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A platform for research: civil engineering, architecture and urbanism
Mathematical Models for Hydrologic Processes
Models of simulation of groundwater flow in sedimentary basins are generally used for water-resources optimization problems; however, a byproduct of their building may be additional information on the structure of the basins themselves.
In the first stage of the simulation procedure, the hydraulic parameters of the sediments (permeability, porosity) have to be determined, using lithostratigraphical and hydrological data. The values of these parameters are closely related to the sedimentation process itself.
Two different techniques of identification of these parameters are presented. Practical examples on Tertiary marine sediments in Aquitaine, and Quaternary alluvial sediments, will show the complement of information gained in this manner on the structure of the basins.
Mathematical Models for Hydrologic Processes
Models of simulation of groundwater flow in sedimentary basins are generally used for water-resources optimization problems; however, a byproduct of their building may be additional information on the structure of the basins themselves.
In the first stage of the simulation procedure, the hydraulic parameters of the sediments (permeability, porosity) have to be determined, using lithostratigraphical and hydrological data. The values of these parameters are closely related to the sedimentation process itself.
Two different techniques of identification of these parameters are presented. Practical examples on Tertiary marine sediments in Aquitaine, and Quaternary alluvial sediments, will show the complement of information gained in this manner on the structure of the basins.
Mathematical Models for Hydrologic Processes
Merriam, Daniel F. (editor) / de Marsily, G. (author)
1972-01-01
28 pages
Article/Chapter (Book)
Electronic Resource
English
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