JEQ Journal of Natural Resources and Life Sciences Education
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Published in J Environ Qual 25:584-593 (1996)
© 1996 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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Movement of Nitrate Fertilizer to Glacial Till and Runoff from a Claypan Soil

D. W. Blevins*, D. H. Wilkison and B. P. Kelly

U.S. Geological Survey, 301 W. Lexington, Room 227, Federal Building, Independence, MO 64050;

S. R. Silva

U.S. Geological Survey, Western Region Branch of Regional Research, Groundwater1 Chemistry, 345 Middlefield Road, Mail Stop 434, Menlo Park, CA 94025.

* Corresponding author.

ABSTRACT

Although water from 20 to 25% of shallow farmstead wells in northern Missouri has concentrations of nitrate (NO3) exceeding 10 mg L–1 as nitrogen (N), many potential sources for this NO3 are usually present. A field experiment was designed to trace and isolate the amount of a single application of N fertilizer lost to a glacial-till aquifer and runoffrom a 400 m2 corn (Zea mays L.) plot with bromide (Br) and isotopically labeled (15N) fertilizer. Soil at the plot is a Albaquic Hapludalf of the Adco Series containing a 61 cm claypan beneath 41 to 43 cm of topsoil. Groundwater levels ranged from 0.38 to 2.40 m below the land surface. Transport of water and NO3 to the saturated zone was not substantially retarded by the claypan. Labeled-N fertilizer accounted for as much as 8.6 mg L–1 of the NO3 (as N) in groundwater, but only in the top 1 to 2 m of the saturated zone. After two growing seasons (16 mo), <2% of the labeled-N fertilizer was lost to runoff, about 30% was in the saturated zone, 27.3% was removed with the grain, and about 5% remained in the unsaturated zone. A large part of the remaining labeled N may have been lost in gaseous N forms. The presence of labeled NO3 only in the top 2 m of the aquifer, slow horizontal transport, and winter recharge indicate grass crops such as wheat (Triticum aestivum L.) or rye (Secale cereale L.) might be used to extract near-surface N during the winter recharge period. Also, fall fertilizations can be expected to readily leach. Because groundwater concentrations of labeled NO3 were still increasing after two growing seasons, rotation of crops requiring small N inputs could be expected to limit the cumulative effect of large annual fertilizer applications on groundwater.


NOTES

The U.S. Geological Survey spells ground water as two words.

Received for publication April 3, 1995.


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