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 45:1210-1214 (1981)
© 1981 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 Cruse, R. M.
Right arrow Articles by Averette, F. G.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Cruse, R. M.
Right arrow Articles by Averette, F. G.
Agricola
Right arrow Articles by Cruse, R. M.
Right arrow Articles by Averette, F. G.

Effect of Particle Surface Roughness on Mechanical Impedance of Coarse-Textured Soil Materials1

R. M. Cruse, D. K. Cassel, R. E. Stitt and F. G. Averette2

ABSTRACT

Packing energy required to increase bulk density in coarse-textured soils is influenced by particle surface roughness, i.e., by interparticle friction. It was, therefore, hypothesized that particle surface roughness would influence soil resistance to movement of a cone penetrometer, because soil bulk density is increased in the zone surrounding the penetrometer tip during its advance. The cone index (C.I.) was calculated for all penetrometer measurements, and C.I. was compared in both disturbed and undisturbed coarse-textured soil material, with each soil having a unique particle surface roughness as determined by the dense soil angle of repose measurement. For soil materials with similar particle size distributions and bulk densities, C.I. increased as particle surface roughness increased.

The role of particle surface roughness in tillage pan formation and in root growth restriction is discussed. It is suggested that, due to poorer aeration during rainy periods and higher mechanical resistance during drier conditions, tillage pans formed in soil materials having smoother-surfaced particles will be more restrictive to root growth compared to those pans formed in soil materials having rougher-surfaced particles. Consequently, among soils having root-restricting tillage pans, the greater enhancement of rooting depth due to subsoiling would likely occur on soils with smooth particles compared to soils with rough soil particles.


NOTES

1 Contribution from the Dep. of Soil Science, North Carolina State Univ. Paper no. 6,788 of the Journal Ser. of the North Carolina Agric. Res. Service, Raleigh, NC 27650.

2 Asst. Professor, Professor, Research Assistant, and Research Technician, respectively, North Carolina State Univ., Raleigh, NC 27650. The Senior Author is currently with the Dep. of Agron., Iowa State Univ., Ames.

Received for publication February 2, 1981. Accepted for publication July 24, 1981.







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 © 1981 by the Soil Science Society of America.