Forces (2) Flashcards

(38 cards)

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
  • A resultant force acting perpendicular to the velocity, toward the centre of the circular path.
  • Essential for maintaining uniform circular motion (constant speed but changing direction).

===

Examples

  • Planetary orbits: Gravity provides (F_{centripetal}).
  • Car turning: Friction between tyres and road.
  • Swinging a bucket: Tension in the rope.
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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:
    • Time period (T) remains constant, regardless of amplitude (true for small angles/displacements).
  2. Central Equilibrium Point:
    • Oscillates about a fixed equilibrium position.
  3. Sinusoidal Variation:
    • Displacement (x), velocity (v), and acceleration (a) follow sinusoidal functions:
      • x = A cos(ωt)
      • v = -Aω sin(ωt)
      • a = -Aω² cos(ωt)
  4. Restoring Force:
    • Always opposes displacement, directed toward equilibrium:
      • F = -kx (Hooke’s Law).
  5. Hooke’s Law:
    • Force ∝ displacement (k = force constant).
    • Leads to acceleration ∝ -displacement (a = -ω²x).
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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

Key Characteristics

  • No energy transfer to/from surroundings (closed system).
  • Oscillates at the natural frequency (resonant frequency, f₀).
  • Amplitude remains constant (ideal case; no damping).
  • Only internal restoring forces act (e.g., spring force, gravity).

===

Energy Transfers

  • Ek ⇄ Ep: Continuous interchange between:
    • Maximum Ek at equilibrium position.
    • Maximum Ep at maximum displacement.
  • Total energy conserved (no dissipative forces).

===

Examples

  • Pendulum in vacuum: No air resistance → undamped motion.
  • Mass-spring system: Frictionless surface → perfect SHM.
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14
Q

Forced Oscillations

A
  • Driving Force: An external periodic force maintains oscillations, does work against damping forces (e.g., friction).
  • Frequency: The system oscillates at the driver’s frequency (fd), not its natural frequency (f0).
  • Amplitude: Depends on:
    • Damping level (more damping → smaller amplitude).
    • Frequency match (max amplitude at fd = f0resonance).

===

Energy Transfer

  • The driving force replaces lost energy, counteracting damping.
  • Power input = Energy dissipated per cycle (steady-state oscillations).

===

OCR Exam Focus

  • Resonance:
    • Large amplitude when fd ≈ f0.
    • Examples: Bridges (wind/earthquakes), radio tuners.
  • Graphs:
    • Amplitude vs. driver frequency (peak at f0).
    • Effect of light/heavy damping on resonance curves.
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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 region of space where any mass experiences an attractive force due to another mass.
  • Created by all objects with mass (from planets to particles).

Key Properties

  • Force direction: Always attractive (unlike electric/magnetic fields).
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
Radial Vs Uniform field lines
**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
Newton's Law of Gravitation
**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
Gravitational field strength in radial
**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
GPE in a radial field
- **Definition**: Work done per unit mass to move a test mass from **infinity** to a point in the field. - **Key Properties**: - **Always negative** (attractive force). - **Zero at infinity** (reference point). - **Less negative** with increasing \(r\). === **2. Gravitational Potential Energy (\(E_p\))** - **Definition**: Energy of a mass \(m\) due to its position in a gravitational field. - **Key Points**: - **Increases** (becomes less negative) as \(r\) increases. - **Maximum \(E_p = 0\)** at infinity.
29
Gravitational potential difference
- **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
Escape velocity
**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
Centripetal Force on a Planet
**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
Orbital period
- 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
Force Distance Graphs for gravitational force
**Force-Distance Graph for Gravitational Fields**: - The graph is a **curve** because **force (F)** is inversely proportional to **r²**. - 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
Geostationary satellite
**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
Kepler's Three Laws of Motion
**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
Circular Motion on a Banked Track/Vertical Loop
**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
SHM in a pendulum
**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
Weight on equator Vs weight on north pole
Less on equator because some of the weight is used as centripetal force