JEQ Grow Your Career With ASA
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in J Environ Qual 11:482-486 (1982)
© 1982 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 HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Wall, G. J.
Right arrow Articles by van Vliet, L. J. P.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Wall, G. J.
Right arrow Articles by van Vliet, L. J. P.
Agricola
Right arrow Articles by Wall, G. J.
Right arrow Articles by van Vliet, L. J. P.

Agriculture and Water Quality in the Canadian Great Lakes Basin: II. Fluvial Sediments1

G. J. Wall, W. T. Dickinson and L. J. P. van Vliet2

ABSTRACT

Unit-area yields of suspended sediments discharged from 11 small (<6,000 ha) agricultural watersheds in southern Ontario ranged from <100 to 1,000 kg ha–1 year–1 in a 2-year study. Estimated bank erosion contributed between 0 and 30% of the suspended sediment, while estimated cropland sheet and rill erosion contributed 70–100%. Regression analyses relating 14 watershed characteristics to unit-area yields showed that percent clay of the surface soil and percent row crop were the most significant (R2 = 0.64) factors in estimating suspended sediment yields.

Detailed studies in the agricultural watersheds were used to generate and test three independent methods for the prediction of suspended sediment yields from cropland. The agricultural contribution to suspended sediment were predicted for the Grand and Saugeen river basins and for the over 300 subbasins of the Canadian Great Lakes Basin. It was estimated that agricultural land-use activities contribute over 650 x 103 t of suspended sediment to the Great Lakes annually.

Key Words: water pollution • sheet erosion • streambank erosion


NOTES

1 This paper reports in part studies conducted under the auspices of the Pollution from Land Use Activities Reference Group (PLUARG) of the International Joint Commission. The financial support of the Ontario Ministry of Agriculture and Food and Agriculture Canada is gratefully acknowledged.

2 Pedologist, Agriculture Canada, Ontario Inst. of Pedology, Univ. of Guelph, Guelph, Ontario; Professor, School of Engineering, Univ. of Guelph; and Pedologist, Agriculture Canada, 6660 N.W. Marine Dr., Vancouver, British Columbia, respectively. Land Resource Research Institute Contribution no. 82-32.

Received for publication December 4, 1980.


This article has been cited by other articles:


Home page
J. Environ. Qual.Home page
G. Matisoff, E. C. Bonniwell, and P. J. Whiting
Radionuclides as Indicators of Sediment Transport in Agricultural Watersheds that Drain to Lake Erie
J. Environ. Qual., January 1, 2002; 31(1): 62 - 72.
[Abstract] [Full Text] [PDF]


Home page
Progress in Physical GeographyHome page
P. Ashmore and P. Ashmore
Contemporary erosion of the Canadian landscape
Progress in Physical Geography, June 1, 1993; 17(2): 190 - 204.
[Abstract] [PDF]




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
Soil Science Society of America Journal
Copyright © 1982 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.