A platform for research: civil engineering, architecture and urbanism
Unconfined ground water flow to multiple wells
Effect of capillary fringe on location of free surface, form of flow patterns, zone of validity of Dupuit equation, shape of free surface near well, and variation in stream surface spacing; fundamental dimensionless parameter consisting of ratio of Froud's to Reynolds numbers characterizes shape of cone of depression around well.
Unconfined ground water flow to multiple wells
Effect of capillary fringe on location of free surface, form of flow patterns, zone of validity of Dupuit equation, shape of free surface near well, and variation in stream surface spacing; fundamental dimensionless parameter consisting of ratio of Froud's to Reynolds numbers characterizes shape of cone of depression around well.
Unconfined ground water flow to multiple wells
Unconfined Ground Water Flow to Multiple Wells
Hansen, V.E. (author)
1952
18 pages
Article (Journal)
English
© Metadata Copyright Elsevier B. V. All rights reserved.
Unconfined Ground-Water Flow to Multiple Wells
ASCE | 2021
|Hydraulics of wells in unconfined aquifers
Engineering Index Backfile | 1962
|Hydraulics of Wells in Unconfined Aquifers
ASCE | 2021
|Unconfined Expansion of Supercritical Water Flow
Online Contents | 1997
|Modeling Ground Water Mounding in a Heterogeneous Unconfined Aquifer
British Library Conference Proceedings | 1993
|