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In signal processing, the Nyquist–Shannon sampling theorem says you need at least 2 samples of a frequency to be able to perfectly reconstruct it. So in your question, a sampling rate of $200\: \mathrm{MHz}$ means you can perfectly reconstruct frequencies in the range of $0 - 100\: \mathrm{MHz}$. So what happens when frequencies above $100\: \mathrm{MHz}$ ...
You have $\left(\frac{\partial P}{\partial T}\right)_V=\frac{\alpha_V}{\beta_T},$ where the two constants are the thermal expansion (dimension $[T]^{-1}$) and the isothermal compressibility (dimension $[P]^{-1}$), respectively. One derives at it as $|_V$ leads one to consider $0\overset{!}{=}\mathrm dV(P,T) = \left(\frac{\partial V}{\partial ... 1 Warning : I absolutely don't know nothing about the subject. If you are a french locutor, applyed notion of kinematical inversion (and dynamical inversion) to the Tottori earthquake are explained in this thesis (Sara Di Carli), see page$4$for a abstract, and pages$11-29$for details. The Haskell Model(1964) seems to be the first model. In the ... 1 Actually I think I disagree with the answer by BMS (the group of asymptotic symmetries of asymptotically flat spacetimes?). However I am not sure to have understood BMS'answer completely. In my opinion, there is no difference between the definition of work in pure mechanics and work in thermodynamics (I stress that I am speaking of thermodynamics and not ... 1 Here is one issue where thermodynamics and mechanics could differ in the definitions of work. In mechanics, a non-careful, ambiguous, but common definition for the work done by a force$\vec{F}$is$\int\vec{F}\cdot d\vec{s}$. The problem with this is that we're not told which infinitesimal displacement$d\vec{s}\$ to use; one could use (1) the infinitesimal ...