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R. Freeze (1972)
Role of subsurface flow in generating surface runoff: 1. Base flow contributions to channel flowWater Resources Research, 8
T. Dunne, R. Black (1971)
Runoff Processes during SnowmeltWater Resources Research, 7
Schreiber Schreiber (1972)
Solution of a two‐dimensional, steady‐state watershed flow system, 2, Evaluation by field dataTrans. Amer. Soc. Agr. Eng., 15
R. Jeppson, D. Schreiber (1972)
Solution of a Two-Dimensional, Steady-State Watershed Flow System Part I. Description of Mathematical ModelTransactions of the ASABE, 15
R., Allan, Freeze, Ibm, T. Watson (1971)
Three-Dimensional, Transient, Saturated-Unsaturated Flow in a Groundwater BasinWater Resources Research, 7
R. Jeppson (1970)
Solution to Transient Vertical Moisture Movement Based Upon Saturation--Capillary Pressure Data and Modified Burdine Theory
T. Dunne, R. Black (1970)
An Experimental Investigation of Runoff Production in Permeable SoilsWater Resources Research, 6
R. Freeze (1972)
Role of subsurface flow in generating surface runoff: 2. Upstream source areasWater Resources Research, 8
Burdine (1953)
Relative permeability calculations from pore-size distribution dataTrans. AIME, 198
J. Robins, L. Kelly, W. Hamon (1965)
Reynolds Creek in southwest Idaho: An outdoor hydrologic laboratoryWater Resources Research, 1
McIntyre McIntyre (1972)
Cenozoic geology of the Reynolds Creek Experimental Watershed, Owyhee County, IdahoIdaho Bur. Mines Geol. Pamp., 151
J. Hewlett, A. Hibbert (1963)
Moisture and energy conditions within a sloping soil mass during drainageJournal of Geophysical Research, 68
N. Burdine (1953)
Relative Permeability Calculations From Pore Size Distribution DataJournal of Petroleum Technology, 5
D. Schreiber, R. Jeppson, G. Stephenson, C. Johnson, C. Cox, G. Schumaker (1972)
Solution of a Two-Dimensional, Steady-State Watershed Flow System Part It Evaluation by Field DataTransactions of the ASABE, 15
Jeppson Jeppson, Schreiber Schreiber (1972)
Solution of a two‐dimensional, steady‐state watershed flow system, 1, Description of mathematical modelTrans. Amer. Soc. Agr. Eng., 15
A mathematical model of subsurface flow is used to complement a field study of snowmelt runoff in a small upstream source area in the Reynolds Creek Experimental Watershed near Boise, Idaho. Field measurements from an instrumented cross section of this small watershed show that the mechanism of streamflow generation is subsurface delivery of meltwater over limited distances through shallow high‐permeability low‐porosity formations of altered and fractured basalt. The mathematical model provides a two‐dimensional transient saturated‐unsaturated analysis of the subsurface flow at the field site. It proved to be a valuable aid to a unified interpretation of the field measurements. For mathematical models that consist of boundary value problems with boundary conditions that are time and space dependent, the boundary condition sensitivity can thwart the rational calibration‐validation procedure. This, together with the more serious limitations of data availability, funds for data acquisition, and computer capacity, precludes the imminent use of fully deterministic hydrologic response models on a regional scale.
Water Resources Research – Wiley
Published: Apr 1, 1974
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