Abstract
We describe the method used by Fowler and Krantz (1993) which reduces the Miller model of frost heave to two linear ordinary differential equations. Numerical solutions are presented and qualitative comparison is made with a numerical solution to the full system of equations given by O'Neill and Miller (1985).
Original language | English |
---|---|
Pages (from-to) | 327-336 |
Number of pages | 10 |
Journal | Cold Regions Science and Technology |
Volume | 21 |
Issue number | 4 |
DOIs | |
Publication status | Published - Jul 1993 |
Externally published | Yes |