Hydraulic boundary conditions as a controlling factor in karst genesis: A numerical modeling study on artesian conduit development in gypsum
- 9 January 2003
- journal article
- Published by American Geophysical Union (AGU) in Water Resources Research
- Vol. 39 (1), SBH 2-1-SBH 2-14
- https://doi.org/10.1029/2002wr001308
Abstract
No abstract availableKeywords
This publication has 30 references indexed in Scilit:
- A model of the early evolution of karst aquifers in limestone in the dimensions of length and depthJournal of Hydrology, 2001
- Karst Aquifer evolution in fractured, porous rocksWater Resources Research, 2000
- Simulation of the development of karst aquifers: role of the epikarstInternational Journal of Earth Sciences, 1999
- Floods, channel change, and the hyporheic zoneWater Resources Research, 1999
- Early development of Karst aquifers on percolation networks of fractures in limestoneWater Resources Research, 1998
- Principles of Early Development of Karst Conduits Under Natural and Man‐Made Conditions Revealed by Mathematical Analysis of Numerical ModelsWater Resources Research, 1996
- Minimum hydrochemical conditions allowing limestone cave developmentWater Resources Research, 1994
- The role of the subcutaneous zone in karst hydrologyJournal of Hydrology, 1983
- Seasonal fluctuations in the chemistry of lime-stone springs: A possible means for characterizing carbonate aquifersJournal of Hydrology, 1971
- Basic concepts in the theory of seepage of homogeneous liquids in fissured rocks [strata]Journal of Applied Mathematics and Mechanics, 1960