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pro vyhledávání: '"Salem Al-Shidi"'
Publikováno v:
Hydrological Sciences Journal. 54:174-188
Decay or rise of the water table from a disturbed (mound or trough) position to a quiescent flat state is studied by a linear potential theory that does not rely on the Dupuit-Forchheimer vertical averaging but is a solution to the full Laplace equat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ac37f63cfd1649f79b6a90049f9ee4ac
https://doi.org/10.1623/hysj.54.1.174
https://doi.org/10.1623/hysj.54.1.174
