Anisotropy and depth-related heterogeneity of hydraulic conductivity in a bog peat. II: modelling the effects on groundwater flow
- 13 November 2002
- journal article
- research article
- Published by Wiley in Hydrological Processes
- Vol. 17 (1), 103-113
- https://doi.org/10.1002/hyp.1117
Abstract
No abstract availableKeywords
This publication has 19 references indexed in Scilit:
- Fine-scale characteristics of groundwater flow in a peatlandHydrological Processes, 1999
- Regional and local hydrogeology of calcareous fens in the Minnesota River basin, USAWetlands, 1998
- The baseflow and storm flow hydrology of a precambrian shield headwater peatlandHydrological Processes, 1998
- Groundwater-surface water interactions in headwater forested wetlands of the Canadian ShieldJournal of Hydrology, 1996
- Hydrological model of peat‐mound form with vertically varying hydraulic conductivityEarth Surface Processes and Landforms, 1995
- The Bouwer and Rice Slug Test — An UpdateaGroundwater, 1989
- HYDRAULIC CONDUCTIVITY AND RELATED PHYSICAL PROPERTIES OF PEAT, LOST RIVER PEATLAND, NORTHERN MINNESOTASoil Science, 1986
- Theoretical Analysis of Regional Ground Water Flow: 3. Quantitative InterpretationsWater Resources Research, 1968
- Theoretical analysis of regional groundwater flow: 2. Effect of water‐table configuration and subsurface permeability variationWater Resources Research, 1967
- Theoretical analysis of regional groundwater flow: 1. Analytical and numerical solutions to the mathematical modelWater Resources Research, 1966