Water flow in a hummocky landscape in central Saskatchewan, Canada, II. Saturated flow and groundwater recharge
- 1 September 1989
- journal article
- research article
- Published by Elsevier in Journal of Hydrology
- Vol. 110 (1-2) , 181-198
- https://doi.org/10.1016/0022-1694(89)90243-6
Abstract
No abstract availableThis publication has 14 references indexed in Scilit:
- Transient seepage model for saturated–unsaturated soil systems: a geotechnical engineering approachCanadian Geotechnical Journal, 1987
- Fracture permeability and groundwater flow in clayey till near Saskatoon, SaskatchewanCanadian Geotechnical Journal, 1986
- TRANSIENT GROUNDWATER FLOW SURROUNDING A RECHARGE SLOUGH IN A TILL PLAINCanadian Journal of Soil Science, 1986
- GROUNDWATER DISCHARGE FROM GLACIAL AND BEDROCK AQUIFERS AS A SOIL SALINIZATION FACTOR IN SASKATCHEWANCanadian Journal of Soil Science, 1985
- THE EFFECT OF GROUNDWATER ON SOIL FORMATION IN A MORAINAL LANDSCAPE IN SASKATCHEWANCanadian Journal of Soil Science, 1985
- Natural groundwater recharge in an upland area of central North Dakota, U.S.A.Journal of Hydrology, 1982
- SOIL GENESIS IN RELATION TO GROUNDWATER AND SOIL MOISTURE REGIMES NEAR VEGREVILLE, ALBERTA1European Journal of Soil Science, 1975
- Unsteady groundwater flow near a willow ring in hummocky moraineJournal of Hydrology, 1966
- The Theory Of Seepage From Clay-Blanketed ReservoirsGéotechnique, 1959
- METHODS OF MAKING MECHANICAL ANALYSES OF SOILSSoil Science, 1949