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ABSTRACT
Nitrate reduction in water-unsaturated Columbia silt loam columns was examined at 19.5C and 34.5C with three levels of oxygen (0.5, 5, and 20%) in an aerating gas passing through the soil. Following a continuous application of NH4+ solution, a pulse of a NO3- solution was leached through these columns. After the decay of the pulse, a continuous application of NO3- solution allowed mathematical analysis leading to ascertaining NO3- reduction rate coefficients. The temperature dependence of these constants as a function of oxygen composition was discussed and the need for microbial population and activity analysis is emphasized.
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 8, 1973. Accepted for publication December 10, 1973.
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