Natural groundwater recharge in an upland area of central North Dakota, U.S.A.
- 1 November 1982
- journal article
- research article
- Published by Elsevier in Journal of Hydrology
- Vol. 59 (3-4), 293-314
- https://doi.org/10.1016/0022-1694(82)90093-2
Abstract
No abstract availableThis publication has 14 references indexed in Scilit:
- An analysis of areal infiltration considering spatial variabilityJournal of Hydrology, 1981
- Effects of spatial variability of soil hydraulic properties in water budget modelingWater Resources Research, 1977
- Hydrology of Saline Seeps in the Northern Great PlainsTransactions of the ASAE, 1976
- SPATIAL VARIABILITY OF IN SITU UNSATURATED HYDRAULIC CONDUCTIVITY OF MADDOCK SANDY LOAMSoil Science, 1976
- The Fracture Porosity of Glacial TillCanadian Journal of Earth Sciences, 1975
- The mechanism of natural ground‐water recharge and discharge: 2. Laboratory column experiments and field measurementsWater Resources Research, 1970
- The Mechanism of Natural Ground‐Water Recharge and Discharge: 1. One‐dimensional, Vertical, Unsteady, Unsaturated Flow above a Recharging or Discharging Ground‐Water Flow SystemWater Resources Research, 1969
- Soil water translocation in a high water table areaWater Resources Research, 1968
- Unsteady groundwater flow near a willow ring in hummocky moraineJournal of Hydrology, 1966
- The nonsteady state of the water table in drained landJournal of Geophysical Research, 1960