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ABSTRACT
Nitrogen transformations were examined by means of a miscible displacement technique that permitted passage of air with different levels of oxygen through the soil. With the use of steady state solutions of equations describing the convective transport of NH4+ and NO3- ions in Columbia silt loam, first-order reaction rate constants k1 and k2 were ascertained for NH4+-oxidation and NO3--reduction, respectively. Values of k1 were measured to be ten-fold greater than those of k2. At an oxygen level of 0.5% in the gaseous phase, nitrification was apparently inhibited.
1 Contribution from the Dep. of Water Science and Engineering, Univ. of California, Davis 95616.
2 Graduate Student and Professors of Water Science, respectively. The senior author is now Lecturer, Univ. of Agriculture and Technology, Orissa, India.
Received for publication August 6, 1973. Accepted for publication December 10, 1973.
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