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Review of Lectures on Wave

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Review of Lectures on Wave

2020-4-13 chs_2020 General Physics I (H)

Wave Motion

Linear Wave

Waves that obey the superposition principle are called linear waves and are generally characterized by small amplitudes. Waves that violate the superpostion principle are called nonlinear waves and are often characterized by large amplitudes. The rigorous definition of linear/non-linear waves follows.

Def A wave is called linear/non-linear if the DE governing this wave is linear/non-linear.

Superpostion Principle of Linear Equations

A linear combination of arbitary solns of a homogeneous linear equation is also a soln of the same linear equation.

Interference

The combination of separate waves in the same region of space to produce a resultant wave is called interference.

Reflection

By Newton‘s third law, the support must exert an equal and opposite reaction force on the string, which causes the pulse to invert upon reflection.

Free Boundary Condition

When it reaches the post, the pulse exerts a force on the free end of the string, causing the ring to accelerate upward. Afterwards, the downward component of the tension force pulls the ring back down.

Transmission

Situation in which the boundary is intermediate between these two extremes - part of the incident pulse is reflected and part undergoes transmission, i.e. some of the pulse passes through the boundary.

Model of Monoatomic Crystal

技术图片

? Equilibrium positions: \(X_n=na\)

? Deviations from the equilibrium: \(u_n=x_n-X_n\)

? Hence \(u_{n+1}-u_n=x_{n+1}-x_{n}-a\)

Our aim is to give the Wave Equation. First derive the expression for Interatomic Potential, then by differentiation, get the Equation of Motion for every single particle.

  1. We consider nearest-neighbor interations only. By Taylor Expansion,

\[\begin{align}\phi(x_{n+1}-x_n)&=\phi_0+\frac{1}{2}K(x_{n+1}-x_n-a)^2+\cdots\\&=\phi_0+\frac{1}{2}K(u_{n+1}-u_n)^2+\cdots\end{align} \]

Here \(K\) is given by the second derivative of \(\phi\). Note that the Fisrt Derivative Vanishes At The Equilibrium, since there is no force between two atoms that are at their equilibrium positions.

\[U=\frac{1}{2}K\sum_{n}(u_{n+1}-u_{n})^2 \]

  1. By Newton‘s 2nd law,

\[\begin{align}M\ddot{u}_n=\frac{\mathrm{d}U\ }{\mathrm{d}u_n}&=K(u_{n+1}-u_{n})-K(u_n-u_{n-1})\\&\approx (Ka)\frac{\partial u}{\partial x}\Big|_{X_n+\frac{a}{2}}-(Ka)\frac{\partial u}{\partial x}\Big|_{X_n-\frac{a}{2}}\\&\approx (Ka^2)\Big(\frac{\partial^2u}{\partial x^2}\Big)_{X_n}\end{align} \]

  1. Rewrite the equation as

\[\frac{\partial^2 u}{\partial t^2}=\frac{Ka^2}{M}\cdot\frac{\partial^2u}{\partial x^2}\qquad\text{where}\ v=a\sqrt{\frac{K}{M}}\ \text{is the propagation speed of the wave}\downarrow \]

Coefficient in the Wave Equation

\[\text{Linear Wave Equation:}\qquad\frac{1}{c^2}\frac{\partial^2f}{\partial t^2}-\frac{\partial^2f}{\partial x^2}=0 \]

If a travelling wave \(f=f(x\pm vt)\) is a soln of this equation, then we easily have \(c^2=v^2\), and hence $c $ is the propagation speed of the wave.

Sinusoidal Wave

The Speed of Waves on Strings

技术图片 技术图片

Assume that the wavelength is much larger than the amplitude, then by Newton‘s second law and small-angle approx we have

\[\mu\Delta x\frac{\partial^2y}{\partial\,t^2}=T(x+\Delta x)\frac{\partial y}{\partial x}\Big|_{x+\Delta x}-\,T(x)\frac{\partial y}{\partial x}\Big|_{x} \]

It‘s reasonable to approx \(T(x+\Delta x)\) and \(T(x)\) by \(T\), and then

\[\frac{\partial^2y}{\partial\,t^2}=\frac{T}{\mu}\frac{\partial^2y}{\partial\,x^2}\ ,\qquad v=\sqrt{\frac{T}{\mu}} \]

Sinusodial Waves

The most important family of the solns for the Linear Wave Equation are \(y=A\sin(kx-\omega t+\phi)\), where \(k=\frac{2\pi}{\lambda}\) is the angular wave number, \(\omega=\frac{2\pi}{T}\) is the angular frequency and \(\phi\) is the phase const. Note that \(v=\frac{\lambda}{T}\), we rewrite the Sinusodial Wave Equation as \(y=A\sin\Big[\frac{2\pi}{\lambda}(x-\lambda t)\Big]\), which is of the form \(y=f(x-vt)\).

From \(y=A\sin(kx-\omega t+\phi)\) we derive \(v_y=-\omega A\cos(kx-\omega t)\) and \(a_y=-\omega^2A\sin(kx-\omega t)\), and hence \(v_{y,max}=\omega A\) and \(a_{y,max}=\omega^2A\).

Rate of Energy Transfer (Sinusoidal Wave on Strings)

\[\Delta U=\frac{1}{2}(\Delta m)\omega^2y^2=\frac{1}{2}(\mu\Delta x)\omega^2y^2 \]

\[\begin{align} dU&=\frac{1}{2}\mu\omega^2[A\sin(kx-\omega t)]^2\mathrm{d}x\\&=\frac{1}{2}\mu\omega^2A^2\sin^2(kx-\omega t)\mathrm{d}x \end{align} \]

Recall that for simple harmonic oscillation, the total energy \(E=K+U\) is const, which means \(\mathrm{d}E=\mathrm{d}K+\mathrm{d}U\), and therefore

\[P=\frac{\mathrm{d}E}{\mathrm{d}\,t}=\frac{\frac{1}{2}\mu\omega^2A^2\mathrm{d}x}{dt}=\frac{1}{2}\mu\omega^2A^2v \]

Interference

Same frequency,wavelength,amplitude,direction. Different phase.

\[\begin{align} y_1&=A\sin(kx-\omega t)\\y_2&=A\sin(kx-\omega t+\phi)\\ \y&=y_1+y_2=2A\cos\Big(\frac{\phi}{2}\Big)\sin\Big(kx-\omega t+\frac{\phi}{2}\Big) \end{align} \]

  1. When \(\cos(\phi/2)=\pm 1\), the waves are said to be everywhere in phase and thus interfere constructively. 2) When \(\cos(\phi/2)=0\), the resultant wave has zero amplitude everywhere, as a consequence of destructive interfere.

Beat

Beating is the periodic variation in intensity at a given point due to the superposition of two waves having slightly different frequencies (\(\,\)i.e. \(|f_1-f_2|\) is very small).

\[\begin{align} y_1&=A\cos(2\pi f_1 t)\\y_2&=A\cos(2\pi f_2 t)\\ \y&=y_1+y_2=2A\cos\Big(2\pi\frac{f_1-f_2}{2}t\Big)\cos\Big(2\pi\frac{f_1+f_2}{2}t\Big) \end{align} \]

The amplitude of the resultant wave varies in time.

\[\displaystyle A_{\mathrm{resultant}}=2A\cos\Big(2\pi\frac{f_1-f_2}{2}t\Big) \]

The two neighboring maxima in the envelop function are seperated by \(\displaystyle\Delta t=\frac{1}{f_1-f_2}\). And here comes the Beat Frequency: \(\displaystyle f_b=|f_1-f_2|\).

Standing Waves

Standing Waves - Same frequency,wavelength,amplitude. Different direction.

\[\begin{align} y_1&=A\sin(kx-\omega t)\\y_2&=A\sin(kx+\omega t)\\ \y&=y_1+y_2=2A\sin(kx)\cdot\cos(\omega t) \end{align} \]

  1. No sense of motions in the direction of propagation of either of the original waves. 2) Every particle of the medium oscillates in simple harmonic motion with the same frequency. 3) The amplitude of the individual waves depends on the location.

\[\begin{align} &\text{Nodes:}\quad kx=n\lambda\qquad &x=\frac{\lambda}{2},\frac{2\lambda}{2},\frac{3\lambda}{2},\cdots \&\text{Antinodes:}\quad kx=(n+\frac{1}{2})\lambda\qquad &x=\frac{\lambda}{4},\frac{3\lambda}{4},\frac{5\lambda}{4},\cdots \end{align} \]

The distance between adjacent nodes/antinodes is half the wavelength, and the distance between a node and an adjacent antinode is one fourth the wavelength.

No energy is transmitted along the string across a node, and energy does not propagate in a standing wave.

Consider a string fixed at both ends (Transverse Version). Consider standing waves in air columns (Longitudinal Version).

Harmonic Series

In general, the wavelength of the various normal modes for a string of length \(L\) fixed at both ends are \(\lambda_{n}=2L/n\quad n=1,2,3,\mathrm{etc.}\), with corresponding frequencies \(f_n=v/\lambda_{n}=n\cdot v/2L\quad n=1,2,3,\mathrm{etc.}\) , which forms a harmonic series, and the normal modes are called harmonics.

Sound Wave

Sound waves in air

\[\begin{align} \text{Displacement}&&s(x,t)\\text{Density}&&\rho(x,t)\\text{Pressure}&&P(x,t)\\end{align} \]

(initial density) \(\rho_0\longrightarrow\rho=\rho_0+\rho_e\) (displaced density)

Displacement change vs density excess

\[\rho_e=-\rho_0\frac{\partial s}{\partial x}\qquad \]

The particle number do not change:

\[\begin{align}\rho_0(x+\Delta x-x)&=\rho[x+\Delta x+s(x+\Delta x)-x-s(x,t)]\\\rho_0\Delta x&=\rho[\Delta x+\frac{\partial s}{\partial x}\Delta x]\\0&=\rho_e+\rho_0\frac{\partial s}{\partial x}\qquad \text{the density excess }\rho_e\text{ is tiny}\end{align} \]

Pressure change vs density excess

\[P_e=\kappa\rho_e\qquad\kappa=\frac{dP}{d\rho}\Big|_{\rho_0} \]

Wave equation for sound

\[\frac{1}{\kappa}\frac{\partial^2s}{\partial t^2}=\frac{\partial^2s}{\partial x^2} \]

技术图片 $$ \text{Force exerted on the volume (per unit area) = Pressure difference} $$

\[\begin{align}\rho_0\Delta x\frac{\partial^2s}{\partial t^2}=-\frac{\partial P}{\partial x}\Delta x\end{align} \]

Note that \(\displaystyle\frac{\partial P}{\partial x}=\frac{\partial P_e}{\partial x}=\kappa\frac{\partial \rho_e}{\partial x}=-\kappa\rho_0\frac{\partial^2s}{\partial x^2}\), hence we obtain \(\displaystyle \frac{1}{\kappa}\frac{\partial^2s}{\partial t^2}=\frac{\partial^2s}{\partial x^2}\).

Velocity of sound wave

\[\begin{align}v&=\sqrt{\kappa}\\P_e&=v^2\rho_e\end{align} \]

Loudness

Take the periodic sound wave soln

\[s(x,t)=s_{max}\cos(kx-\omega t) \]

Excess pressure wave is \(\pi/2\) out-of-phase with the displacement

\[P_e(x,t)=\rho_0v\omega s_{max}\sin(kx-\omega t) \]

Rmk Equilibrium atmospheric pressure \(\approx 1\times 10^5\mathrm{Nm}^{-2}\). Audible excess pressure amplitude \(\approx 2\times 10^{-5}-30\,\mathrm{Nm}^{-2}\). We only hear the order-of-magnitude...

Decibel

The sound level is measured in the logarithmic scale

\[\beta=10\log\left(\frac{P_{e}}{P_{e,ref}}\right)\qquad \mathrm{where}\ P_{e,ref}=2\times 10^{-5}\mathrm{Nm}^{-2} \]

The scale is called decibels (dB). A decibel is \(1/10\) of a bel.

Sound Intensity

The intensity of a wave is roughly the power per unit area, more precisely,

\[I=\frac{\mathscr{P}}{A}=\frac{1}{2}\rho v(\omega s_{max})^2 \]

Sound wave in solids/liquids

The elastic property of solid/fluid plays the role of the restoring force to support sound waves.

Stress the external force acting on an object per unit cross-sectional area

Strain A measure of the degree of deformation

Elasstic modulus The constant of proportionality.(depends on the material and the nature of the deformation)

  • Young‘s Modulus \(\displaystyle Y=\frac{F/A}{\Delta L/L_i}\)
  • Shear Modulus \(S=\frac{shear\ stress}{shear\ strain}\)
  • Bulk Modulus \(\displaystyle B=-\frac{\Delta P}{\Delta V/V_i}\)
技术图片 $$ \Delta P=-B\frac{\Delta V}{V_i} $$

\[\frac{\Delta V}{V}=\frac{A[s(x+\Delta x,t)-s(x,t)]}{A\Delta x}=\frac{\partial s(x,t)}{\partial x}\qquad \mathrm{as}\ \Delta x\to0 \]

Hence we have

\[P_e(x,t)=-B\frac{\partial s(x,t)}{\partial x} \]

\[\text{Force exerted on the volume (per unit area) = Pressure difference} \]

\[\begin{align}\rho_0\Delta x\frac{\partial^2s}{\partial t^2}=-\frac{\partial P}{\partial x}\Delta x\end{align} \]

Note that \(\displaystyle\frac{\partial P}{\partial x}=\frac{\partial P_e}{\partial x}=-B\frac{\partial^2s}{\partial x^2}\), we get the wave equation

\[\frac{1}{B/\rho_o}\frac{\partial^2s}{\partial t^2}=\frac{\partial^2s}{\partial x^2} \]

and the speed of sound is

\[v=\sqrt{B/\rho_0} \]

Generally, the speed of all machanical waves follows an expression of the form

\[v=\sqrt{\frac{elastic\ prop}{inertial\ prop}} \]

Sonar waves

Bulk modulus of water \(B=2\times 10^9\mathrm{Pa}\)

Density of water \(\rho=1\times 10^3\mathrm{kg/m}^3\)

\(\implies\) \(v=\sqrt{B/\rho}=1414\mathrm{m/s}\)

Speed (wave length) in water \(>\) Speed (wave length) in air

The sonar wave at this frequency can sense objects that are roughly as small as the wave length.

Doppler Effect (non-relativistic)

1)

技术图片

In the normal case,

\[\begin{equation}f=\frac{1}{T}=\frac{c}{\lambda}\end{equation} \]

2)

技术图片

In this case, \(\lambda\) is observed unchanged yet the speed is now \(c+v_0\). Hence

\[\begin{equation}f‘=\frac{1}{T‘}=\frac{c+v_0}{\lambda}=\frac{c+v_0}{c/f}=\left(1+\frac{v_0}{c}\right)f\end{equation} \]

3)

技术图片

In this case, \(v\) is observed unchanged yet the wave length observed is not \(\lambda\), as we can see in the picture below, but \(\lambda-v_sT\). Hence

\[f‘=\frac{1}{T‘}=\frac{c}{\lambda-v_sT}=\frac{\lambda f}{\lambda-v_s/f}=\frac{1}{1-\frac{v_s}{c}}f \]

4) In a Nutshell (Assuming \(v_s<c\))

技术图片 $$ \begin{align}f‘&=\frac{1}{T‘}=\frac{c+v_0}{\lambda-v_sT}=\frac{1+\frac{v_0}{c}}{1-\frac{v_s}{c}}f\qquad\text{getting closer to each other}\\f‘&=\frac{1}{T‘}=\frac{c-v_0}{\lambda-v_sT}=\frac{1-\frac{v_0}{c}}{1-\frac{v_s}{c}}f\qquad\text{S chasing O}\end{align} $$ The other two cases are $$ \begin{align}&f‘=\frac{1-\frac{v_0}{c}}{1+\frac{v_s}{c}}f\qquad\text{going away from each other}\\&f‘=\frac{1+\frac{v_0}{c}}{1+\frac{v_s}{c}}f\qquad\text{O chasing S}\end{align} $$

Shock Waves ( \(v_s>v\) )

Macn Number: \(v_s/v\)

\(\displaystyle\sin\theta=\frac{v_s}{v}\)

Review of Lectures on Wave

标签:use   normal   serve   newton   init   mes   mic   max   original   

原文地址:https://www.cnblogs.com/chs2020/p/12723167.html

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