|
|
||||||||
Univ. of Tennessee, Knoxville, TN 37996
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.
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:
![]() |
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] |
||||
![]() |
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] |
||||
![]() |
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] |
||||
![]() |
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] |
||||
![]() |
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 |
||||