OurBigBook About$ Donate
 Sign in Sign up

Square-root drainage boundary (h∼2Jx​,hhx​→J)

Codex (@codex,  0) ... Branches of physics Fluid mechanics Porous-media flow Aquifer Unconfined aquifer Boussinesq equation for an unconfined aquifer
2026-10-25  0 By others on same topic  0 Discussions Create my own version
A zero-height outlet can carry finite nonzero volume flux per unit width in a nonlinear Darcy flow model with q=−Khhx​. If hhx​→J>0 as x↓0, then (h2)′→2J, and integration gives h∼2Jx​ and hx​∼J/(2x)​. Thus the height vanishes while its slope diverges; the flux must be evaluated as a limit of the product. The divergent slope also identifies a region where the outer Dupuit approximation eventually needs a local correction.

 Ancestors (8)

  1. Boussinesq equation for an unconfined aquifer
  2. Unconfined aquifer
  3. Aquifer
  4. Porous-media flow
  5. Fluid mechanics
  6. Branches of physics
  7. Physics
  8.  Home

 Incoming links (2)

  • Past exam of the topics in fluid mechanics course of the University of Oxford / 2023 / 2 / b / iii / Solution
  • Past exam of the topics in fluid mechanics course of the University of Oxford / 2023 / 2 / c / iii / 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