VZJ Download to Citation Manager
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published online 16 November 2005
Published in Vadose Zone J 4:1004-1010 (2005)
DOI: 10.2136/vzj2005.0028
© 2005 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Figures Only
Right arrow Full Text Free
Right arrow Full Text (PDF) Free
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 Similar articles in ISI Web of Science
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 ISI Web of Science (2)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Polyakov, V.
Right arrow Articles by Ryder, M. H.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Polyakov, V.
Right arrow Articles by Ryder, M. H.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Polyakov, V.
Right arrow Articles by Ryder, M. H.
Related Collections
Right arrow Water Content
Right arrow Soil Methods/Instrumentation

SPECIAL SECTION: SOIL WATER SENSING

Calibration of a Capacitance System for Measuring Water Content of Tropical Soil

V. Polyakov*, A. Fares and M. H. Ryder

Department of Natural Resources and Environmental Management, University of Hawaii, 1910 East-West Road, Honolulu, HI 96822
* Corresponding author (viktor{at}hawaii.edu)

Received 22 February 2005.

Capacitance sensors have improved substantially in the last decades, resulting in their wide acceptance. A new generation of multisensor capacitance systems (MCS) is now available that are easy to install and use. Calibration of capacitance sensors was conducted for a weathered clay loam soil and silica sand in field and laboratory conditions. The specific objectives of this research were to (i) conduct field and laboratory calibration of a new MCS in silica sand and soil, (ii) evaluate the performance of MCS for a shrinking–swelling tropical soil, and (iii) evaluate the effect of medium temperature on the MCS reading at constant water content. Three-parameter power type calibration equations were developed. The laboratory column calibration had higher correlation coefficients (R2 = 0.96 and 0.97 for soil and sand, respectively) than the rangeland (R2 = 0.73) and cultivated soils (R2 = 0.74). The manufacturer default model fitted the field data reasonably well in the higher moisture range (0.35–0.45 cm3 cm–3). However, it performed poorly in the dryer range (0.2–0.35 cm3 cm–3), severely underestimating soil moisture content. Shrinking and swelling of soil and the presence of bound water might have affected the sensor's performance. Across the 45°C interval, there was 15% overestimation of the actual water content for soil and only 10% for sand. The relationship was statistically highly significant (P < 0.001) with an R2 = 0.99 for both sand and soil. Use of MCS is suitable for tropical soil; however, site specific calibration is needed to improve the estimates of soil water content.

Abbreviations: MCS, multisensor capacitance system • TDR, time domain reflectometry




This article has been cited by other articles:


Home page
Vadose Zone JHome page
S. R. Evett and G. W. Parkin
Advances in Soil Water Content Sensing: The Continuing Maturation of Technology and Theory
Vadose Zone J., November 11, 2005; 4(4): 986 - 991.
[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
Soil Science Society of America Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 2005 by the Soil Science Society of America.