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 55:787-794 (1991)
© 1991 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 Manrique, L. A.
Right arrow Articles by Dyke, P. T.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Manrique, L. A.
Right arrow Articles by Dyke, P. T.
Agricola
Right arrow Articles by Manrique, L. A.
Right arrow Articles by Dyke, P. T.

Predicting Cation-Exchange Capacity from Soil Physical and Chemical Properties

L. A. Manrique*

1290-D Maunakea St. 349, Honolulu, HI 96817

C. A. Jones and P. T. Dyke

Blackland Research Center, Texas Agric. Exp. Stn., Temple, TX 76502

* Corresponding author.

ABSTRACT

Cation-exchange capacity (CEC) is an important soil property in describing nutrient availability for plant growth. Measurements of CEC, however, are often not available or have been measured using different analytical methods. The need, therefore, exists to develop alternative procedures to predict CEC from accessory soil properties. In this study, regression analysis was used to examine the relationships between CEC and clay (CLAY), organic carbon (OC), and other soil properties. Multiple regressions indicated that CLAY, OC, and soil pH accounted for up to 51% of the variation in CEC for all soil (n = 37921). For soil orders, CLAY and OC accounted for up to 67% of the variation in CEC for Alfisols, Inceptisols, Mollisols, and Vertisols, and up to 78% of the variation in CEC for Entisols and Spodosols. The OC alone accounted for up to 73% of the variation in CEC for Spodosols. Poor predictions of CEC resulted from CLAY for Aridisols and Vertisols, indicating that factors other than CLAY interfered with accurate predictions of CEC.

Received for publication March 22, 1990.


This article has been cited by other articles:


Home page
Clay MineralsHome page
Y. YUKSELEN and A. KAYA
Prediction of cation exchange capacity from soil index properties
Clay Minerals, December 1, 2006; 41(4): 827 - 837.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
C. A. Seybold, R. B. Grossman, and T. G. Reinsch
Predicting Cation Exchange Capacity for Soil Survey Using Linear Models
Soil Sci. Soc. Am. J., May 6, 2005; 69(3): 856 - 863.
[Abstract] [Full Text] [PDF]


Home page
Vadose Zone JHome page
P. J. Vaughan, P. J. Vaughan, and D. L. Suarez
Constant Capacitance Model Computation of Boron Speciation for Varying Soil Water Content
Vadose Zone J., May 1, 2003; 2(2): 253 - 258.
[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 © 1991 by the Soil Science Society of America.