JEQ Journal of Natural Resources and Life Sciences Education
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Published in J Environ Qual 6:369-373 (1977)
© 1977 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Nutrient Losses in Surface Runoff from a Native Prairie1

D. R. Timmons and R. F. Holt2

ABSTRACT

Nutrient losses in surface runoff from a native prairie were determined for 5 years. The prairie, dominated by little bluestem (Andropogon scoparius Michx.), was on a Barnes loam soil in westcentral Minnesota. Snowmelt runoff accounted for 80% of the average annual runoff. After spring thaw, rainfall caused appreciable runoff (37% of annual) during 1 year only. Depending on chemical parameter, 63 to 88% of the average annual nutrient loads were transported by snowmelt runoff. Average annual total nitrogen (N) and total phosphorus (P) losses were 0.8 and 0.1 kg/ha, respectively, and organic N and organic (+ hydrolyzable) P comprised 68 and 82% of their respective annual losses. Average annual cation losses ranged from about 0.1 to 1.8 kg/ha and, except for 1 year, were in the order K > Ca> Mg > Na. Average weighted concentrations for all parameters were higher for rainfall runoff than for snowmelt runoff. Nutrient losses from native prairie represent natural levels for comparing the effects of different land uses on nutrient loads in surface runoff.

Key Words: nitrogen • phosphorus • potassium • sodium • calcium • magnesium • chemical oxygen demand • snowmelt


NOTES

1 Contribution from the North Central Soil Conservation Research Center, North Central Region, USDA-ARS, Morris, MN 56267, in cooperation with the Minnesota Agric. Exp. Stn. Sci. J. Series no. 9554.

2 Soil Scientists, USDA, Morris, Minn.

Received for publication July 26, 1976.


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Vadose Zone Journal
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Copyright © 1977 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.