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 55:481-485 (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 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 ISI Web of Science (9)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Rolston, D. E.
Right arrow Articles by Bedaiwy, M. N. A.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Rolston, D. E.
Right arrow Articles by Bedaiwy, M. N. A.
Agricola
Right arrow Articles by Rolston, D. E.
Right arrow Articles by Bedaiwy, M. N. A.

Micropenetrometer for In Situ Measurement of Soil Surface Strength

D. E. Rolston* and D. T. Louie

Dep. of Land, Air and Water Resources, Univ. of California, Davis, CA 95616

M. N. A. Bedaiwy

Faculty of Agriculture, Soil and Water Science Dep., Univ. of Alexandria, El-Chatby Alexandria, Egypt

*Corresponding author.

ABSTRACT

Soil surface characteristics greatly influence seedling emergence, water infiltration, and soil erosion. A portable micropenetrometer was designed to measure the strength of the soil surface (or crust) as an indirect measure of soil surface characteristics in the field. The penetrometer is designed to operate on a 12 V DC battery and is controlled by a portable microcomputer. Penetrometer measurements can be made a few millimeters apart along 1-m long transects with a small (1.6 mm) probe in order to evaluate spatial patterns of crust strength. Laboratory and field measurements show that the penetrometer is capable of detecting detailed differences in the nearsurface soil (0–4 mm depth) that result from different physical, chemical, and management-related conditions. Penetration measurements from 0 to 30-mm depth at 0.1-mm depth increments reflected differences in the structure of the surface soil layer due to irrigation method by detecting sequences of aggregates and pores as the probe penetrated the soil. These results indicate that the micropenetrometer is capable of detecting and quantifying differences in soil surface characteristics influencing physical processes at the soil surface.


NOTES

Contribution from the Dep. of Land, Air and Water Resources, and the California Agric. Exp. Stn., Univ. of California. Research was conducted with funding from the Kearney Foudnation of Soil Science.

Received for publication March 12, 1990.





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 © 1991 by the Soil Science Society of America.