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Analytical Solutions for Steady Phreatic Flow Appearing/Re-emerging Toward/from a Bedrock/Caprock Isobaric Breach: The Polubarinova-Kochina–Numerov and Pavlovsky Problems Revisited analytical solutions, the aquifers are sloping and the “window” is a finite-size isobaric segment, which due
Analytical Solutions for Steady Phreatic Flow Appearing/Re-emerging Toward/from a Bedrock/Caprock Isobaric Breach: The Polubarinova-Kochina–Numerov and Pavlovsky Problems Revisited analytical solutions, the aquifers are sloping and the “window” is a finite-size isobaric segment, which due
Hydrogeological conditions of extra-heavy oil fields in western slope of South-Tatarian Arch and eastern flank of melekess depression in Tatarstan to the fore. In Tatarstan, heavy oil accumulations are confined to the western slope of the South
Optimization of the drainage system of overburden dumps using geofiltration modeling aquifers, precipitation infiltration, as well as the projected dumps are located on the slope surface
Groundwater flow in hillslopes: Analytical solutions by the theory of holomorphic functions and hydraulic theory© 2014 Elsevier Inc. Three 2-D steady Darcian flows in an aquifer with a subjacent confining layer
Groundwater flow in hillslopes: Analytical solutions by the theory of holomorphic functions and hydraulic theory© 2014 Elsevier Inc. Three 2-D steady Darcian flows in an aquifer with a subjacent confining layer
Simulation of contaminant transport in a fractured porous aquiferSolute transport in the fractured porous confined aquifer is modeled by the advection
Modelling of Natural Attenuation of Chlorinated Solvents constituents Of Emplaced Source in Virtual Aquifer Aquifer
Simulation of contaminant transport in a fractured porous aquiferSolute transport in the fractured porous confined aquifer is modeled by the advection
An exact analytical solution for steady seepage from a perched Aquifer to a low-permeable sublayer: Kirkham-Brock's legacy revisitedAn exact analytical solution for steady seepage from a perched Aquifer to a low-permeable sublayer
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