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====== Wave Packets ====== | ====== Wave Packets ====== | ||
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+ | The wavefunction $\psi(x,t) = e^{i(kx-\omega t)}$ represents a free particle with definite momentum $p=\hbar k$ abd $E = \hbar \omega$. | ||
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+ | The wavefunction $\psi(x) = \delta(x-x_0)$ is localized at $x_0$, but has infinite momentum uncertainty. | ||
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+ | We can get more realistic solutions by superposing different momentum states: | ||
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+ | \[\psi(x,t) = \frac{1}{\sqrt{2\pi\hbar}} \int_{-\infty}^{+\infty} \phi(p) e^{i(px-Et)/ | ||
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+ | For the Gaussian wavepacker | ||
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+ | \[\psi_0(x) = \left ( \frac{1}{2\pi\sigma_2}\right )^{\frac{1}{4}} e^{-x^2/ | ||
+ | we derived $\Delta x = \sigma$, $\Delta p = \hbar/ | ||
+ | \[\Delta x \Delta p \geq \frac{\hbar}{2}.\] | ||
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+ | They are well-localized in both position and momentum, as illustrated below. | ||
+ | {{ : | ||
===== Phase and Group Velocity ===== | ===== Phase and Group Velocity ===== | ||
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+ | {{ : | ||
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+ | The relationship $\omega(k)$ between angular frequency and wave number is called the // | ||
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+ | Generally, the //**phase velocity**// | ||
+ | \[v_p = \frac{\omega}{k}.\] | ||
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+ | The //**group velocity**// | ||
+ | \[v_g = \frac{\D \omega}{\D k}.\] | ||
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+ | When there is dispersion, i.e. $\omega \neq ck$, the group and phase velocities differ. | ||
+ | \[H = \frac{p^2}{2m} + V,\] | ||
+ | with $V$ constant, we have | ||
+ | \begin{align*} | ||
+ | v_p & = \frac{p}{2m} + \frac{V}{p}, | ||
+ | \end{align*} | ||
+ | so the group velocity corresponds to the velocity of a classical particle. | ||
===== Spreading of Wave Packets ===== | ===== Spreading of Wave Packets ===== | ||
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+ | {{ :: | ||
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+ | When there is dispersion, wave packets spread in time. For a Gaussian wave packet with initial position uncertainty $\sigma_0$, the uncertainty at time $t$ grows to | ||
+ | \[\sigma_t = \sigma_0 \sqrt{1 + \frac{\hbar^2 t^2}{4m^2\sigma_0^4}}.\] | ||
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