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Publication Date
12-9-2003
Publication Title
Speleogenesis and Evolution of Karst Aquifers
Volume Number
1
Issue Number
4
Abstract
Audra, Bigot and Monochain (2003) proposed an explanation for the development of a hydrothermal cave in Provence (France), referring to the Szunyogh model (1989). Dreybrodt (2003) then shows by calculations that this model is unlikely. We will discuss Dreybrodt's answer here. Our conclusions will ephasise that Dreybrodt's hypothesis (transient conduction in a semi-infinite solid) is not the only possibility. When other conditions are considered (steady-state conduction with constant temperature at a finite distance), this cupola-development model can be valid.
Document Type
Article
Language
English
Identifier
K26-04219
Recommended Citation
Lismonde, Baudouin, "Limestone Wall Retreat in a Ceiling Cupola Controlled by Hydrothermal Degassing with Wall Condensation (Szunyogh model)" (2003). KIP Articles. 4795.
https://digitalcommons.usf.edu/kip_articles/4795
