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Author Capstone Axis

Chapter 13 / 13.5 Velocity and Acceleration in Simple Harmonic Motion

Velocity & Acceleration in Simple Harmonic Motion Velocity & Acceleration in Simple Harmonic Motion 🚀 Quick Recap of SHM ➡️ Displacement: \(x(t)=A\cos(\omega t+\phi)\) Amplitude \(A\) is the farthest distance from the mean position. Angular frequency \(\omega=\dfrac{2\pi}{T}\), where \(T\) is the period. Instantaneous Velocity 🏃‍♂️ In a circle of radius \(A\) the speed is \(v=\omega A\). […]

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Chapter 13 / 13.6 Force Law for Simple Harmonic Motion

Simple Harmonic Motion – Force Law, Motion & Energy 🚀 1. How the motion looks in time ⏱️ Displacement: \(x(t)=A\cos(\omega t+\phi)\) — a comfy cosine ride starting at amplitude \(A\). :contentReference[oaicite:0]{index=0} Speed: \(v(t)=-\omega A\sin(\omega t+\phi)\) — reaches \(\pm\,\omega A\) at the mid-points. :contentReference[oaicite:1]{index=1} Acceleration: \(a(t)=-\omega^{2}A\cos(\omega t+\phi)\) — maxes out at \(\pm\,\omega^{2}A\) right at the ends.

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Chapter 14 / 14.2 Transverse and Longitudinal Waves

Transverse & Longitudinal Waves 🎸🌊 1. Waves in a Nutshell Mechanical waves move energy from one place to another by making the medium’s particles oscillate while the material itself stays put. Think of a crowd doing “the wave” at a stadium —the cheer travels, people don’t! 🌊:contentReference[oaicite:0]{index=0} 2. Two Main Flavors 😉 2.1 Transverse Waves

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Chapter 14 / 14.3 Displacement Relation in a Progressive Wave

Displacement Relation in a Progressive Wave 🌊 Picture a travelling wave as a moving “wiggle” that carries energy without dragging the material along. For a smooth (sinusoidal) wave moving in the +x-direction you use \(y(x,t)=a\sin\bigl(kx-\omega t+\varphi\bigr)\) :contentReference[oaicite:0]{index=0} \(y(x,t)\): displacement of the particle at position \(x\) and time \(t\). \(a\): amplitude – the largest distance a

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Chapter 14 / 14.4 The Speed of a Travelling Wave

Speed of Travelling Waves 🚀 1 • Chasing the Crest Track a point of fixed phase on the wave—say the crest—and keep its phase constant: \(k\,x – \omega\,t = \text{constant}\) 🙂 From this condition you get the speed \(v = \dfrac{\omega}{k}\). Because \(k = \dfrac{2\pi}{λ}\) and \(\omega = 2\pi\nu = \dfrac{2\pi}{T}\), the same speed appears in the more familiar

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Chapter 14 / 14.5 The Principle of Superposition of Waves

1. Principle of Superposition 🌊➕🌊 When two wave pulses travel toward each other, nothing dramatic happens—they simply glide through one another. While they overlap, every particle shifts by the straight-forward sum of the individual shifts. For two waves this reads: \( y(x,t)=y_1(x,t)+y_2(x,t) \)   (Eq. 14.25) :contentReference[oaicite:0]{index=0} If more than two waves meet, just keep adding

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Chapter 14 / 14.6 Reflection of Waves

Superposition & Interference 🎶 The disturbance in a medium adds up algebraically. For many individual disturbances \(y_1,\,y_2,\dots,y_n\) travelling with the same speed \(v\), the combined wave is $$y(x,t)=\sum_{i=1}^{n}f_i\!\bigl(x-vt\bigr) \tag{14.26}$$ :contentReference[oaicite:0]{index=0} With just two harmonic waves of equal amplitude \(a\) and wavelength \(\lambda\), but a phase gap \(\phi\), the net displacement becomes $$y(x,t)=2a\cos\!\Bigl(\tfrac{\phi}{2}\Bigr)\,\sin(kx-\omega t+\tfrac{\phi}{2}) \tag{14.31}$$ :contentReference[oaicite:1]{index=1}

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