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 59:83-87 (1995)
© 1995 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 Google Scholar
Google Scholar
Right arrow Articles by Rasiah, V.
Right arrow Articles by Kay, B. D.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Rasiah, V.
Right arrow Articles by Kay, B. D.
Agricola
Right arrow Articles by Rasiah, V.
Right arrow Articles by Kay, B. D.

Linear and Nonlinear Estimates of Fractal Dimension for Soil Aggregate Fragmentation

V. Rasiah*

Research Station, Box 1030, Swift Current, SK, Canada S9H 3X2

E. Perfect and B. D. Kay

Dep. of Land Resource Science, Univ. of Guelph, Guelph, ON, Canada N1G 2W1

* Corresponding author.

ABSTRACT

Estimates of nonlinear parameters may vary with the fitting procedure (linear or nonlinear) used. The objectives of this study were to compare (i) values of the fractal dimension, D, and the constant, k, obtained using linear (defined D1 and k1) and nonlinear (defined Dnl and knl) fitting procedures and (ii) the sensitivity of D1, Dnl, k1, and knl to variations in cropping and tillage practices and soil properties. Using aggregate mass-size distribution data, from five different soils under two cropping and two tillage systems, obtained after wet sieving, 90 values were obtained for each of D1, Dnl, knl, and kl. The nonexistence of a 1:1 relation between Dnl and D1 indicated that the population of Dnl was different from that of D1. A similar trend was observed between knl and k1. The standard error of the estimates of Dnl was less than that of D1. Soil properties and cropping and tillage systems accounted for 84% of the variability in Dnl, 87% of knl, 81% of D1, and 46% of k1. The estimates of Dnl are accurate and can be predicted with greater confidence than those obtained using the linear procedure.

Received for publication December 21, 1993.





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 © 1995 by the Soil Science Society of America.