SSSAJ Grow Your Career with SSSA
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in Soil Sci Soc Am J 53:679-685 (1989)
© 1989 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Wilson, G. V.
Right arrow Articles by Alfonsi, J. M.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Wilson, G. V.
Right arrow Articles by Alfonsi, J. M.
Agricola
Right arrow Articles by Wilson, G. V.
Right arrow Articles by Alfonsi, J. M.

Spatial Variability of Saturated Hydraulic Conductivity of the Subsoil of Two Forested Watersheds

G. V. Wilson* and P. M. Jardine

Univ. of Tennessee, Knoxville, TN 37996

James M. Alfonsi

Central Michigan Univ., Mount Pleasant, MI 48859

* Corresponding author.

ABSTRACT

Subsurface flow has been shown to be greater in soils with spatially dependent hydraulic properties. The objective of this study was to quantify the spatial dependency in saturated hydraulic conductivity, Ksat, of two potential shallow waste disposal sites in eastern Tennessee. The Guelph Permeameter was used to determine Ksat of the subsoil of two forested watersheds, Walker Branch and Melton Branch. The simultaneous equations approach resulted in more than 50% negative Ksat values and was concluded to be invalid for these forested subsoils. As an alternative, flux density was used as an index of the saturated hydraulic conductivity for spatial correlation analysis and for determination of scaling factors. the spatial realizations of hydraulic conductivity for both watersheds were found to be intrinsic random functions of order zero, i.e., stationary, with a generalized covariance function for Walker Branch consisting of a pure nugget and for Melton Branch a nugget with a linear term. Semivariograms revealed no spatial dependency for separation distances >4.2 m at Walker Branch. Spatial dependency at Melton Branch for separation distances <30 m was described by an exponential model. The hydraulic conductivity of Walker Branch subsoils had a greater arithmetic mean (1.50 vs. 0.76 x 10–5 m s–1) and greater random variability than Melton Branch subsoils. These findings suggest that soils common to Walker Branch Watershed are hydrologically preferable for shallow waste disposal.


NOTES

Contribution from Environmental Sciences Div., Oak Ridge National Lab., Oak Ridge, TN 37831-6038. Research sponsored by the Ecological Research Division, Office of Health and Environmental Research, U.S. Dep. of Energy, under contract DE-AC05-840R21400 with Martin Marietta Energy Systems, Inc. Publication no. 3263, ESD, ORNL.

Received for publication February 25, 1988.


This article has been cited by other articles:


Home page
Vadose Zone JHome page
P. M. Jardine, M. A. Mayes, P. J. Mulholland, P. J. Hanson, J. R. Tarver, R. J. Luxmoore, J. F. McCarthy, and G. V. Wilson
Vadose Zone Flow and Transport of Dissolved Organic Carbon at Multiple Scales in Humid Regimes
Vadose Zone J., March 8, 2006; 5(1): 140 - 152.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
T. B. Zeleke and B. C. Si
Scaling Relationships between Saturated Hydraulic Conductivity and Soil Physical Properties
Soil Sci. Soc. Am. J., September 29, 2005; 69(6): 1691 - 1702.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
P. J. Hanson, C. W. Swanston, C. T. Garten Jr., D. E. Todd, and S. E. Trumbore
Reconciling Change in Oi-Horizon Carbon-14 with Mass Loss for an Oak Forest
Soil Sci. Soc. Am. J., August 4, 2005; 69(5): 1492 - 1502.
[Abstract] [Full Text] [PDF]


Home page
Vadose Zone JHome page
E. Perfect, L. D. McKay, S. C. Cropper, S. G. Driese, G. Kammerer, and J. H. Dane
Capillary Pressure-Saturation Relations for Saprolite: Scaling With and Without Correction for Column Height
Vadose Zone J., May 1, 2004; 3(2): 493 - 501.
[Abstract] [Full Text] [PDF]


Home page
J. Environ. Qual.Home page
L.D. McKay, A.D. Harton, and G.V. Wilson
Influence of Flow Rate on Transport of Bacteriophage in Shale Saprolite
J. Environ. Qual., July 1, 2002; 31(4): 1095 - 1105.
[Abstract] [Full Text] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Vadose Zone Journal Journal of Plant Registrations
Journal of Natural Resources
and Life Sciences Education
Journal of
Environmental Quality
Copyright © 1989 by the Soil Science Society of America.