infinity is the reference point where gravitational potential is zero.
  • Potential becomes less negative as mass is moved away from the source.

===

Gravitational Potential Energy (G.P.E.):

  • The energy an object has due to its position in a gravitational field.
29
Q

Gravitational potential difference

A
  • Gravitational potential difference (ΔV) is the difference in gravitational potential between two points at different distances from a mass.
  • ΔV is given by ΔV = Vf – Vi, where Vf is the final potential and Vi is the initial potential.
30
Q

Escape velocity

A

Escape Velocity:

  • The minimum speed required for an object to escape a gravitational field without further energy input.
  • Depends on the mass (M) and radius (r) of the object creating the gravitational field.
  • Same for all objects in the same gravitational field.

===

Equation:

  • v = √(2GM/r), where:
    • v = escape velocity.
    • G = gravitational constant.
    • M = mass of the object.
    • r = distance from the object’s center.

===

Key Point:

  • An object reaches escape velocity when all its kinetic energy is transferred to gravitational potential energy.
31
Q

Centripetal Force on a Planet

A

Satellite Motion:

  • The gravitational force on a satellite acts as the centripetal force, always perpendicular to the direction of travel.

===

Orbital Speed Equation:

  • Equating gravitational force to centripetal force gives:
    v = √(GM/r), where:
    • v = orbital speed.
    • G = gravitational constant.
    • M = mass of the central object.
    • r = distance from the center of the object to the satellite.

===

Key Point:

  • The mass of the satellite (m) cancels out, showing that orbital speed is independent of the satellite’s mass.
32
Q

Orbital period

A
  • The orbital speed 𝑣 of a planet or satellite in a circular orbit is given by the circular motion formula v = 2π/T
  • v2 = GM/R
  • Equal the two and solve for T2
33
Q

Force Distance Graphs for gravitational force

A

Force-Distance Graph for Gravitational Fields:

  • The graph is a curve because force (F) is inversely proportional to .
  • The area under the graph represents work done or energy transferred.

===

Gravitational Potential Energy:

  • When a mass m moves further from mass M, its gravitational potential energy increases, requiring work to be done.
  • The area between two points on the graph gives the change in gravitational potential energy of mass m.
34
Q

Geostationary satellite

A

Geostationary Orbit:

  • A satellite remains directly above the equator, in the plane of the equator, and always at the same point above Earth’s surface.
  • The satellite moves west to east with an orbital period of 24 hours, matching Earth’s rotation.

===

Applications:

  • Used for telecommunication transmissions and television broadcasts, where the satellite amplifies and sends signals back to Earth.
  • Receiver dishes on Earth can be fixed, as they always point to the same spot in the sky due to the satellite’s fixed position.
35
Q

Kepler’s Three Laws of Motion

A

Kepler’s First Law:

  • The orbit of a planet is an ellipse with the Sun at one of the two foci.
  • Orbits can be circular or highly elliptical.

===

Kepler’s Second Law:

  • A line joining a planet and the Sun sweeps out equal areas in equal time intervals.
  • Planets move faster when closer to the Sun and slower when farther away.

===

Kepler’s Third Law:

  • The square of the orbital period (T) is directly proportional to the cube of the orbital radius (r):
    T² ∝ r³
  • A constant (k) applies to all planets in the same system.
36
Q

Circular Motion on a Banked Track/Vertical Loop

A

Circular Motion in a Vertical Loop:

  • Bottom of the Loop:
    • Centripetal Force (F) = R - mg (difference between upward force R and weight mg).
  • Top of the Loop:
    • Centripetal Force (F) = R + mg (sum of upward force R and weight mg).
  • Side of the Loop:
    • Centripetal Force (F) = R (equal to the upward force).

===

Circular Motion on a Banked Track:

  • Forces:
    • Weight (mg): Acts vertically downward.
    • Normal Force (N): Acts perpendicular to the surface.
  • Components of Normal Force (N):
    • Vertical: Balances weight.
    • Horizontal: Provides centripetal force.
  • Angle of Banking (θ): Determines the ratio of the normal force’s components, reducing reliance on friction.
37
Q

SHM in a pendulum

A

Height Difference in Pendulum Motion:

  • The height difference is not the amplitude.
  • Use mgh = KE to relate height to kinetic energy.
  • Maximum velocity (vₘₐₓ) can be found using the energy equation.
38
Q

Weight on equator Vs weight on north pole

A

Less on equator because some of the weight is used as centripetal force