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


     


Published online 1 May 2009
Published in Soil Sci Soc Am J 73:886-897 (2009)
DOI: 10.2136/sssaj2008.0194
© 2009 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Figures Only
Right arrow Full Text
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 Schwartz, R. C.
Right arrow Articles by Bell, J. M.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Schwartz, R. C.
Right arrow Articles by Bell, J. M.
Agricola
Right arrow Articles by Schwartz, R. C.
Right arrow Articles by Bell, J. M.
Related Collections
Right arrow Soil Methods/Instrumentation
Right arrow Water Content
Right arrow Time Domain Reflectometry, TDR

SOIL PHYSICS

Complex Permittivity Model for Time Domain Reflectometry Soil Water Content Sensing: I. Theory

R. C. Schwartza,*, S. R. Evetta, M. G. Pelletierb and J. M. Bella

a USDA-ARS, Conservation and Production Research Lab., Bushland, TX 79012
b USDA-ARS, Cropping Systems Research Lab., Lubbock, TX 79403

* Corresponding author (robert.schwartz{at}ars.usda.gov).

Despite numerous applications of time-domain reflectometry (TDR), serious difficulties remain in estimating accurate soil water contents under field conditions, especially in fine-textured soils. We developed a physically based calibration model to predict the frequency- and temperature-dependent complex dielectric response of soils. The model was used to predict frequency-dependent attenuation and a single "effective" frequency approximation of apparent permittivity of the soil. Effective frequency was predicted to decline from 450 to 160 MHz as water contents increased from air dry to saturation. Predicted frequency decline was small for an input bandwidth of 130 MHz, reflecting that modeled polarization mechanisms associated with relaxation frequencies above 100 MHz were responsible for most of the frequency-dependent attenuation. For specific surface areas ranging from 150 to 300 m2 g–1, simulations indicate that ignoring dielectric and conductive losses or the associated decline in effective frequency results in a 5 to 22% underestimation of the apparent permittivity. Both the power-law and de Loor–Dobson mixing models gave a reasonable approximation to the measured apparent permittivity for a silty clay loam (34% clay) across the entire water content range. Moreover, the models were able to describe the behavior of apparent permittivity in response to temperature for two soils with contrasting bulk electrical conductivity contributions to losses. These results demonstrate that loss mechanisms and declines in effective frequency need to be considered to accurately predict the soil water content of fine-textured soils.

Abbreviations: dc, direct current • PDF, probability density function • TDR, time domain reflectometry




This article has been cited by other articles:


Home page
Soil Sci.Home page
R.C. Schwartz, S.R. Evett, and J.M. Bell
Complex Permittivity Model for Time Domain Reflectometry Soil Water Content Sensing: II. Calibration
Soil Sci. Soc. Am. J., May 1, 2009; 73(3): 898 - 909.
[Abstract] [Full Text] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 2009 by the Soil Science Society of America.