SSSAJ Grow Your Career with SSSA
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


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 (4)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Thomas, P.J.
Right arrow Articles by Zelazny, L.W.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Thomas, P.J.
Right arrow Articles by Zelazny, L.W.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Thomas, P.J.
Right arrow Articles by Zelazny, L.W.
Soil Science Society of America Journal 64:268-274 (2000)
© 2000 Soil Science Society of America

DIVISION S-5-PEDOLOGY

An Expansive Soil Index for Predicting Shrink–Swell Potential

P.J. Thomasa, J.C. Bakera and L.W. Zelaznya

a Dep. of Crop and Soil Environmental Sciences, Virginia Polytechnic Inst. and St. Univ., Blacksburg, VA 24061-0404 USA

pthomas{at}vt.edu

Soil properties indicative of shrink–swell potential were studied for 12 soils encompassing several parent materials in Virginia. Soils are rated from moderate to very high shrink–swell potential. The mineralogy classes, soil series, and (parent materials) examined include: smectitic—Iredell (hornblende gneiss), Jackland and Waxpool (diabase); vermiculitic—Kelly (thermal shale); kaolinitic—Cecil (granite gneiss) and Davidson (diabase); and mixed—Carbo and Frederick (limestone), Craven and Peawick (Coastal Plain sediments), and Mayodan and Creedmoor (Triassic sandstones). Soil properties measured were swell index, coefficient of linear extensibility (COLE), particle-size distribution, cation-exchange capacity (CEC), liquid limit, plasticity index (PI), and clay mineralogy. Soils with estimated high or very high shrink–swell potential were clayey, with clay contents exceeding 60%. These expansive soils also exhibited high CEC (>15 cmolc kg-1 soil), high liquid limits (>70), and appreciable swelling 2:1 mineral content (>15% montmorillonite + 1/2 vermiculite on whole-soil basis). An expansive soil rating system, termed the Expansive Soil Index (ESI), was developed using the soil properties most correlated with shrink–swell potential. The sum of swelling 2:1 minerals, swell index, liquid limit, and CEC gave ESI ratings for each soil series. The higher the ESI, the greater the shrink–swell potential. Where less-detailed information is required, such as for initial feasibility studies, an ESI consisting of liquid limit and CEC is recommended. Finally, the soils were grouped into risk categories based on parent material to allow for classification of similar soils into the ESI rating system. Soils with restricted drainage formed from mafic rocks, carbonate parent material, and metamorphic shales are at high risk for expansive soil behavior.

Abbreviations: CEC, cation-exchange capacity • COLE, coefficient of linear extensibility • ESI, Expansive Soil Index • LEP, linear extensibility percentage • PI, plasticity index • PVC, potential volume change • SSA, specific surface area




This article has been cited by other articles:


Home page
Soil Sci.Home page
R. Vaught, K. R. Brye, and D. M. Miller
Relationships among Coefficient of Linear Extensibility and Clay Fractions in Expansive, Stoney Soils
Soil Sci. Soc. Am. J., October 27, 2006; 70(6): 1983 - 1990.
[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 © 2000 by the Soil Science Society of America.