SSSAJ Journal of Natural Resources and Life Sciences Education
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Published in Soil Sci Soc Am J 29:176-178 (1965)
© 1965 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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The Effect of Nitrite and Organic Matter on Aerobic Gaseous Losses of Nitrogen from a Calcareous Soil1

B. D. Meek and A. J. MacKenzie2

ABSTRACT

The loss of gaseous nitrogen compounds when nitrite accumulates in a calcareous silty clay loam during nitrification was investigated under aerobic conditions.

Soil to which either (NH4)2SO4, NaNO2, or (NH4)2SO4 + barley straw was added, was incubated at 28C and 31% moisture for 28 days. Samples were maintained under aerobic conditions in a N-free atmosphere of 21% oxygen and 79% helium. Gas samples were taken every 7 days from the incubation flasks and analyzed, using a gas chromatograph, for gaseous N products evolved. The accumulation of nitrite was measured on separate soil samples incubated in the same manner as the flasks used to secure gas samples.

The gaseous N forms produced were N2O and N2. It was found that losses were low even when large amounts (250 ppm) of nitrite-N accumulated. The gaseous N loss was 1.3% for (NH4)2SO4 and NaNO2 and 3.6% for the (NH4)2SO4 + barley straw treatment.


NOTES

1 Contribution from the Southwest Branch, Soil and Water Conservation Research Division, ARS, USDA.

2 Soil Scientists USDA, Southwestern Irrigation Field Station, Brawley, Calif.

Received for publication September 28, 1964. Accepted for publication November 23, 1964.







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Copyright © 1965 by the Soil Science Society of America.