Fluid Mechanics and order of magnitude calculation

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SUMMARY

The discussion focuses on the order of magnitude calculations in fluid mechanics, specifically regarding the Mach number (M) and its implications on the expression involving velocity (u) and density (\rho). The participants debate the validity of discarding terms of order \mathcal O(M^3) in the context of the equation uu\partial_t \rho \approx \rho_0 uu\nabla u. It is established that the derivative of velocity (du/dx) does not necessarily align with the order of M, and assumptions about flow smoothness and characteristic length scales are critical. The conversation highlights the need for a more detailed order-of-magnitude analysis akin to that used in Prandtl's boundary layer equations.

PREREQUISITES
  • Understanding of Mach number (M) in fluid dynamics
  • Familiarity with order of magnitude analysis
  • Knowledge of Prandtl's boundary layer theory
  • Basic principles of fluid mechanics and velocity gradients
NEXT STEPS
  • Study the implications of Mach number in compressible flow
  • Learn advanced order of magnitude techniques in fluid dynamics
  • Explore Prandtl's boundary layer equations and their applications
  • Investigate the role of viscous effects in fluid flow analysis
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Fluid mechanics students, researchers in aerodynamics, and engineers involved in high-speed flow analysis will benefit from this discussion.

Niles
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Hi

In my lecture notes we making some calculations and all terms \mathcal O(M^3) are to be thrown away. Here M is the Mach number. Now, there is the expression (u denotes the velocity):
<br /> uu\partial_t \rho \approx \rho_0 uu\nabla u<br />
which in my notes are thrown away because they claim it is \mathcal O(M^3). But is it really true, I mean the derivative of u will not necessarily be on the same order as Ma, right?
 
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That's right. The gradient also contains a length scale in each direction. In many cases one simply asserts on physical grounds that du/dx is same order as u (so the flow is sufficiently "smooth") or that there is some characteristic length scale of order one. Does the problem assume M << 1 and also no viscous effects?
 
I'd also postulate that there is some more complicated order-of-magnitude analysis that can be done here a la that done in deriving Prandtl's boundary layer equations, but it would be difficult to carry that out without more information from the OP on what assumptions were made and what the physical situation is.
 

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