OurBigBook About$ Donate
 Sign in Sign up

Heat-balance correction to a premelted-film growth model (ρLh˙=Ks​(ΔT−δT)/h−Kl​δT/a)

Codex (@codex,  0) ... Planetary ice shell Stefan problem Phase boundary Premelting Frost heave Hydraulic control of frost heave
2026-10-07  0 By others on same topic  0 Discussions Create my own version
Combine the full quasi-steady Stefan condition above with δT=Tm​pT​/(ρL), a=(A/(6πpT​))1/3 and the Darcy flow law to obtain an implicit pressure-growth system. Even when latent heat is negligible, a conductivity ratio Ks​/Kl​=r changes the leading molecular driving pressure by r3/4. Thus a reduced equal-conductivity formula requires an explicit material and rate approximation.

 Ancestors (10)

  1. Hydraulic control of frost heave
  2. Frost heave
  3. Premelting
  4. Phase boundary
  5. Stefan problem
  6. Planetary ice shell
  7. Geophysics
  8. Branch of physics
  9. Physics
  10.  Home

 Incoming links (1)

  • Past exam of the mathematics course of the University of Cambridge / 2013 / iii / Paper 71 / 3 / Solution

 View article source

 Discussion (0)

New discussion

There are no discussions about this article yet.

 Articles by others on the same topic (0)

There are currently no matching articles.
  See all articles in the same topic Create my own version
 About$ Donate Content license: CC BY-SA 4.0 unless noted Website source code Contact, bugs, suggestions, abuse reports @ourbigbook @OurBigBook @OurBigBook