SSSAJ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in Soil Sci Soc Am J 61:742-745 (1997)
© 1997 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 Friedman, S. P.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Friedman, S. P.
Agricola
Right arrow Articles by Friedman, S. P.

Statistical Mixing Model for the Apparent Dielectric Constant of Unsaturated Porous Media

Shmulik P. Friedman*

Institute of Soils and Water, The Volcani Center, Agricultural Research Organization, Bet Dagan 50250, Israel

*Corresponding author (vwsfried{at}volcani.agri.gov.il).

ABSTRACT

A statistical model is proposed that relates the apparent dielectric constant of an unsaturated porous medium to its porosity and volumetric water content. It is assumed that the solid, water, and air components are randomly distributed in space. The unsaturated soil, or other porous media, are considered as a three-dimensional network of capacitors, with a distribution of capacitance values according to the volume fractions of the three components. Taking into consideration the simplifying assumptions embedded in the model and the fact that no calibration is required, a fair agreement was demonstrated between its prediction and the widely used empirical function of Topp. The basic model presented can be further developed to account for other soil properties by lifting some of the simplifying assumptions. The objectives of this study were to provide some additional insight into the way the volume fractions of the three soil phases determine its apparent dielectric constant, and to introduce a new approach for further investigation of this phenomenon. It is not intended to propose a new universal model relating the volumetric water content to its measured apparent dielectric constant.

Received for publication February 19, 1996.


This article has been cited by other articles:


Home page
Soil Sci.Home page
D. A. Robinson, S. B. Jones, J. M. Blonquist Jr., and S. P. Friedman
A Physically Derived Water Content/Permittivity Calibration Model for Coarse-Textured, Layered Soils
Soil Sci. Soc. Am. J., August 4, 2005; 69(5): 1372 - 1378.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
T. Miyamoto, T. Annaka, and J. Chikushi
Extended Dual Composite Sphere Model for Determining Dielectric Permittivity of Andisols
Soil Sci. Soc. Am. J., January 1, 2005; 69(1): 23 - 29.
[Abstract] [Full Text] [PDF]


Home page
Vadose Zone JHome page
D. A. Robinson, D. A. Robinson, S. B. Jones, J. M. Wraith, D. Or, and S. P. Friedman
A Review of Advances in Dielectric and Electrical Conductivity Measurement in Soils Using Time Domain Reflectometry
Vadose Zone J., November 1, 2003; 2(4): 444 - 475.
[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 © 1997 by the Soil Science Society of America.