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Published in Soil Sci Soc Am J 38:465-471 (1974)
© 1974 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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The Amount and Nitrogen-15 Content of Nitrate in Soil Profiles from two Central Illinois Fields in a Corn-Soybean Rotation1

Amos Feigin, Georgia Shearer, Daniel H. Kohl and Barry Commoner2

ABSTRACT

This paper reports the concentration and the {delta}15N (per mill 15N excess) of nitrate present in soil cores as a function of depth and time. The cores were taken at approximately monthly intervals from two central Illinois fields which were in a corn and soybean rotation.

During the period of October 1971 through April 1972, the mean {delta}15N value of nitrate present at all depths of both fields was + 1.2 ± 1.5. The most striking variation from this mean occurred after the application, on 4 May 1972, of anhydrous ammonia to the field being sown to corn, when a dramatic decrease was observed in the {delta}15N values of the nitrate in the 0–30 layer of that field. The difference in the {delta}15N values of the nitrate found in the two fields disappeared after about 2 months. The {delta}15N values of the ammonium ion found in the soil after application of fertilizer increased with time as the concentration of ammonium decreased and the concentration of nitrate increased. These observations indicate that the observed changes following fertilization in {delta}15N of nitrate were due primarily to isotopic discrimination associated with incomplete conversion of ammonium to nitrate. The {delta}15N values of the nitrate in both fertilzed and unfertilized fields were higher in late summer than in the period October to May.

The nitrate content of the 150-cm profile did not show significant variation with time in either field from October 1971 until 4 May 1972, when anhydrous ammonia was applied to the field being sown to corn. The nitrate concentration in the soil profiles of both fields decreased during the period of crop growth. Fertilizer application and crop uptake appeared to exert a larger influence on the total amount of nitrate in the soil profile than did movement of nitrate out of the 150-cm profile by leaching, since rainfall in amounts sufficient to redistribute the nitrate within the profile did not lower the total amount of nitrate in the profile.


NOTES

1 The work is supported by the National Science Foundation under the Project Number GI-29925 X1.

2 Research Associate, Center for the Biology of Natural Systems & Soil Scientist, Institute of Soils & Water, Agricultural Research Organization, Volcani Center, Bet-Dagan, Israel; Research Associate, Center for the Biology of Natural Systems; Associate Professor of Biology, Washington University and Senior Fellow, Center for the Biology of Natural Systems; Director, Center for the Biology of Natural Systems, Washington University, St. Louis, Missouri, respectively.

Received for publication August 3, 1973. Accepted for publication February 7, 1974.







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Copyright © 1974 by the Soil Science Society of America.