The Laplace formula is a result in fluid mechanics that gives the surface pressure between two continuous media. The surface of separation is really a transitional layer, but it is so thin that in classical mechanics it can be considered a dividing surface between the two media.

Definition

Consider two continuous media (top and bottom) whose surface of separation undergoes a small displacement. If \(r_t\) and \(r_b\) are the principal radii of curvature of the surface in some sample region, then the difference of pressures is

\[\Delta P = \alpha\left(\frac{1}{r_t}+\frac{1}{r_b}\right)\]

where \(\alpha\) is the surface pressure.

See also

References

  • Landau, L.D. and Lifschitz, E.M. Fluid Mechanics. Oxford : Butterworth-Heinemann, 1987.


ar:صيغة لابلاس