Abstract
Governing equations for a one-phase Stefan melting problem with variable latent heat are presented. It is shown that these equations model the movement of the shoreline in a sedimentary basin. An analytical solution for the sedimentation rate and shoreline movement - based on a similarity variable - shows a square root dependence of shoreline position with time.
Original language | English (US) |
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Pages (from-to) | 5387-5390 |
Number of pages | 4 |
Journal | International Journal of Heat and Mass Transfer |
Volume | 47 |
Issue number | 24 |
DOIs | |
State | Published - Nov 2004 |
Bibliographical note
Funding Information:This work was supported by the STC program of the National Science Foundation via the National Center for Earth-surface Dynamics under the agreement number EAR-0120914. The authors acknowledge useful discussion with Gary Parker.