JEQ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in J Environ Qual 20:403-407 (1991)
© 1991 American Society of Agronomy, Crop Science Society of America, and 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
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Edwards, L. M.
Right arrow Articles by Burney, J.R.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Edwards, L. M.
Right arrow Articles by Burney, J.R.
Agricola
Right arrow Articles by Edwards, L. M.
Right arrow Articles by Burney, J.R.

Sediment Concentration of Interrill Runoff under Varying Soil, Ground Cover, Soil Compaction, and Freezing Regimes

Linnell M. Edwards*

Agriculture Canada, Research Branch, Prince Edward Island, Canada C1A 7M8;

J.R. Burney

Technical University of Nova Scotia, Dep. of Agricultural Engineering, Nova Scotia, Canada B3J 2X4.

* Corresponding author.

ABSTRACT

Sediment concentration (SC) was the focus of this study, which is part of a wider investigation into runoff volume and sediment mass. In the present study, SC of runoff was measured from three Prince Edward Island (Canada) soils (loam, sandy loam, and fine sandy loam surface texture) subjected to laboratory rainfall simulation to assess the effect of ground cover [winter rye (Secale cereale L.) or straw], subsoil compaction, and freezing (10 days' continuous freeze or daily freeze/thaw). Sediment concentration for the loam was 47 and 50% greater than the other soils. Straw cover gave SC of 23% < bare surface, and winter rye 25% < bare surface. Freezing treatment had no first-order effect on SC but interacted with soil type and with ground cover. The loam showed 30% greater SC based on lower runoff volume with daily freeze/thaw than with continuous freeze. Freeze/thaw resulted in a 54% greater SC than continuous freeze. Freeze/thaw caused numerous surface cracks in the soil and enhanced internal drainage, thus resulting in less runoff than continuous freeze. A regression analysis of the relationship between SC and winter rye cover showed that variations in SC were dominated, 53%, by sediment mass (compared with 18% by runoff volume). Variations in rye cover were dominated, 49%, by leaf area (compared with 8% by leaf mass and 5% by root mass). Although this study found increasing SC to occur with subsurface soil compaction for all three soils, and the loam to be particularly susceptible to daily freeze/thaw, any adverse impact of these factors on erosion or erosion control was minimized with the use of winter rye or straw as ground cover.


NOTES

Contribution no. 712.

Received for publication March 22, 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
Soil Science Society of America Journal Journal of Plant Registrations The Plant Genome
Copyright © 1991 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.