- Why is the speed distribution not a bell curve (Gaussian) like the individual velocity components?
- The distribution of a single velocity component is Gaussian, but speed (v = √(v_x²+v_y²+v_z²)) is a positive quantity derived from three independent Gaussians. The probability of finding a particle with a given speed v is proportional to the surface area of a sphere of radius v in velocity space (4πv²) multiplied by the Gaussian probability density at that radius. The v² term causes the distribution to start at zero, peak, and then decay exponentially, creating its characteristic skewed shape.
- What does increasing the temperature actually do to the gas molecules?
- Increasing temperature increases the average kinetic energy of the molecules. In the simulator, this is seen as a broadening and shifting of the speed distribution to higher speeds. The entire curve becomes flatter and wider, meaning a greater fraction of molecules have very high speeds. This explains phenomena like increased rates of chemical reaction and evaporation with temperature.
- Why does the histogram sometimes look 'lumpy' and not perfectly smooth like the theoretical curve?
- The histogram is built from a finite number of random samples. With a small sample size (e.g., 100 particles), statistical fluctuations are significant, making the histogram jagged. This is a key lesson in statistics: the theoretical PDF describes the probability for an infinite ensemble. Increasing the sample size in the simulator reduces these fluctuations, causing the histogram to converge smoothly onto the predicted curve, illustrating the Law of Large Numbers.
- Is the Maxwell–Boltzmann distribution applicable to real gases?
- It is an excellent approximation for real gases under ordinary conditions (low density, moderate temperatures) where intermolecular forces are negligible. At very high densities or near condensation points, interactions between particles become significant, and the distribution can deviate. It also assumes the gas is in thermal equilibrium, meaning it does not describe systems with strong temperature gradients or flows.