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Published in J Environ Qual 5:93-96 (1976)
© 1976 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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Geologic Nitrogen in Pleistocene Loess of Nebraska1

J. S. Boyce, John Muir, A. P. Edwards, E. C. Seim and R. A. Olson2

ABSTRACT

Research into the relationship between fertilizer use and water quality in Nebraska has resulted in the discovery of large quantities of geologic nitrate within the deep loess mantle of southwestern and central Nebraska. The NO3 is first encountered at a depth of about 7 m and continues to an unknown depth in excess of 30 m. Nitrate-N values of 25 to 45 ppm characterize the N zone, but values to 87 ppm have been recorded. The NO3 exists only under the leveler uplands of the region; however, it is on this plain that rapid development of irrigation is taking place and it has been shown that the NO3 has been leached from beneath older irrigation sites on the plain.

Key Words: nitrate • water pollution • irrigation


NOTES

1 Published with the approval of the Director as Paper No. 4055 Journal Ser., Nebraska Agric. Exp. Sta., Lincoln, NE 68503. Work reported was supported in part by the Office of Water Resourc. Res., USDI, under P.L. 88-379.

2 Research Associate, Instructor, Visiting Associate Professor of Agronomy, Univ. of Nebraska, Lincoln; Senior Agronomist, Hunt-Wesson Foods; and Professor of Agronomy, Univ. of Nebraska, respectively.







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Vadose Zone Journal Journal of Plant Registrations
Journal of Natural Resources
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Copyright © 1976 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.