Spatial Variability of Saturated Hydraulic Conductivity of the Subsoil of Two Forested Watersheds
- 1 May 1989
- journal article
- research article
- Published by Wiley in Soil Science Society of America Journal
- Vol. 53 (3) , 679-685
- https://doi.org/10.2136/sssaj1989.03615995005300030005x
Abstract
No abstract availableFunding Information
- U.S. Department of Energy (DE‐AC05‐840R21400)
This publication has 9 references indexed in Scilit:
- Infiltration, Macroporosity, and Mesoporosity Distributions on Two Forested WatershedsSoil Science Society of America Journal, 1988
- Kriging with Generalized CovariancesSoil Science Society of America Journal, 1987
- SPATIAL DEPENDENCE OF SOIL-WATER POTENTIALS ASSOCIATED WITH SEPTIC SYSTEMSSoil Science, 1987
- AN ANALYSIS OF THE PERCOLATION TEST BASED ON THREE-DIMENSIONAL SATURATED-UNSATURATED FLOW FROM A CYLINDRICAL TEST HOLESoil Science, 1986
- IN SITU MEASUREMENT OF FIELD-SATURATED HYDRAULIC CONDUCTIVITY, SORPTIVITY, AND THE α-PARAMETER USING THE GUELPH PERMEAMETERSoil Science, 1985
- A COMPARISON OF THREE FIELD METHODS FOR MEASURING SATURATED HYDRAULIC CONDUCTIVITYCanadian Journal of Soil Science, 1985
- THE CONSTANT HEAD WELL PERMEAMETERSoil Science, 1985
- Areal Variation and Chemical Modification of Weathered Shale Infiltration CharacteristicsSoil Science Society of America Journal, 1981
- Scaling field‐measured soil hydraulic properties using a similar media conceptWater Resources Research, 1977