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

Linear Velocity

A
  • velocity of an object in uniform circular motion with respect to linear displacement, not angular displacement.
  • As the radius (r) of the circular path increases, the linear velocity (v) also increases.
  • Angular speed and angular velocity are independent of the radius of the circle.
  • 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 are periodic and can be described using sine and cosine curves.
  • Displacement-time graph:
    • Amplitude A is the maximum value of displacement x.
    • Time period T is the time for one full cycle.
    • The graph might not start at 0; maximum displacement indicates the amplitude.
  • Velocity-time graph:
    • It is 90° out of phase with the displacement-time graph.
    • Velocity is the rate of change of displacement and can be determined from the gradient of the displacement-time graph.
    • Maximum velocity occurs at equilibrium when displacement is zero.
  • Acceleration-time graph:
    • It is a reflection of the displacement graph along the x-axis.
    • Acceleration is 90° out of phase with the velocity-time graph and can be determined from 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
  • The oscillations are isochronous:
  • There is a central equilibrium point:
  • The object’s displacement, velocity, and acceleration change continuously: These quantities vary over time in a sinusoidal manner.
  • There is a restoring force always directed towards the equilibrium point:
  • The magnitude of the restoring force is proportional to the displacement: (Hooke’s law),( displacement from the equilibrium)
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11
Q

Potential and Kinetic energy in SHM

A
  • In simple harmonic motion (SHM), an object exchanges kinetic energy (KE) and potential energy (PE) as it oscillates.
  • The type of potential energy depends on the restoring force (e.g., gravitational or elastic potential energy).
  • At equilibrium, the object’s PE is zero and KE is maximum (velocity is also maximum).
  • At maximum displacement (amplitude), PE is maximum, and KE is zero (velocity is zero).
  • The total mechanical energy (sum of KE and PE) remains constant throughout the motion (assuming no damping).
  • The total energy of system undergoing simple harmonic motion is defined by:
    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
  • Free oscillations occur when an oscillating system is displaced and left to oscillate without any energy transfer to or from the surroundings; they oscillate at their natural (resonant) frequency.
  • Only internal forces act during free oscillations, with no external forces or energy input, and the oscillations continue with a constant amplitude.
  • Energy alternates between kinetic (Ek) and potential energy (Ep) without loss in ideal free oscillations (e.g., in a vacuum).
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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, 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
  • the frequency of an oscillation when the oscillating system is allowed to oscillate freely
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16
Q

Resonance

A
  • Definition: Resonance is when the frequency of an applied force equals the system’s natural frequency (or a multiple of), causing a significant increase in amplitude.
  • Resonance occurs when the driving frequency matches the natural frequency of an oscillating system.
  • At resonance, energy transfer from the driving force to the system is most efficient.
  • The system achieves maximum kinetic energy and vibrates with maximum amplitude.
17
Q

Damping

A
  • Definition: Damping is the reduction of energy and amplitude caused by resistive forces on the oscillating system
  • Damping reduces the energy and amplitude of oscillations due to resistive forces like friction or air resistance.
    (** Energy is proportional to amplitude^2**)
  • Damped oscillations decrease in amplitude over time and eventually come to rest at the equilibrium position.
  • The frequency of damped 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.
    • The frequency and time period remain constant.
  • Critical Damping:
    • The oscillator returns to equilibrium without oscillating in the shortest time possible.
    • The displacement-time graph shows no oscillations, with a fast decrease to zero.
    • Example: car suspension systems.
  • Heavy Damping:
    • The oscillator returns to equilibrium slowly without oscillating.
    • The displacement-time graph shows a 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) versus amplitude (A) of oscillations.
  • When f < f₀: The amplitude of oscillations increases as the driving frequency approaches the natural frequency.
  • At f = f₀ (resonance): The amplitude reaches its maximum. This is the point of resonance.
  • When f > f₀: The amplitude of oscillations decreases as the 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.
  • Natural Frequency (f₀): The natural frequency remains the same despite damping.
  • Changes with Increased Damping:
    • The 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 use electromagnetic radiation at a specific frequency that resonates with the natural frequency of water molecules in food.
  • Resonance causes water molecules to oscillate, generating heat energy through molecular friction.
  • Unlike conventional cooking methods (which use conduction or convection), microwaves transfer heat directly via radiation to the food’s water molecules.
  • Resonance ensures efficient energy transfer, as the microwave frequency matches the natural frequency of water molecules for optimal energy absorption.
  • The principle of forced oscillations and resonance allows microwaves to heat food more efficiently than traditional methods.
22
Q

force field

A
  • any region of space in which a specific type of 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
  • Gravitational field lines (or vectors) show the direction of the gravitational force on a mass and always point toward the center of mass due to the attractive nature of gravity.
  • The field around a point mass is radial, with lines converging toward the center.
  • Field lines also represent the direction of acceleration for a mass placed in the field.
25
Q

Radial Vs Uniform field lines

A
  • Radial fields are 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 throughout.
  • 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) and inversely proportional to the square of their separation (r).
  • The negative sign indicates that the gravitational force is attractive.
  • The distance r is measured between the centers of the two masses. Add the planet’s radius to the height above the surface when calculating r.
27
Q

Gravitational field strength in radial

A
  • Gravitational field strength (g) in a radial field decreases with distance (r) according to the equation:
    g = -GM/r², where G is the gravitational constant, M is the mass, and r is the distance from the center of the mass.
  • The negative sign shows that the field is attractive, and field lines point toward the mass causing the field.
  • g decreases as r increases 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 is the work done per unit mass in bringing a mass from infinity to a defined point.
  • Gravitational potential energy (G.P.E.) is the energy an object has due to its position in a gravitational field.
  • Gravitational potential is always negative because work is required to move mass away from the gravitational source (attractive)
  • Infinity is the reference point where the gravitational potential is defined as zero.
  • The potential becomes less negative as mass is moved away from the source.
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 is the minimum speed required for an object to escape a gravitational field without further energy input.
  • It depends on the mass and radius of the object creating the gravitational field and is the same for all objects in the same field.
  • The escape velocity can be calculated using the equation v = √(2GM/r), where v is the escape velocity, G is the gravitational constant, M is the mass of the object creating the field, and r is the distance from the object’s center.
  • An object reaches escape velocity when all its kinetic energy has been transferred to gravitational potential energy.
31
Q

Centripetal Force on a Planet

A
  • The gravitational force on a satellite is centripetal, meaning it is always perpendicular to the direction of travel.
  • Equating the gravitational force to the centripetal force gives:
    F = Fcentripetal.
  • This simplifies to the equation for the orbital speed v of a satellite in a circular orbit:
    v = √(GM/r), where G is the gravitational constant, M is the mass of the central object, and r is the distance from the center of the object to the satellite.
  • The mass of the satellite m cancels out from both sides of the equation, showing that orbital speed does not depend on 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
  • A force-distance graph for gravitational fields would be a curve since force (F) is inversely proportional to .
  • The area under the graph represents work done or energy transferred.
  • When a mass m moves further away from a mass M, its gravitational potential energy increases, requiring work to be done on the mass.
  • 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 is a special orbit where 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 from west to east, with an orbital period of 24 hours, matching Earth’s rotational period.
  • Used for telecommunication transmissions and television broadcasts, where the satellite amplifies and sends signals back to Earth.
  • Receiver dishes on the Earth’s surface 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. Planet orbits can be circular or highly elliptical.
  • Kepler’s Second Law: A line segment joining a planet and the Sun sweeps out equal areas in equal time intervals, meaning planets move faster when closer to the Sun and slower when farther away.
  • Kepler’s Third Law: The square of the orbital time period (T) is directly proportional to the cube of the orbital radius (r), expressed as T² ∝ r³, with a constant (k) for 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) = S - mg (difference between upward force S and weight mg).
- Top of the Loop:
- Centripetal Force (F) = S + mg (sum of upward force S and weight mg).
- Side of the Loop:
- Centripetal Force (F) = S (equal to the upward force).

Circular Motion on a Banked Track
- Forces on a Banked Track:
- Centripetal force results from the combination of:
- Weight (mg): Acts vertically downward.
- Normal Force (N): Acts perpendicular to the surface.
- Components of Normal Force (N):
- Vertical Component: Balances weight
- Horizontal Component: Provides centripetal force
- Angle of Banking (θ):
- The angle determines the ratio of the normal force’s components, reducing reliance on friction.

37
Q

SHM in a pendulum

A

If given the height difference for pendulum, this is NOT amplitude!
The only thing you cao do with this is mgh = KE
WA=V max