Comparison of laplace transform and finite difference solutions for an evolving permafrost region

Abstract Laplace transform solutions are derived for an evolving permafrost region in saturated ground when the freezing interface moves with constant speed. The solution is inverse in the sense that the melting temperature at the interface and the groud surface temperature are prescribed functions...

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Bibliographic Details
Published in:International Journal for Numerical and Analytical Methods in Geomechanics
Main Authors: Morland, L. W., Kelly, R. J.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1990
Subjects:
Online Access:http://dx.doi.org/10.1002/nag.1610140904
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fnag.1610140904
https://onlinelibrary.wiley.com/doi/pdf/10.1002/nag.1610140904