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A combined model of water table and river stage evolution
Author(s) -
MorelSeytoux H. J.
Publication year - 1975
Publication title -
water resources research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.863
H-Index - 217
eISSN - 1944-7973
pISSN - 0043-1397
DOI - 10.1029/wr011i006p00968
Subject(s) - stage (stratigraphy) , aquifer , hydrology (agriculture) , water table , groundwater , flooding (psychology) , function (biology) , geology , water level , environmental science , mathematics , geotechnical engineering , geography , paleontology , psychology , cartography , evolutionary biology , psychotherapist , biology
An integral equation is derived which completely characterizes the interaction between a stream and the alluvial aquifer. Expressed in finite difference form, the equation is of great practical utility to solve pure flooding problems (i.e., negligible effect of pumping on river flows) as it relates river stages to return flows, pure conjunctive use of surface water and groundwater problems (i.e., negligible river stage fluctuations) as it relates return flows to pumping rates, or to solve composite problems. The numerical procedures to calculate the response function coefficients in terms of the physical characteristics of the system are given in detail.

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